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20:30:00", "2023-06-27 15:12:00", "2023-06-27 15:29:00", "2023-06-27 17:00:00", "2023-06-30 15:45:00", "2023-06-30 16:39:00", "2023-07-02 18:28:00", "2023-07-02 19:01:00", "2023-07-03 18:40:00", "2023-07-04 00:33:00", "2023-07-06 13:10:00", "2023-07-07 12:03:00", "2023-07-07 15:04:00", "2023-07-09 14:17:00", "2023-07-21 03:29:00", "2023-07-21 03:56:00", "2023-07-25 13:14:00", "2023-07-25 11:30:00", "2023-07-25 13:15:00", "2023-07-25 13:14:00", "2023-07-28 19:24:00", "2023-07-28 20:35:00", "2023-07-28 20:43:00", "2023-07-29 16:00:00", "2023-07-29 17:00:00", "2023-07-29 16:30:00", "2023-08-07 17:17:00", "2023-08-07 18:05:00", "2023-08-14 17:35:00", "2023-08-15 14:55:00", "2023-09-08 03:23:00", "2023-09-08 19:09:00", "2023-09-08 23:04:00", "2023-09-09 16:49:00", "2023-09-13 00:35:00", "2023-09-12 23:40:00", "2023-09-12 23:08:00", "2023-12-18 10:15:00", "2023-12-28 04:15:00" ], "NEWS": [ "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 33.1115 km away, between 2003-05-31 15:40:00 and 2003-05-31 18:51:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 6000.0 and crop damage of 0.0. \n\nEpisode Narrative: Thunderstorms with high winds, heavy rainfall, and frequent lightning moved through Central and Western Maryland during the afternoon and evening of the 31st. In Washington County, several trees were downed across the county. Several roads were also flooded, including Ed Sears Road. In Frederick County, heavy downpours caused a pond to overflow in Knoxville. A new home near the pond was damaged by the high water. Street flooding was also reported in town. Flooding was also reported on Interstate 270 near the Montgomery County border. Pea to marble sized hail fell in Frederick. Also in Frederick, a wind gust of 53 MPH was recorded and a tree was downed onto a car on West College Parkway. In Carroll County, small streams overflowed their banks. Flooding was reported on Twin Arch Road in Mt. Airy. Trees were downed in Winfield on Dennings, Buckhorn, and John Pickett roads. A home in Marriottsville burned to the ground after being struck by lightning. In Montgomery County, wires were downed onto Route 108 near New Hampshire Avenue in Olney. Large tree branches were downed onto cars in Gaithersburg. Minor flooding was reported in a parking lot and a field in Germantown. Minor flooding was also reported on Route 355 near Route 118. In Anne Arundel County, tree limbs were downed onto electrical wires in Arnold. In Prince George's County, a wind gust of 61 MPH was recorded at Andrews Air Force Base. Power outages were reported along Walker Mill Road and Marlboro Pike. A portion of Route 50 between routes 197 and 301 in Bowie was closed for 30 minutes after a backed up storm drain caused flooding. Thunderstorms with high winds, heavy rainfall, and frequent lightning moved through Central and Western Maryland during the afternoon and evening of the 31st. In Washington County, several trees were downed across the county. Several roads were also flooded, including Ed Sears Road. In Frederick County, heavy downpours caused a pond to overflow in Knoxville. A new home near the pond was damaged by the high water. Street flooding was also reported in town. Flooding was also reported on Interstate 270 near the Montgomery County border. Pea to marble sized hail fell in Frederick. Also in Frederick, a wind gust of 53 MPH was recorded and a tree was downed onto a car on West College Parkway. In Carroll County, small streams overflowed their banks. Flooding was reported on Twin Arch Road in Mt. Airy. Trees were downed in Winfield on Dennings, Buckhorn, and John Pickett roads. A home in Marriottsville burned to the ground after being struck by lightning. In Montgomery County, wires were downed onto Route 108 near New Hampshire Avenue in Olney. Large tree branches were downed onto cars in Gaithersburg. Minor flooding was reported in a parking lot and a field in Germantown. Minor flooding was also reported on Route 355 near Route 118. In Anne Arundel County, tree limbs were downed onto electrical wires in Arnold. In Prince George's County, a wind gust of 61 MPH was recorded at Andrews Air Force Base. Power outages were reported along Walker Mill Road and Marlboro Pike. A portion of Route 50 between routes 197 and 301 in Bowie was closed for 30 minutes after a backed up storm drain caused flooding. Thunderstorms with high winds, heavy rainfall, and frequent lightning moved through Central and Western Maryland during the afternoon and evening of the 31st. In Washington County, several trees were downed across the county. Several roads were also flooded, including Ed Sears Road. In Frederick County, heavy downpours caused a pond to overflow in Knoxville. A new home near the pond was damaged by the high water. Street flooding was also reported in town. Flooding was also reported on Interstate 270 near the Montgomery County border. Pea to marble sized hail fell in Frederick. Also in Frederick, a wind gust of 53 MPH was recorded and a tree was downed onto a car on West College Parkway. In Carroll County, small streams overflowed their banks. Flooding was reported on Twin Arch Road in Mt. Airy. Trees were downed in Winfield on Dennings, Buckhorn, and John Pickett roads. A home in Marriottsville burned to the ground after being struck by lightning. In Montgomery County, wires were downed onto Route 108 near New Hampshire Avenue in Olney. Large tree branches were downed onto cars in Gaithersburg. Minor flooding was reported in a parking lot and a field in Germantown. Minor flooding was also reported on Route 355 near Route 118. In Anne Arundel County, tree limbs were downed onto electrical wires in Arnold. In Prince George's County, a wind gust of 61 MPH was recorded at Andrews Air Force Base. Power outages were reported along Walker Mill Road and Marlboro Pike. A portion of Route 50 between routes 197 and 301 in Bowie was closed for 30 minutes after a backed up storm drain caused flooding.\nEvent Narrative: Trees were downed onto three roads. The time was estimated. Wires were downed onto Route 108. Tree limbs were felled onto power lines.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 22.5575 km away, between 2003-06-11 19:45:00 and 2003-06-11 20:15:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 2000.0 and crop damage of 0.0. \n\nEpisode Narrative: Thunderstorms with high winds and frequent lighting moved through Central and Southern Maryland during the evening of the 11th. In Montgomery County, trees and wires were downed in several locations. In addition, a handful of homes caught fire after being hit by lightning in Rockville, Germantown, and Takoma Park. In Howard County, trees were downed in Columbia and Ellicott City. In Prince George's County, trees and wires were downed in Hyattsville. In Calvert County, a few trees were downed in Huntingtown. A house on Coring Drive in Huntingtown was struck by lightning. In Charles County, trees were downed south of La Plata. In St. Mary's County, trees were downed onto Route 236 three miles west of Mechanicsville.\nEvent Narrative: Many trees and wires were downed.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 6.2445 km away, between 2003-06-12 17:15:00 and 2003-06-12 17:30:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 2000.0 and crop damage of 0.0. \n\nEpisode Narrative: Thunderstorms with very heavy rainfall, frequent lightning, and damaging winds moved through central Maryland during the afternoon and evening of the 12th. Several locations reported downed trees and power lines in addition to flooding. In Frederick County, trees and wires were downed in Urbana and Green Valley. Up to 40 trees were downed in New Market, including some which had to be cleared from roads. A tree fell onto a house on Lewisdale Road in Hyattstown. A home in New Midway and in New Market were struck by lightning. In Carroll County, a county road was inundated with water. A stream that runs through Wakefield Valley Golf Course in Westminster overflowed onto low lying areas. In Baltimore County, a stream overflowed its banks and a road and several basements were flooded in Towson. An observer in Towson recorded 2.52 inches of rain and two inches of this total fell in 45 minutes. Five roads were flooded in Parkville. In Baltimore, six roads were flooded. In addition, pea sized hail fell in Towson and Baltimore. An observer in Kingsville recorded 1.8 inches of rain in 2 hours. In Harford County, 2.06 inches of rain was recorded in Fallston. A handful of basements were flooded. Hail of unknown size also fell. In Montgomery County, trees were downed onto Sleepy Hollow Lane in Rockville. Trees were also downed onto Shannondale Drive and Pretoria Drive in Silver Spring and in the communities of Brookeville and Laytonsville. A wind gust of 60 MPH was reported in Germantown. Route 355 in Gaithersburg was closed by high water. A low water bridge on Hyattstown Road near Prescott Road was underwater. Little Seneca Creek overflowed its banks, reaching a stage of 8.1 feet at Dawsonville around 9 PM. Flood stage at this location is 8 feet. Goshen Branch near Damascus also flooded. A handful of motorists were caught in rising water and had to be rescued by emergency personnel. Rescuers also rescued a dog that was caught on a rock in the raging Potomac River near Old Angler's Inn. In addition, a few homes were struck by lightning. A 30 vehicle pileup on Interstate 270 near Montrose Road was also blamed on the storm. In Anne Arundel County, trees and power lines were downed in Riviera Beach, Annapolis, Arnold and Cape St. Claire. Some roads were blocked and four homes were slightly damaged by the fallen trees. Large trees and power lines were also downed along College Parkway and Alemeda Parkway. A wind gust of 43 MPH was recorded in Shadyside and a gust of 41 MPH was recorded in Annapolis. Lightning struck five houses an a few trees across the county. In Prince George's County, a wind gust of 83 MPH was recorded at Andrews Air Force Base. A gust of 49 MPH was recorded in Bladensburg and a gust of 42 MPH was recorded in Landover. Trees were downed onto the Baltimore-Washington Parkway near the intersection of Route 410 in Greenbelt. The intersection of Route 450 and Greenvale Parkway was flooded in Landover Hills. In Mt. Rainer, Queens Chapel Road and other low lying areas were flooded. Fire fighters had to rescue several drivers from their cars countywide. Countywide, several homes and a commercial structure were struck by lightning and two serious fires were reported. In Charles County, many trees were downed south of La Plata. A wind gust of 41 MPH was recorded in Waldorf. In St. Mary's County, trees were downed in Thompson's Corner, Compton, Chaptico, Country Lakes, and Mechanicsville. A home in Compton was damaged by a felled tree.\nEvent Narrative: Trees and power lines were downed.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 38.1139 km away, between 2003-06-12 17:15:00 and 2003-06-12 17:15:00. The events included records with estimated wind gusts of 52.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A severe thunderstorm knocked down trees and wires in Stevensville.\nEvent Narrative:", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 40.8073 km away, between 2003-06-12 17:48:00 and 2003-06-12 17:48:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A severe thunderstorm knocked down several trees and numerous power lines in and around Skinners Neck.\nEvent Narrative:", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 27.9428 km away, between 2003-06-13 17:50:00 and 2003-06-13 19:05:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 5000.0 and crop damage of 0.0. \n\nEpisode Narrative: Thunderstorms with very heavy downpours and gusty winds moved through North Central Maryland for the third straight day on the 13th. In Washington County, an underpass was flooded in Hagerstown. Roads were also flooded in Williamsport. In Montgomery County, a 60 MPH gust was reported in Germantown. Trees were downed in Brookeville and Laytonsville. Route 108 and Woodfield Road in Damascus were flooded after 3 inches of rain fell. In Howard County, trees were downed in Glenwood. Several roads were closed by flooding or mudslides in the Lisbon area. In Anne Arundel County, a home on Polling House Road in Harwood was struck by lightning three times. The attic of the home was largely destroyed by the resulting fire. In Baltimore County, several trees were downed in Baltimore, Towson, and Parkville. Severe flash flooding was reported in the northeast part of Baltimore. Two streets became rushing rapids, washing several cars hundreds of yards away. Several motorists had to be rescued from their cars or had to swim to safety. The hardest hit areas included Hillen Road, 35th Street, and Aisquith Street near 25th Street. The wall of water reached a height of 10 feet near the intersection of Hillen Road and 35th Street. A pile of vehicles found in this location after the water receded testified to the power of the flood. One woman was injured at this same intersection after flooding weakened the floor in the first level of her home and she fell through when it collapsed. Numerous other homes were damaged by flood waters in this part of town as well. At the intersection of Aisquith Street and 25th Street, the wall of water reached 6 feet in height. Six cars were stuck in water beneath a railroad overpass. Minor street flooding was reported at the intersection of Northern Parkway and Walther Boulevard. Street flooding was also reported in Parkville and Towson. In Carroll County, flood waters covered a bridge along Route 97 in Mayberry. In Harford County, flooding was reported in Whiteford, Norrisville, and other low lying areas along the Pennsylvania border. Flash flooding was also reported in Fallston where several feet of water was seen rushing down roads and basements were flooded. Thunderstorms with very heavy downpours and gusty winds moved through North Central Maryland for the third straight day on the 13th. In Washington County, an underpass was flooded in Hagerstown. Roads were also flooded in Williamsport. In Montgomery County, a 60 MPH gust was reported in Germantown. Trees were downed in Brookeville and Laytonsville. Route 108 and Woodfield Road in Damascus were flooded after 3 inches of rain fell. In Howard County, trees were downed in Glenwood. Several roads were closed by flooding or mudslides in the Lisbon area. In Anne Arundel County, a home on Polling House Road in Harwood was struck by lightning three times. The attic of the home was largely destroyed by the resulting fire. In Baltimore County, several trees were downed in Baltimore, Towson, and Parkville. Severe flash flooding was reported in the northeast part of Baltimore. Two streets became rushing rapids, washing several cars hundreds of yards away. Several motorists had to be rescued from their cars or had to swim to safety. The hardest hit areas included Hillen Road, 35th Street, and Aisquith Street near 25th Street. The wall of water reached a height of 10 feet near the intersection of Hillen Road and 35th Street. A pile of vehicles found in this location after the water receded testified to the power of the flood. One woman was injured at this same intersection after flooding weakened the floor in the first level of her home and she fell through when it collapsed. Numerous other homes were damaged by flood waters in this part of town as well. At the intersection of Aisquith Street and 25th Street, the wall of water reached 6 feet in height. Six cars were stuck in water beneath a railroad overpass. Minor street flooding was reported at the intersection of Northern Parkway and Walther Boulevard. Street flooding was also reported in Parkville and Towson. In Carroll County, flood waters covered a bridge along Route 97 in Mayberry. In Harford County, flooding was reported in Whiteford, Norrisville, and other low lying areas along the Pennsylvania border. Flash flooding was also reported in Fallston where several feet of water was seen rushing down roads and basements were flooded. Thunderstorms with very heavy downpours and gusty winds moved through North Central Maryland for the third straight day on the 13th. In Washington County, an underpass was flooded in Hagerstown. Roads were also flooded in Williamsport. In Montgomery County, a 60 MPH gust was reported in Germantown. Trees were downed in Brookeville and Laytonsville. Route 108 and Woodfield Road in Damascus were flooded after 3 inches of rain fell. In Howard County, trees were downed in Glenwood. Several roads were closed by flooding or mudslides in the Lisbon area. In Anne Arundel County, a home on Polling House Road in Harwood was struck by lightning three times. The attic of the home was largely destroyed by the resulting fire. In Baltimore County, several trees were downed in Baltimore, Towson, and Parkville. Severe flash flooding was reported in the northeast part of Baltimore. Two streets became rushing rapids, washing several cars hundreds of yards away. Several motorists had to be rescued from their cars or had to swim to safety. The hardest hit areas included Hillen Road, 35th Street, and Aisquith Street near 25th Street. The wall of water reached a height of 10 feet near the intersection of Hillen Road and 35th Street. A pile of vehicles found in this location after the water receded testified to the power of the flood. One woman was injured at this same intersection after flooding weakened the floor in the first level of her home and she fell through when it collapsed. Numerous other homes were damaged by flood waters in this part of town as well. At the intersection of Aisquith Street and 25th Street, the wall of water reached 6 feet in height. Six cars were stuck in water beneath a railroad overpass. Minor street flooding was reported at the intersection of Northern Parkway and Walther Boulevard. Street flooding was also reported in Parkville and Towson. In Carroll County, flood waters covered a bridge along Route 97 in Mayberry. In Harford County, flooding was reported in Whiteford, Norrisville, and other low lying areas along the Pennsylvania border. Flash flooding was also reported in Fallston where several feet of water was seen rushing down roads and basements were flooded. Thunderstorms with very heavy downpours and gusty winds moved through North Central Maryland for the third straight day on the 13th. In Washington County, an underpass was flooded in Hagerstown. Roads were also flooded in Williamsport. In Montgomery County, a 60 MPH gust was reported in Germantown. Trees were downed in Brookeville and Laytonsville. Route 108 and Woodfield Road in Damascus were flooded after 3 inches of rain fell. In Howard County, trees were downed in Glenwood. Several roads were closed by flooding or mudslides in the Lisbon area. In Anne Arundel County, a home on Polling House Road in Harwood was struck by lightning three times. The attic of the home was largely destroyed by the resulting fire. In Baltimore County, several trees were downed in Baltimore, Towson, and Parkville. Severe flash flooding was reported in the northeast part of Baltimore. Two streets became rushing rapids, washing several cars hundreds of yards away. Several motorists had to be rescued from their cars or had to swim to safety. The hardest hit areas included Hillen Road, 35th Street, and Aisquith Street near 25th Street. The wall of water reached a height of 10 feet near the intersection of Hillen Road and 35th Street. A pile of vehicles found in this location after the water receded testified to the power of the flood. One woman was injured at this same intersection after flooding weakened the floor in the first level of her home and she fell through when it collapsed. Numerous other homes were damaged by flood waters in this part of town as well. At the intersection of Aisquith Street and 25th Street, the wall of water reached 6 feet in height. Six cars were stuck in water beneath a railroad overpass. Minor street flooding was reported at the intersection of Northern Parkway and Walther Boulevard. Street flooding was also reported in Parkville and Towson. In Carroll County, flood waters covered a bridge along Route 97 in Mayberry. In Harford County, flooding was reported in Whiteford, Norrisville, and other low lying areas along the Pennsylvania border. Flash flooding was also reported in Fallston where several feet of water was seen rushing down roads and basements were flooded.\nEvent Narrative: Several trees were downed. Trees were downed in Parkville and Towson. Trees were downed. Trees were downed.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 16.4596 km away, between 2003-06-14 15:15:00 and 2003-06-14 15:15:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 500.0 and crop damage of 0.0. \n\nEpisode Narrative: Scattered thunderstorms with high winds and heavy rainfall moved through the suburbs of Washington D.C. during the afternoon of the 14th. In Prince George's County, large trees were downed at the intersection of Brooklyn Bridge Road and Supplee Lane in Laurel. Large tree branches were downed in Accokeek. In Montgomery County, heavy downpours caused water to collect on Beach Drive. In Charles County, trees were downed in Waldorf and Cobb Island.\nEvent Narrative: A few trees were downed.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 21.0841 km away, between 2003-06-27 14:35:00 and 2003-06-27 14:35:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 500.0 and crop damage of 0.0. \n\nEpisode Narrative: A thunderstorm with high winds moved through South Central Maryland during the afternoon of the 27th. In Prince George's County, a tree and wires were downed in Oxon Hill. A tree was blown across a telephone cable in Bowie. In Charles County, trees and power lines were downed between White Plains and Waldorf. In Calvert County, trees were downed in Owings. Pea sized hail was reported in Owings and Dunkirk.\nEvent Narrative: A tree was downed onto a telephone cable. The time was estimated.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 29.1185 km away, between 2003-07-04 18:37:00 and 2003-07-04 18:37:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 10000.0 and crop damage of 0.0. \n\nEpisode Narrative: Thunderstorms with high wind moved through Central Maryland during the afternoon and early evening of the 4th. In Frederick County, a few trees were downed in Middletown and Myersville. A wind gust of 43 MPH was recorded in Frederick. In Carroll County, a 44 MPH wind gust was recorded in Westminster. In Howard County, a large barn used by community organizations was destroyed by a downburst of winds estimated at 80 MPH on Sharp Road in Glenelg. Trees were also downed in Glenelg at the intersection of Route 32 and Triadelphia.\nEvent Narrative: Trees were downed at the intersection of Route 32 and Triadelphia Road. A large barn on Sharp Road was destroyed.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 24.8039 km away, between 2003-07-06 20:10:00 and 2003-07-06 21:20:00. The events included records with estimated wind gusts of 52.2 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 22000.0 and crop damage of 0.0. \n\nEpisode Narrative: Thunderstorms with heavy downpours and wind gusts over 60 MPH moved through Central Maryland during the evening of the 6th. In Frederick County, trees were downed in Brunswick and Frederick. In Montgomery County, trees were downed on Wisconsin Avenue and the Beltway in Bethesda. Several trees were also downed in Woodsboro, Wheaton, Kensington, Forest Glen, and Silver Spring, some onto cars and buildings. Pea sized hail was also reported in Silver Spring and Forest Glen. Quarter size hail fell in Bethesda. A wind gust of 44 MPH was recorded in Clarksburg. A total of 2 inches of rainfall in Damascus caused small stream flooding. In Howard County, many trees were downed in West Friendship. A wind gust of 44 MPH was recorded in Laurel. In Anne Arundel County, several trees were downed north of Annapolis, including in the community of Brooklyn Park. In Carroll County, several trees were downed in Union Mills. In Baltimore County, widespread trees and power lines were downed in Baltimore. The hardest hit area was in the north side of town. Trees were also downed in Cockeysville and Hunt Valley. A wind gust of 43 MPH was recorded in Parkton. In Harford County, a downburst of winds estimated around 70 MPH downed numerous trees near Fallston in the community of Glen Elyn. The downburst struck Gunpowder Falls State Park west of Moores Road first, downing 30 to 40 trees up to 3 feet in diameter. Then the winds fanned out across a residential area and downed a few additional trees. Thunderstorms with heavy downpours and wind gusts over 60 MPH moved through Central Maryland during the evening of the 6th. In Frederick County, trees were downed in Brunswick and Frederick. In Montgomery County, trees were downed on Wisconsin Avenue and the Beltway in Bethesda. Several trees were also downed in Woodsboro, Wheaton, Kensington, Forest Glen, and Silver Spring, some onto cars and buildings. Pea sized hail was also reported in Silver Spring and Forest Glen. Quarter size hail fell in Bethesda. A wind gust of 44 MPH was recorded in Clarksburg. A total of 2 inches of rainfall in Damascus caused small stream flooding. In Howard County, many trees were downed in West Friendship. A wind gust of 44 MPH was recorded in Laurel. In Anne Arundel County, several trees were downed north of Annapolis, including in the community of Brooklyn Park. In Carroll County, several trees were downed in Union Mills. In Baltimore County, widespread trees and power lines were downed in Baltimore. The hardest hit area was in the north side of town. Trees were also downed in Cockeysville and Hunt Valley. A wind gust of 43 MPH was recorded in Parkton. In Harford County, a downburst of winds estimated around 70 MPH downed numerous trees near Fallston in the community of Glen Elyn. The downburst struck Gunpowder Falls State Park west of Moores Road first, downing 30 to 40 trees up to 3 feet in diameter. Then the winds fanned out across a residential area and downed a few additional trees. Thunderstorms with heavy downpours and wind gusts over 60 MPH moved through Central Maryland during the evening of the 6th. In Frederick County, trees were downed in Brunswick and Frederick. In Montgomery County, trees were downed on Wisconsin Avenue and the Beltway in Bethesda. Several trees were also downed in Woodsboro, Wheaton, Kensington, Forest Glen, and Silver Spring, some onto cars and buildings. Pea sized hail was also reported in Silver Spring and Forest Glen. Quarter size hail fell in Bethesda. A wind gust of 44 MPH was recorded in Clarksburg. A total of 2 inches of rainfall in Damascus caused small stream flooding. In Howard County, many trees were downed in West Friendship. A wind gust of 44 MPH was recorded in Laurel. In Anne Arundel County, several trees were downed north of Annapolis, including in the community of Brooklyn Park. In Carroll County, several trees were downed in Union Mills. In Baltimore County, widespread trees and power lines were downed in Baltimore. The hardest hit area was in the north side of town. Trees were also downed in Cockeysville and Hunt Valley. A wind gust of 43 MPH was recorded in Parkton. In Harford County, a downburst of winds estimated around 70 MPH downed numerous trees near Fallston in the community of Glen Elyn. The downburst struck Gunpowder Falls State Park west of Moores Road first, downing 30 to 40 trees up to 3 feet in diameter. Then the winds fanned out across a residential area and downed a few additional trees. Thunderstorms with heavy downpours and wind gusts over 60 MPH moved through Central Maryland during the evening of the 6th. In Frederick County, trees were downed in Brunswick and Frederick. In Montgomery County, trees were downed on Wisconsin Avenue and the Beltway in Bethesda. Several trees were also downed in Woodsboro, Wheaton, Kensington, Forest Glen, and Silver Spring, some onto cars and buildings. Pea sized hail was also reported in Silver Spring and Forest Glen. Quarter size hail fell in Bethesda. A wind gust of 44 MPH was recorded in Clarksburg. A total of 2 inches of rainfall in Damascus caused small stream flooding. In Howard County, many trees were downed in West Friendship. A wind gust of 44 MPH was recorded in Laurel. In Anne Arundel County, several trees were downed north of Annapolis, including in the community of Brooklyn Park. In Carroll County, several trees were downed in Union Mills. In Baltimore County, widespread trees and power lines were downed in Baltimore. The hardest hit area was in the north side of town. Trees were also downed in Cockeysville and Hunt Valley. A wind gust of 43 MPH was recorded in Parkton. In Harford County, a downburst of winds estimated around 70 MPH downed numerous trees near Fallston in the community of Glen Elyn. The downburst struck Gunpowder Falls State Park west of Moores Road first, downing 30 to 40 trees up to 3 feet in diameter. Then the winds fanned out across a residential area and downed a few additional trees. Thunderstorms with heavy downpours and wind gusts over 60 MPH moved through Central Maryland during the evening of the 6th. In Frederick County, trees were downed in Brunswick and Frederick. In Montgomery County, trees were downed on Wisconsin Avenue and the Beltway in Bethesda. Several trees were also downed in Woodsboro, Wheaton, Kensington, Forest Glen, and Silver Spring, some onto cars and buildings. Pea sized hail was also reported in Silver Spring and Forest Glen. Quarter size hail fell in Bethesda. A wind gust of 44 MPH was recorded in Clarksburg. A total of 2 inches of rainfall in Damascus caused small stream flooding. In Howard County, many trees were downed in West Friendship. A wind gust of 44 MPH was recorded in Laurel. In Anne Arundel County, several trees were downed north of Annapolis, including in the community of Brooklyn Park. In Carroll County, several trees were downed in Union Mills. In Baltimore County, widespread trees and power lines were downed in Baltimore. The hardest hit area was in the north side of town. Trees were also downed in Cockeysville and Hunt Valley. A wind gust of 43 MPH was recorded in Parkton. In Harford County, a downburst of winds estimated around 70 MPH downed numerous trees near Fallston in the community of Glen Elyn. The downburst struck Gunpowder Falls State Park west of Moores Road first, downing 30 to 40 trees up to 3 feet in diameter. Then the winds fanned out across a residential area and downed a few additional trees.\nEvent Narrative: Numerous trees and power lines were downed. A wind gust estimated at 70 MPH downed numerous trees in Glen Elyn. Numerous trees were downed. Many trees were downed. Many trees were downed north of Annapolis.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 14.461 km away, between 2003-07-09 16:45:00 and 2003-07-09 16:45:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 2000.0 and crop damage of 0.0. \n\nEpisode Narrative: A cluster of thunderstorms with high winds and heavy downpours moved through Central Maryland during the early evening of the 9th. In Montgomery County, trees were downed in Bethesda and Wheaton. In Prince George's County, trees and wires were downed near Lanham Hills. In Anne Arundel County, 3.09 inches of rain was recorded in Rivera Beach. Trees and power lines were downed nearby.\nEvent Narrative: Trees and power lines were downed. The time was estimated.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 22.2456 km away, between 2003-07-11 00:30:00 and 2003-07-11 00:30:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 5000.0 and crop damage of 0.0. \n\nEpisode Narrative: Thunderstorms with high winds and frequent lightning moved through Central Maryland between 8 PM on the 10th and 2 AM on the 11th. In Charles County, trees were downed near Nanjemoy. In St. Mary's County, a tree was downed onto a house in Mechanicsville. In Anne Arundel County, six trees were downed at a residence on Windsong Drive in Arnold. One tree landed on a carport, and another fell onto the roof of a patio. In Montgomery County, a home was damaged by a lightning-related fire.\nEvent Narrative: Six trees were downed. A carport and a patio were damaged.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 40.7936 km away, between 2003-07-12 16:40:00 and 2003-07-12 17:10:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 5000.0 and crop damage of 0.0. \n\nEpisode Narrative: Thunderstorms with frequent lightning and high winds moved through North Central Maryland during the evening of the 12th. In Frederick County, lightning struck a barn near Walkersville. A mother in her 30s and her daughter, age 11, inside the barn were knocked down by the bolt which apparently traveled inside the building along metal structure supports. They were taken to a local hospital for observation and were released a short time later. In addition, high winds downed trees in Libertytown, Wolfsville, and Meyersville. Marble sized hail was reported in Mt. Airy. In Carroll County, trees and power lines were downed in Finksburg. In Baltimore County, several trees and power lines were downed across the central and northern portion of the county. In Harford County, widespread tree and power line damage was reported across the eastern portion of the county. The hardest hit areas included Churchville and near the Conowingo Dam.\nEvent Narrative: Trees were downed in Libertytown, Wolfsville, and Myersville.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 21.0841 km away, between 2003-07-18 14:40:00 and 2003-07-18 14:40:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 2000.0 and crop damage of 0.0. \n\nEpisode Narrative: Isolated thunderstorms with high wind and hail moved through South Central Maryland during the afternoon of the 18th. In Calvert County, trees and wires were downed in Huntingtown. Pea sized hail was also reported. In Prince George's County, several trees were downed in the Tall Oaks and Pointer Ridge communities of southern Bowie. Pea to marble sized hail also fell in Bowie.\nEvent Narrative: Several trees were downed in the south part of town.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 38.1139 km away, between 2003-08-05 21:19:00 and 2003-08-05 21:19:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A severe thunderstorm tore down several power lines on Kent Island.\nEvent Narrative:", "The following events were reported: Heavy Rain, Lightning. These occurred near station USW00093721, approximately 34.7001 km away, between 2003-08-16 13:30:00 and 2003-08-16 17:00:00.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 80000.0 and crop damage of 0.0. \n\nEpisode Narrative: Thunderstorms with heavy rainfall, frequent lightning, large hail, and damaging winds moved through Maryland between midday and late evening on the 16th. In Washington County, trees were downed and penny sized hail fell in Clear Spring. Rainfall totals included 2.37 inches in Smithsburg and 2.0 inches in Willamsport. Lightning struck a home on Woodstock Lane in Boonsboro. The resulting fire caused $70,000 damage to the structure. In Frederick County, a total of 2.2 inches of rain was recorded in Thurmont. In Carroll County, trees were downed in Pleasant Valley. In Baltimore County, trees were downed in Kingsville. Wires were downed in Cockeysville. In Harford County, several trees were downed, especially in the Bel Air, Fallston, and Darlington areas. Quarter sized hail was also reported in Darlington. In Bel Air, a tree was downed onto a home on Young Avenue. Across the county 7 roads were blocked by fallen trees. In Fallston, a home on Ryan Road was damaged by a fallen tree and Tollgate Road was closed after a tree downed a utility pole. Heavy downpours caused water to flood the following roads in the Fallston area: Harford Road, Route 152, Carrs Mill Road, Ryan Road, Tollgate Road, Route 1, Pleasantville Road, and Fork Road. A total of 2.24 inches of rain was recorded in Fallston. County officials said that over 85% of the gravel roads in the county would need reconditioning after rushing water caused ruts to form on the roads. In Montgomery County, trees were downed in Poolesville on Mt. Nebo Road. In Prince George's County, wires were downed near Brandywine. In Calvert County, trees were downed in Sunderland. In Charles County, trees were downed in Wicomico and La Plata. Wires were downed in Waldorf. In St. Mary's County, lightning struck a chimney at a boiler plant at Patuxent River Naval Air Station. The chimney fell onto parked cars and caused $10,000 damage. Thunderstorms with heavy rainfall, frequent lightning, large hail, and damaging winds moved through Maryland between midday and late evening on the 16th. In Washington County, trees were downed and penny sized hail fell in Clear Spring. Rainfall totals included 2.37 inches in Smithsburg and 2.0 inches in Willamsport. Lightning struck a home on Woodstock Lane in Boonsboro. The resulting fire caused $70,000 damage to the structure. In Frederick County, a total of 2.2 inches of rain was recorded in Thurmont. In Carroll County, trees were downed in Pleasant Valley. In Baltimore County, trees were downed in Kingsville. Wires were downed in Cockeysville. In Harford County, several trees were downed, especially in the Bel Air, Fallston, and Darlington areas. Quarter sized hail was also reported in Darlington. In Bel Air, a tree was downed onto a home on Young Avenue. Across the county 7 roads were blocked by fallen trees. In Fallston, a home on Ryan Road was damaged by a fallen tree and Tollgate Road was closed after a tree downed a utility pole. Heavy downpours caused water to flood the following roads in the Fallston area: Harford Road, Route 152, Carrs Mill Road, Ryan Road, Tollgate Road, Route 1, Pleasantville Road, and Fork Road. A total of 2.24 inches of rain was recorded in Fallston. County officials said that over 85% of the gravel roads in the county would need reconditioning after rushing water caused ruts to form on the roads. In Montgomery County, trees were downed in Poolesville on Mt. Nebo Road. In Prince George's County, wires were downed near Brandywine. In Calvert County, trees were downed in Sunderland. In Charles County, trees were downed in Wicomico and La Plata. Wires were downed in Waldorf. In St. Mary's County, lightning struck a chimney at a boiler plant at Patuxent River Naval Air Station. The chimney fell onto parked cars and caused $10,000 damage. Thunderstorms with heavy rainfall, frequent lightning, large hail, and damaging winds moved through Maryland between midday and late evening on the 16th. In Washington County, trees were downed and penny sized hail fell in Clear Spring. Rainfall totals included 2.37 inches in Smithsburg and 2.0 inches in Willamsport. Lightning struck a home on Woodstock Lane in Boonsboro. The resulting fire caused $70,000 damage to the structure. In Frederick County, a total of 2.2 inches of rain was recorded in Thurmont. In Carroll County, trees were downed in Pleasant Valley. In Baltimore County, trees were downed in Kingsville. Wires were downed in Cockeysville. In Harford County, several trees were downed, especially in the Bel Air, Fallston, and Darlington areas. Quarter sized hail was also reported in Darlington. In Bel Air, a tree was downed onto a home on Young Avenue. Across the county 7 roads were blocked by fallen trees. In Fallston, a home on Ryan Road was damaged by a fallen tree and Tollgate Road was closed after a tree downed a utility pole. Heavy downpours caused water to flood the following roads in the Fallston area: Harford Road, Route 152, Carrs Mill Road, Ryan Road, Tollgate Road, Route 1, Pleasantville Road, and Fork Road. A total of 2.24 inches of rain was recorded in Fallston. County officials said that over 85% of the gravel roads in the county would need reconditioning after rushing water caused ruts to form on the roads. In Montgomery County, trees were downed in Poolesville on Mt. Nebo Road. In Prince George's County, wires were downed near Brandywine. In Calvert County, trees were downed in Sunderland. In Charles County, trees were downed in Wicomico and La Plata. Wires were downed in Waldorf. In St. Mary's County, lightning struck a chimney at a boiler plant at Patuxent River Naval Air Station. The chimney fell onto parked cars and caused $10,000 damage.\nEvent Narrative: Lightning started a fire at a home. Lightning knocked a chimney off a building.", "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00093721, approximately 22.2516 km away, between 2003-08-22 18:15:00 and 2003-08-22 19:00:00. The events included records with hailstones measuring 40.35 inches.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 17000.0 and crop damage of 0.0. \n\nEpisode Narrative: Thunderstorms with high winds, frequent lightning, and large hail moved through Central Maryland during the evening of the 22nd. In Frederick County, trees were downed in several locations near Urbana. In Howard County, trees and power lines were downed in the western portion of the county. In Anne Arundel County, a power line was downed onto a car, a trailer, and a house in Pasadena. The truck and trailer were destroyed by the resulting fire and the house sustained minor damage. A dozen other power lines were downed across the northern portion of the county. In Baltimore County, golfball sized hail was reported in Towson. Trees were downed in Cockeysville, Dundalk, Hunt Valley, and Baltimore. In Harford County, 8 trees were downed onto roads across the county. The hardest hit areas included Bel Air and Fallston. Thunderstorms with high winds, frequent lightning, and large hail moved through Central Maryland during the evening of the 22nd. In Frederick County, trees were downed in several locations near Urbana. In Howard County, trees and power lines were downed in the western portion of the county. In Anne Arundel County, a power line was downed onto a car, a trailer, and a house in Pasadena. The truck and trailer were destroyed by the resulting fire and the house sustained minor damage. A dozen other power lines were downed across the northern portion of the county. In Baltimore County, golfball sized hail was reported in Towson. Trees were downed in Cockeysville, Dundalk, Hunt Valley, and Baltimore. In Harford County, 8 trees were downed onto roads across the county. The hardest hit areas included Bel Air and Fallston. Thunderstorms with high winds, frequent lightning, and large hail moved through Central Maryland during the evening of the 22nd. In Frederick County, trees were downed in several locations near Urbana. In Howard County, trees and power lines were downed in the western portion of the county. In Anne Arundel County, a power line was downed onto a car, a trailer, and a house in Pasadena. The truck and trailer were destroyed by the resulting fire and the house sustained minor damage. A dozen other power lines were downed across the northern portion of the county. In Baltimore County, golfball sized hail was reported in Towson. Trees were downed in Cockeysville, Dundalk, Hunt Valley, and Baltimore. In Harford County, 8 trees were downed onto roads across the county. The hardest hit areas included Bel Air and Fallston. Thunderstorms with high winds, frequent lightning, and large hail moved through Central Maryland during the evening of the 22nd. In Frederick County, trees were downed in several locations near Urbana. In Howard County, trees and power lines were downed in the western portion of the county. In Anne Arundel County, a power line was downed onto a car, a trailer, and a house in Pasadena. The truck and trailer were destroyed by the resulting fire and the house sustained minor damage. A dozen other power lines were downed across the northern portion of the county. In Baltimore County, golfball sized hail was reported in Towson. Trees were downed in Cockeysville, Dundalk, Hunt Valley, and Baltimore. In Harford County, 8 trees were downed onto roads across the county. The hardest hit areas included Bel Air and Fallston. Thunderstorms with high winds, frequent lightning, and large hail moved through Central Maryland during the evening of the 22nd. In Frederick County, trees were downed in several locations near Urbana. In Howard County, trees and power lines were downed in the western portion of the county. In Anne Arundel County, a power line was downed onto a car, a trailer, and a house in Pasadena. The truck and trailer were destroyed by the resulting fire and the house sustained minor damage. A dozen other power lines were downed across the northern portion of the county. In Baltimore County, golfball sized hail was reported in Towson. Trees were downed in Cockeysville, Dundalk, Hunt Valley, and Baltimore. In Harford County, 8 trees were downed onto roads across the county. The hardest hit areas included Bel Air and Fallston.\nEvent Narrative: Trees were downed. Several trees were downed. Over a dozen power lines were downed. Trees and power lines were downed. Golfball sized hail was reported.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 21.0981 km away, between 2003-08-26 15:30:00 and 2003-08-26 16:15:00. The events included records with estimated wind gusts of 55.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 73000.0 and crop damage of 0.0. \n\nEpisode Narrative: A line of thunderstorms with winds up to 78 MPH, hail, and frequent lightning moved from northwest to southeast across Maryland during the afternoon and evening of the 26th. Widespread damage was reported from downed trees and power lines in addition to lightning strikes. Over 150,000 customers lost power as a direct result of the storms. In Washington County, numerous trees and power lines were downed, especially across the western and central portion of the county. The hardest hit areas included Hancock, Williamsport, Fairplay, Pleasant Valley, Sharpsburg, Boonesboro, and Mt. Edna. A wind gust of 65 MPH was recorded by a spotter in Sharpsburg. House fires caused by lightning were reported in Clear Spring and Brunswick. In Frederick County, downed trees and power lines blocked 19 roads countywide, including Gapland Road in Burkittsville, Route 144 just south of Interstate 70, and Route 40 just west of Middletown. Other areas where damage was reported included Gapland, Emmitsburg, Brunswick, Petersville, Rosemont, Knoxville, and Frederick. A wind gust of 60 MPH was recorded in Point of Rocks. A gust of 52 MPH was recorded in Frederick. A garage in Knoxville burned to the ground after being struck by lightning. In Carroll County, several trees and power lines were downed. A roof under construction was damaged at Carrolltown Center in Eldersburg. In Westminster, West Main Street was closed for several hours by a live downed power line. In Baltimore County, numerous downed trees and power lines caused power outages, including in the community of Garrison. Twenty trees were downed in the city of Baltimore. In Howard County, numerous downed trees and power lines were reported. In Montgomery County, a 59 MPH wind gust was recorded in Damascus and Potomac. A wind gust of 57 MPH was reported in Rockville. Downed trees and power lines were reported on Route 104 north of Laytonsville in addition to several other roads across the county. Communities reporting damage included Gaithersburg, Bethesda, Wheaton, Germantown, Takoma Park, Burtonsville, Silver Spring, Damascus, Rockville, Potomac, and Montgomery Village. In addition, over a dozen buildings were struck by lightning, including a barn in Poolesville and apartment buildings in Silver Spring and Gaithersburg. Unknown injures were reported at house fires in Potomac and Aspen Hill. In Anne Arundel County, hundreds of trees and power lines were felled. Damage was reported in Severna Park, Arden on the Severn, Cape St. John, Annapolis, Glen Burnie, Odenton, and Millersville. One woman and five children were trapped in a van when trees came down on it in Crofton. A wind gust of 49 MPH was recorded at BWI Airport. In addition, a lightning strike started a fire which burned an unoccupied trailer home to the ground in Severna Park. In Prince George's County, officials were quoted as saying parts of the county looked like a \"war zone\" after numerous trees and power lines were downed onto roads and structures. In Bowie, numerous homes, porches, sheds, cars, and fences were damaged. Over 60 dump truck loads of debris were removed from the city following the storm. So many trees came down on the Whitemarsh Park nature trail that it was closed for weeks. In addition, damage was reported in Lanham, Hyattsville, Bladensburg, and Beltsville where a 78 MPH gust was recorded. A power line was downed onto the Capitol Beltway in Greenbelt and electrified a guard rail which led to the closure of the road for several hours. Penny sized hail fell in Brandywine. In Charles County, trees and power lines were downed in Bryantown. Penny to quarter sized hail fell in Ironsides and penny sized hail was reported in Waldorf. In Calvert County, numerous trees and power lines were felled. The hardest hit communities included Dunkirk and North Beach. In St. Mary's County, power poles were downed in Wicomico Shores. A line of thunderstorms with winds up to 78 MPH, hail, and frequent lightning moved from northwest to southeast across Maryland during the afternoon and evening of the 26th. Widespread damage was reported from downed trees and power lines in addition to lightning strikes. Over 150,000 customers lost power as a direct result of the storms. In Washington County, numerous trees and power lines were downed, especially across the western and central portion of the county. The hardest hit areas included Hancock, Williamsport, Fairplay, Pleasant Valley, Sharpsburg, Boonesboro, and Mt. Edna. A wind gust of 65 MPH was recorded by a spotter in Sharpsburg. House fires caused by lightning were reported in Clear Spring and Brunswick. In Frederick County, downed trees and power lines blocked 19 roads countywide, including Gapland Road in Burkittsville, Route 144 just south of Interstate 70, and Route 40 just west of Middletown. Other areas where damage was reported included Gapland, Emmitsburg, Brunswick, Petersville, Rosemont, Knoxville, and Frederick. A wind gust of 60 MPH was recorded in Point of Rocks. A gust of 52 MPH was recorded in Frederick. A garage in Knoxville burned to the ground after being struck by lightning. In Carroll County, several trees and power lines were downed. A roof under construction was damaged at Carrolltown Center in Eldersburg. In Westminster, West Main Street was closed for several hours by a live downed power line. In Baltimore County, numerous downed trees and power lines caused power outages, including in the community of Garrison. Twenty trees were downed in the city of Baltimore. In Howard County, numerous downed trees and power lines were reported. In Montgomery County, a 59 MPH wind gust was recorded in Damascus and Potomac. A wind gust of 57 MPH was reported in Rockville. Downed trees and power lines were reported on Route 104 north of Laytonsville in addition to several other roads across the county. Communities reporting damage included Gaithersburg, Bethesda, Wheaton, Germantown, Takoma Park, Burtonsville, Silver Spring, Damascus, Rockville, Potomac, and Montgomery Village. In addition, over a dozen buildings were struck by lightning, including a barn in Poolesville and apartment buildings in Silver Spring and Gaithersburg. Unknown injures were reported at house fires in Potomac and Aspen Hill. In Anne Arundel County, hundreds of trees and power lines were felled. Damage was reported in Severna Park, Arden on the Severn, Cape St. John, Annapolis, Glen Burnie, Odenton, and Millersville. One woman and five children were trapped in a van when trees came down on it in Crofton. A wind gust of 49 MPH was recorded at BWI Airport. In addition, a lightning strike started a fire which burned an unoccupied trailer home to the ground in Severna Park. In Prince George's County, officials were quoted as saying parts of the county looked like a \"war zone\" after numerous trees and power lines were downed onto roads and structures. In Bowie, numerous homes, porches, sheds, cars, and fences were damaged. Over 60 dump truck loads of debris were removed from the city following the storm. So many trees came down on the Whitemarsh Park nature trail that it was closed for weeks. In addition, damage was reported in Lanham, Hyattsville, Bladensburg, and Beltsville where a 78 MPH gust was recorded. A power line was downed onto the Capitol Beltway in Greenbelt and electrified a guard rail which led to the closure of the road for several hours. Penny sized hail fell in Brandywine. In Charles County, trees and power lines were downed in Bryantown. Penny to quarter sized hail fell in Ironsides and penny sized hail was reported in Waldorf. In Calvert County, numerous trees and power lines were felled. The hardest hit communities included Dunkirk and North Beach. In St. Mary's County, power poles were downed in Wicomico Shores. A line of thunderstorms with winds up to 78 MPH, hail, and frequent lightning moved from northwest to southeast across Maryland during the afternoon and evening of the 26th. Widespread damage was reported from downed trees and power lines in addition to lightning strikes. Over 150,000 customers lost power as a direct result of the storms. In Washington County, numerous trees and power lines were downed, especially across the western and central portion of the county. The hardest hit areas included Hancock, Williamsport, Fairplay, Pleasant Valley, Sharpsburg, Boonesboro, and Mt. Edna. A wind gust of 65 MPH was recorded by a spotter in Sharpsburg. House fires caused by lightning were reported in Clear Spring and Brunswick. In Frederick County, downed trees and power lines blocked 19 roads countywide, including Gapland Road in Burkittsville, Route 144 just south of Interstate 70, and Route 40 just west of Middletown. Other areas where damage was reported included Gapland, Emmitsburg, Brunswick, Petersville, Rosemont, Knoxville, and Frederick. A wind gust of 60 MPH was recorded in Point of Rocks. A gust of 52 MPH was recorded in Frederick. A garage in Knoxville burned to the ground after being struck by lightning. In Carroll County, several trees and power lines were downed. A roof under construction was damaged at Carrolltown Center in Eldersburg. In Westminster, West Main Street was closed for several hours by a live downed power line. In Baltimore County, numerous downed trees and power lines caused power outages, including in the community of Garrison. Twenty trees were downed in the city of Baltimore. In Howard County, numerous downed trees and power lines were reported. In Montgomery County, a 59 MPH wind gust was recorded in Damascus and Potomac. A wind gust of 57 MPH was reported in Rockville. Downed trees and power lines were reported on Route 104 north of Laytonsville in addition to several other roads across the county. Communities reporting damage included Gaithersburg, Bethesda, Wheaton, Germantown, Takoma Park, Burtonsville, Silver Spring, Damascus, Rockville, Potomac, and Montgomery Village. In addition, over a dozen buildings were struck by lightning, including a barn in Poolesville and apartment buildings in Silver Spring and Gaithersburg. Unknown injures were reported at house fires in Potomac and Aspen Hill. In Anne Arundel County, hundreds of trees and power lines were felled. Damage was reported in Severna Park, Arden on the Severn, Cape St. John, Annapolis, Glen Burnie, Odenton, and Millersville. One woman and five children were trapped in a van when trees came down on it in Crofton. A wind gust of 49 MPH was recorded at BWI Airport. In addition, a lightning strike started a fire which burned an unoccupied trailer home to the ground in Severna Park. In Prince George's County, officials were quoted as saying parts of the county looked like a \"war zone\" after numerous trees and power lines were downed onto roads and structures. In Bowie, numerous homes, porches, sheds, cars, and fences were damaged. Over 60 dump truck loads of debris were removed from the city following the storm. So many trees came down on the Whitemarsh Park nature trail that it was closed for weeks. In addition, damage was reported in Lanham, Hyattsville, Bladensburg, and Beltsville where a 78 MPH gust was recorded. A power line was downed onto the Capitol Beltway in Greenbelt and electrified a guard rail which led to the closure of the road for several hours. Penny sized hail fell in Brandywine. In Charles County, trees and power lines were downed in Bryantown. Penny to quarter sized hail fell in Ironsides and penny sized hail was reported in Waldorf. In Calvert County, numerous trees and power lines were felled. The hardest hit communities included Dunkirk and North Beach. In St. Mary's County, power poles were downed in Wicomico Shores. A line of thunderstorms with winds up to 78 MPH, hail, and frequent lightning moved from northwest to southeast across Maryland during the afternoon and evening of the 26th. Widespread damage was reported from downed trees and power lines in addition to lightning strikes. Over 150,000 customers lost power as a direct result of the storms. In Washington County, numerous trees and power lines were downed, especially across the western and central portion of the county. The hardest hit areas included Hancock, Williamsport, Fairplay, Pleasant Valley, Sharpsburg, Boonesboro, and Mt. Edna. A wind gust of 65 MPH was recorded by a spotter in Sharpsburg. House fires caused by lightning were reported in Clear Spring and Brunswick. In Frederick County, downed trees and power lines blocked 19 roads countywide, including Gapland Road in Burkittsville, Route 144 just south of Interstate 70, and Route 40 just west of Middletown. Other areas where damage was reported included Gapland, Emmitsburg, Brunswick, Petersville, Rosemont, Knoxville, and Frederick. A wind gust of 60 MPH was recorded in Point of Rocks. A gust of 52 MPH was recorded in Frederick. A garage in Knoxville burned to the ground after being struck by lightning. In Carroll County, several trees and power lines were downed. A roof under construction was damaged at Carrolltown Center in Eldersburg. In Westminster, West Main Street was closed for several hours by a live downed power line. In Baltimore County, numerous downed trees and power lines caused power outages, including in the community of Garrison. Twenty trees were downed in the city of Baltimore. In Howard County, numerous downed trees and power lines were reported. In Montgomery County, a 59 MPH wind gust was recorded in Damascus and Potomac. A wind gust of 57 MPH was reported in Rockville. Downed trees and power lines were reported on Route 104 north of Laytonsville in addition to several other roads across the county. Communities reporting damage included Gaithersburg, Bethesda, Wheaton, Germantown, Takoma Park, Burtonsville, Silver Spring, Damascus, Rockville, Potomac, and Montgomery Village. In addition, over a dozen buildings were struck by lightning, including a barn in Poolesville and apartment buildings in Silver Spring and Gaithersburg. Unknown injures were reported at house fires in Potomac and Aspen Hill. In Anne Arundel County, hundreds of trees and power lines were felled. Damage was reported in Severna Park, Arden on the Severn, Cape St. John, Annapolis, Glen Burnie, Odenton, and Millersville. One woman and five children were trapped in a van when trees came down on it in Crofton. A wind gust of 49 MPH was recorded at BWI Airport. In addition, a lightning strike started a fire which burned an unoccupied trailer home to the ground in Severna Park. In Prince George's County, officials were quoted as saying parts of the county looked like a \"war zone\" after numerous trees and power lines were downed onto roads and structures. In Bowie, numerous homes, porches, sheds, cars, and fences were damaged. Over 60 dump truck loads of debris were removed from the city following the storm. So many trees came down on the Whitemarsh Park nature trail that it was closed for weeks. In addition, damage was reported in Lanham, Hyattsville, Bladensburg, and Beltsville where a 78 MPH gust was recorded. A power line was downed onto the Capitol Beltway in Greenbelt and electrified a guard rail which led to the closure of the road for several hours. Penny sized hail fell in Brandywine. In Charles County, trees and power lines were downed in Bryantown. Penny to quarter sized hail fell in Ironsides and penny sized hail was reported in Waldorf. In Calvert County, numerous trees and power lines were felled. The hardest hit communities included Dunkirk and North Beach. In St. Mary's County, power poles were downed in Wicomico Shores.\nEvent Narrative: Hundreds of trees and power lines were downed. Numerous trees were downed. Twenty trees were downed. Numerous trees and power lines were downed.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 39.1304 km away, between 2003-08-26 16:05:00 and 2003-08-26 16:05:00. The events included records with estimated wind gusts of 52.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A severe thunderstorm knocked down a few trees and wires in Rock Hall. The series of severe thunderstorms knocked out power to about 5,500 Conectiv Energy and Choptank Electric Cooperative customers in the Delmarva Peninsula.\nEvent Narrative:", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 44.2516 km away, between 2003-08-26 16:10:00 and 2003-08-26 16:10:00. The events included records with estimated wind gusts of 56.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A severe thunderstorm knocked down several trees in the southern half of Kent Island. A telephone pole snapped on Maryland State Route 8 and cut power to about 1,700 Conectiv Energy customers on the southern half of the island. This represented about one-third of the total outages that occurred across the Delmarva Peninsula from the thunderstorms that afternoon and evening. Power was restored around midnight EDT that night. Power was also lost for about three hours on one of the spans on the William Preston Lane Jr. Memorial Bridge that crosses Chesapeake Bay.\nEvent Narrative:", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 14.3981 km away, between 2003-08-27 17:55:00 and 2003-08-27 17:55:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 500.0 and crop damage of 0.0. \n\nEpisode Narrative: Thunderstorms with high winds, frequent lightning, and hail moved through much of Maryland during the evening of the 27th. In Allegany County, a large tree was downed onto a road in Cumberland. In Frederick County, a man on the 15th hole at the Maryland National Golf Course near Middletown was injured when lightning struck nearby. The bolt caused him to fall down and hit his head. He lost feeling in his legs for a while and was transported to a local trauma center. In Baltimore County, lightning struck the cupola on historic Sheppard Pratt Hospital in Towson. A 4-alarm blaze ensued and 60 people had to be evacuated from the structure. One person was injured during the evacuation. In addition, another bolt struck about 100 feet away from Carroll Manor Elementary School in Baldwin. The bolt damaged the electrical system at the school. In Howard County, a tree was downed onto Ellicott Mills Drive in Ellicott City. In Montgomery County, penny sized hail fell in Aspen Hill. In Prince George's County, trees were downed in Beltsville, Rockville, and Kensington. In St. Mary's County, trees and power lines were downed in Clements, Morganza, and Budds Creek.\nEvent Narrative: A tree was downed onto Ellicott Mills Drive.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 39.1304 km away, between 2003-10-14 21:30:00 and 2003-10-14 22:00:00. The events included records with estimated wind gusts of 65.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A severe thunderstorm pulled down several trees and power lines in Kent County from Rock Hall east through Galena. In Rock Hall, trees as wide as 4 to 5 feet at their base were snapped. Shingles were torn from one home. A boat was blown from the bay inland. In Galena, a store front sign was torn down.\nEvent Narrative:", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 49.415 km away, between 2003-10-14 21:40:00 and 2003-10-14 22:00:00. The events included records with estimated wind gusts of 52.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A severe thunderstorm pulled down trees and power lines from Queenstown east through Centreville and Sudlersville in Queen Anne's County.\nEvent Narrative:", "The following events were reported: Hail. These occurred near station USW00093721, approximately 16.4596 km away, between 2003-10-22 15:40:00 and 2003-10-22 15:40:00. The events included records with hailstones measuring 0.75 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Scattered showers and isolated thunderstorms moved through Central Maryland on the afternoon of the 22nd.Penny sized hail was reported at Laurel. Pea sized hail was also reported in the Baltimore Metro area.\nEvent Narrative: Penny sized hail fell.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 14.5993 km away, between 2003-11-05 15:55:00 and 2003-11-05 16:20:00.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 2500.0 and crop damage of 0.0. \n\nEpisode Narrative: A line of strong to severe thunderstorms developed ahead of an approaching cold front on the 5th and caused widespread wind damage and some flash flooding from Northern Virginia to Eastern Maryland. Flash flooding was reported on Beech Drive in Bethesda. Over 2 inches of rain fell in some locations. A line of strong to severe thunderstorms developed ahead of an approaching cold front on the 5th and caused widespread wind damage and some flash flooding from Northern Virginia to Eastern Maryland. Flash flooding was reported on Beech Drive in Bethesda. Over 2 inches of rain fell in some locations. A line of strong to severe thunderstorms developed ahead of an approaching cold front on the 5th and caused widespread wind damage and some flash flooding from Northern Virginia to Eastern Maryland. Flash flooding was reported on Beech Drive in Bethesda. Over 2 inches of rain fell in some locations.\nEvent Narrative: A very large tree was knocked down. Large tree downed. Trees downed across the county.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 39.3081 km away, between 2003-11-19 13:20:00 and 2003-11-19 14:25:00.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 750.0 and crop damage of 0.0. \n\nEpisode Narrative: A line of strong to severe thunderstorms moved across the region on the 19th. These storms preceded a cold front and produced gusty, damaging winds and heavy rainfall. Rainfall amounts averaged 2 to 4 inches. Widespread power outages were reported due to downed trees and power lines. The heavy rainfall led to flash flooding across the Potomac Highlands and Northeast and Central Maryland. Four deaths were attributed to flooding in Baltimore City. A student drowned after falling into Herring Run Creek and three workers were washed away while working in a storm drain. Emergency and rescue officials also had to perform swift water rescues for vehicles trapped in high water in Poolesville. Several cars were flooded in the Germantown area. A line of strong to severe thunderstorms moved across the region on the 19th. These storms preceded a cold front and produced gusty, damaging winds and heavy rainfall. Rainfall amounts averaged 2 to 4 inches. Widespread power outages were reported due to downed trees and power lines. The heavy rainfall led to flash flooding across the Potomac Highlands and Northeast and Central Maryland. Four deaths were attributed to flooding in Baltimore City. A student drowned after falling into Herring Run Creek and three workers were washed away while working in a storm drain. Emergency and rescue officials also had to perform swift water rescues for vehicles trapped in high water in Poolesville. Several cars were flooded in the Germantown area.\nEvent Narrative: Large tree downed. Downed trees.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 39.1304 km away, between 2003-11-19 14:50:00 and 2003-11-19 14:50:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A severe thunderstorm knocked down a couple of trees and power lines in Rock Hall.\nEvent Narrative:", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 29.7222 km away, between 2004-05-02 20:10:00 and 2004-05-02 20:40:00. The events included records with estimated wind gusts of 53.6 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 24000.0 and crop damage of 0.0. \n\nEpisode Narrative: \nEvent Narrative: Downed trees and powerlines. Downed trees. Downed trees. Downed trees. Downed trees and power lines.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 32.4592 km away, between 2004-05-02 20:10:00 and 2004-05-02 20:10:00. The events included records with estimated wind gusts of 57.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 4000.0 and crop damage of 0.0. \n\nEpisode Narrative: \nEvent Narrative: Numerous trees and power lines down.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 34.0402 km away, between 2004-05-02 20:10:00 and 2004-05-02 20:10:00. The events included records with estimated wind gusts of 57.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 3000.0 and crop damage of 0.0. \n\nEpisode Narrative: \nEvent Narrative: Numerous trees and power lines down.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 21.0841 km away, between 2004-05-02 20:30:00 and 2004-05-02 20:30:00. The events included records with estimated wind gusts of 55.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 5000.0 and crop damage of 0.0. \n\nEpisode Narrative: \nEvent Narrative: Trees and power lines down.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 14.3981 km away, between 2004-05-02 20:30:00 and 2004-05-02 20:30:00. The events included records with estimated wind gusts of 54.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 3000.0 and crop damage of 0.0. \n\nEpisode Narrative: \nEvent Narrative: Downed trees.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 15.2417 km away, between 2004-05-02 20:40:00 and 2004-05-02 20:40:00. The events included records with estimated wind gusts of 53.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 5000.0 and crop damage of 0.0. \n\nEpisode Narrative: \nEvent Narrative: Trees down.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 26.2288 km away, between 2004-05-02 20:40:00 and 2004-05-02 20:40:00. The events included records with estimated wind gusts of 55.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 3000.0 and crop damage of 0.0. \n\nEpisode Narrative: \nEvent Narrative: Numerous trees and power lines down.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 4.4469 km away, between 2004-05-02 20:45:00 and 2004-05-02 20:45:00. The events included records with estimated wind gusts of 55.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 3000.0 and crop damage of 0.0. \n\nEpisode Narrative: \nEvent Narrative: Trees and power lines down.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 44.5294 km away, between 2004-05-02 21:05:00 and 2004-05-02 21:05:00. The events included records with estimated wind gusts of 57.5 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 105000.0 and crop damage of 0.0. \n\nEpisode Narrative: A strong cold front moved through the region on May 2nd. Numerous showers and very strong thunderstorms developed ahead of the front. The thunderstorms produced widespread damage over Maryland, and most of the damage was concentrated in the northeast counties of Carroll, Harford, and Baltimore. In Eldersburg,Carroll County,winds knocked down a wall at the South Carroll Sports Arena during a soccer game. In Bel Air, Harford County, A tree crashed onto the roof of the Parks and Recreation Department's Headquarters. Estimated damages were between 80,000 and 100,000 dollars. 25 to 30 trees also fell on the Ma and Pa Hiking and Biking Trail, located between the Winter Run Golf Course and the Howard Park neighborhood. In Kingsville and Parksville, Baltimore County, 50 to 60 downed trees were reported. Power outages closed several schools in Baltimore County and the City of Baltimoreon May 3rd. A strong cold front moved through the region on May 2nd. Numerous showers and very strong thunderstorms developed ahead of the front. The thunderstorms produced widespread damage over Maryland, and most of the damage was concentrated in the northeast counties of Carroll, Harford, and Baltimore. In Eldersburg,Carroll County,winds knocked down a wall at the South Carroll Sports Arena during a soccer game. In Bel Air, Harford County, A tree crashed onto the roof of the Parks and Recreation Department's Headquarters. Estimated damages were between 80,000 and 100,000 dollars. 25 to 30 trees also fell on the Ma and Pa Hiking and Biking Trail, located between the Winter Run Golf Course and the Howard Park neighborhood. In Kingsville and Parksville, Baltimore County, 50 to 60 downed trees were reported. Power outages closed several schools in Baltimore County and the City of Baltimoreon May 3rd.\nEvent Narrative: Trees and powerlines down. Trees and power lines down.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 16.4939 km away, between 2004-05-15 20:20:00 and 2004-05-15 20:20:00. The events included records with estimated wind gusts of 55.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 500.0 and crop damage of 0.0. \n\nEpisode Narrative: Scattered thunderstorms moved across Northeast Maryland on the evening of May 15 th. Downed trees and power lines were reportedFrederick and Baltimore Counties.\nEvent Narrative: Tree down.", "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00093721, approximately 19.2101 km away, between 2004-05-17 14:05:00 and 2004-05-17 17:45:00. The events included records with hailstones measuring 16.304285714285715 inches.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 5000.0 and crop damage of 0.0. \n\nEpisode Narrative: Scattered afternoon thunderstorms produced damage across portions of Northeast Maryland. Reports included downed trees, downed power lines, and penny to nickel size hail. Scattered afternoon thunderstorms produced damage across portions of Northeast Maryland. Reports included downed trees, downed power lines, and penny to nickel size hail. Scattered afternoon thunderstorms produced damage across portions of Northeast Maryland. Reports included downed trees, downed power lines, and penny to nickel size hail. Scattered afternoon thunderstorms produced damage across portions of Northeast Maryland. Reports included downed trees, downed power lines, and penny to nickel size hail. Scattered afternoon thunderstorms produced damage across portions of Northeast Maryland. Reports included downed trees, downed power lines, and penny to nickel size hail. Scattered afternoon thunderstorms produced damage across portions of Northeast Maryland. Reports included downed trees, downed power lines, and penny to nickel size hail. Scattered afternoon thunderstorms produced damage across portions of Northeast Maryland. Reports included downed trees, downed power lines, and penny to nickel size hail.\nEvent Narrative: Penny size hail reported. Quarter size hail reported in Hampton. Trees down around the city. Nickel size hail reported. Penny size hail reported. Penny size hail reported. A few large limbs and power lines down.", "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00093721, approximately 12.4553 km away, between 2004-05-18 16:48:00 and 2004-05-18 17:15:00. The events included records with hailstones measuring 18.87666666666667 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front moved through the region late on May 19th. The numerous to scattered thunderstorms ahead of the front produced some wind damage, as well as hail ranging in size from pennies to nickels. A cold front moved through the region late on May 19th. The numerous to scattered thunderstorms ahead of the front produced some wind damage, as well as hail ranging in size from pennies to nickels. A cold front moved through the region late on May 19th. The numerous to scattered thunderstorms ahead of the front produced some wind damage, as well as hail ranging in size from pennies to nickels.\nEvent Narrative: Penny size hail reported by trained spotter. Nickel size hail reported. Several trees down.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 26.0555 km away, between 2004-05-25 18:05:00 and 2004-05-25 18:50:00. The events included records with estimated wind gusts of 57.5 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 13000.0 and crop damage of 0.0. \n\nEpisode Narrative: Thunderstorms spawned tornadoes in Washington and Frederick Counties. Other strong thunderstorms also produced wind and hail damage across North Central Maryland and the Metropolitan areas of Baltimore and Washington DC. Downed trees and power lines caused power outages for over 100,000 customers. Penny to golfball size hail damaged cars and gardens. Lightning strikes started a number of house fires according to Fire and Rescue Personnel. Maryland State Police responded to several accidents blamed on the pelting hail and ponding of water on roadways. Thunderstorms spawned tornadoes in Washington and Frederick Counties. Other strong thunderstorms also produced wind and hail damage across North Central Maryland and the Metropolitan areas of Baltimore and Washington DC. Downed trees and power lines caused power outages for over 100,000 customers. Penny to golfball size hail damaged cars and gardens. Lightning strikes started a number of house fires according to Fire and Rescue Personnel. Maryland State Police responded to several accidents blamed on the pelting hail and ponding of water on roadways. Thunderstorms spawned tornadoes in Washington and Frederick Counties. Other strong thunderstorms also produced wind and hail damage across North Central Maryland and the Metropolitan areas of Baltimore and Washington DC. Downed trees and power lines caused power outages for over 100,000 customers. Penny to golfball size hail damaged cars and gardens. Lightning strikes started a number of house fires according to Fire and Rescue Personnel. Maryland State Police responded to several accidents blamed on the pelting hail and ponding of water on roadways. Thunderstorms spawned tornadoes in Washington and Frederick Counties. Other strong thunderstorms also produced wind and hail damage across North Central Maryland and the Metropolitan areas of Baltimore and Washington DC. Downed trees and power lines caused power outages for over 100,000 customers. Penny to golfball size hail damaged cars and gardens. Lightning strikes started a number of house fires according to Fire and Rescue Personnel. Maryland State Police responded to several accidents blamed on the pelting hail and ponding of water on roadways.\nEvent Narrative: Trees down. Trees and power lines down across the county. Many trees and power lines down in north Anne Arundel County. Trees and power lines down countywide.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 5.5755 km away, between 2004-05-25 18:15:00 and 2004-05-25 18:15:00. The events included records with estimated wind gusts of 60.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 1000.0 and crop damage of 0.0. \n\nEpisode Narrative: \nEvent Narrative: Strong thunderstorm winds knocked down trees.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 24.8699 km away, between 2004-06-01 14:10:00 and 2004-06-01 14:45:00. The events included records with estimated wind gusts of 55.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 5000.0 and crop damage of 0.0. \n\nEpisode Narrative: A stalled frontal boundary and a passing upper level disturbance produced scattered showers and thunderstorms across Northeast Maryland and the Washington Metro area. The thunderstorms were accompanied by strong winds that downed trees and power lines. A stalled frontal boundary and a passing upper level disturbance produced scattered showers and thunderstorms across Northeast Maryland and the Washington Metro area. The thunderstorms were accompanied by strong winds that downed trees and power lines.\nEvent Narrative: Trees down. Trees down.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 38.1139 km away, between 2004-06-01 15:05:00 and 2004-06-01 15:05:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A severe thunderstorm pulled down large tree limbs and wires on Kent Island.\nEvent Narrative:", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 38.1139 km away, between 2004-06-02 19:41:00 and 2004-06-02 20:07:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A severe thunderstorm knocked down several large tree limbs and wires across the southern tier of Queen Anne's County.\nEvent Narrative:", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 34.599 km away, between 2004-06-14 18:45:00 and 2004-06-14 18:45:00. The events included records with estimated wind gusts of 55.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 2000.0 and crop damage of 0.0. \n\nEpisode Narrative: A strong cluster of thunderstorms moved across Northeast Maryland on the evening of the 14th. The storms downed trees and power lines, spawned a couple of weak tornadoes, and produced some very heavy rainfall. The downed trees and power lines lead to power outages for over 5000 customers. Storm surveys by NWS personnel confirmed two weak tornadoes, one in Frederick County and another in Harford County. The damage was confined uprooted and topped trees. Flash flooding was also an issue with these storms. The Department of Natural Resources State Forestry and Park service reported problems in Cunningham Falls State Park, Frederick County. Four to five inches of rain caused ditches to overflow, the Park's lakes to fill with debris, and the bridge on Catoctin Hollow Road to washout. Rocks State Park, Harford County, also reported water damage. Roads in Darlington, Pylesville, Norrisville, and Whiteford were closed due to water covering the roadways. Water rescues saved the lives of a 7 year old Frederick County and a Harford County couple. The child fell into a creek and was swept through a gully and drain pipe before the Fire and Rescue team saved him. The couple's jeep was stranded in high water and they had to be lifted out.\nEvent Narrative: Trees down in Central Baltimore County.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 35.1239 km away, between 2004-06-17 14:20:00 and 2004-06-17 14:20:00. The events included records with estimated wind gusts of 65.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 2000.0 and crop damage of 0.0. \n\nEpisode Narrative: Thunderstorms accompanied by strong winds and heavy rainfall affected the Mid Atlantic region during the evening of the 17th. Reports of downed trees, a weak tornado, lightning strikes, and torrential rainfall came from Northeast and Lower Southern Maryland. A weak tornado touched down just outside of LaPlata in Charles County. Many homes and structures were damaged by fire and water. Firemen reported several fires caused by lightning in St. Mary's and Prince Georges Counties. Emergency personnel also reported the ceiling of a restaurant in Inverson Mall in Hill Crest Heights collapsed under the weight of rain water, and flash flooding necessitated a water rescue on the Suitland Parkway.\nEvent Narrative: Trees down.", "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00093721, approximately 26.2273 km away, between 2004-07-01 15:25:00 and 2004-07-01 15:59:00. The events included records with hailstones measuring 42.6875 inches.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 6000.0 and crop damage of 0.0. \n\nEpisode Narrative: A warm front lifted north into Southern Pennsylvania on the 1st. The airmass was very moist and unstable by the afternoon. Scattered showers and thunderstorms developed over the region. Some of the storms produced large hail ranging from a penny to baseball size in Baltimore, Montgomery and Prince Georges Counties. The storms were also accompanied by strong winds that downed trees and power lines. A warm front lifted north into Southern Pennsylvania on the 1st. The airmass was very moist and unstable by the afternoon. Scattered showers and thunderstorms developed over the region. Some of the storms produced large hail ranging from a penny to baseball size in Baltimore, Montgomery and Prince Georges Counties. The storms were also accompanied by strong winds that downed trees and power lines. A warm front lifted north into Southern Pennsylvania on the 1st. The airmass was very moist and unstable by the afternoon. Scattered showers and thunderstorms developed over the region. Some of the storms produced large hail ranging from a penny to baseball size in Baltimore, Montgomery and Prince Georges Counties. The storms were also accompanied by strong winds that downed trees and power lines. A warm front lifted north into Southern Pennsylvania on the 1st. The airmass was very moist and unstable by the afternoon. Scattered showers and thunderstorms developed over the region. Some of the storms produced large hail ranging from a penny to baseball size in Baltimore, Montgomery and Prince Georges Counties. The storms were also accompanied by strong winds that downed trees and power lines.\nEvent Narrative: Large limbs down on powerlines. Trees down. Trees and powerlines down. Baseball size hail reported by law enforcement officers.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 31.7106 km away, between 2004-07-05 15:17:00 and 2004-07-05 17:15:00. The events included records with estimated wind gusts of 57.5 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 34500.0 and crop damage of 0.0. \n\nEpisode Narrative: Showers and thunderstorms developed ahead of an approaching cold front on the 5th. Some storms produced heavy rainfall, strong winds and nickel to walnut size hail over North Central and Northeast Maryland. The winds downed trees and power lines. In Baltimore County alone, 25 to 35 trees were downed at the intersection of Harford and Hutschenreuter Roads in Perry Hall. At the height of the storms thousands of customers in Anne Arundel, Harford, and Baltimore Counties were without power. Showers and thunderstorms developed ahead of an approaching cold front on the 5th. Some storms produced heavy rainfall, strong winds and nickel to walnut size hail over North Central and Northeast Maryland. The winds downed trees and power lines. In Baltimore County alone, 25 to 35 trees were downed at the intersection of Harford and Hutschenreuter Roads in Perry Hall. At the height of the storms thousands of customers in Anne Arundel, Harford, and Baltimore Counties were without power. Showers and thunderstorms developed ahead of an approaching cold front on the 5th. Some storms produced heavy rainfall, strong winds and nickel to walnut size hail over North Central and Northeast Maryland. The winds downed trees and power lines. In Baltimore County alone, 25 to 35 trees were downed at the intersection of Harford and Hutschenreuter Roads in Perry Hall. At the height of the storms thousands of customers in Anne Arundel, Harford, and Baltimore Counties were without power. Showers and thunderstorms developed ahead of an approaching cold front on the 5th. Some storms produced heavy rainfall, strong winds and nickel to walnut size hail over North Central and Northeast Maryland. The winds downed trees and power lines. In Baltimore County alone, 25 to 35 trees were downed at the intersection of Harford and Hutschenreuter Roads in Perry Hall. At the height of the storms thousands of customers in Anne Arundel, Harford, and Baltimore Counties were without power.\nEvent Narrative: Widespread trees and wires down in northeast Baltimore County. Tree down on a house in Bowie. Large tree and branches down around the area.", "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00093721, approximately 21.6096 km away, between 2004-07-07 14:41:00 and 2004-07-07 16:09:00. The events included records with hailstones measuring 45.55 inches.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 10500.0 and crop damage of 0.0. \n\nEpisode Narrative: Scattered showers and thunderstorms developed over the region on the 7th as a warm front lifted north into southern Pennsylvania. The thunderstorms across Northeast Maryland produced strong winds that downed trees and power lines, penny size hail, and flooding. Two to four inches of rain fell in Northeast Maryland with local amounts up to six inches. Dozens of water rescues were performed throughout the county, several motorists were trapped/stranded in stalled cars. A cyclist was rescued from a fence after he emerged his bike in the fast moving, deep watersIn the City of Baltimore, stores and businesses along the Jones Falls closed early to allow clients, shoppers and employees to get out before the waters started to rise. A portion of the historic Meadow Mill building in the Woodberry neighborhood was flooded, and nearly 30 cars in the parking lot were almost submerged. The Mount Washington neighborhood also witnessed some impressive flooding. The Meadow Hill Athletic Club reported a loss of 500,000 dollars in exercise equipment. A newly opened men clothing store reported damages around 400,000 dollars. In Southern Baltimore County, a mechanic in Catonsville barely escaped injury when the roof of his Auto repair shop collapsed due to the weight of the water.In north Anne Arundel County, lightning struck the historical Linthicum Heights United Methodist Church in Linthicum. Fire and water damaged a hand painted fresco on the ceiling of the church. Pieces of the building dated back to the 19th-century. Several other minor house fires were reported and attributed to lightning according to fire and rescue personnel, but no other major damage or injuries were cited. Scattered showers and thunderstorms developed over the region on the 7th as a warm front lifted north into southern Pennsylvania. The thunderstorms across Northeast Maryland produced strong winds that downed trees and power lines, penny size hail, and flooding. Two to four inches of rain fell in Northeast Maryland with local amounts up to six inches. Dozens of water rescues were performed throughout the county, several motorists were trapped/stranded in stalled cars. A cyclist was rescued from a fence after he emerged his bike in the fast moving, deep watersIn the City of Baltimore, stores and businesses along the Jones Falls closed early to allow clients, shoppers and employees to get out before the waters started to rise. A portion of the historic Meadow Mill building in the Woodberry neighborhood was flooded, and nearly 30 cars in the parking lot were almost submerged. The Mount Washington neighborhood also witnessed some impressive flooding. The Meadow Hill Athletic Club reported a loss of 500,000 dollars in exercise equipment. A newly opened men clothing store reported damages around 400,000 dollars. In Southern Baltimore County, a mechanic in Catonsville barely escaped injury when the roof of his Auto repair shop collapsed due to the weight of the water.In north Anne Arundel County, lightning struck the historical Linthicum Heights United Methodist Church in Linthicum. Fire and water damaged a hand painted fresco on the ceiling of the church. Pieces of the building dated back to the 19th-century. Several other minor house fires were reported and attributed to lightning according to fire and rescue personnel, but no other major damage or injuries were cited. Scattered showers and thunderstorms developed over the region on the 7th as a warm front lifted north into southern Pennsylvania. The thunderstorms across Northeast Maryland produced strong winds that downed trees and power lines, penny size hail, and flooding. Two to four inches of rain fell in Northeast Maryland with local amounts up to six inches. Dozens of water rescues were performed throughout the county, several motorists were trapped/stranded in stalled cars. A cyclist was rescued from a fence after he emerged his bike in the fast moving, deep watersIn the City of Baltimore, stores and businesses along the Jones Falls closed early to allow clients, shoppers and employees to get out before the waters started to rise. A portion of the historic Meadow Mill building in the Woodberry neighborhood was flooded, and nearly 30 cars in the parking lot were almost submerged. The Mount Washington neighborhood also witnessed some impressive flooding. The Meadow Hill Athletic Club reported a loss of 500,000 dollars in exercise equipment. A newly opened men clothing store reported damages around 400,000 dollars. In Southern Baltimore County, a mechanic in Catonsville barely escaped injury when the roof of his Auto repair shop collapsed due to the weight of the water.In north Anne Arundel County, lightning struck the historical Linthicum Heights United Methodist Church in Linthicum. Fire and water damaged a hand painted fresco on the ceiling of the church. Pieces of the building dated back to the 19th-century. Several other minor house fires were reported and attributed to lightning according to fire and rescue personnel, but no other major damage or injuries were cited. Scattered showers and thunderstorms developed over the region on the 7th as a warm front lifted north into southern Pennsylvania. The thunderstorms across Northeast Maryland produced strong winds that downed trees and power lines, penny size hail, and flooding. Two to four inches of rain fell in Northeast Maryland with local amounts up to six inches. Dozens of water rescues were performed throughout the county, several motorists were trapped/stranded in stalled cars. A cyclist was rescued from a fence after he emerged his bike in the fast moving, deep watersIn the City of Baltimore, stores and businesses along the Jones Falls closed early to allow clients, shoppers and employees to get out before the waters started to rise. A portion of the historic Meadow Mill building in the Woodberry neighborhood was flooded, and nearly 30 cars in the parking lot were almost submerged. The Mount Washington neighborhood also witnessed some impressive flooding. The Meadow Hill Athletic Club reported a loss of 500,000 dollars in exercise equipment. A newly opened men clothing store reported damages around 400,000 dollars. In Southern Baltimore County, a mechanic in Catonsville barely escaped injury when the roof of his Auto repair shop collapsed due to the weight of the water.In north Anne Arundel County, lightning struck the historical Linthicum Heights United Methodist Church in Linthicum. Fire and water damaged a hand painted fresco on the ceiling of the church. Pieces of the building dated back to the 19th-century. Several other minor house fires were reported and attributed to lightning according to fire and rescue personnel, but no other major damage or injuries were cited. Scattered showers and thunderstorms developed over the region on the 7th as a warm front lifted north into southern Pennsylvania. The thunderstorms across Northeast Maryland produced strong winds that downed trees and power lines, penny size hail, and flooding. Two to four inches of rain fell in Northeast Maryland with local amounts up to six inches. Dozens of water rescues were performed throughout the county, several motorists were trapped/stranded in stalled cars. A cyclist was rescued from a fence after he emerged his bike in the fast moving, deep watersIn the City of Baltimore, stores and businesses along the Jones Falls closed early to allow clients, shoppers and employees to get out before the waters started to rise. A portion of the historic Meadow Mill building in the Woodberry neighborhood was flooded, and nearly 30 cars in the parking lot were almost submerged. The Mount Washington neighborhood also witnessed some impressive flooding. The Meadow Hill Athletic Club reported a loss of 500,000 dollars in exercise equipment. A newly opened men clothing store reported damages around 400,000 dollars. In Southern Baltimore County, a mechanic in Catonsville barely escaped injury when the roof of his Auto repair shop collapsed due to the weight of the water.In north Anne Arundel County, lightning struck the historical Linthicum Heights United Methodist Church in Linthicum. Fire and water damaged a hand painted fresco on the ceiling of the church. Pieces of the building dated back to the 19th-century. Several other minor house fires were reported and attributed to lightning according to fire and rescue personnel, but no other major damage or injuries were cited.\nEvent Narrative: Penny size hail reported by the EOC. Downed trees. Large tree limbs down on powerlines in several locations. Trees down. Several trees and powerlines down countywide.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 31.8071 km away, between 2004-07-12 10:20:00 and 2004-07-12 10:20:00. The events included records with estimated wind gusts of 60.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 1500.0 and crop damage of 0.0. \n\nEpisode Narrative: A quasi-stationary boundary over the area provided a focus for shower and thunderstorm activity on the 12th. The thunderstorms produced very heavy rainfall and strong gusty winds. Baltimore and Harford Counties had downed trees and power lines. Portions of southern Harford County were drenched from the heavy down pours, especially Aberdeen and Harve de Grace. Several roads and streets were completely covered by high water. Route 40 between Aberdeen and Harve de Grace was closed for several hours. The Union Hotel in Port Deposit sustained significant flood damage. Over 20 homes were damaged, mostly by basement flooding. At least 32 people were rescued from stranded cars and flooded homes. Fifteen Amtrak passenger trains had delays due to water flowing over the tracks. Reports from the Harford EOC cited several feet of standing water in many areas. Some roads were completely washed out, causing the Governor to declare a limited State of Emergency.\nEvent Narrative: Trees down along Route 40.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 23.2075 km away, between 2004-08-04 17:15:00 and 2004-08-04 19:05:00. The events included records with estimated wind gusts of 54.8 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 13000.0 and crop damage of 0.0. \n\nEpisode Narrative: Strong thunderstorms moved through the region on August 4th. The storms toppled trees and downed power lines. At the height of the storm Baltimore Gas and Electric Company reported about 14,000 customers without power in portions of Prince Georges, Baltimore and Anne Arundel Counties. The storms even caused a 57 minute delay to the Baltimore Orioles and Seattle Mariners baseball game at Camden Yards Stadium, in downtown Baltimore. Strong thunderstorms moved through the region on August 4th. The storms toppled trees and downed power lines. At the height of the storm Baltimore Gas and Electric Company reported about 14,000 customers without power in portions of Prince Georges, Baltimore and Anne Arundel Counties. The storms even caused a 57 minute delay to the Baltimore Orioles and Seattle Mariners baseball game at Camden Yards Stadium, in downtown Baltimore. Strong thunderstorms moved through the region on August 4th. The storms toppled trees and downed power lines. At the height of the storm Baltimore Gas and Electric Company reported about 14,000 customers without power in portions of Prince Georges, Baltimore and Anne Arundel Counties. The storms even caused a 57 minute delay to the Baltimore Orioles and Seattle Mariners baseball game at Camden Yards Stadium, in downtown Baltimore. Strong thunderstorms moved through the region on August 4th. The storms toppled trees and downed power lines. At the height of the storm Baltimore Gas and Electric Company reported about 14,000 customers without power in portions of Prince Georges, Baltimore and Anne Arundel Counties. The storms even caused a 57 minute delay to the Baltimore Orioles and Seattle Mariners baseball game at Camden Yards Stadium, in downtown Baltimore. Strong thunderstorms moved through the region on August 4th. The storms toppled trees and downed power lines. At the height of the storm Baltimore Gas and Electric Company reported about 14,000 customers without power in portions of Prince Georges, Baltimore and Anne Arundel Counties. The storms even caused a 57 minute delay to the Baltimore Orioles and Seattle Mariners baseball game at Camden Yards Stadium, in downtown Baltimore.\nEvent Narrative: Trees and power lines down. Large branches and power lines. down. Downed trees and power lines. Trees and power lines down. TREES DOWNED", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 17.4172 km away, between 2004-08-11 15:10:00 and 2004-08-11 15:10:00. The events included records with estimated wind gusts of 55.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 2000.0 and crop damage of 0.0. \n\nEpisode Narrative: Strong thunderstorms downed trees and power lines in east Maryland. Around 20,000 people were without power. The three regional international airports, Reagan National, Dulles International, and Baltimore-Washington, reported 1 to 3 hour weather delays for flights departing to the northeast.\nEvent Narrative: Trees and power lines down across the area.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 35.0531 km away, between 2004-08-12 16:45:00 and 2004-08-12 16:45:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 1500.0 and crop damage of 0.0. \n\nEpisode Narrative: \nEvent Narrative: Several large trees down.", "The following events were reported: Tornado. These occurred near station USW00093721, approximately 39.7802 km away, between 2004-09-17 17:35:00 and 2004-09-17 17:39:00.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 120000.0 and crop damage of 0.0. \n\nEpisode Narrative: \nEvent Narrative: A thunderstorm moved north out of Loudoun County, Virginia into Montgomery County, Maryland. A tornado touched down and damaged a few structures in the Poolesville area and snapped and uprooted trees in the wooded area and farm land leading to Beallsville.", "The following events were reported: Flood. These occurred near station USW00093721, approximately 31.0773 km away, between 2005-01-14 06:30:00 and 2005-01-14 09:00:00. The flood was caused by . Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: \nEvent Narrative: High water on several roads.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 32.5736 km away, between 2005-02-16 13:20:00 and 2005-02-16 17:00:00. The events included records with measured wind gusts of 36.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A strong cold front moved into the marine forecast area. Numerous reports were received of wind gusts 35-40 kt over a short period of time in the late afternoon on 16 February. A strong cold front moved into the marine forecast area. Numerous reports were received of wind gusts 35-40 kt over a short period of time in the late afternoon on 16 February. A strong cold front moved into the marine forecast area. Numerous reports were received of wind gusts 35-40 kt over a short period of time in the late afternoon on 16 February.\nEvent Narrative: Wind gust measured at Thomas Point Light", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 25.892 km away, between 2005-03-28 15:30:00 and 2005-03-28 16:10:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A significant severe weather event occurred on March 28. This was due to a strong low pressure system which pulled warm and unstable air into the region during the daytime. Several of these gusty showers continued to move from the Washington, DC area into the coastal waters of the Chesapeake Bay and Tidal Potomac River. A significant severe weather event occurred on March 28. This was due to a strong low pressure system which pulled warm and unstable air into the region during the daytime. Several of these gusty showers continued to move from the Washington, DC area into the coastal waters of the Chesapeake Bay and Tidal Potomac River.\nEvent Narrative:", "The following events were reported: Flash Flood, Thunderstorm Wind. These occurred near station USW00093721, approximately 22.9057 km away, between 2005-04-02 11:40:00 and 2005-04-02 23:00:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A strong cold front crossed the Mid Atlantic Saturday, April 2nd. This front brought severe thunderstorms that downed trees and power lines as well as heavy downpours that flooded rivers, streams, and roadways. After the front passed, strong winds downed trees and power lines mainly in the higher terrain of western Maryland. A strong cold front crossed the Mid Atlantic Saturday, April 2nd. This front brought severe thunderstorms that downed trees and power lines as well as heavy downpours that flooded rivers, streams, and roadways. After the front passed, strong winds downed trees and power lines mainly in the higher terrain of western Maryland. A strong cold front crossed the Mid Atlantic Saturday, April 2nd. This front brought severe thunderstorms that downed trees and power lines as well as heavy downpours that flooded rivers, streams, and roadways. After the front passed, strong winds downed trees and power lines mainly in the higher terrain of western Maryland.\nEvent Narrative: Roads closed county wide Road closed due to flooding Trees and powerlines down", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 27.0296 km away, between 2005-04-02 12:22:00 and 2005-04-02 20:25:00. The events included records with measured wind gusts of 38.666666666666664 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A strong cold front crossed the Chesapeake Bay waters on Saturday, April 2nd. This front brought scattered thunderstorms causing strong wind gusts. A strong cold front crossed the Chesapeake Bay waters on Saturday, April 2nd. This front brought scattered thunderstorms causing strong wind gusts. A strong cold front crossed the Chesapeake Bay waters on Saturday, April 2nd. This front brought scattered thunderstorms causing strong wind gusts.\nEvent Narrative:", "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00093721, approximately 26.6501 km away, between 2005-04-23 16:30:00 and 2005-04-23 16:50:00. The events included records with hailstones measuring 25.4075 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A very strong cold front moved across the mid-Atlantic region on April 23, 2005. This front interacted with a moist and unstable airmass to generate significant strong to severe thunderstorms and high winds. Wind damage was reported across portions of central and northern Virginia, and southern and central Maryland, as well as across the Tidal Potomac and upper Chesapeake Bay marine waters. Damaging large hail was also reported in many locations with this storm system. A very strong cold front moved across the mid-Atlantic region on April 23, 2005. This front interacted with a moist and unstable airmass to generate significant strong to severe thunderstorms and high winds. Wind damage was reported across portions of central and northern Virginia, and southern and central Maryland, as well as across the Tidal Potomac and upper Chesapeake Bay marine waters. Damaging large hail was also reported in many locations with this storm system. A very strong cold front moved across the mid-Atlantic region on April 23, 2005. This front interacted with a moist and unstable airmass to generate significant strong to severe thunderstorms and high winds. Wind damage was reported across portions of central and northern Virginia, and southern and central Maryland, as well as across the Tidal Potomac and upper Chesapeake Bay marine waters. Damaging large hail was also reported in many locations with this storm system. A very strong cold front moved across the mid-Atlantic region on April 23, 2005. This front interacted with a moist and unstable airmass to generate significant strong to severe thunderstorms and high winds. Wind damage was reported across portions of central and northern Virginia, and southern and central Maryland, as well as across the Tidal Potomac and upper Chesapeake Bay marine waters. Damaging large hail was also reported in many locations with this storm system.\nEvent Narrative: Powerlines down Powerlines down", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 37.323 km away, between 2005-04-23 16:38:00 and 2005-04-23 16:38:00. The events included records with measured wind gusts of 34.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A very strong cold front moved across the mid-Atlantic region on April 23, 2005. This front interacted with a moist and unstable airmass to generate significant strong to severe thunderstorms and high winds. Wind damage was reported across portions of central and northern Virginia, and southern and central Maryland, as well as across the Tidal Potomac and upper Chesapeake Bay marine waters. Damaging large hail was also reported in many locations with this storm system.\nEvent Narrative:", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 42.5961 km away, between 2005-05-14 18:33:00 and 2005-05-14 18:33:00. The events included records with estimated wind gusts of 52.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A severe thunderstorm knocked down a couple of trees in Dominion.\nEvent Narrative:", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 34.8012 km away, between 2005-05-28 12:50:00 and 2005-05-28 13:24:00. The events included records with measured wind gusts of 37.5 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: An area of low pressure moved along a stationary front over the coastal waters. Low level moisture combined with strong winds to trigger thunderstorms during the afternoon hours. An area of low pressure moved along a stationary front over the coastal waters. Low level moisture combined with strong winds to trigger thunderstorms during the afternoon hours.\nEvent Narrative: Measured at Martin State Airport observing station.", "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00093721, approximately 23.9355 km away, between 2005-06-06 17:15:00 and 2005-06-06 21:25:00. The events included records with hailstones measuring 45.888888888888886 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: An upper level disturbance, in conjunction with a very warm, moist, and unstable airmass, caused a large outbreak of severe weather. Associated with this event was a large squall line of strong to severe thunderstorms. Damage was reported in portions of the Washington and Baltimore Metropolitan areas. Strong winds also occurred on the maritime waters of the Potomac River and Chesapeake Bay. An upper level disturbance, in conjunction with a very warm, moist, and unstable airmass, caused a large outbreak of severe weather. Associated with this event was a large squall line of strong to severe thunderstorms. Damage was reported in portions of the Washington and Baltimore Metropolitan areas. Strong winds also occurred on the maritime waters of the Potomac River and Chesapeake Bay. An upper level disturbance, in conjunction with a very warm, moist, and unstable airmass, caused a large outbreak of severe weather. Associated with this event was a large squall line of strong to severe thunderstorms. Damage was reported in portions of the Washington and Baltimore Metropolitan areas. Strong winds also occurred on the maritime waters of the Potomac River and Chesapeake Bay. An upper level disturbance, in conjunction with a very warm, moist, and unstable airmass, caused a large outbreak of severe weather. Associated with this event was a large squall line of strong to severe thunderstorms. Damage was reported in portions of the Washington and Baltimore Metropolitan areas. Strong winds also occurred on the maritime waters of the Potomac River and Chesapeake Bay. An upper level disturbance, in conjunction with a very warm, moist, and unstable airmass, caused a large outbreak of severe weather. Associated with this event was a large squall line of strong to severe thunderstorms. Damage was reported in portions of the Washington and Baltimore Metropolitan areas. Strong winds also occurred on the maritime waters of the Potomac River and Chesapeake Bay. An upper level disturbance, in conjunction with a very warm, moist, and unstable airmass, caused a large outbreak of severe weather. Associated with this event was a large squall line of strong to severe thunderstorms. Damage was reported in portions of the Washington and Baltimore Metropolitan areas. Strong winds also occurred on the maritime waters of the Potomac River and Chesapeake Bay. An upper level disturbance, in conjunction with a very warm, moist, and unstable airmass, caused a large outbreak of severe weather. Associated with this event was a large squall line of strong to severe thunderstorms. Damage was reported in portions of the Washington and Baltimore Metropolitan areas. Strong winds also occurred on the maritime waters of the Potomac River and Chesapeake Bay. An upper level disturbance, in conjunction with a very warm, moist, and unstable airmass, caused a large outbreak of severe weather. Associated with this event was a large squall line of strong to severe thunderstorms. Damage was reported in portions of the Washington and Baltimore Metropolitan areas. Strong winds also occurred on the maritime waters of the Potomac River and Chesapeake Bay. An upper level disturbance, in conjunction with a very warm, moist, and unstable airmass, caused a large outbreak of severe weather. Associated with this event was a large squall line of strong to severe thunderstorms. Damage was reported in portions of the Washington and Baltimore Metropolitan areas. Strong winds also occurred on the maritime waters of the Potomac River and Chesapeake Bay.\nEvent Narrative: Powerlines downed near Johns Hopkins University. Tree down Several large limbs down Trees and powerlines down Trees down on Loch Raven Road Powerlines down Trees down Six trees down Power outages occurred and small limbs were downed as well.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 24.9529 km away, between 2005-06-06 18:05:00 and 2005-06-06 22:42:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: An upper level disturbance, in conjunction with a very warm, moist, and unstable airmass, caused a large outbreak of severe weather. Associated with this event was a large squall line of strong to severe thunderstorms. Damage was reported in portions of the Washington and Baltimore Metropolitan areas. Strong winds also occurred on the maritime waters of the Potomac River and Chesapeake Bay. An upper level disturbance, in conjunction with a very warm, moist, and unstable airmass, caused a large outbreak of severe weather. Associated with this event was a large squall line of strong to severe thunderstorms. Damage was reported in portions of the Washington and Baltimore Metropolitan areas. Strong winds also occurred on the maritime waters of the Potomac River and Chesapeake Bay. An upper level disturbance, in conjunction with a very warm, moist, and unstable airmass, caused a large outbreak of severe weather. Associated with this event was a large squall line of strong to severe thunderstorms. Damage was reported in portions of the Washington and Baltimore Metropolitan areas. Strong winds also occurred on the maritime waters of the Potomac River and Chesapeake Bay.\nEvent Narrative: Measured at Thomas Point Light Strong winds were measured at Hart-Millers Island, Glen Burnie, and Tolchester Beach.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 39.1304 km away, between 2005-06-06 18:55:00 and 2005-06-06 18:55:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A severe thunderstorm knocked down a couple of trees and large limbs and caused power outages in and around Rock Hall.\nEvent Narrative:", "The following events were reported: Flash Flood. These occurred near station USW00093721, approximately 37.4324 km away, between 2005-06-09 18:25:00 and 2005-06-09 19:00:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: \nEvent Narrative: A strong thunderstorm caused flash flooding and a water rescue at the intersection of Florence Road and Shaffersville Road along Cabin Branch. Other roads were reported closed near the town of Lisbon.", "The following events were reported: Flash Flood, Thunderstorm Wind. These occurred near station USW00093721, approximately 23.9156 km away, between 2005-06-28 15:00:00 and 2005-06-28 18:30:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: With a tropical airmass in place, strong to severe thunderstorms occurred. These thunderstorms produced damaging wind gusts and heavy rainfall across a large portion of the Mid-Appalachian and Mid-Atlantic regions. With a tropical airmass in place, strong to severe thunderstorms occurred. These thunderstorms produced damaging wind gusts and heavy rainfall across a large portion of the Mid-Appalachian and Mid-Atlantic regions. With a tropical airmass in place, strong to severe thunderstorms occurred. These thunderstorms produced damaging wind gusts and heavy rainfall across a large portion of the Mid-Appalachian and Mid-Atlantic regions. With a tropical airmass in place, strong to severe thunderstorms occurred. These thunderstorms produced damaging wind gusts and heavy rainfall across a large portion of the Mid-Appalachian and Mid-Atlantic regions.\nEvent Narrative: Trees and powerwires down in the eastern portion of Carroll county Water flooded a vehicle up to the hood Trees were reported down in the northwestern portion of Baltimore City. There were several reports of powerwires down.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 33.5678 km away, between 2005-06-28 16:15:00 and 2005-06-28 17:00:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A stagnant airmass was in place, allowing for abundant moisture and instability to help generate heavy rainfall-producing strong to severe thunderstorms. A weak upper level disturbance also helped to kick off the activity. A stagnant airmass was in place, allowing for abundant moisture and instability to help generate heavy rainfall-producing strong to severe thunderstorms. A weak upper level disturbance also helped to kick off the activity.\nEvent Narrative: Trees down; also in the southern portion of the county Trees down", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 6.9534 km away, between 2005-06-29 17:52:00 and 2005-06-29 17:52:00. The events included records with measured wind gusts of 34.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A stagnant airmass was in place, allowing for abundant moisture and instability to help generate heavy rainfall-producing strong to severe thunderstorms. A weak upper level disturbance also helped to kick off the activity.\nEvent Narrative: A wind gust associated with the thunderstorms was measured at Baltimore Washington International Airport.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 21.0841 km away, between 2005-07-05 17:10:00 and 2005-07-05 17:10:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Scattered showers and thunderstorms developed ahead of an approaching cold front. Several reports were received of significant property damage due to these storms.\nEvent Narrative: Power lines were downed in Bowie.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 40.2538 km away, between 2005-07-05 17:38:00 and 2005-07-05 23:06:00. The events included records with measured wind gusts of 34.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Scattered showers and thunderstorms developed ahead of an approaching cold front. Several reports were received of significant property damage due to these storms. Scattered showers and thunderstorms developed ahead of an approaching cold front. Several reports were received of significant property damage due to these storms.\nEvent Narrative: Measured at Thomas Point Marine Station", "The following events were reported: Flash Flood, Flood, Thunderstorm Wind. These occurred near station USW00093721, approximately 35.3107 km away, between 2005-07-07 15:15:00 and 2005-07-08 09:00:00. The flood was caused by . Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: The remnants of Tropical Storm Cindy moved across the Mid Atlantic on Thursday and Friday, July 7 and July 8. The primary hazardous conditions that developed were from the torrential rainfall associated with this storm. Additionally, there were isolated reports of damage due to severe thunderstorm activity. The remnants of Tropical Storm Cindy moved across the Mid Atlantic on Thursday and Friday, July 7 and July 8. The primary hazardous conditions that developed were from the torrential rainfall associated with this storm. Additionally, there were isolated reports of damage due to severe thunderstorm activity. The remnants of Tropical Storm Cindy moved across the Mid Atlantic on Thursday and Friday, July 7 and July 8. The primary hazardous conditions that developed were from the torrential rainfall associated with this storm. Additionally, there were isolated reports of damage due to severe thunderstorm activity.\nEvent Narrative: Roads were under water. In Cockeysville, MD, there was scattered tree damage and trees were downed. There were also funnel cloud reports from the public, and unconfirmed reports of a tornado, but a survey by NWS officials found no evidence of a tornado. Big Pipe Creek flooded its banks, and flooding was also reported in Union Mills, Maryland. High water was reported on roughly a half dozen roads. Flooding and road closures were also reported in Pleasant Valley, Manchester, and Lineboro, Maryland. Two teenagers were injured when the Nissan vehicle they were riding in skidded on a slick roadway and struck a tree. This accident occurred in Sykesville, Maryland. The injured occupants were both treated at a local hospital.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 37.323 km away, between 2005-07-13 18:22:00 and 2005-07-13 18:22:00. The events included records with estimated wind gusts of 34.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Several frontal boundaries were draped across the mid-Atlantic during this period. These fronts provided a focus for the development of thunderstorms across central Virginia and western Maryland.\nEvent Narrative:", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 27.9423 km away, between 2005-07-16 17:00:00 and 2005-07-16 17:00:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A moist, tropical airmass led to the development of some thunderstorms across Lower Southern Maryland. Torrential rainfall caused several reports of road closures. Damaged trees and utility poles were also reported.\nEvent Narrative: Tree and power line damage was reported in the area. Reports indicated more than 10,000 power outages at one time.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 40.2538 km away, between 2005-07-25 04:43:00 and 2005-07-25 18:48:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: An overnight thunderstorm complex moved through the mid-Atlantic. This system caused a few strong to severe thunderstorms during the early morning. An overnight thunderstorm complex moved through the mid-Atlantic. This system caused a few strong to severe thunderstorms during the early morning.\nEvent Narrative: Wind estimated based on report from Tolchester Beach. Wind gust was measured at the Thomas Point Marine Station.", "The following events were reported: Lightning, Thunderstorm Wind. These occurred near station USW00093721, approximately 20.3829 km away, between 2005-07-27 17:25:00 and 2005-07-27 18:00:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front moved through the region during the late afternoon and evening. This cold front, combined with moist and unstable conditions, triggered widespread showers and storms across the region. The strongest of these storms downed trees and powerlines, as well as producing very large hail. Intense lightning caused fires and several personal injuries. Torrential rainfall flooded a few areas, and was also responsible for sweeping away a young boy. Damage estimates by print media were in the hundreds of thousands, possibly more. A cold front moved through the region during the late afternoon and evening. This cold front, combined with moist and unstable conditions, triggered widespread showers and storms across the region. The strongest of these storms downed trees and powerlines, as well as producing very large hail. Intense lightning caused fires and several personal injuries. Torrential rainfall flooded a few areas, and was also responsible for sweeping away a young boy. Damage estimates by print media were in the hundreds of thousands, possibly more. A cold front moved through the region during the late afternoon and evening. This cold front, combined with moist and unstable conditions, triggered widespread showers and storms across the region. The strongest of these storms downed trees and powerlines, as well as producing very large hail. Intense lightning caused fires and several personal injuries. Torrential rainfall flooded a few areas, and was also responsible for sweeping away a young boy. Damage estimates by print media were in the hundreds of thousands, possibly more. A cold front moved through the region during the late afternoon and evening. This cold front, combined with moist and unstable conditions, triggered widespread showers and storms across the region. The strongest of these storms downed trees and powerlines, as well as producing very large hail. Intense lightning caused fires and several personal injuries. Torrential rainfall flooded a few areas, and was also responsible for sweeping away a young boy. Damage estimates by print media were in the hundreds of thousands, possibly more. A cold front moved through the region during the late afternoon and evening. This cold front, combined with moist and unstable conditions, triggered widespread showers and storms across the region. The strongest of these storms downed trees and powerlines, as well as producing very large hail. Intense lightning caused fires and several personal injuries. Torrential rainfall flooded a few areas, and was also responsible for sweeping away a young boy. Damage estimates by print media were in the hundreds of thousands, possibly more.\nEvent Narrative: Lightning ignited a few fires in the city and damaged the chimney of a local civic organization. Numerous trees were downed near Hickory, Maryland. Trees and power lines were downed countywide. Also, a tree landed on a car located on Chestnut Hill Road. Trees were downed in Woodlawn and Parkville. A tree fell on a power line on Marston Road which is located near New Windsor. Another tree was downed on Sandymouth Road, which is located north of Maryland State Route 140. This information was compiled through local print media information. Trees and powerlines downed at several locations.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 40.2538 km away, between 2005-07-27 17:39:00 and 2005-07-27 18:15:00. The events included records with measured wind gusts of 47.5 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front moved through the region during the late afternoon and evening. This cold front, combined with moist and unstable conditions, triggered widespread showers and storms across the region. The strongest of these storms downed trees and powerlines, and also produced large hail. Intense lightning caused fires and several personal injuries. Torrential rainfall flooded a few areas, and was also responsible for flooding which swept away a young boy. A cold front moved through the region during the late afternoon and evening. This cold front, combined with moist and unstable conditions, triggered widespread showers and storms across the region. The strongest of these storms downed trees and powerlines, and also produced large hail. Intense lightning caused fires and several personal injuries. Torrential rainfall flooded a few areas, and was also responsible for flooding which swept away a young boy.\nEvent Narrative: Confirmed wind gust measured at the Thomas Point Marine Station. The strongest winds were reported at Baltimore/Washington International Airport, however, strong wind gusts also occurred during the period at Tolchester, FSK Bridge, and Hart-Millers Island.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 38.1139 km away, between 2005-07-27 18:15:00 and 2005-07-27 18:15:00. The events included records with measured wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A Skywarn spotter measured a wind gust to 58 mph in Stevensville. The severe thunderstorm sheared the tops from several oak trees.\nEvent Narrative:", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 26.8063 km away, between 2005-08-05 15:35:00 and 2005-08-05 19:10:00. The events included records with measured wind gusts of 40.333333333333336 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A weak cold front moved east from the Appalachian Mountains and interacted with the moist and unstable airmass that was already in place around the mid-Atlantic. This situation sparked off scattered thunderstorms during the afternoon and evening. A few of these thunderstorms reached severe criteria. The principal hazard associated with these storms was damaging wind gusts. Additionally, a few of the storms generated large hail. A weak cold front moved east from the Appalachian Mountains and interacted with the moist and unstable airmass that was already in place around the mid-Atlantic. This situation sparked off scattered thunderstorms during the afternoon and evening. A few of these thunderstorms reached severe criteria. The principal hazard associated with these storms was damaging wind gusts. Additionally, a few of the storms generated large hail. A weak cold front moved east from the Appalachian Mountains and interacted with the moist and unstable airmass that was already in place around the mid-Atlantic. This situation sparked off scattered thunderstorms during the afternoon and evening. A few of these thunderstorms reached severe criteria. The principal hazard associated with these storms was damaging wind gusts. Additionally, a few of the storms generated large hail.\nEvent Narrative: Wind gust measured at Baltimore/Washington Airport. Wind gust measured at Kent Island. Wind gust measured at Kent Island.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 38.1139 km away, between 2005-08-05 19:17:00 and 2005-08-05 19:32:00. The events included records with estimated wind gusts of 52.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A severe thunderstorm knocked down several trees and wires in Queen Anne's County from Kent Island eastward through Grasonville. About 3,300 homes and businesses lost power.\nEvent Narrative:", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 41.8265 km away, between 2005-08-07 10:30:00 and 2005-08-07 10:30:00. The events included records with estimated wind gusts of 52.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A severe thunderstorm knocked down a couple of trees in Kent County between Rock Hall and Fairlee.\nEvent Narrative:", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 27.3815 km away, between 2005-08-08 14:25:00 and 2005-08-08 18:06:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 10000.0 and crop damage of 0.0. \n\nEpisode Narrative: For the fourth day in a row, a stalled frontal boundary helped to produce scattered afternoon thunderstorms in the mid-Atlantic. In addition, the level of moisture in the atmosphere on this day was quite high, and allowed a few thunderstorms to produce torrential rainfall amounts, and some reports of flooding. There were also a few thunderstorms that reached severe limits, primarily causing some thunderstorm wind damage reports. Finally, in part due to a difference in winds just above the surface of the Earth, there was a report of a waterspout in the middle Chesapeake Bay. This waterspout was not reported to have come ashore. For the fourth day in a row, a stalled frontal boundary helped to produce scattered afternoon thunderstorms in the mid-Atlantic. In addition, the level of moisture in the atmosphere on this day was quite high, and allowed a few thunderstorms to produce torrential rainfall amounts, and some reports of flooding. There were also a few thunderstorms that reached severe limits, primarily causing some thunderstorm wind damage reports. Finally, in part due to a difference in winds just above the surface of the Earth, there was a report of a waterspout in the middle Chesapeake Bay. This waterspout was not reported to have come ashore. For the fourth day in a row, a stalled frontal boundary helped to produce scattered afternoon thunderstorms in the mid-Atlantic. In addition, the level of moisture in the atmosphere on this day was quite high, and allowed a few thunderstorms to produce torrential rainfall amounts, and some reports of flooding. There were also a few thunderstorms that reached severe limits, primarily causing some thunderstorm wind damage reports. Finally, in part due to a difference in winds just above the surface of the Earth, there was a report of a waterspout in the middle Chesapeake Bay. This waterspout was not reported to have come ashore.\nEvent Narrative: Trees and powerlines downed. Trees down. Trees downed.", "The following events were reported: Waterspout. These occurred near station USW00093721, approximately 23.2478 km away, between 2005-08-27 09:25:00 and 2005-08-27 09:35:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: The weather pattern across the mid-Atlantic was fairly complex on August 27. Hurricane Katrina had not yet come ashore in the Gulf Coast area, however the larger wind circulations from the hurricane were causing warm and moist southerly winds to impact the mid-Atlantic. This flow pattern allowed a few thunderstorms to develop and cause torrential rainfall and a few reports of flooding. In addition, the wind flow just above the ground was such that a persistent waterspout formed near Baltimore in the Chesapeake Bay. There may have been other waterspouts form, however there were no additional reports of waterspouts received at the National Weather Service office in Sterling.\nEvent Narrative: The waterspout was associated with gusty showers moving through the area at the time. The waterspout formed near the entrance to Middle River in the Chesapeake Bay, and then moved north to near Carroll Island, before quickly dissipating. There were no reports that the waterspout moved onshore.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 43.1846 km away, between 2005-11-06 20:36:00 and 2005-11-06 20:36:00. The events included records with measured wind gusts of 35.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: \nEvent Narrative: Winds were measured at Tolchester Beach station. Slightly lower winds of 29 knots were also measured at the Francis Scott Key Bridge.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 23.0746 km away, between 2005-11-16 16:15:00 and 2005-11-16 16:15:00. The events included records with measured wind gusts of 34.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: \nEvent Narrative:", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 37.323 km away, between 2006-01-14 03:43:00 and 2006-01-14 03:43:00. The events included records with estimated wind gusts of 34.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: \nEvent Narrative:", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 25.5085 km away, between 2006-01-24 22:00:00 and 2006-01-24 23:05:00. The events included records with measured wind gusts of 41.5 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: \nEvent Narrative:", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 46.7686 km away, between 2006-02-04 20:00:00 and 2006-02-04 20:00:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 10000.0 and crop damage of 0.0. \n\nEpisode Narrative: Newspaper reports indicated significant damage to a log house near Libertytown in Frederick County, which occurred during the evening. A large old oak tree was downed, as well as a few other smaller trees. Trees and powerlines were also downed near Ridgeville and Westminster.\nEvent Narrative:", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 30.1988 km away, between 2006-02-04 20:41:00 and 2006-02-04 20:51:00. The events included records with estimated wind gusts of 34.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: \nEvent Narrative:", "The following events were reported: Hail. These occurred near station USW00093721, approximately 24.6137 km away, between 2006-04-03 18:15:00 and 2006-04-03 19:31:00. The events included records with hailstones measuring 0.8181818181818182 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front combined with strong instability to cause numerous severe thunderstorms to occur on April 3 across the Mid Atlantic. The majority of the severe weather reports were from large hail and damaging wind gusts. A cold front combined with strong instability to cause numerous severe thunderstorms to occur on April 3 across the Mid Atlantic. The majority of the severe weather reports were from large hail and damaging wind gusts. A cold front combined with strong instability to cause numerous severe thunderstorms to occur on April 3 across the Mid Atlantic. The majority of the severe weather reports were from large hail and damaging wind gusts. A cold front combined with strong instability to cause numerous severe thunderstorms to occur on April 3 across the Mid Atlantic. The majority of the severe weather reports were from large hail and damaging wind gusts. A cold front combined with strong instability to cause numerous severe thunderstorms to occur on April 3 across the Mid Atlantic. The majority of the severe weather reports were from large hail and damaging wind gusts. A cold front combined with strong instability to cause numerous severe thunderstorms to occur on April 3 across the Mid Atlantic. The majority of the severe weather reports were from large hail and damaging wind gusts. A cold front combined with strong instability to cause numerous severe thunderstorms to occur on April 3 across the Mid Atlantic. The majority of the severe weather reports were from large hail and damaging wind gusts. A cold front combined with strong instability to cause numerous severe thunderstorms to occur on April 3 across the Mid Atlantic. The majority of the severe weather reports were from large hail and damaging wind gusts. A cold front combined with strong instability to cause numerous severe thunderstorms to occur on April 3 across the Mid Atlantic. The majority of the severe weather reports were from large hail and damaging wind gusts. A cold front combined with strong instability to cause numerous severe thunderstorms to occur on April 3 across the Mid Atlantic. The majority of the severe weather reports were from large hail and damaging wind gusts. A cold front combined with strong instability to cause numerous severe thunderstorms to occur on April 3 across the Mid Atlantic. The majority of the severe weather reports were from large hail and damaging wind gusts.\nEvent Narrative: Penny-sized hail report from Pikesville Hail lasted for 6 minutes", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 40.2538 km away, between 2006-04-03 19:12:00 and 2006-04-03 19:24:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front combined with strong instability to cause numerous severe thunderstorms to occur on April 3 across the Mid Atlantic. The majority of the severe weather reports were from large hail and damaging wind gusts. A cold front combined with strong instability to cause numerous severe thunderstorms to occur on April 3 across the Mid Atlantic. The majority of the severe weather reports were from large hail and damaging wind gusts.\nEvent Narrative: Measured at Thomas Point Light", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 25.7173 km away, between 2006-04-05 06:41:00 and 2006-04-05 10:48:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A fast moving upper level disturbance caused rain and snow squalls, containing thunder and lightning, to drop quickly from Pennsylvania south into central and eastern Maryland, early in the morning of April 5. Strong winds occurred on the tidal waters of the Chesapeake Bay and Tidal Potomac River in conjunction with these squalls. A fast moving upper level disturbance caused rain and snow squalls, containing thunder and lightning, to drop quickly from Pennsylvania south into central and eastern Maryland, early in the morning of April 5. Strong winds occurred on the tidal waters of the Chesapeake Bay and Tidal Potomac River in conjunction with these squalls. A fast moving upper level disturbance caused rain and snow squalls, containing thunder and lightning, to drop quickly from Pennsylvania south into central and eastern Maryland, early in the morning of April 5. Strong winds occurred on the tidal waters of the Chesapeake Bay and Tidal Potomac River in conjunction with these squalls. A fast moving upper level disturbance caused rain and snow squalls, containing thunder and lightning, to drop quickly from Pennsylvania south into central and eastern Maryland, early in the morning of April 5. Strong winds occurred on the tidal waters of the Chesapeake Bay and Tidal Potomac River in conjunction with these squalls. A fast moving upper level disturbance caused rain and snow squalls, containing thunder and lightning, to drop quickly from Pennsylvania south into central and eastern Maryland, early in the morning of April 5. Strong winds occurred on the tidal waters of the Chesapeake Bay and Tidal Potomac River in conjunction with these squalls.\nEvent Narrative: Measured at Annapolis Automated Station (KNAK) Max wind gust of 52 knots was measured at Tolchester Beach Max wind gust of 46 knots was measured at Thomas Point Light", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 26.8942 km away, between 2006-04-05 08:50:00 and 2006-04-05 08:50:00. The events included records with measured wind gusts of 51.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A fast moving upper level disturbance caused rain and snow squalls, containing thunder and lightning, to drop quickly from Pennsylvania south into central and eastern Maryland, early in the morning of April 5. Damaging wind gusts occurred in conjunction with these squalls.\nEvent Narrative: Wind gust was measured at Martin-State Airport during a heavy snow squall.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 21.8829 km away, between 2006-04-07 20:39:00 and 2006-04-07 20:42:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Ahead of a cold front, the airmass was warm and unstable, and conducive to shower and thunderstorm development. With strong winds aloft, a few thunderstorms reached severe criteria, producing damaging wind gusts across portions of the area. Ahead of a cold front, the airmass was warm and unstable, and conducive to shower and thunderstorm development. With strong winds aloft, a few thunderstorms reached severe criteria, producing damaging wind gusts across portions of the area.\nEvent Narrative: Measured at Thomas Point Light", "The following events were reported: Flash Flood. These occurred near station USW00093721, approximately 14.3633 km away, between 2006-04-22 19:30:00 and 2006-04-22 20:00:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: High moisture content and relatively light winds created prime conditions for flash flooding to occur with rain and thunderstorms on the evening of April 22. There were several reports of flooding and flash flooding due to the heavy rainfall across portions of the region.\nEvent Narrative: Flooded roads and one road closure in the northwest part of the county, including the town of Catonsville.", "The following events were reported: Marine Hail, Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 29.4723 km away, between 2006-04-23 20:18:00 and 2006-04-24 23:59:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Strong thunderstorms were capable of producing very large hail during the late evening of April 23, due to very cold air aloft in the atmosphere. Severe criteria large hail reports were received from areas near Baltimore, Maryland, including the adjacent waters of the Chesapeake Bay. Strong thunderstorms were capable of producing very large hail during the late evening of April 23, due to very cold air aloft in the atmosphere. Severe criteria large hail reports were received from areas near Baltimore, Maryland, including the adjacent waters of the Chesapeake Bay.\nEvent Narrative:", "The following events were reported: Hail. These occurred near station USW00093721, approximately 26.8165 km away, between 2006-04-23 20:18:00 and 2006-04-23 23:59:00. The events included records with hailstones measuring 0.976 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Strong thunderstorms were capable of producing very large hail during the late evening of April 23, due to very cold air aloft in the atmosphere. Severe criteria large hail reports were received from areas near Baltimore, Maryland, including the adjacent waters of the Chesapeake Bay. Later that evening, wet grounds contributed to the development of areas of dense fog, mainly in the Washington and Baltimore region. Strong thunderstorms were capable of producing very large hail during the late evening of April 23, due to very cold air aloft in the atmosphere. Severe criteria large hail reports were received from areas near Baltimore, Maryland, including the adjacent waters of the Chesapeake Bay. Later that evening, wet grounds contributed to the development of areas of dense fog, mainly in the Washington and Baltimore region. Strong thunderstorms were capable of producing very large hail during the late evening of April 23, due to very cold air aloft in the atmosphere. Severe criteria large hail reports were received from areas near Baltimore, Maryland, including the adjacent waters of the Chesapeake Bay. Later that evening, wet grounds contributed to the development of areas of dense fog, mainly in the Washington and Baltimore region. Strong thunderstorms were capable of producing very large hail during the late evening of April 23, due to very cold air aloft in the atmosphere. Severe criteria large hail reports were received from areas near Baltimore, Maryland, including the adjacent waters of the Chesapeake Bay. Later that evening, wet grounds contributed to the development of areas of dense fog, mainly in the Washington and Baltimore region. Strong thunderstorms were capable of producing very large hail during the late evening of April 23, due to very cold air aloft in the atmosphere. Severe criteria large hail reports were received from areas near Baltimore, Maryland, including the adjacent waters of the Chesapeake Bay. Later that evening, wet grounds contributed to the development of areas of dense fog, mainly in the Washington and Baltimore region.\nEvent Narrative: Quarter-sized hail reported near Columbia Ping-pong ball sized hail Reported near Bowley Bar Nickel sized hail reported at junction of MD route 152 and Interstate 95.", "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00093721, approximately 20.3464 km away, between 2006-06-01 18:10:00 and 2006-06-01 18:30:00. The events included records with hailstones measuring 33.626666666666665 inches.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 45000.0 and crop damage of 0.0. \n\nEpisode Narrative: A trough of low pressure was draped across the Mid Atlantic on June 1. This feature combined with high moisture content and instability in the atmosphere to promote scattered strong to severe thunderstorms. The thunderstorms first developed across the higher terrain of the Appalachian Mountains, then moved east across the Washington/Baltimore corridor. A trough of low pressure was draped across the Mid Atlantic on June 1. This feature combined with high moisture content and instability in the atmosphere to promote scattered strong to severe thunderstorms. The thunderstorms first developed across the higher terrain of the Appalachian Mountains, then moved east across the Washington/Baltimore corridor. A trough of low pressure was draped across the Mid Atlantic on June 1. This feature combined with high moisture content and instability in the atmosphere to promote scattered strong to severe thunderstorms. The thunderstorms first developed across the higher terrain of the Appalachian Mountains, then moved east across the Washington/Baltimore corridor.\nEvent Narrative: Trees downed on the east side of the city. Numerous trees were downed. A trained spotter reported nickel sized hail on Belair Road near Interstate 695.", "The following events were reported: Hail. These occurred near station USW00093721, approximately 47.6344 km away, between 2006-06-09 12:00:00 and 2006-06-09 12:00:00. The events included records with hailstones measuring 0.88 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Daytime heating combined with an unstable lower atmosphere and favorable amounts of moisture contributed to scattered afternoon and evening thunderstorms. A few of these storms reached severe limits with large hail and damaging wind gusts.\nEvent Narrative: Nickel sized hail was reported.", "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00093721, approximately 28.9336 km away, between 2006-07-02 17:28:00 and 2006-07-02 18:30:00. The events included records with hailstones measuring 37.0 inches.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 1510000.0 and crop damage of 0.0. \n\nEpisode Narrative: A frontal boundary sagged south into the Mid Atlantic on July 2, and combined with very strong daytime heating and instability, contributed to scattered severe thunderstorm activity. Much of the state of Maryland experienced damages from the severe thunderstorms. The worst damages occurred in the Wheaton area of Montgomery County, and also in the Cape St. Claire section of Anne Arundel County. NWS site surveys of the damages confirmed the damages were caused by straight line winds. A buoy just 5 miles from Annapolis in the Chesapeake Bay measured winds of 69 mph with these storms. Extensive property damage occurred, including numerous downed trees and powerlines. Newspaper reports indicated in excess of 100,000 customers without power in the Washington Metro Region. A frontal boundary sagged south into the Mid Atlantic on July 2, and combined with very strong daytime heating and instability, contributed to scattered severe thunderstorm activity. Much of the state of Maryland experienced damages from the severe thunderstorms. The worst damages occurred in the Wheaton area of Montgomery County, and also in the Cape St. Claire section of Anne Arundel County. NWS site surveys of the damages confirmed the damages were caused by straight line winds. A buoy just 5 miles from Annapolis in the Chesapeake Bay measured winds of 69 mph with these storms. Extensive property damage occurred, including numerous downed trees and powerlines. Newspaper reports indicated in excess of 100,000 customers without power in the Washington Metro Region. A frontal boundary sagged south into the Mid Atlantic on July 2, and combined with very strong daytime heating and instability, contributed to scattered severe thunderstorm activity. Much of the state of Maryland experienced damages from the severe thunderstorms. The worst damages occurred in the Wheaton area of Montgomery County, and also in the Cape St. Claire section of Anne Arundel County. NWS site surveys of the damages confirmed the damages were caused by straight line winds. A buoy just 5 miles from Annapolis in the Chesapeake Bay measured winds of 69 mph with these storms. Extensive property damage occurred, including numerous downed trees and powerlines. Newspaper reports indicated in excess of 100,000 customers without power in the Washington Metro Region.\nEvent Narrative: Extensive property damage occurred in the Cape St. Claire area due to straight-line wind damages. Two houses were extensively damaged and a van was also damaged. Numerous trees and powerlines were downed due to the severe thunderstorms. Several very large trees were also downed, including as a 125 foot red oak tree which was uprooted by the severe winds. Trees downed. Quarter-sized hail occurred.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 38.1139 km away, between 2006-07-02 17:40:00 and 2006-07-02 17:40:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A severe thunderstorm knocked down large tree limbs and wires on Kent Island. About 1,000 residents lost power.\nEvent Narrative:", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 36.4935 km away, between 2006-07-04 14:20:00 and 2006-07-04 16:35:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 285000.0 and crop damage of 0.0. \n\nEpisode Narrative: Scattered severe thunderstorms developed on July 4 due to an approaching cold front and a very unstable airmass residing over the Mid-Atlantic. The severe storms formed along the Blue Ridge Mountains and moved east into the Washington and Baltimore suburbs during the evening. The hardest hit areas included a large portion of Prince Georges County in suburban Washington, and a section of Annapolis that experienced extensive tree damages. Many 4th of July festivities were affected by this bout of severe weather. Scattered severe thunderstorms developed on July 4 due to an approaching cold front and a very unstable airmass residing over the Mid-Atlantic. The severe storms formed along the Blue Ridge Mountains and moved east into the Washington and Baltimore suburbs during the evening. The hardest hit areas included a large portion of Prince Georges County in suburban Washington, and a section of Annapolis that experienced extensive tree damages. Many 4th of July festivities were affected by this bout of severe weather. Scattered severe thunderstorms developed on July 4 due to an approaching cold front and a very unstable airmass residing over the Mid-Atlantic. The severe storms formed along the Blue Ridge Mountains and moved east into the Washington and Baltimore suburbs during the evening. The hardest hit areas included a large portion of Prince Georges County in suburban Washington, and a section of Annapolis that experienced extensive tree damages. Many 4th of July festivities were affected by this bout of severe weather.\nEvent Narrative: 20 to 30 trees were downed on houses in Annapolis. Tree downed which knocked out power to 35 homes. Tree downed on a vehicle passing by on Interstate 83 north of Baltimore City.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 47.3914 km away, between 2006-07-04 17:00:00 and 2006-07-04 17:25:00. The events included records with estimated wind gusts of 52.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A severe thunderstorm knocked down a few trees and wires throughout Queen Anne's County.\nEvent Narrative:", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 39.1304 km away, between 2006-07-12 15:15:00 and 2006-07-12 15:15:00. The events included records with estimated wind gusts of 52.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A severe thunderstorm knocked down a couple of trees and wires in Rock Hall.\nEvent Narrative:", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 38.2844 km away, between 2006-07-18 15:31:00 and 2006-07-18 19:35:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 36000.0 and crop damage of 0.0. \n\nEpisode Narrative: An approaching cold front combined with a very hot and humid airmass to generate severe thunderstorms around much of the Mid Atlantic on July 18. Reports of severe weather were received from the Eastern Panhandle of West Virginia, through the Washington/Baltimore corridor, to the Chesapeake Bay. The most intense of the severe storms occurred in Eastern Panhandle of West Virginia, where the worst damages occurred, and a report of tennis-ball sized hall was also reported. Extensive damages also occurred in the Frederick and Hagerstown areas of Central Maryland due to the severe thunderstorms. An approaching cold front combined with a very hot and humid airmass to generate severe thunderstorms around much of the Mid Atlantic on July 18. Reports of severe weather were received from the Eastern Panhandle of West Virginia, through the Washington/Baltimore corridor, to the Chesapeake Bay. The most intense of the severe storms occurred in Eastern Panhandle of West Virginia, where the worst damages occurred, and a report of tennis-ball sized hall was also reported. Extensive damages also occurred in the Frederick and Hagerstown areas of Central Maryland due to the severe thunderstorms. An approaching cold front combined with a very hot and humid airmass to generate severe thunderstorms around much of the Mid Atlantic on July 18. Reports of severe weather were received from the Eastern Panhandle of West Virginia, through the Washington/Baltimore corridor, to the Chesapeake Bay. The most intense of the severe storms occurred in Eastern Panhandle of West Virginia, where the worst damages occurred, and a report of tennis-ball sized hall was also reported. Extensive damages also occurred in the Frederick and Hagerstown areas of Central Maryland due to the severe thunderstorms.\nEvent Narrative: Trees down along Interstate 68 near Orleans Road. The downed trees blocked the interstate temporarily. Trees and powerlines downed. Powerlines downed.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 39.1304 km away, between 2006-07-18 19:45:00 and 2006-07-18 19:45:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A severe thunderstorm pulled down large tree limbs and wires in Rock Hall.\nEvent Narrative:", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 36.9906 km away, between 2006-08-07 20:30:00 and 2006-08-07 20:30:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 50000.0 and crop damage of 0.0. \n\nEpisode Narrative: Isolated severe thunderstorms occurred in response to a very hot and humid airmass and a passing upper-level disturbance.\nEvent Narrative: Several large trees were downed with property damage to a local church retreat center, where significant roof damage occurred due to the falling trees.", "The following events were reported: Hail, Thunderstorm Wind, Tornado. These occurred near station USW00093721, approximately 28.4296 km away, between 2006-09-28 15:30:00 and 2006-09-28 17:44:00. The events included records with hailstones measuring 40.1875 inches.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 6120000.0 and crop damage of 0.0. \n\nEpisode Narrative: Significant severe thunderstorms occurred on September 28 across the region. A strong cold front moved from the Appalachian Mountains to the Mid Atlantic during the afternoon. The cold front reached to along the Chesapeake Bay around midnight. The most intense thunderstorms occurred along the Interstate 95 corridor, with one confirmed F1 tornado in Anne Arundel County, Maryland. Intense thunderstorm winds also occurred across the tidal waters of the Potomac and Chesapeake. Significant severe thunderstorms occurred on September 28 across the region. A strong cold front moved from the Appalachian Mountains to the Mid Atlantic during the afternoon. The cold front reached to along the Chesapeake Bay around midnight. The most intense thunderstorms occurred along the Interstate 95 corridor, with one confirmed F1 tornado in Anne Arundel County, Maryland. Intense thunderstorm winds also occurred across the tidal waters of the Potomac and Chesapeake. Significant severe thunderstorms occurred on September 28 across the region. A strong cold front moved from the Appalachian Mountains to the Mid Atlantic during the afternoon. The cold front reached to along the Chesapeake Bay around midnight. The most intense thunderstorms occurred along the Interstate 95 corridor, with one confirmed F1 tornado in Anne Arundel County, Maryland. Intense thunderstorm winds also occurred across the tidal waters of the Potomac and Chesapeake. Significant severe thunderstorms occurred on September 28 across the region. A strong cold front moved from the Appalachian Mountains to the Mid Atlantic during the afternoon. The cold front reached to along the Chesapeake Bay around midnight. The most intense thunderstorms occurred along the Interstate 95 corridor, with one confirmed F1 tornado in Anne Arundel County, Maryland. Intense thunderstorm winds also occurred across the tidal waters of the Potomac and Chesapeake. Significant severe thunderstorms occurred on September 28 across the region. A strong cold front moved from the Appalachian Mountains to the Mid Atlantic during the afternoon. The cold front reached to along the Chesapeake Bay around midnight. The most intense thunderstorms occurred along the Interstate 95 corridor, with one confirmed F1 tornado in Anne Arundel County, Maryland. Intense thunderstorm winds also occurred across the tidal waters of the Potomac and Chesapeake.\nEvent Narrative: Measured wind gust by a trained SKYWARN spotter. Significant roof damage also occurred to a home in Bowie. No injuries were reported. Penny sized hail reported near the intersection of John Hanson Highway and Maryland Route 197. Powerlines down. The National Weather Service conducted a storm survey in Severna Park and Pasadena Maryland, rating the tornado an F1 on the Fujita scale of tornado intensity. It was determined that a the tornado touched down in the area of Severna Park about 6:34 pm, and traveled two miles before lifting in Pasadena around 6:44 pm. At its maximum the storm was 250 yards wide with winds of 90 mph. 34 homes were severely damaged by falling trees with 13 of those homes rendered uninhabitable. Initial minor damage was located near the intersection of Ritchie Highway and McKinsey Avenue. A hardware store had its sign blown down and a small tree was downed near the Severna Park Marketplace Shopping Center. A few trees were also downed immediately behind the shopping center along Leelynn Road. The tornado gathered strength as it progressed through West Ridge and towards Cattail Creek off of the Magothy River. Five large hardwood trees of one to two feet in diameter were uprooted, and several others were snapped off along Whittier Parkway. Two of the large trees had fallen through houses. These trees, as most of the trees were in the survey, were blown down nearly perpendicular to the path of the tornado (knocked down towards the west). The tornado then reached its most intense and widest extent as it passed through the community of Lower Magothy Beach. Many of these trees knocked down in this area were large two foot diameter hardwood trees that were 60 to 80 feet tall. Leaf spatter was noted on the sides of homes and vehicles. Slight siding damage was noted on one home. Many wires and telephone poles were knocked down in this area. The width of the tornado at this point was 250 yards. Damage became much more limited as the tornado continued north across Norwich Road and Inverness Road in Riverdale. By the time the storm crossed the Magothy for the final time and traveled over the community of Beachwood Park, only leaf litter and small downed branches were noted. Several trees down.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 39.1304 km away, between 2006-09-28 18:00:00 and 2006-09-28 18:00:00. The events included records with estimated wind gusts of 52.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A severe thunderstorm knocked down some trees and wires in and around Rock Hall. A wind gust to 57 mph was measured at Tolchester Beach at 706 p.m. EDT.\nEvent Narrative:", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 48.2052 km away, between 2006-09-28 18:15:00 and 2006-09-28 18:15:00. The events included records with estimated wind gusts of 52.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A severe thunderstorm knocked down trees and wires near and along the Chester River. The same storm also knocked down smaller tree branches when it passed across Kent Island.\nEvent Narrative:", "The following events were reported: Flash Flood, Flood, Thunderstorm Wind. These occurred near station USW00093721, approximately 25.5763 km away, between 2006-11-16 13:20:00 and 2006-11-17 01:30:00. The flood was caused by Heavy Rain. Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A deep low pressure system moved from the Tennessee Valley to the eastern great Lakes on November 16, sweeping a strong cold front across the Mid Atlantic. This system brought widespread moderate to heavy rain to the region after sunrise, then strong thunderstorms during the early afternoon. These thunderstorms produced periods of heavier rainfall as well as gusty and isolated damaging winds. Although rain ended across the region during the mid afternoon hours, some locations continued to experience flooding until just after midnight.|Heavy rain across Anne Arundel County closed numerous roadways from the early afternoon until after midnight on November 17th. Some of these roads include Governor Bridge Road and Saint George Barber, Routes 10 and 648 (Baltimore-Annapolis Blvd.) and Burns Crossing Road at Severn Run in the town of Severn. Maryland Route 176 (Dorsey Road) and 648 (Baltimore-Annapolis Blvd) continued to be submerged in about two feet of water until after midnight. |Flash Flooding was reported in Baltimore County and the City of Baltimore. Gunpowder River rose out of its banks, allowing water to flow over the bridge at Second Mine Road. Flash flooding was also reported at Hydes Road and Long Green Pike as well as near White Hall and Gunpowder Falls State Park. Numerous roads were closed across Baltimore County, including a portion of Pulaski Highway (Route 40). Several roads in the City of Baltimore were also closed due to flash flooding. Jones Falls flooded the bridge at Interstate 83 and 41st Street. Other roadways affected by flash flooding include Erdman Avenue on the east side of the city and Caroline and Fleet Streets near downtown.|In Carroll County, water up to 2 feet deep across Twin Arch Road. An elderly woman became trapped in her car in Sykesville on River Road on the Howard/Carroll County line where the South branch of the Patapsco River rose our of its banks. The South Branch of the Patapsco River also rose out of it's banks onto Old Frederick Road, about 5 miles west of Woodbine. Route 32 was closed due to flooding near Sykesville. Numerous roads closed due to flooding near Keymar.|Numerous roads were closed across Charles County, especially near La Plata, Port Tobacco, Bryans Road and Waldorf. One roadway closed due to flooding include Billingsley Road between White Plains and Bryans Roads. Buses were forced to return students to school due to flooded roadways. |In Harford County, Deer Creek was out of its banks near Norrisville, causing localized flooding of some subdivision. High water on was reported on roads near Bel Air, with several water rescues of stranded motorists. Two water rescues were conducted near the intersection of Walters Mill and Ady Roads near Bel Air.|Thunderstorms brought damaging winds to Montgomery County between 1:00 PM and 2:00 PM, downing trees and power lines in Woodhaven, Gaithersburg, Layhill, Silver Spring and Bowie. A tree was downed on the Penn Line by a thunderstorm in Bowie. Heavy rain with these thunderstorms produced flooding that continued through early evening across Montgomery County. The Northwest Branch rose out of its banks at Route 29. Water covered Old Georgetown Road and Battery Lane near Huntington, MD. More than a dozen water rescues occurred across the county when people became trapped in their cars when trying to cross a flooded roadway. One such rescue was conducted in Germantown along Game Preserve Road.|In Prince George\ufffd\ufffd\ufffds County, Routes 301 and 5 were flooded. Several roads were closed near Andrews Air Force Base due to flooding, including a section of the Interstate 495 Capital Beltway. A farm equipment store was inundated by water in Upper Marlboro, MD.|In St. Mary\ufffd\ufffd\ufffds County, Route 235 and Saint John Road flooded in St. Mary\ufffd\ufffd\ufffds City, MD.|Tidal flooding occurred during the afternoon and early evening around the time of high tide in Baltimore. Strong onshore winds occurred due to a coastal low pressure system. Flooding of tidal areas and along the shoreline occurred in several communities, including Bowley Bar, Bowley Quarters, Millers Island and near Middle River. Twelve to 18 inches of water was reported to cover roadways in Millers Island and near Bowleys Quarters. Water approached some houses during high tide. There was also some coastal flooding at the Harborplace shopping facilities located at the Baltimore Inner Harbor. A deep low pressure system moved from the Tennessee Valley to the eastern great Lakes on November 16, sweeping a strong cold front across the Mid Atlantic. This system brought widespread moderate to heavy rain to the region after sunrise, then strong thunderstorms during the early afternoon. These thunderstorms produced periods of heavier rainfall as well as gusty and isolated damaging winds. Although rain ended across the region during the mid afternoon hours, some locations continued to experience flooding until just after midnight.|Heavy rain across Anne Arundel County closed numerous roadways from the early afternoon until after midnight on November 17th. Some of these roads include Governor Bridge Road and Saint George Barber, Routes 10 and 648 (Baltimore-Annapolis Blvd.) and Burns Crossing Road at Severn Run in the town of Severn. Maryland Route 176 (Dorsey Road) and 648 (Baltimore-Annapolis Blvd) continued to be submerged in about two feet of water until after midnight. |Flash Flooding was reported in Baltimore County and the City of Baltimore. Gunpowder River rose out of its banks, allowing water to flow over the bridge at Second Mine Road. Flash flooding was also reported at Hydes Road and Long Green Pike as well as near White Hall and Gunpowder Falls State Park. Numerous roads were closed across Baltimore County, including a portion of Pulaski Highway (Route 40). Several roads in the City of Baltimore were also closed due to flash flooding. Jones Falls flooded the bridge at Interstate 83 and 41st Street. Other roadways affected by flash flooding include Erdman Avenue on the east side of the city and Caroline and Fleet Streets near downtown.|In Carroll County, water up to 2 feet deep across Twin Arch Road. An elderly woman became trapped in her car in Sykesville on River Road on the Howard/Carroll County line where the South branch of the Patapsco River rose our of its banks. The South Branch of the Patapsco River also rose out of it's banks onto Old Frederick Road, about 5 miles west of Woodbine. Route 32 was closed due to flooding near Sykesville. Numerous roads closed due to flooding near Keymar.|Numerous roads were closed across Charles County, especially near La Plata, Port Tobacco, Bryans Road and Waldorf. One roadway closed due to flooding include Billingsley Road between White Plains and Bryans Roads. Buses were forced to return students to school due to flooded roadways. |In Harford County, Deer Creek was out of its banks near Norrisville, causing localized flooding of some subdivision. High water on was reported on roads near Bel Air, with several water rescues of stranded motorists. Two water rescues were conducted near the intersection of Walters Mill and Ady Roads near Bel Air.|Thunderstorms brought damaging winds to Montgomery County between 1:00 PM and 2:00 PM, downing trees and power lines in Woodhaven, Gaithersburg, Layhill, Silver Spring and Bowie. A tree was downed on the Penn Line by a thunderstorm in Bowie. Heavy rain with these thunderstorms produced flooding that continued through early evening across Montgomery County. The Northwest Branch rose out of its banks at Route 29. Water covered Old Georgetown Road and Battery Lane near Huntington, MD. More than a dozen water rescues occurred across the county when people became trapped in their cars when trying to cross a flooded roadway. One such rescue was conducted in Germantown along Game Preserve Road.|In Prince George\ufffd\ufffd\ufffds County, Routes 301 and 5 were flooded. Several roads were closed near Andrews Air Force Base due to flooding, including a section of the Interstate 495 Capital Beltway. A farm equipment store was inundated by water in Upper Marlboro, MD.|In St. Mary\ufffd\ufffd\ufffds County, Route 235 and Saint John Road flooded in St. Mary\ufffd\ufffd\ufffds City, MD.|Tidal flooding occurred during the afternoon and early evening around the time of high tide in Baltimore. Strong onshore winds occurred due to a coastal low pressure system. Flooding of tidal areas and along the shoreline occurred in several communities, including Bowley Bar, Bowley Quarters, Millers Island and near Middle River. Twelve to 18 inches of water was reported to cover roadways in Millers Island and near Bowleys Quarters. Water approached some houses during high tide. There was also some coastal flooding at the Harborplace shopping facilities located at the Baltimore Inner Harbor. A deep low pressure system moved from the Tennessee Valley to the eastern great Lakes on November 16, sweeping a strong cold front across the Mid Atlantic. This system brought widespread moderate to heavy rain to the region after sunrise, then strong thunderstorms during the early afternoon. These thunderstorms produced periods of heavier rainfall as well as gusty and isolated damaging winds. Although rain ended across the region during the mid afternoon hours, some locations continued to experience flooding until just after midnight.|Heavy rain across Anne Arundel County closed numerous roadways from the early afternoon until after midnight on November 17th. Some of these roads include Governor Bridge Road and Saint George Barber, Routes 10 and 648 (Baltimore-Annapolis Blvd.) and Burns Crossing Road at Severn Run in the town of Severn. Maryland Route 176 (Dorsey Road) and 648 (Baltimore-Annapolis Blvd) continued to be submerged in about two feet of water until after midnight. |Flash Flooding was reported in Baltimore County and the City of Baltimore. Gunpowder River rose out of its banks, allowing water to flow over the bridge at Second Mine Road. Flash flooding was also reported at Hydes Road and Long Green Pike as well as near White Hall and Gunpowder Falls State Park. Numerous roads were closed across Baltimore County, including a portion of Pulaski Highway (Route 40). Several roads in the City of Baltimore were also closed due to flash flooding. Jones Falls flooded the bridge at Interstate 83 and 41st Street. Other roadways affected by flash flooding include Erdman Avenue on the east side of the city and Caroline and Fleet Streets near downtown.|In Carroll County, water up to 2 feet deep across Twin Arch Road. An elderly woman became trapped in her car in Sykesville on River Road on the Howard/Carroll County line where the South branch of the Patapsco River rose our of its banks. The South Branch of the Patapsco River also rose out of it's banks onto Old Frederick Road, about 5 miles west of Woodbine. Route 32 was closed due to flooding near Sykesville. Numerous roads closed due to flooding near Keymar.|Numerous roads were closed across Charles County, especially near La Plata, Port Tobacco, Bryans Road and Waldorf. One roadway closed due to flooding include Billingsley Road between White Plains and Bryans Roads. Buses were forced to return students to school due to flooded roadways. |In Harford County, Deer Creek was out of its banks near Norrisville, causing localized flooding of some subdivision. High water on was reported on roads near Bel Air, with several water rescues of stranded motorists. Two water rescues were conducted near the intersection of Walters Mill and Ady Roads near Bel Air.|Thunderstorms brought damaging winds to Montgomery County between 1:00 PM and 2:00 PM, downing trees and power lines in Woodhaven, Gaithersburg, Layhill, Silver Spring and Bowie. A tree was downed on the Penn Line by a thunderstorm in Bowie. Heavy rain with these thunderstorms produced flooding that continued through early evening across Montgomery County. The Northwest Branch rose out of its banks at Route 29. Water covered Old Georgetown Road and Battery Lane near Huntington, MD. More than a dozen water rescues occurred across the county when people became trapped in their cars when trying to cross a flooded roadway. One such rescue was conducted in Germantown along Game Preserve Road.|In Prince George\ufffd\ufffd\ufffds County, Routes 301 and 5 were flooded. Several roads were closed near Andrews Air Force Base due to flooding, including a section of the Interstate 495 Capital Beltway. A farm equipment store was inundated by water in Upper Marlboro, MD.|In St. Mary\ufffd\ufffd\ufffds County, Route 235 and Saint John Road flooded in St. Mary\ufffd\ufffd\ufffds City, MD.|Tidal flooding occurred during the afternoon and early evening around the time of high tide in Baltimore. Strong onshore winds occurred due to a coastal low pressure system. Flooding of tidal areas and along the shoreline occurred in several communities, including Bowley Bar, Bowley Quarters, Millers Island and near Middle River. Twelve to 18 inches of water was reported to cover roadways in Millers Island and near Bowleys Quarters. Water approached some houses during high tide. There was also some coastal flooding at the Harborplace shopping facilities located at the Baltimore Inner Harbor. A deep low pressure system moved from the Tennessee Valley to the eastern great Lakes on November 16, sweeping a strong cold front across the Mid Atlantic. This system brought widespread moderate to heavy rain to the region after sunrise, then strong thunderstorms during the early afternoon. These thunderstorms produced periods of heavier rainfall as well as gusty and isolated damaging winds. Although rain ended across the region during the mid afternoon hours, some locations continued to experience flooding until just after midnight.|Heavy rain across Anne Arundel County closed numerous roadways from the early afternoon until after midnight on November 17th. Some of these roads include Governor Bridge Road and Saint George Barber, Routes 10 and 648 (Baltimore-Annapolis Blvd.) and Burns Crossing Road at Severn Run in the town of Severn. Maryland Route 176 (Dorsey Road) and 648 (Baltimore-Annapolis Blvd) continued to be submerged in about two feet of water until after midnight. |Flash Flooding was reported in Baltimore County and the City of Baltimore. Gunpowder River rose out of its banks, allowing water to flow over the bridge at Second Mine Road. Flash flooding was also reported at Hydes Road and Long Green Pike as well as near White Hall and Gunpowder Falls State Park. Numerous roads were closed across Baltimore County, including a portion of Pulaski Highway (Route 40). Several roads in the City of Baltimore were also closed due to flash flooding. Jones Falls flooded the bridge at Interstate 83 and 41st Street. Other roadways affected by flash flooding include Erdman Avenue on the east side of the city and Caroline and Fleet Streets near downtown.|In Carroll County, water up to 2 feet deep across Twin Arch Road. An elderly woman became trapped in her car in Sykesville on River Road on the Howard/Carroll County line where the South branch of the Patapsco River rose our of its banks. The South Branch of the Patapsco River also rose out of it's banks onto Old Frederick Road, about 5 miles west of Woodbine. Route 32 was closed due to flooding near Sykesville. Numerous roads closed due to flooding near Keymar.|Numerous roads were closed across Charles County, especially near La Plata, Port Tobacco, Bryans Road and Waldorf. One roadway closed due to flooding include Billingsley Road between White Plains and Bryans Roads. Buses were forced to return students to school due to flooded roadways. |In Harford County, Deer Creek was out of its banks near Norrisville, causing localized flooding of some subdivision. High water on was reported on roads near Bel Air, with several water rescues of stranded motorists. Two water rescues were conducted near the intersection of Walters Mill and Ady Roads near Bel Air.|Thunderstorms brought damaging winds to Montgomery County between 1:00 PM and 2:00 PM, downing trees and power lines in Woodhaven, Gaithersburg, Layhill, Silver Spring and Bowie. A tree was downed on the Penn Line by a thunderstorm in Bowie. Heavy rain with these thunderstorms produced flooding that continued through early evening across Montgomery County. The Northwest Branch rose out of its banks at Route 29. Water covered Old Georgetown Road and Battery Lane near Huntington, MD. More than a dozen water rescues occurred across the county when people became trapped in their cars when trying to cross a flooded roadway. One such rescue was conducted in Germantown along Game Preserve Road.|In Prince George\ufffd\ufffd\ufffds County, Routes 301 and 5 were flooded. Several roads were closed near Andrews Air Force Base due to flooding, including a section of the Interstate 495 Capital Beltway. A farm equipment store was inundated by water in Upper Marlboro, MD.|In St. Mary\ufffd\ufffd\ufffds County, Route 235 and Saint John Road flooded in St. Mary\ufffd\ufffd\ufffds City, MD.|Tidal flooding occurred during the afternoon and early evening around the time of high tide in Baltimore. Strong onshore winds occurred due to a coastal low pressure system. Flooding of tidal areas and along the shoreline occurred in several communities, including Bowley Bar, Bowley Quarters, Millers Island and near Middle River. Twelve to 18 inches of water was reported to cover roadways in Millers Island and near Bowleys Quarters. Water approached some houses during high tide. There was also some coastal flooding at the Harborplace shopping facilities located at the Baltimore Inner Harbor. A deep low pressure system moved from the Tennessee Valley to the eastern great Lakes on November 16, sweeping a strong cold front across the Mid Atlantic. This system brought widespread moderate to heavy rain to the region after sunrise, then strong thunderstorms during the early afternoon. These thunderstorms produced periods of heavier rainfall as well as gusty and isolated damaging winds. Although rain ended across the region during the mid afternoon hours, some locations continued to experience flooding until just after midnight.|Heavy rain across Anne Arundel County closed numerous roadways from the early afternoon until after midnight on November 17th. Some of these roads include Governor Bridge Road and Saint George Barber, Routes 10 and 648 (Baltimore-Annapolis Blvd.) and Burns Crossing Road at Severn Run in the town of Severn. Maryland Route 176 (Dorsey Road) and 648 (Baltimore-Annapolis Blvd) continued to be submerged in about two feet of water until after midnight. |Flash Flooding was reported in Baltimore County and the City of Baltimore. Gunpowder River rose out of its banks, allowing water to flow over the bridge at Second Mine Road. Flash flooding was also reported at Hydes Road and Long Green Pike as well as near White Hall and Gunpowder Falls State Park. Numerous roads were closed across Baltimore County, including a portion of Pulaski Highway (Route 40). Several roads in the City of Baltimore were also closed due to flash flooding. Jones Falls flooded the bridge at Interstate 83 and 41st Street. Other roadways affected by flash flooding include Erdman Avenue on the east side of the city and Caroline and Fleet Streets near downtown.|In Carroll County, water up to 2 feet deep across Twin Arch Road. An elderly woman became trapped in her car in Sykesville on River Road on the Howard/Carroll County line where the South branch of the Patapsco River rose our of its banks. The South Branch of the Patapsco River also rose out of it's banks onto Old Frederick Road, about 5 miles west of Woodbine. Route 32 was closed due to flooding near Sykesville. Numerous roads closed due to flooding near Keymar.|Numerous roads were closed across Charles County, especially near La Plata, Port Tobacco, Bryans Road and Waldorf. One roadway closed due to flooding include Billingsley Road between White Plains and Bryans Roads. Buses were forced to return students to school due to flooded roadways. |In Harford County, Deer Creek was out of its banks near Norrisville, causing localized flooding of some subdivision. High water on was reported on roads near Bel Air, with several water rescues of stranded motorists. Two water rescues were conducted near the intersection of Walters Mill and Ady Roads near Bel Air.|Thunderstorms brought damaging winds to Montgomery County between 1:00 PM and 2:00 PM, downing trees and power lines in Woodhaven, Gaithersburg, Layhill, Silver Spring and Bowie. A tree was downed on the Penn Line by a thunderstorm in Bowie. Heavy rain with these thunderstorms produced flooding that continued through early evening across Montgomery County. The Northwest Branch rose out of its banks at Route 29. Water covered Old Georgetown Road and Battery Lane near Huntington, MD. More than a dozen water rescues occurred across the county when people became trapped in their cars when trying to cross a flooded roadway. One such rescue was conducted in Germantown along Game Preserve Road.|In Prince George\ufffd\ufffd\ufffds County, Routes 301 and 5 were flooded. Several roads were closed near Andrews Air Force Base due to flooding, including a section of the Interstate 495 Capital Beltway. A farm equipment store was inundated by water in Upper Marlboro, MD.|In St. Mary\ufffd\ufffd\ufffds County, Route 235 and Saint John Road flooded in St. Mary\ufffd\ufffd\ufffds City, MD.|Tidal flooding occurred during the afternoon and early evening around the time of high tide in Baltimore. Strong onshore winds occurred due to a coastal low pressure system. Flooding of tidal areas and along the shoreline occurred in several communities, including Bowley Bar, Bowley Quarters, Millers Island and near Middle River. Twelve to 18 inches of water was reported to cover roadways in Millers Island and near Bowleys Quarters. Water approached some houses during high tide. There was also some coastal flooding at the Harborplace shopping facilities located at the Baltimore Inner Harbor. A deep low pressure system moved from the Tennessee Valley to the eastern great Lakes on November 16, sweeping a strong cold front across the Mid Atlantic. This system brought widespread moderate to heavy rain to the region after sunrise, then strong thunderstorms during the early afternoon. These thunderstorms produced periods of heavier rainfall as well as gusty and isolated damaging winds. Although rain ended across the region during the mid afternoon hours, some locations continued to experience flooding until just after midnight.|Heavy rain across Anne Arundel County closed numerous roadways from the early afternoon until after midnight on November 17th. Some of these roads include Governor Bridge Road and Saint George Barber, Routes 10 and 648 (Baltimore-Annapolis Blvd.) and Burns Crossing Road at Severn Run in the town of Severn. Maryland Route 176 (Dorsey Road) and 648 (Baltimore-Annapolis Blvd) continued to be submerged in about two feet of water until after midnight. |Flash Flooding was reported in Baltimore County and the City of Baltimore. Gunpowder River rose out of its banks, allowing water to flow over the bridge at Second Mine Road. Flash flooding was also reported at Hydes Road and Long Green Pike as well as near White Hall and Gunpowder Falls State Park. Numerous roads were closed across Baltimore County, including a portion of Pulaski Highway (Route 40). Several roads in the City of Baltimore were also closed due to flash flooding. Jones Falls flooded the bridge at Interstate 83 and 41st Street. Other roadways affected by flash flooding include Erdman Avenue on the east side of the city and Caroline and Fleet Streets near downtown.|In Carroll County, water up to 2 feet deep across Twin Arch Road. An elderly woman became trapped in her car in Sykesville on River Road on the Howard/Carroll County line where the South branch of the Patapsco River rose our of its banks. The South Branch of the Patapsco River also rose out of it's banks onto Old Frederick Road, about 5 miles west of Woodbine. Route 32 was closed due to flooding near Sykesville. Numerous roads closed due to flooding near Keymar.|Numerous roads were closed across Charles County, especially near La Plata, Port Tobacco, Bryans Road and Waldorf. One roadway closed due to flooding include Billingsley Road between White Plains and Bryans Roads. Buses were forced to return students to school due to flooded roadways. |In Harford County, Deer Creek was out of its banks near Norrisville, causing localized flooding of some subdivision. High water on was reported on roads near Bel Air, with several water rescues of stranded motorists. Two water rescues were conducted near the intersection of Walters Mill and Ady Roads near Bel Air.|Thunderstorms brought damaging winds to Montgomery County between 1:00 PM and 2:00 PM, downing trees and power lines in Woodhaven, Gaithersburg, Layhill, Silver Spring and Bowie. A tree was downed on the Penn Line by a thunderstorm in Bowie. Heavy rain with these thunderstorms produced flooding that continued through early evening across Montgomery County. The Northwest Branch rose out of its banks at Route 29. Water covered Old Georgetown Road and Battery Lane near Huntington, MD. More than a dozen water rescues occurred across the county when people became trapped in their cars when trying to cross a flooded roadway. One such rescue was conducted in Germantown along Game Preserve Road.|In Prince George\ufffd\ufffd\ufffds County, Routes 301 and 5 were flooded. Several roads were closed near Andrews Air Force Base due to flooding, including a section of the Interstate 495 Capital Beltway. A farm equipment store was inundated by water in Upper Marlboro, MD.|In St. Mary\ufffd\ufffd\ufffds County, Route 235 and Saint John Road flooded in St. Mary\ufffd\ufffd\ufffds City, MD.|Tidal flooding occurred during the afternoon and early evening around the time of high tide in Baltimore. Strong onshore winds occurred due to a coastal low pressure system. Flooding of tidal areas and along the shoreline occurred in several communities, including Bowley Bar, Bowley Quarters, Millers Island and near Middle River. Twelve to 18 inches of water was reported to cover roadways in Millers Island and near Bowleys Quarters. Water approached some houses during high tide. There was also some coastal flooding at the Harborplace shopping facilities located at the Baltimore Inner Harbor. A deep low pressure system moved from the Tennessee Valley to the eastern great Lakes on November 16, sweeping a strong cold front across the Mid Atlantic. This system brought widespread moderate to heavy rain to the region after sunrise, then strong thunderstorms during the early afternoon. These thunderstorms produced periods of heavier rainfall as well as gusty and isolated damaging winds. Although rain ended across the region during the mid afternoon hours, some locations continued to experience flooding until just after midnight.|Heavy rain across Anne Arundel County closed numerous roadways from the early afternoon until after midnight on November 17th. Some of these roads include Governor Bridge Road and Saint George Barber, Routes 10 and 648 (Baltimore-Annapolis Blvd.) and Burns Crossing Road at Severn Run in the town of Severn. Maryland Route 176 (Dorsey Road) and 648 (Baltimore-Annapolis Blvd) continued to be submerged in about two feet of water until after midnight. |Flash Flooding was reported in Baltimore County and the City of Baltimore. Gunpowder River rose out of its banks, allowing water to flow over the bridge at Second Mine Road. Flash flooding was also reported at Hydes Road and Long Green Pike as well as near White Hall and Gunpowder Falls State Park. Numerous roads were closed across Baltimore County, including a portion of Pulaski Highway (Route 40). Several roads in the City of Baltimore were also closed due to flash flooding. Jones Falls flooded the bridge at Interstate 83 and 41st Street. Other roadways affected by flash flooding include Erdman Avenue on the east side of the city and Caroline and Fleet Streets near downtown.|In Carroll County, water up to 2 feet deep across Twin Arch Road. An elderly woman became trapped in her car in Sykesville on River Road on the Howard/Carroll County line where the South branch of the Patapsco River rose our of its banks. The South Branch of the Patapsco River also rose out of it's banks onto Old Frederick Road, about 5 miles west of Woodbine. Route 32 was closed due to flooding near Sykesville. Numerous roads closed due to flooding near Keymar.|Numerous roads were closed across Charles County, especially near La Plata, Port Tobacco, Bryans Road and Waldorf. One roadway closed due to flooding include Billingsley Road between White Plains and Bryans Roads. Buses were forced to return students to school due to flooded roadways. |In Harford County, Deer Creek was out of its banks near Norrisville, causing localized flooding of some subdivision. High water on was reported on roads near Bel Air, with several water rescues of stranded motorists. Two water rescues were conducted near the intersection of Walters Mill and Ady Roads near Bel Air.|Thunderstorms brought damaging winds to Montgomery County between 1:00 PM and 2:00 PM, downing trees and power lines in Woodhaven, Gaithersburg, Layhill, Silver Spring and Bowie. A tree was downed on the Penn Line by a thunderstorm in Bowie. Heavy rain with these thunderstorms produced flooding that continued through early evening across Montgomery County. The Northwest Branch rose out of its banks at Route 29. Water covered Old Georgetown Road and Battery Lane near Huntington, MD. More than a dozen water rescues occurred across the county when people became trapped in their cars when trying to cross a flooded roadway. One such rescue was conducted in Germantown along Game Preserve Road.|In Prince George\ufffd\ufffd\ufffds County, Routes 301 and 5 were flooded. Several roads were closed near Andrews Air Force Base due to flooding, including a section of the Interstate 495 Capital Beltway. A farm equipment store was inundated by water in Upper Marlboro, MD.|In St. Mary\ufffd\ufffd\ufffds County, Route 235 and Saint John Road flooded in St. Mary\ufffd\ufffd\ufffds City, MD.|Tidal flooding occurred during the afternoon and early evening around the time of high tide in Baltimore. Strong onshore winds occurred due to a coastal low pressure system. Flooding of tidal areas and along the shoreline occurred in several communities, including Bowley Bar, Bowley Quarters, Millers Island and near Middle River. Twelve to 18 inches of water was reported to cover roadways in Millers Island and near Bowleys Quarters. Water approached some houses during high tide. There was also some coastal flooding at the Harborplace shopping facilities located at the Baltimore Inner Harbor. A deep low pressure system moved from the Tennessee Valley to the eastern great Lakes on November 16, sweeping a strong cold front across the Mid Atlantic. This system brought widespread moderate to heavy rain to the region after sunrise, then strong thunderstorms during the early afternoon. These thunderstorms produced periods of heavier rainfall as well as gusty and isolated damaging winds. Although rain ended across the region during the mid afternoon hours, some locations continued to experience flooding until just after midnight.|Heavy rain across Anne Arundel County closed numerous roadways from the early afternoon until after midnight on November 17th. Some of these roads include Governor Bridge Road and Saint George Barber, Routes 10 and 648 (Baltimore-Annapolis Blvd.) and Burns Crossing Road at Severn Run in the town of Severn. Maryland Route 176 (Dorsey Road) and 648 (Baltimore-Annapolis Blvd) continued to be submerged in about two feet of water until after midnight. |Flash Flooding was reported in Baltimore County and the City of Baltimore. Gunpowder River rose out of its banks, allowing water to flow over the bridge at Second Mine Road. Flash flooding was also reported at Hydes Road and Long Green Pike as well as near White Hall and Gunpowder Falls State Park. Numerous roads were closed across Baltimore County, including a portion of Pulaski Highway (Route 40). Several roads in the City of Baltimore were also closed due to flash flooding. Jones Falls flooded the bridge at Interstate 83 and 41st Street. Other roadways affected by flash flooding include Erdman Avenue on the east side of the city and Caroline and Fleet Streets near downtown.|In Carroll County, water up to 2 feet deep across Twin Arch Road. An elderly woman became trapped in her car in Sykesville on River Road on the Howard/Carroll County line where the South branch of the Patapsco River rose our of its banks. The South Branch of the Patapsco River also rose out of it's banks onto Old Frederick Road, about 5 miles west of Woodbine. Route 32 was closed due to flooding near Sykesville. Numerous roads closed due to flooding near Keymar.|Numerous roads were closed across Charles County, especially near La Plata, Port Tobacco, Bryans Road and Waldorf. One roadway closed due to flooding include Billingsley Road between White Plains and Bryans Roads. Buses were forced to return students to school due to flooded roadways. |In Harford County, Deer Creek was out of its banks near Norrisville, causing localized flooding of some subdivision. High water on was reported on roads near Bel Air, with several water rescues of stranded motorists. Two water rescues were conducted near the intersection of Walters Mill and Ady Roads near Bel Air.|Thunderstorms brought damaging winds to Montgomery County between 1:00 PM and 2:00 PM, downing trees and power lines in Woodhaven, Gaithersburg, Layhill, Silver Spring and Bowie. A tree was downed on the Penn Line by a thunderstorm in Bowie. Heavy rain with these thunderstorms produced flooding that continued through early evening across Montgomery County. The Northwest Branch rose out of its banks at Route 29. Water covered Old Georgetown Road and Battery Lane near Huntington, MD. More than a dozen water rescues occurred across the county when people became trapped in their cars when trying to cross a flooded roadway. One such rescue was conducted in Germantown along Game Preserve Road.|In Prince George\ufffd\ufffd\ufffds County, Routes 301 and 5 were flooded. Several roads were closed near Andrews Air Force Base due to flooding, including a section of the Interstate 495 Capital Beltway. A farm equipment store was inundated by water in Upper Marlboro, MD.|In St. Mary\ufffd\ufffd\ufffds County, Route 235 and Saint John Road flooded in St. Mary\ufffd\ufffd\ufffds City, MD.|Tidal flooding occurred during the afternoon and early evening around the time of high tide in Baltimore. Strong onshore winds occurred due to a coastal low pressure system. Flooding of tidal areas and along the shoreline occurred in several communities, including Bowley Bar, Bowley Quarters, Millers Island and near Middle River. Twelve to 18 inches of water was reported to cover roadways in Millers Island and near Bowleys Quarters. Water approached some houses during high tide. There was also some coastal flooding at the Harborplace shopping facilities located at the Baltimore Inner Harbor.\nEvent Narrative: Several roads in the City of Baltimore were closed due to flash flooding. Jones Falls flooded the bridge at Interstate 83 and 41st Street. Other roadways affected by flash flooding include Erdman Avenue on the east side of the city and Caroline and Fleet Streets near downtown. Heavy rain across Anne Arundel County closed numerous roadways from the early afternoon until after midnight on November 17th. Some of these roads include Governor Bridge Road and Saint George Barber, Routes 10 and 648 (Baltimore-Annapolis Blvd.) and Burns Crossing Road at Severn Run in the town of Severn. Maryland Route 176 (Dorsey Road) and 648 (Baltimore-Annapolis Blvd) continued to be submerged in about two feet of water until after midnight. Roads were closed due to high water in the Cockeysville area. A tree was downed on the Penn Line by a thunderstorm in Bowie. Deer Creek was out of its banks near Norrisville, causing localized flooding of some subdivision. High water on was reported on roads near Bel Air, with several water rescues of stranded motorists. Two water rescues were conducted near the intersection of Walters Mill and Ady Roads near Bel Air. Route 32 was closed near the Howard/Carroll County line due to flooding. An elderly woman became trapped in her car in Sykesville on River Road on the Howard/Carroll County line where the South branch of the Patapsco River rose our of its banks. Flash Flooding was reported in Baltimore County and the City of Baltimore. Gunpowder River rose out of its banks, allowing water to flow over the bridge at Second Mine Road. Flash flooding was also reported at Hydes Road and Long Green Pike as well as near White Hall and Gunpowder Falls State Park. Numerous roads were closed across Baltimore County, including a portion of Pulaski Highway (Route 40). Roads were also closed due to flooding in the Cockeysville area. Emergency Management reported water up to 2 feet deep across Twin Arch Road. An elderly woman became trapped in her car in Sykesville on River Road on the Howard/Carroll County line where the South branch of the Patapsco River rose our of its banks. The South Branch of the Patapsco River also rose out of it's banks onto Old Frederick Road, about 5 miles west of Woodbine. Route 32 was closed due to flooding near Sykesville. Numerous roads closed due to flooding near Keymar.", "The following events were reported: Flood. These occurred near station USW00093721, approximately 10.7345 km away, between 2007-03-16 13:00:00 and 2007-03-16 16:00:00. The flood was caused by Heavy Rain. Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A strong cold front crossed the region on the afternoon of March 15th, ushering in drastically colder temperatures. A low pressure system approached the region that night and moved north along the Atlantic coast on March 16th. As the low approached the region early on the 16th, precipitation became widespread and continued through much day. |Warm air briefly surged ahead of the low pressure system, allowing precipitation to begin in the form of rain. Several roads were closed due to flooding across Anne Arundel, St. Mary\ufffd\ufffd\ufffds and Northern Baltimore Counties. |Colder air was brought into the region by the low. This forced rain to change to snow and sleet before changing to all snow. Snowfall amounts ranged from 2 to 10 inches. Hazardous driving conditions led to numerous minor car accidents. A vehicle in President Bush\ufffd\ufffd\ufffds motorcade traveling from Washington DC to the Camp David presidential retreat collided with another car along Interstate 270 in Urbana, MD., in Frederick County. No injuries were reported. A strong cold front crossed the region on the afternoon of March 15th, ushering in drastically colder temperatures. A low pressure system approached the region that night and moved north along the Atlantic coast on March 16th. As the low approached the region early on the 16th, precipitation became widespread and continued through much day. |Warm air briefly surged ahead of the low pressure system, allowing precipitation to begin in the form of rain. Several roads were closed due to flooding across Anne Arundel, St. Mary\ufffd\ufffd\ufffds and Northern Baltimore Counties. |Colder air was brought into the region by the low. This forced rain to change to snow and sleet before changing to all snow. Snowfall amounts ranged from 2 to 10 inches. Hazardous driving conditions led to numerous minor car accidents. A vehicle in President Bush\ufffd\ufffd\ufffds motorcade traveling from Washington DC to the Camp David presidential retreat collided with another car along Interstate 270 in Urbana, MD., in Frederick County. No injuries were reported.\nEvent Narrative: A Newspaper reported that West Furnace Branch Road was closed due to flooding. County Officials reported Orems Road at Golden Ring Road closed due to flooding.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 14.1629 km away, between 2007-03-27 18:00:00 and 2007-03-27 18:15:00. The events included records with measured wind gusts of 39.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A weak cold front crossing over the Maryland Chesapeake Bay triggered strong showers and thunderstorms with gusty winds on the evening of March 27th.\nEvent Narrative: A wind gust of 39 knots was reported by buoy FSKM2 and a gust of 34 knots was reported at Villa Julie College near Baltimore.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 6.2256 km away, between 2007-04-12 16:25:00 and 2007-04-12 17:10:00. The events included records with measured wind gusts of 38.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Widely scattered showers and thunderstorms developed during the afternoon of April 12th across northern Virginia and central Maryland. These storms moved east over the northern Chesapeake Bay, producing wind gusts between 32 and 38 knots.\nEvent Narrative: The ASOS at Baltimore-Washington Airport reported a gust of 38 knots. The Buoy at Tolchester Beach reported a gust of 33 knots.", "The following events were reported: Heavy Rain. These occurred near station USW00093721, approximately 43.4462 km away, between 2007-04-15 03:00:00 and 2007-04-16 00:00:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: An intense nor'easter brought heavy rain and flooding to the Maryland Eastern Shore on the 15th and strong winds to the region on the 16th. Rain began falling during the evening on the 14th, but fell at its heaviest from about Midnight EDT through about 3 p.m. EDT on the 15th. The rain ended before sunrise during the early morning of the 16th. Event precipitation totals averaged between 3 and 6 inches. The strongest winds occurred as the nor'easter pulled northeast of the region on the 16th from the early morning into the afternoon. Peak wind gusts averaged around 50 mph.|The worst reported flooding was in Cecil County on the 15th where four roadways were closed (including Delaware Avenue) in Elkton as the Big Elk Creek flooded. Flooding was also reported along Maryland State Route 7 at Broad and Peddler Creeks in Charlestown. The Trinity Woods subdivision experienced yard and roadway flooding. Elsewhere similar flooding conditions occurred as mainly poor drainage, yard and field flooding was reported. The gusty northwest winds on Monday the 16th caused scattered power outages for both Delmarva Power and Choptank Electric Cooperative.|Storm totals included 5.63 inches in American Corner (Caroline County), 3.80 inches in Federalsburg (Caroline County), 3.50 inches in Stevensville (Queen Anne's County) and 3.37 inches at the Conowingo Dam (Cecil County). Peak wind gusts included 54 mph in Salisbury (Dorchester County), 53 mph at the Baltimore-Washington International Airport, 48 mph in Easton (Talbot County), 47 mph in Annapolis (Anne Arundel County) and 46 mph in Chesapeake City (Cecil County) and Tolchester Beach (Kent County). |The nor'easter low pressure system initially formed in the southern Rockies on the 12th and moved to Arkansas on the morning of the 14th. At 8 p.m. EDT on the 14th, there were two low pressure systems, one in Kentucky and the other in western Alabama. The southern low pressure system became the predominate one overnight and at 8 a.m. EDT on the 15th, it (996 millibar low) was located in western North Carolina. As the 15th continued, it moved northeast and intensified rapidly. At 2 p.m. EDT the nor'easter (989 millibars) was near Raleigh, North Carolina. At 8 p.m. EDT, the nor'easter was a 979 millibar low pressure system near Virginia Beach, Virginia. Another low pressure system formed on its warm front during the afternoon over Chesapeake Bay and at 8 p.m. EDT it (982 millibars) was over extreme southwest New Jersey. The lows consolidated into one again overnight and a very intense 973 millibar low pressure system was located over Monmouth County, New Jersey at 2 a.m. EDT on the 16th. At 8 a.m. EDT on the 16th the nor'easter was down to 968 millibars and located over New York City. That was a drop in central pressure of 28 millibars in 24 hours which qualified it as a meteorological bomb (a drop in central pressure of at least 24 millibars in 24 hours) low pressure system. The nor'easter bottomed at a pressure of about 966 millibars (28.53 inches) at 11 a.m. EDT just south of Long Island, New York. To put into prospective how low the pressure was with this nor'easter, that central pressure is near the border of the pressure defined category 2 and category 3 hurricane once used on the Saffir-Simpson Hurricane Scale. As the 16th continued, the nor'easter weakened and meandered across southwest New England and the New York and New Jersey coastal waters. By 2 a.m. EDT on the 17th, the nor'easter's central pressure rose to 988 millibars and a second storm formed on the triple point of its fronts south of Nova Scotia. This became the main low pressure system. The low pressure system then slowly moved southeast over the next couple of days. The heaviest precipitation fell as the low pressure system was rapidly intensifying on the 15th into the early part of the 16th. The strongest winds ceased after the low pressure system started to fill on the afternoon of the 16th. An intense nor'easter brought heavy rain and flooding to the Maryland Eastern Shore on the 15th and strong winds to the region on the 16th. Rain began falling during the evening on the 14th, but fell at its heaviest from about Midnight EDT through about 3 p.m. EDT on the 15th. The rain ended before sunrise during the early morning of the 16th. Event precipitation totals averaged between 3 and 6 inches. The strongest winds occurred as the nor'easter pulled northeast of the region on the 16th from the early morning into the afternoon. Peak wind gusts averaged around 50 mph.|The worst reported flooding was in Cecil County on the 15th where four roadways were closed (including Delaware Avenue) in Elkton as the Big Elk Creek flooded. Flooding was also reported along Maryland State Route 7 at Broad and Peddler Creeks in Charlestown. The Trinity Woods subdivision experienced yard and roadway flooding. Elsewhere similar flooding conditions occurred as mainly poor drainage, yard and field flooding was reported. The gusty northwest winds on Monday the 16th caused scattered power outages for both Delmarva Power and Choptank Electric Cooperative.|Storm totals included 5.63 inches in American Corner (Caroline County), 3.80 inches in Federalsburg (Caroline County), 3.50 inches in Stevensville (Queen Anne's County) and 3.37 inches at the Conowingo Dam (Cecil County). Peak wind gusts included 54 mph in Salisbury (Dorchester County), 53 mph at the Baltimore-Washington International Airport, 48 mph in Easton (Talbot County), 47 mph in Annapolis (Anne Arundel County) and 46 mph in Chesapeake City (Cecil County) and Tolchester Beach (Kent County). |The nor'easter low pressure system initially formed in the southern Rockies on the 12th and moved to Arkansas on the morning of the 14th. At 8 p.m. EDT on the 14th, there were two low pressure systems, one in Kentucky and the other in western Alabama. The southern low pressure system became the predominate one overnight and at 8 a.m. EDT on the 15th, it (996 millibar low) was located in western North Carolina. As the 15th continued, it moved northeast and intensified rapidly. At 2 p.m. EDT the nor'easter (989 millibars) was near Raleigh, North Carolina. At 8 p.m. EDT, the nor'easter was a 979 millibar low pressure system near Virginia Beach, Virginia. Another low pressure system formed on its warm front during the afternoon over Chesapeake Bay and at 8 p.m. EDT it (982 millibars) was over extreme southwest New Jersey. The lows consolidated into one again overnight and a very intense 973 millibar low pressure system was located over Monmouth County, New Jersey at 2 a.m. EDT on the 16th. At 8 a.m. EDT on the 16th the nor'easter was down to 968 millibars and located over New York City. That was a drop in central pressure of 28 millibars in 24 hours which qualified it as a meteorological bomb (a drop in central pressure of at least 24 millibars in 24 hours) low pressure system. The nor'easter bottomed at a pressure of about 966 millibars (28.53 inches) at 11 a.m. EDT just south of Long Island, New York. To put into prospective how low the pressure was with this nor'easter, that central pressure is near the border of the pressure defined category 2 and category 3 hurricane once used on the Saffir-Simpson Hurricane Scale. As the 16th continued, the nor'easter weakened and meandered across southwest New England and the New York and New Jersey coastal waters. By 2 a.m. EDT on the 17th, the nor'easter's central pressure rose to 988 millibars and a second storm formed on the triple point of its fronts south of Nova Scotia. This became the main low pressure system. The low pressure system then slowly moved southeast over the next couple of days. The heaviest precipitation fell as the low pressure system was rapidly intensifying on the 15th into the early part of the 16th. The strongest winds ceased after the low pressure system started to fill on the afternoon of the 16th.\nEvent Narrative:", "The following events were reported: Flood. These occurred near station USW00093721, approximately 15.975 km away, between 2007-04-15 08:00:00 and 2007-04-15 20:00:00. The flood was caused by Heavy Rain. Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A Nor'Easter impacted the Mid Atlantic region on April 15th and 16th. Low pressure off the southeastern coast moved north along the Delmarva. Heavy rain spread north across the region early April 15th, causing flooding by the afternoon and evening. As the low pressure area pushed north and intensified, colder air advanced from the northwest. This allowed rain to change to snow along the upslope region of the Allegheny Front. Winds also increased in the wake of the low, downing trees and power lines across central and lower southern Maryland. A Nor'Easter impacted the Mid Atlantic region on April 15th and 16th. Low pressure off the southeastern coast moved north along the Delmarva. Heavy rain spread north across the region early April 15th, causing flooding by the afternoon and evening. As the low pressure area pushed north and intensified, colder air advanced from the northwest. This allowed rain to change to snow along the upslope region of the Allegheny Front. Winds also increased in the wake of the low, downing trees and power lines across central and lower southern Maryland. A Nor'Easter impacted the Mid Atlantic region on April 15th and 16th. Low pressure off the southeastern coast moved north along the Delmarva. Heavy rain spread north across the region early April 15th, causing flooding by the afternoon and evening. As the low pressure area pushed north and intensified, colder air advanced from the northwest. This allowed rain to change to snow along the upslope region of the Allegheny Front. Winds also increased in the wake of the low, downing trees and power lines across central and lower southern Maryland. A Nor'Easter impacted the Mid Atlantic region on April 15th and 16th. Low pressure off the southeastern coast moved north along the Delmarva. Heavy rain spread north across the region early April 15th, causing flooding by the afternoon and evening. As the low pressure area pushed north and intensified, colder air advanced from the northwest. This allowed rain to change to snow along the upslope region of the Allegheny Front. Winds also increased in the wake of the low, downing trees and power lines across central and lower southern Maryland.\nEvent Narrative: Newspapers reported several roads closed due to flooding across the eastern portion of the county. Heavy rains caused a mudslide which closed the Baltimore/Washington Parkway near Linthicum. A Trained Spotter reported flooding at Fort Meade. A Trained Spotter reported flooding along the Jones Falls on Greenspring Valley Road in Stevenson, MD. A Trained Spotter reported flooding in the Hampden area of Baltimore. A Trained Spotter reported that the Little Patuxent River overflowed its banks along Brock Bridge Road southeast of Savage, MD.", "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00093721, approximately 22.4357 km away, between 2007-05-16 15:32:00 and 2007-05-16 16:15:00. The events included records with hailstones measuring 33.583333333333336 inches.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 3000.0 and crop damage of 0.0. \n\nEpisode Narrative: A strong cold front approaching the region from the north and west triggered thunderstorms during the afternoon of May 16th. Some storms became severe, downing trees and power lines and producing large hail. A strong cold front approaching the region from the north and west triggered thunderstorms during the afternoon of May 16th. Some storms became severe, downing trees and power lines and producing large hail. A strong cold front approaching the region from the north and west triggered thunderstorms during the afternoon of May 16th. Some storms became severe, downing trees and power lines and producing large hail.\nEvent Narrative: A Trained Spotter reported a tree down in Columbia, MD. A Trained Spotter reported penny size hail in Parole, MD. Trees were downed in Riva, MD.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 16.932 km away, between 2007-05-16 15:48:00 and 2007-05-16 16:30:00. The events included records with measured wind gusts of 42.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A strong cold front crossing the approaching the region from the north and west triggered thunderstorms during the afternoon of May 16th. Some storms became severe, producing wind gusts over 30 knots along the Tidal Potomac River and Maryland Chesapeake Bay. A strong cold front crossing the approaching the region from the north and west triggered thunderstorms during the afternoon of May 16th. Some storms became severe, producing wind gusts over 30 knots along the Tidal Potomac River and Maryland Chesapeake Bay.\nEvent Narrative: The Buoy at Thomas Point, MD., reported a wind gusts of 42 knots. An Automated Observation from the US Naval Academy in Annapolis, MD., reported a wind gust of 33 knots. An Automated Observation from Baltimore/Washington International Thurgood Marshall Airport reported a wind gust of 42 knots. Wind gusts between 29 and 33 knots were reported at Francis Scott Key Bridge and at Tolchester Beach.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 27.6109 km away, between 2007-05-27 17:40:00 and 2007-05-27 18:20:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 2000.0 and crop damage of 0.0. \n\nEpisode Narrative: A weak frontal boundary remained draped across the Mid Atlantic for several days at the end of May. Scattered showers and thunderstorms developed in a warm and unstable airmass on May 27th. Some of these storms became severe, producing damaging winds across northern and central Maryland. A weak frontal boundary remained draped across the Mid Atlantic for several days at the end of May. Scattered showers and thunderstorms developed in a warm and unstable airmass on May 27th. Some of these storms became severe, producing damaging winds across northern and central Maryland. A weak frontal boundary remained draped across the Mid Atlantic for several days at the end of May. Scattered showers and thunderstorms developed in a warm and unstable airmass on May 27th. Some of these storms became severe, producing damaging winds across northern and central Maryland.\nEvent Narrative: Emergency Management reported a tree down near Georgia Avenue and Highway 108 in Olney, MD. Emergency Management reported two trees down on power lines in Linthicum, MD. Emergency Management reported a tree down near the intersection of Falls Road and Mt. Carmel Road north of Butler, MD.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 20.9028 km away, between 2007-05-27 18:14:00 and 2007-05-27 19:00:00. The events included records with measured wind gusts of 40.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A weak frontal boundary remained draped across the Mid Atlantic for several days at the end of May. Scattered showers and thunderstorms developed in a warm and unstable airmass on May 27th. Some of these storms became severe, producing wind gusts up to 40 knots along the Tidal Potomac River and Maryland Chesapeake Bay. A weak frontal boundary remained draped across the Mid Atlantic for several days at the end of May. Scattered showers and thunderstorms developed in a warm and unstable airmass on May 27th. Some of these storms became severe, producing wind gusts up to 40 knots along the Tidal Potomac River and Maryland Chesapeake Bay.\nEvent Narrative: A buoy at Thomas Point, MD., reported a wind gust of 40 knots. Several separate automated observations reported wind gusts between 34 and 40 knots between Pooles Island and Sandy Point.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 22.7782 km away, between 2007-06-03 16:44:00 and 2007-06-03 16:50:00. The events included records with measured wind gusts of 34.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: The weakening remnants of Tropical Storm Barry pushed north along the Mid Atlantic Coast on June 3rd. Showers and thunderstorms spread north across the region throughout the day. Some of these storms produced wind gusts in excess of 30 knots over the Maryland Chesapeake Bay during the evening hours.\nEvent Narrative: A wind gust of 34 knots was measured at Millers Island, MD.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 43.4659 km away, between 2007-06-04 16:25:00 and 2007-06-04 17:00:00. The events included records with measured wind gusts of 39.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Scattered thunderstorms continued to develop across the Mid Atlantic as the remnants of tropical Storm Barry moved north along the east coast. Storms developed over the Maryland Chesapeake Bay during the afternoon and evening of June 4th, producing wind gusts in excess of 30 knots.\nEvent Narrative: A Buoy near Tolchester Beach reported a wind gust of 39 knots. Winds further west on the Bay reported wind gusts near 30 knots beginning 30 minutes earlier.", "The following events were reported: Hail. These occurred near station USW00093721, approximately 39.4601 km away, between 2007-06-04 17:40:00 and 2007-06-04 17:40:00. The events included records with hailstones measuring 0.75 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A severe thunderstorm that crossed Chesapeake Bay dropped penny size hail in Rock Hall. The Thunderstorm also produced a measured wind gust to 52 mph at Tolchester Beach.\nEvent Narrative:", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 24.8892 km away, between 2007-06-08 20:42:00 and 2007-06-08 21:06:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A strong cold front pushed across the Mid Atlantic on the evening of June 8th. Ahead of the front, a warm and unstable airmass allowed scattered showers and thunderstorms to develop over northern Virginia and central Maryland. These storms pushed east over the Tidal Potomac River and Maryland Chesapeake Bay during the late evening hours, producing wind gusts in excess of 30 knots. A strong cold front pushed across the Mid Atlantic on the evening of June 8th. Ahead of the front, a warm and unstable airmass allowed scattered showers and thunderstorms to develop over northern Virginia and central Maryland. These storms pushed east over the Tidal Potomac River and Maryland Chesapeake Bay during the late evening hours, producing wind gusts in excess of 30 knots.\nEvent Narrative: The buoy at Hart-Millers Island measured a wind gust of 43 knots. A buoy at Thomas Point Lighthouse estimated a wind gust of 34 knots.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 46.3562 km away, between 2007-06-12 15:01:00 and 2007-06-12 15:01:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 1000.0 and crop damage of 0.0. \n\nEpisode Narrative: Upper Level disturbances combined with a warm and unstable airmass to produce widespread showers and thunderstorms across the Mid Atlantic. Some of these storms became severe, producing large hail and damaging winds across much of Maryland during the afternoon and evening of June 12th.\nEvent Narrative: Trees were downed in Upperco, MD.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 16.932 km away, between 2007-06-12 16:00:00 and 2007-06-12 16:52:00. The events included records with measured wind gusts of 41.5 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Upper Level disturbances combined with a warm and unstable airmass to produce widespread showers and thunderstorms across the Mid Atlantic. Some of these storms crossed the Tidal Potomac River and Maryland Chesapeake Bay during the afternoon and evening of June 12th, producing wind gusts in excess of 30 knots. Upper Level disturbances combined with a warm and unstable airmass to produce widespread showers and thunderstorms across the Mid Atlantic. Some of these storms crossed the Tidal Potomac River and Maryland Chesapeake Bay during the afternoon and evening of June 12th, producing wind gusts in excess of 30 knots.\nEvent Narrative: The buoy at Tolchester Beach measured a wind gust of 39 knots. Winds in excess of 30 knots were also reported at Sandy Point and Francis Scott Key Bridge. The buoy at Thomas Point Light House measured a wind gust of 44 knots. Winds in excess of 30 knots were also reported at Sandy Point and the US Naval Academy in Annapolis, MD.", "The following events were reported: Hail. These occurred near station USW00093721, approximately 49.3165 km away, between 2007-06-12 16:10:00 and 2007-06-12 16:10:00. The events included records with hailstones measuring 0.88 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: The combination of unseasonably cold air aloft and daytime heating helped produce some strong to severe thunderstorms across the Maryland Eastern Shore on the afternoon of the 12th.\nEvent Narrative: A SKYWARN Spotter reported nickel size hail fell in Queenstown.", "The following events were reported: Hail, Thunderstorm Wind, Tornado. These occurred near station USW00093721, approximately 30.3867 km away, between 2007-06-13 16:10:00 and 2007-06-13 17:10:00. The events included records with hailstones measuring 33.626666666666665 inches.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 2000.0 and crop damage of 0.0. \n\nEpisode Narrative: A series of weak surface low pressure troughs over the Mid Atlantic triggered numerous showers and thunderstorms across western and central Maryland. These storms moved east into the Baltimore Metro area and south into lower southern Maryland. Some of these storms became severe, producing damaging winds and large hail. A series of weak surface low pressure troughs over the Mid Atlantic triggered numerous showers and thunderstorms across western and central Maryland. These storms moved east into the Baltimore Metro area and south into lower southern Maryland. Some of these storms became severe, producing damaging winds and large hail. A series of weak surface low pressure troughs over the Mid Atlantic triggered numerous showers and thunderstorms across western and central Maryland. These storms moved east into the Baltimore Metro area and south into lower southern Maryland. Some of these storms became severe, producing damaging winds and large hail. A series of weak surface low pressure troughs over the Mid Atlantic triggered numerous showers and thunderstorms across western and central Maryland. These storms moved east into the Baltimore Metro area and south into lower southern Maryland. Some of these storms became severe, producing damaging winds and large hail.\nEvent Narrative: An NWS Storm Survey concluded that a small tornado, rated at EF0, did touch down north of the town of Butler in Baltimore County. The length of damage that the tornado produced was between 1 and 2 miles, with an approximate width of 75 yards. This conclusion was reached based on fall patterns of trees, branches and the defoliation of deciduous trees. No structural damage was found and no injuries were reported. Emergency Management and Trained Spotters reported trees and power lines down from Cockeysville and Bentley Springs. Howard County Fire and Rescue reported a tree down on Murray Hill and Vollmerhausen.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 16.932 km away, between 2007-06-21 16:25:00 and 2007-06-21 17:26:00. The events included records with measured wind gusts of 44.5 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A secondary cold front crossed the region late June 21st. A warm and humid airmass ahead of the front combined with the approaching front allowed thunderstorms to develop across the Ohio Valley and move southeast towards the Tidal Potomac River and Maryland Chesapeake Bay. Some of these storms became severe, producing wind gusts in excess of 35 knots. A secondary cold front crossed the region late June 21st. A warm and humid airmass ahead of the front combined with the approaching front allowed thunderstorms to develop across the Ohio Valley and move southeast towards the Tidal Potomac River and Maryland Chesapeake Bay. Some of these storms became severe, producing wind gusts in excess of 35 knots.\nEvent Narrative: Wind gusts of 37 knots were measured at the Baltimore Approaches Buoy and at Francis Scott Key bridge. A wind gust of 52 knots was reported at Baltimore/Washington International Airport (BWI). An Automated Observation from the US Naval Academy measured a wind gust of 37 knots.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 13.2941 km away, between 2007-06-21 16:33:00 and 2007-06-21 16:55:00. The events included records with estimated wind gusts of 50.4 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 5000.0 and crop damage of 0.0. \n\nEpisode Narrative: A secondary cold front crossed the region late June 21st. A warm and humid airmass ahead of the front combined with the approaching front allowed thunderstorms to develop across the Ohio Valley and move southeast towards northern and central Maryland. Some of these storms became severe, producing damaging winds. A secondary cold front crossed the region late June 21st. A warm and humid airmass ahead of the front combined with the approaching front allowed thunderstorms to develop across the Ohio Valley and move southeast towards northern and central Maryland. Some of these storms became severe, producing damaging winds. A secondary cold front crossed the region late June 21st. A warm and humid airmass ahead of the front combined with the approaching front allowed thunderstorms to develop across the Ohio Valley and move southeast towards northern and central Maryland. Some of these storms became severe, producing damaging winds. A secondary cold front crossed the region late June 21st. A warm and humid airmass ahead of the front combined with the approaching front allowed thunderstorms to develop across the Ohio Valley and move southeast towards northern and central Maryland. Some of these storms became severe, producing damaging winds. A secondary cold front crossed the region late June 21st. A warm and humid airmass ahead of the front combined with the approaching front allowed thunderstorms to develop across the Ohio Valley and move southeast towards northern and central Maryland. Some of these storms became severe, producing damaging winds.\nEvent Narrative: Law Enforcement reported trees down in Ellicott City, MD. An Automated Observation from Baltimore/Washington International Thurgood Marshall Airport reported a wind gust of 52 knots (60 MPH). The Baltimore City Fire Department reported trees down. Law Enforcement reported power lines down in Bowie, MD. A Trained Spotter reported a tree down on a camper in Greenbelt, MD. Law Enforcement reported large tree limbs downed in Catonsville, MD.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 20.9908 km away, between 2007-06-27 14:15:00 and 2007-06-27 14:15:00. The events included records with measured wind gusts of 39.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A warm and humid airmass developed as high pressure moved offshore and a cold front approached from the west. Scattered thunderstorms developed across northern Virginia and central Maryland during the afternoon of June 27th. Some storms became severe, producing wind gusts in excess of 35 knots over the Tidal Potomac River and Maryland Chesapeake Bay.\nEvent Narrative: A wind gust of 39 knots was measured 2 miles north of Edgemere, MD.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 6.2256 km away, between 2007-06-28 20:21:00 and 2007-06-28 21:24:00. The events included records with measured wind gusts of 39.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Scattered showers and thunderstorms developed across northern Virginia and central Maryland on the afternoon of June 28th. These storms moved quickly east across the Tidal Potomac River and Maryland Chesapeake Bay during the evening. Some of these storms produced wind gusts in excess of 30 knots.\nEvent Narrative: An Automated Observation at Baltimore/Washington International Airport measured a wind gust of 39 knots.", "The following events were reported: Funnel Cloud, Hail, Thunderstorm Wind. These occurred near station USW00093721, approximately 21.2363 km away, between 2007-07-04 15:30:00 and 2007-07-04 18:55:00. The events included records with hailstones measuring 25.416666666666668 inches.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 2000.0 and crop damage of 0.0. \n\nEpisode Narrative: Showers and thunderstorms developed during the afternoon and evening of July 4th and moved east across northern Virginia and western Maryland. Some became severe, producing large hail and damaging winds. Showers and thunderstorms developed during the afternoon and evening of July 4th and moved east across northern Virginia and western Maryland. Some became severe, producing large hail and damaging winds. Showers and thunderstorms developed during the afternoon and evening of July 4th and moved east across northern Virginia and western Maryland. Some became severe, producing large hail and damaging winds. Showers and thunderstorms developed during the afternoon and evening of July 4th and moved east across northern Virginia and western Maryland. Some became severe, producing large hail and damaging winds. Showers and thunderstorms developed during the afternoon and evening of July 4th and moved east across northern Virginia and western Maryland. Some became severe, producing large hail and damaging winds. Showers and thunderstorms developed during the afternoon and evening of July 4th and moved east across northern Virginia and western Maryland. Some became severe, producing large hail and damaging winds. Showers and thunderstorms developed during the afternoon and evening of July 4th and moved east across northern Virginia and western Maryland. Some became severe, producing large hail and damaging winds.\nEvent Narrative: Anne Arundel County Officials reported trees down on power lines near Beverly Road and Evergreen in Severn, MD. A Trained Spotter reported penny size hail in North Laurel, MD. The Baltimore City Department of Public Works reported trees down on Frederick Ave. A Funnel Cloud was reported southeast of Damascus. Local media also reported footage of the funnel cloud on the evening news. Law Enforcement reported power lines down near Green Bridge Road near Dayton, MD. A Trained Spotter reported penny size hail southwest of West Friendship, MD. A Trained Spotter reported penny to quarter size hail near Catonsville, MD.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 6.2256 km away, between 2007-07-04 19:12:00 and 2007-07-04 19:30:00. The events included records with measured wind gusts of 41.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Widespread showers and thunderstorms developed across northern and central Virginia, central Maryland and Washington DC. These storms spread east curing the late afternoon. One of these storms became severe, producing 40 knot winds over a portion of the Maryland Chesapeake Bay.\nEvent Narrative: An Automated Surface Observation from Baltimore/Washington International Airport (BWI) measured a wind gust of 41 knots.", "The following events were reported: Marine Hail, Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 2.4862 km away, between 2007-07-10 12:26:00 and 2007-07-10 12:50:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: High pressure across the western Atlantic brought hot and humid conditions to the Mid Atlantic on July 10th. Showers and thunderstorms developed along and east of the Interstate 95 corridor, including the Washington DC and Baltimore metro areas, in the very hot and unstable air mass ahead of a cold front approaching the region from the Ohio Valley. Some of these storms became severe as they approached the Tidal Potomac River and Maryland Chesapeake Bay, producing wind gusts in excess of 40 knots and even large hail along the western shore of the Bay. High pressure across the western Atlantic brought hot and humid conditions to the Mid Atlantic on July 10th. Showers and thunderstorms developed along and east of the Interstate 95 corridor, including the Washington DC and Baltimore metro areas, in the very hot and unstable air mass ahead of a cold front approaching the region from the Ohio Valley. Some of these storms became severe as they approached the Tidal Potomac River and Maryland Chesapeake Bay, producing wind gusts in excess of 40 knots and even large hail along the western shore of the Bay.\nEvent Narrative: A Trained Spotter reported downed trees in Linthicum Heights, MD, near the shore of the Bay. Trained Spotter reported quarter size hail in Linthicum Heights, MD near the shore of the Bay. Hail was also reported in the City of Baltimore near the Inner Harbor.", "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00093721, approximately 16.8263 km away, between 2007-07-10 12:35:00 and 2007-07-10 13:05:00. The events included records with hailstones measuring 30.4 inches.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 4000.0 and crop damage of 0.0. \n\nEpisode Narrative: High pressure across the western Atlantic brought hot and humid conditions to the Mid Atlantic on July 10th. Showers and thunderstorms developed along and east of the Interstate 95 corridor, including the Washington DC and Baltimore metro areas, in the very hot and unstable air mass ahead of a cold front approaching the region from the Ohio Valley. Some of these storms became severe, producing damaging winds and large hail across the eastern Baltimore metro and south across lower southern Maryland. High pressure across the western Atlantic brought hot and humid conditions to the Mid Atlantic on July 10th. Showers and thunderstorms developed along and east of the Interstate 95 corridor, including the Washington DC and Baltimore metro areas, in the very hot and unstable air mass ahead of a cold front approaching the region from the Ohio Valley. Some of these storms became severe, producing damaging winds and large hail across the eastern Baltimore metro and south across lower southern Maryland. High pressure across the western Atlantic brought hot and humid conditions to the Mid Atlantic on July 10th. Showers and thunderstorms developed along and east of the Interstate 95 corridor, including the Washington DC and Baltimore metro areas, in the very hot and unstable air mass ahead of a cold front approaching the region from the Ohio Valley. Some of these storms became severe, producing damaging winds and large hail across the eastern Baltimore metro and south across lower southern Maryland. High pressure across the western Atlantic brought hot and humid conditions to the Mid Atlantic on July 10th. Showers and thunderstorms developed along and east of the Interstate 95 corridor, including the Washington DC and Baltimore metro areas, in the very hot and unstable air mass ahead of a cold front approaching the region from the Ohio Valley. Some of these storms became severe, producing damaging winds and large hail across the eastern Baltimore metro and south across lower southern Maryland. High pressure across the western Atlantic brought hot and humid conditions to the Mid Atlantic on July 10th. Showers and thunderstorms developed along and east of the Interstate 95 corridor, including the Washington DC and Baltimore metro areas, in the very hot and unstable air mass ahead of a cold front approaching the region from the Ohio Valley. Some of these storms became severe, producing damaging winds and large hail across the eastern Baltimore metro and south across lower southern Maryland.\nEvent Narrative: Baltimore County Fire and Rescue Department reported multiple trees down in Cockeysville, MD. A Trained Spotter reported quarter size hail in Druid, MD. Mail measuring one half inch in diameter was reported in the northern portion of Baltimore City. A Trained Spotter reported trees down in northern Baltimore City. A Trained Spotter reported quarter size hail in Linthicum Heights, MD. A Trained Spotter reported trees down in Linthicum Heights, MD.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 38.0834 km away, between 2007-07-11 13:25:00 and 2007-07-11 13:30:00. The events included records with measured wind gusts of 34.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A slow moving cold front moving east across the Mid Atlantic combined with a hot and humid air mass to trigger showers and thunderstorms across the Maryland Chesapeake Bay. One storm moving across the Bay became severe, producing wind gusts in excess of 30 knots. Other strong thunderstorms over the Bay produced wind gusts around 20 to 25 knots.\nEvent Narrative: An Automated Observation from Stevensville, MD., measured a wind gust of 34 knots.", "The following events were reported: Hail, Thunderstorm Wind, Tornado. These occurred near station USW00093721, approximately 43.7689 km away, between 2007-07-16 16:32:00 and 2007-07-16 17:27:00. The events included records with hailstones measuring 33.666666666666664 inches.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 22000.0 and crop damage of 0.0. \n\nEpisode Narrative: A strong cold front moving east across the Ohio Valley stalled as it moved over the Mid Atlantic. This allowed numerous showers and thunderstorms to develop across the region during the afternoon of July 16th. Many of these storms became severe, producing large hail and damaging winds that downed large trees and power lines. One severe thunderstorm that moved across Harford County produced a tornado. A strong cold front moving east across the Ohio Valley stalled as it moved over the Mid Atlantic. This allowed numerous showers and thunderstorms to develop across the region during the afternoon of July 16th. Many of these storms became severe, producing large hail and damaging winds that downed large trees and power lines. One severe thunderstorm that moved across Harford County produced a tornado. A strong cold front moving east across the Ohio Valley stalled as it moved over the Mid Atlantic. This allowed numerous showers and thunderstorms to develop across the region during the afternoon of July 16th. Many of these storms became severe, producing large hail and damaging winds that downed large trees and power lines. One severe thunderstorm that moved across Harford County produced a tornado. A strong cold front moving east across the Ohio Valley stalled as it moved over the Mid Atlantic. This allowed numerous showers and thunderstorms to develop across the region during the afternoon of July 16th. Many of these storms became severe, producing large hail and damaging winds that downed large trees and power lines. One severe thunderstorm that moved across Harford County produced a tornado.\nEvent Narrative: Baltimore County Emergency Management reported a tree down near Corbett Road north of Phoenix, MD., and a tree down near Old York Road near Troyer, southeast of Monkton. A Newspaper reported that more than 40 trees were downed on private property off Corbett Road in Monkton. The home on the property sustained minor damages, including a broken window and missing roof shingles. Harford County Emergency Management reported multiple trees down near Connolly Road in Fallston. An NWS Storm Survey concluded that an EF1 tornado on the Enhanced Fujita Scale occurred near Fallston, MD., on July 16th. Maximum path width was 150 yards and the length was approximately 4 miles. There was extensive tree damage, with some softwood trees snapped and many hardwoods toppled. Structural damage observed was limited to trees and limbs falling onto structures. Many power lines were also downed. No injuries were reported. A Trained Spotter reported quarter size hail in Fallston.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 43.142 km away, between 2007-07-19 15:25:00 and 2007-07-19 15:30:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 3000.0 and crop damage of 0.0. \n\nEpisode Narrative: A warm and moist air mass settled over the Mid Atlantic as a strong cold front approached the region from the Ohio Valley on July 19th. This allowed scattered thunderstorms to develop across north central Virginia during the early afternoon hours and spread east into Maryland through the evening. Storms became better organized as they moved east across lower southern Maryland, eventually forming a bow echo. Surface winds with the bow echo were measured between 60 and 80 mph. These strong thunderstorm winds downed numerous trees and power lines across lower southern Maryland.\nEvent Narrative: Harford County Fire and Rescue reported trees and power lines down in Stockton and trees down in Jarrettsville.", "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00093721, approximately 48.9786 km away, between 2007-07-29 05:15:00 and 2007-07-29 05:25:00. The events included records with hailstones measuring 25.375 inches.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 20000.0 and crop damage of 0.0. \n\nEpisode Narrative: A cold front combined with an upper level low pressure system to trigger thunderstorms in Harford County during the early morning hours of July 29th. The first thunderstorm became severe, producing damaging winds and large hail. A second storm followed close behind and actually became a wet microburst. Significant wind damage was reported in Bel Air, MD. A cold front combined with an upper level low pressure system to trigger thunderstorms in Harford County during the early morning hours of July 29th. The first thunderstorm became severe, producing damaging winds and large hail. A second storm followed close behind and actually became a wet microburst. Significant wind damage was reported in Bel Air, MD.\nEvent Narrative: Harford County Emergency Management reported that a roof made of aluminum corrugated sheet metal was torn off building in downtown Bel Air in the 100 block of Business Route 1 and Archer Street. A large party tent was blown down nearby when its support ropes were snapped. A Cooperative Observer reported penny size hail in Bel Air.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 27.0862 km away, between 2007-08-03 14:34:00 and 2007-08-03 15:07:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Widely scattered showers and thunderstorms developed in a hot and humid air mass on the afternoon of August 3rd. A storm in Baltimore County became severe, downing trees and producing small hail. Widely scattered showers and thunderstorms developed in a hot and humid air mass on the afternoon of August 3rd. A storm in Baltimore County became severe, downing trees and producing small hail.\nEvent Narrative: Baltimore County officials reported a tree down in White Marsh. A Trained Spotter measured a wind gust of 58 mph, as well as half inch hail, in Rosedale. A Baltimore County official reported a tree down on Crafton Road in Essex.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 14.1982 km away, between 2007-08-03 15:03:00 and 2007-08-03 15:36:00. The events included records with measured wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Widely scattered showers and thunderstorms developed in a hot and humid air mass on the afternoon of August 3rd across northern Virginia and central Maryland. Some of these storms became severe as they approached the Tidal Potomac River and Maryland Chesapeake Bay, producing wind gusts in excess of 30 knots.\nEvent Narrative: A Trained Spotter measured a 50 knots wind gust and half inch hail in Rosedale, MD. The buoy at Francis Scott Key Bridge measured a wind gust of 34 knots.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 27.6384 km away, between 2007-08-05 17:45:00 and 2007-08-05 18:12:00. The events included records with measured wind gusts of 37.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front stalled over the Mid Atlantic kept moisture and unsettled conditions across the region. Scattered showers and thunderstorms developed across central Maryland and northern Virginia. Some of these storms became severe as they approached the Tidal Potomac River and Maryland Chesapeake Bay, producing wind gusts in excess of 30 knots. A cold front stalled over the Mid Atlantic kept moisture and unsettled conditions across the region. Scattered showers and thunderstorms developed across central Maryland and northern Virginia. Some of these storms became severe as they approached the Tidal Potomac River and Maryland Chesapeake Bay, producing wind gusts in excess of 30 knots.\nEvent Narrative: A buoy at Thomas Point Light measured a wind gust of 35 knots. An Automated Surface Observation at the US Naval Academy measured a wind gust of 34 knots. An Automated Surface Observation at the Patuxent River Naval Air Station measured a wind gust up to 39 knots. A buoy at Solomons Island measured a wind gust of 30 knots.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 20.9028 km away, between 2007-08-09 12:05:00 and 2007-08-09 12:54:00. The events included records with measured wind gusts of 37.5 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A strong cold front combined with a humid and unstable air mass across the Mid Atlantic on August 9th. Scattered showers and thunderstorms developed across northern Virginia and central Maryland during the late morning and spread east into the early and mid afternoon. Many of these storms became severe, producing wind gusts in excess of 30 knots and large hail over the Tidal Potomac River and Maryland Chesapeake Bay. A strong cold front combined with a humid and unstable air mass across the Mid Atlantic on August 9th. Scattered showers and thunderstorms developed across northern Virginia and central Maryland during the late morning and spread east into the early and mid afternoon. Many of these storms became severe, producing wind gusts in excess of 30 knots and large hail over the Tidal Potomac River and Maryland Chesapeake Bay.\nEvent Narrative: Automated Surface Observations and buoys reported several wind gusts between 30 and 40 knots from Pooles Island to Sandy Point. The buoy at Thomas Point light measured a wind gust of 35 knots. The buoy at Kent Island measured a wind gust of 30 knots.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 14.588 km away, between 2007-08-16 09:02:00 and 2007-08-16 09:30:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A very warm and humid air mass over the Mid Atlantic combined with an upper level disturbance during the mid morning hours of August 16th. Scattered showers and thunderstorms developed over north central Maryland and moved east towards the Baltimore metro. Some of these storms became severe, producing winds in excess of 30 knots across the Tidal Potomac River and Maryland Chesapeake Bay. A very warm and humid air mass over the Mid Atlantic combined with an upper level disturbance during the mid morning hours of August 16th. Scattered showers and thunderstorms developed over north central Maryland and moved east towards the Baltimore metro. Some of these storms became severe, producing winds in excess of 30 knots across the Tidal Potomac River and Maryland Chesapeake Bay.\nEvent Narrative: A wind gust of 38 knots was reported by a Maryland Department of Transportation sensor at the intersection of US Route 50 and MD Route 2 north of Annapolis. A wind gust of 34 knots was reported at Thomas Point Light. Several buoys and Automated Surface Observations reported wind gusts in excess of 30 knots.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 24.1377 km away, between 2007-08-25 17:15:00 and 2007-08-25 19:40:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 13000.0 and crop damage of 0.0. \n\nEpisode Narrative: A hot and humid air mass developed over the Mid Atlantic ahead of a strong cold front on August 25th. Temperatures climbed into the mid 90s by noon. These temperatures combined with high humidity created heat index values around 105. Showers and thunderstorms developed during the late afternoon as the cold front approached the region. Some of these storms became severe, producing large hail and damaging winds that downed trees and power lines. A hot and humid air mass developed over the Mid Atlantic ahead of a strong cold front on August 25th. Temperatures climbed into the mid 90s by noon. These temperatures combined with high humidity created heat index values around 105. Showers and thunderstorms developed during the late afternoon as the cold front approached the region. Some of these storms became severe, producing large hail and damaging winds that downed trees and power lines. A hot and humid air mass developed over the Mid Atlantic ahead of a strong cold front on August 25th. Temperatures climbed into the mid 90s by noon. These temperatures combined with high humidity created heat index values around 105. Showers and thunderstorms developed during the late afternoon as the cold front approached the region. Some of these storms became severe, producing large hail and damaging winds that downed trees and power lines. A hot and humid air mass developed over the Mid Atlantic ahead of a strong cold front on August 25th. Temperatures climbed into the mid 90s by noon. These temperatures combined with high humidity created heat index values around 105. Showers and thunderstorms developed during the late afternoon as the cold front approached the region. Some of these storms became severe, producing large hail and damaging winds that downed trees and power lines. A hot and humid air mass developed over the Mid Atlantic ahead of a strong cold front on August 25th. Temperatures climbed into the mid 90s by noon. These temperatures combined with high humidity created heat index values around 105. Showers and thunderstorms developed during the late afternoon as the cold front approached the region. Some of these storms became severe, producing large hail and damaging winds that downed trees and power lines.\nEvent Narrative: Carroll County Emergency Management reported trees down throughout the county, including between Mount Airy and Winfield. Emergency Management reports tress down across the county. Baltimore County Emergency Management reported power lines down in Reisterstown, MD. A Trained Spotter reported wind damage near Edwin Raynor Road and Mountain Road in Pasadena, MD. Baltimore Emergency Management reported trees down in the City of Baltimore.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 22.623 km away, between 2007-08-25 18:09:00 and 2007-08-25 20:18:00. The events included records with measured wind gusts of 45.333333333333336 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A hot and humid air mass developed over the Mid Atlantic ahead of a cold front on August 25th. Showers and thunderstorms developed across northern Virginia and central Maryland during the late afternoon and pushed east towards the Tidal Potomac River and Maryland Chesapeake Bay during the evening and overnight hours. Some of these storms became severe, producing wind gusts in excess of 30 knots. A hot and humid air mass developed over the Mid Atlantic ahead of a cold front on August 25th. Showers and thunderstorms developed across northern Virginia and central Maryland during the late afternoon and pushed east towards the Tidal Potomac River and Maryland Chesapeake Bay during the evening and overnight hours. Some of these storms became severe, producing wind gusts in excess of 30 knots. A hot and humid air mass developed over the Mid Atlantic ahead of a cold front on August 25th. Showers and thunderstorms developed across northern Virginia and central Maryland during the late afternoon and pushed east towards the Tidal Potomac River and Maryland Chesapeake Bay during the evening and overnight hours. Some of these storms became severe, producing wind gusts in excess of 30 knots.\nEvent Narrative: Automated Surface Observations and buoys reported wind gusts between 32 and 45 knots. Automated Surface Observations and buoys reported wind gusts between 31 and 48 knots. Buoys reported wind gusts between 34 and 43 knots.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 48.241 km away, between 2007-08-25 20:00:00 and 2007-08-25 20:06:00. The events included records with estimated wind gusts of 55.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: An area of low pressure moved across the eastern Great Lakes region during the morning of August 25th. A cold front associated with this low pressure system was located in the Ohio Valley. A hot and especially humid airmass was found ahead of this front across the Middle Atlantic region on August 25th. As the front approached, showers and thunderstorms developed and several of the storms became severe. The actual cold front however did not clear the region until the morning of the 26th. An area of low pressure moved across the eastern Great Lakes region during the morning of August 25th. A cold front associated with this low pressure system was located in the Ohio Valley. A hot and especially humid airmass was found ahead of this front across the Middle Atlantic region on August 25th. As the front approached, showers and thunderstorms developed and several of the storms became severe. The actual cold front however did not clear the region until the morning of the 26th.\nEvent Narrative: A severe thunderstorm rumbled through Kent County during the evening of the 25th. Strong winds associated with this severe thunderstorm knocked down trees on Eastern Neck Island at 9:00 PM EDT. A severe thunderstorm tore through Queen Anne's County during the evening of the 25th. Damaging winds associated with this severe thunderstorm knocked down trees and power lines throughout the county. The most damage was located in Centreville and also between Queenstown and Queen Anne. County Officials reported that there was structural damage to several barns along with overturned farm equipment. As a result of the damaging winds, two horses were killed while another horse was injured.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 42.0564 km away, between 2007-10-09 20:28:00 and 2007-10-09 20:28:00. The events included records with estimated wind gusts of 34.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front moving across the Mid Atlantic triggered scattered thunderstorms across northern Virginia and central Maryland. These storms produced wind gusts in excess of 30 knots as they pushed east across the Tidal Potomac River and the Maryland Chesapeake Bay.\nEvent Narrative: A buoy at Kent Island reported a wind gust in excess of 30 knots.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 28.7549 km away, between 2007-10-19 20:30:00 and 2007-10-19 21:21:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front pushing east from the Ohio Valley moved across the Mid Atlantic October 19th. Strong thunderstorms associated with this front produced wind gusts in excess of 40 knots as they moved across the Tidal Potomac River and Maryland Chesapeake Bay during the late evening. A cold front pushing east from the Ohio Valley moved across the Mid Atlantic October 19th. Strong thunderstorms associated with this front produced wind gusts in excess of 40 knots as they moved across the Tidal Potomac River and Maryland Chesapeake Bay during the late evening. A cold front pushing east from the Ohio Valley moved across the Mid Atlantic October 19th. Strong thunderstorms associated with this front produced wind gusts in excess of 40 knots as they moved across the Tidal Potomac River and Maryland Chesapeake Bay during the late evening. A cold front pushing east from the Ohio Valley moved across the Mid Atlantic October 19th. Strong thunderstorms associated with this front produced wind gusts in excess of 40 knots as they moved across the Tidal Potomac River and Maryland Chesapeake Bay during the late evening. A cold front pushing east from the Ohio Valley moved across the Mid Atlantic October 19th. Strong thunderstorms associated with this front produced wind gusts in excess of 40 knots as they moved across the Tidal Potomac River and Maryland Chesapeake Bay during the late evening.\nEvent Narrative: The buoy at Stevensville measured a wind gust of 35 knots. The buoy at Tolchester Beach reported wind gusts in excess of 30 knots. Automated surface observations and buoys from Annapolis to Thomas Point Light measured several wind gusts in excess of 30 knots. The buoy at the Francis Scott Key Bridge measured wind gusts up to 40 knots. The automated surface observation at Martin State Airport measured a wind gust of 34 knots.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 14.2666 km away, between 2007-11-27 00:06:00 and 2007-11-27 01:00:00. The events included records with estimated wind gusts of 34.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front moving from west to east across the Mid Atlantic triggered showers and isolated thunderstorms during the early morning hours of November 27th. Some of the storms that crossed the Tidal Potomac River and Maryland Chesapeake Bay produced wind gusts in excess of 30 knots.\nEvent Narrative: A buoy at Baltimore Key Bridge measured wind gusts in excess of 30 knots.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 14.2666 km away, between 2008-01-15 14:12:00 and 2008-01-15 14:13:00. The events included records with estimated wind gusts of 34.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Snow squalls crossed the Tidal Potomac River and Maryland Chesapeake Bay during the early afternoon hours on January 15th. Wind gusts near 40 knots were measured across the waters.\nEvent Narrative: A buoy near Key Bridge reported a wind gust near 34 knots.", "The following events were reported: Flood. These occurred near station USW00093721, approximately 25.1022 km away, between 2008-02-01 16:00:00 and 2008-02-01 18:00:00. The flood was caused by Heavy Rain. Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: An area of low pressure over the Lower Mississippi River Valley moved up the Appalachians on February 1st. Warmer temperatures aloft combined with subfreezing temperatures at the surface to produce widespread freezing rain across the Mid Atlantic. A quarter of an inch of ice was reported in western Allegany County, with between a trace to a tenth of an inch as far east as northern Baltimore County. Numerous traffic accidents and power outages were reported across the region.||Precipitation continued through the afternoon and early evening as temperatures rose above freezing. Rainfall amounts between 1 and 3 inches were measured across much of Maryland, with highest amounts from the Baltimore metro area south through lower southern Maryland. Flooding was reported in Baltimore County. An area of low pressure over the Lower Mississippi River Valley moved up the Appalachians on February 1st. Warmer temperatures aloft combined with subfreezing temperatures at the surface to produce widespread freezing rain across the Mid Atlantic. A quarter of an inch of ice was reported in western Allegany County, with between a trace to a tenth of an inch as far east as northern Baltimore County. Numerous traffic accidents and power outages were reported across the region.||Precipitation continued through the afternoon and early evening as temperatures rose above freezing. Rainfall amounts between 1 and 3 inches were measured across much of Maryland, with highest amounts from the Baltimore metro area south through lower southern Maryland. Flooding was reported in Baltimore County.\nEvent Narrative: Baltimore County Fire and Rescue reported flooding and a road closure at the intersection of Ruxton Road and Circle Road in Towson. Baltimore County Fire and Rescue reported flooding and a road closure at the intersection of Race Road and Golden Ring Road in Rosedale.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 30.1781 km away, between 2008-02-07 00:00:00 and 2008-02-07 00:45:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Showers and thunderstorms moved across the Mid Atlantic region during the overnight hours of February 6th through early February 7th. These storms produced wind gusts in excess of 30 knots across portions of the Tidal Potomac River and Maryland Chesapeake Bay. Showers and thunderstorms moved across the Mid Atlantic region during the overnight hours of February 6th through early February 7th. These storms produced wind gusts in excess of 30 knots across portions of the Tidal Potomac River and Maryland Chesapeake Bay. Showers and thunderstorms moved across the Mid Atlantic region during the overnight hours of February 6th through early February 7th. These storms produced wind gusts in excess of 30 knots across portions of the Tidal Potomac River and Maryland Chesapeake Bay. Showers and thunderstorms moved across the Mid Atlantic region during the overnight hours of February 6th through early February 7th. These storms produced wind gusts in excess of 30 knots across portions of the Tidal Potomac River and Maryland Chesapeake Bay. Showers and thunderstorms moved across the Mid Atlantic region during the overnight hours of February 6th through early February 7th. These storms produced wind gusts in excess of 30 knots across portions of the Tidal Potomac River and Maryland Chesapeake Bay. Showers and thunderstorms moved across the Mid Atlantic region during the overnight hours of February 6th through early February 7th. These storms produced wind gusts in excess of 30 knots across portions of the Tidal Potomac River and Maryland Chesapeake Bay.\nEvent Narrative: An automated observation at Kent Island High School measured a wind gust of 39 knots. An automated observation from the Maryland Department of Transportation at US-50 and MD-2 in Arnold measured a wind gust of 34 knots. An automated observation at Hart Miller Island reported a wind gust in excess of 34 knots. An automated observation in Stevensville reported a wind gusts in excess of 30 knots. The buoy at Thomas Point Light measured a wind gust of 45 knots. The buoy at Baltimore Key Bridge reported a wind gust in excess of 34 knots.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 36.9916 km away, between 2008-02-18 15:59:00 and 2008-02-18 16:05:00. The events included records with estimated wind gusts of 34.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front moving southeast across the Mid Atlantic triggered scattered showers and thunderstorms on the afternoon of February 18th. The stronger thunderstorms produced wind gusts in excess of 30 knots.\nEvent Narrative: The buoy at Thomas Point Light measured a wind gust in excess of 30 knots.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 19.4582 km away, between 2008-03-05 01:15:00 and 2008-03-05 01:30:00.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 22000.0 and crop damage of 0.0. \n\nEpisode Narrative: An area of low pressure moving over West Virginia pushed a strong cold front through the region during the early morning hours of March 5th. This front triggered several strong to severe thunderstorms with gusty winds as well as heavy rain. Several lines of thunderstorms crossed the region from the evening of March 4th through the early morning of March 5th. Heavy rain lead to several road closures due to flooding and several flooded basements. Wind gusts in excess of 50 mph were measured at several locations, with a maximum wind gust of 73 mph measured in White Plains, MD. There were numerous reports of trees and power lines down across northern and central Maryland. The most significant wind damage occurred in St. Mary\ufffd\ufffd\ufffds County, with numerous trees and power lines downed and several homes destroyed. Storm surveys in St. Marys County were conducted by NWS and St. Marys Country Emergency Management. An area of low pressure moving over West Virginia pushed a strong cold front through the region during the early morning hours of March 5th. This front triggered several strong to severe thunderstorms with gusty winds as well as heavy rain. Several lines of thunderstorms crossed the region from the evening of March 4th through the early morning of March 5th. Heavy rain lead to several road closures due to flooding and several flooded basements. Wind gusts in excess of 50 mph were measured at several locations, with a maximum wind gust of 73 mph measured in White Plains, MD. There were numerous reports of trees and power lines down across northern and central Maryland. The most significant wind damage occurred in St. Mary\ufffd\ufffd\ufffds County, with numerous trees and power lines downed and several homes destroyed. Storm surveys in St. Marys County were conducted by NWS and St. Marys Country Emergency Management. An area of low pressure moving over West Virginia pushed a strong cold front through the region during the early morning hours of March 5th. This front triggered several strong to severe thunderstorms with gusty winds as well as heavy rain. Several lines of thunderstorms crossed the region from the evening of March 4th through the early morning of March 5th. Heavy rain lead to several road closures due to flooding and several flooded basements. Wind gusts in excess of 50 mph were measured at several locations, with a maximum wind gust of 73 mph measured in White Plains, MD. There were numerous reports of trees and power lines down across northern and central Maryland. The most significant wind damage occurred in St. Mary\ufffd\ufffd\ufffds County, with numerous trees and power lines downed and several homes destroyed. Storm surveys in St. Marys County were conducted by NWS and St. Marys Country Emergency Management.\nEvent Narrative: Harford County Emergency Management reported over a dozen trees and power lines down across the county. Reports began in Joppa and spread northeast. A Maryland Department of Transportation automated observation measured a wind gust of 58 mph in Glen Burnie at the intersection of Interstate 97 and Route 100. Baltimore City Fire reported 2 trees down within the city.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 49.3165 km away, between 2008-03-05 01:15:00 and 2008-03-05 01:30:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A squall line of severe thunderstorms moved across the Delmarva Peninsula overnight on the 4th and produced wind damage.\nEvent Narrative: A line of severe thunderstorms knocked down several trees, tree limbs, poles and wires in southwestern Queen Anne's County from Queenstown to Centreville. About 300 Delmarva Power and Light customers lost power because of the wind damage.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 28.3818 km away, between 2008-03-05 01:21:00 and 2008-03-05 01:21:00. The events included records with measured wind gusts of 56.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: An area of low pressure moving over West Virginia pushed a strong cold front through the region during the early morning hours of March 5th. This front triggered several strong to severe thunderstorms with gusty winds in excess of 50 knots. Numerous locations reported sustained wind speeds and gusts in excess of 35 knots, but a gale Warning was in effect for the overnight hours.\nEvent Narrative: An automated observation in Hart/Millers Island measured a wind gust of 56 knots.", "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00093721, approximately 29.7867 km away, between 2008-03-08 16:00:00 and 2008-03-08 17:00:00. The events included records with hailstones measuring 46.638888888888886 inches.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 55000.0 and crop damage of 0.0. \n\nEpisode Narrative: Low pressure crossed the Mid Atlantic March 8th, bringing a strong cold front through the region during the late afternoon and evening. This front triggered several strong to severe thunderstorms that produced large hail and gusty, damaging winds. There were numerous reports of downed trees and power lines, with several reports of trees falling into homes. One fatality was reported in Harford County when a tree fell onto a moving truck, killing the passenger. Low pressure crossed the Mid Atlantic March 8th, bringing a strong cold front through the region during the late afternoon and evening. This front triggered several strong to severe thunderstorms that produced large hail and gusty, damaging winds. There were numerous reports of downed trees and power lines, with several reports of trees falling into homes. One fatality was reported in Harford County when a tree fell onto a moving truck, killing the passenger. Low pressure crossed the Mid Atlantic March 8th, bringing a strong cold front through the region during the late afternoon and evening. This front triggered several strong to severe thunderstorms that produced large hail and gusty, damaging winds. There were numerous reports of downed trees and power lines, with several reports of trees falling into homes. One fatality was reported in Harford County when a tree fell onto a moving truck, killing the passenger. Low pressure crossed the Mid Atlantic March 8th, bringing a strong cold front through the region during the late afternoon and evening. This front triggered several strong to severe thunderstorms that produced large hail and gusty, damaging winds. There were numerous reports of downed trees and power lines, with several reports of trees falling into homes. One fatality was reported in Harford County when a tree fell onto a moving truck, killing the passenger. Low pressure crossed the Mid Atlantic March 8th, bringing a strong cold front through the region during the late afternoon and evening. This front triggered several strong to severe thunderstorms that produced large hail and gusty, damaging winds. There were numerous reports of downed trees and power lines, with several reports of trees falling into homes. One fatality was reported in Harford County when a tree fell onto a moving truck, killing the passenger. Low pressure crossed the Mid Atlantic March 8th, bringing a strong cold front through the region during the late afternoon and evening. This front triggered several strong to severe thunderstorms that produced large hail and gusty, damaging winds. There were numerous reports of downed trees and power lines, with several reports of trees falling into homes. One fatality was reported in Harford County when a tree fell onto a moving truck, killing the passenger. Low pressure crossed the Mid Atlantic March 8th, bringing a strong cold front through the region during the late afternoon and evening. This front triggered several strong to severe thunderstorms that produced large hail and gusty, damaging winds. There were numerous reports of downed trees and power lines, with several reports of trees falling into homes. One fatality was reported in Harford County when a tree fell onto a moving truck, killing the passenger. Low pressure crossed the Mid Atlantic March 8th, bringing a strong cold front through the region during the late afternoon and evening. This front triggered several strong to severe thunderstorms that produced large hail and gusty, damaging winds. There were numerous reports of downed trees and power lines, with several reports of trees falling into homes. One fatality was reported in Harford County when a tree fell onto a moving truck, killing the passenger. Low pressure crossed the Mid Atlantic March 8th, bringing a strong cold front through the region during the late afternoon and evening. This front triggered several strong to severe thunderstorms that produced large hail and gusty, damaging winds. There were numerous reports of downed trees and power lines, with several reports of trees falling into homes. One fatality was reported in Harford County when a tree fell onto a moving truck, killing the passenger.\nEvent Narrative: A trained spotter reported trees down in Finksburg. Harford County Fire and Rescue reported trees and power lines down in Bel Air. A trained spotter reported numerous trees down in Edgewater. A roof was blown off a building. An automated observation in Severn measured a wind gust of 68 mph. Several sheds were damaged when six trees were uprooted and another 6 trees snapped off at the base on Almart Road in in Owings Mills. An NWS employee reported a large downed tree blocking the right lane of Interstate 70 at Route 32. An automated observation at the Maryland Emergency Management (MEMA) building measured a wind gust of 59 mph. A trained spotter reported trees down in Cockeysville.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 26.7638 km away, between 2008-04-11 22:08:00 and 2008-04-11 22:18:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A warm front moved north of the region April 11th. Scattered showers and thunderstorms developed in the wake of the warm front in advance of a strengthening cold front to the west. These storms moved east of the Tidal Potomac and Maryland Chesapeake Bay, producing wind gusts between 30 and 45 knots. A warm front moved north of the region April 11th. Scattered showers and thunderstorms developed in the wake of the warm front in advance of a strengthening cold front to the west. These storms moved east of the Tidal Potomac and Maryland Chesapeake Bay, producing wind gusts between 30 and 45 knots. A warm front moved north of the region April 11th. Scattered showers and thunderstorms developed in the wake of the warm front in advance of a strengthening cold front to the west. These storms moved east of the Tidal Potomac and Maryland Chesapeake Bay, producing wind gusts between 30 and 45 knots.\nEvent Narrative: The buoy at Thomas Point Light measured a wind gust of 44 knots. A mesonet observation at Anne Arundel County Club in Glen Burnie estimated a wind gust of 34 knots. The buoy at Tolchester Beach reported a wind gust near 34 knots.", "The following events were reported: Hail, Lightning, Thunderstorm Wind. These occurred near station USW00093721, approximately 27.5034 km away, between 2008-04-20 13:25:00 and 2008-04-20 17:30:00. The events included records with hailstones measuring 37.6875 inches.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 38000.0 and crop damage of 0.0. \n\nEpisode Narrative: A deep low pressure system moving east across the Great Lakes pushed a strong cold front across the region on late April 20th into early April 21st. Numerous strong to severe thunderstorms developed during the afternoon and evening hours across the region and continued into the following morning. High moisture content and training storms lead to flooding across potions of the region with several road closures due to high water. Several storms produced damaging winds that downed trees and power lines. There were also two confirmed tornadoes in Charles and Prince Georges counties. A deep low pressure system moving east across the Great Lakes pushed a strong cold front across the region on late April 20th into early April 21st. Numerous strong to severe thunderstorms developed during the afternoon and evening hours across the region and continued into the following morning. High moisture content and training storms lead to flooding across potions of the region with several road closures due to high water. Several storms produced damaging winds that downed trees and power lines. There were also two confirmed tornadoes in Charles and Prince Georges counties. A deep low pressure system moving east across the Great Lakes pushed a strong cold front across the region on late April 20th into early April 21st. Numerous strong to severe thunderstorms developed during the afternoon and evening hours across the region and continued into the following morning. High moisture content and training storms lead to flooding across potions of the region with several road closures due to high water. Several storms produced damaging winds that downed trees and power lines. There were also two confirmed tornadoes in Charles and Prince Georges counties. A deep low pressure system moving east across the Great Lakes pushed a strong cold front across the region on late April 20th into early April 21st. Numerous strong to severe thunderstorms developed during the afternoon and evening hours across the region and continued into the following morning. High moisture content and training storms lead to flooding across potions of the region with several road closures due to high water. Several storms produced damaging winds that downed trees and power lines. There were also two confirmed tornadoes in Charles and Prince Georges counties. A deep low pressure system moving east across the Great Lakes pushed a strong cold front across the region on late April 20th into early April 21st. Numerous strong to severe thunderstorms developed during the afternoon and evening hours across the region and continued into the following morning. High moisture content and training storms lead to flooding across potions of the region with several road closures due to high water. Several storms produced damaging winds that downed trees and power lines. There were also two confirmed tornadoes in Charles and Prince Georges counties. A deep low pressure system moving east across the Great Lakes pushed a strong cold front across the region on late April 20th into early April 21st. Numerous strong to severe thunderstorms developed during the afternoon and evening hours across the region and continued into the following morning. High moisture content and training storms lead to flooding across potions of the region with several road closures due to high water. Several storms produced damaging winds that downed trees and power lines. There were also two confirmed tornadoes in Charles and Prince Georges counties.\nEvent Narrative: Baltimore County Emergency Management reported trees down at the intersection of Dalecrest Court and Chetwood Drive. Baltimore County Emergency Management reported trees down at the intersection of Wight Ave and McCormick Road. A newspaper reported that lightning struck a home under construction on Wrights Mill Road in Randallstown. A newspaper reported that a 2-story house on the 770 block of Ricker Road was struck by lightning and caught fire. Baltimore County Emergency Management reported trees down at the intersection of Ruxton Road and Alvern Ave.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 33.4301 km away, between 2008-04-20 16:58:00 and 2008-04-20 16:58:00. The events included records with measured wind gusts of 40.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A deep low pressure system moving east across the Great Lakes pushed a strong cold front across the region on late April 20th into early April 21st. Numerous strong to severe thunderstorms developed during the afternoon and evening hours across the region and continued into the following morning. These storms produced wind gusts in excess of 30 knots.\nEvent Narrative: The automated observation at Tolly Point measured a wind gust of 40 knots.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 13.3822 km away, between 2008-04-28 14:17:00 and 2008-04-28 14:17:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 5000.0 and crop damage of 0.0. \n\nEpisode Narrative: A weak cold front crossed the Mid Atlantic on April 28th, triggering scattered showers and thunderstorms across lower southern Maryland. A storm over Anne Arundel County became severe, producing damaging winds that downed trees near Maryland City.\nEvent Narrative: Anne Arundel County Emergency Management reported trees down on the southbound lane of the Baltimore/Washington parkway at Route 198.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 35.2109 km away, between 2008-05-09 03:58:00 and 2008-05-09 04:06:00. The events included records with measured wind gusts of 35.5 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A strong low pressure system crossed the Mid Atlantic during the afternoon and evening hours of May 8th and into the early morning hours of May 9th. This system along with warm temperatures and high dew points triggered numerous strong to severe showers and thunderstorms across the region. Thunderstorms that moved over the Tidal Potomac River and Maryland Chesapeake Bay produced wind gusts to nearly 50 knots. A strong low pressure system crossed the Mid Atlantic during the afternoon and evening hours of May 8th and into the early morning hours of May 9th. This system along with warm temperatures and high dew points triggered numerous strong to severe showers and thunderstorms across the region. Thunderstorms that moved over the Tidal Potomac River and Maryland Chesapeake Bay produced wind gusts to nearly 50 knots.\nEvent Narrative: The automated observation at Tolly Point measured a wind gust of 34 knots. The buoy at Thomas Point Light measured a peak wind gust of 37 knots.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 29.6208 km away, between 2008-05-09 04:05:00 and 2008-05-09 04:05:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 15000.0 and crop damage of 0.0. \n\nEpisode Narrative: A strong low pressure system crossed the Mid Atlantic during the afternoon and evening hours of May 8th. This system along with warm temperatures and high dew points triggered numerous strong to severe showers and thunderstorms across the region. Several storms produced damaging winds that downed trees and power lines in lower southern Maryland. A few locations reported flooding as storms trained over the same area through the afternoon and evening.\nEvent Narrative: The public reported roof and trailer damage at the foot of the Bay Bridge.", "The following events were reported: Marine High Wind. These occurred near station USW00093721, approximately 37.6083 km away, between 2008-05-11 23:00:00 and 2008-05-12 01:00:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 10000.0 and crop damage of 0.0. \n\nEpisode Narrative: A potent storm system crossed the region May 12th. Warm and moist air filtered in ahead of the system, bringing widespread showers and thunderstorms with heavy rain. The pressure gradient with the low pressure system produced strong gusty winds across the Tidal Potomac River and Maryland Chesapeake Bay late on the 11th and into the early morning hours of the 12th. The Coast Guard received a call of a 49-ft ship with a broken mast suffered during one storm in the West River portion of the Chesapeake Bay. They rescued 14 midshipmen and coaches, but none were injured.\nEvent Narrative: The Coast Guard rescued a crew of 14 midshipmen and their coaches when a gust of wind broke the mast of their 49 ft ship. No injuries were reported.", "The following events were reported: Flood. These occurred near station USW00093721, approximately 28.8739 km away, between 2008-05-12 00:00:00 and 2008-05-12 14:00:00. The flood was caused by Heavy Rain. Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 100000.0 and crop damage of 0.0. \n\nEpisode Narrative: A potent storm system crossed the region May 12th. Warm and moist air filtered in ahead of the system, bringing widespread showers and thunderstorms with heavy rain. Heavy rain began to overspread the region during the evening of the 11th and continued through the morning of the 12th. The pressure gradient with the low pressure system produced strong gusty winds across lower southern Maryland during the late evening. With the ground already saturated dozens of trees and power lines fell across the region. ||The tight pressure gradient and strong southeasterly flow, despite the quarter moon phase, allowed tidal departures of 2 feet or more along the Maryland Chesapeake Bay in lower southern Maryland. Several roads were closed and homes flooded due to the high tides. A potent storm system crossed the region May 12th. Warm and moist air filtered in ahead of the system, bringing widespread showers and thunderstorms with heavy rain. Heavy rain began to overspread the region during the evening of the 11th and continued through the morning of the 12th. The pressure gradient with the low pressure system produced strong gusty winds across lower southern Maryland during the late evening. With the ground already saturated dozens of trees and power lines fell across the region. ||The tight pressure gradient and strong southeasterly flow, despite the quarter moon phase, allowed tidal departures of 2 feet or more along the Maryland Chesapeake Bay in lower southern Maryland. Several roads were closed and homes flooded due to the high tides. A potent storm system crossed the region May 12th. Warm and moist air filtered in ahead of the system, bringing widespread showers and thunderstorms with heavy rain. Heavy rain began to overspread the region during the evening of the 11th and continued through the morning of the 12th. The pressure gradient with the low pressure system produced strong gusty winds across lower southern Maryland during the late evening. With the ground already saturated dozens of trees and power lines fell across the region. ||The tight pressure gradient and strong southeasterly flow, despite the quarter moon phase, allowed tidal departures of 2 feet or more along the Maryland Chesapeake Bay in lower southern Maryland. Several roads were closed and homes flooded due to the high tides. A potent storm system crossed the region May 12th. Warm and moist air filtered in ahead of the system, bringing widespread showers and thunderstorms with heavy rain. Heavy rain began to overspread the region during the evening of the 11th and continued through the morning of the 12th. The pressure gradient with the low pressure system produced strong gusty winds across lower southern Maryland during the late evening. With the ground already saturated dozens of trees and power lines fell across the region. ||The tight pressure gradient and strong southeasterly flow, despite the quarter moon phase, allowed tidal departures of 2 feet or more along the Maryland Chesapeake Bay in lower southern Maryland. Several roads were closed and homes flooded due to the high tides.\nEvent Narrative: Anne Arundel Emergency Management as well as newspapers reported widespread flooding that closed roads across Anne Arundel County. There were several water rescues with cars washed away and driven into flooded roadways. Montgomery County Emergency Management and newspapers reported numerous roads closed due to high water, especially in eastern portions of the county towards the Prince Georges County line. Harford County Emergency Management numerous road closures across the county due to high water. Stoney Run in Patapsco Valley State Park overflowed its banks, leaving Furnace Ave. under 2 feet of water.", "The following events were reported: Hail. These occurred near station USW00093721, approximately 24.4163 km away, between 2008-05-18 16:09:00 and 2008-05-18 16:10:00. The events included records with hailstones measuring 0.75 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front crossed the Mid Atlantic from west to east during the late evening of May 18th. Scattered strong thunderstorms developed ahead of the front. One of the storms produced hail in southern Baltimore County.\nEvent Narrative: A trained spotter reported penny-size hail at Reisterstown Road just northwest of Interstate 695.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 32.7576 km away, between 2008-05-21 17:48:00 and 2008-05-21 18:12:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Scattered showers and thunderstorms developed in the wake of a cold front as an upper low pressure system intensified on May 21st. These storms produce wind gusts to nearly 50 knots over portions of the Tidal Potomac River and Maryland Chesapeake Bay during the early evening hours. Scattered showers and thunderstorms developed in the wake of a cold front as an upper low pressure system intensified on May 21st. These storms produce wind gusts to nearly 50 knots over portions of the Tidal Potomac River and Maryland Chesapeake Bay during the early evening hours. Scattered showers and thunderstorms developed in the wake of a cold front as an upper low pressure system intensified on May 21st. These storms produce wind gusts to nearly 50 knots over portions of the Tidal Potomac River and Maryland Chesapeake Bay during the early evening hours. Scattered showers and thunderstorms developed in the wake of a cold front as an upper low pressure system intensified on May 21st. These storms produce wind gusts to nearly 50 knots over portions of the Tidal Potomac River and Maryland Chesapeake Bay during the early evening hours.\nEvent Narrative: The automated observation at Hart/Millers Island measured a wind gust of 38 knots. The buoy at Thomas Point Light reported a wind gust in excess of 30 knots. The automated observation at the US Naval Academy in Annapolis measured a wind gust of 34 knots. The buoy at Tolchester Beach measured a wind gust of 36 knots.", "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00093721, approximately 26.0877 km away, between 2008-05-31 12:25:00 and 2008-05-31 13:50:00. The events included records with hailstones measuring 17.166666666666668 inches.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 1000.0 and crop damage of 0.0. \n\nEpisode Narrative: A cold front moved south across the Mid Atlantic on May 31st. Scattered to numerous showers and thunderstorms developed ahead of the cold front. Several of these storms became severe, producing damaging winds that downed trees and power lines and large hail over an inch in diameter. A cold front moved south across the Mid Atlantic on May 31st. Scattered to numerous showers and thunderstorms developed ahead of the cold front. Several of these storms became severe, producing damaging winds that downed trees and power lines and large hail over an inch in diameter. A cold front moved south across the Mid Atlantic on May 31st. Scattered to numerous showers and thunderstorms developed ahead of the cold front. Several of these storms became severe, producing damaging winds that downed trees and power lines and large hail over an inch in diameter.\nEvent Narrative: An amateur radio operator reported penny sized hail at the Duncan Gap Campground. A trained spotter reported penny sized hail in Edgewater. An amateur radio operator reported a tree down in Lothian.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 47.1467 km away, between 2008-05-31 13:00:00 and 2008-05-31 13:00:00. The events included records with estimated wind gusts of 55.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front gradually moved through the region during the afternoon and evening of the 31st. Ahead of this front, showers and thunderstorms occurred mainly in the afternoon. Some of the thunderstorms turned locally severe given the unstable air mass that was in place.\nEvent Narrative: A line of showers and thunderstorms raced east southeastward across Maryland during the afternoon of the 31st. Some of the thunderstorms producing locally very strong wind gusts, which knocked down numerous trees in Gransonville at around 2:00 PM EDT.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 14.3202 km away, between 2008-06-01 13:44:00 and 2008-06-01 15:06:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A strong upper level disturbance moved across the Mid Atlantic during the afternoon and evening hours of June 1st. This system along with high dew points and an unstable atmosphere sparked scattered strong to severe thunderstorms. These thunderstorms produced gusty winds across the Tidal Potomac River and Maryland Chesapeake Bay. The highest wind gust of 51 knots was recorded at Point Lookout. A strong upper level disturbance moved across the Mid Atlantic during the afternoon and evening hours of June 1st. This system along with high dew points and an unstable atmosphere sparked scattered strong to severe thunderstorms. These thunderstorms produced gusty winds across the Tidal Potomac River and Maryland Chesapeake Bay. The highest wind gust of 51 knots was recorded at Point Lookout.\nEvent Narrative: An automated observation in Baltimore City measured a wind gust of 35 KT. The buoy at Baltimore Key Bridge reported a wind gust in excess of 30 KT.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 21.4939 km away, between 2008-06-01 15:55:00 and 2008-06-01 15:55:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 3000.0 and crop damage of 0.0. \n\nEpisode Narrative: A strong upper level disturbance moved across the Mid Atlantic during the afternoon and evening hours of June 1st. This system along with high dew points and an unstable atmosphere sparked scattered strong to severe thunderstorms. A few thunderstorms resulted in downed trees and power lines.\nEvent Narrative: Anne Arundel County Emergency Management reported trees down into telephone wires on Crownsville Road near Chesterfield Road.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 36.9916 km away, between 2008-06-03 19:50:00 and 2008-06-03 20:07:00. The events included records with measured wind gusts of 36.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front approached the Mid Atlantic during the evening of June 3. Warm, moist and unstable air developed ahead of the front, allowing scattered strong to severe thunderstorms to develop. These thunderstorms produced gusty winds of 30 to 40 knots across the Tidal Potomac River and Maryland Chesapeake Bay. A waterspout was also observed near Indian Head.\nEvent Narrative: The buoy at Thomas Point Light measured a wind gust of 36 KT.", "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00093721, approximately 25.1659 km away, between 2008-06-04 14:24:00 and 2008-06-04 20:48:00. The events included records with hailstones measuring 48.87 inches.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 336000.0 and crop damage of 0.0. \n\nEpisode Narrative: A stalled front resided across the Mid Atlantic during the afternoon and evening of June 4th, allowing moisture and instability to pool along the boundary. This combined with several strong upper level disturbances resulted in numerous thunderstorms during the afternoon and evening. Many of these thunderstorms became severe. While penny sized was reported in spots, damaging winds from the thunderstorms was widespread. An EF-0 tornado was also confirmed in the community of Chesapeake Beach in Calvert County. A stalled front resided across the Mid Atlantic during the afternoon and evening of June 4th, allowing moisture and instability to pool along the boundary. This combined with several strong upper level disturbances resulted in numerous thunderstorms during the afternoon and evening. Many of these thunderstorms became severe. While penny sized was reported in spots, damaging winds from the thunderstorms was widespread. An EF-0 tornado was also confirmed in the community of Chesapeake Beach in Calvert County. A stalled front resided across the Mid Atlantic during the afternoon and evening of June 4th, allowing moisture and instability to pool along the boundary. This combined with several strong upper level disturbances resulted in numerous thunderstorms during the afternoon and evening. Many of these thunderstorms became severe. While penny sized was reported in spots, damaging winds from the thunderstorms was widespread. An EF-0 tornado was also confirmed in the community of Chesapeake Beach in Calvert County. A stalled front resided across the Mid Atlantic during the afternoon and evening of June 4th, allowing moisture and instability to pool along the boundary. This combined with several strong upper level disturbances resulted in numerous thunderstorms during the afternoon and evening. Many of these thunderstorms became severe. While penny sized was reported in spots, damaging winds from the thunderstorms was widespread. An EF-0 tornado was also confirmed in the community of Chesapeake Beach in Calvert County. A stalled front resided across the Mid Atlantic during the afternoon and evening of June 4th, allowing moisture and instability to pool along the boundary. This combined with several strong upper level disturbances resulted in numerous thunderstorms during the afternoon and evening. Many of these thunderstorms became severe. While penny sized was reported in spots, damaging winds from the thunderstorms was widespread. An EF-0 tornado was also confirmed in the community of Chesapeake Beach in Calvert County. A stalled front resided across the Mid Atlantic during the afternoon and evening of June 4th, allowing moisture and instability to pool along the boundary. This combined with several strong upper level disturbances resulted in numerous thunderstorms during the afternoon and evening. Many of these thunderstorms became severe. While penny sized was reported in spots, damaging winds from the thunderstorms was widespread. An EF-0 tornado was also confirmed in the community of Chesapeake Beach in Calvert County. A stalled front resided across the Mid Atlantic during the afternoon and evening of June 4th, allowing moisture and instability to pool along the boundary. This combined with several strong upper level disturbances resulted in numerous thunderstorms during the afternoon and evening. Many of these thunderstorms became severe. While penny sized was reported in spots, damaging winds from the thunderstorms was widespread. An EF-0 tornado was also confirmed in the community of Chesapeake Beach in Calvert County. A stalled front resided across the Mid Atlantic during the afternoon and evening of June 4th, allowing moisture and instability to pool along the boundary. This combined with several strong upper level disturbances resulted in numerous thunderstorms during the afternoon and evening. Many of these thunderstorms became severe. While penny sized was reported in spots, damaging winds from the thunderstorms was widespread. An EF-0 tornado was also confirmed in the community of Chesapeake Beach in Calvert County. A stalled front resided across the Mid Atlantic during the afternoon and evening of June 4th, allowing moisture and instability to pool along the boundary. This combined with several strong upper level disturbances resulted in numerous thunderstorms during the afternoon and evening. Many of these thunderstorms became severe. While penny sized was reported in spots, damaging winds from the thunderstorms was widespread. An EF-0 tornado was also confirmed in the community of Chesapeake Beach in Calvert County. A stalled front resided across the Mid Atlantic during the afternoon and evening of June 4th, allowing moisture and instability to pool along the boundary. This combined with several strong upper level disturbances resulted in numerous thunderstorms during the afternoon and evening. Many of these thunderstorms became severe. While penny sized was reported in spots, damaging winds from the thunderstorms was widespread. An EF-0 tornado was also confirmed in the community of Chesapeake Beach in Calvert County. A stalled front resided across the Mid Atlantic during the afternoon and evening of June 4th, allowing moisture and instability to pool along the boundary. This combined with several strong upper level disturbances resulted in numerous thunderstorms during the afternoon and evening. Many of these thunderstorms became severe. While penny sized was reported in spots, damaging winds from the thunderstorms was widespread. An EF-0 tornado was also confirmed in the community of Chesapeake Beach in Calvert County. A stalled front resided across the Mid Atlantic during the afternoon and evening of June 4th, allowing moisture and instability to pool along the boundary. This combined with several strong upper level disturbances resulted in numerous thunderstorms during the afternoon and evening. Many of these thunderstorms became severe. While penny sized was reported in spots, damaging winds from the thunderstorms was widespread. An EF-0 tornado was also confirmed in the community of Chesapeake Beach in Calvert County. A stalled front resided across the Mid Atlantic during the afternoon and evening of June 4th, allowing moisture and instability to pool along the boundary. This combined with several strong upper level disturbances resulted in numerous thunderstorms during the afternoon and evening. Many of these thunderstorms became severe. While penny sized was reported in spots, damaging winds from the thunderstorms was widespread. An EF-0 tornado was also confirmed in the community of Chesapeake Beach in Calvert County. A stalled front resided across the Mid Atlantic during the afternoon and evening of June 4th, allowing moisture and instability to pool along the boundary. This combined with several strong upper level disturbances resulted in numerous thunderstorms during the afternoon and evening. Many of these thunderstorms became severe. While penny sized was reported in spots, damaging winds from the thunderstorms was widespread. An EF-0 tornado was also confirmed in the community of Chesapeake Beach in Calvert County. A stalled front resided across the Mid Atlantic during the afternoon and evening of June 4th, allowing moisture and instability to pool along the boundary. This combined with several strong upper level disturbances resulted in numerous thunderstorms during the afternoon and evening. Many of these thunderstorms became severe. While penny sized was reported in spots, damaging winds from the thunderstorms was widespread. An EF-0 tornado was also confirmed in the community of Chesapeake Beach in Calvert County. A stalled front resided across the Mid Atlantic during the afternoon and evening of June 4th, allowing moisture and instability to pool along the boundary. This combined with several strong upper level disturbances resulted in numerous thunderstorms during the afternoon and evening. Many of these thunderstorms became severe. While penny sized was reported in spots, damaging winds from the thunderstorms was widespread. An EF-0 tornado was also confirmed in the community of Chesapeake Beach in Calvert County. A stalled front resided across the Mid Atlantic during the afternoon and evening of June 4th, allowing moisture and instability to pool along the boundary. This combined with several strong upper level disturbances resulted in numerous thunderstorms during the afternoon and evening. Many of these thunderstorms became severe. While penny sized was reported in spots, damaging winds from the thunderstorms was widespread. An EF-0 tornado was also confirmed in the community of Chesapeake Beach in Calvert County. A stalled front resided across the Mid Atlantic during the afternoon and evening of June 4th, allowing moisture and instability to pool along the boundary. This combined with several strong upper level disturbances resulted in numerous thunderstorms during the afternoon and evening. Many of these thunderstorms became severe. While penny sized was reported in spots, damaging winds from the thunderstorms was widespread. An EF-0 tornado was also confirmed in the community of Chesapeake Beach in Calvert County. A stalled front resided across the Mid Atlantic during the afternoon and evening of June 4th, allowing moisture and instability to pool along the boundary. This combined with several strong upper level disturbances resulted in numerous thunderstorms during the afternoon and evening. Many of these thunderstorms became severe. While penny sized was reported in spots, damaging winds from the thunderstorms was widespread. An EF-0 tornado was also confirmed in the community of Chesapeake Beach in Calvert County. A stalled front resided across the Mid Atlantic during the afternoon and evening of June 4th, allowing moisture and instability to pool along the boundary. This combined with several strong upper level disturbances resulted in numerous thunderstorms during the afternoon and evening. Many of these thunderstorms became severe. While penny sized was reported in spots, damaging winds from the thunderstorms was widespread. An EF-0 tornado was also confirmed in the community of Chesapeake Beach in Calvert County. A stalled front resided across the Mid Atlantic during the afternoon and evening of June 4th, allowing moisture and instability to pool along the boundary. This combined with several strong upper level disturbances resulted in numerous thunderstorms during the afternoon and evening. Many of these thunderstorms became severe. While penny sized was reported in spots, damaging winds from the thunderstorms was widespread. An EF-0 tornado was also confirmed in the community of Chesapeake Beach in Calvert County. A stalled front resided across the Mid Atlantic during the afternoon and evening of June 4th, allowing moisture and instability to pool along the boundary. This combined with several strong upper level disturbances resulted in numerous thunderstorms during the afternoon and evening. Many of these thunderstorms became severe. While penny sized was reported in spots, damaging winds from the thunderstorms was widespread. An EF-0 tornado was also confirmed in the community of Chesapeake Beach in Calvert County. A stalled front resided across the Mid Atlantic during the afternoon and evening of June 4th, allowing moisture and instability to pool along the boundary. This combined with several strong upper level disturbances resulted in numerous thunderstorms during the afternoon and evening. Many of these thunderstorms became severe. While penny sized was reported in spots, damaging winds from the thunderstorms was widespread. An EF-0 tornado was also confirmed in the community of Chesapeake Beach in Calvert County. A stalled front resided across the Mid Atlantic during the afternoon and evening of June 4th, allowing moisture and instability to pool along the boundary. This combined with several strong upper level disturbances resulted in numerous thunderstorms during the afternoon and evening. Many of these thunderstorms became severe. While penny sized was reported in spots, damaging winds from the thunderstorms was widespread. An EF-0 tornado was also confirmed in the community of Chesapeake Beach in Calvert County. A stalled front resided across the Mid Atlantic during the afternoon and evening of June 4th, allowing moisture and instability to pool along the boundary. This combined with several strong upper level disturbances resulted in numerous thunderstorms during the afternoon and evening. Many of these thunderstorms became severe. While penny sized was reported in spots, damaging winds from the thunderstorms was widespread. An EF-0 tornado was also confirmed in the community of Chesapeake Beach in Calvert County.\nEvent Narrative: Anne Arundel County Emergency Management reported trees and power lines down near Ridgeway. A trained spotter reported numerous trees and wires down on Bayberry Drive in Arnold. One home on Bayberry Drive had a tree fall through the damage, crushing a car. A local newspaper reported several trees down on Dunran, Dunhill and Dunglow roads. One tree fell on a car while another tree fell onto a house, causing minor damage. A local newspaper reported a tree fell onto a home on Bellvue Ave in Kingsville. A local newspaper reported a branch went through a roof of a house on Church Road in Owings Mills. A local newspaper reported a crane collapsed at Sparrows Point. No one was injured. A trained spotter estimated a wind gust of 65 MPH in northern Baltimore City. A local newspaper reported a tree down on St. Paul Street. A local newspaper reported a tree into a house on the 3600 block of Turnbridge Road in Forest Hills. The second and third floors were destroyed. Several trees were downed around Philadelphia and Forge roads. Several trees were snapped or uprooted on Creston Road near Dundalk. A local newspaper reported a tree fell onto a car on Severn Ave in near Severna Park. An NWS Storm Survey concluded that straight line winds downed numerous trees in Severna Park. A large number of hardwood trees, some up to 4 feet in diameter were uprooted. Several trees fell onto houses. Gusty winds downed several trees and lifted a barn on Governor Bridge Road in Davidsonville. Gusty winds downed several trees and a radio tower in Crownsville. A local newspaper reported trees and power lines down in Cape St. Claire. An NWS Storm Survey concluded that straight line winds were responsible for several downed trees along Patxuent River and Governor Bridge roads. A barn roof on Governor Bridge Road was lifted off its foundation. A local newspaper reported trees down on Governors Bridge Road in Bowie. Harford County Emergency Management reported trees and power lines down on Old Joppa Road. A trained spotter reported a tree down and several damaged in Columbia. Dozens of downed trees were reported along Gamewell Road. A CoCoRahs observer reported penny-sized hail in Bowie. An amateur radio operator relayed a report of trees and power lines downed on Beach Road. A local newspaper reported downed trees and power lines at a camp in Edgewater. Eight canoes, a shed and a canoe stand were destroyed. Maryland Department of Highways reported trees down on Reynolds Road, Bradshaw Road and Gerwell Court in the Upper Falls area.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 31.3145 km away, between 2008-06-04 14:50:00 and 2008-06-04 19:34:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A stalled front resided across the Mid Atlantic during the afternoon and evening of June 4th, allowing moisture and instability to pool along the boundary. This combined with several strong upper level disturbances resulted in numerous thunderstorms during the afternoon and evening. Many of these thunderstorms became severe, resulting in gusty winds at or above 50 knots across the Tidal Potomac River and Maryland Chesapeake Bay. A stalled front resided across the Mid Atlantic during the afternoon and evening of June 4th, allowing moisture and instability to pool along the boundary. This combined with several strong upper level disturbances resulted in numerous thunderstorms during the afternoon and evening. Many of these thunderstorms became severe, resulting in gusty winds at or above 50 knots across the Tidal Potomac River and Maryland Chesapeake Bay. A stalled front resided across the Mid Atlantic during the afternoon and evening of June 4th, allowing moisture and instability to pool along the boundary. This combined with several strong upper level disturbances resulted in numerous thunderstorms during the afternoon and evening. Many of these thunderstorms became severe, resulting in gusty winds at or above 50 knots across the Tidal Potomac River and Maryland Chesapeake Bay. A stalled front resided across the Mid Atlantic during the afternoon and evening of June 4th, allowing moisture and instability to pool along the boundary. This combined with several strong upper level disturbances resulted in numerous thunderstorms during the afternoon and evening. Many of these thunderstorms became severe, resulting in gusty winds at or above 50 knots across the Tidal Potomac River and Maryland Chesapeake Bay. A stalled front resided across the Mid Atlantic during the afternoon and evening of June 4th, allowing moisture and instability to pool along the boundary. This combined with several strong upper level disturbances resulted in numerous thunderstorms during the afternoon and evening. Many of these thunderstorms became severe, resulting in gusty winds at or above 50 knots across the Tidal Potomac River and Maryland Chesapeake Bay. A stalled front resided across the Mid Atlantic during the afternoon and evening of June 4th, allowing moisture and instability to pool along the boundary. This combined with several strong upper level disturbances resulted in numerous thunderstorms during the afternoon and evening. Many of these thunderstorms became severe, resulting in gusty winds at or above 50 knots across the Tidal Potomac River and Maryland Chesapeake Bay. A stalled front resided across the Mid Atlantic during the afternoon and evening of June 4th, allowing moisture and instability to pool along the boundary. This combined with several strong upper level disturbances resulted in numerous thunderstorms during the afternoon and evening. Many of these thunderstorms became severe, resulting in gusty winds at or above 50 knots across the Tidal Potomac River and Maryland Chesapeake Bay. A stalled front resided across the Mid Atlantic during the afternoon and evening of June 4th, allowing moisture and instability to pool along the boundary. This combined with several strong upper level disturbances resulted in numerous thunderstorms during the afternoon and evening. Many of these thunderstorms became severe, resulting in gusty winds at or above 50 knots across the Tidal Potomac River and Maryland Chesapeake Bay. A stalled front resided across the Mid Atlantic during the afternoon and evening of June 4th, allowing moisture and instability to pool along the boundary. This combined with several strong upper level disturbances resulted in numerous thunderstorms during the afternoon and evening. Many of these thunderstorms became severe, resulting in gusty winds at or above 50 knots across the Tidal Potomac River and Maryland Chesapeake Bay. A stalled front resided across the Mid Atlantic during the afternoon and evening of June 4th, allowing moisture and instability to pool along the boundary. This combined with several strong upper level disturbances resulted in numerous thunderstorms during the afternoon and evening. Many of these thunderstorms became severe, resulting in gusty winds at or above 50 knots across the Tidal Potomac River and Maryland Chesapeake Bay. A stalled front resided across the Mid Atlantic during the afternoon and evening of June 4th, allowing moisture and instability to pool along the boundary. This combined with several strong upper level disturbances resulted in numerous thunderstorms during the afternoon and evening. Many of these thunderstorms became severe, resulting in gusty winds at or above 50 knots across the Tidal Potomac River and Maryland Chesapeake Bay. A stalled front resided across the Mid Atlantic during the afternoon and evening of June 4th, allowing moisture and instability to pool along the boundary. This combined with several strong upper level disturbances resulted in numerous thunderstorms during the afternoon and evening. Many of these thunderstorms became severe, resulting in gusty winds at or above 50 knots across the Tidal Potomac River and Maryland Chesapeake Bay. A stalled front resided across the Mid Atlantic during the afternoon and evening of June 4th, allowing moisture and instability to pool along the boundary. This combined with several strong upper level disturbances resulted in numerous thunderstorms during the afternoon and evening. Many of these thunderstorms became severe, resulting in gusty winds at or above 50 knots across the Tidal Potomac River and Maryland Chesapeake Bay. A stalled front resided across the Mid Atlantic during the afternoon and evening of June 4th, allowing moisture and instability to pool along the boundary. This combined with several strong upper level disturbances resulted in numerous thunderstorms during the afternoon and evening. Many of these thunderstorms became severe, resulting in gusty winds at or above 50 knots across the Tidal Potomac River and Maryland Chesapeake Bay.\nEvent Narrative: The automated observation at Annapolis reported a wind gust in excess of 30 KT. The automated observation at Tolly Point measured a wind gust of 45 KT. The buoy at Thomas Point Light measured a wind gust of 39 KT. The buoy at Thomas Point Light measured a wind gust of 54 KT. The automated observation at Martin State Airport measured a wind gust of 42 KT. The automated observation at Gunpowder Falls State Park measured a wind gust of 34 KT. The buoy at Tolchester Beach measured a wind gust of 39 KT. The Patapsco buoy measured a wind gust of 45 KT. The automated observation at Tolly Point measured a wind gust of 35 KT. The automated observation at Kent Island reported a wind gust in excess of 30 KT. The automated observation at Greenbury Point measured a wind gust of 38 KT. The automated observation at Annapolis measured a wind gust of 34 KT. The buoy at Annapolis measured a wind gust of 38 KT. The buoy at Francis Scott Key Bridge reported a wind gust in excess of 30 KT.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 37.142 km away, between 2008-06-04 14:55:00 and 2008-06-04 20:08:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A pair of squall line thunderstorms produced damaging wind gusts as they moved across the Eastern Shore late in the afternoon and during the evening on the 4th. The first squall line caused the worst damage of the day and also spawned a tornado. About 5,000 Delmarva Power and Light customers lost power across the Eastern Shore because of the damaging winds and lightning. A pair of squall line thunderstorms produced damaging wind gusts as they moved across the Eastern Shore late in the afternoon and during the evening on the 4th. The first squall line caused the worst damage of the day and also spawned a tornado. About 5,000 Delmarva Power and Light customers lost power across the Eastern Shore because of the damaging winds and lightning. A pair of squall line thunderstorms produced damaging wind gusts as they moved across the Eastern Shore late in the afternoon and during the evening on the 4th. The first squall line caused the worst damage of the day and also spawned a tornado. About 5,000 Delmarva Power and Light customers lost power across the Eastern Shore because of the damaging winds and lightning. A pair of squall line thunderstorms produced damaging wind gusts as they moved across the Eastern Shore late in the afternoon and during the evening on the 4th. The first squall line caused the worst damage of the day and also spawned a tornado. About 5,000 Delmarva Power and Light customers lost power across the Eastern Shore because of the damaging winds and lightning.\nEvent Narrative: A severe thunderstorm knocked down trees and wires on Harbor Drive in Bay City. As the squall line of severe thunderstorms moved through Queen Anne's County, several trees were knocked down across Kent Island. Another tree was also knocked down near the intersection of U.S. Route 50 and Maryland State Route 310 in Queenstown. A severe thunderstorm knocked down large tree limbs and wires in Love Point. The downed wires apparently was the cause of a home in the area that filled with smoke. A severe thunderstorm knocked down a tree in Craney Creek just off of Maryland State Route 8 on Kent Island. The same severe storm downed a tree onto a vehicle in the Acme Parking lot and in front of a car wash in Centreville. Several trees were knocked down along Crouse Mill Road near Tuckahoe Lake south of Ruthsburg. About 1,000 homes and businesses lost power because of the series of thunderstorms throughout the day on the 4th in Queen Anne's County.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 17.1143 km away, between 2008-06-07 19:06:00 and 2008-06-07 19:53:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 40000.0 and crop damage of 0.0. \n\nEpisode Narrative: A very warm and humid air mass was entrenched across the Mid Atlantic during the late afternoon and evening hours of June 7th. As an upper level disturbance moved across the area, scattered strong to severe thunderstorms developed. Damaging winds brought down some trees and power lines across Maryland. The largest diameter hail recorded was quarter-sized, and occurred in Hillandale in Prince Georges County. A very warm and humid air mass was entrenched across the Mid Atlantic during the late afternoon and evening hours of June 7th. As an upper level disturbance moved across the area, scattered strong to severe thunderstorms developed. Damaging winds brought down some trees and power lines across Maryland. The largest diameter hail recorded was quarter-sized, and occurred in Hillandale in Prince Georges County. A very warm and humid air mass was entrenched across the Mid Atlantic during the late afternoon and evening hours of June 7th. As an upper level disturbance moved across the area, scattered strong to severe thunderstorms developed. Damaging winds brought down some trees and power lines across Maryland. The largest diameter hail recorded was quarter-sized, and occurred in Hillandale in Prince Georges County. A very warm and humid air mass was entrenched across the Mid Atlantic during the late afternoon and evening hours of June 7th. As an upper level disturbance moved across the area, scattered strong to severe thunderstorms developed. Damaging winds brought down some trees and power lines across Maryland. The largest diameter hail recorded was quarter-sized, and occurred in Hillandale in Prince Georges County. A very warm and humid air mass was entrenched across the Mid Atlantic during the late afternoon and evening hours of June 7th. As an upper level disturbance moved across the area, scattered strong to severe thunderstorms developed. Damaging winds brought down some trees and power lines across Maryland. The largest diameter hail recorded was quarter-sized, and occurred in Hillandale in Prince Georges County. A very warm and humid air mass was entrenched across the Mid Atlantic during the late afternoon and evening hours of June 7th. As an upper level disturbance moved across the area, scattered strong to severe thunderstorms developed. Damaging winds brought down some trees and power lines across Maryland. The largest diameter hail recorded was quarter-sized, and occurred in Hillandale in Prince Georges County.\nEvent Narrative: Dozens of trees were downed on Gamewell Road in Silver Spring. A trained spotter reported trees downed on power lines at Generals Highway and Revolution Way. A trained spotter reported trees downed in Severna Park along Route 2. A trained spotter reported several trees down near Columbia. Howard County Fire and Rescue Department reported wires down in the Columbia area. Howard County Fire and Rescue Department reported roof damage to a house near Savage.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 21.3242 km away, between 2008-06-07 19:36:00 and 2008-06-07 20:04:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A very warm and humid air mass was entrenched across the Mid Atlantic during the late afternoon and evening hours of June 7th. As an upper level disturbance moved across the area, scattered strong to severe thunderstorms developed. Gusty winds of 30 to 40 knots occurred across the Tidal Potomac River and Maryland Chesapeake Bay. A very warm and humid air mass was entrenched across the Mid Atlantic during the late afternoon and evening hours of June 7th. As an upper level disturbance moved across the area, scattered strong to severe thunderstorms developed. Gusty winds of 30 to 40 knots occurred across the Tidal Potomac River and Maryland Chesapeake Bay.\nEvent Narrative: The automated observation at Hart Millers Island reported a wind gust in excess of 30 KT. The buoy at Baltimore Key Bridge measured wind gust of 36 KT.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 42.6659 km away, between 2008-06-07 20:14:00 and 2008-06-07 20:14:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A unseasonably hot and humid air mass caused isolated pulse type severe thunderstorms to occur.\nEvent Narrative: A severe thunderstorm knocked a few trees and wires down along Eastern Neck Island Road (State Route 445) south of Rock Hall.", "The following events were reported: Funnel Cloud, Hail, Thunderstorm Wind. These occurred near station USW00093721, approximately 36.3677 km away, between 2008-06-10 16:36:00 and 2008-06-10 19:50:00. The events included records with hailstones measuring 33.667142857142856 inches.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 254000.0 and crop damage of 0.0. \n\nEpisode Narrative: A strong cold front moved through the Mid Atlantic states June 10th afternoon and evening. Cooler and drier air behind the front clashed with very warm and moist air ahead of it, resulting in scattered to numerous strong to severe thunderstorms. Storms that became severe brought down trees and power lines across the state of Maryland. Frostburg in Allegany County recorded a 65 mph wind gust. Golf ball-sized hail was reported further east in Baltimore County, in Timonium. A strong cold front moved through the Mid Atlantic states June 10th afternoon and evening. Cooler and drier air behind the front clashed with very warm and moist air ahead of it, resulting in scattered to numerous strong to severe thunderstorms. Storms that became severe brought down trees and power lines across the state of Maryland. Frostburg in Allegany County recorded a 65 mph wind gust. Golf ball-sized hail was reported further east in Baltimore County, in Timonium. A strong cold front moved through the Mid Atlantic states June 10th afternoon and evening. Cooler and drier air behind the front clashed with very warm and moist air ahead of it, resulting in scattered to numerous strong to severe thunderstorms. Storms that became severe brought down trees and power lines across the state of Maryland. Frostburg in Allegany County recorded a 65 mph wind gust. Golf ball-sized hail was reported further east in Baltimore County, in Timonium. A strong cold front moved through the Mid Atlantic states June 10th afternoon and evening. Cooler and drier air behind the front clashed with very warm and moist air ahead of it, resulting in scattered to numerous strong to severe thunderstorms. Storms that became severe brought down trees and power lines across the state of Maryland. Frostburg in Allegany County recorded a 65 mph wind gust. Golf ball-sized hail was reported further east in Baltimore County, in Timonium. A strong cold front moved through the Mid Atlantic states June 10th afternoon and evening. Cooler and drier air behind the front clashed with very warm and moist air ahead of it, resulting in scattered to numerous strong to severe thunderstorms. Storms that became severe brought down trees and power lines across the state of Maryland. Frostburg in Allegany County recorded a 65 mph wind gust. Golf ball-sized hail was reported further east in Baltimore County, in Timonium. A strong cold front moved through the Mid Atlantic states June 10th afternoon and evening. Cooler and drier air behind the front clashed with very warm and moist air ahead of it, resulting in scattered to numerous strong to severe thunderstorms. Storms that became severe brought down trees and power lines across the state of Maryland. Frostburg in Allegany County recorded a 65 mph wind gust. Golf ball-sized hail was reported further east in Baltimore County, in Timonium. A strong cold front moved through the Mid Atlantic states June 10th afternoon and evening. Cooler and drier air behind the front clashed with very warm and moist air ahead of it, resulting in scattered to numerous strong to severe thunderstorms. Storms that became severe brought down trees and power lines across the state of Maryland. Frostburg in Allegany County recorded a 65 mph wind gust. Golf ball-sized hail was reported further east in Baltimore County, in Timonium. A strong cold front moved through the Mid Atlantic states June 10th afternoon and evening. Cooler and drier air behind the front clashed with very warm and moist air ahead of it, resulting in scattered to numerous strong to severe thunderstorms. Storms that became severe brought down trees and power lines across the state of Maryland. Frostburg in Allegany County recorded a 65 mph wind gust. Golf ball-sized hail was reported further east in Baltimore County, in Timonium. A strong cold front moved through the Mid Atlantic states June 10th afternoon and evening. Cooler and drier air behind the front clashed with very warm and moist air ahead of it, resulting in scattered to numerous strong to severe thunderstorms. Storms that became severe brought down trees and power lines across the state of Maryland. Frostburg in Allegany County recorded a 65 mph wind gust. Golf ball-sized hail was reported further east in Baltimore County, in Timonium. A strong cold front moved through the Mid Atlantic states June 10th afternoon and evening. Cooler and drier air behind the front clashed with very warm and moist air ahead of it, resulting in scattered to numerous strong to severe thunderstorms. Storms that became severe brought down trees and power lines across the state of Maryland. Frostburg in Allegany County recorded a 65 mph wind gust. Golf ball-sized hail was reported further east in Baltimore County, in Timonium. A strong cold front moved through the Mid Atlantic states June 10th afternoon and evening. Cooler and drier air behind the front clashed with very warm and moist air ahead of it, resulting in scattered to numerous strong to severe thunderstorms. Storms that became severe brought down trees and power lines across the state of Maryland. Frostburg in Allegany County recorded a 65 mph wind gust. Golf ball-sized hail was reported further east in Baltimore County, in Timonium. A strong cold front moved through the Mid Atlantic states June 10th afternoon and evening. Cooler and drier air behind the front clashed with very warm and moist air ahead of it, resulting in scattered to numerous strong to severe thunderstorms. Storms that became severe brought down trees and power lines across the state of Maryland. Frostburg in Allegany County recorded a 65 mph wind gust. Golf ball-sized hail was reported further east in Baltimore County, in Timonium. A strong cold front moved through the Mid Atlantic states June 10th afternoon and evening. Cooler and drier air behind the front clashed with very warm and moist air ahead of it, resulting in scattered to numerous strong to severe thunderstorms. Storms that became severe brought down trees and power lines across the state of Maryland. Frostburg in Allegany County recorded a 65 mph wind gust. Golf ball-sized hail was reported further east in Baltimore County, in Timonium. A strong cold front moved through the Mid Atlantic states June 10th afternoon and evening. Cooler and drier air behind the front clashed with very warm and moist air ahead of it, resulting in scattered to numerous strong to severe thunderstorms. Storms that became severe brought down trees and power lines across the state of Maryland. Frostburg in Allegany County recorded a 65 mph wind gust. Golf ball-sized hail was reported further east in Baltimore County, in Timonium. A strong cold front moved through the Mid Atlantic states June 10th afternoon and evening. Cooler and drier air behind the front clashed with very warm and moist air ahead of it, resulting in scattered to numerous strong to severe thunderstorms. Storms that became severe brought down trees and power lines across the state of Maryland. Frostburg in Allegany County recorded a 65 mph wind gust. Golf ball-sized hail was reported further east in Baltimore County, in Timonium. A strong cold front moved through the Mid Atlantic states June 10th afternoon and evening. Cooler and drier air behind the front clashed with very warm and moist air ahead of it, resulting in scattered to numerous strong to severe thunderstorms. Storms that became severe brought down trees and power lines across the state of Maryland. Frostburg in Allegany County recorded a 65 mph wind gust. Golf ball-sized hail was reported further east in Baltimore County, in Timonium. A strong cold front moved through the Mid Atlantic states June 10th afternoon and evening. Cooler and drier air behind the front clashed with very warm and moist air ahead of it, resulting in scattered to numerous strong to severe thunderstorms. Storms that became severe brought down trees and power lines across the state of Maryland. Frostburg in Allegany County recorded a 65 mph wind gust. Golf ball-sized hail was reported further east in Baltimore County, in Timonium. A strong cold front moved through the Mid Atlantic states June 10th afternoon and evening. Cooler and drier air behind the front clashed with very warm and moist air ahead of it, resulting in scattered to numerous strong to severe thunderstorms. Storms that became severe brought down trees and power lines across the state of Maryland. Frostburg in Allegany County recorded a 65 mph wind gust. Golf ball-sized hail was reported further east in Baltimore County, in Timonium. A strong cold front moved through the Mid Atlantic states June 10th afternoon and evening. Cooler and drier air behind the front clashed with very warm and moist air ahead of it, resulting in scattered to numerous strong to severe thunderstorms. Storms that became severe brought down trees and power lines across the state of Maryland. Frostburg in Allegany County recorded a 65 mph wind gust. Golf ball-sized hail was reported further east in Baltimore County, in Timonium. A strong cold front moved through the Mid Atlantic states June 10th afternoon and evening. Cooler and drier air behind the front clashed with very warm and moist air ahead of it, resulting in scattered to numerous strong to severe thunderstorms. Storms that became severe brought down trees and power lines across the state of Maryland. Frostburg in Allegany County recorded a 65 mph wind gust. Golf ball-sized hail was reported further east in Baltimore County, in Timonium. A strong cold front moved through the Mid Atlantic states June 10th afternoon and evening. Cooler and drier air behind the front clashed with very warm and moist air ahead of it, resulting in scattered to numerous strong to severe thunderstorms. Storms that became severe brought down trees and power lines across the state of Maryland. Frostburg in Allegany County recorded a 65 mph wind gust. Golf ball-sized hail was reported further east in Baltimore County, in Timonium. A strong cold front moved through the Mid Atlantic states June 10th afternoon and evening. Cooler and drier air behind the front clashed with very warm and moist air ahead of it, resulting in scattered to numerous strong to severe thunderstorms. Storms that became severe brought down trees and power lines across the state of Maryland. Frostburg in Allegany County recorded a 65 mph wind gust. Golf ball-sized hail was reported further east in Baltimore County, in Timonium.\nEvent Narrative: Carroll County Emergency Management and law enforcement reported 100 trees down, with several on houses on Christy Drive. A trained spotter reported a tree and power pole down at the intersection of Putnam Road and Route 165. A trained spotter reported trees down on houses and business sign damage along York Road. There were also trees on several homes on Belfast Road. A local newspaper reported a tree fell on a car at the intersection of Dulaney Valley Road and Loch Raven Drive, trapping the driver in the car for 15 minutes. A local newspaper reported multiple trees down along Klee Mill Road between Routes 32 and 26. Around 20 trees were downed southwest of Upperco. Several small trees and large metal stands were blown over at Meadowood Regional Park. Baltimore County Emergency Management reported a tree down on a house on Carrbridge Court. Baltimore County Emergency Management reported trees down on homes in Cockeysville. A trained spotter reported trees down 5 miles west of Route 83. Baltimore County Emergency Management reported several windows broken due to nickel-sized hail. Baltimore County Emergency Management reported penny-sized hail in Hunt Valley. A trained spotter reported quarter-sized hail in Lutherville. A trained spotter reported golf ball-sized hail in Timonium. Minor siding damage was reported on Belfast Road. Howard County 911 Center reported trees down in Columbia. A local newspaper reported a line down on Brookville Avenue west of Georgia Avenue. A trained spotter reported penny-sized hail in Long Green. A trained spotter reported nickel-sized hail in Mount Airy. A trained spotter reported quarter-sized hail near Putnam Road and Route 165. A trained spotter, as well as local newspapers, reported several funnel clouds in Fallston. Baltimore County Emergency Management reported a home severely damaged in Lutherville. It was declared unsafe for living with a large tree through the roof that was pushing the side walls out. Carroll County Emergency Management reported trees through houses on Ridgemont Drive and in the Finksburg area.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 14.2666 km away, between 2008-06-10 20:06:00 and 2008-06-10 20:06:00. The events included records with estimated wind gusts of 34.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A strong cold front moved through the Mid Atlantic states June 10th afternoon and evening. Cooler and drier air behind the front clashed with very warm and moist air ahead of it, resulting in scattered to numerous strong to severe thunderstorms. Wind gusts up to 50 knots occurred across portions of the Tidal Potomac River and Maryland Chesapeake Bay.\nEvent Narrative: The buoy at Baltimore Key Bridge reported a wind gust in excess of 30 KT.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 42.9595 km away, between 2008-06-14 16:55:00 and 2008-06-14 16:55:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 5000.0 and crop damage of 0.0. \n\nEpisode Narrative: A cold front pushed into the Mid Atlantic region on June 14. With strong afternoon heating, scattered strong to severe thunderstorms developed ahead of the front in the afternoon and evening. Some of the storms resulted in downed trees and power lines. Penny-sized hail also occurred in St. Mary\ufffd\ufffd\ufffds County.\nEvent Narrative: Harford County Emergency Management reported trees down in Edgewood.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 29.5806 km away, between 2008-06-16 15:36:00 and 2008-06-16 17:30:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front moved into the Mid Atlantic during the afternoon of June 16. With a warm moist atmosphere in place, numerous strong to severe thunderstorms developed in the afternoon and evening. Gusty winds exceeded 40 knots across portions of the Tidal Potomac River and Maryland Chesapeake Bay. Reagan National reported a wind gust to 46 knots, while several observation points on the Chesapeake Bay gusted to 41 knots. A cold front moved into the Mid Atlantic during the afternoon of June 16. With a warm moist atmosphere in place, numerous strong to severe thunderstorms developed in the afternoon and evening. Gusty winds exceeded 40 knots across portions of the Tidal Potomac River and Maryland Chesapeake Bay. Reagan National reported a wind gust to 46 knots, while several observation points on the Chesapeake Bay gusted to 41 knots. A cold front moved into the Mid Atlantic during the afternoon of June 16. With a warm moist atmosphere in place, numerous strong to severe thunderstorms developed in the afternoon and evening. Gusty winds exceeded 40 knots across portions of the Tidal Potomac River and Maryland Chesapeake Bay. Reagan National reported a wind gust to 46 knots, while several observation points on the Chesapeake Bay gusted to 41 knots. A cold front moved into the Mid Atlantic during the afternoon of June 16. With a warm moist atmosphere in place, numerous strong to severe thunderstorms developed in the afternoon and evening. Gusty winds exceeded 40 knots across portions of the Tidal Potomac River and Maryland Chesapeake Bay. Reagan National reported a wind gust to 46 knots, while several observation points on the Chesapeake Bay gusted to 41 knots.\nEvent Narrative: The buoy at Baltimore Key Bridge reported a wind gust in excess of 30 KT. The buoy at Tolchester Beach reported a wind gust in excess of 30 KT. The buoy at Tolchester Beach measured a wind gust of 36 KT. An automated observation at the US Naval Academy in Annapolis reported a wind gust in excess of 30 KT.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 26.6552 km away, between 2008-06-18 18:59:00 and 2008-06-18 19:30:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: An upper level disturbance moved across the Mid Atlantic during the afternoon and evening of June 18. Heat and humidity in place over the region helped to triggered strong to severe thunderstorms over the Tidal Potomac River and Maryland Chesapeake Bay. Some storms produced wind gusts between 30 and 40 knots. An upper level disturbance moved across the Mid Atlantic during the afternoon and evening of June 18. Heat and humidity in place over the region helped to triggered strong to severe thunderstorms over the Tidal Potomac River and Maryland Chesapeake Bay. Some storms produced wind gusts between 30 and 40 knots. An upper level disturbance moved across the Mid Atlantic during the afternoon and evening of June 18. Heat and humidity in place over the region helped to triggered strong to severe thunderstorms over the Tidal Potomac River and Maryland Chesapeake Bay. Some storms produced wind gusts between 30 and 40 knots. An upper level disturbance moved across the Mid Atlantic during the afternoon and evening of June 18. Heat and humidity in place over the region helped to triggered strong to severe thunderstorms over the Tidal Potomac River and Maryland Chesapeake Bay. Some storms produced wind gusts between 30 and 40 knots.\nEvent Narrative: An automated observation in the City of Baltimore measured a wind gust of 35 KT. The buoy at Tolchester Beach measured a wind gust of 34 KT. An automated observation at Kent Island measured a wind gust of 41 KT. The buoy at Baltimore Key Bridge reported a wind gust in excess of 30 KT.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 22.1265 km away, between 2008-06-23 17:25:00 and 2008-06-23 17:50:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 4000.0 and crop damage of 0.0. \n\nEpisode Narrative: A cold front over the Mid Atlantic combined with a warm and moist atmosphere sparked scattered thunderstorms during the afternoon and evening of June 23rd. Some of the thunderstorms became severe, producing damaging winds and large hail. Winds lead to tent damage at the Smithburg Fire Station Carnival. Near Ringgold, large hail destroyed hundreds of acres of corn, and the hail covered the ground with a depth of 1.4 inches. A cold front over the Mid Atlantic combined with a warm and moist atmosphere sparked scattered thunderstorms during the afternoon and evening of June 23rd. Some of the thunderstorms became severe, producing damaging winds and large hail. Winds lead to tent damage at the Smithburg Fire Station Carnival. Near Ringgold, large hail destroyed hundreds of acres of corn, and the hail covered the ground with a depth of 1.4 inches.\nEvent Narrative: Law enforcement reported trees down near Bowie. Law enforcement reported trees down near Chesterfield and St. Stephens Church Roads.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 33.8397 km away, between 2008-06-23 18:05:00 and 2008-06-23 18:15:00. The events included records with measured wind gusts of 38.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front over the Mid Atlantic combined with a warm and moist atmosphere sparked scattered thunderstorms during the afternoon and evening of June 23rd. Gusty winds produced 35 to 45 knots over portions of the Tidal Potomac River and Maryland Chesapeake Bay. One of the highest gusts was 41 knots at Kent Island. A cold front over the Mid Atlantic combined with a warm and moist atmosphere sparked scattered thunderstorms during the afternoon and evening of June 23rd. Gusty winds produced 35 to 45 knots over portions of the Tidal Potomac River and Maryland Chesapeake Bay. One of the highest gusts was 41 knots at Kent Island.\nEvent Narrative: The buoy at Annapolis measured a wind gust of 35 KT. The automated observation at Kent Island measured a wind gust of 41 KT.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 47.1467 km away, between 2008-06-23 18:31:00 and 2008-06-23 18:31:00. The events included records with estimated wind gusts of 52.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A slow moving cold front helped trigger a pair of severe thunderstorms over Queen Anne's County on the evening of the 23rd.\nEvent Narrative: A severe thunderstorm tore down a couple of trees and wires in Grasonville.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 33.8699 km away, between 2008-06-27 12:49:00 and 2008-06-27 17:51:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A warm and humid air mass helped to support the development of isolated to scattered thunderstorms on June 27th. Some storms moving across the Tidal Potomac River and Maryland Chesapeake Bay produced gusty winds up to 40 knots. A warm and humid air mass helped to support the development of isolated to scattered thunderstorms on June 27th. Some storms moving across the Tidal Potomac River and Maryland Chesapeake Bay produced gusty winds up to 40 knots. A warm and humid air mass helped to support the development of isolated to scattered thunderstorms on June 27th. Some storms moving across the Tidal Potomac River and Maryland Chesapeake Bay produced gusty winds up to 40 knots. A warm and humid air mass helped to support the development of isolated to scattered thunderstorms on June 27th. Some storms moving across the Tidal Potomac River and Maryland Chesapeake Bay produced gusty winds up to 40 knots. A warm and humid air mass helped to support the development of isolated to scattered thunderstorms on June 27th. Some storms moving across the Tidal Potomac River and Maryland Chesapeake Bay produced gusty winds up to 40 knots. A warm and humid air mass helped to support the development of isolated to scattered thunderstorms on June 27th. Some storms moving across the Tidal Potomac River and Maryland Chesapeake Bay produced gusty winds up to 40 knots.\nEvent Narrative: The automated observation at Tolly Point reported a wind gust in excess of 30 KT. The automated observation at Kent Island reported a wind gust in excess of 30 KT. The buoy at the US Naval Academy in Annapolis reported a wind gust in excess of 30 KT. The buoy at Thomas Point Light measured wind gusts up to 51 KT. The buoy at Thomas Point Light measured a wind gust of 35 KT. The automated observation at Hart-Miller Island reported a wind gust in excess of 30 KT.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 27.1109 km away, between 2008-06-28 14:07:00 and 2008-06-28 21:17:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Heat and humidity strengthened across the Mid Atlantic ahead of a cold front during the afternoon and evening of June 28th. This led to scattered thunderstorms which produced gusty winds across the Tidal Potomac River and Maryland Chesapeake Bay. Winds averaged between 30 and 40 knots. Heat and humidity strengthened across the Mid Atlantic ahead of a cold front during the afternoon and evening of June 28th. This led to scattered thunderstorms which produced gusty winds across the Tidal Potomac River and Maryland Chesapeake Bay. Winds averaged between 30 and 40 knots. Heat and humidity strengthened across the Mid Atlantic ahead of a cold front during the afternoon and evening of June 28th. This led to scattered thunderstorms which produced gusty winds across the Tidal Potomac River and Maryland Chesapeake Bay. Winds averaged between 30 and 40 knots. Heat and humidity strengthened across the Mid Atlantic ahead of a cold front during the afternoon and evening of June 28th. This led to scattered thunderstorms which produced gusty winds across the Tidal Potomac River and Maryland Chesapeake Bay. Winds averaged between 30 and 40 knots. Heat and humidity strengthened across the Mid Atlantic ahead of a cold front during the afternoon and evening of June 28th. This led to scattered thunderstorms which produced gusty winds across the Tidal Potomac River and Maryland Chesapeake Bay. Winds averaged between 30 and 40 knots. Heat and humidity strengthened across the Mid Atlantic ahead of a cold front during the afternoon and evening of June 28th. This led to scattered thunderstorms which produced gusty winds across the Tidal Potomac River and Maryland Chesapeake Bay. Winds averaged between 30 and 40 knots. Heat and humidity strengthened across the Mid Atlantic ahead of a cold front during the afternoon and evening of June 28th. This led to scattered thunderstorms which produced gusty winds across the Tidal Potomac River and Maryland Chesapeake Bay. Winds averaged between 30 and 40 knots.\nEvent Narrative: An automated observation at the intersection of US 50 and MD 2 reported a wind gust in excess of 30 KT. An automated observation at Kent Island reported a wind gust in excess of 30 KT. The buoy at Baltimore Key Bridge reported a wind gust in excess of 30 KT. An automated observation in the City of Baltimore measured a wind gust of 42 KT. An automated observation at Hart/Miller Island measured a wind gust of 37 KT. The buoy at Thomas Point Light measured a wind gust of 39 KT. An automated observation at Tolly Point reported a wind gust in excess of 30 KT.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 6.4012 km away, between 2008-06-28 20:07:00 and 2008-06-28 20:07:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 1000.0 and crop damage of 0.0. \n\nEpisode Narrative: Heat and humidity strengthened across the Mid Atlantic ahead of a cold front during the afternoon and evening of June 28th. This led to scattered thunderstorms which produced damaging winds in some locations across north central Maryland. These winds brought down trees and power lines.\nEvent Narrative: Howard County Emergency Management reported trees down in the Elk Ridge area.", "The following events were reported: Marine Hail, Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 18.8467 km away, between 2008-06-29 15:14:00 and 2008-06-29 15:26:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front moved into the Mid Atlantic region on June 29th. With afternoon heat and humidity in place, scattered strong to severe thunderstorms developed during the afternoon and evening hours. These thunderstorms produced gusty winds across the Tidal Potomac and Maryland Chesapeake Bay. 34 knots occurred at Lewisetta, Point Lookout and Bishops Head. A cold front moved into the Mid Atlantic region on June 29th. With afternoon heat and humidity in place, scattered strong to severe thunderstorms developed during the afternoon and evening hours. These thunderstorms produced gusty winds across the Tidal Potomac and Maryland Chesapeake Bay. 34 knots occurred at Lewisetta, Point Lookout and Bishops Head.\nEvent Narrative: A trained spotter reported nickel-size hail near Essex. An automated observation at Oriole Park at Camden Yards measured a wind gust of 34 KT.", "The following events were reported: Hail. These occurred near station USW00093721, approximately 24.6034 km away, between 2008-06-29 15:25:00 and 2008-06-29 15:25:00. The events included records with hailstones measuring 0.88 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front moved into the Mid Atlantic region on June 29th. With afternoon heat and humidity in place, scattered strong to severe thunderstorms developed during the afternoon and evening hours. Damaging winds brought down power lines in Hagerstown. Penny sized hail also was observed in Essex.\nEvent Narrative: Nickel-sized hail was reported near Essex.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 30.5328 km away, between 2008-06-30 21:15:00 and 2008-06-30 21:15:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 3000.0 and crop damage of 0.0. \n\nEpisode Narrative: An upper level disturbance swung across the Mid Atlantic during the afternoon and evening of June 30th. With lingering moisture in place, scattered thunderstorms developed in the afternoon. One storm became severe over Anne Arundel County, downing trees and power lines 2 miles southwest of Davidsonville.\nEvent Narrative: Anne Arundel County Fire and Rescue Department reported trees and wires down near Davidsonville.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 38.2866 km away, between 2008-06-30 21:26:00 and 2008-06-30 21:33:00. The events included records with measured wind gusts of 35.5 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: An upper level disturbance swung across the Mid Atlantic during the afternoon and evening of June 30th. With lingering moisture in place, scattered thunderstorms developed in the afternoon. Thunderstorms produce several wind gust reports between 30 and 40 knots. Lewisetta observed 37 knots. An upper level disturbance swung across the Mid Atlantic during the afternoon and evening of June 30th. With lingering moisture in place, scattered thunderstorms developed in the afternoon. Thunderstorms produce several wind gust reports between 30 and 40 knots. Lewisetta observed 37 knots.\nEvent Narrative: The buoy at Thomas Point Light measured a wind gust of 37 KT. An automated observation at Kent Island measured a wind gust of 34 KT.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 28.3911 km away, between 2008-07-22 22:22:00 and 2008-07-22 22:22:00. The events included records with measured wind gusts of 39.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A strong cold front combined with an upper level disturbance during the afternoon and evening hours of July 22nd. Cold air aloft combined with warm and humid air at the surface allowed for scattered to numerous showers and thunderstorms to develop across northern Virginia and lower southern Maryland. One storm produced a wind gust near 40 knots on the Chesapeake Bay.\nEvent Narrative: An automated observation at Hart/Miller Island measured a wind gust of 39 knots.", "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00093721, approximately 18.4608 km away, between 2008-07-22 22:24:00 and 2008-07-22 22:24:00. The events included records with hailstones measuring 25.875 inches.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 3000.0 and crop damage of 0.0. \n\nEpisode Narrative: A strong cold front combined with an upper level disturbance during the afternoon and evening hours of July 22nd. Cold air aloft combined with warm and humid air at the surface allowed for scattered to numerous showers and thunderstorms to develop across the Mid Atlantic. Some storms became severe, downing trees and power lines and producing large hail across portions of northern Maryland. A strong cold front combined with an upper level disturbance during the afternoon and evening hours of July 22nd. Cold air aloft combined with warm and humid air at the surface allowed for scattered to numerous showers and thunderstorms to develop across the Mid Atlantic. Some storms became severe, downing trees and power lines and producing large hail across portions of northern Maryland.\nEvent Narrative: A trained spotter reported downed power lines. A trained spotter reported hail to the size of golf balls.", "The following events were reported: Flash Flood, Hail, Thunderstorm Wind. These occurred near station USW00093721, approximately 20.8051 km away, between 2008-07-23 14:35:00 and 2008-07-23 23:00:00. The events included records with hailstones measuring 37.6875 inches.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 11000.0 and crop damage of 0.0. \n\nEpisode Narrative: A slow moving cold front moved towards the Mid Atlantic Coast on July 23rd. This front provided the focus for scattered to numerous showers and thunderstorms to develop during the afternoon and evening hours. With high amounts of moisture in place, some storms produced heavy rainfall. Storms also moved repeatedly over the same areas. This allowed flash flooding to occur across the Baltimore metro area, resulting in several road closures and water rescues. Severe thunderstorms also occurred, with gusty winds downing trees and power lines. There were also a few reports of large hail. A slow moving cold front moved towards the Mid Atlantic Coast on July 23rd. This front provided the focus for scattered to numerous showers and thunderstorms to develop during the afternoon and evening hours. With high amounts of moisture in place, some storms produced heavy rainfall. Storms also moved repeatedly over the same areas. This allowed flash flooding to occur across the Baltimore metro area, resulting in several road closures and water rescues. Severe thunderstorms also occurred, with gusty winds downing trees and power lines. There were also a few reports of large hail. A slow moving cold front moved towards the Mid Atlantic Coast on July 23rd. This front provided the focus for scattered to numerous showers and thunderstorms to develop during the afternoon and evening hours. With high amounts of moisture in place, some storms produced heavy rainfall. Storms also moved repeatedly over the same areas. This allowed flash flooding to occur across the Baltimore metro area, resulting in several road closures and water rescues. Severe thunderstorms also occurred, with gusty winds downing trees and power lines. There were also a few reports of large hail. A slow moving cold front moved towards the Mid Atlantic Coast on July 23rd. This front provided the focus for scattered to numerous showers and thunderstorms to develop during the afternoon and evening hours. With high amounts of moisture in place, some storms produced heavy rainfall. Storms also moved repeatedly over the same areas. This allowed flash flooding to occur across the Baltimore metro area, resulting in several road closures and water rescues. Severe thunderstorms also occurred, with gusty winds downing trees and power lines. There were also a few reports of large hail. A slow moving cold front moved towards the Mid Atlantic Coast on July 23rd. This front provided the focus for scattered to numerous showers and thunderstorms to develop during the afternoon and evening hours. With high amounts of moisture in place, some storms produced heavy rainfall. Storms also moved repeatedly over the same areas. This allowed flash flooding to occur across the Baltimore metro area, resulting in several road closures and water rescues. Severe thunderstorms also occurred, with gusty winds downing trees and power lines. There were also a few reports of large hail. A slow moving cold front moved towards the Mid Atlantic Coast on July 23rd. This front provided the focus for scattered to numerous showers and thunderstorms to develop during the afternoon and evening hours. With high amounts of moisture in place, some storms produced heavy rainfall. Storms also moved repeatedly over the same areas. This allowed flash flooding to occur across the Baltimore metro area, resulting in several road closures and water rescues. Severe thunderstorms also occurred, with gusty winds downing trees and power lines. There were also a few reports of large hail. A slow moving cold front moved towards the Mid Atlantic Coast on July 23rd. This front provided the focus for scattered to numerous showers and thunderstorms to develop during the afternoon and evening hours. With high amounts of moisture in place, some storms produced heavy rainfall. Storms also moved repeatedly over the same areas. This allowed flash flooding to occur across the Baltimore metro area, resulting in several road closures and water rescues. Severe thunderstorms also occurred, with gusty winds downing trees and power lines. There were also a few reports of large hail.\nEvent Narrative: Montgomery County Law Enforcement reported trees down on Ansted Court. Local broadcast media reported 3 lanes of Interstate 95 closed due to high water. A local newspaper reported downed trees along Hillen Road near Argonne Drive. A trained spotter reported hail to the size of a penny. Baltimore County Fire and Rescue reported several water rescues in southwestern Baltimore County. Local broadcast media reported a water rescue at Exeter Hall Avenue and Aisquith Street. Northbound ramps of the Jones Falls Expressway at President Street and Monument Street were closed. A local newspaper reported downed trees and power lines in Annapolis.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 38.2747 km away, between 2008-07-23 18:48:00 and 2008-07-23 19:14:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A slow moving cold front moved towards the Mid Atlantic Coast on July 23rd. This front provided the focus for scattered to numerous showers and thunderstorms to develop during the afternoon and evening hours. Some storms became severe and produced wind gusts of 30 to 50 knots over the Tidal Potomac River and Maryland Chesapeake Bay. A slow moving cold front moved towards the Mid Atlantic Coast on July 23rd. This front provided the focus for scattered to numerous showers and thunderstorms to develop during the afternoon and evening hours. Some storms became severe and produced wind gusts of 30 to 50 knots over the Tidal Potomac River and Maryland Chesapeake Bay.\nEvent Narrative: An automated observation at Kent Island reported a wind gust in excess of 30 knots. A buoy at Thomas Point measured a wind gust of 34 knots.", "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00093721, approximately 14.3433 km away, between 2008-07-27 11:43:00 and 2008-07-27 16:00:00. The events included records with hailstones measuring 15.812999999999999 inches.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 3000.0 and crop damage of 0.0. \n\nEpisode Narrative: A cold front approached the region on July 27th as a strong upper level low pressure system remained over the northeast. Warm and humid air at the surface interacted with cooler air aloft to produce scattered to numerous showers and thunderstorms during the afternoon hours. Many of the storms became severe, producing damaging winds that downed trees and power lines. Large hail to the size of quarters was also reported. A cold front approached the region on July 27th as a strong upper level low pressure system remained over the northeast. Warm and humid air at the surface interacted with cooler air aloft to produce scattered to numerous showers and thunderstorms during the afternoon hours. Many of the storms became severe, producing damaging winds that downed trees and power lines. Large hail to the size of quarters was also reported. A cold front approached the region on July 27th as a strong upper level low pressure system remained over the northeast. Warm and humid air at the surface interacted with cooler air aloft to produce scattered to numerous showers and thunderstorms during the afternoon hours. Many of the storms became severe, producing damaging winds that downed trees and power lines. Large hail to the size of quarters was also reported. A cold front approached the region on July 27th as a strong upper level low pressure system remained over the northeast. Warm and humid air at the surface interacted with cooler air aloft to produce scattered to numerous showers and thunderstorms during the afternoon hours. Many of the storms became severe, producing damaging winds that downed trees and power lines. Large hail to the size of quarters was also reported. A cold front approached the region on July 27th as a strong upper level low pressure system remained over the northeast. Warm and humid air at the surface interacted with cooler air aloft to produce scattered to numerous showers and thunderstorms during the afternoon hours. Many of the storms became severe, producing damaging winds that downed trees and power lines. Large hail to the size of quarters was also reported. A cold front approached the region on July 27th as a strong upper level low pressure system remained over the northeast. Warm and humid air at the surface interacted with cooler air aloft to produce scattered to numerous showers and thunderstorms during the afternoon hours. Many of the storms became severe, producing damaging winds that downed trees and power lines. Large hail to the size of quarters was also reported. A cold front approached the region on July 27th as a strong upper level low pressure system remained over the northeast. Warm and humid air at the surface interacted with cooler air aloft to produce scattered to numerous showers and thunderstorms during the afternoon hours. Many of the storms became severe, producing damaging winds that downed trees and power lines. Large hail to the size of quarters was also reported. A cold front approached the region on July 27th as a strong upper level low pressure system remained over the northeast. Warm and humid air at the surface interacted with cooler air aloft to produce scattered to numerous showers and thunderstorms during the afternoon hours. Many of the storms became severe, producing damaging winds that downed trees and power lines. Large hail to the size of quarters was also reported. A cold front approached the region on July 27th as a strong upper level low pressure system remained over the northeast. Warm and humid air at the surface interacted with cooler air aloft to produce scattered to numerous showers and thunderstorms during the afternoon hours. Many of the storms became severe, producing damaging winds that downed trees and power lines. Large hail to the size of quarters was also reported. A cold front approached the region on July 27th as a strong upper level low pressure system remained over the northeast. Warm and humid air at the surface interacted with cooler air aloft to produce scattered to numerous showers and thunderstorms during the afternoon hours. Many of the storms became severe, producing damaging winds that downed trees and power lines. Large hail to the size of quarters was also reported.\nEvent Narrative: A trained spotter measured a wind gust of 60 MPH. An NWS employee reported hail to the size of pennies east of Laurel. A trained spotter reported trees down in Severn. Howard County Emergency Management reported a downed tree blocking Corina Court. A trained spotter reported hail to the size of pennies. A trained spotter reported hail to the size of pennies. An amateur radio operator reported hail to the size of nickels in Bel Air. A trained spotter reported hail to the size of quarters. The hail caused a hole in a car windshield. A trained spotter reported hail to the size of quarters. Trained spotters reported hail to the size of quarters along Route 32 and at Fort Meade.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 14.2666 km away, between 2008-07-27 12:00:00 and 2008-07-27 12:00:00. The events included records with measured wind gusts of 34.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front approached the region on July 27th as a strong upper level low pressure system remained over the northeast. Warm and humid air at the surface interacted with cooler air aloft to produce scattered to numerous showers and thunderstorms during the afternoon hours. Many of the storms became severe, producing wind gusts of 30 to nearly 60 knots over the Tidal Potomac River and Maryland Chesapeake Bay. One storm moved over Fairview Beach during an afternoon festival. Boats near the beach were hit by 4 foot waves, with several people being rescued from the water. Only minor injuries were reported.\nEvent Narrative: The buoy at Baltimore Key Bridge measured a wind gust of 34 knots.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 30.4927 km away, between 2008-07-30 16:00:00 and 2008-07-30 16:04:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 13000.0 and crop damage of 0.0. \n\nEpisode Narrative: A warm front moved north through the Mid Atlantic on the morning of July 30th, bringing increased heat and humidity to the region. An upper level disturbance then moved through the region during the afternoon. This helped to trigger isolated showers and thunderstorms during the late afternoon and evening. A storm that moved over Baltimore County downed several trees and power lines. A warm front moved north through the Mid Atlantic on the morning of July 30th, bringing increased heat and humidity to the region. An upper level disturbance then moved through the region during the afternoon. This helped to trigger isolated showers and thunderstorms during the late afternoon and evening. A storm that moved over Baltimore County downed several trees and power lines. A warm front moved north through the Mid Atlantic on the morning of July 30th, bringing increased heat and humidity to the region. An upper level disturbance then moved through the region during the afternoon. This helped to trigger isolated showers and thunderstorms during the late afternoon and evening. A storm that moved over Baltimore County downed several trees and power lines.\nEvent Narrative: A trained spotter reported several trees uprooted or snapped near the intersection of Gateridge Road and Stillway Court. Baltimore County Emergency Management reported several trees down in Cockeysville. Local broadcast media reported a tree fell onto a moving train at the Falls Road Station.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 28.7977 km away, between 2008-07-30 16:45:00 and 2008-07-30 16:46:00. The events included records with estimated wind gusts of 34.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A warm front moved north through the Mid Atlantic on the morning of July 30th, bringing increased heat and humidity to the region. An upper level disturbance then moved through the region during the afternoon. This helped to trigger isolated showers and thunderstorms during the late afternoon and evening. A storm moving over the northern Chesapeake Bay produced winds in excess of 30 knots.\nEvent Narrative: An automated observation at Martin State Airport reported a wind gust in excess of 30 knots.", "The following events were reported: Hail. These occurred near station USW00093721, approximately 13.5459 km away, between 2008-08-02 03:55:00 and 2008-08-02 03:55:00. The events included records with hailstones measuring 0.75 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: An upper-level disturbance passed through the Mid-Atlantic during the morning hours. This disturbance combined with an unstable atmosphere to trigger showers and thunderstorms. Some of these thunderstorms were severe, producing gusty winds and large hail.\nEvent Narrative: A trained spotter reported penny sized hail in Pasadena.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 33.1341 km away, between 2008-08-02 04:00:00 and 2008-08-02 05:04:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: An upper-level disturbance passed through the Mid-Atlantic during the morning hours. This disturbance combined with an unstable atmosphere to trigger showers and thunderstorms. Some of these thunderstorms were severe, producing gusty winds over the Chesapeake Bay. An upper-level disturbance passed through the Mid-Atlantic during the morning hours. This disturbance combined with an unstable atmosphere to trigger showers and thunderstorms. Some of these thunderstorms were severe, producing gusty winds over the Chesapeake Bay. An upper-level disturbance passed through the Mid-Atlantic during the morning hours. This disturbance combined with an unstable atmosphere to trigger showers and thunderstorms. Some of these thunderstorms were severe, producing gusty winds over the Chesapeake Bay. An upper-level disturbance passed through the Mid-Atlantic during the morning hours. This disturbance combined with an unstable atmosphere to trigger showers and thunderstorms. Some of these thunderstorms were severe, producing gusty winds over the Chesapeake Bay. An upper-level disturbance passed through the Mid-Atlantic during the morning hours. This disturbance combined with an unstable atmosphere to trigger showers and thunderstorms. Some of these thunderstorms were severe, producing gusty winds over the Chesapeake Bay. An upper-level disturbance passed through the Mid-Atlantic during the morning hours. This disturbance combined with an unstable atmosphere to trigger showers and thunderstorms. Some of these thunderstorms were severe, producing gusty winds over the Chesapeake Bay. An upper-level disturbance passed through the Mid-Atlantic during the morning hours. This disturbance combined with an unstable atmosphere to trigger showers and thunderstorms. Some of these thunderstorms were severe, producing gusty winds over the Chesapeake Bay. An upper-level disturbance passed through the Mid-Atlantic during the morning hours. This disturbance combined with an unstable atmosphere to trigger showers and thunderstorms. Some of these thunderstorms were severe, producing gusty winds over the Chesapeake Bay.\nEvent Narrative: An automated weather observation in Stevensville reported a wind gust of 34 knots. An automated observation in Tolly Point reported a wind gust of 35 knots. An automated observation at Kent Island reported a wind gust in excess of 30 knots. A buoy at Tolchester beach reported a wind gust of 34 knots. An automated surface observation in Annapolis reported a wind gust in excess of 30 knots. A surface observation at Miller Island reported a wind gust of 44 knots. An automated observation at Edgemere measured a wind gust of 35 knots. A buoy at Tolchester Beach measured a wind gust of 50 knots.", "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00093721, approximately 38.902 km away, between 2008-08-02 04:42:00 and 2008-08-02 16:11:00. The events included records with hailstones measuring 37.0 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A slow moving cold front located in central Pennsylvania and northern West Virginia around sunrise on the 2nd helped trigger strong to severe thunderstorms over the Eastern Shore through the late afternoon. A slow moving cold front located in central Pennsylvania and northern West Virginia around sunrise on the 2nd helped trigger strong to severe thunderstorms over the Eastern Shore through the late afternoon. A slow moving cold front located in central Pennsylvania and northern West Virginia around sunrise on the 2nd helped trigger strong to severe thunderstorms over the Eastern Shore through the late afternoon.\nEvent Narrative: A thunderstorm wind gust to 58 mph was measured at Tolchester Beach C-man station. A severe thunderstorm tore down numerous trees and wires as well as transmission poles in western Kent County. Quarter size hail also fell with the severe thunderstorm. About 760 homes and businesses lost power, mainly in the Tolchester Beach area. Power was not restored until the 3rd. A wind gust to 69 mph was measured at the Tolchester Beach C-man station.", "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00093721, approximately 37.9208 km away, between 2008-08-02 14:50:00 and 2008-08-02 17:42:00. The events included records with hailstones measuring 12.07 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front passing through the region combined with an unstable atmosphere to trigger showers and thunderstorms. Some thunderstorms were severe, producing damaging winds and large hail. A cold front passing through the region combined with an unstable atmosphere to trigger showers and thunderstorms. Some thunderstorms were severe, producing damaging winds and large hail. A cold front passing through the region combined with an unstable atmosphere to trigger showers and thunderstorms. Some thunderstorms were severe, producing damaging winds and large hail. A cold front passing through the region combined with an unstable atmosphere to trigger showers and thunderstorms. Some thunderstorms were severe, producing damaging winds and large hail. A cold front passing through the region combined with an unstable atmosphere to trigger showers and thunderstorms. Some thunderstorms were severe, producing damaging winds and large hail. A cold front passing through the region combined with an unstable atmosphere to trigger showers and thunderstorms. Some thunderstorms were severe, producing damaging winds and large hail. A cold front passing through the region combined with an unstable atmosphere to trigger showers and thunderstorms. Some thunderstorms were severe, producing damaging winds and large hail. A cold front passing through the region combined with an unstable atmosphere to trigger showers and thunderstorms. Some thunderstorms were severe, producing damaging winds and large hail. A cold front passing through the region combined with an unstable atmosphere to trigger showers and thunderstorms. Some thunderstorms were severe, producing damaging winds and large hail.\nEvent Narrative: Trees were down on Falls Road and Gadd Road. A report of nickel sized hail came from the public near Bowleys Quarters. A trained spotter reported hail one inch in diameter near Middle River. A trained spotter reported hail one inch in diameter near White Marsh. Golf ball sized hail was reported by a trained spotter about 3 miles west-southwest of Annapolis. The Fire Department found numerous trees down in Bel Air. A trained spotter reported penny sized hail about 4 miles west of Bel Air. A National Weather Service employee reported hail 1.5 inches in diameter 2 miles west of Bel Air. A report of golf ball sized hail came from the public in Bel Air.", "The following events were reported: Marine Hail, Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 30.1018 km away, between 2008-08-02 15:35:00 and 2008-08-02 18:03:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front passing through the waters combined with an unstable atmosphere to trigger showers and thunderstorms. Some thunderstorms were severe, producing gusty winds and large hail. A cold front passing through the waters combined with an unstable atmosphere to trigger showers and thunderstorms. Some thunderstorms were severe, producing gusty winds and large hail. A cold front passing through the waters combined with an unstable atmosphere to trigger showers and thunderstorms. Some thunderstorms were severe, producing gusty winds and large hail. A cold front passing through the waters combined with an unstable atmosphere to trigger showers and thunderstorms. Some thunderstorms were severe, producing gusty winds and large hail. A cold front passing through the waters combined with an unstable atmosphere to trigger showers and thunderstorms. Some thunderstorms were severe, producing gusty winds and large hail. A cold front passing through the waters combined with an unstable atmosphere to trigger showers and thunderstorms. Some thunderstorms were severe, producing gusty winds and large hail. A cold front passing through the waters combined with an unstable atmosphere to trigger showers and thunderstorms. Some thunderstorms were severe, producing gusty winds and large hail. A cold front passing through the waters combined with an unstable atmosphere to trigger showers and thunderstorms. Some thunderstorms were severe, producing gusty winds and large hail.\nEvent Narrative: Hail to the size of quarters was reported by a trained spotter. Hail to the size of nickels was reported by the public. A wind gust estimated in excess of 30 knots occurred at Kent Island. A wind gust of 36 knots was measured at Thomas Point Lighthouse. A wind gust of 60 knots was measured at Tolchester beach. A buoy at Baltimore Key Bridge estimated wind gusts in excess of 30 knots. Hail to the size of golf balls was reported near the coast by a trained spotter. A wind gust in excess of 30 knots was estimated at Annapolis.", "The following events were reported: Hail. These occurred near station USW00093721, approximately 22.7009 km away, between 2008-08-07 16:13:00 and 2008-08-07 16:13:00. The events included records with hailstones measuring 0.75 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: An upper-level disturbance along with an unstable atmosphere triggered showers and thunderstorms. Some storms were severe, producing damaging winds and large hail.\nEvent Narrative: Penny size hail was reported about 4 miles west-northwest of Bowie.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 28.3911 km away, between 2008-08-07 18:11:00 and 2008-08-07 18:11:00. The events included records with measured wind gusts of 37.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: An upper-level disturbance along with an unstable atmosphere triggered showers and thunderstorms. Some storms were severe, producing gusty winds over the Tidal Potomac and Chesapeake Bay and Tidal Potomac.\nEvent Narrative: A wind of 37 knots was measured at Miller Island.", "The following events were reported: Hail. These occurred near station USW00093721, approximately 24.1841 km away, between 2008-08-10 12:10:00 and 2008-08-10 16:58:00. The events included records with hailstones measuring 0.852 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A trough of low pressure along with a cold front triggered showers and thunderstorms. Some of the thunderstorms produced large hail. A trough of low pressure along with a cold front triggered showers and thunderstorms. Some of the thunderstorms produced large hail. A trough of low pressure along with a cold front triggered showers and thunderstorms. Some of the thunderstorms produced large hail. A trough of low pressure along with a cold front triggered showers and thunderstorms. Some of the thunderstorms produced large hail. A trough of low pressure along with a cold front triggered showers and thunderstorms. Some of the thunderstorms produced large hail.\nEvent Narrative: Nickel size hail was reported. Quarter size hail was reported. Penny size hail was reported in Franklinville. Penny size hail was reported in near Joppatowne. Nickel size hail was reported.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 36.9916 km away, between 2008-08-10 17:59:00 and 2008-08-10 17:59:00. The events included records with estimated wind gusts of 34.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A trough of low pressure along with a cold front triggered showers and thunderstorms. Some of the thunderstorms produced gusty winds across the Tidal Potomac and Chesapeake Bay.\nEvent Narrative: A wind gust in excess of 30 knots was estimated at Thomas Point Lighthouse.", "The following events were reported: Hail. These occurred near station USW00093721, approximately 35.8181 km away, between 2008-08-14 14:13:00 and 2008-08-14 15:10:00. The events included records with hailstones measuring 0.8125 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: An upper-level low produced an unstable atmosphere, triggering showers and thunderstorms. Some of the thunderstorms produced large hail. An upper-level low produced an unstable atmosphere, triggering showers and thunderstorms. Some of the thunderstorms produced large hail. An upper-level low produced an unstable atmosphere, triggering showers and thunderstorms. Some of the thunderstorms produced large hail. An upper-level low produced an unstable atmosphere, triggering showers and thunderstorms. Some of the thunderstorms produced large hail.\nEvent Narrative: Penny size hail was reported about six miles north-northwest of Olney. Penny size hail was reported near Sykesville. Penny size hail was reported near Reisterstown. Quarter size hail was reported near Finksburg.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 35.2982 km away, between 2008-08-14 16:36:00 and 2008-08-14 16:59:00. The events included records with estimated wind gusts of 34.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: An upper-level low produced an unstable atmosphere, triggering showers and thunderstorms. Some of the thunderstorms produced gusty winds over the Chesapeake Bay. An upper-level low produced an unstable atmosphere, triggering showers and thunderstorms. Some of the thunderstorms produced gusty winds over the Chesapeake Bay. An upper-level low produced an unstable atmosphere, triggering showers and thunderstorms. Some of the thunderstorms produced gusty winds over the Chesapeake Bay.\nEvent Narrative: A wind gust in excess of 30 knots was estimated at Thomas Point Lighthouse. A wind gust in excess of 30 knots was reported at Tolly Point. A wind gust in excess of 30 knots was reported at Kent Island.", "The following events were reported: Flash Flood. These occurred near station USW00093721, approximately 49.673 km away, between 2008-09-06 16:30:00 and 2008-09-06 18:30:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Tropical Storm Hanna tracked up the Mid-Atlantic coast on the 6th with maximum sustained winds around 50 mph. Hanna originally made landfall near the border of North and South Carolina around 3:20 AM on the 6th. Hanna tracked across eastern North Carolina during the early afternoon hours before turning northeast across southeastern Virginia later in the afternoon. Hanna eventually tracked across the Chesapeake Bay and into Delaware during the evening hours. With the track of Hanna being to the east, the strongest winds were also confined to our east. However, Hanna was still responsible for heavy rain along with Tropical Storm force winds across Maryland. Rainfall amounts totaled around 4 to 8 inches across many locations. Numerous roads were closed throughout Maryland due to flash flooding. Tropical Storm force winds were responsible for downed trees and power lines across Maryland as well. The worst conditions occurred during the late morning and afternoon hours as the storm passed by just to the east.\nEvent Narrative: A small creek near James Run was over its banks around Route 7.", "The following events were reported: Flash Flood. These occurred near station USW00093721, approximately 26.2224 km away, between 2008-09-27 07:49:00 and 2008-09-27 18:30:00.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 3000.0 and crop damage of 0.0. \n\nEpisode Narrative: The combination of an unstable atmosphere along with plenty of moisture triggered showers and thunderstorms on September 27th. Some thunderstorms produced heavy rain in short periods of time, resulting in flash flooding. The combination of an unstable atmosphere along with plenty of moisture triggered showers and thunderstorms on September 27th. Some thunderstorms produced heavy rain in short periods of time, resulting in flash flooding. The combination of an unstable atmosphere along with plenty of moisture triggered showers and thunderstorms on September 27th. Some thunderstorms produced heavy rain in short periods of time, resulting in flash flooding. The combination of an unstable atmosphere along with plenty of moisture triggered showers and thunderstorms on September 27th. Some thunderstorms produced heavy rain in short periods of time, resulting in flash flooding. The combination of an unstable atmosphere along with plenty of moisture triggered showers and thunderstorms on September 27th. Some thunderstorms produced heavy rain in short periods of time, resulting in flash flooding. The combination of an unstable atmosphere along with plenty of moisture triggered showers and thunderstorms on September 27th. Some thunderstorms produced heavy rain in short periods of time, resulting in flash flooding. The combination of an unstable atmosphere along with plenty of moisture triggered showers and thunderstorms on September 27th. Some thunderstorms produced heavy rain in short periods of time, resulting in flash flooding.\nEvent Narrative: Ruxton Road at Circle road was closed due to flash flooding. Owings Mills Boulevard at Red Run Boulevard was also closed due to flash flooding. German Hill and North Point Roads were closed due to flash flooding. There were water rescues due to flash flooding near Pikesville. Jones Falls was out of its banks near Falls Road and Smith Avenue. Bridges were closed along Smith Avenue. Parking lots were under water. Old Court Road at Park Heights Avenue was closed due to flash flooding. Water rescues were needed. Western Run Road was closed due to flash flooding. Beaver Dam Road was closed near Interstate 83 due to flash flooding. York Road was also closed at Wight Avenue due to flash flooding.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 28.7977 km away, between 2008-09-30 19:15:00 and 2008-09-30 19:15:00. The events included records with estimated wind gusts of 34.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: An approaching cold front combined with an unstable atmosphere to trigger showers and thunderstorms. An isolated thunderstorm produced gusty winds over the Chesapeake Bay.\nEvent Narrative: A wind gust in excess of 30 knots was reported at Martin State Airport.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 38.106 km away, between 2008-10-01 14:30:00 and 2008-10-01 14:30:00. The events included records with estimated wind gusts of 34.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front combined with an unstable atmosphere to trigger showers and isolated thunderstorms. An isolated thunderstorm produced gusty winds over the Chesapeake Bay.\nEvent Narrative: A wind gust in excess of 30 knots was occurred at Tolchester Beach.", "The following events were reported: Heavy Rain. These occurred near station USW00093721, approximately 42.0433 km away, between 2008-12-11 12:00:00 and 2008-12-12 01:00:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Heavy rain and poor drainage flooding affected Maryland on the 11th into the 12th. Rain began during the afternoon of the 10th and continued through the 11th into the early morning on the 12th. Rain fell at its heaviest from the afternoon of the 11th until just after Midnight EST on the 12th. Event precipitation totals averaged between one and a half and three and a half inches. ||The heavy rain was caused by a low pressure system that developed along the Gulf Coast States on the 10th. This intensifying low pressure system moved northeast from Alabama on the morning of the 11th, to central North Carolina early in the evening on the 11th to near Bridgeport, Connecticut at 7 a.m. EST on the 12th. Heavy rain and poor drainage flooding affected Maryland on the 11th into the 12th. Rain began during the afternoon of the 10th and continued through the 11th into the early morning on the 12th. Rain fell at its heaviest from the afternoon of the 11th until just after Midnight EST on the 12th. Event precipitation totals averaged between one and a half and three and a half inches. ||The heavy rain was caused by a low pressure system that developed along the Gulf Coast States on the 10th. This intensifying low pressure system moved northeast from Alabama on the morning of the 11th, to central North Carolina early in the evening on the 11th to near Bridgeport, Connecticut at 7 a.m. EST on the 12th.\nEvent Narrative: Event precipitation totals included 3.16 inches in Millington. Event precipitation totals included 2.21 inches in Stevensville.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 13.9057 km away, between 2009-02-11 22:14:00 and 2009-02-11 22:14:00. The events included records with measured wind gusts of 34.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A potent cold front passed through the Tidal Potomac and Chesapeake Bay during the evening of the 11th. A warm moist flow ahead of the front caused more instability than usual for this time of year. The combination of the cold front and instability caused showers and thunderstorms to develop. Some thunderstorms were severe, producing damaging winds.\nEvent Narrative: A wind gust of 34 knots was measured 2 miles southeast of Baltimore.", "The following events were reported: Hail. These occurred near station USW00093721, approximately 47.7666 km away, between 2009-03-29 16:56:00 and 2009-03-29 16:56:00. The events included records with hailstones measuring 0.88 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front passed through the Mid-Atlantic on the 29th. A southerly flow ahead of the front ushered in plenty of warm and moist air from the Gulf of Mexico. This air mass was unstable enough to trigger showers and thunderstorms on the 29th as the cold front moved through. A few thunderstorms did become severe, producing large hail.\nEvent Narrative: Penny to nickel sized hail was reported just west-northwest of Hereford.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 13.5337 km away, between 2009-03-29 17:00:00 and 2009-03-29 17:00:00. The events included records with estimated wind gusts of 34.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front passed through the Mid-Atlantic on the 29th. A southerly flow ahead of the front ushered in plenty of warm and moist air from the Gulf of Mexico. This air mass was unstable enough to trigger showers and thunderstorms on the 29th as the cold front moved through. Some thunderstorms did produce gusty winds over the Tidal Potomac and Chesapeake Bay.\nEvent Narrative: A wind gust was estimated over 30 knots at the Maryland Science Center.", "The following events were reported: Hail. These occurred near station USW00093721, approximately 13.5459 km away, between 2009-04-21 17:37:00 and 2009-04-21 17:37:00. The events included records with hailstones measuring 0.75 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A boundary remained stationary over the region. This boundary combined with unstable air to trigger showers and thunderstorms across Maryland. Some thunderstorms during the late afternoon and early evening hours were severe, producing damaging winds and large hail.\nEvent Narrative: Penny sized hail was reported near Pasadena.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 34.3245 km away, between 2009-04-21 18:15:00 and 2009-04-21 18:40:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front combined with plenty of instability to trigger showers and thunderstorms across the Tidal Potomac and Chesapeake Bay. Some thunderstorms produced gusty winds. A cold front combined with plenty of instability to trigger showers and thunderstorms across the Tidal Potomac and Chesapeake Bay. Some thunderstorms produced gusty winds.\nEvent Narrative: A wind gust in excess of 30 knots was measured at Sandy Point. Wind gusts up to 35 knots were measured at Tolchester Beach.", "The following events were reported: Hail. These occurred near station USW00093721, approximately 13.5459 km away, between 2009-04-22 14:40:00 and 2009-04-22 14:40:00. The events included records with hailstones measuring 0.75 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front triggered showers and thunderstorms. An isolated thunderstorm did produce large hail in southern Maryland.\nEvent Narrative: Penny sized hail was reported in Pasadena.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 33.2485 km away, between 2009-04-22 16:55:00 and 2009-04-22 17:20:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Showers and thunderstorms popped up over the Tidal Potomac and Chesapeake Bay. There was enough instability for some thunderstorms to contain gusty winds. Showers and thunderstorms popped up over the Tidal Potomac and Chesapeake Bay. There was enough instability for some thunderstorms to contain gusty winds.\nEvent Narrative: A wind gust of 35 knots was measured at Hartmiller Island. A wind gust in excess of 30 knots was measured at Tolchester Beach.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 19.8142 km away, between 2009-05-25 14:50:00 and 2009-05-25 14:50:00. The events included records with estimated wind gusts of 52.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front combined with an unstable atmosphere to trigger showers and thunderstorms across portions of Maryland on the 25th. An isolated thunderstorm did produce damaging winds.\nEvent Narrative: A thunderstorm wind gust was estimated at 60 mph.", "The following events were reported: Flash Flood. These occurred near station USW00093721, approximately 17.3041 km away, between 2009-05-26 06:48:00 and 2009-05-26 08:00:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A wave of low pressure riding along a stalled boundary triggered rain and thunderstorms. Heavy amounts of rain in a short period of time lead to isolated areas of flash flooding. A wave of low pressure riding along a stalled boundary triggered rain and thunderstorms. Heavy amounts of rain in a short period of time lead to isolated areas of flash flooding.\nEvent Narrative: Flash flooding was reported just east of Laurel. Muirkirk Road was closed near Route 1 due to flash flooding.", "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00093721, approximately 18.4716 km away, between 2009-05-29 13:27:00 and 2009-05-29 14:30:00. The events included records with hailstones measuring 37.70375 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front combined with plenty of instability to trigger showers and thunderstorms. With plenty of instability and strong winds aloft, thunderstorms did become severe producing damaging winds and large hail. A cold front combined with plenty of instability to trigger showers and thunderstorms. With plenty of instability and strong winds aloft, thunderstorms did become severe producing damaging winds and large hail. A cold front combined with plenty of instability to trigger showers and thunderstorms. With plenty of instability and strong winds aloft, thunderstorms did become severe producing damaging winds and large hail. A cold front combined with plenty of instability to trigger showers and thunderstorms. With plenty of instability and strong winds aloft, thunderstorms did become severe producing damaging winds and large hail. A cold front combined with plenty of instability to trigger showers and thunderstorms. With plenty of instability and strong winds aloft, thunderstorms did become severe producing damaging winds and large hail. A cold front combined with plenty of instability to trigger showers and thunderstorms. With plenty of instability and strong winds aloft, thunderstorms did become severe producing damaging winds and large hail. A cold front combined with plenty of instability to trigger showers and thunderstorms. With plenty of instability and strong winds aloft, thunderstorms did become severe producing damaging winds and large hail. A cold front combined with plenty of instability to trigger showers and thunderstorms. With plenty of instability and strong winds aloft, thunderstorms did become severe producing damaging winds and large hail.\nEvent Narrative: Several large branches were broken by thunderstorm winds. Several mid-size branches were down from thunderstorm winds. Trees were down near Route 70 and Andover Road. Trees were down on homes in Herald Harbor. A tree was down in Belvedere Heights. Trees were down near Forked Creek Road and Shore Acres. Penny size hail was reported near Severna Park. Nickel size hail was reported near Arnold.", "The following events were reported: Marine Hail, Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 27.4787 km away, between 2009-05-29 14:22:00 and 2009-05-29 15:00:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front combined with plenty of instability to trigger showers and thunderstorms. Thunderstorms produced gusty winds and large hail over the Tidal Potomac and Chesapeake Bay. A cold front combined with plenty of instability to trigger showers and thunderstorms. Thunderstorms produced gusty winds and large hail over the Tidal Potomac and Chesapeake Bay. A cold front combined with plenty of instability to trigger showers and thunderstorms. Thunderstorms produced gusty winds and large hail over the Tidal Potomac and Chesapeake Bay.\nEvent Narrative: Penny size hail was reported near Severna Park. A wind gust in excess of 30 knots was reported at Stevensville. A wind gust in excess of 30 knots was reported at Sandy Point.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 41.1359 km away, between 2009-05-29 14:45:00 and 2009-05-29 14:45:00. The events included records with estimated wind gusts of 52.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 50000.0 and crop damage of 0.0. \n\nEpisode Narrative: Strong to locally severe thunderstorms moved across the Maryland Eastern Shore during the afternoon of the 29th. The thunderstorms preceded a cold front that moved through the Middle Atlantic States during the night of the 29th.\nEvent Narrative: A severe thunderstorm knocked down a line of trees along Eastern Neck Road south of Rock Hall. A travel trailer was destroyed by a downed tree.", "The following events were reported: Hail, Thunderstorm Wind, Tornado. These occurred near station USW00093721, approximately 26.4689 km away, between 2009-06-09 15:28:00 and 2009-06-09 16:43:00. The events included records with hailstones measuring 28.19454545454545 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front approached the area on the 9th. Ahead of the front, warm and humid air led to unstable conditions. The instability combined with the boundary and an upper-level disturbance to trigger showers and thunderstorms on the afternoon and evening hours of the 9th. Some thunderstorms became severe, producing large hail and damaging winds. A cold front approached the area on the 9th. Ahead of the front, warm and humid air led to unstable conditions. The instability combined with the boundary and an upper-level disturbance to trigger showers and thunderstorms on the afternoon and evening hours of the 9th. Some thunderstorms became severe, producing large hail and damaging winds. A cold front approached the area on the 9th. Ahead of the front, warm and humid air led to unstable conditions. The instability combined with the boundary and an upper-level disturbance to trigger showers and thunderstorms on the afternoon and evening hours of the 9th. Some thunderstorms became severe, producing large hail and damaging winds. A cold front approached the area on the 9th. Ahead of the front, warm and humid air led to unstable conditions. The instability combined with the boundary and an upper-level disturbance to trigger showers and thunderstorms on the afternoon and evening hours of the 9th. Some thunderstorms became severe, producing large hail and damaging winds. A cold front approached the area on the 9th. Ahead of the front, warm and humid air led to unstable conditions. The instability combined with the boundary and an upper-level disturbance to trigger showers and thunderstorms on the afternoon and evening hours of the 9th. Some thunderstorms became severe, producing large hail and damaging winds. A cold front approached the area on the 9th. Ahead of the front, warm and humid air led to unstable conditions. The instability combined with the boundary and an upper-level disturbance to trigger showers and thunderstorms on the afternoon and evening hours of the 9th. Some thunderstorms became severe, producing large hail and damaging winds. A cold front approached the area on the 9th. Ahead of the front, warm and humid air led to unstable conditions. The instability combined with the boundary and an upper-level disturbance to trigger showers and thunderstorms on the afternoon and evening hours of the 9th. Some thunderstorms became severe, producing large hail and damaging winds. A cold front approached the area on the 9th. Ahead of the front, warm and humid air led to unstable conditions. The instability combined with the boundary and an upper-level disturbance to trigger showers and thunderstorms on the afternoon and evening hours of the 9th. Some thunderstorms became severe, producing large hail and damaging winds. A cold front approached the area on the 9th. Ahead of the front, warm and humid air led to unstable conditions. The instability combined with the boundary and an upper-level disturbance to trigger showers and thunderstorms on the afternoon and evening hours of the 9th. Some thunderstorms became severe, producing large hail and damaging winds. A cold front approached the area on the 9th. Ahead of the front, warm and humid air led to unstable conditions. The instability combined with the boundary and an upper-level disturbance to trigger showers and thunderstorms on the afternoon and evening hours of the 9th. Some thunderstorms became severe, producing large hail and damaging winds. A cold front approached the area on the 9th. Ahead of the front, warm and humid air led to unstable conditions. The instability combined with the boundary and an upper-level disturbance to trigger showers and thunderstorms on the afternoon and evening hours of the 9th. Some thunderstorms became severe, producing large hail and damaging winds. A cold front approached the area on the 9th. Ahead of the front, warm and humid air led to unstable conditions. The instability combined with the boundary and an upper-level disturbance to trigger showers and thunderstorms on the afternoon and evening hours of the 9th. Some thunderstorms became severe, producing large hail and damaging winds.\nEvent Narrative: Nickel size hail was reported near Butler. An tree eight inches in diameter was blown down. Trees and large branches were down, and there were also power outages in Towson. A large tree was down at Seven Courts Drive and Bourbon Street. Winds were estimated at 50 knots. Penny size hail was reported near Ridgeway. Nickel size hail was reported near Essex. Nickel size hail was reported near Rossville. Penny size hail was reported near Magnolia. A wind gust of 65 mph was measured near Crownsville. Thunderstorm wind gusts were estimated around 50 knots. National Weather Service survey indicated that a tornado touched down near the Oak Lawn Cemetery and it continued towards Plainfield Road. The path length was about one mile and the path width was 150 yards. The tornado was an EF-0 with peak winds estimated at 70 mph. ||Several trees were snapped or uprooted along the path. The tornado was also responsible for structure damage to three townhouses on Berkshire Lane.", "The following events were reported: Marine Hail, Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 32.2132 km away, between 2009-06-09 16:31:00 and 2009-06-09 17:27:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front approached the waters on the 9th. Ahead of the front, warm and humid air led to unstable conditions. The instability combined with the boundary and an upper-level disturbance to trigger showers and thunderstorms on the afternoon and evening hours of the 9th. Some thunderstorms became severe, producing large hail and gusty winds. A cold front approached the waters on the 9th. Ahead of the front, warm and humid air led to unstable conditions. The instability combined with the boundary and an upper-level disturbance to trigger showers and thunderstorms on the afternoon and evening hours of the 9th. Some thunderstorms became severe, producing large hail and gusty winds. A cold front approached the waters on the 9th. Ahead of the front, warm and humid air led to unstable conditions. The instability combined with the boundary and an upper-level disturbance to trigger showers and thunderstorms on the afternoon and evening hours of the 9th. Some thunderstorms became severe, producing large hail and gusty winds. A cold front approached the waters on the 9th. Ahead of the front, warm and humid air led to unstable conditions. The instability combined with the boundary and an upper-level disturbance to trigger showers and thunderstorms on the afternoon and evening hours of the 9th. Some thunderstorms became severe, producing large hail and gusty winds. A cold front approached the waters on the 9th. Ahead of the front, warm and humid air led to unstable conditions. The instability combined with the boundary and an upper-level disturbance to trigger showers and thunderstorms on the afternoon and evening hours of the 9th. Some thunderstorms became severe, producing large hail and gusty winds. A cold front approached the waters on the 9th. Ahead of the front, warm and humid air led to unstable conditions. The instability combined with the boundary and an upper-level disturbance to trigger showers and thunderstorms on the afternoon and evening hours of the 9th. Some thunderstorms became severe, producing large hail and gusty winds. A cold front approached the waters on the 9th. Ahead of the front, warm and humid air led to unstable conditions. The instability combined with the boundary and an upper-level disturbance to trigger showers and thunderstorms on the afternoon and evening hours of the 9th. Some thunderstorms became severe, producing large hail and gusty winds. A cold front approached the waters on the 9th. Ahead of the front, warm and humid air led to unstable conditions. The instability combined with the boundary and an upper-level disturbance to trigger showers and thunderstorms on the afternoon and evening hours of the 9th. Some thunderstorms became severe, producing large hail and gusty winds.\nEvent Narrative: A wind gust of 50 knots was estimated about five miles west-southwest of Annapolis. Wind gusts from 35 knots to 46 knots were reported at Kent Island. Wind gusts of 35 knots was measured at Sandy Point. Wind gusts ranged from 35 to 41 knots at Miller Island. A wind gust in excess of 30 knots was reported at Martin State. Penny size hail was reported near Magnolia. A wind gust of 36 knots was reported at Annapolis. A wind gust of 37 knots was reported at GunPowder Falls State Park.", "The following events were reported: Flash Flood. These occurred near station USW00093721, approximately 26.7816 km away, between 2009-06-09 16:50:00 and 2009-06-09 19:50:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: An upper-level disturbance combined with plenty of moisture and an unstable atmosphere to trigger showers and thunderstorms during on the 9th. With locally heavy rain in a short period of time, this lead to isolated areas of flash flooding.\nEvent Narrative: Flash flooding was reported along a creek near Victory Villa Elementary School.", "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00093721, approximately 40.3836 km away, between 2009-06-10 17:46:00 and 2009-06-10 18:17:00. The events included records with hailstones measuring 18.87666666666667 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A stationary boundary remained over the region while an upper-level disturbance passed through. These systems combined with warm and humid air ahead of the boundary to trigger showers and thunderstorms. Some thunderstorms were severe, producing large hail. A stationary boundary remained over the region while an upper-level disturbance passed through. These systems combined with warm and humid air ahead of the boundary to trigger showers and thunderstorms. Some thunderstorms were severe, producing large hail. A stationary boundary remained over the region while an upper-level disturbance passed through. These systems combined with warm and humid air ahead of the boundary to trigger showers and thunderstorms. Some thunderstorms were severe, producing large hail.\nEvent Narrative: Penny size hail was reported near Patapsco. Two dozen trees were down due to thunderstorm winds. A tree also fell on a house at the intersection of Cockeys Mill Road and Franklin Valley Circle. Nickel size hail was reported near Finksburg.", "The following events were reported: Flash Flood. These occurred near station USW00093721, approximately 28.6805 km away, between 2009-06-10 20:00:00 and 2009-06-10 23:00:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Showers and thunderstorms developed due to plenty of instability in the atmosphere. Thunderstorms produced locally heavy rain. Since the ground was already saturated from previous rainfall, this lead to areas of flash flooding.\nEvent Narrative: Pleasant Hill Road and Red Run Road were closed due to flash flooding. The intersection of Dolfield Road and Pleasant Hill Road was also closed due to flash flooding.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 45.0478 km away, between 2009-06-11 17:08:00 and 2009-06-11 17:08:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Widely scattered strong to severe thunderstorms moved across the Maryland Eastern Shore during the early evening of June 11th. These thunderstorms formed close to a nearly stationary frontal boundary.\nEvent Narrative: A severe thunderstorm tore down large tree limbs and wires on the southern part of Kent Island.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 44.0281 km away, between 2009-06-11 17:11:00 and 2009-06-11 17:11:00. The events included records with measured wind gusts of 35.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: An unstable atmosphere lead to the development of scattered showers and thunderstorms. An isolated thunderstorm did produce gusty winds.\nEvent Narrative: A wind gust of 35 knots was reported about seven miles southeast of Highland Beach.", "The following events were reported: Heavy Rain. These occurred near station USW00093721, approximately 36.8966 km away, between 2009-06-18 06:30:00 and 2009-06-18 08:00:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Heavy rain associated with an approaching warm front that coincided with the high tide produced some flooding in and around Kent Island in Queen Anne's County.\nEvent Narrative: Heavy rain fell from about 730 a.m. EDT and 900 a.m. EDT on the morning of the 18th in and around Kent Island. Doppler Radar storm total estimates reached about one inch. But, the heavy rain coincided with the high tide which was higher than normal because of the approaching new moon and an up the bay wind flow. This caused roadway and field flooding around the region. On Kent Island, Thompson Creek Road flooded as did the Thompson Creek Public Landing. At the Kent Narrows, Wharf Drive flooded as did the parking lot of a seafood market. On the Eastern Shore, Winchester Creek flooded some front yards in Grasonville. Standing water was on Main Street in Queenstown. The high tide that morning at Tolchester Beach (Kent County) and Cambridge (Dorchester County) reached 3.50 feet above mean lower low water. That is the level at which minor tidal flooding begins.", "The following events were reported: Hail, Tornado. These occurred near station USW00093721, approximately 32.107 km away, between 2009-06-20 14:31:00 and 2009-06-20 14:52:00. The events included records with hailstones measuring 1.25 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: An unstable atmosphere lead to the development of scattered showers and thunderstorms across Maryland. Some thunderstorms did become severe, producing damaging winds and large hail. An unstable atmosphere lead to the development of scattered showers and thunderstorms across Maryland. Some thunderstorms did become severe, producing damaging winds and large hail. An unstable atmosphere lead to the development of scattered showers and thunderstorms across Maryland. Some thunderstorms did become severe, producing damaging winds and large hail.\nEvent Narrative: Half dollar size hail was reported near Middle River. National Weather Service survey indicated an EF-0 tornado touched down near Pleasant Hills before dissipating near the Atkisson Resorvoir. Peak wind speeds were estimated around 75 mph. ||Several trees were down in Pleasant Hills and also near the intersection of Hollingsworth Drive and Ring Factory Road. National Weather Service survey indicated that a tornado touched down near Essex as an EF-0. Peak winds were estimated around 70 mph. Several trees were down and there was minor shingle and siding damage reported throughout the community of Essex. ||The tornado intensified as it approached Browns Creek and Balliston Point. The tornado uprooted or snapped down a significant portion of large trees in the community along Island View Road. The tornado across this area was classified as an EF-1 with peak winds of 90 mph. The tornado finally weakened as it moved over the Bay.", "The following events were reported: Waterspout. These occurred near station USW00093721, approximately 23.2123 km away, between 2009-06-20 14:44:00 and 2009-06-20 14:52:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: An unstable atmosphere lead to the development of scattered showers and thunderstorms across the Tidal Potomac and Chesapeake Bay. Some thunderstorms did become severe, producing damaging winds.\nEvent Narrative: A waterspout developed over the Chesapeake Bay near Essex and it tracked across the Bay before dissipating towards the Chester River. Several motorists were able to see the waterspout from the Bay Bridge. No damage was reported.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 40.0884 km away, between 2009-06-20 15:07:00 and 2009-06-20 15:07:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Strong to locally severe thunderstorms occurred in the Maryland Eastern Shore during the afternoon of the 20th. The area barely made it into the warm sector (south of the warm front and east of the approaching cold front) of a low pressure system that moved through Pennsylvania and New Jersey on the 20th.\nEvent Narrative: The gust front from a severe thunderstorm flattened a corn field (was year old corn) off of Auckland Road near Love Point on Kent Island. This was the same parent thunderstorm that produced waterspouts on Chesapeake Bay.", "The following events were reported: Hail. These occurred near station USW00093721, approximately 29.9609 km away, between 2009-06-26 19:37:00 and 2009-06-26 19:37:00. The events included records with hailstones measuring 0.75 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A potent cold front combined with plenty of instability to trigger showers and thunderstorms. Some thunderstorms were severe, producing damaging winds and large hail.\nEvent Narrative: Penny size hail was reported near Annapolis.", "The following events were reported: Hail. These occurred near station USW00093721, approximately 44.624 km away, between 2009-07-24 17:02:00 and 2009-07-24 18:00:00. The events included records with hailstones measuring 0.75 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A trough of low pressure over the region caused showers and thunderstorms to develop. There was enough cold air aloft for some thunderstorms to become severe. A trough of low pressure over the region caused showers and thunderstorms to develop. There was enough cold air aloft for some thunderstorms to become severe.\nEvent Narrative: Penny size hail was reported in Finksburg. Penny size hail was reported in Sewell.", "The following events were reported: Marine Hail. These occurred near station USW00093721, approximately 49.8343 km away, between 2009-07-24 18:08:00 and 2009-07-24 18:08:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front passed through the waters triggering showers and thunderstorms. There was enough instability ahead of the front for an isolated thunderstorm to produce large hail.\nEvent Narrative: Penny size hail was reported near Belcamp.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 26.9242 km away, between 2009-07-25 19:06:00 and 2009-07-25 20:35:00. The events included records with measured wind gusts of 36.5 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Showers and thunderstorms developed ahead of a cold front on the 25th. There was enough instability along with strong winds aloft for a couple thunderstorms to produce gusty winds. Showers and thunderstorms developed ahead of a cold front on the 25th. There was enough instability along with strong winds aloft for a couple thunderstorms to produce gusty winds.\nEvent Narrative: A wind gust of 38 knots was measured at Kent Island. Wind gusts up to 35 knots were reported at Baltimore Key Bridge.", "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00093721, approximately 33.0902 km away, between 2009-07-26 16:35:00 and 2009-07-26 17:17:00. The events included records with hailstones measuring 42.17307692307692 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: An upper-level low over the Great lakes provided cooler air aloft. The warm and humid air at the surface combined with the cooler air aloft to allow for an unstable atmosphere. Showers and thunderstorms popped up on the 26th over Maryland. The winds aloft were strong enough for some thunderstorms to become severe. An upper-level low over the Great lakes provided cooler air aloft. The warm and humid air at the surface combined with the cooler air aloft to allow for an unstable atmosphere. Showers and thunderstorms popped up on the 26th over Maryland. The winds aloft were strong enough for some thunderstorms to become severe. An upper-level low over the Great lakes provided cooler air aloft. The warm and humid air at the surface combined with the cooler air aloft to allow for an unstable atmosphere. Showers and thunderstorms popped up on the 26th over Maryland. The winds aloft were strong enough for some thunderstorms to become severe. An upper-level low over the Great lakes provided cooler air aloft. The warm and humid air at the surface combined with the cooler air aloft to allow for an unstable atmosphere. Showers and thunderstorms popped up on the 26th over Maryland. The winds aloft were strong enough for some thunderstorms to become severe. An upper-level low over the Great lakes provided cooler air aloft. The warm and humid air at the surface combined with the cooler air aloft to allow for an unstable atmosphere. Showers and thunderstorms popped up on the 26th over Maryland. The winds aloft were strong enough for some thunderstorms to become severe. An upper-level low over the Great lakes provided cooler air aloft. The warm and humid air at the surface combined with the cooler air aloft to allow for an unstable atmosphere. Showers and thunderstorms popped up on the 26th over Maryland. The winds aloft were strong enough for some thunderstorms to become severe. An upper-level low over the Great lakes provided cooler air aloft. The warm and humid air at the surface combined with the cooler air aloft to allow for an unstable atmosphere. Showers and thunderstorms popped up on the 26th over Maryland. The winds aloft were strong enough for some thunderstorms to become severe. An upper-level low over the Great lakes provided cooler air aloft. The warm and humid air at the surface combined with the cooler air aloft to allow for an unstable atmosphere. Showers and thunderstorms popped up on the 26th over Maryland. The winds aloft were strong enough for some thunderstorms to become severe. An upper-level low over the Great lakes provided cooler air aloft. The warm and humid air at the surface combined with the cooler air aloft to allow for an unstable atmosphere. Showers and thunderstorms popped up on the 26th over Maryland. The winds aloft were strong enough for some thunderstorms to become severe. An upper-level low over the Great lakes provided cooler air aloft. The warm and humid air at the surface combined with the cooler air aloft to allow for an unstable atmosphere. Showers and thunderstorms popped up on the 26th over Maryland. The winds aloft were strong enough for some thunderstorms to become severe. An upper-level low over the Great lakes provided cooler air aloft. The warm and humid air at the surface combined with the cooler air aloft to allow for an unstable atmosphere. Showers and thunderstorms popped up on the 26th over Maryland. The winds aloft were strong enough for some thunderstorms to become severe. An upper-level low over the Great lakes provided cooler air aloft. The warm and humid air at the surface combined with the cooler air aloft to allow for an unstable atmosphere. Showers and thunderstorms popped up on the 26th over Maryland. The winds aloft were strong enough for some thunderstorms to become severe. An upper-level low over the Great lakes provided cooler air aloft. The warm and humid air at the surface combined with the cooler air aloft to allow for an unstable atmosphere. Showers and thunderstorms popped up on the 26th over Maryland. The winds aloft were strong enough for some thunderstorms to become severe.\nEvent Narrative: Trees and power lines were down on Deer Park Road. A tree fell onto a house. Trees and power lines were down on Cherry Hill Court. A tree fell on a house. Numerous trees were down and trees fell on houses at the intersection of Berrymans and Church Road. Trees and wires were down on Sunbrook Road. Trees were down along Route 94. A tree was blown down on Lyons Mill Road. Several tree branches were down in Eldersburg. Multiple trees were down in Owings Mills. Trees and power lines were down on Deer Park Road. Numerous trees were down. Trees fell on houses in the Church Road Area. Penny size hail was reported in Lisbon. Penny size hail was reported in Owings Mills. Golf ball size hail was reported near Fallston.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 30.543 km away, between 2009-07-29 18:22:00 and 2009-07-29 18:22:00. The events included records with measured wind gusts of 37.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: An area of low pressure and its associated cold front passed through the region on the 29th. Strong winds aloft combined with an unstable atmosphere for showers and thunderstorms to develop. Some thunderstorms did produce gusty winds.\nEvent Narrative: A wind gust of 37 knots was measured at Sandy Point.", "The following events were reported: Thunderstorm Wind, Tornado. These occurred near station USW00093721, approximately 32.4841 km away, between 2009-07-31 13:24:00 and 2009-07-31 14:29:00.The events resulted in 1 injuries and 0 fatalities. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front and its associated trough of low pressure triggered showers and thunderstorms across Maryland. A southwest flow ahead of the front ushered in plenty of moisture from the Gulf of Mexico, resulting in an unstable atmosphere. The moderate amounts of instability combined with the forcing from the front and strong winds aloft for some thunderstorms to become severe. A cold front and its associated trough of low pressure triggered showers and thunderstorms across Maryland. A southwest flow ahead of the front ushered in plenty of moisture from the Gulf of Mexico, resulting in an unstable atmosphere. The moderate amounts of instability combined with the forcing from the front and strong winds aloft for some thunderstorms to become severe. A cold front and its associated trough of low pressure triggered showers and thunderstorms across Maryland. A southwest flow ahead of the front ushered in plenty of moisture from the Gulf of Mexico, resulting in an unstable atmosphere. The moderate amounts of instability combined with the forcing from the front and strong winds aloft for some thunderstorms to become severe. A cold front and its associated trough of low pressure triggered showers and thunderstorms across Maryland. A southwest flow ahead of the front ushered in plenty of moisture from the Gulf of Mexico, resulting in an unstable atmosphere. The moderate amounts of instability combined with the forcing from the front and strong winds aloft for some thunderstorms to become severe. A cold front and its associated trough of low pressure triggered showers and thunderstorms across Maryland. A southwest flow ahead of the front ushered in plenty of moisture from the Gulf of Mexico, resulting in an unstable atmosphere. The moderate amounts of instability combined with the forcing from the front and strong winds aloft for some thunderstorms to become severe. A cold front and its associated trough of low pressure triggered showers and thunderstorms across Maryland. A southwest flow ahead of the front ushered in plenty of moisture from the Gulf of Mexico, resulting in an unstable atmosphere. The moderate amounts of instability combined with the forcing from the front and strong winds aloft for some thunderstorms to become severe. A cold front and its associated trough of low pressure triggered showers and thunderstorms across Maryland. A southwest flow ahead of the front ushered in plenty of moisture from the Gulf of Mexico, resulting in an unstable atmosphere. The moderate amounts of instability combined with the forcing from the front and strong winds aloft for some thunderstorms to become severe. A cold front and its associated trough of low pressure triggered showers and thunderstorms across Maryland. A southwest flow ahead of the front ushered in plenty of moisture from the Gulf of Mexico, resulting in an unstable atmosphere. The moderate amounts of instability combined with the forcing from the front and strong winds aloft for some thunderstorms to become severe. A cold front and its associated trough of low pressure triggered showers and thunderstorms across Maryland. A southwest flow ahead of the front ushered in plenty of moisture from the Gulf of Mexico, resulting in an unstable atmosphere. The moderate amounts of instability combined with the forcing from the front and strong winds aloft for some thunderstorms to become severe. A cold front and its associated trough of low pressure triggered showers and thunderstorms across Maryland. A southwest flow ahead of the front ushered in plenty of moisture from the Gulf of Mexico, resulting in an unstable atmosphere. The moderate amounts of instability combined with the forcing from the front and strong winds aloft for some thunderstorms to become severe. A cold front and its associated trough of low pressure triggered showers and thunderstorms across Maryland. A southwest flow ahead of the front ushered in plenty of moisture from the Gulf of Mexico, resulting in an unstable atmosphere. The moderate amounts of instability combined with the forcing from the front and strong winds aloft for some thunderstorms to become severe.\nEvent Narrative: Numerous trees were down. A tree top fell into the driveway and large branches were down along Cypress Creek. Damage was reported to mobile homes near Finksburg. Trees and power lines were down on Klee Mill Road near Sykesville Road. Trees and power lines were down at Salem Bottom Road and Bloom Road. Numerous trees were down near Alpha. Numerous trees were down across the northern portion of Baltimore. Nine large hardwood trees were down near Mount Airy. Trees were down in Arnold due to thunderstorm winds. A large tree limb was down just west of Deer Park Road. Two pine trees were down on the westernmost portion of Constellation Way. Two residents suffered a significant loss of roof covering material. Several pine trees were uprooted at several locations along with numerous tree limbs broken. A portion of a corn field was blown over along Kays Mill Road. Multiple trees were down along Route 97 including at the intersection of Cattail Creek Drive.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 33.9864 km away, between 2009-07-31 14:41:00 and 2009-07-31 14:48:00. The events included records with measured wind gusts of 36.5 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front and its associated trough of low pressure triggered showers and thunderstorms across the Tidal Potomac and Chesapeake Bay. A southwest flow ahead of the front ushered in plenty of moisture from the Gulf of Mexico, resulting in an unstable atmosphere. The moderate amounts of instability combined with the forcing from the front and strong winds aloft for some thunderstorms to produce gusty winds. A cold front and its associated trough of low pressure triggered showers and thunderstorms across the Tidal Potomac and Chesapeake Bay. A southwest flow ahead of the front ushered in plenty of moisture from the Gulf of Mexico, resulting in an unstable atmosphere. The moderate amounts of instability combined with the forcing from the front and strong winds aloft for some thunderstorms to produce gusty winds.\nEvent Narrative: A wind gust of 35 knots was reported at Kent Island. A wind gust of 38 knots was reported at Miller Island.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 38.5116 km away, between 2009-07-31 14:45:00 and 2009-07-31 14:45:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front that moved through the Eastern Shore Friday afternoon helped produce strong to severe thunderstorms during the late afternoon of the 31st. Most of the wind damage occurred as a line of severe thunderstorms known as a bow echo moved across the region. Delmarva Power and Light reported about 8,000 homes and businesses lost power across the Delmarva Peninsula. Power was fully restored by August 1st.\nEvent Narrative: A severe thunderstorm knocked down trees and wires in Rock Hall.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 28.3911 km away, between 2009-08-09 18:17:00 and 2009-08-09 18:17:00. The events included records with measured wind gusts of 36.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Strong surface heating triggered an unstable atmosphere on the 9th. Despite a lack of strong forcing aloft, scattered showers and thunderstorms developed due to the instability. Isolated thunderstorms did produce gusty winds.\nEvent Narrative: A wind gust of 36 knots was measured at Miller Island.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 21.3289 km away, between 2009-08-10 20:12:00 and 2009-08-10 20:50:00. The events included records with measured wind gusts of 47.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Strong surface heating triggered an unstable atmosphere on the 10th. Despite a lack of strong forcing aloft, scattered showers and thunderstorms developed due to the instability. Isolated thunderstorms did produce gusty winds over the Chesapeake Bay. Strong surface heating triggered an unstable atmosphere on the 10th. Despite a lack of strong forcing aloft, scattered showers and thunderstorms developed due to the instability. Isolated thunderstorms did produce gusty winds over the Chesapeake Bay.\nEvent Narrative: Wind gusts ranged between 36 and 48 knots at the Baltimore Key Bridge. Wind gusts of 45 to 46 knots were measured at Miller Island.", "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00093721, approximately 26.7941 km away, between 2009-08-18 16:15:00 and 2009-08-18 16:56:00. The events included records with hailstones measuring 40.15 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A southwest flow around high pressure over the western Atlantic ushered in plenty of low-level moisture across Maryland. The moisture combined with strong surface heating for an unstable atmosphere. Showers and thunderstorms developed due to the instability, and some of the thunderstorms were severe. A southwest flow around high pressure over the western Atlantic ushered in plenty of low-level moisture across Maryland. The moisture combined with strong surface heating for an unstable atmosphere. Showers and thunderstorms developed due to the instability, and some of the thunderstorms were severe. A southwest flow around high pressure over the western Atlantic ushered in plenty of low-level moisture across Maryland. The moisture combined with strong surface heating for an unstable atmosphere. Showers and thunderstorms developed due to the instability, and some of the thunderstorms were severe. A southwest flow around high pressure over the western Atlantic ushered in plenty of low-level moisture across Maryland. The moisture combined with strong surface heating for an unstable atmosphere. Showers and thunderstorms developed due to the instability, and some of the thunderstorms were severe. A southwest flow around high pressure over the western Atlantic ushered in plenty of low-level moisture across Maryland. The moisture combined with strong surface heating for an unstable atmosphere. Showers and thunderstorms developed due to the instability, and some of the thunderstorms were severe.\nEvent Narrative: Penny size hail was reported near Riverdale. A tree was down near Severna Park. A tree was down near the intersection of Harford Road and Putty Hill Avenue. A tree was down on Harford Road and Cub Hill Road. A tree was down on Forest Drive.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 39.4601 km away, between 2009-08-21 14:43:00 and 2009-08-21 14:45:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A hot and humid air mass was in place on the 21st ahead of a cold front. This resulted in the development of some thunderstorms from west to east, some of which were strong to locally severe.\nEvent Narrative: A squall line of strong to severe thunderstorms knocked down about 5 trees in Rock Hall and Fairee.", "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00093721, approximately 35.3156 km away, between 2009-08-21 18:30:00 and 2009-08-21 20:45:00. The events included records with hailstones measuring 30.3 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A southwest flow between an upper-level low over the Great Lakes and high pressure over the western Atlantic ushered in plenty of moisture from the Gulf of Mexico. The moisture combined with strong surface heating to produce an unstable atmosphere. Showers and thunderstorms developed due to the unstable atmosphere and some thunderstorms were severe. A southwest flow between an upper-level low over the Great Lakes and high pressure over the western Atlantic ushered in plenty of moisture from the Gulf of Mexico. The moisture combined with strong surface heating to produce an unstable atmosphere. Showers and thunderstorms developed due to the unstable atmosphere and some thunderstorms were severe. A southwest flow between an upper-level low over the Great Lakes and high pressure over the western Atlantic ushered in plenty of moisture from the Gulf of Mexico. The moisture combined with strong surface heating to produce an unstable atmosphere. Showers and thunderstorms developed due to the unstable atmosphere and some thunderstorms were severe. A southwest flow between an upper-level low over the Great Lakes and high pressure over the western Atlantic ushered in plenty of moisture from the Gulf of Mexico. The moisture combined with strong surface heating to produce an unstable atmosphere. Showers and thunderstorms developed due to the unstable atmosphere and some thunderstorms were severe. A southwest flow between an upper-level low over the Great Lakes and high pressure over the western Atlantic ushered in plenty of moisture from the Gulf of Mexico. The moisture combined with strong surface heating to produce an unstable atmosphere. Showers and thunderstorms developed due to the unstable atmosphere and some thunderstorms were severe.\nEvent Narrative: A tree was down near Daisy. A tree was down along Watersville Road. A tree was down along Cars Mill Road. Penny size hail was reported in Reisterstown. Penny size hail was reported near Bowleys Quarters.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 28.3911 km away, between 2009-08-21 20:46:00 and 2009-08-21 20:46:00. The events included records with estimated wind gusts of 34.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A southwest flow between an upper-level low over the Great Lakes and high pressure over the western Atlantic ushered in plenty of moisture from the Gulf of Mexico. The moisture combined with strong surface heating to produce an unstable atmosphere. Showers and thunderstorms developed due to the unstable atmosphere and a few thunderstorms produced gusty winds over the Chesapeake Bay and the Potomac River.\nEvent Narrative: A wind gust in excess of 30 knots was measured at Miller Island.", "The following events were reported: Flash Flood. These occurred near station USW00093721, approximately 26.5977 km away, between 2009-08-22 17:00:00 and 2009-08-22 20:15:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: With the Mid-Atlantic States sandwiched between a cold front approaching from the west and Hurricane Bill several hundred miles offshore, an extremely moist atmosphere in place. A mesoscale area of low pressure formed over central Virginia and worked east-northeastward toward lower southern Maryland during the late afternoon and evening of the 22nd, produce a wide area of rain and thunderstorms that produced heavy rain and flash flooding. Numerous rainfall reports of 3 to 5 inches were received, with one report of 6.35 inches in North Beach. With the Mid-Atlantic States sandwiched between a cold front approaching from the west and Hurricane Bill several hundred miles offshore, an extremely moist atmosphere in place. A mesoscale area of low pressure formed over central Virginia and worked east-northeastward toward lower southern Maryland during the late afternoon and evening of the 22nd, produce a wide area of rain and thunderstorms that produced heavy rain and flash flooding. Numerous rainfall reports of 3 to 5 inches were received, with one report of 6.35 inches in North Beach. With the Mid-Atlantic States sandwiched between a cold front approaching from the west and Hurricane Bill several hundred miles offshore, an extremely moist atmosphere in place. A mesoscale area of low pressure formed over central Virginia and worked east-northeastward toward lower southern Maryland during the late afternoon and evening of the 22nd, produce a wide area of rain and thunderstorms that produced heavy rain and flash flooding. Numerous rainfall reports of 3 to 5 inches were received, with one report of 6.35 inches in North Beach. With the Mid-Atlantic States sandwiched between a cold front approaching from the west and Hurricane Bill several hundred miles offshore, an extremely moist atmosphere in place. A mesoscale area of low pressure formed over central Virginia and worked east-northeastward toward lower southern Maryland during the late afternoon and evening of the 22nd, produce a wide area of rain and thunderstorms that produced heavy rain and flash flooding. Numerous rainfall reports of 3 to 5 inches were received, with one report of 6.35 inches in North Beach. With the Mid-Atlantic States sandwiched between a cold front approaching from the west and Hurricane Bill several hundred miles offshore, an extremely moist atmosphere in place. A mesoscale area of low pressure formed over central Virginia and worked east-northeastward toward lower southern Maryland during the late afternoon and evening of the 22nd, produce a wide area of rain and thunderstorms that produced heavy rain and flash flooding. Numerous rainfall reports of 3 to 5 inches were received, with one report of 6.35 inches in North Beach.\nEvent Narrative: Road near the intersection of Route 214 and Beard's Point was closed due to flash flooding. Spotter reported 2.96 inches of rain near the event. Flash flooding reported on Hudson Street. Spotter reported 5.25 inches of rain just east of event. The intersection of Muddy Creek Road and Holly Landing was closed due to flash flooding. Rainfall measurement of 4.25 inches near the event reported by COCORAHS network. The intersection of Crownsville Road and Honeysuckle Lane was closed due to flash flooding. Road closed due to flash flooding near the intersection of Defense Highway and the Ridges. Rainfall report of 3.25 inches from COCORAHS observer just southeast of event area.", "The following events were reported: Flash Flood. These occurred near station USW00093721, approximately 38.1923 km away, between 2009-08-22 18:00:00 and 2009-08-22 21:00:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A strong cold front was approaching from the west during the 22nd, while Hurricane Bill passed well to our east. An abundance of moisture in place combined with enough instability, which resulted in showers and thunderstorms with locally torrential rainfall and flooding. Two day event totals averaged 3 to 6 inches, but amounts exceeded one foot locally in Ridgely in Caroline County.\nEvent Narrative: Nearly stationary thunderstorms with torrential downpours caused considerable roadway flooding as well as flooding of smaller streams in central and southern Queen Anne's County. Water on roadways were described as waist deep. Side streets were flooded and closed in Centreville. Flooding was also reported along Maryland State Route 404. Doppler Radar storm total estimates for the afternoon and evening of the 22nd averaged around three inches.", "The following events were reported: Flash Flood. These occurred near station USW00093721, approximately 37.1267 km away, between 2009-08-27 23:45:00 and 2009-08-28 04:30:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Moisture streaming northeastward from an upper low over the Deep South with additional moisture from Tropical Storm Danny off the North Carolina coast pooled up against a stationary boundary near the Mason-Dixon Line. Several Rounds of heavy rain-producing showers and thunderstorms pushed eastward along this boundary from the early morning hours through the evening of the 28th. This produced flash flooding over northeast Maryland. Numerous reports of rainfall totals of 3 to 5 inches, with isolated reports of over 7 inches in southeastern Harford and north central Carroll counties. Moisture streaming northeastward from an upper low over the Deep South with additional moisture from Tropical Storm Danny off the North Carolina coast pooled up against a stationary boundary near the Mason-Dixon Line. Several Rounds of heavy rain-producing showers and thunderstorms pushed eastward along this boundary from the early morning hours through the evening of the 28th. This produced flash flooding over northeast Maryland. Numerous reports of rainfall totals of 3 to 5 inches, with isolated reports of over 7 inches in southeastern Harford and north central Carroll counties. Moisture streaming northeastward from an upper low over the Deep South with additional moisture from Tropical Storm Danny off the North Carolina coast pooled up against a stationary boundary near the Mason-Dixon Line. Several Rounds of heavy rain-producing showers and thunderstorms pushed eastward along this boundary from the early morning hours through the evening of the 28th. This produced flash flooding over northeast Maryland. Numerous reports of rainfall totals of 3 to 5 inches, with isolated reports of over 7 inches in southeastern Harford and north central Carroll counties. Moisture streaming northeastward from an upper low over the Deep South with additional moisture from Tropical Storm Danny off the North Carolina coast pooled up against a stationary boundary near the Mason-Dixon Line. Several Rounds of heavy rain-producing showers and thunderstorms pushed eastward along this boundary from the early morning hours through the evening of the 28th. This produced flash flooding over northeast Maryland. Numerous reports of rainfall totals of 3 to 5 inches, with isolated reports of over 7 inches in southeastern Harford and north central Carroll counties.\nEvent Narrative: Route 7 near Abingdon Road closed due to high water. Flash flooding reported at Timber Grove Road near Owings Mills Blvd. Spotter reported 2.71 inches of rain near the event. A vehicle was stranded in 4 feet of water on Franklin Road near Reisterstown Road. Flash flooding reported on White Rock Road as well as report of flooded basement. Piney Run IFLOWS gauge measured 2.72 inches of rainfall.", "The following events were reported: Flash Flood. These occurred near station USW00093721, approximately 14.2324 km away, between 2009-09-06 17:21:00 and 2009-09-06 18:45:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Deep layer easterly flow allowed a surge of Atlantic moisture to spread westward across the Chesapeake Bay. Scattered slowly moving showers developed as this area of enhanced moisture moved over lower southern Maryland, creating an isolated flash flood event in Anne Arundel County.\nEvent Narrative: Sunrise Beach Road between General's Highway and Old Herald Harbor Road was closed due to flooding. COOP Observer near the area reported 2.75 inches of rain around an hour.", "The following events were reported: Flood. These occurred near station USW00093721, approximately 37.2827 km away, between 2009-09-11 11:55:00 and 2009-09-11 19:30:00. The flood was caused by Heavy Rain. Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A strong coastal low pressure system slowly moved up the Delmarva Peninsula through the day, bringing a prolonged period of light to moderate rain to northeastern Maryland, with several rounds of heavy rain during a 24 hour period. This led to flooding across Harford and Baltimore Counties. Widespread rainfall of 3 to 5 inches was observed over these areas, with the highest total reported near Jacksonville, where 5.26 inches was reported. A strong coastal low pressure system slowly moved up the Delmarva Peninsula through the day, bringing a prolonged period of light to moderate rain to northeastern Maryland, with several rounds of heavy rain during a 24 hour period. This led to flooding across Harford and Baltimore Counties. Widespread rainfall of 3 to 5 inches was observed over these areas, with the highest total reported near Jacksonville, where 5.26 inches was reported.\nEvent Narrative: Flooded forced the closure of Patterson Mill Road between Woodring Drive and Wheel Road. A trained spotter measured a rainfall amount of 4.15 inches in a 24 hour period. Flooding was reported at Ruxton Road and Circle Road. Numerous rainfall reports north and east of the area were received of 4 to 5 inches.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 38.106 km away, between 2009-10-24 16:00:00 and 2009-10-24 16:00:00. The events included records with measured wind gusts of 39.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A strong cold front passed through the Tidal Potomac and Chesapeake Bay on the 24th of October. Despite limited instability, strong winds aloft were able to mix down to the surface in heavier showers. The gusty showers occurred during the afternoon and evening.\nEvent Narrative: A wind gust of 39 knots was reported at Tolchester Beach.", "The following events were reported: Heavy Rain. These occurred near station USW00093721, approximately 37.735 km away, between 2009-12-09 01:00:00 and 2009-12-09 08:00:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: An intense low pressure system that moved through the Great Lakes on the 9th produced a strong southerly flow of moist air from the Gulf of Mexico and Atlantic Ocean. Rain began falling during the evening of the 8th and ended by Noon EST on the 9th. It fell heavy at times during the early morning of the 9th. Event precipitation totals averaged two to three inches across the Eastern Shore. The concentration of the heavy rain in a relatively short period of time produced poor drainage flooding and field flooding. It also caused a couple of waterways in Caroline County to flood. An intense low pressure system that moved through the Great Lakes on the 9th produced a strong southerly flow of moist air from the Gulf of Mexico and Atlantic Ocean. Rain began falling during the evening of the 8th and ended by Noon EST on the 9th. It fell heavy at times during the early morning of the 9th. Event precipitation totals averaged two to three inches across the Eastern Shore. The concentration of the heavy rain in a relatively short period of time produced poor drainage flooding and field flooding. It also caused a couple of waterways in Caroline County to flood.\nEvent Narrative: Event precipitation totals included 1.88 inches in Stevensville.", "The following events were reported: Heavy Rain. These occurred near station USW00093721, approximately 43.4462 km away, between 2010-03-13 01:00:00 and 2010-03-13 13:00:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Four days of rain, heaviest on the 13th, culminated with poor drainage, field and some river flooding in northeast Maryland. Storm totals averaged around 3 inches. Periods of rain started during the morning of the 12th and fell at the heaviest during the first half of the day on the 13th. Periods of lighter rain persisted into the 14th and 15th. The area avoided the heaviest rain that fell with the system in New Jersey. ||The heavy rain was caused by a slow moving low pressure system that had a tremendous fetch of moist air from the Atlantic Ocean. The low pressure system moved from the South Carolina coast on the morning of the 12th, into Virginia on the morning of the 13th, to Delaware on the morning of the 14th and then drifted slowly east over the next two days as it was captured by an upper level system. Four days of rain, heaviest on the 13th, culminated with poor drainage, field and some river flooding in northeast Maryland. Storm totals averaged around 3 inches. Periods of rain started during the morning of the 12th and fell at the heaviest during the first half of the day on the 13th. Periods of lighter rain persisted into the 14th and 15th. The area avoided the heaviest rain that fell with the system in New Jersey. ||The heavy rain was caused by a slow moving low pressure system that had a tremendous fetch of moist air from the Atlantic Ocean. The low pressure system moved from the South Carolina coast on the morning of the 12th, into Virginia on the morning of the 13th, to Delaware on the morning of the 14th and then drifted slowly east over the next two days as it was captured by an upper level system.\nEvent Narrative: Event precipitation totals included 2.41 inches in Stevensville and 2.21 inches in Queenstown. In addition to the poor drainage and field flooding, minor tidal flooding occurred with the late afternoon high tide on the 13th along Chesapeake Bay. The high tide at Tolchester Beach reached 3.56 feet above mean lower low water. Minor tidal flooding starts at 3.5 feet above mean lower low water.", "The following events were reported: Flood. These occurred near station USW00093721, approximately 11.2884 km away, between 2010-03-13 11:30:00 and 2010-03-13 18:25:00. The flood was caused by Heavy Rain. Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A slow moving low pressure moved up the Mid-Atlantic coast producing widespread heavy rainfall. The 2 to 4 inches of rain combined with nearly saturated antecedent conditions to produce flooding over northern Maryland. A slow moving low pressure moved up the Mid-Atlantic coast producing widespread heavy rainfall. The 2 to 4 inches of rain combined with nearly saturated antecedent conditions to produce flooding over northern Maryland. A slow moving low pressure moved up the Mid-Atlantic coast producing widespread heavy rainfall. The 2 to 4 inches of rain combined with nearly saturated antecedent conditions to produce flooding over northern Maryland. A slow moving low pressure moved up the Mid-Atlantic coast producing widespread heavy rainfall. The 2 to 4 inches of rain combined with nearly saturated antecedent conditions to produce flooding over northern Maryland. A slow moving low pressure moved up the Mid-Atlantic coast producing widespread heavy rainfall. The 2 to 4 inches of rain combined with nearly saturated antecedent conditions to produce flooding over northern Maryland. A slow moving low pressure moved up the Mid-Atlantic coast producing widespread heavy rainfall. The 2 to 4 inches of rain combined with nearly saturated antecedent conditions to produce flooding over northern Maryland. A slow moving low pressure moved up the Mid-Atlantic coast producing widespread heavy rainfall. The 2 to 4 inches of rain combined with nearly saturated antecedent conditions to produce flooding over northern Maryland.\nEvent Narrative: Flooding was reported on Race Road between Furnace Avenue and Hanover Road. A rainfall report of 3.28 inches was received from the area. Flooding was reported on Levering Avenue from Route 1 to Lawyers Avenue. A rainfall report of 3.23 inches was received from the area. Flooding was on River Road in Patapsco State Park. A rainfall report of 3.21 inches was received from the area. Flooding was observed along River Road from Frederick Road to Thistle Road. Flooding was reported on Furnace Avenue. Spotter in the area observed 4.79 inches of rain. Flooding on Golden Ring Road at the intersections of Orems Road and Race Road. Flooding was observed at the intersection of Frederick Road and Thistle Road.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 8.1378 km away, between 2010-04-08 19:18:00 and 2010-04-08 19:28:00. The events included records with estimated wind gusts of 50.666666666666664 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 2000.0 and crop damage of 0.0. \n\nEpisode Narrative: A strong area of low pressure over the Great Lakes slowly tracked to our north on the 8th. The cold front associated with the low moved into the region during the afternoon and evening hours. A moist southerly flow ahead of the front provided instability. The instability combined with the forcing from the front to trigger showers and thunderstorms during the afternoon and evening hours of the 8th. Due to strong winds aloft, some thunderstorms became severe with damaging winds. A strong area of low pressure over the Great Lakes slowly tracked to our north on the 8th. The cold front associated with the low moved into the region during the afternoon and evening hours. A moist southerly flow ahead of the front provided instability. The instability combined with the forcing from the front to trigger showers and thunderstorms during the afternoon and evening hours of the 8th. Due to strong winds aloft, some thunderstorms became severe with damaging winds. A strong area of low pressure over the Great Lakes slowly tracked to our north on the 8th. The cold front associated with the low moved into the region during the afternoon and evening hours. A moist southerly flow ahead of the front provided instability. The instability combined with the forcing from the front to trigger showers and thunderstorms during the afternoon and evening hours of the 8th. Due to strong winds aloft, some thunderstorms became severe with damaging winds.\nEvent Narrative: A wind gust was estimated around 60 mph near Glenn Burnie Park. A tree was down near Elvaton Road and Foxwell Road. A large tree was down near Route 32 and 198.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 30.8177 km away, between 2010-04-08 19:35:00 and 2010-04-08 19:55:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A strong area of low pressure over the Great Lakes slowly tracked to our north on the 8th. The cold front associated with the low moved into the region during the afternoon and evening hours. A moist southerly flow ahead of the front provided instability. The instability combined with the forcing from the front to trigger showers and thunderstorms during the afternoon and evening hours of the 8th. Due to strong winds aloft, some thunderstorms produced gusty winds over the Tidal Potomac and Chesapeake Bay. A strong area of low pressure over the Great Lakes slowly tracked to our north on the 8th. The cold front associated with the low moved into the region during the afternoon and evening hours. A moist southerly flow ahead of the front provided instability. The instability combined with the forcing from the front to trigger showers and thunderstorms during the afternoon and evening hours of the 8th. Due to strong winds aloft, some thunderstorms produced gusty winds over the Tidal Potomac and Chesapeake Bay. A strong area of low pressure over the Great Lakes slowly tracked to our north on the 8th. The cold front associated with the low moved into the region during the afternoon and evening hours. A moist southerly flow ahead of the front provided instability. The instability combined with the forcing from the front to trigger showers and thunderstorms during the afternoon and evening hours of the 8th. Due to strong winds aloft, some thunderstorms produced gusty winds over the Tidal Potomac and Chesapeake Bay. A strong area of low pressure over the Great Lakes slowly tracked to our north on the 8th. The cold front associated with the low moved into the region during the afternoon and evening hours. A moist southerly flow ahead of the front provided instability. The instability combined with the forcing from the front to trigger showers and thunderstorms during the afternoon and evening hours of the 8th. Due to strong winds aloft, some thunderstorms produced gusty winds over the Tidal Potomac and Chesapeake Bay. A strong area of low pressure over the Great Lakes slowly tracked to our north on the 8th. The cold front associated with the low moved into the region during the afternoon and evening hours. A moist southerly flow ahead of the front provided instability. The instability combined with the forcing from the front to trigger showers and thunderstorms during the afternoon and evening hours of the 8th. Due to strong winds aloft, some thunderstorms produced gusty winds over the Tidal Potomac and Chesapeake Bay. A strong area of low pressure over the Great Lakes slowly tracked to our north on the 8th. The cold front associated with the low moved into the region during the afternoon and evening hours. A moist southerly flow ahead of the front provided instability. The instability combined with the forcing from the front to trigger showers and thunderstorms during the afternoon and evening hours of the 8th. Due to strong winds aloft, some thunderstorms produced gusty winds over the Tidal Potomac and Chesapeake Bay. A strong area of low pressure over the Great Lakes slowly tracked to our north on the 8th. The cold front associated with the low moved into the region during the afternoon and evening hours. A moist southerly flow ahead of the front provided instability. The instability combined with the forcing from the front to trigger showers and thunderstorms during the afternoon and evening hours of the 8th. Due to strong winds aloft, some thunderstorms produced gusty winds over the Tidal Potomac and Chesapeake Bay.\nEvent Narrative: Wind gusts between 34 and 45 knots were measured at Miller Island. A wind gust in excess of 30 knots was measured at Sandy Point. A wind gust of 35 knots was reported at Kent Island. A wind gust of 43 knots was reported at Tolly Point. A wind gust of 37 knots was reported at Greenbury Point. A wind gust of 37 knots was reported at Patapsco Buoy. A wind gust of 35 knots was reported at Annapolis.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 43.2199 km away, between 2010-04-16 15:47:00 and 2010-04-16 15:47:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 1000.0 and crop damage of 0.0. \n\nEpisode Narrative: A cold front passed through Maryland on the 16th. There was just enough instability ahead of the front for a couple severe thunderstorms that produced strong winds.\nEvent Narrative: A large tree was down in Lisbon near Shaffersville Road and Long Corner.", "The following events were reported: Hail. These occurred near station USW00093721, approximately 32.1651 km away, between 2010-04-25 18:43:00 and 2010-04-25 19:40:00. The events included records with hailstones measuring 1.0833333333333333 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A strong upper-level low slowly tracked through the central portion of the country on the 25th. A southwest flow ahead of this system ushered in warm and humid air. A cold front dropped into the region from the northeast during the afternoon and evening hours of the 25th. The cold front combined with plenty of instability for showers and thunderstorms to develop. Due to plenty of cold air aloft, thunderstorms produced large hail. A strong upper-level low slowly tracked through the central portion of the country on the 25th. A southwest flow ahead of this system ushered in warm and humid air. A cold front dropped into the region from the northeast during the afternoon and evening hours of the 25th. The cold front combined with plenty of instability for showers and thunderstorms to develop. Due to plenty of cold air aloft, thunderstorms produced large hail. A strong upper-level low slowly tracked through the central portion of the country on the 25th. A southwest flow ahead of this system ushered in warm and humid air. A cold front dropped into the region from the northeast during the afternoon and evening hours of the 25th. The cold front combined with plenty of instability for showers and thunderstorms to develop. Due to plenty of cold air aloft, thunderstorms produced large hail.\nEvent Narrative: Half dollar size hail was reported in Eldersburg. Quarter size hail was reported near Glenelg. Quarter size hail was reported near Chase.", "The following events were reported: Marine Hail. These occurred near station USW00093721, approximately 35.022 km away, between 2010-04-25 19:40:00 and 2010-04-25 19:40:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A strong upper-level low slowly tracked through the central portion of the country on the 25th. A southwest flow ahead of this system ushered in warm and humid air. A cold front dropped into the region from the northeast during the afternoon and evening hours of the 25th. The cold front combined with plenty of instability for showers and thunderstorms to develop. An isolated thunderstorm did produce large hail over the Chesapeake Bay.\nEvent Narrative: Quarter size hail was reported near Chase.", "The following events were reported: Hail. These occurred near station USW00093721, approximately 18.225 km away, between 2010-05-14 17:59:00 and 2010-05-14 18:35:00. The events included records with hailstones measuring 1.0625 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: High pressure over the western Atlantic pumped in plenty of warm and humid air on the 14th. An upper-level disturbance passed through the region during the afternoon and evening hours, bringing showers and thunderstorms. Moderate to high amounts of instability was present due to relatively colder air aloft and warm, moist air at the surface. This caused thunderstorms to become severe with large hail being the primary threat. High pressure over the western Atlantic pumped in plenty of warm and humid air on the 14th. An upper-level disturbance passed through the region during the afternoon and evening hours, bringing showers and thunderstorms. Moderate to high amounts of instability was present due to relatively colder air aloft and warm, moist air at the surface. This caused thunderstorms to become severe with large hail being the primary threat. High pressure over the western Atlantic pumped in plenty of warm and humid air on the 14th. An upper-level disturbance passed through the region during the afternoon and evening hours, bringing showers and thunderstorms. Moderate to high amounts of instability was present due to relatively colder air aloft and warm, moist air at the surface. This caused thunderstorms to become severe with large hail being the primary threat. High pressure over the western Atlantic pumped in plenty of warm and humid air on the 14th. An upper-level disturbance passed through the region during the afternoon and evening hours, bringing showers and thunderstorms. Moderate to high amounts of instability was present due to relatively colder air aloft and warm, moist air at the surface. This caused thunderstorms to become severe with large hail being the primary threat.\nEvent Narrative: Hail was estimated to be the size of half dollars in Odenton. Quarter size hail was reported near the intersection of Interstates 695 and 95. Quarter size hail was reported near Towson. Hail up to the size of quarters was reported about one mile northeast of Towson.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 14.2666 km away, between 2010-05-14 18:39:00 and 2010-05-14 18:39:00. The events included records with measured wind gusts of 42.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: High pressure over the western Atlantic provided warm and humid air over the Chesapeake Bay on the 14th. An upper-level disturbance passed through triggering showers and thunderstorms. There was just enough instability for an isolated thunderstorm to produce gusty winds.\nEvent Narrative: A wind gust of 42 knots was reported at Key Bridge.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 7.5544 km away, between 2010-06-03 16:37:00 and 2010-06-03 16:37:00. The events included records with estimated wind gusts of 52.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 2000.0 and crop damage of 0.0. \n\nEpisode Narrative: A cold front stalled out over the region on the 3rd. Warm and humid air ahead of the front combined with the forcing from the front to trigger showers and thunderstorms. There was enough instability along with stronger winds aloft for some thunderstorms to produce damaging wind and large hail across lower southern Maryland.\nEvent Narrative: A tree was down along Sellner Road.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 32.5869 km away, between 2010-06-03 17:05:00 and 2010-06-03 17:24:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front stalled out over the waters on the 3rd. Warm and humid air ahead of the front combined with the forcing from the front to trigger showers and thunderstorms. There was enough instability along with stronger winds aloft for some thunderstorms to produce damaging wind gusts across the Tidal Potomac River as well as the Chesapeake Bay. A cold front stalled out over the waters on the 3rd. Warm and humid air ahead of the front combined with the forcing from the front to trigger showers and thunderstorms. There was enough instability along with stronger winds aloft for some thunderstorms to produce damaging wind gusts across the Tidal Potomac River as well as the Chesapeake Bay. A cold front stalled out over the waters on the 3rd. Warm and humid air ahead of the front combined with the forcing from the front to trigger showers and thunderstorms. There was enough instability along with stronger winds aloft for some thunderstorms to produce damaging wind gusts across the Tidal Potomac River as well as the Chesapeake Bay. A cold front stalled out over the waters on the 3rd. Warm and humid air ahead of the front combined with the forcing from the front to trigger showers and thunderstorms. There was enough instability along with stronger winds aloft for some thunderstorms to produce damaging wind gusts across the Tidal Potomac River as well as the Chesapeake Bay.\nEvent Narrative: A wind gust in excess of 30 knots was reported at the Patapsco River. A wind gust of 40 knots was measured at Annapolis. A wind gust of 42 knots was measured at Stevensville. Wind gusts up to 41 knots were reported at Kent Island.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 38.0834 km away, between 2010-06-03 17:15:00 and 2010-06-03 17:15:00. The events included records with estimated wind gusts of 52.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A bow echo that contained strong to severe thunderstorms moved across the Maryland Eastern Shore during the early evening of the 3rd.\nEvent Narrative: A severe thunderstorm tore down a few trees in Stevensville.", "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00093721, approximately 45.0843 km away, between 2010-06-04 16:28:00 and 2010-06-04 16:42:00. The events included records with hailstones measuring 36.75 inches.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 11500.0 and crop damage of 0.0. \n\nEpisode Narrative: An upper-level disturbance passed through the region while a pressure trough at the surface remained nearly stationary. These systems provided the forcing to combine with a warm and humid air mass to bring showers and thunderstorms to the area. There was enough instability along with stronger winds aloft for some thunderstorms to produce large hail and damaging winds. An upper-level disturbance passed through the region while a pressure trough at the surface remained nearly stationary. These systems provided the forcing to combine with a warm and humid air mass to bring showers and thunderstorms to the area. There was enough instability along with stronger winds aloft for some thunderstorms to produce large hail and damaging winds. An upper-level disturbance passed through the region while a pressure trough at the surface remained nearly stationary. These systems provided the forcing to combine with a warm and humid air mass to bring showers and thunderstorms to the area. There was enough instability along with stronger winds aloft for some thunderstorms to produce large hail and damaging winds. An upper-level disturbance passed through the region while a pressure trough at the surface remained nearly stationary. These systems provided the forcing to combine with a warm and humid air mass to bring showers and thunderstorms to the area. There was enough instability along with stronger winds aloft for some thunderstorms to produce large hail and damaging winds. An upper-level disturbance passed through the region while a pressure trough at the surface remained nearly stationary. These systems provided the forcing to combine with a warm and humid air mass to bring showers and thunderstorms to the area. There was enough instability along with stronger winds aloft for some thunderstorms to produce large hail and damaging winds. An upper-level disturbance passed through the region while a pressure trough at the surface remained nearly stationary. These systems provided the forcing to combine with a warm and humid air mass to bring showers and thunderstorms to the area. There was enough instability along with stronger winds aloft for some thunderstorms to produce large hail and damaging winds. An upper-level disturbance passed through the region while a pressure trough at the surface remained nearly stationary. These systems provided the forcing to combine with a warm and humid air mass to bring showers and thunderstorms to the area. There was enough instability along with stronger winds aloft for some thunderstorms to produce large hail and damaging winds. An upper-level disturbance passed through the region while a pressure trough at the surface remained nearly stationary. These systems provided the forcing to combine with a warm and humid air mass to bring showers and thunderstorms to the area. There was enough instability along with stronger winds aloft for some thunderstorms to produce large hail and damaging winds. An upper-level disturbance passed through the region while a pressure trough at the surface remained nearly stationary. These systems provided the forcing to combine with a warm and humid air mass to bring showers and thunderstorms to the area. There was enough instability along with stronger winds aloft for some thunderstorms to produce large hail and damaging winds.\nEvent Narrative: Hail to the size of half dollars was reported near Fallston. Trees were down along Pleasantville Road. Wind gusts were estimated to be around 60 mph. Trees were down at the Fallston Swim Club. Trees and lines were down along Oakmont Road. A tree was uprooted onto Route 152 between Route 165 and Pleasantville Road. Hail to the size of ping pong balls was reported about three miles southwest of Jarrettsville. Hail to the size of quarters was reported near Fallston. Branches were broken off a maple tree.", "The following events were reported: Marine Hail, Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 37.0417 km away, between 2010-06-22 18:16:00 and 2010-06-22 18:16:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: The subtropical ridge was to our south while the subtropical jet remained just to our north. An upper-level disturbance in the jet stream passed through on the 22nd. Warm and humid air was in place due to a west-southwest flow around the ridge. Moderate amounts of instability along with the upper-level disturbance caused showers and thunderstorms to develop. Some thunderstorms produced gusty winds over the waters. The subtropical ridge was to our south while the subtropical jet remained just to our north. An upper-level disturbance in the jet stream passed through on the 22nd. Warm and humid air was in place due to a west-southwest flow around the ridge. Moderate amounts of instability along with the upper-level disturbance caused showers and thunderstorms to develop. Some thunderstorms produced gusty winds over the waters.\nEvent Narrative: A wind gust of 60 mph was estimated due to thunderstorm wind damage about five miles northeast of the Martin State Airport. Penny size hail was reported about five miles northeast of the Martin State Airport.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 22.9091 km away, between 2010-06-22 18:16:00 and 2010-06-22 19:57:00. The events included records with estimated wind gusts of 55.36363636363637 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 29000.0 and crop damage of 0.0. \n\nEpisode Narrative: The subtropical ridge was to our south while the subtropical jet remained just to our north. An upper-level disturbance in the jet stream passed through on the 22nd. Warm and humid air was in place due to a west-southwest flow around the ridge. Moderate amounts of instability along with the upper-level disturbance caused showers and thunderstorms to develop. Some thunderstorms became severe with damaging winds and large hail. The subtropical ridge was to our south while the subtropical jet remained just to our north. An upper-level disturbance in the jet stream passed through on the 22nd. Warm and humid air was in place due to a west-southwest flow around the ridge. Moderate amounts of instability along with the upper-level disturbance caused showers and thunderstorms to develop. Some thunderstorms became severe with damaging winds and large hail. The subtropical ridge was to our south while the subtropical jet remained just to our north. An upper-level disturbance in the jet stream passed through on the 22nd. Warm and humid air was in place due to a west-southwest flow around the ridge. Moderate amounts of instability along with the upper-level disturbance caused showers and thunderstorms to develop. Some thunderstorms became severe with damaging winds and large hail. The subtropical ridge was to our south while the subtropical jet remained just to our north. An upper-level disturbance in the jet stream passed through on the 22nd. Warm and humid air was in place due to a west-southwest flow around the ridge. Moderate amounts of instability along with the upper-level disturbance caused showers and thunderstorms to develop. Some thunderstorms became severe with damaging winds and large hail. The subtropical ridge was to our south while the subtropical jet remained just to our north. An upper-level disturbance in the jet stream passed through on the 22nd. Warm and humid air was in place due to a west-southwest flow around the ridge. Moderate amounts of instability along with the upper-level disturbance caused showers and thunderstorms to develop. Some thunderstorms became severe with damaging winds and large hail. The subtropical ridge was to our south while the subtropical jet remained just to our north. An upper-level disturbance in the jet stream passed through on the 22nd. Warm and humid air was in place due to a west-southwest flow around the ridge. Moderate amounts of instability along with the upper-level disturbance caused showers and thunderstorms to develop. Some thunderstorms became severe with damaging winds and large hail. The subtropical ridge was to our south while the subtropical jet remained just to our north. An upper-level disturbance in the jet stream passed through on the 22nd. Warm and humid air was in place due to a west-southwest flow around the ridge. Moderate amounts of instability along with the upper-level disturbance caused showers and thunderstorms to develop. Some thunderstorms became severe with damaging winds and large hail. The subtropical ridge was to our south while the subtropical jet remained just to our north. An upper-level disturbance in the jet stream passed through on the 22nd. Warm and humid air was in place due to a west-southwest flow around the ridge. Moderate amounts of instability along with the upper-level disturbance caused showers and thunderstorms to develop. Some thunderstorms became severe with damaging winds and large hail. The subtropical ridge was to our south while the subtropical jet remained just to our north. An upper-level disturbance in the jet stream passed through on the 22nd. Warm and humid air was in place due to a west-southwest flow around the ridge. Moderate amounts of instability along with the upper-level disturbance caused showers and thunderstorms to develop. Some thunderstorms became severe with damaging winds and large hail. The subtropical ridge was to our south while the subtropical jet remained just to our north. An upper-level disturbance in the jet stream passed through on the 22nd. Warm and humid air was in place due to a west-southwest flow around the ridge. Moderate amounts of instability along with the upper-level disturbance caused showers and thunderstorms to develop. Some thunderstorms became severe with damaging winds and large hail. The subtropical ridge was to our south while the subtropical jet remained just to our north. An upper-level disturbance in the jet stream passed through on the 22nd. Warm and humid air was in place due to a west-southwest flow around the ridge. Moderate amounts of instability along with the upper-level disturbance caused showers and thunderstorms to develop. Some thunderstorms became severe with damaging winds and large hail.\nEvent Narrative: Large trees were down about one mile west of Mayo. A thunderstorm wind gust was estimated to be around 60 mph. Trees and power lines were down in the Laurel area. Large trees were down due to thunderstorm winds. A wind gust from a thunderstorm was estimated to be around 60 mph near Brinklow. Numerous trees were down in the Severn and Jessup areas. Full grown pine oak trees were snapped in half. Three trees fifteen inches in diameter were blown down in thunderstorm winds. Trees were down near Edgewater. Several large trees were down between Laytonsville and Olney. A spotter estimated straight line wind gusts around 65 mph.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 38.1778 km away, between 2010-06-22 20:25:00 and 2010-06-22 20:28:00. The events included records with estimated wind gusts of 52.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: An approaching and passing warm front triggered strong to severe thunderstorms during the evening of the 22nd across the Maryland Eastern Shore.\nEvent Narrative: A severe thunderstorm caused tree damage along Maryland State Route 8 (Romancoke Road) south of the William Preston Lane Junior Bridge. The most extensive damage was between Batts Neck Road and Matapeake Farm Lane.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 22.1685 km away, between 2010-06-28 13:00:00 and 2010-06-28 14:12:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front moved over the waters on the 28th. A southwest flow ahead of the front pumped in plenty of moisture from the Gulf of Mexico. Dewpoints were in the lower to middle 70s across most locations. The cold front combined with the warm and moist air to trigger showers and thunderstorms. Moderate to high amounts of instability along with stronger winds aloft caused some thunderstorms to produce gusty winds. A cold front moved over the waters on the 28th. A southwest flow ahead of the front pumped in plenty of moisture from the Gulf of Mexico. Dewpoints were in the lower to middle 70s across most locations. The cold front combined with the warm and moist air to trigger showers and thunderstorms. Moderate to high amounts of instability along with stronger winds aloft caused some thunderstorms to produce gusty winds. A cold front moved over the waters on the 28th. A southwest flow ahead of the front pumped in plenty of moisture from the Gulf of Mexico. Dewpoints were in the lower to middle 70s across most locations. The cold front combined with the warm and moist air to trigger showers and thunderstorms. Moderate to high amounts of instability along with stronger winds aloft caused some thunderstorms to produce gusty winds.\nEvent Narrative: A wind gust in excess of 30 knots was reported near Rivera Beach. A wind gust of 36 knots was reported near Baltimore. A wind gust of 36 knots was reported at Kent Island.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 39.7132 km away, between 2010-06-28 14:15:00 and 2010-06-28 14:35:00. The events included records with estimated wind gusts of 52.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: An approaching cold front helped trigger strong to locally severe thunderstorms during the afternoon of the 28th across central portions of the Eastern Shore.\nEvent Narrative: A severe thunderstorm knocked down several trees in the southwestern part of Queen Anne's County.", "The following events were reported: Flash Flood. These occurred near station USW00093721, approximately 43.1963 km away, between 2010-07-10 06:50:00 and 2010-07-10 08:00:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Low pressure moved east toward the Chesapeake Bay during the early morning, encountering a very moist low-level atmosphere. Lift was sufficient to produce thunderstorms, a series of which trained across southern Harford county for several hours, producing 2-4 inches of rain and a report of flash flooding.\nEvent Narrative: Edgewood Road at the CSX Railroad Overpass was flooded and closed. A spotter near the event reported 3.75 inches of rain in 2.5 hours.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 26.3275 km away, between 2010-07-10 11:40:00 and 2010-07-10 11:40:00. The events included records with measured wind gusts of 42.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front triggered showers and thunderstorms over Chesapeake Bay. There was enough instability for an isolated thunderstorm to produce gusty winds.\nEvent Narrative: A wind gust of 42 knots was reported at Annapolis.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 15.8629 km away, between 2010-07-12 13:45:00 and 2010-07-12 14:53:00. The events included records with estimated wind gusts of 52.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 18000.0 and crop damage of 0.0. \n\nEpisode Narrative: A pressure trough remained over Maryland on the 12th while an upper-level disturbance passed through in a zonal flow aloft. The forcing from these two systems were responsible for the development of showers and thunderstorms. Due to moderate amounts of instability, some thunderstorms became severe with damaging winds. A pressure trough remained over Maryland on the 12th while an upper-level disturbance passed through in a zonal flow aloft. The forcing from these two systems were responsible for the development of showers and thunderstorms. Due to moderate amounts of instability, some thunderstorms became severe with damaging winds. A pressure trough remained over Maryland on the 12th while an upper-level disturbance passed through in a zonal flow aloft. The forcing from these two systems were responsible for the development of showers and thunderstorms. Due to moderate amounts of instability, some thunderstorms became severe with damaging winds. A pressure trough remained over Maryland on the 12th while an upper-level disturbance passed through in a zonal flow aloft. The forcing from these two systems were responsible for the development of showers and thunderstorms. Due to moderate amounts of instability, some thunderstorms became severe with damaging winds. A pressure trough remained over Maryland on the 12th while an upper-level disturbance passed through in a zonal flow aloft. The forcing from these two systems were responsible for the development of showers and thunderstorms. Due to moderate amounts of instability, some thunderstorms became severe with damaging winds. A pressure trough remained over Maryland on the 12th while an upper-level disturbance passed through in a zonal flow aloft. The forcing from these two systems were responsible for the development of showers and thunderstorms. Due to moderate amounts of instability, some thunderstorms became severe with damaging winds. A pressure trough remained over Maryland on the 12th while an upper-level disturbance passed through in a zonal flow aloft. The forcing from these two systems were responsible for the development of showers and thunderstorms. Due to moderate amounts of instability, some thunderstorms became severe with damaging winds. A pressure trough remained over Maryland on the 12th while an upper-level disturbance passed through in a zonal flow aloft. The forcing from these two systems were responsible for the development of showers and thunderstorms. Due to moderate amounts of instability, some thunderstorms became severe with damaging winds. A pressure trough remained over Maryland on the 12th while an upper-level disturbance passed through in a zonal flow aloft. The forcing from these two systems were responsible for the development of showers and thunderstorms. Due to moderate amounts of instability, some thunderstorms became severe with damaging winds. A pressure trough remained over Maryland on the 12th while an upper-level disturbance passed through in a zonal flow aloft. The forcing from these two systems were responsible for the development of showers and thunderstorms. Due to moderate amounts of instability, some thunderstorms became severe with damaging winds. A pressure trough remained over Maryland on the 12th while an upper-level disturbance passed through in a zonal flow aloft. The forcing from these two systems were responsible for the development of showers and thunderstorms. Due to moderate amounts of instability, some thunderstorms became severe with damaging winds. A pressure trough remained over Maryland on the 12th while an upper-level disturbance passed through in a zonal flow aloft. The forcing from these two systems were responsible for the development of showers and thunderstorms. Due to moderate amounts of instability, some thunderstorms became severe with damaging winds.\nEvent Narrative: Several trees were down along Highbridge Road at the intersection with Route 450. A tree was down on Standard Drive near Parkway Drive. A tree was down near the intersection of Light Street Avenue and West Earleigh Heights Road. Three to four trees were down on Stone Haven Drive. Some trees were eighteen inches in diameter. A tree was down over the 2400 Block of Chelsea Terrace. A tree fell onto Alto Road. A tree was knocked down onto the highway near Gwynnoak. A tree was down on the 2100 Block of Carterdale Road. A tree was down on the 1200 Block of West Cold Spring Lane. A tree was down on the 3800 Block of Crescent Street. A tree was over the roadway on West 30th Street. A tree was down at the Milford Academy.", "The following events were reported: Flood. These occurred near station USW00093721, approximately 13.9796 km away, between 2010-07-12 14:25:00 and 2010-07-12 21:45:00. The flood was caused by Heavy Rain. Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A pressure trough remained over Maryland on the 12th while an upper-level disturbance passed through in a zonal flow aloft. The forcing from these two systems were responsible for the development of showers and thunderstorms. As thunderstorms passed across the Baltimore metropolitan area during the afternoon locally heavy rainfall of 1 to 2 inches produced minor street flooding. A pressure trough remained over Maryland on the 12th while an upper-level disturbance passed through in a zonal flow aloft. The forcing from these two systems were responsible for the development of showers and thunderstorms. As thunderstorms passed across the Baltimore metropolitan area during the afternoon locally heavy rainfall of 1 to 2 inches produced minor street flooding. A pressure trough remained over Maryland on the 12th while an upper-level disturbance passed through in a zonal flow aloft. The forcing from these two systems were responsible for the development of showers and thunderstorms. As thunderstorms passed across the Baltimore metropolitan area during the afternoon locally heavy rainfall of 1 to 2 inches produced minor street flooding. A pressure trough remained over Maryland on the 12th while an upper-level disturbance passed through in a zonal flow aloft. The forcing from these two systems were responsible for the development of showers and thunderstorms. As thunderstorms passed across the Baltimore metropolitan area during the afternoon locally heavy rainfall of 1 to 2 inches produced minor street flooding. A pressure trough remained over Maryland on the 12th while an upper-level disturbance passed through in a zonal flow aloft. The forcing from these two systems were responsible for the development of showers and thunderstorms. As thunderstorms passed across the Baltimore metropolitan area during the afternoon locally heavy rainfall of 1 to 2 inches produced minor street flooding.\nEvent Narrative: Flooding was reported along parts of Gwynns Falls Parkway. Flooding was reported along parts of Fulton Avenue. Flooding was reported along portions of Uplands Parkway. Flooding was reported along parts of Frederick Avenue. Flooding was reported along parts of Hickory Avenue. A spotter in the area observed 2.25 inches of rain.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 25.8526 km away, between 2010-07-12 14:54:00 and 2010-07-12 15:24:00. The events included records with estimated wind gusts of 34.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A pressure trough remained over the Tidal Potomac River and Chesapeake Bay while an upper-level disturbance passed through in a zonal flow aloft. The forcing from these two systems were responsible for the development of showers and thunderstorms. Due to moderate amounts of instability, some thunderstorms produced gusty winds. A pressure trough remained over the Tidal Potomac River and Chesapeake Bay while an upper-level disturbance passed through in a zonal flow aloft. The forcing from these two systems were responsible for the development of showers and thunderstorms. Due to moderate amounts of instability, some thunderstorms produced gusty winds. A pressure trough remained over the Tidal Potomac River and Chesapeake Bay while an upper-level disturbance passed through in a zonal flow aloft. The forcing from these two systems were responsible for the development of showers and thunderstorms. Due to moderate amounts of instability, some thunderstorms produced gusty winds.\nEvent Narrative: A wind gust in excess of 30 knots was recorded at the Francis Scott Key Bridge. A wind gust in excess of 30 knots was reported at the Patapsco Buoy. A wind gust in excess of 30 knots was reported at Tolchester Beach.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 30.0239 km away, between 2010-07-13 19:59:00 and 2010-07-13 19:59:00. The events included records with estimated wind gusts of 34.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A return flow around high pressure over the western Atlantic was responsible for hot and humid conditions. An upper-level disturbance combined with the hot and humid conditions to trigger showers and thunderstorms over the Tidal Potomac River and Chesapeake Bay. An isolated thunderstorm produced gusty winds.\nEvent Narrative: Wind gusts in excess of 30 knots were reported at Greenbury Point.", "The following events were reported: Flash Flood. These occurred near station USW00093721, approximately 13.1488 km away, between 2010-07-14 00:15:00 and 2010-07-14 01:15:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A surface trough combined with an upper-level disturbance to trigger showers and thunderstorms over the area overnight on the 13th into the morning of the 14th. With ground already saturatured from numerous rounds of rainfall over the past few days, heavy downpours from thunderstorms created flash flooding in the Baltimore metropolitan area.\nEvent Narrative: Vehicle stranded in flowing water on North Rolling Road near the Baltimore National Pike. Trained spotter in the area measured storm total precipitation of 5.27 inches.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 32.0146 km away, between 2010-07-17 00:04:00 and 2010-07-17 00:14:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: High pressure over the western Atlantic continued to usher in hot and humid air due to a southwest flow. An upper-level disturbance in the zonal flow triggered showers and thunderstorms across portions of the Tidal Potomac River and Chesapeake Bay. Moderate amounts of instability due to the hot and humid air mass caused some thunderstorms to produce gusty winds. High pressure over the western Atlantic continued to usher in hot and humid air due to a southwest flow. An upper-level disturbance in the zonal flow triggered showers and thunderstorms across portions of the Tidal Potomac River and Chesapeake Bay. Moderate amounts of instability due to the hot and humid air mass caused some thunderstorms to produce gusty winds.\nEvent Narrative: Wind gusts up to 40 knots were reported at Greenbury Point. A wind gust in excess of 30 knots was reported at Tolly Point.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 16.1906 km away, between 2010-07-18 22:30:00 and 2010-07-18 23:25:00.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 8000.0 and crop damage of 0.0. \n\nEpisode Narrative: High pressure over the western Atlantic continued to usher in hot and humid air with a southwest flow. An upper-level disturbance in the zonal flow triggered showers and thunderstorms across portions of Maryland. Moderate amounts of instability due to the hot and humid air mass caused some thunderstorms to produce damaging winds. High pressure over the western Atlantic continued to usher in hot and humid air with a southwest flow. An upper-level disturbance in the zonal flow triggered showers and thunderstorms across portions of Maryland. Moderate amounts of instability due to the hot and humid air mass caused some thunderstorms to produce damaging winds. High pressure over the western Atlantic continued to usher in hot and humid air with a southwest flow. An upper-level disturbance in the zonal flow triggered showers and thunderstorms across portions of Maryland. Moderate amounts of instability due to the hot and humid air mass caused some thunderstorms to produce damaging winds. High pressure over the western Atlantic continued to usher in hot and humid air with a southwest flow. An upper-level disturbance in the zonal flow triggered showers and thunderstorms across portions of Maryland. Moderate amounts of instability due to the hot and humid air mass caused some thunderstorms to produce damaging winds. High pressure over the western Atlantic continued to usher in hot and humid air with a southwest flow. An upper-level disturbance in the zonal flow triggered showers and thunderstorms across portions of Maryland. Moderate amounts of instability due to the hot and humid air mass caused some thunderstorms to produce damaging winds. High pressure over the western Atlantic continued to usher in hot and humid air with a southwest flow. An upper-level disturbance in the zonal flow triggered showers and thunderstorms across portions of Maryland. Moderate amounts of instability due to the hot and humid air mass caused some thunderstorms to produce damaging winds. High pressure over the western Atlantic continued to usher in hot and humid air with a southwest flow. An upper-level disturbance in the zonal flow triggered showers and thunderstorms across portions of Maryland. Moderate amounts of instability due to the hot and humid air mass caused some thunderstorms to produce damaging winds. High pressure over the western Atlantic continued to usher in hot and humid air with a southwest flow. An upper-level disturbance in the zonal flow triggered showers and thunderstorms across portions of Maryland. Moderate amounts of instability due to the hot and humid air mass caused some thunderstorms to produce damaging winds. High pressure over the western Atlantic continued to usher in hot and humid air with a southwest flow. An upper-level disturbance in the zonal flow triggered showers and thunderstorms across portions of Maryland. Moderate amounts of instability due to the hot and humid air mass caused some thunderstorms to produce damaging winds.\nEvent Narrative: Trees were down around Ellicott City. A wind gust of 62 mph was measured at the Baltimore-Washington International Airport. A wind gust of 72 mph was measured at the Baltimore-Washington International Airport. A wind gust of 58 mph was measured at Glen Burnie. A tree that was two feet in diameter was snapped. Large limbs were down from Bowleys Quarters to Middle River. A tree was down along West Central Avenue. A tree was down at College Parkway and Shore Acres Road. A wind gust was estimated around 60 mph at White Marsh.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 31.6785 km away, between 2010-07-18 22:54:00 and 2010-07-18 23:24:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: High pressure over the western Atlantic continued to usher in hot and humid air due to a southwest flow. An upper-level disturbance in the zonal flow triggered showers and thunderstorms across portions of the Tidal Potomac River and Chesapeake Bay. Moderate amounts of instability due to the hot and humid air mass caused some thunderstorms to produce gusty winds. High pressure over the western Atlantic continued to usher in hot and humid air due to a southwest flow. An upper-level disturbance in the zonal flow triggered showers and thunderstorms across portions of the Tidal Potomac River and Chesapeake Bay. Moderate amounts of instability due to the hot and humid air mass caused some thunderstorms to produce gusty winds. High pressure over the western Atlantic continued to usher in hot and humid air due to a southwest flow. An upper-level disturbance in the zonal flow triggered showers and thunderstorms across portions of the Tidal Potomac River and Chesapeake Bay. Moderate amounts of instability due to the hot and humid air mass caused some thunderstorms to produce gusty winds. High pressure over the western Atlantic continued to usher in hot and humid air due to a southwest flow. An upper-level disturbance in the zonal flow triggered showers and thunderstorms across portions of the Tidal Potomac River and Chesapeake Bay. Moderate amounts of instability due to the hot and humid air mass caused some thunderstorms to produce gusty winds. High pressure over the western Atlantic continued to usher in hot and humid air due to a southwest flow. An upper-level disturbance in the zonal flow triggered showers and thunderstorms across portions of the Tidal Potomac River and Chesapeake Bay. Moderate amounts of instability due to the hot and humid air mass caused some thunderstorms to produce gusty winds. High pressure over the western Atlantic continued to usher in hot and humid air due to a southwest flow. An upper-level disturbance in the zonal flow triggered showers and thunderstorms across portions of the Tidal Potomac River and Chesapeake Bay. Moderate amounts of instability due to the hot and humid air mass caused some thunderstorms to produce gusty winds. High pressure over the western Atlantic continued to usher in hot and humid air due to a southwest flow. An upper-level disturbance in the zonal flow triggered showers and thunderstorms across portions of the Tidal Potomac River and Chesapeake Bay. Moderate amounts of instability due to the hot and humid air mass caused some thunderstorms to produce gusty winds. High pressure over the western Atlantic continued to usher in hot and humid air due to a southwest flow. An upper-level disturbance in the zonal flow triggered showers and thunderstorms across portions of the Tidal Potomac River and Chesapeake Bay. Moderate amounts of instability due to the hot and humid air mass caused some thunderstorms to produce gusty winds. High pressure over the western Atlantic continued to usher in hot and humid air due to a southwest flow. An upper-level disturbance in the zonal flow triggered showers and thunderstorms across portions of the Tidal Potomac River and Chesapeake Bay. Moderate amounts of instability due to the hot and humid air mass caused some thunderstorms to produce gusty winds.\nEvent Narrative: Wind gusts in excess of 30 knots were reported near Baltimore. Wind gusts between 36 and 64 knots were reported at Greenbury Point. A wind gust of 43 knots was reported at Annapolis Buoy. A wind gust of 36 knots was reported at Tolly Point. A wind gust of 43 knots was reported at Kent Island. A wind gust of 34 knots was reported at Kent Island. A wind gust of 44 knots was reported at Tolchester Beach. A wind gust of 34 knots was reported at Thomas Point Lighthouse. A wind gust of 37 knots was reported at Patapsco Buoy.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 41.3842 km away, between 2010-07-18 23:10:00 and 2010-07-18 23:20:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Strong to severe thunderstorms formed to the lee of the Blue Ridge Mountains during the late evening of the 18th and passed across the central Eastern Shore around Midnight EDT before weakening. Strong to severe thunderstorms formed to the lee of the Blue Ridge Mountains during the late evening of the 18th and passed across the central Eastern Shore around Midnight EDT before weakening.\nEvent Narrative: A severe thunderstorm knocked down large tree limbs near Chester. A severe thunderstorm knocked down large tree limbs, poles and wires in the Great Oak area of Kent County.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 27.6247 km away, between 2010-07-25 14:00:00 and 2010-07-25 15:17:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A strong upper-level disturbance and its associated cold front moved over the waters on the 25th. Hot and humid conditions ahead of the front led to high amounts of instability. Showers and thunderstorms developed along and ahead of the cold front. Due to the high amounts of instability, some thunderstorms were able to mix down strong winds from aloft. A strong upper-level disturbance and its associated cold front moved over the waters on the 25th. Hot and humid conditions ahead of the front led to high amounts of instability. Showers and thunderstorms developed along and ahead of the cold front. Due to the high amounts of instability, some thunderstorms were able to mix down strong winds from aloft. A strong upper-level disturbance and its associated cold front moved over the waters on the 25th. Hot and humid conditions ahead of the front led to high amounts of instability. Showers and thunderstorms developed along and ahead of the cold front. Due to the high amounts of instability, some thunderstorms were able to mix down strong winds from aloft. A strong upper-level disturbance and its associated cold front moved over the waters on the 25th. Hot and humid conditions ahead of the front led to high amounts of instability. Showers and thunderstorms developed along and ahead of the cold front. Due to the high amounts of instability, some thunderstorms were able to mix down strong winds from aloft. A strong upper-level disturbance and its associated cold front moved over the waters on the 25th. Hot and humid conditions ahead of the front led to high amounts of instability. Showers and thunderstorms developed along and ahead of the cold front. Due to the high amounts of instability, some thunderstorms were able to mix down strong winds from aloft. A strong upper-level disturbance and its associated cold front moved over the waters on the 25th. Hot and humid conditions ahead of the front led to high amounts of instability. Showers and thunderstorms developed along and ahead of the cold front. Due to the high amounts of instability, some thunderstorms were able to mix down strong winds from aloft. A strong upper-level disturbance and its associated cold front moved over the waters on the 25th. Hot and humid conditions ahead of the front led to high amounts of instability. Showers and thunderstorms developed along and ahead of the cold front. Due to the high amounts of instability, some thunderstorms were able to mix down strong winds from aloft. A strong upper-level disturbance and its associated cold front moved over the waters on the 25th. Hot and humid conditions ahead of the front led to high amounts of instability. Showers and thunderstorms developed along and ahead of the cold front. Due to the high amounts of instability, some thunderstorms were able to mix down strong winds from aloft.\nEvent Narrative: A wind gust of 54 knots was measured at Annapolis. A wind gust in excess of 30 knots was reported near Fells Point. A wind gust of 54 knots was measured at Annapolis. A wind gust in excess of 30 knots was reported at Tolchester Beach. A wind gust of 50 knots was measured at Tolly Point. A wind gust in excess of 30 knots was reported at Kent Island. A wind gust in excess of 30 knots was reported near Fells Point. A wind gust of 54 knots was measured at Eastport.", "The following events were reported: Lightning, Thunderstorm Wind. These occurred near station USW00093721, approximately 24.9145 km away, between 2010-07-25 14:07:00 and 2010-07-25 15:04:00.The events resulted in 0 injuries and 1 fatalities. The events caused property damage valued at 43000.0 and crop damage of 0.0. \n\nEpisode Narrative: A strong upper-level disturbance and its associated cold front moved into Maryland on the 25th. Hot and humid conditions ahead of the front led to high amounts of instability. Showers and thunderstorms developed along and ahead of the cold front. Due to the high amounts of instability, thunderstorms were able to mix down strong winds from aloft causing significant amounts of damage across portions of Maryland. A strong upper-level disturbance and its associated cold front moved into Maryland on the 25th. Hot and humid conditions ahead of the front led to high amounts of instability. Showers and thunderstorms developed along and ahead of the cold front. Due to the high amounts of instability, thunderstorms were able to mix down strong winds from aloft causing significant amounts of damage across portions of Maryland. A strong upper-level disturbance and its associated cold front moved into Maryland on the 25th. Hot and humid conditions ahead of the front led to high amounts of instability. Showers and thunderstorms developed along and ahead of the cold front. Due to the high amounts of instability, thunderstorms were able to mix down strong winds from aloft causing significant amounts of damage across portions of Maryland. A strong upper-level disturbance and its associated cold front moved into Maryland on the 25th. Hot and humid conditions ahead of the front led to high amounts of instability. Showers and thunderstorms developed along and ahead of the cold front. Due to the high amounts of instability, thunderstorms were able to mix down strong winds from aloft causing significant amounts of damage across portions of Maryland. A strong upper-level disturbance and its associated cold front moved into Maryland on the 25th. Hot and humid conditions ahead of the front led to high amounts of instability. Showers and thunderstorms developed along and ahead of the cold front. Due to the high amounts of instability, thunderstorms were able to mix down strong winds from aloft causing significant amounts of damage across portions of Maryland. A strong upper-level disturbance and its associated cold front moved into Maryland on the 25th. Hot and humid conditions ahead of the front led to high amounts of instability. Showers and thunderstorms developed along and ahead of the cold front. Due to the high amounts of instability, thunderstorms were able to mix down strong winds from aloft causing significant amounts of damage across portions of Maryland. A strong upper-level disturbance and its associated cold front moved into Maryland on the 25th. Hot and humid conditions ahead of the front led to high amounts of instability. Showers and thunderstorms developed along and ahead of the cold front. Due to the high amounts of instability, thunderstorms were able to mix down strong winds from aloft causing significant amounts of damage across portions of Maryland. A strong upper-level disturbance and its associated cold front moved into Maryland on the 25th. Hot and humid conditions ahead of the front led to high amounts of instability. Showers and thunderstorms developed along and ahead of the cold front. Due to the high amounts of instability, thunderstorms were able to mix down strong winds from aloft causing significant amounts of damage across portions of Maryland. A strong upper-level disturbance and its associated cold front moved into Maryland on the 25th. Hot and humid conditions ahead of the front led to high amounts of instability. Showers and thunderstorms developed along and ahead of the cold front. Due to the high amounts of instability, thunderstorms were able to mix down strong winds from aloft causing significant amounts of damage across portions of Maryland. A strong upper-level disturbance and its associated cold front moved into Maryland on the 25th. Hot and humid conditions ahead of the front led to high amounts of instability. Showers and thunderstorms developed along and ahead of the cold front. Due to the high amounts of instability, thunderstorms were able to mix down strong winds from aloft causing significant amounts of damage across portions of Maryland. A strong upper-level disturbance and its associated cold front moved into Maryland on the 25th. Hot and humid conditions ahead of the front led to high amounts of instability. Showers and thunderstorms developed along and ahead of the cold front. Due to the high amounts of instability, thunderstorms were able to mix down strong winds from aloft causing significant amounts of damage across portions of Maryland. A strong upper-level disturbance and its associated cold front moved into Maryland on the 25th. Hot and humid conditions ahead of the front led to high amounts of instability. Showers and thunderstorms developed along and ahead of the cold front. Due to the high amounts of instability, thunderstorms were able to mix down strong winds from aloft causing significant amounts of damage across portions of Maryland. A strong upper-level disturbance and its associated cold front moved into Maryland on the 25th. Hot and humid conditions ahead of the front led to high amounts of instability. Showers and thunderstorms developed along and ahead of the cold front. Due to the high amounts of instability, thunderstorms were able to mix down strong winds from aloft causing significant amounts of damage across portions of Maryland. A strong upper-level disturbance and its associated cold front moved into Maryland on the 25th. Hot and humid conditions ahead of the front led to high amounts of instability. Showers and thunderstorms developed along and ahead of the cold front. Due to the high amounts of instability, thunderstorms were able to mix down strong winds from aloft causing significant amounts of damage across portions of Maryland. A strong upper-level disturbance and its associated cold front moved into Maryland on the 25th. Hot and humid conditions ahead of the front led to high amounts of instability. Showers and thunderstorms developed along and ahead of the cold front. Due to the high amounts of instability, thunderstorms were able to mix down strong winds from aloft causing significant amounts of damage across portions of Maryland. A strong upper-level disturbance and its associated cold front moved into Maryland on the 25th. Hot and humid conditions ahead of the front led to high amounts of instability. Showers and thunderstorms developed along and ahead of the cold front. Due to the high amounts of instability, thunderstorms were able to mix down strong winds from aloft causing significant amounts of damage across portions of Maryland. A strong upper-level disturbance and its associated cold front moved into Maryland on the 25th. Hot and humid conditions ahead of the front led to high amounts of instability. Showers and thunderstorms developed along and ahead of the cold front. Due to the high amounts of instability, thunderstorms were able to mix down strong winds from aloft causing significant amounts of damage across portions of Maryland. A strong upper-level disturbance and its associated cold front moved into Maryland on the 25th. Hot and humid conditions ahead of the front led to high amounts of instability. Showers and thunderstorms developed along and ahead of the cold front. Due to the high amounts of instability, thunderstorms were able to mix down strong winds from aloft causing significant amounts of damage across portions of Maryland.\nEvent Narrative: Trees were uprooted in the GreenCastle Lakes subdivision. Several trees of four to five inches in diameter were down along English Avenue and McKay Street. A fatality occurred due to lightning about a half mile south of the Bay Bridge. A man was struck by lightning while riding on jet skis. A wind gust of 64 mph was reported near Laytonsville. Numerous branches were down near Bowie. A large Gazebo was also blown across a yard. A tree twelve inches in diameter was down at the intersection of Morning Dove Road and Tern Wing Road. A wind gust of 58 mph was measured in Laytonsville. Numerous trees were down near Cape St. Claire. A branch ten inches in diameter fell onto a house. A wind gust of 62 mph was recorded at Annapolis. A wind gust of 60 mph was recorded near Eastport. Several trees six to eight inches in diameter were down along Mapes Road and Cooper Avenue. Several trees twelve inches in diameter were down along Mapes Road and Obrien Road. A tree fell into a house along River Road and Palisades Boulevard. A wind gust of 60 mph was reported near Glenn Dale. A tree twenty inches in diameter fell along Old Chapel Road and Waldorf Way. Widespread branches two inches in diameter were down due to thunderstorm winds. Several large trees were down in the vicinity of Stoneybrook Road and Superior Road.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 38.6023 km away, between 2010-07-25 15:10:00 and 2010-07-25 15:15:00. The events included records with measured wind gusts of 54.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A strong cold frontal passage triggered strong to severe thunderstorms across the Maryland Eastern Shore during the second half of the afternoon on the 25th.\nEvent Narrative: A severe thunderstorm caused wind damage in and near Kent Island in Queen Anne's County. The Kent Island Volunteer Fire Department had their tents blown down. A greater than 100-year-old linden tree fell onto the Kent Island Federation of Art Building in Stevensville. Elsewhere in Stevensville, a grill was tossed into a pool. A motorcyclist was not injured after he rode into a downed tree. Wind damage extended into Grasonville where some large tree limbs were pulled down. Scattered outages on Kent Island lasted up to six hours. A Skywarn spotter measured a wind gust of 62 mph on Kent Island. Also 0.70 inches of rain fell in ten minutes and caused poor drainage flooding.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 27.7876 km away, between 2010-07-29 11:55:00 and 2010-07-29 15:06:00. The events included records with estimated wind gusts of 55.5 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 14500.0 and crop damage of 0.0. \n\nEpisode Narrative: A cold front passed through Maryland on the 29th triggering showers and thunderstorms. Warm and humid conditions ahead of the front led to moderate amounts of instability. Some thunderstorms became severe due to the instability along with strong winds aloft. A cold front passed through Maryland on the 29th triggering showers and thunderstorms. Warm and humid conditions ahead of the front led to moderate amounts of instability. Some thunderstorms became severe due to the instability along with strong winds aloft. A cold front passed through Maryland on the 29th triggering showers and thunderstorms. Warm and humid conditions ahead of the front led to moderate amounts of instability. Some thunderstorms became severe due to the instability along with strong winds aloft. A cold front passed through Maryland on the 29th triggering showers and thunderstorms. Warm and humid conditions ahead of the front led to moderate amounts of instability. Some thunderstorms became severe due to the instability along with strong winds aloft.\nEvent Narrative: Trees and wires were down in Laytonsville. Hardwood and softwood trees were dnapped. Large Limbs were also down near Greenberry Drive and Griffith Road. Five to ten trees were down in Baltimore. Two trees were down in Gwynn Oak.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 28.4012 km away, between 2010-07-29 12:24:00 and 2010-07-29 13:13:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front passed through the waters on the 29th, triggering showers and thunderstorms. Warm and humid conditions ahead of the front led to moderate amounts of instability. Some thunderstorms produced gusty winds due to the instability along with strong winds aloft. A cold front passed through the waters on the 29th, triggering showers and thunderstorms. Warm and humid conditions ahead of the front led to moderate amounts of instability. Some thunderstorms produced gusty winds due to the instability along with strong winds aloft. A cold front passed through the waters on the 29th, triggering showers and thunderstorms. Warm and humid conditions ahead of the front led to moderate amounts of instability. Some thunderstorms produced gusty winds due to the instability along with strong winds aloft. A cold front passed through the waters on the 29th, triggering showers and thunderstorms. Warm and humid conditions ahead of the front led to moderate amounts of instability. Some thunderstorms produced gusty winds due to the instability along with strong winds aloft. A cold front passed through the waters on the 29th, triggering showers and thunderstorms. Warm and humid conditions ahead of the front led to moderate amounts of instability. Some thunderstorms produced gusty winds due to the instability along with strong winds aloft. A cold front passed through the waters on the 29th, triggering showers and thunderstorms. Warm and humid conditions ahead of the front led to moderate amounts of instability. Some thunderstorms produced gusty winds due to the instability along with strong winds aloft. A cold front passed through the waters on the 29th, triggering showers and thunderstorms. Warm and humid conditions ahead of the front led to moderate amounts of instability. Some thunderstorms produced gusty winds due to the instability along with strong winds aloft. A cold front passed through the waters on the 29th, triggering showers and thunderstorms. Warm and humid conditions ahead of the front led to moderate amounts of instability. Some thunderstorms produced gusty winds due to the instability along with strong winds aloft. A cold front passed through the waters on the 29th, triggering showers and thunderstorms. Warm and humid conditions ahead of the front led to moderate amounts of instability. Some thunderstorms produced gusty winds due to the instability along with strong winds aloft. A cold front passed through the waters on the 29th, triggering showers and thunderstorms. Warm and humid conditions ahead of the front led to moderate amounts of instability. Some thunderstorms produced gusty winds due to the instability along with strong winds aloft.\nEvent Narrative: A wind gust of 37 knots was measured at Annapolis. A wind gust of 39 knots was measured near Eastport. Wind gusts between 34 and 38 knots were measured near Fells Point. Wind gusts up to 40 knots were reported at the Patapsco Buoy. A wind gust in excess of 30 knots was reported at Tolchester Beach. A wind gust was estimated around 37 knots near Annapolis. A wind gust of 39 knots was measured at Greenbury Point. A wind gust in excess of 30 knots was measured at Kent Island. A wind gust in excess of 30 knots was measured at Tolchester Beach. A wind gust of 34 knots was reported at Key Bridge.", "The following events were reported: Flash Flood. These occurred near station USW00093721, approximately 9.6113 km away, between 2010-07-29 13:10:00 and 2010-07-29 14:00:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front passed through Maryland on the 29th triggering showers and thunderstorms. Some of these thunderstorms produced locally heavy rainfall in a very brief period of time, triggering flash flooding in some urban areas. A cold front passed through Maryland on the 29th triggering showers and thunderstorms. Some of these thunderstorms produced locally heavy rainfall in a very brief period of time, triggering flash flooding in some urban areas.\nEvent Narrative: Hanover Street at Harbor View Hospital was reported impassable due to high water. A spotter in the area measured 1.01 inches of rain. Childs Street at Franklin Street had 6 inches of flowing water on it. A mesonet station recorded 1.30 inches of rain in the area.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 26.3275 km away, between 2010-08-05 17:01:00 and 2010-08-05 17:01:00. The events included records with measured wind gusts of 35.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A hot and humid air mass remained over the waters on the 5th. A series of upper-level disturbances in a zonal flow passed through the Mid-Atlantic during this time. Showers and thunderstorms developed during the afternoon and evening hours. There was enough instability from the hot and humid air mass for some thunderstorms to contain gusty winds.\nEvent Narrative: A wind gust of 35 knots was reported at Annapolis.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 38.1395 km away, between 2010-08-12 06:05:00 and 2010-08-12 16:14:00. The events included records with estimated wind gusts of 55.5 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 11000.0 and crop damage of 0.0. \n\nEpisode Narrative: A backdoor cold front stalled out over the region on the 12th while and upper-level disturbance passed through the area. A hot and humid air mass ahead of the cold front produced moderate amounts of instability. Some thunderstorms that developed were able to produce damaging wind and large hail. A backdoor cold front stalled out over the region on the 12th while and upper-level disturbance passed through the area. A hot and humid air mass ahead of the cold front produced moderate amounts of instability. Some thunderstorms that developed were able to produce damaging wind and large hail.\nEvent Narrative: Numerous large trees were blown down along and across Woodville Road and also near the intersection of Woodville Road and Old Annapolis Road. Small trees were down near Spencerville.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 27.6983 km away, between 2010-08-12 06:19:00 and 2010-08-12 07:25:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A backdoor cold front stalled out near the waters on the 12th while and upper-level disturbance passed through the area. A hot and humid air mass ahead of the cold front produced moderate amounts of instability. Some thunderstorms that developed were able to produce gusty winds. A backdoor cold front stalled out near the waters on the 12th while and upper-level disturbance passed through the area. A hot and humid air mass ahead of the cold front produced moderate amounts of instability. Some thunderstorms that developed were able to produce gusty winds. A backdoor cold front stalled out near the waters on the 12th while and upper-level disturbance passed through the area. A hot and humid air mass ahead of the cold front produced moderate amounts of instability. Some thunderstorms that developed were able to produce gusty winds. A backdoor cold front stalled out near the waters on the 12th while and upper-level disturbance passed through the area. A hot and humid air mass ahead of the cold front produced moderate amounts of instability. Some thunderstorms that developed were able to produce gusty winds.\nEvent Narrative: A wind gust in excess of 30 knots was reported at Kent Island. A wind gust of 36 knots was reported at Greenbury Point. A wind gust in excess of 30 knots was reported at Annapolis. A wind gust of 37 knots was measured at Oriole Park.", "The following events were reported: Flash Flood. These occurred near station USW00093721, approximately 24.7935 km away, between 2010-08-12 06:36:00 and 2010-08-12 23:48:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A northwest to southeast oriented cold front drifted into the area as an upper level disturbance moved southeast across the region. Thunderstorms initiated along the boundary during the morning, producing torrential downpours northern parts of the Washington metropolitan area. Rainfall amounts of 2 to 4 inches in under 3 hours were enough to produce flash flooding. Additional thunderstorms developed in the evening over saturated ground in the Baltimore metropolitan area, resulting in more flash flooding. A northwest to southeast oriented cold front drifted into the area as an upper level disturbance moved southeast across the region. Thunderstorms initiated along the boundary during the morning, producing torrential downpours northern parts of the Washington metropolitan area. Rainfall amounts of 2 to 4 inches in under 3 hours were enough to produce flash flooding. Additional thunderstorms developed in the evening over saturated ground in the Baltimore metropolitan area, resulting in more flash flooding. A northwest to southeast oriented cold front drifted into the area as an upper level disturbance moved southeast across the region. Thunderstorms initiated along the boundary during the morning, producing torrential downpours northern parts of the Washington metropolitan area. Rainfall amounts of 2 to 4 inches in under 3 hours were enough to produce flash flooding. Additional thunderstorms developed in the evening over saturated ground in the Baltimore metropolitan area, resulting in more flash flooding.\nEvent Narrative: Water rescue at railroad underpass on Maryland Route 755. Rainfall in the area measured 2.22 inches. Route 1 at Lincoln Avenue was closed in both directions as a result of high water. A rainfall total was reported from near the area of 3.51 inches. High water was reported on Norfolk Road.", "The following events were reported: Flood. These occurred near station USW00093721, approximately 17.4122 km away, between 2010-08-18 07:05:00 and 2010-08-18 09:57:00. The flood was caused by Heavy Rain. Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Low pressure moved west to east along a stationary boundary draped across Maryland. Thunderstorms associated with this low pressure produced very high rainfall rates with the aide of a moisture laden atmosphere. Flooding occurred across northern portions of the Washington metropolitan area during the morning from rainfall amounts of 3 to 4 inches in less than 3 hours. Low pressure moved west to east along a stationary boundary draped across Maryland. Thunderstorms associated with this low pressure produced very high rainfall rates with the aide of a moisture laden atmosphere. Flooding occurred across northern portions of the Washington metropolitan area during the morning from rainfall amounts of 3 to 4 inches in less than 3 hours. Low pressure moved west to east along a stationary boundary draped across Maryland. Thunderstorms associated with this low pressure produced very high rainfall rates with the aide of a moisture laden atmosphere. Flooding occurred across northern portions of the Washington metropolitan area during the morning from rainfall amounts of 3 to 4 inches in less than 3 hours.\nEvent Narrative: Flooding was reported at the intersection of Route 2 and College Parkway. Rainfall in the area was measured at 3.75 inches. A portion of Ritchie Highway was flooded near Whites Road. A rain gauge in the area measured 3.86 inches. Brockbridge Road was flooded near Maryland City Park. A rain gauge in the area measured 4.60 inches.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 27.7263 km away, between 2010-09-22 18:53:00 and 2010-09-22 19:51:00. The events included records with estimated wind gusts of 57.2 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 34000.0 and crop damage of 0.0. \n\nEpisode Narrative: An upper level disturbance and cold front moved out of the Ohio Valley into a very warm and relatively moist atmosphere in the Mid-Atlantic. Thunderstorms developed along this front as well as a lee trough during the afternoon. Instability, steep lapse rates, and moderate shear aided in some thunderstorms becoming severe, producing damaging winds during the evening. An upper level disturbance and cold front moved out of the Ohio Valley into a very warm and relatively moist atmosphere in the Mid-Atlantic. Thunderstorms developed along this front as well as a lee trough during the afternoon. Instability, steep lapse rates, and moderate shear aided in some thunderstorms becoming severe, producing damaging winds during the evening. An upper level disturbance and cold front moved out of the Ohio Valley into a very warm and relatively moist atmosphere in the Mid-Atlantic. Thunderstorms developed along this front as well as a lee trough during the afternoon. Instability, steep lapse rates, and moderate shear aided in some thunderstorms becoming severe, producing damaging winds during the evening. An upper level disturbance and cold front moved out of the Ohio Valley into a very warm and relatively moist atmosphere in the Mid-Atlantic. Thunderstorms developed along this front as well as a lee trough during the afternoon. Instability, steep lapse rates, and moderate shear aided in some thunderstorms becoming severe, producing damaging winds during the evening. An upper level disturbance and cold front moved out of the Ohio Valley into a very warm and relatively moist atmosphere in the Mid-Atlantic. Thunderstorms developed along this front as well as a lee trough during the afternoon. Instability, steep lapse rates, and moderate shear aided in some thunderstorms becoming severe, producing damaging winds during the evening. An upper level disturbance and cold front moved out of the Ohio Valley into a very warm and relatively moist atmosphere in the Mid-Atlantic. Thunderstorms developed along this front as well as a lee trough during the afternoon. Instability, steep lapse rates, and moderate shear aided in some thunderstorms becoming severe, producing damaging winds during the evening. An upper level disturbance and cold front moved out of the Ohio Valley into a very warm and relatively moist atmosphere in the Mid-Atlantic. Thunderstorms developed along this front as well as a lee trough during the afternoon. Instability, steep lapse rates, and moderate shear aided in some thunderstorms becoming severe, producing damaging winds during the evening. An upper level disturbance and cold front moved out of the Ohio Valley into a very warm and relatively moist atmosphere in the Mid-Atlantic. Thunderstorms developed along this front as well as a lee trough during the afternoon. Instability, steep lapse rates, and moderate shear aided in some thunderstorms becoming severe, producing damaging winds during the evening. An upper level disturbance and cold front moved out of the Ohio Valley into a very warm and relatively moist atmosphere in the Mid-Atlantic. Thunderstorms developed along this front as well as a lee trough during the afternoon. Instability, steep lapse rates, and moderate shear aided in some thunderstorms becoming severe, producing damaging winds during the evening. An upper level disturbance and cold front moved out of the Ohio Valley into a very warm and relatively moist atmosphere in the Mid-Atlantic. Thunderstorms developed along this front as well as a lee trough during the afternoon. Instability, steep lapse rates, and moderate shear aided in some thunderstorms becoming severe, producing damaging winds during the evening. An upper level disturbance and cold front moved out of the Ohio Valley into a very warm and relatively moist atmosphere in the Mid-Atlantic. Thunderstorms developed along this front as well as a lee trough during the afternoon. Instability, steep lapse rates, and moderate shear aided in some thunderstorms becoming severe, producing damaging winds during the evening. An upper level disturbance and cold front moved out of the Ohio Valley into a very warm and relatively moist atmosphere in the Mid-Atlantic. Thunderstorms developed along this front as well as a lee trough during the afternoon. Instability, steep lapse rates, and moderate shear aided in some thunderstorms becoming severe, producing damaging winds during the evening. An upper level disturbance and cold front moved out of the Ohio Valley into a very warm and relatively moist atmosphere in the Mid-Atlantic. Thunderstorms developed along this front as well as a lee trough during the afternoon. Instability, steep lapse rates, and moderate shear aided in some thunderstorms becoming severe, producing damaging winds during the evening. An upper level disturbance and cold front moved out of the Ohio Valley into a very warm and relatively moist atmosphere in the Mid-Atlantic. Thunderstorms developed along this front as well as a lee trough during the afternoon. Instability, steep lapse rates, and moderate shear aided in some thunderstorms becoming severe, producing damaging winds during the evening. An upper level disturbance and cold front moved out of the Ohio Valley into a very warm and relatively moist atmosphere in the Mid-Atlantic. Thunderstorms developed along this front as well as a lee trough during the afternoon. Instability, steep lapse rates, and moderate shear aided in some thunderstorms becoming severe, producing damaging winds during the evening.\nEvent Narrative: Multiple trees down near the intersection of Governors Bridge Road and U.S. 301. Numerous trees were down near retail locations along the 4100 block of Crain Highway. A tree was down at Maryland Route 424 and Maryland Route 450 2 miles southeast of Crofton. Several trees had their tops sheared off. Many large branches were also snapped 2 miles west-northwest of Riva. A tree was down at the intersection of Mount Airy Road and Royal Glen Avenue 1 mile west-northwest of Davidsonville. Multiple large trees were downed. Trees were snapped off at the tops and many large limbs were down 1 mile west-northwest of Hydes. A tree was down at Piney Orchard and Patuxent Road. Tree branches were broken by strong thunderstorm wind 1 mile west-southwest of Odenton. Several trees were down on Northview Drive 1 mile south of Bowie. Numerous trees were down near U.S. 301 and U.S. 50 interchange 1 mile east-southeast of Bowie. A tree was down at Maryland Route 3 and St. Stephens Church Road. Trees were down along Old York Road 4 miles east-northeast of Monkton. Multiple trees were down in Long Green. A few trees were down on Baldwin Mill Road south of Sweet Air Road and on Long Green Pike north of Hydes Road. Two large trees downed and fell onto powerlines at the corner of Muddy Creek Road and Cumberstone Road 1 mile northwest of Galesville.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 32.7199 km away, between 2010-09-22 19:10:00 and 2010-09-22 20:00:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: An upper level disturbance and cold front moved out of the Ohio Valley into a very warm and relatively moist atmosphere in the Mid-Atlantic. Thunderstorms developed along this front as well as a lee trough during the afternoon. Instability, steep lapse rates, and moderate shear aided in some thunderstorms becoming severe, producing strong winds over the waters during the afternoon and evening. An upper level disturbance and cold front moved out of the Ohio Valley into a very warm and relatively moist atmosphere in the Mid-Atlantic. Thunderstorms developed along this front as well as a lee trough during the afternoon. Instability, steep lapse rates, and moderate shear aided in some thunderstorms becoming severe, producing strong winds over the waters during the afternoon and evening. An upper level disturbance and cold front moved out of the Ohio Valley into a very warm and relatively moist atmosphere in the Mid-Atlantic. Thunderstorms developed along this front as well as a lee trough during the afternoon. Instability, steep lapse rates, and moderate shear aided in some thunderstorms becoming severe, producing strong winds over the waters during the afternoon and evening. An upper level disturbance and cold front moved out of the Ohio Valley into a very warm and relatively moist atmosphere in the Mid-Atlantic. Thunderstorms developed along this front as well as a lee trough during the afternoon. Instability, steep lapse rates, and moderate shear aided in some thunderstorms becoming severe, producing strong winds over the waters during the afternoon and evening.\nEvent Narrative: Wind gust of 34 knots estimated at Annapolis CBIBS buoy. Estimated wind gusts of 40 knots at Columbia Beach. Wind gusts from 34 to 38 knots were measured at the Annapolis Naval Academy. Wind gust of 34 knots measured at Annapolis CBIBS buoy.", "The following events were reported: Flash Flood, Flood. These occurred near station USW00093721, approximately 18.7413 km away, between 2010-09-30 05:00:00 and 2010-09-30 23:59:00. The flood was caused by Heavy Rain. Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A corridor of moisture funnelled up the eastern seaboard. Bands of heavy rain began to rapidly move into Maryland just after midnight on Thursday morning, September 30. After the initial low pressure passed north of the area late Thursday morning after producing up to 8 inches of rain across portions of Maryland and numerous reports of flash flooding, a brief lull in precipitation occurred Thursday afternoon, before the remnant circulation of former Tropical Storm Nicole moved up the Delmarva Peninsula, reinvigorating heavy rainfall. Storm total rainfall exceeded one foot across many areas along the shore of the Chesapeake Bay, with reported measurements of over 14 inches in several locations in St. Mary\ufffd\ufffd\ufffds County, MD. Hundreds of roads were closed due to high water across the area, and high water rescues and roadway washouts were frequent. There no reported injuries or deaths. At Baltimore-Washington International, the rainfall amount of 6.02\ufffd\ufffd\ufffd on September 30 was the 2nd highest daily total ever recorded, with only August 23, 1933 receiving a higher amount in a single calendar day. Events associated with this episode continued into October 1. A corridor of moisture funnelled up the eastern seaboard. Bands of heavy rain began to rapidly move into Maryland just after midnight on Thursday morning, September 30. After the initial low pressure passed north of the area late Thursday morning after producing up to 8 inches of rain across portions of Maryland and numerous reports of flash flooding, a brief lull in precipitation occurred Thursday afternoon, before the remnant circulation of former Tropical Storm Nicole moved up the Delmarva Peninsula, reinvigorating heavy rainfall. Storm total rainfall exceeded one foot across many areas along the shore of the Chesapeake Bay, with reported measurements of over 14 inches in several locations in St. Mary\ufffd\ufffd\ufffds County, MD. Hundreds of roads were closed due to high water across the area, and high water rescues and roadway washouts were frequent. There no reported injuries or deaths. At Baltimore-Washington International, the rainfall amount of 6.02\ufffd\ufffd\ufffd on September 30 was the 2nd highest daily total ever recorded, with only August 23, 1933 receiving a higher amount in a single calendar day. Events associated with this episode continued into October 1. A corridor of moisture funnelled up the eastern seaboard. Bands of heavy rain began to rapidly move into Maryland just after midnight on Thursday morning, September 30. After the initial low pressure passed north of the area late Thursday morning after producing up to 8 inches of rain across portions of Maryland and numerous reports of flash flooding, a brief lull in precipitation occurred Thursday afternoon, before the remnant circulation of former Tropical Storm Nicole moved up the Delmarva Peninsula, reinvigorating heavy rainfall. Storm total rainfall exceeded one foot across many areas along the shore of the Chesapeake Bay, with reported measurements of over 14 inches in several locations in St. Mary\ufffd\ufffd\ufffds County, MD. Hundreds of roads were closed due to high water across the area, and high water rescues and roadway washouts were frequent. There no reported injuries or deaths. At Baltimore-Washington International, the rainfall amount of 6.02\ufffd\ufffd\ufffd on September 30 was the 2nd highest daily total ever recorded, with only August 23, 1933 receiving a higher amount in a single calendar day. Events associated with this episode continued into October 1. A corridor of moisture funnelled up the eastern seaboard. Bands of heavy rain began to rapidly move into Maryland just after midnight on Thursday morning, September 30. After the initial low pressure passed north of the area late Thursday morning after producing up to 8 inches of rain across portions of Maryland and numerous reports of flash flooding, a brief lull in precipitation occurred Thursday afternoon, before the remnant circulation of former Tropical Storm Nicole moved up the Delmarva Peninsula, reinvigorating heavy rainfall. Storm total rainfall exceeded one foot across many areas along the shore of the Chesapeake Bay, with reported measurements of over 14 inches in several locations in St. Mary\ufffd\ufffd\ufffds County, MD. Hundreds of roads were closed due to high water across the area, and high water rescues and roadway washouts were frequent. There no reported injuries or deaths. At Baltimore-Washington International, the rainfall amount of 6.02\ufffd\ufffd\ufffd on September 30 was the 2nd highest daily total ever recorded, with only August 23, 1933 receiving a higher amount in a single calendar day. Events associated with this episode continued into October 1. A corridor of moisture funnelled up the eastern seaboard. Bands of heavy rain began to rapidly move into Maryland just after midnight on Thursday morning, September 30. After the initial low pressure passed north of the area late Thursday morning after producing up to 8 inches of rain across portions of Maryland and numerous reports of flash flooding, a brief lull in precipitation occurred Thursday afternoon, before the remnant circulation of former Tropical Storm Nicole moved up the Delmarva Peninsula, reinvigorating heavy rainfall. Storm total rainfall exceeded one foot across many areas along the shore of the Chesapeake Bay, with reported measurements of over 14 inches in several locations in St. Mary\ufffd\ufffd\ufffds County, MD. Hundreds of roads were closed due to high water across the area, and high water rescues and roadway washouts were frequent. There no reported injuries or deaths. At Baltimore-Washington International, the rainfall amount of 6.02\ufffd\ufffd\ufffd on September 30 was the 2nd highest daily total ever recorded, with only August 23, 1933 receiving a higher amount in a single calendar day. Events associated with this episode continued into October 1. A corridor of moisture funnelled up the eastern seaboard. Bands of heavy rain began to rapidly move into Maryland just after midnight on Thursday morning, September 30. After the initial low pressure passed north of the area late Thursday morning after producing up to 8 inches of rain across portions of Maryland and numerous reports of flash flooding, a brief lull in precipitation occurred Thursday afternoon, before the remnant circulation of former Tropical Storm Nicole moved up the Delmarva Peninsula, reinvigorating heavy rainfall. Storm total rainfall exceeded one foot across many areas along the shore of the Chesapeake Bay, with reported measurements of over 14 inches in several locations in St. Mary\ufffd\ufffd\ufffds County, MD. Hundreds of roads were closed due to high water across the area, and high water rescues and roadway washouts were frequent. There no reported injuries or deaths. At Baltimore-Washington International, the rainfall amount of 6.02\ufffd\ufffd\ufffd on September 30 was the 2nd highest daily total ever recorded, with only August 23, 1933 receiving a higher amount in a single calendar day. Events associated with this episode continued into October 1. A corridor of moisture funnelled up the eastern seaboard. Bands of heavy rain began to rapidly move into Maryland just after midnight on Thursday morning, September 30. After the initial low pressure passed north of the area late Thursday morning after producing up to 8 inches of rain across portions of Maryland and numerous reports of flash flooding, a brief lull in precipitation occurred Thursday afternoon, before the remnant circulation of former Tropical Storm Nicole moved up the Delmarva Peninsula, reinvigorating heavy rainfall. Storm total rainfall exceeded one foot across many areas along the shore of the Chesapeake Bay, with reported measurements of over 14 inches in several locations in St. Mary\ufffd\ufffd\ufffds County, MD. Hundreds of roads were closed due to high water across the area, and high water rescues and roadway washouts were frequent. There no reported injuries or deaths. At Baltimore-Washington International, the rainfall amount of 6.02\ufffd\ufffd\ufffd on September 30 was the 2nd highest daily total ever recorded, with only August 23, 1933 receiving a higher amount in a single calendar day. Events associated with this episode continued into October 1. A corridor of moisture funnelled up the eastern seaboard. Bands of heavy rain began to rapidly move into Maryland just after midnight on Thursday morning, September 30. After the initial low pressure passed north of the area late Thursday morning after producing up to 8 inches of rain across portions of Maryland and numerous reports of flash flooding, a brief lull in precipitation occurred Thursday afternoon, before the remnant circulation of former Tropical Storm Nicole moved up the Delmarva Peninsula, reinvigorating heavy rainfall. Storm total rainfall exceeded one foot across many areas along the shore of the Chesapeake Bay, with reported measurements of over 14 inches in several locations in St. Mary\ufffd\ufffd\ufffds County, MD. Hundreds of roads were closed due to high water across the area, and high water rescues and roadway washouts were frequent. There no reported injuries or deaths. At Baltimore-Washington International, the rainfall amount of 6.02\ufffd\ufffd\ufffd on September 30 was the 2nd highest daily total ever recorded, with only August 23, 1933 receiving a higher amount in a single calendar day. Events associated with this episode continued into October 1. A corridor of moisture funnelled up the eastern seaboard. Bands of heavy rain began to rapidly move into Maryland just after midnight on Thursday morning, September 30. After the initial low pressure passed north of the area late Thursday morning after producing up to 8 inches of rain across portions of Maryland and numerous reports of flash flooding, a brief lull in precipitation occurred Thursday afternoon, before the remnant circulation of former Tropical Storm Nicole moved up the Delmarva Peninsula, reinvigorating heavy rainfall. Storm total rainfall exceeded one foot across many areas along the shore of the Chesapeake Bay, with reported measurements of over 14 inches in several locations in St. Mary\ufffd\ufffd\ufffds County, MD. Hundreds of roads were closed due to high water across the area, and high water rescues and roadway washouts were frequent. There no reported injuries or deaths. At Baltimore-Washington International, the rainfall amount of 6.02\ufffd\ufffd\ufffd on September 30 was the 2nd highest daily total ever recorded, with only August 23, 1933 receiving a higher amount in a single calendar day. Events associated with this episode continued into October 1. A corridor of moisture funnelled up the eastern seaboard. Bands of heavy rain began to rapidly move into Maryland just after midnight on Thursday morning, September 30. After the initial low pressure passed north of the area late Thursday morning after producing up to 8 inches of rain across portions of Maryland and numerous reports of flash flooding, a brief lull in precipitation occurred Thursday afternoon, before the remnant circulation of former Tropical Storm Nicole moved up the Delmarva Peninsula, reinvigorating heavy rainfall. Storm total rainfall exceeded one foot across many areas along the shore of the Chesapeake Bay, with reported measurements of over 14 inches in several locations in St. Mary\ufffd\ufffd\ufffds County, MD. Hundreds of roads were closed due to high water across the area, and high water rescues and roadway washouts were frequent. There no reported injuries or deaths. At Baltimore-Washington International, the rainfall amount of 6.02\ufffd\ufffd\ufffd on September 30 was the 2nd highest daily total ever recorded, with only August 23, 1933 receiving a higher amount in a single calendar day. Events associated with this episode continued into October 1. A corridor of moisture funnelled up the eastern seaboard. Bands of heavy rain began to rapidly move into Maryland just after midnight on Thursday morning, September 30. After the initial low pressure passed north of the area late Thursday morning after producing up to 8 inches of rain across portions of Maryland and numerous reports of flash flooding, a brief lull in precipitation occurred Thursday afternoon, before the remnant circulation of former Tropical Storm Nicole moved up the Delmarva Peninsula, reinvigorating heavy rainfall. Storm total rainfall exceeded one foot across many areas along the shore of the Chesapeake Bay, with reported measurements of over 14 inches in several locations in St. Mary\ufffd\ufffd\ufffds County, MD. Hundreds of roads were closed due to high water across the area, and high water rescues and roadway washouts were frequent. There no reported injuries or deaths. At Baltimore-Washington International, the rainfall amount of 6.02\ufffd\ufffd\ufffd on September 30 was the 2nd highest daily total ever recorded, with only August 23, 1933 receiving a higher amount in a single calendar day. Events associated with this episode continued into October 1. A corridor of moisture funnelled up the eastern seaboard. Bands of heavy rain began to rapidly move into Maryland just after midnight on Thursday morning, September 30. After the initial low pressure passed north of the area late Thursday morning after producing up to 8 inches of rain across portions of Maryland and numerous reports of flash flooding, a brief lull in precipitation occurred Thursday afternoon, before the remnant circulation of former Tropical Storm Nicole moved up the Delmarva Peninsula, reinvigorating heavy rainfall. Storm total rainfall exceeded one foot across many areas along the shore of the Chesapeake Bay, with reported measurements of over 14 inches in several locations in St. Mary\ufffd\ufffd\ufffds County, MD. Hundreds of roads were closed due to high water across the area, and high water rescues and roadway washouts were frequent. There no reported injuries or deaths. At Baltimore-Washington International, the rainfall amount of 6.02\ufffd\ufffd\ufffd on September 30 was the 2nd highest daily total ever recorded, with only August 23, 1933 receiving a higher amount in a single calendar day. Events associated with this episode continued into October 1. A corridor of moisture funnelled up the eastern seaboard. Bands of heavy rain began to rapidly move into Maryland just after midnight on Thursday morning, September 30. After the initial low pressure passed north of the area late Thursday morning after producing up to 8 inches of rain across portions of Maryland and numerous reports of flash flooding, a brief lull in precipitation occurred Thursday afternoon, before the remnant circulation of former Tropical Storm Nicole moved up the Delmarva Peninsula, reinvigorating heavy rainfall. Storm total rainfall exceeded one foot across many areas along the shore of the Chesapeake Bay, with reported measurements of over 14 inches in several locations in St. Mary\ufffd\ufffd\ufffds County, MD. Hundreds of roads were closed due to high water across the area, and high water rescues and roadway washouts were frequent. There no reported injuries or deaths. At Baltimore-Washington International, the rainfall amount of 6.02\ufffd\ufffd\ufffd on September 30 was the 2nd highest daily total ever recorded, with only August 23, 1933 receiving a higher amount in a single calendar day. Events associated with this episode continued into October 1. A corridor of moisture funnelled up the eastern seaboard. Bands of heavy rain began to rapidly move into Maryland just after midnight on Thursday morning, September 30. After the initial low pressure passed north of the area late Thursday morning after producing up to 8 inches of rain across portions of Maryland and numerous reports of flash flooding, a brief lull in precipitation occurred Thursday afternoon, before the remnant circulation of former Tropical Storm Nicole moved up the Delmarva Peninsula, reinvigorating heavy rainfall. Storm total rainfall exceeded one foot across many areas along the shore of the Chesapeake Bay, with reported measurements of over 14 inches in several locations in St. Mary\ufffd\ufffd\ufffds County, MD. Hundreds of roads were closed due to high water across the area, and high water rescues and roadway washouts were frequent. There no reported injuries or deaths. At Baltimore-Washington International, the rainfall amount of 6.02\ufffd\ufffd\ufffd on September 30 was the 2nd highest daily total ever recorded, with only August 23, 1933 receiving a higher amount in a single calendar day. Events associated with this episode continued into October 1.\nEvent Narrative: Spotter observed 6 to 12 inches of flowing water over Merritt Blvd. A rain gage in the area measured 8.51 inches. Flash Flooding was reported in the vicinity of Race Road, Furnance Road, and Park Center Drive. A rainfall report of 6.18 inches was received from the area. One foot of standing water was observed on southbound Maryland Route 2 at the junction with Route 50 and Route 450. A rainfall report of 10.49 was also received from the area. West Patapsco Road was closed due to flash flooding. Rain gages in the area measured as much as 8.06. Meadowridge Drive was closed. A rainfall report of 4.70 was observed near the area. Spotter observed 10300 block of Route 40 closed due to flash flooding. Rain gage in the area measured 9.52 inches of rain. Route 7 was closed just west of Campbell Blvd. A rain gage in the region measured 10.17 of rain. Numerous basements were flooded in the area. A rainfall total from the area was reported at 9.90 inches. Mace Avenue was closed due to flash flooding at the Southeast Freeway. A mesonet site in the area observed 8.60 inches of rain. The intersection of Glider Drive and Rossville Blvd. was closed. A rain gage in the area measured 7.90 inches of rainfall. North Point Road was closed between German Hill Road and Willow Road. A mesonet site measured 8.47 inches of rain near the event. Geneva Road was closed at Fort Smallwood Road. A rain gage in the area measured 11.52 inches of rain. Orems Road was closed at Sunnyside Lane. Rainfall reported in the region included a 7.68 total near the event. Route 450 was closed due to high water at Huntwood Drive. A rain gage in the area measured 9.79 inches.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 33.3755 km away, between 2010-09-30 08:41:00 and 2010-09-30 10:20:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A surface low pressure system moved northward up the eastern seaboard along a north-to-south oriented stationary front. Very moist low level atmosphere and 70 knot southeasterly winds combined with modest instability to produce strong winds in the strongest thunderstorms that developed. A surface low pressure system moved northward up the eastern seaboard along a north-to-south oriented stationary front. Very moist low level atmosphere and 70 knot southeasterly winds combined with modest instability to produce strong winds in the strongest thunderstorms that developed.\nEvent Narrative: Wind gust of 34 knots observed at Greenbury Point. A wind gust of 48.7 knots was measured at Thomas Point Lighthouse.", "The following events were reported: Tornado. These occurred near station USW00093721, approximately 21.3327 km away, between 2010-09-30 08:46:00 and 2010-09-30 08:49:00.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 15000.0 and crop damage of 0.0. \n\nEpisode Narrative: A surface low pressure system moved northward up the eastern seaboard along a north-to-south oriented stationary front. Very moist low level atmosphere and 70 knot southeasterly winds combined with modest instability to produce damaging winds in the strongest thunderstorms that developed. An isolated tornado also touched down in Anne Arundel County.\nEvent Narrative: Damage consisted of uprooted and snapped trees, most along Milburn Circle. One tree fell on a vehicle; another crushed a shed. There was also minor siding and shingle damage.", "The following events were reported: Flash Flood. These occurred near station USW00093721, approximately 11.9822 km away, between 2010-10-01 00:00:00 and 2010-10-01 01:45:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A corridor of moisture funnelled up the eastern seaboard. Bands of heavy rain began to rapidly move into Maryland just after midnight on Thursday morning, September 30. After the initial low pressure passed north of the area late Thursday morning after producing up to 8 inches of rain across portions of Maryland and numerous reports of flash flooding, a brief lull in precipitation occurred Thursday afternoon, before the remnant circulation of former Tropical Storm Nicole moved up the Delmarva Peninsula, reinvigorating heavy rainfall. The heavy rainfall on September 30th caused flash flooding that continued into October 1st.\nEvent Narrative: Numerous basements were flooded in the area. A rainfall total from the area was reported at 9.90 inches.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 16.6549 km away, between 2010-10-11 21:02:00 and 2010-10-11 21:02:00. The events included records with estimated wind gusts of 51.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 200.0 and crop damage of 0.0. \n\nEpisode Narrative: High pressure off the East Coast pumped in warm and moist air over Maryland. An upper-level disturbance passed through in the westerly flow aloft during the evening of the 11th. The upper-level disturbance combined with limited instability to trigger showers and thunderstorms. A couple thunderstorms were able to produce damaging winds. High pressure off the East Coast pumped in warm and moist air over Maryland. An upper-level disturbance passed through in the westerly flow aloft during the evening of the 11th. The upper-level disturbance combined with limited instability to trigger showers and thunderstorms. A couple thunderstorms were able to produce damaging winds.\nEvent Narrative: A wind gust of 60 mph was estimated by a Mariner near Magothy Beach Road and Riverside Drive. A branch that was two inches in diameter was blown down at Longmeadow North.", "The following events were reported: Marine Hail. These occurred near station USW00093721, approximately 24.1459 km away, between 2010-10-11 21:11:00 and 2010-10-11 21:11:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: High pressure off the East Coast pumped in warm and moist air over the waters. An upper-level disturbance passed through in the westerly flow aloft during the evening of the 11th. The upper-level disturbance combined with limited instability to trigger showers and thunderstorms. An isolated thunderstorm was able to produce large hail.\nEvent Narrative: Nickel size hail was reported near Gibson Island.", "The following events were reported: Thunderstorm Wind, Tornado. These occurred near station USW00093721, approximately 25.9331 km away, between 2010-11-17 01:05:00 and 2010-11-17 01:44:00.The events resulted in 3 injuries and 0 fatalities. The events caused property damage valued at 301000.0 and crop damage of 0.0. \n\nEpisode Narrative: A strong cold front passed through the region late during the early morning morning hours of the 17th. A strong southerly flow ahead of the cold front transported plenty of moisture into the area allowing for limited instability to develop. Strong forcing associated with the frontal passage combined with limited instability to trigger showers and thunderstorms. Thunderstorms were able to mix down very strong winds aloft causing damaging winds across some locations. A strong cold front passed through the region late during the early morning morning hours of the 17th. A strong southerly flow ahead of the cold front transported plenty of moisture into the area allowing for limited instability to develop. Strong forcing associated with the frontal passage combined with limited instability to trigger showers and thunderstorms. Thunderstorms were able to mix down very strong winds aloft causing damaging winds across some locations. A strong cold front passed through the region late during the early morning morning hours of the 17th. A strong southerly flow ahead of the cold front transported plenty of moisture into the area allowing for limited instability to develop. Strong forcing associated with the frontal passage combined with limited instability to trigger showers and thunderstorms. Thunderstorms were able to mix down very strong winds aloft causing damaging winds across some locations. A strong cold front passed through the region late during the early morning morning hours of the 17th. A strong southerly flow ahead of the cold front transported plenty of moisture into the area allowing for limited instability to develop. Strong forcing associated with the frontal passage combined with limited instability to trigger showers and thunderstorms. Thunderstorms were able to mix down very strong winds aloft causing damaging winds across some locations. A strong cold front passed through the region late during the early morning morning hours of the 17th. A strong southerly flow ahead of the cold front transported plenty of moisture into the area allowing for limited instability to develop. Strong forcing associated with the frontal passage combined with limited instability to trigger showers and thunderstorms. Thunderstorms were able to mix down very strong winds aloft causing damaging winds across some locations. A strong cold front passed through the region late during the early morning morning hours of the 17th. A strong southerly flow ahead of the cold front transported plenty of moisture into the area allowing for limited instability to develop. Strong forcing associated with the frontal passage combined with limited instability to trigger showers and thunderstorms. Thunderstorms were able to mix down very strong winds aloft causing damaging winds across some locations. A strong cold front passed through the region late during the early morning morning hours of the 17th. A strong southerly flow ahead of the cold front transported plenty of moisture into the area allowing for limited instability to develop. Strong forcing associated with the frontal passage combined with limited instability to trigger showers and thunderstorms. Thunderstorms were able to mix down very strong winds aloft causing damaging winds across some locations. A strong cold front passed through the region late during the early morning morning hours of the 17th. A strong southerly flow ahead of the cold front transported plenty of moisture into the area allowing for limited instability to develop. Strong forcing associated with the frontal passage combined with limited instability to trigger showers and thunderstorms. Thunderstorms were able to mix down very strong winds aloft causing damaging winds across some locations. A strong cold front passed through the region late during the early morning morning hours of the 17th. A strong southerly flow ahead of the cold front transported plenty of moisture into the area allowing for limited instability to develop. Strong forcing associated with the frontal passage combined with limited instability to trigger showers and thunderstorms. Thunderstorms were able to mix down very strong winds aloft causing damaging winds across some locations. A strong cold front passed through the region late during the early morning morning hours of the 17th. A strong southerly flow ahead of the cold front transported plenty of moisture into the area allowing for limited instability to develop. Strong forcing associated with the frontal passage combined with limited instability to trigger showers and thunderstorms. Thunderstorms were able to mix down very strong winds aloft causing damaging winds across some locations. A strong cold front passed through the region late during the early morning morning hours of the 17th. A strong southerly flow ahead of the cold front transported plenty of moisture into the area allowing for limited instability to develop. Strong forcing associated with the frontal passage combined with limited instability to trigger showers and thunderstorms. Thunderstorms were able to mix down very strong winds aloft causing damaging winds across some locations.\nEvent Narrative: Multiple trees were down near Hillendale. Trees fell onto a couple houses. A wind gust of 65 mph was estimated by a trained spotter. A tree was down near Montpelier Hills. A wind gust of 50 knots was measured near Flamewood. Large branches and old trees were down at Chinquapin Crest. Winds moved multiple secured airplanes from their parking lots at Lee Airport. One plane was significantly damaged. Numerous trees were down along Bay View Drive. Numerous trees were down near Morgan State University. The path of tree damage continued to the northeast into southern Baltimore County. Numerous trees were down from thunderstorm wind gusts from the city of Baltimore northeast to Gunpowder Falls State Park. Three of the units in the Dutch Village Apartment complex had their roofs blown off. There was also extensive tree damage across the area and several cars were shifted by the force of the wind.||Three minor injuries were reported in Baltimore. One of those was a child. The path of the tornado continued into Baltimore County. The damage was centered on the Perring Parkway Shopping Center in Parkville. Evidence of the tornado included retail property surveillance cameras which showed debris blowing in different directions. Trees and light poles were falling in a convergent pattern and leaf spatter was noted on all four sides of automobiles and structures.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 29.0344 km away, between 2010-11-17 01:26:00 and 2010-11-17 01:52:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A strong cold front passed through the waters during the early morning hours of the 17th. A strong southerly flow ahead of the cold front transported plenty of moisture into the area allowing for limited instability to develop. Strong forcing associated with the frontal passage combined with limited instability to trigger showers and thunderstorms. Thunderstorms were able to mix down gusty winds from aloft. A strong cold front passed through the waters during the early morning hours of the 17th. A strong southerly flow ahead of the cold front transported plenty of moisture into the area allowing for limited instability to develop. Strong forcing associated with the frontal passage combined with limited instability to trigger showers and thunderstorms. Thunderstorms were able to mix down gusty winds from aloft. A strong cold front passed through the waters during the early morning hours of the 17th. A strong southerly flow ahead of the cold front transported plenty of moisture into the area allowing for limited instability to develop. Strong forcing associated with the frontal passage combined with limited instability to trigger showers and thunderstorms. Thunderstorms were able to mix down gusty winds from aloft. A strong cold front passed through the waters during the early morning hours of the 17th. A strong southerly flow ahead of the cold front transported plenty of moisture into the area allowing for limited instability to develop. Strong forcing associated with the frontal passage combined with limited instability to trigger showers and thunderstorms. Thunderstorms were able to mix down gusty winds from aloft. A strong cold front passed through the waters during the early morning hours of the 17th. A strong southerly flow ahead of the cold front transported plenty of moisture into the area allowing for limited instability to develop. Strong forcing associated with the frontal passage combined with limited instability to trigger showers and thunderstorms. Thunderstorms were able to mix down gusty winds from aloft. A strong cold front passed through the waters during the early morning hours of the 17th. A strong southerly flow ahead of the cold front transported plenty of moisture into the area allowing for limited instability to develop. Strong forcing associated with the frontal passage combined with limited instability to trigger showers and thunderstorms. Thunderstorms were able to mix down gusty winds from aloft.\nEvent Narrative: A wind gust in excess of 30 knots was reported at Sandy Point. A wind gust of 35 knots was measured at the Patapsco Buoy. A wind gust of 35 knots was measured Annapolis. A wind gust of 42 knots was measured at Kent Island. A wind gust of 40 knots was reported at Key Bridge. A wind gust of 34 knots was measured at Tolchester Beach.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 16.8768 km away, between 2010-12-01 09:35:00 and 2010-12-01 09:40:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 4000.0 and crop damage of 0.0. \n\nEpisode Narrative: A strong cold front passed through the region early on the first of December. Southerly winds ahead of the front were able to pump in plenty of warm and moist air for this time of year. Strong forcing from the front combined with limited instability to trigger showers and thunderstorms. Strong winds aloft were able to mix down to the surface in some of the stronger thunderstorms. A strong cold front passed through the region early on the first of December. Southerly winds ahead of the front were able to pump in plenty of warm and moist air for this time of year. Strong forcing from the front combined with limited instability to trigger showers and thunderstorms. Strong winds aloft were able to mix down to the surface in some of the stronger thunderstorms.\nEvent Narrative: A tree fell onto wires near Greenspring Avenue. Trees were down near Dorchester Road and Wilkens Avenue.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 26.3242 km away, between 2011-02-25 13:16:00 and 2011-02-25 14:00:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Strong low pressure tracked through the Ohio Valley on the 25th. The cold front associated with this system passed through the waters during the afternoon. There was enough instability for showers and thunderstorms ahead of the front. The stronger thunderstorms were able to mix down gusty winds from aloft. Strong low pressure tracked through the Ohio Valley on the 25th. The cold front associated with this system passed through the waters during the afternoon. There was enough instability for showers and thunderstorms ahead of the front. The stronger thunderstorms were able to mix down gusty winds from aloft. Strong low pressure tracked through the Ohio Valley on the 25th. The cold front associated with this system passed through the waters during the afternoon. There was enough instability for showers and thunderstorms ahead of the front. The stronger thunderstorms were able to mix down gusty winds from aloft. Strong low pressure tracked through the Ohio Valley on the 25th. The cold front associated with this system passed through the waters during the afternoon. There was enough instability for showers and thunderstorms ahead of the front. The stronger thunderstorms were able to mix down gusty winds from aloft. Strong low pressure tracked through the Ohio Valley on the 25th. The cold front associated with this system passed through the waters during the afternoon. There was enough instability for showers and thunderstorms ahead of the front. The stronger thunderstorms were able to mix down gusty winds from aloft.\nEvent Narrative: A wind gust of 46 knots was reported at Thomas Point Lighthouse. A wind gust in excess of 30 knots was measured at the Baltimore Buoy. Wind gusts up to 37 knots were recorded at the Baltimore Key Bridge. Wind gusts up to 36 knots were reported at Miller Island. A wind gust of 38 knots was recorded at Tolchester Beach.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 6.7131 km away, between 2011-02-25 13:32:00 and 2011-02-25 13:32:00. The events included records with estimated wind gusts of 56.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Strong low pressure tracked through the Ohio Valley on the 25th. The cold front associated with this system passed through Maryland during the afternoon. There was enough instability for showers and thunderstorms ahead of the front. The stronger thunderstorms were able to mix down strong winds from aloft.\nEvent Narrative: Wind gusts were estimated to be between 60 and 70 mph.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 36.9916 km away, between 2011-03-06 19:00:00 and 2011-03-06 19:00:00. The events included records with measured wind gusts of 37.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Low pressure tracked up the Mid-Atlantic Coast spreading showers across the waters on the 6th. Gusty winds from aloft were able to mix down in the heavier showers during the evening hours.\nEvent Narrative: A wind gust of 37 knots was reported at Thomas Point Lighthouse.", "The following events were reported: Flash Flood. These occurred near station USW00093721, approximately 17.8753 km away, between 2011-03-10 22:00:00 and 2011-03-10 22:30:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Low pressure passed through the Great Lakes on the 10th. A strong cold front associated with this system slowly moved through Maryland during the afternoon and evening hours. A southeast wind between this system and high pressure over the Atlantic Ocean pumped in copious amounts of moisture across the region. The deep moisture combined with strong lift from the front and limited instability to trigger showers and thunderstorms. Some thunderstorms produced locally heavy amounts of rain in a short period of time which led to flash flooding.\nEvent Narrative: Both the Meadow Mill and Jones Falls parking lots were closed due to flash flooding.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 30.0239 km away, between 2011-04-02 14:22:00 and 2011-04-02 14:22:00. The events included records with estimated wind gusts of 34.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A mid-level trough of low pressure provided enough instability for scattered showers and thunderstorms on the 2nd. Showers and thunderstorms that developed were able to mix down gusty winds from aloft.\nEvent Narrative: A wind gust in excess of 30 knots was reported at Greenberry Point.", "The following events were reported: Thunderstorm Wind, Tornado. These occurred near station USW00093721, approximately 25.6309 km away, between 2011-04-05 03:55:00 and 2011-04-05 04:08:00.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 4000.0 and crop damage of 0.0. \n\nEpisode Narrative: A strong cold front slowly traced through the area during the morning hours of the 5th. A southerly flow ahead of the front caused copious amounts of moisture to move into the region from the Atlantic Ocean and Gulf of Mexico. The deep moisture combined with a mid-level trough that was associated with the cold front to produce moderate amounts of instability. Lift from the cold front along with moderate instability triggered showers and thunderstorms across the area. ||Thunderstorms were able to mix down strong winds from aloft causing damaging wind gusts. Wind speeds that changed rapidly in speed and direction with height caused the stronger storms to produce isolated tornadoes. A strong cold front slowly traced through the area during the morning hours of the 5th. A southerly flow ahead of the front caused copious amounts of moisture to move into the region from the Atlantic Ocean and Gulf of Mexico. The deep moisture combined with a mid-level trough that was associated with the cold front to produce moderate amounts of instability. Lift from the cold front along with moderate instability triggered showers and thunderstorms across the area. ||Thunderstorms were able to mix down strong winds from aloft causing damaging wind gusts. Wind speeds that changed rapidly in speed and direction with height caused the stronger storms to produce isolated tornadoes. A strong cold front slowly traced through the area during the morning hours of the 5th. A southerly flow ahead of the front caused copious amounts of moisture to move into the region from the Atlantic Ocean and Gulf of Mexico. The deep moisture combined with a mid-level trough that was associated with the cold front to produce moderate amounts of instability. Lift from the cold front along with moderate instability triggered showers and thunderstorms across the area. ||Thunderstorms were able to mix down strong winds from aloft causing damaging wind gusts. Wind speeds that changed rapidly in speed and direction with height caused the stronger storms to produce isolated tornadoes.\nEvent Narrative: A wind gust of 65 mph was estimated by a trained spotter. Several pine trees were topped fifteen feet up just south of the Patuxent Preserve. Several pine trees were blown over in the Sherwood Manor area. The tornado continued into Anne Arundel County.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 26.2047 km away, between 2011-04-05 08:00:00 and 2011-04-05 09:11:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A strong cold front slowly traced through the area during the morning hours of the 5th. A southerly flow ahead of the front caused copious amounts of moisture to move into the region from the Atlantic Ocean and Gulf of Mexico. The deep moisture combined with a mid-level trough that was associated with the cold front to produce moderate amounts of instability. Lift from the cold front along with moderate instability triggered showers and thunderstorms across the waters. ||Thunderstorms were able to mix down gusty winds from aloft. A strong cold front slowly traced through the area during the morning hours of the 5th. A southerly flow ahead of the front caused copious amounts of moisture to move into the region from the Atlantic Ocean and Gulf of Mexico. The deep moisture combined with a mid-level trough that was associated with the cold front to produce moderate amounts of instability. Lift from the cold front along with moderate instability triggered showers and thunderstorms across the waters. ||Thunderstorms were able to mix down gusty winds from aloft. A strong cold front slowly traced through the area during the morning hours of the 5th. A southerly flow ahead of the front caused copious amounts of moisture to move into the region from the Atlantic Ocean and Gulf of Mexico. The deep moisture combined with a mid-level trough that was associated with the cold front to produce moderate amounts of instability. Lift from the cold front along with moderate instability triggered showers and thunderstorms across the waters. ||Thunderstorms were able to mix down gusty winds from aloft. A strong cold front slowly traced through the area during the morning hours of the 5th. A southerly flow ahead of the front caused copious amounts of moisture to move into the region from the Atlantic Ocean and Gulf of Mexico. The deep moisture combined with a mid-level trough that was associated with the cold front to produce moderate amounts of instability. Lift from the cold front along with moderate instability triggered showers and thunderstorms across the waters. ||Thunderstorms were able to mix down gusty winds from aloft. A strong cold front slowly traced through the area during the morning hours of the 5th. A southerly flow ahead of the front caused copious amounts of moisture to move into the region from the Atlantic Ocean and Gulf of Mexico. The deep moisture combined with a mid-level trough that was associated with the cold front to produce moderate amounts of instability. Lift from the cold front along with moderate instability triggered showers and thunderstorms across the waters. ||Thunderstorms were able to mix down gusty winds from aloft. A strong cold front slowly traced through the area during the morning hours of the 5th. A southerly flow ahead of the front caused copious amounts of moisture to move into the region from the Atlantic Ocean and Gulf of Mexico. The deep moisture combined with a mid-level trough that was associated with the cold front to produce moderate amounts of instability. Lift from the cold front along with moderate instability triggered showers and thunderstorms across the waters. ||Thunderstorms were able to mix down gusty winds from aloft. A strong cold front slowly traced through the area during the morning hours of the 5th. A southerly flow ahead of the front caused copious amounts of moisture to move into the region from the Atlantic Ocean and Gulf of Mexico. The deep moisture combined with a mid-level trough that was associated with the cold front to produce moderate amounts of instability. Lift from the cold front along with moderate instability triggered showers and thunderstorms across the waters. ||Thunderstorms were able to mix down gusty winds from aloft. A strong cold front slowly traced through the area during the morning hours of the 5th. A southerly flow ahead of the front caused copious amounts of moisture to move into the region from the Atlantic Ocean and Gulf of Mexico. The deep moisture combined with a mid-level trough that was associated with the cold front to produce moderate amounts of instability. Lift from the cold front along with moderate instability triggered showers and thunderstorms across the waters. ||Thunderstorms were able to mix down gusty winds from aloft. A strong cold front slowly traced through the area during the morning hours of the 5th. A southerly flow ahead of the front caused copious amounts of moisture to move into the region from the Atlantic Ocean and Gulf of Mexico. The deep moisture combined with a mid-level trough that was associated with the cold front to produce moderate amounts of instability. Lift from the cold front along with moderate instability triggered showers and thunderstorms across the waters. ||Thunderstorms were able to mix down gusty winds from aloft. A strong cold front slowly traced through the area during the morning hours of the 5th. A southerly flow ahead of the front caused copious amounts of moisture to move into the region from the Atlantic Ocean and Gulf of Mexico. The deep moisture combined with a mid-level trough that was associated with the cold front to produce moderate amounts of instability. Lift from the cold front along with moderate instability triggered showers and thunderstorms across the waters. ||Thunderstorms were able to mix down gusty winds from aloft.\nEvent Narrative: Wind gusts between 37 and 38 knots were reported at Miller Island. A wind gust of 41 knots was measured at the Thomas Point Lighthouse. A wind gust of 36 knots was measured at Greenberry Point. A wind gust of 34 knots was reported at Greenberry Point. Wind gust between 36 and 37 knots were reported at the Francis Scott Key Bridge. Wind gusts up to 39 knots were reported at Tide Point. A wind gust of 37 knots was reported at Orioles Park. Wind gusts in excess of 30 knots was reported at the Maryland Science Center. A wind gust of 34 knot was measured at the Deerfield Elementary School. A wind gust in excess of 30 knots was measured at Tolchester Beach.", "The following events were reported: Thunderstorm Wind, Tornado. These occurred near station USW00093721, approximately 45.5785 km away, between 2011-04-16 16:40:00 and 2011-04-16 19:03:00.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 33000.0 and crop damage of 0.0. \n\nEpisode Narrative: Strong low pressure over the Midwest remained cutoff from the jet stream on the 16th. The warm front associated with this system passed through during the morning. Warm and moist southerly winds behind the front provided moderate amounts of instability. The instability combined with forcing from the low for showers and thunderstorms to develop. ||There was enough instability along with strong winds aloft for some thunderstorms to become severe. Strong low pressure over the Midwest remained cutoff from the jet stream on the 16th. The warm front associated with this system passed through during the morning. Warm and moist southerly winds behind the front provided moderate amounts of instability. The instability combined with forcing from the low for showers and thunderstorms to develop. ||There was enough instability along with strong winds aloft for some thunderstorms to become severe. Strong low pressure over the Midwest remained cutoff from the jet stream on the 16th. The warm front associated with this system passed through during the morning. Warm and moist southerly winds behind the front provided moderate amounts of instability. The instability combined with forcing from the low for showers and thunderstorms to develop. ||There was enough instability along with strong winds aloft for some thunderstorms to become severe. Strong low pressure over the Midwest remained cutoff from the jet stream on the 16th. The warm front associated with this system passed through during the morning. Warm and moist southerly winds behind the front provided moderate amounts of instability. The instability combined with forcing from the low for showers and thunderstorms to develop. ||There was enough instability along with strong winds aloft for some thunderstorms to become severe. Strong low pressure over the Midwest remained cutoff from the jet stream on the 16th. The warm front associated with this system passed through during the morning. Warm and moist southerly winds behind the front provided moderate amounts of instability. The instability combined with forcing from the low for showers and thunderstorms to develop. ||There was enough instability along with strong winds aloft for some thunderstorms to become severe. Strong low pressure over the Midwest remained cutoff from the jet stream on the 16th. The warm front associated with this system passed through during the morning. Warm and moist southerly winds behind the front provided moderate amounts of instability. The instability combined with forcing from the low for showers and thunderstorms to develop. ||There was enough instability along with strong winds aloft for some thunderstorms to become severe.\nEvent Narrative: A tree was down near Route 140. A few trees were toppled along Benrose Lane. Large branches that were about three to four inches in diameter were brought down from thunderstorms winds near Carrollton. Several small branches were brought down from thunderstorm winds. Tree damage was found near the intersection of MD-26 and MD-27. A power pole was also snapped near the intersection. Substantial tree damage was noted near Talbot Run road. Pine trees were snapped near Buffalo Road and there was also a report of siding and trim torn from a home near Buffalo Road.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 33.5077 km away, between 2011-04-16 18:00:00 and 2011-04-16 18:12:00. The events included records with measured wind gusts of 51.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Strong low pressure over the Midwest remained cutoff from the jet stream on the 16th. The warm front associated with this system passed through during the morning. Warm and moist southerly winds behind the front provided moderate amounts of instability. The instability combined with forcing from the low for showers and thunderstorms to develop. ||There was enough instability for thunderstorms to mix down gusty winds from aloft. Strong low pressure over the Midwest remained cutoff from the jet stream on the 16th. The warm front associated with this system passed through during the morning. Warm and moist southerly winds behind the front provided moderate amounts of instability. The instability combined with forcing from the low for showers and thunderstorms to develop. ||There was enough instability for thunderstorms to mix down gusty winds from aloft.\nEvent Narrative: A wind gust of 52 knots was reported at the Thomas Point Lighthouse. A wind gust of 50 knots was reported at Greenberry Point.", "The following events were reported: Flood. These occurred near station USW00093721, approximately 24.8349 km away, between 2011-04-17 13:30:00 and 2011-04-17 20:30:00. The flood was caused by Heavy Rain. Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A strong and closed low pressure system over the Ohio Valley remained nearly stationary through the 16th, bringing copious moisture northward up the eastern seaboard. Lift to produce showers and thunderstorms was focused along a warm front that passed north through the mid-Atlantic during the morning. With ground already saturated from several rounds of significant rainfall in the past week, flooding and flash flooding resulted. Rainfall amounts exceeded 4 inches along the Blue Ridge Mountains.\nEvent Narrative: High water rescue was performed for 3 people on a flooded roadway.", "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00093721, approximately 14.951 km away, between 2011-04-24 15:30:00 and 2011-04-24 18:55:00. The events included records with hailstones measuring 45.44444444444444 inches.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 3000.0 and crop damage of 0.0. \n\nEpisode Narrative: A southerly flow around high pressure over the Atlantic Ocean provided a warm and moist airmass across the region. A pressure trough combined with the warm and moist conditions to trigger showers and thunderstorms. There was enough instability for some thunderstorms to produce damaging winds and large hail. A southerly flow around high pressure over the Atlantic Ocean provided a warm and moist airmass across the region. A pressure trough combined with the warm and moist conditions to trigger showers and thunderstorms. There was enough instability for some thunderstorms to produce damaging winds and large hail. A southerly flow around high pressure over the Atlantic Ocean provided a warm and moist airmass across the region. A pressure trough combined with the warm and moist conditions to trigger showers and thunderstorms. There was enough instability for some thunderstorms to produce damaging winds and large hail. A southerly flow around high pressure over the Atlantic Ocean provided a warm and moist airmass across the region. A pressure trough combined with the warm and moist conditions to trigger showers and thunderstorms. There was enough instability for some thunderstorms to produce damaging winds and large hail. A southerly flow around high pressure over the Atlantic Ocean provided a warm and moist airmass across the region. A pressure trough combined with the warm and moist conditions to trigger showers and thunderstorms. There was enough instability for some thunderstorms to produce damaging winds and large hail. A southerly flow around high pressure over the Atlantic Ocean provided a warm and moist airmass across the region. A pressure trough combined with the warm and moist conditions to trigger showers and thunderstorms. There was enough instability for some thunderstorms to produce damaging winds and large hail. A southerly flow around high pressure over the Atlantic Ocean provided a warm and moist airmass across the region. A pressure trough combined with the warm and moist conditions to trigger showers and thunderstorms. There was enough instability for some thunderstorms to produce damaging winds and large hail. A southerly flow around high pressure over the Atlantic Ocean provided a warm and moist airmass across the region. A pressure trough combined with the warm and moist conditions to trigger showers and thunderstorms. There was enough instability for some thunderstorms to produce damaging winds and large hail. A southerly flow around high pressure over the Atlantic Ocean provided a warm and moist airmass across the region. A pressure trough combined with the warm and moist conditions to trigger showers and thunderstorms. There was enough instability for some thunderstorms to produce damaging winds and large hail.\nEvent Narrative: A tree was down near Elk Ridge. Small limbs were down through the area. Hail up to the size of quarters was reported near Crofton. Small limbs were down at the intersection of Damascus Road and Route 97. A tree was down at Harpers Farm Road and Clarksville Pike. A tree was down at the intersection of Folly Quarter Road and Homewood Road. A tree was down at Silver Trumpet Drive and Tamar Drive. A wind gust of 58 mph was reported near Elkridge. A wind gust of 58 mph was reported near Elkridge.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 20.9956 km away, between 2011-04-24 16:00:00 and 2011-04-24 20:10:00. The events included records with measured wind gusts of 37.5 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A southerly flow around high pressure over the Atlantic Ocean provided a warm and moist airmass across the region. A pressure trough combined with the warm and moist conditions to trigger showers and thunderstorms. There was enough instability for some thunderstorms to produce gusty winds across the waters. A southerly flow around high pressure over the Atlantic Ocean provided a warm and moist airmass across the region. A pressure trough combined with the warm and moist conditions to trigger showers and thunderstorms. There was enough instability for some thunderstorms to produce gusty winds across the waters.\nEvent Narrative: A wind gust of 34 knots was measured at Tide Point. A wind gust of 41 knots was reported at the Annapolis Buoy.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 36.9916 km away, between 2011-04-27 16:00:00 and 2011-04-27 19:00:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: High pressure remained over the western Atlantic while a strong cold front slowly tracked through the Midwest. A southerly flow pumped in copious amounts of moisture from the Atlantic and Gulf of Mexico. The trough of low pressure associated with the cold front provided enough cold air aloft for moderate instability to develop. The instability combined with an upper-level disturbance rotating around the trough to trigger showers and thunderstorms. ||There was enough instability along with stronger winds aloft for some thunderstorms to produce gusty winds. High pressure remained over the western Atlantic while a strong cold front slowly tracked through the Midwest. A southerly flow pumped in copious amounts of moisture from the Atlantic and Gulf of Mexico. The trough of low pressure associated with the cold front provided enough cold air aloft for moderate instability to develop. The instability combined with an upper-level disturbance rotating around the trough to trigger showers and thunderstorms. ||There was enough instability along with stronger winds aloft for some thunderstorms to produce gusty winds.\nEvent Narrative: A wind gust of 35 knots was reported at the Thomas Point Lighthouse. A wind gust in excess of 30 knots was reported at the Thomas Point Lighthouse.", "The following events were reported: Thunderstorm Wind, Tornado. These occurred near station USW00093721, approximately 41.7055 km away, between 2011-04-28 08:54:00 and 2011-04-28 10:25:00.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 1500.0 and crop damage of 0.0. \n\nEpisode Narrative: A strong cold front slowly passed through the region during the morning and early afternoon hours of the 28th. A southerly flow ahead of the front caused deep moisture over the area. The deep moisture combined with a mid-level trough to produce moderate amounts of instability. The cold front combined with the instability to trigger showers and thunderstorms. Some thunderstorms were able to mix down strong winds from aloft. ||Low level wind speed and direction changed rapidly with height causing tornadoes to develop in some of the stronger thunderstorms. A strong cold front slowly passed through the region during the morning and early afternoon hours of the 28th. A southerly flow ahead of the front caused deep moisture over the area. The deep moisture combined with a mid-level trough to produce moderate amounts of instability. The cold front combined with the instability to trigger showers and thunderstorms. Some thunderstorms were able to mix down strong winds from aloft. ||Low level wind speed and direction changed rapidly with height causing tornadoes to develop in some of the stronger thunderstorms.\nEvent Narrative: A large hardwood limb was snapped near Rhode River. An aerial survey conducted by Baltimore county showed that a tornado touched down briefly just north of Evna Road in a heavily wooded area. The tornado snapped and uprooted about two dozen trees and down large branches.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 36.1526 km away, between 2011-04-28 10:25:00 and 2011-04-28 10:25:00. The events included records with estimated wind gusts of 52.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A strong cold front slowly passed through the waters during the morning and early afternoon hours of the 28th. A southerly flow ahead of the front caused deep moisture over the area. The deep moisture combined with a mid-level trough to produce moderate amounts of instability. The cold front combined with the instability to trigger showers and thunderstorms. Some thunderstorms were able to mix down gusty winds from aloft.\nEvent Narrative: A thunderstorm wind gust was estimated to be around 60 mph based on thunderstorm wind damage near Rhode River.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 33.2485 km away, between 2011-05-04 17:50:00 and 2011-05-04 18:06:00. The events included records with estimated wind gusts of 34.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front passed through the waters during the morning hours of the 4th. Showers and thunderstorms developed along and ahead of the front. Thunderstorms were able to mix down gusty winds from aloft across portions of the waters. A cold front passed through the waters during the morning hours of the 4th. Showers and thunderstorms developed along and ahead of the front. Thunderstorms were able to mix down gusty winds from aloft across portions of the waters.\nEvent Narrative: A wind gust in excess of 30 knots was reported at Miller Island. Wind gusts in excess of 30 knots were reported at Tolchester Beach.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 21.7333 km away, between 2011-05-06 19:00:00 and 2011-05-06 20:00:00. The events included records with estimated wind gusts of 34.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A mid-level trough of low pressure passed through the waters during the afternoon and evening hours of the 6th. Showers and thunderstorms developed ahead of the trough axis. There was enough instability ahead of the trough axis for some thunderstorms to mix down gusty winds. A mid-level trough of low pressure passed through the waters during the afternoon and evening hours of the 6th. Showers and thunderstorms developed ahead of the trough axis. There was enough instability ahead of the trough axis for some thunderstorms to mix down gusty winds. A mid-level trough of low pressure passed through the waters during the afternoon and evening hours of the 6th. Showers and thunderstorms developed ahead of the trough axis. There was enough instability ahead of the trough axis for some thunderstorms to mix down gusty winds.\nEvent Narrative: Wind gusts over 30 knots were reported at Tide Point. A wind gust in excess of 30 knots was reported at Key Bridge. A wind gust in excess of 30 knots was reported at Thomas Point Lighthouse.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 26.3275 km away, between 2011-05-15 18:40:00 and 2011-05-15 18:40:00. The events included records with measured wind gusts of 39.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Upper-level low pressure was over the waters on the 15th. Limited instability developed due to colder air aloft associated with the upper-level low. There was enough instability for an isolated thunderstorm to produce gusty winds.\nEvent Narrative: A wind gust of 39 knots was reported at the Annapolis Buoy.", "The following events were reported: Flood. These occurred near station USW00093721, approximately 36.8118 km away, between 2011-05-16 17:00:00 and 2011-05-16 19:00:00. The flood was caused by Heavy Rain. Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A nearly stationary area of low pressure over the Ohio Valley produced several days of intermittent showers and thunderstorms across the mid-Atlantic leading up to May 16th. On the afternoon and evening of May 16, creeks and streams rose high enough to flood a highway in Baltimore County.\nEvent Narrative: Eastbound lanes of Route 40 near Jones Road in the White Marsh area was closed due to flooding.", "The following events were reported: Hail. These occurred near station USW00093721, approximately 32.6397 km away, between 2011-05-24 15:49:00 and 2011-05-24 15:49:00. The events included records with hailstones measuring 1.0 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A surface trough combined with moderate amounts of instability to trigger showers and thunderstorms during the 24th. A few thunderstorm did produce large hail due to the moderate amounts of instability. A surface trough combined with moderate amounts of instability to trigger showers and thunderstorms during the 24th. A few thunderstorm did produce large hail due to the moderate amounts of instability.\nEvent Narrative: Quarter sized hail was reported at Glenwood. Quarter sized hail was reported at Glenwood.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 27.7809 km away, between 2011-05-27 19:50:00 and 2011-05-27 19:50:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 1000.0 and crop damage of 0.0. \n\nEpisode Narrative: A warm and moist airmass remained over the region during the 27th. A surface trough provided the lifting mechanism for more showers and thunderstorms to develop. Copious amounts of instability caused some thunderstorms to become severe.\nEvent Narrative: A tree was down blocking the roadway near the intersection of Reisterstown Road and St. Thomas lane.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 28.0977 km away, between 2011-06-01 18:10:00 and 2011-06-01 18:10:00. The events included records with measured wind gusts of 34.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front passed through the waters on the first. Warm and humid conditions ahead of the front allowed moderate amounts of instability to develop. The instability combined with forcing from the front to trigger showers and thunderstorms. Some thunderstorms were able to produce gusty winds and large hail.\nEvent Narrative: A wind gust of 34 knots was reported at the Annapolis Buoy.", "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00093721, approximately 18.5672 km away, between 2011-06-09 19:15:00 and 2011-06-09 22:45:00. The events included records with hailstones measuring 47.90909090909091 inches.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 16500.0 and crop damage of 0.0. \n\nEpisode Narrative: Plenty of moisture continued to rotate around high pressure over the southeastern Conus. Hot conditions combined with the moisture to cause moderate amounts of instability to develop. The instability combined with forcing from a surface trough to trigger showers and thunderstorms during the afternoon and evening hours. The moderate instability caused some thunderstorms to produce damaging wind gusts and large hail. Plenty of moisture continued to rotate around high pressure over the southeastern Conus. Hot conditions combined with the moisture to cause moderate amounts of instability to develop. The instability combined with forcing from a surface trough to trigger showers and thunderstorms during the afternoon and evening hours. The moderate instability caused some thunderstorms to produce damaging wind gusts and large hail. Plenty of moisture continued to rotate around high pressure over the southeastern Conus. Hot conditions combined with the moisture to cause moderate amounts of instability to develop. The instability combined with forcing from a surface trough to trigger showers and thunderstorms during the afternoon and evening hours. The moderate instability caused some thunderstorms to produce damaging wind gusts and large hail. Plenty of moisture continued to rotate around high pressure over the southeastern Conus. Hot conditions combined with the moisture to cause moderate amounts of instability to develop. The instability combined with forcing from a surface trough to trigger showers and thunderstorms during the afternoon and evening hours. The moderate instability caused some thunderstorms to produce damaging wind gusts and large hail. Plenty of moisture continued to rotate around high pressure over the southeastern Conus. Hot conditions combined with the moisture to cause moderate amounts of instability to develop. The instability combined with forcing from a surface trough to trigger showers and thunderstorms during the afternoon and evening hours. The moderate instability caused some thunderstorms to produce damaging wind gusts and large hail. Plenty of moisture continued to rotate around high pressure over the southeastern Conus. Hot conditions combined with the moisture to cause moderate amounts of instability to develop. The instability combined with forcing from a surface trough to trigger showers and thunderstorms during the afternoon and evening hours. The moderate instability caused some thunderstorms to produce damaging wind gusts and large hail. Plenty of moisture continued to rotate around high pressure over the southeastern Conus. Hot conditions combined with the moisture to cause moderate amounts of instability to develop. The instability combined with forcing from a surface trough to trigger showers and thunderstorms during the afternoon and evening hours. The moderate instability caused some thunderstorms to produce damaging wind gusts and large hail. Plenty of moisture continued to rotate around high pressure over the southeastern Conus. Hot conditions combined with the moisture to cause moderate amounts of instability to develop. The instability combined with forcing from a surface trough to trigger showers and thunderstorms during the afternoon and evening hours. The moderate instability caused some thunderstorms to produce damaging wind gusts and large hail. Plenty of moisture continued to rotate around high pressure over the southeastern Conus. Hot conditions combined with the moisture to cause moderate amounts of instability to develop. The instability combined with forcing from a surface trough to trigger showers and thunderstorms during the afternoon and evening hours. The moderate instability caused some thunderstorms to produce damaging wind gusts and large hail. Plenty of moisture continued to rotate around high pressure over the southeastern Conus. Hot conditions combined with the moisture to cause moderate amounts of instability to develop. The instability combined with forcing from a surface trough to trigger showers and thunderstorms during the afternoon and evening hours. The moderate instability caused some thunderstorms to produce damaging wind gusts and large hail. Plenty of moisture continued to rotate around high pressure over the southeastern Conus. Hot conditions combined with the moisture to cause moderate amounts of instability to develop. The instability combined with forcing from a surface trough to trigger showers and thunderstorms during the afternoon and evening hours. The moderate instability caused some thunderstorms to produce damaging wind gusts and large hail.\nEvent Narrative: Large tree limbs were down along Walker Avenue. Large trees were down on North Charles Street. Three limbs and a tree were blown over near Park Heights. A wind gust of 62 mph was measured near South River. Quarter sized hail was reported near Oakland. Small trees were down along Old Washington Road and Augustine Avenue. Trees were down along the intersection of Nursery Road and Route 295. A small tree was down on Highland Road. Several trees and large limbs were down between Walton and Church Streets. A wind gust of 60 mph was measured near Dundalk. A few large limbs were down near Oakland.", "The following events were reported: Marine Hail, Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 27.8941 km away, between 2011-06-09 19:24:00 and 2011-06-10 00:31:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Plenty of moisture continued to rotate around high pressure over the southeastern Conus. Hot conditions combined with the moisture to cause moderate amounts of instability to develop. The instability combined with forcing from a surface trough to trigger showers and thunderstorms during the afternoon and evening hours. The moderate instability caused some thunderstorms to produce gusty winds and large hail. Plenty of moisture continued to rotate around high pressure over the southeastern Conus. Hot conditions combined with the moisture to cause moderate amounts of instability to develop. The instability combined with forcing from a surface trough to trigger showers and thunderstorms during the afternoon and evening hours. The moderate instability caused some thunderstorms to produce gusty winds and large hail. Plenty of moisture continued to rotate around high pressure over the southeastern Conus. Hot conditions combined with the moisture to cause moderate amounts of instability to develop. The instability combined with forcing from a surface trough to trigger showers and thunderstorms during the afternoon and evening hours. The moderate instability caused some thunderstorms to produce gusty winds and large hail. Plenty of moisture continued to rotate around high pressure over the southeastern Conus. Hot conditions combined with the moisture to cause moderate amounts of instability to develop. The instability combined with forcing from a surface trough to trigger showers and thunderstorms during the afternoon and evening hours. The moderate instability caused some thunderstorms to produce gusty winds and large hail. Plenty of moisture continued to rotate around high pressure over the southeastern Conus. Hot conditions combined with the moisture to cause moderate amounts of instability to develop. The instability combined with forcing from a surface trough to trigger showers and thunderstorms during the afternoon and evening hours. The moderate instability caused some thunderstorms to produce gusty winds and large hail. Plenty of moisture continued to rotate around high pressure over the southeastern Conus. Hot conditions combined with the moisture to cause moderate amounts of instability to develop. The instability combined with forcing from a surface trough to trigger showers and thunderstorms during the afternoon and evening hours. The moderate instability caused some thunderstorms to produce gusty winds and large hail. Plenty of moisture continued to rotate around high pressure over the southeastern Conus. Hot conditions combined with the moisture to cause moderate amounts of instability to develop. The instability combined with forcing from a surface trough to trigger showers and thunderstorms during the afternoon and evening hours. The moderate instability caused some thunderstorms to produce gusty winds and large hail. Plenty of moisture continued to rotate around high pressure over the southeastern Conus. Hot conditions combined with the moisture to cause moderate amounts of instability to develop. The instability combined with forcing from a surface trough to trigger showers and thunderstorms during the afternoon and evening hours. The moderate instability caused some thunderstorms to produce gusty winds and large hail. Plenty of moisture continued to rotate around high pressure over the southeastern Conus. Hot conditions combined with the moisture to cause moderate amounts of instability to develop. The instability combined with forcing from a surface trough to trigger showers and thunderstorms during the afternoon and evening hours. The moderate instability caused some thunderstorms to produce gusty winds and large hail. Plenty of moisture continued to rotate around high pressure over the southeastern Conus. Hot conditions combined with the moisture to cause moderate amounts of instability to develop. The instability combined with forcing from a surface trough to trigger showers and thunderstorms during the afternoon and evening hours. The moderate instability caused some thunderstorms to produce gusty winds and large hail. Plenty of moisture continued to rotate around high pressure over the southeastern Conus. Hot conditions combined with the moisture to cause moderate amounts of instability to develop. The instability combined with forcing from a surface trough to trigger showers and thunderstorms during the afternoon and evening hours. The moderate instability caused some thunderstorms to produce gusty winds and large hail. Plenty of moisture continued to rotate around high pressure over the southeastern Conus. Hot conditions combined with the moisture to cause moderate amounts of instability to develop. The instability combined with forcing from a surface trough to trigger showers and thunderstorms during the afternoon and evening hours. The moderate instability caused some thunderstorms to produce gusty winds and large hail. Plenty of moisture continued to rotate around high pressure over the southeastern Conus. Hot conditions combined with the moisture to cause moderate amounts of instability to develop. The instability combined with forcing from a surface trough to trigger showers and thunderstorms during the afternoon and evening hours. The moderate instability caused some thunderstorms to produce gusty winds and large hail.\nEvent Narrative: A wind gust of 34 knots was measured at Key Bridge. A wind gust in excess of 30 knots was reported at the Annapolis Buoy. A wind gust in excess of 30 knots was reported at Tolly Point. A wind gust of 38 knots was reported at Tolly Point. Nickel sized hail was reported near Highland Beach. A wind gust in excess of 30 knots was reported at the Federal Hill Elementary School. A wind gust in excess of 30 knots was reported at the Hampstead Elementary School. Wind gusts up to 42 knots were measured at Miller Island. Wind gust up to 56 knots were reported at Tolchester Beach. Wind gusts up to 40 knots were reported at Stevensville. Wind gusts in excess of 30 knots were reported at Sandy Point. Wind gusts were estimated to be around 60 mph. A wind gust of 44 knots was reported at Thomas Point Lighthouse.", "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00093721, approximately 38.7083 km away, between 2011-06-09 20:00:00 and 2011-06-09 23:05:00. The events included records with hailstones measuring 36.6 inches.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 25000.0 and crop damage of 0.0. \n\nEpisode Narrative: The combination of an unseasonably hot and humid air mass and an approaching cold front helped trigger scattered strong to severe thunderstorms that moved across the Maryland Eastern Shore during the evening and overnight of the 9th. The combination of an unseasonably hot and humid air mass and an approaching cold front helped trigger scattered strong to severe thunderstorms that moved across the Maryland Eastern Shore during the evening and overnight of the 9th. The combination of an unseasonably hot and humid air mass and an approaching cold front helped trigger scattered strong to severe thunderstorms that moved across the Maryland Eastern Shore during the evening and overnight of the 9th.\nEvent Narrative: A severe thunderstorm knocked down numerous trees across central Kent Island from Matapeake east through Stevensville. Around Matapeake, a house under reconstruction was damaged and some poles were also snapped. Hail slightly larger than golf balls fell from a severe thunderstorm on Kent Island. A severe thunderstorm knocked down a couple of trees in Tolchester.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 32.5446 km away, between 2011-06-10 00:00:00 and 2011-06-10 01:30:00. The events included records with measured wind gusts of 38.5 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A surface trough combined with moderate amounts of instability to trigger showers and thunderstorms over the waters. A few thunderstorms were able to produce gusty winds. A surface trough combined with moderate amounts of instability to trigger showers and thunderstorms over the waters. A few thunderstorms were able to produce gusty winds.\nEvent Narrative: A wind gust of 38 knots was reported at Thomas Point Lighthouse. Wind gusts up to 39 knots were reported at the Annapolis Buoy.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 17.2674 km away, between 2011-06-12 16:03:00 and 2011-06-12 16:12:00. The events included records with estimated wind gusts of 52.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 10000.0 and crop damage of 0.0. \n\nEpisode Narrative: A cold front combined with moderate instability to trigger showers and thunderstorms on the twelfth. Stronger winds aloft due to an upper-level low over New England caused thunderstorms to become well organized. Thunderstorms were able to produce damaging wind gusts along wit large hail. A cold front combined with moderate instability to trigger showers and thunderstorms on the twelfth. Stronger winds aloft due to an upper-level low over New England caused thunderstorms to become well organized. Thunderstorms were able to produce damaging wind gusts along wit large hail.\nEvent Narrative: Multiple trees were down in northern parts of Baltimore. Trees were down in the eastern parts of Baltimore.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 23.144 km away, between 2011-06-12 16:12:00 and 2011-06-12 18:00:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front combined with moderate instability to trigger showers and thunderstorms on the twelfth. Stronger winds aloft due to an upper-level low over New England caused thunderstorms to become well organized. Thunderstorms were able to produce gusty winds over the waters. A cold front combined with moderate instability to trigger showers and thunderstorms on the twelfth. Stronger winds aloft due to an upper-level low over New England caused thunderstorms to become well organized. Thunderstorms were able to produce gusty winds over the waters. A cold front combined with moderate instability to trigger showers and thunderstorms on the twelfth. Stronger winds aloft due to an upper-level low over New England caused thunderstorms to become well organized. Thunderstorms were able to produce gusty winds over the waters. A cold front combined with moderate instability to trigger showers and thunderstorms on the twelfth. Stronger winds aloft due to an upper-level low over New England caused thunderstorms to become well organized. Thunderstorms were able to produce gusty winds over the waters. A cold front combined with moderate instability to trigger showers and thunderstorms on the twelfth. Stronger winds aloft due to an upper-level low over New England caused thunderstorms to become well organized. Thunderstorms were able to produce gusty winds over the waters. A cold front combined with moderate instability to trigger showers and thunderstorms on the twelfth. Stronger winds aloft due to an upper-level low over New England caused thunderstorms to become well organized. Thunderstorms were able to produce gusty winds over the waters. A cold front combined with moderate instability to trigger showers and thunderstorms on the twelfth. Stronger winds aloft due to an upper-level low over New England caused thunderstorms to become well organized. Thunderstorms were able to produce gusty winds over the waters. A cold front combined with moderate instability to trigger showers and thunderstorms on the twelfth. Stronger winds aloft due to an upper-level low over New England caused thunderstorms to become well organized. Thunderstorms were able to produce gusty winds over the waters.\nEvent Narrative: A wind gust of 35 knots was reported at Tide Point. A wind gust of 34 knots was reported at the Baltimore Buoy. A wind gust of 35 knots was measured at the Hampstead Elementary School. A wind gust of 37 knots was reported at Tolly Point. A wind gust of 37 knots was reported at the Annapolis Buoy. A wind gust of 36 knots was reported at the Thomas Point Lighthouse. A wind gust of 34 knots was reported at Miller Island. A wind gust in excess of 30 knots was reported at the Francis Scott Key Bridge.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 28.0977 km away, between 2011-06-17 00:00:00 and 2011-06-17 00:30:00. The events included records with measured wind gusts of 36.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A return flow around high pressure pumped in plenty of warm and moist air over the region. Colder air aloft associated with an upper-level trough combined with the warm and moist air at the surface to develop moderate amounts of instability. A surface trough acted as the lifting mechanism for showers and thunderstorms to develop during the afternoon and evening hours. Thunderstorms were able to produce gusty winds. A return flow around high pressure pumped in plenty of warm and moist air over the region. Colder air aloft associated with an upper-level trough combined with the warm and moist air at the surface to develop moderate amounts of instability. A surface trough acted as the lifting mechanism for showers and thunderstorms to develop during the afternoon and evening hours. Thunderstorms were able to produce gusty winds.\nEvent Narrative: A wind gust of 37 knots was measured at the Annapolis Buoy. A wind gust of 35 knots was measured at the Annapolis Buoy.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 32.5446 km away, between 2011-07-03 03:10:00 and 2011-07-03 19:00:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front passed through the area during the 3rd. A southerly flow ahead of the front caused enough warm and moist air for moderate instability to develop. The combination of lift associated with the front and instability triggered showers and thunderstorms. Some thunderstorms produced gusty winds. A cold front passed through the area during the 3rd. A southerly flow ahead of the front caused enough warm and moist air for moderate instability to develop. The combination of lift associated with the front and instability triggered showers and thunderstorms. Some thunderstorms produced gusty winds.\nEvent Narrative: A wind gust in excess of 30 knots was reported at the Annapolis Buoy. A wind gust of 43 knots was reported at Thomas Point Lighthouse.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 10.5341 km away, between 2011-07-03 17:11:00 and 2011-07-03 17:11:00. The events included records with estimated wind gusts of 61.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 5000.0 and crop damage of 0.0. \n\nEpisode Narrative: A cold front passed through the area during the 3rd. A southerly flow ahead of the front caused enough warm and moist air for moderate instability to develop. The combination of lift associated with the front and instability triggered showers and thunderstorms. Some thunderstorms became severe with damaging winds and large hail.\nEvent Narrative: Many hardwood trees were uprooted and limbs were snapped in thunderstorm winds.", "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00093721, approximately 19.8226 km away, between 2011-07-07 17:10:00 and 2011-07-07 23:13:00. The events included records with hailstones measuring 44.07692307692308 inches.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 220000.0 and crop damage of 0.0. \n\nEpisode Narrative: A mid-level trough of low pressure remained over the area, providing cooler air aloft. A southerly flow around high pressure over the Atlantic ushered in plenty of warm and moist air. the combination of warm and moist air at the surface along with cooler air aloft caused moderate amounts of instability to develop. Some thunderstorms that developed due to the instability were able to cause damaging winds and large hail. A mid-level trough of low pressure remained over the area, providing cooler air aloft. A southerly flow around high pressure over the Atlantic ushered in plenty of warm and moist air. the combination of warm and moist air at the surface along with cooler air aloft caused moderate amounts of instability to develop. Some thunderstorms that developed due to the instability were able to cause damaging winds and large hail. A mid-level trough of low pressure remained over the area, providing cooler air aloft. A southerly flow around high pressure over the Atlantic ushered in plenty of warm and moist air. the combination of warm and moist air at the surface along with cooler air aloft caused moderate amounts of instability to develop. Some thunderstorms that developed due to the instability were able to cause damaging winds and large hail. A mid-level trough of low pressure remained over the area, providing cooler air aloft. A southerly flow around high pressure over the Atlantic ushered in plenty of warm and moist air. the combination of warm and moist air at the surface along with cooler air aloft caused moderate amounts of instability to develop. Some thunderstorms that developed due to the instability were able to cause damaging winds and large hail. A mid-level trough of low pressure remained over the area, providing cooler air aloft. A southerly flow around high pressure over the Atlantic ushered in plenty of warm and moist air. the combination of warm and moist air at the surface along with cooler air aloft caused moderate amounts of instability to develop. Some thunderstorms that developed due to the instability were able to cause damaging winds and large hail. A mid-level trough of low pressure remained over the area, providing cooler air aloft. A southerly flow around high pressure over the Atlantic ushered in plenty of warm and moist air. the combination of warm and moist air at the surface along with cooler air aloft caused moderate amounts of instability to develop. Some thunderstorms that developed due to the instability were able to cause damaging winds and large hail. A mid-level trough of low pressure remained over the area, providing cooler air aloft. A southerly flow around high pressure over the Atlantic ushered in plenty of warm and moist air. the combination of warm and moist air at the surface along with cooler air aloft caused moderate amounts of instability to develop. Some thunderstorms that developed due to the instability were able to cause damaging winds and large hail. A mid-level trough of low pressure remained over the area, providing cooler air aloft. A southerly flow around high pressure over the Atlantic ushered in plenty of warm and moist air. the combination of warm and moist air at the surface along with cooler air aloft caused moderate amounts of instability to develop. Some thunderstorms that developed due to the instability were able to cause damaging winds and large hail. A mid-level trough of low pressure remained over the area, providing cooler air aloft. A southerly flow around high pressure over the Atlantic ushered in plenty of warm and moist air. the combination of warm and moist air at the surface along with cooler air aloft caused moderate amounts of instability to develop. Some thunderstorms that developed due to the instability were able to cause damaging winds and large hail. A mid-level trough of low pressure remained over the area, providing cooler air aloft. A southerly flow around high pressure over the Atlantic ushered in plenty of warm and moist air. the combination of warm and moist air at the surface along with cooler air aloft caused moderate amounts of instability to develop. Some thunderstorms that developed due to the instability were able to cause damaging winds and large hail. A mid-level trough of low pressure remained over the area, providing cooler air aloft. A southerly flow around high pressure over the Atlantic ushered in plenty of warm and moist air. the combination of warm and moist air at the surface along with cooler air aloft caused moderate amounts of instability to develop. Some thunderstorms that developed due to the instability were able to cause damaging winds and large hail. A mid-level trough of low pressure remained over the area, providing cooler air aloft. A southerly flow around high pressure over the Atlantic ushered in plenty of warm and moist air. the combination of warm and moist air at the surface along with cooler air aloft caused moderate amounts of instability to develop. Some thunderstorms that developed due to the instability were able to cause damaging winds and large hail. A mid-level trough of low pressure remained over the area, providing cooler air aloft. A southerly flow around high pressure over the Atlantic ushered in plenty of warm and moist air. the combination of warm and moist air at the surface along with cooler air aloft caused moderate amounts of instability to develop. Some thunderstorms that developed due to the instability were able to cause damaging winds and large hail.\nEvent Narrative: Multiple trees were down due to thunderstorm winds. Quarter sized hail was reported near Dundalk. Quarter sized hail was reported near Dundalk. Six trees between four and ten inches in diameter were down along Merrit Boulevard. Roofs were partially taken off of several units in an Apartment Complex along the intersection of Mornington Road and Meadow Way. Multiple trees that were three to four feet in diameter were blown down. Many limbs were also down. A large tree that was three feet in diameter was knocked down. Roofs were blown off town homes in Catawba Court. Large tree limbs were down along Falls Road. A tree that was one foot in diameter fell onto a house near the intersection of Sollers Point Road and Mornington Road. A tree fell onto wires along the 2300 block of West Joppa Road. Roof damage was reported to apartment buildings. Quarter sized hail was reported near Essex.", "The following events were reported: Flash Flood, Flood. These occurred near station USW00093721, approximately 17.8869 km away, between 2011-07-07 17:20:00 and 2011-07-08 18:00:00. The flood was caused by Heavy Rain. Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A nearly stationary low pressure trough existing in a moist and unstable atmosphere aided in the development of showers and thunderstorms across northern Maryland. Slow storm movement caused flash flooding across the Baltimore metropolitan area as rainfall rates of over 1 inch per hour occurred. Rainfall totals reached as high as 3.10 in Montgomery County. A nearly stationary low pressure trough existing in a moist and unstable atmosphere aided in the development of showers and thunderstorms across northern Maryland. Slow storm movement caused flash flooding across the Baltimore metropolitan area as rainfall rates of over 1 inch per hour occurred. Rainfall totals reached as high as 3.10 in Montgomery County. A nearly stationary low pressure trough existing in a moist and unstable atmosphere aided in the development of showers and thunderstorms across northern Maryland. Slow storm movement caused flash flooding across the Baltimore metropolitan area as rainfall rates of over 1 inch per hour occurred. Rainfall totals reached as high as 3.10 in Montgomery County. A nearly stationary low pressure trough existing in a moist and unstable atmosphere aided in the development of showers and thunderstorms across northern Maryland. Slow storm movement caused flash flooding across the Baltimore metropolitan area as rainfall rates of over 1 inch per hour occurred. Rainfall totals reached as high as 3.10 in Montgomery County. A nearly stationary low pressure trough existing in a moist and unstable atmosphere aided in the development of showers and thunderstorms across northern Maryland. Slow storm movement caused flash flooding across the Baltimore metropolitan area as rainfall rates of over 1 inch per hour occurred. Rainfall totals reached as high as 3.10 in Montgomery County. A nearly stationary low pressure trough existing in a moist and unstable atmosphere aided in the development of showers and thunderstorms across northern Maryland. Slow storm movement caused flash flooding across the Baltimore metropolitan area as rainfall rates of over 1 inch per hour occurred. Rainfall totals reached as high as 3.10 in Montgomery County. A nearly stationary low pressure trough existing in a moist and unstable atmosphere aided in the development of showers and thunderstorms across northern Maryland. Slow storm movement caused flash flooding across the Baltimore metropolitan area as rainfall rates of over 1 inch per hour occurred. Rainfall totals reached as high as 3.10 in Montgomery County. A nearly stationary low pressure trough existing in a moist and unstable atmosphere aided in the development of showers and thunderstorms across northern Maryland. Slow storm movement caused flash flooding across the Baltimore metropolitan area as rainfall rates of over 1 inch per hour occurred. Rainfall totals reached as high as 3.10 in Montgomery County. A nearly stationary low pressure trough existing in a moist and unstable atmosphere aided in the development of showers and thunderstorms across northern Maryland. Slow storm movement caused flash flooding across the Baltimore metropolitan area as rainfall rates of over 1 inch per hour occurred. Rainfall totals reached as high as 3.10 in Montgomery County. A nearly stationary low pressure trough existing in a moist and unstable atmosphere aided in the development of showers and thunderstorms across northern Maryland. Slow storm movement caused flash flooding across the Baltimore metropolitan area as rainfall rates of over 1 inch per hour occurred. Rainfall totals reached as high as 3.10 in Montgomery County. A nearly stationary low pressure trough existing in a moist and unstable atmosphere aided in the development of showers and thunderstorms across northern Maryland. Slow storm movement caused flash flooding across the Baltimore metropolitan area as rainfall rates of over 1 inch per hour occurred. Rainfall totals reached as high as 3.10 in Montgomery County. A nearly stationary low pressure trough existing in a moist and unstable atmosphere aided in the development of showers and thunderstorms across northern Maryland. Slow storm movement caused flash flooding across the Baltimore metropolitan area as rainfall rates of over 1 inch per hour occurred. Rainfall totals reached as high as 3.10 in Montgomery County. A nearly stationary low pressure trough existing in a moist and unstable atmosphere aided in the development of showers and thunderstorms across northern Maryland. Slow storm movement caused flash flooding across the Baltimore metropolitan area as rainfall rates of over 1 inch per hour occurred. Rainfall totals reached as high as 3.10 in Montgomery County. A nearly stationary low pressure trough existing in a moist and unstable atmosphere aided in the development of showers and thunderstorms across northern Maryland. Slow storm movement caused flash flooding across the Baltimore metropolitan area as rainfall rates of over 1 inch per hour occurred. Rainfall totals reached as high as 3.10 in Montgomery County. A nearly stationary low pressure trough existing in a moist and unstable atmosphere aided in the development of showers and thunderstorms across northern Maryland. Slow storm movement caused flash flooding across the Baltimore metropolitan area as rainfall rates of over 1 inch per hour occurred. Rainfall totals reached as high as 3.10 in Montgomery County. A nearly stationary low pressure trough existing in a moist and unstable atmosphere aided in the development of showers and thunderstorms across northern Maryland. Slow storm movement caused flash flooding across the Baltimore metropolitan area as rainfall rates of over 1 inch per hour occurred. Rainfall totals reached as high as 3.10 in Montgomery County. A nearly stationary low pressure trough existing in a moist and unstable atmosphere aided in the development of showers and thunderstorms across northern Maryland. Slow storm movement caused flash flooding across the Baltimore metropolitan area as rainfall rates of over 1 inch per hour occurred. Rainfall totals reached as high as 3.10 in Montgomery County. A nearly stationary low pressure trough existing in a moist and unstable atmosphere aided in the development of showers and thunderstorms across northern Maryland. Slow storm movement caused flash flooding across the Baltimore metropolitan area as rainfall rates of over 1 inch per hour occurred. Rainfall totals reached as high as 3.10 in Montgomery County. A nearly stationary low pressure trough existing in a moist and unstable atmosphere aided in the development of showers and thunderstorms across northern Maryland. Slow storm movement caused flash flooding across the Baltimore metropolitan area as rainfall rates of over 1 inch per hour occurred. Rainfall totals reached as high as 3.10 in Montgomery County. A nearly stationary low pressure trough existing in a moist and unstable atmosphere aided in the development of showers and thunderstorms across northern Maryland. Slow storm movement caused flash flooding across the Baltimore metropolitan area as rainfall rates of over 1 inch per hour occurred. Rainfall totals reached as high as 3.10 in Montgomery County. A nearly stationary low pressure trough existing in a moist and unstable atmosphere aided in the development of showers and thunderstorms across northern Maryland. Slow storm movement caused flash flooding across the Baltimore metropolitan area as rainfall rates of over 1 inch per hour occurred. Rainfall totals reached as high as 3.10 in Montgomery County. A nearly stationary low pressure trough existing in a moist and unstable atmosphere aided in the development of showers and thunderstorms across northern Maryland. Slow storm movement caused flash flooding across the Baltimore metropolitan area as rainfall rates of over 1 inch per hour occurred. Rainfall totals reached as high as 3.10 in Montgomery County. A nearly stationary low pressure trough existing in a moist and unstable atmosphere aided in the development of showers and thunderstorms across northern Maryland. Slow storm movement caused flash flooding across the Baltimore metropolitan area as rainfall rates of over 1 inch per hour occurred. Rainfall totals reached as high as 3.10 in Montgomery County. A nearly stationary low pressure trough existing in a moist and unstable atmosphere aided in the development of showers and thunderstorms across northern Maryland. Slow storm movement caused flash flooding across the Baltimore metropolitan area as rainfall rates of over 1 inch per hour occurred. Rainfall totals reached as high as 3.10 in Montgomery County. A nearly stationary low pressure trough existing in a moist and unstable atmosphere aided in the development of showers and thunderstorms across northern Maryland. Slow storm movement caused flash flooding across the Baltimore metropolitan area as rainfall rates of over 1 inch per hour occurred. Rainfall totals reached as high as 3.10 in Montgomery County. A nearly stationary low pressure trough existing in a moist and unstable atmosphere aided in the development of showers and thunderstorms across northern Maryland. Slow storm movement caused flash flooding across the Baltimore metropolitan area as rainfall rates of over 1 inch per hour occurred. Rainfall totals reached as high as 3.10 in Montgomery County. A nearly stationary low pressure trough existing in a moist and unstable atmosphere aided in the development of showers and thunderstorms across northern Maryland. Slow storm movement caused flash flooding across the Baltimore metropolitan area as rainfall rates of over 1 inch per hour occurred. Rainfall totals reached as high as 3.10 in Montgomery County. A nearly stationary low pressure trough existing in a moist and unstable atmosphere aided in the development of showers and thunderstorms across northern Maryland. Slow storm movement caused flash flooding across the Baltimore metropolitan area as rainfall rates of over 1 inch per hour occurred. Rainfall totals reached as high as 3.10 in Montgomery County. A nearly stationary low pressure trough existing in a moist and unstable atmosphere aided in the development of showers and thunderstorms across northern Maryland. Slow storm movement caused flash flooding across the Baltimore metropolitan area as rainfall rates of over 1 inch per hour occurred. Rainfall totals reached as high as 3.10 in Montgomery County. A nearly stationary low pressure trough existing in a moist and unstable atmosphere aided in the development of showers and thunderstorms across northern Maryland. Slow storm movement caused flash flooding across the Baltimore metropolitan area as rainfall rates of over 1 inch per hour occurred. Rainfall totals reached as high as 3.10 in Montgomery County.\nEvent Narrative: A swift water rescue was performed at the intersection of York Road and Beaver Run Lane. Multiple roadways were reported closed due to flash flooding in and around Cockeysville. Northbound Route 1 was closed between North 2nd Street and Davis due to flash flooding. Water was about 3 feet deep. Rainfall totals near the event measured 2.93 inches. A vehicle was stranded in floodwaters at the intersection of Routes 24 and 40. A nearby rain gage measured 2.20 inches. Mountain Road was closed due to flash flooding at intersection with Tick Neck Road. A nearby rain gage measured 2.80 inches. Up to 6 inches of water was flooding across Eastern Avenue between Wiltshire and Mace Avenues. Rainfall Rates of up to one inch per hour were measured near this location. Route 40 was closed near Stevens Road. Portions of Quarantine Road were flooded. The intersection of North Point Blvd. and Norris Lane was closed due to overflowing creek. A nearby spotter measured 1.72 inches of rain. Intersection of St. Stephens Road and Route 450 were closed due to flash flooding. Mountain Road at Catherine Avenue was flooded by about one foot of standing water. North Point Road was flooded between Kane Street and Quad Avenue. A swift water rescue was performed at the intersection of North Avondale Road and Sellers Point Road. A swift water rescue was performed on Dundalk Avenue. A swift water rescue was performed at the intersection of North Point Road and German Hill Road. A swift water rescue was performed on Dundalk Avenue. The intersection of Fort Smallwood Road and Hawkins Point Road was closed due to flash flooding. A swift water rescue was performed at the intersection of Myrtle and Tulip Avenues. A swift water rescue was performed on Halthorpe Avenue. Intersection of West Patapsco Avenue and Marmenco Court was closed due to flash flooding. Portion of South Hanover Street was closed due to flooding. Waterview Avenue was closed due to flash flooding at its intersection with Interstate 95. Intersection of Aliceanna and Caroline Streets closed due to flash flooding. Washington Blvd. was closed at Interstate 95 due to flash flooding. Intersection of Fleet and South Caroline Streets were closed due to flash flooding. Flooding on Haines Street. Intersection of Washington Blvd and Monroe Street was closed due to flash flooding. Benson Avenue was closed at South Grantley Street due to flash flooding. Flash flooding forced closure of Ashland and York Roads intersection. Several inches of water were covering various sections of Mountain Road. A nearby rain gage measured 0.81 inches.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 13.2462 km away, between 2011-07-07 17:24:00 and 2011-07-07 19:09:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A mid-level trough of low pressure remained over the area, providing cooler air aloft. A southerly flow around high pressure over the Atlantic ushered in plenty of warm and moist air. The combination of warm and moist air at the surface along with cooler air aloft caused moderate amounts of instability to develop. Some thunderstorms that developed due to the instability were able to produce gusty winds. A mid-level trough of low pressure remained over the area, providing cooler air aloft. A southerly flow around high pressure over the Atlantic ushered in plenty of warm and moist air. The combination of warm and moist air at the surface along with cooler air aloft caused moderate amounts of instability to develop. Some thunderstorms that developed due to the instability were able to produce gusty winds. A mid-level trough of low pressure remained over the area, providing cooler air aloft. A southerly flow around high pressure over the Atlantic ushered in plenty of warm and moist air. The combination of warm and moist air at the surface along with cooler air aloft caused moderate amounts of instability to develop. Some thunderstorms that developed due to the instability were able to produce gusty winds. A mid-level trough of low pressure remained over the area, providing cooler air aloft. A southerly flow around high pressure over the Atlantic ushered in plenty of warm and moist air. The combination of warm and moist air at the surface along with cooler air aloft caused moderate amounts of instability to develop. Some thunderstorms that developed due to the instability were able to produce gusty winds. A mid-level trough of low pressure remained over the area, providing cooler air aloft. A southerly flow around high pressure over the Atlantic ushered in plenty of warm and moist air. The combination of warm and moist air at the surface along with cooler air aloft caused moderate amounts of instability to develop. Some thunderstorms that developed due to the instability were able to produce gusty winds.\nEvent Narrative: A wind gust of 35 knots was reported at the Baltimore Buoy. A wind gust around 65 mph was estimated due to thunderstorm wind damage nearby. A wind gust in excess of 30 knots was reported at Orioles Park. A wind gust in excess of 30 knots was reported in Lakeland. Wind gusts up to 59 knots were reported at the Baltimore Key Bridge.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 36.0557 km away, between 2011-07-08 15:31:00 and 2011-07-08 16:00:00. The events included records with measured wind gusts of 35.5 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A surface trough remained over the region during the 8th. Moderate instability ahead of the trough caused thunderstorms to develop. A few thunderstorms produced gusty winds. A surface trough remained over the region during the 8th. Moderate instability ahead of the trough caused thunderstorms to develop. A few thunderstorms produced gusty winds.\nEvent Narrative: A wind gust of 36 knots was reported at Tolly Point. Wind gusts up to 35 knots were reported at Tolchester Beach.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 21.5582 km away, between 2011-07-11 19:17:00 and 2011-07-11 19:55:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 6000.0 and crop damage of 0.0. \n\nEpisode Narrative: An upper-level disturbance passed through the area on the 11th. The atmosphere was very unstable due to a hot and humid air mass in place. The combination of forcing from the upper-level disturbance along with high amounts of instability led to the development of showers and thunderstorms. Thunderstorms produced damaging winds and large hail. An upper-level disturbance passed through the area on the 11th. The atmosphere was very unstable due to a hot and humid air mass in place. The combination of forcing from the upper-level disturbance along with high amounts of instability led to the development of showers and thunderstorms. Thunderstorms produced damaging winds and large hail. An upper-level disturbance passed through the area on the 11th. The atmosphere was very unstable due to a hot and humid air mass in place. The combination of forcing from the upper-level disturbance along with high amounts of instability led to the development of showers and thunderstorms. Thunderstorms produced damaging winds and large hail. An upper-level disturbance passed through the area on the 11th. The atmosphere was very unstable due to a hot and humid air mass in place. The combination of forcing from the upper-level disturbance along with high amounts of instability led to the development of showers and thunderstorms. Thunderstorms produced damaging winds and large hail.\nEvent Narrative: A tree was down at Prestwick Drive and Highland. A tree fell onto power lines on Belgaro Road. Scattered trees were down. A tree fell onto power lines on Graeloch Road.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 28.0977 km away, between 2011-07-11 20:30:00 and 2011-07-11 20:30:00. The events included records with estimated wind gusts of 34.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: An upper-level disturbance passed through the waters on the 11th. The atmosphere was very unstable due to a hot and humid air mass in place. The combination of forcing from the upper-level disturbance along with high amounts of instability led to the development of showers and thunderstorms. Thunderstorms produced gusty winds.\nEvent Narrative: A wind gust in excess of 30 knots was reported at the Annapolis Buoy.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 32.8153 km away, between 2011-07-13 14:49:00 and 2011-07-13 15:00:00. The events included records with estimated wind gusts of 34.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front passed through Maryland on the 13th. Moderate instability ahead of the front combined with the forcing that was associated with the front to trigger showers and thunderstorms. Some thunderstorms were able to mix down gusty winds from aloft. A cold front passed through Maryland on the 13th. Moderate instability ahead of the front combined with the forcing that was associated with the front to trigger showers and thunderstorms. Some thunderstorms were able to mix down gusty winds from aloft.\nEvent Narrative: A wind gust in excess of 30 knots was measured at Thomas Point. A wind gust in excess of 30 knots was measured near Annapolis.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 17.2545 km away, between 2011-07-19 15:15:00 and 2011-07-19 15:15:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front passed through the area on the 19th. A warm and moist air mass ahead of the boundary caused moderate amounts of instability to develop. The instability combined with forcing from the front to trigger showers and thunderstorms. Some thunderstorms produced damaging wind gusts.\nEvent Narrative: A large branch fell across a drive way in Severna Park.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 27.2126 km away, between 2011-07-19 15:15:00 and 2011-07-19 15:30:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front passed through the area on the 19th. A warm and moist air mass ahead of the boundary caused moderate amounts of instability to develop. The instability combined with forcing from the front to trigger showers and thunderstorms. Some thunderstorms produced gusty winds. A cold front passed through the area on the 19th. A warm and moist air mass ahead of the boundary caused moderate amounts of instability to develop. The instability combined with forcing from the front to trigger showers and thunderstorms. Some thunderstorms produced gusty winds.\nEvent Narrative: A wind gust of 45 knots was measured at the Annapolis Buoy. A wind gust in excess of 30 knots was reported at Annapolis.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 24.1833 km away, between 2011-07-25 13:22:00 and 2011-07-25 14:55:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 2000.0 and crop damage of 0.0. \n\nEpisode Narrative: A cold front stalled over the area on the 25th. Showers and thunderstorms developed along and ahead of the front. Moderate instability due to a warm and humid air mass caused some thunderstorms to produce damaging wind gusts. A cold front stalled over the area on the 25th. Showers and thunderstorms developed along and ahead of the front. Moderate instability due to a warm and humid air mass caused some thunderstorms to produce damaging wind gusts. A cold front stalled over the area on the 25th. Showers and thunderstorms developed along and ahead of the front. Moderate instability due to a warm and humid air mass caused some thunderstorms to produce damaging wind gusts.\nEvent Narrative: A tree was knocked down at Bellemore Road. A tree was knocked down on Green Spring road. A couple of tree limbs were down Harwood Road and Sands Road.", "The following events were reported: Flash Flood. These occurred near station USW00093721, approximately 24.8232 km away, between 2011-07-25 13:52:00 and 2011-07-25 16:00:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Showers and thunderstorms developed along a stationary front over Maryland. Very heavy rainfall rates from activity training repeatedly across the same area produced flash flooding in some locations. Up to 3.20 inches of rain was measured in Howard County. Showers and thunderstorms developed along a stationary front over Maryland. Very heavy rainfall rates from activity training repeatedly across the same area produced flash flooding in some locations. Up to 3.20 inches of rain was measured in Howard County. Showers and thunderstorms developed along a stationary front over Maryland. Very heavy rainfall rates from activity training repeatedly across the same area produced flash flooding in some locations. Up to 3.20 inches of rain was measured in Howard County. Showers and thunderstorms developed along a stationary front over Maryland. Very heavy rainfall rates from activity training repeatedly across the same area produced flash flooding in some locations. Up to 3.20 inches of rain was measured in Howard County. Showers and thunderstorms developed along a stationary front over Maryland. Very heavy rainfall rates from activity training repeatedly across the same area produced flash flooding in some locations. Up to 3.20 inches of rain was measured in Howard County.\nEvent Narrative: A car was washed off the road near the intersection of Forsythe Road and West Friendship due to water of several feet depth. A nearby spotter observed 2.98 inches of rain. Areas near intersection of Liberty Road and Marriottsville Road experienced flash flooding. A nearby rain gage measured 1.59 inches. High water forced the closures of Route 424 at Bottner Road and Route 450 at Huntwood Drive. Also, a portion of Governor's Bridge Road was also closed. A nearby rain gage recorded 2.74 inches. Van Dusen Road was closed due to flash flooding on Bear Branch. A nearby rain gage observed 1.95 inches. Road closed near the intersection of Marriottsville Road and Wards Chapel Road due to flash flooding. A nearby rain gage measured 1.61 inches.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 44.6138 km away, between 2011-08-01 16:35:00 and 2011-08-01 16:40:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: An approaching cold front helped trigger strong to locally severe thunderstorms during the late afternoon and early evening of the 1st mainly in southeastern Pennsylvania. An approaching cold front helped trigger strong to locally severe thunderstorms during the late afternoon and early evening of the 1st mainly in southeastern Pennsylvania.\nEvent Narrative: A severe thunderstorm knocked down a few trees in Fairlee. A severe thunderstorm knocked down a few trees in Chestertown.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 26.4798 km away, between 2011-08-01 17:17:00 and 2011-08-01 17:18:00. The events included records with estimated wind gusts of 52.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 2000.0 and crop damage of 0.0. \n\nEpisode Narrative: An upper-level ridge was centered over the southern Plains while an upper-level low was located over central Canada. A northwest flow between these two systems caused colder air aloft to move overhead. Warm and moist air at the surface combined with the colder air aloft to produce moderate amounts of instability. A pressure trough at the surface caused showers and thunderstorms to develop. Moderate instability caused some thunderstorms to produce damaging wind gusts and large hail. An upper-level ridge was centered over the southern Plains while an upper-level low was located over central Canada. A northwest flow between these two systems caused colder air aloft to move overhead. Warm and moist air at the surface combined with the colder air aloft to produce moderate amounts of instability. A pressure trough at the surface caused showers and thunderstorms to develop. Moderate instability caused some thunderstorms to produce damaging wind gusts and large hail. An upper-level ridge was centered over the southern Plains while an upper-level low was located over central Canada. A northwest flow between these two systems caused colder air aloft to move overhead. Warm and moist air at the surface combined with the colder air aloft to produce moderate amounts of instability. A pressure trough at the surface caused showers and thunderstorms to develop. Moderate instability caused some thunderstorms to produce damaging wind gusts and large hail.\nEvent Narrative: A tree that was two feet in diameter was blocking the road. Multiple small branches were down. A tree that was twelve inches in diameter was blocking Tucker Lane.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 25.4666 km away, between 2011-08-01 18:00:00 and 2011-08-01 19:44:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: An upper-level ridge was centered over the southern Plains while an upper-level low was located over central Canada. A northwest flow between these two systems caused colder air aloft to move overhead. Warm and moist air at the surface combined with the colder air aloft to produce moderate amounts of instability. A pressure trough at the surface caused showers and thunderstorms to develop. Moderate instability caused some thunderstorms to produce gusty winds. An upper-level ridge was centered over the southern Plains while an upper-level low was located over central Canada. A northwest flow between these two systems caused colder air aloft to move overhead. Warm and moist air at the surface combined with the colder air aloft to produce moderate amounts of instability. A pressure trough at the surface caused showers and thunderstorms to develop. Moderate instability caused some thunderstorms to produce gusty winds.\nEvent Narrative: A wind gust of 34 knots was measured at Tide Point. Wind gusts in excess of 30 knots were reported at the Thomas Point Lighthouse.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 19.4436 km away, between 2011-08-02 23:34:00 and 2011-08-03 00:24:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A pressure trough was located over Maryland during the nighttime and early morning hours of the 2nd and 3rd. Instability ahead of the trough caused a couple thunderstorms to produce gusty winds. A pressure trough was located over Maryland during the nighttime and early morning hours of the 2nd and 3rd. Instability ahead of the trough caused a couple thunderstorms to produce gusty winds. A pressure trough was located over Maryland during the nighttime and early morning hours of the 2nd and 3rd. Instability ahead of the trough caused a couple thunderstorms to produce gusty winds. A pressure trough was located over Maryland during the nighttime and early morning hours of the 2nd and 3rd. Instability ahead of the trough caused a couple thunderstorms to produce gusty winds. A pressure trough was located over Maryland during the nighttime and early morning hours of the 2nd and 3rd. Instability ahead of the trough caused a couple thunderstorms to produce gusty winds. A pressure trough was located over Maryland during the nighttime and early morning hours of the 2nd and 3rd. Instability ahead of the trough caused a couple thunderstorms to produce gusty winds.\nEvent Narrative: Wind gusts up to 37 knots were measured at Tolchester Beach. Wind gust in excess of 30 knots were estimated near the Maryland Science Center. Wind gusts around 34 knots were estimated near Oriole Park at Camden Yards. Wind gusts up to 37 knots were measured at Miller Island. Wind gust in excess of 30 knots were reported at Tide Point. Wind gusts in excess of 30 knots were estimated near the Lakeland Elementary School.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 49.6002 km away, between 2011-08-02 23:54:00 and 2011-08-02 23:54:00. The events included records with estimated wind gusts of 56.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 110000.0 and crop damage of 0.0. \n\nEpisode Narrative: A pressure trough was located over Maryland during the nighttime and early morning hours of the 2nd and 3rd. Instability ahead of the trough caused a couple thunderstorms to produce damaging wind gusts. A pressure trough was located over Maryland during the nighttime and early morning hours of the 2nd and 3rd. Instability ahead of the trough caused a couple thunderstorms to produce damaging wind gusts.\nEvent Narrative: Many large trees were down and snapped between Vale Road and Williams Street. Five cars were damaged by falling trees. Many large trees were down near Hall Street.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 4.525 km away, between 2011-08-09 15:43:00 and 2011-08-09 15:43:00. The events included records with estimated wind gusts of 52.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 1000.0 and crop damage of 0.0. \n\nEpisode Narrative: A cold front passed through Maryland during the 9th. Moderate instability ahead of the front caused an isolated thunderstorm to produce damaging wind gusts.\nEvent Narrative: A tree was blown down onto power line.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 17.836 km away, between 2011-08-13 13:17:00 and 2011-08-13 13:17:00. The events included records with estimated wind gusts of 61.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 5000.0 and crop damage of 0.0. \n\nEpisode Narrative: A stationary boundary remained over the region during the 13th. Moderate instability ahead of the stationary boundary caused an isolated thunderstorm to produce damaging wind gusts.\nEvent Narrative: Trees were down from Cedar Street to Norwood Elementary School. Minor damage was reported to siding and shingles.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 13.7293 km away, between 2011-08-13 13:19:00 and 2011-08-13 13:19:00. The events included records with estimated wind gusts of 34.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A stationary boundary remained over the waters during the 13th. Moderate instability ahead of the stationary boundary caused a few thunderstorms to produce gusty winds.\nEvent Narrative: Wind gusts in excess of 30 knots were estimated at Oriole Park at Camden Yards.", "The following events were reported: Flash Flood, Flood. These occurred near station USW00093721, approximately 11.462 km away, between 2011-08-14 09:22:00 and 2011-08-15 14:00:00. The flood was caused by Heavy Rain. Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Deep layer southerly flow advected a moist, tropical airmass into the Mid-Atlantic. As low pressure approached from the west, periods of heavy rain and thunderstorms moved across Maryland. Flash flooding occurred in a number of places, with rainfall totals as high as 4.75 inches in Baltimore County. Deep layer southerly flow advected a moist, tropical airmass into the Mid-Atlantic. As low pressure approached from the west, periods of heavy rain and thunderstorms moved across Maryland. Flash flooding occurred in a number of places, with rainfall totals as high as 4.75 inches in Baltimore County. Deep layer southerly flow advected a moist, tropical airmass into the Mid-Atlantic. As low pressure approached from the west, periods of heavy rain and thunderstorms moved across Maryland. Flash flooding occurred in a number of places, with rainfall totals as high as 4.75 inches in Baltimore County. Deep layer southerly flow advected a moist, tropical airmass into the Mid-Atlantic. As low pressure approached from the west, periods of heavy rain and thunderstorms moved across Maryland. Flash flooding occurred in a number of places, with rainfall totals as high as 4.75 inches in Baltimore County. Deep layer southerly flow advected a moist, tropical airmass into the Mid-Atlantic. As low pressure approached from the west, periods of heavy rain and thunderstorms moved across Maryland. Flash flooding occurred in a number of places, with rainfall totals as high as 4.75 inches in Baltimore County. Deep layer southerly flow advected a moist, tropical airmass into the Mid-Atlantic. As low pressure approached from the west, periods of heavy rain and thunderstorms moved across Maryland. Flash flooding occurred in a number of places, with rainfall totals as high as 4.75 inches in Baltimore County. Deep layer southerly flow advected a moist, tropical airmass into the Mid-Atlantic. As low pressure approached from the west, periods of heavy rain and thunderstorms moved across Maryland. Flash flooding occurred in a number of places, with rainfall totals as high as 4.75 inches in Baltimore County. Deep layer southerly flow advected a moist, tropical airmass into the Mid-Atlantic. As low pressure approached from the west, periods of heavy rain and thunderstorms moved across Maryland. Flash flooding occurred in a number of places, with rainfall totals as high as 4.75 inches in Baltimore County. Deep layer southerly flow advected a moist, tropical airmass into the Mid-Atlantic. As low pressure approached from the west, periods of heavy rain and thunderstorms moved across Maryland. Flash flooding occurred in a number of places, with rainfall totals as high as 4.75 inches in Baltimore County. Deep layer southerly flow advected a moist, tropical airmass into the Mid-Atlantic. As low pressure approached from the west, periods of heavy rain and thunderstorms moved across Maryland. Flash flooding occurred in a number of places, with rainfall totals as high as 4.75 inches in Baltimore County. Deep layer southerly flow advected a moist, tropical airmass into the Mid-Atlantic. As low pressure approached from the west, periods of heavy rain and thunderstorms moved across Maryland. Flash flooding occurred in a number of places, with rainfall totals as high as 4.75 inches in Baltimore County. Deep layer southerly flow advected a moist, tropical airmass into the Mid-Atlantic. As low pressure approached from the west, periods of heavy rain and thunderstorms moved across Maryland. Flash flooding occurred in a number of places, with rainfall totals as high as 4.75 inches in Baltimore County. Deep layer southerly flow advected a moist, tropical airmass into the Mid-Atlantic. As low pressure approached from the west, periods of heavy rain and thunderstorms moved across Maryland. Flash flooding occurred in a number of places, with rainfall totals as high as 4.75 inches in Baltimore County. Deep layer southerly flow advected a moist, tropical airmass into the Mid-Atlantic. As low pressure approached from the west, periods of heavy rain and thunderstorms moved across Maryland. Flash flooding occurred in a number of places, with rainfall totals as high as 4.75 inches in Baltimore County. Deep layer southerly flow advected a moist, tropical airmass into the Mid-Atlantic. As low pressure approached from the west, periods of heavy rain and thunderstorms moved across Maryland. Flash flooding occurred in a number of places, with rainfall totals as high as 4.75 inches in Baltimore County. Deep layer southerly flow advected a moist, tropical airmass into the Mid-Atlantic. As low pressure approached from the west, periods of heavy rain and thunderstorms moved across Maryland. Flash flooding occurred in a number of places, with rainfall totals as high as 4.75 inches in Baltimore County.\nEvent Narrative: The intersection of Rutherford Road and Ambassador Road were closed due to flash flooding. A nearby spotter measured 3.13 inches of rain. Flooding was reported in the 500 block of Compass Road. A nearby rain gage observed 2.29 inches. Numerous high water rescues were performed. A rain gage in the city recorded 2.47 inches. One to 1.5 feet of water forced the closed of Nursey Road and Hammonds Ferry Road. A spotter nearby recorded 2.20 inches of rain. Twelve to 18 inches of water forced closure of Belle Grove and Camp Mead Roads. A nearby rain gage measured 1.88 inches. One to 1.5 feet of water forced the closure of Maple Road and Route 648. A nearby rain gage measured 2.83 inches. Twelve to 18 inches of water forced the closure of 10th Avenue and Belle Grove Road. A nearby rain gage tallied 1.68 inches. One to 1.5 feet of water forced the closure of Ritchie Highway and Shelley Road. A spotter in the area measured 1.36 inches of rain. Over two inches of rain caused an apartment complex to flood. Thirty-four people were rescued by firefighters. South Gilmore Street was closed due to high water. Annapolis Road was closed at Waterview Road and Route 295. Reedbird Road was closed due to high water. West Patapsco Road was closed due to high water. Bloomingdale Road was closed due to high water. North Fulton Avenue was closed due to high water. Police were evacuating areas of Spelman Road. Basements were reported flooded with over 5 feet of water.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 35.4985 km away, between 2011-08-14 22:56:00 and 2011-08-14 23:00:00. The events included records with measured wind gusts of 41.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: An upper-level trough was over the waters on the 14th. Colder air aloft due to the upper trough caused moderate amounts of instability to develop. A surface trough triggered showers and thunderstorms and some thunderstorms produced gusty winds due to the instability. An upper-level trough was over the waters on the 14th. Colder air aloft due to the upper trough caused moderate amounts of instability to develop. A surface trough triggered showers and thunderstorms and some thunderstorms produced gusty winds due to the instability.\nEvent Narrative: A wind gust of 36 knots was reported at Tolly Point. A wind gust of 46 knots was measured at the Thomas Point Lighthouse.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 13.9416 km away, between 2011-08-17 17:35:00 and 2011-08-17 17:35:00. The events included records with measured wind gusts of 38.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A trough of low pressure triggered a few showers and thunderstorms over the waters. An isolated thunderstorm produced gusty winds.\nEvent Narrative: A wind gust of 38 knots was measured at Tide Point.", "The following events were reported: Hail, Lightning, Thunderstorm Wind. These occurred near station USW00093721, approximately 23.1336 km away, between 2011-08-18 15:50:00 and 2011-08-18 18:20:00. The events included records with hailstones measuring 17.210526315789473 inches.The events resulted in 1 injuries and 0 fatalities. The events caused property damage valued at 18000.0 and crop damage of 0.0. \n\nEpisode Narrative: A southerly flow around high pressure off the east coast produced hot and humid conditions. The hot and humid conditions combined with colder air aloft associated with an upper-level trough to produce moderate amounts of instability. Some thunderstorms that developed produced damaging wind gusts and large hail. A southerly flow around high pressure off the east coast produced hot and humid conditions. The hot and humid conditions combined with colder air aloft associated with an upper-level trough to produce moderate amounts of instability. Some thunderstorms that developed produced damaging wind gusts and large hail. A southerly flow around high pressure off the east coast produced hot and humid conditions. The hot and humid conditions combined with colder air aloft associated with an upper-level trough to produce moderate amounts of instability. Some thunderstorms that developed produced damaging wind gusts and large hail. A southerly flow around high pressure off the east coast produced hot and humid conditions. The hot and humid conditions combined with colder air aloft associated with an upper-level trough to produce moderate amounts of instability. Some thunderstorms that developed produced damaging wind gusts and large hail. A southerly flow around high pressure off the east coast produced hot and humid conditions. The hot and humid conditions combined with colder air aloft associated with an upper-level trough to produce moderate amounts of instability. Some thunderstorms that developed produced damaging wind gusts and large hail. A southerly flow around high pressure off the east coast produced hot and humid conditions. The hot and humid conditions combined with colder air aloft associated with an upper-level trough to produce moderate amounts of instability. Some thunderstorms that developed produced damaging wind gusts and large hail. A southerly flow around high pressure off the east coast produced hot and humid conditions. The hot and humid conditions combined with colder air aloft associated with an upper-level trough to produce moderate amounts of instability. Some thunderstorms that developed produced damaging wind gusts and large hail. A southerly flow around high pressure off the east coast produced hot and humid conditions. The hot and humid conditions combined with colder air aloft associated with an upper-level trough to produce moderate amounts of instability. Some thunderstorms that developed produced damaging wind gusts and large hail. A southerly flow around high pressure off the east coast produced hot and humid conditions. The hot and humid conditions combined with colder air aloft associated with an upper-level trough to produce moderate amounts of instability. Some thunderstorms that developed produced damaging wind gusts and large hail. A southerly flow around high pressure off the east coast produced hot and humid conditions. The hot and humid conditions combined with colder air aloft associated with an upper-level trough to produce moderate amounts of instability. Some thunderstorms that developed produced damaging wind gusts and large hail. A southerly flow around high pressure off the east coast produced hot and humid conditions. The hot and humid conditions combined with colder air aloft associated with an upper-level trough to produce moderate amounts of instability. Some thunderstorms that developed produced damaging wind gusts and large hail. A southerly flow around high pressure off the east coast produced hot and humid conditions. The hot and humid conditions combined with colder air aloft associated with an upper-level trough to produce moderate amounts of instability. Some thunderstorms that developed produced damaging wind gusts and large hail. A southerly flow around high pressure off the east coast produced hot and humid conditions. The hot and humid conditions combined with colder air aloft associated with an upper-level trough to produce moderate amounts of instability. Some thunderstorms that developed produced damaging wind gusts and large hail. A southerly flow around high pressure off the east coast produced hot and humid conditions. The hot and humid conditions combined with colder air aloft associated with an upper-level trough to produce moderate amounts of instability. Some thunderstorms that developed produced damaging wind gusts and large hail. A southerly flow around high pressure off the east coast produced hot and humid conditions. The hot and humid conditions combined with colder air aloft associated with an upper-level trough to produce moderate amounts of instability. Some thunderstorms that developed produced damaging wind gusts and large hail. A southerly flow around high pressure off the east coast produced hot and humid conditions. The hot and humid conditions combined with colder air aloft associated with an upper-level trough to produce moderate amounts of instability. Some thunderstorms that developed produced damaging wind gusts and large hail. A southerly flow around high pressure off the east coast produced hot and humid conditions. The hot and humid conditions combined with colder air aloft associated with an upper-level trough to produce moderate amounts of instability. Some thunderstorms that developed produced damaging wind gusts and large hail. A southerly flow around high pressure off the east coast produced hot and humid conditions. The hot and humid conditions combined with colder air aloft associated with an upper-level trough to produce moderate amounts of instability. Some thunderstorms that developed produced damaging wind gusts and large hail. A southerly flow around high pressure off the east coast produced hot and humid conditions. The hot and humid conditions combined with colder air aloft associated with an upper-level trough to produce moderate amounts of instability. Some thunderstorms that developed produced damaging wind gusts and large hail. A southerly flow around high pressure off the east coast produced hot and humid conditions. The hot and humid conditions combined with colder air aloft associated with an upper-level trough to produce moderate amounts of instability. Some thunderstorms that developed produced damaging wind gusts and large hail.\nEvent Narrative: Quarter sized hail was reported near Laurel. Quarter sized hail was reported at Glen Burnie. Quarter sized hail was reported near Severn. Quarter sized hail was reported at Fort Meade. Wind gusts were estimated to be around 60 mph. A tree was blown onto a garage crushing the roof. A car was also damaged in the garage. Multiple 150 year old trees were blown down. A tree that was one to one and one half feet in diameter was blown down. Hail up to quarters in size was reported near Mount Airy. Quarter sized hail was reported near Boring. Hail up to the size of golf balls was reported. A tree was down along High Point Road. Golf ball sized hail was reported. Quarter sized hail was reported. A tree was blocking the roadway near Patterson Mill Road and Route 924. Quarter sized hail was reported. Hail up to the size of ping pong balls was reported in Laurel. Quarter sized hail was reported near Green Haven. A person was injured by lightning while using an ATM machine. Quarter sized hail was reported in Fort Meade. A tree about one to one and one half feet in diameter was blown down from thunderstorm winds.", "The following events were reported: Flash Flood. These occurred near station USW00093721, approximately 4.8384 km away, between 2011-08-18 16:10:00 and 2011-08-18 18:00:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Isolated thunderstorms developed across Maryland when an upper level disturbance tracked across a moist and unstable atmosphere. High rainfall rates over Anne Arundel County cased an isolated flash flood.\nEvent Narrative: Intersection of Steven Road and Quarterfield Road was flooded.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 14.1041 km away, between 2011-08-18 16:34:00 and 2011-08-18 18:36:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A southerly flow around high pressure off the east coast produced hot and humid conditions. The hot and humid conditions combined with colder air aloft associated with an upper-level trough to produce moderate amounts of instability. Thunderstorms developed and a few were able to produce gusty winds over the waters. A southerly flow around high pressure off the east coast produced hot and humid conditions. The hot and humid conditions combined with colder air aloft associated with an upper-level trough to produce moderate amounts of instability. Thunderstorms developed and a few were able to produce gusty winds over the waters.\nEvent Narrative: A wind gust in excess of 30 knots was reported at Tide Point. A wind gust of 41 knots was reported at the Baltimore Key Bridge.", "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00093721, approximately 21.4606 km away, between 2011-08-19 16:50:00 and 2011-08-19 17:50:00. The events included records with hailstones measuring 25.818181818181817 inches.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 17000.0 and crop damage of 0.0. \n\nEpisode Narrative: An upper-level trough provided cold air aloft while warm and moist air remained at the surface. Moderate amounts of instability developed during the afternoon and evening hours. Some thunderstorms that developed along and ahead of a pressure trough were able to produce damaging wind gusts and large hail. An upper-level trough provided cold air aloft while warm and moist air remained at the surface. Moderate amounts of instability developed during the afternoon and evening hours. Some thunderstorms that developed along and ahead of a pressure trough were able to produce damaging wind gusts and large hail. An upper-level trough provided cold air aloft while warm and moist air remained at the surface. Moderate amounts of instability developed during the afternoon and evening hours. Some thunderstorms that developed along and ahead of a pressure trough were able to produce damaging wind gusts and large hail. An upper-level trough provided cold air aloft while warm and moist air remained at the surface. Moderate amounts of instability developed during the afternoon and evening hours. Some thunderstorms that developed along and ahead of a pressure trough were able to produce damaging wind gusts and large hail. An upper-level trough provided cold air aloft while warm and moist air remained at the surface. Moderate amounts of instability developed during the afternoon and evening hours. Some thunderstorms that developed along and ahead of a pressure trough were able to produce damaging wind gusts and large hail. An upper-level trough provided cold air aloft while warm and moist air remained at the surface. Moderate amounts of instability developed during the afternoon and evening hours. Some thunderstorms that developed along and ahead of a pressure trough were able to produce damaging wind gusts and large hail. An upper-level trough provided cold air aloft while warm and moist air remained at the surface. Moderate amounts of instability developed during the afternoon and evening hours. Some thunderstorms that developed along and ahead of a pressure trough were able to produce damaging wind gusts and large hail. An upper-level trough provided cold air aloft while warm and moist air remained at the surface. Moderate amounts of instability developed during the afternoon and evening hours. Some thunderstorms that developed along and ahead of a pressure trough were able to produce damaging wind gusts and large hail. An upper-level trough provided cold air aloft while warm and moist air remained at the surface. Moderate amounts of instability developed during the afternoon and evening hours. Some thunderstorms that developed along and ahead of a pressure trough were able to produce damaging wind gusts and large hail. An upper-level trough provided cold air aloft while warm and moist air remained at the surface. Moderate amounts of instability developed during the afternoon and evening hours. Some thunderstorms that developed along and ahead of a pressure trough were able to produce damaging wind gusts and large hail. An upper-level trough provided cold air aloft while warm and moist air remained at the surface. Moderate amounts of instability developed during the afternoon and evening hours. Some thunderstorms that developed along and ahead of a pressure trough were able to produce damaging wind gusts and large hail.\nEvent Narrative: Quarter sized hail was reported in Essex. Quarter sized hail was reported near the Fort Smallwood State Park. Quarter sized hail was reported near the intersection of eastern Avenue and Old Eastern Avenue. Siding was being removed from homes due to thunderstorm winds. Wind gusts were estimated to be around 60 mph. Quarter sized hail was reported. Multiple power poles were torn down and a tree that was six inches in diameter was uprooted. Quarter sized hail was reported near Lake Shore. A large tree was uprooted by a thunderstorm wind gust. A tree was down near the intersection of Wildwood Beach Road and Riverview Road. Quarter sized hail was reported on Placid Avenue.", "The following events were reported: Flash Flood. These occurred near station USW00093721, approximately 26.3156 km away, between 2011-08-19 17:10:00 and 2011-08-19 18:45:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: An upper-level disturbance combined with a moist, unstable airmass to induce scattered thunderstorms during the afternoon and evening hours. Several reports of flash flooding were received as this activity moved across the saturated ground along the Interstate 95 corridor. A rain gage in Prince Georges County measured 3.90 inches in under 2 hours and 3.04 inches in one hour. An upper-level disturbance combined with a moist, unstable airmass to induce scattered thunderstorms during the afternoon and evening hours. Several reports of flash flooding were received as this activity moved across the saturated ground along the Interstate 95 corridor. A rain gage in Prince Georges County measured 3.90 inches in under 2 hours and 3.04 inches in one hour.\nEvent Narrative: North Point Road in North Point State Park was inundated by over 6 inches of water flowing over the roadway. A creek filled and overflowed into a field.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 35.2237 km away, between 2011-08-19 18:00:00 and 2011-08-19 19:00:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: An upper-level trough provided cold air aloft while warm and moist air remained at the surface. Moderate amounts of instability developed during the afternoon and evening hours. Some thunderstorms that developed along and ahead of a pressure trough were able to produce gusty winds. An upper-level trough provided cold air aloft while warm and moist air remained at the surface. Moderate amounts of instability developed during the afternoon and evening hours. Some thunderstorms that developed along and ahead of a pressure trough were able to produce gusty winds. An upper-level trough provided cold air aloft while warm and moist air remained at the surface. Moderate amounts of instability developed during the afternoon and evening hours. Some thunderstorms that developed along and ahead of a pressure trough were able to produce gusty winds. An upper-level trough provided cold air aloft while warm and moist air remained at the surface. Moderate amounts of instability developed during the afternoon and evening hours. Some thunderstorms that developed along and ahead of a pressure trough were able to produce gusty winds. An upper-level trough provided cold air aloft while warm and moist air remained at the surface. Moderate amounts of instability developed during the afternoon and evening hours. Some thunderstorms that developed along and ahead of a pressure trough were able to produce gusty winds.\nEvent Narrative: A wind gust in excess of 30 knots was reported at Sandy Point. A wind gust of 36 knots was measured at the Thomas Point Lighthouse. A wind gust in excess of 30 knots was measured at the Stevensville Airport. A wind gust in excess of 30 knots was measured at the Thomas Point Lighthouse. A wind gust of 34 knots was measured at Tolly Point.", "The following events were reported: Marine Hail, Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 19.8943 km away, between 2011-08-21 12:06:00 and 2011-08-21 14:06:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front approached the waters from the Ohio Valley on the 21st. Warm and moist air ahead of the boundary caused an unstable atmosphere. Some thunderstorms ahead of the cold front produced gusty winds. A cold front approached the waters from the Ohio Valley on the 21st. Warm and moist air ahead of the boundary caused an unstable atmosphere. Some thunderstorms ahead of the cold front produced gusty winds. A cold front approached the waters from the Ohio Valley on the 21st. Warm and moist air ahead of the boundary caused an unstable atmosphere. Some thunderstorms ahead of the cold front produced gusty winds. A cold front approached the waters from the Ohio Valley on the 21st. Warm and moist air ahead of the boundary caused an unstable atmosphere. Some thunderstorms ahead of the cold front produced gusty winds. A cold front approached the waters from the Ohio Valley on the 21st. Warm and moist air ahead of the boundary caused an unstable atmosphere. Some thunderstorms ahead of the cold front produced gusty winds. A cold front approached the waters from the Ohio Valley on the 21st. Warm and moist air ahead of the boundary caused an unstable atmosphere. Some thunderstorms ahead of the cold front produced gusty winds.\nEvent Narrative: Wind gusts between 36 and 53 knots were measured at the Baltimore Key Bridge. Wind gusts up to 42 knots were measured at Tolchester Beach. Half dollar sized hail was estimated. Quarter sized hail was estimated. Wind gusts were estimated to be around 52 knots based on thunderstorm wind damage nearby. Wind gusts up to 42 knots were measured at the Baltimore Buoy.", "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00093721, approximately 18.6094 km away, between 2011-08-21 12:14:00 and 2011-08-21 13:41:00. The events included records with hailstones measuring 18.02777777777778 inches.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 2000.0 and crop damage of 0.0. \n\nEpisode Narrative: A cold front approached the area from the Ohio Valley on the 21st. Warm and moist air ahead of the boundary caused an unstable atmosphere. Some thunderstorms ahead of the cold front produced damaging winds and large hail. A cold front approached the area from the Ohio Valley on the 21st. Warm and moist air ahead of the boundary caused an unstable atmosphere. Some thunderstorms ahead of the cold front produced damaging winds and large hail. A cold front approached the area from the Ohio Valley on the 21st. Warm and moist air ahead of the boundary caused an unstable atmosphere. Some thunderstorms ahead of the cold front produced damaging winds and large hail. A cold front approached the area from the Ohio Valley on the 21st. Warm and moist air ahead of the boundary caused an unstable atmosphere. Some thunderstorms ahead of the cold front produced damaging winds and large hail. A cold front approached the area from the Ohio Valley on the 21st. Warm and moist air ahead of the boundary caused an unstable atmosphere. Some thunderstorms ahead of the cold front produced damaging winds and large hail. A cold front approached the area from the Ohio Valley on the 21st. Warm and moist air ahead of the boundary caused an unstable atmosphere. Some thunderstorms ahead of the cold front produced damaging winds and large hail. A cold front approached the area from the Ohio Valley on the 21st. Warm and moist air ahead of the boundary caused an unstable atmosphere. Some thunderstorms ahead of the cold front produced damaging winds and large hail. A cold front approached the area from the Ohio Valley on the 21st. Warm and moist air ahead of the boundary caused an unstable atmosphere. Some thunderstorms ahead of the cold front produced damaging winds and large hail. A cold front approached the area from the Ohio Valley on the 21st. Warm and moist air ahead of the boundary caused an unstable atmosphere. Some thunderstorms ahead of the cold front produced damaging winds and large hail.\nEvent Narrative: Quarter sized hail was reported. Half dollar sized hail was reported near Dundalk. Quarter sized hail was reported near Dundalk. Quarter sized hail was reported near Back River. Quarter sized hail was reported near Bodkin Point. Wind gusts were estimated to be around 60 mph. Large tree branches were blocking Ranch Lane near Trappe Road. Quarter sized hail was reported on Admiral Boulevard. A tree was uprooted in Fort Howard.", "The following events were reported: Flash Flood. These occurred near station USW00093721, approximately 21.0211 km away, between 2011-08-21 12:45:00 and 2011-08-21 15:00:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Thunderstorms developed in association with a trof moving through the Mid-Atlantic. As they moved over the saturated ground of Baltimore County, their rain led to flash flooding. Thunderstorms developed in association with a trof moving through the Mid-Atlantic. As they moved over the saturated ground of Baltimore County, their rain led to flash flooding. Thunderstorms developed in association with a trof moving through the Mid-Atlantic. As they moved over the saturated ground of Baltimore County, their rain led to flash flooding. Thunderstorms developed in association with a trof moving through the Mid-Atlantic. As they moved over the saturated ground of Baltimore County, their rain led to flash flooding. Thunderstorms developed in association with a trof moving through the Mid-Atlantic. As they moved over the saturated ground of Baltimore County, their rain led to flash flooding.\nEvent Narrative: Six feet of water was blocking North Point Boulevard. Two feet of water was flowing over the intersection of Old North Point and German Hill roads from Bread and Cheese Creek. A swift water rescue was performed near the intersection of Virginia and Marie Avenues. Three swift water rescues were conducted near the intersection of Church and Trappe Roads. The intersection of Willow Avenue and North Point Road was flooded with 18 inches of flowing water.", "The following events were reported: Flash Flood. These occurred near station USW00093721, approximately 47.3802 km away, between 2011-08-21 15:30:00 and 2011-08-21 18:30:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A series of thunderstorms with heavy rain mainly during the mid to late afternoon of the 21st across the Eastern Shore caused flash flooding in Kent County.\nEvent Narrative: Thunderstorms with heavy rain caused field, poor drainage and small stream flash flooding in southwestern Kent County. A few roadways were flooded and closed. Doppler Radar storm total estimates reached 3 to 5 inches.", "The following events were reported: Flash Flood, Flood. These occurred near station USW00093721, approximately 23.5713 km away, between 2011-08-27 17:24:00 and 2011-08-28 08:00:00. The flood was caused by Heavy Rain. Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Hurricane Irene tracked up the Mid-Atlantic Coast during the afternoon and evening hours of the 27th. Heavy rains associated with Irene and her rainbands fell over saturated soils of Maryland. Flash flooding resulted in some areas and flooding continued into the 28th as waters rose. Storm total rainfall from Irene reached 12.00 in spots. Hurricane Irene tracked up the Mid-Atlantic Coast during the afternoon and evening hours of the 27th. Heavy rains associated with Irene and her rainbands fell over saturated soils of Maryland. Flash flooding resulted in some areas and flooding continued into the 28th as waters rose. Storm total rainfall from Irene reached 12.00 in spots. Hurricane Irene tracked up the Mid-Atlantic Coast during the afternoon and evening hours of the 27th. Heavy rains associated with Irene and her rainbands fell over saturated soils of Maryland. Flash flooding resulted in some areas and flooding continued into the 28th as waters rose. Storm total rainfall from Irene reached 12.00 in spots. Hurricane Irene tracked up the Mid-Atlantic Coast during the afternoon and evening hours of the 27th. Heavy rains associated with Irene and her rainbands fell over saturated soils of Maryland. Flash flooding resulted in some areas and flooding continued into the 28th as waters rose. Storm total rainfall from Irene reached 12.00 in spots. Hurricane Irene tracked up the Mid-Atlantic Coast during the afternoon and evening hours of the 27th. Heavy rains associated with Irene and her rainbands fell over saturated soils of Maryland. Flash flooding resulted in some areas and flooding continued into the 28th as waters rose. Storm total rainfall from Irene reached 12.00 in spots. Hurricane Irene tracked up the Mid-Atlantic Coast during the afternoon and evening hours of the 27th. Heavy rains associated with Irene and her rainbands fell over saturated soils of Maryland. Flash flooding resulted in some areas and flooding continued into the 28th as waters rose. Storm total rainfall from Irene reached 12.00 in spots. Hurricane Irene tracked up the Mid-Atlantic Coast during the afternoon and evening hours of the 27th. Heavy rains associated with Irene and her rainbands fell over saturated soils of Maryland. Flash flooding resulted in some areas and flooding continued into the 28th as waters rose. Storm total rainfall from Irene reached 12.00 in spots. Hurricane Irene tracked up the Mid-Atlantic Coast during the afternoon and evening hours of the 27th. Heavy rains associated with Irene and her rainbands fell over saturated soils of Maryland. Flash flooding resulted in some areas and flooding continued into the 28th as waters rose. Storm total rainfall from Irene reached 12.00 in spots. Hurricane Irene tracked up the Mid-Atlantic Coast during the afternoon and evening hours of the 27th. Heavy rains associated with Irene and her rainbands fell over saturated soils of Maryland. Flash flooding resulted in some areas and flooding continued into the 28th as waters rose. Storm total rainfall from Irene reached 12.00 in spots. Hurricane Irene tracked up the Mid-Atlantic Coast during the afternoon and evening hours of the 27th. Heavy rains associated with Irene and her rainbands fell over saturated soils of Maryland. Flash flooding resulted in some areas and flooding continued into the 28th as waters rose. Storm total rainfall from Irene reached 12.00 in spots.\nEvent Narrative: State route 450 was flooded and closed near Rutland Road. A nearby rain gage had a storm total of 6.20 inches. Maryland State Route 176 was flooded and closed between Central Avenue and Baltimore-Annapolis Boulevard. A nearby rain gage measured 5.92 inches during the event. Harford Road near Montibello Terrace was closed due to flash flooding. A nearby rain gage tallied 4.59 inches. The 600 Block of West Patapsco Avenue was closed due to flooding. A nearby rain gage tallied 3.34 inches. McElderry Street near North Patterson Park Avenue was closed due to flooding. A rain gage in downtown Baltimore measured 3.63 inches during the event. State Route 214 closed at State Route 2 due to flash flooding. A rain gage near the event recorded 5.77 inches. State Route 7 was flooded and closed at Mohrs Lane. A nearby rain gage recorded 4.45 inches. State Route 150 was flooded and closed at Earls Road. A nearby rain gage totaled 4.90 inches. State Route 7 was flooded and closed between Edgewood Road and Maryland Route 24. The highest total from a rain gauge nearby was 5.26 inches. State Route 150 was closed due to flooding from earlier rainfall. A nearby rain gauge recorded 4.44 inches during the storm.", "The following events were reported: Flash Flood, Flood. These occurred near station USW00093721, approximately 42.4829 km away, between 2011-08-27 19:30:00 and 2011-08-28 17:00:00. The flood was caused by Heavy Rain / Tropical System. Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 1100000.0 and crop damage of 0.0. \n\nEpisode Narrative: Hurricane Irene produced heavy flooding rain, tropical storm force wind gusts and caused one wind related death across the Eastern Shore. Preliminary damage estimates were around three million dollars and approximately 85,000 homes and businesses lost power. Power was not fully restored until September 1st. The combination of heavy rain and wind closed numerous roadways across the Eastern Shore and downed thousands of trees. Some schools were unable to open on Monday August 29th. There was a temporary ban on harvesting shellfish along Chesapeake Bay because of the excessive runoff. Some tomato, corn, watermelon and cantaloupe crops were destroyed. It was estimated that 30,000 chickens were also killed by the effects of Irene.||Tropical storm force wind gusts overspread the Eastern Shore during the afternoon and early evening of the 27th and persisted into the afternoon of the 28th. Peak wind gusts averaged 50 to 60 mph. The strongest winds associated with Irene occurred at two distinct times. The first surge occurred during bands of heavier rain during the evening and late night of the 27th. The second peak occurred during the late morning and early afternoon of the 28th when skies were clearing and deeper mixing of the atmosphere brought stronger winds to the ground. The rain associated with Irene overspread the Eastern Shore between 7 a.m. EDT and Noon EDT on the 27th, fell at its heaviest from the late afternoon of the 27th into the early morning of the 28th and ended around Noon EDT on the 28th. Event precipitation totals averaged 6 to 12 inches and caused widespread field and roadway flooding. Because the flash flooding and flooding blended into one, all flooding related county entries were combined into one under flood events. ||On August 25, Maryland Governor Martin O'Malley declared a state of emergency in preparation for Irene. The Chesapeake Bay Bridge was closed to vehicular traffic. In Queen Anne's County, in Queenstown, an 88-year-old woman was killed when a tree fell on a chimney, sending bricks through the glass roof of a sun room where she had taken refuge since it had emergency power. About 13,000 utility customers lost power. Sections of Maryland State Routes 18, 19 and 802 were also closed because of high winds and or debris on roadways. In Cecil County, sections of Maryland State Routes 273, 213 and 272 were closed. About seventy-percent of all Delmarva Power customers lost power. In Kent County, multiple parts of Maryland State Routes 20 and 445 were closed. In all twenty-seven roadways were closed by downed trees. In Talbot County, debris closed Maryland State Route 662C. About 100 properties and 50 roadways and bridges were damaged by the flooding and wind. In Caroline County, sections of Maryland State Routes 287, 313, 31 and 311 were among twenty roadways that were closed. Two dozen homes were damaged by the flooding and wind. About 5,500 homes and businesses lost power. ||The highest wind gusts recorded during Hurricane Irene were 61 mph in Salisbury (Wicomico County), 60 mph in Tolchester Beach (Kent County) and 51 mph at the Baltimore-Washington International Airport.||Hurricane Irene formed east of the Leeward Islands on Saturday the 20th. It moved northeast and passed over Puerto Rico overnight on the 21st. As Irene moved off the island, it intensified into a hurricane. Irene just bypassed the island of Hispaniola to its north and then passed over the Eastern Bahamas on the 25th as it reached category three hurricane strength. From the Bahamas, Irene moved nearly due north and slowly weakened to a category two hurricane on the 26th and a category one hurricane on the 27th. Irene made her initial landfall near Cape Lookout, North Carolina at 8 a.m. EDT on the 27th and then proceeded to the northnortheast and went back over the Atlantic Ocean near the Virginia and North Carolina border at 7 p.m. EDT on the 27th. From there Irene paralleled the Delmarva Peninsula and the center passed about 15 miles east of Delaware between 3 a.m. and 4 a.m. EDT on the 28th. Irene made her second landfall as a tropical storm on Brigantine Island, just north of Atlantic City, New Jersey at 535 a.m. EDT on the 28th. Hurricane Irene produced heavy flooding rain, tropical storm force wind gusts and caused one wind related death across the Eastern Shore. Preliminary damage estimates were around three million dollars and approximately 85,000 homes and businesses lost power. Power was not fully restored until September 1st. The combination of heavy rain and wind closed numerous roadways across the Eastern Shore and downed thousands of trees. Some schools were unable to open on Monday August 29th. There was a temporary ban on harvesting shellfish along Chesapeake Bay because of the excessive runoff. Some tomato, corn, watermelon and cantaloupe crops were destroyed. It was estimated that 30,000 chickens were also killed by the effects of Irene.||Tropical storm force wind gusts overspread the Eastern Shore during the afternoon and early evening of the 27th and persisted into the afternoon of the 28th. Peak wind gusts averaged 50 to 60 mph. The strongest winds associated with Irene occurred at two distinct times. The first surge occurred during bands of heavier rain during the evening and late night of the 27th. The second peak occurred during the late morning and early afternoon of the 28th when skies were clearing and deeper mixing of the atmosphere brought stronger winds to the ground. The rain associated with Irene overspread the Eastern Shore between 7 a.m. EDT and Noon EDT on the 27th, fell at its heaviest from the late afternoon of the 27th into the early morning of the 28th and ended around Noon EDT on the 28th. Event precipitation totals averaged 6 to 12 inches and caused widespread field and roadway flooding. Because the flash flooding and flooding blended into one, all flooding related county entries were combined into one under flood events. ||On August 25, Maryland Governor Martin O'Malley declared a state of emergency in preparation for Irene. The Chesapeake Bay Bridge was closed to vehicular traffic. In Queen Anne's County, in Queenstown, an 88-year-old woman was killed when a tree fell on a chimney, sending bricks through the glass roof of a sun room where she had taken refuge since it had emergency power. About 13,000 utility customers lost power. Sections of Maryland State Routes 18, 19 and 802 were also closed because of high winds and or debris on roadways. In Cecil County, sections of Maryland State Routes 273, 213 and 272 were closed. About seventy-percent of all Delmarva Power customers lost power. In Kent County, multiple parts of Maryland State Routes 20 and 445 were closed. In all twenty-seven roadways were closed by downed trees. In Talbot County, debris closed Maryland State Route 662C. About 100 properties and 50 roadways and bridges were damaged by the flooding and wind. In Caroline County, sections of Maryland State Routes 287, 313, 31 and 311 were among twenty roadways that were closed. Two dozen homes were damaged by the flooding and wind. About 5,500 homes and businesses lost power. ||The highest wind gusts recorded during Hurricane Irene were 61 mph in Salisbury (Wicomico County), 60 mph in Tolchester Beach (Kent County) and 51 mph at the Baltimore-Washington International Airport.||Hurricane Irene formed east of the Leeward Islands on Saturday the 20th. It moved northeast and passed over Puerto Rico overnight on the 21st. As Irene moved off the island, it intensified into a hurricane. Irene just bypassed the island of Hispaniola to its north and then passed over the Eastern Bahamas on the 25th as it reached category three hurricane strength. From the Bahamas, Irene moved nearly due north and slowly weakened to a category two hurricane on the 26th and a category one hurricane on the 27th. Irene made her initial landfall near Cape Lookout, North Carolina at 8 a.m. EDT on the 27th and then proceeded to the northnortheast and went back over the Atlantic Ocean near the Virginia and North Carolina border at 7 p.m. EDT on the 27th. From there Irene paralleled the Delmarva Peninsula and the center passed about 15 miles east of Delaware between 3 a.m. and 4 a.m. EDT on the 28th. Irene made her second landfall as a tropical storm on Brigantine Island, just north of Atlantic City, New Jersey at 535 a.m. EDT on the 28th. Hurricane Irene produced heavy flooding rain, tropical storm force wind gusts and caused one wind related death across the Eastern Shore. Preliminary damage estimates were around three million dollars and approximately 85,000 homes and businesses lost power. Power was not fully restored until September 1st. The combination of heavy rain and wind closed numerous roadways across the Eastern Shore and downed thousands of trees. Some schools were unable to open on Monday August 29th. There was a temporary ban on harvesting shellfish along Chesapeake Bay because of the excessive runoff. Some tomato, corn, watermelon and cantaloupe crops were destroyed. It was estimated that 30,000 chickens were also killed by the effects of Irene.||Tropical storm force wind gusts overspread the Eastern Shore during the afternoon and early evening of the 27th and persisted into the afternoon of the 28th. Peak wind gusts averaged 50 to 60 mph. The strongest winds associated with Irene occurred at two distinct times. The first surge occurred during bands of heavier rain during the evening and late night of the 27th. The second peak occurred during the late morning and early afternoon of the 28th when skies were clearing and deeper mixing of the atmosphere brought stronger winds to the ground. The rain associated with Irene overspread the Eastern Shore between 7 a.m. EDT and Noon EDT on the 27th, fell at its heaviest from the late afternoon of the 27th into the early morning of the 28th and ended around Noon EDT on the 28th. Event precipitation totals averaged 6 to 12 inches and caused widespread field and roadway flooding. Because the flash flooding and flooding blended into one, all flooding related county entries were combined into one under flood events. ||On August 25, Maryland Governor Martin O'Malley declared a state of emergency in preparation for Irene. The Chesapeake Bay Bridge was closed to vehicular traffic. In Queen Anne's County, in Queenstown, an 88-year-old woman was killed when a tree fell on a chimney, sending bricks through the glass roof of a sun room where she had taken refuge since it had emergency power. About 13,000 utility customers lost power. Sections of Maryland State Routes 18, 19 and 802 were also closed because of high winds and or debris on roadways. In Cecil County, sections of Maryland State Routes 273, 213 and 272 were closed. About seventy-percent of all Delmarva Power customers lost power. In Kent County, multiple parts of Maryland State Routes 20 and 445 were closed. In all twenty-seven roadways were closed by downed trees. In Talbot County, debris closed Maryland State Route 662C. About 100 properties and 50 roadways and bridges were damaged by the flooding and wind. In Caroline County, sections of Maryland State Routes 287, 313, 31 and 311 were among twenty roadways that were closed. Two dozen homes were damaged by the flooding and wind. About 5,500 homes and businesses lost power. ||The highest wind gusts recorded during Hurricane Irene were 61 mph in Salisbury (Wicomico County), 60 mph in Tolchester Beach (Kent County) and 51 mph at the Baltimore-Washington International Airport.||Hurricane Irene formed east of the Leeward Islands on Saturday the 20th. It moved northeast and passed over Puerto Rico overnight on the 21st. As Irene moved off the island, it intensified into a hurricane. Irene just bypassed the island of Hispaniola to its north and then passed over the Eastern Bahamas on the 25th as it reached category three hurricane strength. From the Bahamas, Irene moved nearly due north and slowly weakened to a category two hurricane on the 26th and a category one hurricane on the 27th. Irene made her initial landfall near Cape Lookout, North Carolina at 8 a.m. EDT on the 27th and then proceeded to the northnortheast and went back over the Atlantic Ocean near the Virginia and North Carolina border at 7 p.m. EDT on the 27th. From there Irene paralleled the Delmarva Peninsula and the center passed about 15 miles east of Delaware between 3 a.m. and 4 a.m. EDT on the 28th. Irene made her second landfall as a tropical storm on Brigantine Island, just north of Atlantic City, New Jersey at 535 a.m. EDT on the 28th. Hurricane Irene produced heavy flooding rain, tropical storm force wind gusts and caused one wind related death across the Eastern Shore. Preliminary damage estimates were around three million dollars and approximately 85,000 homes and businesses lost power. Power was not fully restored until September 1st. The combination of heavy rain and wind closed numerous roadways across the Eastern Shore and downed thousands of trees. Some schools were unable to open on Monday August 29th. There was a temporary ban on harvesting shellfish along Chesapeake Bay because of the excessive runoff. Some tomato, corn, watermelon and cantaloupe crops were destroyed. It was estimated that 30,000 chickens were also killed by the effects of Irene.||Tropical storm force wind gusts overspread the Eastern Shore during the afternoon and early evening of the 27th and persisted into the afternoon of the 28th. Peak wind gusts averaged 50 to 60 mph. The strongest winds associated with Irene occurred at two distinct times. The first surge occurred during bands of heavier rain during the evening and late night of the 27th. The second peak occurred during the late morning and early afternoon of the 28th when skies were clearing and deeper mixing of the atmosphere brought stronger winds to the ground. The rain associated with Irene overspread the Eastern Shore between 7 a.m. EDT and Noon EDT on the 27th, fell at its heaviest from the late afternoon of the 27th into the early morning of the 28th and ended around Noon EDT on the 28th. Event precipitation totals averaged 6 to 12 inches and caused widespread field and roadway flooding. Because the flash flooding and flooding blended into one, all flooding related county entries were combined into one under flood events. ||On August 25, Maryland Governor Martin O'Malley declared a state of emergency in preparation for Irene. The Chesapeake Bay Bridge was closed to vehicular traffic. In Queen Anne's County, in Queenstown, an 88-year-old woman was killed when a tree fell on a chimney, sending bricks through the glass roof of a sun room where she had taken refuge since it had emergency power. About 13,000 utility customers lost power. Sections of Maryland State Routes 18, 19 and 802 were also closed because of high winds and or debris on roadways. In Cecil County, sections of Maryland State Routes 273, 213 and 272 were closed. About seventy-percent of all Delmarva Power customers lost power. In Kent County, multiple parts of Maryland State Routes 20 and 445 were closed. In all twenty-seven roadways were closed by downed trees. In Talbot County, debris closed Maryland State Route 662C. About 100 properties and 50 roadways and bridges were damaged by the flooding and wind. In Caroline County, sections of Maryland State Routes 287, 313, 31 and 311 were among twenty roadways that were closed. Two dozen homes were damaged by the flooding and wind. About 5,500 homes and businesses lost power. ||The highest wind gusts recorded during Hurricane Irene were 61 mph in Salisbury (Wicomico County), 60 mph in Tolchester Beach (Kent County) and 51 mph at the Baltimore-Washington International Airport.||Hurricane Irene formed east of the Leeward Islands on Saturday the 20th. It moved northeast and passed over Puerto Rico overnight on the 21st. As Irene moved off the island, it intensified into a hurricane. Irene just bypassed the island of Hispaniola to its north and then passed over the Eastern Bahamas on the 25th as it reached category three hurricane strength. From the Bahamas, Irene moved nearly due north and slowly weakened to a category two hurricane on the 26th and a category one hurricane on the 27th. Irene made her initial landfall near Cape Lookout, North Carolina at 8 a.m. EDT on the 27th and then proceeded to the northnortheast and went back over the Atlantic Ocean near the Virginia and North Carolina border at 7 p.m. EDT on the 27th. From there Irene paralleled the Delmarva Peninsula and the center passed about 15 miles east of Delaware between 3 a.m. and 4 a.m. EDT on the 28th. Irene made her second landfall as a tropical storm on Brigantine Island, just north of Atlantic City, New Jersey at 535 a.m. EDT on the 28th. Hurricane Irene produced heavy flooding rain, tropical storm force wind gusts and caused one wind related death across the Eastern Shore. Preliminary damage estimates were around three million dollars and approximately 85,000 homes and businesses lost power. Power was not fully restored until September 1st. The combination of heavy rain and wind closed numerous roadways across the Eastern Shore and downed thousands of trees. Some schools were unable to open on Monday August 29th. There was a temporary ban on harvesting shellfish along Chesapeake Bay because of the excessive runoff. Some tomato, corn, watermelon and cantaloupe crops were destroyed. It was estimated that 30,000 chickens were also killed by the effects of Irene.||Tropical storm force wind gusts overspread the Eastern Shore during the afternoon and early evening of the 27th and persisted into the afternoon of the 28th. Peak wind gusts averaged 50 to 60 mph. The strongest winds associated with Irene occurred at two distinct times. The first surge occurred during bands of heavier rain during the evening and late night of the 27th. The second peak occurred during the late morning and early afternoon of the 28th when skies were clearing and deeper mixing of the atmosphere brought stronger winds to the ground. The rain associated with Irene overspread the Eastern Shore between 7 a.m. EDT and Noon EDT on the 27th, fell at its heaviest from the late afternoon of the 27th into the early morning of the 28th and ended around Noon EDT on the 28th. Event precipitation totals averaged 6 to 12 inches and caused widespread field and roadway flooding. Because the flash flooding and flooding blended into one, all flooding related county entries were combined into one under flood events. ||On August 25, Maryland Governor Martin O'Malley declared a state of emergency in preparation for Irene. The Chesapeake Bay Bridge was closed to vehicular traffic. In Queen Anne's County, in Queenstown, an 88-year-old woman was killed when a tree fell on a chimney, sending bricks through the glass roof of a sun room where she had taken refuge since it had emergency power. About 13,000 utility customers lost power. Sections of Maryland State Routes 18, 19 and 802 were also closed because of high winds and or debris on roadways. In Cecil County, sections of Maryland State Routes 273, 213 and 272 were closed. About seventy-percent of all Delmarva Power customers lost power. In Kent County, multiple parts of Maryland State Routes 20 and 445 were closed. In all twenty-seven roadways were closed by downed trees. In Talbot County, debris closed Maryland State Route 662C. About 100 properties and 50 roadways and bridges were damaged by the flooding and wind. In Caroline County, sections of Maryland State Routes 287, 313, 31 and 311 were among twenty roadways that were closed. Two dozen homes were damaged by the flooding and wind. About 5,500 homes and businesses lost power. ||The highest wind gusts recorded during Hurricane Irene were 61 mph in Salisbury (Wicomico County), 60 mph in Tolchester Beach (Kent County) and 51 mph at the Baltimore-Washington International Airport.||Hurricane Irene formed east of the Leeward Islands on Saturday the 20th. It moved northeast and passed over Puerto Rico overnight on the 21st. As Irene moved off the island, it intensified into a hurricane. Irene just bypassed the island of Hispaniola to its north and then passed over the Eastern Bahamas on the 25th as it reached category three hurricane strength. From the Bahamas, Irene moved nearly due north and slowly weakened to a category two hurricane on the 26th and a category one hurricane on the 27th. Irene made her initial landfall near Cape Lookout, North Carolina at 8 a.m. EDT on the 27th and then proceeded to the northnortheast and went back over the Atlantic Ocean near the Virginia and North Carolina border at 7 p.m. EDT on the 27th. From there Irene paralleled the Delmarva Peninsula and the center passed about 15 miles east of Delaware between 3 a.m. and 4 a.m. EDT on the 28th. Irene made her second landfall as a tropical storm on Brigantine Island, just north of Atlantic City, New Jersey at 535 a.m. EDT on the 28th.\nEvent Narrative: Flooding rains forced the closure of Maryland State Route 300 at Dudley Corner Road. Event rainfall totals included 4.70 inches in Stevensville. About a dozen roadways were closed by flooding. In Millington (along the Chester River) the flooding was described as the worst since Hurricane Floyd. Several people were rescued from stranded vehicles. The Sassafras River also flooded along the county line with Cecil County.", "The following events were reported: Flood. These occurred near station USW00093721, approximately 28.3749 km away, between 2011-09-06 00:45:00 and 2011-09-06 05:00:00. The flood was caused by Heavy Rain. Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Deep tropical moisture associated with the remnants of Tropical Depression Lee interacted with a slow-moving cold front to produce widespread showers across the area. High rainfall amounts associated with some of this activity prompted flooding and flash flooding in a few locations. Rainfall totals were a high as 3 inches in Montgomery County.\nEvent Narrative: Standing water forced the closure of Pike Ridge Road. A rain gauge near the event recorded 2.29 inches.", "The following events were reported: Flash Flood, Flood. These occurred near station USW00093721, approximately 19.0392 km away, between 2011-09-07 09:22:00 and 2011-09-08 08:00:00. The flood was caused by Heavy Rain. The events resulted in 0 injuries and 1 fatalities. No significant property or crop damage was reported. \n\nEpisode Narrative: Abnormally moist atmosphere across the mid-Atlantic allowed showers and thunderstorms to produce exceptional rainfall rates across portions of Maryland as the remnants of Tropical Depression Lee interacted with a nearly stationary boundary near the Mason-Dixon line. Major flooding and flash flooding occurred in numerous areas. The highest rainfall and worst flooding happened in a band from Charles County northeastward into Baltimore County. The highest measured rainfall report during this period was 10.70 inches in Anne Arundel County. Abnormally moist atmosphere across the mid-Atlantic allowed showers and thunderstorms to produce exceptional rainfall rates across portions of Maryland as the remnants of Tropical Depression Lee interacted with a nearly stationary boundary near the Mason-Dixon line. Major flooding and flash flooding occurred in numerous areas. The highest rainfall and worst flooding happened in a band from Charles County northeastward into Baltimore County. The highest measured rainfall report during this period was 10.70 inches in Anne Arundel County. Abnormally moist atmosphere across the mid-Atlantic allowed showers and thunderstorms to produce exceptional rainfall rates across portions of Maryland as the remnants of Tropical Depression Lee interacted with a nearly stationary boundary near the Mason-Dixon line. Major flooding and flash flooding occurred in numerous areas. The highest rainfall and worst flooding happened in a band from Charles County northeastward into Baltimore County. The highest measured rainfall report during this period was 10.70 inches in Anne Arundel County. Abnormally moist atmosphere across the mid-Atlantic allowed showers and thunderstorms to produce exceptional rainfall rates across portions of Maryland as the remnants of Tropical Depression Lee interacted with a nearly stationary boundary near the Mason-Dixon line. Major flooding and flash flooding occurred in numerous areas. The highest rainfall and worst flooding happened in a band from Charles County northeastward into Baltimore County. The highest measured rainfall report during this period was 10.70 inches in Anne Arundel County. Abnormally moist atmosphere across the mid-Atlantic allowed showers and thunderstorms to produce exceptional rainfall rates across portions of Maryland as the remnants of Tropical Depression Lee interacted with a nearly stationary boundary near the Mason-Dixon line. Major flooding and flash flooding occurred in numerous areas. The highest rainfall and worst flooding happened in a band from Charles County northeastward into Baltimore County. The highest measured rainfall report during this period was 10.70 inches in Anne Arundel County. Abnormally moist atmosphere across the mid-Atlantic allowed showers and thunderstorms to produce exceptional rainfall rates across portions of Maryland as the remnants of Tropical Depression Lee interacted with a nearly stationary boundary near the Mason-Dixon line. Major flooding and flash flooding occurred in numerous areas. The highest rainfall and worst flooding happened in a band from Charles County northeastward into Baltimore County. The highest measured rainfall report during this period was 10.70 inches in Anne Arundel County. Abnormally moist atmosphere across the mid-Atlantic allowed showers and thunderstorms to produce exceptional rainfall rates across portions of Maryland as the remnants of Tropical Depression Lee interacted with a nearly stationary boundary near the Mason-Dixon line. Major flooding and flash flooding occurred in numerous areas. The highest rainfall and worst flooding happened in a band from Charles County northeastward into Baltimore County. The highest measured rainfall report during this period was 10.70 inches in Anne Arundel County. Abnormally moist atmosphere across the mid-Atlantic allowed showers and thunderstorms to produce exceptional rainfall rates across portions of Maryland as the remnants of Tropical Depression Lee interacted with a nearly stationary boundary near the Mason-Dixon line. Major flooding and flash flooding occurred in numerous areas. The highest rainfall and worst flooding happened in a band from Charles County northeastward into Baltimore County. The highest measured rainfall report during this period was 10.70 inches in Anne Arundel County. Abnormally moist atmosphere across the mid-Atlantic allowed showers and thunderstorms to produce exceptional rainfall rates across portions of Maryland as the remnants of Tropical Depression Lee interacted with a nearly stationary boundary near the Mason-Dixon line. Major flooding and flash flooding occurred in numerous areas. The highest rainfall and worst flooding happened in a band from Charles County northeastward into Baltimore County. The highest measured rainfall report during this period was 10.70 inches in Anne Arundel County. Abnormally moist atmosphere across the mid-Atlantic allowed showers and thunderstorms to produce exceptional rainfall rates across portions of Maryland as the remnants of Tropical Depression Lee interacted with a nearly stationary boundary near the Mason-Dixon line. Major flooding and flash flooding occurred in numerous areas. The highest rainfall and worst flooding happened in a band from Charles County northeastward into Baltimore County. The highest measured rainfall report during this period was 10.70 inches in Anne Arundel County. Abnormally moist atmosphere across the mid-Atlantic allowed showers and thunderstorms to produce exceptional rainfall rates across portions of Maryland as the remnants of Tropical Depression Lee interacted with a nearly stationary boundary near the Mason-Dixon line. Major flooding and flash flooding occurred in numerous areas. The highest rainfall and worst flooding happened in a band from Charles County northeastward into Baltimore County. The highest measured rainfall report during this period was 10.70 inches in Anne Arundel County. Abnormally moist atmosphere across the mid-Atlantic allowed showers and thunderstorms to produce exceptional rainfall rates across portions of Maryland as the remnants of Tropical Depression Lee interacted with a nearly stationary boundary near the Mason-Dixon line. Major flooding and flash flooding occurred in numerous areas. The highest rainfall and worst flooding happened in a band from Charles County northeastward into Baltimore County. The highest measured rainfall report during this period was 10.70 inches in Anne Arundel County. Abnormally moist atmosphere across the mid-Atlantic allowed showers and thunderstorms to produce exceptional rainfall rates across portions of Maryland as the remnants of Tropical Depression Lee interacted with a nearly stationary boundary near the Mason-Dixon line. Major flooding and flash flooding occurred in numerous areas. The highest rainfall and worst flooding happened in a band from Charles County northeastward into Baltimore County. The highest measured rainfall report during this period was 10.70 inches in Anne Arundel County. Abnormally moist atmosphere across the mid-Atlantic allowed showers and thunderstorms to produce exceptional rainfall rates across portions of Maryland as the remnants of Tropical Depression Lee interacted with a nearly stationary boundary near the Mason-Dixon line. Major flooding and flash flooding occurred in numerous areas. The highest rainfall and worst flooding happened in a band from Charles County northeastward into Baltimore County. The highest measured rainfall report during this period was 10.70 inches in Anne Arundel County. Abnormally moist atmosphere across the mid-Atlantic allowed showers and thunderstorms to produce exceptional rainfall rates across portions of Maryland as the remnants of Tropical Depression Lee interacted with a nearly stationary boundary near the Mason-Dixon line. Major flooding and flash flooding occurred in numerous areas. The highest rainfall and worst flooding happened in a band from Charles County northeastward into Baltimore County. The highest measured rainfall report during this period was 10.70 inches in Anne Arundel County. Abnormally moist atmosphere across the mid-Atlantic allowed showers and thunderstorms to produce exceptional rainfall rates across portions of Maryland as the remnants of Tropical Depression Lee interacted with a nearly stationary boundary near the Mason-Dixon line. Major flooding and flash flooding occurred in numerous areas. The highest rainfall and worst flooding happened in a band from Charles County northeastward into Baltimore County. The highest measured rainfall report during this period was 10.70 inches in Anne Arundel County. Abnormally moist atmosphere across the mid-Atlantic allowed showers and thunderstorms to produce exceptional rainfall rates across portions of Maryland as the remnants of Tropical Depression Lee interacted with a nearly stationary boundary near the Mason-Dixon line. Major flooding and flash flooding occurred in numerous areas. The highest rainfall and worst flooding happened in a band from Charles County northeastward into Baltimore County. The highest measured rainfall report during this period was 10.70 inches in Anne Arundel County. Abnormally moist atmosphere across the mid-Atlantic allowed showers and thunderstorms to produce exceptional rainfall rates across portions of Maryland as the remnants of Tropical Depression Lee interacted with a nearly stationary boundary near the Mason-Dixon line. Major flooding and flash flooding occurred in numerous areas. The highest rainfall and worst flooding happened in a band from Charles County northeastward into Baltimore County. The highest measured rainfall report during this period was 10.70 inches in Anne Arundel County. Abnormally moist atmosphere across the mid-Atlantic allowed showers and thunderstorms to produce exceptional rainfall rates across portions of Maryland as the remnants of Tropical Depression Lee interacted with a nearly stationary boundary near the Mason-Dixon line. Major flooding and flash flooding occurred in numerous areas. The highest rainfall and worst flooding happened in a band from Charles County northeastward into Baltimore County. The highest measured rainfall report during this period was 10.70 inches in Anne Arundel County. Abnormally moist atmosphere across the mid-Atlantic allowed showers and thunderstorms to produce exceptional rainfall rates across portions of Maryland as the remnants of Tropical Depression Lee interacted with a nearly stationary boundary near the Mason-Dixon line. Major flooding and flash flooding occurred in numerous areas. The highest rainfall and worst flooding happened in a band from Charles County northeastward into Baltimore County. The highest measured rainfall report during this period was 10.70 inches in Anne Arundel County. Abnormally moist atmosphere across the mid-Atlantic allowed showers and thunderstorms to produce exceptional rainfall rates across portions of Maryland as the remnants of Tropical Depression Lee interacted with a nearly stationary boundary near the Mason-Dixon line. Major flooding and flash flooding occurred in numerous areas. The highest rainfall and worst flooding happened in a band from Charles County northeastward into Baltimore County. The highest measured rainfall report during this period was 10.70 inches in Anne Arundel County. Abnormally moist atmosphere across the mid-Atlantic allowed showers and thunderstorms to produce exceptional rainfall rates across portions of Maryland as the remnants of Tropical Depression Lee interacted with a nearly stationary boundary near the Mason-Dixon line. Major flooding and flash flooding occurred in numerous areas. The highest rainfall and worst flooding happened in a band from Charles County northeastward into Baltimore County. The highest measured rainfall report during this period was 10.70 inches in Anne Arundel County. Abnormally moist atmosphere across the mid-Atlantic allowed showers and thunderstorms to produce exceptional rainfall rates across portions of Maryland as the remnants of Tropical Depression Lee interacted with a nearly stationary boundary near the Mason-Dixon line. Major flooding and flash flooding occurred in numerous areas. The highest rainfall and worst flooding happened in a band from Charles County northeastward into Baltimore County. The highest measured rainfall report during this period was 10.70 inches in Anne Arundel County. Abnormally moist atmosphere across the mid-Atlantic allowed showers and thunderstorms to produce exceptional rainfall rates across portions of Maryland as the remnants of Tropical Depression Lee interacted with a nearly stationary boundary near the Mason-Dixon line. Major flooding and flash flooding occurred in numerous areas. The highest rainfall and worst flooding happened in a band from Charles County northeastward into Baltimore County. The highest measured rainfall report during this period was 10.70 inches in Anne Arundel County. Abnormally moist atmosphere across the mid-Atlantic allowed showers and thunderstorms to produce exceptional rainfall rates across portions of Maryland as the remnants of Tropical Depression Lee interacted with a nearly stationary boundary near the Mason-Dixon line. Major flooding and flash flooding occurred in numerous areas. The highest rainfall and worst flooding happened in a band from Charles County northeastward into Baltimore County. The highest measured rainfall report during this period was 10.70 inches in Anne Arundel County. Abnormally moist atmosphere across the mid-Atlantic allowed showers and thunderstorms to produce exceptional rainfall rates across portions of Maryland as the remnants of Tropical Depression Lee interacted with a nearly stationary boundary near the Mason-Dixon line. Major flooding and flash flooding occurred in numerous areas. The highest rainfall and worst flooding happened in a band from Charles County northeastward into Baltimore County. The highest measured rainfall report during this period was 10.70 inches in Anne Arundel County. Abnormally moist atmosphere across the mid-Atlantic allowed showers and thunderstorms to produce exceptional rainfall rates across portions of Maryland as the remnants of Tropical Depression Lee interacted with a nearly stationary boundary near the Mason-Dixon line. Major flooding and flash flooding occurred in numerous areas. The highest rainfall and worst flooding happened in a band from Charles County northeastward into Baltimore County. The highest measured rainfall report during this period was 10.70 inches in Anne Arundel County. Abnormally moist atmosphere across the mid-Atlantic allowed showers and thunderstorms to produce exceptional rainfall rates across portions of Maryland as the remnants of Tropical Depression Lee interacted with a nearly stationary boundary near the Mason-Dixon line. Major flooding and flash flooding occurred in numerous areas. The highest rainfall and worst flooding happened in a band from Charles County northeastward into Baltimore County. The highest measured rainfall report during this period was 10.70 inches in Anne Arundel County. Abnormally moist atmosphere across the mid-Atlantic allowed showers and thunderstorms to produce exceptional rainfall rates across portions of Maryland as the remnants of Tropical Depression Lee interacted with a nearly stationary boundary near the Mason-Dixon line. Major flooding and flash flooding occurred in numerous areas. The highest rainfall and worst flooding happened in a band from Charles County northeastward into Baltimore County. The highest measured rainfall report during this period was 10.70 inches in Anne Arundel County. Abnormally moist atmosphere across the mid-Atlantic allowed showers and thunderstorms to produce exceptional rainfall rates across portions of Maryland as the remnants of Tropical Depression Lee interacted with a nearly stationary boundary near the Mason-Dixon line. Major flooding and flash flooding occurred in numerous areas. The highest rainfall and worst flooding happened in a band from Charles County northeastward into Baltimore County. The highest measured rainfall report during this period was 10.70 inches in Anne Arundel County. Abnormally moist atmosphere across the mid-Atlantic allowed showers and thunderstorms to produce exceptional rainfall rates across portions of Maryland as the remnants of Tropical Depression Lee interacted with a nearly stationary boundary near the Mason-Dixon line. Major flooding and flash flooding occurred in numerous areas. The highest rainfall and worst flooding happened in a band from Charles County northeastward into Baltimore County. The highest measured rainfall report during this period was 10.70 inches in Anne Arundel County. Abnormally moist atmosphere across the mid-Atlantic allowed showers and thunderstorms to produce exceptional rainfall rates across portions of Maryland as the remnants of Tropical Depression Lee interacted with a nearly stationary boundary near the Mason-Dixon line. Major flooding and flash flooding occurred in numerous areas. The highest rainfall and worst flooding happened in a band from Charles County northeastward into Baltimore County. The highest measured rainfall report during this period was 10.70 inches in Anne Arundel County. Abnormally moist atmosphere across the mid-Atlantic allowed showers and thunderstorms to produce exceptional rainfall rates across portions of Maryland as the remnants of Tropical Depression Lee interacted with a nearly stationary boundary near the Mason-Dixon line. Major flooding and flash flooding occurred in numerous areas. The highest rainfall and worst flooding happened in a band from Charles County northeastward into Baltimore County. The highest measured rainfall report during this period was 10.70 inches in Anne Arundel County. Abnormally moist atmosphere across the mid-Atlantic allowed showers and thunderstorms to produce exceptional rainfall rates across portions of Maryland as the remnants of Tropical Depression Lee interacted with a nearly stationary boundary near the Mason-Dixon line. Major flooding and flash flooding occurred in numerous areas. The highest rainfall and worst flooding happened in a band from Charles County northeastward into Baltimore County. The highest measured rainfall report during this period was 10.70 inches in Anne Arundel County. Abnormally moist atmosphere across the mid-Atlantic allowed showers and thunderstorms to produce exceptional rainfall rates across portions of Maryland as the remnants of Tropical Depression Lee interacted with a nearly stationary boundary near the Mason-Dixon line. Major flooding and flash flooding occurred in numerous areas. The highest rainfall and worst flooding happened in a band from Charles County northeastward into Baltimore County. The highest measured rainfall report during this period was 10.70 inches in Anne Arundel County. Abnormally moist atmosphere across the mid-Atlantic allowed showers and thunderstorms to produce exceptional rainfall rates across portions of Maryland as the remnants of Tropical Depression Lee interacted with a nearly stationary boundary near the Mason-Dixon line. Major flooding and flash flooding occurred in numerous areas. The highest rainfall and worst flooding happened in a band from Charles County northeastward into Baltimore County. The highest measured rainfall report during this period was 10.70 inches in Anne Arundel County.\nEvent Narrative: Route 108 was closed near Thunder Hill due to flash flooding. A nearby rain gauge measured 6.78 inches. Route 1 was completely closed at Ritz Way. A nearby rain gauge measured 7.09 inches. Three inches of water were flowing across Frederick Avenue at its intersection with Rolling and Overbrook Roads. A rain gauge in the vicinity measured 7.67 inches. Portions of Main Street in Ellicott City was evacuated due to high water. A spotter nearby measured 6.33 inches of rain. Route 50 Westbound was closed at Davidsonville Road due to flash flooding. A rain gauge near the event received a total of 7 inches. Valley Mede neighbor was evacuated due to high water. A nearby spotter recorded a storm total of 6.20 inches near the time of this event. Frederick road leading into the east side of Ellicott City is closed due to flash flooding. Water was at a depth above the bumpers of cars. A nearby spotter observed 9.40 inches of rain for a storm total. Route 648 was flooded and closed between Lake Front Drive and Nursery Road. Storm total precipitation at Baltimore-Washington International Airport, nearby, was 7.97 inches. Route 1 was closed in both directions at Assateague Drive. A nearby rain gauge tallied 5.24 inches during the day. The intersection of Slade Avenue and Park Heights Avenue was closed at the Baltimore County and Baltimore City border. A nearby rain gauge had 7.21 inches in it. Route 45 was closed at Beaver Run Lane due to flash flooding. The nearest rain gauge to the event measured 10.09 inches. High water was blocking the northbound lanes of Route 29 between Routes 32 and 175. A spotter in Columbia measured 5.18 inches of rain. Route 145 was closed at Ashland Road due to flash flooding. A nearby rain gauge tallied 6.64 inches. The intersection of Houkes Mill and Turner roads was closed due to flash floodin. A nearby rain gauge recorded 3.84 inches. Route 140 was closed at Kenmar Avenue due to flash flooding. A rain gauge near the event tallied 5.74 inches. Route 450 was closed at Saint Stephens Church Road due to flash flooding. A nearby rain gauge at 6.76 inches. The Little Patuxent River at Volmerhausen Road topped the bridge and flooded it. Paper Mill Road was closed at Poplar Hill Road due to flash flooding. Rainfall in the area was measured at 4.80 inches. Route 7 was closed from Route 136 to Route 543 due to flash flooding. Rainfall near the event was measured at 3.12 inches. Route 198 was closed at the Baltimore-Washington Parkway. A rain gauge near the event recorded 5.98 inches. Multiple roadways were closed in and around Bowie due to flash flooding. A nearby rain gauge totalled 4.53 inches. Intersection of Liberty Parkway and Dunman Way was closed due to flash flooding. A nearby rain gauge measured 4.60 inches. Meritt Boulevard at Rabon Avenue was closed due to flash flooding. North Point Road was closed at German Hill Road due to flash flooding. Route 214 was closed near Beards Point Road due to flash flooding. A nearby rain gauge had a measurement of 5.30 inches. Flash flooding caused landslide on Saint Paul Street. A tree was downed and landslide affected automobiles in the area. Route 176 was closed between Route 648 and Central Avenue due to flooding. A nearby rain gauge had a measurement of 5.16 inches. All westbound lanes of Route 40 west of Saint Johns Lane were closed due to flash flooding. A rain gauge near the event totalled 10.29 inches. Intersection of Roosevelt and Meadowridge Roads closed due to flash flooding. A nearby rain gauge reported 7.70 inches. Route 1 is closed at Patuxent Ridge due to flash flood. A trained spotter measured 7.93 inches of rain near this event. Stevens Forest Road was closed near Broken Land due to flash flooding. A rain gauge recorded 6.54 inches. A 49 year old male drowned in floodwaters of the Magothy River on Riverside Drive. The ramp from Route 295 northbound to Interstate 95 was closed due to flash flooding. A nearby rain gauge measured 4.33 inches. Route 40 was closed at Normandy due to flash flooding. A nearby spotter observed 8.49 inches of rain. State Route 122 ramps were closed at Interstate 695 due to flash flooding. A nearby rain gauge totalled 7.87 inches. Route 103 was closed at Roosevelt Boulevard due to flash flooding.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 31.1866 km away, between 2011-09-07 12:50:00 and 2011-09-07 12:56:00. The events included records with estimated wind gusts of 34.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Low pressure developed over the Ohio Valley while high pressure remained off the East Coast. A southerly flow between these two systems pumped in plenty of moisture across the region. A warm front combined with the deep moisture to produce showers and thunderstorms. Moderate instability behind the warm front caused some thunderstorms to produce gusty winds. Low-level winds caused enough rotation for an isolated thunderstorm to produce a water spout. Low pressure developed over the Ohio Valley while high pressure remained off the East Coast. A southerly flow between these two systems pumped in plenty of moisture across the region. A warm front combined with the deep moisture to produce showers and thunderstorms. Moderate instability behind the warm front caused some thunderstorms to produce gusty winds. Low-level winds caused enough rotation for an isolated thunderstorm to produce a water spout.\nEvent Narrative: Wind gusts in excess of 30 knots were measured at Patapsco Buoy. Wind gusts in excess of 30 knots were measured at the Thomas Point Lighthouse.", "The following events were reported: Flash Flood, Flood. These occurred near station USW00093721, approximately 29.1225 km away, between 2011-09-08 23:35:00 and 2011-09-09 08:00:00. The flood was caused by Heavy Rain. Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Ground across Maryland was saturated from record-setting rainfall on the 7th and 8th. Rich tropical moisture continued to funnel northward into the mid-Atlantic and daytime heating aided in steep enouhg lapse rates to produced additional showers and thunderstorms. Where rain wasn't particularly heavy, ongoing aeral flooding continues, though in areas of heavy rain, additional flash flooding resulted. Storm total precipitation in Anne Arundel County was as high as 12.10 inches, as measured by a trained spotter. Ground across Maryland was saturated from record-setting rainfall on the 7th and 8th. Rich tropical moisture continued to funnel northward into the mid-Atlantic and daytime heating aided in steep enouhg lapse rates to produced additional showers and thunderstorms. Where rain wasn't particularly heavy, ongoing aeral flooding continues, though in areas of heavy rain, additional flash flooding resulted. Storm total precipitation in Anne Arundel County was as high as 12.10 inches, as measured by a trained spotter.\nEvent Narrative: Numerous roadways were closed across Anne Arundel County due to flooding. Baltimore-Washington International Airport received a storm total of 8.11 inches. Route 150 was flooded and closed at Earls Road. A nearby spotter had a storm total rainfall amount of 11.65 inches.", "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00093721, approximately 14.425 km away, between 2011-09-11 14:11:00 and 2011-09-11 20:07:00. The events included records with hailstones measuring 18.0 inches.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 1000.0 and crop damage of 0.0. \n\nEpisode Narrative: Upper-level low pressure triggered showers and thunderstorms on the 11th. A few thunderstorms produced damaging wind gusts and large hail due to colder air aloft associated with the upper-level low. Upper-level low pressure triggered showers and thunderstorms on the 11th. A few thunderstorms produced damaging wind gusts and large hail due to colder air aloft associated with the upper-level low. Upper-level low pressure triggered showers and thunderstorms on the 11th. A few thunderstorms produced damaging wind gusts and large hail due to colder air aloft associated with the upper-level low.\nEvent Narrative: Quarter sized hail was reported at BWI Airport. Quarter sized hail was reported at the BWI Airport. Two trees were down near the intersection of Woodbine Road and Hoods Mill Road.", "The following events were reported: Flash Flood. These occurred near station USW00093721, approximately 27.3002 km away, between 2011-09-23 14:50:00 and 2011-09-23 16:30:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Rich tropical moisture streamed northward up the eastern seaboard, while a shortwave trough pivoted across the Mid-Atlantic as it rotated around a stationary closed upper low pressure over the Great Lakes. A band of moderate to heavy rain set up across much of Maryland, and flood and flash flooding occurred across portions of northern Maryland. Rainfall totals reached as high as 4.48 inches in Baltimore County. Rich tropical moisture streamed northward up the eastern seaboard, while a shortwave trough pivoted across the Mid-Atlantic as it rotated around a stationary closed upper low pressure over the Great Lakes. A band of moderate to heavy rain set up across much of Maryland, and flood and flash flooding occurred across portions of northern Maryland. Rainfall totals reached as high as 4.48 inches in Baltimore County. Rich tropical moisture streamed northward up the eastern seaboard, while a shortwave trough pivoted across the Mid-Atlantic as it rotated around a stationary closed upper low pressure over the Great Lakes. A band of moderate to heavy rain set up across much of Maryland, and flood and flash flooding occurred across portions of northern Maryland. Rainfall totals reached as high as 4.48 inches in Baltimore County. Rich tropical moisture streamed northward up the eastern seaboard, while a shortwave trough pivoted across the Mid-Atlantic as it rotated around a stationary closed upper low pressure over the Great Lakes. A band of moderate to heavy rain set up across much of Maryland, and flood and flash flooding occurred across portions of northern Maryland. Rainfall totals reached as high as 4.48 inches in Baltimore County.\nEvent Narrative: Route 1 was flooded and closed at Ridgely's Choice Drive. A nearby observed recorded 4.13 inches. Route 147 was flooded and closed near Cowen Run north of Notch Cliff. An observed nearby measured a total of 2.92 inches. Route 176 was closed at Route 648 at Sawmill Creek due to flash flooding. A nearby spotter measured 3.57 inches of rain. Route 1 was closed north of New Cut Road due to flash flooding on Little Gunpowder Falls. A nearby spotter observed 2.80 inches of rain.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 45.9012 km away, between 2011-10-14 10:02:00 and 2011-10-14 10:02:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 1000.0 and crop damage of 0.0. \n\nEpisode Narrative: A cold front passed through Maryland on the 14th. Moderate instability along with forcing associated with the front caused a couple thunderstorms to become severe.\nEvent Narrative: A fifteen-foot pine tree was down due to thunderstorm winds.", "The following events were reported: Flood. These occurred near station USW00093721, approximately 21.3134 km away, between 2011-12-07 19:45:00 and 2011-12-08 05:00:00. The flood was caused by Heavy Rain. Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front stalled across southern Virginia and along the Mid-Atlantic seaboard. Several weak low pressure systems moved along the boundary, with an intense low pressure passing along it on the afternoon of the 7th. An extended period of moderate to heavy rain resulted across portions of Maryland. Rainfall amounts reached as high as 4.36 in Prince Georges County. A cold front stalled across southern Virginia and along the Mid-Atlantic seaboard. Several weak low pressure systems moved along the boundary, with an intense low pressure passing along it on the afternoon of the 7th. An extended period of moderate to heavy rain resulted across portions of Maryland. Rainfall amounts reached as high as 4.36 in Prince Georges County. A cold front stalled across southern Virginia and along the Mid-Atlantic seaboard. Several weak low pressure systems moved along the boundary, with an intense low pressure passing along it on the afternoon of the 7th. An extended period of moderate to heavy rain resulted across portions of Maryland. Rainfall amounts reached as high as 4.36 in Prince Georges County. A cold front stalled across southern Virginia and along the Mid-Atlantic seaboard. Several weak low pressure systems moved along the boundary, with an intense low pressure passing along it on the afternoon of the 7th. An extended period of moderate to heavy rain resulted across portions of Maryland. Rainfall amounts reached as high as 4.36 in Prince Georges County. A cold front stalled across southern Virginia and along the Mid-Atlantic seaboard. Several weak low pressure systems moved along the boundary, with an intense low pressure passing along it on the afternoon of the 7th. An extended period of moderate to heavy rain resulted across portions of Maryland. Rainfall amounts reached as high as 4.36 in Prince Georges County. A cold front stalled across southern Virginia and along the Mid-Atlantic seaboard. Several weak low pressure systems moved along the boundary, with an intense low pressure passing along it on the afternoon of the 7th. An extended period of moderate to heavy rain resulted across portions of Maryland. Rainfall amounts reached as high as 4.36 in Prince Georges County.\nEvent Narrative: High water rescue was performed at Baltimore Avenue near Ammendale Road. A rain gauge near Brandywine tallied 4.27 inches. Portion of West Patapsco Avenue was closed due to high water. A rain gauge near Hamilton observed 2.55 inches. Ruxton Road was closed due to high water. A rain gauge near Towson measured 2.62 inches. Portion of Ebony Road was closed due to high water. A rain gauge near Catonsville tallied 2.56 inches. Furnace Avenue was closed near the Anne Arundel County line due to flooding. A rain gauge near Savage observed 2.60 inches. Florence Road was closed near Mullinix Mill Road due to flooding. A rain gauge near Columbia tallied 2.42 inches.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 32.4436 km away, between 2012-01-27 08:22:00 and 2012-01-27 14:00:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A strong cold front passed through waters during the morning hours of the 27th. Despite limited instability, winds aloft were strong just a few thousand feet from the surface. Showers and isolated thunderstorms were able to mix down some of the gusty winds from aloft. A strong cold front passed through waters during the morning hours of the 27th. Despite limited instability, winds aloft were strong just a few thousand feet from the surface. Showers and isolated thunderstorms were able to mix down some of the gusty winds from aloft. A strong cold front passed through waters during the morning hours of the 27th. Despite limited instability, winds aloft were strong just a few thousand feet from the surface. Showers and isolated thunderstorms were able to mix down some of the gusty winds from aloft. A strong cold front passed through waters during the morning hours of the 27th. Despite limited instability, winds aloft were strong just a few thousand feet from the surface. Showers and isolated thunderstorms were able to mix down some of the gusty winds from aloft. A strong cold front passed through waters during the morning hours of the 27th. Despite limited instability, winds aloft were strong just a few thousand feet from the surface. Showers and isolated thunderstorms were able to mix down some of the gusty winds from aloft. A strong cold front passed through waters during the morning hours of the 27th. Despite limited instability, winds aloft were strong just a few thousand feet from the surface. Showers and isolated thunderstorms were able to mix down some of the gusty winds from aloft. A strong cold front passed through waters during the morning hours of the 27th. Despite limited instability, winds aloft were strong just a few thousand feet from the surface. Showers and isolated thunderstorms were able to mix down some of the gusty winds from aloft. A strong cold front passed through waters during the morning hours of the 27th. Despite limited instability, winds aloft were strong just a few thousand feet from the surface. Showers and isolated thunderstorms were able to mix down some of the gusty winds from aloft.\nEvent Narrative: A wind gust of 34 knots was reported at Miller Island. A wind gust in excess of 30 knots was reported at Sandy Point. A wind gust in excess of 30 knots was reported at Sandy Point. A wind gust in excess of 30 knots was reported at Thomas Point Lighthouse. A wind gust in excess of 30 knots was reported at Greenberry Point. A wind gust of 35 knots was reported at Greenberry Point. A wind gust of 35 knots was reported at Tolly Point. A wind gust of 36 knots was reported at Thomas Point Lighthouse.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 30.371 km away, between 2012-01-29 23:06:00 and 2012-01-30 00:00:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A strong cold front passed through waters during late evening of the 29th into the early morning of the 30th. Rain and snow showers associated with the cold front produced gusty winds. A strong cold front passed through waters during late evening of the 29th into the early morning of the 30th. Rain and snow showers associated with the cold front produced gusty winds. A strong cold front passed through waters during late evening of the 29th into the early morning of the 30th. Rain and snow showers associated with the cold front produced gusty winds. A strong cold front passed through waters during late evening of the 29th into the early morning of the 30th. Rain and snow showers associated with the cold front produced gusty winds. A strong cold front passed through waters during late evening of the 29th into the early morning of the 30th. Rain and snow showers associated with the cold front produced gusty winds. A strong cold front passed through waters during late evening of the 29th into the early morning of the 30th. Rain and snow showers associated with the cold front produced gusty winds.\nEvent Narrative: Wind gusts up to 37 knots were reported at Key Bridge. A wind gust of 34 knots was reported at Miller Island. Wind gusts in excess of 30 knots were reported at Tolchester Beach. Wind gusts in excess of 30 knots were reported at Greenbury Point. A wind gust of 38 knots was reported at Thomas Point Lighthouse. Wind gusts in excess of 30 knots were reported at Greenbury Point.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 31.253 km away, between 2012-02-11 16:12:00 and 2012-02-11 18:12:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: An upper-level trough passed through the waters on the 11th. Cold air aloft associated with the trough provided limited instability. The instability trigger showers over the waters and some of the showers were able to mix down gusty winds from aloft. An upper-level trough passed through the waters on the 11th. Cold air aloft associated with the trough provided limited instability. The instability trigger showers over the waters and some of the showers were able to mix down gusty winds from aloft. An upper-level trough passed through the waters on the 11th. Cold air aloft associated with the trough provided limited instability. The instability trigger showers over the waters and some of the showers were able to mix down gusty winds from aloft. An upper-level trough passed through the waters on the 11th. Cold air aloft associated with the trough provided limited instability. The instability trigger showers over the waters and some of the showers were able to mix down gusty winds from aloft. An upper-level trough passed through the waters on the 11th. Cold air aloft associated with the trough provided limited instability. The instability trigger showers over the waters and some of the showers were able to mix down gusty winds from aloft. An upper-level trough passed through the waters on the 11th. Cold air aloft associated with the trough provided limited instability. The instability trigger showers over the waters and some of the showers were able to mix down gusty winds from aloft.\nEvent Narrative: A wind gust in excess of 30 knots was measured at the Francis Scott Key Bridge. A wind gust in excess of 30 knots was reported at Greenbury Point. Wind gusts up to 36 knots were reported at Tolchester Beach. Wind gusts up to 36 knots were reported at Tolchester Beach. A wind gust of 36 knots was reported at the Thomas Point Lighthouse. A wind gust in excess of 30 knots was measured at Greenbury Point.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 14.2666 km away, between 2012-03-09 01:00:00 and 2012-03-09 01:06:00. The events included records with estimated wind gusts of 34.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front passed through the waters on the 9th. Strong forcing combined with limited instability, causing showers to develop. An isolated shower produced gusty winds.\nEvent Narrative: A wind gust in excess of 30 knots was reported at Key Bridge.", "The following events were reported: Hail, Thunderstorm Wind, Tornado. These occurred near station USW00093721, approximately 22.8075 km away, between 2012-06-01 13:48:00 and 2012-06-01 18:45:00. The events included records with hailstones measuring 53.733870967741936 inches.The events resulted in 2 injuries and 0 fatalities. The events caused property damage valued at 751500.0 and crop damage of 0.0. \n\nEpisode Narrative: Low pressure tracked through the Ohio Valley and into the Great Lakes. The warm front associated with this system passed through our region during the first. Plenty of moisture from the Gulf of Mexico and the Atlantic Ocean combined with strong forcing associated with the warm front, causing thunderstorms to develop. Moderate instability along with strong forcing caused some thunderstorms to become severe. ||Wind speed and direction changed rapidly with height near the warm front. This caused rotating thunderstorms, and some of them were able to produce tornadoes. Low pressure tracked through the Ohio Valley and into the Great Lakes. The warm front associated with this system passed through our region during the first. Plenty of moisture from the Gulf of Mexico and the Atlantic Ocean combined with strong forcing associated with the warm front, causing thunderstorms to develop. Moderate instability along with strong forcing caused some thunderstorms to become severe. ||Wind speed and direction changed rapidly with height near the warm front. This caused rotating thunderstorms, and some of them were able to produce tornadoes. Low pressure tracked through the Ohio Valley and into the Great Lakes. The warm front associated with this system passed through our region during the first. Plenty of moisture from the Gulf of Mexico and the Atlantic Ocean combined with strong forcing associated with the warm front, causing thunderstorms to develop. Moderate instability along with strong forcing caused some thunderstorms to become severe. ||Wind speed and direction changed rapidly with height near the warm front. This caused rotating thunderstorms, and some of them were able to produce tornadoes. Low pressure tracked through the Ohio Valley and into the Great Lakes. The warm front associated with this system passed through our region during the first. Plenty of moisture from the Gulf of Mexico and the Atlantic Ocean combined with strong forcing associated with the warm front, causing thunderstorms to develop. Moderate instability along with strong forcing caused some thunderstorms to become severe. ||Wind speed and direction changed rapidly with height near the warm front. This caused rotating thunderstorms, and some of them were able to produce tornadoes. Low pressure tracked through the Ohio Valley and into the Great Lakes. The warm front associated with this system passed through our region during the first. Plenty of moisture from the Gulf of Mexico and the Atlantic Ocean combined with strong forcing associated with the warm front, causing thunderstorms to develop. Moderate instability along with strong forcing caused some thunderstorms to become severe. ||Wind speed and direction changed rapidly with height near the warm front. This caused rotating thunderstorms, and some of them were able to produce tornadoes. Low pressure tracked through the Ohio Valley and into the Great Lakes. The warm front associated with this system passed through our region during the first. Plenty of moisture from the Gulf of Mexico and the Atlantic Ocean combined with strong forcing associated with the warm front, causing thunderstorms to develop. Moderate instability along with strong forcing caused some thunderstorms to become severe. ||Wind speed and direction changed rapidly with height near the warm front. This caused rotating thunderstorms, and some of them were able to produce tornadoes. Low pressure tracked through the Ohio Valley and into the Great Lakes. The warm front associated with this system passed through our region during the first. Plenty of moisture from the Gulf of Mexico and the Atlantic Ocean combined with strong forcing associated with the warm front, causing thunderstorms to develop. Moderate instability along with strong forcing caused some thunderstorms to become severe. ||Wind speed and direction changed rapidly with height near the warm front. This caused rotating thunderstorms, and some of them were able to produce tornadoes. Low pressure tracked through the Ohio Valley and into the Great Lakes. The warm front associated with this system passed through our region during the first. Plenty of moisture from the Gulf of Mexico and the Atlantic Ocean combined with strong forcing associated with the warm front, causing thunderstorms to develop. Moderate instability along with strong forcing caused some thunderstorms to become severe. ||Wind speed and direction changed rapidly with height near the warm front. This caused rotating thunderstorms, and some of them were able to produce tornadoes. Low pressure tracked through the Ohio Valley and into the Great Lakes. The warm front associated with this system passed through our region during the first. Plenty of moisture from the Gulf of Mexico and the Atlantic Ocean combined with strong forcing associated with the warm front, causing thunderstorms to develop. Moderate instability along with strong forcing caused some thunderstorms to become severe. ||Wind speed and direction changed rapidly with height near the warm front. This caused rotating thunderstorms, and some of them were able to produce tornadoes. Low pressure tracked through the Ohio Valley and into the Great Lakes. The warm front associated with this system passed through our region during the first. Plenty of moisture from the Gulf of Mexico and the Atlantic Ocean combined with strong forcing associated with the warm front, causing thunderstorms to develop. Moderate instability along with strong forcing caused some thunderstorms to become severe. ||Wind speed and direction changed rapidly with height near the warm front. This caused rotating thunderstorms, and some of them were able to produce tornadoes. Low pressure tracked through the Ohio Valley and into the Great Lakes. The warm front associated with this system passed through our region during the first. Plenty of moisture from the Gulf of Mexico and the Atlantic Ocean combined with strong forcing associated with the warm front, causing thunderstorms to develop. Moderate instability along with strong forcing caused some thunderstorms to become severe. ||Wind speed and direction changed rapidly with height near the warm front. This caused rotating thunderstorms, and some of them were able to produce tornadoes. Low pressure tracked through the Ohio Valley and into the Great Lakes. The warm front associated with this system passed through our region during the first. Plenty of moisture from the Gulf of Mexico and the Atlantic Ocean combined with strong forcing associated with the warm front, causing thunderstorms to develop. Moderate instability along with strong forcing caused some thunderstorms to become severe. ||Wind speed and direction changed rapidly with height near the warm front. This caused rotating thunderstorms, and some of them were able to produce tornadoes. Low pressure tracked through the Ohio Valley and into the Great Lakes. The warm front associated with this system passed through our region during the first. Plenty of moisture from the Gulf of Mexico and the Atlantic Ocean combined with strong forcing associated with the warm front, causing thunderstorms to develop. Moderate instability along with strong forcing caused some thunderstorms to become severe. ||Wind speed and direction changed rapidly with height near the warm front. This caused rotating thunderstorms, and some of them were able to produce tornadoes. Low pressure tracked through the Ohio Valley and into the Great Lakes. The warm front associated with this system passed through our region during the first. Plenty of moisture from the Gulf of Mexico and the Atlantic Ocean combined with strong forcing associated with the warm front, causing thunderstorms to develop. Moderate instability along with strong forcing caused some thunderstorms to become severe. ||Wind speed and direction changed rapidly with height near the warm front. This caused rotating thunderstorms, and some of them were able to produce tornadoes. Low pressure tracked through the Ohio Valley and into the Great Lakes. The warm front associated with this system passed through our region during the first. Plenty of moisture from the Gulf of Mexico and the Atlantic Ocean combined with strong forcing associated with the warm front, causing thunderstorms to develop. Moderate instability along with strong forcing caused some thunderstorms to become severe. ||Wind speed and direction changed rapidly with height near the warm front. This caused rotating thunderstorms, and some of them were able to produce tornadoes. Low pressure tracked through the Ohio Valley and into the Great Lakes. The warm front associated with this system passed through our region during the first. Plenty of moisture from the Gulf of Mexico and the Atlantic Ocean combined with strong forcing associated with the warm front, causing thunderstorms to develop. Moderate instability along with strong forcing caused some thunderstorms to become severe. ||Wind speed and direction changed rapidly with height near the warm front. This caused rotating thunderstorms, and some of them were able to produce tornadoes. Low pressure tracked through the Ohio Valley and into the Great Lakes. The warm front associated with this system passed through our region during the first. Plenty of moisture from the Gulf of Mexico and the Atlantic Ocean combined with strong forcing associated with the warm front, causing thunderstorms to develop. Moderate instability along with strong forcing caused some thunderstorms to become severe. ||Wind speed and direction changed rapidly with height near the warm front. This caused rotating thunderstorms, and some of them were able to produce tornadoes. Low pressure tracked through the Ohio Valley and into the Great Lakes. The warm front associated with this system passed through our region during the first. Plenty of moisture from the Gulf of Mexico and the Atlantic Ocean combined with strong forcing associated with the warm front, causing thunderstorms to develop. Moderate instability along with strong forcing caused some thunderstorms to become severe. ||Wind speed and direction changed rapidly with height near the warm front. This caused rotating thunderstorms, and some of them were able to produce tornadoes. Low pressure tracked through the Ohio Valley and into the Great Lakes. The warm front associated with this system passed through our region during the first. Plenty of moisture from the Gulf of Mexico and the Atlantic Ocean combined with strong forcing associated with the warm front, causing thunderstorms to develop. Moderate instability along with strong forcing caused some thunderstorms to become severe. ||Wind speed and direction changed rapidly with height near the warm front. This caused rotating thunderstorms, and some of them were able to produce tornadoes. Low pressure tracked through the Ohio Valley and into the Great Lakes. The warm front associated with this system passed through our region during the first. Plenty of moisture from the Gulf of Mexico and the Atlantic Ocean combined with strong forcing associated with the warm front, causing thunderstorms to develop. Moderate instability along with strong forcing caused some thunderstorms to become severe. ||Wind speed and direction changed rapidly with height near the warm front. This caused rotating thunderstorms, and some of them were able to produce tornadoes. Low pressure tracked through the Ohio Valley and into the Great Lakes. The warm front associated with this system passed through our region during the first. Plenty of moisture from the Gulf of Mexico and the Atlantic Ocean combined with strong forcing associated with the warm front, causing thunderstorms to develop. Moderate instability along with strong forcing caused some thunderstorms to become severe. ||Wind speed and direction changed rapidly with height near the warm front. This caused rotating thunderstorms, and some of them were able to produce tornadoes. Low pressure tracked through the Ohio Valley and into the Great Lakes. The warm front associated with this system passed through our region during the first. Plenty of moisture from the Gulf of Mexico and the Atlantic Ocean combined with strong forcing associated with the warm front, causing thunderstorms to develop. Moderate instability along with strong forcing caused some thunderstorms to become severe. ||Wind speed and direction changed rapidly with height near the warm front. This caused rotating thunderstorms, and some of them were able to produce tornadoes. Low pressure tracked through the Ohio Valley and into the Great Lakes. The warm front associated with this system passed through our region during the first. Plenty of moisture from the Gulf of Mexico and the Atlantic Ocean combined with strong forcing associated with the warm front, causing thunderstorms to develop. Moderate instability along with strong forcing caused some thunderstorms to become severe. ||Wind speed and direction changed rapidly with height near the warm front. This caused rotating thunderstorms, and some of them were able to produce tornadoes. Low pressure tracked through the Ohio Valley and into the Great Lakes. The warm front associated with this system passed through our region during the first. Plenty of moisture from the Gulf of Mexico and the Atlantic Ocean combined with strong forcing associated with the warm front, causing thunderstorms to develop. Moderate instability along with strong forcing caused some thunderstorms to become severe. ||Wind speed and direction changed rapidly with height near the warm front. This caused rotating thunderstorms, and some of them were able to produce tornadoes. Low pressure tracked through the Ohio Valley and into the Great Lakes. The warm front associated with this system passed through our region during the first. Plenty of moisture from the Gulf of Mexico and the Atlantic Ocean combined with strong forcing associated with the warm front, causing thunderstorms to develop. Moderate instability along with strong forcing caused some thunderstorms to become severe. ||Wind speed and direction changed rapidly with height near the warm front. This caused rotating thunderstorms, and some of them were able to produce tornadoes. Low pressure tracked through the Ohio Valley and into the Great Lakes. The warm front associated with this system passed through our region during the first. Plenty of moisture from the Gulf of Mexico and the Atlantic Ocean combined with strong forcing associated with the warm front, causing thunderstorms to develop. Moderate instability along with strong forcing caused some thunderstorms to become severe. ||Wind speed and direction changed rapidly with height near the warm front. This caused rotating thunderstorms, and some of them were able to produce tornadoes. Low pressure tracked through the Ohio Valley and into the Great Lakes. The warm front associated with this system passed through our region during the first. Plenty of moisture from the Gulf of Mexico and the Atlantic Ocean combined with strong forcing associated with the warm front, causing thunderstorms to develop. Moderate instability along with strong forcing caused some thunderstorms to become severe. ||Wind speed and direction changed rapidly with height near the warm front. This caused rotating thunderstorms, and some of them were able to produce tornadoes. Low pressure tracked through the Ohio Valley and into the Great Lakes. The warm front associated with this system passed through our region during the first. Plenty of moisture from the Gulf of Mexico and the Atlantic Ocean combined with strong forcing associated with the warm front, causing thunderstorms to develop. Moderate instability along with strong forcing caused some thunderstorms to become severe. ||Wind speed and direction changed rapidly with height near the warm front. This caused rotating thunderstorms, and some of them were able to produce tornadoes. Low pressure tracked through the Ohio Valley and into the Great Lakes. The warm front associated with this system passed through our region during the first. Plenty of moisture from the Gulf of Mexico and the Atlantic Ocean combined with strong forcing associated with the warm front, causing thunderstorms to develop. Moderate instability along with strong forcing caused some thunderstorms to become severe. ||Wind speed and direction changed rapidly with height near the warm front. This caused rotating thunderstorms, and some of them were able to produce tornadoes. Low pressure tracked through the Ohio Valley and into the Great Lakes. The warm front associated with this system passed through our region during the first. Plenty of moisture from the Gulf of Mexico and the Atlantic Ocean combined with strong forcing associated with the warm front, causing thunderstorms to develop. Moderate instability along with strong forcing caused some thunderstorms to become severe. ||Wind speed and direction changed rapidly with height near the warm front. This caused rotating thunderstorms, and some of them were able to produce tornadoes. Low pressure tracked through the Ohio Valley and into the Great Lakes. The warm front associated with this system passed through our region during the first. Plenty of moisture from the Gulf of Mexico and the Atlantic Ocean combined with strong forcing associated with the warm front, causing thunderstorms to develop. Moderate instability along with strong forcing caused some thunderstorms to become severe. ||Wind speed and direction changed rapidly with height near the warm front. This caused rotating thunderstorms, and some of them were able to produce tornadoes. Low pressure tracked through the Ohio Valley and into the Great Lakes. The warm front associated with this system passed through our region during the first. Plenty of moisture from the Gulf of Mexico and the Atlantic Ocean combined with strong forcing associated with the warm front, causing thunderstorms to develop. Moderate instability along with strong forcing caused some thunderstorms to become severe. ||Wind speed and direction changed rapidly with height near the warm front. This caused rotating thunderstorms, and some of them were able to produce tornadoes. Low pressure tracked through the Ohio Valley and into the Great Lakes. The warm front associated with this system passed through our region during the first. Plenty of moisture from the Gulf of Mexico and the Atlantic Ocean combined with strong forcing associated with the warm front, causing thunderstorms to develop. Moderate instability along with strong forcing caused some thunderstorms to become severe. ||Wind speed and direction changed rapidly with height near the warm front. This caused rotating thunderstorms, and some of them were able to produce tornadoes. Low pressure tracked through the Ohio Valley and into the Great Lakes. The warm front associated with this system passed through our region during the first. Plenty of moisture from the Gulf of Mexico and the Atlantic Ocean combined with strong forcing associated with the warm front, causing thunderstorms to develop. Moderate instability along with strong forcing caused some thunderstorms to become severe. ||Wind speed and direction changed rapidly with height near the warm front. This caused rotating thunderstorms, and some of them were able to produce tornadoes. Low pressure tracked through the Ohio Valley and into the Great Lakes. The warm front associated with this system passed through our region during the first. Plenty of moisture from the Gulf of Mexico and the Atlantic Ocean combined with strong forcing associated with the warm front, causing thunderstorms to develop. Moderate instability along with strong forcing caused some thunderstorms to become severe. ||Wind speed and direction changed rapidly with height near the warm front. This caused rotating thunderstorms, and some of them were able to produce tornadoes. Low pressure tracked through the Ohio Valley and into the Great Lakes. The warm front associated with this system passed through our region during the first. Plenty of moisture from the Gulf of Mexico and the Atlantic Ocean combined with strong forcing associated with the warm front, causing thunderstorms to develop. Moderate instability along with strong forcing caused some thunderstorms to become severe. ||Wind speed and direction changed rapidly with height near the warm front. This caused rotating thunderstorms, and some of them were able to produce tornadoes. Low pressure tracked through the Ohio Valley and into the Great Lakes. The warm front associated with this system passed through our region during the first. Plenty of moisture from the Gulf of Mexico and the Atlantic Ocean combined with strong forcing associated with the warm front, causing thunderstorms to develop. Moderate instability along with strong forcing caused some thunderstorms to become severe. ||Wind speed and direction changed rapidly with height near the warm front. This caused rotating thunderstorms, and some of them were able to produce tornadoes. Low pressure tracked through the Ohio Valley and into the Great Lakes. The warm front associated with this system passed through our region during the first. Plenty of moisture from the Gulf of Mexico and the Atlantic Ocean combined with strong forcing associated with the warm front, causing thunderstorms to develop. Moderate instability along with strong forcing caused some thunderstorms to become severe. ||Wind speed and direction changed rapidly with height near the warm front. This caused rotating thunderstorms, and some of them were able to produce tornadoes.\nEvent Narrative: Strong thunderstorm winds caused damage at the Fort Meade Commissary. Trees were blown down by strong thunderstorm winds. Initial tree damage was noted in the Stoneybrook Community along Streamside Drive. The tornado crossed Mountain Road and then traveled along the many Strip Malls and Businesses along the Route 1-Belair Road Corridor in Pleasant Hills. Many downed trees and business signs were blown out. Roof and siding damage was also noted on several properties. ||A dentist office in Bel Air lost a portion of its roof. Some signs and debris were carried a half mile along the tornado track. ||The tornado reached its peak intensity along West Grove Avenue and Eutaw Place. The businesses in this area were severely damaged. Warehouses had their front doors and windows blown out and then had significant roof and wall damage as winds exited the structures. A light pickup truck was picked up by the wind and overturned. A small office and storage concrete block structure was unroofed and then had its walls blown in. The falling blocks fell on two men sheltering inside who were injured. ||A nearby Wal-Mart parking lot had street sign and some tree damage. The tornado created chaotic tree damage along Harford Road just west of Connelly Road in a residential area before lifting. A swath of mainly tree damage south of the tornado track appear to have been caused by winds from a rear flank downdraft. Trees were blown down by strong thunderstorm winds. Trees were blown down along Chinquapin Parkway. Damage encountered along the circulation path was primarily trees, consisting of uprooted and snapped trees and limbs. ||Minor damage was noted to eaves and siding at an apartment complex along Disney Road, where tree damage was also found. Damage to trees was encountered along Carriage drive, Golden Pine Circle and Gesna Road, and to trees and house siding along Fairbanks Drive. A sun room on one house in this area suffered uplift of a portion of its roof, but uplift appears to be the result in large part of channeled wind. ||A decaying tornado was observed by tower personnel and airport patrons crossing the western portion of a runway. The report was taken during the NWS Storm Survey of the Scaggsville tornado. Trees were knocked down near the intersection of Rustling Leaf and Snowden River Parkway. Multiple trees were blown down near the intersection of Old Annapolis Rd. and Red Branch Rd. Large tree limbs were knocked down along Clipper Mill Rd. Trees were blown down by strong thunderstorm winds. Multiple trees were knocked down near the intersection of Broken Land Parkway and Cradlerock Way. A tree was blocking the roadway near the intersection of Route 1 and Rowanberry Dr. A tree fell onto a house along Westchester Avenue. Trees were blown down by strong thunderstorm winds. Trees were knocked down by strong thunderstorm winds along Druid Park Dr. Large tree limbs were blown down along Cloverhill Rd. Trees were blown down by strong thunderstorm winds. Trees were blown down along Halwyn Ave. Trees were blown down along Deepdene Rd. The tornado produced sporadic damage near Twin Arch road. There were about two dozen trees uprooted along with large limbs snapped. Intitial tornado damage occurred to trees along west Watersville Road just north of Old Frederick Road. The tornado tracked northeast across a large wooded area of West Watersville Road where a swath of large Hardwood trees were either snapped or uprooted. ||An area of intense damage consistent with EF-1 level winds was noted in the 500 Block of West Watersville Road where 30 to 40 large Hardwood trees up to two feet in diameter were uprooted or snapped twenty feet up. The tornado snapped and uprooted several trees along the 2600 Block of Bird View Road. The most concentrated damage was focused along and north off Green Mill Road where numerous hardwood trees were uprooted and snapped, with some tree trunk diameters in excess of two feet. A tree fell onto a house, leaving that residence uninhabitable. ||The tornado tracked across MD State Route 140, after passing near the Finksburg Library, producing scattered tree damage. Large tree limbs were knocked down from strong thunderstorm winds. Large tree limbs were blown down along Putney Way. Trees were knocked down along Dartmouth Rd. A tree was blown down along Maryland 147 between Glen Arm and Fort Rd. Trees were blown down along Interstate 83. Large trees were uprooted and snapped in the area of Fellowship Forest. Several of the trees fell onto houses. A large tree was uprooted along Stevenson Lane. The tornado topped a few trees in a neighborhood just north of Hammond Middle School and south of the 10500 Block of Gorman Road. ||The tornado uprooted and topped trees at the end of Broad Cloth Way. The most intense damage was in the 7400 Block of Weather Worn Way near the intersection with Eden Brook Drive, where about two dozen mature hardwood trees were uprooted and snapped behind two homes. There was roof damage to a house after a large tree fell onto it, and another home across fro a Day Care Center on Eden Brook had its chimney blown over. ||After passing north of Eden Brook Driver near First League, tornado damage was more intermittent, with several trees topped. One large limb fell on a house on Kindler Road at Single Wheel Path. The tornado lifted before crossing Route 32. An eyewitness on Route 32 near Interstate 95 approximately two miles away observed the tornado just before it lifted. Damage consisted entirely of uprooted and snapped healthy trees along a brief and concentrated path that began near Lemon Bridge Road and Wildlife Loop South and ended near South Road and Wildlife South. In this portion of the forest, several trees were uprooted or snapped, with other adjacent trees exhibiting snapped limbs. Trees were blown down along Burleith Ave. Trees were blown down by strong thunderstorm winds. A large tree fell on a home along Chestnut Ave. There was damage from trees blown down by strong thunderstorm winds at the Pine Ridge Golf Course and the adjacent neighborhood. Two trees were blown down near Coon Club Road at Academy Drive.", "The following events were reported: Flash Flood, Flood. These occurred near station USW00093721, approximately 29.9459 km away, between 2012-06-01 14:55:00 and 2012-06-02 05:00:00. The flood was caused by Heavy Rain. Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Low pressure tracked through the Ohio Valley and into the Great Lakes. The warm front associated with this system passed through our region during the first. Plenty of moisture from the Gulf of Mexico and the Atlantic Ocean combined with strong forcing associated with the warm front, causing thunderstorms to develop. Nearly saturated low levels and training activity supported very heavy rainfall and flash flooding was reported. The highest rainfall total observed in Baltimore County, where 4.56 inches of rain was recorded. Low pressure tracked through the Ohio Valley and into the Great Lakes. The warm front associated with this system passed through our region during the first. Plenty of moisture from the Gulf of Mexico and the Atlantic Ocean combined with strong forcing associated with the warm front, causing thunderstorms to develop. Nearly saturated low levels and training activity supported very heavy rainfall and flash flooding was reported. The highest rainfall total observed in Baltimore County, where 4.56 inches of rain was recorded. Low pressure tracked through the Ohio Valley and into the Great Lakes. The warm front associated with this system passed through our region during the first. Plenty of moisture from the Gulf of Mexico and the Atlantic Ocean combined with strong forcing associated with the warm front, causing thunderstorms to develop. Nearly saturated low levels and training activity supported very heavy rainfall and flash flooding was reported. The highest rainfall total observed in Baltimore County, where 4.56 inches of rain was recorded. Low pressure tracked through the Ohio Valley and into the Great Lakes. The warm front associated with this system passed through our region during the first. Plenty of moisture from the Gulf of Mexico and the Atlantic Ocean combined with strong forcing associated with the warm front, causing thunderstorms to develop. Nearly saturated low levels and training activity supported very heavy rainfall and flash flooding was reported. The highest rainfall total observed in Baltimore County, where 4.56 inches of rain was recorded. Low pressure tracked through the Ohio Valley and into the Great Lakes. The warm front associated with this system passed through our region during the first. Plenty of moisture from the Gulf of Mexico and the Atlantic Ocean combined with strong forcing associated with the warm front, causing thunderstorms to develop. Nearly saturated low levels and training activity supported very heavy rainfall and flash flooding was reported. The highest rainfall total observed in Baltimore County, where 4.56 inches of rain was recorded. Low pressure tracked through the Ohio Valley and into the Great Lakes. The warm front associated with this system passed through our region during the first. Plenty of moisture from the Gulf of Mexico and the Atlantic Ocean combined with strong forcing associated with the warm front, causing thunderstorms to develop. Nearly saturated low levels and training activity supported very heavy rainfall and flash flooding was reported. The highest rainfall total observed in Baltimore County, where 4.56 inches of rain was recorded. Low pressure tracked through the Ohio Valley and into the Great Lakes. The warm front associated with this system passed through our region during the first. Plenty of moisture from the Gulf of Mexico and the Atlantic Ocean combined with strong forcing associated with the warm front, causing thunderstorms to develop. Nearly saturated low levels and training activity supported very heavy rainfall and flash flooding was reported. The highest rainfall total observed in Baltimore County, where 4.56 inches of rain was recorded.\nEvent Narrative: Route 564 was closed at Greenbelt due to flash flooding. Rainfall totals were as high at 1.90. Route 144 at Nine Mile Circle was closed due to flash flooding. Nearby spotters observed 2.72 inches. Interstate 695 was closed at Exit 26 due to flash flooding. A nearby rain gauge recorded 3.84 inches. Route 147 from Fork Road to Glen Arm Road was closed due to flash flooding. A nearby spotter observed 2.72 inches of rain. Sandymount Road was closed near Baltimore Boulevard. A nearby rain gauge had 3.24 inches. The exit ramp from Interstate 695 to Security Boulevard was closed due to flash flooding. A nearby rain gauge totaled 3.99 inches. Hoffman Mill Road was closed due to stream flooding on tributaries of the Northwest Branch Patapsco River.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 37.9177 km away, between 2012-06-01 18:00:00 and 2012-06-01 22:29:00. The events included records with measured wind gusts of 34.75 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Low pressure tracked through the Ohio Valley and into the Great Lakes. The warm front associated with this system passed through the waters during the first. Plenty of moisture from the Gulf of Mexico and the Atlantic Ocean combined with strong forcing associated with the warm front, causing thunderstorms to develop. Moderate instability along with strong forcing caused some thunderstorms to produce gusty winds. Low pressure tracked through the Ohio Valley and into the Great Lakes. The warm front associated with this system passed through the waters during the first. Plenty of moisture from the Gulf of Mexico and the Atlantic Ocean combined with strong forcing associated with the warm front, causing thunderstorms to develop. Moderate instability along with strong forcing caused some thunderstorms to produce gusty winds. Low pressure tracked through the Ohio Valley and into the Great Lakes. The warm front associated with this system passed through the waters during the first. Plenty of moisture from the Gulf of Mexico and the Atlantic Ocean combined with strong forcing associated with the warm front, causing thunderstorms to develop. Moderate instability along with strong forcing caused some thunderstorms to produce gusty winds. Low pressure tracked through the Ohio Valley and into the Great Lakes. The warm front associated with this system passed through the waters during the first. Plenty of moisture from the Gulf of Mexico and the Atlantic Ocean combined with strong forcing associated with the warm front, causing thunderstorms to develop. Moderate instability along with strong forcing caused some thunderstorms to produce gusty winds.\nEvent Narrative: Wind gusts up to 35 knots were reported at the Thomas Point Lighthouse. Wind gusts up to 35 knots were reported. A wind gust of 34 knots was reported at Kent Island. A wind gust of 35 knots was reported.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 38.4025 km away, between 2012-06-03 18:04:00 and 2012-06-03 18:18:00. The events included records with estimated wind gusts of 52.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 4000.0 and crop damage of 0.0. \n\nEpisode Narrative: The passage of a cold front and upper-level trough helped to trigger thunderstorms across northeastern Maryland on the third. Strong winds above the surface combined with high humidity at mid-levels caused damaging winds to mix down to the surface. The passage of a cold front and upper-level trough helped to trigger thunderstorms across northeastern Maryland on the third. Strong winds above the surface combined with high humidity at mid-levels caused damaging winds to mix down to the surface. The passage of a cold front and upper-level trough helped to trigger thunderstorms across northeastern Maryland on the third. Strong winds above the surface combined with high humidity at mid-levels caused damaging winds to mix down to the surface. The passage of a cold front and upper-level trough helped to trigger thunderstorms across northeastern Maryland on the third. Strong winds above the surface combined with high humidity at mid-levels caused damaging winds to mix down to the surface. The passage of a cold front and upper-level trough helped to trigger thunderstorms across northeastern Maryland on the third. Strong winds above the surface combined with high humidity at mid-levels caused damaging winds to mix down to the surface. The passage of a cold front and upper-level trough helped to trigger thunderstorms across northeastern Maryland on the third. Strong winds above the surface combined with high humidity at mid-levels caused damaging winds to mix down to the surface.\nEvent Narrative: A tree was blown down and blocked a driveway along Hutchins Mill Rd. A tree was knocked down onto power lines near the intersection of Regwood Rd. and Catalpa Rd. A tree was knocked down a quarter of a mile east of the intersection of Shawan Rd. and Cuba Rd. A tree was blown down onto power lines along Markoe Rd. near Monkton Rd. A second tree that was 40 to 50 feet tall and 18 inches in diameter was knocked down. A tree was knocked down near the intersection of Crondall Ln. and Garrison Forest Rd. A tree was blown down near the intersection of Sherwood Rd. and Warren Rd.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 34.5041 km away, between 2012-06-03 18:40:00 and 2012-06-03 19:18:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front passed through the waters on the 3rd. Scattered showers and thunderstorms developed along and ahead of the front. A couple thunderstorms produced gusty winds. A cold front passed through the waters on the 3rd. Scattered showers and thunderstorms developed along and ahead of the front. A couple thunderstorms produced gusty winds. A cold front passed through the waters on the 3rd. Scattered showers and thunderstorms developed along and ahead of the front. A couple thunderstorms produced gusty winds.\nEvent Narrative: A wind gust of 41 mph was measured. Wind gusts in excess of 30 knots were reported at Miller Island. Wind gusts in excess of 30 knots were reported at Tolchester Beach.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 14.2666 km away, between 2012-06-07 18:42:00 and 2012-06-07 18:54:00. The events included records with measured wind gusts of 35.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Scattered showers developed due to a trough of low pressure overhead. An isolated shower contained gusty winds.\nEvent Narrative: Wind gusts up to 35 knots were reported at Key Bridge.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 38.6039 km away, between 2012-06-22 16:59:00 and 2012-06-22 17:36:00. The events included records with estimated wind gusts of 52.333333333333336 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 3000.0 and crop damage of 0.0. \n\nEpisode Narrative: An upper-level trough and associated cold front moved across Maryland, northern Virginia and eastern West Virginia during the afternoon and evening of the 22nd. High humidity and instability values provided the ingredients for severe storms to develop early in the afternoon and linger into the late evening hours. An upper-level trough and associated cold front moved across Maryland, northern Virginia and eastern West Virginia during the afternoon and evening of the 22nd. High humidity and instability values provided the ingredients for severe storms to develop early in the afternoon and linger into the late evening hours. An upper-level trough and associated cold front moved across Maryland, northern Virginia and eastern West Virginia during the afternoon and evening of the 22nd. High humidity and instability values provided the ingredients for severe storms to develop early in the afternoon and linger into the late evening hours.\nEvent Narrative: A 25 inch diameter tree was blown down. This report was gathered through the RITIS system. A 3 inch tree limb was blown down onto a porch from a measured 50 mph wind gust. A part of a large tree approximately two and a half feet in diameter fell onto a house along Marshall Wood Rd.", "The following events were reported: Flash Flood. These occurred near station USW00093721, approximately 38.8327 km away, between 2012-06-22 17:15:00 and 2012-06-22 19:00:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A trough of low pressure triggered showers and thunderstorms during the 22nd. An isolated flash flood occurred in Carroll County due to one of these thunderstorms.\nEvent Narrative: Flash flooding occurred to do creek overflowing onto Hollingsworth Road.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 23.6573 km away, between 2012-06-22 17:42:00 and 2012-06-22 18:42:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A trough of low pressure triggered showers and thunderstorms during the 22nd. Moderate amounts of instability caused thunderstorms to produce gusty winds. A trough of low pressure triggered showers and thunderstorms during the 22nd. Moderate amounts of instability caused thunderstorms to produce gusty winds. A trough of low pressure triggered showers and thunderstorms during the 22nd. Moderate amounts of instability caused thunderstorms to produce gusty winds. A trough of low pressure triggered showers and thunderstorms during the 22nd. Moderate amounts of instability caused thunderstorms to produce gusty winds.\nEvent Narrative: Wind gusts in excess of 30 knots were reported. Wind gusts up to 40 knots were reported at Key Bridge. A wind gust of 34 knots was reported at Miller Island. Wind gusts in excess of 30 knots was reported at Tolchester Beach.", "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00093721, approximately 23.0297 km away, between 2012-06-29 04:05:00 and 2012-06-29 22:48:00. The events included records with hailstones measuring 56.16044776119403 inches.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 777000.0 and crop damage of 0.0. \n\nEpisode Narrative: A strong upper-level disturbance passed through the region in a northwest flow aloft. Extremely hot and humid conditions caused high amounts of instability. The upper-level disturbance triggered a line of thunderstorms that moved through the area. Due to the high instability, thunderstorms caused widespread wind damage. A strong upper-level disturbance passed through the region in a northwest flow aloft. Extremely hot and humid conditions caused high amounts of instability. The upper-level disturbance triggered a line of thunderstorms that moved through the area. Due to the high instability, thunderstorms caused widespread wind damage. A strong upper-level disturbance passed through the region in a northwest flow aloft. Extremely hot and humid conditions caused high amounts of instability. The upper-level disturbance triggered a line of thunderstorms that moved through the area. Due to the high instability, thunderstorms caused widespread wind damage. A strong upper-level disturbance passed through the region in a northwest flow aloft. Extremely hot and humid conditions caused high amounts of instability. The upper-level disturbance triggered a line of thunderstorms that moved through the area. Due to the high instability, thunderstorms caused widespread wind damage. A strong upper-level disturbance passed through the region in a northwest flow aloft. Extremely hot and humid conditions caused high amounts of instability. The upper-level disturbance triggered a line of thunderstorms that moved through the area. Due to the high instability, thunderstorms caused widespread wind damage. A strong upper-level disturbance passed through the region in a northwest flow aloft. Extremely hot and humid conditions caused high amounts of instability. The upper-level disturbance triggered a line of thunderstorms that moved through the area. Due to the high instability, thunderstorms caused widespread wind damage. A strong upper-level disturbance passed through the region in a northwest flow aloft. Extremely hot and humid conditions caused high amounts of instability. The upper-level disturbance triggered a line of thunderstorms that moved through the area. Due to the high instability, thunderstorms caused widespread wind damage. A strong upper-level disturbance passed through the region in a northwest flow aloft. Extremely hot and humid conditions caused high amounts of instability. The upper-level disturbance triggered a line of thunderstorms that moved through the area. Due to the high instability, thunderstorms caused widespread wind damage. A strong upper-level disturbance passed through the region in a northwest flow aloft. Extremely hot and humid conditions caused high amounts of instability. The upper-level disturbance triggered a line of thunderstorms that moved through the area. Due to the high instability, thunderstorms caused widespread wind damage. A strong upper-level disturbance passed through the region in a northwest flow aloft. Extremely hot and humid conditions caused high amounts of instability. The upper-level disturbance triggered a line of thunderstorms that moved through the area. Due to the high instability, thunderstorms caused widespread wind damage. A strong upper-level disturbance passed through the region in a northwest flow aloft. Extremely hot and humid conditions caused high amounts of instability. The upper-level disturbance triggered a line of thunderstorms that moved through the area. Due to the high instability, thunderstorms caused widespread wind damage. A strong upper-level disturbance passed through the region in a northwest flow aloft. Extremely hot and humid conditions caused high amounts of instability. The upper-level disturbance triggered a line of thunderstorms that moved through the area. Due to the high instability, thunderstorms caused widespread wind damage. A strong upper-level disturbance passed through the region in a northwest flow aloft. Extremely hot and humid conditions caused high amounts of instability. The upper-level disturbance triggered a line of thunderstorms that moved through the area. Due to the high instability, thunderstorms caused widespread wind damage. A strong upper-level disturbance passed through the region in a northwest flow aloft. Extremely hot and humid conditions caused high amounts of instability. The upper-level disturbance triggered a line of thunderstorms that moved through the area. Due to the high instability, thunderstorms caused widespread wind damage. A strong upper-level disturbance passed through the region in a northwest flow aloft. Extremely hot and humid conditions caused high amounts of instability. The upper-level disturbance triggered a line of thunderstorms that moved through the area. Due to the high instability, thunderstorms caused widespread wind damage. A strong upper-level disturbance passed through the region in a northwest flow aloft. Extremely hot and humid conditions caused high amounts of instability. The upper-level disturbance triggered a line of thunderstorms that moved through the area. Due to the high instability, thunderstorms caused widespread wind damage. A strong upper-level disturbance passed through the region in a northwest flow aloft. Extremely hot and humid conditions caused high amounts of instability. The upper-level disturbance triggered a line of thunderstorms that moved through the area. Due to the high instability, thunderstorms caused widespread wind damage. A strong upper-level disturbance passed through the region in a northwest flow aloft. Extremely hot and humid conditions caused high amounts of instability. The upper-level disturbance triggered a line of thunderstorms that moved through the area. Due to the high instability, thunderstorms caused widespread wind damage. A strong upper-level disturbance passed through the region in a northwest flow aloft. Extremely hot and humid conditions caused high amounts of instability. The upper-level disturbance triggered a line of thunderstorms that moved through the area. Due to the high instability, thunderstorms caused widespread wind damage. A strong upper-level disturbance passed through the region in a northwest flow aloft. Extremely hot and humid conditions caused high amounts of instability. The upper-level disturbance triggered a line of thunderstorms that moved through the area. Due to the high instability, thunderstorms caused widespread wind damage. A strong upper-level disturbance passed through the region in a northwest flow aloft. Extremely hot and humid conditions caused high amounts of instability. The upper-level disturbance triggered a line of thunderstorms that moved through the area. Due to the high instability, thunderstorms caused widespread wind damage. A strong upper-level disturbance passed through the region in a northwest flow aloft. Extremely hot and humid conditions caused high amounts of instability. The upper-level disturbance triggered a line of thunderstorms that moved through the area. Due to the high instability, thunderstorms caused widespread wind damage. A strong upper-level disturbance passed through the region in a northwest flow aloft. Extremely hot and humid conditions caused high amounts of instability. The upper-level disturbance triggered a line of thunderstorms that moved through the area. Due to the high instability, thunderstorms caused widespread wind damage. A strong upper-level disturbance passed through the region in a northwest flow aloft. Extremely hot and humid conditions caused high amounts of instability. The upper-level disturbance triggered a line of thunderstorms that moved through the area. Due to the high instability, thunderstorms caused widespread wind damage. A strong upper-level disturbance passed through the region in a northwest flow aloft. Extremely hot and humid conditions caused high amounts of instability. The upper-level disturbance triggered a line of thunderstorms that moved through the area. Due to the high instability, thunderstorms caused widespread wind damage. A strong upper-level disturbance passed through the region in a northwest flow aloft. Extremely hot and humid conditions caused high amounts of instability. The upper-level disturbance triggered a line of thunderstorms that moved through the area. Due to the high instability, thunderstorms caused widespread wind damage. A strong upper-level disturbance passed through the region in a northwest flow aloft. Extremely hot and humid conditions caused high amounts of instability. The upper-level disturbance triggered a line of thunderstorms that moved through the area. Due to the high instability, thunderstorms caused widespread wind damage. A strong upper-level disturbance passed through the region in a northwest flow aloft. Extremely hot and humid conditions caused high amounts of instability. The upper-level disturbance triggered a line of thunderstorms that moved through the area. Due to the high instability, thunderstorms caused widespread wind damage. A strong upper-level disturbance passed through the region in a northwest flow aloft. Extremely hot and humid conditions caused high amounts of instability. The upper-level disturbance triggered a line of thunderstorms that moved through the area. Due to the high instability, thunderstorms caused widespread wind damage. A strong upper-level disturbance passed through the region in a northwest flow aloft. Extremely hot and humid conditions caused high amounts of instability. The upper-level disturbance triggered a line of thunderstorms that moved through the area. Due to the high instability, thunderstorms caused widespread wind damage. A strong upper-level disturbance passed through the region in a northwest flow aloft. Extremely hot and humid conditions caused high amounts of instability. The upper-level disturbance triggered a line of thunderstorms that moved through the area. Due to the high instability, thunderstorms caused widespread wind damage. A strong upper-level disturbance passed through the region in a northwest flow aloft. Extremely hot and humid conditions caused high amounts of instability. The upper-level disturbance triggered a line of thunderstorms that moved through the area. Due to the high instability, thunderstorms caused widespread wind damage. A strong upper-level disturbance passed through the region in a northwest flow aloft. Extremely hot and humid conditions caused high amounts of instability. The upper-level disturbance triggered a line of thunderstorms that moved through the area. Due to the high instability, thunderstorms caused widespread wind damage. A strong upper-level disturbance passed through the region in a northwest flow aloft. Extremely hot and humid conditions caused high amounts of instability. The upper-level disturbance triggered a line of thunderstorms that moved through the area. Due to the high instability, thunderstorms caused widespread wind damage. A strong upper-level disturbance passed through the region in a northwest flow aloft. Extremely hot and humid conditions caused high amounts of instability. The upper-level disturbance triggered a line of thunderstorms that moved through the area. Due to the high instability, thunderstorms caused widespread wind damage. A strong upper-level disturbance passed through the region in a northwest flow aloft. Extremely hot and humid conditions caused high amounts of instability. The upper-level disturbance triggered a line of thunderstorms that moved through the area. Due to the high instability, thunderstorms caused widespread wind damage. A strong upper-level disturbance passed through the region in a northwest flow aloft. Extremely hot and humid conditions caused high amounts of instability. The upper-level disturbance triggered a line of thunderstorms that moved through the area. Due to the high instability, thunderstorms caused widespread wind damage. A strong upper-level disturbance passed through the region in a northwest flow aloft. Extremely hot and humid conditions caused high amounts of instability. The upper-level disturbance triggered a line of thunderstorms that moved through the area. Due to the high instability, thunderstorms caused widespread wind damage. A strong upper-level disturbance passed through the region in a northwest flow aloft. Extremely hot and humid conditions caused high amounts of instability. The upper-level disturbance triggered a line of thunderstorms that moved through the area. Due to the high instability, thunderstorms caused widespread wind damage. A strong upper-level disturbance passed through the region in a northwest flow aloft. Extremely hot and humid conditions caused high amounts of instability. The upper-level disturbance triggered a line of thunderstorms that moved through the area. Due to the high instability, thunderstorms caused widespread wind damage. A strong upper-level disturbance passed through the region in a northwest flow aloft. Extremely hot and humid conditions caused high amounts of instability. The upper-level disturbance triggered a line of thunderstorms that moved through the area. Due to the high instability, thunderstorms caused widespread wind damage. A strong upper-level disturbance passed through the region in a northwest flow aloft. Extremely hot and humid conditions caused high amounts of instability. The upper-level disturbance triggered a line of thunderstorms that moved through the area. Due to the high instability, thunderstorms caused widespread wind damage. A strong upper-level disturbance passed through the region in a northwest flow aloft. Extremely hot and humid conditions caused high amounts of instability. The upper-level disturbance triggered a line of thunderstorms that moved through the area. Due to the high instability, thunderstorms caused widespread wind damage. A strong upper-level disturbance passed through the region in a northwest flow aloft. Extremely hot and humid conditions caused high amounts of instability. The upper-level disturbance triggered a line of thunderstorms that moved through the area. Due to the high instability, thunderstorms caused widespread wind damage. A strong upper-level disturbance passed through the region in a northwest flow aloft. Extremely hot and humid conditions caused high amounts of instability. The upper-level disturbance triggered a line of thunderstorms that moved through the area. Due to the high instability, thunderstorms caused widespread wind damage. A strong upper-level disturbance passed through the region in a northwest flow aloft. Extremely hot and humid conditions caused high amounts of instability. The upper-level disturbance triggered a line of thunderstorms that moved through the area. Due to the high instability, thunderstorms caused widespread wind damage. A strong upper-level disturbance passed through the region in a northwest flow aloft. Extremely hot and humid conditions caused high amounts of instability. The upper-level disturbance triggered a line of thunderstorms that moved through the area. Due to the high instability, thunderstorms caused widespread wind damage. A strong upper-level disturbance passed through the region in a northwest flow aloft. Extremely hot and humid conditions caused high amounts of instability. The upper-level disturbance triggered a line of thunderstorms that moved through the area. Due to the high instability, thunderstorms caused widespread wind damage. A strong upper-level disturbance passed through the region in a northwest flow aloft. Extremely hot and humid conditions caused high amounts of instability. The upper-level disturbance triggered a line of thunderstorms that moved through the area. Due to the high instability, thunderstorms caused widespread wind damage. A strong upper-level disturbance passed through the region in a northwest flow aloft. Extremely hot and humid conditions caused high amounts of instability. The upper-level disturbance triggered a line of thunderstorms that moved through the area. Due to the high instability, thunderstorms caused widespread wind damage. A strong upper-level disturbance passed through the region in a northwest flow aloft. Extremely hot and humid conditions caused high amounts of instability. The upper-level disturbance triggered a line of thunderstorms that moved through the area. Due to the high instability, thunderstorms caused widespread wind damage. A strong upper-level disturbance passed through the region in a northwest flow aloft. Extremely hot and humid conditions caused high amounts of instability. The upper-level disturbance triggered a line of thunderstorms that moved through the area. Due to the high instability, thunderstorms caused widespread wind damage. A strong upper-level disturbance passed through the region in a northwest flow aloft. Extremely hot and humid conditions caused high amounts of instability. The upper-level disturbance triggered a line of thunderstorms that moved through the area. Due to the high instability, thunderstorms caused widespread wind damage. A strong upper-level disturbance passed through the region in a northwest flow aloft. Extremely hot and humid conditions caused high amounts of instability. The upper-level disturbance triggered a line of thunderstorms that moved through the area. Due to the high instability, thunderstorms caused widespread wind damage. A strong upper-level disturbance passed through the region in a northwest flow aloft. Extremely hot and humid conditions caused high amounts of instability. The upper-level disturbance triggered a line of thunderstorms that moved through the area. Due to the high instability, thunderstorms caused widespread wind damage. A strong upper-level disturbance passed through the region in a northwest flow aloft. Extremely hot and humid conditions caused high amounts of instability. The upper-level disturbance triggered a line of thunderstorms that moved through the area. Due to the high instability, thunderstorms caused widespread wind damage. A strong upper-level disturbance passed through the region in a northwest flow aloft. Extremely hot and humid conditions caused high amounts of instability. The upper-level disturbance triggered a line of thunderstorms that moved through the area. Due to the high instability, thunderstorms caused widespread wind damage. A strong upper-level disturbance passed through the region in a northwest flow aloft. Extremely hot and humid conditions caused high amounts of instability. The upper-level disturbance triggered a line of thunderstorms that moved through the area. Due to the high instability, thunderstorms caused widespread wind damage. A strong upper-level disturbance passed through the region in a northwest flow aloft. Extremely hot and humid conditions caused high amounts of instability. The upper-level disturbance triggered a line of thunderstorms that moved through the area. Due to the high instability, thunderstorms caused widespread wind damage. A strong upper-level disturbance passed through the region in a northwest flow aloft. Extremely hot and humid conditions caused high amounts of instability. The upper-level disturbance triggered a line of thunderstorms that moved through the area. Due to the high instability, thunderstorms caused widespread wind damage. A strong upper-level disturbance passed through the region in a northwest flow aloft. Extremely hot and humid conditions caused high amounts of instability. The upper-level disturbance triggered a line of thunderstorms that moved through the area. Due to the high instability, thunderstorms caused widespread wind damage. A strong upper-level disturbance passed through the region in a northwest flow aloft. Extremely hot and humid conditions caused high amounts of instability. The upper-level disturbance triggered a line of thunderstorms that moved through the area. Due to the high instability, thunderstorms caused widespread wind damage. A strong upper-level disturbance passed through the region in a northwest flow aloft. Extremely hot and humid conditions caused high amounts of instability. The upper-level disturbance triggered a line of thunderstorms that moved through the area. Due to the high instability, thunderstorms caused widespread wind damage. A strong upper-level disturbance passed through the region in a northwest flow aloft. Extremely hot and humid conditions caused high amounts of instability. The upper-level disturbance triggered a line of thunderstorms that moved through the area. Due to the high instability, thunderstorms caused widespread wind damage. A strong upper-level disturbance passed through the region in a northwest flow aloft. Extremely hot and humid conditions caused high amounts of instability. The upper-level disturbance triggered a line of thunderstorms that moved through the area. Due to the high instability, thunderstorms caused widespread wind damage. A strong upper-level disturbance passed through the region in a northwest flow aloft. Extremely hot and humid conditions caused high amounts of instability. The upper-level disturbance triggered a line of thunderstorms that moved through the area. Due to the high instability, thunderstorms caused widespread wind damage. A strong upper-level disturbance passed through the region in a northwest flow aloft. Extremely hot and humid conditions caused high amounts of instability. The upper-level disturbance triggered a line of thunderstorms that moved through the area. Due to the high instability, thunderstorms caused widespread wind damage.\nEvent Narrative: A few two-foot diameter trees were knocked over. Tree limbs were down in the neighborhood. An outbuilding suffered complete loss of roofing material at a horse racing track. A plane flipped at Tipton Airport. A wind gust of 57 knots was measured at BWI Airport. A tree fell down into a house on Mission Road. A tree fell into a house on Reservoir Road. Trees fell onto houses along Old Tucker Row and Woodenhawk Circle. A tree fell onto a house at Homewood. A tree fell onto a house along Eden Brook Drive. A tree fell onto a house along Faulkner Ridge Circle. A tree fell into a house on Nottingham Way. Trees fell onto houses on Keeton Road and Baja Way. A tree fell into a house on Meadowfield Court. A tree fell onto a house on Grooms Lane. Quarter sized hail was reported near Jacksonville. Several large trees and large branches were knocked down near the intersection of Route 108 and 175. Numerous trees were down on houses. A tree fell onto a house on Brantly Court. Two trees fell onto houses on Celbridge Drive and also along Burntwoods Road. A tree fell into a house on Garratt Court. A tree fell into a house on Browns Bridge Road. A tree fell onto a house on River Clyde Drive. A tree fell onto a house on Carlinda Avenue. A tree fell down into a house on Font Hill Drive. A wind gust of 60 mph was measured. A wind gust of 60 mph was estimated. Tree limbs were blown down. Tree branches were broken near the intersection of Routes 100 and 170. Quarter sized hail was reported. A wind gust of 58 mph was measured at Annapolis. A wind gust of 61 knots was measured at Lee Airport. A wind gust around 50 knots was measured near the Baltimore Harbor. A wind gust around 51 knots was measured near Lochearn. A wind gust of 67 mph was measured. A wind gust of 58 mph was measured at Martin State. Several trees were down due to thunderstorm winds. Golf ball sized hail was reported. Several trees were knocked down near the intersection of Kenwood Avenue and Coco Road. A tree branch was thrown through windshield of a car along South Fulton Street. A tree was down at MD-543 and Smithson Road. Several branches and small trees were down. A wind gust around 50 knots was measured Towson. A branch that was one foot in diameter was blown down. A tree that was two feet in diameter was down off Newfield Road. A large Oak Tree was knocked down. A tree was down on Rolling Road near the intersection with Edmondson Avenue. Two trees fell into two houses along Hallmark Road. Small branches were blown away. Several trees and numerous branches were down. Several trees were down. A tree fell down on Pfeffers Road. A wind gust of 68 mph was measured. A wind gust of 61 mph was measured. A wind gust of 61 mph was measured. Several power poles were snapped. Homes lost shingles and blown out upper windows. Widespread tree damage was also reported. A chimney was broken off a home on Sandy Ridge Court. Trees and wires were down on Greene Road. Trees were down across Ipswich Drive. Large trees were down along the Bel Air Bypass. A tree was down on a townhouse along Plaza Circle. Tree debris was on the roadway. Trees were down in Edgewood. A tree was down on Laburnum Road. Trees were down near Brookeville. Limbs of varying size were on the roads. Large branches about eight inches in diameter were blown down.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 25.22 km away, between 2012-06-29 22:09:00 and 2012-06-29 23:59:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A strong upper-level disturbance passed through the waters in a northwest flow aloft. Extremely hot and humid conditions caused high amounts of instability. The upper-level disturbance triggered a line of thunderstorms that moved through the waters. Due to the high instability, thunderstorms caused widespread gusty winds. A strong upper-level disturbance passed through the waters in a northwest flow aloft. Extremely hot and humid conditions caused high amounts of instability. The upper-level disturbance triggered a line of thunderstorms that moved through the waters. Due to the high instability, thunderstorms caused widespread gusty winds. A strong upper-level disturbance passed through the waters in a northwest flow aloft. Extremely hot and humid conditions caused high amounts of instability. The upper-level disturbance triggered a line of thunderstorms that moved through the waters. Due to the high instability, thunderstorms caused widespread gusty winds. A strong upper-level disturbance passed through the waters in a northwest flow aloft. Extremely hot and humid conditions caused high amounts of instability. The upper-level disturbance triggered a line of thunderstorms that moved through the waters. Due to the high instability, thunderstorms caused widespread gusty winds. A strong upper-level disturbance passed through the waters in a northwest flow aloft. Extremely hot and humid conditions caused high amounts of instability. The upper-level disturbance triggered a line of thunderstorms that moved through the waters. Due to the high instability, thunderstorms caused widespread gusty winds. A strong upper-level disturbance passed through the waters in a northwest flow aloft. Extremely hot and humid conditions caused high amounts of instability. The upper-level disturbance triggered a line of thunderstorms that moved through the waters. Due to the high instability, thunderstorms caused widespread gusty winds. A strong upper-level disturbance passed through the waters in a northwest flow aloft. Extremely hot and humid conditions caused high amounts of instability. The upper-level disturbance triggered a line of thunderstorms that moved through the waters. Due to the high instability, thunderstorms caused widespread gusty winds. A strong upper-level disturbance passed through the waters in a northwest flow aloft. Extremely hot and humid conditions caused high amounts of instability. The upper-level disturbance triggered a line of thunderstorms that moved through the waters. Due to the high instability, thunderstorms caused widespread gusty winds. A strong upper-level disturbance passed through the waters in a northwest flow aloft. Extremely hot and humid conditions caused high amounts of instability. The upper-level disturbance triggered a line of thunderstorms that moved through the waters. Due to the high instability, thunderstorms caused widespread gusty winds. A strong upper-level disturbance passed through the waters in a northwest flow aloft. Extremely hot and humid conditions caused high amounts of instability. The upper-level disturbance triggered a line of thunderstorms that moved through the waters. Due to the high instability, thunderstorms caused widespread gusty winds. A strong upper-level disturbance passed through the waters in a northwest flow aloft. Extremely hot and humid conditions caused high amounts of instability. The upper-level disturbance triggered a line of thunderstorms that moved through the waters. Due to the high instability, thunderstorms caused widespread gusty winds. A strong upper-level disturbance passed through the waters in a northwest flow aloft. Extremely hot and humid conditions caused high amounts of instability. The upper-level disturbance triggered a line of thunderstorms that moved through the waters. Due to the high instability, thunderstorms caused widespread gusty winds. A strong upper-level disturbance passed through the waters in a northwest flow aloft. Extremely hot and humid conditions caused high amounts of instability. The upper-level disturbance triggered a line of thunderstorms that moved through the waters. Due to the high instability, thunderstorms caused widespread gusty winds. A strong upper-level disturbance passed through the waters in a northwest flow aloft. Extremely hot and humid conditions caused high amounts of instability. The upper-level disturbance triggered a line of thunderstorms that moved through the waters. Due to the high instability, thunderstorms caused widespread gusty winds. A strong upper-level disturbance passed through the waters in a northwest flow aloft. Extremely hot and humid conditions caused high amounts of instability. The upper-level disturbance triggered a line of thunderstorms that moved through the waters. Due to the high instability, thunderstorms caused widespread gusty winds.\nEvent Narrative: A wind gust of 61 knots was estimated based on thunderstorm wind damage nearby. Wind gusts up to 41 knots were measured at St. Annes School. Wind gusts up to 42 knots were measured at Kent Island. Wind gusts up to 44 knots were reported at the Patapsco Buoy. Wind gusts up to 49 knots were reported at Annapolis. Wind gusts up to 41 knots were reported at St. Mary's Elementary School. Wind gusts up to 59 knots were reported at the Hampstead Hill Elementary School. Wind gusts up to 45 knots were measured at the Maryland Science Center. Wind gusts up to 42 knots were measured at Sparrows Point High School. Wind gusts up to 35 knots was reported at the Francis Scott Key Bridge. Wind gusts up to 49 knots were measured at Kent Island. Wind gusts up to 36 knots were measured at Tolchester Beach. Wind gusts up to 45 knots were measured. A wind gust in excess of 30 knots was measured at the Thomas Point Lighthouse. A wind gust of 58 knots was estimated based on observations nearby.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 38.7717 km away, between 2012-06-29 22:22:00 and 2012-06-29 23:31:00.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 120000.0 and crop damage of 0.0. \n\nEpisode Narrative: A well-organized cluster of thunderstorms with a history of producing widespread damaging winds advanced into a hot, unstable airmass over the Mid Atlantic. This derecho produced widespread, significant wind damage from southern New Jersey southward into the Delmarva during the late evening and overnight of the 29th.||Strong thunderstorm development began across the Midwest and Lower Great Lakes regions during the afternoon of the 29th, with storms initiating across northern Illinois, near Chicago. Strong mid-level winds and an unstable airmass contributed to rapid development as well-organized storms progressed from northern Illinois through Indiana and Ohio. This robust convection continued to track southeastward into an airmass that was even more unstable due to abundant daytime surface heating. Late afternoon temperatures had peaked mainly in the mid to upper 90s with high humidity throughout the Mid Atlantic states, and as the potent thunderstorm cluster progressed from the Great Lakes to the central Appalachians and into the Mid Atlantic by late evening, thunderstorm activity was reinvigorated.||A robust gust front outpaced the main thunderstorm line, producing strong wind gusts as it traveled from the eastern shore of Maryland into Delaware and southern New Jersey. Shortly thereafter, the potent thunderstorm line tracked through the region, with additional damaging wind gusts. One cell in particular around Baltimore, MD experienced rapid intensification and expansion as it raced eastward into northern Delaware and southern New Jersey. This massive cell produced extreme damage throughout Salem, Cumberland, and Atlantic counties in New Jersey. Damage to trees, power lines, and buildings was also significant throughout Delaware and the eastern shore of Maryland. Thunderstorms also dropped hail in several locations, ranging from penny to golf-ball size. Destructive wind gusts, between 65 mph to nearly 90 mph, were measured as this derecho tracked from the Lower Great Lakes to the Mid Atlantic coast. A well-organized cluster of thunderstorms with a history of producing widespread damaging winds advanced into a hot, unstable airmass over the Mid Atlantic. This derecho produced widespread, significant wind damage from southern New Jersey southward into the Delmarva during the late evening and overnight of the 29th.||Strong thunderstorm development began across the Midwest and Lower Great Lakes regions during the afternoon of the 29th, with storms initiating across northern Illinois, near Chicago. Strong mid-level winds and an unstable airmass contributed to rapid development as well-organized storms progressed from northern Illinois through Indiana and Ohio. This robust convection continued to track southeastward into an airmass that was even more unstable due to abundant daytime surface heating. Late afternoon temperatures had peaked mainly in the mid to upper 90s with high humidity throughout the Mid Atlantic states, and as the potent thunderstorm cluster progressed from the Great Lakes to the central Appalachians and into the Mid Atlantic by late evening, thunderstorm activity was reinvigorated.||A robust gust front outpaced the main thunderstorm line, producing strong wind gusts as it traveled from the eastern shore of Maryland into Delaware and southern New Jersey. Shortly thereafter, the potent thunderstorm line tracked through the region, with additional damaging wind gusts. One cell in particular around Baltimore, MD experienced rapid intensification and expansion as it raced eastward into northern Delaware and southern New Jersey. This massive cell produced extreme damage throughout Salem, Cumberland, and Atlantic counties in New Jersey. Damage to trees, power lines, and buildings was also significant throughout Delaware and the eastern shore of Maryland. Thunderstorms also dropped hail in several locations, ranging from penny to golf-ball size. Destructive wind gusts, between 65 mph to nearly 90 mph, were measured as this derecho tracked from the Lower Great Lakes to the Mid Atlantic coast.\nEvent Narrative: A gust front outrunning a cluster of severe thunderstorms entered near Stevensville in western Queen Anne's County at approximately 11:22 pm EDT on the 29th. This gust front produced damaging wind gusts estimated at 65 mph as it traversed eastward across the county. Within approximately 20 minutes of the gust front passage, a potent line of severe thunderstorms tracked eastward through Queen Anne's County, producing another round of destructive wind gusts, estimated at 65 mph. Large tree limbs and electric wires were reported down across the county, with damage initially reported in the Stevensville area. Damage to a large chimney and the exterior walls of a home was also reported in Stevensville. Severe thunderstorms exited eastern Queen Anne's County, including the town of Sudlersville, at approximately 12:31 am EDT on the 30th. A gust front outrunning a cluster of severe thunderstorms entered near Rock Hall in western Kent County at approximately 11:22 pm EDT on the 29th. This gust front produced damaging wind gusts estimated at 65 mph as it traversed eastward across the county. Within approximately 20 minutes of the gust front passage, a potent line of severe thunderstorms tracked eastward through Kent County, producing another round of destructive wind gusts, estimated at 65 mph. Many large tree limbs were reported down across the county, including in the Millington area. Severe thunderstorms exited eastern Kent County, near Massey, at approximately 12:31 am EDT on the 30th. A peak wind gust of 66 mph was measured at Tolchester Beach.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 13.5628 km away, between 2012-07-02 00:28:00 and 2012-07-02 00:28:00. The events included records with estimated wind gusts of 56.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 15000.0 and crop damage of 0.0. \n\nEpisode Narrative: A cold front passed through during the early morning hours of the 2nd. The boundary triggered showers and thunderstorms. Some thunderstorms were able to produce damaging wind gusts.\nEvent Narrative: Two trees fell into houses in Westview.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 25.8199 km away, between 2012-07-02 02:10:00 and 2012-07-02 02:48:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front passed through the waters during the early morning hours of the 2nd. The boundary triggered showers and thunderstorms. Some thunderstorms were able to produce gusty winds. A cold front passed through the waters during the early morning hours of the 2nd. The boundary triggered showers and thunderstorms. Some thunderstorms were able to produce gusty winds.\nEvent Narrative: A wind gust in excess of 30 knots was reported at the Maryland Science Center. Wind gusts up to 36 knots were reported at Tolchester Beach.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 43.5124 km away, between 2012-07-05 17:44:00 and 2012-07-05 17:58:00. The events included records with estimated wind gusts of 52.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 3000.0 and crop damage of 0.0. \n\nEpisode Narrative: An upper-level disturbance combined with moderate instability to trigger showers and thunderstorms during the 5th. A couple thunderstorms produced damaging wind gusts and large hail. An upper-level disturbance combined with moderate instability to trigger showers and thunderstorms during the 5th. A couple thunderstorms produced damaging wind gusts and large hail. An upper-level disturbance combined with moderate instability to trigger showers and thunderstorms during the 5th. A couple thunderstorms produced damaging wind gusts and large hail.\nEvent Narrative: A tree was down on the 1600 Block of Sparks Road. A tree was down on wires along Hess Road between Jarettsville Pike and Man Road near Monkton. A tree was down across the roadway on Scarff Road off of Baldwin Mill Road.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 30.4641 km away, between 2012-07-18 15:30:00 and 2012-07-18 16:41:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A surface trough combined with moderate instability caused showers and thunderstorms to develop. There was enough instability for thunderstorms to produce gusty winds. A surface trough combined with moderate instability caused showers and thunderstorms to develop. There was enough instability for thunderstorms to produce gusty winds. A surface trough combined with moderate instability caused showers and thunderstorms to develop. There was enough instability for thunderstorms to produce gusty winds. A surface trough combined with moderate instability caused showers and thunderstorms to develop. There was enough instability for thunderstorms to produce gusty winds. A surface trough combined with moderate instability caused showers and thunderstorms to develop. There was enough instability for thunderstorms to produce gusty winds. A surface trough combined with moderate instability caused showers and thunderstorms to develop. There was enough instability for thunderstorms to produce gusty winds. A surface trough combined with moderate instability caused showers and thunderstorms to develop. There was enough instability for thunderstorms to produce gusty winds. A surface trough combined with moderate instability caused showers and thunderstorms to develop. There was enough instability for thunderstorms to produce gusty winds. A surface trough combined with moderate instability caused showers and thunderstorms to develop. There was enough instability for thunderstorms to produce gusty winds. A surface trough combined with moderate instability caused showers and thunderstorms to develop. There was enough instability for thunderstorms to produce gusty winds. A surface trough combined with moderate instability caused showers and thunderstorms to develop. There was enough instability for thunderstorms to produce gusty winds.\nEvent Narrative: A wind gust of 47 knots was reported at Patapsco Buoy. A wind gust of 34 knots was measured. Wind gusts up to 41 knots were measured at the Annapolis Buoy. Wind gusts up to 42 knots were measured at Greenberry Point. A wind gust of 38 knots was measured at Annapolis. A wind gust of 36 knots was measured at Kent Island. A wind gust of 40 knots was measured at Stevensville. Wind gusts up to 41 knots were measured at Tolly Point. A wind gust of 36 knots was measured at the Thomas Point Lighthouse. Wind gusts around 50 knots were estimated due to thunderstorm wind damage nearby. A wind gust in excess of 30 knots was reported at Tolchester Beach.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 17.9257 km away, between 2012-07-18 15:45:00 and 2012-07-18 16:20:00. The events included records with estimated wind gusts of 52.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 3000.0 and crop damage of 0.0. \n\nEpisode Narrative: A surface trough combined with moderate instability caused showers and thunderstorms to develop. There was enough instability for thunderstorms to produce damaging wind gusts and large hail. A surface trough combined with moderate instability caused showers and thunderstorms to develop. There was enough instability for thunderstorms to produce damaging wind gusts and large hail.\nEvent Narrative: Several trees were down due to thunderstorm wind gusts. Two snapped trees and a large branch were down at a residence.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 41.5425 km away, between 2012-07-18 16:30:00 and 2012-07-18 17:15:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: An approaching back door cold front (from the north) and an unseasonably hot as well as humid air mass combined to trigger scattered strong to severe thunderstorms across the Eastern Shore during the late afternoon and early evening on the 18th. An approaching back door cold front (from the north) and an unseasonably hot as well as humid air mass combined to trigger scattered strong to severe thunderstorms across the Eastern Shore during the late afternoon and early evening on the 18th. An approaching back door cold front (from the north) and an unseasonably hot as well as humid air mass combined to trigger scattered strong to severe thunderstorms across the Eastern Shore during the late afternoon and early evening on the 18th.\nEvent Narrative: The Chesapeake Bay Bridge (William Preston Lane Jr. Memorial Bridge) was closed in both directions after a severe thunderstorm produced a wind gust of 59 mph. The eastbound lanes were reopened at 6 p.m. EDT. A westbound lane was reopened at 7 p.m. EDT, a second lane was reopened at 730 p.m. EDT and the third lane remained closed until any wind damage was checked. A severe thunderstorm produced estimated wind gusts of around 60 mph in Kent Island Estates. A severe thunderstorm knocked down several trees across Queen Anne's County from Centreville east to around Crumpton.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 16.0275 km away, between 2012-07-19 17:48:00 and 2012-07-19 19:10:00. The events included records with measured wind gusts of 46.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A surface trough combined with moderate instability caused showers and thunderstorms to develop. There was enough instability for some thunderstorms to produce gusty winds. A surface trough combined with moderate instability caused showers and thunderstorms to develop. There was enough instability for some thunderstorms to produce gusty winds. A surface trough combined with moderate instability caused showers and thunderstorms to develop. There was enough instability for some thunderstorms to produce gusty winds. A surface trough combined with moderate instability caused showers and thunderstorms to develop. There was enough instability for some thunderstorms to produce gusty winds. A surface trough combined with moderate instability caused showers and thunderstorms to develop. There was enough instability for some thunderstorms to produce gusty winds.\nEvent Narrative: Wind gusts up to 37 knots were measured at the Patapsco Buoy. Wind gusts up to 45 knots were measured at the Maryland Science Center. Wind gusts up to 51 knots were measured. A wind gust of 40 knots was measured at Camden Yards. Wind gusts up to 57 knots were measured at Key Bridge.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 14.5872 km away, between 2012-07-19 18:06:00 and 2012-07-19 18:06:00. The events included records with measured wind gusts of 51.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A surface trough combined with moderate instability caused showers and thunderstorms to develop. There was enough instability for some thunderstorms to produce damaging wind gusts.\nEvent Narrative: A wind gust of 59 mph was measured at Fells Point.", "The following events were reported: Flash Flood. These occurred near station USW00093721, approximately 15.3322 km away, between 2012-07-19 18:20:00 and 2012-07-20 00:53:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Low pressure drifted eastward across the Mid-Atlantic along a stalled front. Afternoon showers and thunderstorms erupted in a highly moist and unstable atmosphere. Heavy rain associated with some of the activity caused flash flooding. Observed rainfall amounts were as high as 4.30 inches in Baltimore County. Low pressure drifted eastward across the Mid-Atlantic along a stalled front. Afternoon showers and thunderstorms erupted in a highly moist and unstable atmosphere. Heavy rain associated with some of the activity caused flash flooding. Observed rainfall amounts were as high as 4.30 inches in Baltimore County. Low pressure drifted eastward across the Mid-Atlantic along a stalled front. Afternoon showers and thunderstorms erupted in a highly moist and unstable atmosphere. Heavy rain associated with some of the activity caused flash flooding. Observed rainfall amounts were as high as 4.30 inches in Baltimore County.\nEvent Narrative: Flash flooding forced the closure of Aliceanna Street at South Caroline Street. A weather station nearby reported 3.00 inches of rain. Two feet of water was flowing down North Kenwood Avenue. A nearby rain gauge tallied 3.30 inches of rain. Flash flooding stranded vehicles on North Caroline Street near East Madison Street. A nearby rain gauge recorded 3.27 inches.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 32.9228 km away, between 2012-07-24 15:23:00 and 2012-07-24 16:34:00. The events included records with estimated wind gusts of 52.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 1000.0 and crop damage of 0.0. \n\nEpisode Narrative: A surface trough along with an upper-level disturbance triggered some showers and thunderstorms. There was enough instability and flow aloft for a few thunderstorms to produce damaging winds. A surface trough along with an upper-level disturbance triggered some showers and thunderstorms. There was enough instability and flow aloft for a few thunderstorms to produce damaging winds.\nEvent Narrative: A tree was down along Route 43 near the Baltimore Beltway. A tree was down at Phoenix and Carroll Road.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 41.3986 km away, between 2012-07-26 20:08:00 and 2012-07-26 21:01:00. The events included records with estimated wind gusts of 52.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 4000.0 and crop damage of 0.0. \n\nEpisode Narrative: A cold front passed through the area on the 26th. Hot and humid conditions ahead of the front caused moderate amounts of instability. The cold front triggered showers and thunderstorms. There was enough instability for a few thunderstorms to produce damaging wind gusts. A cold front passed through the area on the 26th. Hot and humid conditions ahead of the front caused moderate amounts of instability. The cold front triggered showers and thunderstorms. There was enough instability for a few thunderstorms to produce damaging wind gusts. A cold front passed through the area on the 26th. Hot and humid conditions ahead of the front caused moderate amounts of instability. The cold front triggered showers and thunderstorms. There was enough instability for a few thunderstorms to produce damaging wind gusts. A cold front passed through the area on the 26th. Hot and humid conditions ahead of the front caused moderate amounts of instability. The cold front triggered showers and thunderstorms. There was enough instability for a few thunderstorms to produce damaging wind gusts.\nEvent Narrative: A tree was down on route 30. A tree was down at Railroad Avenue and York Road. A tree was down on Reckord Road between Harford Road and Bel Air Road. A tree was down at U.S. Route 1 and Harford Road.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 32.1499 km away, between 2012-07-26 20:23:00 and 2012-07-26 21:45:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front passed through the waters on the 26th. Hot and humid conditions ahead of the front caused moderate amounts of instability. The cold front triggered showers and thunderstorms. There was enough instability for thunderstorms to produce gusty winds. A cold front passed through the waters on the 26th. Hot and humid conditions ahead of the front caused moderate amounts of instability. The cold front triggered showers and thunderstorms. There was enough instability for thunderstorms to produce gusty winds. A cold front passed through the waters on the 26th. Hot and humid conditions ahead of the front caused moderate amounts of instability. The cold front triggered showers and thunderstorms. There was enough instability for thunderstorms to produce gusty winds. A cold front passed through the waters on the 26th. Hot and humid conditions ahead of the front caused moderate amounts of instability. The cold front triggered showers and thunderstorms. There was enough instability for thunderstorms to produce gusty winds. A cold front passed through the waters on the 26th. Hot and humid conditions ahead of the front caused moderate amounts of instability. The cold front triggered showers and thunderstorms. There was enough instability for thunderstorms to produce gusty winds. A cold front passed through the waters on the 26th. Hot and humid conditions ahead of the front caused moderate amounts of instability. The cold front triggered showers and thunderstorms. There was enough instability for thunderstorms to produce gusty winds.\nEvent Narrative: A wind gust in excess of 30 knots was reported. A wind gust of 39 knots was reported at the Patapsco Buoy. A wind gust of 39 knots was measured at Tolchester Beach. Wind gusts up to 36 knots were reported at Greenbury Point. Wind gusts in excess of 30 knots were measured at Tolly Point. A wind gust of 39 knots was measured at Thomas Point Lighthouse.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 34.0269 km away, between 2012-07-28 18:00:00 and 2012-07-28 20:10:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front along with an upper-level trough moved into the waters on the 28th. Showers and thunderstorms developed near the cold front. There was enough instability from cooler air aloft associated with the upper-level trough for thunderstorms to produce gusty winds. A cold front along with an upper-level trough moved into the waters on the 28th. Showers and thunderstorms developed near the cold front. There was enough instability from cooler air aloft associated with the upper-level trough for thunderstorms to produce gusty winds. A cold front along with an upper-level trough moved into the waters on the 28th. Showers and thunderstorms developed near the cold front. There was enough instability from cooler air aloft associated with the upper-level trough for thunderstorms to produce gusty winds.\nEvent Narrative: Wind gusts in excess of 30 knots were measured at the Annapolis Buoy. A wind gust of 36 knots was measured at Thomas Point. A wind gust of 36 knots was measured at the Thomas Point Lighthouse.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 21.2386 km away, between 2012-08-05 15:38:00 and 2012-08-05 16:11:00. The events included records with estimated wind gusts of 56.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 3000.0 and crop damage of 0.0. \n\nEpisode Narrative: A cold front moved eastward through the Mid Atlantic in the evening. Ample amounts of instability and moisture combined to cause severe thunderstorms with damaging winds and hail. A cold front moved eastward through the Mid Atlantic in the evening. Ample amounts of instability and moisture combined to cause severe thunderstorms with damaging winds and hail. A cold front moved eastward through the Mid Atlantic in the evening. Ample amounts of instability and moisture combined to cause severe thunderstorms with damaging winds and hail. A cold front moved eastward through the Mid Atlantic in the evening. Ample amounts of instability and moisture combined to cause severe thunderstorms with damaging winds and hail. A cold front moved eastward through the Mid Atlantic in the evening. Ample amounts of instability and moisture combined to cause severe thunderstorms with damaging winds and hail.\nEvent Narrative: Several trees down near intersection Murray Hill Rd and Vollmerhausen Drive. Tree branches 5-6 inches in diameter were blown down. Four inch diameter tree limbs drown near intesection of Riverside Drive and Margaret Ave. Large tree down near intersection of Eastern and White Marsh Ave. There were trees down at Loch Raven Blvd and Pentwood Rd from damaging winds.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 21.3416 km away, between 2012-08-05 15:54:00 and 2012-08-05 16:52:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front moved eastward through the Mid Atlantic in the evening. Ample amounts of instability and moisture combined to cause severe thunderstorms with damaging winds and hail. A cold front moved eastward through the Mid Atlantic in the evening. Ample amounts of instability and moisture combined to cause severe thunderstorms with damaging winds and hail. A cold front moved eastward through the Mid Atlantic in the evening. Ample amounts of instability and moisture combined to cause severe thunderstorms with damaging winds and hail. A cold front moved eastward through the Mid Atlantic in the evening. Ample amounts of instability and moisture combined to cause severe thunderstorms with damaging winds and hail. A cold front moved eastward through the Mid Atlantic in the evening. Ample amounts of instability and moisture combined to cause severe thunderstorms with damaging winds and hail. A cold front moved eastward through the Mid Atlantic in the evening. Ample amounts of instability and moisture combined to cause severe thunderstorms with damaging winds and hail. A cold front moved eastward through the Mid Atlantic in the evening. Ample amounts of instability and moisture combined to cause severe thunderstorms with damaging winds and hail.\nEvent Narrative: Wind gusts of 40 knots were reported at Hart Miller Island. A wind gust of 37 knots was reported at Hampstead Hill Academy. Wind gusts of 37 knots were reported at Oriole Park at Camden Yard. Wind gusts of excess of 31 knots was reported at Francis Scott Key Bridge. Wind gusts of 31 knots was reported at Patapsco CBIBS Buoy. Wind gusts in excess of 32 knots were reported at Baltimore. Wind gusts up to 42 knots were reported at Tolchester.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 44.6138 km away, between 2012-08-05 17:04:00 and 2012-08-05 17:05:00. The events included records with estimated wind gusts of 52.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A series of strong to severe thunderstorms that culminated with a squall late in the afternoon affected the Eastern Shore and Cecil County the hardest. Delmarva Power and Light reported about 13,000 of its customers lost power in Cecil County, over twenty-five percent of the county.\nEvent Narrative: A severe thunderstorm knocked down several trees and wires in Kent County from Fairlee to Chestertown.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 14.3041 km away, between 2012-08-09 16:20:00 and 2012-08-09 16:20:00. The events included records with estimated wind gusts of 52.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 500.0 and crop damage of 0.0. \n\nEpisode Narrative: A cold front approached the Mid Atlantic from the west during the afternoon. Instability and wind shear led to the development of severe thunderstorms that produced damaging winds and hail.\nEvent Narrative: Tree down at Nuwood Drive and Baltimore National Pike.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 26.2326 km away, between 2012-08-11 17:00:00 and 2012-08-11 20:30:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A weak cold front situated along the Blue Ridge drifted eastward throughout the day and showers and thunderstorms formed over the waters. A weak cold front situated along the Blue Ridge drifted eastward throughout the day and showers and thunderstorms formed over the waters. A weak cold front situated along the Blue Ridge drifted eastward throughout the day and showers and thunderstorms formed over the waters. A weak cold front situated along the Blue Ridge drifted eastward throughout the day and showers and thunderstorms formed over the waters. A weak cold front situated along the Blue Ridge drifted eastward throughout the day and showers and thunderstorms formed over the waters. A weak cold front situated along the Blue Ridge drifted eastward throughout the day and showers and thunderstorms formed over the waters. A weak cold front situated along the Blue Ridge drifted eastward throughout the day and showers and thunderstorms formed over the waters. A weak cold front situated along the Blue Ridge drifted eastward throughout the day and showers and thunderstorms formed over the waters. A weak cold front situated along the Blue Ridge drifted eastward throughout the day and showers and thunderstorms formed over the waters. A weak cold front situated along the Blue Ridge drifted eastward throughout the day and showers and thunderstorms formed over the waters. A weak cold front situated along the Blue Ridge drifted eastward throughout the day and showers and thunderstorms formed over the waters.\nEvent Narrative: Wind gusts of 33 knots were reported at Gunpowder. Wind gusts of 34 knots were reported at Hart Miller Island. Wind gusts of 34 knots were reported at Oriole Park at Camden Yard. Wind gusts of 34 knots were reported at Hart Miller Island. Wind gusts of 34 knots were reported at Francis Scott Key Bridge. Wind gusts of 34 knots were measured at Annapolis. Wind gusts up to 36 knots were reported at Tolly Point. Wind gusts up to 40 knots were reported at Thomas Point. Wind gusts up to 33 knots were reported at Patapsco CBIBS Buoy. Wind gusts up to 32 knots were reported at Francis Scott Key Bridge. Wind gusts in excess of 31 knots were reported at Annapolis CBIBS Buoy.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 37.391 km away, between 2012-08-14 00:10:00 and 2012-08-14 22:00:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front moved through the Mid Atlantic in the afternoon and evening. Scattered thunderstorms occurred with damaging winds and hail as the main threat. A cold front moved through the Mid Atlantic in the afternoon and evening. Scattered thunderstorms occurred with damaging winds and hail as the main threat. A cold front moved through the Mid Atlantic in the afternoon and evening. Scattered thunderstorms occurred with damaging winds and hail as the main threat.\nEvent Narrative: Wind gusts of 33 knots were reported at Gunpowder. Wind gusts in excess of 31 knots were reported at Gunpowder. Wind gusts up to 38 knots were reported at Deerfield Elementary.", "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00093721, approximately 25.9198 km away, between 2012-08-14 20:15:00 and 2012-08-14 21:14:00. The events included records with hailstones measuring 9.583333333333334 inches.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 1000.0 and crop damage of 0.0. \n\nEpisode Narrative: A cold front moved through the Mid Atlantic in the afternoon and evening. Scattered thunderstorms occurred with damaging winds and hail as the main threat. A cold front moved through the Mid Atlantic in the afternoon and evening. Scattered thunderstorms occurred with damaging winds and hail as the main threat. A cold front moved through the Mid Atlantic in the afternoon and evening. Scattered thunderstorms occurred with damaging winds and hail as the main threat. A cold front moved through the Mid Atlantic in the afternoon and evening. Scattered thunderstorms occurred with damaging winds and hail as the main threat. A cold front moved through the Mid Atlantic in the afternoon and evening. Scattered thunderstorms occurred with damaging winds and hail as the main threat. A cold front moved through the Mid Atlantic in the afternoon and evening. Scattered thunderstorms occurred with damaging winds and hail as the main threat.\nEvent Narrative: Tree down on West Chesapeake Ave at Woodbine Ave. Verified from a picture on Patch.com website.", "The following events were reported: Flash Flood. These occurred near station USW00093721, approximately 29.8774 km away, between 2012-08-14 21:03:00 and 2012-08-15 01:27:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front moved through the Mid Atlantic in the afternoon and evening. Scattered thunderstorms occurred with damaging winds and hail. Some storms produced flash flooding. A cold front moved through the Mid Atlantic in the afternoon and evening. Scattered thunderstorms occurred with damaging winds and hail. Some storms produced flash flooding. A cold front moved through the Mid Atlantic in the afternoon and evening. Scattered thunderstorms occurred with damaging winds and hail. Some storms produced flash flooding. A cold front moved through the Mid Atlantic in the afternoon and evening. Scattered thunderstorms occurred with damaging winds and hail. Some storms produced flash flooding. A cold front moved through the Mid Atlantic in the afternoon and evening. Scattered thunderstorms occurred with damaging winds and hail. Some storms produced flash flooding.\nEvent Narrative: There were swift water rescues ongoing in Towson. There was water, at least one foot deep, flowing into a plant nursery. Flooding continued to around Wednesday. The intersection at Route 146 and Old Bosley Road was closed due to flash flooding. This intersection reopened at 400 AM EDT. Flash flooding caused a swift water rescue along Pulaski Highway near Baltimore and Harford county lines. Taylor Ave was closed and Route 41 due to flash flooding. The road re opened at 7 am EDT.", "The following events were reported: Flood. These occurred near station USW00093721, approximately 33.12 km away, between 2012-08-15 02:30:00 and 2012-08-15 08:30:00. The flood was caused by Heavy Rain. Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: An exiting cold front over the DelMarVa became diffuse over southern Maryland and Central VA. Showers and thunderstorms formed and were mainly east of the Blue Ridge. Isolated severe was possible with damaging winds and heavy rain.\nEvent Narrative: Route 146 at Old Bosley Road was closed due to flooding.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 27.3585 km away, between 2012-08-17 19:15:00 and 2012-08-17 20:06:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front moved through the region and stalled south of the Chesapeake Bay. Continuous moisture along boundary aided in thunderstorm development with strong winds. A cold front moved through the region and stalled south of the Chesapeake Bay. Continuous moisture along boundary aided in thunderstorm development with strong winds. A cold front moved through the region and stalled south of the Chesapeake Bay. Continuous moisture along boundary aided in thunderstorm development with strong winds.\nEvent Narrative: Wind gusts in excess of 33 knots were reported at Hart Miller Island. Wind gusts in excess of 31 knots were reported at Tolchester. Wind gusts up to 47 knots were reported at Gunpowder.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 29.6128 km away, between 2012-08-26 07:00:00 and 2012-08-26 13:30:00. The events included records with estimated wind gusts of 34.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: An area of low pressure was located over the Mid Atlantic which increased tropical southerly flow to the region. Heavy rain was the main threat but isolated thunderstorms produced damaging winds and lightning. An area of low pressure was located over the Mid Atlantic which increased tropical southerly flow to the region. Heavy rain was the main threat but isolated thunderstorms produced damaging winds and lightning. An area of low pressure was located over the Mid Atlantic which increased tropical southerly flow to the region. Heavy rain was the main threat but isolated thunderstorms produced damaging winds and lightning. An area of low pressure was located over the Mid Atlantic which increased tropical southerly flow to the region. Heavy rain was the main threat but isolated thunderstorms produced damaging winds and lightning.\nEvent Narrative: Wind gusts in excess of 32 knots were reported at Thomas Point. Wind gusts in excess of 31 knots were reported at Greenbury Point. Wind gusts in excess of 31 knots were reported at Thomas Point. Wind gusts in excess of 31 knots were reported at Francis Scott Key Bridge.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 26.2336 km away, between 2012-08-26 12:45:00 and 2012-08-26 12:45:00. The events included records with estimated wind gusts of 52.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 1000.0 and crop damage of 0.0. \n\nEpisode Narrative: An area of low pressure was located over the Mid Atlantic which increased tropical southerly flow to the region. Heavy rain was the main threat but isolated thunderstorms produced damaging winds and lightning.\nEvent Narrative: There was a tree down onto power lines near the intersection of Hambleton Rd and Riva Rd.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 13.0759 km away, between 2012-08-26 13:20:00 and 2012-08-26 13:20:00. The events included records with estimated wind gusts of 52.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 500.0 and crop damage of 0.0. \n\nEpisode Narrative: An area of low pressure was located over the Mid Atlantic which increased tropical southerly flow to the region. Heavy rain was the main threat but isolated thunderstorms produced damaging winds and lightning.\nEvent Narrative: There was a tree down near intersection of Woodlawn Ave and Duvall Highway.", "The following events were reported: Flash Flood. These occurred near station USW00093721, approximately 25.1328 km away, between 2012-08-26 13:30:00 and 2012-08-26 20:00:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: An area of low pressure was located over the Mid Atlantic which increased tropical southerly flow to the region. Heavy rain was the main threat but isolated thunderstorms produced damaging winds and lightning. An area of low pressure was located over the Mid Atlantic which increased tropical southerly flow to the region. Heavy rain was the main threat but isolated thunderstorms produced damaging winds and lightning. An area of low pressure was located over the Mid Atlantic which increased tropical southerly flow to the region. Heavy rain was the main threat but isolated thunderstorms produced damaging winds and lightning. An area of low pressure was located over the Mid Atlantic which increased tropical southerly flow to the region. Heavy rain was the main threat but isolated thunderstorms produced damaging winds and lightning. An area of low pressure was located over the Mid Atlantic which increased tropical southerly flow to the region. Heavy rain was the main threat but isolated thunderstorms produced damaging winds and lightning. An area of low pressure was located over the Mid Atlantic which increased tropical southerly flow to the region. Heavy rain was the main threat but isolated thunderstorms produced damaging winds and lightning. An area of low pressure was located over the Mid Atlantic which increased tropical southerly flow to the region. Heavy rain was the main threat but isolated thunderstorms produced damaging winds and lightning. An area of low pressure was located over the Mid Atlantic which increased tropical southerly flow to the region. Heavy rain was the main threat but isolated thunderstorms produced damaging winds and lightning. An area of low pressure was located over the Mid Atlantic which increased tropical southerly flow to the region. Heavy rain was the main threat but isolated thunderstorms produced damaging winds and lightning. An area of low pressure was located over the Mid Atlantic which increased tropical southerly flow to the region. Heavy rain was the main threat but isolated thunderstorms produced damaging winds and lightning. An area of low pressure was located over the Mid Atlantic which increased tropical southerly flow to the region. Heavy rain was the main threat but isolated thunderstorms produced damaging winds and lightning. An area of low pressure was located over the Mid Atlantic which increased tropical southerly flow to the region. Heavy rain was the main threat but isolated thunderstorms produced damaging winds and lightning. An area of low pressure was located over the Mid Atlantic which increased tropical southerly flow to the region. Heavy rain was the main threat but isolated thunderstorms produced damaging winds and lightning. An area of low pressure was located over the Mid Atlantic which increased tropical southerly flow to the region. Heavy rain was the main threat but isolated thunderstorms produced damaging winds and lightning. An area of low pressure was located over the Mid Atlantic which increased tropical southerly flow to the region. Heavy rain was the main threat but isolated thunderstorms produced damaging winds and lightning. An area of low pressure was located over the Mid Atlantic which increased tropical southerly flow to the region. Heavy rain was the main threat but isolated thunderstorms produced damaging winds and lightning.\nEvent Narrative: Route 25 was closed at Ridge Road due to flash flooding. Water was flowing over the road. Three of five lanes on the I-695 outer loop were closed due to flash flooding. There was water flowing over the road. Route 129 was closed between Old Court Road and Slade Avenue. High water was present at the intersection of Falls Road and Old Pimlico Road. A vehicle was stuck in high water near Tufton Ave and Mantua Mill Road. Heavy rain caused evacuations on the 2300 block on East Monument Street due to flash flooding. Route 122 closed at I-695 due to flash flooding. Route 25 was closed at Swawan Road due to flash flooding. There was high water at the intersection of Cockeysville Road and Beaver Dam Road. There was high water at the intersection of Thornton Mill Road and York Road. There was a road closed at the intersection of MD 450 and Crownsville Road. High water was reported at Boulevard Place and South Old Annapolis Road. There was a swift water rescue at Stevenson Road and Old Valley Road. There was a road closure at Route 45 at Beaver Run due to flash flooding.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 27.9939 km away, between 2012-09-01 17:55:00 and 2012-09-01 17:55:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 500.0 and crop damage of 0.0. \n\nEpisode Narrative: A weak frontal boundary was located across the Mid Atlantic. A shortwave trough interacted with the front and scattered thunderstorms produced hail and damaging winds.\nEvent Narrative: There was a tree blocking the intersection of Greenspring Valley Road and Greenspring Ave.", "The following events were reported: Lightning. These occurred near station USW00093721, approximately 38.7873 km away, between 2012-09-01 19:05:00 and 2012-09-01 19:05:00.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 5000.0 and crop damage of 0.0. \n\nEpisode Narrative: Scattered thunderstorms that moved along a stationary front affected the Eastern Shore during the evening of the 1st.\nEvent Narrative: Lightning struck a home in Rock Hall. No injuries were reported. Lightning also caused about 170 Delmarva Power customers to lose power in Kent County.", "The following events were reported: Flash Flood. These occurred near station USW00093721, approximately 21.0724 km away, between 2012-09-03 15:45:00 and 2012-09-03 17:45:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A warm front moved north through the region as remnants of Isaac continued to influence the region. Heavy rain was the main impact during the morning but localized strong winds occurred over the Bay. A warm front moved north through the region as remnants of Isaac continued to influence the region. Heavy rain was the main impact during the morning but localized strong winds occurred over the Bay.\nEvent Narrative: The intersection of Falls Road and Clark Hill Road was closed. The intersection of Roland Avenue at Wyndhurst Road was closed.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 43.5092 km away, between 2012-09-08 13:39:00 and 2012-09-08 13:39:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 500.0 and crop damage of 0.0. \n\nEpisode Narrative: A cold front crossed WV in the morning and made it to the I-95 corridor by the evening. Increased instability led to pre frontal showers and thunderstorms that were capable of damaging winds.\nEvent Narrative: There was a tree down at Dark Hallow Road and Dover Road.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 26.5928 km away, between 2012-09-08 15:05:00 and 2012-09-08 15:29:00.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 3000.0 and crop damage of 0.0. \n\nEpisode Narrative: A cold front crossed WV in the morning and made it to the I-95 corridor by the evening. Increased instability led to pre frontal showers and thunderstorms that were capable of damaging winds. A cold front crossed WV in the morning and made it to the I-95 corridor by the evening. Increased instability led to pre frontal showers and thunderstorms that were capable of damaging winds. A cold front crossed WV in the morning and made it to the I-95 corridor by the evening. Increased instability led to pre frontal showers and thunderstorms that were capable of damaging winds. A cold front crossed WV in the morning and made it to the I-95 corridor by the evening. Increased instability led to pre frontal showers and thunderstorms that were capable of damaging winds. A cold front crossed WV in the morning and made it to the I-95 corridor by the evening. Increased instability led to pre frontal showers and thunderstorms that were capable of damaging winds.\nEvent Narrative: There was a tree down near US 50 and the US 301 North interchange. There was a six inch diameter tree down blocking the road. There was a tree down in the roadway at US 301 North at Collington Road. There was a tree down at Route 2 and Jordan Taylor Lane.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 31.9015 km away, between 2012-09-08 15:18:00 and 2012-09-08 16:00:00. The events included records with measured wind gusts of 39.09090909090909 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front crossed WV in the morning and made it to the I-95 corridor by the evening. Increased instability led to pre frontal showers and thunderstorms that were capable of damaging winds. A cold front crossed WV in the morning and made it to the I-95 corridor by the evening. Increased instability led to pre frontal showers and thunderstorms that were capable of damaging winds. A cold front crossed WV in the morning and made it to the I-95 corridor by the evening. Increased instability led to pre frontal showers and thunderstorms that were capable of damaging winds. A cold front crossed WV in the morning and made it to the I-95 corridor by the evening. Increased instability led to pre frontal showers and thunderstorms that were capable of damaging winds. A cold front crossed WV in the morning and made it to the I-95 corridor by the evening. Increased instability led to pre frontal showers and thunderstorms that were capable of damaging winds. A cold front crossed WV in the morning and made it to the I-95 corridor by the evening. Increased instability led to pre frontal showers and thunderstorms that were capable of damaging winds. A cold front crossed WV in the morning and made it to the I-95 corridor by the evening. Increased instability led to pre frontal showers and thunderstorms that were capable of damaging winds. A cold front crossed WV in the morning and made it to the I-95 corridor by the evening. Increased instability led to pre frontal showers and thunderstorms that were capable of damaging winds. A cold front crossed WV in the morning and made it to the I-95 corridor by the evening. Increased instability led to pre frontal showers and thunderstorms that were capable of damaging winds. A cold front crossed WV in the morning and made it to the I-95 corridor by the evening. Increased instability led to pre frontal showers and thunderstorms that were capable of damaging winds. A cold front crossed WV in the morning and made it to the I-95 corridor by the evening. Increased instability led to pre frontal showers and thunderstorms that were capable of damaging winds.\nEvent Narrative: Wind gusts up to 36 knots were reported at the Baltimore Key Bridge. Wind gusts up to 43 knots were reported at Patapsco Buoy. Wind gusts up to 34 knots were reported at St Mary's Elementary School. Wind gusts up to 40 knots were reported at Greenbury Point. Wind gusts up to 45 knots were reported at Tolly Point Bayside Elementary. Wind gusts up to 37 knots were reported at Stevensville. Wind gusts up to 36 knots were reported at Kent Island. Wind gusts up to 35 knots were reported at CBIBS Annapolis Buoy. Wind gusts up to 34 knots were reported at Stevensville MD. Wind gusts up to 52 knots were reported at Thomas Point Lighthouse. Wind gusts up to 38 knots were reported at St Anne's School in Annapolis.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 25.4154 km away, between 2012-09-18 14:00:00 and 2012-09-18 14:58:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 5000.0 and crop damage of 0.0. \n\nEpisode Narrative: A cold front moved through the region and showers and severe thunderstorms occurred across the Mid Atlantic. A strong low level jet drove activity through the Interstate 95 corridor and abundant amounts of moisture produced heavy rain. A cold front moved through the region and showers and severe thunderstorms occurred across the Mid Atlantic. A strong low level jet drove activity through the Interstate 95 corridor and abundant amounts of moisture produced heavy rain. A cold front moved through the region and showers and severe thunderstorms occurred across the Mid Atlantic. A strong low level jet drove activity through the Interstate 95 corridor and abundant amounts of moisture produced heavy rain. A cold front moved through the region and showers and severe thunderstorms occurred across the Mid Atlantic. A strong low level jet drove activity through the Interstate 95 corridor and abundant amounts of moisture produced heavy rain. A cold front moved through the region and showers and severe thunderstorms occurred across the Mid Atlantic. A strong low level jet drove activity through the Interstate 95 corridor and abundant amounts of moisture produced heavy rain. A cold front moved through the region and showers and severe thunderstorms occurred across the Mid Atlantic. A strong low level jet drove activity through the Interstate 95 corridor and abundant amounts of moisture produced heavy rain. A cold front moved through the region and showers and severe thunderstorms occurred across the Mid Atlantic. A strong low level jet drove activity through the Interstate 95 corridor and abundant amounts of moisture produced heavy rain.\nEvent Narrative: There were tree limbs down that closed Coon Club Road. There was a tree onto wires along Tank Road. There was a tree blown down in Severna Park. There were large tree limbs snapped off tree on 700 block of Macsherry Drive. There were downed trees covering right lane of Maryland State Route 295 near 197. A pear tree was split in half by thunderstorm winds. There were wind gusts estimated of 50 to 60 mph.", "The following events were reported: Flash Flood. These occurred near station USW00093721, approximately 13.3307 km away, between 2012-09-18 14:41:00 and 2012-09-18 17:30:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front moved through the region and showers and severe thunderstorms occurred across the Mid Atlantic. A strong low level jet drove activity through the Interstate 95 corridor and abundant amounts of moisture produced heavy rain.\nEvent Narrative: There was approximately one foot of water over National Pike near Ingleside Road.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 28.4014 km away, between 2012-09-18 23:25:00 and 2012-09-18 23:25:00. The events included records with measured wind gusts of 36.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front moved through the region and showers and severe thunderstorms occurred across the Mid Atlantic. A strong low level jet drove activity through the Interstate 95 corridor and abundant amounts of moisture produced heavy rain.\nEvent Narrative: Wind gusts of up to 36 knots were reported at Hartmiller Island.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 38.106 km away, between 2012-09-22 18:42:00 and 2012-09-22 18:42:00. The events included records with measured wind gusts of 40.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front moved through the Mid Atlantic in the evening. Convection formed due to low level moisture transport ahead the cold front and low level convergence near the upper Chesapeake Bay. Storms were capable of gusty winds.\nEvent Narrative: Wind gusts up to 40 knots were reported at Tolchester Beach.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 38.106 km away, between 2012-09-30 16:30:00 and 2012-09-30 16:30:00. The events included records with estimated wind gusts of 34.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A large upper trough of low pressure was over the Northeast U.S. Shortwave energy rounded the base of the upper trough and scattered showers capable of hail and gusty winds were able to form over parts of the Chesapeake Bay and Potomac River.\nEvent Narrative: Wind gusts in excess of 31 knots were reported at Tolchester Beach.", "The following events were reported: Flood. These occurred near station USW00093721, approximately 29.0666 km away, between 2012-10-02 10:00:00 and 2012-10-02 15:30:00. The flood was caused by Heavy Rain. Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 1000.0 and crop damage of 0.0. \n\nEpisode Narrative: An upper level low over the Ohio Valley aided in moisture advection from the south-southeast as a warm front moved north through Virginia. Low pressure to the west moved north and showers with heavy rainfall continued. An upper level low over the Ohio Valley aided in moisture advection from the south-southeast as a warm front moved north through Virginia. Low pressure to the west moved north and showers with heavy rainfall continued. An upper level low over the Ohio Valley aided in moisture advection from the south-southeast as a warm front moved north through Virginia. Low pressure to the west moved north and showers with heavy rainfall continued.\nEvent Narrative: There was a road closed near the intersection of Emery Road and Hollingsworth Road due to water across the roadway. There was a road closed near the intersection of Bushy Park Road and Carrs Mill Road due to water across the roadway. There was a road closed near the intersection of Shaffers Mill Road and Shaffersville Road due to water across the roadway. A tree fell on a car near the intersection of Washington Blvd and Patuxent Park Road and it was believed to be due to high water not strong winds.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 38.106 km away, between 2012-10-19 20:06:00 and 2012-10-19 20:06:00. The events included records with estimated wind gusts of 34.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front moved eastward through the Mid Atlantic and was located east of the Blue Ridge Mountains in the evening. Conditions were favorable for showers and thunderstorms to develop with high shear values. Tornado-genesis occurred in Northeast Maryland.\nEvent Narrative: Wind gusts in excess of 31 knots were reported at Tolchester Buoy.", "The following events were reported: Flood. These occurred near station USW00093721, approximately 35.2575 km away, between 2012-10-29 08:00:00 and 2012-10-29 23:00:00. The flood was caused by Heavy Rain. Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 700000.0 and crop damage of 0.0. \n\nEpisode Narrative: Post Tropical Storm Sandy caused an initial estimate of $5 million dollars in damage in the Eastern Shore of Maryland. Most of the damages were due to flooding caused by excessive rainfall, as up to 13 inches of rain were reported, and due to the high winds, which caused trees and wires to come down across the state. Delmarva Power, which serves portions of the eastern shore counties, reported over 30,000 households without power during the peak of the storm. The majority of residents had power returned by the morning of the 30th. Hundreds of roads were closed due to numerous downed trees and flooding. | |No direct deaths were reported on the Eastern Shore of Maryland due to the storm.||Tropical Storm Sandy formed in the Caribbean Sea on the 22nd of October. After drifting slowly southwest into the 23rd, Sandy turned to the north and intensified to a hurricane on the 24th just before making landfall in Jamaica during that afternoon. Hurricane Sandy continued to the north and intensified to a strong category two hurricane before making landfall again in Cuba shortly after Midnight EDT on the 25th. Hurricane Sandy emerged on the other side of Cuba during the morning of the 25th and proceeded to drift northwest as a category one or two hurricane as it moved through the Bahamas on the 25th and 26th. Overnight on the 26th, Hurricane Sandy (Category 1) started to move toward the north-northeast, a motion that continued into the evening of the 28th. From there, Sandy\ufffd\ufffd\ufffds motion became driven by two factors. An anomalously strong blocking ridge over the Canadian Maritimes prevented Sandy from escaping to the east. Simultaneously, an approaching and deepening middle latitude trough was about to capture Sandy. The combination of the two, turned Sandy to the north overnight on the 28th and then to the northwest on the 29th. Hurricane Sandy received one last jolt of tropical energy as it passed across the Gulf Stream during the morning of the 29th. The lowest recorded central pressure of 940 millibars (27.76 inches) occurred when Category 1 Hurricane Sandy was about 110 miles southeast of Atlantic City at 2 p.m. EDT on the 29th. As Sandy continued to move northwest and interact with the mid latitude trough, its interaction continued to make it less tropical, but did not weaken it much. Sandy continued to make a harder turn to the left (west) and made landfall in Atlantic County as a post tropical storm in Brigantine City just north of Atlantic City at 730 p.m. EDT on the 29th. The estimated minimum central pressure was 945 millibars. The lowest recorded central pressure was 945.6 millibars at the Atlantic City Marina at 734 p.m. EDT. From there, Sandy continued to weaken or fill as it moved west. At 9 p.m. EDT, the low pressure system was in western Atlantic County and continued to move west-northwest. At 11 p.m. EDT, the post tropical storm (about 954 millibars) was located in southern Chester County. Post tropical storm Sandy continued to move west-northwest and weaken. At 2 a.m. EDT on the 30th, the 962 millibar low was located near Harrisburg, Pennsylvania and at 8 a.m. EDT the 979 millibar low was near Altoona, Pennsylvania. From there, the rapidly weakening low pressure system moved northwest and reached Lake Erie (993 millibars) at 8 p.m. EDT that evening and from there drifted north into Canada. ||Prior to Sandy's arrival, Governor Martin O'Malley declared a State of Emergency for Maryland. No mandatory evacuations were ordered prior to or during the storm on the Eastern Shore. The Chesapeake Bay Bridge was closed due to high winds just before 3 p.m. on the 29th and remained closed through about 9 a.m. on the 30th. The state also closed the Millard E. Tydings Memorial Bridge, where Interstate 95 crosses the Susquehanna River. A swift water rescue teams from South Carolina were on standby throughout the storm and thankfully were not utilized. In addition, several shelters were opened across the state, including three in Cecil County and two each in Kent, Queen Anne's and Caroline Counties.||In the Chesapeake Bay, moderate tidal flooding occurred during the afternoon high tide cycle on the 29th at Cambridge and during the early morning high tide on the 30th at Tolchester Beach. The storm surge was 3 to 3.5 feet. The region was spared higher surges as Sandy made landfall in New Jersey and the winds prior to landfall pushed water down the Chesapeake Bay. Minor tidal flooding also occurred at Tolchester Beach during the subsequent afternoon high tide cycle on the 30th. ||Heavy rains fell across the area as Sandy approached and then moved through the region. This made it easier for shallow rooted and leafed trees to be uprooted, it also complicated the tidal flooding. Event rainfall totals ranged from just under 6 inches across the northern areas to up near 13 inches across the southern areas of the Eastern Shore. The steady rain associated with Sandy spread into the Eastern Shore during the day on the 28th and slowly edged north. The heaviest rain fell overnight on the 28th into the early evening of the 29th. The rain ended during the middle of the day on the 30th.||Peak wind gusts included 60 mph in Tolchester Beach (Kent County), 59 mph in Bay City (Queen Anne's County), 55 mph in Royal Oak (Talbot County), 53 mph at the Stevensville Airport (Queen Anne's County), 48 mph at the Easton Airport (Talbot County), 47 mph in Colora (Cecil County) and 41 mph near Jumptown (Caroline County). Strong winds spread northward along the Wastern Shore on the morning of the 29th with the highest winds (from the west) occurring during the evening of the 29th. Winds decreased rapidly during the early morning (shortly after Midnight) on the 30th.\nEvent Narrative: The heavy rain that fell across Queen Anne's County not only caused poor drainage flooding, but exacerbated the tidal flooding along the Chesapeake Bay. Event precipitation totals included 9.89 inches in Queenstown, 6.77 inches in Stevensville and 4.50 inches in Centreville.", "The following events were reported: Flood. These occurred near station USW00093721, approximately 16.2022 km away, between 2012-10-29 10:29:00 and 2012-10-31 05:15:00. The flood was caused by Heavy Rain. Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Hurricane Sandy moved up the Atlantic coast and then turned Northwest and made landfall northeast of MD. Heavy rain and high winds over spread coastal regions and most of Maryland. Heavy rain caused flood and river flooding. Hurricane Sandy moved up the Atlantic coast and then turned Northwest and made landfall northeast of MD. Heavy rain and high winds over spread coastal regions and most of Maryland. Heavy rain caused flood and river flooding. Hurricane Sandy moved up the Atlantic coast and then turned Northwest and made landfall northeast of MD. Heavy rain and high winds over spread coastal regions and most of Maryland. Heavy rain caused flood and river flooding. Hurricane Sandy moved up the Atlantic coast and then turned Northwest and made landfall northeast of MD. Heavy rain and high winds over spread coastal regions and most of Maryland. Heavy rain caused flood and river flooding.\nEvent Narrative: Theses places were flooded: MD 450 was flooded and closed by streams between Huntwood Drive and Saint Stephens Church Road and MD176 flooded between Central Ave and MD 648. There roads were impacted: Wolfsville Rd flooded at Crow Rock Road where it meets the Middle Creek and MD 103 was closed at Business Parkway. Maryland 542 was flooded at I-695. There were reports of flooding: the right lane was closed of US 50 east between exits 11 and 13 and the western branch was flooded at Water Street in Upper Marlboro. The stream gauge there crested at 930am at over 15 feet.", "The following events were reported: Flash Flood. These occurred near station USW00093721, approximately 37.7823 km away, between 2013-01-30 20:55:00 and 2013-01-31 04:00:00.The events resulted in 0 injuries and 1 fatalities. No significant property or crop damage was reported. \n\nEpisode Narrative: A upper level trough was moving eastward and across most of the eastern U.S. with a surface low pressure center across the eastern Great Lakes. A cold front moved through the Mid Atlantic with dew points in the low 60s ahead of frontal passage. A strong low level jet on the eastern side of trough aided in strong winds reaching the surface. Flood and flash flood also occurred along or just ahead of the frontal passage. A upper level trough was moving eastward and across most of the eastern U.S. with a surface low pressure center across the eastern Great Lakes. A cold front moved through the Mid Atlantic with dew points in the low 60s ahead of frontal passage. A strong low level jet on the eastern side of trough aided in strong winds reaching the surface. Flood and flash flood also occurred along or just ahead of the frontal passage. A upper level trough was moving eastward and across most of the eastern U.S. with a surface low pressure center across the eastern Great Lakes. A cold front moved through the Mid Atlantic with dew points in the low 60s ahead of frontal passage. A strong low level jet on the eastern side of trough aided in strong winds reaching the surface. Flood and flash flood also occurred along or just ahead of the frontal passage. A upper level trough was moving eastward and across most of the eastern U.S. with a surface low pressure center across the eastern Great Lakes. A cold front moved through the Mid Atlantic with dew points in the low 60s ahead of frontal passage. A strong low level jet on the eastern side of trough aided in strong winds reaching the surface. Flood and flash flood also occurred along or just ahead of the frontal passage.\nEvent Narrative: There was flooding at the intersection of Dutrow Road and Carrollton Road. Road was damaged. There was a bridge under water near the intersection of Marston Road and Sims Creek Road. Shaffersville Road was flooded at Shaffers Mill Road. A homeless woman drowned as rains flooded a homeless camp in Maryland City near the Patuxent River. Also, there were two females extracted from their vehicle stuck in standing water at Brock Bridge Road and Whiskey Bottom Road.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 33.9935 km away, between 2013-01-31 01:48:00 and 2013-01-31 01:48:00. The events included records with measured wind gusts of 51.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A upper level trough was moving eastward and across most of the eastern U.S. with a surface low pressure center across the eastern Great Lakes. A cold front moved through the Mid Atlantic with dew points in the low 60s ahead of frontal passage. A strong low level jet on the eastern side of trough aided in strong winds reaching the surface. Flood and flash flood also occurred along or just ahead of the frontal passage.\nEvent Narrative: Wind gusts up to 51 knots were reported at Tolly Point.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 34.4426 km away, between 2013-04-12 07:30:00 and 2013-04-12 08:00:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: An upper level disturbance moved through the Mid Atlantic ahead of an approaching cold front. Showers and thunderstorms moved across the waters producing gusty winds. An upper level disturbance moved through the Mid Atlantic ahead of an approaching cold front. Showers and thunderstorms moved across the waters producing gusty winds. An upper level disturbance moved through the Mid Atlantic ahead of an approaching cold front. Showers and thunderstorms moved across the waters producing gusty winds. An upper level disturbance moved through the Mid Atlantic ahead of an approaching cold front. Showers and thunderstorms moved across the waters producing gusty winds.\nEvent Narrative: Winds of 41 knots were measured at Annapolis Buoy. Winds of 34 knots were measured at Greenbury Point. Winds in excess of 31 knots were measured at Kent Island. Winds in excess of 32 knots were measured at Thomas Point Lighthouse.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 22.7279 km away, between 2013-04-19 18:27:00 and 2013-04-19 18:27:00. The events included records with estimated wind gusts of 60.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 20000.0 and crop damage of 10000.0. \n\nEpisode Narrative: A cold front moved across the Mid Atlantic and was accompanied by showers and thunderstorms that produced gusty winds. A strong jet of 50 knot winds was located at 850 mb or about a mile off the surface.\nEvent Narrative: There were 80 trees down in a community. The trees were into homes and across roads.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 33.9935 km away, between 2013-04-19 18:44:00 and 2013-04-19 18:44:00. The events included records with measured wind gusts of 48.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front moved across the waters and was accompanied by showers and thunderstorms that produced gusty winds. A strong jet of 50 knot winds was located at 850 mb or about a mile off the surface.\nEvent Narrative: Winds in excess of 48 knots were measured at Tolly Point.", "The following events were reported: Hail. These occurred near station USW00093721, approximately 10.4488 km away, between 2013-05-08 14:54:00 and 2013-05-08 14:54:00. The events included records with hailstones measuring 1.0 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Low pressure tracked northeast of the Mid Atlantic. While most of the forcing was north of the region, easterly flow transported moisture into the region and surface convergence led to storms that produced heavy rainfall, large hail and damaging winds.\nEvent Narrative:", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 25.5973 km away, between 2013-05-10 20:38:00 and 2013-05-10 22:00:00. The events included records with estimated wind gusts of 34.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Low pressure over the Ohio Valley and an associated cold front approached the mountains. Southerly flow transported moisture into the region. Upper level jet dynamics were stronger across the Ohio Valley. Low pressure over the Ohio Valley and an associated cold front approached the mountains. Southerly flow transported moisture into the region. Upper level jet dynamics were stronger across the Ohio Valley. Low pressure over the Ohio Valley and an associated cold front approached the mountains. Southerly flow transported moisture into the region. Upper level jet dynamics were stronger across the Ohio Valley.\nEvent Narrative: Wind gusts in excess of 31 knots were measured at Key Bridge. Wind gusts in excess of 31 knots were measured at Patapsco Buoy. Wind gusts in excess of 33 knots were measured at Thomas Point Lighthouse.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 46.3866 km away, between 2013-05-11 14:37:00 and 2013-05-11 14:37:00. The events included records with estimated wind gusts of 52.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 0.0 and crop damage of 1000.0. \n\nEpisode Narrative: Low pressure and an associated cold front crossed the Mid Atlantic. Ahead of this system, southerly flow transported moisture into the region. Thunderstorm wind damage was the main threat.\nEvent Narrative: There were trees down near intersection of Carrs Mill Road and Wildwood Drive.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 25.373 km away, between 2013-05-11 17:20:00 and 2013-05-11 17:20:00. The events included records with estimated wind gusts of 35.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Low pressure and an associated cold front crossed the Mid Atlantic. Ahead of this system, southerly flow transported moisture into the region. Thunderstorm wind damage was the main threat.\nEvent Narrative: Winds gusts of 35 knots were measured at the Patapsco Buoy.", "The following events were reported: Flash Flood. These occurred near station USW00093721, approximately 18.1094 km away, between 2013-05-23 18:43:00 and 2013-05-23 21:30:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front was approaching from the west. Ahead of it temperatures reached their convective temps and wind speeds increased. Thunderstorms formed along a lee trough. A cold front was approaching from the west. Ahead of it temperatures reached their convective temps and wind speeds increased. Thunderstorms formed along a lee trough.\nEvent Narrative: MD state route 97 was flooded and closed at the intersection with MD route 144 near Cooksville. There was a swift water rescue at Mcendree and Rover Mill Roads.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 27.9129 km away, between 2013-06-02 17:30:00 and 2013-06-02 18:37:00. The events included records with estimated wind gusts of 34.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Low pressure across the Southern Great Lakes with a associated cold front moved eastward through the Ohio Valley. A surface trough was located along Potomac Highlands and dew points rose into the low 70s. Showers and thunderstorms moved across the region. Low pressure across the Southern Great Lakes with a associated cold front moved eastward through the Ohio Valley. A surface trough was located along Potomac Highlands and dew points rose into the low 70s. Showers and thunderstorms moved across the region. Low pressure across the Southern Great Lakes with a associated cold front moved eastward through the Ohio Valley. A surface trough was located along Potomac Highlands and dew points rose into the low 70s. Showers and thunderstorms moved across the region.\nEvent Narrative: Wind gusts in excess of 33 knots were measured at the Baltimore Key Bridge. Wind gusts in excess of 31 knots were measured at Annapolis Buoy. Wind gusts in excess of 34 knots were measured at Kent Island.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 33.6934 km away, between 2013-06-03 15:32:00 and 2013-06-03 15:32:00. The events included records with estimated wind gusts of 34.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front moved slowly through the Mid Atlantic and surface heating in the afternoon led to showers and thunderstorms to form in an unstable environment.\nEvent Narrative: Wind gusts in excess of 32 knots were measured at Hartmiller Island.", "The following events were reported: Tornado. These occurred near station USW00093721, approximately 25.278 km away, between 2013-06-10 14:24:00 and 2013-06-10 14:45:00.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 11000.0 and crop damage of 3000.0. \n\nEpisode Narrative: A warm front moved through the region and the Mid Atlantic was located in the warm moist sector. Convergence led to numerous showers and thunderstorms to develop in an atmosphere with high shear. Heavy rain, damaging winds and tornadoes were observed. A warm front moved through the region and the Mid Atlantic was located in the warm moist sector. Convergence led to numerous showers and thunderstorms to develop in an atmosphere with high shear. Heavy rain, damaging winds and tornadoes were observed.\nEvent Narrative: Eyewitness accounts and storm damage survey concluded a small tornado occurred in Fork, MD, from approximately 3:28 to 3:30 PM EDT on June 10, 2013. ||About six trees were uprooted in the Mount Vista Estates subdivision of Fork along Vista View Court. These trees were a mix of hardwood and softwood, some falling at angles of up to 120 degrees from each other. Several eyewitnesses saw swirling debris within the wind field as the damage was occurring. Additional tree damage along with damage to a wood fence was located across the street from Fork United Methodist Church on Fork Road, approximately 0.5 miles North of the damage in Mount Vista Estates. The survey team crossed the path between these two points, as well as up to two miles on either end of the damage, but no further damage could be found. A metal building structure in the south Locust Point Marine Terminal was damaged when a waterspout over the Patapsco River came onshore, transforming to a small tornado from approximately 3:44 to 3:45 PM EDT on June 10, 2013.||The metal building structure had a portion of its northeast roof peeled up, wrapping it back and folding it over the east-facing side of the building. Additionally, a small trailer on wheels was demolished as it was propelled to the northwest about 60 feet from its position on Cinder Blocks. An air conditioning unit which was permanently installed in the wall of an office on the north facing side of the building in proximity to where the roof damage occurred was blown-in. A large amount of debris was seen plastered to a east-facing chain link fence on the north side of the parking lot.||Areas to the north Marine Terminal were also surveyed, and no further damage was found.", "The following events were reported: Flash Flood. These occurred near station USW00093721, approximately 23.9717 km away, between 2013-06-10 15:00:00 and 2013-06-10 23:50:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A warm front moved through the region and the Mid Atlantic was located in the warm moist sector. Convergence led to numerous showers and thunderstorms to develop in an atmosphere with high shear. Heavy rain, damaging winds and tornadoes were observed. A warm front moved through the region and the Mid Atlantic was located in the warm moist sector. Convergence led to numerous showers and thunderstorms to develop in an atmosphere with high shear. Heavy rain, damaging winds and tornadoes were observed. A warm front moved through the region and the Mid Atlantic was located in the warm moist sector. Convergence led to numerous showers and thunderstorms to develop in an atmosphere with high shear. Heavy rain, damaging winds and tornadoes were observed. A warm front moved through the region and the Mid Atlantic was located in the warm moist sector. Convergence led to numerous showers and thunderstorms to develop in an atmosphere with high shear. Heavy rain, damaging winds and tornadoes were observed.\nEvent Narrative: The Baltimore beltway was flooded at Frederick Road. There was high water at Route 1 business which closed at two locations in Bel Air. There was water observed up to the hoods of cars in the 500 block of South Charles Street. There was a road closed due to flooding at Annapolis Road and Superior Lane.", "The following events were reported: Flash Flood. These occurred near station USW00093721, approximately 19.5744 km away, between 2013-06-10 15:30:00 and 2013-06-13 17:30:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front stalled across the Mid Atlantic and low pressure formed and moved along it. Southerly flow advected gulf moisture into the region and showers and thunderstorms easily formed. Heavy rain, hail, damaging winds and tornadoes occurred throughout the day. A cold front stalled across the Mid Atlantic and low pressure formed and moved along it. Southerly flow advected gulf moisture into the region and showers and thunderstorms easily formed. Heavy rain, hail, damaging winds and tornadoes occurred throughout the day. A cold front stalled across the Mid Atlantic and low pressure formed and moved along it. Southerly flow advected gulf moisture into the region and showers and thunderstorms easily formed. Heavy rain, hail, damaging winds and tornadoes occurred throughout the day.\nEvent Narrative: Falls Road was flooded just south of Shawan Road near Oregon Branch. There was flooding on Meadowridge Road at Roosevelt Blvd in Elkridge. Security Blvd was flooded and closed at the Baltimore Beltway.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 32.4165 km away, between 2013-06-10 20:00:00 and 2013-06-10 21:10:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A warm front moved through the region and the Mid Atlantic was located in the warm moist sector. Convergence led to numerous showers and thunderstorms to develop in an atmosphere with high shear. Heavy rain, damaging winds and tornadoes were observed. A warm front moved through the region and the Mid Atlantic was located in the warm moist sector. Convergence led to numerous showers and thunderstorms to develop in an atmosphere with high shear. Heavy rain, damaging winds and tornadoes were observed. A warm front moved through the region and the Mid Atlantic was located in the warm moist sector. Convergence led to numerous showers and thunderstorms to develop in an atmosphere with high shear. Heavy rain, damaging winds and tornadoes were observed. A warm front moved through the region and the Mid Atlantic was located in the warm moist sector. Convergence led to numerous showers and thunderstorms to develop in an atmosphere with high shear. Heavy rain, damaging winds and tornadoes were observed. A warm front moved through the region and the Mid Atlantic was located in the warm moist sector. Convergence led to numerous showers and thunderstorms to develop in an atmosphere with high shear. Heavy rain, damaging winds and tornadoes were observed. A warm front moved through the region and the Mid Atlantic was located in the warm moist sector. Convergence led to numerous showers and thunderstorms to develop in an atmosphere with high shear. Heavy rain, damaging winds and tornadoes were observed.\nEvent Narrative: Wind gusts of 31 knots were measured at Thomas Point Light. Wind gusts of 37 knots were measured at Tolly Point. Wind gusts of 32 knots were measured at Greenbury Point. Wind gusts of 46 knots were measured at Thomas Point Lighthouse. Wind gusts in excess of 35 knots were measured at Patapsco Buoy. Wind gusts of 33 knots were measured at Annapolis Buoy.", "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00093721, approximately 24.8259 km away, between 2013-06-13 07:17:00 and 2013-06-13 15:45:00. The events included records with hailstones measuring 47.31818181818182 inches.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 7500.0 and crop damage of 4750.0. \n\nEpisode Narrative: A cold front stalled across the Mid Atlantic and low pressure formed and moved along it. Southerly flow advected gulf moisture into the region and showers and thunderstorms easily formed. Heavy rain, hail, damaging winds and tornadoes occurred throughout the day. A cold front stalled across the Mid Atlantic and low pressure formed and moved along it. Southerly flow advected gulf moisture into the region and showers and thunderstorms easily formed. Heavy rain, hail, damaging winds and tornadoes occurred throughout the day. A cold front stalled across the Mid Atlantic and low pressure formed and moved along it. Southerly flow advected gulf moisture into the region and showers and thunderstorms easily formed. Heavy rain, hail, damaging winds and tornadoes occurred throughout the day. A cold front stalled across the Mid Atlantic and low pressure formed and moved along it. Southerly flow advected gulf moisture into the region and showers and thunderstorms easily formed. Heavy rain, hail, damaging winds and tornadoes occurred throughout the day. A cold front stalled across the Mid Atlantic and low pressure formed and moved along it. Southerly flow advected gulf moisture into the region and showers and thunderstorms easily formed. Heavy rain, hail, damaging winds and tornadoes occurred throughout the day. A cold front stalled across the Mid Atlantic and low pressure formed and moved along it. Southerly flow advected gulf moisture into the region and showers and thunderstorms easily formed. Heavy rain, hail, damaging winds and tornadoes occurred throughout the day. A cold front stalled across the Mid Atlantic and low pressure formed and moved along it. Southerly flow advected gulf moisture into the region and showers and thunderstorms easily formed. Heavy rain, hail, damaging winds and tornadoes occurred throughout the day. A cold front stalled across the Mid Atlantic and low pressure formed and moved along it. Southerly flow advected gulf moisture into the region and showers and thunderstorms easily formed. Heavy rain, hail, damaging winds and tornadoes occurred throughout the day. A cold front stalled across the Mid Atlantic and low pressure formed and moved along it. Southerly flow advected gulf moisture into the region and showers and thunderstorms easily formed. Heavy rain, hail, damaging winds and tornadoes occurred throughout the day. A cold front stalled across the Mid Atlantic and low pressure formed and moved along it. Southerly flow advected gulf moisture into the region and showers and thunderstorms easily formed. Heavy rain, hail, damaging winds and tornadoes occurred throughout the day. A cold front stalled across the Mid Atlantic and low pressure formed and moved along it. Southerly flow advected gulf moisture into the region and showers and thunderstorms easily formed. Heavy rain, hail, damaging winds and tornadoes occurred throughout the day.\nEvent Narrative: There was a large tree limb six inches in diameter down. There was one tree down at 14910 Dunston Lane. A large tree fell next to the Annapolis Police Station on Taylor Street damaging a fence, a vehicle and breaking a window in the building. There was one tree uprooted into a house at 5900 Parkway Drive. There was a tree down on Park Hall Drive near Sandy Spring Road. There was a tree down at 10700 Scaggsville Road. There was a tree down along All Saints Road. A tree fell onto a house in Jessup while another tree was down around Apple Ave and Orchard Av. There were trees and wires down.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 33.2364 km away, between 2013-06-13 08:26:00 and 2013-06-13 16:01:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front stalled across the Mid Atlantic and low pressure formed and moved along it. Southerly flow advected gulf moisture into the region and showers and thunderstorms easily formed. Heavy rain, hail, damaging winds and tornadoes occurred throughout the day. A cold front stalled across the Mid Atlantic and low pressure formed and moved along it. Southerly flow advected gulf moisture into the region and showers and thunderstorms easily formed. Heavy rain, hail, damaging winds and tornadoes occurred throughout the day. A cold front stalled across the Mid Atlantic and low pressure formed and moved along it. Southerly flow advected gulf moisture into the region and showers and thunderstorms easily formed. Heavy rain, hail, damaging winds and tornadoes occurred throughout the day. A cold front stalled across the Mid Atlantic and low pressure formed and moved along it. Southerly flow advected gulf moisture into the region and showers and thunderstorms easily formed. Heavy rain, hail, damaging winds and tornadoes occurred throughout the day. A cold front stalled across the Mid Atlantic and low pressure formed and moved along it. Southerly flow advected gulf moisture into the region and showers and thunderstorms easily formed. Heavy rain, hail, damaging winds and tornadoes occurred throughout the day. A cold front stalled across the Mid Atlantic and low pressure formed and moved along it. Southerly flow advected gulf moisture into the region and showers and thunderstorms easily formed. Heavy rain, hail, damaging winds and tornadoes occurred throughout the day. A cold front stalled across the Mid Atlantic and low pressure formed and moved along it. Southerly flow advected gulf moisture into the region and showers and thunderstorms easily formed. Heavy rain, hail, damaging winds and tornadoes occurred throughout the day. A cold front stalled across the Mid Atlantic and low pressure formed and moved along it. Southerly flow advected gulf moisture into the region and showers and thunderstorms easily formed. Heavy rain, hail, damaging winds and tornadoes occurred throughout the day. A cold front stalled across the Mid Atlantic and low pressure formed and moved along it. Southerly flow advected gulf moisture into the region and showers and thunderstorms easily formed. Heavy rain, hail, damaging winds and tornadoes occurred throughout the day. A cold front stalled across the Mid Atlantic and low pressure formed and moved along it. Southerly flow advected gulf moisture into the region and showers and thunderstorms easily formed. Heavy rain, hail, damaging winds and tornadoes occurred throughout the day. A cold front stalled across the Mid Atlantic and low pressure formed and moved along it. Southerly flow advected gulf moisture into the region and showers and thunderstorms easily formed. Heavy rain, hail, damaging winds and tornadoes occurred throughout the day. A cold front stalled across the Mid Atlantic and low pressure formed and moved along it. Southerly flow advected gulf moisture into the region and showers and thunderstorms easily formed. Heavy rain, hail, damaging winds and tornadoes occurred throughout the day. A cold front stalled across the Mid Atlantic and low pressure formed and moved along it. Southerly flow advected gulf moisture into the region and showers and thunderstorms easily formed. Heavy rain, hail, damaging winds and tornadoes occurred throughout the day. A cold front stalled across the Mid Atlantic and low pressure formed and moved along it. Southerly flow advected gulf moisture into the region and showers and thunderstorms easily formed. Heavy rain, hail, damaging winds and tornadoes occurred throughout the day. A cold front stalled across the Mid Atlantic and low pressure formed and moved along it. Southerly flow advected gulf moisture into the region and showers and thunderstorms easily formed. Heavy rain, hail, damaging winds and tornadoes occurred throughout the day.\nEvent Narrative: Wind gusts of 40 knots were measured at Bayside Elementary School. Wind gusts of 35 knots were measured at Kent Island(KNT). Wind gusts in excess of 31 knots were measured at Patapsco Buoy. Wind gusts in excess of 39 knots were measured at Hartmiller Island. Wind gusts in excess of 39 knots were measured at Patapsco Buoy. Wind gusts in excess of 39 knots at Tolchester Beach. Wind gusts in excess of 37 knots were reported at Greenbury Point. Wind gusts in excess of 33 knots were measured at Annapolis Buoy. Wind gusts of 40 knots were measured at Tolly Point. Wind gusts of 36 knots were measured at Thomas Point Lighthouse. Wind gusts of 59 knots were measured at Greenbury Point (GBY). Wind gusts of 40 knots were measured at Annapolis Buoy. Wind gusts of 50 knots were measured at Tolly Point. Wind gusts of 50 knots were measured at Tolchester Beach. Wind gusts of 48 knots were measured at Stevenville.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 38.0834 km away, between 2013-06-13 15:40:00 and 2013-06-13 15:49:00.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 1000.0 and crop damage of 0.0. \n\nEpisode Narrative: An early morning low end derecho moved through the region on the 13th which caused strong to severe thunderstorms to develop across eastern Maryland. The derecho moved off the New Jersey coast by late morning leaving a boundary across parts of the region. Later in the day, a strong low pressure system brought a cold front through the region, which sparked off more strong to severe thunderstorms across the area.||In addition to wind, heavy rain was reported with these storms. Most locations saw up to an inch of rain fall, with locally higher amounts of up to 2 inches reported. Rainfall amounts included 1.81 inches in Worton (Kent County), 0.98 inches in Elkton (Cecil County) and 0.88 inches in Greensboro (Caroline County). An early morning low end derecho moved through the region on the 13th which caused strong to severe thunderstorms to develop across eastern Maryland. The derecho moved off the New Jersey coast by late morning leaving a boundary across parts of the region. Later in the day, a strong low pressure system brought a cold front through the region, which sparked off more strong to severe thunderstorms across the area.||In addition to wind, heavy rain was reported with these storms. Most locations saw up to an inch of rain fall, with locally higher amounts of up to 2 inches reported. Rainfall amounts included 1.81 inches in Worton (Kent County), 0.98 inches in Elkton (Cecil County) and 0.88 inches in Greensboro (Caroline County).\nEvent Narrative: A severe thunderstorm produced a 68 mph wind gust in Stevensville. The roof and fence were damaged at Kent Island High School. In addition, Kent Island High School baseball dugout was destroyed by a large gust of wind.", "The following events were reported: Flash Flood. These occurred near station USW00093721, approximately 41.3332 km away, between 2013-06-17 21:20:00 and 2013-06-18 00:30:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Thunderstorms with torrential downpours caused flash flooding in Kent County during the evening of the 17th.\nEvent Narrative: Thunderstorms with torrential downpours caused flash flooding in the western half of Kent County. Doppler Radar storm total estimates reached 3 to 5 inches. Roadways were impassable due to the flooding in Kennedyville and Fairlee. One water rescue was performed in Chestertown.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 31.1083 km away, between 2013-06-18 14:40:00 and 2013-06-18 14:40:00. The events included records with measured wind gusts of 58.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A weak cold front was stalled over the area. Convergence along the boundary led to heavy showers. A few breaks in the clouds led to an increase in instability and thunderstorms that produced heavy rain in activity.\nEvent Narrative: Wind gusts of 58 knots were measured at Annapolis Buoy.", "The following events were reported: Flash Flood. These occurred near station USW00093721, approximately 43.5579 km away, between 2013-06-18 15:23:00 and 2013-06-18 17:23:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A weak cold front was stalled over the area. Convergence along the boundary led to heavy showers. A few breaks in the clouds led to an increase in instability and thunderstorms that produced heavy rain in activity.\nEvent Narrative: Route 468 and other major roads were flooded in several places. There was 2.7 inches of rainfall in 2.25 hours.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 39.4857 km away, between 2013-06-25 20:50:00 and 2013-06-25 21:48:00.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 1000.0 and crop damage of 2750.0. \n\nEpisode Narrative: A subtropical ridge was over the Mid Atlantic with northwesterly flow leading to hot and humid conditions. This led to a unstable atmosphere and thunderstorms formed. A subtropical ridge was over the Mid Atlantic with northwesterly flow leading to hot and humid conditions. This led to a unstable atmosphere and thunderstorms formed. A subtropical ridge was over the Mid Atlantic with northwesterly flow leading to hot and humid conditions. This led to a unstable atmosphere and thunderstorms formed. A subtropical ridge was over the Mid Atlantic with northwesterly flow leading to hot and humid conditions. This led to a unstable atmosphere and thunderstorms formed. A subtropical ridge was over the Mid Atlantic with northwesterly flow leading to hot and humid conditions. This led to a unstable atmosphere and thunderstorms formed.\nEvent Narrative: There was one large pine tree snapped and several other large limbs downed from other trees. One limb was on a vehicle. The damage was isolated to three homes in the community. There was a large tree down blocking northbound lanes of MD 152 at Rochelle Road. There were a couple of five inch diameter tree limbs broken.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 30.537 km away, between 2013-06-25 21:30:00 and 2013-06-25 23:00:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A subtropical ridge was over the Mid Atlantic with northwesterly flow leading to hot and humid conditions. This led to a unstable atmosphere and thunderstorms formed. A subtropical ridge was over the Mid Atlantic with northwesterly flow leading to hot and humid conditions. This led to a unstable atmosphere and thunderstorms formed. A subtropical ridge was over the Mid Atlantic with northwesterly flow leading to hot and humid conditions. This led to a unstable atmosphere and thunderstorms formed. A subtropical ridge was over the Mid Atlantic with northwesterly flow leading to hot and humid conditions. This led to a unstable atmosphere and thunderstorms formed. A subtropical ridge was over the Mid Atlantic with northwesterly flow leading to hot and humid conditions. This led to a unstable atmosphere and thunderstorms formed. A subtropical ridge was over the Mid Atlantic with northwesterly flow leading to hot and humid conditions. This led to a unstable atmosphere and thunderstorms formed. A subtropical ridge was over the Mid Atlantic with northwesterly flow leading to hot and humid conditions. This led to a unstable atmosphere and thunderstorms formed. A subtropical ridge was over the Mid Atlantic with northwesterly flow leading to hot and humid conditions. This led to a unstable atmosphere and thunderstorms formed. A subtropical ridge was over the Mid Atlantic with northwesterly flow leading to hot and humid conditions. This led to a unstable atmosphere and thunderstorms formed. A subtropical ridge was over the Mid Atlantic with northwesterly flow leading to hot and humid conditions. This led to a unstable atmosphere and thunderstorms formed. A subtropical ridge was over the Mid Atlantic with northwesterly flow leading to hot and humid conditions. This led to a unstable atmosphere and thunderstorms formed. A subtropical ridge was over the Mid Atlantic with northwesterly flow leading to hot and humid conditions. This led to a unstable atmosphere and thunderstorms formed.\nEvent Narrative: Wind gusts of 35 knots were measured at Greenbury Point. Wind gusts of 37 knots were measured at Annapolis Buoy. Wind gusts of 37 knots were measured at Tolly Point. Wind gusts in excess of 33 knots were measured at Kent Island. Wind gusts of 36 knots were measured at Thomas Point. Wind gusts of 36 knots were measured at Thomas Point. Wind gusts of 32 knots were measured at Baltimore. Wind gusts of 35 knots were measured at Baltimore Key Bridge. Wind gusts of 42 knots were measured at Hartmiller Island. Wind gusts of 37 knots were measured at Patpsco Buoy. Wind gusts of 35 knots were measured at Tolchester Beach. Wind gusts in excess of 32 knots were measured at Stevenville.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 13.4848 km away, between 2013-06-26 16:20:00 and 2013-06-26 16:20:00. The events included records with estimated wind gusts of 52.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 0.0 and crop damage of 500.0. \n\nEpisode Narrative: A subtropical ridge was present over the Mid Atlantic and hot and humid conditions persisted. This led to an unstable atmosphere. A shortwave trough moved into the Mid Atlantic and showers and thunderstorms formed that were capable of strong winds.\nEvent Narrative: There was a tree down on West Lombard Street.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 38.106 km away, between 2013-06-26 17:06:00 and 2013-06-26 17:12:00. The events included records with measured wind gusts of 36.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A subtropical ridge was present over the Mid Atlantic and hot and humid conditions persisted. This led to an unstable atmosphere. A shortwave trough moved into the Mid Atlantic and showers and thunderstorms formed that were capable of strong winds.\nEvent Narrative: Wind gusts of 36 knots were measured at Tolchester Beach.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 35.0305 km away, between 2013-06-28 16:00:00 and 2013-06-28 18:50:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: High pressure was anchored off shore while low pressure spun over the Great Lakes. A shortwave trough moved over the region initiating showers and thunderstorms in vicinity of a surface trough. High pressure was anchored off shore while low pressure spun over the Great Lakes. A shortwave trough moved over the region initiating showers and thunderstorms in vicinity of a surface trough. High pressure was anchored off shore while low pressure spun over the Great Lakes. A shortwave trough moved over the region initiating showers and thunderstorms in vicinity of a surface trough.\nEvent Narrative: Wind gusts in excess of 32 knots were measured at Thomas Point Lighthouse. Wind gusts of 37 knots were measured at Annapolis Buoy. Wind gusts in excess of 31 knots were measured at Thomas Point Lighthouse.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 30.0409 km away, between 2013-06-30 11:18:00 and 2013-06-30 11:18:00. The events included records with estimated wind gusts of 34.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A plume of moisture continued along the eastern seaboard and multiple shortwave troughs moved over the region. A few showers and thunderstorms formed along a diffuse dew point boundary.\nEvent Narrative: Wind gusts in excess of 33 knots were measured at Greenbury Point.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 27.9384 km away, between 2013-07-07 17:40:00 and 2013-07-07 17:58:00. The events included records with estimated wind gusts of 34.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: An upper level disturbance moved over the Mid Atlantic. Hot and humid conditions persisted across the Mid Atlantic. Marginal instability helped produce strong winds. An upper level disturbance moved over the Mid Atlantic. Hot and humid conditions persisted across the Mid Atlantic. Marginal instability helped produce strong winds. An upper level disturbance moved over the Mid Atlantic. Hot and humid conditions persisted across the Mid Atlantic. Marginal instability helped produce strong winds.\nEvent Narrative: Wind gusts of 31 knots were estimated at Hartmiller Island. Wind gusts of 31 knots were estimated at Patapsco Buoy. Wind gusts of 32 knots were estimated at Tolchester Beach.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 32.8695 km away, between 2013-07-10 18:30:00 and 2013-07-10 20:22:00. The events included records with estimated wind gusts of 40.2 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A Bermuda High continued to usher tropical moisture into the Mid Atlantic. A shortwave trough ahead of the main trough produced showers and thunderstorms in the unsettled region. A Bermuda High continued to usher tropical moisture into the Mid Atlantic. A shortwave trough ahead of the main trough produced showers and thunderstorms in the unsettled region. A Bermuda High continued to usher tropical moisture into the Mid Atlantic. A shortwave trough ahead of the main trough produced showers and thunderstorms in the unsettled region. A Bermuda High continued to usher tropical moisture into the Mid Atlantic. A shortwave trough ahead of the main trough produced showers and thunderstorms in the unsettled region. A Bermuda High continued to usher tropical moisture into the Mid Atlantic. A shortwave trough ahead of the main trough produced showers and thunderstorms in the unsettled region. A Bermuda High continued to usher tropical moisture into the Mid Atlantic. A shortwave trough ahead of the main trough produced showers and thunderstorms in the unsettled region. A Bermuda High continued to usher tropical moisture into the Mid Atlantic. A shortwave trough ahead of the main trough produced showers and thunderstorms in the unsettled region. A Bermuda High continued to usher tropical moisture into the Mid Atlantic. A shortwave trough ahead of the main trough produced showers and thunderstorms in the unsettled region. A Bermuda High continued to usher tropical moisture into the Mid Atlantic. A shortwave trough ahead of the main trough produced showers and thunderstorms in the unsettled region. A Bermuda High continued to usher tropical moisture into the Mid Atlantic. A shortwave trough ahead of the main trough produced showers and thunderstorms in the unsettled region.\nEvent Narrative: Wind gusts of 45 knots were measured at Thomas Point Lighthouse. Wind gusts of 39 knots were measured at Tolly Point. Wind gusts of 31 knots were estimated at Kent Island. Wind gusts of 48 knots were measured at Greenbury Point. Wind gusts of 41 knots were measured at Annapolis Buoy. Wind gusts of 37 knots were measured at Patapsco Buoy. Wind gusts of 37 knots were measured at Hartmiller Island. Wind gusts of 36 knots were measured at Tolchester Beach. Wind gusts of 39 knots were measured at Annapolis Buoy. Wind gusts of 46 knots were measured at Thomas Point Lighthouse.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 36.8716 km away, between 2013-07-12 03:28:00 and 2013-07-12 05:00:00. The events included records with estimated wind gusts of 37.333333333333336 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A frontal boundary moved northward and stalled over the Mid-Atlantic/I-95 corridor overnight. An upper level low approached the region and a upper level jet added to enhanced lift in the region. Heavy rain caused a lot of flash flooding with amounts up to seven inches in less than 6 hours recorded near Washington Dulles Airport. Showers also produced gusty winds on the waters. A frontal boundary moved northward and stalled over the Mid-Atlantic/I-95 corridor overnight. An upper level low approached the region and a upper level jet added to enhanced lift in the region. Heavy rain caused a lot of flash flooding with amounts up to seven inches in less than 6 hours recorded near Washington Dulles Airport. Showers also produced gusty winds on the waters. A frontal boundary moved northward and stalled over the Mid-Atlantic/I-95 corridor overnight. An upper level low approached the region and a upper level jet added to enhanced lift in the region. Heavy rain caused a lot of flash flooding with amounts up to seven inches in less than 6 hours recorded near Washington Dulles Airport. Showers also produced gusty winds on the waters.\nEvent Narrative: Wind gusts of 35 knots were measured at Kent Island. Wind gusts of 40 knots were measured at Thomas Point Lighthouse. Wind gusts of 37 knots were measured at Tolly Point.", "The following events were reported: Flash Flood. These occurred near station USW00093721, approximately 37.5595 km away, between 2013-07-12 04:30:00 and 2013-07-12 07:30:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A low pressure system that developed along a cold frontal boundary brought showers and thunderstorms with very heavy downpours to the Eastern Shore, especially during the first half of the day into the early afternoon on the 12th. This caused flash flooding in parts of Queen Anne's, Caroline and Talbot Counties and poor drainage flooding in other parts of the Eastern Shore. Doppler Radar storm total estimates reached 3 to 7 inches in sections of the latter counties.\nEvent Narrative: Thunderstorms with torrential doownpours caused flash flooding on Kent Island during the morning of the 12th. Doppler Radar storm total estimates reached 7 inches south of Stevensville. Flash flooding was reported on Maryland State Route 8 from Batts Neck Road southward. Event precipitation totals included 5.64 inches in Stevensville and 3.60 inches in Centreville.", "The following events were reported: Flash Flood. These occurred near station USW00093721, approximately 31.5014 km away, between 2013-07-12 04:50:00 and 2013-07-12 06:50:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A frontal boundary moved northward and stalled over the Mid-Atlantic/I-95 corridor overnight. An upper level low approached the region and a upper level jet added to enhanced lift in the region. Heavy rain caused a lot of flash flooding with amounts up to seven inches in less than 6 hours recorded near Washington Dulles Airport.\nEvent Narrative: The 400 block of Walnut Drive was closed due to flooding.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 10.4222 km away, between 2013-07-19 16:50:00 and 2013-07-19 16:50:00. The events included records with estimated wind gusts of 52.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 0.0 and crop damage of 250.0. \n\nEpisode Narrative: High pressure was off the South Carolina coast. Warm and humid conditions existed across the Mid Atlantic and isolated thunderstorms formed over the higher terrain.\nEvent Narrative: There was a tree down on Baltimore Washington Parkway.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 30.5746 km away, between 2013-07-21 15:50:00 and 2013-07-21 15:53:00. The events included records with estimated wind gusts of 34.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A weak cold front moved southward into the Mid Atlantic. A line of showers and thunderstorms formed and moved southward and heavy rain and gusty winds were observed. A weak cold front moved southward into the Mid Atlantic. A line of showers and thunderstorms formed and moved southward and heavy rain and gusty winds were observed.\nEvent Narrative: Wind gusts of 33 knots were measured at Annapolis Buoy. Wind gusts of 34 knots were measured at Greenbury Point.", "The following events were reported: Flash Flood. These occurred near station USW00093721, approximately 30.7106 km away, between 2013-07-21 16:30:00 and 2013-07-21 18:30:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A weak cold front moved southward into the Mid Atlantic. A line of showers and thunderstorms formed and moved southward and heavy rain was observed.\nEvent Narrative: There were two roads with 6 to 12 inches of flowing water over them. One of the roads had a foot of ponding and one swift water rescue.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 38.106 km away, between 2013-07-23 00:00:00 and 2013-07-23 00:00:00. The events included records with estimated wind gusts of 34.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A surface trough was over the area while an upper level disturbance moved overhead. Showers and thunderstorms produced heavy rainfall as they moved eastward towards the I-95 corridor and surrounding waters.\nEvent Narrative: Wind gusts of 34 knots were measured at Tolchester Beach.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 49.5487 km away, between 2013-07-28 22:50:00 and 2013-07-28 22:50:00. The events included records with estimated wind gusts of 52.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 0.0 and crop damage of 250.0. \n\nEpisode Narrative: An upper level low was over the Great Lakes and a cold front moved through the Mid Atlantic. Warm and humid conditions, with dew points in the 70s, were ahead of the cold front and led to destabilization. The majority of the thunderstorms with wind damage moved through North Central MD.\nEvent Narrative: There was a tree down on the 1400 block of Boggs Road.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 32.9273 km away, between 2013-08-09 16:00:00 and 2013-08-09 17:00:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front moved through the Mid Atlantic the evening. Warm conditions during the day led to increased instability and showers and thunderstorms formed due to convergence. A cold front moved through the Mid Atlantic the evening. Warm conditions during the day led to increased instability and showers and thunderstorms formed due to convergence. A cold front moved through the Mid Atlantic the evening. Warm conditions during the day led to increased instability and showers and thunderstorms formed due to convergence. A cold front moved through the Mid Atlantic the evening. Warm conditions during the day led to increased instability and showers and thunderstorms formed due to convergence. A cold front moved through the Mid Atlantic the evening. Warm conditions during the day led to increased instability and showers and thunderstorms formed due to convergence. A cold front moved through the Mid Atlantic the evening. Warm conditions during the day led to increased instability and showers and thunderstorms formed due to convergence.\nEvent Narrative: Wind gusts in excess of 34 knots were measured at Annapolis. Wind gusts in excess of 37 knots were measured at Greenbury Point. Wind gusts in excess of 40 knots were measured at Tolly Point. Wind gusts in excess of 39 knots were measured at Annapolis Buoy. Wind gusts in excess of 33 knots were measured at Stevensville. Wind gusts in excess of 33 knots were measured at Thomas Point Lighthouse.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 43.704 km away, between 2013-08-13 16:52:00 and 2013-08-13 16:52:00. The events included records with estimated wind gusts of 52.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 0.0 and crop damage of 2000.0. \n\nEpisode Narrative: An upper level disturbance moved ahead of an approaching cold front. Southerly flow ahead of system led to increased moisture and warmer temperatures. There was enough instability to produce gusty winds, heavy rain and a tornado.\nEvent Narrative: There were trees down with debris.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 36.9916 km away, between 2013-09-02 01:00:00 and 2013-09-02 01:00:00. The events included records with measured wind gusts of 34.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A shortwave moved over the region overnight and showers and thunderstorms formed in the I-95 corridor.\nEvent Narrative: Wind gusts of 34 knots were measured at Thomas Point Lighthouse.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 22.9765 km away, between 2013-09-12 12:24:00 and 2013-09-12 15:47:00. The events included records with estimated wind gusts of 52.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 0.0 and crop damage of 3500.0. \n\nEpisode Narrative: A cold front moved through the region and a surface trough was located near the I-95 corridor. Southerly flow ahead of the cold front brought warm and humid conditions to the area. This led to instability and showers and thunderstorms formed near the pressure trough. A cold front moved through the region and a surface trough was located near the I-95 corridor. Southerly flow ahead of the cold front brought warm and humid conditions to the area. This led to instability and showers and thunderstorms formed near the pressure trough. A cold front moved through the region and a surface trough was located near the I-95 corridor. Southerly flow ahead of the cold front brought warm and humid conditions to the area. This led to instability and showers and thunderstorms formed near the pressure trough. A cold front moved through the region and a surface trough was located near the I-95 corridor. Southerly flow ahead of the cold front brought warm and humid conditions to the area. This led to instability and showers and thunderstorms formed near the pressure trough. A cold front moved through the region and a surface trough was located near the I-95 corridor. Southerly flow ahead of the cold front brought warm and humid conditions to the area. This led to instability and showers and thunderstorms formed near the pressure trough.\nEvent Narrative: There were several trees down in the 8000 Block of Philadelphia Road. There were trees down on Whites Road in Severna Park. There were trees down near the intersection of Cypress Ridge Drive and Governor Ritchie Highway. A five inch in diameter tree was reported uprooted blocking Baltimore Annapolis Boulevard at Address 802. There was a tree down near the intersection of Reese Road and Carrollton Road.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 31.1576 km away, between 2013-09-12 13:10:00 and 2013-09-12 17:40:00. The events included records with measured wind gusts of 36.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front moved through the region and a surface trough was located near the I-95 corridor. Southerly flow ahead of the cold front brought warm and humid conditions to the area. This led to instability and showers and thunderstorms formed near the pressure trough. A cold front moved through the region and a surface trough was located near the I-95 corridor. Southerly flow ahead of the cold front brought warm and humid conditions to the area. This led to instability and showers and thunderstorms formed near the pressure trough. A cold front moved through the region and a surface trough was located near the I-95 corridor. Southerly flow ahead of the cold front brought warm and humid conditions to the area. This led to instability and showers and thunderstorms formed near the pressure trough.\nEvent Narrative: Wind gusts of 35 knots were measured at Patapsco Buoy. Wind gusts of 39 knots were measured at Thomas Point Lighthouse. Wind gusts of 33 knots were measured at Annapolis Buoy.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 34.1268 km away, between 2013-10-07 11:30:00 and 2013-10-07 13:00:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: An upper level trough moved through the Mid West and warm moist air was in place across the Mid Atlantic. Showers and thunderstorms crossed the Potomac Highlands in the morning and across the I-95 corridor by early afternoon. Thunderstorms were capable of damaging wind gusts. An upper level trough moved through the Mid West and warm moist air was in place across the Mid Atlantic. Showers and thunderstorms crossed the Potomac Highlands in the morning and across the I-95 corridor by early afternoon. Thunderstorms were capable of damaging wind gusts. An upper level trough moved through the Mid West and warm moist air was in place across the Mid Atlantic. Showers and thunderstorms crossed the Potomac Highlands in the morning and across the I-95 corridor by early afternoon. Thunderstorms were capable of damaging wind gusts. An upper level trough moved through the Mid West and warm moist air was in place across the Mid Atlantic. Showers and thunderstorms crossed the Potomac Highlands in the morning and across the I-95 corridor by early afternoon. Thunderstorms were capable of damaging wind gusts. An upper level trough moved through the Mid West and warm moist air was in place across the Mid Atlantic. Showers and thunderstorms crossed the Potomac Highlands in the morning and across the I-95 corridor by early afternoon. Thunderstorms were capable of damaging wind gusts. An upper level trough moved through the Mid West and warm moist air was in place across the Mid Atlantic. Showers and thunderstorms crossed the Potomac Highlands in the morning and across the I-95 corridor by early afternoon. Thunderstorms were capable of damaging wind gusts. An upper level trough moved through the Mid West and warm moist air was in place across the Mid Atlantic. Showers and thunderstorms crossed the Potomac Highlands in the morning and across the I-95 corridor by early afternoon. Thunderstorms were capable of damaging wind gusts. An upper level trough moved through the Mid West and warm moist air was in place across the Mid Atlantic. Showers and thunderstorms crossed the Potomac Highlands in the morning and across the I-95 corridor by early afternoon. Thunderstorms were capable of damaging wind gusts. An upper level trough moved through the Mid West and warm moist air was in place across the Mid Atlantic. Showers and thunderstorms crossed the Potomac Highlands in the morning and across the I-95 corridor by early afternoon. Thunderstorms were capable of damaging wind gusts.\nEvent Narrative: Wind gusts of 36 knots were measured at Gunpowder. Wind gusts of 36 knots were measured at Deerfield Elementary School. Wind gusts of 33 knots were measured at Patapsco Buoy. Wind gusts of 34 knots were measured at Greenbury Point. Wind gusts of 32 knots were measured at Sandy Point. Wind gusts of 45 knots were measured at Tolchester. Wind gusts of 35 knots were measured at Annapolis Buoy. Wind gusts of 32 knots were measured at Thomas Point. Wind gusts of 34 knots were measured at Thomas Point.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 36.363 km away, between 2013-11-01 06:45:00 and 2013-11-01 06:48:00. The events included records with estimated wind gusts of 52.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 0.0 and crop damage of 500.0. \n\nEpisode Narrative: A cold front crossed the Mid Atlantic in the morning and showers and thunderstorms moved across the highlands. Strong winds above the surface were able to mix down and damaging wind gusts were reported. A cold front crossed the Mid Atlantic in the morning and showers and thunderstorms moved across the highlands. Strong winds above the surface were able to mix down and damaging wind gusts were reported.\nEvent Narrative: There was a tree down at Liberty High School on Bartholow Road. There was a tree down at Louisville Road near the county line.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 33.0514 km away, between 2013-11-18 02:57:00 and 2013-11-18 03:20:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A strong cold front moved across the Mid Atlantic early in the morning. Showers and thunderstorms were able to tap into a strong low level jet and bring strong gusts to the surface. A strong cold front moved across the Mid Atlantic early in the morning. Showers and thunderstorms were able to tap into a strong low level jet and bring strong gusts to the surface. A strong cold front moved across the Mid Atlantic early in the morning. Showers and thunderstorms were able to tap into a strong low level jet and bring strong gusts to the surface. A strong cold front moved across the Mid Atlantic early in the morning. Showers and thunderstorms were able to tap into a strong low level jet and bring strong gusts to the surface. A strong cold front moved across the Mid Atlantic early in the morning. Showers and thunderstorms were able to tap into a strong low level jet and bring strong gusts to the surface.\nEvent Narrative: Wind gust of 32 knots were measured at Annapolis. Wind gusts of 31 knots were measured at Greenbury Point. Wind gusts of 40 knots were measured at Thomas Point Lighthouse. Wind gusts of 31 knots were measured at Tolly Point. Wind gusts of 32 knots were measured at the Bay Bridge.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 33.4902 km away, between 2014-01-06 05:50:00 and 2014-01-06 06:00:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front moved through the Mid Atlantic in the morning. Showers brought down strong winds across the waters. A cold front moved through the Mid Atlantic in the morning. Showers brought down strong winds across the waters. A cold front moved through the Mid Atlantic in the morning. Showers brought down strong winds across the waters.\nEvent Narrative: Wind gusts of 31 knots were measured at CBIBS Patapsco Buoy. Wind gusts of 38 knots were measured at Tochester. Wind gusts of 32 knots were measured at Thomas Point.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 35.4925 km away, between 2014-01-11 12:31:00 and 2014-01-11 14:50:00. The events included records with estimated wind gusts of 34.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front moved through the Mid Atlantic and surface heating ahead of the front led to an unstable air mass in Southern Maryland. A line of showers with embedded thunderstorms led to gusty winds. A cold front moved through the Mid Atlantic and surface heating ahead of the front led to an unstable air mass in Southern Maryland. A line of showers with embedded thunderstorms led to gusty winds.\nEvent Narrative: Wind gusts of 34 knots were measured at Thomas Point. Wind gusts of 32 knots were measured at Tolly Point.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 25.5432 km away, between 2014-02-21 12:53:00 and 2014-02-21 14:07:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Southerly flow ahead of an advancing cold front brought warm and moist conditions into the Mid Atlantic. An upper level jet along with a cold front led to showers and thunderstorms to move across the region. Southerly flow ahead of an advancing cold front brought warm and moist conditions into the Mid Atlantic. An upper level jet along with a cold front led to showers and thunderstorms to move across the region. Southerly flow ahead of an advancing cold front brought warm and moist conditions into the Mid Atlantic. An upper level jet along with a cold front led to showers and thunderstorms to move across the region. Southerly flow ahead of an advancing cold front brought warm and moist conditions into the Mid Atlantic. An upper level jet along with a cold front led to showers and thunderstorms to move across the region.\nEvent Narrative: Wind gusts of 34 knots were measured at Maryland Science Center. Wind gusts of 32 knots were measured at Tolchester. Wind gusts of 31 knots were measured at Thomas Point. Wind gusts of 34 knots were measured at Maryland Science Center.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 44.9678 km away, between 2014-03-12 18:20:00 and 2014-03-12 18:20:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A line of strong to isolated severe thunderstorms preceding a strong cold front moved through the Eastern Shore during the early evening of the 12th.\nEvent Narrative: A severe thunderstorm knocked down a few large tree limbs and caused isolated power outages along Main Street in Kent Narrows.", "The following events were reported: Flood. These occurred near station USW00093721, approximately 49.6431 km away, between 2014-04-15 15:14:00 and 2014-04-15 18:14:00. The flood was caused by Heavy Rain. Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front moved across the I-95 corridor in the afternoon. Showers were passing through the I-95 corridor throughout the day and localized flooding occurred in areas with low flash flood guidance which led to rises on rivers and flooding on roadways.\nEvent Narrative: Route 7 was reported closed between routes 136 and 543 due to flooding.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 32.5509 km away, between 2014-04-25 17:31:00 and 2014-04-25 18:00:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A shortwave trough moved across the Mid Atlantic while a cold front lagged behind. Southerly flow led to unstable conditions and showers and thunderstorms developed in the afternoon and evening. A few thunderstorms produced gusty winds across the waters. A shortwave trough moved across the Mid Atlantic while a cold front lagged behind. Southerly flow led to unstable conditions and showers and thunderstorms developed in the afternoon and evening. A few thunderstorms produced gusty winds across the waters.\nEvent Narrative: Wind gusts of 32 knots were reported at Tolly Point. Wind gusts of 31 knots were reported at CBIBS Annapolis Buoy.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 36.2403 km away, between 2014-04-26 19:02:00 and 2014-04-30 16:36:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front moved across the Mid Atlantic and gusty winds occurred with showers and isolated thunderstorms across the waters. A cold front moved across the Mid Atlantic and gusty winds occurred with showers and isolated thunderstorms across the waters. A cold front moved across the Mid Atlantic and gusty winds occurred with showers and isolated thunderstorms across the waters. A cold front moved across the Mid Atlantic and gusty winds occurred with showers and isolated thunderstorms across the waters. A cold front moved across the Mid Atlantic and gusty winds occurred with showers and isolated thunderstorms across the waters. A cold front moved across the Mid Atlantic and gusty winds occurred with showers and isolated thunderstorms across the waters.\nEvent Narrative: Wind gusts of 34 knots were reported at Bay Bridge Airport. Wind gusts of 34 knots were reported at Bayside Elementary School. Wind gusts of 32 knots were reported at Thomas Point. Wind gusts of 32 knots were reported at Tolly Point. Wind gusts of 41 knots were reported at Thomas Point. Wind gusts of 36 knots were reported at Tolly Point.", "The following events were reported: Flash Flood, Flood. These occurred near station USW00093721, approximately 24.6932 km away, between 2014-04-30 09:30:00 and 2014-04-30 23:59:00. The flood was caused by Heavy Rain. Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: The eastern half of the United States was under cyclonic flow and moisture from the Atlantic and Gulf continued to move into the Mid Atlantic. A warm front moved northward and showers and thunderstorms broke out across the area. Heavy rain produced flash flooding and rapid rises on streams and creeks. The eastern half of the United States was under cyclonic flow and moisture from the Atlantic and Gulf continued to move into the Mid Atlantic. A warm front moved northward and showers and thunderstorms broke out across the area. Heavy rain produced flash flooding and rapid rises on streams and creeks. The eastern half of the United States was under cyclonic flow and moisture from the Atlantic and Gulf continued to move into the Mid Atlantic. A warm front moved northward and showers and thunderstorms broke out across the area. Heavy rain produced flash flooding and rapid rises on streams and creeks. The eastern half of the United States was under cyclonic flow and moisture from the Atlantic and Gulf continued to move into the Mid Atlantic. A warm front moved northward and showers and thunderstorms broke out across the area. Heavy rain produced flash flooding and rapid rises on streams and creeks. The eastern half of the United States was under cyclonic flow and moisture from the Atlantic and Gulf continued to move into the Mid Atlantic. A warm front moved northward and showers and thunderstorms broke out across the area. Heavy rain produced flash flooding and rapid rises on streams and creeks. The eastern half of the United States was under cyclonic flow and moisture from the Atlantic and Gulf continued to move into the Mid Atlantic. A warm front moved northward and showers and thunderstorms broke out across the area. Heavy rain produced flash flooding and rapid rises on streams and creeks. The eastern half of the United States was under cyclonic flow and moisture from the Atlantic and Gulf continued to move into the Mid Atlantic. A warm front moved northward and showers and thunderstorms broke out across the area. Heavy rain produced flash flooding and rapid rises on streams and creeks. The eastern half of the United States was under cyclonic flow and moisture from the Atlantic and Gulf continued to move into the Mid Atlantic. A warm front moved northward and showers and thunderstorms broke out across the area. Heavy rain produced flash flooding and rapid rises on streams and creeks. The eastern half of the United States was under cyclonic flow and moisture from the Atlantic and Gulf continued to move into the Mid Atlantic. A warm front moved northward and showers and thunderstorms broke out across the area. Heavy rain produced flash flooding and rapid rises on streams and creeks. The eastern half of the United States was under cyclonic flow and moisture from the Atlantic and Gulf continued to move into the Mid Atlantic. A warm front moved northward and showers and thunderstorms broke out across the area. Heavy rain produced flash flooding and rapid rises on streams and creeks. The eastern half of the United States was under cyclonic flow and moisture from the Atlantic and Gulf continued to move into the Mid Atlantic. A warm front moved northward and showers and thunderstorms broke out across the area. Heavy rain produced flash flooding and rapid rises on streams and creeks. The eastern half of the United States was under cyclonic flow and moisture from the Atlantic and Gulf continued to move into the Mid Atlantic. A warm front moved northward and showers and thunderstorms broke out across the area. Heavy rain produced flash flooding and rapid rises on streams and creeks. The eastern half of the United States was under cyclonic flow and moisture from the Atlantic and Gulf continued to move into the Mid Atlantic. A warm front moved northward and showers and thunderstorms broke out across the area. Heavy rain produced flash flooding and rapid rises on streams and creeks. The eastern half of the United States was under cyclonic flow and moisture from the Atlantic and Gulf continued to move into the Mid Atlantic. A warm front moved northward and showers and thunderstorms broke out across the area. Heavy rain produced flash flooding and rapid rises on streams and creeks. The eastern half of the United States was under cyclonic flow and moisture from the Atlantic and Gulf continued to move into the Mid Atlantic. A warm front moved northward and showers and thunderstorms broke out across the area. Heavy rain produced flash flooding and rapid rises on streams and creeks. The eastern half of the United States was under cyclonic flow and moisture from the Atlantic and Gulf continued to move into the Mid Atlantic. A warm front moved northward and showers and thunderstorms broke out across the area. Heavy rain produced flash flooding and rapid rises on streams and creeks. The eastern half of the United States was under cyclonic flow and moisture from the Atlantic and Gulf continued to move into the Mid Atlantic. A warm front moved northward and showers and thunderstorms broke out across the area. Heavy rain produced flash flooding and rapid rises on streams and creeks. The eastern half of the United States was under cyclonic flow and moisture from the Atlantic and Gulf continued to move into the Mid Atlantic. A warm front moved northward and showers and thunderstorms broke out across the area. Heavy rain produced flash flooding and rapid rises on streams and creeks. The eastern half of the United States was under cyclonic flow and moisture from the Atlantic and Gulf continued to move into the Mid Atlantic. A warm front moved northward and showers and thunderstorms broke out across the area. Heavy rain produced flash flooding and rapid rises on streams and creeks. The eastern half of the United States was under cyclonic flow and moisture from the Atlantic and Gulf continued to move into the Mid Atlantic. A warm front moved northward and showers and thunderstorms broke out across the area. Heavy rain produced flash flooding and rapid rises on streams and creeks. The eastern half of the United States was under cyclonic flow and moisture from the Atlantic and Gulf continued to move into the Mid Atlantic. A warm front moved northward and showers and thunderstorms broke out across the area. Heavy rain produced flash flooding and rapid rises on streams and creeks. The eastern half of the United States was under cyclonic flow and moisture from the Atlantic and Gulf continued to move into the Mid Atlantic. A warm front moved northward and showers and thunderstorms broke out across the area. Heavy rain produced flash flooding and rapid rises on streams and creeks. The eastern half of the United States was under cyclonic flow and moisture from the Atlantic and Gulf continued to move into the Mid Atlantic. A warm front moved northward and showers and thunderstorms broke out across the area. Heavy rain produced flash flooding and rapid rises on streams and creeks. The eastern half of the United States was under cyclonic flow and moisture from the Atlantic and Gulf continued to move into the Mid Atlantic. A warm front moved northward and showers and thunderstorms broke out across the area. Heavy rain produced flash flooding and rapid rises on streams and creeks. The eastern half of the United States was under cyclonic flow and moisture from the Atlantic and Gulf continued to move into the Mid Atlantic. A warm front moved northward and showers and thunderstorms broke out across the area. Heavy rain produced flash flooding and rapid rises on streams and creeks. The eastern half of the United States was under cyclonic flow and moisture from the Atlantic and Gulf continued to move into the Mid Atlantic. A warm front moved northward and showers and thunderstorms broke out across the area. Heavy rain produced flash flooding and rapid rises on streams and creeks. The eastern half of the United States was under cyclonic flow and moisture from the Atlantic and Gulf continued to move into the Mid Atlantic. A warm front moved northward and showers and thunderstorms broke out across the area. Heavy rain produced flash flooding and rapid rises on streams and creeks. The eastern half of the United States was under cyclonic flow and moisture from the Atlantic and Gulf continued to move into the Mid Atlantic. A warm front moved northward and showers and thunderstorms broke out across the area. Heavy rain produced flash flooding and rapid rises on streams and creeks. The eastern half of the United States was under cyclonic flow and moisture from the Atlantic and Gulf continued to move into the Mid Atlantic. A warm front moved northward and showers and thunderstorms broke out across the area. Heavy rain produced flash flooding and rapid rises on streams and creeks. The eastern half of the United States was under cyclonic flow and moisture from the Atlantic and Gulf continued to move into the Mid Atlantic. A warm front moved northward and showers and thunderstorms broke out across the area. Heavy rain produced flash flooding and rapid rises on streams and creeks. The eastern half of the United States was under cyclonic flow and moisture from the Atlantic and Gulf continued to move into the Mid Atlantic. A warm front moved northward and showers and thunderstorms broke out across the area. Heavy rain produced flash flooding and rapid rises on streams and creeks. The eastern half of the United States was under cyclonic flow and moisture from the Atlantic and Gulf continued to move into the Mid Atlantic. A warm front moved northward and showers and thunderstorms broke out across the area. Heavy rain produced flash flooding and rapid rises on streams and creeks. The eastern half of the United States was under cyclonic flow and moisture from the Atlantic and Gulf continued to move into the Mid Atlantic. A warm front moved northward and showers and thunderstorms broke out across the area. Heavy rain produced flash flooding and rapid rises on streams and creeks. The eastern half of the United States was under cyclonic flow and moisture from the Atlantic and Gulf continued to move into the Mid Atlantic. A warm front moved northward and showers and thunderstorms broke out across the area. Heavy rain produced flash flooding and rapid rises on streams and creeks. The eastern half of the United States was under cyclonic flow and moisture from the Atlantic and Gulf continued to move into the Mid Atlantic. A warm front moved northward and showers and thunderstorms broke out across the area. Heavy rain produced flash flooding and rapid rises on streams and creeks. The eastern half of the United States was under cyclonic flow and moisture from the Atlantic and Gulf continued to move into the Mid Atlantic. A warm front moved northward and showers and thunderstorms broke out across the area. Heavy rain produced flash flooding and rapid rises on streams and creeks.\nEvent Narrative: New Hampshire Ave was closed between Brighton Knolls Drive and Gold Mine Road. Governors Bridge Road was closed due to flooding. There was water flowing across the road near the intersection of Papermill Road and Allison Road. There was water about 2 inches deep flowing across the road near 2838 Paper Mill Road. There was one to two inches of water flowing across Paper Mill Road near Hunt Valley Inn Golf Course. The Golf Course was also flooded. The stream gauge on Hawlings River at Sandy Spring exceeded the flood stage of 6.5 feet. Nearby roads were flooded. There was a stream gauge on the Patuxent River at Unity exceeded flood stage of 8 feet which flooded a nearby parking area and caused significant inflow above Brighton Dam which led to further flooding downstream. There was a small landslide the closed eastbound US 40 in Patapsco State Park near the Baltimore County Line. The stream gauge on Gwynns Falls at Villa NOVA exceeded flood stage of 11 feet flooding nearby roadways. The stream rose two feet in an hour around the time it exceeded flood stage. There were several inches of flowing water over Paper Mill Road from Western Run. The stream gauge at Little Gunpowder in Laurel Brook reached flood stage. This event peaked at 8.74 feet. At 8 feet, portions of Guyton Road began to flood. The stream gauge at Little Patuxent in Guilford reached flood stage. This event peaked at 14.02 feet. At 13 feet, water approaches the very end of Owen Brown Road. At 12 feet, water covers the bridge at South Entrance Road. Several trail bridges also begin to flood. The stream gauge at Patuxent River in Laurel reached flood stage. This event peaked at 14.72 feet. At 13 feet, the parking lot of a car dealership in Laurel begins to flood. At 10.5 feet, the MARC commuter lot near Laurel begins to flood. The stream gauge at Patapsco River in Hollofield reached flood stage. This event peaked at 12.33 feet. At 11 feet, water covers the bridge at Hollofield Road and it crosses the railroad tracks in spots. The Middle Patuxent river rose three and a half feet in less than an hour. Old Columbia road was flooded. There were numerous road closures reported within the county including water from the Middle Patuxent River flowing over Carroll Mill Road. Paper Mill Road was flooded with at least six inches of water flowing across it between Popular Hill Road and Phoenix Road. There was a landslide near North Charles St and East 26th Street. Maple Avenue was closed near Deep Run due to flooding. The stream gauge at Gwynns Falls in Baltimore reached flood stage. This event peaked at 15.68 feet. At 13 feet, water covers the bike path alongside the stream and approaches the end of Berlin Street. The stream gauge on Hawlings River near Sandy Spring exceeded flood stage flooding nearby roadways. The stream crested during the early evening hours. Backwater from Holly Creek flooded Nursery Road between Patapsco Road and Route 648. Maryland Route 176 flooded and closed between Central Avenue and Baltimore Annapolis Boulevard. South Entrance Road was flooded and closed at the Little Patuxent River. Shaffersville Road was flooded between Shaffers Mill Road and Florence Road. Shaffersville Road was flooded north of Shaffers Mill Road. The stream gauge on Beaverdam Run at Cockeysville exceeded its flood stage of 9 feet. Nearby roads were closed. Flooding became widespread near the intersection of York Road and Beaver Run Road with numerous buildings flooded and water flowing across York Road. This event peaked at 10.94 feet. The stream gauge on Whitemarsh Run in White Marsh exceeded the flood stage of 10 feet. Town Center Court began to flood. This event peaked at 13.27 feet. The stream gauge on the Little Patuxent River exceeded the flood stage of 10 feet. Laurel-Fort Mead Road was covered by water. Jones Falls was out of its banks. There was flooded reported at the Mount Washington Mill Complex and water moving across Clipper Mill Road. Water covered almost all of the pedestrian bridge paralleling Water Street, and covered Water Street from the MD 4 Westbound exit ramps to Judges Street. The stream gauge on the Patuxent River below Brighton Dam exceeded its flood stage of 9 feet. Roads below the Dam were flooded. Havilland Mill Road began to flood. The stream gauge on the Patapsco River at Catonsville exceeded its flood stage of 20 feet. River Road began to flood. The Patapsco River gauge in Elkridge at the Patapsco Valley State Park exceeded flood stage of 15 feet. Water approached structures near Patpapsco Valley State Park. The stream gauge on Gunpowder Falls at Glencoe exceeded its flood stage of 7 feet. Portions of the NC RR Trail began to flood near Glencoe. There was two feet of slowly flowing water over Governor Bridge Road. There was a car stalled in it with Occupant. York Road flooded at Beaver Run.", "The following events were reported: Flood. These occurred near station USW00093721, approximately 43.0105 km away, between 2014-04-30 17:00:00 and 2014-04-30 23:00:00. The flood was caused by Heavy Rain. Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A slow moving low pressure system and a deep southerly flow from the Gulf of Mexico and then the Atlantic Ocean dropped heavy rain across the Eastern Shore centered on the 30th. Event precipitation totals averaged from 3.5 inches to 5.5 inches, with the highest amounts in Cecil County. This caused poor drainage and field flooding as well as flooding of some creeks, mainly in Cecil County. Creek flooding in parts of Cecil County were the highest since Tropical Storm Floyd in September of 1999. The flow up the Chesapeake Bay coupled with spring astronomical tides associated with the new moon also caused minor tidal flooding. The steady rain began during the afternoon of the 29th and fell at its heaviest during the morning and afternoon of the 30th. The rain ended during the evening of the 30th.||Minor tidal flooding in Chesapeake Bay occurred during both high tide cycles on the 30th and the morning high tide cycle on May 1st. The highest tides occurred with the late afternoon and evening high tide cycle on the 30th. At Tolchester Beach, the highest tide reached 3.82 feet above mean lower low water at 842 p.m. EDT on the 30th. Minor tidal flooding starts at 3.5 feet above mean lower low water.||The heavy rain and tidal flooding was caused by the combination of a strong high pressure system that built over the Canadian Maritimes that initiated the onshore flow and a strong, but slow moving low pressure system. The low pressure system was located in northwest Missouri on the morning of the 29th. It moved northeast to near Chicago during the afternoon of the 29th. The low pressure system then became nearly stationary in southern Wisconsin as its cold front reached Ohio early on the 30th. Then a new low pressure system developed on the frontal boundary and was over Eastern Tennessee on the morning of the 30th. The low pressure system reached West Virginia during the late afternoon on the 30th as its warm front started to move through Delmarva. The low pressure system reached north central Maryland at 11 p.m. EDT on the 30th as its warm front reached extreme southeast Pennsylvania and central New Jersey. The low pressure system reached the Allentown, Pennsylvania area at 5 a.m. EDT on May 1st and then was absorbed again into the frontal boundary associated with the original low as it moved into New York State that morning. The steady rain ended as the low pressure system passed north of the Eastern Shore. But the formation of the second low pressure system and the passage of the warm front helped veer the winds from the east to the south and enhanced the surface flow that produced the tidal flooding.\nEvent Narrative: Runoff from the heavy rain that was slowed by the unusually high tide caused considerable ponding of water and flooding in poor drainage locations on Kent Island. At Tolchester Beach in Kent County, the high tide reached 3.82 feet above mean lower low water at 842 p.m. EDT on the 30th. Minor tidal flooding starts at 3.5 feet above mean lower low water.||Event precipitation totals included 4.06 inches in Stevensville.", "The following events were reported: Flood. These occurred near station USW00093721, approximately 18.6047 km away, between 2014-05-01 00:00:00 and 2014-05-01 15:52:00. The flood was caused by Heavy Rain. Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: The eastern half of the United States was under cyclonic flow and moisture from the Atlantic and Gulf continued to move into the Mid Atlantic. A warm front moved northward and showers and thunderstorms broke out across the area. Heavy rain produced flash flooding and rapid rises on streams and creeks. The eastern half of the United States was under cyclonic flow and moisture from the Atlantic and Gulf continued to move into the Mid Atlantic. A warm front moved northward and showers and thunderstorms broke out across the area. Heavy rain produced flash flooding and rapid rises on streams and creeks. The eastern half of the United States was under cyclonic flow and moisture from the Atlantic and Gulf continued to move into the Mid Atlantic. A warm front moved northward and showers and thunderstorms broke out across the area. Heavy rain produced flash flooding and rapid rises on streams and creeks. The eastern half of the United States was under cyclonic flow and moisture from the Atlantic and Gulf continued to move into the Mid Atlantic. A warm front moved northward and showers and thunderstorms broke out across the area. Heavy rain produced flash flooding and rapid rises on streams and creeks. The eastern half of the United States was under cyclonic flow and moisture from the Atlantic and Gulf continued to move into the Mid Atlantic. A warm front moved northward and showers and thunderstorms broke out across the area. Heavy rain produced flash flooding and rapid rises on streams and creeks. The eastern half of the United States was under cyclonic flow and moisture from the Atlantic and Gulf continued to move into the Mid Atlantic. A warm front moved northward and showers and thunderstorms broke out across the area. Heavy rain produced flash flooding and rapid rises on streams and creeks. The eastern half of the United States was under cyclonic flow and moisture from the Atlantic and Gulf continued to move into the Mid Atlantic. A warm front moved northward and showers and thunderstorms broke out across the area. Heavy rain produced flash flooding and rapid rises on streams and creeks.\nEvent Narrative: The stream gauge at Little Patuxent at Guilford reached flood stage. This event peaked at 14.02 feet. At 13 feet, water approached the very end of Owen Brown Road. At 12 feet water covered the bridge at South Entrance Road. Several trail bridges also began to flood. The stream gauge at Patuxent River in Laurel reached flood stage. This event peaked at 14.72 feet. At 13 feet, the parking lot of a car dealership in Laurel begins to flood. The stream gauge on Gunpowder Falls at Glencoe exceeded its flood stage of 7 feet. This event peaked at 11.63 feet. At 10.5 feet, portions of the NC RR Trail begin to flood near Glencoe. The stream gauge on the Little Patuxent River exceeded the flood stage of 10 feet. The river was still rising at 530 pm EDT and had exceeded moderate flood level at that time. This event peaked at 18.64 feet. At 16 ft, Laurel-Fort Mead Road is covered by water. The Patapsco river gauge in Elkridge at the Patapsco Valley State Park exceeded flood stage of 15 feet. The river was still rising as of 530 PM EDT and had risen to major flood level. This event peaked at 21.15 feet. At 21 feet, water approaches structures near Patpapsco Valley State Park. The stream gauge on the Patapsco river at Catonsville exceeded its flood stage of 20 feet. The river was near crest at 530 PM EDT at 23.83 feet. The stream gauge on the Patuxent River below Brighton Dam exceeded its flood stage of 9 feet. Roads below the dam were flooded. This event peaked at 12.52 feet. At 9 ft, Havilland Mill Road begins to flood.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 13.916 km away, between 2014-05-10 12:48:00 and 2014-05-10 13:02:00. The events included records with estimated wind gusts of 34.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Moisture moved into the the region as a upper level trough moved across the Great Lakes. Destabilization occurred as cloud cover led to many breaks of sunshine across the Mid Atlantic. Showers and thunderstorms formed near and the Blue Ridge Mountains and tracked eastward. Moisture moved into the the region as a upper level trough moved across the Great Lakes. Destabilization occurred as cloud cover led to many breaks of sunshine across the Mid Atlantic. Showers and thunderstorms formed near and the Blue Ridge Mountains and tracked eastward.\nEvent Narrative: Wind gusts of 32 knots were measured at the Baltimore Key Bridge. Wind gusts of 31 knots were measured at Oriole Park at Camden Yards.", "The following events were reported: Flood. These occurred near station USW00093721, approximately 22.8368 km away, between 2014-05-16 06:58:00 and 2014-05-16 20:00:00. The flood was caused by Heavy Rain. Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A deep upper level trough tapped into Gulf and Atlantic moisture which led to heavy rain across the Mid Atlantic. Tropical-like conditions resulted in showers and thunderstorms to persist before a cold front moved through later in the day. A deep upper level trough tapped into Gulf and Atlantic moisture which led to heavy rain across the Mid Atlantic. Tropical-like conditions resulted in showers and thunderstorms to persist before a cold front moved through later in the day. A deep upper level trough tapped into Gulf and Atlantic moisture which led to heavy rain across the Mid Atlantic. Tropical-like conditions resulted in showers and thunderstorms to persist before a cold front moved through later in the day. A deep upper level trough tapped into Gulf and Atlantic moisture which led to heavy rain across the Mid Atlantic. Tropical-like conditions resulted in showers and thunderstorms to persist before a cold front moved through later in the day.\nEvent Narrative: The river gauge at Glencoe reached flood stage. The river gauge at Unity reached flood stage. The river gauge at Savage reached flood stage. There was flooding on MD 176 and MD 648.", "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00093721, approximately 27.8919 km away, between 2014-05-22 04:55:00 and 2014-05-22 15:29:00. The events included records with hailstones measuring 19.25 inches.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 0.0 and crop damage of 3250.0. \n\nEpisode Narrative: A warm front lifted northward across the Mid-Atlantic and showers and thunderstorms formed across the Central Foothills where breaks in the clouds led to increased instability. Thunderstorms spread east and north as the boundary moved northward. A warm front lifted northward across the Mid-Atlantic and showers and thunderstorms formed across the Central Foothills where breaks in the clouds led to increased instability. Thunderstorms spread east and north as the boundary moved northward. A warm front lifted northward across the Mid-Atlantic and showers and thunderstorms formed across the Central Foothills where breaks in the clouds led to increased instability. Thunderstorms spread east and north as the boundary moved northward. A warm front lifted northward across the Mid-Atlantic and showers and thunderstorms formed across the Central Foothills where breaks in the clouds led to increased instability. Thunderstorms spread east and north as the boundary moved northward. A warm front lifted northward across the Mid-Atlantic and showers and thunderstorms formed across the Central Foothills where breaks in the clouds led to increased instability. Thunderstorms spread east and north as the boundary moved northward. A warm front lifted northward across the Mid-Atlantic and showers and thunderstorms formed across the Central Foothills where breaks in the clouds led to increased instability. Thunderstorms spread east and north as the boundary moved northward. A warm front lifted northward across the Mid-Atlantic and showers and thunderstorms formed across the Central Foothills where breaks in the clouds led to increased instability. Thunderstorms spread east and north as the boundary moved northward. A warm front lifted northward across the Mid-Atlantic and showers and thunderstorms formed across the Central Foothills where breaks in the clouds led to increased instability. Thunderstorms spread east and north as the boundary moved northward. A warm front lifted northward across the Mid-Atlantic and showers and thunderstorms formed across the Central Foothills where breaks in the clouds led to increased instability. Thunderstorms spread east and north as the boundary moved northward. A warm front lifted northward across the Mid-Atlantic and showers and thunderstorms formed across the Central Foothills where breaks in the clouds led to increased instability. Thunderstorms spread east and north as the boundary moved northward. A warm front lifted northward across the Mid-Atlantic and showers and thunderstorms formed across the Central Foothills where breaks in the clouds led to increased instability. Thunderstorms spread east and north as the boundary moved northward. A warm front lifted northward across the Mid-Atlantic and showers and thunderstorms formed across the Central Foothills where breaks in the clouds led to increased instability. Thunderstorms spread east and north as the boundary moved northward. A warm front lifted northward across the Mid-Atlantic and showers and thunderstorms formed across the Central Foothills where breaks in the clouds led to increased instability. Thunderstorms spread east and north as the boundary moved northward. A warm front lifted northward across the Mid-Atlantic and showers and thunderstorms formed across the Central Foothills where breaks in the clouds led to increased instability. Thunderstorms spread east and north as the boundary moved northward. A warm front lifted northward across the Mid-Atlantic and showers and thunderstorms formed across the Central Foothills where breaks in the clouds led to increased instability. Thunderstorms spread east and north as the boundary moved northward. A warm front lifted northward across the Mid-Atlantic and showers and thunderstorms formed across the Central Foothills where breaks in the clouds led to increased instability. Thunderstorms spread east and north as the boundary moved northward. A warm front lifted northward across the Mid-Atlantic and showers and thunderstorms formed across the Central Foothills where breaks in the clouds led to increased instability. Thunderstorms spread east and north as the boundary moved northward.\nEvent Narrative: There was a tree down on Brock Bridge Road at Laurel Fort Meade Road. There was a tree reported down on power lines on Gold Mine Road at Chandlee Mill Road. There were two trees down just west of Highland. One pine tree was one foot in diameter snapped halfway up fell on power lines. The other tree was a large Bradford Pear Tree. There was a tree down near the intersection of Maddox Lane and Laurel Bowie Road. There was a tree down in the driveway on Oxhill Court in Bowie. There was a tree reported down at the entrance to Bowie State University.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 39.9347 km away, between 2014-05-22 16:01:00 and 2014-05-22 16:01:00. The events included records with estimated wind gusts of 34.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A warm front lifted northward across the Mid-Atlantic and showers and thunderstorms formed across the Central Foothills where breaks in the clouds led to increased instability. Thunderstorms spread east and north as the boundary moved northward.\nEvent Narrative: Wind gusts of 32 knots were measured at Shady Side Elementary School.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 24.2308 km away, between 2014-05-27 13:00:00 and 2014-05-27 17:01:00. The events included records with estimated wind gusts of 34.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A strong cold front moved through the Mid Atlantic. Southerly flow ahead of the frontal boundary led to increased instability. Showers and thunderstorms formed along a pre-frontal trough east of the Blue Ridge. Some storms were capable of damaging winds and large hail. A strong cold front moved through the Mid Atlantic. Southerly flow ahead of the frontal boundary led to increased instability. Showers and thunderstorms formed along a pre-frontal trough east of the Blue Ridge. Some storms were capable of damaging winds and large hail. A strong cold front moved through the Mid Atlantic. Southerly flow ahead of the frontal boundary led to increased instability. Showers and thunderstorms formed along a pre-frontal trough east of the Blue Ridge. Some storms were capable of damaging winds and large hail.\nEvent Narrative: Wind gusts of 31 knots were measured at North Bay. Wind gusts of 32 knots were measured at Baltimore Key Bridge. Wind gusts of 31 knots were measured at Baltimore.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 36.1695 km away, between 2014-06-03 22:30:00 and 2014-06-03 22:54:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A upper level disturbance moved across the Mid Atlantic and showers and thunderstorms produced gusty winds across the waters. A upper level disturbance moved across the Mid Atlantic and showers and thunderstorms produced gusty winds across the waters.\nEvent Narrative: Wind gusts of 31 knots were measured at Gunpowder. Wind gusts of 36 knots were measured at Tolchester Beach.", "The following events were reported: Flash Flood. These occurred near station USW00093721, approximately 27.657 km away, between 2014-06-12 18:00:00 and 2014-06-12 20:00:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Warm and moist conditions led to showers and thunderstorms to develop as a upper level trough passed the region. Some thunderstorms led to large hail, damaging winds and heavy rain. Warm and moist conditions led to showers and thunderstorms to develop as a upper level trough passed the region. Some thunderstorms led to large hail, damaging winds and heavy rain.\nEvent Narrative: Defense highway was closed near Windermere Court due to flooding. Route 214 was closed between Beards Point Road and Riva Road due to flooding.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 22.9681 km away, between 2014-06-13 13:12:00 and 2014-06-13 13:18:00. The events included records with estimated wind gusts of 52.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 0.0 and crop damage of 1000.0. \n\nEpisode Narrative: A upper level trough was across the Mid Atlantic and humid conditions existed ahead of a approaching cold front. Surface heating led to thunderstorms to form in Northeast MD and produce gusty winds. A upper level trough was across the Mid Atlantic and humid conditions existed ahead of a approaching cold front. Surface heating led to thunderstorms to form in Northeast MD and produce gusty winds. A upper level trough was across the Mid Atlantic and humid conditions existed ahead of a approaching cold front. Surface heating led to thunderstorms to form in Northeast MD and produce gusty winds. A upper level trough was across the Mid Atlantic and humid conditions existed ahead of a approaching cold front. Surface heating led to thunderstorms to form in Northeast MD and produce gusty winds.\nEvent Narrative: There was a tree down blocking Cove Road near the beltway. There was a large tree uprooted at Coxs Point. There was a tree down blocking the road at Sandlewood and Thomas Blvd. There was a tree down blocking the road at Diamond Point and Oriole Avenue.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 34.2694 km away, between 2014-06-13 14:12:00 and 2014-06-13 15:00:00. The events included records with measured wind gusts of 41.2 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A upper level trough was across the Mid Atlantic and humid conditions existed ahead of a approaching cold front. Surface heating led to thunderstorms to form in Northeast MD and produce gusty winds. A upper level trough was across the Mid Atlantic and humid conditions existed ahead of a approaching cold front. Surface heating led to thunderstorms to form in Northeast MD and produce gusty winds. A upper level trough was across the Mid Atlantic and humid conditions existed ahead of a approaching cold front. Surface heating led to thunderstorms to form in Northeast MD and produce gusty winds. A upper level trough was across the Mid Atlantic and humid conditions existed ahead of a approaching cold front. Surface heating led to thunderstorms to form in Northeast MD and produce gusty winds. A upper level trough was across the Mid Atlantic and humid conditions existed ahead of a approaching cold front. Surface heating led to thunderstorms to form in Northeast MD and produce gusty winds.\nEvent Narrative: Wind gusts of 41-43 knots were measured at Annapolis Buoy. Wind gusts of 36 knots were measured at Tolly Point. Wind gusts of 35-42 knots were measured at Kent Island. Wind gusts of 39 knots were measured at Thomas Point. Wind gusts of 34-46 knots were measured at Greenbury Point.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 24.0009 km away, between 2014-06-18 22:00:00 and 2014-06-19 00:50:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A weak cold front moved across the Mid Atlantic region while hot and humid conditions led to a unstable environment. Showers and thunderstorms formed in vicinity of the front in the afternoon and some thunderstorms led to damaging winds. A weak cold front moved across the Mid Atlantic region while hot and humid conditions led to a unstable environment. Showers and thunderstorms formed in vicinity of the front in the afternoon and some thunderstorms led to damaging winds. A weak cold front moved across the Mid Atlantic region while hot and humid conditions led to a unstable environment. Showers and thunderstorms formed in vicinity of the front in the afternoon and some thunderstorms led to damaging winds. A weak cold front moved across the Mid Atlantic region while hot and humid conditions led to a unstable environment. Showers and thunderstorms formed in vicinity of the front in the afternoon and some thunderstorms led to damaging winds. A weak cold front moved across the Mid Atlantic region while hot and humid conditions led to a unstable environment. Showers and thunderstorms formed in vicinity of the front in the afternoon and some thunderstorms led to damaging winds. A weak cold front moved across the Mid Atlantic region while hot and humid conditions led to a unstable environment. Showers and thunderstorms formed in vicinity of the front in the afternoon and some thunderstorms led to damaging winds. A weak cold front moved across the Mid Atlantic region while hot and humid conditions led to a unstable environment. Showers and thunderstorms formed in vicinity of the front in the afternoon and some thunderstorms led to damaging winds. A weak cold front moved across the Mid Atlantic region while hot and humid conditions led to a unstable environment. Showers and thunderstorms formed in vicinity of the front in the afternoon and some thunderstorms led to damaging winds. A weak cold front moved across the Mid Atlantic region while hot and humid conditions led to a unstable environment. Showers and thunderstorms formed in vicinity of the front in the afternoon and some thunderstorms led to damaging winds.\nEvent Narrative: Wind gusts of 32-35 knots were measured at Key Bridge. Wind gusts of 40 knots were measured at Tolchester Beach. Wind gusts of 34-43 knots were measured at Oriole Park at Camden Yards. Wind gusts of 33 knots were measured at Gunpowder. Wind gusts of 31 knots were measured at Annapolis. Wind gusts of 38-41 knots were measured at Baltimore. Wind gusts of 43 knots were measured at Patapsco Buoy. Wind gusts of 49 knots were measured at Key Bridge. Wind gusts of 34-36 knots were measured at Gunpowder.", "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00093721, approximately 22.7727 km away, between 2014-06-18 23:10:00 and 2014-06-19 00:19:00. The events included records with hailstones measuring 40.583333333333336 inches.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 0.0 and crop damage of 1500.0. \n\nEpisode Narrative: A weak cold front moved across the Mid Atlantic region while hot and humid conditions led to a unstable environment. Showers and thunderstorms formed in vicinity of the front in the afternoon and some thunderstorms led to damaging winds. A weak cold front moved across the Mid Atlantic region while hot and humid conditions led to a unstable environment. Showers and thunderstorms formed in vicinity of the front in the afternoon and some thunderstorms led to damaging winds. A weak cold front moved across the Mid Atlantic region while hot and humid conditions led to a unstable environment. Showers and thunderstorms formed in vicinity of the front in the afternoon and some thunderstorms led to damaging winds. A weak cold front moved across the Mid Atlantic region while hot and humid conditions led to a unstable environment. Showers and thunderstorms formed in vicinity of the front in the afternoon and some thunderstorms led to damaging winds. A weak cold front moved across the Mid Atlantic region while hot and humid conditions led to a unstable environment. Showers and thunderstorms formed in vicinity of the front in the afternoon and some thunderstorms led to damaging winds. A weak cold front moved across the Mid Atlantic region while hot and humid conditions led to a unstable environment. Showers and thunderstorms formed in vicinity of the front in the afternoon and some thunderstorms led to damaging winds. A weak cold front moved across the Mid Atlantic region while hot and humid conditions led to a unstable environment. Showers and thunderstorms formed in vicinity of the front in the afternoon and some thunderstorms led to damaging winds. A weak cold front moved across the Mid Atlantic region while hot and humid conditions led to a unstable environment. Showers and thunderstorms formed in vicinity of the front in the afternoon and some thunderstorms led to damaging winds. A weak cold front moved across the Mid Atlantic region while hot and humid conditions led to a unstable environment. Showers and thunderstorms formed in vicinity of the front in the afternoon and some thunderstorms led to damaging winds.\nEvent Narrative: There was a 30 foot tree was uprooted and picked up. There was a tree blocking the right lane southbound US Route 29 at US 40. There was a tree down near Falls Road and Shawan Road. A tree was down blocking one lane of I-83 southbound near the Padonia Road exit. There were several three inch in diameter tree branches down. There were 3 to 4 inch in diameter tree branches down.", "The following events were reported: Flash Flood. These occurred near station USW00093721, approximately 11.3148 km away, between 2014-06-19 00:20:00 and 2014-06-19 02:27:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: An upper level disturbance moved north of the region while instability was still present overnight. A cold front approached the Mason Dixon line and showers and thunderstorms moved across northeast Maryland. Localized heavy rain led to flash flooding in Baltimore. An upper level disturbance moved north of the region while instability was still present overnight. A cold front approached the Mason Dixon line and showers and thunderstorms moved across northeast Maryland. Localized heavy rain led to flash flooding in Baltimore. An upper level disturbance moved north of the region while instability was still present overnight. A cold front approached the Mason Dixon line and showers and thunderstorms moved across northeast Maryland. Localized heavy rain led to flash flooding in Baltimore. An upper level disturbance moved north of the region while instability was still present overnight. A cold front approached the Mason Dixon line and showers and thunderstorms moved across northeast Maryland. Localized heavy rain led to flash flooding in Baltimore.\nEvent Narrative: There was flooding blocking one lane of Maryland 295 near Waterview Avenue. There were multiple water rescues near the intersection of Patapsco Avenue and Magnolia Avenue. There was flowing water up over the sidewalk in Baltimore. There was a basement and kitchen of a home flooded in Brooklyn.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 49.772 km away, between 2014-06-19 00:42:00 and 2014-06-19 00:42:00. The events included records with estimated wind gusts of 52.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A low pressure system that developed along a frontal boundary helped produce clusters of showers and some strong to locally severe thunderstorms that moved through the Eastern Shore during the early morning of the 19th.\nEvent Narrative: A severe thunderstorm knocked down trees along Maryland State Route 18 in Queenstown.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 18.9297 km away, between 2014-06-25 20:49:00 and 2014-06-25 20:49:00. The events included records with estimated wind gusts of 52.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 1000.0 and crop damage of 250.0. \n\nEpisode Narrative: A cold front moved across the region and showers and thunderstorms formed in a warm moist environment. Some thunderstorms produced damaging winds and heavy rain that led to flash flooding.\nEvent Narrative: There was a tree down on wires at the intersection of Baltimore Avenue and Contee Place.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 32.6707 km away, between 2014-06-26 21:45:00 and 2014-06-26 21:50:00. The events included records with estimated wind gusts of 34.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front moved across the waters and showers and thunderstorms led to gusty winds. A cold front moved across the waters and showers and thunderstorms led to gusty winds.\nEvent Narrative: Wind gusts of 31 knots were measured at Gunpowder. Wind gusts of 33 knots were measured at Annapolis Buoy.", "The following events were reported: Hail. These occurred near station USW00093721, approximately 48.007 km away, between 2014-07-02 16:45:00 and 2014-07-02 16:50:00. The events included records with hailstones measuring 1.0833333333333333 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Hot and humid conditions led to an unstable environment across the Mid Atlantic. Showers and Thunderstorms were capable of producing damaging winds and large hail. Hot and humid conditions led to an unstable environment across the Mid Atlantic. Showers and Thunderstorms were capable of producing damaging winds and large hail. Hot and humid conditions led to an unstable environment across the Mid Atlantic. Showers and Thunderstorms were capable of producing damaging winds and large hail.\nEvent Narrative:", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 35.4003 km away, between 2014-07-02 17:35:00 and 2014-07-02 22:39:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Hot and humid conditions led to an unstable environment across the Mid Atlantic. Showers and Thunderstorms were capable of producing damaging winds and large hail. Hot and humid conditions led to an unstable environment across the Mid Atlantic. Showers and Thunderstorms were capable of producing damaging winds and large hail. Hot and humid conditions led to an unstable environment across the Mid Atlantic. Showers and Thunderstorms were capable of producing damaging winds and large hail. Hot and humid conditions led to an unstable environment across the Mid Atlantic. Showers and Thunderstorms were capable of producing damaging winds and large hail. Hot and humid conditions led to an unstable environment across the Mid Atlantic. Showers and Thunderstorms were capable of producing damaging winds and large hail. Hot and humid conditions led to an unstable environment across the Mid Atlantic. Showers and Thunderstorms were capable of producing damaging winds and large hail.\nEvent Narrative: Wind gusts of 31-34 knots were measured at Gunpowder. Wind gusts of 31 knots were measured at Annapolis. Wind gusts of 31 knots were measured at Tolly Point. Wind gusts of 35 knots were measured at Bayside Elementary School. Wind gusts of 45 knots were measured at Thomas Point. Wind gusts of 32 knots were measured at Bay Bridge.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 47.1467 km away, between 2014-07-02 22:45:00 and 2014-07-02 22:45:00. The events included records with estimated wind gusts of 52.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A weakening approaching cold front triggered a series of strong to severe thunderstorms that affected the Eastern Shore during the evening and overnight on the 2nd. The severe thunderstorms occurred closer to Midnight EDT in the lower part of the Eastern Shore.\nEvent Narrative: A severe thunderstorm knocked down several trees and wires in Grasonville.", "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00093721, approximately 36.0826 km away, between 2014-07-03 14:42:00 and 2014-07-03 16:35:00. The events included records with hailstones measuring 26.708333333333332 inches.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 3000.0 and crop damage of 4500.0. \n\nEpisode Narrative: The Mid-Atlantic was in between a cold front approaching form the Appalachian Mountains and Hurricane Arthur off the Delaware Coast. Warm and humid conditions were across the region and showers and thunderstorms led to heavy rain. Unstable conditions led to severe thunderstorms that produced damaging winds and large hail. The Mid-Atlantic was in between a cold front approaching form the Appalachian Mountains and Hurricane Arthur off the Delaware Coast. Warm and humid conditions were across the region and showers and thunderstorms led to heavy rain. Unstable conditions led to severe thunderstorms that produced damaging winds and large hail. The Mid-Atlantic was in between a cold front approaching form the Appalachian Mountains and Hurricane Arthur off the Delaware Coast. Warm and humid conditions were across the region and showers and thunderstorms led to heavy rain. Unstable conditions led to severe thunderstorms that produced damaging winds and large hail. The Mid-Atlantic was in between a cold front approaching form the Appalachian Mountains and Hurricane Arthur off the Delaware Coast. Warm and humid conditions were across the region and showers and thunderstorms led to heavy rain. Unstable conditions led to severe thunderstorms that produced damaging winds and large hail. The Mid-Atlantic was in between a cold front approaching form the Appalachian Mountains and Hurricane Arthur off the Delaware Coast. Warm and humid conditions were across the region and showers and thunderstorms led to heavy rain. Unstable conditions led to severe thunderstorms that produced damaging winds and large hail. The Mid-Atlantic was in between a cold front approaching form the Appalachian Mountains and Hurricane Arthur off the Delaware Coast. Warm and humid conditions were across the region and showers and thunderstorms led to heavy rain. Unstable conditions led to severe thunderstorms that produced damaging winds and large hail. The Mid-Atlantic was in between a cold front approaching form the Appalachian Mountains and Hurricane Arthur off the Delaware Coast. Warm and humid conditions were across the region and showers and thunderstorms led to heavy rain. Unstable conditions led to severe thunderstorms that produced damaging winds and large hail. The Mid-Atlantic was in between a cold front approaching form the Appalachian Mountains and Hurricane Arthur off the Delaware Coast. Warm and humid conditions were across the region and showers and thunderstorms led to heavy rain. Unstable conditions led to severe thunderstorms that produced damaging winds and large hail. The Mid-Atlantic was in between a cold front approaching form the Appalachian Mountains and Hurricane Arthur off the Delaware Coast. Warm and humid conditions were across the region and showers and thunderstorms led to heavy rain. Unstable conditions led to severe thunderstorms that produced damaging winds and large hail. The Mid-Atlantic was in between a cold front approaching form the Appalachian Mountains and Hurricane Arthur off the Delaware Coast. Warm and humid conditions were across the region and showers and thunderstorms led to heavy rain. Unstable conditions led to severe thunderstorms that produced damaging winds and large hail. The Mid-Atlantic was in between a cold front approaching form the Appalachian Mountains and Hurricane Arthur off the Delaware Coast. Warm and humid conditions were across the region and showers and thunderstorms led to heavy rain. Unstable conditions led to severe thunderstorms that produced damaging winds and large hail. The Mid-Atlantic was in between a cold front approaching form the Appalachian Mountains and Hurricane Arthur off the Delaware Coast. Warm and humid conditions were across the region and showers and thunderstorms led to heavy rain. Unstable conditions led to severe thunderstorms that produced damaging winds and large hail.\nEvent Narrative: There were tree limbs reported down on Woodbine Road south of Highway 26. There were several trees uprooted and snapped in the Kendall Ridge neighborhood of Columbia. There were trees reported down in Elkridge. There were trees down blocking Route 1 Southbound. There were wires down closing Route 7. There was a tree reported down on power lines on Bloom Road at Salem Bottom Road.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 32.5707 km away, between 2014-07-03 16:40:00 and 2014-07-03 16:55:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: The Mid-Atlantic was in between a cold front approaching form the Appalachian Mountains and Hurricane Arthur off the Delaware Coast. Warm and humid conditions were across the region and showers and thunderstorms led to heavy rain. Unstable conditions led to severe thunderstorms that produced damaging winds and large hail. The Mid-Atlantic was in between a cold front approaching form the Appalachian Mountains and Hurricane Arthur off the Delaware Coast. Warm and humid conditions were across the region and showers and thunderstorms led to heavy rain. Unstable conditions led to severe thunderstorms that produced damaging winds and large hail. The Mid-Atlantic was in between a cold front approaching form the Appalachian Mountains and Hurricane Arthur off the Delaware Coast. Warm and humid conditions were across the region and showers and thunderstorms led to heavy rain. Unstable conditions led to severe thunderstorms that produced damaging winds and large hail.\nEvent Narrative: Wind gusts of 35-53 knots were measured at Gunpowder. Wind gusts of 31 knots were measured at Patapsco Buoy. Wind gusts of 31 knots were measured at Tolchester.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 22.6463 km away, between 2014-07-08 18:05:00 and 2014-07-08 18:30:00.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 0.0 and crop damage of 1250.0. \n\nEpisode Narrative: A cold front moved through the Mid-Atlantic from west to east. Hot and humid conditions were ahead of the frontal boundary and led to an unstable environment. Severe thunderstorms were capable of damaging winds. A cold front moved through the Mid-Atlantic from west to east. Hot and humid conditions were ahead of the frontal boundary and led to an unstable environment. Severe thunderstorms were capable of damaging winds. A cold front moved through the Mid-Atlantic from west to east. Hot and humid conditions were ahead of the frontal boundary and led to an unstable environment. Severe thunderstorms were capable of damaging winds.\nEvent Narrative: There were large tree limbs down. There were five trees down and one of them were large.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 29.6673 km away, between 2014-07-08 18:20:00 and 2014-07-08 20:40:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front moved through the Mid-Atlantic from west to east. Hot and humid conditions were ahead of the frontal boundary and led to an unstable environment. Severe thunderstorms were capable of damaging winds. A cold front moved through the Mid-Atlantic from west to east. Hot and humid conditions were ahead of the frontal boundary and led to an unstable environment. Severe thunderstorms were capable of damaging winds. A cold front moved through the Mid-Atlantic from west to east. Hot and humid conditions were ahead of the frontal boundary and led to an unstable environment. Severe thunderstorms were capable of damaging winds. A cold front moved through the Mid-Atlantic from west to east. Hot and humid conditions were ahead of the frontal boundary and led to an unstable environment. Severe thunderstorms were capable of damaging winds. A cold front moved through the Mid-Atlantic from west to east. Hot and humid conditions were ahead of the frontal boundary and led to an unstable environment. Severe thunderstorms were capable of damaging winds. A cold front moved through the Mid-Atlantic from west to east. Hot and humid conditions were ahead of the frontal boundary and led to an unstable environment. Severe thunderstorms were capable of damaging winds. A cold front moved through the Mid-Atlantic from west to east. Hot and humid conditions were ahead of the frontal boundary and led to an unstable environment. Severe thunderstorms were capable of damaging winds. A cold front moved through the Mid-Atlantic from west to east. Hot and humid conditions were ahead of the frontal boundary and led to an unstable environment. Severe thunderstorms were capable of damaging winds. A cold front moved through the Mid-Atlantic from west to east. Hot and humid conditions were ahead of the frontal boundary and led to an unstable environment. Severe thunderstorms were capable of damaging winds. A cold front moved through the Mid-Atlantic from west to east. Hot and humid conditions were ahead of the frontal boundary and led to an unstable environment. Severe thunderstorms were capable of damaging winds. A cold front moved through the Mid-Atlantic from west to east. Hot and humid conditions were ahead of the frontal boundary and led to an unstable environment. Severe thunderstorms were capable of damaging winds. A cold front moved through the Mid-Atlantic from west to east. Hot and humid conditions were ahead of the frontal boundary and led to an unstable environment. Severe thunderstorms were capable of damaging winds. A cold front moved through the Mid-Atlantic from west to east. Hot and humid conditions were ahead of the frontal boundary and led to an unstable environment. Severe thunderstorms were capable of damaging winds. A cold front moved through the Mid-Atlantic from west to east. Hot and humid conditions were ahead of the frontal boundary and led to an unstable environment. Severe thunderstorms were capable of damaging winds.\nEvent Narrative: Wind gusts of 35-38 knots were measured at Tolly Point. Wind gusts of 31-39 knots were measured at Annapolis. Wind gusts of 41 knots were measured at Bay Bridge. Wind gusts of 42-43 knots were measured at Orioles Park. Wind gusts of 31 knots were measured at Baltimore. Wind gusts of 43 knots were measured at Key Bridge in Baltimore. Wind gusts of 37 knots were measured at Gunpowder. Wind gusts of 37 knots were measured at Patapsco Buoy. Wind gusts of 31-42 knots were measured at Greenbury Point. Wind gusts of 32-41 knots were measured at Tolchester. Wind gusts of 31 knots were measured at Sandy Point. Wind gusts of 32 knots were measured at Bayside Elementary School. Wind gusts of 39-42 knots were measured at Thomas Point. Wind gusts of 39-42 knots were measured at Thomas Point.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 39.788 km away, between 2014-07-09 14:40:00 and 2014-07-09 15:34:00. The events included records with estimated wind gusts of 52.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 0.0 and crop damage of 3250.0. \n\nEpisode Narrative: A cold front approached the Mid Atlantic while a surface trough was located across the Potomac Highlands. Southerly flow ahead of both features led to humid and warm conditions across the region. Showers and thunderstorms formed in vicinity of the surface trough and moved eastward. Some storms became severe producing damaging winds and large hail. A cold front approached the Mid Atlantic while a surface trough was located across the Potomac Highlands. Southerly flow ahead of both features led to humid and warm conditions across the region. Showers and thunderstorms formed in vicinity of the surface trough and moved eastward. Some storms became severe producing damaging winds and large hail. A cold front approached the Mid Atlantic while a surface trough was located across the Potomac Highlands. Southerly flow ahead of both features led to humid and warm conditions across the region. Showers and thunderstorms formed in vicinity of the surface trough and moved eastward. Some storms became severe producing damaging winds and large hail. A cold front approached the Mid Atlantic while a surface trough was located across the Potomac Highlands. Southerly flow ahead of both features led to humid and warm conditions across the region. Showers and thunderstorms formed in vicinity of the surface trough and moved eastward. Some storms became severe producing damaging winds and large hail. A cold front approached the Mid Atlantic while a surface trough was located across the Potomac Highlands. Southerly flow ahead of both features led to humid and warm conditions across the region. Showers and thunderstorms formed in vicinity of the surface trough and moved eastward. Some storms became severe producing damaging winds and large hail. A cold front approached the Mid Atlantic while a surface trough was located across the Potomac Highlands. Southerly flow ahead of both features led to humid and warm conditions across the region. Showers and thunderstorms formed in vicinity of the surface trough and moved eastward. Some storms became severe producing damaging winds and large hail. A cold front approached the Mid Atlantic while a surface trough was located across the Potomac Highlands. Southerly flow ahead of both features led to humid and warm conditions across the region. Showers and thunderstorms formed in vicinity of the surface trough and moved eastward. Some storms became severe producing damaging winds and large hail. A cold front approached the Mid Atlantic while a surface trough was located across the Potomac Highlands. Southerly flow ahead of both features led to humid and warm conditions across the region. Showers and thunderstorms formed in vicinity of the surface trough and moved eastward. Some storms became severe producing damaging winds and large hail. A cold front approached the Mid Atlantic while a surface trough was located across the Potomac Highlands. Southerly flow ahead of both features led to humid and warm conditions across the region. Showers and thunderstorms formed in vicinity of the surface trough and moved eastward. Some storms became severe producing damaging winds and large hail.\nEvent Narrative: There were trees down at Sandymount Elementary School. There were four large trees 3-4 feet in diameter uprooted and topped on Falls Road. There was a tree reported down on Interstate 83 Southbound near Shawan Road. There were large tree branches down. There were several large limbs down. There was a tree reported down near Finksburg. There was a tree reported down in a parking lot in Hunt Valley. There was a tree reported down blocking Jarrettsville Pike near Paper Mill Road. There was a 12 inch in diameter tree snapped near Phoenix.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 34.233 km away, between 2014-07-09 16:35:00 and 2014-07-09 16:35:00. The events included records with measured wind gusts of 36.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front approached the Mid Atlantic while a surface trough was located across the Potomac Highlands. Southerly flow ahead of both features led to humid and warm conditions across the region. Showers and thunderstorms formed in vicinity of the surface trough and moved eastward. Some storms became severe producing damaging winds and large hail.\nEvent Narrative: Wind gusts of 36 knots were measured at Gunpowder.", "The following events were reported: Hail. These occurred near station USW00093721, approximately 26.4713 km away, between 2014-07-10 13:28:00 and 2014-07-10 13:28:00. The events included records with hailstones measuring 1.0 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A upper level disturbance moved across the region while a surface trough was across the Mid-Atlantic. Warm and humid conditions led to a unstable atmosphere and showers and thunderstorms formed across the Potomac Highlands.\nEvent Narrative:", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 23.0518 km away, between 2014-07-13 20:30:00 and 2014-07-13 21:08:00. The events included records with estimated wind gusts of 52.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 4000.0 and crop damage of 1500.0. \n\nEpisode Narrative: High pressure across the western Atlantic led to southerly flow across the region. This led to hot and humid conditions ahead of an advancing cold front. Showers and thunderstorms moved across the region and some thunderstorms produced damaging winds. High pressure across the western Atlantic led to southerly flow across the region. This led to hot and humid conditions ahead of an advancing cold front. Showers and thunderstorms moved across the region and some thunderstorms produced damaging winds. High pressure across the western Atlantic led to southerly flow across the region. This led to hot and humid conditions ahead of an advancing cold front. Showers and thunderstorms moved across the region and some thunderstorms produced damaging winds. High pressure across the western Atlantic led to southerly flow across the region. This led to hot and humid conditions ahead of an advancing cold front. Showers and thunderstorms moved across the region and some thunderstorms produced damaging winds. High pressure across the western Atlantic led to southerly flow across the region. This led to hot and humid conditions ahead of an advancing cold front. Showers and thunderstorms moved across the region and some thunderstorms produced damaging winds.\nEvent Narrative: There was a tree down on wires at 4029 St Johns Lane. There was a tree limb down on wires at 4029 St Johns Lane. There were three large trees and several smaller trees down in Hawthorne in Middle River. There was a tree down blocking Old Annapolis Road at Columbia Pike. There was a tree down on Green Glade Road.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 18.9007 km away, between 2014-07-13 20:45:00 and 2014-07-13 21:05:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: High pressure across the western Atlantic led to southerly flow across the region. This led to hot and humid conditions ahead of an advancing cold front. Showers and thunderstorms moved across the region and some thunderstorms produced damaging winds. High pressure across the western Atlantic led to southerly flow across the region. This led to hot and humid conditions ahead of an advancing cold front. Showers and thunderstorms moved across the region and some thunderstorms produced damaging winds. High pressure across the western Atlantic led to southerly flow across the region. This led to hot and humid conditions ahead of an advancing cold front. Showers and thunderstorms moved across the region and some thunderstorms produced damaging winds. High pressure across the western Atlantic led to southerly flow across the region. This led to hot and humid conditions ahead of an advancing cold front. Showers and thunderstorms moved across the region and some thunderstorms produced damaging winds.\nEvent Narrative: Wind gusts of 45 knots were measured at Orioles Park. Wind gusts of 43 knots were measured at Maryland Science Center. Wind gusts of 31-39 knots were measured at Key Bridge. Wind gusts of 32 knots were measured at Gunpowder.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 36.0303 km away, between 2014-07-14 16:26:00 and 2014-07-14 17:22:00.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 4000.0 and crop damage of 1500.0. \n\nEpisode Narrative: High pressure was over the western Atlantic Ocean and southerly flow brought hot and humid conditions into the Mid-Atlantic leading to a unstable atmosphere. Showers and thunderstorms moved across the region in the afternoon and evening and some thunderstorms were capable of damaging wind gusts. High pressure was over the western Atlantic Ocean and southerly flow brought hot and humid conditions into the Mid-Atlantic leading to a unstable atmosphere. Showers and thunderstorms moved across the region in the afternoon and evening and some thunderstorms were capable of damaging wind gusts. High pressure was over the western Atlantic Ocean and southerly flow brought hot and humid conditions into the Mid-Atlantic leading to a unstable atmosphere. Showers and thunderstorms moved across the region in the afternoon and evening and some thunderstorms were capable of damaging wind gusts. High pressure was over the western Atlantic Ocean and southerly flow brought hot and humid conditions into the Mid-Atlantic leading to a unstable atmosphere. Showers and thunderstorms moved across the region in the afternoon and evening and some thunderstorms were capable of damaging wind gusts. High pressure was over the western Atlantic Ocean and southerly flow brought hot and humid conditions into the Mid-Atlantic leading to a unstable atmosphere. Showers and thunderstorms moved across the region in the afternoon and evening and some thunderstorms were capable of damaging wind gusts.\nEvent Narrative: There were multiple tree limbs down on Jerusalem Road near the Baltimore County Line. There were wires down on the roadway at the intersection of Route 152 and Harford Road. There were 5 inch in diameter cherry tree branches down. There were trees and power lines down on Wheel Road.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 33.1322 km away, between 2014-07-14 16:55:00 and 2014-07-14 18:00:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: High pressure was over the western Atlantic Ocean and southerly flow brought hot and humid conditions into the Mid-Atlantic leading to a unstable atmosphere. Showers and thunderstorms moved across the region in the afternoon and evening and some thunderstorms were capable of damaging wind gusts. High pressure was over the western Atlantic Ocean and southerly flow brought hot and humid conditions into the Mid-Atlantic leading to a unstable atmosphere. Showers and thunderstorms moved across the region in the afternoon and evening and some thunderstorms were capable of damaging wind gusts. High pressure was over the western Atlantic Ocean and southerly flow brought hot and humid conditions into the Mid-Atlantic leading to a unstable atmosphere. Showers and thunderstorms moved across the region in the afternoon and evening and some thunderstorms were capable of damaging wind gusts. High pressure was over the western Atlantic Ocean and southerly flow brought hot and humid conditions into the Mid-Atlantic leading to a unstable atmosphere. Showers and thunderstorms moved across the region in the afternoon and evening and some thunderstorms were capable of damaging wind gusts. High pressure was over the western Atlantic Ocean and southerly flow brought hot and humid conditions into the Mid-Atlantic leading to a unstable atmosphere. Showers and thunderstorms moved across the region in the afternoon and evening and some thunderstorms were capable of damaging wind gusts. High pressure was over the western Atlantic Ocean and southerly flow brought hot and humid conditions into the Mid-Atlantic leading to a unstable atmosphere. Showers and thunderstorms moved across the region in the afternoon and evening and some thunderstorms were capable of damaging wind gusts.\nEvent Narrative: Wind gusts of 33 knots were measured at Patapsco Buoy. Wind gusts of 33 knots were measured at Sandy Point. Wind gusts of 33-39 knots were measured at Tolchester. Wind gusts of 46-48 knots were measured at Thomas Point. Wind gusts of 34 knots were measured at Annapolis. Wind gusts of 40 knots were measured at Shady Side Elementary School.", "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00093721, approximately 14.7772 km away, between 2014-07-15 14:01:00 and 2014-07-15 14:20:00. The events included records with hailstones measuring 40.666666666666664 inches.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 5000.0 and crop damage of 2000.0. \n\nEpisode Narrative: High pressure was over the western Atlantic Ocean and southerly flow brought hot and humid conditions into the Mid-Atlantic leading to a unstable atmosphere. A cold front approached the region and showers and thunderstorms occurred in Maryland and were capable of damaging wind gusts. High pressure was over the western Atlantic Ocean and southerly flow brought hot and humid conditions into the Mid-Atlantic leading to a unstable atmosphere. A cold front approached the region and showers and thunderstorms occurred in Maryland and were capable of damaging wind gusts. High pressure was over the western Atlantic Ocean and southerly flow brought hot and humid conditions into the Mid-Atlantic leading to a unstable atmosphere. A cold front approached the region and showers and thunderstorms occurred in Maryland and were capable of damaging wind gusts. High pressure was over the western Atlantic Ocean and southerly flow brought hot and humid conditions into the Mid-Atlantic leading to a unstable atmosphere. A cold front approached the region and showers and thunderstorms occurred in Maryland and were capable of damaging wind gusts. High pressure was over the western Atlantic Ocean and southerly flow brought hot and humid conditions into the Mid-Atlantic leading to a unstable atmosphere. A cold front approached the region and showers and thunderstorms occurred in Maryland and were capable of damaging wind gusts. High pressure was over the western Atlantic Ocean and southerly flow brought hot and humid conditions into the Mid-Atlantic leading to a unstable atmosphere. A cold front approached the region and showers and thunderstorms occurred in Maryland and were capable of damaging wind gusts. High pressure was over the western Atlantic Ocean and southerly flow brought hot and humid conditions into the Mid-Atlantic leading to a unstable atmosphere. A cold front approached the region and showers and thunderstorms occurred in Maryland and were capable of damaging wind gusts. High pressure was over the western Atlantic Ocean and southerly flow brought hot and humid conditions into the Mid-Atlantic leading to a unstable atmosphere. A cold front approached the region and showers and thunderstorms occurred in Maryland and were capable of damaging wind gusts. High pressure was over the western Atlantic Ocean and southerly flow brought hot and humid conditions into the Mid-Atlantic leading to a unstable atmosphere. A cold front approached the region and showers and thunderstorms occurred in Maryland and were capable of damaging wind gusts.\nEvent Narrative: There was a tree down blocking the roadway on Benfield Road near Lynwood Drive. There was a power pole and wires down on the 700 Block of Old Herald Harbor Road. There was a tree down on Benfield Road. There was a large tree down on the property on the 1100 Block of Summit Drive. There were numerous large trees and power lines down near the intersection of Generals Highway and Waterbury Road. There were trees and a power line down at the residence on the 300 block of Beech Trail Drive. There was a tree down on a vehicle on the 300 Block of South Riverside Drive and Hazel Trail.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 37.5488 km away, between 2014-07-15 14:40:00 and 2014-07-15 14:42:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: High pressure was over the western Atlantic Ocean and southerly flow brought hot and humid conditions into the Mid-Atlantic leading to a unstable atmosphere. A cold front approached the region and showers and thunderstorms occurred in Maryland and were capable of damaging wind gusts. High pressure was over the western Atlantic Ocean and southerly flow brought hot and humid conditions into the Mid-Atlantic leading to a unstable atmosphere. A cold front approached the region and showers and thunderstorms occurred in Maryland and were capable of damaging wind gusts.\nEvent Narrative: Wind gusts of 34 knots were measured at Thomas Point. Wind gusts of 31 knots were measured at Tolchester.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 45.55 km away, between 2014-07-23 17:49:00 and 2014-07-23 17:49:00. The events included records with estimated wind gusts of 52.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 2000.0 and crop damage of 250.0. \n\nEpisode Narrative: A Bermuda high was to the east and southerly flow across the Mid-Atlantic led to warm and humid conditions. A cold front approached from the Great Lakes and showers and thunderstorms moved across the region leading to large hail and damaging wind gusts.\nEvent Narrative: There was a tree down on wires on Carrollton Road between Wesley Road and Lees Mill Road.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 21.0819 km away, between 2014-07-23 18:49:00 and 2014-07-23 19:02:00. The events included records with estimated wind gusts of 34.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A Bermuda high was to the east and southerly flow across the Mid-Atlantic led to warm and humid conditions. A cold front approached from the Great Lakes and showers and thunderstorms moved across the region leading to large hail and damaging wind gusts. A Bermuda high was to the east and southerly flow across the Mid-Atlantic led to warm and humid conditions. A cold front approached from the Great Lakes and showers and thunderstorms moved across the region leading to large hail and damaging wind gusts.\nEvent Narrative: Wind gusts of 31 knots were measured at Orioles Park. Wind gusts of 34 knots were measured at Martins State Airport.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 44.4652 km away, between 2014-07-27 22:35:00 and 2014-07-27 23:29:00. The events included records with estimated wind gusts of 52.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 0.0 and crop damage of 1000.0. \n\nEpisode Narrative: An upper level disturbance approached the Mid Atlantic while warm and humid surface conditions led to an unstable atmosphere. Strong winds aloft led to strong thunderstorms that produced large hail and damaging winds. An upper level disturbance approached the Mid Atlantic while warm and humid surface conditions led to an unstable atmosphere. Strong winds aloft led to strong thunderstorms that produced large hail and damaging winds. An upper level disturbance approached the Mid Atlantic while warm and humid surface conditions led to an unstable atmosphere. Strong winds aloft led to strong thunderstorms that produced large hail and damaging winds.\nEvent Narrative: There was a tree down on Falls Road near the intersection of Mt Carmel Road. There were several large tree branches down on the property. There was a large tree onto a house in the 1600 Block of Clayton Road. Several other large trees were down along Clayton Road.", "The following events were reported: Hail. These occurred near station USW00093721, approximately 25.5317 km away, between 2014-08-03 20:27:00 and 2014-08-03 20:27:00. The events included records with hailstones measuring 1.0 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A surface trough was across the Mid-Atlantic and warm and humid conditions led to a unstable environment. Showers and thunderstorms formed near the surface trough. Damaging winds and large hail were reported in some thunderstorms.\nEvent Narrative:", "The following events were reported: Flash Flood, Flood. These occurred near station USW00093721, approximately 8.6999 km away, between 2014-08-12 11:45:00 and 2014-08-12 19:15:00. The flood was caused by Heavy Rain. Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 3450000.0 and crop damage of 0.0. \n\nEpisode Narrative: High pressure resided across the east coast while a warm front was located across the Carolinas. Moist air continued to move into the Mid Atlantic as showers intensified ahead of the warm front. Heavy rain produced flooding in parts of the Washington DC and Baltimore Metro Areas. High pressure resided across the east coast while a warm front was located across the Carolinas. Moist air continued to move into the Mid Atlantic as showers intensified ahead of the warm front. Heavy rain produced flooding in parts of the Washington DC and Baltimore Metro Areas. High pressure resided across the east coast while a warm front was located across the Carolinas. Moist air continued to move into the Mid Atlantic as showers intensified ahead of the warm front. Heavy rain produced flooding in parts of the Washington DC and Baltimore Metro Areas. High pressure resided across the east coast while a warm front was located across the Carolinas. Moist air continued to move into the Mid Atlantic as showers intensified ahead of the warm front. Heavy rain produced flooding in parts of the Washington DC and Baltimore Metro Areas. High pressure resided across the east coast while a warm front was located across the Carolinas. Moist air continued to move into the Mid Atlantic as showers intensified ahead of the warm front. Heavy rain produced flooding in parts of the Washington DC and Baltimore Metro Areas. High pressure resided across the east coast while a warm front was located across the Carolinas. Moist air continued to move into the Mid Atlantic as showers intensified ahead of the warm front. Heavy rain produced flooding in parts of the Washington DC and Baltimore Metro Areas. High pressure resided across the east coast while a warm front was located across the Carolinas. Moist air continued to move into the Mid Atlantic as showers intensified ahead of the warm front. Heavy rain produced flooding in parts of the Washington DC and Baltimore Metro Areas. High pressure resided across the east coast while a warm front was located across the Carolinas. Moist air continued to move into the Mid Atlantic as showers intensified ahead of the warm front. Heavy rain produced flooding in parts of the Washington DC and Baltimore Metro Areas. High pressure resided across the east coast while a warm front was located across the Carolinas. Moist air continued to move into the Mid Atlantic as showers intensified ahead of the warm front. Heavy rain produced flooding in parts of the Washington DC and Baltimore Metro Areas. High pressure resided across the east coast while a warm front was located across the Carolinas. Moist air continued to move into the Mid Atlantic as showers intensified ahead of the warm front. Heavy rain produced flooding in parts of the Washington DC and Baltimore Metro Areas. High pressure resided across the east coast while a warm front was located across the Carolinas. Moist air continued to move into the Mid Atlantic as showers intensified ahead of the warm front. Heavy rain produced flooding in parts of the Washington DC and Baltimore Metro Areas. High pressure resided across the east coast while a warm front was located across the Carolinas. Moist air continued to move into the Mid Atlantic as showers intensified ahead of the warm front. Heavy rain produced flooding in parts of the Washington DC and Baltimore Metro Areas. High pressure resided across the east coast while a warm front was located across the Carolinas. Moist air continued to move into the Mid Atlantic as showers intensified ahead of the warm front. Heavy rain produced flooding in parts of the Washington DC and Baltimore Metro Areas. High pressure resided across the east coast while a warm front was located across the Carolinas. Moist air continued to move into the Mid Atlantic as showers intensified ahead of the warm front. Heavy rain produced flooding in parts of the Washington DC and Baltimore Metro Areas. High pressure resided across the east coast while a warm front was located across the Carolinas. Moist air continued to move into the Mid Atlantic as showers intensified ahead of the warm front. Heavy rain produced flooding in parts of the Washington DC and Baltimore Metro Areas. High pressure resided across the east coast while a warm front was located across the Carolinas. Moist air continued to move into the Mid Atlantic as showers intensified ahead of the warm front. Heavy rain produced flooding in parts of the Washington DC and Baltimore Metro Areas. High pressure resided across the east coast while a warm front was located across the Carolinas. Moist air continued to move into the Mid Atlantic as showers intensified ahead of the warm front. Heavy rain produced flooding in parts of the Washington DC and Baltimore Metro Areas. High pressure resided across the east coast while a warm front was located across the Carolinas. Moist air continued to move into the Mid Atlantic as showers intensified ahead of the warm front. Heavy rain produced flooding in parts of the Washington DC and Baltimore Metro Areas.\nEvent Narrative: There was water more than halfway up the wheels of cars in the parking lots near Linthicum Heights. Flooding was reported at the maintenance shop at BWI. There was water flowing over roadways and there was damage to up to 100 vehicles in Long Term Parking Lots A and B at BWI Airport. The stream gauge on Sawmill Creek exceeded its flood stage of 5 feet. Numerous roads were closed and flooding was reported in two businesses. This is the highest creek level ever recorded at this location and records date back to 1983. The record crest of 7.61 feet at 4:30 PM EDT. Maryland Emergency Management Agency and FEMA estimated that many roads, bridges, buildings, and equipment were damaged or destroyed in Anne Arundel County during this flash flood event. There was water up to the headlights of cars off Bowie Road east of Route 1. The road was closed. The east branch Herbert Run exceeded its flood stage of 7 feet. The stream was out of its banks and covering yards near the stream. It went above flood stage at 1:10 PM EDT and peaked at 9.08 feet at 1:45 PM EDT. Dorsey Road was flooded and closed at Sawmill Creek between Central Avenue and Route 648. Aviation Boulevard was reported to be flooded and completely closed at the road leading to the MARC and Amtrack Station. All lanes on route 3 were flooded by Sawmill Creek and closed near Furnace Branch Road. Gwynns Falls exceeded its flood stage of 13 feet with minor overbank flooding occurring for about an hour near the Gwynns Falls Trail. It went above flood stage at 2:03 PM EDT and peaked at 13.78 feet at 2:20 PM EDT. It went below flood stage at 3:02 PM EDT. The outer loop of the Baltimore Beltway was flooded and completely closed at Quarantine Road. All traffic was diverted. Maryland 295 was flooded and closed between the Baltimore Beltway and Westport. The Baltimore Harbor Tunnel was closed due to flooding. There was at least six inches of water flowing across Benson Avenue in Arbutus. The Baltimore Annapolis Boulevard was flooded and closed at Magothy River crossing near Pasadena. There was a water rescue on West Street at Hudson Street. The car was stranded in three feet of water. There were fields and trails flooded near the Little Patuxent River. It went above flood stage at 1740 UTC and peaked at 10.88 feet at 2045 UTC. It went below flood stage at 0006 UTC.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 35.4925 km away, between 2014-08-12 16:20:00 and 2014-08-12 17:29:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: High pressure resided across the east coast while a warm front was located across the Carolinas. Moist air continued to move into the Mid Atlantic as showers intensified ahead of the warm front. Heavy rain produced gusty winds and flooding in parts of the Washington DC and Baltimore Metro Areas. Thunderstorms produced damaging winds west of the Blue Ridge. High pressure resided across the east coast while a warm front was located across the Carolinas. Moist air continued to move into the Mid Atlantic as showers intensified ahead of the warm front. Heavy rain produced gusty winds and flooding in parts of the Washington DC and Baltimore Metro Areas. Thunderstorms produced damaging winds west of the Blue Ridge.\nEvent Narrative: Wind gusts of 33 knots were measured at Thomas Point. Wind gusts of 34 knots were measured at Tolly Point.", "The following events were reported: Flash Flood. These occurred near station USW00093721, approximately 41.3539 km away, between 2014-08-12 17:20:00 and 2014-08-13 00:00:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A slow moving warm front and a low pressure system that formed along it that enhanced the convergence brought flash flooding rains to the Eastern Shore on the 12th. Rainfall amounts reached as high as ten inches. A series of thunderstorms with very heavy rain formed and moved along a very slowly northward moving warm frontal boundary. The rain did not end until an occluded front neared the Eastern Shore overnight on the 12th. Numerous showers and thunderstorms started during the morning of the 12th and the heaviest rain fell during the late afternoon and early evening. The rain ended late that evening on the 12th. Event precipitation totals averaged 3 to 10 inches with the highest amounts in Queen Anne's County. A slow moving warm front and a low pressure system that formed along it that enhanced the convergence brought flash flooding rains to the Eastern Shore on the 12th. Rainfall amounts reached as high as ten inches. A series of thunderstorms with very heavy rain formed and moved along a very slowly northward moving warm frontal boundary. The rain did not end until an occluded front neared the Eastern Shore overnight on the 12th. Numerous showers and thunderstorms started during the morning of the 12th and the heaviest rain fell during the late afternoon and early evening. The rain ended late that evening on the 12th. Event precipitation totals averaged 3 to 10 inches with the highest amounts in Queen Anne's County.\nEvent Narrative: Thunderstorms with very heavy rain caused flash flooding in and around Rock Hall. Many roadways were flooded and closed and included Chesapeake Avenue, Walnut Street, Crosby Road and Eastern Neck Island Road. Event precipitation totals included 5.75 inches in Kennedyville, 4.60 inches in Rock Hall and 3.64 inches in Galena. Thunderstorms with very heavy rain caused flash flooding at the southern end of Kent Island. Kent Point Road was closed due to flash flooding. Doppler Radar storm total estimates reached 4 inches on Kent Island.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 41.3421 km away, between 2014-08-21 19:45:00 and 2014-08-21 19:45:00. The events included records with estimated wind gusts of 52.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A shortwave trough approached the Mid-Atlantic while a stationary boundary was across the region. Warm and moist conditions led to a unstable environment and showers and thunderstorms moved across the region. Some storms led to damaging winds.\nEvent Narrative: There was a tree down near the intersection of Carroll Road and Sparks Road.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 18.6886 km away, between 2014-09-02 18:37:00 and 2014-09-02 19:22:00. The events included records with estimated wind gusts of 52.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 10000.0 and crop damage of 1750.0. \n\nEpisode Narrative: Hot and humid conditions persisted across the Mid Atlantic ahead of a advancing cold front. Showers and thunderstorms formed in the vicinity of a surface trough. Some thunderstorms became severe leading to damaging winds. Hot and humid conditions persisted across the Mid Atlantic ahead of a advancing cold front. Showers and thunderstorms formed in the vicinity of a surface trough. Some thunderstorms became severe leading to damaging winds. Hot and humid conditions persisted across the Mid Atlantic ahead of a advancing cold front. Showers and thunderstorms formed in the vicinity of a surface trough. Some thunderstorms became severe leading to damaging winds. Hot and humid conditions persisted across the Mid Atlantic ahead of a advancing cold front. Showers and thunderstorms formed in the vicinity of a surface trough. Some thunderstorms became severe leading to damaging winds. Hot and humid conditions persisted across the Mid Atlantic ahead of a advancing cold front. Showers and thunderstorms formed in the vicinity of a surface trough. Some thunderstorms became severe leading to damaging winds. Hot and humid conditions persisted across the Mid Atlantic ahead of a advancing cold front. Showers and thunderstorms formed in the vicinity of a surface trough. Some thunderstorms became severe leading to damaging winds.\nEvent Narrative: There were two trees down on houses causing significant damage near each other, one on the 1000 Block of Evergreen Ave and one on the 6400 Block of Bellview Ave. There were large tree limbs down at the intersection of Seneca and Groveleigh. There was a tree down across the road near the intersection of Abingdon Road and Route 40. There was a tree down at the intersection of Quiet Hours and Cradlerock Way. There was a tree down at the intersection of Brokenland Parkway and Cradlerock Way. There was a tree down at the intersection of Mayfield Avenue and Meadowridge Road.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 38.3107 km away, between 2014-09-02 22:30:00 and 2014-09-02 22:50:00. The events included records with estimated wind gusts of 34.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Hot and humid conditions persisted across the Mid Atlantic ahead of a advancing cold front. Showers and thunderstorms formed in the vicinity of a surface trough. Some thunderstorms became severe leading to damaging winds. Hot and humid conditions persisted across the Mid Atlantic ahead of a advancing cold front. Showers and thunderstorms formed in the vicinity of a surface trough. Some thunderstorms became severe leading to damaging winds.\nEvent Narrative: Wind gusts of 32 knots were measured at Thomas Point. Wind gusts of 31 knots were measured at Kent Island.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 1.4199 km away, between 2014-09-06 18:34:00 and 2014-09-06 18:34:00. The events included records with measured wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Hot and humid conditions were present across the Mid-Atlantic while a cold front approached from the Ohio Valley. A surface trough strengthen across the region and showers and thunderstorms formed. Some thunderstorms formed and produced damaging winds.\nEvent Narrative:", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 32.9273 km away, between 2014-09-06 19:00:00 and 2014-09-06 19:29:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Hot and humid conditions were present across the Mid-Atlantic while a cold front approached from the Ohio Valley. A surface trough strengthen across the region and showers and thunderstorms formed. Some thunderstorms formed and produced damaging winds. Hot and humid conditions were present across the Mid-Atlantic while a cold front approached from the Ohio Valley. A surface trough strengthen across the region and showers and thunderstorms formed. Some thunderstorms formed and produced damaging winds. Hot and humid conditions were present across the Mid-Atlantic while a cold front approached from the Ohio Valley. A surface trough strengthen across the region and showers and thunderstorms formed. Some thunderstorms formed and produced damaging winds. Hot and humid conditions were present across the Mid-Atlantic while a cold front approached from the Ohio Valley. A surface trough strengthen across the region and showers and thunderstorms formed. Some thunderstorms formed and produced damaging winds. Hot and humid conditions were present across the Mid-Atlantic while a cold front approached from the Ohio Valley. A surface trough strengthen across the region and showers and thunderstorms formed. Some thunderstorms formed and produced damaging winds. Hot and humid conditions were present across the Mid-Atlantic while a cold front approached from the Ohio Valley. A surface trough strengthen across the region and showers and thunderstorms formed. Some thunderstorms formed and produced damaging winds.\nEvent Narrative: Wind gusts of 33 knots were measured at Annapolis. Wind gusts of 38 knots were measured at Annapolis. Wind gusts of 38 knots were measured at Thomas Point. Wind gusts of 33 knots were measured at Bay Bridge. Wind gusts of 33-43 knots were measured at Greenbury Point. Wind gusts of 36 knots were measured at Tolly Point.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 34.4589 km away, between 2014-10-07 20:50:00 and 2014-10-07 23:46:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Upper level trough swinging through the region ahead of an approaching combining with increasing shear led to the development of scattered thunderstorms with strong winds across the waters. Upper level trough swinging through the region ahead of an approaching combining with increasing shear led to the development of scattered thunderstorms with strong winds across the waters. Upper level trough swinging through the region ahead of an approaching combining with increasing shear led to the development of scattered thunderstorms with strong winds across the waters. Upper level trough swinging through the region ahead of an approaching combining with increasing shear led to the development of scattered thunderstorms with strong winds across the waters. Upper level trough swinging through the region ahead of an approaching combining with increasing shear led to the development of scattered thunderstorms with strong winds across the waters. Upper level trough swinging through the region ahead of an approaching combining with increasing shear led to the development of scattered thunderstorms with strong winds across the waters. Upper level trough swinging through the region ahead of an approaching combining with increasing shear led to the development of scattered thunderstorms with strong winds across the waters. Upper level trough swinging through the region ahead of an approaching combining with increasing shear led to the development of scattered thunderstorms with strong winds across the waters.\nEvent Narrative: Annapolis Buoy 44063 reported a gust of 37 kts. Kent Island WxFlow reported a gust of 32 kts. Sandy Point WxFlow reported a gust of 32 kts. Thomas Point C-MAN station reported a gust of 31 kts. Kent Island WxFlow reported a gust of 32 knots. Sandy Point WxFlow reported a gust of 32 knots. TPLM2 reported a gust of 31 knots. Tolly Point WxFlow reported gusts between 31-34 knots.", "The following events were reported: Tornado. These occurred near station USW00093721, approximately 13.1419 km away, between 2014-10-15 12:13:00 and 2014-10-15 12:14:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cut off low over the Midwest pushed a cold front through the Mid Atlantic during the morning hours. Scattered showers with embedded thunderstorms formed along this front in a strong directional and magnitudinal sheared environment. Diurnal heating led to minimal instability. The combination of the strong sheared environment and low CAPE resulted in a weak tornado across Howard County.\nEvent Narrative: After a review of radar observations, 911-center and broadcast|media reports relaying ground observations, and the NWS storm survey|results, the National Weather Service in Baltimore MD/Washington|DC has confirmed an EF-0 tornado touched down near Savage in|Howard County, Maryland. This review is based on corroborating |evidence between intermittent damage reports along the path and |rotational velocity couplets from the Federal Aviation Administration's|Thurgood Marshall Baltimore/Washington International Airport|Terminal Doppler Weather Radar and National Weather Service KLWX|WSR-88D radar. ||The tornado is estimated to have touched down at 1:13 pm, |approximately two hundred yards south of Knights Bridge|Road in Savage. The tornado then uprooted and downed a large tree|that fell onto the south-facing side of an apartment complex on Stebbing Way.|Other large branches were snapped off nearby trees along the hill|side south of Stebbing Way. A nearby street sign was also snapped.|The radar couplet signature weakened and dissipated after 1:14 pm|prior to reaching Gorman Road. Estimated maximum wind speeds were 55-65 mph.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 33.9935 km away, between 2014-10-15 15:19:00 and 2014-10-15 15:19:00. The events included records with estimated wind gusts of 34.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A vigorous cold front extending from low pressure over the Great Lakes swung through the Mid Atlantic during the morning and early afternoon hours. Heavy rain showers and embedded thunderstorms ahead of the approaching front mixed down strong winds aloft for gusty winds over all the waters.\nEvent Narrative: Tolly Point WxFlow reported a gust of 31 kts.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 36.9916 km away, between 2014-11-06 15:25:00 and 2014-11-06 15:25:00. The events included records with estimated wind gusts of 34.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A line of showers with embedded thunderstorms formed along a cold front as it swung through the Mid-Atlantic region. Strong winds aloft mixed down with the heavier precipitation, resulting in gusty winds.\nEvent Narrative: Measured gust of 32 kts.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 30.671 km away, between 2015-01-04 19:35:00 and 2015-01-04 20:24:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A line of convective formed along a cold front as it swung through the Mid Atlantic. Strong winds aloft, between 30 and 50 mph, were mixed to the surface with the heavier precipitation. A line of convective formed along a cold front as it swung through the Mid Atlantic. Strong winds aloft, between 30 and 50 mph, were mixed to the surface with the heavier precipitation. A line of convective formed along a cold front as it swung through the Mid Atlantic. Strong winds aloft, between 30 and 50 mph, were mixed to the surface with the heavier precipitation. A line of convective formed along a cold front as it swung through the Mid Atlantic. Strong winds aloft, between 30 and 50 mph, were mixed to the surface with the heavier precipitation. A line of convective formed along a cold front as it swung through the Mid Atlantic. Strong winds aloft, between 30 and 50 mph, were mixed to the surface with the heavier precipitation. A line of convective formed along a cold front as it swung through the Mid Atlantic. Strong winds aloft, between 30 and 50 mph, were mixed to the surface with the heavier precipitation. A line of convective formed along a cold front as it swung through the Mid Atlantic. Strong winds aloft, between 30 and 50 mph, were mixed to the surface with the heavier precipitation. A line of convective formed along a cold front as it swung through the Mid Atlantic. Strong winds aloft, between 30 and 50 mph, were mixed to the surface with the heavier precipitation. A line of convective formed along a cold front as it swung through the Mid Atlantic. Strong winds aloft, between 30 and 50 mph, were mixed to the surface with the heavier precipitation. A line of convective formed along a cold front as it swung through the Mid Atlantic. Strong winds aloft, between 30 and 50 mph, were mixed to the surface with the heavier precipitation. A line of convective formed along a cold front as it swung through the Mid Atlantic. Strong winds aloft, between 30 and 50 mph, were mixed to the surface with the heavier precipitation. A line of convective formed along a cold front as it swung through the Mid Atlantic. Strong winds aloft, between 30 and 50 mph, were mixed to the surface with the heavier precipitation. A line of convective formed along a cold front as it swung through the Mid Atlantic. Strong winds aloft, between 30 and 50 mph, were mixed to the surface with the heavier precipitation. A line of convective formed along a cold front as it swung through the Mid Atlantic. Strong winds aloft, between 30 and 50 mph, were mixed to the surface with the heavier precipitation.\nEvent Narrative: Reported at Mesonet EW0112. Reported at Gun. Gusts between 31 and 34 knots were reported. Gusts between 31 and 34 knots were reported. Gusts between 32 and 34 knots were reported. Gusts between 31 and 34 knots were reported. Gusts between 33 and 34 knots were reported. Gusts between 31 and 34 knots were reported. Gusts between 31 and 34 knots were reported. Reported at Thomas Point. Multiple gusts between 31 and 34 knots were reported between 1935 and 2000. Gusts between 31 and 34 knots were reported. Gusts between 31 and 34 knots were reported.", "The following events were reported: Flood. These occurred near station USW00093721, approximately 42.0623 km away, between 2015-03-05 06:15:00 and 2015-03-05 19:38:00. The flood was caused by Ice Jam. Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Warmer temperatures and rain led to ice-induced stream rises on many rivers across the Hydrologic Service Area.\nEvent Narrative: The Gundpowder Falls near Glencoe gauge peaked at 10.95. Flooding was reported due to a ice jam on a small portion of Gunpowder Falls. Roads were closed in the area.", "The following events were reported: Flood. These occurred near station USW00093721, approximately 42.0484 km away, between 2015-03-11 04:41:00 and 2015-03-12 03:21:00. The flood was caused by Heavy Rain / Snow Melt. Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Low pressure moved along a warm front across the Mid-Atlantic. The combination of heavy rain and snow melt led to isolated areas of flooding. Low pressure moved along a warm front across the Mid-Atlantic. The combination of heavy rain and snow melt led to isolated areas of flooding.\nEvent Narrative: Moderate rainfall and snow melt caused minor flooding along Gunpowder Falls in Glencoe community overnight. The gauge peaked at 7.69 feet at 0630 UTC. Snowmelt along with releases from an upstream dam caused minor flooding along Gunpowder Falls in the Glencoe community.", "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00093721, approximately 14.8581 km away, between 2015-04-20 19:30:00 and 2015-04-20 20:03:00. The events included records with hailstones measuring 25.5 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A warm front was draped across the Mason-Dixon Line as a cold front slowly approached from the northwest, leaving the Mid Atlantic warm sectored. Increasing instability and shear ahead of the approaching front coupled with a passing jet streak providing forcing aloft led to scattered strong to severe thunderstorms. A warm front was draped across the Mason-Dixon Line as a cold front slowly approached from the northwest, leaving the Mid Atlantic warm sectored. Increasing instability and shear ahead of the approaching front coupled with a passing jet streak providing forcing aloft led to scattered strong to severe thunderstorms.\nEvent Narrative: A tree was reported down on New Cut Rd at Old Oak Rd.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 30.9082 km away, between 2015-04-20 20:30:00 and 2015-04-20 20:53:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A warm front was draped across the Mason-Dixon Line as a cold front slowly approached from the northwest, leaving the Mid Atlantic warm sectored. Increasing instability and shear ahead of the approaching front coupled with a passing jet streak providing forcing aloft led to scattered strong to severe thunderstorms. A warm front was draped across the Mason-Dixon Line as a cold front slowly approached from the northwest, leaving the Mid Atlantic warm sectored. Increasing instability and shear ahead of the approaching front coupled with a passing jet streak providing forcing aloft led to scattered strong to severe thunderstorms.\nEvent Narrative: Between 33 and 34 knots were reported.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 34.4694 km away, between 2015-05-16 17:39:00 and 2015-05-16 17:54:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Increasing warmth and moisture as return flow on backside of high pressure sitting off the coast led to increased instability. Shear remained on the low end, but enough instability resulted in pulse showers and thunderstorms during the evening over most of the marine zones. Increasing warmth and moisture as return flow on backside of high pressure sitting off the coast led to increased instability. Shear remained on the low end, but enough instability resulted in pulse showers and thunderstorms during the evening over most of the marine zones. Increasing warmth and moisture as return flow on backside of high pressure sitting off the coast led to increased instability. Shear remained on the low end, but enough instability resulted in pulse showers and thunderstorms during the evening over most of the marine zones.\nEvent Narrative: Hart Miller Wxflow. Gunpowder Wxflow. Multiple gusts between 32 and 34 knots were reported at TCBM2.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 48.5388 km away, between 2015-05-16 18:00:00 and 2015-05-16 18:00:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A lee side trough coupled with an unseasonably warm air mass helped trigger a line of strong to locally severe thunderstorms that moved through the Eastern Shore during the early evening on the 16th.\nEvent Narrative: A severe thunderstorm knocked down large tree limbs and wires on Saint James Newtown Road in Worton.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 42.0493 km away, between 2015-05-18 18:42:00 and 2015-05-18 18:42:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A stationary boundary triggered showers and thunderstorms. The main threat was heavy rain, but there was an isolated severe thunderstorm due to the unstable atmosphere.\nEvent Narrative: A tree was snapped off at the trunk. The tree was one foot in diameter.", "The following events were reported: Flash Flood, Flood. These occurred near station USW00093721, approximately 18.0928 km away, between 2015-05-19 00:34:00 and 2015-05-19 05:30:00. The flood was caused by Heavy Rain. The events resulted in 0 injuries and 1 fatalities. The events caused property damage valued at 15000.0 and crop damage of 0.0. \n\nEpisode Narrative: A cold front was located to the north of the Mid-Atlantic and warm and humid conditions persisted through the evening hours. A bay breeze formed across North-Central Maryland and led to multiple rounds of showers and thunderstorms in this area. Heavy showers also moved into the region from West Virginia and led to heavy rain across north-central Maryland. A cold front was located to the north of the Mid-Atlantic and warm and humid conditions persisted through the evening hours. A bay breeze formed across North-Central Maryland and led to multiple rounds of showers and thunderstorms in this area. Heavy showers also moved into the region from West Virginia and led to heavy rain across north-central Maryland. A cold front was located to the north of the Mid-Atlantic and warm and humid conditions persisted through the evening hours. A bay breeze formed across North-Central Maryland and led to multiple rounds of showers and thunderstorms in this area. Heavy showers also moved into the region from West Virginia and led to heavy rain across north-central Maryland. A cold front was located to the north of the Mid-Atlantic and warm and humid conditions persisted through the evening hours. A bay breeze formed across North-Central Maryland and led to multiple rounds of showers and thunderstorms in this area. Heavy showers also moved into the region from West Virginia and led to heavy rain across north-central Maryland. A cold front was located to the north of the Mid-Atlantic and warm and humid conditions persisted through the evening hours. A bay breeze formed across North-Central Maryland and led to multiple rounds of showers and thunderstorms in this area. Heavy showers also moved into the region from West Virginia and led to heavy rain across north-central Maryland.\nEvent Narrative: High water closed all westbound lanes on Maryland-108/Olney Mill Road. Defense Highway was closed due to high water. There were two vehicles stranded in high water on Brock Bridge Road. A pickup truck was swept off Brock Bridge Road by flood waters. The truck moved 150 feet south and ended in the Patuxent River. The stream gauge at Savage River reached flood stage of 10 feet. The river peaked at 12 feet at 245 AM EST. At 10 feet, Riverside trails begin to flood. Water also approaches fields off Bald Eagle Drive and approach Brock Bridge Road.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 36.9916 km away, between 2015-05-27 16:55:00 and 2015-05-27 16:55:00. The events included records with estimated wind gusts of 34.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: An unstable air mass with marginal shear resulted in scattered convection with embedded stronger thunderstorms as a wave of low pressure moved through the region.\nEvent Narrative: Between 31 and 34 knots was reported at TPLM2.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 38.1238 km away, between 2015-05-31 19:00:00 and 2015-05-31 22:50:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 4000.0 and crop damage of 0.0. \n\nEpisode Narrative: An upper-level disturbance passed through, triggering some showers and thunderstorms. A few thunderstorms became severe due to an unstable atmosphere. An upper-level disturbance passed through, triggering some showers and thunderstorms. A few thunderstorms became severe due to an unstable atmosphere. An upper-level disturbance passed through, triggering some showers and thunderstorms. A few thunderstorms became severe due to an unstable atmosphere.\nEvent Narrative: A tree was down at Locust Lane and Route 26. A tree was also down on Georgetown Boulevard and Route 26. Multiple trees down. A tree was down along the 1500 Block of Buckhorn Road.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 31.8446 km away, between 2015-06-01 16:12:00 and 2015-06-01 17:06:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front slowly approached and moved south through the Mid Atlantic late in the day. Ahead of the front, southerly flow ushered in a warm and moisture air mass, resulting in MLCAPE values between 1000-1500 J/kg with marginal shear. Numerous showers and thunderstorms with embedded severe formed to the southwest and progressed to the northeast prior to the cold frontal passage. A cold front slowly approached and moved south through the Mid Atlantic late in the day. Ahead of the front, southerly flow ushered in a warm and moisture air mass, resulting in MLCAPE values between 1000-1500 J/kg with marginal shear. Numerous showers and thunderstorms with embedded severe formed to the southwest and progressed to the northeast prior to the cold frontal passage. A cold front slowly approached and moved south through the Mid Atlantic late in the day. Ahead of the front, southerly flow ushered in a warm and moisture air mass, resulting in MLCAPE values between 1000-1500 J/kg with marginal shear. Numerous showers and thunderstorms with embedded severe formed to the southwest and progressed to the northeast prior to the cold frontal passage. A cold front slowly approached and moved south through the Mid Atlantic late in the day. Ahead of the front, southerly flow ushered in a warm and moisture air mass, resulting in MLCAPE values between 1000-1500 J/kg with marginal shear. Numerous showers and thunderstorms with embedded severe formed to the southwest and progressed to the northeast prior to the cold frontal passage. A cold front slowly approached and moved south through the Mid Atlantic late in the day. Ahead of the front, southerly flow ushered in a warm and moisture air mass, resulting in MLCAPE values between 1000-1500 J/kg with marginal shear. Numerous showers and thunderstorms with embedded severe formed to the southwest and progressed to the northeast prior to the cold frontal passage. A cold front slowly approached and moved south through the Mid Atlantic late in the day. Ahead of the front, southerly flow ushered in a warm and moisture air mass, resulting in MLCAPE values between 1000-1500 J/kg with marginal shear. Numerous showers and thunderstorms with embedded severe formed to the southwest and progressed to the northeast prior to the cold frontal passage. A cold front slowly approached and moved south through the Mid Atlantic late in the day. Ahead of the front, southerly flow ushered in a warm and moisture air mass, resulting in MLCAPE values between 1000-1500 J/kg with marginal shear. Numerous showers and thunderstorms with embedded severe formed to the southwest and progressed to the northeast prior to the cold frontal passage.\nEvent Narrative: TPLM2 reported gusts between 32 and 34 knots. FSKM2 reported gusts between 32 and 34 knots. KNAK reported gusts of 41 knots. TOL reported gusts between 47 to 49 knots. KNT reported gusts of 38 knots. GBY reported gusts between 31 and 39 knots. TCBM2 reported gusts between 32 to 38 knots.", "The following events were reported: Flash Flood, Flood. These occurred near station USW00093721, approximately 36.092 km away, between 2015-06-01 17:25:00 and 2015-06-02 00:00:00. The flood was caused by Heavy Rain. Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front slowly approached and moved south through the Mid Atlantic late in the day. Ahead of the front, southerly flow ushered in a warm and moist air mass. Numerous showers and thunderstorms with embedded strong to severe storms formed to the southwest and progressed to the northeast prior to the cold frontal passage. This activity produced copious amounts rain and led to flash flooding across northeast Maryland. A cold front slowly approached and moved south through the Mid Atlantic late in the day. Ahead of the front, southerly flow ushered in a warm and moist air mass. Numerous showers and thunderstorms with embedded strong to severe storms formed to the southwest and progressed to the northeast prior to the cold frontal passage. This activity produced copious amounts rain and led to flash flooding across northeast Maryland. A cold front slowly approached and moved south through the Mid Atlantic late in the day. Ahead of the front, southerly flow ushered in a warm and moist air mass. Numerous showers and thunderstorms with embedded strong to severe storms formed to the southwest and progressed to the northeast prior to the cold frontal passage. This activity produced copious amounts rain and led to flash flooding across northeast Maryland. A cold front slowly approached and moved south through the Mid Atlantic late in the day. Ahead of the front, southerly flow ushered in a warm and moist air mass. Numerous showers and thunderstorms with embedded strong to severe storms formed to the southwest and progressed to the northeast prior to the cold frontal passage. This activity produced copious amounts rain and led to flash flooding across northeast Maryland.\nEvent Narrative: Harford road was flooded and closed north of Reckord road near Rocky Branch. There was a flood water rescue reported at Belair road and Talmadge drive. The raod was closed in both directions. There was two feet of flowing water reported across the roadway near the intersection of Loch Raven Boulevard and Taylor Avenue. Maryland route 97 was reported flooded and closed at Reddy Branch in Brookeville.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 37.5985 km away, between 2015-06-08 18:34:00 and 2015-06-08 19:02:00. The events included records with estimated wind gusts of 52.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 6000.0 and crop damage of 0.0. \n\nEpisode Narrative: Destabilization occurred along and west of the Blue Ridge with MLCAPE 1500-2000 J/Kg forming by the afternoon hours. Backing of winds also led to increased shear profiles, which combined with the increased instability produced isolated thunderstorms ahead of an approaching cold front and a line of showers and thunderstorms right along the line. Destabilization occurred along and west of the Blue Ridge with MLCAPE 1500-2000 J/Kg forming by the afternoon hours. Backing of winds also led to increased shear profiles, which combined with the increased instability produced isolated thunderstorms ahead of an approaching cold front and a line of showers and thunderstorms right along the line. Destabilization occurred along and west of the Blue Ridge with MLCAPE 1500-2000 J/Kg forming by the afternoon hours. Backing of winds also led to increased shear profiles, which combined with the increased instability produced isolated thunderstorms ahead of an approaching cold front and a line of showers and thunderstorms right along the line. Destabilization occurred along and west of the Blue Ridge with MLCAPE 1500-2000 J/Kg forming by the afternoon hours. Backing of winds also led to increased shear profiles, which combined with the increased instability produced isolated thunderstorms ahead of an approaching cold front and a line of showers and thunderstorms right along the line.\nEvent Narrative: A tree was reported down at the intersection of Mink Hollow Rd and Deer Valley Rd. A tree fell on wires at the intersection of Guyton Rd and Reckford Rd. A tree was reported down on wires at the intersection of Oakmont Rd and Pleasantville Rd. A tree was reported down at the intersection of Western Run Rd and Shawn Rd.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 31.5646 km away, between 2015-06-08 20:10:00 and 2015-06-08 20:24:00. The events included records with estimated wind gusts of 34.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Destabilization occurred west of the Blue Ridge with MLCAPE 1500-2000 J/Kg forming by the afternoon hours. Backing of winds also led to increased shear profiles, which combined with the increased instability produced isolated thunderstorms ahead of an approaching cold front and a line of showers and strong thunderstorms right along the line. Destabilization occurred west of the Blue Ridge with MLCAPE 1500-2000 J/Kg forming by the afternoon hours. Backing of winds also led to increased shear profiles, which combined with the increased instability produced isolated thunderstorms ahead of an approaching cold front and a line of showers and strong thunderstorms right along the line.\nEvent Narrative: Patapsco Buoy 44043 reported gusts between 33 and 34 knots. KW29 reported gusts between 31 and 34 knots.", "The following events were reported: Flash Flood. These occurred near station USW00093721, approximately 41.0919 km away, between 2015-06-08 20:48:00 and 2015-06-09 02:32:00.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 10000.0 and crop damage of 0.0. \n\nEpisode Narrative: Destabilization occurred along and west of the Blue Ridge with MLCAPE 1500-2000 J/Kg forming by the afternoon hours. Thunderstorms formed ahead of a cold front and were capable of heavy rain that led to flash flooding in northeast Maryland. Destabilization occurred along and west of the Blue Ridge with MLCAPE 1500-2000 J/Kg forming by the afternoon hours. Thunderstorms formed ahead of a cold front and were capable of heavy rain that led to flash flooding in northeast Maryland. Destabilization occurred along and west of the Blue Ridge with MLCAPE 1500-2000 J/Kg forming by the afternoon hours. Thunderstorms formed ahead of a cold front and were capable of heavy rain that led to flash flooding in northeast Maryland.\nEvent Narrative: There was a swift water rescue from Jones Falls near the intersection of Old Valley Road and Stevenson Road. A car tried to cross the flooded bridge and stalled. A road was closed near route 7 and route 136. South Tollgate road was closed at Ruth Road.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 26.9059 km away, between 2015-06-14 17:18:00 and 2015-06-14 17:54:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A weak surface boundary slipped south into northern Virginia during the day. Plenty of warming and increasing moisture advection led to destabilization, with SBCAPE values between 1000-2000 J/kg across much of the area. Increasing unidirectional 0-6 km bulk shear late in the day, with values between 20-25 knots, combined with the unstable air mass and with a passing shortwave, produced scattered thunderstorms. A weak surface boundary slipped south into northern Virginia during the day. Plenty of warming and increasing moisture advection led to destabilization, with SBCAPE values between 1000-2000 J/kg across much of the area. Increasing unidirectional 0-6 km bulk shear late in the day, with values between 20-25 knots, combined with the unstable air mass and with a passing shortwave, produced scattered thunderstorms. A weak surface boundary slipped south into northern Virginia during the day. Plenty of warming and increasing moisture advection led to destabilization, with SBCAPE values between 1000-2000 J/kg across much of the area. Increasing unidirectional 0-6 km bulk shear late in the day, with values between 20-25 knots, combined with the unstable air mass and with a passing shortwave, produced scattered thunderstorms.\nEvent Narrative: Patapsco Buoy 44043 reported a gusts between 31 and 34 knots. TCBM2 reported a gusts between 32 and 34 knots. FSKM2 reported a gust of 37 knots.", "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00093721, approximately 37.1695 km away, between 2015-06-18 15:22:00 and 2015-06-18 15:29:00. The events included records with hailstones measuring 26.75 inches.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 1000.0 and crop damage of 0.0. \n\nEpisode Narrative: The Mid-Atlantic remained in the warm sector as a nearly stalled warm front lingered just north of the Mason-Dixon line and the associated cold front swung in from the west by the evening. The unstable air mass led to SBCAPE values between 2000-3500 J/kg while effective shear values were between 30-40 knots. The Mid-Atlantic remained in the warm sector as a nearly stalled warm front lingered just north of the Mason-Dixon line and the associated cold front swung in from the west by the evening. The unstable air mass led to SBCAPE values between 2000-3500 J/kg while effective shear values were between 30-40 knots.\nEvent Narrative: A large tree was reported down along the 22200 block of Georgia Ave.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 33.4301 km away, between 2015-06-18 20:27:00 and 2015-06-18 20:27:00. The events included records with measured wind gusts of 36.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: The Mid-Atlantic remained in the warm sector as a nearly stalled warm front lingered just north of the Mason-Dixon line and the associated cold front swung in from the west by the evening. The unstable air mass led to SBCAPE values between 2000-3500 J/kg while effective shear values were between 30-40 knots.\nEvent Narrative: CRS reported gusts of 36 knots.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 15.6627 km away, between 2015-06-20 15:15:00 and 2015-06-20 20:25:00.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 11000.0 and crop damage of 0.0. \n\nEpisode Narrative: A stalled frontal boundary acted as the triggering point for an initial line of showers and thunderstorms, with many of the storms becoming severe with strong moisture advection combining with diurnal heating and leading to an unstable air mass. The remnants of Tropical System Bill moved through the Mid-Atlantic overnight, continuing the severe threat late into the early part of the overnight hours. As winds backed with the tropical system, increasing directional and magnitude shear led to the development of tornadoes. A stalled frontal boundary acted as the triggering point for an initial line of showers and thunderstorms, with many of the storms becoming severe with strong moisture advection combining with diurnal heating and leading to an unstable air mass. The remnants of Tropical System Bill moved through the Mid-Atlantic overnight, continuing the severe threat late into the early part of the overnight hours. As winds backed with the tropical system, increasing directional and magnitude shear led to the development of tornadoes. A stalled frontal boundary acted as the triggering point for an initial line of showers and thunderstorms, with many of the storms becoming severe with strong moisture advection combining with diurnal heating and leading to an unstable air mass. The remnants of Tropical System Bill moved through the Mid-Atlantic overnight, continuing the severe threat late into the early part of the overnight hours. As winds backed with the tropical system, increasing directional and magnitude shear led to the development of tornadoes. A stalled frontal boundary acted as the triggering point for an initial line of showers and thunderstorms, with many of the storms becoming severe with strong moisture advection combining with diurnal heating and leading to an unstable air mass. The remnants of Tropical System Bill moved through the Mid-Atlantic overnight, continuing the severe threat late into the early part of the overnight hours. As winds backed with the tropical system, increasing directional and magnitude shear led to the development of tornadoes. A stalled frontal boundary acted as the triggering point for an initial line of showers and thunderstorms, with many of the storms becoming severe with strong moisture advection combining with diurnal heating and leading to an unstable air mass. The remnants of Tropical System Bill moved through the Mid-Atlantic overnight, continuing the severe threat late into the early part of the overnight hours. As winds backed with the tropical system, increasing directional and magnitude shear led to the development of tornadoes. A stalled frontal boundary acted as the triggering point for an initial line of showers and thunderstorms, with many of the storms becoming severe with strong moisture advection combining with diurnal heating and leading to an unstable air mass. The remnants of Tropical System Bill moved through the Mid-Atlantic overnight, continuing the severe threat late into the early part of the overnight hours. As winds backed with the tropical system, increasing directional and magnitude shear led to the development of tornadoes. A stalled frontal boundary acted as the triggering point for an initial line of showers and thunderstorms, with many of the storms becoming severe with strong moisture advection combining with diurnal heating and leading to an unstable air mass. The remnants of Tropical System Bill moved through the Mid-Atlantic overnight, continuing the severe threat late into the early part of the overnight hours. As winds backed with the tropical system, increasing directional and magnitude shear led to the development of tornadoes. A stalled frontal boundary acted as the triggering point for an initial line of showers and thunderstorms, with many of the storms becoming severe with strong moisture advection combining with diurnal heating and leading to an unstable air mass. The remnants of Tropical System Bill moved through the Mid-Atlantic overnight, continuing the severe threat late into the early part of the overnight hours. As winds backed with the tropical system, increasing directional and magnitude shear led to the development of tornadoes. A stalled frontal boundary acted as the triggering point for an initial line of showers and thunderstorms, with many of the storms becoming severe with strong moisture advection combining with diurnal heating and leading to an unstable air mass. The remnants of Tropical System Bill moved through the Mid-Atlantic overnight, continuing the severe threat late into the early part of the overnight hours. As winds backed with the tropical system, increasing directional and magnitude shear led to the development of tornadoes. A stalled frontal boundary acted as the triggering point for an initial line of showers and thunderstorms, with many of the storms becoming severe with strong moisture advection combining with diurnal heating and leading to an unstable air mass. The remnants of Tropical System Bill moved through the Mid-Atlantic overnight, continuing the severe threat late into the early part of the overnight hours. As winds backed with the tropical system, increasing directional and magnitude shear led to the development of tornadoes. A stalled frontal boundary acted as the triggering point for an initial line of showers and thunderstorms, with many of the storms becoming severe with strong moisture advection combining with diurnal heating and leading to an unstable air mass. The remnants of Tropical System Bill moved through the Mid-Atlantic overnight, continuing the severe threat late into the early part of the overnight hours. As winds backed with the tropical system, increasing directional and magnitude shear led to the development of tornadoes. A stalled frontal boundary acted as the triggering point for an initial line of showers and thunderstorms, with many of the storms becoming severe with strong moisture advection combining with diurnal heating and leading to an unstable air mass. The remnants of Tropical System Bill moved through the Mid-Atlantic overnight, continuing the severe threat late into the early part of the overnight hours. As winds backed with the tropical system, increasing directional and magnitude shear led to the development of tornadoes. A stalled frontal boundary acted as the triggering point for an initial line of showers and thunderstorms, with many of the storms becoming severe with strong moisture advection combining with diurnal heating and leading to an unstable air mass. The remnants of Tropical System Bill moved through the Mid-Atlantic overnight, continuing the severe threat late into the early part of the overnight hours. As winds backed with the tropical system, increasing directional and magnitude shear led to the development of tornadoes.\nEvent Narrative: A tree was reported down on Harbarts Court at Sigfriend Court. A tree was reported down near the 900 block of Cathedral St. A tree was reported down near the 5500 block of Race Rd. A tree was reported down on Valley Rd between Wilkens Ave and Hilltop Ave. Measured at Umbc1. A tree about 10 ft tall was reported down. A tree was reported down on I-95. Reported by WBAL-TV Baltimore. A tree was reported down on Old Montgomery Rd near Brightfield Rd. A tree was reported down on Meadow Ridge Rd near Huntshire Dr. A tree was reported down on Rivendell Lane near Harpers Farm Rd. A tree was reported down along Harford Rd. Numerous tree tops were snapped and tree limbs were reported across the ground near the interchange of I-695 and Security Blvd. A tree was reported down at the intersection of Ten Oaks Rd and Smallwood Court.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 27.7359 km away, between 2015-06-20 20:05:00 and 2015-06-20 21:30:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A stalled frontal boundary acted as the triggering point for an initial line of showers and thunderstorms, with many of the storms becoming severe with strong moisture advection combining with diurnal heating and leading to an unstable air mass. The remnants of Tropical System Bill moved through the Mid-Atlantic overnight, continuing the severe threat late into the early part of the overnight hours. A stalled frontal boundary acted as the triggering point for an initial line of showers and thunderstorms, with many of the storms becoming severe with strong moisture advection combining with diurnal heating and leading to an unstable air mass. The remnants of Tropical System Bill moved through the Mid-Atlantic overnight, continuing the severe threat late into the early part of the overnight hours. A stalled frontal boundary acted as the triggering point for an initial line of showers and thunderstorms, with many of the storms becoming severe with strong moisture advection combining with diurnal heating and leading to an unstable air mass. The remnants of Tropical System Bill moved through the Mid-Atlantic overnight, continuing the severe threat late into the early part of the overnight hours. A stalled frontal boundary acted as the triggering point for an initial line of showers and thunderstorms, with many of the storms becoming severe with strong moisture advection combining with diurnal heating and leading to an unstable air mass. The remnants of Tropical System Bill moved through the Mid-Atlantic overnight, continuing the severe threat late into the early part of the overnight hours. A stalled frontal boundary acted as the triggering point for an initial line of showers and thunderstorms, with many of the storms becoming severe with strong moisture advection combining with diurnal heating and leading to an unstable air mass. The remnants of Tropical System Bill moved through the Mid-Atlantic overnight, continuing the severe threat late into the early part of the overnight hours.\nEvent Narrative: FSKM2 reported gusts between 32 and 40 knots. KNT reported gusts between 31 and 34 knots. TOL reported gusts between 31 and 35 knots. KW29 reported gusts of 43 knots. BLMRE reported gusts of 36 knots.", "The following events were reported: Flash Flood. These occurred near station USW00093721, approximately 8.186 km away, between 2015-06-20 20:46:00 and 2015-06-20 23:30:00.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 10000.0 and crop damage of 0.0. \n\nEpisode Narrative: Remnants of Tropical Storm Bill moved into the Mid-Atlantic causing moisture to increase. Showers and thunderstorms led to heavy rain across the Interstate 95 corridor and flash flooding occurred. Some rivers also went to flood into June 21, 2015. Remnants of Tropical Storm Bill moved into the Mid-Atlantic causing moisture to increase. Showers and thunderstorms led to heavy rain across the Interstate 95 corridor and flash flooding occurred. Some rivers also went to flood into June 21, 2015.\nEvent Narrative: There was a car stranded in high water on East Patapsco Avenue between 6th and 7th Streets. There was a vehicle stranded in high water near the intersection of Nursery Road and Baltimore-Annapolis Boulevard.", "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00093721, approximately 27.7324 km away, between 2015-06-23 16:21:00 and 2015-06-23 18:31:00. The events included records with hailstones measuring 39.286764705882355 inches.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 29000.0 and crop damage of 0.0. \n\nEpisode Narrative: A cold front moved south through the region. Southerly flow ahead of the front led to an unstable air mass, which combined with steepening mid level lapse rates and increased sheer led to numerous severe thunderstorms being triggered right ahead of the front. A cold front moved south through the region. Southerly flow ahead of the front led to an unstable air mass, which combined with steepening mid level lapse rates and increased sheer led to numerous severe thunderstorms being triggered right ahead of the front. A cold front moved south through the region. Southerly flow ahead of the front led to an unstable air mass, which combined with steepening mid level lapse rates and increased sheer led to numerous severe thunderstorms being triggered right ahead of the front. A cold front moved south through the region. Southerly flow ahead of the front led to an unstable air mass, which combined with steepening mid level lapse rates and increased sheer led to numerous severe thunderstorms being triggered right ahead of the front. A cold front moved south through the region. Southerly flow ahead of the front led to an unstable air mass, which combined with steepening mid level lapse rates and increased sheer led to numerous severe thunderstorms being triggered right ahead of the front. A cold front moved south through the region. Southerly flow ahead of the front led to an unstable air mass, which combined with steepening mid level lapse rates and increased sheer led to numerous severe thunderstorms being triggered right ahead of the front. A cold front moved south through the region. Southerly flow ahead of the front led to an unstable air mass, which combined with steepening mid level lapse rates and increased sheer led to numerous severe thunderstorms being triggered right ahead of the front. A cold front moved south through the region. Southerly flow ahead of the front led to an unstable air mass, which combined with steepening mid level lapse rates and increased sheer led to numerous severe thunderstorms being triggered right ahead of the front. A cold front moved south through the region. Southerly flow ahead of the front led to an unstable air mass, which combined with steepening mid level lapse rates and increased sheer led to numerous severe thunderstorms being triggered right ahead of the front. A cold front moved south through the region. Southerly flow ahead of the front led to an unstable air mass, which combined with steepening mid level lapse rates and increased sheer led to numerous severe thunderstorms being triggered right ahead of the front. A cold front moved south through the region. Southerly flow ahead of the front led to an unstable air mass, which combined with steepening mid level lapse rates and increased sheer led to numerous severe thunderstorms being triggered right ahead of the front. A cold front moved south through the region. Southerly flow ahead of the front led to an unstable air mass, which combined with steepening mid level lapse rates and increased sheer led to numerous severe thunderstorms being triggered right ahead of the front. A cold front moved south through the region. Southerly flow ahead of the front led to an unstable air mass, which combined with steepening mid level lapse rates and increased sheer led to numerous severe thunderstorms being triggered right ahead of the front. A cold front moved south through the region. Southerly flow ahead of the front led to an unstable air mass, which combined with steepening mid level lapse rates and increased sheer led to numerous severe thunderstorms being triggered right ahead of the front. A cold front moved south through the region. Southerly flow ahead of the front led to an unstable air mass, which combined with steepening mid level lapse rates and increased sheer led to numerous severe thunderstorms being triggered right ahead of the front. A cold front moved south through the region. Southerly flow ahead of the front led to an unstable air mass, which combined with steepening mid level lapse rates and increased sheer led to numerous severe thunderstorms being triggered right ahead of the front. A cold front moved south through the region. Southerly flow ahead of the front led to an unstable air mass, which combined with steepening mid level lapse rates and increased sheer led to numerous severe thunderstorms being triggered right ahead of the front. A cold front moved south through the region. Southerly flow ahead of the front led to an unstable air mass, which combined with steepening mid level lapse rates and increased sheer led to numerous severe thunderstorms being triggered right ahead of the front. A cold front moved south through the region. Southerly flow ahead of the front led to an unstable air mass, which combined with steepening mid level lapse rates and increased sheer led to numerous severe thunderstorms being triggered right ahead of the front. A cold front moved south through the region. Southerly flow ahead of the front led to an unstable air mass, which combined with steepening mid level lapse rates and increased sheer led to numerous severe thunderstorms being triggered right ahead of the front. A cold front moved south through the region. Southerly flow ahead of the front led to an unstable air mass, which combined with steepening mid level lapse rates and increased sheer led to numerous severe thunderstorms being triggered right ahead of the front. A cold front moved south through the region. Southerly flow ahead of the front led to an unstable air mass, which combined with steepening mid level lapse rates and increased sheer led to numerous severe thunderstorms being triggered right ahead of the front. A cold front moved south through the region. Southerly flow ahead of the front led to an unstable air mass, which combined with steepening mid level lapse rates and increased sheer led to numerous severe thunderstorms being triggered right ahead of the front. A cold front moved south through the region. Southerly flow ahead of the front led to an unstable air mass, which combined with steepening mid level lapse rates and increased sheer led to numerous severe thunderstorms being triggered right ahead of the front. A cold front moved south through the region. Southerly flow ahead of the front led to an unstable air mass, which combined with steepening mid level lapse rates and increased sheer led to numerous severe thunderstorms being triggered right ahead of the front. A cold front moved south through the region. Southerly flow ahead of the front led to an unstable air mass, which combined with steepening mid level lapse rates and increased sheer led to numerous severe thunderstorms being triggered right ahead of the front. A cold front moved south through the region. Southerly flow ahead of the front led to an unstable air mass, which combined with steepening mid level lapse rates and increased sheer led to numerous severe thunderstorms being triggered right ahead of the front. A cold front moved south through the region. Southerly flow ahead of the front led to an unstable air mass, which combined with steepening mid level lapse rates and increased sheer led to numerous severe thunderstorms being triggered right ahead of the front. A cold front moved south through the region. Southerly flow ahead of the front led to an unstable air mass, which combined with steepening mid level lapse rates and increased sheer led to numerous severe thunderstorms being triggered right ahead of the front. A cold front moved south through the region. Southerly flow ahead of the front led to an unstable air mass, which combined with steepening mid level lapse rates and increased sheer led to numerous severe thunderstorms being triggered right ahead of the front. A cold front moved south through the region. Southerly flow ahead of the front led to an unstable air mass, which combined with steepening mid level lapse rates and increased sheer led to numerous severe thunderstorms being triggered right ahead of the front. A cold front moved south through the region. Southerly flow ahead of the front led to an unstable air mass, which combined with steepening mid level lapse rates and increased sheer led to numerous severe thunderstorms being triggered right ahead of the front. A cold front moved south through the region. Southerly flow ahead of the front led to an unstable air mass, which combined with steepening mid level lapse rates and increased sheer led to numerous severe thunderstorms being triggered right ahead of the front. A cold front moved south through the region. Southerly flow ahead of the front led to an unstable air mass, which combined with steepening mid level lapse rates and increased sheer led to numerous severe thunderstorms being triggered right ahead of the front.\nEvent Narrative: A tree was reported down at the intersection of Lavender Court and Muddy Creek Rd. A tree was reported down at the intersection of Route 2 and Route 450. A tree was reported down blocking Carrs Mill Rd. A tree was reported down at the intersection of Route 2 and Route 648. A tree was reported down in North Point State Park. A few large branches 4-5 ft were reported down. Multiple cars and homes reported busted windows. Reported by Kbal-tv Baltimore. Extensive damage was reported just east of Cockeysville, MD with numerous trees reported down, windows of cars and homes smashed and holes in the siding of homes. Reported by Fox 45. Two large trees were reported down, along with 1 tree uprooted and 1 chimney knocked down. Multiple trees were reported down in North Laytonsville. A tree blocked the intersection of Route 147 and Sunshine Ave. A tree was reported down across Route 650 near the intersection of Gold Mine. Multiple trees down along MD Route 214. A tree was reported down at the intersection of College Pkwy and Shore Acres Rd. A tree was reported down at the intersection of Harbor Rd and Dryer Rd. A tree was reported down at the intersection of Old Annapolis Rd and Route 198. A tree was reported down near the intersection of Brock Bridge Rd and Route 198. A tree was reported down near the intersection of Rossback Rd and Patuxent River Rd. A tree was reported down at the intersection of Ferry Point Rd and Harness Creek Rd. Multiple trees were reported down at the intersection of Broadwater Ave and Mago Vista Ave. Multiple trees were reported down at the intersection of Chesterfield Rd and Hawkins Rd. A tree was reported down at the intersection of College Pkwy and Bellerive Rd. A tree was reported down at the intersection of Cottage Run and Birdsville Rd. A tree was reported down at the intersection of Route 2 and Owensville Sudley Rd. A tree was reported down at the intersection of Riggs Ave and Avondale Circle. A small tree and multiple large branches were snapped.", "The following events were reported: Flash Flood. These occurred near station USW00093721, approximately 27.0465 km away, between 2015-06-23 16:55:00 and 2015-06-23 20:45:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front moved south through the region. Southerly flow ahead of the front led to an unstable air mass, which combined with steepening mid level lapse rates and increased sheer led to numerous severe thunderstorms being triggered right ahead of the front. Some thunderstorms produced copious amounts of rainfall and led to flooding around the Baltimore and Washington DC metros. A cold front moved south through the region. Southerly flow ahead of the front led to an unstable air mass, which combined with steepening mid level lapse rates and increased sheer led to numerous severe thunderstorms being triggered right ahead of the front. Some thunderstorms produced copious amounts of rainfall and led to flooding around the Baltimore and Washington DC metros. A cold front moved south through the region. Southerly flow ahead of the front led to an unstable air mass, which combined with steepening mid level lapse rates and increased sheer led to numerous severe thunderstorms being triggered right ahead of the front. Some thunderstorms produced copious amounts of rainfall and led to flooding around the Baltimore and Washington DC metros.\nEvent Narrative: The stream gauge on Whitemarsh Run at White Marsh reached flood stage of 10 feet. The river crested at 11.12 feet at 19:00 EST. Water began to cover parking lots near the stream, particularly near Town Center Court. There was high water flowing and disrupting traffic at the intersection of Greenspring Avenue and Ridge Road. Bear Branch was out of its banks and was flowing over Contee Road.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 28.3902 km away, between 2015-06-23 17:00:00 and 2015-06-23 18:17:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front moved south through the region. Southerly flow ahead of the front led to an unstable air mass, which combined with steepening mid level lapse rates and increased sheer led to numerous severe thunderstorms being triggered right ahead of the front. A cold front moved south through the region. Southerly flow ahead of the front led to an unstable air mass, which combined with steepening mid level lapse rates and increased sheer led to numerous severe thunderstorms being triggered right ahead of the front. A cold front moved south through the region. Southerly flow ahead of the front led to an unstable air mass, which combined with steepening mid level lapse rates and increased sheer led to numerous severe thunderstorms being triggered right ahead of the front. A cold front moved south through the region. Southerly flow ahead of the front led to an unstable air mass, which combined with steepening mid level lapse rates and increased sheer led to numerous severe thunderstorms being triggered right ahead of the front. A cold front moved south through the region. Southerly flow ahead of the front led to an unstable air mass, which combined with steepening mid level lapse rates and increased sheer led to numerous severe thunderstorms being triggered right ahead of the front. A cold front moved south through the region. Southerly flow ahead of the front led to an unstable air mass, which combined with steepening mid level lapse rates and increased sheer led to numerous severe thunderstorms being triggered right ahead of the front. A cold front moved south through the region. Southerly flow ahead of the front led to an unstable air mass, which combined with steepening mid level lapse rates and increased sheer led to numerous severe thunderstorms being triggered right ahead of the front. A cold front moved south through the region. Southerly flow ahead of the front led to an unstable air mass, which combined with steepening mid level lapse rates and increased sheer led to numerous severe thunderstorms being triggered right ahead of the front. A cold front moved south through the region. Southerly flow ahead of the front led to an unstable air mass, which combined with steepening mid level lapse rates and increased sheer led to numerous severe thunderstorms being triggered right ahead of the front. A cold front moved south through the region. Southerly flow ahead of the front led to an unstable air mass, which combined with steepening mid level lapse rates and increased sheer led to numerous severe thunderstorms being triggered right ahead of the front. A cold front moved south through the region. Southerly flow ahead of the front led to an unstable air mass, which combined with steepening mid level lapse rates and increased sheer led to numerous severe thunderstorms being triggered right ahead of the front. A cold front moved south through the region. Southerly flow ahead of the front led to an unstable air mass, which combined with steepening mid level lapse rates and increased sheer led to numerous severe thunderstorms being triggered right ahead of the front. A cold front moved south through the region. Southerly flow ahead of the front led to an unstable air mass, which combined with steepening mid level lapse rates and increased sheer led to numerous severe thunderstorms being triggered right ahead of the front. A cold front moved south through the region. Southerly flow ahead of the front led to an unstable air mass, which combined with steepening mid level lapse rates and increased sheer led to numerous severe thunderstorms being triggered right ahead of the front.\nEvent Narrative: BLTM2 reported gusts between 34 and 39 knots. HRT reported gusts of 38 knots. Patapsco Buoy 44043 reported gusts between 33 and 39 knots. KW29 reported gusts of 38 knots. GUN reported gusts between 33 and 34 knots. BLMRE reported gusts of 36 knots. FSKM2 reported gusts between 32 and 47 knots. TCBM2 reported gusts between 31 and 34 knots. Annapolis Buoy 44063 reported gusts between 31 and 41 knots. KNAK reported gusts between 31 and 40 knots. SPT reported gusts between 32 and 35 knots. TOL reported gusts between 34 and 43 knots. KNT reported gusts between 35 and 38 knots. GBY reported gusts between 34 and 47 knots.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 32.8297 km away, between 2015-06-25 19:06:00 and 2015-06-25 20:27:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front moved south through the region. Southerly flow ahead of the front led to an unstable air mass, which combined with steepening mid level lapse rates and increased sheer led to numerous severe thunderstorms being triggered right ahead of the front. A cold front moved south through the region. Southerly flow ahead of the front led to an unstable air mass, which combined with steepening mid level lapse rates and increased sheer led to numerous severe thunderstorms being triggered right ahead of the front. A cold front moved south through the region. Southerly flow ahead of the front led to an unstable air mass, which combined with steepening mid level lapse rates and increased sheer led to numerous severe thunderstorms being triggered right ahead of the front. A cold front moved south through the region. Southerly flow ahead of the front led to an unstable air mass, which combined with steepening mid level lapse rates and increased sheer led to numerous severe thunderstorms being triggered right ahead of the front. A cold front moved south through the region. Southerly flow ahead of the front led to an unstable air mass, which combined with steepening mid level lapse rates and increased sheer led to numerous severe thunderstorms being triggered right ahead of the front. A cold front moved south through the region. Southerly flow ahead of the front led to an unstable air mass, which combined with steepening mid level lapse rates and increased sheer led to numerous severe thunderstorms being triggered right ahead of the front. A cold front moved south through the region. Southerly flow ahead of the front led to an unstable air mass, which combined with steepening mid level lapse rates and increased sheer led to numerous severe thunderstorms being triggered right ahead of the front.\nEvent Narrative: TCBM2 reported gusts between 33 and 34 knots. KNAK reported gusts between 31 and 34 knots. Annapolis Buoy 44063 reported gusts between 31 and 41 knots. GBY reported gusts between 33 and 36 knots. SPT reported gusts between 33 and 34 knots. TOL reported gusts between 31 and 34 knots. KNT reported gusts between 33 and 34 knots.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 19.9621 km away, between 2015-06-27 12:00:00 and 2015-06-27 12:40:00. The events included records with estimated wind gusts of 34.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Potent low pressure passed by to our west, and the warm front associated with the low moved through our area during this time. Warm and moist air near and south of the boundary led to an unstable atmosphere, while forcing from the warm front provided the lift, resulting in scattered, then a line of thunderstorms. Potent low pressure passed by to our west, and the warm front associated with the low moved through our area during this time. Warm and moist air near and south of the boundary led to an unstable atmosphere, while forcing from the warm front provided the lift, resulting in scattered, then a line of thunderstorms.\nEvent Narrative: FSKM2 reported gusts between 31 and 34 knots. Patapsco Buoy 44043 reported gusts between 31 and 34 knots.", "The following events were reported: Flash Flood, Flood. These occurred near station USW00093721, approximately 23.9069 km away, between 2015-06-27 15:30:00 and 2015-06-28 02:50:00. The flood was caused by Heavy Rain. Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 20000.0 and crop damage of 0.0. \n\nEpisode Narrative: Potent low pressure passed by to our west, and the warm front associated with the low moved through our area during this time. Warm and moist air near and south of the boundary led to an unstable atmosphere, while forcing from the warm front provided the lift. Thunderstorms developed and produced copious amounts of rainfall east of the Blue Ridge Mountains. Potent low pressure passed by to our west, and the warm front associated with the low moved through our area during this time. Warm and moist air near and south of the boundary led to an unstable atmosphere, while forcing from the warm front provided the lift. Thunderstorms developed and produced copious amounts of rainfall east of the Blue Ridge Mountains. Potent low pressure passed by to our west, and the warm front associated with the low moved through our area during this time. Warm and moist air near and south of the boundary led to an unstable atmosphere, while forcing from the warm front provided the lift. Thunderstorms developed and produced copious amounts of rainfall east of the Blue Ridge Mountains. Potent low pressure passed by to our west, and the warm front associated with the low moved through our area during this time. Warm and moist air near and south of the boundary led to an unstable atmosphere, while forcing from the warm front provided the lift. Thunderstorms developed and produced copious amounts of rainfall east of the Blue Ridge Mountains. Potent low pressure passed by to our west, and the warm front associated with the low moved through our area during this time. Warm and moist air near and south of the boundary led to an unstable atmosphere, while forcing from the warm front provided the lift. Thunderstorms developed and produced copious amounts of rainfall east of the Blue Ridge Mountains. Potent low pressure passed by to our west, and the warm front associated with the low moved through our area during this time. Warm and moist air near and south of the boundary led to an unstable atmosphere, while forcing from the warm front provided the lift. Thunderstorms developed and produced copious amounts of rainfall east of the Blue Ridge Mountains. Potent low pressure passed by to our west, and the warm front associated with the low moved through our area during this time. Warm and moist air near and south of the boundary led to an unstable atmosphere, while forcing from the warm front provided the lift. Thunderstorms developed and produced copious amounts of rainfall east of the Blue Ridge Mountains. Potent low pressure passed by to our west, and the warm front associated with the low moved through our area during this time. Warm and moist air near and south of the boundary led to an unstable atmosphere, while forcing from the warm front provided the lift. Thunderstorms developed and produced copious amounts of rainfall east of the Blue Ridge Mountains. Potent low pressure passed by to our west, and the warm front associated with the low moved through our area during this time. Warm and moist air near and south of the boundary led to an unstable atmosphere, while forcing from the warm front provided the lift. Thunderstorms developed and produced copious amounts of rainfall east of the Blue Ridge Mountains. Potent low pressure passed by to our west, and the warm front associated with the low moved through our area during this time. Warm and moist air near and south of the boundary led to an unstable atmosphere, while forcing from the warm front provided the lift. Thunderstorms developed and produced copious amounts of rainfall east of the Blue Ridge Mountains.\nEvent Narrative: High water led to cars stranded on Terrace Avenue. The stream gauge on Minebank Run at Glen Arm reached a flood stage of 8 feet. It crested at 8.35 feet at 16:20 EST. Water covers the access road to Talmar. The stream gauge on the Patuxent River at Unity reached a flood stage of 8 feet. The river crested at 8.76 feet at 20:00 EST. The parking lot for the Patuxent River State Park at Maryland Route 97 began to flood. The stream gauge on the Patapsco River at Elkridge reached a flood stage of 15 feet. The river crested at 15.08 feet at 22:00 EST. Water began to cover a portion of River Road in Patapsco Valley State Park. Large portions of the park began to flood near the playground off Gunn Road. The stream gauge on Little Patuxent River at Savage reached a flood stage of 10 feet. The river crested at 13.06 feet at 16:30 EST. Riverside trails began to flood. Water also approached fields off Bald Eagle Drive, and approached Brock Bridge Road. The stream gauge on Patuxent River at Brighton reached flood stage of 9 feet. It crested at 9.22 feet on 6/28 00:15 EST. Havilland Mill Road was flooded. The stream gauge on Honeygo Run at White Marsh reached a flood stage of 6 feet. The river crested at 7.17 feet at 17:30 EST. Water began to flow behind a business on Ebenezer Road. Gaither Road was closed due to high water. There were lanes closed along Interstate 83 at Chase Street. There were water rescues of multiple people on roofs of cars on Pulaski Highway and Rosedale Ave.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 39.4601 km away, between 2015-06-27 17:05:00 and 2015-06-27 17:05:00. The events included records with estimated wind gusts of 52.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A line of strong to locally severe thunderstorms that moved through the Eastern Shore during the early evening of the 27th brought the dual impact of both damaging winds and flooding rains.\nEvent Narrative: A severe thunderstorm knocked down trees in Rock Hall.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 29.0255 km away, between 2015-06-30 14:12:00 and 2015-06-30 16:10:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A warm front passed through the area while an upper-level trough approached from the west. A southerly flow behind the front caused an unstable atmosphere, and moderate amounts of instability developed due to colder air aloft ahead of the approaching trough. There was enough instability for some thunderstorms to become severe as a cold front approached from the west. A warm front passed through the area while an upper-level trough approached from the west. A southerly flow behind the front caused an unstable atmosphere, and moderate amounts of instability developed due to colder air aloft ahead of the approaching trough. There was enough instability for some thunderstorms to become severe as a cold front approached from the west. A warm front passed through the area while an upper-level trough approached from the west. A southerly flow behind the front caused an unstable atmosphere, and moderate amounts of instability developed due to colder air aloft ahead of the approaching trough. There was enough instability for some thunderstorms to become severe as a cold front approached from the west. A warm front passed through the area while an upper-level trough approached from the west. A southerly flow behind the front caused an unstable atmosphere, and moderate amounts of instability developed due to colder air aloft ahead of the approaching trough. There was enough instability for some thunderstorms to become severe as a cold front approached from the west. A warm front passed through the area while an upper-level trough approached from the west. A southerly flow behind the front caused an unstable atmosphere, and moderate amounts of instability developed due to colder air aloft ahead of the approaching trough. There was enough instability for some thunderstorms to become severe as a cold front approached from the west.\nEvent Narrative: GBY reported gusts between 33 and 36 knots. FSKM2 reported gusts of 38 knots. TOL reported gusts between 38 and 41 knots. KNT reported gusts between 31 and 34 knots. Annapolis buoy 44063 reported gusts between 31 and 33 knots.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 47.1467 km away, between 2015-06-30 16:10:00 and 2015-06-30 16:10:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Widely scattered strong to isolated severe thunderstorms affected the Eastern Shore during the late afternoon and early evening of the 30th.\nEvent Narrative: A severe thunderstorm tore down large tree limbs and wires in Grasonville.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 28.4885 km away, between 2015-07-01 00:00:00 and 2015-07-01 01:58:00. The events included records with measured wind gusts of 42.333333333333336 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A line of showers and thunderstorms with embedded severe thunderstorms moved through the region ahead of an approaching cold front. Southerly flow ahead of the front resulted in modest instability and shear. A line of showers and thunderstorms with embedded severe thunderstorms moved through the region ahead of an approaching cold front. Southerly flow ahead of the front resulted in modest instability and shear. A line of showers and thunderstorms with embedded severe thunderstorms moved through the region ahead of an approaching cold front. Southerly flow ahead of the front resulted in modest instability and shear. A line of showers and thunderstorms with embedded severe thunderstorms moved through the region ahead of an approaching cold front. Southerly flow ahead of the front resulted in modest instability and shear. A line of showers and thunderstorms with embedded severe thunderstorms moved through the region ahead of an approaching cold front. Southerly flow ahead of the front resulted in modest instability and shear. A line of showers and thunderstorms with embedded severe thunderstorms moved through the region ahead of an approaching cold front. Southerly flow ahead of the front resulted in modest instability and shear.\nEvent Narrative: TOL reported gusts of 35 knots. HRT reported gusts between 42 and 43 knots. KNAK reported gusts of 45 knots. SPT reported gusts between 35 and 36 knots. GBY reported gusts of 45 knots.", "The following events were reported: Lightning. These occurred near station USW00093721, approximately 38.0834 km away, between 2015-07-01 00:05:00 and 2015-07-01 00:05:00.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 0.0 and crop damage of 1000.0. \n\nEpisode Narrative: Two areas of thunderstorms, one moving north from Virginia and a second line moving east from the higher terrain of Maryland merged over central Maryland early on the 1st. This enhanced the strength of the thunderstorms, one of which remained severe as it crossed Chesapeake Bay. The western thunderstorms formed ahead of an approaching cold front that moved through the Eastern Shore the middle of that evening.\nEvent Narrative: A lightning strike started a quarter acre wildfire in Stevensville. No property was damaged or injuries occurred.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 22.0823 km away, between 2015-07-01 00:18:00 and 2015-07-01 00:25:00. The events included records with estimated wind gusts of 54.25 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 8000.0 and crop damage of 0.0. \n\nEpisode Narrative: A line of showers and thunderstorms with embedded severe thunderstorms moved through the region ahead of an approaching cold front. Southerly flow ahead of the front resulted in modest instability and shear. A line of showers and thunderstorms with embedded severe thunderstorms moved through the region ahead of an approaching cold front. Southerly flow ahead of the front resulted in modest instability and shear. A line of showers and thunderstorms with embedded severe thunderstorms moved through the region ahead of an approaching cold front. Southerly flow ahead of the front resulted in modest instability and shear. A line of showers and thunderstorms with embedded severe thunderstorms moved through the region ahead of an approaching cold front. Southerly flow ahead of the front resulted in modest instability and shear.\nEvent Narrative: A gas station canopy was toppled over. Reported by WUSA 9 CBS. A tree was reported down at the intersection of Springfield Rd and Good Luck Rd. Several branches 8 inches to 1 foot thick were reported down at the intersection of 5th St and Maple Ave. A tree was reported down on Rocky Point Rd between Barrison Point Rd and Parkview Rd.", "The following events were reported: Flash Flood. These occurred near station USW00093721, approximately 34.6916 km away, between 2015-07-06 19:00:00 and 2015-07-07 00:30:00.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 15000.0 and crop damage of 0.0. \n\nEpisode Narrative: A warm front was oriented west to east across northern Maryland. A warm and moist air mass was south of the boundary and led to an unstable environment. Showers and thunderstorms formed and some storms persisted across the same area in northeast Maryland which led to flash flooding. A warm front was oriented west to east across northern Maryland. A warm and moist air mass was south of the boundary and led to an unstable environment. Showers and thunderstorms formed and some storms persisted across the same area in northeast Maryland which led to flash flooding. A warm front was oriented west to east across northern Maryland. A warm and moist air mass was south of the boundary and led to an unstable environment. Showers and thunderstorms formed and some storms persisted across the same area in northeast Maryland which led to flash flooding.\nEvent Narrative: There was a swift water rescue at Old Joppa Road and Janice Court. There was a car stalled in high water on Carrs Mill Road. Gorman Road flooded and was closed between Foundry Street and Freestate Drive. There was a swift water rescue that included one adult and two children.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 28.3295 km away, between 2015-07-09 18:00:00 and 2015-07-09 18:28:00. The events included records with estimated wind gusts of 52.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 4000.0 and crop damage of 0.0. \n\nEpisode Narrative: A potent trough with accompanying surface cold front swung through the Mid-Atlantic. A favorable atmosphere consisting of SBCAPE values around 2000 j/kg and deep layered shear of around 30 kts allowed for scattered showers and thunderstorms to form, with some becoming severe. A potent trough with accompanying surface cold front swung through the Mid-Atlantic. A favorable atmosphere consisting of SBCAPE values around 2000 j/kg and deep layered shear of around 30 kts allowed for scattered showers and thunderstorms to form, with some becoming severe. A potent trough with accompanying surface cold front swung through the Mid-Atlantic. A favorable atmosphere consisting of SBCAPE values around 2000 j/kg and deep layered shear of around 30 kts allowed for scattered showers and thunderstorms to form, with some becoming severe. A potent trough with accompanying surface cold front swung through the Mid-Atlantic. A favorable atmosphere consisting of SBCAPE values around 2000 j/kg and deep layered shear of around 30 kts allowed for scattered showers and thunderstorms to form, with some becoming severe.\nEvent Narrative: A tree was reported down on wires near the intersection of Lees Lane and Wendlyn Way. A tree was reported down on Haverhill Rd near Joppa Farm Rd. A tree was reported down at the intersection of Defense Hwy and Hermitage Hills Dr. Multiple trees and power lines were reported down near the intersection of St Margarets Rd and Browns Woods Rd.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 31.0344 km away, between 2015-07-09 18:00:00 and 2015-07-09 18:50:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A potent trough with accompanying surface cold front swung through the Mid-Atlantic. A favorable atmosphere consisting of SBCAPE values around 2000 j/kg and deep layered shear of around 30 knots allowed for scattered showers and thunderstorms to form, with some becoming strong. A potent trough with accompanying surface cold front swung through the Mid-Atlantic. A favorable atmosphere consisting of SBCAPE values around 2000 j/kg and deep layered shear of around 30 knots allowed for scattered showers and thunderstorms to form, with some becoming strong. A potent trough with accompanying surface cold front swung through the Mid-Atlantic. A favorable atmosphere consisting of SBCAPE values around 2000 j/kg and deep layered shear of around 30 knots allowed for scattered showers and thunderstorms to form, with some becoming strong. A potent trough with accompanying surface cold front swung through the Mid-Atlantic. A favorable atmosphere consisting of SBCAPE values around 2000 j/kg and deep layered shear of around 30 knots allowed for scattered showers and thunderstorms to form, with some becoming strong. A potent trough with accompanying surface cold front swung through the Mid-Atlantic. A favorable atmosphere consisting of SBCAPE values around 2000 j/kg and deep layered shear of around 30 knots allowed for scattered showers and thunderstorms to form, with some becoming strong. A potent trough with accompanying surface cold front swung through the Mid-Atlantic. A favorable atmosphere consisting of SBCAPE values around 2000 j/kg and deep layered shear of around 30 knots allowed for scattered showers and thunderstorms to form, with some becoming strong. A potent trough with accompanying surface cold front swung through the Mid-Atlantic. A favorable atmosphere consisting of SBCAPE values around 2000 j/kg and deep layered shear of around 30 knots allowed for scattered showers and thunderstorms to form, with some becoming strong.\nEvent Narrative: KNT reported gusts between 33 and 34 knots. GUN reported gusts of 34 knots. FSKM2 reported gusts between 33 and 34 knots. GBY reported gusts between 36 and 43 knots. Annapolis Buoy 44063 reported gusts of 35 knots. TOL reported gusts of 38 knots.", "The following events were reported: Flash Flood, Flood. These occurred near station USW00093721, approximately 36.6719 km away, between 2015-07-14 00:58:00 and 2015-07-14 08:40:00. The flood was caused by Heavy Rain. Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A warm front was in vicinity of the Potomac River overnight. A very moist air mass led to very heavy showers that eventually led to flash flooding in Northeast Maryland. A warm front was in vicinity of the Potomac River overnight. A very moist air mass led to very heavy showers that eventually led to flash flooding in Northeast Maryland. A warm front was in vicinity of the Potomac River overnight. A very moist air mass led to very heavy showers that eventually led to flash flooding in Northeast Maryland. A warm front was in vicinity of the Potomac River overnight. A very moist air mass led to very heavy showers that eventually led to flash flooding in Northeast Maryland.\nEvent Narrative: Road was closed near Cromwell Bridge Road and Oakleigh Road due to high water and debris flow. There were several reports of roads closed due to high water in Bel Air and Pleasant Hills. There were several roads that remained flooded and closed by high water near Fallston including Maryland Route 152. The stream gauge on Whitemarsh Run at White Marsh reached a flood stage of 10 feet. It peaked at 12.66 at 04:00 EST. Town Center Court beings to flood.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 42.0623 km away, between 2015-07-15 01:07:00 and 2015-07-15 01:11:00. The events included records with estimated wind gusts of 52.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 2000.0 and crop damage of 0.0. \n\nEpisode Narrative: Scattered thunderstorms formed along a cold front as it swung through the Mid-Atlantic. Isolated severe cells popped up over Harford County. Scattered thunderstorms formed along a cold front as it swung through the Mid-Atlantic. Isolated severe cells popped up over Harford County.\nEvent Narrative: Multiple wires were reported down on Oakmont Rd. A tree was reported down on Shore Dr at the intersection with Towne Center Dr.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 34.1607 km away, between 2015-07-21 19:21:00 and 2015-07-21 19:28:00. The events included records with estimated wind gusts of 52.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 2000.0 and crop damage of 0.0. \n\nEpisode Narrative: Scattered showers and thunderstorms formed along a cold front. Severe thunderstorms were noted over portions of northeastern Maryland where MUCAPE values ranged between 1000-1500 j/kg and 0-6 km shear was around 30 kts. Scattered showers and thunderstorms formed along a cold front. Severe thunderstorms were noted over portions of northeastern Maryland where MUCAPE values ranged between 1000-1500 j/kg and 0-6 km shear was around 30 kts.\nEvent Narrative: Multiple trees were reported down in the Glen Arm area. Multiple trees were reported down in the Long Green area.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 34.5876 km away, between 2015-07-21 19:53:00 and 2015-07-21 20:12:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Scattered showers and thunderstorms formed along a cold front. Severe thunderstorms were noted over portions of northeastern Maryland where MUCAPE values ranged between 1000-1500 J/Kg and 0-6 km shear was around 30 knots. Scattered showers and thunderstorms formed along a cold front. Severe thunderstorms were noted over portions of northeastern Maryland where MUCAPE values ranged between 1000-1500 J/Kg and 0-6 km shear was around 30 knots.\nEvent Narrative: HRT reported gusts of 37 knots. TCBM2 reported gusts between 31 and 34 knots.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 36.2436 km away, between 2015-07-27 01:15:00 and 2015-07-27 01:30:00. The events included records with estimated wind gusts of 52.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 2000.0 and crop damage of 0.0. \n\nEpisode Narrative: Scattered convection formed in a hot and humid air mass as a resulting of southerly flow from high pressure centered just to the east. Scattered convection formed in a hot and humid air mass as a resulting of southerly flow from high pressure centered just to the east.\nEvent Narrative: Twenty five trees were reported down near the intersection of Falls Rd and Padonia Rd. the trees ranged in size 6 to 8 inches in diameter. Reported by spotter BL133. A tree with a 10 inch diameter was reported down on Stansbury Mill Rd. Reported by spotter BL133.", "The following events were reported: Flash Flood. These occurred near station USW00093721, approximately 31.6663 km away, between 2015-07-29 13:55:00 and 2015-07-29 17:00:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: High pressure was in control while a warm and very moist air mass was in place across the Mid-Atlantic. Showers and thunderstorms formed and heavy rain caused localized flash flooding in Baltimore County, MD.\nEvent Narrative: There was five inches or more of flowing water across Padonia Road at Tullamore Road.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 30.5172 km away, between 2015-07-30 14:10:00 and 2015-07-30 14:10:00. The events included records with estimated wind gusts of 34.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A line of pre-frontal thunderstorms formed in an unstable air mass as a result of SBCAPE values between 1500-2000 J/Kg. Weak shear and lapse rates limited severe development, with isolated storms forming over the DC area.\nEvent Narrative: SPT reported gusts between 31 and 34 knots.", "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00093721, approximately 24.6699 km away, between 2015-08-04 03:44:00 and 2015-08-04 04:08:00. The events included records with hailstones measuring 31.65 inches.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 4000.0 and crop damage of 0.0. \n\nEpisode Narrative: Scattered thunderstorms formed overnight as a weak cold front sunk south of the Mason-Dixon. Theta-e ridge axis aligned over Central MD and south into VA allowed for instability to increase overnight, with storms becoming more numerous with a nearly easterly movement. Scattered thunderstorms formed overnight as a weak cold front sunk south of the Mason-Dixon. Theta-e ridge axis aligned over Central MD and south into VA allowed for instability to increase overnight, with storms becoming more numerous with a nearly easterly movement. Scattered thunderstorms formed overnight as a weak cold front sunk south of the Mason-Dixon. Theta-e ridge axis aligned over Central MD and south into VA allowed for instability to increase overnight, with storms becoming more numerous with a nearly easterly movement. Scattered thunderstorms formed overnight as a weak cold front sunk south of the Mason-Dixon. Theta-e ridge axis aligned over Central MD and south into VA allowed for instability to increase overnight, with storms becoming more numerous with a nearly easterly movement. Scattered thunderstorms formed overnight as a weak cold front sunk south of the Mason-Dixon. Theta-e ridge axis aligned over Central MD and south into VA allowed for instability to increase overnight, with storms becoming more numerous with a nearly easterly movement.\nEvent Narrative: Multiple wires were reported down on the 3800 block of Purdum Dr. Multiple trees were reported down on wires along the 4000 block of Jennings Chapel Rd. A tree was down, blocking the 10200 block of Globe Dr. Reported along Cambria Terrace.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 24.2698 km away, between 2015-08-04 04:20:00 and 2015-08-04 04:50:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Scattered thunderstorms formed overnight as a weak cold front sunk south of the Mason-Dixon. Theta-e ridge axis aligned over Central MD and south into VA allowed for instability to increase overnight. Scattered thunderstorms formed overnight as a weak cold front sunk south of the Mason-Dixon. Theta-e ridge axis aligned over Central MD and south into VA allowed for instability to increase overnight. Scattered thunderstorms formed overnight as a weak cold front sunk south of the Mason-Dixon. Theta-e ridge axis aligned over Central MD and south into VA allowed for instability to increase overnight. Scattered thunderstorms formed overnight as a weak cold front sunk south of the Mason-Dixon. Theta-e ridge axis aligned over Central MD and south into VA allowed for instability to increase overnight.\nEvent Narrative: BLMRE reported gusts between 32 and 34 knots. FSKM2 reported gusts of 35 knots. HRT reported gusts of 36 knots. TCMB2 reported gusts between 32 and 34 knots.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 24.7569 km away, between 2015-08-11 14:12:00 and 2015-08-11 14:51:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Scattered showers and isolated thunderstorms formed as an upper level trough swung through the northeast overnight. An abundance of moisture from persistent southerly flow led to enough instability to result in scattered convection and embedded stronger to severe thunderstorms. Scattered showers and isolated thunderstorms formed as an upper level trough swung through the northeast overnight. An abundance of moisture from persistent southerly flow led to enough instability to result in scattered convection and embedded stronger to severe thunderstorms. Scattered showers and isolated thunderstorms formed as an upper level trough swung through the northeast overnight. An abundance of moisture from persistent southerly flow led to enough instability to result in scattered convection and embedded stronger to severe thunderstorms. Scattered showers and isolated thunderstorms formed as an upper level trough swung through the northeast overnight. An abundance of moisture from persistent southerly flow led to enough instability to result in scattered convection and embedded stronger to severe thunderstorms.\nEvent Narrative: GBY reported gusts between 31 and 34 knots. FSKM2 reported gusts between 31 and 34 knots. KMTN reported gusts of 34 knots. Patapsco Buoy 44043 reported gusts of 39 knots.", "The following events were reported: Flash Flood. These occurred near station USW00093721, approximately 46.9277 km away, between 2015-08-20 17:50:00 and 2015-08-20 19:15:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Strong moisture advection over the Mid-Atlantic led to dew points into the upper 70s and isolated spots reporting 80. Showers and thunderstorms formed ahead of an advancing cold front. Strong moisture advection over the Mid-Atlantic led to dew points into the upper 70s and isolated spots reporting 80. Showers and thunderstorms formed ahead of an advancing cold front.\nEvent Narrative: There was a road closure at Wheel Road and Patterson Mill Road. There was a road closure at Winters Run Road and Singer Road on Winters Run.", "The following events were reported: Flash Flood. These occurred near station USW00093721, approximately 26.8346 km away, between 2015-08-24 16:58:00 and 2015-08-25 22:00:00.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 5000.0 and crop damage of 0.0. \n\nEpisode Narrative: A cold front moved through the Mid-Atlantic, triggering showers and thunderstorms. With ample moisture in place from persistent moisture advection along southerly flow, enough instability was in place to produce scattered stronger thunderstorms. Severe potential was limited by weak shear, with any damage more a result of gusty winds accompanying the heavier precipitation. Flash flooding occurred and many some streams went above flood stage. A cold front moved through the Mid-Atlantic, triggering showers and thunderstorms. With ample moisture in place from persistent moisture advection along southerly flow, enough instability was in place to produce scattered stronger thunderstorms. Severe potential was limited by weak shear, with any damage more a result of gusty winds accompanying the heavier precipitation. Flash flooding occurred and many some streams went above flood stage. A cold front moved through the Mid-Atlantic, triggering showers and thunderstorms. With ample moisture in place from persistent moisture advection along southerly flow, enough instability was in place to produce scattered stronger thunderstorms. Severe potential was limited by weak shear, with any damage more a result of gusty winds accompanying the heavier precipitation. Flash flooding occurred and many some streams went above flood stage. A cold front moved through the Mid-Atlantic, triggering showers and thunderstorms. With ample moisture in place from persistent moisture advection along southerly flow, enough instability was in place to produce scattered stronger thunderstorms. Severe potential was limited by weak shear, with any damage more a result of gusty winds accompanying the heavier precipitation. Flash flooding occurred and many some streams went above flood stage.\nEvent Narrative: The stream gauge on Minebank Run at Glen Arm reached flood stage at 8 feet. The river peaked at 9.01 feet at 1855 LST. Loch Raven Road was closed due to flooding. A car was stalled in high water near Bellona Avenue and Ruxton Road. The stream gauge on White Marsh Run at White Marsh reached flood stage of 10 feet. The gauge peaked at 11 feet at 2045 LST.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 30.5752 km away, between 2015-08-24 17:38:00 and 2015-08-24 18:38:00. The events included records with estimated wind gusts of 46.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 6000.0 and crop damage of 0.0. \n\nEpisode Narrative: A cold front moved through the Mid-Atlantic, triggering showers and thunderstorms. With ample moisture in place from persistent moisture advection along southerly flow, enough instability was in place to produce scattered stronger thunderstorms. Severe potential was limited by weak shear, with any damage more a result of gusty winds accompanying the heavier precipitation. A cold front moved through the Mid-Atlantic, triggering showers and thunderstorms. With ample moisture in place from persistent moisture advection along southerly flow, enough instability was in place to produce scattered stronger thunderstorms. Severe potential was limited by weak shear, with any damage more a result of gusty winds accompanying the heavier precipitation. A cold front moved through the Mid-Atlantic, triggering showers and thunderstorms. With ample moisture in place from persistent moisture advection along southerly flow, enough instability was in place to produce scattered stronger thunderstorms. Severe potential was limited by weak shear, with any damage more a result of gusty winds accompanying the heavier precipitation.\nEvent Narrative: A tree was reported down on a vehicle near Black Rock and Falls Rd. Two trees were reported down, blocking lanes of Towsontown Rd and Lock Raven Rd. A large tree was reported down on Westfield Ave near Eastern Parkway. A medium to large tree was reported down on a fence in the vicinity.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 28.3818 km away, between 2015-08-24 19:51:00 and 2015-08-24 19:51:00. The events included records with estimated wind gusts of 34.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front moved through the Mid-Atlantic, triggering showers and thunderstorms. With ample moisture in place from persistent moisture advection along southerly flow, enough instability was in place to produce scattered stronger thunderstorms. Severe potential was limited by weak shear, with any damage more a result of gusty winds accompanying the heavier precipitation.\nEvent Narrative: HRT reported gusts between 31 and 34 knots.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 47.1467 km away, between 2015-08-24 20:34:00 and 2015-08-24 20:34:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A slow moving cold front and leftover daytime instability triggered an area of strong to severe thunderstorms into the central Delmarva Peninsula during the evening of the 24th where damaging wind gusts, lightning strikes, and power outages were reported.\nEvent Narrative: A severe thunderstorm knocked down a tree onto electrical wires and a pole at 9:34 p.m. EDT, causing power outages for approximately 1,530 customers in the Grasonville and Queenstown areas. Delmarva Power was able to restore service to the affected customers shortly after 11:00 p.m. EDT.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 34.233 km away, between 2015-09-04 15:40:00 and 2015-09-04 15:40:00. The events included records with estimated wind gusts of 34.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Showers and thunderstorms were triggered along a nearly stalled back door cold front. Temperatures pushed well into the 80s, with even some 90s, allowing for MLCAPE values of around 2,000 J/kg.\nEvent Narrative: GUN reported gusts between 32 and 34 knots.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 36.5717 km away, between 2015-09-09 18:40:00 and 2015-09-09 18:41:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Lee trough formed out ahead of an approaching cold front, acting as a surface trigger for scattered convection. Lack of shear led to the storms being pulse-like in nature, based upon increased instability values. Some of the storms became stronger with gusty winds. Lee trough formed out ahead of an approaching cold front, acting as a surface trigger for scattered convection. Lack of shear led to the storms being pulse-like in nature, based upon increased instability values. Some of the storms became stronger with gusty winds.\nEvent Narrative: KNT reported gusts of 34 knots. TOL reported gusts between 33 and 34 knots.", "The following events were reported: Flash Flood, Flood. These occurred near station USW00093721, approximately 26.9339 km away, between 2015-09-10 13:47:00 and 2015-09-10 17:15:00. The flood was caused by Heavy Rain. Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 2000.0 and crop damage of 0.0. \n\nEpisode Narrative: An upper level disturbance moved across the Mid-Atlantic. Showers formed in a very moist atmosphere that led to heavy rainfall mainly across the Interstate 95 corridor. Flooding was reported in Baltimore and Anne Arundel Counties including the City of Annapolis. An upper level disturbance moved across the Mid-Atlantic. Showers formed in a very moist atmosphere that led to heavy rainfall mainly across the Interstate 95 corridor. Flooding was reported in Baltimore and Anne Arundel Counties including the City of Annapolis.\nEvent Narrative: The stream gauge on Minebank Rune at Glen Arm exceeded a flood stage of 8 feet. It peaked at 8.12 feet at 13:50 EST. Water covered the backyard of Elk Farm House/Talmar Horticultural Therapy Center and the access road to Talmar. Over three inches of rain fell across the city of Annapolis. Multiple reports of flooding were reported in the city of Annapolis including, King George Street was closed at the College Creek Bridge, Taylor Avenue was closed near Herbert Sachs Boulevard, Hudson Street was closed at West Street. Flooding was also reported at Ridgely Avenue near Melvin Avenue, on Dock Street and on Compromise Street. Flood waters also poured into the bottom floor of Rickover Hall at the U.S. Naval Academy.", "The following events were reported: Thunderstorm Wind, Tornado. These occurred near station USW00093721, approximately 25.9276 km away, between 2015-09-29 21:02:00 and 2015-09-29 23:13:00.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 3000.0 and crop damage of 0.0. \n\nEpisode Narrative: Heavy rain event as low pressure moved through the Mid-Atlantic ahead of a slow moving cold front. Southerly flow ahead of the low pressure tapped into a moisture rich atmosphere over the Gulf of Mexico. While thunderstorms were isolated due to weaker shear and instability, the heaviest of the precipitation was able to bring down gusty winds from aloft. Heavy rain event as low pressure moved through the Mid-Atlantic ahead of a slow moving cold front. Southerly flow ahead of the low pressure tapped into a moisture rich atmosphere over the Gulf of Mexico. While thunderstorms were isolated due to weaker shear and instability, the heaviest of the precipitation was able to bring down gusty winds from aloft. Heavy rain event as low pressure moved through the Mid-Atlantic ahead of a slow moving cold front. Southerly flow ahead of the low pressure tapped into a moisture rich atmosphere over the Gulf of Mexico. While thunderstorms were isolated due to weaker shear and instability, the heaviest of the precipitation was able to bring down gusty winds from aloft. Heavy rain event as low pressure moved through the Mid-Atlantic ahead of a slow moving cold front. Southerly flow ahead of the low pressure tapped into a moisture rich atmosphere over the Gulf of Mexico. While thunderstorms were isolated due to weaker shear and instability, the heaviest of the precipitation was able to bring down gusty winds from aloft.\nEvent Narrative: Five large pine trees were reported down. Multiple large trees were reported down throughout the county. The National Weather Service in Baltimore MD/Washington DC has confirmed a tornado near Laurel and Scaggsville in Prince Georges and Howard counties in Maryland on September 29 2015.||The National Weather Service in Baltimore MD/Washington DC has confirmed a tornado rated EF0 produced scattered damage along a path extending from Laurel, MD in northern Prince Georges County to just east of Scaggsville in southern Howard County.||Based on information obtained from a ground survey conducted by a member of the National Weather Service of storm damage in southern Howard County and a detailed damage report from the Director of Public Works for the City of Laurel, it was determined that an EF0 tornado produced intermittent damage along a 4 mile path extending from just southeast of Laurel, MD to a point about 1 mile east of Scaggsville, MD.||The tornado first produced damage shortly after 10pm Tuesday evening in Laurel, MD. It damaged the facade of a commercial building near the intersection of Fort Meade Rd and Maryland Route 197. It then moved northwest and into downtown Laurel causing multiple tree damage, along with damage to several roofs. A portion of one home had a small part of its roof peeled back and several commercial buildings lost roof material. Damage in Laurel was limited to a several block area bounded by North Second Street, Fetty Alley, Avondale St and the Little Patuxent River. The tornado then crossed the Little Patuxent River into Howard County.||Based upon this ground survey along with analysis of available NWS and FAA radar data and interviews with persons along the path, the NWS in Sterling confirms an EF0 tornado occurred. The National Weather Service in Baltimore MD/Washington DC has confirmed a tornado near Laurel and Scaggsville in Prince Georges and Howard counties in Maryland on September 29 2015.||The National Weather Service in Baltimore MD/Washington DC has confirmed a tornado rated EF0 produced scattered damage along a path extending from Laurel, MD in northern Prince Georges County to just east of Scaggsville in southern Howard County.||Based on information obtained from a ground survey conducted by a member of the National Weather Service of storm damage in southern Howard County and a detailed damage report from the Director of Public Works for the City of Laurel, it was determined that an EF0 tornado produced intermittent damage along a 4 mile path extending from just southeast of Laurel, MD to a point about 1 mile east of Scaggsville, MD.||After crossing the Little Patuxent River into Howard County, the tornado produced little damage and may have lifted briefly as it moved parallel to Route 216. Then after crossing Interstate 95, the tornado produced tree damage along a narrow path that started near the entrance of the High Ridge Substation and then downed several trees as it crossed into a subdivision west of Leishear Road just east of Hammond Middle School. The tornado lifted near Graeloch Rd and Helmart Rd after producing minor tree damage.||Based upon this ground survey along with analysis of available NWS and FAA radar data and interviews with persons along the path, the NWS in Sterling confirms an EF0 tornado occurred.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 28.8343 km away, between 2015-09-29 21:11:00 and 2015-09-29 23:00:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Heavy rain event as low pressure moved through the Mid-Atlantic ahead of a slow moving cold front. Southerly flow ahead of the low pressure tapped into a moisture rich atmosphere over the Gulf of Mexico. While thunderstorms were isolated due to weaker shear and instability, the heaviest of the precipitation was able to bring down gusty winds from aloft. Heavy rain event as low pressure moved through the Mid-Atlantic ahead of a slow moving cold front. Southerly flow ahead of the low pressure tapped into a moisture rich atmosphere over the Gulf of Mexico. While thunderstorms were isolated due to weaker shear and instability, the heaviest of the precipitation was able to bring down gusty winds from aloft. Heavy rain event as low pressure moved through the Mid-Atlantic ahead of a slow moving cold front. Southerly flow ahead of the low pressure tapped into a moisture rich atmosphere over the Gulf of Mexico. While thunderstorms were isolated due to weaker shear and instability, the heaviest of the precipitation was able to bring down gusty winds from aloft. Heavy rain event as low pressure moved through the Mid-Atlantic ahead of a slow moving cold front. Southerly flow ahead of the low pressure tapped into a moisture rich atmosphere over the Gulf of Mexico. While thunderstorms were isolated due to weaker shear and instability, the heaviest of the precipitation was able to bring down gusty winds from aloft. Heavy rain event as low pressure moved through the Mid-Atlantic ahead of a slow moving cold front. Southerly flow ahead of the low pressure tapped into a moisture rich atmosphere over the Gulf of Mexico. While thunderstorms were isolated due to weaker shear and instability, the heaviest of the precipitation was able to bring down gusty winds from aloft. Heavy rain event as low pressure moved through the Mid-Atlantic ahead of a slow moving cold front. Southerly flow ahead of the low pressure tapped into a moisture rich atmosphere over the Gulf of Mexico. While thunderstorms were isolated due to weaker shear and instability, the heaviest of the precipitation was able to bring down gusty winds from aloft. Heavy rain event as low pressure moved through the Mid-Atlantic ahead of a slow moving cold front. Southerly flow ahead of the low pressure tapped into a moisture rich atmosphere over the Gulf of Mexico. While thunderstorms were isolated due to weaker shear and instability, the heaviest of the precipitation was able to bring down gusty winds from aloft. Heavy rain event as low pressure moved through the Mid-Atlantic ahead of a slow moving cold front. Southerly flow ahead of the low pressure tapped into a moisture rich atmosphere over the Gulf of Mexico. While thunderstorms were isolated due to weaker shear and instability, the heaviest of the precipitation was able to bring down gusty winds from aloft. Heavy rain event as low pressure moved through the Mid-Atlantic ahead of a slow moving cold front. Southerly flow ahead of the low pressure tapped into a moisture rich atmosphere over the Gulf of Mexico. While thunderstorms were isolated due to weaker shear and instability, the heaviest of the precipitation was able to bring down gusty winds from aloft.\nEvent Narrative: Pataspco Buoy 44043 reported gusts between 31 and 34 knots. HRT reported gusts of 34 knots. GUN reported gusts between 31 and 34 knots. TOL reported gusts between 31 and 35 knots. SPT reported gusts of 35 knots. GBY reported gusts between 31 and 41 knots. GBY reported gusts between 31 and 35 knots. TOL reported gusts between 33 and 35 knots. FSKM2 reported gusts between 31 and 34 knots.", "The following events were reported: Flash Flood, Flood. These occurred near station USW00093721, approximately 37.1663 km away, between 2015-09-30 00:09:00 and 2015-09-30 10:02:00. The flood was caused by Heavy Rain. Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Heavy rain event as low pressure moved through the Mid-Atlantic ahead of a slow moving cold front. Southerly flow ahead of the low pressure tapped into a moisture rich atmosphere over the Gulf of Mexico. While thunderstorms were isolated due to weaker shear and instability, the heaviest of the precipitation was able to bring down gusty winds from aloft. This also led to flooding across the region. Heavy rain event as low pressure moved through the Mid-Atlantic ahead of a slow moving cold front. Southerly flow ahead of the low pressure tapped into a moisture rich atmosphere over the Gulf of Mexico. While thunderstorms were isolated due to weaker shear and instability, the heaviest of the precipitation was able to bring down gusty winds from aloft. This also led to flooding across the region. Heavy rain event as low pressure moved through the Mid-Atlantic ahead of a slow moving cold front. Southerly flow ahead of the low pressure tapped into a moisture rich atmosphere over the Gulf of Mexico. While thunderstorms were isolated due to weaker shear and instability, the heaviest of the precipitation was able to bring down gusty winds from aloft. This also led to flooding across the region.\nEvent Narrative: The stream gauge on Western Run at Western Run reached flood stage of 8 feet. It peaked at 9.18 feet at 04:45 EST. Pastureland near the gauge began to flood and water began to cover Western Run Road. The stream gauge on Beaverdam Run at Cockeysville reached a flood stage of 9 feet. It peaked at 9.11 feet at 0155 EST. Beaver Run Lane began to flood and water surrounded nearby buildings. The stream gauge on Piney Run at Dover reached a flood stage of 8.5 feet. It peaked at 8.60 feet at 0115 EST. Agricultural fields began to flood.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 26.2199 km away, between 2015-10-09 15:54:00 and 2015-10-09 17:01:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front moved through the region during the afternoon. Deep layer shear values around 40 knots with ML Cape values of around 500 J/kg generated scattered showers with embedded stronger storms. A cold front moved through the region during the afternoon. Deep layer shear values around 40 knots with ML Cape values of around 500 J/kg generated scattered showers with embedded stronger storms. A cold front moved through the region during the afternoon. Deep layer shear values around 40 knots with ML Cape values of around 500 J/kg generated scattered showers with embedded stronger storms. A cold front moved through the region during the afternoon. Deep layer shear values around 40 knots with ML Cape values of around 500 J/kg generated scattered showers with embedded stronger storms. A cold front moved through the region during the afternoon. Deep layer shear values around 40 knots with ML Cape values of around 500 J/kg generated scattered showers with embedded stronger storms.\nEvent Narrative: KMTN reported gusts between 33 and 34 knots. HRT reported gusts between 32 and 34 knots. FSKM2 reported gusts of 35 knots. Patapsco Buoy 44043 reported gusts between 31 and 34 knots. TOL reported gusts between 31 and 34 knots.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 19.9621 km away, between 2015-10-18 12:40:00 and 2015-10-18 14:36:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Shortwave rounding the base of an upper level trough extended over the eastern US triggered scattered showers, with embedded strong storms. Shortwave rounding the base of an upper level trough extended over the eastern US triggered scattered showers, with embedded strong storms.\nEvent Narrative: Patapsco Buoy 44043 reported gusts between 31 and 35 knots. FSKM2 reported gusts between 32 and 34 knots.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 47.8469 km away, between 2015-10-28 20:02:00 and 2015-10-28 20:02:00. The events included records with estimated wind gusts of 52.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 1000.0 and crop damage of 0.0. \n\nEpisode Narrative: A warm front lifted north through the Mid-Atlantic while a trough swung through aloft. Convergence at the surface near the frontal boundary combining with record high P-Wat values and decent shear led to the formation of strong to isolated severe thunderstorms.\nEvent Narrative: Numerous branches at least 4 inches in diameter were reported down.", "The following events were reported: Flash Flood. These occurred near station USW00093721, approximately 24.396 km away, between 2015-12-23 18:53:00 and 2015-12-23 20:00:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A warm front moved through the Mid-Atlantic region. Well above normal temperatures occurred across the region while moisture streamed in from the south. Heavy rain led to localized flash flooding in Northeast Maryland. A warm front moved through the Mid-Atlantic region. Well above normal temperatures occurred across the region while moisture streamed in from the south. Heavy rain led to localized flash flooding in Northeast Maryland.\nEvent Narrative: A swift water rescue took place at North Point Boulevard and Kane Avenue. The river gauge at White Marsh on Whitemarsh Run reached a flood stage of 10 feet. It peaked at 11.21 feet at 19:30 EST. Water began to cover parking lots near the stream, particularly near Town Center Court.", "The following events were reported: Flash Flood. These occurred near station USW00093721, approximately 29.6156 km away, between 2015-12-25 17:57:00 and 2015-12-25 19:50:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A warm front moved through the Mid-Atlantic region and showers and thunderstorms led to very heavy rain capable of flooding across Central Maryland.\nEvent Narrative: The river gauge at Whitemarsh on Whitemarsh Run reached flood stage of 10 feet. It peaked at 11.38 feet at 18:45 EST. Water began to cover parking lots near the stream, particularly near Town Center Court.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 24.9969 km away, between 2017-02-12 22:31:00 and 2017-02-12 23:30:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A strong cold front passed through during the evening hours of the 13th. A line of showers developed along the front and they were able to mix down strong winds from aloft. A strong cold front passed through during the evening hours of the 13th. A line of showers developed along the front and they were able to mix down strong winds from aloft. A strong cold front passed through during the evening hours of the 13th. A line of showers developed along the front and they were able to mix down strong winds from aloft. A strong cold front passed through during the evening hours of the 13th. A line of showers developed along the front and they were able to mix down strong winds from aloft. A strong cold front passed through during the evening hours of the 13th. A line of showers developed along the front and they were able to mix down strong winds from aloft. A strong cold front passed through during the evening hours of the 13th. A line of showers developed along the front and they were able to mix down strong winds from aloft. A strong cold front passed through during the evening hours of the 13th. A line of showers developed along the front and they were able to mix down strong winds from aloft. A strong cold front passed through during the evening hours of the 13th. A line of showers developed along the front and they were able to mix down strong winds from aloft. A strong cold front passed through during the evening hours of the 13th. A line of showers developed along the front and they were able to mix down strong winds from aloft. A strong cold front passed through during the evening hours of the 13th. A line of showers developed along the front and they were able to mix down strong winds from aloft. A strong cold front passed through during the evening hours of the 13th. A line of showers developed along the front and they were able to mix down strong winds from aloft. A strong cold front passed through during the evening hours of the 13th. A line of showers developed along the front and they were able to mix down strong winds from aloft.\nEvent Narrative: There were several reports of trees down in the Browns Bridge Road area. There were several reports of trees down in the Towson area. A tree fell onto a police car near Oella. Two trees were down in Fallston. A tree fell onto power lines on Cape May Road. Multiple trees were down near Fort Meade. Trees were down blocking one lane along Maryland Route 175 at Disney Road. Multiple trees were down along the 3500 Block of Loch Haven Drive. A tree was down on Maryland Route 43 at Interstate 95. A wind gust of 59 mph was reported. Trees were down near Mount Airy. Several reports of trees were down on the Cockeysville area.", "The following events were reported: Hail. These occurred near station USW00093721, approximately 30.8454 km away, between 2017-02-25 14:57:00 and 2017-02-25 15:30:00. The events included records with hailstones measuring 1.05 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A potent cold front passed through the area on the 25th. Southerly winds ahead of the boundary ushered in unusually warm and humid conditions for this time of year which led to some instability. Showers and thunderstorms developed, and this convection was able to pull down strong winds from aloft and also produce hail. A potent cold front passed through the area on the 25th. Southerly winds ahead of the boundary ushered in unusually warm and humid conditions for this time of year which led to some instability. Showers and thunderstorms developed, and this convection was able to pull down strong winds from aloft and also produce hail. A potent cold front passed through the area on the 25th. Southerly winds ahead of the boundary ushered in unusually warm and humid conditions for this time of year which led to some instability. Showers and thunderstorms developed, and this convection was able to pull down strong winds from aloft and also produce hail. A potent cold front passed through the area on the 25th. Southerly winds ahead of the boundary ushered in unusually warm and humid conditions for this time of year which led to some instability. Showers and thunderstorms developed, and this convection was able to pull down strong winds from aloft and also produce hail. A potent cold front passed through the area on the 25th. Southerly winds ahead of the boundary ushered in unusually warm and humid conditions for this time of year which led to some instability. Showers and thunderstorms developed, and this convection was able to pull down strong winds from aloft and also produce hail.\nEvent Narrative: Quarter sized hail was reported near Rossville. Half dollar sized hail was reported at the White Marsh Mall. Quarter sized hail was reported near Reese. Quarter sized hail was located near Fullerton. Quarter sized hail was reported at the intersection of Route 43 and Walter Boulevard.", "The following events were reported: Marine Hail, Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 25.5046 km away, between 2017-02-25 15:18:00 and 2017-02-25 16:06:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A potent cold front passed through the waters on the 25th. Southerly winds ahead of the boundary ushered in unusually warm and humid conditions for this time of year which led to some instability. A line of showers and thunderstorms developed, and this convection was able to pull down strong winds from aloft. A potent cold front passed through the waters on the 25th. Southerly winds ahead of the boundary ushered in unusually warm and humid conditions for this time of year which led to some instability. A line of showers and thunderstorms developed, and this convection was able to pull down strong winds from aloft. A potent cold front passed through the waters on the 25th. Southerly winds ahead of the boundary ushered in unusually warm and humid conditions for this time of year which led to some instability. A line of showers and thunderstorms developed, and this convection was able to pull down strong winds from aloft. A potent cold front passed through the waters on the 25th. Southerly winds ahead of the boundary ushered in unusually warm and humid conditions for this time of year which led to some instability. A line of showers and thunderstorms developed, and this convection was able to pull down strong winds from aloft. A potent cold front passed through the waters on the 25th. Southerly winds ahead of the boundary ushered in unusually warm and humid conditions for this time of year which led to some instability. A line of showers and thunderstorms developed, and this convection was able to pull down strong winds from aloft.\nEvent Narrative: Penny sized hail was reported at Brooklyn Park. Wind gusts in excess of 30 knots were reported Baltimore Key Bridge. A wind gust of 35 knots was reported at Gunpowder. Wind gusts of 34 to 35 knots were reported at Hart Miller Island. Wind gusts of 49 knots were reported at Tolchester Beach.", "The following events were reported: Hail. These occurred near station USW00093721, approximately 38.799 km away, between 2017-02-25 15:50:00 and 2017-02-25 15:50:00. The events included records with hailstones measuring 0.75 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Several days of record warmth was ended with the passage of a cold front. Enough moisture and instability was present ahead of this front to produce a band of showers and thunderstorms. Some of the storms did cause wind damage and had hail.\nEvent Narrative: Penny size hail was measured with a thunderstorm behind the main line.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 25.4077 km away, between 2017-03-01 13:28:00 and 2017-03-01 14:12:00.The events resulted in 1 injuries and 0 fatalities. No significant property or crop damage was reported. \n\nEpisode Narrative: A potent cold front passed through on the 1st. A southwest flow ushered in warm and moist air ahead of the boundary. Showers and a few thunderstorms developed, and they were able to mix down strong winds from aloft. A potent cold front passed through on the 1st. A southwest flow ushered in warm and moist air ahead of the boundary. Showers and a few thunderstorms developed, and they were able to mix down strong winds from aloft. A potent cold front passed through on the 1st. A southwest flow ushered in warm and moist air ahead of the boundary. Showers and a few thunderstorms developed, and they were able to mix down strong winds from aloft. A potent cold front passed through on the 1st. A southwest flow ushered in warm and moist air ahead of the boundary. Showers and a few thunderstorms developed, and they were able to mix down strong winds from aloft. A potent cold front passed through on the 1st. A southwest flow ushered in warm and moist air ahead of the boundary. Showers and a few thunderstorms developed, and they were able to mix down strong winds from aloft. A potent cold front passed through on the 1st. A southwest flow ushered in warm and moist air ahead of the boundary. Showers and a few thunderstorms developed, and they were able to mix down strong winds from aloft. A potent cold front passed through on the 1st. A southwest flow ushered in warm and moist air ahead of the boundary. Showers and a few thunderstorms developed, and they were able to mix down strong winds from aloft. A potent cold front passed through on the 1st. A southwest flow ushered in warm and moist air ahead of the boundary. Showers and a few thunderstorms developed, and they were able to mix down strong winds from aloft. A potent cold front passed through on the 1st. A southwest flow ushered in warm and moist air ahead of the boundary. Showers and a few thunderstorms developed, and they were able to mix down strong winds from aloft. A potent cold front passed through on the 1st. A southwest flow ushered in warm and moist air ahead of the boundary. Showers and a few thunderstorms developed, and they were able to mix down strong winds from aloft. A potent cold front passed through on the 1st. A southwest flow ushered in warm and moist air ahead of the boundary. Showers and a few thunderstorms developed, and they were able to mix down strong winds from aloft. A potent cold front passed through on the 1st. A southwest flow ushered in warm and moist air ahead of the boundary. Showers and a few thunderstorms developed, and they were able to mix down strong winds from aloft. A potent cold front passed through on the 1st. A southwest flow ushered in warm and moist air ahead of the boundary. Showers and a few thunderstorms developed, and they were able to mix down strong winds from aloft. A potent cold front passed through on the 1st. A southwest flow ushered in warm and moist air ahead of the boundary. Showers and a few thunderstorms developed, and they were able to mix down strong winds from aloft. A potent cold front passed through on the 1st. A southwest flow ushered in warm and moist air ahead of the boundary. Showers and a few thunderstorms developed, and they were able to mix down strong winds from aloft. A potent cold front passed through on the 1st. A southwest flow ushered in warm and moist air ahead of the boundary. Showers and a few thunderstorms developed, and they were able to mix down strong winds from aloft. A potent cold front passed through on the 1st. A southwest flow ushered in warm and moist air ahead of the boundary. Showers and a few thunderstorms developed, and they were able to mix down strong winds from aloft. A potent cold front passed through on the 1st. A southwest flow ushered in warm and moist air ahead of the boundary. Showers and a few thunderstorms developed, and they were able to mix down strong winds from aloft. A potent cold front passed through on the 1st. A southwest flow ushered in warm and moist air ahead of the boundary. Showers and a few thunderstorms developed, and they were able to mix down strong winds from aloft. A potent cold front passed through on the 1st. A southwest flow ushered in warm and moist air ahead of the boundary. Showers and a few thunderstorms developed, and they were able to mix down strong winds from aloft. A potent cold front passed through on the 1st. A southwest flow ushered in warm and moist air ahead of the boundary. Showers and a few thunderstorms developed, and they were able to mix down strong winds from aloft. A potent cold front passed through on the 1st. A southwest flow ushered in warm and moist air ahead of the boundary. Showers and a few thunderstorms developed, and they were able to mix down strong winds from aloft.\nEvent Narrative: Several trees were down on Benfield Road. Several large horse trailers were blown over and several Outbuildings were damaged. Numerous trees were down as well. Wires were down closing the road at Route 108 and Sundown. Trees were down in Columbia. Wires were down in Catonsville. Trees were down in Elkridge. Wires were down in Towson. Wires were down in Dundalk. A wind gust of 58 mph was reported in Bowie. A tree was down blocking Hawkins Creamery Road. Annapolis Rock Road was blocked due to a downed tree. Trees were down in Glenelg. Trees were down in West Friendship. Trees were down in Lisbon. Trees and wires were down in Sykesville. A large tree was down on Reisterstown Road near Mcdonogh Road. A tree was down on Interstate 83 near the northern Parkway. Numerous roof shingles and siding were torn off at least four buildings in the Southfield Apartment Complex. A tree was down on Old Harford Road. Shingles and siding was blown off a house. Trees and wires were down in Woodlawn. Part of a roof was blown off and a window was blown out of a Social Security Building. According to the media, one person was taken to the hospital.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 25.6291 km away, between 2017-03-01 14:06:00 and 2017-03-01 14:20:00. The events included records with measured wind gusts of 53.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A potent cold front passed through on the 1st. A southwest flow ushered in warm and moist air ahead of the boundary. Showers and a few thunderstorms developed, and they were able to mix down strong winds from aloft. A potent cold front passed through on the 1st. A southwest flow ushered in warm and moist air ahead of the boundary. Showers and a few thunderstorms developed, and they were able to mix down strong winds from aloft.\nEvent Narrative: A wind gust of 50 knots was reported at Key Bridge. A wind gust of 56 knots was reported at Thomas Point Lighthouse.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 25.6291 km away, between 2017-03-01 14:06:00 and 2017-03-01 14:20:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A potent cold front passed through the waters. Showers were able to mix down strong winds from aloft. A potent cold front passed through the waters. Showers were able to mix down strong winds from aloft.\nEvent Narrative: A wind gust of 50 knots was reported at the Baltimore Key Bridge. A wind gust of 56 knots was reported at Thomas Point Lighthouse.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 27.5576 km away, between 2017-03-08 03:40:00 and 2017-03-08 04:30:00. The events included records with measured wind gusts of 39.9 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A strong cold front passed through the waters on the eighth of March. Showers were able to mix down strong winds from aloft. A strong cold front passed through the waters on the eighth of March. Showers were able to mix down strong winds from aloft. A strong cold front passed through the waters on the eighth of March. Showers were able to mix down strong winds from aloft. A strong cold front passed through the waters on the eighth of March. Showers were able to mix down strong winds from aloft. A strong cold front passed through the waters on the eighth of March. Showers were able to mix down strong winds from aloft. A strong cold front passed through the waters on the eighth of March. Showers were able to mix down strong winds from aloft. A strong cold front passed through the waters on the eighth of March. Showers were able to mix down strong winds from aloft. A strong cold front passed through the waters on the eighth of March. Showers were able to mix down strong winds from aloft. A strong cold front passed through the waters on the eighth of March. Showers were able to mix down strong winds from aloft. A strong cold front passed through the waters on the eighth of March. Showers were able to mix down strong winds from aloft.\nEvent Narrative: Wind gusts up to 34 knots were reported at Tolchester. Wind gusts up to 34 knots were reported at Lakeland Elementary School. Wind gusts up to 42 knots were reported. Wind gusts up to 42 knots were reported at the Baltimore Key Bridge. Wind gusts up to 35 knots were reported at Martin State. Wind gusts up to 38 knots were reported at Gunpowder. Wind gusts of 35 to 50 knots were reported at Greenberry Point. Wind gusts of 38 to 42 knots were reported at Tolly Point. A wind gust of 41 knots was reported at Annapolis. A wind gust of 41 knots was reported at Thomas Point Lighthouse.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 26.8821 km away, between 2017-03-08 03:40:00 and 2017-03-08 04:30:00. The events included records with measured wind gusts of 39.9 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A potent cold front moved through the area during the early morning hours of the 8th. A line of showers developed along the front, and these were able to mix down gusty winds from aloft. A potent cold front moved through the area during the early morning hours of the 8th. A line of showers developed along the front, and these were able to mix down gusty winds from aloft. A potent cold front moved through the area during the early morning hours of the 8th. A line of showers developed along the front, and these were able to mix down gusty winds from aloft. A potent cold front moved through the area during the early morning hours of the 8th. A line of showers developed along the front, and these were able to mix down gusty winds from aloft. A potent cold front moved through the area during the early morning hours of the 8th. A line of showers developed along the front, and these were able to mix down gusty winds from aloft. A potent cold front moved through the area during the early morning hours of the 8th. A line of showers developed along the front, and these were able to mix down gusty winds from aloft. A potent cold front moved through the area during the early morning hours of the 8th. A line of showers developed along the front, and these were able to mix down gusty winds from aloft. A potent cold front moved through the area during the early morning hours of the 8th. A line of showers developed along the front, and these were able to mix down gusty winds from aloft. A potent cold front moved through the area during the early morning hours of the 8th. A line of showers developed along the front, and these were able to mix down gusty winds from aloft. A potent cold front moved through the area during the early morning hours of the 8th. A line of showers developed along the front, and these were able to mix down gusty winds from aloft.\nEvent Narrative: Wind gusts up to 34 knots were reported. Wind gusts of 35 to 42 knots were reported. Wind gusts of 41 to 42 knots were reported at Key Bridge. Wind gusts of 34 to 35 knots were reported at Martin State. Wind gusts of 35 to 38 knots were reported Gunpowder. Wind gusts up to 34 knots were reported at Tolchester. Wind gusts of 35 to 50 knots were reported at Greenbury Point. Wind gusts of 38 to 42 knots were reported at Tolly Point. A wind gust of 41 knots was reported at Annapolis. A wind gust of 41 knots was reported at Thomas Point Lighthouse.", "The following events were reported: Heavy Rain. These occurred near station USW00093721, approximately 38.799 km away, between 2017-03-14 11:54:00 and 2017-03-14 11:54:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Low pressure systems across the Ohio Valley and Carolinas phased. This led to a rapidly developing storm which tracked just offshore. Wind, coastal flooding, heavy rain and snow all occurred.\nEvent Narrative: Heavy rainfall from the nor'easter. 2.7 inches.", "The following events were reported: Flood. These occurred near station USW00093721, approximately 29.1189 km away, between 2017-04-06 12:42:00 and 2017-04-06 20:02:00. The flood was caused by Heavy Rain. Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 5000.0 and crop damage of 0.0. \n\nEpisode Narrative: Cutoff low pressure was over the Ohio Valley. Another area of low pressure strengthened overhead on the occluded boundary. Warm and moist air from the south lead to an unstable atmosphere. Showers and thunderstorms led to heavy rain at times and led to a river gauge reaching flood stage in northeast MD. Cutoff low pressure was over the Ohio Valley. Another area of low pressure strengthened overhead on the occluded boundary. Warm and moist air from the south lead to an unstable atmosphere. Showers and thunderstorms led to heavy rain at times and led to a river gauge reaching flood stage in northeast MD.\nEvent Narrative: There was a car stranded in high water on Brock Bridge Road. The stream gauge at Glencoe at Gundpowder Falls reached flood stage of 7 feet. The river level peaked at 9.17 feet at 17:30 EST. Sparks Road began to flood as well as portions of Upper Glencoe Road and Lower Glencoe Road.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 25.5662 km away, between 2017-04-06 13:00:00 and 2017-04-06 13:51:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Cutoff low pressure was over the Ohio Valley. Another area of low pressure strengthened overhead on the occluded boundary. Warm and moist air from the south lead to an unstable atmosphere. Strong shear profiles were in place due to the cutoff low to the west. Strong lift associated with the developing low combined with strong shear and enough instability to produce severe thunderstorms. Cutoff low pressure was over the Ohio Valley. Another area of low pressure strengthened overhead on the occluded boundary. Warm and moist air from the south lead to an unstable atmosphere. Strong shear profiles were in place due to the cutoff low to the west. Strong lift associated with the developing low combined with strong shear and enough instability to produce severe thunderstorms. Cutoff low pressure was over the Ohio Valley. Another area of low pressure strengthened overhead on the occluded boundary. Warm and moist air from the south lead to an unstable atmosphere. Strong shear profiles were in place due to the cutoff low to the west. Strong lift associated with the developing low combined with strong shear and enough instability to produce severe thunderstorms. Cutoff low pressure was over the Ohio Valley. Another area of low pressure strengthened overhead on the occluded boundary. Warm and moist air from the south lead to an unstable atmosphere. Strong shear profiles were in place due to the cutoff low to the west. Strong lift associated with the developing low combined with strong shear and enough instability to produce severe thunderstorms. Cutoff low pressure was over the Ohio Valley. Another area of low pressure strengthened overhead on the occluded boundary. Warm and moist air from the south lead to an unstable atmosphere. Strong shear profiles were in place due to the cutoff low to the west. Strong lift associated with the developing low combined with strong shear and enough instability to produce severe thunderstorms. Cutoff low pressure was over the Ohio Valley. Another area of low pressure strengthened overhead on the occluded boundary. Warm and moist air from the south lead to an unstable atmosphere. Strong shear profiles were in place due to the cutoff low to the west. Strong lift associated with the developing low combined with strong shear and enough instability to produce severe thunderstorms. Cutoff low pressure was over the Ohio Valley. Another area of low pressure strengthened overhead on the occluded boundary. Warm and moist air from the south lead to an unstable atmosphere. Strong shear profiles were in place due to the cutoff low to the west. Strong lift associated with the developing low combined with strong shear and enough instability to produce severe thunderstorms. Cutoff low pressure was over the Ohio Valley. Another area of low pressure strengthened overhead on the occluded boundary. Warm and moist air from the south lead to an unstable atmosphere. Strong shear profiles were in place due to the cutoff low to the west. Strong lift associated with the developing low combined with strong shear and enough instability to produce severe thunderstorms. Cutoff low pressure was over the Ohio Valley. Another area of low pressure strengthened overhead on the occluded boundary. Warm and moist air from the south lead to an unstable atmosphere. Strong shear profiles were in place due to the cutoff low to the west. Strong lift associated with the developing low combined with strong shear and enough instability to produce severe thunderstorms.\nEvent Narrative: Five large trees were down in the neighborhood off of Moylan Drive. Trees were down on power lines as well as houses and cars in the area of Milan Way. A roof was blown off an apartment building. Trees were down along Route 24 between 7 and Edgewood Road. Wind gusts of 59 mph were reported near Bowie. A wind gust of 58 mph was reported at the Baltimore Washington International Airport. A wind gust of 66 mph reported near White Marsh. A wind gust of 64 mph was reported along the Aberdeen Proving Ground. Trees were down near Bowie.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 32.9038 km away, between 2017-04-06 13:14:00 and 2017-04-06 13:55:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Cutoff low pressure was over the Ohio Valley. Another area of low pressure strengthened overhead on the occluded boundary. Warm and moist air from the south lead to an unstable atmosphere. Strong shear profiles were in place due to the cutoff low to the west. Strong lift associated with the developing low combined with strong shear and enough instability to produce severe thunderstorms. Cutoff low pressure was over the Ohio Valley. Another area of low pressure strengthened overhead on the occluded boundary. Warm and moist air from the south lead to an unstable atmosphere. Strong shear profiles were in place due to the cutoff low to the west. Strong lift associated with the developing low combined with strong shear and enough instability to produce severe thunderstorms. Cutoff low pressure was over the Ohio Valley. Another area of low pressure strengthened overhead on the occluded boundary. Warm and moist air from the south lead to an unstable atmosphere. Strong shear profiles were in place due to the cutoff low to the west. Strong lift associated with the developing low combined with strong shear and enough instability to produce severe thunderstorms. Cutoff low pressure was over the Ohio Valley. Another area of low pressure strengthened overhead on the occluded boundary. Warm and moist air from the south lead to an unstable atmosphere. Strong shear profiles were in place due to the cutoff low to the west. Strong lift associated with the developing low combined with strong shear and enough instability to produce severe thunderstorms. Cutoff low pressure was over the Ohio Valley. Another area of low pressure strengthened overhead on the occluded boundary. Warm and moist air from the south lead to an unstable atmosphere. Strong shear profiles were in place due to the cutoff low to the west. Strong lift associated with the developing low combined with strong shear and enough instability to produce severe thunderstorms. Cutoff low pressure was over the Ohio Valley. Another area of low pressure strengthened overhead on the occluded boundary. Warm and moist air from the south lead to an unstable atmosphere. Strong shear profiles were in place due to the cutoff low to the west. Strong lift associated with the developing low combined with strong shear and enough instability to produce severe thunderstorms. Cutoff low pressure was over the Ohio Valley. Another area of low pressure strengthened overhead on the occluded boundary. Warm and moist air from the south lead to an unstable atmosphere. Strong shear profiles were in place due to the cutoff low to the west. Strong lift associated with the developing low combined with strong shear and enough instability to produce severe thunderstorms. Cutoff low pressure was over the Ohio Valley. Another area of low pressure strengthened overhead on the occluded boundary. Warm and moist air from the south lead to an unstable atmosphere. Strong shear profiles were in place due to the cutoff low to the west. Strong lift associated with the developing low combined with strong shear and enough instability to produce severe thunderstorms. Cutoff low pressure was over the Ohio Valley. Another area of low pressure strengthened overhead on the occluded boundary. Warm and moist air from the south lead to an unstable atmosphere. Strong shear profiles were in place due to the cutoff low to the west. Strong lift associated with the developing low combined with strong shear and enough instability to produce severe thunderstorms. Cutoff low pressure was over the Ohio Valley. Another area of low pressure strengthened overhead on the occluded boundary. Warm and moist air from the south lead to an unstable atmosphere. Strong shear profiles were in place due to the cutoff low to the west. Strong lift associated with the developing low combined with strong shear and enough instability to produce severe thunderstorms. Cutoff low pressure was over the Ohio Valley. Another area of low pressure strengthened overhead on the occluded boundary. Warm and moist air from the south lead to an unstable atmosphere. Strong shear profiles were in place due to the cutoff low to the west. Strong lift associated with the developing low combined with strong shear and enough instability to produce severe thunderstorms. Cutoff low pressure was over the Ohio Valley. Another area of low pressure strengthened overhead on the occluded boundary. Warm and moist air from the south lead to an unstable atmosphere. Strong shear profiles were in place due to the cutoff low to the west. Strong lift associated with the developing low combined with strong shear and enough instability to produce severe thunderstorms. Cutoff low pressure was over the Ohio Valley. Another area of low pressure strengthened overhead on the occluded boundary. Warm and moist air from the south lead to an unstable atmosphere. Strong shear profiles were in place due to the cutoff low to the west. Strong lift associated with the developing low combined with strong shear and enough instability to produce severe thunderstorms.\nEvent Narrative: Wind gusts of 48 to 54 knots were reported at Gunpowder. Wind gusts of 34 to 53 knots were reported at Sandy Point. A wind gust around 50 knots was estimated based on thunderstorm wind damage nearby. A wind gust of 45 knots was reported at the Patapsco Buoy. Wind gusts of 34 to 53 knots were reported at Hartmiller Island. Wind gusts of 38 to 42 knots were reported at Tolchester. A wind gust of 37 knots was reported at Martin State. A wind gust of 56 knots was reported based on thunderstorm wind damage nearby. Wind gusts of 34 to 45 knots were reported. Wind gusts of 36 to 48 knots were reported at Greenberry Point. A wind gust of 48 knots was reported at Thomas Point Lighthouse. A wind gust of 35 knots was reported at Tolly Point. A wind gust of 38 knots was reported at Kent Island.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 44.5638 km away, between 2017-04-06 13:36:00 and 2017-04-06 13:40:00. The events included records with estimated wind gusts of 52.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Low pressure tracked from the Ohio Valley into the Western Great Lakes with a warm front surging northward ahead of the low which was followed by a cold front. Moisture and instability was drawn northwest ahead of the front which led to locally heavy showers and thunderstorms. Some of thunderstorms were strong to severe with gusty winds. Low pressure tracked from the Ohio Valley into the Western Great Lakes with a warm front surging northward ahead of the low which was followed by a cold front. Moisture and instability was drawn northwest ahead of the front which led to locally heavy showers and thunderstorms. Some of thunderstorms were strong to severe with gusty winds.\nEvent Narrative: A tractor trailer was blown over. Wires downed due to thunderstorm winds.", "The following events were reported: Flood. These occurred near station USW00093721, approximately 19.0224 km away, between 2017-05-05 08:22:00 and 2017-05-05 15:00:00. The flood was caused by Heavy Rain. Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Low pressure was located across the Tennessee Valley while a strong low level jet transported moisture into the Mid-Atlantic. Showers and thunderstorms led to heavy rain across northern and central Virginia leading to scattered flooding mainly from rivers and creeks over flowing. Low pressure was located across the Tennessee Valley while a strong low level jet transported moisture into the Mid-Atlantic. Showers and thunderstorms led to heavy rain across northern and central Virginia leading to scattered flooding mainly from rivers and creeks over flowing.\nEvent Narrative: The 11000 Block of Lime Kiln Road was closed due to high water. Brock Bridge Road was closed due to high water near Laurel Bowie Road.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 33.8982 km away, between 2017-05-05 08:23:00 and 2017-05-05 08:40:00. The events included records with measured wind gusts of 40.5 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Low pressure was located across the Tennessee Valley while a strong low level jet transported moisture into the Mid-Atlantic. Showers and thunderstorms developed across the waters. An unstable atmosphere caused a few thunderstorms to produce gusty winds. Low pressure was located across the Tennessee Valley while a strong low level jet transported moisture into the Mid-Atlantic. Showers and thunderstorms developed across the waters. An unstable atmosphere caused a few thunderstorms to produce gusty winds. Low pressure was located across the Tennessee Valley while a strong low level jet transported moisture into the Mid-Atlantic. Showers and thunderstorms developed across the waters. An unstable atmosphere caused a few thunderstorms to produce gusty winds. Low pressure was located across the Tennessee Valley while a strong low level jet transported moisture into the Mid-Atlantic. Showers and thunderstorms developed across the waters. An unstable atmosphere caused a few thunderstorms to produce gusty winds.\nEvent Narrative: A wind gust of 39 knots was reported at Annapolis. A wind gust of 47 knots was reported at Tolly Point. A wind gust of 39 knots was reported. A wind gust of 37 knots was reported at Thomas Point Lighthouse.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 17.6858 km away, between 2017-05-19 18:00:00 and 2017-05-19 21:49:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A warm and humid air mass led to the development of thunderstorms. A few thunderstorms became severe due to stronger winds aloft. A warm and humid air mass led to the development of thunderstorms. A few thunderstorms became severe due to stronger winds aloft. A warm and humid air mass led to the development of thunderstorms. A few thunderstorms became severe due to stronger winds aloft. A warm and humid air mass led to the development of thunderstorms. A few thunderstorms became severe due to stronger winds aloft. A warm and humid air mass led to the development of thunderstorms. A few thunderstorms became severe due to stronger winds aloft. A warm and humid air mass led to the development of thunderstorms. A few thunderstorms became severe due to stronger winds aloft.\nEvent Narrative: A wind gust of 58 mph was reported at Fort Meade. A wind gust of 67 mph was reported. A tree was down near the intersection of Route 450 and Route 3. A tree was down near Rutland Road and St. George Barber Road. Numerous trees were down. Several large branches were down at the Cross Creek Golf Club.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 32.8645 km away, between 2017-05-19 18:33:00 and 2017-05-19 19:10:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A warm and humid air mass led to the development of thunderstorms. Some thunderstorms mixed down gusty winds from aloft. A warm and humid air mass led to the development of thunderstorms. Some thunderstorms mixed down gusty winds from aloft. A warm and humid air mass led to the development of thunderstorms. Some thunderstorms mixed down gusty winds from aloft. A warm and humid air mass led to the development of thunderstorms. Some thunderstorms mixed down gusty winds from aloft.\nEvent Narrative: Wind gusts up to 40 knots were reported at Annapolis. A wind gust in excess of 30 knots was reported at Kent Island. A wind gust in excess of 30 knots was reported at Sandy Point. Wind gusts up to 46 knots were reported at Tolly Point and Thomas Point Lighthouse.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 26.9072 km away, between 2017-05-25 17:26:00 and 2017-05-25 22:10:00. The events included records with measured wind gusts of 38.333333333333336 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Low pressure and an associated cold front moved across the Mid-Atlantic region during the day on May 25th. Warm and humid conditions led to showers and thunderstorms. Some thunderstorms produced gusty winds and large hail. Low pressure and an associated cold front moved across the Mid-Atlantic region during the day on May 25th. Warm and humid conditions led to showers and thunderstorms. Some thunderstorms produced gusty winds and large hail. Low pressure and an associated cold front moved across the Mid-Atlantic region during the day on May 25th. Warm and humid conditions led to showers and thunderstorms. Some thunderstorms produced gusty winds and large hail. Low pressure and an associated cold front moved across the Mid-Atlantic region during the day on May 25th. Warm and humid conditions led to showers and thunderstorms. Some thunderstorms produced gusty winds and large hail. Low pressure and an associated cold front moved across the Mid-Atlantic region during the day on May 25th. Warm and humid conditions led to showers and thunderstorms. Some thunderstorms produced gusty winds and large hail. Low pressure and an associated cold front moved across the Mid-Atlantic region during the day on May 25th. Warm and humid conditions led to showers and thunderstorms. Some thunderstorms produced gusty winds and large hail.\nEvent Narrative: Wind gust of 37 to 48 knots were reported at Tolly Point, Greenbury Point, the Annapolis Buoy and Thomas Point Lighthouse. Wind gusts of 36 to 37 knots were reported at Gunpowder. A wind gust of 36 knots was reported at Key Bridge. A wind gust of 35 knots was reported at the Patapsco Buoy. A wind gust of 35 knots was reported at the Patapsco Buoy. A wind gust of 38 knots was reported at Martin State.", "The following events were reported: Flash Flood, Flood. These occurred near station USW00093721, approximately 32.8278 km away, between 2017-05-25 17:46:00 and 2017-05-26 02:10:00. The flood was caused by Heavy Rain. Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 5000.0 and crop damage of 0.0. \n\nEpisode Narrative: Low pressure and an associated cold front moved across the Mid-Atlantic region during the day on May 25th. Temperatures and moisture increased across the region during the afternoon and showers and thunderstorms formed. This activity led to heavy rainfall that led to flooding. Low pressure and an associated cold front moved across the Mid-Atlantic region during the day on May 25th. Temperatures and moisture increased across the region during the afternoon and showers and thunderstorms formed. This activity led to heavy rainfall that led to flooding. Low pressure and an associated cold front moved across the Mid-Atlantic region during the day on May 25th. Temperatures and moisture increased across the region during the afternoon and showers and thunderstorms formed. This activity led to heavy rainfall that led to flooding. Low pressure and an associated cold front moved across the Mid-Atlantic region during the day on May 25th. Temperatures and moisture increased across the region during the afternoon and showers and thunderstorms formed. This activity led to heavy rainfall that led to flooding. Low pressure and an associated cold front moved across the Mid-Atlantic region during the day on May 25th. Temperatures and moisture increased across the region during the afternoon and showers and thunderstorms formed. This activity led to heavy rainfall that led to flooding. Low pressure and an associated cold front moved across the Mid-Atlantic region during the day on May 25th. Temperatures and moisture increased across the region during the afternoon and showers and thunderstorms formed. This activity led to heavy rainfall that led to flooding.\nEvent Narrative: There was one to two feet of water flowing near the 3600 Block of Brookeville Road. There was a car trapped in three to four feet of flowing water at Georgia Avenue and Brookeville Road. Reddy Branch was out of its banks. There were two feet of water flowing across the 1900 Block of Brighton Dam Road. The 4900 Block of MD-108 Olney Laytonsville Road was closed due to high water. Flooding continued after flash flooding ended. ||There was one to two feet of water flowing near the 3600 Block of Brookeville Road. There was a car trapped in three to four feet of flowing water at Georgia Avenue and Brookeville Road. Reddy Branch was out of its banks. Flooding continued after flash flooding ended. There were two feet of water flowing across the 1900 Block of Brighton Dam Road. The 18700 Block of Olney Mill Road was closed between Winding Strone Circle and Random Ridge Circle due to high water.", "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00093721, approximately 27.3807 km away, between 2017-05-25 18:05:00 and 2017-05-25 18:15:00. The events included records with hailstones measuring 40.2 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Low pressure and an associated cold front moved across the Mid-Atlantic region during the day on May 25th. Warm and humid conditions led to showers and thunderstorms. Some thunderstorms became severe. Low pressure and an associated cold front moved across the Mid-Atlantic region during the day on May 25th. Warm and humid conditions led to showers and thunderstorms. Some thunderstorms became severe. Low pressure and an associated cold front moved across the Mid-Atlantic region during the day on May 25th. Warm and humid conditions led to showers and thunderstorms. Some thunderstorms became severe. Low pressure and an associated cold front moved across the Mid-Atlantic region during the day on May 25th. Warm and humid conditions led to showers and thunderstorms. Some thunderstorms became severe. Low pressure and an associated cold front moved across the Mid-Atlantic region during the day on May 25th. Warm and humid conditions led to showers and thunderstorms. Some thunderstorms became severe.\nEvent Narrative: A tree was down on the 900 Block of Greenspring Valley Road. Quarter sized was reported at Owings Mills. A tree was down along Offutt Road at Samoset Road. A tree was down on Dolfield Boulevard at Lakeside Boulevard. A tree was down on Seminary Avenue at Mays Chapel Road.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 17.8169 km away, between 2017-05-31 17:07:00 and 2017-05-31 17:07:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A weak boundary remained over the region. Warm and humid conditions ahead of the boundary led to the development of showers and thunderstorms. An isolated thunderstorm became severe.\nEvent Narrative: A tree was down at Cedar Wood Drive and Cedar Lane.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 24.1168 km away, between 2017-06-19 14:40:00 and 2017-06-19 15:43:00. The events included records with measured wind gusts of 38.44444444444444 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A potent cold front passed through the area. Warm and humid conditions along with forcing from the boundary caused showers and thunderstorms to develop. Stronger winds aloft caused some storms to produce gusty winds. A potent cold front passed through the area. Warm and humid conditions along with forcing from the boundary caused showers and thunderstorms to develop. Stronger winds aloft caused some storms to produce gusty winds. A potent cold front passed through the area. Warm and humid conditions along with forcing from the boundary caused showers and thunderstorms to develop. Stronger winds aloft caused some storms to produce gusty winds. A potent cold front passed through the area. Warm and humid conditions along with forcing from the boundary caused showers and thunderstorms to develop. Stronger winds aloft caused some storms to produce gusty winds. A potent cold front passed through the area. Warm and humid conditions along with forcing from the boundary caused showers and thunderstorms to develop. Stronger winds aloft caused some storms to produce gusty winds. A potent cold front passed through the area. Warm and humid conditions along with forcing from the boundary caused showers and thunderstorms to develop. Stronger winds aloft caused some storms to produce gusty winds. A potent cold front passed through the area. Warm and humid conditions along with forcing from the boundary caused showers and thunderstorms to develop. Stronger winds aloft caused some storms to produce gusty winds. A potent cold front passed through the area. Warm and humid conditions along with forcing from the boundary caused showers and thunderstorms to develop. Stronger winds aloft caused some storms to produce gusty winds. A potent cold front passed through the area. Warm and humid conditions along with forcing from the boundary caused showers and thunderstorms to develop. Stronger winds aloft caused some storms to produce gusty winds.\nEvent Narrative: Wind gusts of 41 to 46 knots were reported at Tolly Point. A wind gust of 46 knots was reported at Greenberry Point. A wind gust of 43 knots was reported at Thomas Point Lighthouse. A wind gust of 36 knots was reported at Sandy Point. A wind gust of 39 knots was reported at Orioles Park. A wind gust of 35 knots was reported at the Maryland Science Center. A wind gust of 34 knots was reported at Key Bridge. A wind gust of 34 knots was reported at Dundalk Elementary School. Wind gusts up to 37 knots were reported at Hart Miller Island.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 17.8877 km away, between 2017-06-19 15:18:00 and 2017-06-19 15:22:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A potent cold front passed through the area. Warm and humid conditions along with forcing from the boundary caused showers and thunderstorms to develop. Stronger winds aloft caused some storms to become severe. A potent cold front passed through the area. Warm and humid conditions along with forcing from the boundary caused showers and thunderstorms to develop. Stronger winds aloft caused some storms to become severe. A potent cold front passed through the area. Warm and humid conditions along with forcing from the boundary caused showers and thunderstorms to develop. Stronger winds aloft caused some storms to become severe.\nEvent Narrative: A tree was down with wires on the road along the 800 block of South Shore Drive. A tree fell onto a house along the 200 block of Gross Avenue. A wind gust of 58 mph was measured.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 31.3763 km away, between 2017-06-21 17:34:00 and 2017-06-21 17:45:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A couple showers and thunderstorms developed due to an unstable atmosphere. A couple showers and thunderstorms developed due to an unstable atmosphere.\nEvent Narrative: Wind gusts up to 35 knots were measured at Gunpowder. Wind gusts in excess of 30 knots were reported at Martin State.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 29.99 km away, between 2017-07-01 15:14:00 and 2017-07-01 15:22:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front moved into the area triggering showers and thunderstorms. Hot and humid air ahead of the boundary caused an unstable air mass, which led to some thunderstorms becoming severe. A cold front moved into the area triggering showers and thunderstorms. Hot and humid air ahead of the boundary caused an unstable air mass, which led to some thunderstorms becoming severe. A cold front moved into the area triggering showers and thunderstorms. Hot and humid air ahead of the boundary caused an unstable air mass, which led to some thunderstorms becoming severe. A cold front moved into the area triggering showers and thunderstorms. Hot and humid air ahead of the boundary caused an unstable air mass, which led to some thunderstorms becoming severe.\nEvent Narrative: Several trees were down in the Pasadena area. Several trees were down in the Severna Park Area. A tree was down in the 3600 block of Fallston Road. A tree was blocking MD152 Fallston Road at Oakmont Road.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 33.7794 km away, between 2017-07-01 15:24:00 and 2017-07-01 16:00:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front moved into the area triggering showers and thunderstorms. Hot and humid air ahead of the boundary caused an unstable air mass, which led to gusty winds with some thunderstorms. A cold front moved into the area triggering showers and thunderstorms. Hot and humid air ahead of the boundary caused an unstable air mass, which led to gusty winds with some thunderstorms. A cold front moved into the area triggering showers and thunderstorms. Hot and humid air ahead of the boundary caused an unstable air mass, which led to gusty winds with some thunderstorms. A cold front moved into the area triggering showers and thunderstorms. Hot and humid air ahead of the boundary caused an unstable air mass, which led to gusty winds with some thunderstorms. A cold front moved into the area triggering showers and thunderstorms. Hot and humid air ahead of the boundary caused an unstable air mass, which led to gusty winds with some thunderstorms. A cold front moved into the area triggering showers and thunderstorms. Hot and humid air ahead of the boundary caused an unstable air mass, which led to gusty winds with some thunderstorms.\nEvent Narrative: A wind gust of 35 knots was measured at Tolchester Beach. A wind gust of 35 knots was reported at Tolchester. A wind gust in excess of 30 knots was reported. A wind gust of 38 knots was reported at Martin State. Wind gusts up to 35 knots were reported at Tolchester Beach. A wind gust of 37 knots was reported.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 28.3818 km away, between 2017-07-08 19:13:00 and 2017-07-08 19:13:00. The events included records with measured wind gusts of 36.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: An unstable atmosphere led to a few gusty thunderstorms.\nEvent Narrative: A wind gust of 36 knots was reported at Hart Miller Island.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 32.4756 km away, between 2017-07-14 15:08:00 and 2017-07-14 17:00:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front passed through the area. At the same time, an upper-level trough passed through increasing the winds aloft. There was enough shear to combine with an unstable atmosphere for gusty thunderstorms to develop. A cold front passed through the area. At the same time, an upper-level trough passed through increasing the winds aloft. There was enough shear to combine with an unstable atmosphere for gusty thunderstorms to develop. A cold front passed through the area. At the same time, an upper-level trough passed through increasing the winds aloft. There was enough shear to combine with an unstable atmosphere for gusty thunderstorms to develop. A cold front passed through the area. At the same time, an upper-level trough passed through increasing the winds aloft. There was enough shear to combine with an unstable atmosphere for gusty thunderstorms to develop. A cold front passed through the area. At the same time, an upper-level trough passed through increasing the winds aloft. There was enough shear to combine with an unstable atmosphere for gusty thunderstorms to develop. A cold front passed through the area. At the same time, an upper-level trough passed through increasing the winds aloft. There was enough shear to combine with an unstable atmosphere for gusty thunderstorms to develop.\nEvent Narrative: A wind gust in excess of 30 knots was reported at Hart Miller Island. A wind gust in excess of 46 knots was reported at Tolchester Beach. A wind gust of 38 knots was reported at Greenberry Point. Wind gusts of 36 to 37 knots were reported at Tolly Point. A wind gust of 41 knots was measured at Thomas Point. A wind gust of 37 knots was reported.", "The following events were reported: Funnel Cloud. These occurred near station USW00093721, approximately 38.799 km away, between 2017-07-15 10:40:00 and 2017-07-15 10:40:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A hot and humid airmass was present ahead of a frontal boundary which slowly moved southeast toward and then through the state. Several rounds of thunderstorms moved through the region ahead of this front over the course of a few days.\nEvent Narrative: A waterspout was reported over Chesapeake bay which then lifted as it reached the Eastern shore. Several reports came in of the funnel cloud.", "The following events were reported: Waterspout. These occurred near station USW00093721, approximately 46.149 km away, between 2017-07-15 10:49:00 and 2017-07-15 10:49:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: An isolated water spout occurred due to an unstable atmosphere and weak boundary nearby.\nEvent Narrative: A water spout was located near the Chester River to the north of Route 50.", "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00093721, approximately 38.9538 km away, between 2017-07-17 14:30:00 and 2017-07-17 14:58:00. The events included records with hailstones measuring 25.5 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A pressure trough triggered some showers and thunderstorms. Some storms became severe due to hot and humid conditions leading to an unstable atmosphere. A pressure trough triggered some showers and thunderstorms. Some storms became severe due to hot and humid conditions leading to an unstable atmosphere.\nEvent Narrative: Quarter sized hail was reported. A tree was down near Route 140 and Glen Falls Road.", "The following events were reported: Flash Flood. These occurred near station USW00093721, approximately 29.8849 km away, between 2017-07-17 14:59:00 and 2017-07-17 17:45:00.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 10000.0 and crop damage of 0.0. \n\nEpisode Narrative: An upper level trough approached while warm and moist conditions across the Mid-Atlantic region. Sufficient instability led to showers and thunderstorms that moved slowly and led to high rainfall rates mainly across north-central Maryland. An upper level trough approached while warm and moist conditions across the Mid-Atlantic region. Sufficient instability led to showers and thunderstorms that moved slowly and led to high rainfall rates mainly across north-central Maryland.\nEvent Narrative: There was about a foot of water moving quickly at the intersection of Reisterstown and High Falcon Road. There was over three feet of flowing water at 10435 Reisterstown Road. Water inundated an auto shop which included numerous cars.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 25.7105 km away, between 2017-07-22 13:30:00 and 2017-07-22 14:00:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A weak boundary moved into the area, but hot and humid conditions led to moderate to high amounts of instability. An upper-level trough increased winds aloft which caused storms associated with the boundary to become severe. A weak boundary moved into the area, but hot and humid conditions led to moderate to high amounts of instability. An upper-level trough increased winds aloft which caused storms associated with the boundary to become severe. A weak boundary moved into the area, but hot and humid conditions led to moderate to high amounts of instability. An upper-level trough increased winds aloft which caused storms associated with the boundary to become severe. A weak boundary moved into the area, but hot and humid conditions led to moderate to high amounts of instability. An upper-level trough increased winds aloft which caused storms associated with the boundary to become severe. A weak boundary moved into the area, but hot and humid conditions led to moderate to high amounts of instability. An upper-level trough increased winds aloft which caused storms associated with the boundary to become severe. A weak boundary moved into the area, but hot and humid conditions led to moderate to high amounts of instability. An upper-level trough increased winds aloft which caused storms associated with the boundary to become severe. A weak boundary moved into the area, but hot and humid conditions led to moderate to high amounts of instability. An upper-level trough increased winds aloft which caused storms associated with the boundary to become severe. A weak boundary moved into the area, but hot and humid conditions led to moderate to high amounts of instability. An upper-level trough increased winds aloft which caused storms associated with the boundary to become severe.\nEvent Narrative: A tree was down blocking Golden Pass Lane. A tree was down near the intersection of Rossback Road and Rutland Road. A tree was down near the intersection of Solomons Island Road and Harwood Road. A tree was down near the intersection of Brick Church Road and Solomons Island Road. A tree was down along the 2900 Block of Friends Road. A tree was down near the intersection of Chesapeake Place and Dock Road. Several large tree limbs were down along with one large tree in the Southaven neighborhood of Annapolis. A wind gust of 62 mph was also measured. A wind gust of 58 mph was reported.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 35.8931 km away, between 2017-07-22 14:09:00 and 2017-07-23 14:00:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A weak boundary moved into the area, but hot and humid conditions led to moderate to high amounts of instability. An upper-level trough increased winds aloft which caused storms associated with the boundary to produce gusty winds. A weak boundary moved into the area, but hot and humid conditions led to moderate to high amounts of instability. An upper-level trough increased winds aloft which caused storms associated with the boundary to produce gusty winds. A weak boundary moved into the area, but hot and humid conditions led to moderate to high amounts of instability. An upper-level trough increased winds aloft which caused storms associated with the boundary to produce gusty winds. A weak boundary moved into the area, but hot and humid conditions led to moderate to high amounts of instability. An upper-level trough increased winds aloft which caused storms associated with the boundary to produce gusty winds. A weak boundary moved into the area, but hot and humid conditions led to moderate to high amounts of instability. An upper-level trough increased winds aloft which caused storms associated with the boundary to produce gusty winds. A weak boundary moved into the area, but hot and humid conditions led to moderate to high amounts of instability. An upper-level trough increased winds aloft which caused storms associated with the boundary to produce gusty winds. A weak boundary moved into the area, but hot and humid conditions led to moderate to high amounts of instability. An upper-level trough increased winds aloft which caused storms associated with the boundary to produce gusty winds.\nEvent Narrative: Wind gusts up to 44 knots were reported at Greenberry Point. A wind gust of 40 knots was reported at Tolly Point. Wind gusts of 37 to 43 knots were reported at Kent Island. A wind gust of 35 knots was reported at the Bay Bridge. A wind gust of 49 knots was reported at Thomas Point Lighthouse. A wind gusts in excess of 30 knots was reported at Thomas Point Lighthouse. A wind gust in excess of 30 knots was reported at Thomas Point Lighthouse.", "The following events were reported: Thunderstorm Wind, Tornado. These occurred near station USW00093721, approximately 38.8505 km away, between 2017-07-22 14:18:00 and 2017-07-24 00:27:00.The events resulted in 1 injuries and 0 fatalities. No significant property or crop damage was reported. \n\nEpisode Narrative: A stalled frontal boundary was the focus for several rounds of thunderstorms that produced damaging winds and flooding in spots. A stalled frontal boundary was the focus for several rounds of thunderstorms that produced damaging winds and flooding in spots.\nEvent Narrative: A waterspout developed over the Chesapeake Bay between Annapolis|and Stevensville, Maryland just south of the Chesapeake Bay|Bridge as estimated by radar velocity from the Baltimore-|Washington Airport Terminal Doppler Weather Radar. The waterspout |moved ashore at 129 AM in the Bay City Area of Kent Island and |then traveled northeast toward Stevensville, Maryland where it |lifted at 133 AM after being on the ground for about 2 miles.||Maximum winds were estimated at 125 mph which makes this an EF2|tornado. Several wood framed townhomes had the upper floors |entirely lifted off along with the roof; several other homes had |either roofs lifted off and tossed or received other damage. One |business was destroyed. There was one injury to a person who was |punctured by debris. In addition, there were trees and power|lines down and some gas leaks were reported along with a |structure fire to a home.||The damage path began on Bayside Drive near Bay City and Stafford|roads in Bay City. A boat was lifted inland from shore and several|trees were snapped or downed from the tornado. Additional trees|were uprooted and torn apart on Buckingham and MC Kay roads. The|tornado make a S like motion back to the northwest completely |destroying a home at the intersection of Zaidee and Chenowith |drives. A large amount of debris was thrown southeast of the |tornado path. The tornado then resumed a northeast movement and |damaged a roof and snapped trees at the intersection of Victoria |Drive and Irene way. Further northwest on route 8, a produce |stand was destroyed.|||The tornado briefly lifted before impacting a series of townhomes|near Kent Manor drive and Ellendale Blvd. Several townhomes were|destroyed entirely. Also, Several of the townhomes had sides of|the structures blown out. The tornado skipped again then damaged|some roofs near Creekside Commons CT and Butterworth CT. A roof|was torn off of a church along Thompson Creek Rd in addition to |destroying a warehouse. Trees were also downed and uprooted at |this location as well. The tornado skipped one last time across |route 50 and made a final touchdown in the Stevensville Cemetery.|Several trees were downed along with wires down. Metal power |poles were also blown off their foundations on route 18. Measured gust.", "The following events were reported: Lightning, Thunderstorm Wind. These occurred near station USW00093721, approximately 30.3963 km away, between 2017-07-23 23:58:00 and 2017-07-24 20:38:00.The events resulted in 1 injuries and 0 fatalities. No significant property or crop damage was reported. \n\nEpisode Narrative: A boundary remained over Maryland near and east of Interstate 95. The boundary triggered showers and thunderstorms. Moderate to high amounts of instability along with stronger winds aloft led to some storms becoming severe. A boundary remained over Maryland near and east of Interstate 95. The boundary triggered showers and thunderstorms. Moderate to high amounts of instability along with stronger winds aloft led to some storms becoming severe. A boundary remained over Maryland near and east of Interstate 95. The boundary triggered showers and thunderstorms. Moderate to high amounts of instability along with stronger winds aloft led to some storms becoming severe. A boundary remained over Maryland near and east of Interstate 95. The boundary triggered showers and thunderstorms. Moderate to high amounts of instability along with stronger winds aloft led to some storms becoming severe. A boundary remained over Maryland near and east of Interstate 95. The boundary triggered showers and thunderstorms. Moderate to high amounts of instability along with stronger winds aloft led to some storms becoming severe. A boundary remained over Maryland near and east of Interstate 95. The boundary triggered showers and thunderstorms. Moderate to high amounts of instability along with stronger winds aloft led to some storms becoming severe. A boundary remained over Maryland near and east of Interstate 95. The boundary triggered showers and thunderstorms. Moderate to high amounts of instability along with stronger winds aloft led to some storms becoming severe. A boundary remained over Maryland near and east of Interstate 95. The boundary triggered showers and thunderstorms. Moderate to high amounts of instability along with stronger winds aloft led to some storms becoming severe. A boundary remained over Maryland near and east of Interstate 95. The boundary triggered showers and thunderstorms. Moderate to high amounts of instability along with stronger winds aloft led to some storms becoming severe. A boundary remained over Maryland near and east of Interstate 95. The boundary triggered showers and thunderstorms. Moderate to high amounts of instability along with stronger winds aloft led to some storms becoming severe. A boundary remained over Maryland near and east of Interstate 95. The boundary triggered showers and thunderstorms. Moderate to high amounts of instability along with stronger winds aloft led to some storms becoming severe. A boundary remained over Maryland near and east of Interstate 95. The boundary triggered showers and thunderstorms. Moderate to high amounts of instability along with stronger winds aloft led to some storms becoming severe. A boundary remained over Maryland near and east of Interstate 95. The boundary triggered showers and thunderstorms. Moderate to high amounts of instability along with stronger winds aloft led to some storms becoming severe. A boundary remained over Maryland near and east of Interstate 95. The boundary triggered showers and thunderstorms. Moderate to high amounts of instability along with stronger winds aloft led to some storms becoming severe.\nEvent Narrative: A tree was down near the intersection of Giddings Avenue and Tolson Street. A tree was down near the intersection of Cedar Park Road and Taylor Avenue. A tree was down on Hilltop Lane outside Salvation Army. A tree was down on Southgate Avenue. A tree was down near the intersection of Ridge Avenue and Tyler Avenue. A tree was down at the intersection of Warren Drive and janice Drive. A tree was down along Blackwell Road. A tree was down near the intersection of Gloucester Street and Newman Street. A tree was down between Fallston Road and Sweet Air Road. A tree was down on power lines. A tree eight inches in diameter fell down in the 3000 Block of North Ridge Road. A tree one foot in diameter was down near the intersection of Thunder Hill Road and White Acre Road. An individual riding a bike was struck by lightning near the intersection of Pulaski Highway and Long Bar Harbor Road. A tree was down near the intersection of Hilltop Lane and Tyler Avenue.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 29.6122 km away, between 2017-07-24 00:05:00 and 2017-07-24 20:50:00. The events included records with measured wind gusts of 37.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A boundary remained over the waters, triggering showers and thunderstorms. Moderate to high amounts of instability along with stronger winds aloft led to some storms producing gusty winds. A boundary remained over the waters, triggering showers and thunderstorms. Moderate to high amounts of instability along with stronger winds aloft led to some storms producing gusty winds. A boundary remained over the waters, triggering showers and thunderstorms. Moderate to high amounts of instability along with stronger winds aloft led to some storms producing gusty winds. A boundary remained over the waters, triggering showers and thunderstorms. Moderate to high amounts of instability along with stronger winds aloft led to some storms producing gusty winds. A boundary remained over the waters, triggering showers and thunderstorms. Moderate to high amounts of instability along with stronger winds aloft led to some storms producing gusty winds.\nEvent Narrative: Wind gusts up to 37 knots were reported at Sandy Point. A wind gust of 35 knots was measured at Thomas Point Lighthouse. A wind gust of 35knots was reported at the Patapsco Buoy. Wind gusts of 35 to 36 knots were reported at Annapolis. A wind gust of 42 knots was measured.", "The following events were reported: Flash Flood, Flood. These occurred near station USW00093721, approximately 15.6998 km away, between 2017-07-28 13:16:00 and 2017-07-29 08:00:00. The flood was caused by Heavy Rain. Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A strong upper level low interacted with a frontal boundary near the Mid-Atlantic region and low pressure formed along the boundary. High moisture content and thunderstorms led to widespread flooding across the Mid-Atlantic region. A strong upper level low interacted with a frontal boundary near the Mid-Atlantic region and low pressure formed along the boundary. High moisture content and thunderstorms led to widespread flooding across the Mid-Atlantic region. A strong upper level low interacted with a frontal boundary near the Mid-Atlantic region and low pressure formed along the boundary. High moisture content and thunderstorms led to widespread flooding across the Mid-Atlantic region. A strong upper level low interacted with a frontal boundary near the Mid-Atlantic region and low pressure formed along the boundary. High moisture content and thunderstorms led to widespread flooding across the Mid-Atlantic region. A strong upper level low interacted with a frontal boundary near the Mid-Atlantic region and low pressure formed along the boundary. High moisture content and thunderstorms led to widespread flooding across the Mid-Atlantic region. A strong upper level low interacted with a frontal boundary near the Mid-Atlantic region and low pressure formed along the boundary. High moisture content and thunderstorms led to widespread flooding across the Mid-Atlantic region. A strong upper level low interacted with a frontal boundary near the Mid-Atlantic region and low pressure formed along the boundary. High moisture content and thunderstorms led to widespread flooding across the Mid-Atlantic region. A strong upper level low interacted with a frontal boundary near the Mid-Atlantic region and low pressure formed along the boundary. High moisture content and thunderstorms led to widespread flooding across the Mid-Atlantic region. A strong upper level low interacted with a frontal boundary near the Mid-Atlantic region and low pressure formed along the boundary. High moisture content and thunderstorms led to widespread flooding across the Mid-Atlantic region. A strong upper level low interacted with a frontal boundary near the Mid-Atlantic region and low pressure formed along the boundary. High moisture content and thunderstorms led to widespread flooding across the Mid-Atlantic region. A strong upper level low interacted with a frontal boundary near the Mid-Atlantic region and low pressure formed along the boundary. High moisture content and thunderstorms led to widespread flooding across the Mid-Atlantic region. A strong upper level low interacted with a frontal boundary near the Mid-Atlantic region and low pressure formed along the boundary. High moisture content and thunderstorms led to widespread flooding across the Mid-Atlantic region. A strong upper level low interacted with a frontal boundary near the Mid-Atlantic region and low pressure formed along the boundary. High moisture content and thunderstorms led to widespread flooding across the Mid-Atlantic region. A strong upper level low interacted with a frontal boundary near the Mid-Atlantic region and low pressure formed along the boundary. High moisture content and thunderstorms led to widespread flooding across the Mid-Atlantic region. A strong upper level low interacted with a frontal boundary near the Mid-Atlantic region and low pressure formed along the boundary. High moisture content and thunderstorms led to widespread flooding across the Mid-Atlantic region. A strong upper level low interacted with a frontal boundary near the Mid-Atlantic region and low pressure formed along the boundary. High moisture content and thunderstorms led to widespread flooding across the Mid-Atlantic region.\nEvent Narrative: Swift water rescue reported at the intersection of Routes 170 and 648 near Pumphrey. Water flowing across Race Road between Hanover Road and Furnace Avenue due to torrential rains. The 3400 Block of Spelman Road flooded and closed due to torrential rainfall. Wilson Point Road flooded and closed near Eastern Boulevard due to torrential rainfall. The stream gauge on East Branch Herbert Run at Arbutus exceeded the flood stage of 7 feet. It peaked at 7.68 feet at 23:50 EST. Water covered yards near Tom Day Boulevard. Brookeville Road flooded and closed at Georgia Avenue due to flooding of Reddy Branch. The stream gauge on Little Patuxent River at Savage exceeded the flood stage of 10 feet. It peaked at 13.56 feet at 03:15 EST. Riverside trails began to flood. Water also approached fields off Bald Eagle Drive and approached Brock Bridge Road. Brookeville Road was flooded and closed between Zion Road and Georgia Avenue due to flooding of Reddy Branch due to torrential rainfall. Eastern Avenue flooded and closed due to torrential rain near Bowleys Quarters. Furnace Avenue closed at Ridge Road due to flash flooding of Deep Run. Furnace Avenue remained closed at Ridge Road due to flooding of Deep Run. Multiple vehicles reported trapped in high water along West Patapsco Street near Brooklyn Park in the area of Potee Street. Water rescue on Furnace Avenue near Main Street. Defense Highway flooded and closed near Huntwood Drive. The stream gauge on Little Patuxent River at Guilford exceeded the flood stage of 11 feet. It peaked at 12.05 feet at 02:00 EST. Water began to overflow and cover South Entrance Road near the Columbia Mall. The stream gauge on Hawlings River at Sandy Spring exceeded the flood stage of 6.5 feet. It peaked at 7.35 feet at 02:00 EST. Brighton Dam Road flooded at the Hawlings River.", "The following events were reported: Heavy Rain. These occurred near station USW00093721, approximately 40.0775 km away, between 2017-07-29 06:49:00 and 2017-07-29 06:49:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A rare summertime Nor'easter tracked just offshore producing heavy rain and wind.\nEvent Narrative: Two and two thirds inches of rain was measured.", "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00093721, approximately 34.8016 km away, between 2017-08-02 12:04:00 and 2017-08-02 15:01:00. The events included records with hailstones measuring 41.833333333333336 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: High amounts of instability caused thunderstorms to develop. A few thunderstorms became severe. High amounts of instability caused thunderstorms to develop. A few thunderstorms became severe. High amounts of instability caused thunderstorms to develop. A few thunderstorms became severe. High amounts of instability caused thunderstorms to develop. A few thunderstorms became severe. High amounts of instability caused thunderstorms to develop. A few thunderstorms became severe. High amounts of instability caused thunderstorms to develop. A few thunderstorms became severe.\nEvent Narrative: Quarter sized hail was reported. A tree was down. A tree was down on Hallhurst road. A tree was down along the 12200 Block of Stoney Batter Road. A tree was downed near Joppa Road Philadelphia Road. A couple trees were down at the Arbors Apartment Complex.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 37.4453 km away, between 2017-08-02 15:09:00 and 2017-08-02 17:12:00. The events included records with measured wind gusts of 41.5 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: An unstable atmosphere led to isolated gusty winds with thunderstorms. An unstable atmosphere led to isolated gusty winds with thunderstorms.\nEvent Narrative: Wind gusts up to 37 knots were reported at Tolchester. Wind gusts of 37 to 46 knots were reported at Gunpowder.", "The following events were reported: Flood. These occurred near station USW00093721, approximately 43.9951 km away, between 2017-08-02 16:30:00 and 2017-08-02 17:00:00. The flood was caused by Heavy Rain. Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Heavy rains from an isolated thunderstorm caused minor flooding in Harford County, Maryland during the afternoon of August 2nd.\nEvent Narrative: A car became stranded in high water on Edgewood Road under the railroad bridge. A water rescue was successful in removing the vehicle and its occupant.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 49.625 km away, between 2017-08-02 18:11:00 and 2017-08-02 18:11:00. The events included records with estimated wind gusts of 52.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A hot and humid airmass with weak boundaries led to slow moving strong to severe thunderstorms with damaging winds, hail and flooding.\nEvent Narrative: Thunderstorm winds blew trees onto power lines.", "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00093721, approximately 30.5985 km away, between 2017-08-03 15:53:00 and 2017-08-04 16:55:00. The events included records with hailstones measuring 47.421052631578945 inches.The events resulted in 3 injuries and 1 fatalities. No significant property or crop damage was reported. \n\nEpisode Narrative: A weak boundary along with hot and humid air caused thunderstorms to develop. A few thunderstorms became severe due to high amounts of instability. A weak boundary along with hot and humid air caused thunderstorms to develop. A few thunderstorms became severe due to high amounts of instability. A weak boundary along with hot and humid air caused thunderstorms to develop. A few thunderstorms became severe due to high amounts of instability. A weak boundary along with hot and humid air caused thunderstorms to develop. A few thunderstorms became severe due to high amounts of instability. A weak boundary along with hot and humid air caused thunderstorms to develop. A few thunderstorms became severe due to high amounts of instability. A weak boundary along with hot and humid air caused thunderstorms to develop. A few thunderstorms became severe due to high amounts of instability. A weak boundary along with hot and humid air caused thunderstorms to develop. A few thunderstorms became severe due to high amounts of instability. A weak boundary along with hot and humid air caused thunderstorms to develop. A few thunderstorms became severe due to high amounts of instability. A weak boundary along with hot and humid air caused thunderstorms to develop. A few thunderstorms became severe due to high amounts of instability. A weak boundary along with hot and humid air caused thunderstorms to develop. A few thunderstorms became severe due to high amounts of instability. A weak boundary along with hot and humid air caused thunderstorms to develop. A few thunderstorms became severe due to high amounts of instability. A weak boundary along with hot and humid air caused thunderstorms to develop. A few thunderstorms became severe due to high amounts of instability. A weak boundary along with hot and humid air caused thunderstorms to develop. A few thunderstorms became severe due to high amounts of instability. A weak boundary along with hot and humid air caused thunderstorms to develop. A few thunderstorms became severe due to high amounts of instability. A weak boundary along with hot and humid air caused thunderstorms to develop. A few thunderstorms became severe due to high amounts of instability. A weak boundary along with hot and humid air caused thunderstorms to develop. A few thunderstorms became severe due to high amounts of instability. A weak boundary along with hot and humid air caused thunderstorms to develop. A few thunderstorms became severe due to high amounts of instability. A weak boundary along with hot and humid air caused thunderstorms to develop. A few thunderstorms became severe due to high amounts of instability. A weak boundary along with hot and humid air caused thunderstorms to develop. A few thunderstorms became severe due to high amounts of instability.\nEvent Narrative: Quarter sized hail was reported. Multiple downed trees were near Courtney Road and Wilkins Avenue. A tree was down near Rolling Road and Edmondson Avenue. Multiple downed trees were near Gwynndale Avenue and Gwynn Oak Avenue. A downed tree was near Greenspring Avenue Bridle Ridge Lane. A tree was down near Woodbine Avenue and Allegheny Avenue. A tree was down near Crestwinck Road and Providence Road. A tree fell onto a vehicle near Pot Spring Road and Deer Fox Lane. The tree falling onto the vehicle resulted in one fatality and three injuries. A tree was down near Seminary Avenue and Milldam Road. A tree was down near Jarrettsville Pike and Dulaney Valley Road. Multpile trees were down along MD 146. A downed tree was near Flag Marsh Road and Grimville Road. Multiple trees were down in the neighborhood from Sunburst Road to Dairydale Road. A tree was down along the 2900 Block of Moores Road in Baldwin. A tree was down along Jarrettsville Pike and Hess Road. A tree was down along the 3100 Block of Morningside Court. Several six to eight inch diameter tree limbs were down. Several large trees were down and uprooted. A tree was down on Baldwin Mill Road and Greene Road.", "The following events were reported: Flood, Heavy Rain. These occurred near station USW00093721, approximately 43.5096 km away, between 2017-08-07 11:00:00 and 2017-08-07 17:01:00. The flood was caused by Heavy Rain. Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Thunderstorms developed along and north of a warm front. With humid air in place, the storms produced heavy rainfall and flash flooding. Thunderstorms developed along and north of a warm front. With humid air in place, the storms produced heavy rainfall and flash flooding. Thunderstorms developed along and north of a warm front. With humid air in place, the storms produced heavy rainfall and flash flooding.\nEvent Narrative: Water six inches deep in Prospect Bay. Just under 3 inches of rain fell. Two inches fell since last night.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 25.497 km away, between 2017-08-07 11:10:00 and 2017-08-07 11:40:00. The events included records with measured wind gusts of 35.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: An unstable atmosphere led to isolated gusty winds with thunderstorms.\nEvent Narrative: Wind gusts up to 35 knots were reported at the Patapsco Buoy.", "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00093721, approximately 31.2327 km away, between 2017-08-12 17:04:00 and 2017-08-12 19:24:00. The events included records with hailstones measuring 44.375 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front and an unstable atmosphere led to some severe thunderstorms. A cold front and an unstable atmosphere led to some severe thunderstorms. A cold front and an unstable atmosphere led to some severe thunderstorms. A cold front and an unstable atmosphere led to some severe thunderstorms. A cold front and an unstable atmosphere led to some severe thunderstorms. A cold front and an unstable atmosphere led to some severe thunderstorms. A cold front and an unstable atmosphere led to some severe thunderstorms. A cold front and an unstable atmosphere led to some severe thunderstorms.\nEvent Narrative: Quarter sized hail was reported near Friendship. A tree eight inches in diameter was down in the 13000 Block of Penn Shop Road. Two trees were down near the intersection of Long Corner Road and New Cut Road. A tree was down near the intersection off Long Corner Road and Gue Road. A tree was down on a light pole near the intersection of Court Road and Woodholme Avenue. A tree was down in the roadway near the intersection of Southwestern Boulevard and Francis Avenue. A tree was down blocking two right lanes of Governor Ritchie Highway at Cypress Creek Road. A wind gust of 62 mph was reported.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 20.5282 km away, between 2017-08-12 18:35:00 and 2017-08-12 19:42:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front and an unstable atmosphere led to some gusty thunderstorms. A cold front and an unstable atmosphere led to some gusty thunderstorms. A cold front and an unstable atmosphere led to some gusty thunderstorms.\nEvent Narrative: A wind gust of 34 knots was reported at Lakeland Elementary School. A wind gust of 43 knots was reported. A wind gust in excess of 30 knots was reported near Cape St. Claire.", "The following events were reported: Flash Flood, Flood. These occurred near station USW00093721, approximately 30.816 km away, between 2017-08-15 11:00:00 and 2017-08-15 17:00:00. The flood was caused by Heavy Rain. Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Heavy rain developed in the morning of August 15th, as a warm front was forced northward into the region, ahead of Hurricane Gert. The heavy rain continued into early afternoon, producing both flooding and flash flooding in the Baltimore metropolitan area. Heavy rain developed in the morning of August 15th, as a warm front was forced northward into the region, ahead of Hurricane Gert. The heavy rain continued into early afternoon, producing both flooding and flash flooding in the Baltimore metropolitan area. Heavy rain developed in the morning of August 15th, as a warm front was forced northward into the region, ahead of Hurricane Gert. The heavy rain continued into early afternoon, producing both flooding and flash flooding in the Baltimore metropolitan area. Heavy rain developed in the morning of August 15th, as a warm front was forced northward into the region, ahead of Hurricane Gert. The heavy rain continued into early afternoon, producing both flooding and flash flooding in the Baltimore metropolitan area. Heavy rain developed in the morning of August 15th, as a warm front was forced northward into the region, ahead of Hurricane Gert. The heavy rain continued into early afternoon, producing both flooding and flash flooding in the Baltimore metropolitan area. Heavy rain developed in the morning of August 15th, as a warm front was forced northward into the region, ahead of Hurricane Gert. The heavy rain continued into early afternoon, producing both flooding and flash flooding in the Baltimore metropolitan area. Heavy rain developed in the morning of August 15th, as a warm front was forced northward into the region, ahead of Hurricane Gert. The heavy rain continued into early afternoon, producing both flooding and flash flooding in the Baltimore metropolitan area.\nEvent Narrative: The hillside adjacent to Baldwin Mill Road washed out in a landslide, blocking the roadway in the 1800 block. Water two feet deep reported near North Point Road and German Hill Road in Dundalk. Edmonson Avenue flooded near Cooper Branch in the 3200 block. Multiple vehicles trapped in multiple feet of water on Erdman Avenue under the railroad tracks just west of I-95. Flooding due to torrential rain was reported near the intersection of North Point Boulevard and Interstate 695. Flooding on Vale Road near the intersection with North Tollgate Road. Carrs Mill Road flooded and closed adjacent to Winters Run, between the 1300 and 1600 blocks.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 27.7973 km away, between 2017-08-17 13:56:00 and 2017-08-17 13:56:00. The events included records with estimated wind gusts of 34.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Isolated showers and thunderstorms produced locally gusty winds.\nEvent Narrative: Wind gusts in excess of 30 knots were reported at Annapolis.", "The following events were reported: Lightning, Thunderstorm Wind. These occurred near station USW00093721, approximately 18.1566 km away, between 2017-08-18 16:11:00 and 2017-08-18 16:24:00.The events resulted in 10 injuries and 0 fatalities. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front triggered some showers and thunderstorms. A few thunderstorms became severe. A cold front triggered some showers and thunderstorms. A few thunderstorms became severe. A cold front triggered some showers and thunderstorms. A few thunderstorms became severe. A cold front triggered some showers and thunderstorms. A few thunderstorms became severe. A cold front triggered some showers and thunderstorms. A few thunderstorms became severe.\nEvent Narrative: Lightning struck the building at the Harford County 911 Center. Damage occurred to the building and 10 people were injured. Several large trees and limbs were down in the 400 Block of North Hilton Street. Several reports of trees were down in the Catonsville area. A large tree fell onto a vehicle along Willys Avenue between Sulphur Spring Road and June Road. Several other trees were down in the area. Two large tree branches were down near Ice Cream Cottage between Southwestern Boulevard and Linden Avenue.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 27.5899 km away, between 2017-08-18 16:30:00 and 2017-08-18 18:20:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front triggered some showers and thunderstorms and an unstable atmosphere caused storms to produce gusty winds. A cold front triggered some showers and thunderstorms and an unstable atmosphere caused storms to produce gusty winds. A cold front triggered some showers and thunderstorms and an unstable atmosphere caused storms to produce gusty winds. A cold front triggered some showers and thunderstorms and an unstable atmosphere caused storms to produce gusty winds. A cold front triggered some showers and thunderstorms and an unstable atmosphere caused storms to produce gusty winds. A cold front triggered some showers and thunderstorms and an unstable atmosphere caused storms to produce gusty winds. A cold front triggered some showers and thunderstorms and an unstable atmosphere caused storms to produce gusty winds. A cold front triggered some showers and thunderstorms and an unstable atmosphere caused storms to produce gusty winds. A cold front triggered some showers and thunderstorms and an unstable atmosphere caused storms to produce gusty winds. A cold front triggered some showers and thunderstorms and an unstable atmosphere caused storms to produce gusty winds. A cold front triggered some showers and thunderstorms and an unstable atmosphere caused storms to produce gusty winds.\nEvent Narrative: A wind gust of 39 knots was reported at the Patapsco Buoy. A wind gust of 38 knots was reported at the Maryland Science Center. Wind gusts in excess of 30 knots were reported at Thomas Point Lighthouse. A wind gust of 42 knots was reported at Oriole Park. A wind gust of 34 knots was reported at Key Bridge. A wind gust in excess of 30 knots was reported at Hart Miller Island. Wind gusts of 34 to 36 knots were reported at Tolchester. A wind gust of 39 knots was reported at Greenberry Point. A wind gust of 35 knots was reported at the Annapolis Buoy. A wind gust of 34 knots was reported at Kent Island. Wind gusts in excess of 30 knots were reported at Tolly Point.", "The following events were reported: Flash Flood. These occurred near station USW00093721, approximately 43.1654 km away, between 2017-08-18 16:47:00 and 2017-08-18 21:15:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Heavy rain developed late in the afternoon of August 18th mainly across the Baltimore metropolitan area, and in southern Maryland. This heavy rain was ahead of an approaching cold front. The torrential rains caused numerous instances of flash flooding, with some of the flooding in southern Maryland being slow enough to recede that it lasted well into the overnight hours. Heavy rain developed late in the afternoon of August 18th mainly across the Baltimore metropolitan area, and in southern Maryland. This heavy rain was ahead of an approaching cold front. The torrential rains caused numerous instances of flash flooding, with some of the flooding in southern Maryland being slow enough to recede that it lasted well into the overnight hours. Heavy rain developed late in the afternoon of August 18th mainly across the Baltimore metropolitan area, and in southern Maryland. This heavy rain was ahead of an approaching cold front. The torrential rains caused numerous instances of flash flooding, with some of the flooding in southern Maryland being slow enough to recede that it lasted well into the overnight hours. Heavy rain developed late in the afternoon of August 18th mainly across the Baltimore metropolitan area, and in southern Maryland. This heavy rain was ahead of an approaching cold front. The torrential rains caused numerous instances of flash flooding, with some of the flooding in southern Maryland being slow enough to recede that it lasted well into the overnight hours. Heavy rain developed late in the afternoon of August 18th mainly across the Baltimore metropolitan area, and in southern Maryland. This heavy rain was ahead of an approaching cold front. The torrential rains caused numerous instances of flash flooding, with some of the flooding in southern Maryland being slow enough to recede that it lasted well into the overnight hours. Heavy rain developed late in the afternoon of August 18th mainly across the Baltimore metropolitan area, and in southern Maryland. This heavy rain was ahead of an approaching cold front. The torrential rains caused numerous instances of flash flooding, with some of the flooding in southern Maryland being slow enough to recede that it lasted well into the overnight hours. Heavy rain developed late in the afternoon of August 18th mainly across the Baltimore metropolitan area, and in southern Maryland. This heavy rain was ahead of an approaching cold front. The torrential rains caused numerous instances of flash flooding, with some of the flooding in southern Maryland being slow enough to recede that it lasted well into the overnight hours. Heavy rain developed late in the afternoon of August 18th mainly across the Baltimore metropolitan area, and in southern Maryland. This heavy rain was ahead of an approaching cold front. The torrential rains caused numerous instances of flash flooding, with some of the flooding in southern Maryland being slow enough to recede that it lasted well into the overnight hours. Heavy rain developed late in the afternoon of August 18th mainly across the Baltimore metropolitan area, and in southern Maryland. This heavy rain was ahead of an approaching cold front. The torrential rains caused numerous instances of flash flooding, with some of the flooding in southern Maryland being slow enough to recede that it lasted well into the overnight hours.\nEvent Narrative: The USGS stream gage on Otter Point Creek / Winters Run near Edgewood exceeded the 8 foot flood stage for over 2 hours, causing flooding on Winters Run Road near Singer Road. Bynum Run rapidly escaped its banks, causing flooding and a road closure at the intersection of Patterson Mill Road and East Wheel Road. Whitaker Mill Road flooded and closed near Old Joppa Road due to torrential rainfall. Plumtree Run flooded, causing South Tollgate Road to be closed near Ruth Avenue. A foot of water flowing over Main Street in Ellicott City at Belfont Drive due to heavy rainfall. The road had to be closed. Bright Oaks Drive flooded and closed due to torrential rainfall. Flash flooding caused a road closure at Laurel Bush Road and Spruce Pine Road. A swift water rescue was reported near the Amtrak bridge on Edgewood Road. A swift water rescue was reported on Bynum Run at Route 7.", "The following events were reported: Flood. These occurred near station USW00093721, approximately 37.7426 km away, between 2017-08-18 19:10:00 and 2017-08-18 20:10:00. The flood was caused by Heavy Rain. Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Thunderstorms led to minor flooding.\nEvent Narrative: Camp Wright lane was blocked near route 8 due to water.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 23.4118 km away, between 2017-08-19 20:35:00 and 2017-08-19 21:18:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A boundary triggered some thunderstorms and an unstable atmosphere caused storms to produce gusty winds. A boundary triggered some thunderstorms and an unstable atmosphere caused storms to produce gusty winds. A boundary triggered some thunderstorms and an unstable atmosphere caused storms to produce gusty winds. A boundary triggered some thunderstorms and an unstable atmosphere caused storms to produce gusty winds.\nEvent Narrative: A wind gust in excess of 30 knots was reported at Oriole Park. A wind gust of 36 knots was reported at Key Bridge. Wind gusts in excess of 30 knots were reported at the Patapsco Buoy. Wind gusts of 34 to 35 knots were reported at Tolchester.", "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00093721, approximately 31.4711 km away, between 2017-08-21 14:10:00 and 2017-08-22 21:18:00. The events included records with hailstones measuring 17.333333333333332 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: An unstable atmosphere led to a few severe thunderstorms. An unstable atmosphere led to a few severe thunderstorms. An unstable atmosphere led to a few severe thunderstorms.\nEvent Narrative: Dime to quarter sized hail was reported. Quarter sized hail was reported. A tree was down on Priestford Road south of Cool Spring Road.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 26.9394 km away, between 2017-08-21 16:23:00 and 2017-08-21 17:18:00. The events included records with measured wind gusts of 41.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A boundary triggered some thunderstorms and an unstable atmosphere caused storms to produce gusty winds. A boundary triggered some thunderstorms and an unstable atmosphere caused storms to produce gusty winds.\nEvent Narrative: A wind gust of 47 knots was reported at the Patapsco Buoy. Wind gusts up to 35 knots were reported at Hartmiller Island.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 15.0222 km away, between 2017-09-05 16:30:00 and 2017-09-05 16:42:00. The events included records with estimated wind gusts of 34.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front passes through the area. A southerly flow ahead of the boundary led to an unstable atmosphere. Stronger upper-level winds caused deeper shear profiles. The shear profiles combined with lift from the front and an unstable atmosphere to cause some storms to produce gusty winds. A cold front passes through the area. A southerly flow ahead of the boundary led to an unstable atmosphere. Stronger upper-level winds caused deeper shear profiles. The shear profiles combined with lift from the front and an unstable atmosphere to cause some storms to produce gusty winds.\nEvent Narrative: A wind gusts in excess of 30 knots was reported. A wind gusts in excess of 30 knots was reported.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 21.3242 km away, between 2017-12-06 01:30:00 and 2017-12-06 02:30:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A strong cold front caused gusty showers to develop over the waters during the morning hours of the 6th. A strong cold front caused gusty showers to develop over the waters during the morning hours of the 6th.\nEvent Narrative: A wind gust of 35 knots was measured at Hart Miller Island. A wind gust in excess of 30 knots was reported at the Baltimore Key Bridge.", "The following events were reported: Flood. These occurred near station USW00093721, approximately 21.3984 km away, between 2018-02-11 10:27:00 and 2018-02-12 08:00:00. The flood was caused by Heavy Rain. Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Heavy precipitation developed along a stalled front during the overnight hours of February 10th into February 11th, causing flooding in southern Maryland. Stream flooding persisted into February 12th.\nEvent Narrative: Rutland Road was flooded and closed near Route 450.", "The following events were reported: Flood, Heavy Rain. These occurred near station USW00093721, approximately 37.781 km away, between 2018-02-11 12:29:00 and 2018-02-11 17:00:00. The flood was caused by Heavy Rain. Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A stalled frontal boundary brought several periods of heavy rain to the Eastern Shore. A stalled frontal boundary brought several periods of heavy rain to the Eastern Shore. A stalled frontal boundary brought several periods of heavy rain to the Eastern Shore.\nEvent Narrative: Storm total rainfall on Kent Island. Considerable flooding was reported on the northern half of Kent Island. Six inches of rain fell on the northern half of Kent Island. Six inches of rain (average of 3 gages) was also reported in Stevensville.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 22.2166 km away, between 2018-02-16 13:55:00 and 2018-02-16 13:55:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Gusty showers developed ahead of a cold front. Gusty showers developed ahead of a cold front.\nEvent Narrative: A wind gust in excess of 30 knots was reported at the Hampstead Hill Academy. A wind gust of 35 knots was reported at Martin State.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 25.0902 km away, between 2018-03-30 12:00:00 and 2018-03-30 13:00:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A strong cold front passed through. Gusty showers developed along and ahead of the boundary. A strong cold front passed through. Gusty showers developed along and ahead of the boundary. A strong cold front passed through. Gusty showers developed along and ahead of the boundary. A strong cold front passed through. Gusty showers developed along and ahead of the boundary. A strong cold front passed through. Gusty showers developed along and ahead of the boundary.\nEvent Narrative: Wind gusts in excess of 30 knots were reported at the Hampstead Hill Academy. Wind gusts in excess of 30 knots were reported at the Key Bridge. A wind gust of 37 knots was reported at Martin State. A wind gust of 34 to 36 knots at Greenberry Point. A wind gust of 34 knots was reported at Thomas Point.", "The following events were reported: Flash Flood, Flood. These occurred near station USW00093721, approximately 35.2786 km away, between 2018-04-16 02:37:00 and 2018-04-16 10:00:00. The flood was caused by Heavy Rain. Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Low pressure and its associated cold front passed through during the early morning hours of April 16th. Heavy rain of 1 to 3 inches fell in portions of the state, causing flooding mainly in Montgomery and Harford Counties. Upstream water from this same event then moved downstream, causing flooding along the Potomac River on the 18th. Low pressure and its associated cold front passed through during the early morning hours of April 16th. Heavy rain of 1 to 3 inches fell in portions of the state, causing flooding mainly in Montgomery and Harford Counties. Upstream water from this same event then moved downstream, causing flooding along the Potomac River on the 18th. Low pressure and its associated cold front passed through during the early morning hours of April 16th. Heavy rain of 1 to 3 inches fell in portions of the state, causing flooding mainly in Montgomery and Harford Counties. Upstream water from this same event then moved downstream, causing flooding along the Potomac River on the 18th. Low pressure and its associated cold front passed through during the early morning hours of April 16th. Heavy rain of 1 to 3 inches fell in portions of the state, causing flooding mainly in Montgomery and Harford Counties. Upstream water from this same event then moved downstream, causing flooding along the Potomac River on the 18th.\nEvent Narrative: Howard Chapel Road flooded and closed due to flooding from both Haights Branch and Hawlings River. Edgewood Road flooded and closed at the CSX railroad overpass. Maryland State Route 97 was flooded and closed between Brookeville Road and Bordly Drive, in the vicinity of Reddy Branch, due to rapidly rising water. One to 2 feet of moving water was flowing over Brighton Dam Road at the Hawlings River crossing. A car drove into these floodwaters, prompting a swift water rescue.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 24.2666 km away, between 2018-04-19 10:24:00 and 2018-04-19 11:45:00. The events included records with measured wind gusts of 38.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A strong cold front passed through, and showers were able to mix down gusty winds from aloft. A strong cold front passed through, and showers were able to mix down gusty winds from aloft. A strong cold front passed through, and showers were able to mix down gusty winds from aloft. A strong cold front passed through, and showers were able to mix down gusty winds from aloft. A strong cold front passed through, and showers were able to mix down gusty winds from aloft. A strong cold front passed through, and showers were able to mix down gusty winds from aloft. A strong cold front passed through, and showers were able to mix down gusty winds from aloft.\nEvent Narrative: Wind gusts up to 38 knots were reported at Hampstead Hill Academy. Wind gusts up to 36 to 39 knots were reported at Oriole Park. Wind gusts up to 39 knots were reported at Hartmiller Island. Wind gusts of 35 knots were reported at Greenberry Point. A wind gust of 34 knots was reported at Annapolis. Wind gusts up to 38 knots were reported at Tolchester. Wind gusts up to 43 knots were reported at Key Bridge.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 36.9916 km away, between 2018-04-28 19:00:00 and 2018-04-28 19:00:00. The events included records with estimated wind gusts of 34.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front passes through on the 28th. Some showers associated with the boundary were able to mix down gusty winds from aloft.\nEvent Narrative: A wind gust in excess of 30 knots was reported at Thomas Point.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 29.2075 km away, between 2018-05-04 19:25:00 and 2018-05-04 20:04:00. The events included records with estimated wind gusts of 34.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: An isolated storm produced gusty winds over the waters. An isolated storm produced gusty winds over the waters.\nEvent Narrative: A wind gust in excess of 30 knots was reported at Martin State. A wind gust in excess of 30 knots was reported at Greenberry Point.", "The following events were reported: Hail. These occurred near station USW00093721, approximately 41.0297 km away, between 2018-05-10 16:33:00 and 2018-05-10 16:33:00. The events included records with hailstones measuring 1.0 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front passed through the area on the 10th. Warm and humid air ahead of the boundary led to an unstable atmosphere. The instability combined with forcing from the cold front to trigger a few severe thunderstorms.\nEvent Narrative: Quarter sized hail was reported.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 26.9937 km away, between 2018-05-12 18:42:00 and 2018-05-12 21:00:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Low pressure tracked along a boundary and passed through the area on the 12th. Warm and humid air on the southern side of the boundary led to an unstable atmosphere. Some storms produced gusty winds. Low pressure tracked along a boundary and passed through the area on the 12th. Warm and humid air on the southern side of the boundary led to an unstable atmosphere. Some storms produced gusty winds. Low pressure tracked along a boundary and passed through the area on the 12th. Warm and humid air on the southern side of the boundary led to an unstable atmosphere. Some storms produced gusty winds. Low pressure tracked along a boundary and passed through the area on the 12th. Warm and humid air on the southern side of the boundary led to an unstable atmosphere. Some storms produced gusty winds. Low pressure tracked along a boundary and passed through the area on the 12th. Warm and humid air on the southern side of the boundary led to an unstable atmosphere. Some storms produced gusty winds. Low pressure tracked along a boundary and passed through the area on the 12th. Warm and humid air on the southern side of the boundary led to an unstable atmosphere. Some storms produced gusty winds. Low pressure tracked along a boundary and passed through the area on the 12th. Warm and humid air on the southern side of the boundary led to an unstable atmosphere. Some storms produced gusty winds. Low pressure tracked along a boundary and passed through the area on the 12th. Warm and humid air on the southern side of the boundary led to an unstable atmosphere. Some storms produced gusty winds. Low pressure tracked along a boundary and passed through the area on the 12th. Warm and humid air on the southern side of the boundary led to an unstable atmosphere. Some storms produced gusty winds. Low pressure tracked along a boundary and passed through the area on the 12th. Warm and humid air on the southern side of the boundary led to an unstable atmosphere. Some storms produced gusty winds. Low pressure tracked along a boundary and passed through the area on the 12th. Warm and humid air on the southern side of the boundary led to an unstable atmosphere. Some storms produced gusty winds. Low pressure tracked along a boundary and passed through the area on the 12th. Warm and humid air on the southern side of the boundary led to an unstable atmosphere. Some storms produced gusty winds. Low pressure tracked along a boundary and passed through the area on the 12th. Warm and humid air on the southern side of the boundary led to an unstable atmosphere. Some storms produced gusty winds. Low pressure tracked along a boundary and passed through the area on the 12th. Warm and humid air on the southern side of the boundary led to an unstable atmosphere. Some storms produced gusty winds. Low pressure tracked along a boundary and passed through the area on the 12th. Warm and humid air on the southern side of the boundary led to an unstable atmosphere. Some storms produced gusty winds.\nEvent Narrative: Wind gusts in excess of 30 knots were reported at Morrell Park. Wind gusts of 34 to 55 knots were reported at Key Bridge. Wind gusts up to 52 knots were reported at Hart Miller Island. Wind gusts of 34 to 42 knots were reported at Sandy Point. Wind gusts up to 41 knots were reported at the Bay Bridge Airport. Wind gusts up to 43 knots were reported at Kent Island. Wind gusts up to 53 knots were reported at Greenberry Point. Wind gusts of 50 to 54 knots were reported at Annapolis. Wind gusts up to 37 knots were reported at Tolly Point. A wind gust of 47 knots was reported at Thomas Point. Wind gusts up to 42 knots were reported at Tolchester. Wind gusts in excess of 30 knots were reported. Wind gusts up to 35 knots were reported at Lakeland Elementary School. Wind gusts in excess of 30 knots were reported at Hampstead Hill Academy. A wind gust of 45 knots was reported at Thomas Point Lighthouse.", "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00093721, approximately 15.1409 km away, between 2018-05-12 19:00:00 and 2018-05-12 19:50:00. The events included records with hailstones measuring 21.9 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Low pressure tracked along a boundary and passed through the area on the 12th. Warm and humid air on the southern side of the boundary led to an unstable atmosphere. Some storms became severe. Low pressure tracked along a boundary and passed through the area on the 12th. Warm and humid air on the southern side of the boundary led to an unstable atmosphere. Some storms became severe. Low pressure tracked along a boundary and passed through the area on the 12th. Warm and humid air on the southern side of the boundary led to an unstable atmosphere. Some storms became severe. Low pressure tracked along a boundary and passed through the area on the 12th. Warm and humid air on the southern side of the boundary led to an unstable atmosphere. Some storms became severe. Low pressure tracked along a boundary and passed through the area on the 12th. Warm and humid air on the southern side of the boundary led to an unstable atmosphere. Some storms became severe. Low pressure tracked along a boundary and passed through the area on the 12th. Warm and humid air on the southern side of the boundary led to an unstable atmosphere. Some storms became severe. Low pressure tracked along a boundary and passed through the area on the 12th. Warm and humid air on the southern side of the boundary led to an unstable atmosphere. Some storms became severe. Low pressure tracked along a boundary and passed through the area on the 12th. Warm and humid air on the southern side of the boundary led to an unstable atmosphere. Some storms became severe. Low pressure tracked along a boundary and passed through the area on the 12th. Warm and humid air on the southern side of the boundary led to an unstable atmosphere. Some storms became severe. Low pressure tracked along a boundary and passed through the area on the 12th. Warm and humid air on the southern side of the boundary led to an unstable atmosphere. Some storms became severe.\nEvent Narrative: Golf ball sized hail was reported. Quarter sized hail was reported. Quarter sized hail was reported. Half dollar sized hail was reported. Quarter sized hail was reported. A wind gust of 61 mph was reported. A wind gust of 62 mph was reported at Annapolis (KNAK). A wind gust of 60 mph was reported at Hart Miller Island. A wind gust of 61 mph was reported at Greenbury. Quarter sized hail was reported.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 32.2042 km away, between 2018-05-15 18:15:00 and 2018-05-15 18:50:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front passed through the area. Warm and humid conditions led to an unstable atmosphere ahead of the boundary, and that caused a few storms to become severe. A cold front passed through the area. Warm and humid conditions led to an unstable atmosphere ahead of the boundary, and that caused a few storms to become severe.\nEvent Narrative: A tree was down near the intersection of Harrisville Road and Ridge Road. A tree was down on the 2700 Block of Shirley Avenue.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 33.6552 km away, between 2018-05-15 18:42:00 and 2018-05-15 21:00:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front passed through the area. Warm and humid conditions led to an unstable atmosphere ahead of the boundary, and that caused a few storms to become severe. A cold front passed through the area. Warm and humid conditions led to an unstable atmosphere ahead of the boundary, and that caused a few storms to become severe. A cold front passed through the area. Warm and humid conditions led to an unstable atmosphere ahead of the boundary, and that caused a few storms to become severe. A cold front passed through the area. Warm and humid conditions led to an unstable atmosphere ahead of the boundary, and that caused a few storms to become severe. A cold front passed through the area. Warm and humid conditions led to an unstable atmosphere ahead of the boundary, and that caused a few storms to become severe.\nEvent Narrative: Wind gusts up to 39 knots were reported at Hart Miller Island. A wind gust in excess of 30 knots was reported at Tolly Point. Wind gusts of 35 to 43 knots were reported at Thomas Point Lighthouse. Wind gusts in excess of 30 knots were reported at Greenberry Point. Wind gusts in excess of 30 knots were reported at the Kent Island.", "The following events were reported: Flood. These occurred near station USW00093721, approximately 14.6416 km away, between 2018-05-15 21:14:00 and 2018-05-15 23:00:00. The flood was caused by Heavy Rain. Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front slowly sagged southward through Pennsylvania during the afternoon hours of May 15th. A line of storms spread ahead of this front, causing a widespread 1-3 inches of rain across North Central and Northeast Maryland. The western end of this line stalled, producing 3-6 inches of rain in a relatively short period of time in Frederick and extreme southeastern Washington Counties, prompting numerous water rescues and causing somewhat significant damage. The front stalled, and the next evening (May 16th), a second round of extreme rainfall struck much of the same area, with 3-6 inches of rain observed again in Frederick and southeastern Washington Counties. Renewed flooding ensued which continued into the morning hours of May 17th. A cold front slowly sagged southward through Pennsylvania during the afternoon hours of May 15th. A line of storms spread ahead of this front, causing a widespread 1-3 inches of rain across North Central and Northeast Maryland. The western end of this line stalled, producing 3-6 inches of rain in a relatively short period of time in Frederick and extreme southeastern Washington Counties, prompting numerous water rescues and causing somewhat significant damage. The front stalled, and the next evening (May 16th), a second round of extreme rainfall struck much of the same area, with 3-6 inches of rain observed again in Frederick and southeastern Washington Counties. Renewed flooding ensued which continued into the morning hours of May 17th.\nEvent Narrative: Nursery Road was flooded and closed at Holly Creek near Pumphrey. Defense Highway was flooded and closed at Broad Creek near Parole.", "The following events were reported: Flood. These occurred near station USW00093721, approximately 24.6708 km away, between 2018-05-18 08:10:00 and 2018-05-18 10:00:00. The flood was caused by Heavy Rain. Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Heavy rain fell in southern Maryland during the night of May 17th into the morning hours of the 18th. 1-4 inches of rain caused flooding, including of streams. More moderate to heavy rain continued in that area on the 18th and 19th, prolonging some flooding in Saint Mary's County. Meanwhile, the cumulative effects of several days of rain throughout the region caused stream flooding, particularly on the Potomac River. Heavy rain fell in southern Maryland during the night of May 17th into the morning hours of the 18th. 1-4 inches of rain caused flooding, including of streams. More moderate to heavy rain continued in that area on the 18th and 19th, prolonging some flooding in Saint Mary's County. Meanwhile, the cumulative effects of several days of rain throughout the region caused stream flooding, particularly on the Potomac River.\nEvent Narrative: Central Avenue (Maryland Route 214) reported flooded and closed at the Beards Creek crossing near Riva. Maryland Route 450 reported closed due to flooding near North River at Rutland Road.", "The following events were reported: Flash Flood, Flood. These occurred near station USW00093721, approximately 15.2784 km away, between 2018-05-27 13:09:00 and 2018-05-28 06:18:00. The flood was caused by Heavy Rain. The events resulted in 0 injuries and 1 fatalities. The events caused property damage valued at 22110000.0 and crop damage of 0.0. \n\nEpisode Narrative: A cold front sagged into Maryland during the afternoon of May 27th. Heavy rain trained to the northeast of Baltimore early in the afternoon, causing flash flooding. Then, later in the afternoon, the line completely stalled just west of Baltimore, producing 6-12 inches of rain in a very short period of time. Catastrophic flash flooding occurred in the Ellicott City and Catonsville areas, with significant flooding also observed in other nearby areas. Stream flooding continued through the next morning. A cold front sagged into Maryland during the afternoon of May 27th. Heavy rain trained to the northeast of Baltimore early in the afternoon, causing flash flooding. Then, later in the afternoon, the line completely stalled just west of Baltimore, producing 6-12 inches of rain in a very short period of time. Catastrophic flash flooding occurred in the Ellicott City and Catonsville areas, with significant flooding also observed in other nearby areas. Stream flooding continued through the next morning. A cold front sagged into Maryland during the afternoon of May 27th. Heavy rain trained to the northeast of Baltimore early in the afternoon, causing flash flooding. Then, later in the afternoon, the line completely stalled just west of Baltimore, producing 6-12 inches of rain in a very short period of time. Catastrophic flash flooding occurred in the Ellicott City and Catonsville areas, with significant flooding also observed in other nearby areas. Stream flooding continued through the next morning. A cold front sagged into Maryland during the afternoon of May 27th. Heavy rain trained to the northeast of Baltimore early in the afternoon, causing flash flooding. Then, later in the afternoon, the line completely stalled just west of Baltimore, producing 6-12 inches of rain in a very short period of time. Catastrophic flash flooding occurred in the Ellicott City and Catonsville areas, with significant flooding also observed in other nearby areas. Stream flooding continued through the next morning. A cold front sagged into Maryland during the afternoon of May 27th. Heavy rain trained to the northeast of Baltimore early in the afternoon, causing flash flooding. Then, later in the afternoon, the line completely stalled just west of Baltimore, producing 6-12 inches of rain in a very short period of time. Catastrophic flash flooding occurred in the Ellicott City and Catonsville areas, with significant flooding also observed in other nearby areas. Stream flooding continued through the next morning. A cold front sagged into Maryland during the afternoon of May 27th. Heavy rain trained to the northeast of Baltimore early in the afternoon, causing flash flooding. Then, later in the afternoon, the line completely stalled just west of Baltimore, producing 6-12 inches of rain in a very short period of time. Catastrophic flash flooding occurred in the Ellicott City and Catonsville areas, with significant flooding also observed in other nearby areas. Stream flooding continued through the next morning. A cold front sagged into Maryland during the afternoon of May 27th. Heavy rain trained to the northeast of Baltimore early in the afternoon, causing flash flooding. Then, later in the afternoon, the line completely stalled just west of Baltimore, producing 6-12 inches of rain in a very short period of time. Catastrophic flash flooding occurred in the Ellicott City and Catonsville areas, with significant flooding also observed in other nearby areas. Stream flooding continued through the next morning. A cold front sagged into Maryland during the afternoon of May 27th. Heavy rain trained to the northeast of Baltimore early in the afternoon, causing flash flooding. Then, later in the afternoon, the line completely stalled just west of Baltimore, producing 6-12 inches of rain in a very short period of time. Catastrophic flash flooding occurred in the Ellicott City and Catonsville areas, with significant flooding also observed in other nearby areas. Stream flooding continued through the next morning. A cold front sagged into Maryland during the afternoon of May 27th. Heavy rain trained to the northeast of Baltimore early in the afternoon, causing flash flooding. Then, later in the afternoon, the line completely stalled just west of Baltimore, producing 6-12 inches of rain in a very short period of time. Catastrophic flash flooding occurred in the Ellicott City and Catonsville areas, with significant flooding also observed in other nearby areas. Stream flooding continued through the next morning. A cold front sagged into Maryland during the afternoon of May 27th. Heavy rain trained to the northeast of Baltimore early in the afternoon, causing flash flooding. Then, later in the afternoon, the line completely stalled just west of Baltimore, producing 6-12 inches of rain in a very short period of time. Catastrophic flash flooding occurred in the Ellicott City and Catonsville areas, with significant flooding also observed in other nearby areas. Stream flooding continued through the next morning. A cold front sagged into Maryland during the afternoon of May 27th. Heavy rain trained to the northeast of Baltimore early in the afternoon, causing flash flooding. Then, later in the afternoon, the line completely stalled just west of Baltimore, producing 6-12 inches of rain in a very short period of time. Catastrophic flash flooding occurred in the Ellicott City and Catonsville areas, with significant flooding also observed in other nearby areas. Stream flooding continued through the next morning. A cold front sagged into Maryland during the afternoon of May 27th. Heavy rain trained to the northeast of Baltimore early in the afternoon, causing flash flooding. Then, later in the afternoon, the line completely stalled just west of Baltimore, producing 6-12 inches of rain in a very short period of time. Catastrophic flash flooding occurred in the Ellicott City and Catonsville areas, with significant flooding also observed in other nearby areas. Stream flooding continued through the next morning. A cold front sagged into Maryland during the afternoon of May 27th. Heavy rain trained to the northeast of Baltimore early in the afternoon, causing flash flooding. Then, later in the afternoon, the line completely stalled just west of Baltimore, producing 6-12 inches of rain in a very short period of time. Catastrophic flash flooding occurred in the Ellicott City and Catonsville areas, with significant flooding also observed in other nearby areas. Stream flooding continued through the next morning. A cold front sagged into Maryland during the afternoon of May 27th. Heavy rain trained to the northeast of Baltimore early in the afternoon, causing flash flooding. Then, later in the afternoon, the line completely stalled just west of Baltimore, producing 6-12 inches of rain in a very short period of time. Catastrophic flash flooding occurred in the Ellicott City and Catonsville areas, with significant flooding also observed in other nearby areas. Stream flooding continued through the next morning. A cold front sagged into Maryland during the afternoon of May 27th. Heavy rain trained to the northeast of Baltimore early in the afternoon, causing flash flooding. Then, later in the afternoon, the line completely stalled just west of Baltimore, producing 6-12 inches of rain in a very short period of time. Catastrophic flash flooding occurred in the Ellicott City and Catonsville areas, with significant flooding also observed in other nearby areas. Stream flooding continued through the next morning. A cold front sagged into Maryland during the afternoon of May 27th. Heavy rain trained to the northeast of Baltimore early in the afternoon, causing flash flooding. Then, later in the afternoon, the line completely stalled just west of Baltimore, producing 6-12 inches of rain in a very short period of time. Catastrophic flash flooding occurred in the Ellicott City and Catonsville areas, with significant flooding also observed in other nearby areas. Stream flooding continued through the next morning. A cold front sagged into Maryland during the afternoon of May 27th. Heavy rain trained to the northeast of Baltimore early in the afternoon, causing flash flooding. Then, later in the afternoon, the line completely stalled just west of Baltimore, producing 6-12 inches of rain in a very short period of time. Catastrophic flash flooding occurred in the Ellicott City and Catonsville areas, with significant flooding also observed in other nearby areas. Stream flooding continued through the next morning. A cold front sagged into Maryland during the afternoon of May 27th. Heavy rain trained to the northeast of Baltimore early in the afternoon, causing flash flooding. Then, later in the afternoon, the line completely stalled just west of Baltimore, producing 6-12 inches of rain in a very short period of time. Catastrophic flash flooding occurred in the Ellicott City and Catonsville areas, with significant flooding also observed in other nearby areas. Stream flooding continued through the next morning. A cold front sagged into Maryland during the afternoon of May 27th. Heavy rain trained to the northeast of Baltimore early in the afternoon, causing flash flooding. Then, later in the afternoon, the line completely stalled just west of Baltimore, producing 6-12 inches of rain in a very short period of time. Catastrophic flash flooding occurred in the Ellicott City and Catonsville areas, with significant flooding also observed in other nearby areas. Stream flooding continued through the next morning. A cold front sagged into Maryland during the afternoon of May 27th. Heavy rain trained to the northeast of Baltimore early in the afternoon, causing flash flooding. Then, later in the afternoon, the line completely stalled just west of Baltimore, producing 6-12 inches of rain in a very short period of time. Catastrophic flash flooding occurred in the Ellicott City and Catonsville areas, with significant flooding also observed in other nearby areas. Stream flooding continued through the next morning. A cold front sagged into Maryland during the afternoon of May 27th. Heavy rain trained to the northeast of Baltimore early in the afternoon, causing flash flooding. Then, later in the afternoon, the line completely stalled just west of Baltimore, producing 6-12 inches of rain in a very short period of time. Catastrophic flash flooding occurred in the Ellicott City and Catonsville areas, with significant flooding also observed in other nearby areas. Stream flooding continued through the next morning. A cold front sagged into Maryland during the afternoon of May 27th. Heavy rain trained to the northeast of Baltimore early in the afternoon, causing flash flooding. Then, later in the afternoon, the line completely stalled just west of Baltimore, producing 6-12 inches of rain in a very short period of time. Catastrophic flash flooding occurred in the Ellicott City and Catonsville areas, with significant flooding also observed in other nearby areas. Stream flooding continued through the next morning. A cold front sagged into Maryland during the afternoon of May 27th. Heavy rain trained to the northeast of Baltimore early in the afternoon, causing flash flooding. Then, later in the afternoon, the line completely stalled just west of Baltimore, producing 6-12 inches of rain in a very short period of time. Catastrophic flash flooding occurred in the Ellicott City and Catonsville areas, with significant flooding also observed in other nearby areas. Stream flooding continued through the next morning. A cold front sagged into Maryland during the afternoon of May 27th. Heavy rain trained to the northeast of Baltimore early in the afternoon, causing flash flooding. Then, later in the afternoon, the line completely stalled just west of Baltimore, producing 6-12 inches of rain in a very short period of time. Catastrophic flash flooding occurred in the Ellicott City and Catonsville areas, with significant flooding also observed in other nearby areas. Stream flooding continued through the next morning. A cold front sagged into Maryland during the afternoon of May 27th. Heavy rain trained to the northeast of Baltimore early in the afternoon, causing flash flooding. Then, later in the afternoon, the line completely stalled just west of Baltimore, producing 6-12 inches of rain in a very short period of time. Catastrophic flash flooding occurred in the Ellicott City and Catonsville areas, with significant flooding also observed in other nearby areas. Stream flooding continued through the next morning. A cold front sagged into Maryland during the afternoon of May 27th. Heavy rain trained to the northeast of Baltimore early in the afternoon, causing flash flooding. Then, later in the afternoon, the line completely stalled just west of Baltimore, producing 6-12 inches of rain in a very short period of time. Catastrophic flash flooding occurred in the Ellicott City and Catonsville areas, with significant flooding also observed in other nearby areas. Stream flooding continued through the next morning. A cold front sagged into Maryland during the afternoon of May 27th. Heavy rain trained to the northeast of Baltimore early in the afternoon, causing flash flooding. Then, later in the afternoon, the line completely stalled just west of Baltimore, producing 6-12 inches of rain in a very short period of time. Catastrophic flash flooding occurred in the Ellicott City and Catonsville areas, with significant flooding also observed in other nearby areas. Stream flooding continued through the next morning. A cold front sagged into Maryland during the afternoon of May 27th. Heavy rain trained to the northeast of Baltimore early in the afternoon, causing flash flooding. Then, later in the afternoon, the line completely stalled just west of Baltimore, producing 6-12 inches of rain in a very short period of time. Catastrophic flash flooding occurred in the Ellicott City and Catonsville areas, with significant flooding also observed in other nearby areas. Stream flooding continued through the next morning. A cold front sagged into Maryland during the afternoon of May 27th. Heavy rain trained to the northeast of Baltimore early in the afternoon, causing flash flooding. Then, later in the afternoon, the line completely stalled just west of Baltimore, producing 6-12 inches of rain in a very short period of time. Catastrophic flash flooding occurred in the Ellicott City and Catonsville areas, with significant flooding also observed in other nearby areas. Stream flooding continued through the next morning. A cold front sagged into Maryland during the afternoon of May 27th. Heavy rain trained to the northeast of Baltimore early in the afternoon, causing flash flooding. Then, later in the afternoon, the line completely stalled just west of Baltimore, producing 6-12 inches of rain in a very short period of time. Catastrophic flash flooding occurred in the Ellicott City and Catonsville areas, with significant flooding also observed in other nearby areas. Stream flooding continued through the next morning.\nEvent Narrative: A swift water rescue was performed near Parkville along Herring Run. Video footage shows a second wave of floodwaters, with water 1-2 feet deep over the 8600 block of Frederick Road in Ellicott City's West End. The floodwaters entered and damaged homes and vehicles. The culvert underneath Ellicott Mills Drive was undermined as the road was overtopped by floodwaters, washing out the road. Just downstream, the floodwaters caused the collapse of the historic stone cottage locals call The Old Courthouse, which was built in 1840. US Route 1 was flooded and closed at the Patapsco River due to rapid increases in the water level. Lower Main Street in Sykesville flooded due to overwhelmed storm drains during torrential rain. Some water entered two structures in addition to water covering parking lots. The stream gage on the Patapsco River near Catonsville rapidly exceeded the flood stage at the start time indicated. It rose more than seven feet above flood stage within 33 minutes of the flooding beginning, peaking at 27.03 feet. River Road was flooded, and damaged, as a result of this rapid rise. The stream gage on the Little Patuxent River near Columbia Town Center exceeded the flood elevation of 298.5 feet during the times indicated, and had already rapidly exceeded the flood stage due to flash flooding before this time. The peak elevation of 303.76 feet was observed at 8:20pm EST on May 27th. At the peak levels, US 29 was flooded by several feet of water on the southbound side. For the duration of the flood, South Entrance Road was flooded and closed. The first of three waves of flash flooding affected lower Main Street in Ellicott City on the Tiber River. Video footage shows the Tiber escaping its banks near Tiber Alley at 4:19pm, and at the alley in the 8100 block at 4:22pm. Several feet of rushing water began inundating Main Street and buildings in the area. At 4:35pm, the force of the floodwaters buckled the floor within one business, and water pushed through the building, emptying its contents onto Main Street. Video footage shows a third and final flood wave pushing through the 8100 block of Main Street. The water was nearly a foot deep on Main Street and then began entering buildings. Eventually overflow from the Tiber River caused the floodwaters of the Tiber and overland flow on Main Street to join with water surrounding and going through buildings. Catastrophic flash flooding occurred in Ellicott City as a result of torrential short-term rainfall of 6-10 inches. One person died during a lull in the flooding when he attempted to help another person evacuate and was swept away. Floodwaters on the lower portion of Main Street in the 8000 block reached the bottom of second floors of businesses. In all, dozens of water rescues were performed, most from buildings. Several roads flooded in Baltimore City. More than 20 people were rescued from vehicle rooftops during heavy rains. Six people were displaced from their homes, and Frederick Avenue was damaged in the Beechfield neighborhood. West Friendship Road flooded and closed south of Sykesville near the South Branch Patapsco River. Flooding began of South Entrance Road in Columbia, after the Little Patuxent River rapidly came out of its banks. Shortly thereafter, the stream covered the southbound lanes of US 29, with at least one water rescue required. A swift water rescue was conducted on Seven Courts Drive where a man was trapped in rising flood waters, clinging to a tree. The man was successfully rescued. Deep Run overflowed its banks, covering Mayfield Avenue in Elkridge. Widespread flash flooding in downtown Catonsville along Frederick Road. Roads flooded and water entering buildings. Flooding was reported in local schools along with 12 swift water rescues. The stream gage on East Branch Herbert Run at Arbutus rapidly exceeded the 7 foot flood stage during the indicated times. There were two distinct peaks during the times indicated but the higher was the second peak, of 9.21 feet at 5:20pm EST on May 27th. Water levels rapidly fell thereafter. The stream gage on the Patapsco River at Patapsco Valley State Park rapidly exceeded the 15 foot flood stage during the indicated times. Widespread damage occurred within the park, with a peak level reached of 24.36 feet at 5:45pm EST on May 27th. This is preliminarily the highest value reached at this location since at least 2010. The stream gage on the Little Patuxent River at Guilford exceeded the 11 foot flood stage during the times indicated. The peak level of 15.22 feet was observed at 10:15pm EST on May 27th, and was the 3rd highest ever recorded at this location. Vollmerhausen Road was flooded. The stream gage on the Little Patuxent River near Savage exceeded the 10 foot flood stage during the indicated times. The peak level of 16.52 feet occurred at 11:30pm EST on May 27th. Brock Bridge Road significantly flooded during this event. Video footage shows Hudson Branch out of its banks near Court Avenue, flooding yards. Video footage shows a second, more significant flash flood wave moved down Hudson Branch during the times indicated. Cars, dumpsters, and other large debris were swept downstream. Water covered a second-floor deck and entered structures, and was at least a foot deep flowing over Court Avenue at the peak of the flooding. The stream was not fully back in its banks in this area until after 8:00pm due to debris blockage. A second, more intense, flood wave pushed into the Tiber River, with water entering buildings in the 8100 block of Main Street. The water receded from this block of Main Street by 5:20pm. Video footage shows 6-12 inches of water flowing over the 8600 block of Frederick Road east of Rogers Avenue in Ellicott City's West End for a brief period before receding. Moving water observed over the hoods of several cars in multiple locations in the Catonsville area along Frederick Road. Several issues reported near Oella. There was a partial landslide on Old Frederick Road with the road also reported flooded and closed. River Road was flooded and closed. Thistle Road had a washout and was closed. A portion of Westchester Avenue was also flooded and closed. The stream gage on Gwynns Falls at Washington Boulevard in Baltimore rapidly exceeded the 13 foot flood stage, flooding portions of Gwynns Falls Park. The peak level of 17.09 feet was the 4th highest on record, and occurred at 5:31pm EST on May 27th. The stream gage on Whitemarsh Run at White Marsh rapidly exceeded the 11 foot flood stage during the times indicated. Parking lots near the stream, and Town Center Court, were flooded. The peak level of 13.42 feet was observed at 2:45pm EST on May 27th. Video footage shows water covering a deck and entering structures near Court Avenue. Water also flowed across Court Avenue during this time. Maryland Route 648 flooded and closed at Sawmill Creek in Glen Burnie.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 26.2684 km away, between 2018-05-27 14:54:00 and 2018-05-27 16:40:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A weak boundary combined with a warm and humid air mass to trigger some showers and thunderstorms. A few storms produced gusty winds. A weak boundary combined with a warm and humid air mass to trigger some showers and thunderstorms. A few storms produced gusty winds. A weak boundary combined with a warm and humid air mass to trigger some showers and thunderstorms. A few storms produced gusty winds.\nEvent Narrative: A wind gust of 37 knots was reported at the Annapolis Buoy. A wind gust in excess of 30 knots was reported at Key Bridge. A wind gust in excess of 30 knots was reported at Tolly Point.", "The following events were reported: Flood. These occurred near station USW00093721, approximately 11.7055 km away, between 2018-05-31 18:36:00 and 2018-05-31 20:30:00. The flood was caused by Heavy Rain. Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: During the evening as a warm front surged northward, heavy rain developed in the Laurel area, with 1-2 inches of rain falling in a relatively short period of time. This caused one isolated instance of flooding in Howard County.\nEvent Narrative: Guilford Road flooded and closed at Vollmerhausen Road.", "The following events were reported: Flood. These occurred near station USW00093721, approximately 19.3616 km away, between 2018-06-03 15:23:00 and 2018-06-04 05:00:00. The flood was caused by Heavy Rain. Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 15000.0 and crop damage of 0.0. \n\nEpisode Narrative: Heavy rain of 1-4 inches on June 3rd on saturated soils caused several instances of flooding in the western suburbs of Baltimore. Separately, the combined effects of several days of rain created somewhat widespread river flooding which continued to affect portions of the area through the early morning hours of June 6th. Heavy rain of 1-4 inches on June 3rd on saturated soils caused several instances of flooding in the western suburbs of Baltimore. Separately, the combined effects of several days of rain created somewhat widespread river flooding which continued to affect portions of the area through the early morning hours of June 6th. Heavy rain of 1-4 inches on June 3rd on saturated soils caused several instances of flooding in the western suburbs of Baltimore. Separately, the combined effects of several days of rain created somewhat widespread river flooding which continued to affect portions of the area through the early morning hours of June 6th. Heavy rain of 1-4 inches on June 3rd on saturated soils caused several instances of flooding in the western suburbs of Baltimore. Separately, the combined effects of several days of rain created somewhat widespread river flooding which continued to affect portions of the area through the early morning hours of June 6th. Heavy rain of 1-4 inches on June 3rd on saturated soils caused several instances of flooding in the western suburbs of Baltimore. Separately, the combined effects of several days of rain created somewhat widespread river flooding which continued to affect portions of the area through the early morning hours of June 6th. Heavy rain of 1-4 inches on June 3rd on saturated soils caused several instances of flooding in the western suburbs of Baltimore. Separately, the combined effects of several days of rain created somewhat widespread river flooding which continued to affect portions of the area through the early morning hours of June 6th. Heavy rain of 1-4 inches on June 3rd on saturated soils caused several instances of flooding in the western suburbs of Baltimore. Separately, the combined effects of several days of rain created somewhat widespread river flooding which continued to affect portions of the area through the early morning hours of June 6th. Heavy rain of 1-4 inches on June 3rd on saturated soils caused several instances of flooding in the western suburbs of Baltimore. Separately, the combined effects of several days of rain created somewhat widespread river flooding which continued to affect portions of the area through the early morning hours of June 6th. Heavy rain of 1-4 inches on June 3rd on saturated soils caused several instances of flooding in the western suburbs of Baltimore. Separately, the combined effects of several days of rain created somewhat widespread river flooding which continued to affect portions of the area through the early morning hours of June 6th. Heavy rain of 1-4 inches on June 3rd on saturated soils caused several instances of flooding in the western suburbs of Baltimore. Separately, the combined effects of several days of rain created somewhat widespread river flooding which continued to affect portions of the area through the early morning hours of June 6th. Heavy rain of 1-4 inches on June 3rd on saturated soils caused several instances of flooding in the western suburbs of Baltimore. Separately, the combined effects of several days of rain created somewhat widespread river flooding which continued to affect portions of the area through the early morning hours of June 6th.\nEvent Narrative: The stream gage on the Patapsco River at Ellicott City briefly exceeded the 122.50 foot flood elevation during the indicated period. The peak elevation of 122.60 feet was observed at 7:30pm EST on June 3rd. Water briefly reached the top of the inlet where the Patapsco and Tiber meet, but no inundation was reported. The stream gage on the Little Patuxent River near Columbia Town Center exceeded the 298.50 flood elevation during the indicated period. The peak elevation of 298.63 was observed at 8:00pm EST on June 3rd. At the peak level, South Entrance Road floods at the river. The stream gage on the Patapsco River near Catonsville exceeded the 20 foot flood stage during the indicated times, flooding River Road. The peak level of 22.17 feet was observed at 7:30pm EST on June 3rd. The stream gage on the Patapsco River at Elkridge exceeded the 15 foot flood stage during the indicated period. In addition to minor inundation at Patapsco Valley State Park, several roads were closed in the Pumphrey and Linthicum areas due to the flooding or backwater caused by it. The peak stage of 18.01 feet occurred at 9:00pm EST on June 3rd. The stream gage on the Little Patuxent River at Savage exceeded the 10 foot flood stage during the indicated period. The peak of 15.06 feet was observed at 10:00pm EST on June 3rd. Downstream of Savage, flooding occurred on Brock Bridge Road and Laurel-Fort Meade Road. River Road flooded and closed at Route 851. Cedar Lane flooded and closed by the Middle Patuxent River. Brookeville Road flooded and closed. Marriottsville Road flooded and closed. Flooding on Main Street in Sykesville forced the closure of the road. A portion of Fort Meade Road was washed out by flooding of the Little Patuxent River.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 28.7748 km away, between 2018-06-05 17:18:00 and 2018-06-09 16:00:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A few thunderstorms produced gusty winds due to an unstable atmosphere both days. A few thunderstorms produced gusty winds due to an unstable atmosphere both days. A few thunderstorms produced gusty winds due to an unstable atmosphere both days. A few thunderstorms produced gusty winds due to an unstable atmosphere both days. A few thunderstorms produced gusty winds due to an unstable atmosphere both days. A few thunderstorms produced gusty winds due to an unstable atmosphere both days. A few thunderstorms produced gusty winds due to an unstable atmosphere both days. A few thunderstorms produced gusty winds due to an unstable atmosphere both days. A few thunderstorms produced gusty winds due to an unstable atmosphere both days.\nEvent Narrative: A wind gust of 43 knots was reported at the Annapolis Buoy. A wind gust of 35 knots was measured at Tolchester Beach. A wind gust of 34 knots was reported at Lakeland Elementary School. A wind gust of 39 knots was reported at Key Bridge. Wind gusts of 34 to 42 knots were reported at Hartmiller Island. A wind gust of 40 knots was reported at Tolchester Beach. A wind gust in excess of 30 knots was reported at Annapolis. A wind gust in excess of 30 knots was reported at Greenberry Point. A wind gust of 43 knots was reported at Thomas Point Lighthouse.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 27.3332 km away, between 2018-06-18 15:20:00 and 2018-06-18 16:00:00. The events included records with estimated wind gusts of 50.666666666666664 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A weak trough caused thunderstorms to develop in a hot and humid air mass. The heat and humidity led to some storms becoming severe. A weak trough caused thunderstorms to develop in a hot and humid air mass. The heat and humidity led to some storms becoming severe. A weak trough caused thunderstorms to develop in a hot and humid air mass. The heat and humidity led to some storms becoming severe. A weak trough caused thunderstorms to develop in a hot and humid air mass. The heat and humidity led to some storms becoming severe. A weak trough caused thunderstorms to develop in a hot and humid air mass. The heat and humidity led to some storms becoming severe. A weak trough caused thunderstorms to develop in a hot and humid air mass. The heat and humidity led to some storms becoming severe.\nEvent Narrative: Multiple trees and wires were down in the vicinity of Mellor Avenue and Sandosky Road. Four vehicles were also damaged by downed trees and wires. A tree was also blocking College Avenue at Sykesville Road/MD 12. A tree was down at the intersection of Forsythe Road and Gaither Road. A tree was down near the intersection of Henryton Road and Old Frederick Road. Trees and wires were down near Reisterstown Road and Old Court Road. Multiple trees were down along Hooks Lane. Multiple reports of trees were down in the Towson area.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 31.452 km away, between 2018-06-18 17:14:00 and 2018-06-18 17:21:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A weak trough caused thunderstorms to develop in a hot and humid air mass. The heat and humidity led to some storms producing gusty winds. A weak trough caused thunderstorms to develop in a hot and humid air mass. The heat and humidity led to some storms producing gusty winds. A weak trough caused thunderstorms to develop in a hot and humid air mass. The heat and humidity led to some storms producing gusty winds.\nEvent Narrative: Wind gusts of 36 to 52 knots were reported at Greenberry Point. A wind gust of 37 knots was reported at the Annapolis Buoy. A wind gust in excess of 30 knots was reported at Tolly Point.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 22.1388 km away, between 2018-06-24 18:10:00 and 2018-06-24 18:48:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front passed through the area on the 24th and it was accompanied by a potent upper-level trough. The upper-level trough caused stronger winds aloft, and storms that developed were able to drag these stronger winds down to the surface. A cold front passed through the area on the 24th and it was accompanied by a potent upper-level trough. The upper-level trough caused stronger winds aloft, and storms that developed were able to drag these stronger winds down to the surface. A cold front passed through the area on the 24th and it was accompanied by a potent upper-level trough. The upper-level trough caused stronger winds aloft, and storms that developed were able to drag these stronger winds down to the surface. A cold front passed through the area on the 24th and it was accompanied by a potent upper-level trough. The upper-level trough caused stronger winds aloft, and storms that developed were able to drag these stronger winds down to the surface. A cold front passed through the area on the 24th and it was accompanied by a potent upper-level trough. The upper-level trough caused stronger winds aloft, and storms that developed were able to drag these stronger winds down to the surface. A cold front passed through the area on the 24th and it was accompanied by a potent upper-level trough. The upper-level trough caused stronger winds aloft, and storms that developed were able to drag these stronger winds down to the surface. A cold front passed through the area on the 24th and it was accompanied by a potent upper-level trough. The upper-level trough caused stronger winds aloft, and storms that developed were able to drag these stronger winds down to the surface.\nEvent Narrative: A wind gust of 34 knots were reported at Martin State. A wind gust in excess of 30 knots was reported at Oriole Park. Wind gusts up to 34 knots were reported. Wind gusts up to 34 knots were reported at Key Bridge. A wind gust of 36 knots was reported at Hampstead Hill Academy. Wind gusts of 35 to 37 knots were reported at Hartmiller Island. A wind gust in excess of 30 knots was reported at Tolchester Beach.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 14.2666 km away, between 2018-07-16 14:06:00 and 2018-07-16 14:06:00. The events included records with estimated wind gusts of 34.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: An isolated thunderstorm produced gusty winds due to an unstable atmosphere.\nEvent Narrative: A wind gust in excess of 30 knots was reported at Key Bridge.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 49.087 km away, between 2018-07-17 13:47:00 and 2018-07-17 13:47:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front passed through on the 17th, and southwest winds ahead of the boundary led to an unstable atmosphere. The instability combined with the lift from the cold front to produce severe thunderstorms.\nEvent Narrative: A tree was down on wires.", "The following events were reported: Flash Flood, Flood. These occurred near station USW00093721, approximately 16.0592 km away, between 2018-07-17 14:00:00 and 2018-07-17 17:00:00. The flood was caused by Heavy Rain. Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Heavy rain developed in the DC/Baltimore corridor during the afternoon of July 17th ahead of an approaching cold front. Rainfall of 1 to 3 inches caused flooding and isolated flash flooding, mainly in the Baltimore metro area. Heavy rain developed in the DC/Baltimore corridor during the afternoon of July 17th ahead of an approaching cold front. Rainfall of 1 to 3 inches caused flooding and isolated flash flooding, mainly in the Baltimore metro area. Heavy rain developed in the DC/Baltimore corridor during the afternoon of July 17th ahead of an approaching cold front. Rainfall of 1 to 3 inches caused flooding and isolated flash flooding, mainly in the Baltimore metro area. Heavy rain developed in the DC/Baltimore corridor during the afternoon of July 17th ahead of an approaching cold front. Rainfall of 1 to 3 inches caused flooding and isolated flash flooding, mainly in the Baltimore metro area. Heavy rain developed in the DC/Baltimore corridor during the afternoon of July 17th ahead of an approaching cold front. Rainfall of 1 to 3 inches caused flooding and isolated flash flooding, mainly in the Baltimore metro area. Heavy rain developed in the DC/Baltimore corridor during the afternoon of July 17th ahead of an approaching cold front. Rainfall of 1 to 3 inches caused flooding and isolated flash flooding, mainly in the Baltimore metro area.\nEvent Narrative: Dorsey Road (Maryland 176) reported flooded in both directions and closed near Sawmill Creek at Route 648 due to rapidly rising water. High water of unknown depth forced the closure of Maryland 176 between Wirth Road and WB&A Road. The ramp from the Baltimore Beltway to Camp Meade Road at Exit 6A was flooded and closed. Philadelphia Road flooded and closed south of Campbell Boulevard. One foot of water over the roadway on Wheel Road near Cedar Lane. Nursery Road flooded and closed near Maryland 648 due to rapidly rising water.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 36.9916 km away, between 2018-07-17 15:00:00 and 2018-07-17 15:00:00. The events included records with measured wind gusts of 37.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front passed through on the 17th, and southwest winds ahead of the boundary led to an unstable atmosphere. The instability combined with the lift from the cold front to gusty winds from thunderstorms.\nEvent Narrative: A wind gust of 37 knots was reported at Thomas Point Lighthouse.", "The following events were reported: Flash Flood, Flood. These occurred near station USW00093721, approximately 15.3346 km away, between 2018-07-21 16:19:00 and 2018-07-22 11:27:00. The flood was caused by Heavy Rain. Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A coastal low pressure moved up the Atlantic seaboard. Copious moisture spread northward across much of North Central and Northeast Maryland. Rainfall totals of 3 to 6 inches were widespread, with isolated higher amounts, causing fairly widespread flooding. A coastal low pressure moved up the Atlantic seaboard. Copious moisture spread northward across much of North Central and Northeast Maryland. Rainfall totals of 3 to 6 inches were widespread, with isolated higher amounts, causing fairly widespread flooding. A coastal low pressure moved up the Atlantic seaboard. Copious moisture spread northward across much of North Central and Northeast Maryland. Rainfall totals of 3 to 6 inches were widespread, with isolated higher amounts, causing fairly widespread flooding. A coastal low pressure moved up the Atlantic seaboard. Copious moisture spread northward across much of North Central and Northeast Maryland. Rainfall totals of 3 to 6 inches were widespread, with isolated higher amounts, causing fairly widespread flooding. A coastal low pressure moved up the Atlantic seaboard. Copious moisture spread northward across much of North Central and Northeast Maryland. Rainfall totals of 3 to 6 inches were widespread, with isolated higher amounts, causing fairly widespread flooding. A coastal low pressure moved up the Atlantic seaboard. Copious moisture spread northward across much of North Central and Northeast Maryland. Rainfall totals of 3 to 6 inches were widespread, with isolated higher amounts, causing fairly widespread flooding. A coastal low pressure moved up the Atlantic seaboard. Copious moisture spread northward across much of North Central and Northeast Maryland. Rainfall totals of 3 to 6 inches were widespread, with isolated higher amounts, causing fairly widespread flooding. A coastal low pressure moved up the Atlantic seaboard. Copious moisture spread northward across much of North Central and Northeast Maryland. Rainfall totals of 3 to 6 inches were widespread, with isolated higher amounts, causing fairly widespread flooding. A coastal low pressure moved up the Atlantic seaboard. Copious moisture spread northward across much of North Central and Northeast Maryland. Rainfall totals of 3 to 6 inches were widespread, with isolated higher amounts, causing fairly widespread flooding. A coastal low pressure moved up the Atlantic seaboard. Copious moisture spread northward across much of North Central and Northeast Maryland. Rainfall totals of 3 to 6 inches were widespread, with isolated higher amounts, causing fairly widespread flooding.\nEvent Narrative: The USGS stream gage on East Branch Herbert Run near Arbutus rapidly rose well above flood stage during the indicated period. Flooding of yards and outbuildings was reported in the area. The peak level of 10.55 feet occurred at 10:45pm EST. The stream gage on the Patapsco River near Elkridge exceeded the 16 foot flood stage during the indicated period. The peak level of 17.43 feet was observed at 1:50am EST. Hammonds Ferry Road and Furnace Avenue were flooded. Maryland Route 450 (Defense Highway) flooded and closed near Saint Stephens Church Road. The USGS stream gage on the Patuxent River near Unity exceeded the 8 foot flood stage during the indicated period. The peak level of 8.61 feet occurred at 6:00am EST. The parking lot for the Patuxent River State Park near Route 97 flooded. The USGS stream gage on Gwynns Falls in Baltimore rapidly exceeded the 13 foot flood stage during the indicated period. The peak level of 18.29 feet was observed at 12:15am EST on July 22nd. Gwynns Falls Park was flooded during this period. Several different swift water rescues ongoing in the corridor between Arbutus and Woodlawn. Water rescue for vehicle stranded in rapidly rising water on Mill Bottom Road at Bush Creek. Nursery Road flooded and closed. Hammonds Ferry Road also flooded and closed nearby. A water rescue was reported in this same area. Nursery Road flooded and closed. Hammonds Ferry Road also flooded and closed nearby. A water rescue was reported in this same area. The USGS stream gage on Sawmill Creek at Glen Burnie exceeded the 5 foot flood stage during the indicated period. The peak level of 6.80 feet occurred at 11:45pm EST. Central Avenue was flooded. For a portion of the time, near the peak, Crain Highway was reported flooded and closed at Sawmill Creek, and water covered the Northwest Baltimore and Annapolis Trail.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 36.9916 km away, between 2018-07-22 15:00:00 and 2018-07-22 15:00:00. The events included records with estimated wind gusts of 34.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cutoff low from the jet stream developed just to our west on the 22nd. Some thunderstorms produced gusty winds due to an unstable atmosphere and stronger winds that were able to mix down from aloft.\nEvent Narrative: Wind gusts in excess of 30 knots were reported at Thomas Point Lighthouse.", "The following events were reported: Flood. These occurred near station USW00093721, approximately 15.0836 km away, between 2018-07-22 19:18:00 and 2018-07-23 14:14:00. The flood was caused by Heavy Rain. Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Following the passage of a coastal low, bands of moisture pulled northward across the same areas that experienced heavy rain the day before. Rainfall amounts of 1 to 3 inches were common, with isolated higher amounts mainly in Anne Arundel and Calvert Counties. This produced renewed flooding, especially in those areas. Following the passage of a coastal low, bands of moisture pulled northward across the same areas that experienced heavy rain the day before. Rainfall amounts of 1 to 3 inches were common, with isolated higher amounts mainly in Anne Arundel and Calvert Counties. This produced renewed flooding, especially in those areas. Following the passage of a coastal low, bands of moisture pulled northward across the same areas that experienced heavy rain the day before. Rainfall amounts of 1 to 3 inches were common, with isolated higher amounts mainly in Anne Arundel and Calvert Counties. This produced renewed flooding, especially in those areas.\nEvent Narrative: Central Avenue flooded and closed at Beards Creek. More than two dozen roads flooded and closed throughout Baltimore City. The stream gage on the Patapsco River near Elkridge exceeded the 16 foot flood stage during the indicated period. The peak level of 17.36 feet occurred at 6:05am EST. Hammonds Ferry Road and Furnace Avenue were flooded.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 26.0383 km away, between 2018-07-23 02:01:00 and 2018-07-23 02:01:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cutoff low from the jet stream remained just to our west on the 23rd. An isolated thunderstorm became severe due to an unstable atmosphere and stronger winds that were able to mix down from aloft.\nEvent Narrative: Multiple downed trees were near Greenspring Valley Road and Championship Court.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 24.1122 km away, between 2018-07-23 12:10:00 and 2018-07-23 13:25:00. The events included records with estimated wind gusts of 34.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cutoff low from the jet stream remained just to our west on the 23rd. Some thunderstorms produced gusty winds due to an unstable atmosphere and stronger winds that were able to mix down from aloft. A cutoff low from the jet stream remained just to our west on the 23rd. Some thunderstorms produced gusty winds due to an unstable atmosphere and stronger winds that were able to mix down from aloft. A cutoff low from the jet stream remained just to our west on the 23rd. Some thunderstorms produced gusty winds due to an unstable atmosphere and stronger winds that were able to mix down from aloft. A cutoff low from the jet stream remained just to our west on the 23rd. Some thunderstorms produced gusty winds due to an unstable atmosphere and stronger winds that were able to mix down from aloft. A cutoff low from the jet stream remained just to our west on the 23rd. Some thunderstorms produced gusty winds due to an unstable atmosphere and stronger winds that were able to mix down from aloft. A cutoff low from the jet stream remained just to our west on the 23rd. Some thunderstorms produced gusty winds due to an unstable atmosphere and stronger winds that were able to mix down from aloft. A cutoff low from the jet stream remained just to our west on the 23rd. Some thunderstorms produced gusty winds due to an unstable atmosphere and stronger winds that were able to mix down from aloft.\nEvent Narrative: A wind gust in excess of 30 knots was reported at Greenberry Point. A wind gust in excess of 30 knots was reported at Tolly Point. A wind gust in excess of 30 knots was reported at Morrell Park School. A wind gust in excess of 30 knots was reported at Oriole Park. A wind gust in excess of 30 knots was reported at Thomas Point Lighthouse. A wind gust in excess of 30 knots was reported at Annapolis Buoy. A wind gust in excess of 30 knots was reported at Key Bridge.", "The following events were reported: Flash Flood, Flood. These occurred near station USW00093721, approximately 27.7431 km away, between 2018-07-23 20:55:00 and 2018-07-26 21:41:00. The flood was caused by Heavy Rain. Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 30000.0 and crop damage of 0.0. \n\nEpisode Narrative: Following the passage of a coastal low, bands of moisture continued to pull northward across the same areas that had already experienced heavy rain. Heavy rainfall fell in some areas, especially in Baltimore and Carroll Counties, with widespread flooding and flash flooding throughout the period. Following the passage of a coastal low, bands of moisture continued to pull northward across the same areas that had already experienced heavy rain. Heavy rainfall fell in some areas, especially in Baltimore and Carroll Counties, with widespread flooding and flash flooding throughout the period. Following the passage of a coastal low, bands of moisture continued to pull northward across the same areas that had already experienced heavy rain. Heavy rainfall fell in some areas, especially in Baltimore and Carroll Counties, with widespread flooding and flash flooding throughout the period. Following the passage of a coastal low, bands of moisture continued to pull northward across the same areas that had already experienced heavy rain. Heavy rainfall fell in some areas, especially in Baltimore and Carroll Counties, with widespread flooding and flash flooding throughout the period. Following the passage of a coastal low, bands of moisture continued to pull northward across the same areas that had already experienced heavy rain. Heavy rainfall fell in some areas, especially in Baltimore and Carroll Counties, with widespread flooding and flash flooding throughout the period. Following the passage of a coastal low, bands of moisture continued to pull northward across the same areas that had already experienced heavy rain. Heavy rainfall fell in some areas, especially in Baltimore and Carroll Counties, with widespread flooding and flash flooding throughout the period. Following the passage of a coastal low, bands of moisture continued to pull northward across the same areas that had already experienced heavy rain. Heavy rainfall fell in some areas, especially in Baltimore and Carroll Counties, with widespread flooding and flash flooding throughout the period. Following the passage of a coastal low, bands of moisture continued to pull northward across the same areas that had already experienced heavy rain. Heavy rainfall fell in some areas, especially in Baltimore and Carroll Counties, with widespread flooding and flash flooding throughout the period. Following the passage of a coastal low, bands of moisture continued to pull northward across the same areas that had already experienced heavy rain. Heavy rainfall fell in some areas, especially in Baltimore and Carroll Counties, with widespread flooding and flash flooding throughout the period. Following the passage of a coastal low, bands of moisture continued to pull northward across the same areas that had already experienced heavy rain. Heavy rainfall fell in some areas, especially in Baltimore and Carroll Counties, with widespread flooding and flash flooding throughout the period. Following the passage of a coastal low, bands of moisture continued to pull northward across the same areas that had already experienced heavy rain. Heavy rainfall fell in some areas, especially in Baltimore and Carroll Counties, with widespread flooding and flash flooding throughout the period. Following the passage of a coastal low, bands of moisture continued to pull northward across the same areas that had already experienced heavy rain. Heavy rainfall fell in some areas, especially in Baltimore and Carroll Counties, with widespread flooding and flash flooding throughout the period. Following the passage of a coastal low, bands of moisture continued to pull northward across the same areas that had already experienced heavy rain. Heavy rainfall fell in some areas, especially in Baltimore and Carroll Counties, with widespread flooding and flash flooding throughout the period. Following the passage of a coastal low, bands of moisture continued to pull northward across the same areas that had already experienced heavy rain. Heavy rainfall fell in some areas, especially in Baltimore and Carroll Counties, with widespread flooding and flash flooding throughout the period. Following the passage of a coastal low, bands of moisture continued to pull northward across the same areas that had already experienced heavy rain. Heavy rainfall fell in some areas, especially in Baltimore and Carroll Counties, with widespread flooding and flash flooding throughout the period. Following the passage of a coastal low, bands of moisture continued to pull northward across the same areas that had already experienced heavy rain. Heavy rainfall fell in some areas, especially in Baltimore and Carroll Counties, with widespread flooding and flash flooding throughout the period. Following the passage of a coastal low, bands of moisture continued to pull northward across the same areas that had already experienced heavy rain. Heavy rainfall fell in some areas, especially in Baltimore and Carroll Counties, with widespread flooding and flash flooding throughout the period. Following the passage of a coastal low, bands of moisture continued to pull northward across the same areas that had already experienced heavy rain. Heavy rainfall fell in some areas, especially in Baltimore and Carroll Counties, with widespread flooding and flash flooding throughout the period. Following the passage of a coastal low, bands of moisture continued to pull northward across the same areas that had already experienced heavy rain. Heavy rainfall fell in some areas, especially in Baltimore and Carroll Counties, with widespread flooding and flash flooding throughout the period. Following the passage of a coastal low, bands of moisture continued to pull northward across the same areas that had already experienced heavy rain. Heavy rainfall fell in some areas, especially in Baltimore and Carroll Counties, with widespread flooding and flash flooding throughout the period. Following the passage of a coastal low, bands of moisture continued to pull northward across the same areas that had already experienced heavy rain. Heavy rainfall fell in some areas, especially in Baltimore and Carroll Counties, with widespread flooding and flash flooding throughout the period. Following the passage of a coastal low, bands of moisture continued to pull northward across the same areas that had already experienced heavy rain. Heavy rainfall fell in some areas, especially in Baltimore and Carroll Counties, with widespread flooding and flash flooding throughout the period. Following the passage of a coastal low, bands of moisture continued to pull northward across the same areas that had already experienced heavy rain. Heavy rainfall fell in some areas, especially in Baltimore and Carroll Counties, with widespread flooding and flash flooding throughout the period. Following the passage of a coastal low, bands of moisture continued to pull northward across the same areas that had already experienced heavy rain. Heavy rainfall fell in some areas, especially in Baltimore and Carroll Counties, with widespread flooding and flash flooding throughout the period. Following the passage of a coastal low, bands of moisture continued to pull northward across the same areas that had already experienced heavy rain. Heavy rainfall fell in some areas, especially in Baltimore and Carroll Counties, with widespread flooding and flash flooding throughout the period.\nEvent Narrative: Smith Avenue flooded at Jones Falls. The USGS stream gage on Gunpowder Falls near Glencoe exceeded the 7 foot flood stage throughout the indicated period. There were three distinct peaks during the long period above flood stage, the highest of which was 14.41 feet, which occurred at 7:30am EST on July 25th. Throughout the flood, portions of Upper Glencoe Road and Lower Glencoe Road were flooded. For most of the time, Sparks Road was also flooded. Water was in buildings off of Sparks Road for over 24 hours from the morning of the 24th until the afternoon of the 25th, ultimately reaching several feet inside those structures. The water receded during the evening of the 25th but rose again overnight, affecting those buildings a second time. Nicodemus Road flooded and closed near Maryland Route 27 at Morgan Run. Maryland Route 450 flooded and closed between Saint Stephens Church Road and Huntwood Drive. The USGS stream gage on Baisman Run near Broadmoor exceeded the 4 foot flood stage during the brief indicated period. An access road near the gage flooded, with water approaching a porch. The USGS stream gage on Little Falls near Blue Mount exceeded the 8.5 foot flood stage during the indicated period. The peak level of 10.16 feet occurred at 4:00am EST. Water approached a driveway off Wiseburg Road and exceeded the banks in that area. Water also covered Big Falls Road in the area. The USGS gage on Beaverdam Run near Cockeysville exceeded the 9 foot flood stage during the indicated period. The peak level of 9.26 feet occurred at 12:05pm EST. Beaver Run Lane was flooded. Furnace Avenue closed between Race Road and the county line due to flooding. Swift water rescue required on Maryland Route 27 near Morgan Run and Nicodemus Road. Greenspring Avenue flooded and closed near Jones Falls. A school bus was reported stuck in slowly rising flood waters from the Gunpowder Falls near Glencoe. Two adults and one child were successfully rescued, uninjured. Baltimore Annapolis Boulevard flooded and closed near the Patapsco River. A bridge over Peggys Run collapsed on Mount Carmel Road. Ramp from I-70 to I-695 flooded and closed. The USGS stream gage on Gwynns Falls near Villa Nova exceeded the 11 foot flood stage during the indicated period. Queen Anne Road flooded. The peak level was 11.78 feet, which occurred at 2:45am EST. Flooding near the intersection of Gwynn Lake Drive and Gwynn Oak Avenue caused closure of both roads. More than ten roads flooded and closed throughout the city. The USGS gage on Beaverdam Run near Cockeysville exceeded the 9 foot flood stage during the indicated period. The peak level of 11.17 feet occurred at 2:00am EST. Beaver Run Lane was flooded. York Road was also flooded with water approaching nearby businesses. Local media reported one vehicle drove around a road closed sign and got stuck in the floodwaters on York Road. The occupant was rescued. The stream gage on the Patapsco River near Elkridge exceeded the 16 foot flood stage during the indicated period. The peak level of 19.69 feet occurred at 12:50pm EST. Hammonds Ferry Road and Furnace Avenue were flooded. The USGS stream gage on Western Run at this location exceeded the 8 foot flood stage during the indicated period. The peak level of 9.06 feet occurred at 2:00am EST. Western Run Road was flooded. Overflow from Big Gunpowder Falls forced the closure of one southbound lane of US 1. The stream gage on the Patapsco River near Elkridge exceeded the 16 foot flood stage during the indicated period. The peak level of 18.45 feet occurred at 11:05am EST. Hammonds Ferry Road and Furnace Avenue were flooded. The stream gage on the Patapsco River near Elkridge exceeded the 16 foot flood stage during the indicated period. The peak level of 16.37 feet occurred at 9:25pm EST. Hammonds Ferry Road and Furnace Avenue were flooded. The USGS stream gage on Beaver Run near Finksburg exceeded the 5 foot flood stage during the indicated period. The peak level of 6.03 feet occurred at 9:30pm EST. Hughes Road was flooded in the area. Western Run Road flooded and closed at Western Run. The USGS stream gage on Western Run at this location exceeded the 8 foot flood stage during the indicated period. The peak level of 11.35 feet occurred at 2:00am EST.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 28.7304 km away, between 2018-07-24 09:04:00 and 2018-07-24 10:00:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cutoff low from the jet stream remained just to our west on the 24th. Some thunderstorms produced gusty winds due to an unstable atmosphere and stronger winds that were able to mix down from aloft. A cutoff low from the jet stream remained just to our west on the 24th. Some thunderstorms produced gusty winds due to an unstable atmosphere and stronger winds that were able to mix down from aloft. A cutoff low from the jet stream remained just to our west on the 24th. Some thunderstorms produced gusty winds due to an unstable atmosphere and stronger winds that were able to mix down from aloft. A cutoff low from the jet stream remained just to our west on the 24th. Some thunderstorms produced gusty winds due to an unstable atmosphere and stronger winds that were able to mix down from aloft. A cutoff low from the jet stream remained just to our west on the 24th. Some thunderstorms produced gusty winds due to an unstable atmosphere and stronger winds that were able to mix down from aloft.\nEvent Narrative: A wind gust of 36 knots was reported at Annapolis. A wind gust of 35 knots was reported at Greenberry Point. A wind gust of 34 knots was reported at Thomas Point Lighthouse. Wind gusts up to 35 knots were reported at Tolly Point. Wind gusts in excess of 30 knots were reported at Key Bridge.", "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00093721, approximately 38.0349 km away, between 2018-07-27 15:20:00 and 2018-07-27 20:37:00. The events included records with hailstones measuring 47.25 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front passed through the area on the 27th. Ahead of the boundary, a southerly flow led to plenty of moisture an unstable atmosphere. A potent upper-level low caused stronger winds aloft as well. Some thunderstorms associated with the cold front became severe due to the instability and stronger winds aloft. A cold front passed through the area on the 27th. Ahead of the boundary, a southerly flow led to plenty of moisture an unstable atmosphere. A potent upper-level low caused stronger winds aloft as well. Some thunderstorms associated with the cold front became severe due to the instability and stronger winds aloft. A cold front passed through the area on the 27th. Ahead of the boundary, a southerly flow led to plenty of moisture an unstable atmosphere. A potent upper-level low caused stronger winds aloft as well. Some thunderstorms associated with the cold front became severe due to the instability and stronger winds aloft. A cold front passed through the area on the 27th. Ahead of the boundary, a southerly flow led to plenty of moisture an unstable atmosphere. A potent upper-level low caused stronger winds aloft as well. Some thunderstorms associated with the cold front became severe due to the instability and stronger winds aloft. A cold front passed through the area on the 27th. Ahead of the boundary, a southerly flow led to plenty of moisture an unstable atmosphere. A potent upper-level low caused stronger winds aloft as well. Some thunderstorms associated with the cold front became severe due to the instability and stronger winds aloft. A cold front passed through the area on the 27th. Ahead of the boundary, a southerly flow led to plenty of moisture an unstable atmosphere. A potent upper-level low caused stronger winds aloft as well. Some thunderstorms associated with the cold front became severe due to the instability and stronger winds aloft. A cold front passed through the area on the 27th. Ahead of the boundary, a southerly flow led to plenty of moisture an unstable atmosphere. A potent upper-level low caused stronger winds aloft as well. Some thunderstorms associated with the cold front became severe due to the instability and stronger winds aloft. A cold front passed through the area on the 27th. Ahead of the boundary, a southerly flow led to plenty of moisture an unstable atmosphere. A potent upper-level low caused stronger winds aloft as well. Some thunderstorms associated with the cold front became severe due to the instability and stronger winds aloft. A cold front passed through the area on the 27th. Ahead of the boundary, a southerly flow led to plenty of moisture an unstable atmosphere. A potent upper-level low caused stronger winds aloft as well. Some thunderstorms associated with the cold front became severe due to the instability and stronger winds aloft. A cold front passed through the area on the 27th. Ahead of the boundary, a southerly flow led to plenty of moisture an unstable atmosphere. A potent upper-level low caused stronger winds aloft as well. Some thunderstorms associated with the cold front became severe due to the instability and stronger winds aloft. A cold front passed through the area on the 27th. Ahead of the boundary, a southerly flow led to plenty of moisture an unstable atmosphere. A potent upper-level low caused stronger winds aloft as well. Some thunderstorms associated with the cold front became severe due to the instability and stronger winds aloft. A cold front passed through the area on the 27th. Ahead of the boundary, a southerly flow led to plenty of moisture an unstable atmosphere. A potent upper-level low caused stronger winds aloft as well. Some thunderstorms associated with the cold front became severe due to the instability and stronger winds aloft. A cold front passed through the area on the 27th. Ahead of the boundary, a southerly flow led to plenty of moisture an unstable atmosphere. A potent upper-level low caused stronger winds aloft as well. Some thunderstorms associated with the cold front became severe due to the instability and stronger winds aloft. A cold front passed through the area on the 27th. Ahead of the boundary, a southerly flow led to plenty of moisture an unstable atmosphere. A potent upper-level low caused stronger winds aloft as well. Some thunderstorms associated with the cold front became severe due to the instability and stronger winds aloft. A cold front passed through the area on the 27th. Ahead of the boundary, a southerly flow led to plenty of moisture an unstable atmosphere. A potent upper-level low caused stronger winds aloft as well. Some thunderstorms associated with the cold front became severe due to the instability and stronger winds aloft. A cold front passed through the area on the 27th. Ahead of the boundary, a southerly flow led to plenty of moisture an unstable atmosphere. A potent upper-level low caused stronger winds aloft as well. Some thunderstorms associated with the cold front became severe due to the instability and stronger winds aloft. A cold front passed through the area on the 27th. Ahead of the boundary, a southerly flow led to plenty of moisture an unstable atmosphere. A potent upper-level low caused stronger winds aloft as well. Some thunderstorms associated with the cold front became severe due to the instability and stronger winds aloft.\nEvent Narrative: A tree was down on MD 97 south of Roxbury Mill Road. A tree was down at Liberty Road and Wards Chapel Road. A tree was down in the 1000 Block of Hookers Mill Road. A tree was down near the intersection of Westwood Drive and Bonnie Avenue. Multiple trees were down in the Linthicum. A tree was down along the 200 Block of Welford Road. A tree was down at Glen Arm Road and Hartford Road. A tree was down near the intersection of Singer Road and Winters Run Road. A tree was down near the intersection of Grafton Shop Road and Osborne Parkway. A tree was down near the intersection of Federal Lane and Abingdon Road. A tree was down near the intersection of East Wheel Road and Cedar Lane. A tree limb was down blocking the roadway near the intersection of North Tollgate Road and Boulton Street. Large trees were also across the roadway near the intersection of Barnes Street and Powell Avenue. A tree was down across both lanes of Stafford Road near Susuquehanna Stage Park. Two trees were down on James Run Road near the intersection with Tower Road. A tree was down on Wesleyan Drive near the intersection of State Route 136. A tree and wires were down near the intersection of Forest Green Road and Park Beach Drive. Numerous trees were down on Rosemont Avenue. A tree was down on the 2700 Block of Laurel Brook Road. Half dollar sized hail was reported at Oriole Park. A tree was down near the intersection of Laurel Bush Road and Temple Drive.", "The following events were reported: Marine Hail, Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 30.4003 km away, between 2018-07-27 15:26:00 and 2018-07-27 16:30:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front passed through the area on the 27th. Ahead of the boundary, a southerly flow led to plenty of moisture an unstable atmosphere. A potent upper-level low caused stronger winds aloft as well. Some thunderstorms associated with the cold front produced gusty winds due to the instability and stronger winds aloft. A cold front passed through the area on the 27th. Ahead of the boundary, a southerly flow led to plenty of moisture an unstable atmosphere. A potent upper-level low caused stronger winds aloft as well. Some thunderstorms associated with the cold front produced gusty winds due to the instability and stronger winds aloft. A cold front passed through the area on the 27th. Ahead of the boundary, a southerly flow led to plenty of moisture an unstable atmosphere. A potent upper-level low caused stronger winds aloft as well. Some thunderstorms associated with the cold front produced gusty winds due to the instability and stronger winds aloft. A cold front passed through the area on the 27th. Ahead of the boundary, a southerly flow led to plenty of moisture an unstable atmosphere. A potent upper-level low caused stronger winds aloft as well. Some thunderstorms associated with the cold front produced gusty winds due to the instability and stronger winds aloft. A cold front passed through the area on the 27th. Ahead of the boundary, a southerly flow led to plenty of moisture an unstable atmosphere. A potent upper-level low caused stronger winds aloft as well. Some thunderstorms associated with the cold front produced gusty winds due to the instability and stronger winds aloft. A cold front passed through the area on the 27th. Ahead of the boundary, a southerly flow led to plenty of moisture an unstable atmosphere. A potent upper-level low caused stronger winds aloft as well. Some thunderstorms associated with the cold front produced gusty winds due to the instability and stronger winds aloft. A cold front passed through the area on the 27th. Ahead of the boundary, a southerly flow led to plenty of moisture an unstable atmosphere. A potent upper-level low caused stronger winds aloft as well. Some thunderstorms associated with the cold front produced gusty winds due to the instability and stronger winds aloft.\nEvent Narrative: Half dollar sized hail was reported near Baltimore. Wind gusts up to 35 knots were reported at the Annapolis Buoy. Wind gusts of 34 to 47 knots were reported at Tolly Point. Wind gusts up to 38 knots were reported at Greenberry Point. Wind gusts in excess of 30 knots were reported at Hart Miller. Wind gusts in excess of 30 knots were reported at Kent Island. Wind gusts in excess of 30 knots were reported at Thomas Point Lighthouse.", "The following events were reported: Flash Flood, Flood. These occurred near station USW00093721, approximately 25.3406 km away, between 2018-07-27 16:45:00 and 2018-07-27 20:20:00. The flood was caused by Heavy Rain. Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Heavy rain fell on saturated ground during the afternoon and evening of July 27th in the Baltimore metro area. One to three inches of rain was observed, along with numerous instances of flooding. Heavy rain fell on saturated ground during the afternoon and evening of July 27th in the Baltimore metro area. One to three inches of rain was observed, along with numerous instances of flooding. Heavy rain fell on saturated ground during the afternoon and evening of July 27th in the Baltimore metro area. One to three inches of rain was observed, along with numerous instances of flooding. Heavy rain fell on saturated ground during the afternoon and evening of July 27th in the Baltimore metro area. One to three inches of rain was observed, along with numerous instances of flooding. Heavy rain fell on saturated ground during the afternoon and evening of July 27th in the Baltimore metro area. One to three inches of rain was observed, along with numerous instances of flooding. Heavy rain fell on saturated ground during the afternoon and evening of July 27th in the Baltimore metro area. One to three inches of rain was observed, along with numerous instances of flooding. Heavy rain fell on saturated ground during the afternoon and evening of July 27th in the Baltimore metro area. One to three inches of rain was observed, along with numerous instances of flooding. Heavy rain fell on saturated ground during the afternoon and evening of July 27th in the Baltimore metro area. One to three inches of rain was observed, along with numerous instances of flooding. Heavy rain fell on saturated ground during the afternoon and evening of July 27th in the Baltimore metro area. One to three inches of rain was observed, along with numerous instances of flooding. Heavy rain fell on saturated ground during the afternoon and evening of July 27th in the Baltimore metro area. One to three inches of rain was observed, along with numerous instances of flooding.\nEvent Narrative: Two to three feet of water over the road following torrential rains near the intersection of Kensington Parkway and Harrogate Way. Ridge Road closed in the 2400 block due to flooding. Putty Hill Avenue flooded and closed near Towson. Flash flooding due to torrential rain was reported near the intersection of Cromwell Bridge Road and Cowpens Avenue, with road closures. US 40 flooded and closed due to torrential rain near the West Baltimore MARC station. Security Boulevard flooded and closed after torrential rains near Kernan Drive. Notchcliff Road flooded and closed after torrential rains swelled Cowen Run near Glen Arm Road. Torrential rain forced cars to be stuck in high water on Falls Road, with nearby ramps to Interstate 83 also flooded, blocking traffic. The USGS stream gage on East Branch Herbert Run near Arbutus rapidly and briefly exceeded the 7 foot flood stage during the indicated period, sending water into nearby yards. The peak level of 7.28 feet occurred at 5:10pm EST. The USGS stream gage on Otter Point rapidly but briefly exceeded the 8 foot flood stage during the indicated period, causing flooding on Winters Run Road. The peak of 8.39 feet occurred at 8:00pm EST.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 27.7973 km away, between 2018-08-01 00:38:00 and 2018-08-01 00:38:00. The events included records with estimated wind gusts of 35.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front crossing the region combined with high instability and moderate shear values to produce thunderstorms, one of which produced strong winds over the waters.\nEvent Narrative: A wind gust of 35 knots was measured.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 46.8109 km away, between 2018-08-01 21:35:00 and 2018-08-01 21:35:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front crossing the region combined with high instability and moderate shear values to produce thunderstorms, a few of which became severe. A cold front crossing the region combined with high instability and moderate shear values to produce thunderstorms, a few of which became severe.\nEvent Narrative: Tree fell on a house causing a roof collapse. Several trees blown down on Winters Run Golf Course. Wind ripped off part of golf clubhouse roof.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 32.3278 km away, between 2018-08-02 15:19:00 and 2018-08-02 17:00:00. The events included records with estimated wind gusts of 34.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A stalled front near the region combined with high instability and moderate shear values to produce thunderstorms, some of which produced strong winds over the waters. A stalled front near the region combined with high instability and moderate shear values to produce thunderstorms, some of which produced strong winds over the waters. A stalled front near the region combined with high instability and moderate shear values to produce thunderstorms, some of which produced strong winds over the waters. A stalled front near the region combined with high instability and moderate shear values to produce thunderstorms, some of which produced strong winds over the waters. A stalled front near the region combined with high instability and moderate shear values to produce thunderstorms, some of which produced strong winds over the waters.\nEvent Narrative: A wind gust of up to 34 knots was measured. A wind gust of up to 34 knots was measured. A wind gust of up to 34 knots was measured. A wind gust of up to 34 knots was measured. A wind gust of up to 34 knots was measured.", "The following events were reported: Flash Flood, Flood. These occurred near station USW00093721, approximately 37.2364 km away, between 2018-08-04 00:58:00 and 2018-08-05 01:31:00. The flood was caused by Heavy Rain. Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 25000.0 and crop damage of 0.0. \n\nEpisode Narrative: A southerly flow pumped in plenty of moisture from the Atlantic while a slow moving cold moved into the area. Copious amounts of moisture ahead of the boundary led to showers and thunderstorms. Torrential downpours combined with convection training over the same areas led to some flooding and flash flooding. Some of the flooding lingered into the early morning hours of the 5th. A southerly flow pumped in plenty of moisture from the Atlantic while a slow moving cold moved into the area. Copious amounts of moisture ahead of the boundary led to showers and thunderstorms. Torrential downpours combined with convection training over the same areas led to some flooding and flash flooding. Some of the flooding lingered into the early morning hours of the 5th. A southerly flow pumped in plenty of moisture from the Atlantic while a slow moving cold moved into the area. Copious amounts of moisture ahead of the boundary led to showers and thunderstorms. Torrential downpours combined with convection training over the same areas led to some flooding and flash flooding. Some of the flooding lingered into the early morning hours of the 5th. A southerly flow pumped in plenty of moisture from the Atlantic while a slow moving cold moved into the area. Copious amounts of moisture ahead of the boundary led to showers and thunderstorms. Torrential downpours combined with convection training over the same areas led to some flooding and flash flooding. Some of the flooding lingered into the early morning hours of the 5th. A southerly flow pumped in plenty of moisture from the Atlantic while a slow moving cold moved into the area. Copious amounts of moisture ahead of the boundary led to showers and thunderstorms. Torrential downpours combined with convection training over the same areas led to some flooding and flash flooding. Some of the flooding lingered into the early morning hours of the 5th. A southerly flow pumped in plenty of moisture from the Atlantic while a slow moving cold moved into the area. Copious amounts of moisture ahead of the boundary led to showers and thunderstorms. Torrential downpours combined with convection training over the same areas led to some flooding and flash flooding. Some of the flooding lingered into the early morning hours of the 5th.\nEvent Narrative: The stream gage on the Patapsco River near Elkridge exceeded the 16 foot flood stage during the indicated period. The peak level of 21.38 feet occurred at 12:30pm August 4th. Numerous roads were flooded across and near the river. The USGS stream gage on Beaver Run near Finksburg rapidly went from falling stages to above flood stage. The stream was above flood stage during the indicated period, with three different peaks. The highest level was 5.48 feet at 3:00am EST. Hughes Road flooded during this event. A basement wall collapsed due to flooding on Fawn Way. MD-27 Ridge Road was closed due to flooding between Lone Tree Road and Kate Wagner Road. Gillis Falls Road was washed out at Middle Run. The stream gauge at Glencoe crested at 9.64 feet above the flood stage of 7 feet. Sparks Road was flood.", "The following events were reported: Lightning, Thunderstorm Wind. These occurred near station USW00093721, approximately 14.6746 km away, between 2018-08-07 15:40:00 and 2018-08-07 16:10:00.The events resulted in 7 injuries and 0 fatalities. No significant property or crop damage was reported. \n\nEpisode Narrative: An upper level low near the region combined with high instability and increasing winds aloft to produce thunderstorms, some of which became severe. An upper level low near the region combined with high instability and increasing winds aloft to produce thunderstorms, some of which became severe. An upper level low near the region combined with high instability and increasing winds aloft to produce thunderstorms, some of which became severe.\nEvent Narrative: One person was struck by lightning on Colonial Drive sheltering under a tree. They were later released from the hospital. Six people from the set up crew of Anne Arundel County National Night Out event were struck by lightning in a field. All were released from the hospital. Several large tree limbs were blown down on Talister Court near King Avenue.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 27.53 km away, between 2018-08-07 15:48:00 and 2018-08-07 16:30:00. The events included records with measured wind gusts of 34.5 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: An upper level low near the region combined with high instability and increasing winds aloft to produce thunderstorms, some of which produced strong winds over the waters. An upper level low near the region combined with high instability and increasing winds aloft to produce thunderstorms, some of which produced strong winds over the waters.\nEvent Narrative: A wind gust of 35 knots was measured. A wind gust of 34 knots was measured.", "The following events were reported: Flash Flood. These occurred near station USW00093721, approximately 28.2263 km away, between 2018-08-07 17:34:00 and 2018-08-07 19:15:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A weak boundary triggered some showers and thunderstorms. Locally heavy rain caused a few incidents of flooding. A weak boundary triggered some showers and thunderstorms. Locally heavy rain caused a few incidents of flooding. A weak boundary triggered some showers and thunderstorms. Locally heavy rain caused a few incidents of flooding.\nEvent Narrative: MD-7 was closed near Nottinggood Road due to high water on both east and west bound lanes. Ten to twelve roads were reported to be closed due to flooding in White Marsh, Middle river, and Rossville. Pulaski Highway was closed at Martin Boulevard due to flooding.", "The following events were reported: Lightning, Thunderstorm Wind. These occurred near station USW00093721, approximately 39.1919 km away, between 2018-08-08 20:52:00 and 2018-08-08 21:48:00.The events resulted in 1 injuries and 0 fatalities. No significant property or crop damage was reported. \n\nEpisode Narrative: An upper level trough and surface cold front combined with high instability to produce thunderstorms, some of which became severe. An upper level trough and surface cold front combined with high instability to produce thunderstorms, some of which became severe. An upper level trough and surface cold front combined with high instability to produce thunderstorms, some of which became severe. An upper level trough and surface cold front combined with high instability to produce thunderstorms, some of which became severe.\nEvent Narrative: A tree as blown down in the 2400 block of Sams Creek Road. A tree was blown down in the 4600 block of London Bridge Road. A tree was blown down on Deer Park Road. A citizen was struck by lightning while walking their dog near Reistertown Road.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 25.8638 km away, between 2018-08-08 21:12:00 and 2018-08-08 21:12:00. The events included records with measured wind gusts of 36.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: An upper level trough and surface cold front combined with high instability to produce thunderstorms, some of which strong winds over the waters. An upper level trough and surface cold front combined with high instability to produce thunderstorms, some of which strong winds over the waters.\nEvent Narrative: A wind gust of 36 knots was measured. A wind gust to 36 knots was measured.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 48.815 km away, between 2018-08-11 17:58:00 and 2018-08-11 17:58:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Several areas of flash flooding occurred due to heavy rain. Rainfall totals of 1 to 3 inches were reported in northeastern Maryland. Additionally, severe thunderstorms impacted the area.\nEvent Narrative: Social media photos of several large tree branches down at a residence near Grasonville. Time approximated from radar.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 49.5618 km away, between 2018-08-11 18:10:00 and 2018-08-11 19:17:00. The events included records with measured wind gusts of 39.5 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A weak boundary was positioned overhead while an upper-level trough moved into the area. Showers and thunderstorms developed and some produced strong winds over the waters. A weak boundary was positioned overhead while an upper-level trough moved into the area. Showers and thunderstorms developed and some produced strong winds over the waters.\nEvent Narrative: A wind gust of 38 knots was measured. A wind gust of 41 knots was measured.", "The following events were reported: Flash Flood, Flood. These occurred near station USW00093721, approximately 26.4695 km away, between 2018-08-13 02:52:00 and 2018-08-13 19:52:00. The flood was caused by Heavy Rain. Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Upper-level low pressure remained over the region while a warm and humid air mass was in place. This resulted in showers and thunderstorms, some of which produced locally heavy rainfall. Upper-level low pressure remained over the region while a warm and humid air mass was in place. This resulted in showers and thunderstorms, some of which produced locally heavy rainfall. Upper-level low pressure remained over the region while a warm and humid air mass was in place. This resulted in showers and thunderstorms, some of which produced locally heavy rainfall. Upper-level low pressure remained over the region while a warm and humid air mass was in place. This resulted in showers and thunderstorms, some of which produced locally heavy rainfall. Upper-level low pressure remained over the region while a warm and humid air mass was in place. This resulted in showers and thunderstorms, some of which produced locally heavy rainfall. Upper-level low pressure remained over the region while a warm and humid air mass was in place. This resulted in showers and thunderstorms, some of which produced locally heavy rainfall. Upper-level low pressure remained over the region while a warm and humid air mass was in place. This resulted in showers and thunderstorms, some of which produced locally heavy rainfall. Upper-level low pressure remained over the region while a warm and humid air mass was in place. This resulted in showers and thunderstorms, some of which produced locally heavy rainfall. Upper-level low pressure remained over the region while a warm and humid air mass was in place. This resulted in showers and thunderstorms, some of which produced locally heavy rainfall. Upper-level low pressure remained over the region while a warm and humid air mass was in place. This resulted in showers and thunderstorms, some of which produced locally heavy rainfall. Upper-level low pressure remained over the region while a warm and humid air mass was in place. This resulted in showers and thunderstorms, some of which produced locally heavy rainfall.\nEvent Narrative: Two water rescues occurred due to motorists trapped in high water in the Towson area. About a dozen cars were flooded and lifted off Loch Raven Boulevard near Walker Avenue. Four cars were trapped in flood waters near the intersection of Putty Hill Avenue and Goucher Boulevard. Several vehicles were trapped in flood water near the intersection of Warren Road and Bosley Road. Five roads were closed due to flooding in Baltimore City. Magledt Road was impassable due to flooding. The USGS stream gage on West Branch Herring Run near Idlewylde very briefly but rapidly exceeded the 9 foot flood stage, peaking at 9.42 feet. Yards were flooded in the area, along with a portion of parkland downstream in Baltimore City. The stream gage on Minebank Run near Glen Arm briefly, but rapidly, exceeded the 10 foot flood stage during the indicated period, flooding lands and an access road near Talmar for a brief period of time. The peak level of 10.41 feet occurred at 5:30pm EST. A vehicle was trapped in high water near the intersection of Cromwell Bridge Road and Providence Road. The stream gage on Whitemarsh Run exceeded the 11 foot flood stage during the indicated period, flooding parking lots in the vicinity. The peak level of 12.27 feet occurred at 3:15am EST. The stream gauge at Whitemarsh Run indicated that water rapidly rose above flood stage of 11 feet, cresting at 11.34 feet. Water flooded parking lots near the stream, particularly near Town Center Court.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 27.5197 km away, between 2018-08-13 15:36:00 and 2018-08-13 18:00:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: An upper level low pressure system combined with high amounts of moisture and instability to produce thunderstorms. A few storms produced strong winds over the waters. An upper level low pressure system combined with high amounts of moisture and instability to produce thunderstorms. A few storms produced strong winds over the waters. An upper level low pressure system combined with high amounts of moisture and instability to produce thunderstorms. A few storms produced strong winds over the waters. An upper level low pressure system combined with high amounts of moisture and instability to produce thunderstorms. A few storms produced strong winds over the waters. An upper level low pressure system combined with high amounts of moisture and instability to produce thunderstorms. A few storms produced strong winds over the waters. An upper level low pressure system combined with high amounts of moisture and instability to produce thunderstorms. A few storms produced strong winds over the waters. An upper level low pressure system combined with high amounts of moisture and instability to produce thunderstorms. A few storms produced strong winds over the waters.\nEvent Narrative: A wind gust of 43 knots was measured. A wind gust of 35 knots was measured. A wind gust of 35 knots was measured. A wind gust of 36 knots was measured. A wind gust of 34 knots was measured. A wind gust of 43 knots was measured. A wind gust of up to 34 knots was measured.", "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00093721, approximately 24.5047 km away, between 2018-08-13 16:26:00 and 2018-08-13 17:38:00. The events included records with hailstones measuring 43.0 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: An upper level low pressure system combined with high amounts of moisture and instability to produce thunderstorms. A few storms became severe. An upper level low pressure system combined with high amounts of moisture and instability to produce thunderstorms. A few storms became severe. An upper level low pressure system combined with high amounts of moisture and instability to produce thunderstorms. A few storms became severe. An upper level low pressure system combined with high amounts of moisture and instability to produce thunderstorms. A few storms became severe. An upper level low pressure system combined with high amounts of moisture and instability to produce thunderstorms. A few storms became severe. An upper level low pressure system combined with high amounts of moisture and instability to produce thunderstorms. A few storms became severe. An upper level low pressure system combined with high amounts of moisture and instability to produce thunderstorms. A few storms became severe.\nEvent Narrative: Quarter sized hail fell at this location. A tree was blown down on Setting Star Road near Sandchain Road. A tree was blown down on Race Road near Church Avenue. A tree was blown down on Rustling Oak Drive near Shipleys Choice Club. Several trees and wires were blown down in the Kingsville and Perry Hall area. A tree was blown down onto a vehicle. A tree was blown down across the roadway near the intersection of Gunpowder Ridge Road and Loganwood Court.", "The following events were reported: Flood. These occurred near station USW00093721, approximately 40.3371 km away, between 2018-08-21 22:30:00 and 2018-08-22 00:30:00. The flood was caused by Heavy Rain. Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Low pressure passed by to the west toward the Great Lakes. The warm front associated with the low moved through the area while the cold front associated with the low approached from the west. There was enough lift associated with the warm front to combine with a warm and humid atmosphere, resulting in showers and thunderstorms. Rainfall was heavy at times which resulted in flooding. Low pressure passed by to the west toward the Great Lakes. The warm front associated with the low moved through the area while the cold front associated with the low approached from the west. There was enough lift associated with the warm front to combine with a warm and humid atmosphere, resulting in showers and thunderstorms. Rainfall was heavy at times which resulted in flooding. Low pressure passed by to the west toward the Great Lakes. The warm front associated with the low moved through the area while the cold front associated with the low approached from the west. There was enough lift associated with the warm front to combine with a warm and humid atmosphere, resulting in showers and thunderstorms. Rainfall was heavy at times which resulted in flooding.\nEvent Narrative: The USGS stream gage on Beaver Run near Finksburg briefly exceeded the 5 foot flood stage during the indicated period, flooding Hughes Road. The peak level of 5.19 feet occurred at 11:30pm EST. Hollingsworth Road was closed near Glen Falls Road. Lawndale Road was closed due to flooding.", "The following events were reported: Flash Flood, Flood. These occurred near station USW00093721, approximately 24.3235 km away, between 2018-08-31 11:51:00 and 2018-08-31 23:30:00. The flood was caused by Heavy Rain. Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Showers and thunderstorms developed around a stalled boundary. A slow storm motion combined with copious amounts of moisture led to heavy rain. Showers and thunderstorms developed around a stalled boundary. A slow storm motion combined with copious amounts of moisture led to heavy rain. Showers and thunderstorms developed around a stalled boundary. A slow storm motion combined with copious amounts of moisture led to heavy rain. Showers and thunderstorms developed around a stalled boundary. A slow storm motion combined with copious amounts of moisture led to heavy rain. Showers and thunderstorms developed around a stalled boundary. A slow storm motion combined with copious amounts of moisture led to heavy rain. Showers and thunderstorms developed around a stalled boundary. A slow storm motion combined with copious amounts of moisture led to heavy rain. Showers and thunderstorms developed around a stalled boundary. A slow storm motion combined with copious amounts of moisture led to heavy rain. Showers and thunderstorms developed around a stalled boundary. A slow storm motion combined with copious amounts of moisture led to heavy rain. Showers and thunderstorms developed around a stalled boundary. A slow storm motion combined with copious amounts of moisture led to heavy rain. Showers and thunderstorms developed around a stalled boundary. A slow storm motion combined with copious amounts of moisture led to heavy rain. Showers and thunderstorms developed around a stalled boundary. A slow storm motion combined with copious amounts of moisture led to heavy rain. Showers and thunderstorms developed around a stalled boundary. A slow storm motion combined with copious amounts of moisture led to heavy rain. Showers and thunderstorms developed around a stalled boundary. A slow storm motion combined with copious amounts of moisture led to heavy rain. Showers and thunderstorms developed around a stalled boundary. A slow storm motion combined with copious amounts of moisture led to heavy rain. Showers and thunderstorms developed around a stalled boundary. A slow storm motion combined with copious amounts of moisture led to heavy rain. Showers and thunderstorms developed around a stalled boundary. A slow storm motion combined with copious amounts of moisture led to heavy rain. Showers and thunderstorms developed around a stalled boundary. A slow storm motion combined with copious amounts of moisture led to heavy rain. Showers and thunderstorms developed around a stalled boundary. A slow storm motion combined with copious amounts of moisture led to heavy rain.\nEvent Narrative: The stream gauge at Otter Point Creek in Edgewood reached flood stage of 8 feet. This means that flooding occurred on Winters Road near Singer Road. Tollgate Road at Plumtree Road was closed due to flash flooding. The stream gauge at Plumtree Run in Bel Air crested at 6.63 feet, above the flood stage of 6 feet. Plumtree road near Plumtree Run was covered by water. Philadelphia Road near Calvary Road was closed due to flash flooding. The stream gauge at Otter Point Creek in Edgewood passed flood stage of 8 feet and crested at 8.99 feet. This means that flooding occurred on Winters Road near Singer Road. Guilford Road was closed at Mary Lane due to high water. The stream gauge reached the flood stage of 13 feet. At this level, water approaches the bike path alongside the stream. The stream gauge crested at 8.11 feet. At this level, water covers yards near Tom Day Boulevard. Water approaches structures along the creek, and approaches the top of the culvert at Sulphur Spring road. Hollins Ferry Road was closed due to flooding near Lansdowne Road. Hammonds Ferry Road was closed due to flooding at Mine Bank Lane. Benson Avenue was closed due to flooding between Haverhill Road and Knecht Avenue. A water rescue in the 1500 Block of MD-2 Ritchie Highway. MD-450 King George Street Bridge was closed due to high water. A water rescue occurred at the intersection of Taylor Avenue and Melrose Street. High water blocked Mission Road east of Guilford Road. The gauge at Gwynns Falls at Washington Boulevard surpassed flood stage of 13 feet, cresting at 14.11 feet. Water covered the bike path alongside the stream, and approaches the end of Berlin Street. The gauge along the Eastern Branch of Herbert Run at Arbutus surpassed the flood stage of 7 feet, cresting at 8.11 feet. Water approached structures along the creek, and approaches the top of the culvert at Sulphur Spring Road. Water covered yards near Tom Day Boulevard. The stream gauge at Plumtree Run near Bel Air crested at 6.63 feet which is above flood stage of 6 feet. At this level, water flows over both Plumtree Road and Tollgate Road.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 28.3818 km away, between 2018-08-31 18:27:00 and 2018-08-31 18:47:00. The events included records with measured wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A stationary front draped across the region combined with high instability and moisture to generate slow moving showers and thunderstorms, one of which produced strong winds over the waters.\nEvent Narrative: A wind gust of 50 knots was measured.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 19.4223 km away, between 2018-08-31 20:20:00 and 2018-08-31 20:30:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A stationary front draped across the region combined with high instability and moisture to generate slow moving showers and thunderstorms, a couple of which became severe. A stationary front draped across the region combined with high instability and moisture to generate slow moving showers and thunderstorms, a couple of which became severe.\nEvent Narrative: Two trees were blown down near Lakeshore Drive in Pasadena. A tree was blown down near Jones Station Road.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 28.3215 km away, between 2018-09-06 19:15:00 and 2018-09-06 19:15:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: High amounts of instability and an approaching cold front combined to produce scattered showers and thunderstorms during the afternoon and evening, some of which became severe. High amounts of instability and an approaching cold front combined to produce scattered showers and thunderstorms during the afternoon and evening, some of which became severe.\nEvent Narrative: A tree was blown down into an apartment building on Beech Drive. A 52 knot thunderstorm wind gust was measured at KMTN.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 34.7245 km away, between 2018-09-06 19:15:00 and 2018-09-06 19:36:00. The events included records with measured wind gusts of 43.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: High amounts of instability and an approaching cold front combined to produce scattered showers and thunderstorms during the afternoon and evening, some of which produced strong winds over the waters. High amounts of instability and an approaching cold front combined to produce scattered showers and thunderstorms during the afternoon and evening, some of which produced strong winds over the waters.\nEvent Narrative: A wind gust of 34 knots was measured at Tolchester (TCBM2). A wind gust of 52 knots was measured at Martin State Airport (KMTN).", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 19.8828 km away, between 2018-09-07 17:55:00 and 2018-09-07 17:55:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A pair of surface cold fronts interacted with a moist and warm unstable air mass to generate showers and thunderstorms. One thunderstorm became severe.\nEvent Narrative: A tree was blown down in the 6400 block of South Wind Circle.", "The following events were reported: Flood. These occurred near station USW00093721, approximately 23.4078 km away, between 2018-09-07 18:04:00 and 2018-09-07 21:03:00. The flood was caused by Heavy Rain. Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A boundary remain stalled over the region and tropical moisture was in place. This caused locally heavy rainfall. The steering flow aloft was weak so showers and storms moved slowly, which led to instances of flooding and flash flooding. A boundary remain stalled over the region and tropical moisture was in place. This caused locally heavy rainfall. The steering flow aloft was weak so showers and storms moved slowly, which led to instances of flooding and flash flooding. A boundary remain stalled over the region and tropical moisture was in place. This caused locally heavy rainfall. The steering flow aloft was weak so showers and storms moved slowly, which led to instances of flooding and flash flooding.\nEvent Narrative: Six to eight inches of water were flowing over MD-140 Reisterstown Road near Hammershire Road. The road was impassable due to high water along the 6100 Block of Trotter Road. The creek was out of its banks. Harriet Tubman Lane was blocked by high water near Cedar Lane.", "The following events were reported: Flood. These occurred near station USW00093721, approximately 22.5673 km away, between 2018-09-09 07:26:00 and 2018-09-12 20:10:00. The flood was caused by Heavy Rain. Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Low pressure tracked to the west while a nearly stationary boundary was to the south. Warm and moist tropical air overran the surface cooler air in place, resulting in a moderate to heavy rainfall. Excess runoff from the rainfall led to flooding. One and a half to three inches of rain fell across northern Maryland late on the 8th into the 9th, followed by another one to three inches on the 9th into the 10th. This combination produced fairly widespread flooding, including of the mainstem rivers, which continued through the 11th and into the 12th. Low pressure tracked to the west while a nearly stationary boundary was to the south. Warm and moist tropical air overran the surface cooler air in place, resulting in a moderate to heavy rainfall. Excess runoff from the rainfall led to flooding. One and a half to three inches of rain fell across northern Maryland late on the 8th into the 9th, followed by another one to three inches on the 9th into the 10th. This combination produced fairly widespread flooding, including of the mainstem rivers, which continued through the 11th and into the 12th. Low pressure tracked to the west while a nearly stationary boundary was to the south. Warm and moist tropical air overran the surface cooler air in place, resulting in a moderate to heavy rainfall. Excess runoff from the rainfall led to flooding. One and a half to three inches of rain fell across northern Maryland late on the 8th into the 9th, followed by another one to three inches on the 9th into the 10th. This combination produced fairly widespread flooding, including of the mainstem rivers, which continued through the 11th and into the 12th. Low pressure tracked to the west while a nearly stationary boundary was to the south. Warm and moist tropical air overran the surface cooler air in place, resulting in a moderate to heavy rainfall. Excess runoff from the rainfall led to flooding. One and a half to three inches of rain fell across northern Maryland late on the 8th into the 9th, followed by another one to three inches on the 9th into the 10th. This combination produced fairly widespread flooding, including of the mainstem rivers, which continued through the 11th and into the 12th. Low pressure tracked to the west while a nearly stationary boundary was to the south. Warm and moist tropical air overran the surface cooler air in place, resulting in a moderate to heavy rainfall. Excess runoff from the rainfall led to flooding. One and a half to three inches of rain fell across northern Maryland late on the 8th into the 9th, followed by another one to three inches on the 9th into the 10th. This combination produced fairly widespread flooding, including of the mainstem rivers, which continued through the 11th and into the 12th. Low pressure tracked to the west while a nearly stationary boundary was to the south. Warm and moist tropical air overran the surface cooler air in place, resulting in a moderate to heavy rainfall. Excess runoff from the rainfall led to flooding. One and a half to three inches of rain fell across northern Maryland late on the 8th into the 9th, followed by another one to three inches on the 9th into the 10th. This combination produced fairly widespread flooding, including of the mainstem rivers, which continued through the 11th and into the 12th. Low pressure tracked to the west while a nearly stationary boundary was to the south. Warm and moist tropical air overran the surface cooler air in place, resulting in a moderate to heavy rainfall. Excess runoff from the rainfall led to flooding. One and a half to three inches of rain fell across northern Maryland late on the 8th into the 9th, followed by another one to three inches on the 9th into the 10th. This combination produced fairly widespread flooding, including of the mainstem rivers, which continued through the 11th and into the 12th.\nEvent Narrative: Carrs Mill Road was flooded near Bush Park Road due to high water. MD-455 Defense Highway was closed due to flooding between Huntwood Drive and Rutland road. Furnace Branch Road was closed due to flooding near Ritchie Street. The stream gage on the Patapsco River at Elkridge exceeded the 16 foot flood stage during the indicated period. Hammonds Ferry Road flooded and was closed at the Patapsco River. Backwater flooding led to the closure of Furnace Avenue in Elkridge. The peak level of 19.64 feet occurred at 8:05 PM on the 9th. Broadwater Creek was out of its banks onto Battee Drive. The stream gage on the Patapsco River at Elkridge exceeded the 16 foot flood stage during the indicated period. Hammonds Ferry Road flooded and was closed at the Patapsco River. Backwater flooding led to the closure of Furnace Avenue in Elkridge. The peak level of 17 feet occurred at 2:55 PM. Numerous Road closures were reported across Carroll County due to high water.", "The following events were reported: Flash Flood, Flood. These occurred near station USW00093721, approximately 16.3368 km away, between 2018-09-18 00:52:00 and 2018-09-18 17:31:00. The flood was caused by Heavy Rain. Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: The remnants of Florence slowly tracked through the area on the 17th and 18th. Plenty of tropical moisture caused showers and thunderstorms to contain locally heavy rainfall, which led to instances of flooding. The remnants of Florence slowly tracked through the area on the 17th and 18th. Plenty of tropical moisture caused showers and thunderstorms to contain locally heavy rainfall, which led to instances of flooding. The remnants of Florence slowly tracked through the area on the 17th and 18th. Plenty of tropical moisture caused showers and thunderstorms to contain locally heavy rainfall, which led to instances of flooding. The remnants of Florence slowly tracked through the area on the 17th and 18th. Plenty of tropical moisture caused showers and thunderstorms to contain locally heavy rainfall, which led to instances of flooding. The remnants of Florence slowly tracked through the area on the 17th and 18th. Plenty of tropical moisture caused showers and thunderstorms to contain locally heavy rainfall, which led to instances of flooding. The remnants of Florence slowly tracked through the area on the 17th and 18th. Plenty of tropical moisture caused showers and thunderstorms to contain locally heavy rainfall, which led to instances of flooding. The remnants of Florence slowly tracked through the area on the 17th and 18th. Plenty of tropical moisture caused showers and thunderstorms to contain locally heavy rainfall, which led to instances of flooding. The remnants of Florence slowly tracked through the area on the 17th and 18th. Plenty of tropical moisture caused showers and thunderstorms to contain locally heavy rainfall, which led to instances of flooding. The remnants of Florence slowly tracked through the area on the 17th and 18th. Plenty of tropical moisture caused showers and thunderstorms to contain locally heavy rainfall, which led to instances of flooding. The remnants of Florence slowly tracked through the area on the 17th and 18th. Plenty of tropical moisture caused showers and thunderstorms to contain locally heavy rainfall, which led to instances of flooding. The remnants of Florence slowly tracked through the area on the 17th and 18th. Plenty of tropical moisture caused showers and thunderstorms to contain locally heavy rainfall, which led to instances of flooding. The remnants of Florence slowly tracked through the area on the 17th and 18th. Plenty of tropical moisture caused showers and thunderstorms to contain locally heavy rainfall, which led to instances of flooding. The remnants of Florence slowly tracked through the area on the 17th and 18th. Plenty of tropical moisture caused showers and thunderstorms to contain locally heavy rainfall, which led to instances of flooding. The remnants of Florence slowly tracked through the area on the 17th and 18th. Plenty of tropical moisture caused showers and thunderstorms to contain locally heavy rainfall, which led to instances of flooding. The remnants of Florence slowly tracked through the area on the 17th and 18th. Plenty of tropical moisture caused showers and thunderstorms to contain locally heavy rainfall, which led to instances of flooding. The remnants of Florence slowly tracked through the area on the 17th and 18th. Plenty of tropical moisture caused showers and thunderstorms to contain locally heavy rainfall, which led to instances of flooding.\nEvent Narrative: The water level at Whitemarsh Run rapidly surpassed flood stage of 11 feet, cresting at 12.97 feet at 2:15 AM EST on the 18th of September. Town Center Court was flooded, and water covered the parking lots near the stream. Three feet of swift moving water was moving over Hollins Ferry Road near Landsdowne Road. Hill is being washed down the roadway on MD43 at US Route 1. A vehicle was stranded in high water in Golden Ring Plaza. A vehicle was stalled in flowing water over the road on Furnace Avenue near Race road. Deep Run was out of its banks. The USGS stream gage on East Branch Herbert Run near Arbutus rapidly exceeded the 7 foot flood stage during the short period indicated. It rose a foot over flood stage within 20 minutes, peaking at 8.02 feet at 1:35 am EST. Yards near the stream flooded, with water up to the top of the culvert at Sulphur Spring Road. All lanes of MD-197 Laurel Bowie Road were blocked by high water near Montpelier Drive. I-95 northbound was blocked by high water at Exit 50A for US-1 Caton Avenue. A vehicle was stalled in high water on US-40 Pulaski Highway near MD-7 Philadelphia Road. Furnace Avenue was closed due to high water near the Baltimore County line. A car was trapped in high water near the intersection of Race Road and Hanover road. Race Road was closed. The stream gage on Otter Point Creek in Edgewood exceeded the flood stage of 8 feet during the indicated period, flooding Winters Run Road near Singer Road. The peak level of 8.16 feet was observed at 3:15am EST. The stream gage on the Patapsco River at Elkridge exceeded the 16 foot flood stage during the indicated period. Hammonds Ferry Road flooded and was closed at the Patapsco River. Backwater flooding led to the closure of Furnace Avenue in Elkridge. The peak level of 18.72 feet occurred at 3:25 AM. Several vehicles were trapped in high water on MD-197 Laurel Bowie Road. The stream gage on the Patapsco River at Elkridge exceeded the 16 foot flood stage during the indicated period. Hammonds Ferry Road flooded and was closed at the Patapsco River. Backwater flooding led to the closure of Furnace Avenue in Elkridge. The peak level of 16.23 feet occurred at 4:05 PM. The water level at Whitemarsh Run was was above flood stage of 11 feet. Water covered parking lots near the stream, particularly near Town Center Court.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 17.1343 km away, between 2018-09-26 17:32:00 and 2018-09-26 18:05:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front moving into the region combined with with an unstable hot and humid air mass to generate showers and thunderstorms, some of which became severe. A cold front moving into the region combined with with an unstable hot and humid air mass to generate showers and thunderstorms, some of which became severe.\nEvent Narrative: A tree was blown down on MD Route 650 near Haviland Mill Road. A large tree limb was blown down onto a house near the intersection of Burton Road and Baylor Road.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 20.0114 km away, between 2018-09-26 18:00:00 and 2018-09-26 19:24:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front moving into the region combined with with an unstable hot and humid air mass to generate showers and thunderstorms, some of which produced strong winds over the waters. A cold front moving into the region combined with with an unstable hot and humid air mass to generate showers and thunderstorms, some of which produced strong winds over the waters. A cold front moving into the region combined with with an unstable hot and humid air mass to generate showers and thunderstorms, some of which produced strong winds over the waters.\nEvent Narrative: A wind gust of 35 knots was measured at Oriole Park at Camden Yards (BLTPC). A wind gust of up to 34 knots was measured at Annapolis Buoy. A wind gust of up to 34 knots was measured at Hampstead Hill Academy.", "The following events were reported: Flood. These occurred near station USW00093721, approximately 32.742 km away, between 2018-09-28 01:20:00 and 2018-09-29 01:11:00. The flood was caused by Heavy Rain. Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A warm front moved through the area during the morning hours of the 28th. Warm and moist air associated with a tropical air mass overran the relatively cooler air in place, resulting in heavy rainfall. Also, the steering flow aloft was weak so showers and thunderstorms were slow to move. This enhanced the flooding threat. The resulting flooding moved into larger streams and rivers and continued through the 30th. A warm front moved through the area during the morning hours of the 28th. Warm and moist air associated with a tropical air mass overran the relatively cooler air in place, resulting in heavy rainfall. Also, the steering flow aloft was weak so showers and thunderstorms were slow to move. This enhanced the flooding threat. The resulting flooding moved into larger streams and rivers and continued through the 30th. A warm front moved through the area during the morning hours of the 28th. Warm and moist air associated with a tropical air mass overran the relatively cooler air in place, resulting in heavy rainfall. Also, the steering flow aloft was weak so showers and thunderstorms were slow to move. This enhanced the flooding threat. The resulting flooding moved into larger streams and rivers and continued through the 30th. A warm front moved through the area during the morning hours of the 28th. Warm and moist air associated with a tropical air mass overran the relatively cooler air in place, resulting in heavy rainfall. Also, the steering flow aloft was weak so showers and thunderstorms were slow to move. This enhanced the flooding threat. The resulting flooding moved into larger streams and rivers and continued through the 30th. A warm front moved through the area during the morning hours of the 28th. Warm and moist air associated with a tropical air mass overran the relatively cooler air in place, resulting in heavy rainfall. Also, the steering flow aloft was weak so showers and thunderstorms were slow to move. This enhanced the flooding threat. The resulting flooding moved into larger streams and rivers and continued through the 30th.\nEvent Narrative: The EM reported Brighton Dam Road closed due to flooding near New Hampshire Avenue. The water levels at Gunpowder Falls at Glencoe surpassed flood stage of 7 feet. The water levels crested at 8.47 feet at 6:00 AM September 28th. ||Portions of Upper Glencoe Road and Lower Glencoe Road began to flood. The stream gauge on the Patapsco River at Elkridge exceeded the 16 foot flood stage during the indicated period. Hammonds Ferry Road flooded and was closed at the Patapsco River. Backwater flooding led to the closure of Furnace Avenue in Elkridge. The peak level of 20.29 feet occurred at 10:40 AM on the 28th. Woodbine Road was closed at Morgan-Woodbine Road due to flooding. The 3000 Block of Hofmann Mill Road was closed due to flooding.", "The following events were reported: Flash Flood. These occurred near station USW00093721, approximately 41.2465 km away, between 2018-10-12 00:35:00 and 2018-10-12 01:35:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Rainfall totals of 3 to 5 inches fell in parts of northeastern Maryland, Delaware, and southern and central New Jersey on the night of October 11. There were a few reports of rainfall amounts in excess of 5 inches. Rainfall totals of 3 to 5 inches fell in parts of northeastern Maryland, Delaware, and southern and central New Jersey on the night of October 11. There were a few reports of rainfall amounts in excess of 5 inches.\nEvent Narrative: Sections of Maryland Route 8 in Romancoke were closed due to flooding. Maryland Route 20 was closed near Rock Hall in the vicinity of Crosby Road due to flooding.", "The following events were reported: Flood. These occurred near station USW00093721, approximately 20.6037 km away, between 2018-10-12 03:10:00 and 2018-10-12 05:10:00. The flood was caused by Heavy Rain. Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: After Hurricane Michael made landfall near Mexico Beach, Florida with maximum sustained winds of 155 mph and minimum central pressure of 919 mb on Wednesday October 10th, it weakened to a tropical storm as it tracked northeastward through Georgia and South Carolina. The tropical storm then tracked across North Carolina and southeast Virginia Thursday and Thursday night, October 11th, emerging back into the Atlantic Ocean early Friday morning, October 12th. As the system passed south of the region, heavy rain then caused instances of flooding, and strong winds brought down trees. Across Maryland, maximum sustained winds reached 38 mph, peak wind gusts reached 62 mph, and some rainfall totals were observed in excess of 6 inches.\nEvent Narrative: MD-450 Defense Highway was closed due to flooding near Huntwood Drive.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 35.2109 km away, between 2018-10-15 23:16:00 and 2018-10-15 23:59:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front passed across the waters during the evening and overnight hours of October 15th-16th. A band of showers and isolated thunderstorms along the front produced gusty winds across portions of the waters. A cold front passed across the waters during the evening and overnight hours of October 15th-16th. A band of showers and isolated thunderstorms along the front produced gusty winds across portions of the waters.\nEvent Narrative: A wind gust of up to 34 knots was measured at Tolly Point. A wind gust of 35 knots was measured at Thomas Point.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 28.2364 km away, between 2018-10-20 20:54:00 and 2018-10-20 23:00:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front passed across the waters during the evening hours of October 20th. A band of showers and isolated thunderstorms along the front produced gusty winds across portions of the waters. A cold front passed across the waters during the evening hours of October 20th. A band of showers and isolated thunderstorms along the front produced gusty winds across portions of the waters. A cold front passed across the waters during the evening hours of October 20th. A band of showers and isolated thunderstorms along the front produced gusty winds across portions of the waters. A cold front passed across the waters during the evening hours of October 20th. A band of showers and isolated thunderstorms along the front produced gusty winds across portions of the waters. A cold front passed across the waters during the evening hours of October 20th. A band of showers and isolated thunderstorms along the front produced gusty winds across portions of the waters. A cold front passed across the waters during the evening hours of October 20th. A band of showers and isolated thunderstorms along the front produced gusty winds across portions of the waters. A cold front passed across the waters during the evening hours of October 20th. A band of showers and isolated thunderstorms along the front produced gusty winds across portions of the waters. A cold front passed across the waters during the evening hours of October 20th. A band of showers and isolated thunderstorms along the front produced gusty winds across portions of the waters. A cold front passed across the waters during the evening hours of October 20th. A band of showers and isolated thunderstorms along the front produced gusty winds across portions of the waters. A cold front passed across the waters during the evening hours of October 20th. A band of showers and isolated thunderstorms along the front produced gusty winds across portions of the waters. A cold front passed across the waters during the evening hours of October 20th. A band of showers and isolated thunderstorms along the front produced gusty winds across portions of the waters. A cold front passed across the waters during the evening hours of October 20th. A band of showers and isolated thunderstorms along the front produced gusty winds across portions of the waters. A cold front passed across the waters during the evening hours of October 20th. A band of showers and isolated thunderstorms along the front produced gusty winds across portions of the waters. A cold front passed across the waters during the evening hours of October 20th. A band of showers and isolated thunderstorms along the front produced gusty winds across portions of the waters. A cold front passed across the waters during the evening hours of October 20th. A band of showers and isolated thunderstorms along the front produced gusty winds across portions of the waters. A cold front passed across the waters during the evening hours of October 20th. A band of showers and isolated thunderstorms along the front produced gusty winds across portions of the waters. A cold front passed across the waters during the evening hours of October 20th. A band of showers and isolated thunderstorms along the front produced gusty winds across portions of the waters. A cold front passed across the waters during the evening hours of October 20th. A band of showers and isolated thunderstorms along the front produced gusty winds across portions of the waters. A cold front passed across the waters during the evening hours of October 20th. A band of showers and isolated thunderstorms along the front produced gusty winds across portions of the waters. A cold front passed across the waters during the evening hours of October 20th. A band of showers and isolated thunderstorms along the front produced gusty winds across portions of the waters. A cold front passed across the waters during the evening hours of October 20th. A band of showers and isolated thunderstorms along the front produced gusty winds across portions of the waters.\nEvent Narrative: A wind gust of 42 knots was measured at the Baltimore Key Bridge. A wind gust of up to 34 knots was measured in Baltimore. A wind gust of 37 knots was measured at Lakeland Elementary School. A wind gust of 36 knots was measured at Hampstead Hill Academy. A wind gust of 40 knots was measured at Gunpowder. A wind gust of up to 34 knots was measured at Greenbury Point. A wind gust of up to 34 knots was measured at the Maryland Science Center. A wind gust of 39 knots was measured at Tolly Point. A wind gust of 40 knots was measured at Greenbury Point. A wind gust of 35 knots was measured at Kent Island. A wind gust of 42 knots was measured at Hart Miller Island. A wind gust of 40 knots was measured at Tolchester. A wind gust of up to 34 knots was measured at Martin State Airport. A wind gust of up to 34 knots was measured at Annapolis. A wind gust of 40 knots was measured at Thomas Point. A wind gust of 38 knots was measured at the US Naval Academy. A wind gust of 34 knots was measured at Hart Miller Island. A wind gust of up to 34 knots was measured at Tolchester. A wind gust of up to 34 knots was measured at Stevensville. A wind gust of 35 knots was measured at Thomas Point. A wind gust of 36 knots was measured at Camden Yards.", "The following events were reported: Thunderstorm Wind, Tornado. These occurred near station USW00093721, approximately 33.3056 km away, between 2018-11-02 19:18:00 and 2018-11-02 20:48:00.The events resulted in 1 injuries and 2 fatalities. The events caused property damage valued at 915000.0 and crop damage of 0.0. \n\nEpisode Narrative: A dynamic low pressure system tracked through the Mid-Atlantic states on the evening of November 2nd. A squall line developed along the cold front, and while instability was limited, deep and low level shear were strong enough to support the development of a quasi-linear convective system. The most intense portions of the system were able to generate localized severe damaging winds and tornadoes. A dynamic low pressure system tracked through the Mid-Atlantic states on the evening of November 2nd. A squall line developed along the cold front, and while instability was limited, deep and low level shear were strong enough to support the development of a quasi-linear convective system. The most intense portions of the system were able to generate localized severe damaging winds and tornadoes. A dynamic low pressure system tracked through the Mid-Atlantic states on the evening of November 2nd. A squall line developed along the cold front, and while instability was limited, deep and low level shear were strong enough to support the development of a quasi-linear convective system. The most intense portions of the system were able to generate localized severe damaging winds and tornadoes. A dynamic low pressure system tracked through the Mid-Atlantic states on the evening of November 2nd. A squall line developed along the cold front, and while instability was limited, deep and low level shear were strong enough to support the development of a quasi-linear convective system. The most intense portions of the system were able to generate localized severe damaging winds and tornadoes. A dynamic low pressure system tracked through the Mid-Atlantic states on the evening of November 2nd. A squall line developed along the cold front, and while instability was limited, deep and low level shear were strong enough to support the development of a quasi-linear convective system. The most intense portions of the system were able to generate localized severe damaging winds and tornadoes. A dynamic low pressure system tracked through the Mid-Atlantic states on the evening of November 2nd. A squall line developed along the cold front, and while instability was limited, deep and low level shear were strong enough to support the development of a quasi-linear convective system. The most intense portions of the system were able to generate localized severe damaging winds and tornadoes. A dynamic low pressure system tracked through the Mid-Atlantic states on the evening of November 2nd. A squall line developed along the cold front, and while instability was limited, deep and low level shear were strong enough to support the development of a quasi-linear convective system. The most intense portions of the system were able to generate localized severe damaging winds and tornadoes. A dynamic low pressure system tracked through the Mid-Atlantic states on the evening of November 2nd. A squall line developed along the cold front, and while instability was limited, deep and low level shear were strong enough to support the development of a quasi-linear convective system. The most intense portions of the system were able to generate localized severe damaging winds and tornadoes.\nEvent Narrative: Multiple power lines were downed near the intersection of Ten Oaks Road and Linden Church Road. A tree was also blown down in the 7000 block of Mink Hollow Road. Trees were blown down on Pleasantville Road. A large tree was blown down across the road near the 1200 block of Marriottsville Road. A tornado touched down in extreme northwestern Howard County, Maryland, approximately 1 mile south of Interstate 70/US-40/Baltimore National Pike at 8:19 PM EDT. Several wooden power poles were snapped along Penn Shop Road just east of MD-27/Ridge Road, indicative of winds over 100 MPH. The path continued northeastward into Carroll County. A tornado touched down in Baltimore City at about 9:42 PM EDT on Friday evening, November 2, 2018. Initial damage was to a tractor trailer which was blown over on Interstate 95 just north of the Fort McHenry Tunnel. A few trees were topped just west of the interstate, and a fence line blew over on South Newkirk Street just to the east. This damage is consistent with winds of about 70 MPH.||The tornado tracked generally eastward roughly parallel to Holabird Avenue. It blew in large garage doors on both side of the building at Flexi-Van Leasing facility, consistent with wind speeds over 90 MPH.||As it continued eastward, it impacted the north building of the Amazon sorting facility, reaching a peak intensity of around 105 MPH. It blew the roof off a portion of the building, including iron rafters. With the loss of the roof, the eight inch concrete wall panels pushed in and collapsed into the building towards the north end of the west wall. Two fatalities occurred inside the building with the wall collapse. About a dozen truck trailers were pushed over, moved, or rolled by the wind. Two of the trailers were noted to have been blown in an opposite direction of the wind that toppled the wall. Several light stanchions and signs were blown over, and several car windows were blown out by flying debris. Radar data from the FAA's Terminal Doppler Weather Radar near Baltimore-Washington International Thurgood Marshall Airport indicated this was around 9:43 PM EDT, and this is when the strongest velocity signature was noted.||The tornado continued east along the south side of Holabird Avenue, uprooting several large trees, and snapping dozens of large branches, consistent with winds of about 80 MPH.||Damage along the entire path was mainly convergent, and while much of the damage was from west-southwest to east-northeast, there were several notable exceptions of damage in differing directions. An eyewitness fire fighter outside the Baltimore City Fire Department Engine 50 firehouse in the area saw the swirling debris and funnel cloud as it passed. The tornado lifted as it reached the intersection with Dundalk Avenue, which according to radar would have been at about 9:44 PM EDT. A tornado moved northeastward from Howard County and entered Carroll County around 8:20 PM EDT on the evening of November 2nd. Several trees were downed along Bennett Road. Numerous trees were downed in the Pheasant Ridge community just south of MD-144/Frederick Road, and several mobile homes were heavily damaged. Several power poles were snapped along MD-144/Frederick Road.||As the tornado crossed Interstate 70/US-40/Baltimore National Pike, numerous trees and branches were downed in the roadway and on vehicles, which appeared to have been pulled off the roadway by the winds. No injuries were reported.||The tornado proceeded to move into the retail area of Mt. Airy, where a canopy over the gas pumps at High's Dairy Store was partially torn off, and the TJ Maxx roof was lifted up and partially removed. There were also numerous trees snapped and uprooted in a convergent manner behind the shopping center to near the Mt. Airy water tower. In the immediate path, virtually no trees were left undamaged, indicative of winds over 100 MPH.||The tornado continued northward from this point, where several outbuildings at the Knills Farm Market just east of MD-27/Ridge Road were severely damaged or completely destroyed, including a metal silo which twisted and collapsed. Nearby along Watersville Road, several more power poles were snapped purely from wind (not from trees falling on power lines). On either side of the farm, virtually all trees in the tornado's path were downed in a convergent manner, including at a residence along Watersville Road, with some showing signs of bark being stripped by the wind. This was one area where maximum winds are estimated to have been near 120 mph.||The tornado continued northeastward, with several residences experiencing shingle and roof damage/removal along Arrowwood Circle, and downed numerous trees and power lines, consistent with winds around 90 MPH.||Numerous hardwood trees, virtually all in the tornado's path, were snapped with signs of stripped bark along the 6000 block of Runkles Road. At Snell's Greenhouses, water was completely removed from a pond, and several greenhouses were destroyed. A nearby home weather station in the tornado's path just to the northeast measured a wind gust of 112 mph. Based on this, it is likely the tornado's maximum winds again approached 120 mph in this area. This occurred at around 825 PM EDT, when the FAA's Terminal Doppler Weather Radar near Washington Dulles International Airport showed it's strongest rotational signature.||The last evidence of tornadic damage was observed on Gillis Falls Road where a few trees were uprooted in convergent fashion just east of Runkles Road. Radar imagery from the FAA's Terminal Doppler Weather Radar near Washington Dulles International Airport showed the tornadic velocity couplet dissipate just north of Gillis Ford Road at about 826 PM EDT.||The damage estimate was provided by Carroll County Emergency Management. A sign and gazebo were damaged at Lu and Joe's Restaurant. Multiple trees were also down near the 19000 block of Windsor Forest Road. A tornado tracked eastward from Baltimore City into southern Baltimore County near the city of Dundalk, around 9:44 PM EDT. After it initially lifted, the tornado briefly touched down one last time at the Holabird East Apartments on 4 Georges Court in Dundalk. The two adjoined northeast buildings in the complex sustained significant roofing damage, with a large portion of the roof decking removed from the windward side. The building was deemed uninhabitable displacing 42 people. The strong southwest wind hit the building broadside causing the damage. No other damage was noted in the area. A resident reported swirling winds with the event. One resident in the building was treated for cuts. This was the last area of damage, and the tornado signature on radar weakened after this point just after 9:45 PM EDT. The monetary damage is an estimate provided by the county emergency management office.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 28.8513 km away, between 2018-11-02 20:48:00 and 2018-11-02 22:00:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A dynamic low pressure system tracked through the Mid-Atlantic states on the evening of November 2nd. A squall line developed along the cold front, and while instability was limited, deep and low level shear were strong enough to support the development of a quasi-linear convective system. This produced gusty winds across the waters. A dynamic low pressure system tracked through the Mid-Atlantic states on the evening of November 2nd. A squall line developed along the cold front, and while instability was limited, deep and low level shear were strong enough to support the development of a quasi-linear convective system. This produced gusty winds across the waters. A dynamic low pressure system tracked through the Mid-Atlantic states on the evening of November 2nd. A squall line developed along the cold front, and while instability was limited, deep and low level shear were strong enough to support the development of a quasi-linear convective system. This produced gusty winds across the waters. A dynamic low pressure system tracked through the Mid-Atlantic states on the evening of November 2nd. A squall line developed along the cold front, and while instability was limited, deep and low level shear were strong enough to support the development of a quasi-linear convective system. This produced gusty winds across the waters. A dynamic low pressure system tracked through the Mid-Atlantic states on the evening of November 2nd. A squall line developed along the cold front, and while instability was limited, deep and low level shear were strong enough to support the development of a quasi-linear convective system. This produced gusty winds across the waters. A dynamic low pressure system tracked through the Mid-Atlantic states on the evening of November 2nd. A squall line developed along the cold front, and while instability was limited, deep and low level shear were strong enough to support the development of a quasi-linear convective system. This produced gusty winds across the waters. A dynamic low pressure system tracked through the Mid-Atlantic states on the evening of November 2nd. A squall line developed along the cold front, and while instability was limited, deep and low level shear were strong enough to support the development of a quasi-linear convective system. This produced gusty winds across the waters. A dynamic low pressure system tracked through the Mid-Atlantic states on the evening of November 2nd. A squall line developed along the cold front, and while instability was limited, deep and low level shear were strong enough to support the development of a quasi-linear convective system. This produced gusty winds across the waters.\nEvent Narrative: A wind gust of 37 knots was measured at Hart Miller Island. A wind gust of up to 34 knots was observed at Tolchester. A wind gust of up to 34 knots was observed at Greenbury Point. A wind gust of 41 knots was measured at Tolly Point. A wind gust of 35 knots was measured at the Francis Scott Key Bridge. A wind gust of 38 knots was measured at Thomas Point. A wind gust of up to 34 knots was observed at Gunpowder. A wind gust of 34 knots was measured at Oriole Park.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 36.8144 km away, between 2018-11-06 09:59:00 and 2018-11-06 12:00:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Mild and moist air with limited instability moved across the region ahead of an eastward moving cold front. This combined with high amounts of wind shear to create a squall line that moved across the waters, producing gusty winds. Mild and moist air with limited instability moved across the region ahead of an eastward moving cold front. This combined with high amounts of wind shear to create a squall line that moved across the waters, producing gusty winds. Mild and moist air with limited instability moved across the region ahead of an eastward moving cold front. This combined with high amounts of wind shear to create a squall line that moved across the waters, producing gusty winds. Mild and moist air with limited instability moved across the region ahead of an eastward moving cold front. This combined with high amounts of wind shear to create a squall line that moved across the waters, producing gusty winds.\nEvent Narrative: A wind gust of 40 knots was measured at Thomas Point. A wind gust of up to 34 knots was observed at Kent Island. A wind gust of up to 34 knots was observed at Greenbury Point. A wind gust of up to 34 knots was observed at Tolchester.", "The following events were reported: Flood. These occurred near station USW00093721, approximately 28.0565 km away, between 2018-11-24 19:36:00 and 2018-11-25 05:42:00. The flood was caused by Heavy Rain. Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A negatively tilted trough approached the area on the 24th as surface low pressure tracked up toward the Great Lakes and secondary low pressure formed along the Carolina Coast. Lift ahead of the negatively tilted trough/within the left exit region of an upper-level jet streak led to a period of moderate to heavy rain through much of the day on the 24th. Rainfall totals were generally between 1-2 inches across the area, resulting in many instances of flooding. A negatively tilted trough approached the area on the 24th as surface low pressure tracked up toward the Great Lakes and secondary low pressure formed along the Carolina Coast. Lift ahead of the negatively tilted trough/within the left exit region of an upper-level jet streak led to a period of moderate to heavy rain through much of the day on the 24th. Rainfall totals were generally between 1-2 inches across the area, resulting in many instances of flooding. A negatively tilted trough approached the area on the 24th as surface low pressure tracked up toward the Great Lakes and secondary low pressure formed along the Carolina Coast. Lift ahead of the negatively tilted trough/within the left exit region of an upper-level jet streak led to a period of moderate to heavy rain through much of the day on the 24th. Rainfall totals were generally between 1-2 inches across the area, resulting in many instances of flooding. A negatively tilted trough approached the area on the 24th as surface low pressure tracked up toward the Great Lakes and secondary low pressure formed along the Carolina Coast. Lift ahead of the negatively tilted trough/within the left exit region of an upper-level jet streak led to a period of moderate to heavy rain through much of the day on the 24th. Rainfall totals were generally between 1-2 inches across the area, resulting in many instances of flooding. A negatively tilted trough approached the area on the 24th as surface low pressure tracked up toward the Great Lakes and secondary low pressure formed along the Carolina Coast. Lift ahead of the negatively tilted trough/within the left exit region of an upper-level jet streak led to a period of moderate to heavy rain through much of the day on the 24th. Rainfall totals were generally between 1-2 inches across the area, resulting in many instances of flooding. A negatively tilted trough approached the area on the 24th as surface low pressure tracked up toward the Great Lakes and secondary low pressure formed along the Carolina Coast. Lift ahead of the negatively tilted trough/within the left exit region of an upper-level jet streak led to a period of moderate to heavy rain through much of the day on the 24th. Rainfall totals were generally between 1-2 inches across the area, resulting in many instances of flooding. A negatively tilted trough approached the area on the 24th as surface low pressure tracked up toward the Great Lakes and secondary low pressure formed along the Carolina Coast. Lift ahead of the negatively tilted trough/within the left exit region of an upper-level jet streak led to a period of moderate to heavy rain through much of the day on the 24th. Rainfall totals were generally between 1-2 inches across the area, resulting in many instances of flooding.\nEvent Narrative: Car stranded in floodwaters on Brighton Dam Road at the Hawlings River. The stream gage on the Little Patuxent River at Savage exceeded the flood stage of 10 feet during the indicated period. Riverside trains began to flood, and water approached fields off of Bald Eagle Drive, as well as Brock Bridge Road. The peak level of 10.59 feet occurred at 11:00 PM on the 24th. Car stranded in high water near the intersection of Volunteer Drive and Olney-Laytonsville Road. Road closed due to flooding at intersection of Route 108 and Woodland Road. The stream gage on the Patapsco River at Elkridge (ERDM2) exceeded the 15 foot flood stage during the indicated period, leading to flooding along River Road in Patapsco Valley State Park. Large portions of the park also flooded near the playground off Gunn Road. The peak level of 15.3 feet occurred at 1:45 AM on the 25th. The stream gage on Gunpowder Falls at Glencoe exceeded the flood stage of 7 feet during the indicated time period, leading to flooding on portions of Upper Glencoe Road, Lower Glencoe Road, Sparks Road and Home Road. Additionally, water began to enter buildings off of Sparks Road. The peak level of 10.74 feet occurred at 12:15 AM on the 25th. The stream gage on Otter Point Creek at Edgewood exceeded the 8 foot flood stage during the indicated period, leading to flooding along Winters Run Road near Singer Road. The peak level of 8.38 feet occurred at 10:15 PM on the 24th.", "The following events were reported: Flood. These occurred near station USW00093721, approximately 22.6529 km away, between 2018-12-15 19:01:00 and 2018-12-16 19:46:00. The flood was caused by Heavy Rain. Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A potent upper-level low and associated area of surface low pressure approached the region from southwest on the 15th. Strong forcing for ascent and ample moisture transport in advance of the upper-level low led to a prolonged period of rain across the region. Eventually low pressure transferred to the coast before precipitation wound down on the 16th. Widespread rainfall totals of 2-4 inches were observed across the area. A potent upper-level low and associated area of surface low pressure approached the region from southwest on the 15th. Strong forcing for ascent and ample moisture transport in advance of the upper-level low led to a prolonged period of rain across the region. Eventually low pressure transferred to the coast before precipitation wound down on the 16th. Widespread rainfall totals of 2-4 inches were observed across the area. A potent upper-level low and associated area of surface low pressure approached the region from southwest on the 15th. Strong forcing for ascent and ample moisture transport in advance of the upper-level low led to a prolonged period of rain across the region. Eventually low pressure transferred to the coast before precipitation wound down on the 16th. Widespread rainfall totals of 2-4 inches were observed across the area. A potent upper-level low and associated area of surface low pressure approached the region from southwest on the 15th. Strong forcing for ascent and ample moisture transport in advance of the upper-level low led to a prolonged period of rain across the region. Eventually low pressure transferred to the coast before precipitation wound down on the 16th. Widespread rainfall totals of 2-4 inches were observed across the area. A potent upper-level low and associated area of surface low pressure approached the region from southwest on the 15th. Strong forcing for ascent and ample moisture transport in advance of the upper-level low led to a prolonged period of rain across the region. Eventually low pressure transferred to the coast before precipitation wound down on the 16th. Widespread rainfall totals of 2-4 inches were observed across the area. A potent upper-level low and associated area of surface low pressure approached the region from southwest on the 15th. Strong forcing for ascent and ample moisture transport in advance of the upper-level low led to a prolonged period of rain across the region. Eventually low pressure transferred to the coast before precipitation wound down on the 16th. Widespread rainfall totals of 2-4 inches were observed across the area. A potent upper-level low and associated area of surface low pressure approached the region from southwest on the 15th. Strong forcing for ascent and ample moisture transport in advance of the upper-level low led to a prolonged period of rain across the region. Eventually low pressure transferred to the coast before precipitation wound down on the 16th. Widespread rainfall totals of 2-4 inches were observed across the area. A potent upper-level low and associated area of surface low pressure approached the region from southwest on the 15th. Strong forcing for ascent and ample moisture transport in advance of the upper-level low led to a prolonged period of rain across the region. Eventually low pressure transferred to the coast before precipitation wound down on the 16th. Widespread rainfall totals of 2-4 inches were observed across the area. A potent upper-level low and associated area of surface low pressure approached the region from southwest on the 15th. Strong forcing for ascent and ample moisture transport in advance of the upper-level low led to a prolonged period of rain across the region. Eventually low pressure transferred to the coast before precipitation wound down on the 16th. Widespread rainfall totals of 2-4 inches were observed across the area. A potent upper-level low and associated area of surface low pressure approached the region from southwest on the 15th. Strong forcing for ascent and ample moisture transport in advance of the upper-level low led to a prolonged period of rain across the region. Eventually low pressure transferred to the coast before precipitation wound down on the 16th. Widespread rainfall totals of 2-4 inches were observed across the area.\nEvent Narrative: The stream gage on Gunpowder Falls at Glencoe exceeded the 7 foot flood stage during the indicated period. Flooding occurred along portions of Upper Glencoe Road and Lower Glencoe Road. The peak level of 7.76 feet occurred at 5:45 AM on December 16th. The river gage on the Patspsco River at Elkridge exceeded the 15 foot flood stage during the indicated period. Water covered a portion of River Road in Patapsco Valley State Park, and large portions of the park were flooded near the playground off Gunn Road. The peak level of 16.80 feet occurred at 5:50 AM on December 16th. The river gage on the Little Patuxent River at Savage exceeded the 10 foot flood stage during the indicated period. Riverside trails were flooded. Additionally, water approached Brock Bridge Road, as well as fields off of Bald Eagle Drive. The peak level of 12.27 feet occurred at 4:45 AM on December 16th. Water rescue on Brighton Dam Road near Bordly Drive. Road closed, with 1.5 feet of water flowing across roadway. Georgia Avenue closed near Brookeville Road due to flooding. Brighton Dam Road closed due to flooding. Harriet Tubman Lane was closed due to flooding. Furnace Avenue was closed due to flooding. The stream gage on the Patuxent River below Duckett Dam near Laurel exceeded the 9.5 foot flood stage during the indicated period. Water overflowed the banks into nearby park land. The peak level of 9.65 feet occurred at 6:45 PM. Zion Road was closed in both direction at Gregg Road due to high water.", "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00093721, approximately 46.0285 km away, between 2018-12-21 16:48:00 and 2018-12-21 17:08:00. The events included records with hailstones measuring 33.666666666666664 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A surface low tracked northeastward through the Appalachians as a potent jetstreak in the upper levels shifted northward. Unseasonably warm and moist air was transported northward and this, in combination with colder air moving in at the mid-levels, caused the|atmosphere to destabilize, resulting in showers and thunderstorms. A few of these storms became locally severe. A surface low tracked northeastward through the Appalachians as a potent jetstreak in the upper levels shifted northward. Unseasonably warm and moist air was transported northward and this, in combination with colder air moving in at the mid-levels, caused the|atmosphere to destabilize, resulting in showers and thunderstorms. A few of these storms became locally severe. A surface low tracked northeastward through the Appalachians as a potent jetstreak in the upper levels shifted northward. Unseasonably warm and moist air was transported northward and this, in combination with colder air moving in at the mid-levels, caused the|atmosphere to destabilize, resulting in showers and thunderstorms. A few of these storms became locally severe.\nEvent Narrative: Quarter size hail was reported on the southeast side of Westminster. A tree was blown down near the intersection of Bill Moxley Road and Autumn Crest Drive. A tree was blown down near the intersection of Gillis Falls Road and Davis Road.", "The following events were reported: Flood. These occurred near station USW00093721, approximately 35.2667 km away, between 2019-01-24 13:56:00 and 2019-01-24 16:57:00. The flood was caused by Heavy Rain. Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A prolonged period of rain in a warm advection regime ahead of an approaching cold front led to 1-2 inches of rain across portions of Maryland. This resulted in isolated instances of flooding on the 24th.\nEvent Narrative: Zion Road closed due to flooding of the Hawlings River. Water depth on road of about one foot.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 46.5866 km away, between 2019-03-15 18:28:00 and 2019-03-15 18:28:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A surface cold front crossed the region during the afternoon and evening hours as mild southerly flow increased out ahead of it. This led to the development of some minor instability across the central and eastern portions of Maryland, and this, when combined with the frontal boundary and strong mid level winds, was enough to generate showers and thunderstorms, one of which became severe.\nEvent Narrative: A tree was blown down with wires blocking both sides of the bridge in the 1700 block of Carrs Mill Road. Additionally, a tree was also blown down onto a vehicle near the intersection of Wildwood Drive and Wild Orchard Drive. The car was unoccupied at the time.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 21.461 km away, between 2019-03-15 19:45:00 and 2019-03-15 20:00:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A surface cold front crossed the region during the afternoon and evening hours as mild southerly flow increased out ahead of it. This led to the development of some minor instability across the area, and this, when combined with the frontal boundary and strong mid level winds, was enough to generate showers and thunderstorms, some of which produced gusty winds over the waters. A surface cold front crossed the region during the afternoon and evening hours as mild southerly flow increased out ahead of it. This led to the development of some minor instability across the area, and this, when combined with the frontal boundary and strong mid level winds, was enough to generate showers and thunderstorms, some of which produced gusty winds over the waters.\nEvent Narrative: A wind gust of up to 34 knots was observed at Martin State Airport. A wind gust of 34 knots was measured near the Baltimore Francis Scott Key Bridge.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 28.8456 km away, between 2019-03-22 14:35:00 and 2019-03-22 18:00:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A potent upper level trough as well as a surface cold front crossed the region during the afternoon of March 22nd. Out ahead of the trough, surface heating and cold upper levels were able to generate marginal amounts of surface instability. This was enough to generate scattered showers and a few thunderstorms as the front and trough passed across the area. Steep low level lapse rates and low freezing levels allowed for some of these thunderstorms to produce gusty winds over the waters. A potent upper level trough as well as a surface cold front crossed the region during the afternoon of March 22nd. Out ahead of the trough, surface heating and cold upper levels were able to generate marginal amounts of surface instability. This was enough to generate scattered showers and a few thunderstorms as the front and trough passed across the area. Steep low level lapse rates and low freezing levels allowed for some of these thunderstorms to produce gusty winds over the waters. A potent upper level trough as well as a surface cold front crossed the region during the afternoon of March 22nd. Out ahead of the trough, surface heating and cold upper levels were able to generate marginal amounts of surface instability. This was enough to generate scattered showers and a few thunderstorms as the front and trough passed across the area. Steep low level lapse rates and low freezing levels allowed for some of these thunderstorms to produce gusty winds over the waters. A potent upper level trough as well as a surface cold front crossed the region during the afternoon of March 22nd. Out ahead of the trough, surface heating and cold upper levels were able to generate marginal amounts of surface instability. This was enough to generate scattered showers and a few thunderstorms as the front and trough passed across the area. Steep low level lapse rates and low freezing levels allowed for some of these thunderstorms to produce gusty winds over the waters. A potent upper level trough as well as a surface cold front crossed the region during the afternoon of March 22nd. Out ahead of the trough, surface heating and cold upper levels were able to generate marginal amounts of surface instability. This was enough to generate scattered showers and a few thunderstorms as the front and trough passed across the area. Steep low level lapse rates and low freezing levels allowed for some of these thunderstorms to produce gusty winds over the waters. A potent upper level trough as well as a surface cold front crossed the region during the afternoon of March 22nd. Out ahead of the trough, surface heating and cold upper levels were able to generate marginal amounts of surface instability. This was enough to generate scattered showers and a few thunderstorms as the front and trough passed across the area. Steep low level lapse rates and low freezing levels allowed for some of these thunderstorms to produce gusty winds over the waters. A potent upper level trough as well as a surface cold front crossed the region during the afternoon of March 22nd. Out ahead of the trough, surface heating and cold upper levels were able to generate marginal amounts of surface instability. This was enough to generate scattered showers and a few thunderstorms as the front and trough passed across the area. Steep low level lapse rates and low freezing levels allowed for some of these thunderstorms to produce gusty winds over the waters. A potent upper level trough as well as a surface cold front crossed the region during the afternoon of March 22nd. Out ahead of the trough, surface heating and cold upper levels were able to generate marginal amounts of surface instability. This was enough to generate scattered showers and a few thunderstorms as the front and trough passed across the area. Steep low level lapse rates and low freezing levels allowed for some of these thunderstorms to produce gusty winds over the waters. A potent upper level trough as well as a surface cold front crossed the region during the afternoon of March 22nd. Out ahead of the trough, surface heating and cold upper levels were able to generate marginal amounts of surface instability. This was enough to generate scattered showers and a few thunderstorms as the front and trough passed across the area. Steep low level lapse rates and low freezing levels allowed for some of these thunderstorms to produce gusty winds over the waters. A potent upper level trough as well as a surface cold front crossed the region during the afternoon of March 22nd. Out ahead of the trough, surface heating and cold upper levels were able to generate marginal amounts of surface instability. This was enough to generate scattered showers and a few thunderstorms as the front and trough passed across the area. Steep low level lapse rates and low freezing levels allowed for some of these thunderstorms to produce gusty winds over the waters. A potent upper level trough as well as a surface cold front crossed the region during the afternoon of March 22nd. Out ahead of the trough, surface heating and cold upper levels were able to generate marginal amounts of surface instability. This was enough to generate scattered showers and a few thunderstorms as the front and trough passed across the area. Steep low level lapse rates and low freezing levels allowed for some of these thunderstorms to produce gusty winds over the waters. A potent upper level trough as well as a surface cold front crossed the region during the afternoon of March 22nd. Out ahead of the trough, surface heating and cold upper levels were able to generate marginal amounts of surface instability. This was enough to generate scattered showers and a few thunderstorms as the front and trough passed across the area. Steep low level lapse rates and low freezing levels allowed for some of these thunderstorms to produce gusty winds over the waters. A potent upper level trough as well as a surface cold front crossed the region during the afternoon of March 22nd. Out ahead of the trough, surface heating and cold upper levels were able to generate marginal amounts of surface instability. This was enough to generate scattered showers and a few thunderstorms as the front and trough passed across the area. Steep low level lapse rates and low freezing levels allowed for some of these thunderstorms to produce gusty winds over the waters. A potent upper level trough as well as a surface cold front crossed the region during the afternoon of March 22nd. Out ahead of the trough, surface heating and cold upper levels were able to generate marginal amounts of surface instability. This was enough to generate scattered showers and a few thunderstorms as the front and trough passed across the area. Steep low level lapse rates and low freezing levels allowed for some of these thunderstorms to produce gusty winds over the waters. A potent upper level trough as well as a surface cold front crossed the region during the afternoon of March 22nd. Out ahead of the trough, surface heating and cold upper levels were able to generate marginal amounts of surface instability. This was enough to generate scattered showers and a few thunderstorms as the front and trough passed across the area. Steep low level lapse rates and low freezing levels allowed for some of these thunderstorms to produce gusty winds over the waters. A potent upper level trough as well as a surface cold front crossed the region during the afternoon of March 22nd. Out ahead of the trough, surface heating and cold upper levels were able to generate marginal amounts of surface instability. This was enough to generate scattered showers and a few thunderstorms as the front and trough passed across the area. Steep low level lapse rates and low freezing levels allowed for some of these thunderstorms to produce gusty winds over the waters. A potent upper level trough as well as a surface cold front crossed the region during the afternoon of March 22nd. Out ahead of the trough, surface heating and cold upper levels were able to generate marginal amounts of surface instability. This was enough to generate scattered showers and a few thunderstorms as the front and trough passed across the area. Steep low level lapse rates and low freezing levels allowed for some of these thunderstorms to produce gusty winds over the waters. A potent upper level trough as well as a surface cold front crossed the region during the afternoon of March 22nd. Out ahead of the trough, surface heating and cold upper levels were able to generate marginal amounts of surface instability. This was enough to generate scattered showers and a few thunderstorms as the front and trough passed across the area. Steep low level lapse rates and low freezing levels allowed for some of these thunderstorms to produce gusty winds over the waters. A potent upper level trough as well as a surface cold front crossed the region during the afternoon of March 22nd. Out ahead of the trough, surface heating and cold upper levels were able to generate marginal amounts of surface instability. This was enough to generate scattered showers and a few thunderstorms as the front and trough passed across the area. Steep low level lapse rates and low freezing levels allowed for some of these thunderstorms to produce gusty winds over the waters. A potent upper level trough as well as a surface cold front crossed the region during the afternoon of March 22nd. Out ahead of the trough, surface heating and cold upper levels were able to generate marginal amounts of surface instability. This was enough to generate scattered showers and a few thunderstorms as the front and trough passed across the area. Steep low level lapse rates and low freezing levels allowed for some of these thunderstorms to produce gusty winds over the waters. A potent upper level trough as well as a surface cold front crossed the region during the afternoon of March 22nd. Out ahead of the trough, surface heating and cold upper levels were able to generate marginal amounts of surface instability. This was enough to generate scattered showers and a few thunderstorms as the front and trough passed across the area. Steep low level lapse rates and low freezing levels allowed for some of these thunderstorms to produce gusty winds over the waters.\nEvent Narrative: A wind gust of 38 knots was measured at Tolly Point. A wind gust of up to 34 knots was observed at the Bay Bridge Airport. A wind gust of up to 34 knots was observed at Greenbury Point. A wind gust of up to 34 knots was observed at Kent Island. A wind gust of up to 34 knots was observed at Sandy Point. A wind gust of 38 knots was measured at Greenbury Point. A wind gust of up to 34 knots was observed at Tolchester. A wind gust of 36 knots was measured at Martin State Airport. A wind gust of 38 knots was measured at Gunpowder. A wind gust of 47 knots was measured at Hart Miller Island. A wind gust of 48 knots was measured at Oriole Park at Camden Yards. A wind gust of 39 knots was observed at the Maryland Science Center. A wind gust of up to 34 knots was observed near Baltimore. A wind gust of up to 34 knots was observed at Kent Island. A wind gust of 39 knots was measured at Hampstead Hill Academy. A wind gust of 43 knots was measured at Thomas Point. A wind gust of up to 34 knots was measured near the Baltimore Francis Scott Key Bridge. A wind gust of up to 34 knots was observed at Bay Bridge Airport. A wind gust of up to 34 knots was observed at Thomas Point. A wind gust of up to 34 knots was observed at Tolchester. A wind gust of 36 knots was measured near Baltimore.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 38.047 km away, between 2019-03-22 15:30:00 and 2019-03-22 15:30:00. The events included records with measured wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A potent upper level trough as well as a surface cold front crossed the region during the afternoon of March 22nd. Out ahead of the trough, surface heating and cold upper levels were able to generate marginal amounts of surface instability. This was enough to generate scattered showers and a few thunderstorms as the front and trough passed across the area. Steep low level lapse rates and low freezing levels allowed for some of these thunderstorms to become locally severe.\nEvent Narrative: A wind speed of 50 knots (58 mph) was measured at the Galesville mesonet.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 16.5552 km away, between 2019-04-15 00:44:00 and 2019-04-15 01:33:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A warm front crossed the state of Maryland from south to north during the morning hours of April 14th, allowing for increasing warm and moist air to move overhead. During the afternoon and evening, low pressure moved through the Ohio Valley and into the eastern Great Lakes, leading to an increase in the wind field across all levels and therefore an increase in deep layer shear. Instability remained somewhat limited, but was enough to produce showers and scattered thunderstorms during the afternoon and evening hours, a couple of which became severe. A second round of showers and thunderstorms then moved across the state as a strong cold front crossed the region during the late evening and overnight hours. These thunderstorms took the form of a quasi-linear convective system which became severe and produced locally damaging winds. A warm front crossed the state of Maryland from south to north during the morning hours of April 14th, allowing for increasing warm and moist air to move overhead. During the afternoon and evening, low pressure moved through the Ohio Valley and into the eastern Great Lakes, leading to an increase in the wind field across all levels and therefore an increase in deep layer shear. Instability remained somewhat limited, but was enough to produce showers and scattered thunderstorms during the afternoon and evening hours, a couple of which became severe. A second round of showers and thunderstorms then moved across the state as a strong cold front crossed the region during the late evening and overnight hours. These thunderstorms took the form of a quasi-linear convective system which became severe and produced locally damaging winds.\nEvent Narrative: A tree was blown down across Maryland Route 197 at Old Laurel-Bowie Road. A tree was blown down in the 4000 block of Saint John's Lane.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 25.7414 km away, between 2019-04-15 01:00:00 and 2019-04-15 02:10:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A warm front crossed the waters from south to north during the morning hours of April 14th, allowing for increasing warm and moist air to move overhead. During the afternoon and evening, low pressure moved through the Ohio Valley and into the eastern Great Lakes, leading to an increase in the wind field across all levels and therefore an increase in deep layer shear. Instability remained somewhat limited, but was enough to produce showers and scattered thunderstorms during the afternoon and evening hours. A second more potent round of showers and thunderstorms then moved across the waters as a strong cold front crossed the region during the late evening and overnight hours. These thunderstorms took the form of a quasi-linear convective system which produced strong and gusty winds over the waters. A warm front crossed the waters from south to north during the morning hours of April 14th, allowing for increasing warm and moist air to move overhead. During the afternoon and evening, low pressure moved through the Ohio Valley and into the eastern Great Lakes, leading to an increase in the wind field across all levels and therefore an increase in deep layer shear. Instability remained somewhat limited, but was enough to produce showers and scattered thunderstorms during the afternoon and evening hours. A second more potent round of showers and thunderstorms then moved across the waters as a strong cold front crossed the region during the late evening and overnight hours. These thunderstorms took the form of a quasi-linear convective system which produced strong and gusty winds over the waters. A warm front crossed the waters from south to north during the morning hours of April 14th, allowing for increasing warm and moist air to move overhead. During the afternoon and evening, low pressure moved through the Ohio Valley and into the eastern Great Lakes, leading to an increase in the wind field across all levels and therefore an increase in deep layer shear. Instability remained somewhat limited, but was enough to produce showers and scattered thunderstorms during the afternoon and evening hours. A second more potent round of showers and thunderstorms then moved across the waters as a strong cold front crossed the region during the late evening and overnight hours. These thunderstorms took the form of a quasi-linear convective system which produced strong and gusty winds over the waters. A warm front crossed the waters from south to north during the morning hours of April 14th, allowing for increasing warm and moist air to move overhead. During the afternoon and evening, low pressure moved through the Ohio Valley and into the eastern Great Lakes, leading to an increase in the wind field across all levels and therefore an increase in deep layer shear. Instability remained somewhat limited, but was enough to produce showers and scattered thunderstorms during the afternoon and evening hours. A second more potent round of showers and thunderstorms then moved across the waters as a strong cold front crossed the region during the late evening and overnight hours. These thunderstorms took the form of a quasi-linear convective system which produced strong and gusty winds over the waters. A warm front crossed the waters from south to north during the morning hours of April 14th, allowing for increasing warm and moist air to move overhead. During the afternoon and evening, low pressure moved through the Ohio Valley and into the eastern Great Lakes, leading to an increase in the wind field across all levels and therefore an increase in deep layer shear. Instability remained somewhat limited, but was enough to produce showers and scattered thunderstorms during the afternoon and evening hours. A second more potent round of showers and thunderstorms then moved across the waters as a strong cold front crossed the region during the late evening and overnight hours. These thunderstorms took the form of a quasi-linear convective system which produced strong and gusty winds over the waters. A warm front crossed the waters from south to north during the morning hours of April 14th, allowing for increasing warm and moist air to move overhead. During the afternoon and evening, low pressure moved through the Ohio Valley and into the eastern Great Lakes, leading to an increase in the wind field across all levels and therefore an increase in deep layer shear. Instability remained somewhat limited, but was enough to produce showers and scattered thunderstorms during the afternoon and evening hours. A second more potent round of showers and thunderstorms then moved across the waters as a strong cold front crossed the region during the late evening and overnight hours. These thunderstorms took the form of a quasi-linear convective system which produced strong and gusty winds over the waters. A warm front crossed the waters from south to north during the morning hours of April 14th, allowing for increasing warm and moist air to move overhead. During the afternoon and evening, low pressure moved through the Ohio Valley and into the eastern Great Lakes, leading to an increase in the wind field across all levels and therefore an increase in deep layer shear. Instability remained somewhat limited, but was enough to produce showers and scattered thunderstorms during the afternoon and evening hours. A second more potent round of showers and thunderstorms then moved across the waters as a strong cold front crossed the region during the late evening and overnight hours. These thunderstorms took the form of a quasi-linear convective system which produced strong and gusty winds over the waters. A warm front crossed the waters from south to north during the morning hours of April 14th, allowing for increasing warm and moist air to move overhead. During the afternoon and evening, low pressure moved through the Ohio Valley and into the eastern Great Lakes, leading to an increase in the wind field across all levels and therefore an increase in deep layer shear. Instability remained somewhat limited, but was enough to produce showers and scattered thunderstorms during the afternoon and evening hours. A second more potent round of showers and thunderstorms then moved across the waters as a strong cold front crossed the region during the late evening and overnight hours. These thunderstorms took the form of a quasi-linear convective system which produced strong and gusty winds over the waters.\nEvent Narrative: Wind gusts of up to 39 knots were measured near Greenbury Point. Wind gusts of up to 34 knots were observed near Kent Island. Wind gusts of up to 35 knots were measured near the Baltimore Key Bridge. A wind gust of 38 knots was measured near Sandy Point. Wind gusts of up to 38 knots were measured near Hart Miller Island. Wind gusts of up to 42 knots were measured near Tolchester. Wind gusts of up to 34 knots were measured near Lakeland Elementary School. Wind gusts of up to 41 knots were measured near the Maryland Science Center.", "The following events were reported: Thunderstorm Wind, Tornado. These occurred near station USW00093721, approximately 31.8782 km away, between 2019-04-26 13:55:00 and 2019-04-26 14:40:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: An upper level trough east of the Mississippi River on the morning of April 26th deepened and closed off over the eastern Great Lakes by the morning of April 27th. A forced convective line was ongoing in the morning hours of April 26th over West Virginia and progressed eastward into Maryland during the afternoon hours. A few individual cells also formed ahead of this convective line. Modest instability developed during the late morning and early afternoon hours which helped to support showers and thunderstorms across the region, and this combined with moderate levels of wind speed shear, led to strong to severe thunderstorms which produced locally damaging winds. There was also enough low level directional shear to produce a tornado in central Maryland. An upper level trough east of the Mississippi River on the morning of April 26th deepened and closed off over the eastern Great Lakes by the morning of April 27th. A forced convective line was ongoing in the morning hours of April 26th over West Virginia and progressed eastward into Maryland during the afternoon hours. A few individual cells also formed ahead of this convective line. Modest instability developed during the late morning and early afternoon hours which helped to support showers and thunderstorms across the region, and this combined with moderate levels of wind speed shear, led to strong to severe thunderstorms which produced locally damaging winds. There was also enough low level directional shear to produce a tornado in central Maryland. An upper level trough east of the Mississippi River on the morning of April 26th deepened and closed off over the eastern Great Lakes by the morning of April 27th. A forced convective line was ongoing in the morning hours of April 26th over West Virginia and progressed eastward into Maryland during the afternoon hours. A few individual cells also formed ahead of this convective line. Modest instability developed during the late morning and early afternoon hours which helped to support showers and thunderstorms across the region, and this combined with moderate levels of wind speed shear, led to strong to severe thunderstorms which produced locally damaging winds. There was also enough low level directional shear to produce a tornado in central Maryland. An upper level trough east of the Mississippi River on the morning of April 26th deepened and closed off over the eastern Great Lakes by the morning of April 27th. A forced convective line was ongoing in the morning hours of April 26th over West Virginia and progressed eastward into Maryland during the afternoon hours. A few individual cells also formed ahead of this convective line. Modest instability developed during the late morning and early afternoon hours which helped to support showers and thunderstorms across the region, and this combined with moderate levels of wind speed shear, led to strong to severe thunderstorms which produced locally damaging winds. There was also enough low level directional shear to produce a tornado in central Maryland. An upper level trough east of the Mississippi River on the morning of April 26th deepened and closed off over the eastern Great Lakes by the morning of April 27th. A forced convective line was ongoing in the morning hours of April 26th over West Virginia and progressed eastward into Maryland during the afternoon hours. A few individual cells also formed ahead of this convective line. Modest instability developed during the late morning and early afternoon hours which helped to support showers and thunderstorms across the region, and this combined with moderate levels of wind speed shear, led to strong to severe thunderstorms which produced locally damaging winds. There was also enough low level directional shear to produce a tornado in central Maryland. An upper level trough east of the Mississippi River on the morning of April 26th deepened and closed off over the eastern Great Lakes by the morning of April 27th. A forced convective line was ongoing in the morning hours of April 26th over West Virginia and progressed eastward into Maryland during the afternoon hours. A few individual cells also formed ahead of this convective line. Modest instability developed during the late morning and early afternoon hours which helped to support showers and thunderstorms across the region, and this combined with moderate levels of wind speed shear, led to strong to severe thunderstorms which produced locally damaging winds. There was also enough low level directional shear to produce a tornado in central Maryland. An upper level trough east of the Mississippi River on the morning of April 26th deepened and closed off over the eastern Great Lakes by the morning of April 27th. A forced convective line was ongoing in the morning hours of April 26th over West Virginia and progressed eastward into Maryland during the afternoon hours. A few individual cells also formed ahead of this convective line. Modest instability developed during the late morning and early afternoon hours which helped to support showers and thunderstorms across the region, and this combined with moderate levels of wind speed shear, led to strong to severe thunderstorms which produced locally damaging winds. There was also enough low level directional shear to produce a tornado in central Maryland. An upper level trough east of the Mississippi River on the morning of April 26th deepened and closed off over the eastern Great Lakes by the morning of April 27th. A forced convective line was ongoing in the morning hours of April 26th over West Virginia and progressed eastward into Maryland during the afternoon hours. A few individual cells also formed ahead of this convective line. Modest instability developed during the late morning and early afternoon hours which helped to support showers and thunderstorms across the region, and this combined with moderate levels of wind speed shear, led to strong to severe thunderstorms which produced locally damaging winds. There was also enough low level directional shear to produce a tornado in central Maryland. An upper level trough east of the Mississippi River on the morning of April 26th deepened and closed off over the eastern Great Lakes by the morning of April 27th. A forced convective line was ongoing in the morning hours of April 26th over West Virginia and progressed eastward into Maryland during the afternoon hours. A few individual cells also formed ahead of this convective line. Modest instability developed during the late morning and early afternoon hours which helped to support showers and thunderstorms across the region, and this combined with moderate levels of wind speed shear, led to strong to severe thunderstorms which produced locally damaging winds. There was also enough low level directional shear to produce a tornado in central Maryland. An upper level trough east of the Mississippi River on the morning of April 26th deepened and closed off over the eastern Great Lakes by the morning of April 27th. A forced convective line was ongoing in the morning hours of April 26th over West Virginia and progressed eastward into Maryland during the afternoon hours. A few individual cells also formed ahead of this convective line. Modest instability developed during the late morning and early afternoon hours which helped to support showers and thunderstorms across the region, and this combined with moderate levels of wind speed shear, led to strong to severe thunderstorms which produced locally damaging winds. There was also enough low level directional shear to produce a tornado in central Maryland.\nEvent Narrative: A tree was blown down onto wires in Laytonsville. A large wooden sign was blown down on Shawan Road between Falls Road and I-83. A tree was blown down onto power lines on Gambrills Road near Grace Point Church. A tree was also blown down in the 1600 block of Preakness Drive. A tree and wires were blown down along the 15000 block of Carroll Road. A large tree was snapped near the intersection of Sweet Air Road and Fox Run Court. A large tree was down blocking the intersection of Natalie Lane and Carli Court. One tree was blown down a quarter mile south of the intersection of Cuba Road and Gardiner Road. Two trees were also blown down and one other tree topped near the intersection of Cuba Road and Miller Road. One other tree was blown down on Western Run Road just north of Ford Road. A tree was blown down on Big Falls Road a quarter mile south of the Gunpowder Falls Trail parking area. Three trees were also blown down in the 1600 to 1700 block of Wilson Road. A tree was blown down along the ramp from northbound I-95 to westbound I-695 Baltimore Beltway Inner Loop. An EF-1 tornado began at 3:19 PM EDT (2:19 PM EST) on Corbett Road between Monkton Farms Drive and Falls Road, and ended at 323 PM EDT (2:23 PM EST) near the intersection of Shepperd Road and MD-562/138 Troyer Road, resulting in intermittent damage mainly to softwood trees. This time was estimated from rotational velocity signatures evident on both KLWX Sterling National Weather Service Weather Surveillance Radar (88D) and TBWI FAA Terminal Doppler Weather Radar. Several area residents noted sudden, chaotic winds around 3:20 PM EDT (2:20 PM EST). No concentrated or tornadic damage was found southwest or northeast of this location, although there was sporadic tree damage concluded to be from straight line winds throughout much of northeastern Baltimore County into northwestern Harford County.||Most of the damage was to softwood (pine) trees. On Corbett Road, two softwood (pine) trees were snapped a third of the way up on the west side of the road, and fell toward the northeast. Across the street in a wooded area, a third tree (hardwood, birch) snapped halfway up and fell toward the east. A fourth tree (softwood, pine) just to the north snapped halfway up, and fell toward the south. The pattern of the tree damage was convergent in nature, implying a circulation reached the surface at this|point. Other leaf and small branch debris was noted in the area. The damage was confined to a 100-yard wide path at this location.||The tornado continued northeastward with a forward speed of 40 to 50 mph (estimated from TBWI radar), reaching the 2400 block of Monkton Road at 3:20 PM EDT (2:20 PM EST). At this location, four pine trees snapped about halfway up, and fell toward the northeast; one small tree along the southeast side of the path snapped at the base and|fell toward the southwest; two other pine trees snapped halfway up and fell toward the north or northwest. There were also numerous large limbs scattered around this area. Damage was confined to a path that expanded slightly in width to about 125 yards.||The circulation reached JM Pearce Road just east of MD-138 Shepperd Road at 3:21 PM EDT (2:21 PM EST). At least ten trees were snapped in a 150-yard wide path here. Three trees on the northwest side of the path fell toward the south or southeast, with the rest falling toward the northwest to northeast. All of the trees that fell were softwoods (mainly pines).||At 3:22 PM EDT (2:22 PM EST), the tornado reached MD-138 Shepperd Road in the 2900 block. Over a dozen trees were snapped between the base and halfway up at this location. Additionally, half a dozen trees were topped. The trees that were snapped closer to the base were along and southeast of the roadway, and fell facing the northwest, north and northeast. The trees that had their tops snapped off were along the north side of the road, and blew south across the road onto adjacent properties. A house at a horse barn had two screens blown in toward the northeast, and the slide of a swing set on the property was torn off and blew toward the northwest. Steel barns on the property sustained no notable damage, and no shingles or siding were removed from the house.||The last instance of tornadic damage was noted at the intersection of Shepperd Road and MD-562/138 Troyer Road. Several softwood trees were snapped here, as well, facing southwest, south and southeast.||Given the intermittent tree damage (snapped trees), and the fact that very little if any structural damage was noted, it is concluded that maximum wind speeds were 80 to 90 MPH. Above this speed is when most sturdy structures start sustaining notable|damage, like substantial loss of shingles or siding, which was NOT noted anywhere along the path. No injuries or fatalities were reported in this tornado.", "The following events were reported: Marine Hail, Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 31.3922 km away, between 2019-04-26 14:25:00 and 2019-04-26 15:12:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: An upper level trough east of the Mississippi River on the morning of April 26th deepened and closed off over the eastern Great Lakes by the morning of April 27th. A forced convective line was ongoing in the morning hours of April 26th over West Virginia and progressed eastward across the waters during the afternoon hours. A few individual cells also formed ahead of this convective line. Modest instability developed during the late morning and early afternoon hours which combined with moderate levels of wind shear to help support showers and thunderstorms which produced strong gusty winds over the waters. An upper level trough east of the Mississippi River on the morning of April 26th deepened and closed off over the eastern Great Lakes by the morning of April 27th. A forced convective line was ongoing in the morning hours of April 26th over West Virginia and progressed eastward across the waters during the afternoon hours. A few individual cells also formed ahead of this convective line. Modest instability developed during the late morning and early afternoon hours which combined with moderate levels of wind shear to help support showers and thunderstorms which produced strong gusty winds over the waters. An upper level trough east of the Mississippi River on the morning of April 26th deepened and closed off over the eastern Great Lakes by the morning of April 27th. A forced convective line was ongoing in the morning hours of April 26th over West Virginia and progressed eastward across the waters during the afternoon hours. A few individual cells also formed ahead of this convective line. Modest instability developed during the late morning and early afternoon hours which combined with moderate levels of wind shear to help support showers and thunderstorms which produced strong gusty winds over the waters. An upper level trough east of the Mississippi River on the morning of April 26th deepened and closed off over the eastern Great Lakes by the morning of April 27th. A forced convective line was ongoing in the morning hours of April 26th over West Virginia and progressed eastward across the waters during the afternoon hours. A few individual cells also formed ahead of this convective line. Modest instability developed during the late morning and early afternoon hours which combined with moderate levels of wind shear to help support showers and thunderstorms which produced strong gusty winds over the waters. An upper level trough east of the Mississippi River on the morning of April 26th deepened and closed off over the eastern Great Lakes by the morning of April 27th. A forced convective line was ongoing in the morning hours of April 26th over West Virginia and progressed eastward across the waters during the afternoon hours. A few individual cells also formed ahead of this convective line. Modest instability developed during the late morning and early afternoon hours which combined with moderate levels of wind shear to help support showers and thunderstorms which produced strong gusty winds over the waters. An upper level trough east of the Mississippi River on the morning of April 26th deepened and closed off over the eastern Great Lakes by the morning of April 27th. A forced convective line was ongoing in the morning hours of April 26th over West Virginia and progressed eastward across the waters during the afternoon hours. A few individual cells also formed ahead of this convective line. Modest instability developed during the late morning and early afternoon hours which combined with moderate levels of wind shear to help support showers and thunderstorms which produced strong gusty winds over the waters. An upper level trough east of the Mississippi River on the morning of April 26th deepened and closed off over the eastern Great Lakes by the morning of April 27th. A forced convective line was ongoing in the morning hours of April 26th over West Virginia and progressed eastward across the waters during the afternoon hours. A few individual cells also formed ahead of this convective line. Modest instability developed during the late morning and early afternoon hours which combined with moderate levels of wind shear to help support showers and thunderstorms which produced strong gusty winds over the waters. An upper level trough east of the Mississippi River on the morning of April 26th deepened and closed off over the eastern Great Lakes by the morning of April 27th. A forced convective line was ongoing in the morning hours of April 26th over West Virginia and progressed eastward across the waters during the afternoon hours. A few individual cells also formed ahead of this convective line. Modest instability developed during the late morning and early afternoon hours which combined with moderate levels of wind shear to help support showers and thunderstorms which produced strong gusty winds over the waters. An upper level trough east of the Mississippi River on the morning of April 26th deepened and closed off over the eastern Great Lakes by the morning of April 27th. A forced convective line was ongoing in the morning hours of April 26th over West Virginia and progressed eastward across the waters during the afternoon hours. A few individual cells also formed ahead of this convective line. Modest instability developed during the late morning and early afternoon hours which combined with moderate levels of wind shear to help support showers and thunderstorms which produced strong gusty winds over the waters.\nEvent Narrative: Hail of 0.75 inch in diameter was observed in Pasadena, Maryland. Wind gusts of up to 39 knots were measured at Martin State Airport (KMTN). Wind gusts of up to 35 knots were measured at Annapolis (KNAK). Wind gusts of up to 37 knots were measured near Greenbury Point. Wind gusts of up to 43 knots were measured near Thomas Point. Wind gusts of up to 42 knots were measured near Bayside Elementary School. Wind gusts of up to 34 knots were measured near Tolly Point. Wind gusts of up to 34 knots were observed near Gunpowder. Wind gusts of up to 34 knots were observed near Tolchester.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 28.7512 km away, between 2019-04-28 16:25:00 and 2019-04-28 18:00:00. The events included records with estimated wind gusts of 34.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front crossed the waters during the afternoon hours of April 28th. Scattered showers developed along the frontal boundary as it passed across, some of which produced strong gusty winds over the waters. A cold front crossed the waters during the afternoon hours of April 28th. Scattered showers developed along the frontal boundary as it passed across, some of which produced strong gusty winds over the waters. A cold front crossed the waters during the afternoon hours of April 28th. Scattered showers developed along the frontal boundary as it passed across, some of which produced strong gusty winds over the waters. A cold front crossed the waters during the afternoon hours of April 28th. Scattered showers developed along the frontal boundary as it passed across, some of which produced strong gusty winds over the waters. A cold front crossed the waters during the afternoon hours of April 28th. Scattered showers developed along the frontal boundary as it passed across, some of which produced strong gusty winds over the waters.\nEvent Narrative: Wind gusts of up to 34 knots were observed near Hampstead Hill Academy. Wind gusts of up to 34 knots were observed near Tolly Point. Wind gusts of up to 34 knots were observed near Thomas Point. Wind gusts of up to 34 knots were observed near Greenbury Point. Wind gusts of up to 34 knots were observed near Annapolis (KNAK).", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 24.0241 km away, between 2019-05-02 15:30:00 and 2019-05-02 15:30:00. The events included records with estimated wind gusts of 61.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A warm front lifted across the region during the morning hours of May 2nd, with warm and humid conditions developing by the afternoon. This led to ample amounts of instability over the region, and as an upper level disturbance moved into the area providing wind shear and lift, scattered showers and thunderstorms developed, a few of which became severe.\nEvent Narrative: A large tree was blown down on the 2800 block of Haven Road. Multiple trees were also uprooted on a nearby property.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 34.8219 km away, between 2019-05-02 15:40:00 and 2019-05-02 17:00:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A warm front lifted across the waters during the morning hours of May 2nd, with warm and humid conditions developing by the afternoon. This led to ample amounts of instability over the region, and as an upper level disturbance moved into the area providing wind shear and lift, scattered showers and thunderstorms developed, some of which generated gusty winds over the waters. A warm front lifted across the waters during the morning hours of May 2nd, with warm and humid conditions developing by the afternoon. This led to ample amounts of instability over the region, and as an upper level disturbance moved into the area providing wind shear and lift, scattered showers and thunderstorms developed, some of which generated gusty winds over the waters. A warm front lifted across the waters during the morning hours of May 2nd, with warm and humid conditions developing by the afternoon. This led to ample amounts of instability over the region, and as an upper level disturbance moved into the area providing wind shear and lift, scattered showers and thunderstorms developed, some of which generated gusty winds over the waters. A warm front lifted across the waters during the morning hours of May 2nd, with warm and humid conditions developing by the afternoon. This led to ample amounts of instability over the region, and as an upper level disturbance moved into the area providing wind shear and lift, scattered showers and thunderstorms developed, some of which generated gusty winds over the waters. A warm front lifted across the waters during the morning hours of May 2nd, with warm and humid conditions developing by the afternoon. This led to ample amounts of instability over the region, and as an upper level disturbance moved into the area providing wind shear and lift, scattered showers and thunderstorms developed, some of which generated gusty winds over the waters. A warm front lifted across the waters during the morning hours of May 2nd, with warm and humid conditions developing by the afternoon. This led to ample amounts of instability over the region, and as an upper level disturbance moved into the area providing wind shear and lift, scattered showers and thunderstorms developed, some of which generated gusty winds over the waters. A warm front lifted across the waters during the morning hours of May 2nd, with warm and humid conditions developing by the afternoon. This led to ample amounts of instability over the region, and as an upper level disturbance moved into the area providing wind shear and lift, scattered showers and thunderstorms developed, some of which generated gusty winds over the waters. A warm front lifted across the waters during the morning hours of May 2nd, with warm and humid conditions developing by the afternoon. This led to ample amounts of instability over the region, and as an upper level disturbance moved into the area providing wind shear and lift, scattered showers and thunderstorms developed, some of which generated gusty winds over the waters. A warm front lifted across the waters during the morning hours of May 2nd, with warm and humid conditions developing by the afternoon. This led to ample amounts of instability over the region, and as an upper level disturbance moved into the area providing wind shear and lift, scattered showers and thunderstorms developed, some of which generated gusty winds over the waters. A warm front lifted across the waters during the morning hours of May 2nd, with warm and humid conditions developing by the afternoon. This led to ample amounts of instability over the region, and as an upper level disturbance moved into the area providing wind shear and lift, scattered showers and thunderstorms developed, some of which generated gusty winds over the waters.\nEvent Narrative: A wind gust of 46 knots was observed at Annapolis (KNAK). A wind gust of 55 knots was observed at Greenberry Point (GBY). A wind gust of 48 knots was observed at Tolly Point (TOL). Wind gusts of up to 34 knots were observed at Sandy Point (SPT). Wind gusts of up to 34 knots were observed at Saint Mary's Elementary School (ANNAS). Wind gusts of up to 46 knots were observed near Stevensville. Wind gusts of up to 46 knots were observed at Thomas Point (TPLM2). Wind gusts of up to 42 knots were observed at the Bay Bridge Airport (KW29). Wind gusts of up to 46 knots were observed at Kent Island (KNT). Wind gusts of up to 34 knots were observed at Thomas Point.", "The following events were reported: Flood. These occurred near station USW00093721, approximately 15.0177 km away, between 2019-05-10 21:40:00 and 2019-05-10 23:40:00. The flood was caused by Heavy Rain. Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front passed through the area on the 10th, and a few showers and thunderstorms produced heavy rainfall. Localized flooding occurred in northern Maryland.\nEvent Narrative: US-40 Oreleans Street was closed due to floding near North Central Avenue. East Fayette Street was closed at President Street due to flooding.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 33.4817 km away, between 2019-05-18 19:20:00 and 2019-05-18 19:20:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A weak warm front was located across central Maryland southward along the Potomac River during the afternoon hours of May 18th. Enough instability and wind shear was present for thunderstorms to develop near and along this boundary, and some became severe.\nEvent Narrative: Two trees were blown down near the intersection of Jennings Chapel and Howard Chapel Road.", "The following events were reported: Thunderstorm Wind, Tornado. These occurred near station USW00093721, approximately 23.2324 km away, between 2019-05-23 14:11:00 and 2019-05-23 15:10:00.The events resulted in 1 injuries and 0 fatalities. No significant property or crop damage was reported. \n\nEpisode Narrative: A warm front crossed the region during the morning hours of May 23rd, placing the area in the warm sector by the afternoon hours. At the same time, surface low pressure tracked across the northern Great Lakes, with an attendant cold front moving into the Ohio Valley by the evening. A mesoscale convective system (MCS) was ongoing during the morning hours and moved eastward and into the region during the afternoon hours. Out ahead of the MCS, moisture and warmth increased with moderate instability developing. Aloft, wind shear increased throughout the day and became quite substantial by the late afternoon. The MCS entered Maryland by the mid afternoon hours and intensified into a linear feature that produced damaging winds and one tornado before exiting during the evening. A warm front crossed the region during the morning hours of May 23rd, placing the area in the warm sector by the afternoon hours. At the same time, surface low pressure tracked across the northern Great Lakes, with an attendant cold front moving into the Ohio Valley by the evening. A mesoscale convective system (MCS) was ongoing during the morning hours and moved eastward and into the region during the afternoon hours. Out ahead of the MCS, moisture and warmth increased with moderate instability developing. Aloft, wind shear increased throughout the day and became quite substantial by the late afternoon. The MCS entered Maryland by the mid afternoon hours and intensified into a linear feature that produced damaging winds and one tornado before exiting during the evening. A warm front crossed the region during the morning hours of May 23rd, placing the area in the warm sector by the afternoon hours. At the same time, surface low pressure tracked across the northern Great Lakes, with an attendant cold front moving into the Ohio Valley by the evening. A mesoscale convective system (MCS) was ongoing during the morning hours and moved eastward and into the region during the afternoon hours. Out ahead of the MCS, moisture and warmth increased with moderate instability developing. Aloft, wind shear increased throughout the day and became quite substantial by the late afternoon. The MCS entered Maryland by the mid afternoon hours and intensified into a linear feature that produced damaging winds and one tornado before exiting during the evening. A warm front crossed the region during the morning hours of May 23rd, placing the area in the warm sector by the afternoon hours. At the same time, surface low pressure tracked across the northern Great Lakes, with an attendant cold front moving into the Ohio Valley by the evening. A mesoscale convective system (MCS) was ongoing during the morning hours and moved eastward and into the region during the afternoon hours. Out ahead of the MCS, moisture and warmth increased with moderate instability developing. Aloft, wind shear increased throughout the day and became quite substantial by the late afternoon. The MCS entered Maryland by the mid afternoon hours and intensified into a linear feature that produced damaging winds and one tornado before exiting during the evening. A warm front crossed the region during the morning hours of May 23rd, placing the area in the warm sector by the afternoon hours. At the same time, surface low pressure tracked across the northern Great Lakes, with an attendant cold front moving into the Ohio Valley by the evening. A mesoscale convective system (MCS) was ongoing during the morning hours and moved eastward and into the region during the afternoon hours. Out ahead of the MCS, moisture and warmth increased with moderate instability developing. Aloft, wind shear increased throughout the day and became quite substantial by the late afternoon. The MCS entered Maryland by the mid afternoon hours and intensified into a linear feature that produced damaging winds and one tornado before exiting during the evening. A warm front crossed the region during the morning hours of May 23rd, placing the area in the warm sector by the afternoon hours. At the same time, surface low pressure tracked across the northern Great Lakes, with an attendant cold front moving into the Ohio Valley by the evening. A mesoscale convective system (MCS) was ongoing during the morning hours and moved eastward and into the region during the afternoon hours. Out ahead of the MCS, moisture and warmth increased with moderate instability developing. Aloft, wind shear increased throughout the day and became quite substantial by the late afternoon. The MCS entered Maryland by the mid afternoon hours and intensified into a linear feature that produced damaging winds and one tornado before exiting during the evening. A warm front crossed the region during the morning hours of May 23rd, placing the area in the warm sector by the afternoon hours. At the same time, surface low pressure tracked across the northern Great Lakes, with an attendant cold front moving into the Ohio Valley by the evening. A mesoscale convective system (MCS) was ongoing during the morning hours and moved eastward and into the region during the afternoon hours. Out ahead of the MCS, moisture and warmth increased with moderate instability developing. Aloft, wind shear increased throughout the day and became quite substantial by the late afternoon. The MCS entered Maryland by the mid afternoon hours and intensified into a linear feature that produced damaging winds and one tornado before exiting during the evening. A warm front crossed the region during the morning hours of May 23rd, placing the area in the warm sector by the afternoon hours. At the same time, surface low pressure tracked across the northern Great Lakes, with an attendant cold front moving into the Ohio Valley by the evening. A mesoscale convective system (MCS) was ongoing during the morning hours and moved eastward and into the region during the afternoon hours. Out ahead of the MCS, moisture and warmth increased with moderate instability developing. Aloft, wind shear increased throughout the day and became quite substantial by the late afternoon. The MCS entered Maryland by the mid afternoon hours and intensified into a linear feature that produced damaging winds and one tornado before exiting during the evening. A warm front crossed the region during the morning hours of May 23rd, placing the area in the warm sector by the afternoon hours. At the same time, surface low pressure tracked across the northern Great Lakes, with an attendant cold front moving into the Ohio Valley by the evening. A mesoscale convective system (MCS) was ongoing during the morning hours and moved eastward and into the region during the afternoon hours. Out ahead of the MCS, moisture and warmth increased with moderate instability developing. Aloft, wind shear increased throughout the day and became quite substantial by the late afternoon. The MCS entered Maryland by the mid afternoon hours and intensified into a linear feature that produced damaging winds and one tornado before exiting during the evening. A warm front crossed the region during the morning hours of May 23rd, placing the area in the warm sector by the afternoon hours. At the same time, surface low pressure tracked across the northern Great Lakes, with an attendant cold front moving into the Ohio Valley by the evening. A mesoscale convective system (MCS) was ongoing during the morning hours and moved eastward and into the region during the afternoon hours. Out ahead of the MCS, moisture and warmth increased with moderate instability developing. Aloft, wind shear increased throughout the day and became quite substantial by the late afternoon. The MCS entered Maryland by the mid afternoon hours and intensified into a linear feature that produced damaging winds and one tornado before exiting during the evening. A warm front crossed the region during the morning hours of May 23rd, placing the area in the warm sector by the afternoon hours. At the same time, surface low pressure tracked across the northern Great Lakes, with an attendant cold front moving into the Ohio Valley by the evening. A mesoscale convective system (MCS) was ongoing during the morning hours and moved eastward and into the region during the afternoon hours. Out ahead of the MCS, moisture and warmth increased with moderate instability developing. Aloft, wind shear increased throughout the day and became quite substantial by the late afternoon. The MCS entered Maryland by the mid afternoon hours and intensified into a linear feature that produced damaging winds and one tornado before exiting during the evening.\nEvent Narrative: Two large 20 inch in diameter trees were snapped. Multiple trees were blown down. Multiple trees were blown down. Multiple large trees were blown down. Multiple large trees and branches were blown down. Multiple trees and wires were blown down throughout Anne Arundel County. A wind gust of 58 mph (50 knots) was measured near Clarksville. A line of showers and thunderstorms crossed the Blue Ridge Mountains around 2:30 PM EDT (1:30 PM EST) 23 May 2019, then tapped into strong thermodynamics and wind shear, creating a Quasi-Linear Convective System (QLCS) that increased in intensity as it tracked southeast across central and southern Maryland, Washington DC, and northern Virginia. The QLCS spawned an EF1 tornado in Howard County MD between 3:27 PM EDT (2:27 PM EST) and 3:36 PM EDT (2:36 EST), with a discontinuous damage path of 5.5 miles, moving east-southeast at an estimated 40 mph. ||The first evidence of tornadic damage was near the intersection of Brighton Dam Road and MD Route 108 in Clarksville. Several trees were uprooted in this vicinity with large branches pulled towards each other, and fell in multiple directions, except westerly.||As the tornado moved east, more convergent tree damage extended on either side of Cedar Lane around Corina Court in Columbia. One eyewitness in this location who was interviewed saw the tornado knocking down trees, resulting in swirling debris. Most trees in this location were uprooted, but a few were snapped. Trees here were both softwood and hardwood. One tree fell into the roof of a house. Another resident in this area reported getting the wireless emergency alert on their phone, followed moments later by strong winds, which knocked down large trees.||Tree damage was also noted along Shaker Drive between Seneca Farm Road and Wayover Way, where numerous large trees were uprooted, with a couple of trees |snapped, falling to the north.||The most significant damage noted was near the 9400 block of Patuxent Woods Drive, where a grove of hardwood and softwood trees were snapped about midway up their trunks, falling haphazardly. A nearby office building lost part of its roof, which blew towards the east. Trees were down further to the east, but it is likely that this was due to straight-line winds as radar analysis showed the tornado vortex broadening rapidly. A large tree was uprooted, one tree was snapped, and another large branch was snapped on private property. Multiple trees and wires were blown down. Multiple reports of trees and utility poles blown down.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 34.5293 km away, between 2019-05-23 15:05:00 and 2019-05-23 16:00:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A warm front crossed the waters during the morning hours of May 23rd, placing the area in the warm sector by the afternoon hours. At the same time, surface low pressure tracked across the northern Great Lakes, with an attendant cold front moving into the Ohio Valley by the evening. A mesoscale convective system (MCS) was ongoing during the morning hours and moved eastward and into the region during the afternoon hours. Out ahead of the MCS, moisture and warmth increased with moderate instability developing. Aloft, wind shear increased throughout the day and became quite substantial by the late afternoon. The MCS intensified into a linear feature that produced gusty winds over the waters during the afternoon and evening hours. A warm front crossed the waters during the morning hours of May 23rd, placing the area in the warm sector by the afternoon hours. At the same time, surface low pressure tracked across the northern Great Lakes, with an attendant cold front moving into the Ohio Valley by the evening. A mesoscale convective system (MCS) was ongoing during the morning hours and moved eastward and into the region during the afternoon hours. Out ahead of the MCS, moisture and warmth increased with moderate instability developing. Aloft, wind shear increased throughout the day and became quite substantial by the late afternoon. The MCS intensified into a linear feature that produced gusty winds over the waters during the afternoon and evening hours. A warm front crossed the waters during the morning hours of May 23rd, placing the area in the warm sector by the afternoon hours. At the same time, surface low pressure tracked across the northern Great Lakes, with an attendant cold front moving into the Ohio Valley by the evening. A mesoscale convective system (MCS) was ongoing during the morning hours and moved eastward and into the region during the afternoon hours. Out ahead of the MCS, moisture and warmth increased with moderate instability developing. Aloft, wind shear increased throughout the day and became quite substantial by the late afternoon. The MCS intensified into a linear feature that produced gusty winds over the waters during the afternoon and evening hours.\nEvent Narrative: Wind gusts of up to 34 knots were observed at Annapolis (KNAK). Wind gusts of up to 36 knots were observed near Stevensville. Wind gusts of up to 36 knots were observed at Thomas Point.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 22.7566 km away, between 2019-05-26 19:50:00 and 2019-05-26 20:58:00. The events included records with estimated wind gusts of 52.44444444444444 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A warm front moved through the area during the early morning hours of May 26th, placing the region in the warm sector. This allowed for a hot and humid air mass to overspread the region during the afternoon, leading to significant levels of instability. Modest but sufficient wind shear was also present as an upper level disturbance approached the region from the west. This combination of factors led to the development of showers and thunderstorms, some of which became severe. A warm front moved through the area during the early morning hours of May 26th, placing the region in the warm sector. This allowed for a hot and humid air mass to overspread the region during the afternoon, leading to significant levels of instability. Modest but sufficient wind shear was also present as an upper level disturbance approached the region from the west. This combination of factors led to the development of showers and thunderstorms, some of which became severe. A warm front moved through the area during the early morning hours of May 26th, placing the region in the warm sector. This allowed for a hot and humid air mass to overspread the region during the afternoon, leading to significant levels of instability. Modest but sufficient wind shear was also present as an upper level disturbance approached the region from the west. This combination of factors led to the development of showers and thunderstorms, some of which became severe. A warm front moved through the area during the early morning hours of May 26th, placing the region in the warm sector. This allowed for a hot and humid air mass to overspread the region during the afternoon, leading to significant levels of instability. Modest but sufficient wind shear was also present as an upper level disturbance approached the region from the west. This combination of factors led to the development of showers and thunderstorms, some of which became severe. A warm front moved through the area during the early morning hours of May 26th, placing the region in the warm sector. This allowed for a hot and humid air mass to overspread the region during the afternoon, leading to significant levels of instability. Modest but sufficient wind shear was also present as an upper level disturbance approached the region from the west. This combination of factors led to the development of showers and thunderstorms, some of which became severe. A warm front moved through the area during the early morning hours of May 26th, placing the region in the warm sector. This allowed for a hot and humid air mass to overspread the region during the afternoon, leading to significant levels of instability. Modest but sufficient wind shear was also present as an upper level disturbance approached the region from the west. This combination of factors led to the development of showers and thunderstorms, some of which became severe. A warm front moved through the area during the early morning hours of May 26th, placing the region in the warm sector. This allowed for a hot and humid air mass to overspread the region during the afternoon, leading to significant levels of instability. Modest but sufficient wind shear was also present as an upper level disturbance approached the region from the west. This combination of factors led to the development of showers and thunderstorms, some of which became severe. A warm front moved through the area during the early morning hours of May 26th, placing the region in the warm sector. This allowed for a hot and humid air mass to overspread the region during the afternoon, leading to significant levels of instability. Modest but sufficient wind shear was also present as an upper level disturbance approached the region from the west. This combination of factors led to the development of showers and thunderstorms, some of which became severe. A warm front moved through the area during the early morning hours of May 26th, placing the region in the warm sector. This allowed for a hot and humid air mass to overspread the region during the afternoon, leading to significant levels of instability. Modest but sufficient wind shear was also present as an upper level disturbance approached the region from the west. This combination of factors led to the development of showers and thunderstorms, some of which became severe.\nEvent Narrative: A tree was blown down on Haverhill Road near Joppa Farm Road. Multiple trees were blown down and a barn was displaced from its foundation along Tunnell Road between Henryton Road and Marriottsville Road. Trees were also reported down along Barley Field Way. A tree was blown down on Liberty Road. A tree was blown down in Poplar Hill. Multiple trees were reported blown down in Halethorpe. A tree was blown down near the intersection of Waterbury Road and Severn Chapel Road. A tree was also blown down near the interchange of I-97 and Generals Highway. A tree was blown down near the intersection of Sunrise Beach Road and Whitneys Landing Drive. A tree was blown down near the intersection of Herald Harbor Road and Wilson Road. A second tree was also blown down nearby at the intersection of Herald Harbor Road and Rosewood Trail. A tree was blown down on the 1000 block of Plaza Circle. A tree was also blown down at the intersection of Trimble Road and Erwin Drive.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 49.9937 km away, between 2019-05-26 20:15:00 and 2019-05-26 20:15:00. The events included records with estimated wind gusts of 56.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A warm front moved through the mid-Atlantic early on the morning of May 26. Ahead of an approaching cold front that evening, thunderstorms developed, with some of them becoming severe. Several reports of damaging wind were received across eastern Maryland and Delaware.\nEvent Narrative: Seven to ten trees were uprooted or snapped on two adjacent properties near the Chesapeake Bay shoreline. One large tree fell across a road with another destroying part of a metal fence and multiple small holly trees.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 14.2666 km away, between 2019-05-26 20:48:00 and 2019-05-26 20:48:00. The events included records with measured wind gusts of 34.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A warm front moved across the waters during the early morning hours of May 26th, placing the region in the warm sector. This allowed for a hot and humid air mass to overspread the region during the afternoon, leading to significant levels of instability. Modest but sufficient wind shear was also present as an upper level disturbance approached the region from the west. This combination of factors led to the development of showers and thunderstorms, one of which produced gusty winds over the waters.\nEvent Narrative: Wind gusts of up to 34 knots were observed at the Baltimore Key Bridge (FSKM2).", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 33.7553 km away, between 2019-05-28 06:37:00 and 2019-05-28 06:51:00. The events included records with estimated wind gusts of 34.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A frontal boundary was draped across the waters during the early morning hours of May 28th. A weakening line of showers and thunderstorms moved along this boundary and brought localized gusty winds to portions of the waters. A frontal boundary was draped across the waters during the early morning hours of May 28th. A weakening line of showers and thunderstorms moved along this boundary and brought localized gusty winds to portions of the waters.\nEvent Narrative: Wind gusts of up to 34 knots were observed at Annapolis (KNAK). Wind gusts of up to 34 knots were observed at Kent Island.", "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00093721, approximately 33.1603 km away, between 2019-05-29 16:09:00 and 2019-05-29 17:15:00. The events included records with hailstones measuring 52.3125 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A surface frontal boundary was positioned north of the region across Pennsylvania for the majority of the day on May 29th, with pieces of upper level energy moving along the frontal boundary. By late in the day, a weak surface low traversed the front, and the front shifted southward towards northern Maryland as upper level energy approached the region. Hot and humid conditions across the area led to the development of significant amounts of instability, and that combined with modest but sufficient amounts of wind shear and the nearby frontal boundary promoted the development of scattered showers and thunderstorms. Some of these thunderstorms became severe, producing large hail and damaging winds, including two macrobursts across northeastern Maryland. A surface frontal boundary was positioned north of the region across Pennsylvania for the majority of the day on May 29th, with pieces of upper level energy moving along the frontal boundary. By late in the day, a weak surface low traversed the front, and the front shifted southward towards northern Maryland as upper level energy approached the region. Hot and humid conditions across the area led to the development of significant amounts of instability, and that combined with modest but sufficient amounts of wind shear and the nearby frontal boundary promoted the development of scattered showers and thunderstorms. Some of these thunderstorms became severe, producing large hail and damaging winds, including two macrobursts across northeastern Maryland. A surface frontal boundary was positioned north of the region across Pennsylvania for the majority of the day on May 29th, with pieces of upper level energy moving along the frontal boundary. By late in the day, a weak surface low traversed the front, and the front shifted southward towards northern Maryland as upper level energy approached the region. Hot and humid conditions across the area led to the development of significant amounts of instability, and that combined with modest but sufficient amounts of wind shear and the nearby frontal boundary promoted the development of scattered showers and thunderstorms. Some of these thunderstorms became severe, producing large hail and damaging winds, including two macrobursts across northeastern Maryland. A surface frontal boundary was positioned north of the region across Pennsylvania for the majority of the day on May 29th, with pieces of upper level energy moving along the frontal boundary. By late in the day, a weak surface low traversed the front, and the front shifted southward towards northern Maryland as upper level energy approached the region. Hot and humid conditions across the area led to the development of significant amounts of instability, and that combined with modest but sufficient amounts of wind shear and the nearby frontal boundary promoted the development of scattered showers and thunderstorms. Some of these thunderstorms became severe, producing large hail and damaging winds, including two macrobursts across northeastern Maryland. A surface frontal boundary was positioned north of the region across Pennsylvania for the majority of the day on May 29th, with pieces of upper level energy moving along the frontal boundary. By late in the day, a weak surface low traversed the front, and the front shifted southward towards northern Maryland as upper level energy approached the region. Hot and humid conditions across the area led to the development of significant amounts of instability, and that combined with modest but sufficient amounts of wind shear and the nearby frontal boundary promoted the development of scattered showers and thunderstorms. Some of these thunderstorms became severe, producing large hail and damaging winds, including two macrobursts across northeastern Maryland. A surface frontal boundary was positioned north of the region across Pennsylvania for the majority of the day on May 29th, with pieces of upper level energy moving along the frontal boundary. By late in the day, a weak surface low traversed the front, and the front shifted southward towards northern Maryland as upper level energy approached the region. Hot and humid conditions across the area led to the development of significant amounts of instability, and that combined with modest but sufficient amounts of wind shear and the nearby frontal boundary promoted the development of scattered showers and thunderstorms. Some of these thunderstorms became severe, producing large hail and damaging winds, including two macrobursts across northeastern Maryland. A surface frontal boundary was positioned north of the region across Pennsylvania for the majority of the day on May 29th, with pieces of upper level energy moving along the frontal boundary. By late in the day, a weak surface low traversed the front, and the front shifted southward towards northern Maryland as upper level energy approached the region. Hot and humid conditions across the area led to the development of significant amounts of instability, and that combined with modest but sufficient amounts of wind shear and the nearby frontal boundary promoted the development of scattered showers and thunderstorms. Some of these thunderstorms became severe, producing large hail and damaging winds, including two macrobursts across northeastern Maryland. A surface frontal boundary was positioned north of the region across Pennsylvania for the majority of the day on May 29th, with pieces of upper level energy moving along the frontal boundary. By late in the day, a weak surface low traversed the front, and the front shifted southward towards northern Maryland as upper level energy approached the region. Hot and humid conditions across the area led to the development of significant amounts of instability, and that combined with modest but sufficient amounts of wind shear and the nearby frontal boundary promoted the development of scattered showers and thunderstorms. Some of these thunderstorms became severe, producing large hail and damaging winds, including two macrobursts across northeastern Maryland.\nEvent Narrative: Ping pong ball-sized hail (1.5 inch in diameter) was reported. Several trees were blown down near the intersection of MD-32 and Lakeland Drive. A tree was blown down on Jarrettsville Pike near Hess Road. The White Marsh area of eastern Baltimore County was impacted with a macroburst, which caused straight-line wind damage between 5:53 PM EDT (4:53 PM EST) and 6:00 PM EDT (5:00 PM EST). Two wooden telephone poles were snapped along Silver Spring Road, and numerous trees and branches were downed along Saxon Circle. All observed tree damage fell to the northeast. Additionally, the Baltimore County Office of Homeland Security and Emergency Management reported the easternmost wind damage in Middle River, near the intersection of Ebenezer and Bird River Roads. The western most damage reported was near the intersection of Yvonne Ave and Silver Spring Rd in Nottingham. There were approximately 18 instances of tree damage between these two locations, with the horizontal distance of about 4 miles. The snapping of the telephone poles and nature of the reported and observed tree damage produces an estimate of 90 MPH wind. A tree was blown down on Garnett Road near Joppa Farm Road. Multiple trees were blown down near the intersection of Route 2 and Leelyn Drive. A wind gust to 58 mph (50 knots) was measured at Martin State Airport (KMTN). The Fallston and Baldwin area of west-central Harford County was impacted by a macroburst from 6:10 PM EDT (5:10 PM EST) until 6:15 PM EDT (5:15 PM EDT), which produced damaging wind gusts estimated at 90 MPH. A concentrated area of |damage was observed starting at Moores Road in Baldwin, extending discontinuously for approximately 3.25 miles to the east, ending at Pleasantville Road in Fallston. In this area, numerous observations of tree damage were observed. The tree damage |included mainly large limbs of hardwood trees and snaps of about a dozen pine trees. Several single family homes were impacted with limbs falling onto rooftops. All tree damage fell in an easterly direction. An image circulating among residents showed what |appears to be a roll cloud, representing the leading edge of the gusty winds.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 26.2239 km away, between 2019-05-29 16:48:00 and 2019-05-29 19:00:00.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 100000.0 and crop damage of 0.0. \n\nEpisode Narrative: A surface frontal boundary was positioned north of the waters across Pennsylvania for the majority of the day on May 29th, with pieces of upper level energy moving along the frontal boundary. By late in the day, a weak surface low traversed the front, and the front shifted southward towards the waters as upper level energy approached the region. Hot and humid conditions across the area led to the development of significant amounts of instability, and that combined with modest but sufficient amounts of wind shear and the nearby frontal boundary promoted the development of scattered showers and thunderstorms, some of which produced gusty winds over the waters. A surface frontal boundary was positioned north of the waters across Pennsylvania for the majority of the day on May 29th, with pieces of upper level energy moving along the frontal boundary. By late in the day, a weak surface low traversed the front, and the front shifted southward towards the waters as upper level energy approached the region. Hot and humid conditions across the area led to the development of significant amounts of instability, and that combined with modest but sufficient amounts of wind shear and the nearby frontal boundary promoted the development of scattered showers and thunderstorms, some of which produced gusty winds over the waters. A surface frontal boundary was positioned north of the waters across Pennsylvania for the majority of the day on May 29th, with pieces of upper level energy moving along the frontal boundary. By late in the day, a weak surface low traversed the front, and the front shifted southward towards the waters as upper level energy approached the region. Hot and humid conditions across the area led to the development of significant amounts of instability, and that combined with modest but sufficient amounts of wind shear and the nearby frontal boundary promoted the development of scattered showers and thunderstorms, some of which produced gusty winds over the waters. A surface frontal boundary was positioned north of the waters across Pennsylvania for the majority of the day on May 29th, with pieces of upper level energy moving along the frontal boundary. By late in the day, a weak surface low traversed the front, and the front shifted southward towards the waters as upper level energy approached the region. Hot and humid conditions across the area led to the development of significant amounts of instability, and that combined with modest but sufficient amounts of wind shear and the nearby frontal boundary promoted the development of scattered showers and thunderstorms, some of which produced gusty winds over the waters.\nEvent Narrative: Wind gusts of up to 34 knots were observed near Baltimore (BLTM2). Wind gusts of up to 49 knots were observed at Thomas Point. Wind gusts of up to 50 knots were observed at Martin State Airport (KMTN). Wind gusts of up to 50 knots were estimated along the Magothy River. Two boats were flipped over, with no injuries reported. Damage estimate provided by the Magothy River Sailing Association.", "The following events were reported: Hail, Thunderstorm Wind, Tornado. These occurred near station USW00093721, approximately 23.2972 km away, between 2019-05-30 14:17:00 and 2019-05-30 14:53:00. The events included records with hailstones measuring 45.25 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: On the morning of May 30th a surface front was positioned across Pennsylvania, with a surface low positioned west of Chicago, Illinois. Through the day the surface |low moved eastward along the frontal boundary, reaching western Pennsylvania by late in the afternoon. The low then quickly pushed eastward off the NJ coastline by late in the evening, with a cold front crossing the region. In addition, two disturbances aloft moved across the area, one during the mid to late afternoon hours, and another in the evening. Out ahead of the front, warmth and humidity allowed for the development of moderate instability and that coupled with moderate wind shear aloft set the stage for two rounds of scattered showers and thunderstorms, some of which became severe. Two tornadoes occurred across central Maryland. On the morning of May 30th a surface front was positioned across Pennsylvania, with a surface low positioned west of Chicago, Illinois. Through the day the surface |low moved eastward along the frontal boundary, reaching western Pennsylvania by late in the afternoon. The low then quickly pushed eastward off the NJ coastline by late in the evening, with a cold front crossing the region. In addition, two disturbances aloft moved across the area, one during the mid to late afternoon hours, and another in the evening. Out ahead of the front, warmth and humidity allowed for the development of moderate instability and that coupled with moderate wind shear aloft set the stage for two rounds of scattered showers and thunderstorms, some of which became severe. Two tornadoes occurred across central Maryland. On the morning of May 30th a surface front was positioned across Pennsylvania, with a surface low positioned west of Chicago, Illinois. Through the day the surface |low moved eastward along the frontal boundary, reaching western Pennsylvania by late in the afternoon. The low then quickly pushed eastward off the NJ coastline by late in the evening, with a cold front crossing the region. In addition, two disturbances aloft moved across the area, one during the mid to late afternoon hours, and another in the evening. Out ahead of the front, warmth and humidity allowed for the development of moderate instability and that coupled with moderate wind shear aloft set the stage for two rounds of scattered showers and thunderstorms, some of which became severe. Two tornadoes occurred across central Maryland. On the morning of May 30th a surface front was positioned across Pennsylvania, with a surface low positioned west of Chicago, Illinois. Through the day the surface |low moved eastward along the frontal boundary, reaching western Pennsylvania by late in the afternoon. The low then quickly pushed eastward off the NJ coastline by late in the evening, with a cold front crossing the region. In addition, two disturbances aloft moved across the area, one during the mid to late afternoon hours, and another in the evening. Out ahead of the front, warmth and humidity allowed for the development of moderate instability and that coupled with moderate wind shear aloft set the stage for two rounds of scattered showers and thunderstorms, some of which became severe. Two tornadoes occurred across central Maryland. On the morning of May 30th a surface front was positioned across Pennsylvania, with a surface low positioned west of Chicago, Illinois. Through the day the surface |low moved eastward along the frontal boundary, reaching western Pennsylvania by late in the afternoon. The low then quickly pushed eastward off the NJ coastline by late in the evening, with a cold front crossing the region. In addition, two disturbances aloft moved across the area, one during the mid to late afternoon hours, and another in the evening. Out ahead of the front, warmth and humidity allowed for the development of moderate instability and that coupled with moderate wind shear aloft set the stage for two rounds of scattered showers and thunderstorms, some of which became severe. Two tornadoes occurred across central Maryland.\nEvent Narrative: Quarter-sized hail (1.0 inch in diameter) was reported. An EF-1 tornado, with estimated maximum wind speeds around 100 mph, occurred Thursday May 30th 2019 near Glenelg, Maryland. At 3:20 PM EDT (2:20 PM EST), the tornado touched down in a residential community west of Glenelg between Meriweather Drive and Edgewoods Way. As the tornado was passing through the community, it ripped sections of roofing deck off homes. It also snapped and uprooted trees and |large branches, and lofted loose objects hundreds of feet. Moving east-southeast, it crossed over Tridelphia Road and other nearby roads, downing large trees and power lines. As it reached Maryland Route 32 it downed a swath of trees on both sides of the road before moving over and just north of a Howard County Highway Maintenance facility. At the facility, the tornado ripped off its tin roofing, damaged some roof framing, tore a large section of fabric from a salt dome, destroyed garage bay |doors, damaged fencing, and continued to snap and uproot large trees along its path. |Continuing along, it snapped and uprooted large trees in residential areas along Buckskin Lake Drive, Folly Quarter Lane, and Heritage Hill Lane. It also ripped off a section of barn roofing. The tornado lifted at 3:27 PM EDT (2:27 PM EST), over a farm property before it reached Sheppard Lane. A free standing traffic light was blown down at the intersection of Martin Luther King Boulevard and Pennsylvania Avenue. Several trees were also reported blown down in the area. Telephone poles were blown down on Key Highway near McComas Street. A wind gust of 58 knots (67 mph) was measured near Dayton.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 32.4426 km away, between 2019-05-30 15:00:00 and 2019-05-30 16:25:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: On the morning of May 30th a surface front was positioned across Pennsylvania, with a surface low positioned west of Chicago, Illinois. Through the day the surface |low moved eastward along the frontal boundary, reaching western Pennsylvania by late in the afternoon. The low then quickly pushed eastward off the NJ coastline by late in the evening, with a cold front crossing the region. In addition, two disturbances aloft moved across the area, one during the mid to late afternoon hours, and another |in the evening. Out ahead of the front, warmth and humidity allowed for the development of moderate instability and that coupled with moderate wind shear aloft set the stage for two rounds of scattered showers and thunderstorms, some of which produced gusty winds over the waters. On the morning of May 30th a surface front was positioned across Pennsylvania, with a surface low positioned west of Chicago, Illinois. Through the day the surface |low moved eastward along the frontal boundary, reaching western Pennsylvania by late in the afternoon. The low then quickly pushed eastward off the NJ coastline by late in the evening, with a cold front crossing the region. In addition, two disturbances aloft moved across the area, one during the mid to late afternoon hours, and another |in the evening. Out ahead of the front, warmth and humidity allowed for the development of moderate instability and that coupled with moderate wind shear aloft set the stage for two rounds of scattered showers and thunderstorms, some of which produced gusty winds over the waters. On the morning of May 30th a surface front was positioned across Pennsylvania, with a surface low positioned west of Chicago, Illinois. Through the day the surface |low moved eastward along the frontal boundary, reaching western Pennsylvania by late in the afternoon. The low then quickly pushed eastward off the NJ coastline by late in the evening, with a cold front crossing the region. In addition, two disturbances aloft moved across the area, one during the mid to late afternoon hours, and another |in the evening. Out ahead of the front, warmth and humidity allowed for the development of moderate instability and that coupled with moderate wind shear aloft set the stage for two rounds of scattered showers and thunderstorms, some of which produced gusty winds over the waters. On the morning of May 30th a surface front was positioned across Pennsylvania, with a surface low positioned west of Chicago, Illinois. Through the day the surface |low moved eastward along the frontal boundary, reaching western Pennsylvania by late in the afternoon. The low then quickly pushed eastward off the NJ coastline by late in the evening, with a cold front crossing the region. In addition, two disturbances aloft moved across the area, one during the mid to late afternoon hours, and another |in the evening. Out ahead of the front, warmth and humidity allowed for the development of moderate instability and that coupled with moderate wind shear aloft set the stage for two rounds of scattered showers and thunderstorms, some of which produced gusty winds over the waters.\nEvent Narrative: Wind gusts of up to 35 knots were observed at the Baltimore Key Bridge. Wind gusts of up to 34 knots were observed at Kent Island. Wind gusts of up to 48 knots were observed at Thomas Point. Wind gusts of up to 34 knots were observed near Stevensville.", "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00093721, approximately 12.7618 km away, between 2019-06-02 17:15:00 and 2019-06-02 17:36:00. The events included records with hailstones measuring 35.92857142857143 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front approached the region during the day of June 2nd, and that combined with broadly falling heights and increasing instability and wind shear, led to the development of scattered strong to locally severe thunderstorms during the afternoon and evening hours. A cold front approached the region during the day of June 2nd, and that combined with broadly falling heights and increasing instability and wind shear, led to the development of scattered strong to locally severe thunderstorms during the afternoon and evening hours. A cold front approached the region during the day of June 2nd, and that combined with broadly falling heights and increasing instability and wind shear, led to the development of scattered strong to locally severe thunderstorms during the afternoon and evening hours. A cold front approached the region during the day of June 2nd, and that combined with broadly falling heights and increasing instability and wind shear, led to the development of scattered strong to locally severe thunderstorms during the afternoon and evening hours. A cold front approached the region during the day of June 2nd, and that combined with broadly falling heights and increasing instability and wind shear, led to the development of scattered strong to locally severe thunderstorms during the afternoon and evening hours. A cold front approached the region during the day of June 2nd, and that combined with broadly falling heights and increasing instability and wind shear, led to the development of scattered strong to locally severe thunderstorms during the afternoon and evening hours. A cold front approached the region during the day of June 2nd, and that combined with broadly falling heights and increasing instability and wind shear, led to the development of scattered strong to locally severe thunderstorms during the afternoon and evening hours.\nEvent Narrative: Hail up to the size of dimes (0.75 in diameter) was reported. Hail up to the size of dimes (0.75 in diameter) was reported. A tree was blown down in the 10600 block of Guilford Road. A tree was blown down near the intersection of Broken Land Parkway and Cradlerrock Way. A couple of trees were blown down near the intersection of Stevens Forest Road and Broken Land Parkway. A 5-inch in diameter tree limb was blown down onto private property in Elkridge. A 50-knot wind gust was measured at a mesonet near Glen Burnie.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 25.2598 km away, between 2019-06-02 17:42:00 and 2019-06-02 18:35:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front approached the region during the day of June 2nd, and that combined with broadly falling heights and increasing instability and wind shear, led to the development of scattered strong to locally severe thunderstorms during the afternoon and evening hours. A cold front approached the region during the day of June 2nd, and that combined with broadly falling heights and increasing instability and wind shear, led to the development of scattered strong to locally severe thunderstorms during the afternoon and evening hours. A cold front approached the region during the day of June 2nd, and that combined with broadly falling heights and increasing instability and wind shear, led to the development of scattered strong to locally severe thunderstorms during the afternoon and evening hours. A cold front approached the region during the day of June 2nd, and that combined with broadly falling heights and increasing instability and wind shear, led to the development of scattered strong to locally severe thunderstorms during the afternoon and evening hours. A cold front approached the region during the day of June 2nd, and that combined with broadly falling heights and increasing instability and wind shear, led to the development of scattered strong to locally severe thunderstorms during the afternoon and evening hours. A cold front approached the region during the day of June 2nd, and that combined with broadly falling heights and increasing instability and wind shear, led to the development of scattered strong to locally severe thunderstorms during the afternoon and evening hours. A cold front approached the region during the day of June 2nd, and that combined with broadly falling heights and increasing instability and wind shear, led to the development of scattered strong to locally severe thunderstorms during the afternoon and evening hours. A cold front approached the region during the day of June 2nd, and that combined with broadly falling heights and increasing instability and wind shear, led to the development of scattered strong to locally severe thunderstorms during the afternoon and evening hours. A cold front approached the region during the day of June 2nd, and that combined with broadly falling heights and increasing instability and wind shear, led to the development of scattered strong to locally severe thunderstorms during the afternoon and evening hours.\nEvent Narrative: Wind gusts of up to 46 knots were observed. Wind gusts of up to 34 knots were observed. Wind gusts of up to 37 knots were observed. Wind gusts of up to 40 knots were observed. Wind gusts of up to 44 knots were observed. Wind gusts of up to 34 knots were observed. Wind gusts of up to 34 knots were observed. Wind gusts of up to 35 knots were observed. Wind gusts of up to 41 knots were observed.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 47.5049 km away, between 2019-06-13 16:38:00 and 2019-06-13 17:30:00. The events included records with estimated wind gusts of 53.666666666666664 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A potent upper level trough and associated cold front moved into the region during the daylight hours of June 13th. Instability aided by low heights aloft and warm surface temperatures combined with strong wind shear set the stage for scattered strong to locally severe thunderstorms across the region during the afternoon and evening hours. A potent upper level trough and associated cold front moved into the region during the daylight hours of June 13th. Instability aided by low heights aloft and warm surface temperatures combined with strong wind shear set the stage for scattered strong to locally severe thunderstorms across the region during the afternoon and evening hours. A potent upper level trough and associated cold front moved into the region during the daylight hours of June 13th. Instability aided by low heights aloft and warm surface temperatures combined with strong wind shear set the stage for scattered strong to locally severe thunderstorms across the region during the afternoon and evening hours.\nEvent Narrative: A tree was blown down near the intersection of Raintree Avenue and Neudecker Road, closing the roadway. A tree was also blown down at Carrollton Road and Houcksville Road. Eight-inch in diameter trees snapped. A tree was blown down at the intersection of Laurel Bush Road and Point to Point Road. Numerous trees were also blown down along Hunters Run Drive.", "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00093721, approximately 11.6939 km away, between 2019-06-17 15:33:00 and 2019-06-17 16:03:00. The events included records with hailstones measuring 33.666666666666664 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: While large scale forcing was weak across the region on June 17th, a zone of differential heating and a weak lee trough near the Blue Ridge, when combined with local terrain and sea-breeze circulations, were enough to generate scattered thunderstorms across the region during the afternoon and evening hours. Marginal instability and sufficient wind shear promoted the growth of some of these thunderstorms to severe levels. While large scale forcing was weak across the region on June 17th, a zone of differential heating and a weak lee trough near the Blue Ridge, when combined with local terrain and sea-breeze circulations, were enough to generate scattered thunderstorms across the region during the afternoon and evening hours. Marginal instability and sufficient wind shear promoted the growth of some of these thunderstorms to severe levels. While large scale forcing was weak across the region on June 17th, a zone of differential heating and a weak lee trough near the Blue Ridge, when combined with local terrain and sea-breeze circulations, were enough to generate scattered thunderstorms across the region during the afternoon and evening hours. Marginal instability and sufficient wind shear promoted the growth of some of these thunderstorms to severe levels.\nEvent Narrative: Hail up to the size of quarters (1.0 in diameter) was reported. A tree was blown down near the intersection of Stevenson Road and McNelin Way. A tree was blown down on Catherine Avenue near Schramms Crossing.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 31.0543 km away, between 2019-06-17 18:36:00 and 2019-06-17 18:36:00. The events included records with measured wind gusts of 39.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: While large scale forcing was weak across the region on June 17th, a zone of differential heating and a weak lee trough near the Blue Ridge, when combined with local terrain and sea-breeze circulations, were enough to generate scattered thunderstorms across the region during the afternoon and evening hours. Marginal instability and sufficient wind shear promoted the growth of some of these thunderstorms to levels strong enough to produce gusty winds over the waters.\nEvent Narrative: Wind gusts of up to 39 knots were observed.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 34.1063 km away, between 2019-06-20 13:43:00 and 2019-06-20 19:00:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Scattered showers and thunderstorms developed during the afternoon and evening hours, some of which produced gusty winds across the waters. Scattered showers and thunderstorms developed during the afternoon and evening hours, some of which produced gusty winds across the waters. Scattered showers and thunderstorms developed during the afternoon and evening hours, some of which produced gusty winds across the waters. Scattered showers and thunderstorms developed during the afternoon and evening hours, some of which produced gusty winds across the waters. Scattered showers and thunderstorms developed during the afternoon and evening hours, some of which produced gusty winds across the waters. Scattered showers and thunderstorms developed during the afternoon and evening hours, some of which produced gusty winds across the waters.\nEvent Narrative: Wind gusts of up to 34 knots were observed. Wind gusts of up to 40 knots were observed. Wind gusts of up to 35 knots were observed. Wind gusts of up to 35 knots were observed. Wind gusts of up to 34 knots were observed. Wind gusts of up to 39 knots were observed.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 21.3567 km away, between 2019-06-28 14:55:00 and 2019-06-28 14:55:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: While large scale forcing was weak, moderate amounts of instability combined with local terrain circulations and remnant mesoscale boundaries to generate scattered showers and thunderstorms in the afternoon. With steep low level lapse rates, a few of these storms became strong to locally severe.\nEvent Narrative: Multiple trees were down in the Rosedale area, including one onto a house.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 14.0067 km away, between 2019-06-28 17:54:00 and 2019-06-28 18:12:00. The events included records with measured wind gusts of 37.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: While large scale forcing was weak, moderate amounts of instability combined with local terrain circulations and remnant mesoscale boundaries to generate scattered showers and thunderstorms in the afternoon. With steep low level lapse rates, one of these thunderstorms produced gusty winds over the waters.\nEvent Narrative: Wind gusts of up to 37 knots were observed.", "The following events were reported: Flood. These occurred near station USW00093721, approximately 21.3333 km away, between 2019-06-28 18:10:00 and 2019-06-28 20:10:00. The flood was caused by Heavy Rain. Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: An isolated flooding incident occurred in Anne Arundel County due to locally heavy rain.\nEvent Narrative: A vehicle was trapped in high water near the intersection of Defense Highway and Saint Stephens Road.", "The following events were reported: Marine Hail, Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 29.779 km away, between 2019-06-29 15:10:00 and 2019-06-29 22:47:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Heat and humidity through the day on June 29th led to a moderately unstable air mass by the afternoon. A weak pressure trough developed and heights began to fall by the evening as an upper level ridge broke down. Also late in the evening, a cold front began to approach, increasing forcing across the region. Several rounds of scattered showers and thunderstorms developed from the mid afternoon hours through well past sunset. Some thunderstorms produced gusty winds over the waters. Heat and humidity through the day on June 29th led to a moderately unstable air mass by the afternoon. A weak pressure trough developed and heights began to fall by the evening as an upper level ridge broke down. Also late in the evening, a cold front began to approach, increasing forcing across the region. Several rounds of scattered showers and thunderstorms developed from the mid afternoon hours through well past sunset. Some thunderstorms produced gusty winds over the waters. Heat and humidity through the day on June 29th led to a moderately unstable air mass by the afternoon. A weak pressure trough developed and heights began to fall by the evening as an upper level ridge broke down. Also late in the evening, a cold front began to approach, increasing forcing across the region. Several rounds of scattered showers and thunderstorms developed from the mid afternoon hours through well past sunset. Some thunderstorms produced gusty winds over the waters. Heat and humidity through the day on June 29th led to a moderately unstable air mass by the afternoon. A weak pressure trough developed and heights began to fall by the evening as an upper level ridge broke down. Also late in the evening, a cold front began to approach, increasing forcing across the region. Several rounds of scattered showers and thunderstorms developed from the mid afternoon hours through well past sunset. Some thunderstorms produced gusty winds over the waters. Heat and humidity through the day on June 29th led to a moderately unstable air mass by the afternoon. A weak pressure trough developed and heights began to fall by the evening as an upper level ridge broke down. Also late in the evening, a cold front began to approach, increasing forcing across the region. Several rounds of scattered showers and thunderstorms developed from the mid afternoon hours through well past sunset. Some thunderstorms produced gusty winds over the waters. Heat and humidity through the day on June 29th led to a moderately unstable air mass by the afternoon. A weak pressure trough developed and heights began to fall by the evening as an upper level ridge broke down. Also late in the evening, a cold front began to approach, increasing forcing across the region. Several rounds of scattered showers and thunderstorms developed from the mid afternoon hours through well past sunset. Some thunderstorms produced gusty winds over the waters. Heat and humidity through the day on June 29th led to a moderately unstable air mass by the afternoon. A weak pressure trough developed and heights began to fall by the evening as an upper level ridge broke down. Also late in the evening, a cold front began to approach, increasing forcing across the region. Several rounds of scattered showers and thunderstorms developed from the mid afternoon hours through well past sunset. Some thunderstorms produced gusty winds over the waters. Heat and humidity through the day on June 29th led to a moderately unstable air mass by the afternoon. A weak pressure trough developed and heights began to fall by the evening as an upper level ridge broke down. Also late in the evening, a cold front began to approach, increasing forcing across the region. Several rounds of scattered showers and thunderstorms developed from the mid afternoon hours through well past sunset. Some thunderstorms produced gusty winds over the waters. Heat and humidity through the day on June 29th led to a moderately unstable air mass by the afternoon. A weak pressure trough developed and heights began to fall by the evening as an upper level ridge broke down. Also late in the evening, a cold front began to approach, increasing forcing across the region. Several rounds of scattered showers and thunderstorms developed from the mid afternoon hours through well past sunset. Some thunderstorms produced gusty winds over the waters. Heat and humidity through the day on June 29th led to a moderately unstable air mass by the afternoon. A weak pressure trough developed and heights began to fall by the evening as an upper level ridge broke down. Also late in the evening, a cold front began to approach, increasing forcing across the region. Several rounds of scattered showers and thunderstorms developed from the mid afternoon hours through well past sunset. Some thunderstorms produced gusty winds over the waters. Heat and humidity through the day on June 29th led to a moderately unstable air mass by the afternoon. A weak pressure trough developed and heights began to fall by the evening as an upper level ridge broke down. Also late in the evening, a cold front began to approach, increasing forcing across the region. Several rounds of scattered showers and thunderstorms developed from the mid afternoon hours through well past sunset. Some thunderstorms produced gusty winds over the waters. Heat and humidity through the day on June 29th led to a moderately unstable air mass by the afternoon. A weak pressure trough developed and heights began to fall by the evening as an upper level ridge broke down. Also late in the evening, a cold front began to approach, increasing forcing across the region. Several rounds of scattered showers and thunderstorms developed from the mid afternoon hours through well past sunset. Some thunderstorms produced gusty winds over the waters. Heat and humidity through the day on June 29th led to a moderately unstable air mass by the afternoon. A weak pressure trough developed and heights began to fall by the evening as an upper level ridge broke down. Also late in the evening, a cold front began to approach, increasing forcing across the region. Several rounds of scattered showers and thunderstorms developed from the mid afternoon hours through well past sunset. Some thunderstorms produced gusty winds over the waters. Heat and humidity through the day on June 29th led to a moderately unstable air mass by the afternoon. A weak pressure trough developed and heights began to fall by the evening as an upper level ridge broke down. Also late in the evening, a cold front began to approach, increasing forcing across the region. Several rounds of scattered showers and thunderstorms developed from the mid afternoon hours through well past sunset. Some thunderstorms produced gusty winds over the waters. Heat and humidity through the day on June 29th led to a moderately unstable air mass by the afternoon. A weak pressure trough developed and heights began to fall by the evening as an upper level ridge broke down. Also late in the evening, a cold front began to approach, increasing forcing across the region. Several rounds of scattered showers and thunderstorms developed from the mid afternoon hours through well past sunset. Some thunderstorms produced gusty winds over the waters.\nEvent Narrative: Wind gusts of up to 36 knots were observed. Wind gusts of up to 34 knots were observed. Wind gusts of up to 36 knots were observed. Wind gusts of up to 36 knots were observed. Wind gusts of up to 34 knots were observed. Wind gusts of up to 46 knots were observed. Wind gusts of up to 34 knots were observed. Wind gusts of up to 36 knots were observed. Wind gusts of up to 34 knots were observed. Wind gusts of up to 41 knots were observed. Hail up to 1.75 inches in diameter was observed. Wind gusts of up to 37 knots were observed. Wind gusts of up to 34 knots were observed. Wind gusts of up to 34 knots were observed. Wind gusts of up to 38 knots were observed.", "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00093721, approximately 21.331 km away, between 2019-06-29 15:18:00 and 2019-06-29 22:47:00. The events included records with hailstones measuring 41.958333333333336 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Heat and humidity through the day on June 29th led to a moderately unstable air mass by the afternoon. A weak pressure trough developed and heights began to fall by the evening as an upper level ridge broke down. Also late in the evening, a cold front began to approach, increasing forcing across the region. Several rounds of scattered showers and thunderstorms developed from the mid afternoon hours through well past sunset. Some thunderstorms became strong to severe. Heat and humidity through the day on June 29th led to a moderately unstable air mass by the afternoon. A weak pressure trough developed and heights began to fall by the evening as an upper level ridge broke down. Also late in the evening, a cold front began to approach, increasing forcing across the region. Several rounds of scattered showers and thunderstorms developed from the mid afternoon hours through well past sunset. Some thunderstorms became strong to severe. Heat and humidity through the day on June 29th led to a moderately unstable air mass by the afternoon. A weak pressure trough developed and heights began to fall by the evening as an upper level ridge broke down. Also late in the evening, a cold front began to approach, increasing forcing across the region. Several rounds of scattered showers and thunderstorms developed from the mid afternoon hours through well past sunset. Some thunderstorms became strong to severe. Heat and humidity through the day on June 29th led to a moderately unstable air mass by the afternoon. A weak pressure trough developed and heights began to fall by the evening as an upper level ridge broke down. Also late in the evening, a cold front began to approach, increasing forcing across the region. Several rounds of scattered showers and thunderstorms developed from the mid afternoon hours through well past sunset. Some thunderstorms became strong to severe. Heat and humidity through the day on June 29th led to a moderately unstable air mass by the afternoon. A weak pressure trough developed and heights began to fall by the evening as an upper level ridge broke down. Also late in the evening, a cold front began to approach, increasing forcing across the region. Several rounds of scattered showers and thunderstorms developed from the mid afternoon hours through well past sunset. Some thunderstorms became strong to severe. Heat and humidity through the day on June 29th led to a moderately unstable air mass by the afternoon. A weak pressure trough developed and heights began to fall by the evening as an upper level ridge broke down. Also late in the evening, a cold front began to approach, increasing forcing across the region. Several rounds of scattered showers and thunderstorms developed from the mid afternoon hours through well past sunset. Some thunderstorms became strong to severe.\nEvent Narrative: Hail up to the size of golf balls (1.75 in diameter) was reported. Some vehicles sustained damage. A large tree was blown down near the intersection of Race Road and Furnace Road. A tree was blown down on Bucks Haven Lane near Bucks Haven Court. Six trees were blown down, some onto wires, in the Pasadena area. Tree limbs were blown down onto power lines in the Laurel area. A tree was blown down on Annapolis Rock Road between Hipsley Mill Road and the Montgomery and Howard County line.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 34.3074 km away, between 2019-07-02 16:04:00 and 2019-07-02 19:07:00. The events included records with estimated wind gusts of 51.1 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Increasing temperatures and low level moisture led to developing instability across the region during the day of July 2nd. The strongest mid-level forcing remained to the north across northern PA/OH where a stationary boundary lingered. However a weak upper level shortwave trough moving through did help showers and scattered thunderstorms to develop across the state, and given the instability a few became severe. Increasing temperatures and low level moisture led to developing instability across the region during the day of July 2nd. The strongest mid-level forcing remained to the north across northern PA/OH where a stationary boundary lingered. However a weak upper level shortwave trough moving through did help showers and scattered thunderstorms to develop across the state, and given the instability a few became severe. Increasing temperatures and low level moisture led to developing instability across the region during the day of July 2nd. The strongest mid-level forcing remained to the north across northern PA/OH where a stationary boundary lingered. However a weak upper level shortwave trough moving through did help showers and scattered thunderstorms to develop across the state, and given the instability a few became severe. Increasing temperatures and low level moisture led to developing instability across the region during the day of July 2nd. The strongest mid-level forcing remained to the north across northern PA/OH where a stationary boundary lingered. However a weak upper level shortwave trough moving through did help showers and scattered thunderstorms to develop across the state, and given the instability a few became severe. Increasing temperatures and low level moisture led to developing instability across the region during the day of July 2nd. The strongest mid-level forcing remained to the north across northern PA/OH where a stationary boundary lingered. However a weak upper level shortwave trough moving through did help showers and scattered thunderstorms to develop across the state, and given the instability a few became severe. Increasing temperatures and low level moisture led to developing instability across the region during the day of July 2nd. The strongest mid-level forcing remained to the north across northern PA/OH where a stationary boundary lingered. However a weak upper level shortwave trough moving through did help showers and scattered thunderstorms to develop across the state, and given the instability a few became severe. Increasing temperatures and low level moisture led to developing instability across the region during the day of July 2nd. The strongest mid-level forcing remained to the north across northern PA/OH where a stationary boundary lingered. However a weak upper level shortwave trough moving through did help showers and scattered thunderstorms to develop across the state, and given the instability a few became severe. Increasing temperatures and low level moisture led to developing instability across the region during the day of July 2nd. The strongest mid-level forcing remained to the north across northern PA/OH where a stationary boundary lingered. However a weak upper level shortwave trough moving through did help showers and scattered thunderstorms to develop across the state, and given the instability a few became severe. Increasing temperatures and low level moisture led to developing instability across the region during the day of July 2nd. The strongest mid-level forcing remained to the north across northern PA/OH where a stationary boundary lingered. However a weak upper level shortwave trough moving through did help showers and scattered thunderstorms to develop across the state, and given the instability a few became severe. Increasing temperatures and low level moisture led to developing instability across the region during the day of July 2nd. The strongest mid-level forcing remained to the north across northern PA/OH where a stationary boundary lingered. However a weak upper level shortwave trough moving through did help showers and scattered thunderstorms to develop across the state, and given the instability a few became severe.\nEvent Narrative: Multiple trees and power lines were reported down in the Sandy Spring area. A tree was blown down in the 3900 block of Winchester Lane. A tree was blown down onto wires along Ingleside Road. A tree was blown down on a house in the 17900 block of Shotley Bridge Place. A tree was blown down at the intersection of Old Annapolis Road and Collington Road. Wires were also blown down in the 9800 block of Franklin Avenue and in the 12400 block of Canfield Lane. Multiple trees and power lines down on Hamilton Court northeast of Eldersburg. A tree was blown down in the 3600 block of Woodbine Road. A tree was blown down at the intersection of Falls Road and Black Road Road. Several trees were blown down near the intersection of Union Chapel Road and McNeal Road. Multiple reports of trees and power lines down in Laytonsville.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 30.3974 km away, between 2019-07-02 17:08:00 and 2019-07-02 20:00:00. The events included records with measured wind gusts of 35.214285714285715 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Increasing temperatures and low level moisture led to developing instability across the region during the day of July 2nd. The strongest mid-level forcing remained to the north across northern PA/OH where a stationary boundary lingered. However a weak upper level shortwave trough moving through did help showers and scattered thunderstorms to develop across the area, and given the instability a few produced gusty winds over the waters. Increasing temperatures and low level moisture led to developing instability across the region during the day of July 2nd. The strongest mid-level forcing remained to the north across northern PA/OH where a stationary boundary lingered. However a weak upper level shortwave trough moving through did help showers and scattered thunderstorms to develop across the area, and given the instability a few produced gusty winds over the waters. Increasing temperatures and low level moisture led to developing instability across the region during the day of July 2nd. The strongest mid-level forcing remained to the north across northern PA/OH where a stationary boundary lingered. However a weak upper level shortwave trough moving through did help showers and scattered thunderstorms to develop across the area, and given the instability a few produced gusty winds over the waters. Increasing temperatures and low level moisture led to developing instability across the region during the day of July 2nd. The strongest mid-level forcing remained to the north across northern PA/OH where a stationary boundary lingered. However a weak upper level shortwave trough moving through did help showers and scattered thunderstorms to develop across the area, and given the instability a few produced gusty winds over the waters. Increasing temperatures and low level moisture led to developing instability across the region during the day of July 2nd. The strongest mid-level forcing remained to the north across northern PA/OH where a stationary boundary lingered. However a weak upper level shortwave trough moving through did help showers and scattered thunderstorms to develop across the area, and given the instability a few produced gusty winds over the waters. Increasing temperatures and low level moisture led to developing instability across the region during the day of July 2nd. The strongest mid-level forcing remained to the north across northern PA/OH where a stationary boundary lingered. However a weak upper level shortwave trough moving through did help showers and scattered thunderstorms to develop across the area, and given the instability a few produced gusty winds over the waters. Increasing temperatures and low level moisture led to developing instability across the region during the day of July 2nd. The strongest mid-level forcing remained to the north across northern PA/OH where a stationary boundary lingered. However a weak upper level shortwave trough moving through did help showers and scattered thunderstorms to develop across the area, and given the instability a few produced gusty winds over the waters. Increasing temperatures and low level moisture led to developing instability across the region during the day of July 2nd. The strongest mid-level forcing remained to the north across northern PA/OH where a stationary boundary lingered. However a weak upper level shortwave trough moving through did help showers and scattered thunderstorms to develop across the area, and given the instability a few produced gusty winds over the waters. Increasing temperatures and low level moisture led to developing instability across the region during the day of July 2nd. The strongest mid-level forcing remained to the north across northern PA/OH where a stationary boundary lingered. However a weak upper level shortwave trough moving through did help showers and scattered thunderstorms to develop across the area, and given the instability a few produced gusty winds over the waters. Increasing temperatures and low level moisture led to developing instability across the region during the day of July 2nd. The strongest mid-level forcing remained to the north across northern PA/OH where a stationary boundary lingered. However a weak upper level shortwave trough moving through did help showers and scattered thunderstorms to develop across the area, and given the instability a few produced gusty winds over the waters. Increasing temperatures and low level moisture led to developing instability across the region during the day of July 2nd. The strongest mid-level forcing remained to the north across northern PA/OH where a stationary boundary lingered. However a weak upper level shortwave trough moving through did help showers and scattered thunderstorms to develop across the area, and given the instability a few produced gusty winds over the waters. Increasing temperatures and low level moisture led to developing instability across the region during the day of July 2nd. The strongest mid-level forcing remained to the north across northern PA/OH where a stationary boundary lingered. However a weak upper level shortwave trough moving through did help showers and scattered thunderstorms to develop across the area, and given the instability a few produced gusty winds over the waters. Increasing temperatures and low level moisture led to developing instability across the region during the day of July 2nd. The strongest mid-level forcing remained to the north across northern PA/OH where a stationary boundary lingered. However a weak upper level shortwave trough moving through did help showers and scattered thunderstorms to develop across the area, and given the instability a few produced gusty winds over the waters. Increasing temperatures and low level moisture led to developing instability across the region during the day of July 2nd. The strongest mid-level forcing remained to the north across northern PA/OH where a stationary boundary lingered. However a weak upper level shortwave trough moving through did help showers and scattered thunderstorms to develop across the area, and given the instability a few produced gusty winds over the waters.\nEvent Narrative:", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 22.2318 km away, between 2019-07-04 12:47:00 and 2019-07-04 12:47:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Heat and plentiful low level moisture led to the development of instability and therefore scattered showers and thunderstorms during the afternoon of July 4th. While forcing was limited, some of the thunderstorms did briefly become pulse severe.\nEvent Narrative: Large tree limbs were blown down onto power lines in the 3500 block of Madonna Lane.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 31.6019 km away, between 2019-07-06 13:47:00 and 2019-07-06 19:48:00. The events included records with measured wind gusts of 39.25 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: An approaching cold front coupled with upper level shortwave energy and instability across the region led to the development of afternoon scattered showers and thunderstorms. Several of these thunderstorms produced gusty winds over the waters. An approaching cold front coupled with upper level shortwave energy and instability across the region led to the development of afternoon scattered showers and thunderstorms. Several of these thunderstorms produced gusty winds over the waters. An approaching cold front coupled with upper level shortwave energy and instability across the region led to the development of afternoon scattered showers and thunderstorms. Several of these thunderstorms produced gusty winds over the waters. An approaching cold front coupled with upper level shortwave energy and instability across the region led to the development of afternoon scattered showers and thunderstorms. Several of these thunderstorms produced gusty winds over the waters.\nEvent Narrative:", "The following events were reported: Flash Flood, Flood. These occurred near station USW00093721, approximately 31.9746 km away, between 2019-07-08 09:15:00 and 2019-07-08 14:34:00. The flood was caused by Heavy Rain. Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A nearly stationary boundary set up near the Potomac River weak low pressure developed along the boundary. There was plenty of moisture in place from the Atlantic and Gulf of Mexico, and this combined with instability to produce very heavy rainfall rates in convection that developed. Convection was maximized around the boundary across central Maryland, and this led to several instances of flooding and flash flooding. A nearly stationary boundary set up near the Potomac River weak low pressure developed along the boundary. There was plenty of moisture in place from the Atlantic and Gulf of Mexico, and this combined with instability to produce very heavy rainfall rates in convection that developed. Convection was maximized around the boundary across central Maryland, and this led to several instances of flooding and flash flooding. A nearly stationary boundary set up near the Potomac River weak low pressure developed along the boundary. There was plenty of moisture in place from the Atlantic and Gulf of Mexico, and this combined with instability to produce very heavy rainfall rates in convection that developed. Convection was maximized around the boundary across central Maryland, and this led to several instances of flooding and flash flooding. A nearly stationary boundary set up near the Potomac River weak low pressure developed along the boundary. There was plenty of moisture in place from the Atlantic and Gulf of Mexico, and this combined with instability to produce very heavy rainfall rates in convection that developed. Convection was maximized around the boundary across central Maryland, and this led to several instances of flooding and flash flooding. A nearly stationary boundary set up near the Potomac River weak low pressure developed along the boundary. There was plenty of moisture in place from the Atlantic and Gulf of Mexico, and this combined with instability to produce very heavy rainfall rates in convection that developed. Convection was maximized around the boundary across central Maryland, and this led to several instances of flooding and flash flooding.\nEvent Narrative: River Road was closed due to flooding along the South Branch Patapsco River. Trotter road was impassable due to water flowing over the road. Two to three feet of water was flowing over portions of Brighton Dam Road in the 1900 and 2200 Blocks. Gue Road was closed due to flooding. River road was closed due to flooding along the South Branch Patapsco River due to flooding.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 41.0001 km away, between 2019-07-11 15:15:00 and 2019-07-11 15:58:00. The events included records with estimated wind gusts of 52.2 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front approached from the west during the day of July 11th, with warm and moist air advection occurring on southerly flow. This promoted the development of significant amounts of instability, and that coupled with an approaching shortwave trough and modest shear values, led to the generation of scattered showers and thunderstorms, some of which became severe. A cold front approached from the west during the day of July 11th, with warm and moist air advection occurring on southerly flow. This promoted the development of significant amounts of instability, and that coupled with an approaching shortwave trough and modest shear values, led to the generation of scattered showers and thunderstorms, some of which became severe. A cold front approached from the west during the day of July 11th, with warm and moist air advection occurring on southerly flow. This promoted the development of significant amounts of instability, and that coupled with an approaching shortwave trough and modest shear values, led to the generation of scattered showers and thunderstorms, some of which became severe. A cold front approached from the west during the day of July 11th, with warm and moist air advection occurring on southerly flow. This promoted the development of significant amounts of instability, and that coupled with an approaching shortwave trough and modest shear values, led to the generation of scattered showers and thunderstorms, some of which became severe. A cold front approached from the west during the day of July 11th, with warm and moist air advection occurring on southerly flow. This promoted the development of significant amounts of instability, and that coupled with an approaching shortwave trough and modest shear values, led to the generation of scattered showers and thunderstorms, some of which became severe.\nEvent Narrative: Multiple power poles were blown down in the 4000 block of Chapel Road. A tree was blown down onto power lines in the 100 block of Philadelphia Road. A tree was blown down across MD-7 near Joppa Farm Road. A tree was blown down across the roadway near the intersection of Guyton Road and Bottom Road just before the bridge. A large 8-inch diameter tree limb was blown near the intersection of Old Joppa Road and Old Mountain Road North. A tree was blown down in the 2300 block of Dunwood Lane. A tree was also blown down near the intersection of Old Joppa Road and Woodtaker Mill Road. A tree was blown down near the intersection of Pleasantville Road and High Point Road.", "The following events were reported: Flash Flood, Flood. These occurred near station USW00093721, approximately 39.5009 km away, between 2019-07-11 15:25:00 and 2019-07-11 20:31:00. The flood was caused by Heavy Rain. Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front moved into the area on the 11th, and out ahead of the boundary there was a warm and very humid airmass. The warm and humid airmass caused an unstable atmosphere which led to the development of showers and thunderstorms. Storms produced heavy rainfall, and they were slow to move due to a weak flow aloft. This led to instances of flooding and flash flooding. A cold front moved into the area on the 11th, and out ahead of the boundary there was a warm and very humid airmass. The warm and humid airmass caused an unstable atmosphere which led to the development of showers and thunderstorms. Storms produced heavy rainfall, and they were slow to move due to a weak flow aloft. This led to instances of flooding and flash flooding. A cold front moved into the area on the 11th, and out ahead of the boundary there was a warm and very humid airmass. The warm and humid airmass caused an unstable atmosphere which led to the development of showers and thunderstorms. Storms produced heavy rainfall, and they were slow to move due to a weak flow aloft. This led to instances of flooding and flash flooding. A cold front moved into the area on the 11th, and out ahead of the boundary there was a warm and very humid airmass. The warm and humid airmass caused an unstable atmosphere which led to the development of showers and thunderstorms. Storms produced heavy rainfall, and they were slow to move due to a weak flow aloft. This led to instances of flooding and flash flooding. A cold front moved into the area on the 11th, and out ahead of the boundary there was a warm and very humid airmass. The warm and humid airmass caused an unstable atmosphere which led to the development of showers and thunderstorms. Storms produced heavy rainfall, and they were slow to move due to a weak flow aloft. This led to instances of flooding and flash flooding. A cold front moved into the area on the 11th, and out ahead of the boundary there was a warm and very humid airmass. The warm and humid airmass caused an unstable atmosphere which led to the development of showers and thunderstorms. Storms produced heavy rainfall, and they were slow to move due to a weak flow aloft. This led to instances of flooding and flash flooding. A cold front moved into the area on the 11th, and out ahead of the boundary there was a warm and very humid airmass. The warm and humid airmass caused an unstable atmosphere which led to the development of showers and thunderstorms. Storms produced heavy rainfall, and they were slow to move due to a weak flow aloft. This led to instances of flooding and flash flooding. A cold front moved into the area on the 11th, and out ahead of the boundary there was a warm and very humid airmass. The warm and humid airmass caused an unstable atmosphere which led to the development of showers and thunderstorms. Storms produced heavy rainfall, and they were slow to move due to a weak flow aloft. This led to instances of flooding and flash flooding. A cold front moved into the area on the 11th, and out ahead of the boundary there was a warm and very humid airmass. The warm and humid airmass caused an unstable atmosphere which led to the development of showers and thunderstorms. Storms produced heavy rainfall, and they were slow to move due to a weak flow aloft. This led to instances of flooding and flash flooding. A cold front moved into the area on the 11th, and out ahead of the boundary there was a warm and very humid airmass. The warm and humid airmass caused an unstable atmosphere which led to the development of showers and thunderstorms. Storms produced heavy rainfall, and they were slow to move due to a weak flow aloft. This led to instances of flooding and flash flooding. A cold front moved into the area on the 11th, and out ahead of the boundary there was a warm and very humid airmass. The warm and humid airmass caused an unstable atmosphere which led to the development of showers and thunderstorms. Storms produced heavy rainfall, and they were slow to move due to a weak flow aloft. This led to instances of flooding and flash flooding. A cold front moved into the area on the 11th, and out ahead of the boundary there was a warm and very humid airmass. The warm and humid airmass caused an unstable atmosphere which led to the development of showers and thunderstorms. Storms produced heavy rainfall, and they were slow to move due to a weak flow aloft. This led to instances of flooding and flash flooding. A cold front moved into the area on the 11th, and out ahead of the boundary there was a warm and very humid airmass. The warm and humid airmass caused an unstable atmosphere which led to the development of showers and thunderstorms. Storms produced heavy rainfall, and they were slow to move due to a weak flow aloft. This led to instances of flooding and flash flooding. A cold front moved into the area on the 11th, and out ahead of the boundary there was a warm and very humid airmass. The warm and humid airmass caused an unstable atmosphere which led to the development of showers and thunderstorms. Storms produced heavy rainfall, and they were slow to move due to a weak flow aloft. This led to instances of flooding and flash flooding. A cold front moved into the area on the 11th, and out ahead of the boundary there was a warm and very humid airmass. The warm and humid airmass caused an unstable atmosphere which led to the development of showers and thunderstorms. Storms produced heavy rainfall, and they were slow to move due to a weak flow aloft. This led to instances of flooding and flash flooding. A cold front moved into the area on the 11th, and out ahead of the boundary there was a warm and very humid airmass. The warm and humid airmass caused an unstable atmosphere which led to the development of showers and thunderstorms. Storms produced heavy rainfall, and they were slow to move due to a weak flow aloft. This led to instances of flooding and flash flooding. A cold front moved into the area on the 11th, and out ahead of the boundary there was a warm and very humid airmass. The warm and humid airmass caused an unstable atmosphere which led to the development of showers and thunderstorms. Storms produced heavy rainfall, and they were slow to move due to a weak flow aloft. This led to instances of flooding and flash flooding. A cold front moved into the area on the 11th, and out ahead of the boundary there was a warm and very humid airmass. The warm and humid airmass caused an unstable atmosphere which led to the development of showers and thunderstorms. Storms produced heavy rainfall, and they were slow to move due to a weak flow aloft. This led to instances of flooding and flash flooding. A cold front moved into the area on the 11th, and out ahead of the boundary there was a warm and very humid airmass. The warm and humid airmass caused an unstable atmosphere which led to the development of showers and thunderstorms. Storms produced heavy rainfall, and they were slow to move due to a weak flow aloft. This led to instances of flooding and flash flooding. A cold front moved into the area on the 11th, and out ahead of the boundary there was a warm and very humid airmass. The warm and humid airmass caused an unstable atmosphere which led to the development of showers and thunderstorms. Storms produced heavy rainfall, and they were slow to move due to a weak flow aloft. This led to instances of flooding and flash flooding.\nEvent Narrative: Singer Road was flooded in multiple locations including near Mountain Road. The 3200 Block of Clayton Road was completely flooded. There was a swift water rescue with two to three feet of water over the road. A vehicle was stuck in flood waters near the intersection of Garrison Forest Road and Greenspring Valley Road. The water level at Edgewood on Otter Point Creek rapidly rose above flood stage of 8 feet. The level crested at 10.29 feet at 5:30 PM EST. Significant flooding occurred along Winters Run Road in multiple spots between Singer Road and Route 7. The water level at White Marsh Run rapidly rose above the flood stage of 11 feet, cresting at 13.30 feet on July 11th at 5:45 PM EST. This caused flooding near Town Center Court. The water level at Glen Arm along the Minebank Run rapidly rose above the flood stage of 10 feet, cresting at 10.12 feet on July 11th at 4:00 PM EST. Water covered the access road to Talmar. Both sides of Patterson Mill Road were flooded near the intersection of Patterson Mill Road and Wheel Road. Fifty feet of the bridge was washed away near the intersection of Singer Road and Winters Run Bridge. Wheel Road was flooded between Cedar Lane and Laurel Bush Road. A vehicle was stuck in flood waters near the intersection of Bottom Road and Williams Road. Flash flooding caused the road to be impassible at the 8000 Block of Harris Avenue in Parkville. A vehicle was on its side due to flood waters near US 40 and Big Gunpowder Falls. Multiple cars were stuck in flood waters on Honeygo Boulevard in White Marsh. The water level at White Marsh along the Honeygo Run passed flood stage of 6 feet. Water flowed around a business on Ebenezer Road. The water level crested at 7.84 feet at 5:30 PM EST. Route 7 was completely flooded at Fashion Way. Us Route 1 was flooded and closed in both directions at Connolly Road in Bel Air. The water level at Edgewood on Otter Point Creek rapidly remained above the flood stage of 8 feet. Significant flooding occurred along Winters Run Road in multiple spots between Singer Road and Route 7. The road was flooded near the intersection of Old Joppa Road and Woodtaker Mill Road. There was a report of more than eighteen inches of water across the roadway in the 300 Block of Regal Drive.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 34.6834 km away, between 2019-07-11 16:03:00 and 2019-07-11 18:00:00. The events included records with measured wind gusts of 37.714285714285715 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front approached from the west during the day of July 11th, with warm and moist air advection occurring on southerly flow. This promoted the development of significant amounts of instability, and that coupled with an approaching shortwave trough and modest shear values, led to the generation of scattered showers and thunderstorms, some of which produced gusty winds over the waters. A cold front approached from the west during the day of July 11th, with warm and moist air advection occurring on southerly flow. This promoted the development of significant amounts of instability, and that coupled with an approaching shortwave trough and modest shear values, led to the generation of scattered showers and thunderstorms, some of which produced gusty winds over the waters. A cold front approached from the west during the day of July 11th, with warm and moist air advection occurring on southerly flow. This promoted the development of significant amounts of instability, and that coupled with an approaching shortwave trough and modest shear values, led to the generation of scattered showers and thunderstorms, some of which produced gusty winds over the waters. A cold front approached from the west during the day of July 11th, with warm and moist air advection occurring on southerly flow. This promoted the development of significant amounts of instability, and that coupled with an approaching shortwave trough and modest shear values, led to the generation of scattered showers and thunderstorms, some of which produced gusty winds over the waters. A cold front approached from the west during the day of July 11th, with warm and moist air advection occurring on southerly flow. This promoted the development of significant amounts of instability, and that coupled with an approaching shortwave trough and modest shear values, led to the generation of scattered showers and thunderstorms, some of which produced gusty winds over the waters. A cold front approached from the west during the day of July 11th, with warm and moist air advection occurring on southerly flow. This promoted the development of significant amounts of instability, and that coupled with an approaching shortwave trough and modest shear values, led to the generation of scattered showers and thunderstorms, some of which produced gusty winds over the waters. A cold front approached from the west during the day of July 11th, with warm and moist air advection occurring on southerly flow. This promoted the development of significant amounts of instability, and that coupled with an approaching shortwave trough and modest shear values, led to the generation of scattered showers and thunderstorms, some of which produced gusty winds over the waters.\nEvent Narrative:", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 49.3165 km away, between 2019-07-11 16:55:00 and 2019-07-11 16:55:00. The events included records with estimated wind gusts of 55.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A warm front moved through the mid-Atlantic on July 11. As it did so, a long fetch southwesterly flow developed. This brought warm and extremely humid air into the region, with moisture being drawn up from a developing tropical storm in the Gulf of Mexico. In the warm sector, widespread convection developed during the afternoon and evening. The primary impact was severe flash flooding in the tropical air mass. However, with a warm and unstable atmosphere in place and moderate shear thanks to the nearby front, some storms also became severe.\nEvent Narrative: Trees were reported down from Grasonville to Queenstown.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 31.2372 km away, between 2019-07-17 16:28:00 and 2019-07-17 17:20:00. The events included records with estimated wind gusts of 55.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: On July 17th, the remnant circulation of Barry moved into Pennsylvania with a surface pressure trough out ahead of it over the Mid-Atlantic. Out ahead of the circulation, a hot, humid, and unstable air mass was in place, and this helped to initiate scattered to numerous showers and thunderstorms in the afternoon. Some of these thunderstorms became strong to locally severe. On July 17th, the remnant circulation of Barry moved into Pennsylvania with a surface pressure trough out ahead of it over the Mid-Atlantic. Out ahead of the circulation, a hot, humid, and unstable air mass was in place, and this helped to initiate scattered to numerous showers and thunderstorms in the afternoon. Some of these thunderstorms became strong to locally severe. On July 17th, the remnant circulation of Barry moved into Pennsylvania with a surface pressure trough out ahead of it over the Mid-Atlantic. Out ahead of the circulation, a hot, humid, and unstable air mass was in place, and this helped to initiate scattered to numerous showers and thunderstorms in the afternoon. Some of these thunderstorms became strong to locally severe. On July 17th, the remnant circulation of Barry moved into Pennsylvania with a surface pressure trough out ahead of it over the Mid-Atlantic. Out ahead of the circulation, a hot, humid, and unstable air mass was in place, and this helped to initiate scattered to numerous showers and thunderstorms in the afternoon. Some of these thunderstorms became strong to locally severe. On July 17th, the remnant circulation of Barry moved into Pennsylvania with a surface pressure trough out ahead of it over the Mid-Atlantic. Out ahead of the circulation, a hot, humid, and unstable air mass was in place, and this helped to initiate scattered to numerous showers and thunderstorms in the afternoon. Some of these thunderstorms became strong to locally severe. On July 17th, the remnant circulation of Barry moved into Pennsylvania with a surface pressure trough out ahead of it over the Mid-Atlantic. Out ahead of the circulation, a hot, humid, and unstable air mass was in place, and this helped to initiate scattered to numerous showers and thunderstorms in the afternoon. Some of these thunderstorms became strong to locally severe. On July 17th, the remnant circulation of Barry moved into Pennsylvania with a surface pressure trough out ahead of it over the Mid-Atlantic. Out ahead of the circulation, a hot, humid, and unstable air mass was in place, and this helped to initiate scattered to numerous showers and thunderstorms in the afternoon. Some of these thunderstorms became strong to locally severe. On July 17th, the remnant circulation of Barry moved into Pennsylvania with a surface pressure trough out ahead of it over the Mid-Atlantic. Out ahead of the circulation, a hot, humid, and unstable air mass was in place, and this helped to initiate scattered to numerous showers and thunderstorms in the afternoon. Some of these thunderstorms became strong to locally severe. On July 17th, the remnant circulation of Barry moved into Pennsylvania with a surface pressure trough out ahead of it over the Mid-Atlantic. Out ahead of the circulation, a hot, humid, and unstable air mass was in place, and this helped to initiate scattered to numerous showers and thunderstorms in the afternoon. Some of these thunderstorms became strong to locally severe. On July 17th, the remnant circulation of Barry moved into Pennsylvania with a surface pressure trough out ahead of it over the Mid-Atlantic. Out ahead of the circulation, a hot, humid, and unstable air mass was in place, and this helped to initiate scattered to numerous showers and thunderstorms in the afternoon. Some of these thunderstorms became strong to locally severe. On July 17th, the remnant circulation of Barry moved into Pennsylvania with a surface pressure trough out ahead of it over the Mid-Atlantic. Out ahead of the circulation, a hot, humid, and unstable air mass was in place, and this helped to initiate scattered to numerous showers and thunderstorms in the afternoon. Some of these thunderstorms became strong to locally severe.\nEvent Narrative: Up to four dozen reports of trees and wires down in the Dundalk, Essex and Middle River area were received. A couple of trees were blown down near Sykesville. Multiple trees were blown down near the intersection of South Tannery Road and Gorsech Road. Multiple trees were blown down along Liberty Road east of Eldersburg. A tree was blown down near the intersection of East Cold Spring Lane and Marble Hall Road. Multiple trees were blown down in Edgewater, some onto power lines. A tree was blown down on a house near Long Green. An 18-inch diameter tree was blown down blocking the roadway. A large tree was blown down blocking three lanes of I-695 Baltimore Beltway Inner Loop at Greenspring Avenue. Several large trees were blown down on Tintern Court. Multiple trees were blown down near the intersection of Greenspring Avenue and Kelly Avenue in Lutherville.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 27.859 km away, between 2019-07-17 17:00:00 and 2019-07-17 18:00:00. The events included records with measured wind gusts of 38.88235294117647 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: On July 17th, the remnant circulation of Barry moved into Pennsylvania with a surface pressure trough out ahead of it over the Mid-Atlantic. Out ahead of the circulation, a hot, humid, and unstable air mass was in place, and this helped to initiate scattered to numerous showers and thunderstorms in the afternoon. Some of these thunderstorms produced gusty winds over the waters. On July 17th, the remnant circulation of Barry moved into Pennsylvania with a surface pressure trough out ahead of it over the Mid-Atlantic. Out ahead of the circulation, a hot, humid, and unstable air mass was in place, and this helped to initiate scattered to numerous showers and thunderstorms in the afternoon. Some of these thunderstorms produced gusty winds over the waters. On July 17th, the remnant circulation of Barry moved into Pennsylvania with a surface pressure trough out ahead of it over the Mid-Atlantic. Out ahead of the circulation, a hot, humid, and unstable air mass was in place, and this helped to initiate scattered to numerous showers and thunderstorms in the afternoon. Some of these thunderstorms produced gusty winds over the waters. On July 17th, the remnant circulation of Barry moved into Pennsylvania with a surface pressure trough out ahead of it over the Mid-Atlantic. Out ahead of the circulation, a hot, humid, and unstable air mass was in place, and this helped to initiate scattered to numerous showers and thunderstorms in the afternoon. Some of these thunderstorms produced gusty winds over the waters. On July 17th, the remnant circulation of Barry moved into Pennsylvania with a surface pressure trough out ahead of it over the Mid-Atlantic. Out ahead of the circulation, a hot, humid, and unstable air mass was in place, and this helped to initiate scattered to numerous showers and thunderstorms in the afternoon. Some of these thunderstorms produced gusty winds over the waters. On July 17th, the remnant circulation of Barry moved into Pennsylvania with a surface pressure trough out ahead of it over the Mid-Atlantic. Out ahead of the circulation, a hot, humid, and unstable air mass was in place, and this helped to initiate scattered to numerous showers and thunderstorms in the afternoon. Some of these thunderstorms produced gusty winds over the waters. On July 17th, the remnant circulation of Barry moved into Pennsylvania with a surface pressure trough out ahead of it over the Mid-Atlantic. Out ahead of the circulation, a hot, humid, and unstable air mass was in place, and this helped to initiate scattered to numerous showers and thunderstorms in the afternoon. Some of these thunderstorms produced gusty winds over the waters. On July 17th, the remnant circulation of Barry moved into Pennsylvania with a surface pressure trough out ahead of it over the Mid-Atlantic. Out ahead of the circulation, a hot, humid, and unstable air mass was in place, and this helped to initiate scattered to numerous showers and thunderstorms in the afternoon. Some of these thunderstorms produced gusty winds over the waters. On July 17th, the remnant circulation of Barry moved into Pennsylvania with a surface pressure trough out ahead of it over the Mid-Atlantic. Out ahead of the circulation, a hot, humid, and unstable air mass was in place, and this helped to initiate scattered to numerous showers and thunderstorms in the afternoon. Some of these thunderstorms produced gusty winds over the waters. On July 17th, the remnant circulation of Barry moved into Pennsylvania with a surface pressure trough out ahead of it over the Mid-Atlantic. Out ahead of the circulation, a hot, humid, and unstable air mass was in place, and this helped to initiate scattered to numerous showers and thunderstorms in the afternoon. Some of these thunderstorms produced gusty winds over the waters. On July 17th, the remnant circulation of Barry moved into Pennsylvania with a surface pressure trough out ahead of it over the Mid-Atlantic. Out ahead of the circulation, a hot, humid, and unstable air mass was in place, and this helped to initiate scattered to numerous showers and thunderstorms in the afternoon. Some of these thunderstorms produced gusty winds over the waters. On July 17th, the remnant circulation of Barry moved into Pennsylvania with a surface pressure trough out ahead of it over the Mid-Atlantic. Out ahead of the circulation, a hot, humid, and unstable air mass was in place, and this helped to initiate scattered to numerous showers and thunderstorms in the afternoon. Some of these thunderstorms produced gusty winds over the waters. On July 17th, the remnant circulation of Barry moved into Pennsylvania with a surface pressure trough out ahead of it over the Mid-Atlantic. Out ahead of the circulation, a hot, humid, and unstable air mass was in place, and this helped to initiate scattered to numerous showers and thunderstorms in the afternoon. Some of these thunderstorms produced gusty winds over the waters. On July 17th, the remnant circulation of Barry moved into Pennsylvania with a surface pressure trough out ahead of it over the Mid-Atlantic. Out ahead of the circulation, a hot, humid, and unstable air mass was in place, and this helped to initiate scattered to numerous showers and thunderstorms in the afternoon. Some of these thunderstorms produced gusty winds over the waters. On July 17th, the remnant circulation of Barry moved into Pennsylvania with a surface pressure trough out ahead of it over the Mid-Atlantic. Out ahead of the circulation, a hot, humid, and unstable air mass was in place, and this helped to initiate scattered to numerous showers and thunderstorms in the afternoon. Some of these thunderstorms produced gusty winds over the waters. On July 17th, the remnant circulation of Barry moved into Pennsylvania with a surface pressure trough out ahead of it over the Mid-Atlantic. Out ahead of the circulation, a hot, humid, and unstable air mass was in place, and this helped to initiate scattered to numerous showers and thunderstorms in the afternoon. Some of these thunderstorms produced gusty winds over the waters. On July 17th, the remnant circulation of Barry moved into Pennsylvania with a surface pressure trough out ahead of it over the Mid-Atlantic. Out ahead of the circulation, a hot, humid, and unstable air mass was in place, and this helped to initiate scattered to numerous showers and thunderstorms in the afternoon. Some of these thunderstorms produced gusty winds over the waters.\nEvent Narrative:", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 36.4541 km away, between 2019-07-21 19:12:00 and 2019-07-21 19:49:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: An upper level ridge that was in place began to break down during the afternoon hours of July 21st as a cold front moved through the Midwest and an upper-level trough dug into the northern Plains. This allowed additional moisture into the area and when|combined with a weakening capping inversion from height falls it was enough for scattered showers and thunderstorms to develop. With substantial instability, some of these thunderstorms became strong to locally severe. An upper level ridge that was in place began to break down during the afternoon hours of July 21st as a cold front moved through the Midwest and an upper-level trough dug into the northern Plains. This allowed additional moisture into the area and when|combined with a weakening capping inversion from height falls it was enough for scattered showers and thunderstorms to develop. With substantial instability, some of these thunderstorms became strong to locally severe. An upper level ridge that was in place began to break down during the afternoon hours of July 21st as a cold front moved through the Midwest and an upper-level trough dug into the northern Plains. This allowed additional moisture into the area and when|combined with a weakening capping inversion from height falls it was enough for scattered showers and thunderstorms to develop. With substantial instability, some of these thunderstorms became strong to locally severe. An upper level ridge that was in place began to break down during the afternoon hours of July 21st as a cold front moved through the Midwest and an upper-level trough dug into the northern Plains. This allowed additional moisture into the area and when|combined with a weakening capping inversion from height falls it was enough for scattered showers and thunderstorms to develop. With substantial instability, some of these thunderstorms became strong to locally severe. An upper level ridge that was in place began to break down during the afternoon hours of July 21st as a cold front moved through the Midwest and an upper-level trough dug into the northern Plains. This allowed additional moisture into the area and when|combined with a weakening capping inversion from height falls it was enough for scattered showers and thunderstorms to develop. With substantial instability, some of these thunderstorms became strong to locally severe.\nEvent Narrative: Large tree limbs were blown down on Marston Road. Additional trees and wires were blown down in area. A tree was blown down on power lines near the intersection of Main Street and Spout Hill Road. A tree was blown down along Owings Mills Boulevard at South Dolfield Road. Trees were blown down in the 2000 block of Abell Lane. A tree was blown down on West Seminary Avenue at Mays Chapel Road.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 19.8763 km away, between 2019-07-21 19:40:00 and 2019-07-21 20:15:00. The events included records with measured wind gusts of 34.4 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: An upper level ridge that was in place began to break down during the afternoon hours of July 21st as a cold front moved through the Midwest and an upper-level trough dug into the northern Plains. This allowed additional moisture into the area and when|combined with a weakening capping inversion from height falls it was enough for scattered showers and thunderstorms to develop. With substantial instability, some of these thunderstorms producing gusty winds over the waters. An upper level ridge that was in place began to break down during the afternoon hours of July 21st as a cold front moved through the Midwest and an upper-level trough dug into the northern Plains. This allowed additional moisture into the area and when|combined with a weakening capping inversion from height falls it was enough for scattered showers and thunderstorms to develop. With substantial instability, some of these thunderstorms producing gusty winds over the waters. An upper level ridge that was in place began to break down during the afternoon hours of July 21st as a cold front moved through the Midwest and an upper-level trough dug into the northern Plains. This allowed additional moisture into the area and when|combined with a weakening capping inversion from height falls it was enough for scattered showers and thunderstorms to develop. With substantial instability, some of these thunderstorms producing gusty winds over the waters. An upper level ridge that was in place began to break down during the afternoon hours of July 21st as a cold front moved through the Midwest and an upper-level trough dug into the northern Plains. This allowed additional moisture into the area and when|combined with a weakening capping inversion from height falls it was enough for scattered showers and thunderstorms to develop. With substantial instability, some of these thunderstorms producing gusty winds over the waters. An upper level ridge that was in place began to break down during the afternoon hours of July 21st as a cold front moved through the Midwest and an upper-level trough dug into the northern Plains. This allowed additional moisture into the area and when|combined with a weakening capping inversion from height falls it was enough for scattered showers and thunderstorms to develop. With substantial instability, some of these thunderstorms producing gusty winds over the waters.\nEvent Narrative:", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 41.7823 km away, between 2019-07-22 14:09:00 and 2019-07-22 15:27:00. The events included records with estimated wind gusts of 59.44444444444444 mph.The events resulted in 0 injuries and 1 fatalities. No significant property or crop damage was reported. \n\nEpisode Narrative: Falling heights, an increasing southwest flow aloft, an approaching cold front, and strengthening pressure trough overhead combined with instability from a hot and humid air mass in place to trigger showers and thunderstorms during the afternoon hours of July 22nd. With high levels of CAPE and increased shear profiles, thunderstorms became strong to severe as they organized into linear structures. Falling heights, an increasing southwest flow aloft, an approaching cold front, and strengthening pressure trough overhead combined with instability from a hot and humid air mass in place to trigger showers and thunderstorms during the afternoon hours of July 22nd. With high levels of CAPE and increased shear profiles, thunderstorms became strong to severe as they organized into linear structures. Falling heights, an increasing southwest flow aloft, an approaching cold front, and strengthening pressure trough overhead combined with instability from a hot and humid air mass in place to trigger showers and thunderstorms during the afternoon hours of July 22nd. With high levels of CAPE and increased shear profiles, thunderstorms became strong to severe as they organized into linear structures. Falling heights, an increasing southwest flow aloft, an approaching cold front, and strengthening pressure trough overhead combined with instability from a hot and humid air mass in place to trigger showers and thunderstorms during the afternoon hours of July 22nd. With high levels of CAPE and increased shear profiles, thunderstorms became strong to severe as they organized into linear structures. Falling heights, an increasing southwest flow aloft, an approaching cold front, and strengthening pressure trough overhead combined with instability from a hot and humid air mass in place to trigger showers and thunderstorms during the afternoon hours of July 22nd. With high levels of CAPE and increased shear profiles, thunderstorms became strong to severe as they organized into linear structures. Falling heights, an increasing southwest flow aloft, an approaching cold front, and strengthening pressure trough overhead combined with instability from a hot and humid air mass in place to trigger showers and thunderstorms during the afternoon hours of July 22nd. With high levels of CAPE and increased shear profiles, thunderstorms became strong to severe as they organized into linear structures. Falling heights, an increasing southwest flow aloft, an approaching cold front, and strengthening pressure trough overhead combined with instability from a hot and humid air mass in place to trigger showers and thunderstorms during the afternoon hours of July 22nd. With high levels of CAPE and increased shear profiles, thunderstorms became strong to severe as they organized into linear structures. Falling heights, an increasing southwest flow aloft, an approaching cold front, and strengthening pressure trough overhead combined with instability from a hot and humid air mass in place to trigger showers and thunderstorms during the afternoon hours of July 22nd. With high levels of CAPE and increased shear profiles, thunderstorms became strong to severe as they organized into linear structures. Falling heights, an increasing southwest flow aloft, an approaching cold front, and strengthening pressure trough overhead combined with instability from a hot and humid air mass in place to trigger showers and thunderstorms during the afternoon hours of July 22nd. With high levels of CAPE and increased shear profiles, thunderstorms became strong to severe as they organized into linear structures. Falling heights, an increasing southwest flow aloft, an approaching cold front, and strengthening pressure trough overhead combined with instability from a hot and humid air mass in place to trigger showers and thunderstorms during the afternoon hours of July 22nd. With high levels of CAPE and increased shear profiles, thunderstorms became strong to severe as they organized into linear structures. Falling heights, an increasing southwest flow aloft, an approaching cold front, and strengthening pressure trough overhead combined with instability from a hot and humid air mass in place to trigger showers and thunderstorms during the afternoon hours of July 22nd. With high levels of CAPE and increased shear profiles, thunderstorms became strong to severe as they organized into linear structures. Falling heights, an increasing southwest flow aloft, an approaching cold front, and strengthening pressure trough overhead combined with instability from a hot and humid air mass in place to trigger showers and thunderstorms during the afternoon hours of July 22nd. With high levels of CAPE and increased shear profiles, thunderstorms became strong to severe as they organized into linear structures. Falling heights, an increasing southwest flow aloft, an approaching cold front, and strengthening pressure trough overhead combined with instability from a hot and humid air mass in place to trigger showers and thunderstorms during the afternoon hours of July 22nd. With high levels of CAPE and increased shear profiles, thunderstorms became strong to severe as they organized into linear structures. Falling heights, an increasing southwest flow aloft, an approaching cold front, and strengthening pressure trough overhead combined with instability from a hot and humid air mass in place to trigger showers and thunderstorms during the afternoon hours of July 22nd. With high levels of CAPE and increased shear profiles, thunderstorms became strong to severe as they organized into linear structures. Falling heights, an increasing southwest flow aloft, an approaching cold front, and strengthening pressure trough overhead combined with instability from a hot and humid air mass in place to trigger showers and thunderstorms during the afternoon hours of July 22nd. With high levels of CAPE and increased shear profiles, thunderstorms became strong to severe as they organized into linear structures. Falling heights, an increasing southwest flow aloft, an approaching cold front, and strengthening pressure trough overhead combined with instability from a hot and humid air mass in place to trigger showers and thunderstorms during the afternoon hours of July 22nd. With high levels of CAPE and increased shear profiles, thunderstorms became strong to severe as they organized into linear structures. Falling heights, an increasing southwest flow aloft, an approaching cold front, and strengthening pressure trough overhead combined with instability from a hot and humid air mass in place to trigger showers and thunderstorms during the afternoon hours of July 22nd. With high levels of CAPE and increased shear profiles, thunderstorms became strong to severe as they organized into linear structures. Falling heights, an increasing southwest flow aloft, an approaching cold front, and strengthening pressure trough overhead combined with instability from a hot and humid air mass in place to trigger showers and thunderstorms during the afternoon hours of July 22nd. With high levels of CAPE and increased shear profiles, thunderstorms became strong to severe as they organized into linear structures.\nEvent Narrative: A few trees were blown down in the Fallston area. A tree was blown down on Preston Lane near Singer Road. A large tree limb was blown down blocking the roadway near the intersection of Willoughby Beach Road and Harbour Oak Drive. Several large trees were snapped off halfway up or uprooted near Adam Court. Numerous healthy trees and limbs were blown down just north of Friendship. Roof shingles were stripped from at least one home. A tree was blown down on Bethesda Church Road near Purdum Road. A tree was blown down in the 2900 block of Florence Road. Another tree was blown down in the 16400 block of Frederick Road. A tree was blown down on Forsythe Road near West Friendship Road. Another tree was blown down on River Road near MD-32. A couple of large trees were uprooted and a few 10-inch diameter trees were snapped off of Bloom Road. Numerous large trees were blown down in the vicinity of the intersection of Old Kays Mill Road and Deer Park Road, some onto houses. Half a dozen homes in the area had shingles blown off and a barn lost its roof on Black Steer Drive. One fatality occurred when a tree fell onto a man in the 2900 block of Bloom Road in Finksburg. A tree was blown down on Bollinger Road near Hook Road. Several large tree limbs were blown down in the 700 block of Academy Avenue. All lanes of MD-30 were closed due to trees and wires in the roadway between Glen Falls Road and MD-91. Widespread tree damage was reported with snapped and uprooted large trees and limbs in the 1400 block of Emory Church Road. Part of a roof was blown off of a barn. Multiple trees were blown down in the vicinity of Black Road Road and Falls Road. A tree was blown down blocking all lanes of Falls Road at Knox Avenue. Multiple large trees up to 3 feet in diameter were uprooted and snapped, falling in multiple directions on Evna Road just north of MD-137 Mount Carmel Road. Multiple trees were blown down in the vicinity of Monkton Road and Big Falls Road. Several trees were blown down in the vicinity of Greenspring Valley Road and Nacirema Lane. Several trees were blown down west of Jarrettsville.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 25.6921 km away, between 2019-07-22 14:55:00 and 2019-07-23 02:18:00. The events included records with measured wind gusts of 36.75 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Falling heights, an increasing southwest flow aloft, an approaching cold front, and strengthening pressure trough overhead combined with instability from a hot and humid air mass in place to trigger showers and thunderstorms during the afternoon hours of July 22nd. With high levels of CAPE and increased shear profiles, thunderstorms became strong to severe as they organized into linear structures, and produced gusty winds over the waters. Falling heights, an increasing southwest flow aloft, an approaching cold front, and strengthening pressure trough overhead combined with instability from a hot and humid air mass in place to trigger showers and thunderstorms during the afternoon hours of July 22nd. With high levels of CAPE and increased shear profiles, thunderstorms became strong to severe as they organized into linear structures, and produced gusty winds over the waters. Falling heights, an increasing southwest flow aloft, an approaching cold front, and strengthening pressure trough overhead combined with instability from a hot and humid air mass in place to trigger showers and thunderstorms during the afternoon hours of July 22nd. With high levels of CAPE and increased shear profiles, thunderstorms became strong to severe as they organized into linear structures, and produced gusty winds over the waters. Falling heights, an increasing southwest flow aloft, an approaching cold front, and strengthening pressure trough overhead combined with instability from a hot and humid air mass in place to trigger showers and thunderstorms during the afternoon hours of July 22nd. With high levels of CAPE and increased shear profiles, thunderstorms became strong to severe as they organized into linear structures, and produced gusty winds over the waters. Falling heights, an increasing southwest flow aloft, an approaching cold front, and strengthening pressure trough overhead combined with instability from a hot and humid air mass in place to trigger showers and thunderstorms during the afternoon hours of July 22nd. With high levels of CAPE and increased shear profiles, thunderstorms became strong to severe as they organized into linear structures, and produced gusty winds over the waters. Falling heights, an increasing southwest flow aloft, an approaching cold front, and strengthening pressure trough overhead combined with instability from a hot and humid air mass in place to trigger showers and thunderstorms during the afternoon hours of July 22nd. With high levels of CAPE and increased shear profiles, thunderstorms became strong to severe as they organized into linear structures, and produced gusty winds over the waters. Falling heights, an increasing southwest flow aloft, an approaching cold front, and strengthening pressure trough overhead combined with instability from a hot and humid air mass in place to trigger showers and thunderstorms during the afternoon hours of July 22nd. With high levels of CAPE and increased shear profiles, thunderstorms became strong to severe as they organized into linear structures, and produced gusty winds over the waters. Falling heights, an increasing southwest flow aloft, an approaching cold front, and strengthening pressure trough overhead combined with instability from a hot and humid air mass in place to trigger showers and thunderstorms during the afternoon hours of July 22nd. With high levels of CAPE and increased shear profiles, thunderstorms became strong to severe as they organized into linear structures, and produced gusty winds over the waters. Falling heights, an increasing southwest flow aloft, an approaching cold front, and strengthening pressure trough overhead combined with instability from a hot and humid air mass in place to trigger showers and thunderstorms during the afternoon hours of July 22nd. With high levels of CAPE and increased shear profiles, thunderstorms became strong to severe as they organized into linear structures, and produced gusty winds over the waters. Falling heights, an increasing southwest flow aloft, an approaching cold front, and strengthening pressure trough overhead combined with instability from a hot and humid air mass in place to trigger showers and thunderstorms during the afternoon hours of July 22nd. With high levels of CAPE and increased shear profiles, thunderstorms became strong to severe as they organized into linear structures, and produced gusty winds over the waters. Falling heights, an increasing southwest flow aloft, an approaching cold front, and strengthening pressure trough overhead combined with instability from a hot and humid air mass in place to trigger showers and thunderstorms during the afternoon hours of July 22nd. With high levels of CAPE and increased shear profiles, thunderstorms became strong to severe as they organized into linear structures, and produced gusty winds over the waters. Falling heights, an increasing southwest flow aloft, an approaching cold front, and strengthening pressure trough overhead combined with instability from a hot and humid air mass in place to trigger showers and thunderstorms during the afternoon hours of July 22nd. With high levels of CAPE and increased shear profiles, thunderstorms became strong to severe as they organized into linear structures, and produced gusty winds over the waters.\nEvent Narrative:", "The following events were reported: Waterspout. These occurred near station USW00093721, approximately 35.6627 km away, between 2019-07-23 18:05:00 and 2019-07-23 18:05:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Local convergence and the warm waters of the Chesapeake Bay produced localized showers across portions of the Chesapeake Bay. One of these showers produced a waterspout.\nEvent Narrative: A thin waterspout was reported by a local mariner.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 26.4795 km away, between 2019-07-29 17:40:00 and 2019-07-29 17:40:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: High pressure gradually shifted eastward and off the southeastern US coast through the day on July 29th. This promoted the development of southerly flow and the return of low level moisture. This allowed for the development of marginal instability and a few isolated|showers and thunderstorms. One storm became severe.\nEvent Narrative: A large tree was snapped in half blocking the 500 block of Joppa Road. Other large branches and small trees were also reported down in the area.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 29.4458 km away, between 2019-07-31 17:36:00 and 2019-07-31 18:22:00. The events included records with measured wind gusts of 35.666666666666664 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A surface front moved slowly through the Ohio Valley on the afternoon of July 31st, with a secondary surface trough positioned just east of the I-95 corridor. Aloft, an upper level trough slowly moved across the region. As instability increased during the afternoon hours, scattered showers and thunderstorms developed, and a few brought gusty winds to portions of the waters. A surface front moved slowly through the Ohio Valley on the afternoon of July 31st, with a secondary surface trough positioned just east of the I-95 corridor. Aloft, an upper level trough slowly moved across the region. As instability increased during the afternoon hours, scattered showers and thunderstorms developed, and a few brought gusty winds to portions of the waters. A surface front moved slowly through the Ohio Valley on the afternoon of July 31st, with a secondary surface trough positioned just east of the I-95 corridor. Aloft, an upper level trough slowly moved across the region. As instability increased during the afternoon hours, scattered showers and thunderstorms developed, and a few brought gusty winds to portions of the waters.\nEvent Narrative:", "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00093721, approximately 10.3555 km away, between 2019-08-01 12:48:00 and 2019-08-01 14:01:00. The events included records with hailstones measuring 17.438333333333333 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: An upper level trough and its associated energy approached and crossed the region during the late afternoon and evening hours of August 1st. At the surface, a frontal boundary remained stalled across central Virginia and into eastern Maryland. Temperatures in the 80s to around 90F combined with dew points in the 60s to near 70F and led to the development of moderate instability across the area during the afternoon hours.|Scattered showers and thunderstorms then formed in the afternoon and evening, and some of them became locally severe. An upper level trough and its associated energy approached and crossed the region during the late afternoon and evening hours of August 1st. At the surface, a frontal boundary remained stalled across central Virginia and into eastern Maryland. Temperatures in the 80s to around 90F combined with dew points in the 60s to near 70F and led to the development of moderate instability across the area during the afternoon hours.|Scattered showers and thunderstorms then formed in the afternoon and evening, and some of them became locally severe. An upper level trough and its associated energy approached and crossed the region during the late afternoon and evening hours of August 1st. At the surface, a frontal boundary remained stalled across central Virginia and into eastern Maryland. Temperatures in the 80s to around 90F combined with dew points in the 60s to near 70F and led to the development of moderate instability across the area during the afternoon hours.|Scattered showers and thunderstorms then formed in the afternoon and evening, and some of them became locally severe. An upper level trough and its associated energy approached and crossed the region during the late afternoon and evening hours of August 1st. At the surface, a frontal boundary remained stalled across central Virginia and into eastern Maryland. Temperatures in the 80s to around 90F combined with dew points in the 60s to near 70F and led to the development of moderate instability across the area during the afternoon hours.|Scattered showers and thunderstorms then formed in the afternoon and evening, and some of them became locally severe. An upper level trough and its associated energy approached and crossed the region during the late afternoon and evening hours of August 1st. At the surface, a frontal boundary remained stalled across central Virginia and into eastern Maryland. Temperatures in the 80s to around 90F combined with dew points in the 60s to near 70F and led to the development of moderate instability across the area during the afternoon hours.|Scattered showers and thunderstorms then formed in the afternoon and evening, and some of them became locally severe. An upper level trough and its associated energy approached and crossed the region during the late afternoon and evening hours of August 1st. At the surface, a frontal boundary remained stalled across central Virginia and into eastern Maryland. Temperatures in the 80s to around 90F combined with dew points in the 60s to near 70F and led to the development of moderate instability across the area during the afternoon hours.|Scattered showers and thunderstorms then formed in the afternoon and evening, and some of them became locally severe.\nEvent Narrative: A tree was blown down onto a house in the 100 block of Ralph Road. A tree was blown down onto a car partially blocking Rita Drive. Hail up to the size of golf balls (1.75) was reported off of Furnace Branch Road in Glen Burnie. Quarter sized hail (1.0) was reported near Glen Burnie. Quarter-sized hail (1.0) was reported in Severn.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 18.0112 km away, between 2019-08-05 16:55:00 and 2019-08-05 16:55:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: An upper-level trough moved overhead during the afternoon and evening hours of August 5th while a weak surface trough remained positioned near the area as well. A southwest flow aloft ahead of the trough helped to usher in warmth and humidity, which led to the development of marginal instability across the region. This led to the formation of scattered showers and thunderstorms, a couple of which became locally severe.\nEvent Narrative: A tree was blown down on Hesperus Drive near the intersection with Rondel Place. A tree was also blown down in Agail Place.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 14.3559 km away, between 2019-08-06 16:40:00 and 2019-08-06 18:00:00. The events included records with measured wind gusts of 49.5 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A southwest flow out ahead of a frontal boundary ushered in a hot, humid, and therefore unstable air mass into the region during the afternoon and evening hours of August 6th. A weak surface trough along with a sea-breeze boundary caused the development of a few localized showers and thunderstorms along the western shore of the Chesapeake Bay. A few thunderstorms were able to produce gusty winds across the waters. A southwest flow out ahead of a frontal boundary ushered in a hot, humid, and therefore unstable air mass into the region during the afternoon and evening hours of August 6th. A weak surface trough along with a sea-breeze boundary caused the development of a few localized showers and thunderstorms along the western shore of the Chesapeake Bay. A few thunderstorms were able to produce gusty winds across the waters. A southwest flow out ahead of a frontal boundary ushered in a hot, humid, and therefore unstable air mass into the region during the afternoon and evening hours of August 6th. A weak surface trough along with a sea-breeze boundary caused the development of a few localized showers and thunderstorms along the western shore of the Chesapeake Bay. A few thunderstorms were able to produce gusty winds across the waters. A southwest flow out ahead of a frontal boundary ushered in a hot, humid, and therefore unstable air mass into the region during the afternoon and evening hours of August 6th. A weak surface trough along with a sea-breeze boundary caused the development of a few localized showers and thunderstorms along the western shore of the Chesapeake Bay. A few thunderstorms were able to produce gusty winds across the waters. A southwest flow out ahead of a frontal boundary ushered in a hot, humid, and therefore unstable air mass into the region during the afternoon and evening hours of August 6th. A weak surface trough along with a sea-breeze boundary caused the development of a few localized showers and thunderstorms along the western shore of the Chesapeake Bay. A few thunderstorms were able to produce gusty winds across the waters. A southwest flow out ahead of a frontal boundary ushered in a hot, humid, and therefore unstable air mass into the region during the afternoon and evening hours of August 6th. A weak surface trough along with a sea-breeze boundary caused the development of a few localized showers and thunderstorms along the western shore of the Chesapeake Bay. A few thunderstorms were able to produce gusty winds across the waters.\nEvent Narrative:", "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00093721, approximately 15.3012 km away, between 2019-08-06 16:50:00 and 2019-08-06 17:49:00. The events included records with hailstones measuring 42.25 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A southwest flow out ahead of a frontal boundary ushered in a hot, humid, and therefore unstable air mass into the region during the afternoon and evening hours of August 6th. A weak surface trough along with terrain circulations caused isolated showers and|thunderstorms to develop across portions of the region, while a sea-breeze boundary caused the development of a few localized showers and thunderstorms along the western shore of the Chesapeake Bay. A few thunderstorms were able to become locally severe. A southwest flow out ahead of a frontal boundary ushered in a hot, humid, and therefore unstable air mass into the region during the afternoon and evening hours of August 6th. A weak surface trough along with terrain circulations caused isolated showers and|thunderstorms to develop across portions of the region, while a sea-breeze boundary caused the development of a few localized showers and thunderstorms along the western shore of the Chesapeake Bay. A few thunderstorms were able to become locally severe. A southwest flow out ahead of a frontal boundary ushered in a hot, humid, and therefore unstable air mass into the region during the afternoon and evening hours of August 6th. A weak surface trough along with terrain circulations caused isolated showers and|thunderstorms to develop across portions of the region, while a sea-breeze boundary caused the development of a few localized showers and thunderstorms along the western shore of the Chesapeake Bay. A few thunderstorms were able to become locally severe. A southwest flow out ahead of a frontal boundary ushered in a hot, humid, and therefore unstable air mass into the region during the afternoon and evening hours of August 6th. A weak surface trough along with terrain circulations caused isolated showers and|thunderstorms to develop across portions of the region, while a sea-breeze boundary caused the development of a few localized showers and thunderstorms along the western shore of the Chesapeake Bay. A few thunderstorms were able to become locally severe.\nEvent Narrative: Quarter-sized hail (1.0) was reported in the city of Baltimore. A 57-knot (66 mph) wind gust was measured at the Maryland Science Center. Numerous reports of trees down were received across southern and eastern portions of the city of Baltimore. A 50-knot (58 mph) wind gust was measured in Patterson Park in the city of Baltimore. A 61-knot (70 mph) wind gust was measured near Fells Point/Fort McHenry.", "The following events were reported: Flash Flood, Flood. These occurred near station USW00093721, approximately 15.6794 km away, between 2019-08-06 17:37:00 and 2019-08-06 23:01:00. The flood was caused by Heavy Rain. Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 500000.0 and crop damage of 0.0. \n\nEpisode Narrative: A weak upper-level trough remained overhead and there was also a surface trough around the area. A light southerly flow ahead of the boundary caused dewpoints to reach the 70s. A few showers and thunderstorms developed, and some storms produced heavy rainfall that led to flooding and flash flooding. The heaviest rain fell around the Baltimore Metropolitan area due to training convection. A weak upper-level trough remained overhead and there was also a surface trough around the area. A light southerly flow ahead of the boundary caused dewpoints to reach the 70s. A few showers and thunderstorms developed, and some storms produced heavy rainfall that led to flooding and flash flooding. The heaviest rain fell around the Baltimore Metropolitan area due to training convection. A weak upper-level trough remained overhead and there was also a surface trough around the area. A light southerly flow ahead of the boundary caused dewpoints to reach the 70s. A few showers and thunderstorms developed, and some storms produced heavy rainfall that led to flooding and flash flooding. The heaviest rain fell around the Baltimore Metropolitan area due to training convection. A weak upper-level trough remained overhead and there was also a surface trough around the area. A light southerly flow ahead of the boundary caused dewpoints to reach the 70s. A few showers and thunderstorms developed, and some storms produced heavy rainfall that led to flooding and flash flooding. The heaviest rain fell around the Baltimore Metropolitan area due to training convection. A weak upper-level trough remained overhead and there was also a surface trough around the area. A light southerly flow ahead of the boundary caused dewpoints to reach the 70s. A few showers and thunderstorms developed, and some storms produced heavy rainfall that led to flooding and flash flooding. The heaviest rain fell around the Baltimore Metropolitan area due to training convection. A weak upper-level trough remained overhead and there was also a surface trough around the area. A light southerly flow ahead of the boundary caused dewpoints to reach the 70s. A few showers and thunderstorms developed, and some storms produced heavy rainfall that led to flooding and flash flooding. The heaviest rain fell around the Baltimore Metropolitan area due to training convection. A weak upper-level trough remained overhead and there was also a surface trough around the area. A light southerly flow ahead of the boundary caused dewpoints to reach the 70s. A few showers and thunderstorms developed, and some storms produced heavy rainfall that led to flooding and flash flooding. The heaviest rain fell around the Baltimore Metropolitan area due to training convection.\nEvent Narrative: Roads were impassable due to flash flooding in Canton and Fells Point. Several cars were trapped in up to three feet of standing water near the intersection of South Caroline Street in Aliceanna Street. Cars were under water along Central Avenue. Flooding occurred along Charles Street near Penn Station. The Road was closed. Brock Bridge Road was closed near the intersection with Laurel Bowie Road. Southbound MD-197 Laurel Bowie Road was closed due to high water near Montpelier Drive. Flooding was reported in Fells Point, causing roads to be impassable.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 40.3847 km away, between 2019-08-07 13:10:00 and 2019-08-07 14:40:00. The events included records with estimated wind gusts of 52.44444444444444 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: An upper level disturbance and remnant mesoscale convective vortex (MCV) crossed the region during the afternoon hours of August 7th. This, combined with moderate amounts of instability, led to the development of scattered showers and thunderstorms across the state. Some of these thunderstorms became severe. An upper level disturbance and remnant mesoscale convective vortex (MCV) crossed the region during the afternoon hours of August 7th. This, combined with moderate amounts of instability, led to the development of scattered showers and thunderstorms across the state. Some of these thunderstorms became severe. An upper level disturbance and remnant mesoscale convective vortex (MCV) crossed the region during the afternoon hours of August 7th. This, combined with moderate amounts of instability, led to the development of scattered showers and thunderstorms across the state. Some of these thunderstorms became severe. An upper level disturbance and remnant mesoscale convective vortex (MCV) crossed the region during the afternoon hours of August 7th. This, combined with moderate amounts of instability, led to the development of scattered showers and thunderstorms across the state. Some of these thunderstorms became severe. An upper level disturbance and remnant mesoscale convective vortex (MCV) crossed the region during the afternoon hours of August 7th. This, combined with moderate amounts of instability, led to the development of scattered showers and thunderstorms across the state. Some of these thunderstorms became severe. An upper level disturbance and remnant mesoscale convective vortex (MCV) crossed the region during the afternoon hours of August 7th. This, combined with moderate amounts of instability, led to the development of scattered showers and thunderstorms across the state. Some of these thunderstorms became severe. An upper level disturbance and remnant mesoscale convective vortex (MCV) crossed the region during the afternoon hours of August 7th. This, combined with moderate amounts of instability, led to the development of scattered showers and thunderstorms across the state. Some of these thunderstorms became severe. An upper level disturbance and remnant mesoscale convective vortex (MCV) crossed the region during the afternoon hours of August 7th. This, combined with moderate amounts of instability, led to the development of scattered showers and thunderstorms across the state. Some of these thunderstorms became severe. An upper level disturbance and remnant mesoscale convective vortex (MCV) crossed the region during the afternoon hours of August 7th. This, combined with moderate amounts of instability, led to the development of scattered showers and thunderstorms across the state. Some of these thunderstorms became severe.\nEvent Narrative: A tree was blown down on Buckhorn Road near the intersection with MD-97. Three trees were blown down on the northwest side of Eldersburg. A tree was blown down in the 4500 block of London Bridge Road. A tree was blown down on Oklahoma Road near the intersection with Bennett Road. A tree was blown down in the 6000 block of Old Washington Road. A large tree was blown down across Manor Road near the intersection with Kincaid Road. Several other large trees 1 to 2 feet in diameter were blown down in the area. Trees and wires were blown down in the 2900 block of Willoughby Beach Road. A tree was blown down blocking the roadway near the intersection of Trimble Road and Fort Hoyle Road. A tree was blown down at the intersection of Clayton Road and Singer Road.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 35.2419 km away, between 2019-08-07 14:28:00 and 2019-08-07 16:15:00. The events included records with measured wind gusts of 35.6 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: An upper level disturbance and remnant mesoscale convective vortex (MCV) crossed the region during the afternoon hours of August 7th. This, combined with moderate amounts of instability, led to the development of scattered showers and thunderstorms. Some of these thunderstorms produced gusty winds over the waters. An upper level disturbance and remnant mesoscale convective vortex (MCV) crossed the region during the afternoon hours of August 7th. This, combined with moderate amounts of instability, led to the development of scattered showers and thunderstorms. Some of these thunderstorms produced gusty winds over the waters. An upper level disturbance and remnant mesoscale convective vortex (MCV) crossed the region during the afternoon hours of August 7th. This, combined with moderate amounts of instability, led to the development of scattered showers and thunderstorms. Some of these thunderstorms produced gusty winds over the waters. An upper level disturbance and remnant mesoscale convective vortex (MCV) crossed the region during the afternoon hours of August 7th. This, combined with moderate amounts of instability, led to the development of scattered showers and thunderstorms. Some of these thunderstorms produced gusty winds over the waters. An upper level disturbance and remnant mesoscale convective vortex (MCV) crossed the region during the afternoon hours of August 7th. This, combined with moderate amounts of instability, led to the development of scattered showers and thunderstorms. Some of these thunderstorms produced gusty winds over the waters. An upper level disturbance and remnant mesoscale convective vortex (MCV) crossed the region during the afternoon hours of August 7th. This, combined with moderate amounts of instability, led to the development of scattered showers and thunderstorms. Some of these thunderstorms produced gusty winds over the waters. An upper level disturbance and remnant mesoscale convective vortex (MCV) crossed the region during the afternoon hours of August 7th. This, combined with moderate amounts of instability, led to the development of scattered showers and thunderstorms. Some of these thunderstorms produced gusty winds over the waters. An upper level disturbance and remnant mesoscale convective vortex (MCV) crossed the region during the afternoon hours of August 7th. This, combined with moderate amounts of instability, led to the development of scattered showers and thunderstorms. Some of these thunderstorms produced gusty winds over the waters. An upper level disturbance and remnant mesoscale convective vortex (MCV) crossed the region during the afternoon hours of August 7th. This, combined with moderate amounts of instability, led to the development of scattered showers and thunderstorms. Some of these thunderstorms produced gusty winds over the waters. An upper level disturbance and remnant mesoscale convective vortex (MCV) crossed the region during the afternoon hours of August 7th. This, combined with moderate amounts of instability, led to the development of scattered showers and thunderstorms. Some of these thunderstorms produced gusty winds over the waters.\nEvent Narrative:", "The following events were reported: Hail. These occurred near station USW00093721, approximately 15.8694 km away, between 2019-08-17 14:29:00 and 2019-08-17 15:13:00. The events included records with hailstones measuring 0.8333333333333334 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A hot and humid air mass in place led to increasing amounts of instability across the region. This fostered the development of a few showers and thunderstorms, a couple of which became locally severe. A hot and humid air mass in place led to increasing amounts of instability across the region. This fostered the development of a few showers and thunderstorms, a couple of which became locally severe. A hot and humid air mass in place led to increasing amounts of instability across the region. This fostered the development of a few showers and thunderstorms, a couple of which became locally severe.\nEvent Narrative: Quarter-sized (1.0 in diameter) hail was reported near Green Haven.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 11.0566 km away, between 2019-08-18 13:10:00 and 2019-08-18 13:35:00. The events included records with measured wind gusts of 35.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A hot and humid air mass in place led to increasing amounts of instability across the region. This fostered the development of a few showers and thunderstorms, a couple of which produced gusty winds over the waters. A hot and humid air mass in place led to increasing amounts of instability across the region. This fostered the development of a few showers and thunderstorms, a couple of which produced gusty winds over the waters.\nEvent Narrative:", "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00093721, approximately 28.9496 km away, between 2019-08-18 13:14:00 and 2019-08-18 21:35:00. The events included records with hailstones measuring 40.1875 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A hot and humid air mass in place led to increasing amounts of instability across the region. This fostered the development of a few showers and thunderstorms, a couple of which became locally severe. A hot and humid air mass in place led to increasing amounts of instability across the region. This fostered the development of a few showers and thunderstorms, a couple of which became locally severe. A hot and humid air mass in place led to increasing amounts of instability across the region. This fostered the development of a few showers and thunderstorms, a couple of which became locally severe. A hot and humid air mass in place led to increasing amounts of instability across the region. This fostered the development of a few showers and thunderstorms, a couple of which became locally severe. A hot and humid air mass in place led to increasing amounts of instability across the region. This fostered the development of a few showers and thunderstorms, a couple of which became locally severe. A hot and humid air mass in place led to increasing amounts of instability across the region. This fostered the development of a few showers and thunderstorms, a couple of which became locally severe. A hot and humid air mass in place led to increasing amounts of instability across the region. This fostered the development of a few showers and thunderstorms, a couple of which became locally severe. A hot and humid air mass in place led to increasing amounts of instability across the region. This fostered the development of a few showers and thunderstorms, a couple of which became locally severe.\nEvent Narrative: A tree was split in half with large branches down on Washington Boulevard near South Monroe Street. Trees and wires were blown down near Ivy Terrace and Athol Avenue. A large tree was blown down at a residence in the 3900 block of Ridge Road. A tree branch was blown down on wires at Pocock Road and Jarrettsville Pike. Poles and wires were blown down near Fingerboard Road and Green Valley Road. Multiple trees were uprooted and snapped, and damage occurred to vinyl siding on a few homes on Penn Shop Road between Ridge Road and Fingerboard Road.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 33.3829 km away, between 2019-08-20 17:11:00 and 2019-08-20 17:11:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A mesoscale convective system (MCS) and its associated energy was moving across central West Virginia on the morning of August 20th. As this moved eastward into the region during the afternoon and evening hours, it served as the focus for additional shower and thunderstorm development. Significant amounts of instability and steepening low level lapse rates led some of these thunderstorms to become severe.\nEvent Narrative: A tree was blown down onto wires and utility poles near the intersection of Georgia Avenue and Gregg Road.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 35.5565 km away, between 2019-08-21 17:47:00 and 2019-08-21 17:56:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: An upper level trough crossed the Appalachian Mountains during the morning of August 21st and moved through the region during the mid to late afternoon hours, followed by a second weaker trough in the evening. At the surface, a weak pressure trough gradually|pushed eastward through the day as well. Modest amounts of instability and deep layer shear were present during the afternoon and evening when these features moved across and a few isolated strong to locally severe thunderstorms were able to develop in central Maryland near Washington DC. An upper level trough crossed the Appalachian Mountains during the morning of August 21st and moved through the region during the mid to late afternoon hours, followed by a second weaker trough in the evening. At the surface, a weak pressure trough gradually|pushed eastward through the day as well. Modest amounts of instability and deep layer shear were present during the afternoon and evening when these features moved across and a few isolated strong to locally severe thunderstorms were able to develop in central Maryland near Washington DC.\nEvent Narrative: A tree was blown down on MD-2 at Old Birdsville Road. A large tree limb was blown down on Muddy Creek Road at Shady Oaks Road.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 32.9059 km away, between 2019-08-21 17:54:00 and 2019-08-21 19:00:00. The events included records with measured wind gusts of 37.333333333333336 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: An upper level trough crossed the Appalachian Mountains during the morning of August 21st and moved through the region during the mid to late afternoon hours, followed by a second weaker trough in the evening. At the surface, a weak pressure trough gradually|pushed eastward through the day as well. Modest amounts of instability and deep layer shear were present during the afternoon and evening when these features moved across and a few isolated thunderstorms were able to develop and produce gusty winds over the waters. An upper level trough crossed the Appalachian Mountains during the morning of August 21st and moved through the region during the mid to late afternoon hours, followed by a second weaker trough in the evening. At the surface, a weak pressure trough gradually|pushed eastward through the day as well. Modest amounts of instability and deep layer shear were present during the afternoon and evening when these features moved across and a few isolated thunderstorms were able to develop and produce gusty winds over the waters. An upper level trough crossed the Appalachian Mountains during the morning of August 21st and moved through the region during the mid to late afternoon hours, followed by a second weaker trough in the evening. At the surface, a weak pressure trough gradually|pushed eastward through the day as well. Modest amounts of instability and deep layer shear were present during the afternoon and evening when these features moved across and a few isolated thunderstorms were able to develop and produce gusty winds over the waters. An upper level trough crossed the Appalachian Mountains during the morning of August 21st and moved through the region during the mid to late afternoon hours, followed by a second weaker trough in the evening. At the surface, a weak pressure trough gradually|pushed eastward through the day as well. Modest amounts of instability and deep layer shear were present during the afternoon and evening when these features moved across and a few isolated thunderstorms were able to develop and produce gusty winds over the waters. An upper level trough crossed the Appalachian Mountains during the morning of August 21st and moved through the region during the mid to late afternoon hours, followed by a second weaker trough in the evening. At the surface, a weak pressure trough gradually|pushed eastward through the day as well. Modest amounts of instability and deep layer shear were present during the afternoon and evening when these features moved across and a few isolated thunderstorms were able to develop and produce gusty winds over the waters. An upper level trough crossed the Appalachian Mountains during the morning of August 21st and moved through the region during the mid to late afternoon hours, followed by a second weaker trough in the evening. At the surface, a weak pressure trough gradually|pushed eastward through the day as well. Modest amounts of instability and deep layer shear were present during the afternoon and evening when these features moved across and a few isolated thunderstorms were able to develop and produce gusty winds over the waters.\nEvent Narrative:", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 30.8513 km away, between 2019-08-22 19:25:00 and 2019-08-22 20:25:00. The events included records with estimated wind gusts of 56.6 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Hot and humid conditions overspread the area on August 22nd ahead of an approaching cold front and upper level trough. This warmth and humidity allowed for the|development of significant amounts of instability by the afternoon hours. Convection during the afternoon and evening hours was initially focused along a remnant mesoscale convective system across central Virginia. However, additional areas of development occurred as upper level energy from Kentucky and West Virginia moved eastward and into the region and the cold front moved southeastward from Pennsylvania. Some of the thunderstorms became severe. Hot and humid conditions overspread the area on August 22nd ahead of an approaching cold front and upper level trough. This warmth and humidity allowed for the|development of significant amounts of instability by the afternoon hours. Convection during the afternoon and evening hours was initially focused along a remnant mesoscale convective system across central Virginia. However, additional areas of development occurred as upper level energy from Kentucky and West Virginia moved eastward and into the region and the cold front moved southeastward from Pennsylvania. Some of the thunderstorms became severe. Hot and humid conditions overspread the area on August 22nd ahead of an approaching cold front and upper level trough. This warmth and humidity allowed for the|development of significant amounts of instability by the afternoon hours. Convection during the afternoon and evening hours was initially focused along a remnant mesoscale convective system across central Virginia. However, additional areas of development occurred as upper level energy from Kentucky and West Virginia moved eastward and into the region and the cold front moved southeastward from Pennsylvania. Some of the thunderstorms became severe. Hot and humid conditions overspread the area on August 22nd ahead of an approaching cold front and upper level trough. This warmth and humidity allowed for the|development of significant amounts of instability by the afternoon hours. Convection during the afternoon and evening hours was initially focused along a remnant mesoscale convective system across central Virginia. However, additional areas of development occurred as upper level energy from Kentucky and West Virginia moved eastward and into the region and the cold front moved southeastward from Pennsylvania. Some of the thunderstorms became severe. Hot and humid conditions overspread the area on August 22nd ahead of an approaching cold front and upper level trough. This warmth and humidity allowed for the|development of significant amounts of instability by the afternoon hours. Convection during the afternoon and evening hours was initially focused along a remnant mesoscale convective system across central Virginia. However, additional areas of development occurred as upper level energy from Kentucky and West Virginia moved eastward and into the region and the cold front moved southeastward from Pennsylvania. Some of the thunderstorms became severe.\nEvent Narrative: A tree was blown down blocking part of Harford Square Drive near Hanson Road. Several reports of trees being blown down were received in the Laytonsville and Sandy Springs area. Several large trees were blown down in the Abingdon area. A tree was blown down at the intersection of MD-648 and Magothy Bridge Road. Trees, wires, and poles were blown down near the intersection of Marley Neck Boulevard and Creekside Village Boulevard.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 32.8016 km away, between 2019-08-22 19:55:00 and 2019-08-22 20:37:00. The events included records with measured wind gusts of 35.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Hot and humid conditions overspread the area on August 22nd ahead of an approaching cold front and upper level trough. This warmth and humidity allowed for the|development of significant amounts of instability by the afternoon hours. Convection during the afternoon and evening hours was initially focused along a remnant mesoscale convective system across central Virginia. However, additional areas of development occurred as upper level energy from Kentucky and West Virginia moved eastward and into the region and the cold front moved southeastward from Pennsylvania. Some of the thunderstorms produced gusty winds over the waters. Hot and humid conditions overspread the area on August 22nd ahead of an approaching cold front and upper level trough. This warmth and humidity allowed for the|development of significant amounts of instability by the afternoon hours. Convection during the afternoon and evening hours was initially focused along a remnant mesoscale convective system across central Virginia. However, additional areas of development occurred as upper level energy from Kentucky and West Virginia moved eastward and into the region and the cold front moved southeastward from Pennsylvania. Some of the thunderstorms produced gusty winds over the waters. Hot and humid conditions overspread the area on August 22nd ahead of an approaching cold front and upper level trough. This warmth and humidity allowed for the|development of significant amounts of instability by the afternoon hours. Convection during the afternoon and evening hours was initially focused along a remnant mesoscale convective system across central Virginia. However, additional areas of development occurred as upper level energy from Kentucky and West Virginia moved eastward and into the region and the cold front moved southeastward from Pennsylvania. Some of the thunderstorms produced gusty winds over the waters. Hot and humid conditions overspread the area on August 22nd ahead of an approaching cold front and upper level trough. This warmth and humidity allowed for the|development of significant amounts of instability by the afternoon hours. Convection during the afternoon and evening hours was initially focused along a remnant mesoscale convective system across central Virginia. However, additional areas of development occurred as upper level energy from Kentucky and West Virginia moved eastward and into the region and the cold front moved southeastward from Pennsylvania. Some of the thunderstorms produced gusty winds over the waters. Hot and humid conditions overspread the area on August 22nd ahead of an approaching cold front and upper level trough. This warmth and humidity allowed for the|development of significant amounts of instability by the afternoon hours. Convection during the afternoon and evening hours was initially focused along a remnant mesoscale convective system across central Virginia. However, additional areas of development occurred as upper level energy from Kentucky and West Virginia moved eastward and into the region and the cold front moved southeastward from Pennsylvania. Some of the thunderstorms produced gusty winds over the waters. Hot and humid conditions overspread the area on August 22nd ahead of an approaching cold front and upper level trough. This warmth and humidity allowed for the|development of significant amounts of instability by the afternoon hours. Convection during the afternoon and evening hours was initially focused along a remnant mesoscale convective system across central Virginia. However, additional areas of development occurred as upper level energy from Kentucky and West Virginia moved eastward and into the region and the cold front moved southeastward from Pennsylvania. Some of the thunderstorms produced gusty winds over the waters. Hot and humid conditions overspread the area on August 22nd ahead of an approaching cold front and upper level trough. This warmth and humidity allowed for the|development of significant amounts of instability by the afternoon hours. Convection during the afternoon and evening hours was initially focused along a remnant mesoscale convective system across central Virginia. However, additional areas of development occurred as upper level energy from Kentucky and West Virginia moved eastward and into the region and the cold front moved southeastward from Pennsylvania. Some of the thunderstorms produced gusty winds over the waters.\nEvent Narrative:", "The following events were reported: Flood. These occurred near station USW00093721, approximately 16.5218 km away, between 2019-08-22 20:30:00 and 2019-08-22 22:30:00. The flood was caused by Heavy Rain. Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: There was an isolated incident from flooding due to locally heavy rain.\nEvent Narrative: The 1100 block of North Wolfe Street was closed due to flooding.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 28.6555 km away, between 2019-08-28 16:55:00 and 2019-08-28 16:55:00. The events included records with measured wind gusts of 37.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front crossed the region during the afternoon hours of August 28th. A few scattered showers and thunderstorms developed along the boundary, and one produced gusty winds across portions of the waters.\nEvent Narrative:", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 38.9982 km away, between 2019-09-02 17:33:00 and 2019-09-02 17:37:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front crossed the region during the afternoon and evening hours at the same as an upper-level disturbance approached the region. A southerly flow out ahead of the boundary brought increased moisture and that combined with heating from sunshine led to unstable conditions by late in the day. Shear also increased late in the day in response to the approaching upper-level disturbance. This combination of instability, forcing, and wind shear led to showers and thunderstorms, some of which became severe. A cold front crossed the region during the afternoon and evening hours at the same as an upper-level disturbance approached the region. A southerly flow out ahead of the boundary brought increased moisture and that combined with heating from sunshine led to unstable conditions by late in the day. Shear also increased late in the day in response to the approaching upper-level disturbance. This combination of instability, forcing, and wind shear led to showers and thunderstorms, some of which became severe.\nEvent Narrative: Large tree limbs were blown down in Kingsville. Large tree limbs were blown down in Joppatowne.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 40.7935 km away, between 2019-09-02 18:12:00 and 2019-09-02 18:12:00. The events included records with measured wind gusts of 34.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front crossed the region during the afternoon and evening hours at the same as an upper-level disturbance approached the region. A southerly flow out ahead of the boundary brought increased moisture and that combined with heating from sunshine led to unstable conditions by late in the day. Shear also increased late in the day in response to the approaching upper-level disturbance. This combination of instability, forcing, and wind shear led to showers and thunderstorms, some of which produced gusty winds over the waters.\nEvent Narrative:", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 28.3818 km away, between 2019-10-27 09:46:00 and 2019-10-27 09:46:00. The events included records with estimated wind gusts of 34.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A strong cold front passed through on the 27th. Despite limited instability, showers were able to mix down gusty winds from aloft.\nEvent Narrative: Wind gusts in excess of 30 knots were reported at Hart Miller Island.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 32.0341 km away, between 2019-10-31 19:50:00 and 2019-10-31 22:02:00. The events included records with estimated wind gusts of 53.2 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A strong cold front passed through during the evening of the 31st. A southerly flow led to warm and humid conditions ahead of the boundary, which caused an unstable atmosphere. The instability along with the cold front caused showers and isolated thunderstorms, some of which were able to mix down strong winds from aloft. A strong cold front passed through during the evening of the 31st. A southerly flow led to warm and humid conditions ahead of the boundary, which caused an unstable atmosphere. The instability along with the cold front caused showers and isolated thunderstorms, some of which were able to mix down strong winds from aloft. A strong cold front passed through during the evening of the 31st. A southerly flow led to warm and humid conditions ahead of the boundary, which caused an unstable atmosphere. The instability along with the cold front caused showers and isolated thunderstorms, some of which were able to mix down strong winds from aloft. A strong cold front passed through during the evening of the 31st. A southerly flow led to warm and humid conditions ahead of the boundary, which caused an unstable atmosphere. The instability along with the cold front caused showers and isolated thunderstorms, some of which were able to mix down strong winds from aloft. A strong cold front passed through during the evening of the 31st. A southerly flow led to warm and humid conditions ahead of the boundary, which caused an unstable atmosphere. The instability along with the cold front caused showers and isolated thunderstorms, some of which were able to mix down strong winds from aloft. A strong cold front passed through during the evening of the 31st. A southerly flow led to warm and humid conditions ahead of the boundary, which caused an unstable atmosphere. The instability along with the cold front caused showers and isolated thunderstorms, some of which were able to mix down strong winds from aloft. A strong cold front passed through during the evening of the 31st. A southerly flow led to warm and humid conditions ahead of the boundary, which caused an unstable atmosphere. The instability along with the cold front caused showers and isolated thunderstorms, some of which were able to mix down strong winds from aloft. A strong cold front passed through during the evening of the 31st. A southerly flow led to warm and humid conditions ahead of the boundary, which caused an unstable atmosphere. The instability along with the cold front caused showers and isolated thunderstorms, some of which were able to mix down strong winds from aloft. A strong cold front passed through during the evening of the 31st. A southerly flow led to warm and humid conditions ahead of the boundary, which caused an unstable atmosphere. The instability along with the cold front caused showers and isolated thunderstorms, some of which were able to mix down strong winds from aloft. A strong cold front passed through during the evening of the 31st. A southerly flow led to warm and humid conditions ahead of the boundary, which caused an unstable atmosphere. The instability along with the cold front caused showers and isolated thunderstorms, some of which were able to mix down strong winds from aloft. A strong cold front passed through during the evening of the 31st. A southerly flow led to warm and humid conditions ahead of the boundary, which caused an unstable atmosphere. The instability along with the cold front caused showers and isolated thunderstorms, some of which were able to mix down strong winds from aloft. A strong cold front passed through during the evening of the 31st. A southerly flow led to warm and humid conditions ahead of the boundary, which caused an unstable atmosphere. The instability along with the cold front caused showers and isolated thunderstorms, some of which were able to mix down strong winds from aloft. A strong cold front passed through during the evening of the 31st. A southerly flow led to warm and humid conditions ahead of the boundary, which caused an unstable atmosphere. The instability along with the cold front caused showers and isolated thunderstorms, some of which were able to mix down strong winds from aloft. A strong cold front passed through during the evening of the 31st. A southerly flow led to warm and humid conditions ahead of the boundary, which caused an unstable atmosphere. The instability along with the cold front caused showers and isolated thunderstorms, some of which were able to mix down strong winds from aloft. A strong cold front passed through during the evening of the 31st. A southerly flow led to warm and humid conditions ahead of the boundary, which caused an unstable atmosphere. The instability along with the cold front caused showers and isolated thunderstorms, some of which were able to mix down strong winds from aloft.\nEvent Narrative: Several trees down along Old Frederick Road and Forsyth Road near Sykesville. Tree reported down on Johnsville Road near Liberty Road. Trees down along River Road in Sykesville. Tree reported down in the 6200 block of West Hemlock Drive. Tree down at the intersection of Burntwoods Road and Roscommon Drive. Several trees and wires down along Long Corner Road near the intersection with Windsor Forest Road. Tree reported down on Ridge Road near Marriotsville Road. Multiple reports of trees down along Marriotsville Road north of Albeth Heights. Trees down along MD-97 near the Montgomery County Line. Tree down in the 3600 block of Fallston Road. Other trees down in the area. Several trees down on the north side of Columbia, Maryland. Tree down at the intersection of Autumn Hill Drive and Bali Road. Tree down on Woodloo Drive. Tree down on Watervale Road at the intersection with Vale Road. Tree reported down on Philadelphia Road near Joppa Road. Tree down at the intersection of Higgins Drive and Saint Barbara Lane. Multiple trees snapped and uprooted, some fell onto houses. Also, several small boats flipped out of water a couple hundred feet onto land.", "The following events were reported: Flash Flood, Flood. These occurred near station USW00093721, approximately 25.5322 km away, between 2019-10-31 21:30:00 and 2019-10-31 23:59:00. The flood was caused by Heavy Rain. Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A strong cold front passed through the area on the 31st. Strong southerly winds ushered in plenty of moisture ahead of the boundary, and the moisture combined with a strong wind field to produce locally heavy rainfall. A strong cold front passed through the area on the 31st. Strong southerly winds ushered in plenty of moisture ahead of the boundary, and the moisture combined with a strong wind field to produce locally heavy rainfall. A strong cold front passed through the area on the 31st. Strong southerly winds ushered in plenty of moisture ahead of the boundary, and the moisture combined with a strong wind field to produce locally heavy rainfall. A strong cold front passed through the area on the 31st. Strong southerly winds ushered in plenty of moisture ahead of the boundary, and the moisture combined with a strong wind field to produce locally heavy rainfall. A strong cold front passed through the area on the 31st. Strong southerly winds ushered in plenty of moisture ahead of the boundary, and the moisture combined with a strong wind field to produce locally heavy rainfall. A strong cold front passed through the area on the 31st. Strong southerly winds ushered in plenty of moisture ahead of the boundary, and the moisture combined with a strong wind field to produce locally heavy rainfall. A strong cold front passed through the area on the 31st. Strong southerly winds ushered in plenty of moisture ahead of the boundary, and the moisture combined with a strong wind field to produce locally heavy rainfall. A strong cold front passed through the area on the 31st. Strong southerly winds ushered in plenty of moisture ahead of the boundary, and the moisture combined with a strong wind field to produce locally heavy rainfall. A strong cold front passed through the area on the 31st. Strong southerly winds ushered in plenty of moisture ahead of the boundary, and the moisture combined with a strong wind field to produce locally heavy rainfall. A strong cold front passed through the area on the 31st. Strong southerly winds ushered in plenty of moisture ahead of the boundary, and the moisture combined with a strong wind field to produce locally heavy rainfall. A strong cold front passed through the area on the 31st. Strong southerly winds ushered in plenty of moisture ahead of the boundary, and the moisture combined with a strong wind field to produce locally heavy rainfall. A strong cold front passed through the area on the 31st. Strong southerly winds ushered in plenty of moisture ahead of the boundary, and the moisture combined with a strong wind field to produce locally heavy rainfall.\nEvent Narrative: West Forest Park Avenue was closed due to flooding. West Strathmore Road was closed due to flash flooding near the intersection with Cross Country Boulevard. Agricultural flooding took place. Agricultural flooding took place. Water entered buildings off Sparks Road and portions of Home Road began to flood. North Chatham Road was closed due to flooding at Plum Tree Branch. The 4600 Block of Frederick Road was closed at Maidens Choice Run. Hammonds Ferry Road floods and was closed at the Patapsco River. Backwater flooding likely led to the closure of Furnace Avenue in Elkridge. The flooding continued until 11:05 AM EST on November 1st. Three to twelve inches of water were flowing along the road in the 8500 and 8600 Blocks of Frederick Road. A water rescue occurred near the intersection of Gwyndale and Gwynnmore Avenues. A road was closed near Falls Road and Jones Falls Expressway due to flooding. Water entered buildings off Sparks Road and portions of Home Road began to flood. The flooding continued until November 1st at 6:57 AM EST.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 32.8568 km away, between 2019-10-31 21:46:00 and 2019-10-31 23:44:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A strong cold front passed through during the evening of the 31st. A southerly flow led to warm and humid conditions ahead of the boundary, which caused an unstable atmosphere. The instability along with the cold front caused showers and isolated thunderstorms, some of which were able to mix down strong winds from aloft. A strong cold front passed through during the evening of the 31st. A southerly flow led to warm and humid conditions ahead of the boundary, which caused an unstable atmosphere. The instability along with the cold front caused showers and isolated thunderstorms, some of which were able to mix down strong winds from aloft. A strong cold front passed through during the evening of the 31st. A southerly flow led to warm and humid conditions ahead of the boundary, which caused an unstable atmosphere. The instability along with the cold front caused showers and isolated thunderstorms, some of which were able to mix down strong winds from aloft. A strong cold front passed through during the evening of the 31st. A southerly flow led to warm and humid conditions ahead of the boundary, which caused an unstable atmosphere. The instability along with the cold front caused showers and isolated thunderstorms, some of which were able to mix down strong winds from aloft. A strong cold front passed through during the evening of the 31st. A southerly flow led to warm and humid conditions ahead of the boundary, which caused an unstable atmosphere. The instability along with the cold front caused showers and isolated thunderstorms, some of which were able to mix down strong winds from aloft. A strong cold front passed through during the evening of the 31st. A southerly flow led to warm and humid conditions ahead of the boundary, which caused an unstable atmosphere. The instability along with the cold front caused showers and isolated thunderstorms, some of which were able to mix down strong winds from aloft. A strong cold front passed through during the evening of the 31st. A southerly flow led to warm and humid conditions ahead of the boundary, which caused an unstable atmosphere. The instability along with the cold front caused showers and isolated thunderstorms, some of which were able to mix down strong winds from aloft. A strong cold front passed through during the evening of the 31st. A southerly flow led to warm and humid conditions ahead of the boundary, which caused an unstable atmosphere. The instability along with the cold front caused showers and isolated thunderstorms, some of which were able to mix down strong winds from aloft. A strong cold front passed through during the evening of the 31st. A southerly flow led to warm and humid conditions ahead of the boundary, which caused an unstable atmosphere. The instability along with the cold front caused showers and isolated thunderstorms, some of which were able to mix down strong winds from aloft. A strong cold front passed through during the evening of the 31st. A southerly flow led to warm and humid conditions ahead of the boundary, which caused an unstable atmosphere. The instability along with the cold front caused showers and isolated thunderstorms, some of which were able to mix down strong winds from aloft. A strong cold front passed through during the evening of the 31st. A southerly flow led to warm and humid conditions ahead of the boundary, which caused an unstable atmosphere. The instability along with the cold front caused showers and isolated thunderstorms, some of which were able to mix down strong winds from aloft. A strong cold front passed through during the evening of the 31st. A southerly flow led to warm and humid conditions ahead of the boundary, which caused an unstable atmosphere. The instability along with the cold front caused showers and isolated thunderstorms, some of which were able to mix down strong winds from aloft.\nEvent Narrative: Wind gusts in excess of 30 knots were observed at Annapolis buoy. Wind gusts in excess of 30 knots were observed at Bay Bridge Airport.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 38.2826 km away, between 2019-10-31 22:06:00 and 2019-10-31 22:11:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A severe weather outbreak impacted the mid-Atlantic from the evening of October 31 through the pre-dawn hours of November 1. A strong area of low pressure moved through the eastern Great Lakes on the 31st. Ahead of it, strong southerly flow advected an unseasonably warm and moist air mass into the mid-Atlantic. This generated enough instability, combined with extremely strong wind fields, to produce a low topped line of severe convection which tracked across the entire region. Widespread damaging wind occurred as the squall line moved through, along with a couple of short lived embedded tornadoes. A severe weather outbreak impacted the mid-Atlantic from the evening of October 31 through the pre-dawn hours of November 1. A strong area of low pressure moved through the eastern Great Lakes on the 31st. Ahead of it, strong southerly flow advected an unseasonably warm and moist air mass into the mid-Atlantic. This generated enough instability, combined with extremely strong wind fields, to produce a low topped line of severe convection which tracked across the entire region. Widespread damaging wind occurred as the squall line moved through, along with a couple of short lived embedded tornadoes.\nEvent Narrative: Measured by the Tolchester Beach NOS gauge. Trees and wires were downed in the area of MD-802 and Romancoke Rd. An NWS employee in the area conducted an informal survey of storm damage in the area and determined it was caused by straight line winds. Time estimated from radar.", "The following events were reported: Flood. These occurred near station USW00093721, approximately 25.0262 km away, between 2019-11-01 00:40:00 and 2019-11-01 04:13:00. The flood was caused by Heavy Rain. Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A strong cold front passed through the area on the 31st of October. Strong southerly winds ushered in plenty of moisture ahead of the boundary, and the moisture combined with a strong wind field to produce locally heavy rainfall. Streams and rivers flooded into the morning of the first. A strong cold front passed through the area on the 31st of October. Strong southerly winds ushered in plenty of moisture ahead of the boundary, and the moisture combined with a strong wind field to produce locally heavy rainfall. Streams and rivers flooded into the morning of the first.\nEvent Narrative: The parking lot for the Patuxent River State Park at Maryland Route 97 begins to flood. The riverside trails flooded. Water also approached fields of of Bald Eagle Drive. Water approached Brock Bridge Road.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 34.0216 km away, between 2020-01-12 01:01:00 and 2020-01-12 02:00:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A negatively tilted trough and associated surface low tracked into Ohio. Warm, humid air streamed northward into the area in southerly flow well in advance of the low. A band of pre-frontal convection moved across the waters, transporting some of the high winds from aloft down to the surface. A negatively tilted trough and associated surface low tracked into Ohio. Warm, humid air streamed northward into the area in southerly flow well in advance of the low. A band of pre-frontal convection moved across the waters, transporting some of the high winds from aloft down to the surface. A negatively tilted trough and associated surface low tracked into Ohio. Warm, humid air streamed northward into the area in southerly flow well in advance of the low. A band of pre-frontal convection moved across the waters, transporting some of the high winds from aloft down to the surface. A negatively tilted trough and associated surface low tracked into Ohio. Warm, humid air streamed northward into the area in southerly flow well in advance of the low. A band of pre-frontal convection moved across the waters, transporting some of the high winds from aloft down to the surface. A negatively tilted trough and associated surface low tracked into Ohio. Warm, humid air streamed northward into the area in southerly flow well in advance of the low. A band of pre-frontal convection moved across the waters, transporting some of the high winds from aloft down to the surface.\nEvent Narrative: Wind gusts in excess of 30 knots were observed at Bay Bridge Airport. Wind gusts in excess of 30 knots were observed at Hart Miller Island.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 23.5852 km away, between 2020-02-07 07:53:00 and 2020-02-07 09:02:00. The events included records with estimated wind gusts of 52.9 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 18000.0 and crop damage of 0.0. \n\nEpisode Narrative: An area of low pressure formed over the area in response to an impressive longwave trough approaching from the west. A line of low-topped showers and thunderstorms formed along the system's cold front, leading to the formation of multiple tornadoes within the high shear-low CAPE environment. These tornadoes, along with straight-line winds from other storms, produced widespread damage across much of central and northern Maryland. An area of low pressure formed over the area in response to an impressive longwave trough approaching from the west. A line of low-topped showers and thunderstorms formed along the system's cold front, leading to the formation of multiple tornadoes within the high shear-low CAPE environment. These tornadoes, along with straight-line winds from other storms, produced widespread damage across much of central and northern Maryland. An area of low pressure formed over the area in response to an impressive longwave trough approaching from the west. A line of low-topped showers and thunderstorms formed along the system's cold front, leading to the formation of multiple tornadoes within the high shear-low CAPE environment. These tornadoes, along with straight-line winds from other storms, produced widespread damage across much of central and northern Maryland. An area of low pressure formed over the area in response to an impressive longwave trough approaching from the west. A line of low-topped showers and thunderstorms formed along the system's cold front, leading to the formation of multiple tornadoes within the high shear-low CAPE environment. These tornadoes, along with straight-line winds from other storms, produced widespread damage across much of central and northern Maryland. An area of low pressure formed over the area in response to an impressive longwave trough approaching from the west. A line of low-topped showers and thunderstorms formed along the system's cold front, leading to the formation of multiple tornadoes within the high shear-low CAPE environment. These tornadoes, along with straight-line winds from other storms, produced widespread damage across much of central and northern Maryland. An area of low pressure formed over the area in response to an impressive longwave trough approaching from the west. A line of low-topped showers and thunderstorms formed along the system's cold front, leading to the formation of multiple tornadoes within the high shear-low CAPE environment. These tornadoes, along with straight-line winds from other storms, produced widespread damage across much of central and northern Maryland. An area of low pressure formed over the area in response to an impressive longwave trough approaching from the west. A line of low-topped showers and thunderstorms formed along the system's cold front, leading to the formation of multiple tornadoes within the high shear-low CAPE environment. These tornadoes, along with straight-line winds from other storms, produced widespread damage across much of central and northern Maryland. An area of low pressure formed over the area in response to an impressive longwave trough approaching from the west. A line of low-topped showers and thunderstorms formed along the system's cold front, leading to the formation of multiple tornadoes within the high shear-low CAPE environment. These tornadoes, along with straight-line winds from other storms, produced widespread damage across much of central and northern Maryland. An area of low pressure formed over the area in response to an impressive longwave trough approaching from the west. A line of low-topped showers and thunderstorms formed along the system's cold front, leading to the formation of multiple tornadoes within the high shear-low CAPE environment. These tornadoes, along with straight-line winds from other storms, produced widespread damage across much of central and northern Maryland. An area of low pressure formed over the area in response to an impressive longwave trough approaching from the west. A line of low-topped showers and thunderstorms formed along the system's cold front, leading to the formation of multiple tornadoes within the high shear-low CAPE environment. These tornadoes, along with straight-line winds from other storms, produced widespread damage across much of central and northern Maryland.\nEvent Narrative: Multiple trees and branches down at residence in 14900 block of Chelsea Circle. Tree down in 700 block of Lisbon Center Drive. Tree down in 6800 block of Haviland Mill Road. Tree down near intersection of Marriottsville Road and Baltimore National Pike. Tree down near intersection of Driver Road and Marriottsville Road. Tree down near intersection of Cedar Lane and Lightfoot Path. Tree down to the south of the I-70 and US-29 ramp. Tree down near the intersection of Red Branch Road and Old Annapolis Road. Tree down in 5800 block of Thunder Hill Road. Tree down near the intersection of Rogers Avenue and Brightwell Drive. Tree down in 8400 block of High Ridge Road. Tree down near the intersection of Gilford Road and Oakland Mills Road. Tree down near intersection of Race Road and Church Avenue. Tree down near the intersection of Vollmerhausen Road and Dragonclaw Road. Tree down near the intersection of Eaglehill Road and North Shore Road. Tree down near the intersection of Shore Acres Road and Stonington Drive.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 33.4301 km away, between 2020-02-07 09:10:00 and 2020-02-07 09:10:00. The events included records with measured wind gusts of 47.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: An area of low pressure formed over the area in response to an impressive longwave trough approaching from the west. A line of low-topped showers and thunderstorms formed along the system's cold front, leading to instances of high winds over the waters.\nEvent Narrative:", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 38.4788 km away, between 2020-02-07 09:24:00 and 2020-02-07 09:24:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: An area of low pressure moving out of the Southeast began to explosively intensify as it moved over the mid-Atlantic. On the morning of February 7, the eastern mid-Atlantic was briefly within the warm sector of the deepening low. An environment of extreme wind fields was present, and temperatures and dew points rose enough for sufficient instability to develop to sustain convection. A line of low topped but intense convection developed, and despite producing little thunder and lightning it produced a long swath of wind damage over the mid-Atlantic, along with a few tornadoes between Virginia and Maryland.\nEvent Narrative: Reports of downed trees in the area of Rock Hall Ave. Time estimated from radar.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 35.5157 km away, between 2020-02-27 00:20:00 and 2020-02-27 00:25:00. The events included records with measured wind gusts of 38.5 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A developing area of low pressure tracked from northern Virginia toward New Jersey, dragging a cold front across the waters. A narrow band of low-topped thunderstorms developed in the warm humid airmass in advance of the front. These storms produced high winds as they tracked across the waters. A developing area of low pressure tracked from northern Virginia toward New Jersey, dragging a cold front across the waters. A narrow band of low-topped thunderstorms developed in the warm humid airmass in advance of the front. These storms produced high winds as they tracked across the waters.\nEvent Narrative:", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 24.6795 km away, between 2020-03-03 20:54:00 and 2020-03-04 00:15:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: An upper level disturbance and associated cold front progressed across the area, leading to the development of multiple rounds of showers, and even a few low-topped thunderstorms across the area. These showers and storms led to gusts in excess of the 34 knots over the waters. An upper level disturbance and associated cold front progressed across the area, leading to the development of multiple rounds of showers, and even a few low-topped thunderstorms across the area. These showers and storms led to gusts in excess of the 34 knots over the waters. An upper level disturbance and associated cold front progressed across the area, leading to the development of multiple rounds of showers, and even a few low-topped thunderstorms across the area. These showers and storms led to gusts in excess of the 34 knots over the waters. An upper level disturbance and associated cold front progressed across the area, leading to the development of multiple rounds of showers, and even a few low-topped thunderstorms across the area. These showers and storms led to gusts in excess of the 34 knots over the waters. An upper level disturbance and associated cold front progressed across the area, leading to the development of multiple rounds of showers, and even a few low-topped thunderstorms across the area. These showers and storms led to gusts in excess of the 34 knots over the waters. An upper level disturbance and associated cold front progressed across the area, leading to the development of multiple rounds of showers, and even a few low-topped thunderstorms across the area. These showers and storms led to gusts in excess of the 34 knots over the waters. An upper level disturbance and associated cold front progressed across the area, leading to the development of multiple rounds of showers, and even a few low-topped thunderstorms across the area. These showers and storms led to gusts in excess of the 34 knots over the waters. An upper level disturbance and associated cold front progressed across the area, leading to the development of multiple rounds of showers, and even a few low-topped thunderstorms across the area. These showers and storms led to gusts in excess of the 34 knots over the waters. An upper level disturbance and associated cold front progressed across the area, leading to the development of multiple rounds of showers, and even a few low-topped thunderstorms across the area. These showers and storms led to gusts in excess of the 34 knots over the waters. An upper level disturbance and associated cold front progressed across the area, leading to the development of multiple rounds of showers, and even a few low-topped thunderstorms across the area. These showers and storms led to gusts in excess of the 34 knots over the waters. An upper level disturbance and associated cold front progressed across the area, leading to the development of multiple rounds of showers, and even a few low-topped thunderstorms across the area. These showers and storms led to gusts in excess of the 34 knots over the waters.\nEvent Narrative: Wind gusts in excess of 30 knots were observed at Annapolis.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 18.8274 km away, between 2020-03-03 23:29:00 and 2020-03-03 23:59:00.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 22000.0 and crop damage of 0.0. \n\nEpisode Narrative: A shallow convective line with intermittent lightning formed behind a cold front in response to a strong disturbance progressing through aloft. This convective line produced wind damage across portions of central and western Maryland. A shallow convective line with intermittent lightning formed behind a cold front in response to a strong disturbance progressing through aloft. This convective line produced wind damage across portions of central and western Maryland. A shallow convective line with intermittent lightning formed behind a cold front in response to a strong disturbance progressing through aloft. This convective line produced wind damage across portions of central and western Maryland. A shallow convective line with intermittent lightning formed behind a cold front in response to a strong disturbance progressing through aloft. This convective line produced wind damage across portions of central and western Maryland. A shallow convective line with intermittent lightning formed behind a cold front in response to a strong disturbance progressing through aloft. This convective line produced wind damage across portions of central and western Maryland. A shallow convective line with intermittent lightning formed behind a cold front in response to a strong disturbance progressing through aloft. This convective line produced wind damage across portions of central and western Maryland.\nEvent Narrative: Tree down on Watersville Road. Tree down on MD-97 at McKendree Road. Tree down on Jennings Chapel Road. Tree down on Tridelphia Mill Road at Meadow Glenn. Tree down on Tridelphia Mill Road at Highland Road. Trees down on houses along Wild Ginger Court. Tree down on Hesperus Drive. Tree down on Broken Land Parkway at Snowden River Parkway. Tree down on house on Worthington Way. Tree down on Little Patuxent Parkway at Blue February Parkway. Tree on a vehicle in Morning Mews. Tree down on US-1 at I-695.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 36.9916 km away, between 2020-03-06 18:00:00 and 2020-03-06 18:00:00. The events included records with measured wind gusts of 35.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Convective showers developed beneath a deep upper-level trough within strong northwesterly low-level low behind an area of low pressure organizing off the East Coast. These convective showers were cellular in nature, and produced gusts in excess of 34 knots as they passed over the waters.\nEvent Narrative:", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 31.5525 km away, between 2020-03-10 13:05:00 and 2020-03-10 14:00:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Gusty showers formed across the area ahead of a longwave trough and associated surface cold front approaching from the west. Inverted-V profiles and strong winds aloft allowed for efficient transport of strong winds to the surface in the showers that formed, leading to gust in excess of 34 knots over the waters. Gusty showers formed across the area ahead of a longwave trough and associated surface cold front approaching from the west. Inverted-V profiles and strong winds aloft allowed for efficient transport of strong winds to the surface in the showers that formed, leading to gust in excess of 34 knots over the waters. Gusty showers formed across the area ahead of a longwave trough and associated surface cold front approaching from the west. Inverted-V profiles and strong winds aloft allowed for efficient transport of strong winds to the surface in the showers that formed, leading to gust in excess of 34 knots over the waters.\nEvent Narrative: Wind gusts in excess of 30 knots were observed at Annapolis. Wind gusts in excess of 30 knots were observed at Tolly Point.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 32.758 km away, between 2020-04-08 02:55:00 and 2020-04-08 03:07:00. The events included records with estimated wind gusts of 55.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 6000.0 and crop damage of 0.0. \n\nEpisode Narrative: A cold front passed through the area. Despite limited instability, there was a strong wind field aloft along with steep low-level lapse rates. This resulted in some damaging wind gusts with showers and thunderstorms. A cold front passed through the area. Despite limited instability, there was a strong wind field aloft along with steep low-level lapse rates. This resulted in some damaging wind gusts with showers and thunderstorms.\nEvent Narrative: Numerous trees were reported down in the vicinity of MD-97 New Washington Road and Bartholow Road in the Sykesville area. A tree was blown down on MD-125 Old Court Road at Davis Avenue.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 35.3889 km away, between 2020-04-08 03:29:00 and 2020-04-08 04:00:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front passed through the area. Despite limited instability, there was a strong wind field aloft along with steep low-level lapse rates. This resulted in gusty winds that were associated with showers and thunderstorms. A cold front passed through the area. Despite limited instability, there was a strong wind field aloft along with steep low-level lapse rates. This resulted in gusty winds that were associated with showers and thunderstorms. A cold front passed through the area. Despite limited instability, there was a strong wind field aloft along with steep low-level lapse rates. This resulted in gusty winds that were associated with showers and thunderstorms.\nEvent Narrative: A wind gust in excess of 30 knots was reported. A wind gust in excess of 30 knots was reported.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 28.9659 km away, between 2020-04-09 11:15:00 and 2020-04-09 23:06:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front passed through on the 9th. Stronger winds were aloft, and some were able to mix down in heavier showers and thunderstorms. A cold front passed through on the 9th. Stronger winds were aloft, and some were able to mix down in heavier showers and thunderstorms. A cold front passed through on the 9th. Stronger winds were aloft, and some were able to mix down in heavier showers and thunderstorms. A cold front passed through on the 9th. Stronger winds were aloft, and some were able to mix down in heavier showers and thunderstorms. A cold front passed through on the 9th. Stronger winds were aloft, and some were able to mix down in heavier showers and thunderstorms. A cold front passed through on the 9th. Stronger winds were aloft, and some were able to mix down in heavier showers and thunderstorms. A cold front passed through on the 9th. Stronger winds were aloft, and some were able to mix down in heavier showers and thunderstorms. A cold front passed through on the 9th. Stronger winds were aloft, and some were able to mix down in heavier showers and thunderstorms. A cold front passed through on the 9th. Stronger winds were aloft, and some were able to mix down in heavier showers and thunderstorms. A cold front passed through on the 9th. Stronger winds were aloft, and some were able to mix down in heavier showers and thunderstorms. A cold front passed through on the 9th. Stronger winds were aloft, and some were able to mix down in heavier showers and thunderstorms. A cold front passed through on the 9th. Stronger winds were aloft, and some were able to mix down in heavier showers and thunderstorms. A cold front passed through on the 9th. Stronger winds were aloft, and some were able to mix down in heavier showers and thunderstorms. A cold front passed through on the 9th. Stronger winds were aloft, and some were able to mix down in heavier showers and thunderstorms. A cold front passed through on the 9th. Stronger winds were aloft, and some were able to mix down in heavier showers and thunderstorms. A cold front passed through on the 9th. Stronger winds were aloft, and some were able to mix down in heavier showers and thunderstorms. A cold front passed through on the 9th. Stronger winds were aloft, and some were able to mix down in heavier showers and thunderstorms. A cold front passed through on the 9th. Stronger winds were aloft, and some were able to mix down in heavier showers and thunderstorms. A cold front passed through on the 9th. Stronger winds were aloft, and some were able to mix down in heavier showers and thunderstorms. A cold front passed through on the 9th. Stronger winds were aloft, and some were able to mix down in heavier showers and thunderstorms. A cold front passed through on the 9th. Stronger winds were aloft, and some were able to mix down in heavier showers and thunderstorms. A cold front passed through on the 9th. Stronger winds were aloft, and some were able to mix down in heavier showers and thunderstorms. A cold front passed through on the 9th. Stronger winds were aloft, and some were able to mix down in heavier showers and thunderstorms. A cold front passed through on the 9th. Stronger winds were aloft, and some were able to mix down in heavier showers and thunderstorms. A cold front passed through on the 9th. Stronger winds were aloft, and some were able to mix down in heavier showers and thunderstorms. A cold front passed through on the 9th. Stronger winds were aloft, and some were able to mix down in heavier showers and thunderstorms. A cold front passed through on the 9th. Stronger winds were aloft, and some were able to mix down in heavier showers and thunderstorms. A cold front passed through on the 9th. Stronger winds were aloft, and some were able to mix down in heavier showers and thunderstorms. A cold front passed through on the 9th. Stronger winds were aloft, and some were able to mix down in heavier showers and thunderstorms. A cold front passed through on the 9th. Stronger winds were aloft, and some were able to mix down in heavier showers and thunderstorms. A cold front passed through on the 9th. Stronger winds were aloft, and some were able to mix down in heavier showers and thunderstorms. A cold front passed through on the 9th. Stronger winds were aloft, and some were able to mix down in heavier showers and thunderstorms. A cold front passed through on the 9th. Stronger winds were aloft, and some were able to mix down in heavier showers and thunderstorms. A cold front passed through on the 9th. Stronger winds were aloft, and some were able to mix down in heavier showers and thunderstorms. A cold front passed through on the 9th. Stronger winds were aloft, and some were able to mix down in heavier showers and thunderstorms. A cold front passed through on the 9th. Stronger winds were aloft, and some were able to mix down in heavier showers and thunderstorms. A cold front passed through on the 9th. Stronger winds were aloft, and some were able to mix down in heavier showers and thunderstorms. A cold front passed through on the 9th. Stronger winds were aloft, and some were able to mix down in heavier showers and thunderstorms. A cold front passed through on the 9th. Stronger winds were aloft, and some were able to mix down in heavier showers and thunderstorms.\nEvent Narrative: A wind gust in excess of 30 knots was reported. A wind gust in excess of 30 knots was reported. A wind gust in excess of 30 knots was reported. A wind gust in excess of 30 knots was reported. A wind gust in excess of 30 knots was reported. A wind gust in excess of 30 knots was reported. A wind gust in excess of 30 knots was reported. A wind gust in excess of 30 knots was reported. A wind gust in excess of 30 knots was reported. A wind gust in excess of 30 knots was reported. A wind gust in excess of 30 knots was reported. A wind gust in excess of 30 knots was reported. A wind gust in excess of 30 knots was reported. A wind gust in excess of 30 knots was reported. A wind gust in excess of 30 knots was reported.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 46.278 km away, between 2020-04-09 11:20:00 and 2020-04-09 11:45:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 1000.0 and crop damage of 0.0. \n\nEpisode Narrative: A cold front passed through on the 9th. Stronger winds were aloft, and some were able to mix down in heavier showers and thunderstorms. A cold front passed through on the 9th. Stronger winds were aloft, and some were able to mix down in heavier showers and thunderstorms.\nEvent Narrative: A tree was blown down on MD-97 New Washington Road north of Hook Road. Wires were blown down in the 2000 block of Laurel Brook Road.", "The following events were reported: Flood. These occurred near station USW00093721, approximately 28.6414 km away, between 2020-04-13 07:28:00 and 2020-04-13 20:58:00. The flood was caused by Heavy Rain. Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Copious amounts of moisture along with strong lift from a cold front led to areas of heavy rainfall on the 13th. The heavy rain caused instances of flooding. Copious amounts of moisture along with strong lift from a cold front led to areas of heavy rainfall on the 13th. The heavy rain caused instances of flooding. Copious amounts of moisture along with strong lift from a cold front led to areas of heavy rainfall on the 13th. The heavy rain caused instances of flooding.\nEvent Narrative: The water level rose above minor flood stage and it crested at 8.67 feet at 9:15 AM EST. Winter Run Road was flooded near Singer Road. The water level rose above minor flood stage at Beaverdam Run in Cockeysville. The water crested at 9.04 feet at 2:35 PM EST. Beaver Run Lane was flooded. The water level rose above minor flood stage along the Patapsco River at Elkridge. The level crested at 17.56 feet at 4:50 PM EST.", "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00093721, approximately 19.4676 km away, between 2020-04-13 12:36:00 and 2020-04-13 13:43:00. The events included records with hailstones measuring 50.07142857142857 inches.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 36000.0 and crop damage of 0.0. \n\nEpisode Narrative: A very strong cold front passed through the area while a potent upper-level trough was positioned just to our west. Strong winds aloft were able to mix down in heavier showers and thunderstorms due to an unstable atmosphere. Low-level winds changing speed and direction with height combined with a thunderstorm to trigger an isolated tornado. A very strong cold front passed through the area while a potent upper-level trough was positioned just to our west. Strong winds aloft were able to mix down in heavier showers and thunderstorms due to an unstable atmosphere. Low-level winds changing speed and direction with height combined with a thunderstorm to trigger an isolated tornado. A very strong cold front passed through the area while a potent upper-level trough was positioned just to our west. Strong winds aloft were able to mix down in heavier showers and thunderstorms due to an unstable atmosphere. Low-level winds changing speed and direction with height combined with a thunderstorm to trigger an isolated tornado. A very strong cold front passed through the area while a potent upper-level trough was positioned just to our west. Strong winds aloft were able to mix down in heavier showers and thunderstorms due to an unstable atmosphere. Low-level winds changing speed and direction with height combined with a thunderstorm to trigger an isolated tornado. A very strong cold front passed through the area while a potent upper-level trough was positioned just to our west. Strong winds aloft were able to mix down in heavier showers and thunderstorms due to an unstable atmosphere. Low-level winds changing speed and direction with height combined with a thunderstorm to trigger an isolated tornado. A very strong cold front passed through the area while a potent upper-level trough was positioned just to our west. Strong winds aloft were able to mix down in heavier showers and thunderstorms due to an unstable atmosphere. Low-level winds changing speed and direction with height combined with a thunderstorm to trigger an isolated tornado. A very strong cold front passed through the area while a potent upper-level trough was positioned just to our west. Strong winds aloft were able to mix down in heavier showers and thunderstorms due to an unstable atmosphere. Low-level winds changing speed and direction with height combined with a thunderstorm to trigger an isolated tornado. A very strong cold front passed through the area while a potent upper-level trough was positioned just to our west. Strong winds aloft were able to mix down in heavier showers and thunderstorms due to an unstable atmosphere. Low-level winds changing speed and direction with height combined with a thunderstorm to trigger an isolated tornado. A very strong cold front passed through the area while a potent upper-level trough was positioned just to our west. Strong winds aloft were able to mix down in heavier showers and thunderstorms due to an unstable atmosphere. Low-level winds changing speed and direction with height combined with a thunderstorm to trigger an isolated tornado. A very strong cold front passed through the area while a potent upper-level trough was positioned just to our west. Strong winds aloft were able to mix down in heavier showers and thunderstorms due to an unstable atmosphere. Low-level winds changing speed and direction with height combined with a thunderstorm to trigger an isolated tornado. A very strong cold front passed through the area while a potent upper-level trough was positioned just to our west. Strong winds aloft were able to mix down in heavier showers and thunderstorms due to an unstable atmosphere. Low-level winds changing speed and direction with height combined with a thunderstorm to trigger an isolated tornado. A very strong cold front passed through the area while a potent upper-level trough was positioned just to our west. Strong winds aloft were able to mix down in heavier showers and thunderstorms due to an unstable atmosphere. Low-level winds changing speed and direction with height combined with a thunderstorm to trigger an isolated tornado. A very strong cold front passed through the area while a potent upper-level trough was positioned just to our west. Strong winds aloft were able to mix down in heavier showers and thunderstorms due to an unstable atmosphere. Low-level winds changing speed and direction with height combined with a thunderstorm to trigger an isolated tornado. A very strong cold front passed through the area while a potent upper-level trough was positioned just to our west. Strong winds aloft were able to mix down in heavier showers and thunderstorms due to an unstable atmosphere. Low-level winds changing speed and direction with height combined with a thunderstorm to trigger an isolated tornado.\nEvent Narrative: A tree was blown down on Lakeshore Drive. A tree was blown down on Yachtsman Way. A large tree blew down across the roadway on Cattail Lane. Other large branches were blown down in the area. A tree blew down onto a car off of Green Mountain Circle in Columbia. Several trees were blown down in the Laurel area. A tree was uprooted along Edmonson Avenue. A 59-knot (68 MPH) wind gust was measured by a mesonet at the Maryland Science Center in downtown Baltimore. A gazebo was blown over and several large branches were blown down near the intersection of Woodlawn Avenue and Middlegate Court. A 63-knot (72 MPH) wind gust was measured by a mesonet in Glen Burnie. A tree blew down at the intersection of Furnace Road and Durham Road. A large tree (about two feet in diameter) was uprooted near the intersection of Portship Road and Yorkway in Dundalk. Multiple large tree branches were snapped on Montrose Avenue in Essex.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 13.4765 km away, between 2020-04-13 13:39:00 and 2020-04-13 13:39:00. The events included records with measured wind gusts of 59.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A very strong cold front passed through the area while a potent upper-level trough was positioned just to our west. Strong winds aloft were able to mix down in heavier showers and thunderstorms.\nEvent Narrative:", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 38.4788 km away, between 2020-04-13 14:06:00 and 2020-04-13 14:06:00. The events included records with measured wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A highly anomalous weather system affected much of the eastern United States on April 13. From the night of April 12 through the day on April 13, strengthening low pressure tracked in an almost due northerly direction from the Ohio Valley, through the Great Lakes, and into Canada. A record strong low level jet developed ahead of it along the East Coast. In the mid-Atlantic, a warm front moved through the region during the morning of the 13th, bringing showery weather. During and after the warm frontal passage, mixing with the low level jet brought destructive wind gusts to the surface, especially near the coast where gusts were enhanced by a well-defined gravity wave.||During the afternoon hours, a strong cold front approached, providing strong forcing to an environment of strong to extreme wind shear. Instability was limited due to a lack of clearing following the morning warm frontal passage. However, enough heating occurred by mid-afternoon that a line of strong to severe thunderstorms did manage to develop, producing a number of damaging wind reports as it moved towards the coast.\nEvent Narrative:", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 46.3192 km away, between 2020-04-21 13:08:00 and 2020-04-21 13:08:00. The events included records with estimated wind gusts of 52.5 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Strong low pressure tracked through southern Canada on April 21. A warm front associated with the low moved through the mid-Atlantic during the morning hours, with a strong and fast moving cold front following closely behind for the afternoon. This was an unseasonably strong cold front which marked the leading edge of a much colder than average air mass moving into the region behind it. A strongly forced and highly sheared environment existed ahead of the front. Widespread morning cloudiness and rain showers limited instability, but a brief window of clearing allowed for heating and destabilization to occur. A severe squall line developed, producing considerable wind damage over eastern portions of the mid-Atlantic. A weak tornado also occurred along the New Jersey coast. Strong low pressure tracked through southern Canada on April 21. A warm front associated with the low moved through the mid-Atlantic during the morning hours, with a strong and fast moving cold front following closely behind for the afternoon. This was an unseasonably strong cold front which marked the leading edge of a much colder than average air mass moving into the region behind it. A strongly forced and highly sheared environment existed ahead of the front. Widespread morning cloudiness and rain showers limited instability, but a brief window of clearing allowed for heating and destabilization to occur. A severe squall line developed, producing considerable wind damage over eastern portions of the mid-Atlantic. A weak tornado also occurred along the New Jersey coast.\nEvent Narrative: A tree was uprooted in the area. Time estimated from radar. Several trees were downed near MD-298. Time estimated from radar.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 31.1808 km away, between 2020-06-04 19:54:00 and 2020-06-04 21:00:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Thunderstorms initiated along a pressure trough in the lee of the Appalachian Mountains during the mid to late afternoon, and persisted into the evening. Some thunderstorms produced gusty winds over the waters. Thunderstorms initiated along a pressure trough in the lee of the Appalachian Mountains during the mid to late afternoon, and persisted into the evening. Some thunderstorms produced gusty winds over the waters. Thunderstorms initiated along a pressure trough in the lee of the Appalachian Mountains during the mid to late afternoon, and persisted into the evening. Some thunderstorms produced gusty winds over the waters. Thunderstorms initiated along a pressure trough in the lee of the Appalachian Mountains during the mid to late afternoon, and persisted into the evening. Some thunderstorms produced gusty winds over the waters. Thunderstorms initiated along a pressure trough in the lee of the Appalachian Mountains during the mid to late afternoon, and persisted into the evening. Some thunderstorms produced gusty winds over the waters. Thunderstorms initiated along a pressure trough in the lee of the Appalachian Mountains during the mid to late afternoon, and persisted into the evening. Some thunderstorms produced gusty winds over the waters. Thunderstorms initiated along a pressure trough in the lee of the Appalachian Mountains during the mid to late afternoon, and persisted into the evening. Some thunderstorms produced gusty winds over the waters. Thunderstorms initiated along a pressure trough in the lee of the Appalachian Mountains during the mid to late afternoon, and persisted into the evening. Some thunderstorms produced gusty winds over the waters. Thunderstorms initiated along a pressure trough in the lee of the Appalachian Mountains during the mid to late afternoon, and persisted into the evening. Some thunderstorms produced gusty winds over the waters. Thunderstorms initiated along a pressure trough in the lee of the Appalachian Mountains during the mid to late afternoon, and persisted into the evening. Some thunderstorms produced gusty winds over the waters.\nEvent Narrative: Wind gusts up to 36 knots were reported. Wind gusts up to 37 knots were reported. Wind gusts of 39 to 42 knots were reported. Wind gusts in excess of 30 knots were reported. Wind gusts up to 39 knots were reported. Wind gusts in excess of 30 knots were reported. Wind gusts up to 39 knots were reported. Wind gusts up to 39 knots were reported at the Stevensville Marina. Wind gusts up to 37 knots were reported.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 21.3242 km away, between 2020-06-05 17:12:00 and 2020-06-05 17:37:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A couple storms produced gusty winds due to an unstable atmosphere. A couple storms produced gusty winds due to an unstable atmosphere.\nEvent Narrative: A wind gusts in excess of 30 knots was reported.", "The following events were reported: Flood. These occurred near station USW00093721, approximately 20.835 km away, between 2020-06-05 21:50:00 and 2020-06-05 23:50:00. The flood was caused by Heavy Rain. Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: An upper-level trough and a weak cold front triggered some showers and thunderstorms. With deep moisture an a weak flow aloft, slow moving storms caused heavy rainfall that led to areas of flooding and flash flooding.\nEvent Narrative: Defense highway was closed due to high water between Huntwood Drive and St. Stephens Church Road.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 47.3212 km away, between 2020-06-10 20:52:00 and 2020-06-10 21:32:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 2500.0 and crop damage of 0.0. \n\nEpisode Narrative: A few severe thunderstorms developed during the mid afternoon to evening hours across portions of central Maryland. A few severe thunderstorms developed during the mid afternoon to evening hours across portions of central Maryland.\nEvent Narrative: A tree was blown down onto power lines in the 200 block of Wakefield Drive. A tree was blown down on Nicodemus Road between MD-27 Ridge Road and Salem Bottom Road.", "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00093721, approximately 23.4863 km away, between 2020-06-22 16:15:00 and 2020-06-22 17:25:00. The events included records with hailstones measuring 45.666666666666664 inches.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 162000.0 and crop damage of 0.0. \n\nEpisode Narrative: A weak pressure trough/surface front ignited a cluster of strong to severe thunderstorms. The storms began over eastern West Virginia during the early afternoon, then progressed eastward through central Maryland and northern Virginia, producing scattered damaging downburst wind gusts and some hail. A weak pressure trough/surface front ignited a cluster of strong to severe thunderstorms. The storms began over eastern West Virginia during the early afternoon, then progressed eastward through central Maryland and northern Virginia, producing scattered damaging downburst wind gusts and some hail. A weak pressure trough/surface front ignited a cluster of strong to severe thunderstorms. The storms began over eastern West Virginia during the early afternoon, then progressed eastward through central Maryland and northern Virginia, producing scattered damaging downburst wind gusts and some hail. A weak pressure trough/surface front ignited a cluster of strong to severe thunderstorms. The storms began over eastern West Virginia during the early afternoon, then progressed eastward through central Maryland and northern Virginia, producing scattered damaging downburst wind gusts and some hail. A weak pressure trough/surface front ignited a cluster of strong to severe thunderstorms. The storms began over eastern West Virginia during the early afternoon, then progressed eastward through central Maryland and northern Virginia, producing scattered damaging downburst wind gusts and some hail. A weak pressure trough/surface front ignited a cluster of strong to severe thunderstorms. The storms began over eastern West Virginia during the early afternoon, then progressed eastward through central Maryland and northern Virginia, producing scattered damaging downburst wind gusts and some hail. A weak pressure trough/surface front ignited a cluster of strong to severe thunderstorms. The storms began over eastern West Virginia during the early afternoon, then progressed eastward through central Maryland and northern Virginia, producing scattered damaging downburst wind gusts and some hail. A weak pressure trough/surface front ignited a cluster of strong to severe thunderstorms. The storms began over eastern West Virginia during the early afternoon, then progressed eastward through central Maryland and northern Virginia, producing scattered damaging downburst wind gusts and some hail. A weak pressure trough/surface front ignited a cluster of strong to severe thunderstorms. The storms began over eastern West Virginia during the early afternoon, then progressed eastward through central Maryland and northern Virginia, producing scattered damaging downburst wind gusts and some hail.\nEvent Narrative: A tree was blown down onto US-40 Baltimore National Pike near Turf Valley Road. A tree was blown down on westbound I-70 at US-29 Columbia Pike. A tree was blown down on northbound I-83 Baltimore-Harrisburg Expressway prior to Exit 17/West Padonia Road. A tree was reported down on MD-88 Black Rock Road near Benson Mill Road. Quarter size hail was reported in West Laurel. A tree was blown down on US-29 Columbia Pike at MD-216 Lime Kiln Road. A tree blew down onto I-695 Baltimore Beltway Outer Loop near MD-122 Security Boulevard. Numerous (dozens) of trees were blown down in and near Ellicott City. One tree fell on and destroyed a house. A tree was blown down on I-695 Baltimore Beltway near Cromwell Bridge Road.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 36.7117 km away, between 2020-06-22 16:45:00 and 2020-06-22 16:47:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A weak pressure trough/surface front ignited a cluster of strong to severe thunderstorms. The storms began over eastern West Virginia during the early afternoon, then progressed eastward into the waters producing gusty winds. A weak pressure trough/surface front ignited a cluster of strong to severe thunderstorms. The storms began over eastern West Virginia during the early afternoon, then progressed eastward into the waters producing gusty winds. A weak pressure trough/surface front ignited a cluster of strong to severe thunderstorms. The storms began over eastern West Virginia during the early afternoon, then progressed eastward into the waters producing gusty winds.\nEvent Narrative: Wind gusts in excess of 30 knots were reported.", "The following events were reported: Flood. These occurred near station USW00093721, approximately 15.3726 km away, between 2020-06-22 16:50:00 and 2020-06-22 20:22:00. The flood was caused by Heavy Rain. Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A weak boundary and unstable atmosphere led to showers and thunderstorms. Some produced heavy rain that led to flooding. A weak boundary and unstable atmosphere led to showers and thunderstorms. Some produced heavy rain that led to flooding. A weak boundary and unstable atmosphere led to showers and thunderstorms. Some produced heavy rain that led to flooding.\nEvent Narrative: The creek near the 9700 block of Riverside Circle was out of its banks and flowing across the road. The creek was out of its banks near Marshall Avenue. MD-144 River Road was closed due to flooding near Frederick Road.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 22.5733 km away, between 2020-06-23 17:50:00 and 2020-06-23 17:59:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 4000.0 and crop damage of 0.0. \n\nEpisode Narrative: A few isolated severe thunderstorms developed late in the afternoon on Tuesday, June 23rd, 2020. A few isolated severe thunderstorms developed late in the afternoon on Tuesday, June 23rd, 2020.\nEvent Narrative: A tree blew down on Osler Drive in Towson. A tree was blown down near the intersection of Greenspring Avenue and West Northern Parkway. A tree was blown down on Roland Avenue between Union Avenue and West 41st Street.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 21.4323 km away, between 2020-06-27 16:16:00 and 2020-06-27 16:16:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 2000.0 and crop damage of 0.0. \n\nEpisode Narrative: A few isolated severe thunderstorms developed near the Washington, DC, metro area during the late afternoon hours of Saturday, June 27th, 2020.\nEvent Narrative: A tree blew down onto wires at the intersection of MD-450 Defense Highway and Rutland Road.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 32.6831 km away, between 2020-06-27 16:26:00 and 2020-06-27 16:50:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: An unstable atmosphere caused a few thunderstorms with gusty winds over the waters. An unstable atmosphere caused a few thunderstorms with gusty winds over the waters. An unstable atmosphere caused a few thunderstorms with gusty winds over the waters. An unstable atmosphere caused a few thunderstorms with gusty winds over the waters. An unstable atmosphere caused a few thunderstorms with gusty winds over the waters. An unstable atmosphere caused a few thunderstorms with gusty winds over the waters.\nEvent Narrative: Wind gusts up to 48 knots were reported. Wind gusts of 36 to 44 knots were reported. A wind gust in excess of 30 knots was reported. A wind gust of 38 knots was reported at the Stevensville Marina.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 48.1162 km away, between 2020-06-27 16:38:00 and 2020-06-27 16:48:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: An upper level disturbance and associated trough of low pressure over northeast Pennsylvania and northern New Jersey, in conjunction with high dew point temperatures and instability, touched off showers and thunderstorms across the upper portions of the Eastern Shore during the late afternoon and evening hours. An upper level disturbance and associated trough of low pressure over northeast Pennsylvania and northern New Jersey, in conjunction with high dew point temperatures and instability, touched off showers and thunderstorms across the upper portions of the Eastern Shore during the late afternoon and evening hours. An upper level disturbance and associated trough of low pressure over northeast Pennsylvania and northern New Jersey, in conjunction with high dew point temperatures and instability, touched off showers and thunderstorms across the upper portions of the Eastern Shore during the late afternoon and evening hours.\nEvent Narrative: Debris on MD 446 south of Whispering Pines Lane. Time estimated from radar. Debris on MD 446 South at Whispering Pines Lane. Time estimated from radar. |Correction. Several reports of trees and power lines down along Broad Neck Road and near Island Point. Time based on utility company reports.", "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00093721, approximately 21.6903 km away, between 2020-07-01 14:33:00 and 2020-07-01 15:27:00. The events included records with hailstones measuring 9.416666666666666 inches.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 2000.0 and crop damage of 0.0. \n\nEpisode Narrative: A few intense thunderstorms developed during the afternoon hours of Wednesday, July 1st, 2020, mainly east of I-95 in central Maryland. The thunderstorms were notable mainly for the hail they produced relatively late in the season. A few intense thunderstorms developed during the afternoon hours of Wednesday, July 1st, 2020, mainly east of I-95 in central Maryland. The thunderstorms were notable mainly for the hail they produced relatively late in the season. A few intense thunderstorms developed during the afternoon hours of Wednesday, July 1st, 2020, mainly east of I-95 in central Maryland. The thunderstorms were notable mainly for the hail they produced relatively late in the season. A few intense thunderstorms developed during the afternoon hours of Wednesday, July 1st, 2020, mainly east of I-95 in central Maryland. The thunderstorms were notable mainly for the hail they produced relatively late in the season. A few intense thunderstorms developed during the afternoon hours of Wednesday, July 1st, 2020, mainly east of I-95 in central Maryland. The thunderstorms were notable mainly for the hail they produced relatively late in the season. A few intense thunderstorms developed during the afternoon hours of Wednesday, July 1st, 2020, mainly east of I-95 in central Maryland. The thunderstorms were notable mainly for the hail they produced relatively late in the season.\nEvent Narrative: Tree damage was reported in the Benfield area, including numerous large (6-inch in diameter) tree limbs that were blown down near the intersection of Governor Stone Parkway and East West Boulevard. Quarter size hail was reported near Cape Arthur. Quarter size hail was reported near Severna Park, including near the intersection of Governor Ritchie Highway and Chautaugua Road. Quarter to half dollar size hail was reported near Parole and Annapolis, including in the 500 block of Samuel Church Road. Quarter to ping pong ball size hail was reported near Paroles and Annapolis, including near the intersection of Forest Drive and MD-2 Solomons Island Road, and near the intersection of Admiral Cochrane Drive and MD-2 Solomons Island Road. Golf ball size hail was reported near Riva, including near the intersection of Riva Road and Forest Road.", "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00093721, approximately 33.4951 km away, between 2020-07-05 13:57:00 and 2020-07-05 16:12:00. The events included records with hailstones measuring 27.333333333333332 inches.The events resulted in 19 injuries and 0 fatalities. The events caused property damage valued at 110000.0 and crop damage of 0.0. \n\nEpisode Narrative: An upper-level disturbance interacting with a stalled surface front draped over Maryland produced widely scattered severe thunderstorms during the afternoon of Sunday, July 5th, 2020. An upper-level disturbance interacting with a stalled surface front draped over Maryland produced widely scattered severe thunderstorms during the afternoon of Sunday, July 5th, 2020. An upper-level disturbance interacting with a stalled surface front draped over Maryland produced widely scattered severe thunderstorms during the afternoon of Sunday, July 5th, 2020. An upper-level disturbance interacting with a stalled surface front draped over Maryland produced widely scattered severe thunderstorms during the afternoon of Sunday, July 5th, 2020. An upper-level disturbance interacting with a stalled surface front draped over Maryland produced widely scattered severe thunderstorms during the afternoon of Sunday, July 5th, 2020. An upper-level disturbance interacting with a stalled surface front draped over Maryland produced widely scattered severe thunderstorms during the afternoon of Sunday, July 5th, 2020.\nEvent Narrative: Numerous trees were blown down in Lake Ridge, including one large tree which fell on a detached garage causing it to collapse injuring 19 people (1 critically). Half dollar size hail was reported near Abingdon. Ping pong ball size hail was reported in Edgewood. A tree was blown down near the intersection of US-40 Pulaski Highway and the Otter Creek Ramp. A tree was blown down onto a vehicle at the intersection of Abingdon Road and Fereral Lane. Quarter to half dollar size hail was reported near Bowleys Quarters. A wind gust of 50 knots (58 MPH) was measured at the shore of Baltimore Harbor (near Fells Point).", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 13.9391 km away, between 2020-07-05 15:10:00 and 2020-07-05 15:54:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Several strong to severe thunderstorms traversed the western shore of the Chesapeake Bay during the afternoon hours of Sunday, July 5th, 2020. Several strong to severe thunderstorms traversed the western shore of the Chesapeake Bay during the afternoon hours of Sunday, July 5th, 2020. Several strong to severe thunderstorms traversed the western shore of the Chesapeake Bay during the afternoon hours of Sunday, July 5th, 2020. Several strong to severe thunderstorms traversed the western shore of the Chesapeake Bay during the afternoon hours of Sunday, July 5th, 2020.\nEvent Narrative: A thunderstorm produced an estimated wind gust of 34 knots (39 MPH) near Hampstead Hill Academy. Wind gusts of 39 to 50 knots (45 to 58 MPH) were measured at a buoy in Baltimore Harbor/the tidal Patapsco River. A wind gust of 37 knots (43 MPH) was measured by a mesonet at the Maryland Science Center. Multiple wind gusts of 39 knots (45 MPH) were measured at Francis Scott Key Bridge.", "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00093721, approximately 22.0821 km away, between 2020-07-06 17:15:00 and 2020-07-06 18:04:00. The events included records with hailstones measuring 49.63636363636363 inches.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 97000.0 and crop damage of 0.0. \n\nEpisode Narrative: An upper-level disturbance triggered scattered to numerous showers and thunderstorms. The very unstable lower-level air mass resulted in an environment conducive to downburst winds, some of which were significant. An upper-level disturbance triggered scattered to numerous showers and thunderstorms. The very unstable lower-level air mass resulted in an environment conducive to downburst winds, some of which were significant. An upper-level disturbance triggered scattered to numerous showers and thunderstorms. The very unstable lower-level air mass resulted in an environment conducive to downburst winds, some of which were significant. An upper-level disturbance triggered scattered to numerous showers and thunderstorms. The very unstable lower-level air mass resulted in an environment conducive to downburst winds, some of which were significant. An upper-level disturbance triggered scattered to numerous showers and thunderstorms. The very unstable lower-level air mass resulted in an environment conducive to downburst winds, some of which were significant. An upper-level disturbance triggered scattered to numerous showers and thunderstorms. The very unstable lower-level air mass resulted in an environment conducive to downburst winds, some of which were significant. An upper-level disturbance triggered scattered to numerous showers and thunderstorms. The very unstable lower-level air mass resulted in an environment conducive to downburst winds, some of which were significant. An upper-level disturbance triggered scattered to numerous showers and thunderstorms. The very unstable lower-level air mass resulted in an environment conducive to downburst winds, some of which were significant. An upper-level disturbance triggered scattered to numerous showers and thunderstorms. The very unstable lower-level air mass resulted in an environment conducive to downburst winds, some of which were significant. An upper-level disturbance triggered scattered to numerous showers and thunderstorms. The very unstable lower-level air mass resulted in an environment conducive to downburst winds, some of which were significant. An upper-level disturbance triggered scattered to numerous showers and thunderstorms. The very unstable lower-level air mass resulted in an environment conducive to downburst winds, some of which were significant.\nEvent Narrative: A tree was blown down near the intersection of northbound MD-178 Generals Highway and Indian Landing Road. A tree was blown down near the intersection of MD-176 Dorsey Road and New Ridge Road. Parts of the roof on the helicopter hangar at Martin State Regional Airport were damaged. Quarter size hail was reported near the intersection of MD-43 White Marsh Boulevard and MD-150 Eastern Boulevard. Numerous trees and wires were blown down in the 1300 to 1700 block of Wilson Point Road. A trained spotter reported a measured wind gust of 50 knots (58 MPH) near Green Haven. A tree was blown down on northbound MD-2 Solomons Island Road at MD-665 Aris T. Allen Boulevard. Numerous trees and wires blew down in the 8500 to 8700 block of US-40 Pulaski Highway. Multiple trees down in the area of 2800 Lodge Farm Road. A two foot in diameter tree was blown down near the intersection of MD-150 Eastern Boulevard and Carroll Island Road. Trees were blown down in the area of MD-197 Collington Road and US-50 John Hanson Highway.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 29.9559 km away, between 2020-07-06 17:35:00 and 2020-07-06 19:01:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Clusters of strong to severe thunderstorms produced numerous wind gusts over the tidal Potomac River and Maryland portion of the Chesapeake Bay during the early evening hours of Monday, July 6th, 2020. Clusters of strong to severe thunderstorms produced numerous wind gusts over the tidal Potomac River and Maryland portion of the Chesapeake Bay during the early evening hours of Monday, July 6th, 2020. Clusters of strong to severe thunderstorms produced numerous wind gusts over the tidal Potomac River and Maryland portion of the Chesapeake Bay during the early evening hours of Monday, July 6th, 2020. Clusters of strong to severe thunderstorms produced numerous wind gusts over the tidal Potomac River and Maryland portion of the Chesapeake Bay during the early evening hours of Monday, July 6th, 2020. Clusters of strong to severe thunderstorms produced numerous wind gusts over the tidal Potomac River and Maryland portion of the Chesapeake Bay during the early evening hours of Monday, July 6th, 2020. Clusters of strong to severe thunderstorms produced numerous wind gusts over the tidal Potomac River and Maryland portion of the Chesapeake Bay during the early evening hours of Monday, July 6th, 2020. Clusters of strong to severe thunderstorms produced numerous wind gusts over the tidal Potomac River and Maryland portion of the Chesapeake Bay during the early evening hours of Monday, July 6th, 2020. Clusters of strong to severe thunderstorms produced numerous wind gusts over the tidal Potomac River and Maryland portion of the Chesapeake Bay during the early evening hours of Monday, July 6th, 2020. Clusters of strong to severe thunderstorms produced numerous wind gusts over the tidal Potomac River and Maryland portion of the Chesapeake Bay during the early evening hours of Monday, July 6th, 2020. Clusters of strong to severe thunderstorms produced numerous wind gusts over the tidal Potomac River and Maryland portion of the Chesapeake Bay during the early evening hours of Monday, July 6th, 2020. Clusters of strong to severe thunderstorms produced numerous wind gusts over the tidal Potomac River and Maryland portion of the Chesapeake Bay during the early evening hours of Monday, July 6th, 2020. Clusters of strong to severe thunderstorms produced numerous wind gusts over the tidal Potomac River and Maryland portion of the Chesapeake Bay during the early evening hours of Monday, July 6th, 2020.\nEvent Narrative: A wind gust of 34 knots (39 MPH) was measured by a mesonet at Orioles Park at Camden Yards. A thunderstorm produced an estimated wind gust to 34 knots (39 MPH) near a buoy in Baltimore Harbor/the tidal Patapsco River. Wind gusts of 39 to 44 knots (45 to 51 MPH) were measured by a buoy near Kent Island. Wind gusts of 34 to 44 knots were measured by the AWOS at Martin State Airport. Wind gusts of 34 to 41 knots (39 to 47 MPH) were measured by a buoy near Hart Miller Island. A thunderstorm produced an estimated wind gust to 34 knots (39 MPH) near the Maryland Science Center. Wind gusts of 36 to 58 knots (41 to 67 MPH) were measured by a buoy near Tolchester Beach. A thunderstorm produced an estimated wind gust to 34 knots (39 MPH) near a buoy near Tolly Point. A wind gust of 46 knots (53 MPH) was measured by a buoy near Thomas Point. Wind gusts of 37 to 48 knots (43 to 55 MPH) were measured by a mesonet near Stevensville. A wind gust of 39 knots (45 MPH) was measured by the AWOS at Bay Bridge Airport (KW29). A wind gust of 35 knots (40 MPH) was measured by a buoy near Thomas Point.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 45.1413 km away, between 2020-07-06 18:12:00 and 2020-07-06 18:44:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A slow moving backdoor cold front drifted southwest through the mid-Atlantic region on July 6. Meanwhile, a shortwave vorticity impulse, one of several in a series, moved across the region during the day. A very hot and humid air mass was present ahead of the backdoor cold front, leading to the development of strong to extreme instability over the region. The approaching upper level disturbance allowed for the development of moderate wind shear over the region. Combined with the front, it also acted as a trigger mechanism for convection. Severe thunderstorms developed by early afternoon over eastern PA and southern and central New Jersey. These storms produced strong outflow boundaries which served to initiate additional severe convection. The result was a ring of fire in which outflow steadily propagated outward in all directions. This caused severe weather to spread radially outward from its origin near Philadelphia to much of New Jersey, other portions of eastern Pennsylvania, and Delmarva. A slow moving backdoor cold front drifted southwest through the mid-Atlantic region on July 6. Meanwhile, a shortwave vorticity impulse, one of several in a series, moved across the region during the day. A very hot and humid air mass was present ahead of the backdoor cold front, leading to the development of strong to extreme instability over the region. The approaching upper level disturbance allowed for the development of moderate wind shear over the region. Combined with the front, it also acted as a trigger mechanism for convection. Severe thunderstorms developed by early afternoon over eastern PA and southern and central New Jersey. These storms produced strong outflow boundaries which served to initiate additional severe convection. The result was a ring of fire in which outflow steadily propagated outward in all directions. This caused severe weather to spread radially outward from its origin near Philadelphia to much of New Jersey, other portions of eastern Pennsylvania, and Delmarva. A slow moving backdoor cold front drifted southwest through the mid-Atlantic region on July 6. Meanwhile, a shortwave vorticity impulse, one of several in a series, moved across the region during the day. A very hot and humid air mass was present ahead of the backdoor cold front, leading to the development of strong to extreme instability over the region. The approaching upper level disturbance allowed for the development of moderate wind shear over the region. Combined with the front, it also acted as a trigger mechanism for convection. Severe thunderstorms developed by early afternoon over eastern PA and southern and central New Jersey. These storms produced strong outflow boundaries which served to initiate additional severe convection. The result was a ring of fire in which outflow steadily propagated outward in all directions. This caused severe weather to spread radially outward from its origin near Philadelphia to much of New Jersey, other portions of eastern Pennsylvania, and Delmarva. A slow moving backdoor cold front drifted southwest through the mid-Atlantic region on July 6. Meanwhile, a shortwave vorticity impulse, one of several in a series, moved across the region during the day. A very hot and humid air mass was present ahead of the backdoor cold front, leading to the development of strong to extreme instability over the region. The approaching upper level disturbance allowed for the development of moderate wind shear over the region. Combined with the front, it also acted as a trigger mechanism for convection. Severe thunderstorms developed by early afternoon over eastern PA and southern and central New Jersey. These storms produced strong outflow boundaries which served to initiate additional severe convection. The result was a ring of fire in which outflow steadily propagated outward in all directions. This caused severe weather to spread radially outward from its origin near Philadelphia to much of New Jersey, other portions of eastern Pennsylvania, and Delmarva.\nEvent Narrative: MD-20 westbound at Bell Rose Ln was closed due to storm debris. Time estimated from radar. MD-20 westbound was closed at MD-446 due to storm debris. Time estimated from radar. MD-8 was closed at Dorchester Rd due to storm debris. Time estimated from radar. Measured at Tolchester Beach, station TCBM2.", "The following events were reported: Flash Flood, Flood. These occurred near station USW00093721, approximately 28.2148 km away, between 2020-07-06 22:00:00 and 2020-07-07 18:25:00. The flood was caused by Heavy Rain. Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A southerly flow ushered in moisture from the Gulf of Mexico and Atlantic Ocean, while a trough of low pressure remained over the region. Showers and thunderstorms developed, and with a weak flow aloft this caused locally heavy amounts of rain to fall in some locations. A southerly flow ushered in moisture from the Gulf of Mexico and Atlantic Ocean, while a trough of low pressure remained over the region. Showers and thunderstorms developed, and with a weak flow aloft this caused locally heavy amounts of rain to fall in some locations. A southerly flow ushered in moisture from the Gulf of Mexico and Atlantic Ocean, while a trough of low pressure remained over the region. Showers and thunderstorms developed, and with a weak flow aloft this caused locally heavy amounts of rain to fall in some locations.\nEvent Narrative: Pulaski Highway was closed around Rossville Boulevard. A few lanes of Interstate 95 were shut down around White Marsh Boulevard. The water rose above flood stage of 10.8 feet along the Middle River and it crested at 11.38 feet at 6:12 PM EST. Wilson Point was flooded with at least six inches of water over a portion of the road.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 36.8276 km away, between 2020-07-20 17:45:00 and 2020-07-20 18:15:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Several rounds of strong to severe thunderstorms moved from northern Virginia across the tidal Potomac River, central and southern Maryland and into the Maryland portion of the Chesapeake Bay during the afternoon and evening hours of Monday, July 20th, 2020. Several rounds of strong to severe thunderstorms moved from northern Virginia across the tidal Potomac River, central and southern Maryland and into the Maryland portion of the Chesapeake Bay during the afternoon and evening hours of Monday, July 20th, 2020. Several rounds of strong to severe thunderstorms moved from northern Virginia across the tidal Potomac River, central and southern Maryland and into the Maryland portion of the Chesapeake Bay during the afternoon and evening hours of Monday, July 20th, 2020. Several rounds of strong to severe thunderstorms moved from northern Virginia across the tidal Potomac River, central and southern Maryland and into the Maryland portion of the Chesapeake Bay during the afternoon and evening hours of Monday, July 20th, 2020. Several rounds of strong to severe thunderstorms moved from northern Virginia across the tidal Potomac River, central and southern Maryland and into the Maryland portion of the Chesapeake Bay during the afternoon and evening hours of Monday, July 20th, 2020.\nEvent Narrative: A wind gust of 37 knots (43 MPH) was measured by a mesonet near Stevensville. Wind gusts of 34 to 43 knots (39 to 49 MPH) were measured by a mesonet near Galesville. Wind gusts of 34 to 39 knots (39 to 45 MPH) were measured by a buoy near Tolly Point. Wind gusts of 34 to 39 knots (39 to 45 MPH) were measured by a buoy near Thomas Point. A thunderstorm produced an estimated wind gust to 34 knots (39 MPH) near the AWOS at Bay Bridge Airport (KW29).", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 11.2987 km away, between 2020-07-21 19:06:00 and 2020-07-21 19:06:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 3000.0 and crop damage of 0.0. \n\nEpisode Narrative: Scattered strong to severe thunderstorms developed along a stalled front draped across the Middle Atlantic, peaking during the early evening hours.\nEvent Narrative: Trees were blown down on MD-732 Dorsey Run Road near Brock Bridge Road.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 20.1088 km away, between 2020-07-22 15:03:00 and 2020-07-22 15:59:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 8000.0 and crop damage of 0.0. \n\nEpisode Narrative: An upper-level trough interacted with a stalled surface front draped over the Mid-Atlantic resulting in scattered to numerous showers and thunderstorms developing in the lee of the Appalachians Mountains as early as midday. The storms coalesced into a bow echo moved eastward across central Maryland and northern Virginia (including the DC metro) during the mid afternoon. Thunderstorms exited the area by nightfall. An upper-level trough interacted with a stalled surface front draped over the Mid-Atlantic resulting in scattered to numerous showers and thunderstorms developing in the lee of the Appalachians Mountains as early as midday. The storms coalesced into a bow echo moved eastward across central Maryland and northern Virginia (including the DC metro) during the mid afternoon. Thunderstorms exited the area by nightfall. An upper-level trough interacted with a stalled surface front draped over the Mid-Atlantic resulting in scattered to numerous showers and thunderstorms developing in the lee of the Appalachians Mountains as early as midday. The storms coalesced into a bow echo moved eastward across central Maryland and northern Virginia (including the DC metro) during the mid afternoon. Thunderstorms exited the area by nightfall. An upper-level trough interacted with a stalled surface front draped over the Mid-Atlantic resulting in scattered to numerous showers and thunderstorms developing in the lee of the Appalachians Mountains as early as midday. The storms coalesced into a bow echo moved eastward across central Maryland and northern Virginia (including the DC metro) during the mid afternoon. Thunderstorms exited the area by nightfall. An upper-level trough interacted with a stalled surface front draped over the Mid-Atlantic resulting in scattered to numerous showers and thunderstorms developing in the lee of the Appalachians Mountains as early as midday. The storms coalesced into a bow echo moved eastward across central Maryland and northern Virginia (including the DC metro) during the mid afternoon. Thunderstorms exited the area by nightfall. An upper-level trough interacted with a stalled surface front draped over the Mid-Atlantic resulting in scattered to numerous showers and thunderstorms developing in the lee of the Appalachians Mountains as early as midday. The storms coalesced into a bow echo moved eastward across central Maryland and northern Virginia (including the DC metro) during the mid afternoon. Thunderstorms exited the area by nightfall. An upper-level trough interacted with a stalled surface front draped over the Mid-Atlantic resulting in scattered to numerous showers and thunderstorms developing in the lee of the Appalachians Mountains as early as midday. The storms coalesced into a bow echo moved eastward across central Maryland and northern Virginia (including the DC metro) during the mid afternoon. Thunderstorms exited the area by nightfall.\nEvent Narrative: A tree was blown down on MD-97 Roxbury Mills Road near Cattail Creek Drive/Sycamore Valley Run. Trees were blown down on US-40 Baltimore National Pike near Turf Valley Road. A tree blew down on Gilford Road near Edenbrook Road. A tree was blown down on Cromwell Bridge Road between Loch Raven Boulevard and Cub Hill Road. A tree was blown down in the 800 block of West Lombard Street. A tree was blown down in the Perring Parkway area. A tree was blown down on Chesapeake Road.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 28.2345 km away, between 2020-07-22 15:43:00 and 2020-07-22 16:42:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Strong to severe thunderstorms coalesced into a bow echo/squall line which moved eastward across the tidal Potomac River and Maryland portion of the Chesapeake Bay during the mid afternoon hours of Wednesday, July 22nd, 2020. Strong to severe thunderstorms coalesced into a bow echo/squall line which moved eastward across the tidal Potomac River and Maryland portion of the Chesapeake Bay during the mid afternoon hours of Wednesday, July 22nd, 2020. Strong to severe thunderstorms coalesced into a bow echo/squall line which moved eastward across the tidal Potomac River and Maryland portion of the Chesapeake Bay during the mid afternoon hours of Wednesday, July 22nd, 2020. Strong to severe thunderstorms coalesced into a bow echo/squall line which moved eastward across the tidal Potomac River and Maryland portion of the Chesapeake Bay during the mid afternoon hours of Wednesday, July 22nd, 2020. Strong to severe thunderstorms coalesced into a bow echo/squall line which moved eastward across the tidal Potomac River and Maryland portion of the Chesapeake Bay during the mid afternoon hours of Wednesday, July 22nd, 2020. Strong to severe thunderstorms coalesced into a bow echo/squall line which moved eastward across the tidal Potomac River and Maryland portion of the Chesapeake Bay during the mid afternoon hours of Wednesday, July 22nd, 2020. Strong to severe thunderstorms coalesced into a bow echo/squall line which moved eastward across the tidal Potomac River and Maryland portion of the Chesapeake Bay during the mid afternoon hours of Wednesday, July 22nd, 2020. Strong to severe thunderstorms coalesced into a bow echo/squall line which moved eastward across the tidal Potomac River and Maryland portion of the Chesapeake Bay during the mid afternoon hours of Wednesday, July 22nd, 2020. Strong to severe thunderstorms coalesced into a bow echo/squall line which moved eastward across the tidal Potomac River and Maryland portion of the Chesapeake Bay during the mid afternoon hours of Wednesday, July 22nd, 2020. Strong to severe thunderstorms coalesced into a bow echo/squall line which moved eastward across the tidal Potomac River and Maryland portion of the Chesapeake Bay during the mid afternoon hours of Wednesday, July 22nd, 2020. Strong to severe thunderstorms coalesced into a bow echo/squall line which moved eastward across the tidal Potomac River and Maryland portion of the Chesapeake Bay during the mid afternoon hours of Wednesday, July 22nd, 2020. Strong to severe thunderstorms coalesced into a bow echo/squall line which moved eastward across the tidal Potomac River and Maryland portion of the Chesapeake Bay during the mid afternoon hours of Wednesday, July 22nd, 2020. Strong to severe thunderstorms coalesced into a bow echo/squall line which moved eastward across the tidal Potomac River and Maryland portion of the Chesapeake Bay during the mid afternoon hours of Wednesday, July 22nd, 2020.\nEvent Narrative: Wind gusts of 35 to 40 knots (40 to 46 MPH) were measured at a buoy near Greenbury Point. Wind gusts of 34 to 41 knots (39 to 47 MPH) were measured by a buoy near Tolly Point. A wind gust of 36 knots (41 MPH) was measured by the ASOS at the Annapolis Naval Academy (KNAK). Wind gusts of 34 to 36 knots (39 to 41 MPH) were measured by a buoy near Sandy Point. Wind gusts of 34 to 42 knots (39 to 48 MPH) were measured by a buoy near the mouth of the Gunpowder River. Wind gusts of 34 knots (39 MPH) were measured by a buoy in Baltimore Harbor/the tidal Patapsco River. Wind gusts of 37 to 42 knots (43 to 48 MPH) were measured by a buoy near Thomas Point. Wind gusts of 34 to 47 knots (39 to 54 MPH) were measured at Francis Scott Key Bridge. Wind gusts of 39 to 47 knots (45 to 54 MPH) were measured by a buoy near Hart Miller Island. Wind gusts of 34 to 48 knots (39 to 55 MPH) were measured by a buoy near Tolchester Beach. A thunderstorm produced an estimated wind gust to 34 knots (39 MPH) near Saint Mary's Elementary School. A wind gust of 35 knots (40 MPH) was measured by a mesonet at Orioles Park at Camden Yards. A wind gust of 35 knots (40 MPH) was measured by a mesonet near Stevensville.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 43.1031 km away, between 2020-07-22 16:30:00 and 2020-07-22 16:37:00. The events included records with estimated wind gusts of 51.666666666666664 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A slow moving frontal boundary was draped across upstate New York and southern New England on July 22 with multiple waves of low pressure tracking along it. The mid-Atlantic was left in a warm sector air mass south of this front. This led to a very hot and humid day on July 22 with air temperatures rising into the 90s and dew point values near 70. This caused strong instability to develop. Shear values were not overly impressive, but an approaching shortwave disturbance from the Midwest did help to increase shear late in the day. This disturbance also served as forcing for convection to develop in the warm and unstable air mass. Widespread thunderstorm development occurred, with storms eventually developing into a mostly solid squall line. This line of storms produced numerous reports of wind damage across eastern Pennsylvania, New Jersey, and Delmarva. A slow moving frontal boundary was draped across upstate New York and southern New England on July 22 with multiple waves of low pressure tracking along it. The mid-Atlantic was left in a warm sector air mass south of this front. This led to a very hot and humid day on July 22 with air temperatures rising into the 90s and dew point values near 70. This caused strong instability to develop. Shear values were not overly impressive, but an approaching shortwave disturbance from the Midwest did help to increase shear late in the day. This disturbance also served as forcing for convection to develop in the warm and unstable air mass. Widespread thunderstorm development occurred, with storms eventually developing into a mostly solid squall line. This line of storms produced numerous reports of wind damage across eastern Pennsylvania, New Jersey, and Delmarva. A slow moving frontal boundary was draped across upstate New York and southern New England on July 22 with multiple waves of low pressure tracking along it. The mid-Atlantic was left in a warm sector air mass south of this front. This led to a very hot and humid day on July 22 with air temperatures rising into the 90s and dew point values near 70. This caused strong instability to develop. Shear values were not overly impressive, but an approaching shortwave disturbance from the Midwest did help to increase shear late in the day. This disturbance also served as forcing for convection to develop in the warm and unstable air mass. Widespread thunderstorm development occurred, with storms eventually developing into a mostly solid squall line. This line of storms produced numerous reports of wind damage across eastern Pennsylvania, New Jersey, and Delmarva.\nEvent Narrative: A large tree was reported down. Report via social media with a photo. Time estimated from radar. A downed utility was reported on MD-21 between Caulks Field Rd and Bay Shore Rd. Time estimated from radar. Several reports of downed trees and power lines in the area of Johnstown Rd and Quaker Neck Rd in Chestertown. Utility companies reported widespread power outages in the area. Time estimated from radar.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 33.3937 km away, between 2020-07-23 20:43:00 and 2020-07-23 21:00:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Scattered strong thunderstorms produced gusty winds over the tidal Potomac River and upper Chesapeake Bay. Scattered strong thunderstorms produced gusty winds over the tidal Potomac River and upper Chesapeake Bay. Scattered strong thunderstorms produced gusty winds over the tidal Potomac River and upper Chesapeake Bay.\nEvent Narrative: A gust front produced estimated wind gusts to 34 knots (39 MPH) near a buoy near Tolly Point. A gust front produced estimated wind gusts to 34 knots (39 MPH) near a buoy near Greenbury Point. A wind gust of 35 knots (39 MPH) was measured at a buoy near Thomas Point.", "The following events were reported: Flash Flood. These occurred near station USW00093721, approximately 18.7124 km away, between 2020-07-24 17:14:00 and 2020-07-24 19:30:00.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 160000.0 and crop damage of 0.0. \n\nEpisode Narrative: A hot and humid airmass along with a slow moving boundary led to some showers and thunderstorms. Weak winds aloft caused storms to move slowly, and this led to some instances of flooding and flash flooding. A hot and humid airmass along with a slow moving boundary led to some showers and thunderstorms. Weak winds aloft caused storms to move slowly, and this led to some instances of flooding and flash flooding. A hot and humid airmass along with a slow moving boundary led to some showers and thunderstorms. Weak winds aloft caused storms to move slowly, and this led to some instances of flooding and flash flooding. A hot and humid airmass along with a slow moving boundary led to some showers and thunderstorms. Weak winds aloft caused storms to move slowly, and this led to some instances of flooding and flash flooding. A hot and humid airmass along with a slow moving boundary led to some showers and thunderstorms. Weak winds aloft caused storms to move slowly, and this led to some instances of flooding and flash flooding. A hot and humid airmass along with a slow moving boundary led to some showers and thunderstorms. Weak winds aloft caused storms to move slowly, and this led to some instances of flooding and flash flooding.\nEvent Narrative: Heavy rainfall led to flooding that resulted in three water rescues in the Fells Point area. Multiple vehicles were trapped in water near the intersection of US Route 40 (Pulaski Highway) and East Monument Street. The water was two-thirds of the way up the vehicles. Two vehicles were stranded in high water on the ramp from Interstate 95 northbound toward Moravia Road northbound. The water level rose above flood stage of 10 feet along the Minebank Run at Glen Arm, and it crested at 10.16 feet at 5:20 PM EST. Water covered the access road to Talmar. Five water rescues in the vicinity of Kane Street. Many roads were flooded in the western part of Baltimore City. A vehicle was trapped in high water on Hilton Parkway.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 26.6215 km away, between 2020-07-24 17:16:00 and 2020-07-24 17:16:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 5000.0 and crop damage of 0.0. \n\nEpisode Narrative: A few isolated severe thunderstorms developed over central Virginia and near Baltimore.\nEvent Narrative: Trees and wires were blown down in the Parkville area, including on Old Harford Road.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 14.0067 km away, between 2020-07-24 17:30:00 and 2020-07-24 17:30:00. The events included records with estimated wind gusts of 34.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: An isolated strong thunderstorm produced gusty winds of Baltimore Harbor/the tidal Patapsco River.\nEvent Narrative: A thunderstorm produced an estimated wind gust up to 34 knots (39 MPH) near a buoy in Baltimore Harbor/the tidal Patapsco River.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 26.512 km away, between 2020-07-30 19:18:00 and 2020-07-30 20:23:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Scattered strong to severe thunderstorms moved across northern Virginia into the tidal Potomac River, then across central and southern Maryland into the Chesapeake Bay. Scattered strong to severe thunderstorms moved across northern Virginia into the tidal Potomac River, then across central and southern Maryland into the Chesapeake Bay. Scattered strong to severe thunderstorms moved across northern Virginia into the tidal Potomac River, then across central and southern Maryland into the Chesapeake Bay. Scattered strong to severe thunderstorms moved across northern Virginia into the tidal Potomac River, then across central and southern Maryland into the Chesapeake Bay. Scattered strong to severe thunderstorms moved across northern Virginia into the tidal Potomac River, then across central and southern Maryland into the Chesapeake Bay. Scattered strong to severe thunderstorms moved across northern Virginia into the tidal Potomac River, then across central and southern Maryland into the Chesapeake Bay. Scattered strong to severe thunderstorms moved across northern Virginia into the tidal Potomac River, then across central and southern Maryland into the Chesapeake Bay. Scattered strong to severe thunderstorms moved across northern Virginia into the tidal Potomac River, then across central and southern Maryland into the Chesapeake Bay. Scattered strong to severe thunderstorms moved across northern Virginia into the tidal Potomac River, then across central and southern Maryland into the Chesapeake Bay. Scattered strong to severe thunderstorms moved across northern Virginia into the tidal Potomac River, then across central and southern Maryland into the Chesapeake Bay. Scattered strong to severe thunderstorms moved across northern Virginia into the tidal Potomac River, then across central and southern Maryland into the Chesapeake Bay. Scattered strong to severe thunderstorms moved across northern Virginia into the tidal Potomac River, then across central and southern Maryland into the Chesapeake Bay. Scattered strong to severe thunderstorms moved across northern Virginia into the tidal Potomac River, then across central and southern Maryland into the Chesapeake Bay. Scattered strong to severe thunderstorms moved across northern Virginia into the tidal Potomac River, then across central and southern Maryland into the Chesapeake Bay. Scattered strong to severe thunderstorms moved across northern Virginia into the tidal Potomac River, then across central and southern Maryland into the Chesapeake Bay. Scattered strong to severe thunderstorms moved across northern Virginia into the tidal Potomac River, then across central and southern Maryland into the Chesapeake Bay.\nEvent Narrative: Wind gusts of 34 to 46 knots (39 to 53 MPH) were measured by a buoy near the mouth of Gunpowder River. Wind gusts of 39 to 46 knots (45 to 53 MPH) were measured by a buoy near Tolly Point. Wind gusts of 34 to 48 knots (39 to 55 MPH) were measured by a buoy near Greenbury Point. Wind gusts of 34 to 35 knots (39 to 40 MPH) were measured by a buoy near Annapolis. A wind gust of 35 knots (40 MPH) was measured by the ASOS at the Annapolis Naval Academy (KNAK). Wind gusts of 34 to 41 knots (39 to 47 MPH) were measured by a buoy near Sandy Point. A thunderstorm produced an estimated wind gust to 34 knots (39 MPH) near a mesonet near Stevensville. A wind gust of 34 knots (39 MPH) was measured by a mesonet at Saint Mary's Elementary School. A thunderstorm produced an estimated wind gust to 34 knots (39 MPH) near a buoy near Thomas Point. A wind gust to 35 knots (40 MPH) was measured by a mesonet at Orioles Park at Camden Yards. A wind gust of 37 knots (43 MPH) was measured by a mesonet at Hampstead Hill Academy. Wind gusts of 37 to 46 knots (43 to 53 MPH) were measured by a buoy near Hart Miller Island. A thunderstorm produced an estimated wind gust to 34 knots (39 MPH) near a buoy near Baltimore Harbor/the tidal Patapsco River. A thunderstorm produced an estimated wind gust to 34 knots (39 MPH) near a buoy near Francis Scott Key Bridge. A wind gust of 36 knots (41 MPH) was measured by a mesonet at the Maryland Science Center. Wind gusts of 39 to 41 knots (45 to 47 MPH) were measured by a buoy near Tolchester Beach.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 48.5139 km away, between 2020-07-30 20:02:00 and 2020-07-30 20:02:00. The events included records with estimated wind gusts of 55.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A stalled frontal boundary was draped in the area of southern New Jersey and Delmarva on July 30. Meanwhile, another cold front was approaching the region from the northwest. A warm and very humid air mass developed ahead of this second front, leading to the development of moderate to strong instability over much of the mid-Atlantic. The approach of the front also gradually increased wind shear values, though greater shear remained further north over New York and New England. Nonetheless, frontal forcing in the unstable air mass was sufficient to trigger scattered thunderstorms, some of which became strong to severe and produced a number of reports of damaging winds.\nEvent Narrative: Multiple downed trees blocked Hainesville Rd near Worton. Time estimated from radar.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 30.6542 km away, between 2020-07-31 19:33:00 and 2020-07-31 20:40:00. The events included records with estimated wind gusts of 51.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 26000.0 and crop damage of 0.0. \n\nEpisode Narrative: A stalled front ignited scattered strong to severe thunderstorms across east-central Virginia into central/southern Maryland. A stalled front ignited scattered strong to severe thunderstorms across east-central Virginia into central/southern Maryland. A stalled front ignited scattered strong to severe thunderstorms across east-central Virginia into central/southern Maryland. A stalled front ignited scattered strong to severe thunderstorms across east-central Virginia into central/southern Maryland. A stalled front ignited scattered strong to severe thunderstorms across east-central Virginia into central/southern Maryland.\nEvent Narrative: Trees were blown down near the intersection of MD-953 Glenn Dale Road and Old Pond Drive, and near the intersection of MD-424 Davidsonville Road and Gernster Road. A tree blew down in the 5600 block of Cryslar Avenue. A tree blew down on Wabash Avenue. Trees were blown down near Joppatowne and Edgewood, including on Shore Drive and Nuttal Avenue. A tree was blown down on Whitaker Mill Road at West Ring Factory Road. Tree limbs were blown down along Shelburne Road. A tree blew down on MD-152 Mountain Road at Old Joppa Road. A tree blew down on Stockton Road at MD-152 Mountain Road. Trees were blown down near Bel Air and Churchville, including on Blue Silver Road and on Thomas Run Road. A tree blew down on Moores Mill Road. Trees blew down on southbound MD-24 Veterans Memorial Highway near Plumtree Road.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 33.3937 km away, between 2020-08-03 15:15:00 and 2020-08-03 15:28:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A band of showers and thunderstorms well ahead of Tropical Cyclone Isaias produce gusty winds over the tidal Potomac River and portions of the Chesapeake Bay. A band of showers and thunderstorms well ahead of Tropical Cyclone Isaias produce gusty winds over the tidal Potomac River and portions of the Chesapeake Bay. A band of showers and thunderstorms well ahead of Tropical Cyclone Isaias produce gusty winds over the tidal Potomac River and portions of the Chesapeake Bay.\nEvent Narrative: A wind gust of 34 knots (39 MPH) was measured by a buoy near Tolly Point. A thunderstorm produced an estimated wind gust to 34 knots (39 MPH) near a buoy near Greenbury Point. A wind gusts of 34 knots (39 MPH) was measured by a buoy near Thomas Point.", "The following events were reported: Flash Flood. These occurred near station USW00093721, approximately 39.7069 km away, between 2020-08-04 07:25:00 and 2020-08-04 09:00:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Tropical Storm Isaias brought high winds, heavy rain, several tornadoes, and coastal flooding to the mid-Atlantic region, becoming the most impactful tropical cyclone to impact most of the region since Sandy in 2012.\nEvent Narrative: Sections of MD Route 18 in Chester were closed due to flooding.", "The following events were reported: Flash Flood, Flood. These occurred near station USW00093721, approximately 24.1233 km away, between 2020-08-04 09:00:00 and 2020-08-05 07:21:00. The flood was caused by Heavy Rain. Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Tropical Storm Isaias moved up the east coast, passing through southern Maryland on the morning of Tuesday, August 4th, 2020, spawning several tornadoes as well as flooding rain and tropical storm force winds. ||Storm total rainfall ranged from 2 to 4 inches near Interstate 95 to as much as 9 inches in Calvert County east of Interstate 95. The heavy rain led to numerous incidents of flooding and flash flooding, especially near and east of Interstate 95. ||The highest sustained wind of 46 knots was reported at Bishops Head and the highest peak gust of 63 knots was also reported at Bishops Head. ||There were three tornadoes associated with Isaias over southern Maryland and there were also numerous reports of downed trees from tropical storm force winds, especially near and east of Interstate 95. ||A storm surge of 1 to 2 feet occurred along the western shore of the Chesapeake Bay and the shore of the Tidal Potomac River. This did result in minor tidal Flooding in Washington DC. Tropical Storm Isaias moved up the east coast, passing through southern Maryland on the morning of Tuesday, August 4th, 2020, spawning several tornadoes as well as flooding rain and tropical storm force winds. ||Storm total rainfall ranged from 2 to 4 inches near Interstate 95 to as much as 9 inches in Calvert County east of Interstate 95. The heavy rain led to numerous incidents of flooding and flash flooding, especially near and east of Interstate 95. ||The highest sustained wind of 46 knots was reported at Bishops Head and the highest peak gust of 63 knots was also reported at Bishops Head. ||There were three tornadoes associated with Isaias over southern Maryland and there were also numerous reports of downed trees from tropical storm force winds, especially near and east of Interstate 95. ||A storm surge of 1 to 2 feet occurred along the western shore of the Chesapeake Bay and the shore of the Tidal Potomac River. This did result in minor tidal Flooding in Washington DC. Tropical Storm Isaias moved up the east coast, passing through southern Maryland on the morning of Tuesday, August 4th, 2020, spawning several tornadoes as well as flooding rain and tropical storm force winds. ||Storm total rainfall ranged from 2 to 4 inches near Interstate 95 to as much as 9 inches in Calvert County east of Interstate 95. The heavy rain led to numerous incidents of flooding and flash flooding, especially near and east of Interstate 95. ||The highest sustained wind of 46 knots was reported at Bishops Head and the highest peak gust of 63 knots was also reported at Bishops Head. ||There were three tornadoes associated with Isaias over southern Maryland and there were also numerous reports of downed trees from tropical storm force winds, especially near and east of Interstate 95. ||A storm surge of 1 to 2 feet occurred along the western shore of the Chesapeake Bay and the shore of the Tidal Potomac River. This did result in minor tidal Flooding in Washington DC. Tropical Storm Isaias moved up the east coast, passing through southern Maryland on the morning of Tuesday, August 4th, 2020, spawning several tornadoes as well as flooding rain and tropical storm force winds. ||Storm total rainfall ranged from 2 to 4 inches near Interstate 95 to as much as 9 inches in Calvert County east of Interstate 95. The heavy rain led to numerous incidents of flooding and flash flooding, especially near and east of Interstate 95. ||The highest sustained wind of 46 knots was reported at Bishops Head and the highest peak gust of 63 knots was also reported at Bishops Head. ||There were three tornadoes associated with Isaias over southern Maryland and there were also numerous reports of downed trees from tropical storm force winds, especially near and east of Interstate 95. ||A storm surge of 1 to 2 feet occurred along the western shore of the Chesapeake Bay and the shore of the Tidal Potomac River. This did result in minor tidal Flooding in Washington DC. Tropical Storm Isaias moved up the east coast, passing through southern Maryland on the morning of Tuesday, August 4th, 2020, spawning several tornadoes as well as flooding rain and tropical storm force winds. ||Storm total rainfall ranged from 2 to 4 inches near Interstate 95 to as much as 9 inches in Calvert County east of Interstate 95. The heavy rain led to numerous incidents of flooding and flash flooding, especially near and east of Interstate 95. ||The highest sustained wind of 46 knots was reported at Bishops Head and the highest peak gust of 63 knots was also reported at Bishops Head. ||There were three tornadoes associated with Isaias over southern Maryland and there were also numerous reports of downed trees from tropical storm force winds, especially near and east of Interstate 95. ||A storm surge of 1 to 2 feet occurred along the western shore of the Chesapeake Bay and the shore of the Tidal Potomac River. This did result in minor tidal Flooding in Washington DC. Tropical Storm Isaias moved up the east coast, passing through southern Maryland on the morning of Tuesday, August 4th, 2020, spawning several tornadoes as well as flooding rain and tropical storm force winds. ||Storm total rainfall ranged from 2 to 4 inches near Interstate 95 to as much as 9 inches in Calvert County east of Interstate 95. The heavy rain led to numerous incidents of flooding and flash flooding, especially near and east of Interstate 95. ||The highest sustained wind of 46 knots was reported at Bishops Head and the highest peak gust of 63 knots was also reported at Bishops Head. ||There were three tornadoes associated with Isaias over southern Maryland and there were also numerous reports of downed trees from tropical storm force winds, especially near and east of Interstate 95. ||A storm surge of 1 to 2 feet occurred along the western shore of the Chesapeake Bay and the shore of the Tidal Potomac River. This did result in minor tidal Flooding in Washington DC. Tropical Storm Isaias moved up the east coast, passing through southern Maryland on the morning of Tuesday, August 4th, 2020, spawning several tornadoes as well as flooding rain and tropical storm force winds. ||Storm total rainfall ranged from 2 to 4 inches near Interstate 95 to as much as 9 inches in Calvert County east of Interstate 95. The heavy rain led to numerous incidents of flooding and flash flooding, especially near and east of Interstate 95. ||The highest sustained wind of 46 knots was reported at Bishops Head and the highest peak gust of 63 knots was also reported at Bishops Head. ||There were three tornadoes associated with Isaias over southern Maryland and there were also numerous reports of downed trees from tropical storm force winds, especially near and east of Interstate 95. ||A storm surge of 1 to 2 feet occurred along the western shore of the Chesapeake Bay and the shore of the Tidal Potomac River. This did result in minor tidal Flooding in Washington DC. Tropical Storm Isaias moved up the east coast, passing through southern Maryland on the morning of Tuesday, August 4th, 2020, spawning several tornadoes as well as flooding rain and tropical storm force winds. ||Storm total rainfall ranged from 2 to 4 inches near Interstate 95 to as much as 9 inches in Calvert County east of Interstate 95. The heavy rain led to numerous incidents of flooding and flash flooding, especially near and east of Interstate 95. ||The highest sustained wind of 46 knots was reported at Bishops Head and the highest peak gust of 63 knots was also reported at Bishops Head. ||There were three tornadoes associated with Isaias over southern Maryland and there were also numerous reports of downed trees from tropical storm force winds, especially near and east of Interstate 95. ||A storm surge of 1 to 2 feet occurred along the western shore of the Chesapeake Bay and the shore of the Tidal Potomac River. This did result in minor tidal Flooding in Washington DC.\nEvent Narrative: Multiple roads were closed because the Back River was out of its banks. The water level rapidly rose above flood stage along the Otter Point Creek at Edgewood. The water level crested at 8.67 feet at 10:01 AM August 4th. Winter Run Road was flooded near Singer Road. The water rapidly rose above flood stage along the Whitemarsh Run in Whitemarsh. The water crested at 13.02 feet at 10:25 AM EST on August 4th. The Town Center Court was flooded. MD-214 closed due to flooding near Beards Creek. Furnace Ave. closed due to flooding at the Howard/Anne Arundel County line. The river gage on the Western Branch Patuxent River near Upper Marlboro, MD exceeded the 11 foot flood stage during the indicated period. Much of Race Track Rd. flooded between Marlboro Pike and the community center. The peak level of 13.04 feet occurred at 8:15 PM on the 4th. Maryland Route 695 was closed due to high water near Belclare Road. Maryland Route 7 was closed near Mohrs Lane due to high water.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 19.607 km away, between 2020-08-04 19:54:00 and 2020-08-04 22:04:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Several gusty showers and thunderstorms in the wake of Tropical Cyclone Isaias brought strong winds to near the upper Chesapeake Bay and upper tidal Potomac River. Several gusty showers and thunderstorms in the wake of Tropical Cyclone Isaias brought strong winds to near the upper Chesapeake Bay and upper tidal Potomac River.\nEvent Narrative: A wind gust of 35 knots (40 MPH) was measured by a mesonet on the tidal Magothy River. A thunderstorm produced an estimated wind gust to 34 knots (39 MPH) near a mesonet on the tidal Magothy River.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 16.1084 km away, between 2020-08-06 03:37:00 and 2020-08-06 04:10:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 7000.0 and crop damage of 0.0. \n\nEpisode Narrative: A slow-moving warm front sparked multiple rounds of isolated severe thunderstorms across the Middle Atlantic on Thursday, August 6th, 2020. The first moved through the greater DC metro area during the early morning hours. The second was a supercell that moved across the southern Shenandoah River Valley and central Virginia Piedmont, causing significant damage and unusually large hail for so late in the season. A slow-moving warm front sparked multiple rounds of isolated severe thunderstorms across the Middle Atlantic on Thursday, August 6th, 2020. The first moved through the greater DC metro area during the early morning hours. The second was a supercell that moved across the southern Shenandoah River Valley and central Virginia Piedmont, causing significant damage and unusually large hail for so late in the season. A slow-moving warm front sparked multiple rounds of isolated severe thunderstorms across the Middle Atlantic on Thursday, August 6th, 2020. The first moved through the greater DC metro area during the early morning hours. The second was a supercell that moved across the southern Shenandoah River Valley and central Virginia Piedmont, causing significant damage and unusually large hail for so late in the season.\nEvent Narrative: Waugh Chapel Road was closed due to trees blown into the roadway between Seneca Drive and Strawberry Lake Way. Trees were blown down on MD-175 Annapolis Road between Gambrills Road/Dairy Lane and Claffy Avenue. A tree was blown down on MD-2 Solomons Island Road just north of US-50 John Hanson Highway.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 34.5876 km away, between 2020-08-06 04:33:00 and 2020-08-06 04:48:00. The events included records with measured wind gusts of 35.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A few strong storms developed during the early morning hours of Thursday, August 6th, 2020, and moved over the central Chesapeake Bay along a warm front. A few strong storms developed during the early morning hours of Thursday, August 6th, 2020, and moved over the central Chesapeake Bay along a warm front.\nEvent Narrative: A wind gust of 35 knots (40 MPH) was measured by a buoy near Hart Miller Island. A wind gust of 35 knots (40 MPH) was measured by a buoy near Tolchester Beach.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 41.5463 km away, between 2020-08-06 04:45:00 and 2020-08-06 04:50:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: An impulse moving along a stalled boundary draped across the region, in combination with moisture left over from Hurricane Isaias, produced severe thunderstorms with damaging winds and flooding rains over the eastern shore of Maryland during the early morning hours of August 6th. An impulse moving along a stalled boundary draped across the region, in combination with moisture left over from Hurricane Isaias, produced severe thunderstorms with damaging winds and flooding rains over the eastern shore of Maryland during the early morning hours of August 6th.\nEvent Narrative: Several reports of downed trees and wires in Rock Hall. Time estimated from radar. Several reports of downed power lines in the Fairlee area. Time estimated from radar.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 42.7123 km away, between 2020-08-07 17:12:00 and 2020-08-07 17:18:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 10000.0 and crop damage of 0.0. \n\nEpisode Narrative: Isolated severe thunderstorms developed along a stalled front over portions of northern Maryland and eastern West Virginia, with other isolated storms over the southern Shenandoah Valley along a pressure trough. Isolated severe thunderstorms developed along a stalled front over portions of northern Maryland and eastern West Virginia, with other isolated storms over the southern Shenandoah Valley along a pressure trough. Isolated severe thunderstorms developed along a stalled front over portions of northern Maryland and eastern West Virginia, with other isolated storms over the southern Shenandoah Valley along a pressure trough. Isolated severe thunderstorms developed along a stalled front over portions of northern Maryland and eastern West Virginia, with other isolated storms over the southern Shenandoah Valley along a pressure trough.\nEvent Narrative: A tree was blown down in the 1100 block of Clayton Road. Tree limbs and power lines were blown down in the 300 block of Regina Drive. A tree blew down onto wires in the unit block of Chesapeake Court. A large tree was blown down on Park Forrest Lane. Trees were blown down on US-1 Belair Road near New Cut Road. Trees blew down on MD-152 Fallston Road near Connoly Road. A tree was blown down across the roadway near the intersection of Singer Road and Winters Run Road.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 33.7637 km away, between 2020-08-07 17:38:00 and 2020-08-07 19:29:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A couple isolated gusty thunderstorms moved near the tidal Potomac River and Maryland portion of the Chesapeake Bay. A couple isolated gusty thunderstorms moved near the tidal Potomac River and Maryland portion of the Chesapeake Bay.\nEvent Narrative: Wind gusts of 34 to 37 knots (39 to 43 MPH) were measured by a buoy near the mouth of the Gunpowder River. A thunderstorm produced an estimated wind gust to 34 knots (39 MPH) near a buoy near Tolly Point.", "The following events were reported: Flash Flood. These occurred near station USW00093721, approximately 41.5744 km away, between 2020-08-07 18:45:00 and 2020-08-07 20:25:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A nearly stationary boundary remained overhead while an upper-level disturbance passed through the area. Showers and thunderstorms developed, and storms were slow to move which meant heavy amounts of rain fell in short periods of time, resulting in areas of flash flooding and flooding. A nearly stationary boundary remained overhead while an upper-level disturbance passed through the area. Showers and thunderstorms developed, and storms were slow to move which meant heavy amounts of rain fell in short periods of time, resulting in areas of flash flooding and flooding.\nEvent Narrative: US-40 Pulaski Highway was closed in both directions at Little Gunpowder Falls due to flooding. The water level rapidly rose above flood stage along the Otter Point Creek at Edgewood. The water level crested at 9.54 feet at 7:45 PM EST on August 8th. Winter Run Road was flooded near Singer Road.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 29.2272 km away, between 2020-08-11 16:45:00 and 2020-08-11 18:10:00. The events included records with measured wind gusts of 36.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: An isolated thunderstorm produced gust winds near and over the upper Chesapeake Bay. An isolated thunderstorm produced gust winds near and over the upper Chesapeake Bay.\nEvent Narrative: A mesonet maintained by the Maryland State Highway Administration near the upper Chesapeake Bay measured wind gusts of 34 knots (39 MPH). A mesonet maintained by the Maryland State Highway Administration near the upper Chesapeake Bay measured wind gusts of 34 to 38 knots (39 to 44 MPH).", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 11.1518 km away, between 2020-08-12 16:17:00 and 2020-08-12 16:52:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 8000.0 and crop damage of 0.0. \n\nEpisode Narrative: A few thunderstorms with damaging downbursts developed over central Maryland and northern Virginia. A few thunderstorms with damaging downbursts developed over central Maryland and northern Virginia. A few thunderstorms with damaging downbursts developed over central Maryland and northern Virginia.\nEvent Narrative: A tree blew down on Kintop Road near Eleanore Drive. Trees blew down onto power lines near the intersection of Beechwood Road and Bonnie Branch Road. A tree blew down on MD-144 Frederick Road near Oella Avenue. A tree blew down onto wires near the intersection of Kernan Drive and Dogwood Road.", "The following events were reported: Flash Flood, Flood. These occurred near station USW00093721, approximately 10.249 km away, between 2020-08-12 17:02:00 and 2020-08-12 19:50:00. The flood was caused by Heavy Rain. Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Showers and thunderstorms developed, and with little steering flow aloft this caused the storm motion to be slow. The slow storm motion resulted in instances of flooding and flash flooding. Showers and thunderstorms developed, and with little steering flow aloft this caused the storm motion to be slow. The slow storm motion resulted in instances of flooding and flash flooding. Showers and thunderstorms developed, and with little steering flow aloft this caused the storm motion to be slow. The slow storm motion resulted in instances of flooding and flash flooding. Showers and thunderstorms developed, and with little steering flow aloft this caused the storm motion to be slow. The slow storm motion resulted in instances of flooding and flash flooding. Showers and thunderstorms developed, and with little steering flow aloft this caused the storm motion to be slow. The slow storm motion resulted in instances of flooding and flash flooding. Showers and thunderstorms developed, and with little steering flow aloft this caused the storm motion to be slow. The slow storm motion resulted in instances of flooding and flash flooding. Showers and thunderstorms developed, and with little steering flow aloft this caused the storm motion to be slow. The slow storm motion resulted in instances of flooding and flash flooding. Showers and thunderstorms developed, and with little steering flow aloft this caused the storm motion to be slow. The slow storm motion resulted in instances of flooding and flash flooding. Showers and thunderstorms developed, and with little steering flow aloft this caused the storm motion to be slow. The slow storm motion resulted in instances of flooding and flash flooding. Showers and thunderstorms developed, and with little steering flow aloft this caused the storm motion to be slow. The slow storm motion resulted in instances of flooding and flash flooding. Showers and thunderstorms developed, and with little steering flow aloft this caused the storm motion to be slow. The slow storm motion resulted in instances of flooding and flash flooding. Showers and thunderstorms developed, and with little steering flow aloft this caused the storm motion to be slow. The slow storm motion resulted in instances of flooding and flash flooding. Showers and thunderstorms developed, and with little steering flow aloft this caused the storm motion to be slow. The slow storm motion resulted in instances of flooding and flash flooding.\nEvent Narrative: Maryland 648 was flooded and closed at Muddy Bridge Branch near Interstate 97. Dorsey Road was inundated and impassable near BWI Airport. The 21000 Block of Frederick Road was flooded and impassable. Rapidly flowing water was flowing down Westchester Avenue near Ellicott City on the Baltimore County Side. Hammonds Ferry Road was flooded between Ridge Avenue and Hazel Avenue. A vehicle was trapped in floodwaters on Dogwood Road at Dogwood Run. The water level along the East Branch Herbert Run in Arbutus rapidly rose above flood stage, cresting at 8.35 feet at 5:30 PM EST on August 12th. Water covered yards around Tom Day Boulevard and it approached structures along the creek. The water level rapidly rose above flood stage along the Patapsco River at Elkridge. The water level crested at 16.2 feet at 6:15 PM EST on the 12th of August. Water covered a portion of River Road in the Patapsco Valley State Park. A large portion of the park was also flooded near the playground off Gunn Road. The water level rapidly rose above flood stage along the Patapsco River at Elkridge (ELKM2). The water level crested at 18.7 feet at 6:30 PM EST on the 12th of August. Hammonds Ferry Road was flooded and backwater flooding also led to the closure of Furnace Avenue in Elkridge. ||The water level remained above flood stage until 10:24 PM EST on August 12th. Floodwaters up over the hoods of some parked cars near West St. and Leadenhall St. Vehicle in flood waters near the intersection of Baltimore National Pike and North Rolling Rd. Urban/Poor Drainage Flooding in Federal Hill. Vehicle in flood water near the intersection of Myrtle Ave. and Tulip Ave.", "The following events were reported: Flash Flood. These occurred near station USW00093721, approximately 42.4614 km away, between 2020-08-13 09:50:00 and 2020-08-13 12:00:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Thunderstorms brought locally heavy rain to northeastern Maryland on August 13. Rainfall totals were as high as 2 to 3.5 inches. Thunderstorms brought locally heavy rain to northeastern Maryland on August 13. Rainfall totals were as high as 2 to 3.5 inches. Thunderstorms brought locally heavy rain to northeastern Maryland on August 13. Rainfall totals were as high as 2 to 3.5 inches.\nEvent Narrative: Main Street in Stevensville was closed east of Duke Street due to flooding. MD Route 18 was closed at Grasonville Cemetery Road in Grasonville due to flooding. MD Route 18 was closed at Piney Creek Road in Chester due to flooding. Postal Road was closed at Union Wesley Circle in Chester due to flooding.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 27.4307 km away, between 2020-08-17 15:26:00 and 2020-08-17 18:09:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Several strong thunderstorms developed ahead of a cold front, aided by an unseasonably strong upper-level jet stream. Several strong thunderstorms developed ahead of a cold front, aided by an unseasonably strong upper-level jet stream. Several strong thunderstorms developed ahead of a cold front, aided by an unseasonably strong upper-level jet stream. Several strong thunderstorms developed ahead of a cold front, aided by an unseasonably strong upper-level jet stream. Several strong thunderstorms developed ahead of a cold front, aided by an unseasonably strong upper-level jet stream.\nEvent Narrative: A 35 knot (40 MPH) wind gust was measured by a mesonet at Dundalk Marine Terminal. A 34 knot (39 MPH) wind gust was measured by a mesonet at Cape Saint Claire. A thunderstorm produced an estimated wind gust to 34 knots (39 MPH) near a mesonet near Cape Saint Claire. Wind gusts of 41 to 44 knots (47 to 51 MPH) were measured by a buoy near Tolly Point. A wind gust of 35 knots (40 MPH) was measured by a buoy near Thomas Point Light.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 35.7713 km away, between 2020-08-23 16:05:00 and 2020-08-23 19:12:00. The events included records with measured wind gusts of 36.25 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Several strong thunderstorms developed along a pressure trough over northern Maryland and the bay breeze, and moves over the upper portions of the Chesapeake Bay. Several strong thunderstorms developed along a pressure trough over northern Maryland and the bay breeze, and moves over the upper portions of the Chesapeake Bay. Several strong thunderstorms developed along a pressure trough over northern Maryland and the bay breeze, and moves over the upper portions of the Chesapeake Bay. Several strong thunderstorms developed along a pressure trough over northern Maryland and the bay breeze, and moves over the upper portions of the Chesapeake Bay.\nEvent Narrative: Wind gusts of 34 knots (39 MPH) were measured by a buoy near the mouth of the Gunpowder River. Wind gusts of 34 to 38 knots (39 to 44 MPH) were measured by a buoy near the mouth of the Gunpowder River. A wind gust of 36 knots (41 MPH) was measured by a buoy near the mouth of the Gunpowder River. A wind gust of 37 knots (43 MPH) was measured by a buoy near Tolchester Beach.", "The following events were reported: Hail. These occurred near station USW00093721, approximately 20.4748 km away, between 2020-08-23 18:03:00 and 2020-08-23 18:03:00. The events included records with hailstones measuring 1.0 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A few severe thunderstorms developed near a pressure trough over northern Maryland.\nEvent Narrative: Quarter size hail was reported near Rosedale.", "The following events were reported: Flash Flood. These occurred near station USW00093721, approximately 29.0865 km away, between 2020-08-23 18:39:00 and 2020-08-23 20:00:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A few storms led to isolated instances of flooding. A few storms led to isolated instances of flooding.\nEvent Narrative: There were multiple reports of water rescues along MD 150 from Chase MD through Dundalk. The water level along the Middle River rapidly rose above flood stage, and it crested at 12.44 feet at 7:08 PM EST on August 24th. Wilson Point Road was flooded.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 36.9916 km away, between 2020-08-25 19:05:00 and 2020-08-25 19:05:00. The events included records with measured wind gusts of 42.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: An outflow boundary from a decaying convective system triggered an isolated severe thunderstorm over northern Virginia around midday. A cold front then triggered an organized line of thunderstorms which produced scattered to numerous damaging wind gusts over eastern West Virginia, western Maryland, and northern into central Virginia as well as the DC metro area.\nEvent Narrative: A wind gust of 42 knots (48 MPH) was measured by a buoy near Thomas Point.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 38.8983 km away, between 2020-08-27 17:34:00 and 2020-08-27 17:42:00. The events included records with estimated wind gusts of 34.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: An isolated strong thunderstorm produced gusty winds over the upper Chesapeake Bay. An isolated strong thunderstorm produced gusty winds over the upper Chesapeake Bay.\nEvent Narrative: A thunderstorm produced an estimated wind gust to 34 knots (39 MPH) near a mesonet near Haven Harbour Marina near Rock Hall. A thunderstorm produced an estimated wind gust to 34 knots (39 MPH) near a buoy near Tolchester Beach.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 31.8464 km away, between 2020-08-28 14:45:00 and 2020-08-28 15:46:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 9000.0 and crop damage of 0.0. \n\nEpisode Narrative: A broken line of strong to severe thunderstorms developed southward into the area from Pennsylvania during the mid to late afternoon and early evening hours. A broken line of strong to severe thunderstorms developed southward into the area from Pennsylvania during the mid to late afternoon and early evening hours.\nEvent Narrative: A tree was blown down near the intersection of South Klee Mill Road and Terrapin Drive. A large branch was snapped by the wind and downed power lines and a power pole in the 2500 block of MD-198 Spencerville Road near Peach Orchard Road. A tree, wires and a pole were also blown down a few miles to the southwest on Conger Street near Weller Road and in the 12300 block of Barbara Road.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 30.3482 km away, between 2020-08-28 15:20:00 and 2020-08-28 17:00:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Broken lines of showers and thunderstorms produced gusty winds over the Maryland portion of the Chesapeake Bay and its adjoining tidal estuaries as well as the tidal Potomac River during the afternoon and evening hours of Friday, August 28th, 2020. Broken lines of showers and thunderstorms produced gusty winds over the Maryland portion of the Chesapeake Bay and its adjoining tidal estuaries as well as the tidal Potomac River during the afternoon and evening hours of Friday, August 28th, 2020. Broken lines of showers and thunderstorms produced gusty winds over the Maryland portion of the Chesapeake Bay and its adjoining tidal estuaries as well as the tidal Potomac River during the afternoon and evening hours of Friday, August 28th, 2020. Broken lines of showers and thunderstorms produced gusty winds over the Maryland portion of the Chesapeake Bay and its adjoining tidal estuaries as well as the tidal Potomac River during the afternoon and evening hours of Friday, August 28th, 2020. Broken lines of showers and thunderstorms produced gusty winds over the Maryland portion of the Chesapeake Bay and its adjoining tidal estuaries as well as the tidal Potomac River during the afternoon and evening hours of Friday, August 28th, 2020. Broken lines of showers and thunderstorms produced gusty winds over the Maryland portion of the Chesapeake Bay and its adjoining tidal estuaries as well as the tidal Potomac River during the afternoon and evening hours of Friday, August 28th, 2020. Broken lines of showers and thunderstorms produced gusty winds over the Maryland portion of the Chesapeake Bay and its adjoining tidal estuaries as well as the tidal Potomac River during the afternoon and evening hours of Friday, August 28th, 2020. Broken lines of showers and thunderstorms produced gusty winds over the Maryland portion of the Chesapeake Bay and its adjoining tidal estuaries as well as the tidal Potomac River during the afternoon and evening hours of Friday, August 28th, 2020. Broken lines of showers and thunderstorms produced gusty winds over the Maryland portion of the Chesapeake Bay and its adjoining tidal estuaries as well as the tidal Potomac River during the afternoon and evening hours of Friday, August 28th, 2020. Broken lines of showers and thunderstorms produced gusty winds over the Maryland portion of the Chesapeake Bay and its adjoining tidal estuaries as well as the tidal Potomac River during the afternoon and evening hours of Friday, August 28th, 2020.\nEvent Narrative: A wind gust of 39 knots (45 MPH) was measured by the AWOS at Martin State Airport. A thunderstorm produced an estimated wind gust to 34 knots (39 MPH) near a buoy near Hart Miller Island. Wind gusts of 34 to 35 knots (39 to 40 MPH) were measured by a buoy near Tolchester Beach. A wind gust of 34 knots (39 MPH) was measured by the ASOS at the U.S. Naval Academy. Wind gusts of 34 to 37 knots (39 to 42 MPH) were measured by a buoy near Annapolis. Wind gusts of 34 to 37 knots (39 to 42 MPH) were measured by a buoy near Greenbury Point. A thunderstorm produced an estimated wind gust to 34 knots (39 MPH) near a mesonet near Hampstead Hill Academy. A thunderstorm produced an estimated wind gust to 34 knots (39 MPH) near a buoy near Tolly Point. A thunderstorm produced an estimated wind gust to 34 knots (39 MPH) near a buoy near Thomas Point. A thunderstorm produced an estimated wind gust to 34 knots (39 MPH) near a buoy near the mouth of Gunpowder River.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 32.5511 km away, between 2020-09-02 18:46:00 and 2020-09-02 19:12:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 8000.0 and crop damage of 0.0. \n\nEpisode Narrative: A disturbance (the remnant of convection from over the Ohio River Valley the day before) triggered a line of strong to severe thunderstorms that affected mainly northern Maryland and far northern Virginia during the early evening hours of Wednesday, September 2nd, 2020. A disturbance (the remnant of convection from over the Ohio River Valley the day before) triggered a line of strong to severe thunderstorms that affected mainly northern Maryland and far northern Virginia during the early evening hours of Wednesday, September 2nd, 2020. A disturbance (the remnant of convection from over the Ohio River Valley the day before) triggered a line of strong to severe thunderstorms that affected mainly northern Maryland and far northern Virginia during the early evening hours of Wednesday, September 2nd, 2020. A disturbance (the remnant of convection from over the Ohio River Valley the day before) triggered a line of strong to severe thunderstorms that affected mainly northern Maryland and far northern Virginia during the early evening hours of Wednesday, September 2nd, 2020. A disturbance (the remnant of convection from over the Ohio River Valley the day before) triggered a line of strong to severe thunderstorms that affected mainly northern Maryland and far northern Virginia during the early evening hours of Wednesday, September 2nd, 2020. A disturbance (the remnant of convection from over the Ohio River Valley the day before) triggered a line of strong to severe thunderstorms that affected mainly northern Maryland and far northern Virginia during the early evening hours of Wednesday, September 2nd, 2020.\nEvent Narrative: A tree was blown down on MD-26 Liberty Road in Eldersburg blocking one lane. A tree was blown down onto wires on Greenspring Avenue between Garrison Forest Road and Baublitz Road. A tree was blown down onto wires near the intersection of Copper Ridge Drive and Bonnie Ridge Drive. A tree was blown down onto MD-145 Paper Mill Road at Ashland Road. A tree was blown down near the intersection of MD-650 Damascus Road and Griffith Road. A tree was blown down blocking the road near the intersection of Jennings Chapel Road and Howard Chapel Road. A tree blew down near the intersection of Homewood Road and Farside Road/Masters Run.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 32.8775 km away, between 2020-09-02 19:36:00 and 2020-09-03 20:05:00. The events included records with estimated wind gusts of 34.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A line of strong thunderstorms moved over the upper Chesapeake Bay during the evening hours. A line of strong thunderstorms moved over the upper Chesapeake Bay during the evening hours. A line of strong thunderstorms moved over the upper Chesapeake Bay during the evening hours. A line of strong thunderstorms moved over the upper Chesapeake Bay during the evening hours. A line of strong thunderstorms moved over the upper Chesapeake Bay during the evening hours. A line of strong thunderstorms moved over the upper Chesapeake Bay during the evening hours.\nEvent Narrative: A thunderstorm produced an estimated wind gust to 34 knots (39 MPH) near a buoy near Francis Scott Key Bridge. A thunderstorm produced an estimated wind gust to 34 knots (39 MPH) near the AWOS at Bay Bridge Airport. A thunderstorm produced an estimated wind gust to 34 knots (39 MPH) near a mesonet in Stevensville. A thunderstorm produced an estimated wind gust to 34 knots (39 MPH) near a buoy near Tolly Point. A thunderstorm produced an estimated wind gust to 34 knots (39 MPH) near a mesonet in Stevensville. A thunderstorm produced an estimated wind gust to 34 knots (39 MPH) near a buoy near Thomas Point.", "The following events were reported: Thunderstorm Wind, Tornado. These occurred near station USW00093721, approximately 23.5044 km away, between 2020-09-03 16:14:00 and 2020-09-03 17:07:00.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 1455000.0 and crop damage of 0.0. \n\nEpisode Narrative: A disturbance (the remnant of convection from the day before over the Tennessee River Valley) triggered a few supercells and line segments from eastern West Virginia into the Washington/Baltimore metro areas. A disturbance (the remnant of convection from the day before over the Tennessee River Valley) triggered a few supercells and line segments from eastern West Virginia into the Washington/Baltimore metro areas. A disturbance (the remnant of convection from the day before over the Tennessee River Valley) triggered a few supercells and line segments from eastern West Virginia into the Washington/Baltimore metro areas. A disturbance (the remnant of convection from the day before over the Tennessee River Valley) triggered a few supercells and line segments from eastern West Virginia into the Washington/Baltimore metro areas. A disturbance (the remnant of convection from the day before over the Tennessee River Valley) triggered a few supercells and line segments from eastern West Virginia into the Washington/Baltimore metro areas. A disturbance (the remnant of convection from the day before over the Tennessee River Valley) triggered a few supercells and line segments from eastern West Virginia into the Washington/Baltimore metro areas. A disturbance (the remnant of convection from the day before over the Tennessee River Valley) triggered a few supercells and line segments from eastern West Virginia into the Washington/Baltimore metro areas. A disturbance (the remnant of convection from the day before over the Tennessee River Valley) triggered a few supercells and line segments from eastern West Virginia into the Washington/Baltimore metro areas.\nEvent Narrative: A tree blew down near the intersection of Lovat Road and Reservoir Road. A tree was blown down onto power lines near the intersection of Riverton Road and MD-700 Martin Boulevard. A tree was blown down blocking Belle Chasse Boulevard. A tree was blown down onto MD-197 near Muirkirk Road. Dozens of trees were uprooted and snapped in the Davidsonville area, including along MD-450 Defense Highway between Huntwood Drive and Saint Stephens Church Road. A tree was blown down onto US-50 John Hanson Highway just west of the South River. A tree fell onto a house behind Mike's Crab Shack. Dozens of trees were uprooted and snapped in the Riva area, including near the intersection of Homewood Road and Della Way, and along Westbury Drive near Annapolis Landing. Numerous trees were blown down in the vicinity of Ridge Road in Rosedale, several onto cars and houses. The sign of a store was blown down. A supercell thunderstorm tracked east across central Maryland and|produced an EF-1 tornado that touched down late Thursday|afternoon in Edgewater Maryland and continued to the western shore|of the Chesapeake Bay.||Tornadic damage began after the storm crossed Beard`s Creek off|the South River. Trees were first downed near the intersection of|Edgewater Drive and Park Avenue, just north of Lee Airport. The|tornado intensified as it moved east into central Edgewater, and|reached its peak EF-1 strength in the area of the community|bounded by Solomons Island Road (Route 2), Virginia Avenue, and|Ridge Avenue. In this area damage was blown in all directions.|Siding was torn from the wall of one home, and some roof flashing|was damaged on another. A commercial fence was blown down to the|north. However, most of the damage was to trees. Most of the trees|in this area had at least some large branches ripped from their|upper sections. About 10 trees in this wooded community were|entirely uprooted or snapped. Some of those trees fell into power|lines, and at least 2 power poles were snapped because of this. A|few homes and vehicles were damaged from falling trees and|branches.||As the tornado crossed Solomons Island Road, it weakened to an|EF-0 but continued to cause scattered tree damage with uprooted|or snapped trees that were thrown generally left of the tornado|track. Damage was noted on both sides of Warehouse Creek along|Leeland Road and South River Landing Road.||The tornado continued across South River and into Hillsmere|Shores. A large tree was uprooted on the The Key School soccer|field with numerous large branches strung across the 100-yard|field to the left of the track. One large branch caused damage|to the protective netting and metal framing attached to a|scoreboard situated on the west side of the soccer field. The|damage path continued east across Hillsmere Drive where a half|dozen 30-40 foot tall pine trees where uprooted and criss-crossed|in a northeast and southeast fashion.||Further northeast along Sunset Drive, scattered tree damage was|observed with several large trees snapped. One large tree was|uprooted and puncturing a roof resulting in water intrusion|inside the home. Additional scattered tree limb damage was|observed immediately to the east northeast with limbs noted thrown|to the left of the track.||As the tornado tracked east, scattered tree limb damage was|observed along Thomas Point Road and through the Arundel on the|Bay community. A few large trees were observed to be snapped and|uprooted along Cohasset Ave near Walnut Ave. Tree damage became|minor near the shoreline of the Bay between Linden Ave and Walnut|Ave.||While wind damage from this storm was examined between Crofton,|Davidsonville, and Riva, that tree damage was unidirectional,|largely oriented from west east, and falling generally in the|direction of the storm`s motion.", "The following events were reported: Flood. These occurred near station USW00093721, approximately 26.5945 km away, between 2020-09-03 16:54:00 and 2020-09-03 21:50:00. The flood was caused by Heavy Rain. Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A disturbance (the remnant of convection from the day before over the Tennessee River Valley) triggered a few supercells and line segments from eastern West Virginia into the Washington/Baltimore metro areas. This lead to some isolated instances of flooding in parts of MD. A disturbance (the remnant of convection from the day before over the Tennessee River Valley) triggered a few supercells and line segments from eastern West Virginia into the Washington/Baltimore metro areas. This lead to some isolated instances of flooding in parts of MD. A disturbance (the remnant of convection from the day before over the Tennessee River Valley) triggered a few supercells and line segments from eastern West Virginia into the Washington/Baltimore metro areas. This lead to some isolated instances of flooding in parts of MD. A disturbance (the remnant of convection from the day before over the Tennessee River Valley) triggered a few supercells and line segments from eastern West Virginia into the Washington/Baltimore metro areas. This lead to some isolated instances of flooding in parts of MD. A disturbance (the remnant of convection from the day before over the Tennessee River Valley) triggered a few supercells and line segments from eastern West Virginia into the Washington/Baltimore metro areas. This lead to some isolated instances of flooding in parts of MD. A disturbance (the remnant of convection from the day before over the Tennessee River Valley) triggered a few supercells and line segments from eastern West Virginia into the Washington/Baltimore metro areas. This lead to some isolated instances of flooding in parts of MD. A disturbance (the remnant of convection from the day before over the Tennessee River Valley) triggered a few supercells and line segments from eastern West Virginia into the Washington/Baltimore metro areas. This lead to some isolated instances of flooding in parts of MD.\nEvent Narrative: Reports of flooded roadway at the intersection of Tinker Rd. Reports of flooded roadway at the intersection of Tinker Rd. Flooding at the intersection of Orems Rd. and Rossville Blvd. Mayo Rd. closed due to flooding. Defense Hwy. closed due to flooding near Saint Stephens Church Rd. Central Ave. closed due to flooding at Beards Creek. The water level rose above the flood stage along the Middle River. The water level crested at 10.89 feet at 5:08 PM EST. Wilsons Point Road was flooded with at least six inches of water flowing over the road in spots.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 35.9698 km away, between 2020-09-03 17:08:00 and 2020-09-03 18:18:00. The events included records with measured wind gusts of 44.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Several supercells and lines of severe thunderstorms moved into the upper Chesapeake Bay during the late afternoon and early evening hours. Several supercells and lines of severe thunderstorms moved into the upper Chesapeake Bay during the late afternoon and early evening hours. Several supercells and lines of severe thunderstorms moved into the upper Chesapeake Bay during the late afternoon and early evening hours. Several supercells and lines of severe thunderstorms moved into the upper Chesapeake Bay during the late afternoon and early evening hours. Several supercells and lines of severe thunderstorms moved into the upper Chesapeake Bay during the late afternoon and early evening hours. Several supercells and lines of severe thunderstorms moved into the upper Chesapeake Bay during the late afternoon and early evening hours.\nEvent Narrative: Wind gusts of 34 to 38 knots (39 to 44 MPH) were measured by a buoy near Tolly Point. A wind gust of 57 knots (66 MPH) was measured by a buoy near Thomas Point. A wind gust of 42 knots (48 MPH) was measured by a mesonet in Stevensville. A wind gust of 43 knots (49 MPH) was measured by the AWOS at Bay Bridge Airport. A wind gust of 46 knots (53 MPH) was measured by a buoy near Thomas Point. A wind gust of 37 knots (43 MPH) was measured by a buoy near Tolly Point.", "The following events were reported: Flood. These occurred near station USW00093721, approximately 28.3796 km away, between 2020-11-12 04:15:00 and 2020-11-12 06:15:00. The flood was caused by Heavy Rain. Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Heavy rain occurred as tropical moisture (record levels for November) streamed northward into the area and interacted with a stalled frontal zone. This heavy rainfall resulted in widespread flooding across central and southern Maryland.\nEvent Narrative: Central Avenue (MD-214) was closed due to flooding east of Beards Point Road/Brick Church Road.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 26.8149 km away, between 2020-11-15 18:45:00 and 2020-11-15 19:59:00.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 41000.0 and crop damage of 0.0. \n\nEpisode Narrative: A strong cold front spawned a line of low-topped showers and thunderstorms that produced wind gusts of up to 70 MPH and numerous instances of downed trees. A strong cold front spawned a line of low-topped showers and thunderstorms that produced wind gusts of up to 70 MPH and numerous instances of downed trees. A strong cold front spawned a line of low-topped showers and thunderstorms that produced wind gusts of up to 70 MPH and numerous instances of downed trees. A strong cold front spawned a line of low-topped showers and thunderstorms that produced wind gusts of up to 70 MPH and numerous instances of downed trees. A strong cold front spawned a line of low-topped showers and thunderstorms that produced wind gusts of up to 70 MPH and numerous instances of downed trees. A strong cold front spawned a line of low-topped showers and thunderstorms that produced wind gusts of up to 70 MPH and numerous instances of downed trees. A strong cold front spawned a line of low-topped showers and thunderstorms that produced wind gusts of up to 70 MPH and numerous instances of downed trees. A strong cold front spawned a line of low-topped showers and thunderstorms that produced wind gusts of up to 70 MPH and numerous instances of downed trees. A strong cold front spawned a line of low-topped showers and thunderstorms that produced wind gusts of up to 70 MPH and numerous instances of downed trees. A strong cold front spawned a line of low-topped showers and thunderstorms that produced wind gusts of up to 70 MPH and numerous instances of downed trees. A strong cold front spawned a line of low-topped showers and thunderstorms that produced wind gusts of up to 70 MPH and numerous instances of downed trees. A strong cold front spawned a line of low-topped showers and thunderstorms that produced wind gusts of up to 70 MPH and numerous instances of downed trees. A strong cold front spawned a line of low-topped showers and thunderstorms that produced wind gusts of up to 70 MPH and numerous instances of downed trees. A strong cold front spawned a line of low-topped showers and thunderstorms that produced wind gusts of up to 70 MPH and numerous instances of downed trees. A strong cold front spawned a line of low-topped showers and thunderstorms that produced wind gusts of up to 70 MPH and numerous instances of downed trees. A strong cold front spawned a line of low-topped showers and thunderstorms that produced wind gusts of up to 70 MPH and numerous instances of downed trees. A strong cold front spawned a line of low-topped showers and thunderstorms that produced wind gusts of up to 70 MPH and numerous instances of downed trees. A strong cold front spawned a line of low-topped showers and thunderstorms that produced wind gusts of up to 70 MPH and numerous instances of downed trees. A strong cold front spawned a line of low-topped showers and thunderstorms that produced wind gusts of up to 70 MPH and numerous instances of downed trees. A strong cold front spawned a line of low-topped showers and thunderstorms that produced wind gusts of up to 70 MPH and numerous instances of downed trees. A strong cold front spawned a line of low-topped showers and thunderstorms that produced wind gusts of up to 70 MPH and numerous instances of downed trees.\nEvent Narrative: A tree blew down on Hobbs Road. A tree blew down on Frederick Road. A tree blew down on Howard Chapel Road at Jennings Chapel Road. A tree blew down on MD-138 at Big Falls Road. A tree blew down on MD-482 at Sisters Church Road. A wind gust of 57 knots (66 MPH) was measured by a mesonet in Dayton. A tree blew down on Pine Bark Court. A tree blew down on Clarksville Pike at Hall Shop Road. A tree blew down on Manorstone Lane. A tree blew down on Harpers Farm Road at Twin Rivers Road. A tree blew down on Little Patuxent Parkway near Governor Warfield Parkway. A tree blew down on Clarksville Pike. A tree blew down on Summer Day Lane. A tree blew down on Pricemanor Way at Johns Hopkins Road. A tree blew down on Pimlico Road at Greenspring Avenue. A tree blew down on Bonner Road. A tree blew down on Taney Road. A tree blew down on Carlisle Avenue. A tree blew down on MD-25 at Old Pimlico Road. Trees blew down near the intersection of Falls Road and Northern Parkway. A tree blew down on Falls Road at Cold Spring Lane. Trees blew down along Hilton Parkway. Trees blew down along Edmondson Avenue. A tree blew down on Paddington Road. A tree blew down on Perring Parkway at Northern Parkway. A tree blew down along Baldwin Mill Road. A tree blew down along Green Road. A tree blew down on East 36th Street. A tree blew down on Mission Road at Pleasant Chase Road. A tree blew down on US-1 at Ducketts Lane. A tree blew down on Ramsey Street at Calhoun Street. A tree blew down on Monroe Street near MD-295. A tree blew down along Red Pump Road. A tree blew down on Paterson Mill Road. A tree blew down on Old Orchard Road. A tree blew down on Aldino Road. A wind gust of 50 knots (58 MPH) was measured by a mesonet near the Bay Bridge. A tree blew down at the intersection of MD-97 and MD-144. A tree blew down at the intersection of US-40 and Marriottsville Road.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 20.4702 km away, between 2020-11-15 19:20:00 and 2020-11-15 19:59:00. The events included records with measured wind gusts of 49.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A strong cold front spawned a line of thunderstorms which produced storm force winds over portions of the Chesapeake Bay and tidal Potomac River during the evening hours. A strong cold front spawned a line of thunderstorms which produced storm force winds over portions of the Chesapeake Bay and tidal Potomac River during the evening hours.\nEvent Narrative: A wind gust of 48 knots (55 MPH) was measured by a mesonet at Oriole Park at Camden Yard adjacent to Baltimore Harbor. A wind gust of 50 knots (58 MPH) was measured by a mesonet near the Bay Bridge.", "The following events were reported: Flood. These occurred near station USW00093721, approximately 36.3854 km away, between 2020-11-30 12:58:00 and 2020-11-30 17:22:00. The flood was caused by Heavy Rain. Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Multiple rounds of rain moved through the area as low pressure tracked to the west. This resulted in a few instances of flooding across northeastern Maryland. Multiple rounds of rain moved through the area as low pressure tracked to the west. This resulted in a few instances of flooding across northeastern Maryland. Multiple rounds of rain moved through the area as low pressure tracked to the west. This resulted in a few instances of flooding across northeastern Maryland. Multiple rounds of rain moved through the area as low pressure tracked to the west. This resulted in a few instances of flooding across northeastern Maryland. Multiple rounds of rain moved through the area as low pressure tracked to the west. This resulted in a few instances of flooding across northeastern Maryland.\nEvent Narrative: MD-7 (Philadelphia Road) closed due to flooding near Calvary Road. MD-7 was closed due to flooding near Campbell Boulevard. Whitemarsh Run at White Marsh was in Minor Flood stage during the indicated time period, reaching a peak level of 11.39 feet at 1:15 PM on the 30th. Water covered parking lots near Town Center Court. Whitemarsh Run at White Marsh was in Minor Flood stage during the indicated time period, reaching a peak level of 11.46 feet at 3:20 PM on the 30th. Water covered parking lots near Town Center Court. Otter Point Creek at Edgewood was in Minor Flood stage during the indicated time period, reaching a peak level of 9.38 feet at 3:30 PM on the 30th. Winters Run Road was flooded near Singer Road.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 36.9916 km away, between 2020-12-24 18:55:00 and 2020-12-24 19:00:00. The events included records with measured wind gusts of 54.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A strong cold front produced several rounds of convection that resulted in high wind over the waters.\nEvent Narrative: Wind gusts of up to 54 knots (62 MPH) were measured by a buoy near Thomas Point.", "The following events were reported: Flood. These occurred near station USW00093721, approximately 20.3247 km away, between 2020-12-25 01:06:00 and 2020-12-25 10:11:00. The flood was caused by Heavy Rain. Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A strong cold front pushed through the area during the evening Dec 24th. An area of low pressure formed along this front and slid across the region. This brought some heavy showers to the region, and even a few isolated thunderstorms. Several instances of flooding resulted from this event. There were then a few large stem rivers that crept up to flood stage in the couple of days following the main event. A strong cold front pushed through the area during the evening Dec 24th. An area of low pressure formed along this front and slid across the region. This brought some heavy showers to the region, and even a few isolated thunderstorms. Several instances of flooding resulted from this event. There were then a few large stem rivers that crept up to flood stage in the couple of days following the main event. A strong cold front pushed through the area during the evening Dec 24th. An area of low pressure formed along this front and slid across the region. This brought some heavy showers to the region, and even a few isolated thunderstorms. Several instances of flooding resulted from this event. There were then a few large stem rivers that crept up to flood stage in the couple of days following the main event.\nEvent Narrative: The stream gage on the Little Patuxent River in Savage rose above flood stage during the specified timeframe, reaching a peak stream level of 10.72 feet. At 10 feet, riverside trails begin to flood. Water also approaches fields off Bald Eagle Drive, and approach Brock Bridge Road. The stream gage on Big Gunpowder Falls near Glencoe, MD, rose above flood stage during the specified time, reaching a max flood stage of 8.96 feet at 05:40 AM EST. At 9 feet Sparks Road begins to flood. The stream gage on the Patuxent River in Elkridge rose above flood stage during the specified timeframe, reaching a peak stream level of 17.11 feet. At 16 feet, Hammonds Ferry Road floods and is closed at the Patapsco River. Backwater flooding likely also leads to the closure of Furnace Avenue in Elkridge.", "The following events were reported: Flood. These occurred near station USW00093721, approximately 6.5468 km away, between 2021-03-24 17:10:00 and 2021-03-24 17:44:00. The flood was caused by Heavy Rain. Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Low pressure moved across the Delmarva Peninsula during the day on March 24th, bringing a steady rain to the region. There were a few instances of flooding across the forecast area as a result, particularly in central and southern MD.\nEvent Narrative: The stream gauge on the Patuxent River near Elkridge reached flood stage during the specified timeframe, reaching a peak of 16.08 feet at 5:30 PM EDT. At 16 feet, Hammonds Ferry Road floods and is closed at the Patapsco River. Backwater flooding likely also leads to the closure of Furnace Avenue in Elkridge.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 28.6671 km away, between 2021-03-28 16:30:00 and 2021-03-28 17:00:00. The events included records with estimated wind gusts of 51.875 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 59000.0 and crop damage of 0.0. \n\nEpisode Narrative: Brief clearing occurred ahead of a strong cold front, spawning a line of thunderstorms that producing wind gusts of around 50 to up to 70 mph as it tracked across northern Maryland and extreme northwestern Virginia during the mid to late afternoon hours. Brief clearing occurred ahead of a strong cold front, spawning a line of thunderstorms that producing wind gusts of around 50 to up to 70 mph as it tracked across northern Maryland and extreme northwestern Virginia during the mid to late afternoon hours. Brief clearing occurred ahead of a strong cold front, spawning a line of thunderstorms that producing wind gusts of around 50 to up to 70 mph as it tracked across northern Maryland and extreme northwestern Virginia during the mid to late afternoon hours. Brief clearing occurred ahead of a strong cold front, spawning a line of thunderstorms that producing wind gusts of around 50 to up to 70 mph as it tracked across northern Maryland and extreme northwestern Virginia during the mid to late afternoon hours. Brief clearing occurred ahead of a strong cold front, spawning a line of thunderstorms that producing wind gusts of around 50 to up to 70 mph as it tracked across northern Maryland and extreme northwestern Virginia during the mid to late afternoon hours. Brief clearing occurred ahead of a strong cold front, spawning a line of thunderstorms that producing wind gusts of around 50 to up to 70 mph as it tracked across northern Maryland and extreme northwestern Virginia during the mid to late afternoon hours. Brief clearing occurred ahead of a strong cold front, spawning a line of thunderstorms that producing wind gusts of around 50 to up to 70 mph as it tracked across northern Maryland and extreme northwestern Virginia during the mid to late afternoon hours. Brief clearing occurred ahead of a strong cold front, spawning a line of thunderstorms that producing wind gusts of around 50 to up to 70 mph as it tracked across northern Maryland and extreme northwestern Virginia during the mid to late afternoon hours.\nEvent Narrative: Power lines were down near the intersection of Gregg Road and MD-97 Georgia Avenue, probably as a result of a downed tree. The Baltimore County 911 Call Center received about a dozen reports of trees blown down in the Owings Mills and Randallstown area, including two large oak trees that fell onto the roof of a house near the intersection of Bridle Brook Drive and Birkenhead Court. A tree was blown down on MD-25 Falls Road near Deep Run Court. A tree was blown down on US-40 Baltimore National Pike at Tyson Road. Power lines were down in the 4600 block of South Leisure Road. A tree was blown down on MD-139 Charles Street near West Joppa Road. Multiple trees were blown down in Perry Hall, including on Perry Hall Road where wires and a couple poles were also down (probably as a result of falling trees). A large tree was blown down in the 10000 block of southbound US-1 Washington Boulevard (near Davis Avenue). A large tree was blown down near the intersection of Stockton Road and Atkisson Road.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 29.7041 km away, between 2021-03-28 17:08:00 and 2021-03-28 17:24:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A line of strong to severe thunderstorms ahead of a cold front caused an abrupt wind shift and wind gusts to near storm force during the late afternoon hours. A line of strong to severe thunderstorms ahead of a cold front caused an abrupt wind shift and wind gusts to near storm force during the late afternoon hours.\nEvent Narrative: A thunderstorm produced an estimated wind gust to 48 knots (55 MPH) near a buoy near Hart Miller Island. A wind gust of 51 knots (59 MPH) was measured by a buoy near Annapolis.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 34.9687 km away, between 2021-04-01 00:05:00 and 2021-04-01 00:42:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A strong cold front spawned a line of showers that produced a sudden onset of gale-force wind over portions of the tidal Potomac River and Chesapeake Bay during the overnight hours. A strong cold front spawned a line of showers that produced a sudden onset of gale-force wind over portions of the tidal Potomac River and Chesapeake Bay during the overnight hours. A strong cold front spawned a line of showers that produced a sudden onset of gale-force wind over portions of the tidal Potomac River and Chesapeake Bay during the overnight hours. A strong cold front spawned a line of showers that produced a sudden onset of gale-force wind over portions of the tidal Potomac River and Chesapeake Bay during the overnight hours. A strong cold front spawned a line of showers that produced a sudden onset of gale-force wind over portions of the tidal Potomac River and Chesapeake Bay during the overnight hours. A strong cold front spawned a line of showers that produced a sudden onset of gale-force wind over portions of the tidal Potomac River and Chesapeake Bay during the overnight hours. A strong cold front spawned a line of showers that produced a sudden onset of gale-force wind over portions of the tidal Potomac River and Chesapeake Bay during the overnight hours.\nEvent Narrative: Wind gusts of up to 34 knots (39 MPH) were measured by a buoy near Greenbury Point. Wind gusts of up to 36 knots (41 MPH) were measured by a buoy near Annapolis. Wind gusts of up to 34 knots (39 MPH) were measured by a buoy near Tolly Point. A wind gust of 34 knots (39 MPH) was estimated near a mesonet near Crab Alley Bay. A wind gust of 39 knots (45 MPH) was measured by a buoy near Thomas Point. Wind gusts of up to 43 knots (49 MPH) were measured by a buoy offshore of Annapolis. A wind gust of 35 knots (40 MPH) was measured by a buoy near Kent Island.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 33.2867 km away, between 2021-04-11 19:54:00 and 2021-04-11 20:00:00. The events included records with estimated wind gusts of 34.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front spawned a line of thunderstorms that produced gusty winds over northern portions of the tidal Potomac River and Chesapeake Bay during the evening hours. A cold front spawned a line of thunderstorms that produced gusty winds over northern portions of the tidal Potomac River and Chesapeake Bay during the evening hours.\nEvent Narrative: A thunderstorm produced an estimated wind gust of 34 knots (39 MPH) near a buoy near Hart Miller Island. A thunderstorm produced an estimated wind gust of 34 knots (39 MPH) near a buoy near Tolchester Beach.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 31.9826 km away, between 2021-04-30 15:51:00 and 2021-04-30 16:12:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 2000.0 and crop damage of 0.0. \n\nEpisode Narrative: A strong cold front spawned a shallow line of convection that produced severe wind gusts. A strong cold front spawned a shallow line of convection that produced severe wind gusts.\nEvent Narrative: A tree blew down on MD-108 between Hawkins Creamery Road and Rocky Road blocking all southbound lanes. A tree blew down on westbound US-50 John Hanson Highway prior to MD-424 Davidsonville Road.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 32.5291 km away, between 2021-04-30 16:00:00 and 2021-04-30 16:23:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A strong cold front spawned a shallow line of convection that produced storm-force wind gusts. A strong cold front spawned a shallow line of convection that produced storm-force wind gusts. A strong cold front spawned a shallow line of convection that produced storm-force wind gusts. A strong cold front spawned a shallow line of convection that produced storm-force wind gusts. A strong cold front spawned a shallow line of convection that produced storm-force wind gusts. A strong cold front spawned a shallow line of convection that produced storm-force wind gusts.\nEvent Narrative: Wind gusts of up to 52 knots (60 MPH) were measured by a buoy near Annapolis. A wind gust of 51 knots (59 MPH) was measured by a buoy near Saunders Point Lighthouse. A shallow line of convection produced an estimated wind gust to 48 knots (55 MPH) near a buoy near Thomas Point. A shallow line of convection produced an estimated wind gust to 48 knots (55 MPH) near a buoy near Tolly Point. A shallow line of convection produced an estimated wind gust of 48 knots (55 MPH) near a buoy near Hart Miller Island. A shallow line of convection produced an estimated wind gust to 48 knots (55 MPH) near the U.S. Naval Academy in Annapolis.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 43.6232 km away, between 2021-05-03 20:04:00 and 2021-05-03 20:24:00. The events included records with estimated wind gusts of 55.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 6000.0 and crop damage of 0.0. \n\nEpisode Narrative: An isolated, cyclic supercell thunderstorm tracking along a warm front produced sporadic straight-line wind damage and spawned several tornadoes. An isolated, cyclic supercell thunderstorm tracking along a warm front produced sporadic straight-line wind damage and spawned several tornadoes.\nEvent Narrative: A tree was blown down on southbound MD-30 just north of Mount Gilead Road. Several trees were topped or uprooted all facing in the same direction near the 2000 block of Browns Road.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 31.3611 km away, between 2021-05-08 12:48:00 and 2021-05-08 15:38:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: An unseasonably deep upper-level low produced numerous convective showers with small hail and gusty winds. An unseasonably deep upper-level low produced numerous convective showers with small hail and gusty winds. An unseasonably deep upper-level low produced numerous convective showers with small hail and gusty winds. An unseasonably deep upper-level low produced numerous convective showers with small hail and gusty winds. An unseasonably deep upper-level low produced numerous convective showers with small hail and gusty winds. An unseasonably deep upper-level low produced numerous convective showers with small hail and gusty winds. An unseasonably deep upper-level low produced numerous convective showers with small hail and gusty winds. An unseasonably deep upper-level low produced numerous convective showers with small hail and gusty winds. An unseasonably deep upper-level low produced numerous convective showers with small hail and gusty winds. An unseasonably deep upper-level low produced numerous convective showers with small hail and gusty winds. An unseasonably deep upper-level low produced numerous convective showers with small hail and gusty winds. An unseasonably deep upper-level low produced numerous convective showers with small hail and gusty winds. An unseasonably deep upper-level low produced numerous convective showers with small hail and gusty winds. An unseasonably deep upper-level low produced numerous convective showers with small hail and gusty winds. An unseasonably deep upper-level low produced numerous convective showers with small hail and gusty winds. An unseasonably deep upper-level low produced numerous convective showers with small hail and gusty winds. An unseasonably deep upper-level low produced numerous convective showers with small hail and gusty winds.\nEvent Narrative: Wind gusts of up to 41 knots (47 MPH) were measured by a buoy near Annapolis. Wind gusts of up to 35 knots (40 MPH) were measured by a buoy near Greenbury Point. A wind gust of 34 knots (39 MPH) was measured by a buoy near Tolly Point. A wind gust of 43 knots (49 MPH) was measured by a buoy near Thomas Point. Wind gusts of up to 34 knots (39 MPH) were measured by a buoy near Kent Island. A convective shower produced an estimated wind gust to 34 knots (39 MPH) near a buoy near Tolchester Beach. A wind gust of 36 knots (41 MPH) was measured by the ASOS at the U.S. Naval Academy in Annapolis adjacent to the Chesapeake Bay. A wind gust of 36 knots (41 MPH) was measured by a buoy near Greenbury Point. Wind gusts of up to 41 knots (47 MPH) were measured by a buoy near Annapolis. Wind gusts of up to 38 knots (44 MPH) were measured by a buoy near Annapolis. Wind gusts of up to 40 knots (46 MPH) were measured by a buoy near Tolly Point. A wind gust of 39 knots (45 MPH) was measured by a buoy near Thomas Point. A wind gust of 35 knots (40 MPH) was measured by a buoy near Kent Island. A convective shower produced an estimated wind gust to 34 knots (39 MPH) near a mesonet near Hampstead Hill Academy. A convective shower produced an estimated wind gust to 34 knots (39 MPH) near a buoy near Francis Scott Key Bridge near Baltimore. A convective shower produced an estimated wind gust to 34 knots (39 MPH) near a buoy near Hart Miller Island. A convective shower produced an estimated wind gust to 34 knots (39 MPH) near a buoy near Tolchester Beach.", "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00093721, approximately 20.6728 km away, between 2021-05-26 16:19:00 and 2021-05-26 19:30:00. The events included records with hailstones measuring 47.675 inches.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 44000.0 and crop damage of 0.0. \n\nEpisode Narrative: A pre-frontal trough and approaching cold front ignited multiple rounds of severe thunderstorms during the afternoon and evening hours. Some thunderstorms produced significant microbursts. A pre-frontal trough and approaching cold front ignited multiple rounds of severe thunderstorms during the afternoon and evening hours. Some thunderstorms produced significant microbursts. A pre-frontal trough and approaching cold front ignited multiple rounds of severe thunderstorms during the afternoon and evening hours. Some thunderstorms produced significant microbursts. A pre-frontal trough and approaching cold front ignited multiple rounds of severe thunderstorms during the afternoon and evening hours. Some thunderstorms produced significant microbursts. A pre-frontal trough and approaching cold front ignited multiple rounds of severe thunderstorms during the afternoon and evening hours. Some thunderstorms produced significant microbursts. A pre-frontal trough and approaching cold front ignited multiple rounds of severe thunderstorms during the afternoon and evening hours. Some thunderstorms produced significant microbursts. A pre-frontal trough and approaching cold front ignited multiple rounds of severe thunderstorms during the afternoon and evening hours. Some thunderstorms produced significant microbursts. A pre-frontal trough and approaching cold front ignited multiple rounds of severe thunderstorms during the afternoon and evening hours. Some thunderstorms produced significant microbursts. A pre-frontal trough and approaching cold front ignited multiple rounds of severe thunderstorms during the afternoon and evening hours. Some thunderstorms produced significant microbursts. A pre-frontal trough and approaching cold front ignited multiple rounds of severe thunderstorms during the afternoon and evening hours. Some thunderstorms produced significant microbursts.\nEvent Narrative: Wires blew down on US-29 Columbia Pike near Briggs Chaney Road. Tree damage was reported near Simpsonville, including trees and large tree limbs across the roadway in several locations on Murray Hill Road near the Middle Patuxent River to the intersection of Vollmerhausen Road. A tree blew down onto one lane of US-40 Baltimore National Pike near Nuwood Drive. Other tree damage was reported in the area. Quarter to golf ball size hail was reported in Elkridge. A tree blew down on MD-295 Baltimore-Washington Parkway near Ridge Road. A tree was blown down across Furnace Road. There were about a dozen calls for trees and wires down in the Mount Airy area. There were about a dozen calls for trees and wires down in the Sykesville area. Trees were blown down on MD-97 New Washington Road near MD-32 East Main Street/Old Westminster Pike. A tree blew down on MD-30 Hanover Pike near Kemp Road. There were five calls for trees blown down in the Reisterstown and Owings Mills area. Trees down in Baltimore, including in the 4600 block of Windsor Avenue.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 21.8436 km away, between 2021-05-26 17:15:00 and 2021-05-26 20:08:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A pre-frontal trough and approaching cold front ignited multiple rounds of severe thunderstorms during the afternoon and evening hours. Some thunderstorms produced significant microbursts. A pre-frontal trough and approaching cold front ignited multiple rounds of severe thunderstorms during the afternoon and evening hours. Some thunderstorms produced significant microbursts. A pre-frontal trough and approaching cold front ignited multiple rounds of severe thunderstorms during the afternoon and evening hours. Some thunderstorms produced significant microbursts. A pre-frontal trough and approaching cold front ignited multiple rounds of severe thunderstorms during the afternoon and evening hours. Some thunderstorms produced significant microbursts. A pre-frontal trough and approaching cold front ignited multiple rounds of severe thunderstorms during the afternoon and evening hours. Some thunderstorms produced significant microbursts. A pre-frontal trough and approaching cold front ignited multiple rounds of severe thunderstorms during the afternoon and evening hours. Some thunderstorms produced significant microbursts. A pre-frontal trough and approaching cold front ignited multiple rounds of severe thunderstorms during the afternoon and evening hours. Some thunderstorms produced significant microbursts. A pre-frontal trough and approaching cold front ignited multiple rounds of severe thunderstorms during the afternoon and evening hours. Some thunderstorms produced significant microbursts.\nEvent Narrative: A wind gust of 36 knots (41 MPH) was measured by a buoy near Francis Scott Key Bridge. A wind gust of 47 knots (54 MPH) was measured by a mesonet at Oriole Park at Camden Yards adjacent to Baltimore Inner Harbor. Wind gusts of up to 34 knots (39 MPH) were measured by a mesonet at Hampstead Hill Academy adjacent to Baltimore Inner Harbor. Wind gusts of up to 36 knots (41 MPH) were measured by a buoy near Francis Scott Key Bridge. A wind gust of 38 knots (44 MPH) was measured by a mesonet at Maryland Science Center adjacent to Baltimore Inner Harbor. Wind gusts of up to 38 knots (44 MPH) were measured by a buoy near Hart Miller Island. A thunderstorm produced an estimated wind gust to 34 knots (39 MPH) near a buoy near Tolchester Beach. A thunderstorm produced an estimated wind gust to 34 knots (39 MPH) near a buoy near Thomas Point.", "The following events were reported: Hail, Thunderstorm Wind, Tornado. These occurred near station USW00093721, approximately 30.4564 km away, between 2021-06-03 15:16:00 and 2021-06-03 17:54:00. The events included records with hailstones measuring 44.63636363636363 inches.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 263500.0 and crop damage of 0.0. \n\nEpisode Narrative: A pressure trough ignited numerous showers and thunderstorms, several of which produced localized damaging winds, hail, and a tornado. A pressure trough ignited numerous showers and thunderstorms, several of which produced localized damaging winds, hail, and a tornado. A pressure trough ignited numerous showers and thunderstorms, several of which produced localized damaging winds, hail, and a tornado. A pressure trough ignited numerous showers and thunderstorms, several of which produced localized damaging winds, hail, and a tornado. A pressure trough ignited numerous showers and thunderstorms, several of which produced localized damaging winds, hail, and a tornado. A pressure trough ignited numerous showers and thunderstorms, several of which produced localized damaging winds, hail, and a tornado. A pressure trough ignited numerous showers and thunderstorms, several of which produced localized damaging winds, hail, and a tornado. A pressure trough ignited numerous showers and thunderstorms, several of which produced localized damaging winds, hail, and a tornado. A pressure trough ignited numerous showers and thunderstorms, several of which produced localized damaging winds, hail, and a tornado. A pressure trough ignited numerous showers and thunderstorms, several of which produced localized damaging winds, hail, and a tornado. A pressure trough ignited numerous showers and thunderstorms, several of which produced localized damaging winds, hail, and a tornado. A pressure trough ignited numerous showers and thunderstorms, several of which produced localized damaging winds, hail, and a tornado.\nEvent Narrative: Trees were blown down onto the right southbound shoulder of I-95 just south of Exit 35/MD-216. A tree blew down on Ivy Terrace near Cozy Lane. Trees were blown down on MD-147 Harford Road at Reckford Road. A couple of trees blew down on Patterson Mill Road. A tree blew down in the 7500 block of John Pickett Road. A tree blew down in the 600 block of River Road. A tree blew down in the 1300 block of Raincliffe Road. A tree blew down on Cherry Tree Lane near Bartholow Road. A tree blew down near the intersection of MD-129 Park Heights Avenue and Velvet Ridge Drive. A tree blew down near the intersection of Woodholme Avenue and MD-140 Reisterstown Road. A tree blew down near the intersection of Church Lane and Greenwood Road. Quarter size hail was reported in northwest Baltimore. A tornado touched down just north of the intersection of Merrymans Mill Road and MD-146 Jarrettsville Pike, where minor tree damage and snapped tree tops were observed.||The tornado continued moving northeastward producing more significant tree damage as it moved east of MD-146 Jarrettsville Pike towards the southern end of Overshot Court. The most extensive tree damage was noted along Overshot Court where multiple hardwood and softwood trees were uprooted and snapped. About 100 trees were damaged on Overshot Court, with many uprooted trees falling in a convergent, crossing manner and pointed to the west-to-north (generally along and left of the tornado track). At least 20 hardwood trees ranging between 10 and 20 inches in diameter were snapped off about 10 feet above the ground. Some of the uprooted trees also fell towards the east. A house on Overshot Court had siding damage, lost a portion of its eave on the northeast side of the house, had a shutter blown off, and a flagpole blown down. Siding from this house was found 120 yards to the northwest of the house.||Eyewitness accounts were taken from several residents along Overshot Court. They all relayed a similar story of relatively quiet conditions followed by a loud and incessant roaring sound, with reduced visibility due to heavy rain and swirling winds. One resident texted that they entered their basement when they heard the loud roar, with the timestamp of that text being 4:57 PM EDT. All residents noted the damage occurred quickly lasting well less than one minute.||As the tornado moved northeastward, it crossed wooded areas south of the Carroll Manor Recreation Council Building on MD-145 Sweet Air Road, where limited tree damage was noted. No damage was noted along Fox Run Court, but as the tornado crossed the 14000 block of Blenheim Road, several trees were damaged; several were uprooted and several were topped. One large 2-foot-in-diameter tree was uprooted facing toward the west, while a trampoline from a residence was blown over 200 yards toward the east, and several softwood pine trees were snapped. The large uprooted tree damaged a section of a covered porch.||The tornado produced only minor tree damage as it moved northeastward from Blenheim Road, and may have lifted briefly as it crossed MD-145 Sweet Air Road just west of Manor Road. As the tornado crossed Manor Road just north of MD-145 Sweet Air Road, minor tree damage was noted mainly with mainly a few large tree branches down.||Farther to the northeast, the tornado produced tree damage to a residence at the end of Cremson Drive off of Manor Road. A large hardwood tree about 20 inches in diameter was twisted off 10 feet up from the ground. A resident at this location described hearing a loud sound akin to a freight train and observed the tornado cause the aforementioned damage. The resident noted he was in his basement because of a Tornado Warning, with the damage occurring 5 minutes after his phone had alerted him to the Tornado Warning.||No further damage was noted to the northeast of the location on Cremson Drive, and the tornado likely lifted before crossing Maple Ridge Court.", "The following events were reported: Flash Flood, Flood. These occurred near station USW00093721, approximately 42.9223 km away, between 2021-06-03 16:44:00 and 2021-06-03 22:00:00. The flood was caused by Heavy Rain. Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 10000.0 and crop damage of 0.0. \n\nEpisode Narrative: Showers and thunderstorms developed, and due to higher amounts of instability and moisture, heavy rain led to instances of flooding and flash flooding in northeastern Maryland. Showers and thunderstorms developed, and due to higher amounts of instability and moisture, heavy rain led to instances of flooding and flash flooding in northeastern Maryland. Showers and thunderstorms developed, and due to higher amounts of instability and moisture, heavy rain led to instances of flooding and flash flooding in northeastern Maryland. Showers and thunderstorms developed, and due to higher amounts of instability and moisture, heavy rain led to instances of flooding and flash flooding in northeastern Maryland.\nEvent Narrative: Cromwell Bridge Road near Cowpens Avenue was closed due to flooding. The stream gauge on Plumtree Run in Bel Air indicated that water rose five feet in less than two hours, reaching minor flood stage of 6 feet. The stream gauge crested at 6.7 feet before falling back below minor flood stage. Water covered Plumtree Road near Plumtree Run. A swift water rescue took place on Patterson Mill Road and East Wheel Road. A swift water rescue took place at the 3900 and 2100 Blocks of Philadelphia Road.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 25.8647 km away, between 2021-06-08 14:59:00 and 2021-06-08 14:59:00. The events included records with measured wind gusts of 39.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A few thunderstorms produced sporadic gusty winds near the upper Chesapeake Bay.\nEvent Narrative: A wind gust of 39 knots (45 MPH) was measured by a mesonet near Annapolis.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 19.6294 km away, between 2021-06-10 11:51:00 and 2021-06-10 14:12:00. The events included records with estimated wind gusts of 43.333333333333336 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 9000.0 and crop damage of 0.0. \n\nEpisode Narrative: Thunderstorms with very heavy rain produced sporadic, minor wind damage. All but one storm seemed to produce sub-severe winds based on the sporadic nature of the damage and the environment unfavorable for severe wind. Thunderstorms with very heavy rain produced sporadic, minor wind damage. All but one storm seemed to produce sub-severe winds based on the sporadic nature of the damage and the environment unfavorable for severe wind. Thunderstorms with very heavy rain produced sporadic, minor wind damage. All but one storm seemed to produce sub-severe winds based on the sporadic nature of the damage and the environment unfavorable for severe wind.\nEvent Narrative: A tree was reported down near the intersection of Court House Drive and Ellicott Mills Drive. Another tree was reported down near the intersection of Church Road and Sylvan Lane. A tree was reported down on MD-175 Jessup Road near Old Jessup Road. Trees blew down on MD-146 Dulaney Valley Road near East Timonium Road. Trees and wires blew down near the intersection of Glen Arm Road and Hooper Lane.", "The following events were reported: Flash Flood, Flood. These occurred near station USW00093721, approximately 26.3614 km away, between 2021-06-10 14:10:00 and 2021-06-10 20:30:00. The flood was caused by Heavy Rain. Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A slow moving cold front dropped into the area from the northeast. The airmass was very warm and humid ahead of the boundary, and that led to the development of showers and thunderstorms with heavy rainfall. The storm motion was slow due to light winds aloft, so the heavy rain led to instances of flooding and flash flooding. A slow moving cold front dropped into the area from the northeast. The airmass was very warm and humid ahead of the boundary, and that led to the development of showers and thunderstorms with heavy rainfall. The storm motion was slow due to light winds aloft, so the heavy rain led to instances of flooding and flash flooding. A slow moving cold front dropped into the area from the northeast. The airmass was very warm and humid ahead of the boundary, and that led to the development of showers and thunderstorms with heavy rainfall. The storm motion was slow due to light winds aloft, so the heavy rain led to instances of flooding and flash flooding. A slow moving cold front dropped into the area from the northeast. The airmass was very warm and humid ahead of the boundary, and that led to the development of showers and thunderstorms with heavy rainfall. The storm motion was slow due to light winds aloft, so the heavy rain led to instances of flooding and flash flooding. A slow moving cold front dropped into the area from the northeast. The airmass was very warm and humid ahead of the boundary, and that led to the development of showers and thunderstorms with heavy rainfall. The storm motion was slow due to light winds aloft, so the heavy rain led to instances of flooding and flash flooding. A slow moving cold front dropped into the area from the northeast. The airmass was very warm and humid ahead of the boundary, and that led to the development of showers and thunderstorms with heavy rainfall. The storm motion was slow due to light winds aloft, so the heavy rain led to instances of flooding and flash flooding. A slow moving cold front dropped into the area from the northeast. The airmass was very warm and humid ahead of the boundary, and that led to the development of showers and thunderstorms with heavy rainfall. The storm motion was slow due to light winds aloft, so the heavy rain led to instances of flooding and flash flooding.\nEvent Narrative: Water was higher than fences in the area of Hillen Road and 35th Street. There were dozens of streets closed in the northeast side of Baltimore City per DPW. Maryland Route 542 Loch Raven Boulevard flooded at Joan Avenue. Vehicle was stranded in high water near the intersection of Joppa Road and Satyr Hill Road. High water was reported in the 2300 Block of Ellen Avenue and the road was impassable. A car was stranded in water near the intersection of Harris Avenue and Rader Avenue. Cars were stranded in water in the parking lot of the Harford Hills Elementary School. Cub Hill Road was closed due to flooding and debris near Cromwell Bride Road and Glen Arm Road.", "The following events were reported: Flood. These occurred near station USW00093721, approximately 21.7782 km away, between 2021-06-11 12:25:00 and 2021-06-11 17:22:00. The flood was caused by Heavy Rain. Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A slow moving cold front continued to drop to the south and west, but low pressure developed along the boundary and there was still anomalously high amounts of moisture in place. Therefore, more heavy rain developed and this led to instances of flooding and flash flooding. A slow moving cold front continued to drop to the south and west, but low pressure developed along the boundary and there was still anomalously high amounts of moisture in place. Therefore, more heavy rain developed and this led to instances of flooding and flash flooding.\nEvent Narrative: A car was stalled in high water on Ruxton Road near Roland Run. The road was in the process of being closed. Jones Falls was out of its banks and onto Union Avenue.", "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00093721, approximately 13.6065 km away, between 2021-06-14 20:39:00 and 2021-06-14 21:20:00. The events included records with hailstones measuring 28.535714285714285 inches.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 135000.0 and crop damage of 0.0. \n\nEpisode Narrative: A cold front spawned several clusters of supercells that produced hail and wind during the evening hours. A cold front spawned several clusters of supercells that produced hail and wind during the evening hours. A cold front spawned several clusters of supercells that produced hail and wind during the evening hours. A cold front spawned several clusters of supercells that produced hail and wind during the evening hours. A cold front spawned several clusters of supercells that produced hail and wind during the evening hours. A cold front spawned several clusters of supercells that produced hail and wind during the evening hours. A cold front spawned several clusters of supercells that produced hail and wind during the evening hours. A cold front spawned several clusters of supercells that produced hail and wind during the evening hours. A cold front spawned several clusters of supercells that produced hail and wind during the evening hours. A cold front spawned several clusters of supercells that produced hail and wind during the evening hours. A cold front spawned several clusters of supercells that produced hail and wind during the evening hours. A cold front spawned several clusters of supercells that produced hail and wind during the evening hours. A cold front spawned several clusters of supercells that produced hail and wind during the evening hours. A cold front spawned several clusters of supercells that produced hail and wind during the evening hours.\nEvent Narrative: Quarter size hail was reported just inside the Baltimore City line east of Catonsville. A tree blew down near a residence on South Beechfield Avenue near Ridge Drive. Two trees blew down near the intersection of Joh Avenue and Coolidge Avenue. Quarter size hail was reported near Arbutus. A tree blew down on Kessler Road. Other trees also blew down in the area, including on I-695 Baltimore Beltway. Quarter size hail was reported in downtown Baltimore City. Golf ball size hail was reported near Columbia. Multiple trees limbs snapped off of trees near the intersection of Ruth Avenue and Lodge Farm Road. Quarter size hail was reported in Elkridge. Quarter to golf ball size hail was reported near Edgemere. Quarter size hail was reported in Rosedale. Trees blew down on MD-270 Furnace Branch Road near MD-10 Arundel Expressway. Around 10:15 PM, a severe thunderstorm produced another, stronger damaging wind gust over Edgemere, Maryland. This most significantly impacted the community along Jones Creek, and then to the southeast along North Point Road. The hardest hit areas were along Waldman, Hughes, and Geise Avenues. About six to twelve large trees were uprooted in various areas in this community, and several large branches were snapped, in addition to numerous downed small branches and leaf debris. Some homes were damaged by falling trees and branches. As the gust moved southeastward, it snapped two power poles along North Point Road near the intersection with Avenue C. However, no damage was noted to trees and farm sheds across the street from the poles. All noted damage was due to a wind gust blowing from the northwest toward the southeast. Peak winds were estimaed to have been 75 MPH. At least one fell onto a structure near the intersection of Lincoln Avenue and Shady Grove Circle. Trees blew down on MD-2 Ritchie Highway near 5th Avenue. Around 9:44 PM, a severe thunderstorm produced a wind gust around 70 MPH in Norwood Heights/Yale Heights, Maryland, in the southwestern portion of Baltimore City. The gust uprooted a few trees in the community, and snapped several large branches. One tree fell on and crushed a parked vehicle. No structural damage to homes was noted by the National Weather Service or emergency management. Along MD-372 Wilkins Avenue, across from the cross street of Calwell Road, three large trees were uprooted on the edge of Loudon Park Cemetery. All damage was blown in one direction from the severe wind gust, toward the southeast. Peak winds were estimated to have been 70 MPH.", "The following events were reported: Marine Hail, Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 18.9674 km away, between 2021-06-14 20:48:00 and 2021-06-14 22:00:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Several clusters of strong to severe thunderstorms produced high winds over the Chesapeake Bay and tidal Potomac River. Several clusters of strong to severe thunderstorms produced high winds over the Chesapeake Bay and tidal Potomac River. Several clusters of strong to severe thunderstorms produced high winds over the Chesapeake Bay and tidal Potomac River. Several clusters of strong to severe thunderstorms produced high winds over the Chesapeake Bay and tidal Potomac River. Several clusters of strong to severe thunderstorms produced high winds over the Chesapeake Bay and tidal Potomac River. Several clusters of strong to severe thunderstorms produced high winds over the Chesapeake Bay and tidal Potomac River. Several clusters of strong to severe thunderstorms produced high winds over the Chesapeake Bay and tidal Potomac River. Several clusters of strong to severe thunderstorms produced high winds over the Chesapeake Bay and tidal Potomac River. Several clusters of strong to severe thunderstorms produced high winds over the Chesapeake Bay and tidal Potomac River. Several clusters of strong to severe thunderstorms produced high winds over the Chesapeake Bay and tidal Potomac River. Several clusters of strong to severe thunderstorms produced high winds over the Chesapeake Bay and tidal Potomac River. Several clusters of strong to severe thunderstorms produced high winds over the Chesapeake Bay and tidal Potomac River. Several clusters of strong to severe thunderstorms produced high winds over the Chesapeake Bay and tidal Potomac River. Several clusters of strong to severe thunderstorms produced high winds over the Chesapeake Bay and tidal Potomac River. Several clusters of strong to severe thunderstorms produced high winds over the Chesapeake Bay and tidal Potomac River.\nEvent Narrative: A wind gust of 43 knots (49 MPH) was measured by a mesonet at Lakeland Elementary and Middle School adjacent to Baltimore Inner Harbor. Wind gusts of up to 39 knots (45 MPH) were measured by a buoy in Baltimore Inner Harbor. A wind gust of 45 knots (52 MPH) was measured by a mesonet at Oriole Park at Camden Yards adjacent to Baltimore Inner Harbor. A thunderstorm produced an estimated wind gust to 34 knots (39 MPH) near a mesonet near Maryland Science Center adjacent to Baltimore Inner Harbor. Wind gusts of up to 58 knots (67 MPH) were measured by a buoy near Francis Scott Key Bridge. A wind gust of 37 knots (43 MPH) was measured by a mesonet at Morrell Park School adjacent to Baltimore Inner Harbor. Wind gusts of up to 39 knots (45 MPH) were measured by a buoy near Hart Miller Island. Wind gusts of up to 43 knots (49 MPH) were measured by a buoy near Tolchester Beach. A wind gust of 35 knots (40 MPH) was measured by a buoy near Greenbury Point. A thunderstorm produced an estimated wind gust to 34 knots (39 MPH) at a buoy near Sandy Point. Wind gusts of up to 42 knots (48 MPH) were measured by a mesonet at Bayside Beach. A wind gust of 37 knots (43 MPH) was measured by a mesonet near Arbutus adjacent to Baltimore Inner Harbor. A wind gust of 57 MPH (50 knots) was measured by a mesonet at the Baltimore Water Taxi terminal adjacent to Baltimore Inner Harbor. A wind gust of 47 knots (54 MPH) was measured by a mesonet at Holly Farm Beach adjacent to the Chesapeake Bay. Penny size hail was reported near Fells Point adjacent to Baltimore Inner Harbor.", "The following events were reported: Flash Flood, Flood. These occurred near station USW00093721, approximately 17.8684 km away, between 2021-06-14 20:58:00 and 2021-06-15 00:00:00. The flood was caused by Heavy Rain. Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front passed through the area during the afternoon of the 14th into the evening and overnight hours. Ahead of the cold front, there was plenty of instability and moisture, so thunderstorms produced heavy rainfall. This led to instances of flooding and flash flooding. A cold front passed through the area during the afternoon of the 14th into the evening and overnight hours. Ahead of the cold front, there was plenty of instability and moisture, so thunderstorms produced heavy rainfall. This led to instances of flooding and flash flooding. A cold front passed through the area during the afternoon of the 14th into the evening and overnight hours. Ahead of the cold front, there was plenty of instability and moisture, so thunderstorms produced heavy rainfall. This led to instances of flooding and flash flooding.\nEvent Narrative: A water rescue occurred near the intersection of Mornington Road and Liberty Parkway. MD-450/Defense Highway was closed between Hermitage Hills Drive and St. Stephens Church Road due to flooding. Several roads were closed due to high water on the western side of the city of Baltimore.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 44.3556 km away, between 2021-06-14 21:49:00 and 2021-06-14 22:13:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front and associated weak area of surface low pressure approached the mid-Atlantic on June 14. A seasonably warm air mass was present ahead of the front, allowing a moderate amount of instability to build over the mid-Atlantic. Moderate to strong wind shear was also present thanks to the presence of a robust upper level disturbance approaching the region. This disturbance, along with the front, provided sufficient forcing for scattered to widespread convection to develop in the interior mid-Atlantic and propagate towards the coast. Some storms became strong to severe in the rather favorable convective environment, posing a primary risk of damaging winds along with some hail. Convection also continued well into the overnight over portions of the area thanks to the good shear and forcing, with convection eventually moving offshore in the pre-dawn hours of the 15th. A cold front and associated weak area of surface low pressure approached the mid-Atlantic on June 14. A seasonably warm air mass was present ahead of the front, allowing a moderate amount of instability to build over the mid-Atlantic. Moderate to strong wind shear was also present thanks to the presence of a robust upper level disturbance approaching the region. This disturbance, along with the front, provided sufficient forcing for scattered to widespread convection to develop in the interior mid-Atlantic and propagate towards the coast. Some storms became strong to severe in the rather favorable convective environment, posing a primary risk of damaging winds along with some hail. Convection also continued well into the overnight over portions of the area thanks to the good shear and forcing, with convection eventually moving offshore in the pre-dawn hours of the 15th.\nEvent Narrative: Tree limbs were downed on MD-289 near Johnsontown Rd. Time estimated from radar. Tree limbs were downed on MD-20 at Rock Hall Ave. Time estimated from radar.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 25.8152 km away, between 2021-06-21 16:53:00 and 2021-06-21 18:04:00.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 46000.0 and crop damage of 0.0. \n\nEpisode Narrative: Lines of severe thunderstorms produced scattered to numerous instances of wind damage across eastern West Virginia, northern Maryland, and northern Virginia. Lines of severe thunderstorms produced scattered to numerous instances of wind damage across eastern West Virginia, northern Maryland, and northern Virginia. Lines of severe thunderstorms produced scattered to numerous instances of wind damage across eastern West Virginia, northern Maryland, and northern Virginia. Lines of severe thunderstorms produced scattered to numerous instances of wind damage across eastern West Virginia, northern Maryland, and northern Virginia. Lines of severe thunderstorms produced scattered to numerous instances of wind damage across eastern West Virginia, northern Maryland, and northern Virginia. Lines of severe thunderstorms produced scattered to numerous instances of wind damage across eastern West Virginia, northern Maryland, and northern Virginia. Lines of severe thunderstorms produced scattered to numerous instances of wind damage across eastern West Virginia, northern Maryland, and northern Virginia. Lines of severe thunderstorms produced scattered to numerous instances of wind damage across eastern West Virginia, northern Maryland, and northern Virginia. Lines of severe thunderstorms produced scattered to numerous instances of wind damage across eastern West Virginia, northern Maryland, and northern Virginia. Lines of severe thunderstorms produced scattered to numerous instances of wind damage across eastern West Virginia, northern Maryland, and northern Virginia. Lines of severe thunderstorms produced scattered to numerous instances of wind damage across eastern West Virginia, northern Maryland, and northern Virginia. Lines of severe thunderstorms produced scattered to numerous instances of wind damage across eastern West Virginia, northern Maryland, and northern Virginia. Lines of severe thunderstorms produced scattered to numerous instances of wind damage across eastern West Virginia, northern Maryland, and northern Virginia. Lines of severe thunderstorms produced scattered to numerous instances of wind damage across eastern West Virginia, northern Maryland, and northern Virginia. Lines of severe thunderstorms produced scattered to numerous instances of wind damage across eastern West Virginia, northern Maryland, and northern Virginia. Lines of severe thunderstorms produced scattered to numerous instances of wind damage across eastern West Virginia, northern Maryland, and northern Virginia.\nEvent Narrative: A tree blew down in the 4400 block of Cherry Tree Lane. A tree blew down on eastbound I-70 near Exit 87A/US-29 Columbia Pike. Trees blew down near the intersection of Ivy Mill Road and Cockeys Mill Road. Trees blew down near the intersection of Trenton Road and Dark Hollow Road. A couple of trees blew down on Gunpowder Road. Trees blew down on Cotter Road. Trees blew down near the intersection of Mount Zion Road and Dover Road. Trees blew down on Church Lane. Trees blew down on Log Trail Way. Trees blew down near the intersection of Gwynnbrook Avenue and Owings Mills Boulevard. Trees blew down near the intersection of Garrison Forest Road and Saint Thomas Lane. A tree blew down on eastbound I-70 near Exit 91A/northbound I-695 Baltimore Beltway Inner Loop. Trees blew down near the intersection of Sugarcone Road and Greenspring Avenue, and on Greenspring Avenue near Green Summit Road. There were at least half a dozen reports of trees blown down in the northwestern part of Baltimore City. A tree blew down on Bellona Avenue near Dunlora Road. A tree blew down near the intersection of Stevenson Lane and Mitten Lane. Trees blew down near the intersection of Hampton Lane and MD-146 Dulaney Valley Road. A tree blew down on Brock Bridge Road near River Bridge Way. There were three reports of trees and wires blown down in the Catonsville area. A tree blew down on Pleasantville Road near Laurel Brook Road. A tree blew down on Benfield Boulevard near Veterans Highway. A wind gust of 65 MPH (56 knots) was measured by a mesonet near Cape Saint Claire. Trees blew down on hole 16 at Bay Hills Golf Club.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 23.1145 km away, between 2021-06-21 17:20:00 and 2021-06-21 22:25:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Several lines of thunderstorms produced strong wind gusts over the Chesapeake Bay. Several lines of thunderstorms produced strong wind gusts over the Chesapeake Bay. Several lines of thunderstorms produced strong wind gusts over the Chesapeake Bay. Several lines of thunderstorms produced strong wind gusts over the Chesapeake Bay. Several lines of thunderstorms produced strong wind gusts over the Chesapeake Bay. Several lines of thunderstorms produced strong wind gusts over the Chesapeake Bay. Several lines of thunderstorms produced strong wind gusts over the Chesapeake Bay.\nEvent Narrative: A wind gust of 34 knots (39 MPH) was measured by a mesonet at Oriole Park at Camden Yards adjacent to Baltimore Inner Harbor. A thunderstorm produced an estimated wind gust to 34 knots (39 MPH) near a mesonet at Maryland Science Center adjacent to Baltimore Inner Harbor. A thunderstorm produced an estimated wind gust to 34 knots (39 MPH) near a buoy near Francis Scott Key Bridge. A wind gust of 35 knots (40 MPH) was measured by a buoy near Hart Miller Island. A thunderstorm produced an estimated wind gust to 34 knots (39 MPH) near a buoy near Annapolis. A thunderstorm produced an estimated wind gust to 34 knots (39 MPH) near the ASOS at Annapolis U.S. Naval Academy adjacent to the Chesapeake Bay. A thunderstorm produced an estimated wind gust to 34 knots (39 MPH) near a buoy near Thomas Point.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 17.467 km away, between 2021-06-30 19:05:00 and 2021-06-30 19:20:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A line of thunderstorms produced gusty winds during the early to mid evening hours, mainly over the upper Chesapeake Bay. A line of thunderstorms produced gusty winds during the early to mid evening hours, mainly over the upper Chesapeake Bay. A line of thunderstorms produced gusty winds during the early to mid evening hours, mainly over the upper Chesapeake Bay. A line of thunderstorms produced gusty winds during the early to mid evening hours, mainly over the upper Chesapeake Bay.\nEvent Narrative: A wind gust of 34 knots (39 MPH) was measured by a mesonet at the Maryland Science Center in Baltimore adjacent to Baltimore Inner Harbor. A wind gust of 34 knots (39 MPH) was measured by the AWOS at Martin State Airport adjacent to the upper Chesapeake Bay. A thunderstorm produced estimated wind gusts to 34 knots (39 MPH) near a mesonet at Oriole Park at Camden Yards adjacent to Baltimore Inner Harbor. A thunderstorm produced an estimated wind gust to 34 knots (39 MPH) near a buoy near Francis Scott Key Bridge.", "The following events were reported: Funnel Cloud, Hail, Thunderstorm Wind. These occurred near station USW00093721, approximately 25.594 km away, between 2021-07-01 13:21:00 and 2021-07-01 18:37:00. The events included records with hailstones measuring 35.61666666666667 inches.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 259000.0 and crop damage of 0.0. \n\nEpisode Narrative: Two rounds of severe thunderstorms produced two tornadoes, hail, and widespread wind damage (some significant) across the DC metro and central Maryland, with spottier wind damage extending into the Baltimore area. Two rounds of severe thunderstorms produced two tornadoes, hail, and widespread wind damage (some significant) across the DC metro and central Maryland, with spottier wind damage extending into the Baltimore area. Two rounds of severe thunderstorms produced two tornadoes, hail, and widespread wind damage (some significant) across the DC metro and central Maryland, with spottier wind damage extending into the Baltimore area. Two rounds of severe thunderstorms produced two tornadoes, hail, and widespread wind damage (some significant) across the DC metro and central Maryland, with spottier wind damage extending into the Baltimore area. Two rounds of severe thunderstorms produced two tornadoes, hail, and widespread wind damage (some significant) across the DC metro and central Maryland, with spottier wind damage extending into the Baltimore area. Two rounds of severe thunderstorms produced two tornadoes, hail, and widespread wind damage (some significant) across the DC metro and central Maryland, with spottier wind damage extending into the Baltimore area. Two rounds of severe thunderstorms produced two tornadoes, hail, and widespread wind damage (some significant) across the DC metro and central Maryland, with spottier wind damage extending into the Baltimore area. Two rounds of severe thunderstorms produced two tornadoes, hail, and widespread wind damage (some significant) across the DC metro and central Maryland, with spottier wind damage extending into the Baltimore area. Two rounds of severe thunderstorms produced two tornadoes, hail, and widespread wind damage (some significant) across the DC metro and central Maryland, with spottier wind damage extending into the Baltimore area. Two rounds of severe thunderstorms produced two tornadoes, hail, and widespread wind damage (some significant) across the DC metro and central Maryland, with spottier wind damage extending into the Baltimore area. Two rounds of severe thunderstorms produced two tornadoes, hail, and widespread wind damage (some significant) across the DC metro and central Maryland, with spottier wind damage extending into the Baltimore area. Two rounds of severe thunderstorms produced two tornadoes, hail, and widespread wind damage (some significant) across the DC metro and central Maryland, with spottier wind damage extending into the Baltimore area. Two rounds of severe thunderstorms produced two tornadoes, hail, and widespread wind damage (some significant) across the DC metro and central Maryland, with spottier wind damage extending into the Baltimore area. Two rounds of severe thunderstorms produced two tornadoes, hail, and widespread wind damage (some significant) across the DC metro and central Maryland, with spottier wind damage extending into the Baltimore area. Two rounds of severe thunderstorms produced two tornadoes, hail, and widespread wind damage (some significant) across the DC metro and central Maryland, with spottier wind damage extending into the Baltimore area. Two rounds of severe thunderstorms produced two tornadoes, hail, and widespread wind damage (some significant) across the DC metro and central Maryland, with spottier wind damage extending into the Baltimore area.\nEvent Narrative: Quarter size hail was reported near Glenn Dale. Quarter size hail was reported southeast of Glenn Dale. Hail up to golf ball size was reported northwest of Bowie. Quarter size hail was reported just north of Bowie. Hail up to ping pong ball size was reported near Crofton. Quarter size hail was reported just south of Crofton. A tree blew down on MD-450 Defense Highway. There were about a half a dozen calls for trees blown down in western Baltimore City. A couple dozen trees and large limbs were blown down near Bowie. Trees blew down near the intersection of MD-197 Collington Road near Lyle Lane, Gallant Fox Lane, and Tulip Grove Drive. Trees blew down on MD-165 Baldwin Mill Road. Numerous trees blew down just southeast of Bowie, including at residence where about a dozen 100 foot tall trees snapped near the top. Several dozen trees, wires, and poles blew down near Parole and Annapolis. Trees blew down on US-50 John Hanson Highway near MD-2 Solomons Island Road. Trees and wires blew down near the intersection of MD-450 Governor Ritchie Highway and Brice Road. A wind gust of 55 knots (63 MPH) was measured by a mesonet at the Chesapeake Bay Bridge. A trained spotter reported a funnel cloud briefly descending from a rotating wall cloud to the south of Westminster. No touchdown was visible and no damage was observed. Several dozen trees, wires, and poles blew down near Riva and Londontowne. Trees blew down on MD-424 Davidsonville Road near Governor Bridge Road, and near the intersection of MD-450 Defense Highway and MD-424 Davidsonville Road. A large Leyland Cyprus tree was blown over at a nearby residence. Trees blew down near the intersection of Riva Road and Beards Point Road. A wind gust of 58 knots (66 MPH) was measured by the ASOS at the U.S. Naval Academy (KNAK).", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 34.64 km away, between 2021-07-01 14:12:00 and 2021-07-01 21:18:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Multiple lines of severe thunderstorms produced gusty winds over the tidal Potomac River and Chesapeake Bay, and a brief waterspout as a tornado crossed the upper tidal Potomac River between Arlington and DC. Multiple lines of severe thunderstorms produced gusty winds over the tidal Potomac River and Chesapeake Bay, and a brief waterspout as a tornado crossed the upper tidal Potomac River between Arlington and DC. Multiple lines of severe thunderstorms produced gusty winds over the tidal Potomac River and Chesapeake Bay, and a brief waterspout as a tornado crossed the upper tidal Potomac River between Arlington and DC. Multiple lines of severe thunderstorms produced gusty winds over the tidal Potomac River and Chesapeake Bay, and a brief waterspout as a tornado crossed the upper tidal Potomac River between Arlington and DC. Multiple lines of severe thunderstorms produced gusty winds over the tidal Potomac River and Chesapeake Bay, and a brief waterspout as a tornado crossed the upper tidal Potomac River between Arlington and DC. Multiple lines of severe thunderstorms produced gusty winds over the tidal Potomac River and Chesapeake Bay, and a brief waterspout as a tornado crossed the upper tidal Potomac River between Arlington and DC. Multiple lines of severe thunderstorms produced gusty winds over the tidal Potomac River and Chesapeake Bay, and a brief waterspout as a tornado crossed the upper tidal Potomac River between Arlington and DC. Multiple lines of severe thunderstorms produced gusty winds over the tidal Potomac River and Chesapeake Bay, and a brief waterspout as a tornado crossed the upper tidal Potomac River between Arlington and DC. Multiple lines of severe thunderstorms produced gusty winds over the tidal Potomac River and Chesapeake Bay, and a brief waterspout as a tornado crossed the upper tidal Potomac River between Arlington and DC. Multiple lines of severe thunderstorms produced gusty winds over the tidal Potomac River and Chesapeake Bay, and a brief waterspout as a tornado crossed the upper tidal Potomac River between Arlington and DC. Multiple lines of severe thunderstorms produced gusty winds over the tidal Potomac River and Chesapeake Bay, and a brief waterspout as a tornado crossed the upper tidal Potomac River between Arlington and DC. Multiple lines of severe thunderstorms produced gusty winds over the tidal Potomac River and Chesapeake Bay, and a brief waterspout as a tornado crossed the upper tidal Potomac River between Arlington and DC. Multiple lines of severe thunderstorms produced gusty winds over the tidal Potomac River and Chesapeake Bay, and a brief waterspout as a tornado crossed the upper tidal Potomac River between Arlington and DC. Multiple lines of severe thunderstorms produced gusty winds over the tidal Potomac River and Chesapeake Bay, and a brief waterspout as a tornado crossed the upper tidal Potomac River between Arlington and DC. Multiple lines of severe thunderstorms produced gusty winds over the tidal Potomac River and Chesapeake Bay, and a brief waterspout as a tornado crossed the upper tidal Potomac River between Arlington and DC. Multiple lines of severe thunderstorms produced gusty winds over the tidal Potomac River and Chesapeake Bay, and a brief waterspout as a tornado crossed the upper tidal Potomac River between Arlington and DC. Multiple lines of severe thunderstorms produced gusty winds over the tidal Potomac River and Chesapeake Bay, and a brief waterspout as a tornado crossed the upper tidal Potomac River between Arlington and DC.\nEvent Narrative: A thunderstorm produced an estimated wind gust to 34 knots (39 MPH) near a buoy near Sandy Point. A thunderstorm produced an estimated wind gust to 34 knots (39 MPH) near a buoy near Tolly Point. Wind gusts of up to 50 knots (58 MPH) were measured by a buoy near Greenbury Point. Wind gusts of up to 41 knots (47 MPH) were measured by a buoy near Tolly Point. A wind gust of 40 knots (46 MPH) was measured by a buoy near Saunders Point Light. Wind gusts of up to 43 knots (49 MPH) were measured by a buoy near Sandy Point. Wind gusts of up to 36 knots (41 MPH) were measured by a buoy near Annapolis. Wind gusts of up to 55 knots (63 MPH) were measured by a buoy near Thomas Point. A wind gust of 37 knots (43 MPH) was measured by a mesonet near Wiggins. A thunderstorm produced an estimated wind gust to 34 knots (39 MPH) near a buoy near Annapolis. A wind gust of 57 knots (66 MPH) was measured by a mesonet on the east side of the US-50/US-301 Chesapeake Bay Bridge. A wind gust of 40 knots (46 MPH) was measured by a mesonet in near Crab Alley Bay. A wind gust of 47 knots (54 MPH) was measured by a mesonet on US-50/US-301 Kent Narrows Bridge. A wind gust of 40 knots (46 MPH) was measured by a mesonet at the US-50/US-301 John Hanson Highway/MD-2 Solomons Island Road interchange adjacent to the Chesapeake Bay. A thunderstorm produced an estimated wind gust of 34 knots (39 MPH) near a buoy near Annapolis. A wind gust of 38 knots (44 MPH) was measured by a buoy near Thomas Point. A thunderstorm produced an estimated wind gust to 34 knots (39 MPH) near a buoy near Tolchester Beach.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 38.0261 km away, between 2021-07-01 15:00:00 and 2021-07-01 15:00:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: After a significant heatwave, a cold front approached the mid-Atlantic on July 1, 2021. A potent mid-level trough was also digging southward through southern Ontario and into the Great Lakes region, and a strong upper level jet streak was present downstream the trough axis, over the interior mid-Atlantic and northern New England. This strong upper level forcing combined with the approaching front and a lingering warm, moist air mass ahead of it caused widespread thunderstorm development on July 1. Storms occurred almost exclusively south of Interstate 78, in the environment of best instability. A number of storms became severe, taking the form of mainly linear and multi-cellular clusters but with some embedded supercellular characteristics. Straight line wind damage was the primary hazard, with a number of reports of downed trees and power outages due to winds. With the cold front remaining to the west, some storm activity continued into the overnight, but storm coverage and intensity gradually waned with the loss of daytime heating and the overturning of the atmosphere from earlier storms.\nEvent Narrative: Trees and utility wires were down with debris on the roadway along MD-8 south of Kent Manor Dr. Time estimated from radar.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 14.1413 km away, between 2021-07-07 15:10:00 and 2021-07-07 15:14:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A few thunderstorms produced gusty winds near Baltimore Harbor. A few thunderstorms produced gusty winds near Baltimore Harbor. A few thunderstorms produced gusty winds near Baltimore Harbor.\nEvent Narrative: A wind gust of 36 knots (41 MPH) was measured by a mesonet near Fells Point adjacent to Baltimore Inner Harbor. A thunderstorm produced an estimated wind gust to 34 knots (39 MPH) near a mesonet near the Baltimore Water Taxi terminal. A thunderstorm produced an estimated wind gust to 34 knots (39 MPH) near a mesonet at the Maryland Science Center adjacent to Baltimore Inner Harbor.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 22.0012 km away, between 2021-07-07 15:10:00 and 2021-07-07 15:45:00. The events included records with estimated wind gusts of 52.5 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 75000.0 and crop damage of 0.0. \n\nEpisode Narrative: Isolated severe thunderstorms produced localized wind damage and sporadic hail over portions of northwestern Virginia and northeastern Maryland. Isolated severe thunderstorms produced localized wind damage and sporadic hail over portions of northwestern Virginia and northeastern Maryland. Isolated severe thunderstorms produced localized wind damage and sporadic hail over portions of northwestern Virginia and northeastern Maryland. Isolated severe thunderstorms produced localized wind damage and sporadic hail over portions of northwestern Virginia and northeastern Maryland. Isolated severe thunderstorms produced localized wind damage and sporadic hail over portions of northwestern Virginia and northeastern Maryland. Isolated severe thunderstorms produced localized wind damage and sporadic hail over portions of northwestern Virginia and northeastern Maryland.\nEvent Narrative: A tree blew down onto wires near the intersection of Palladi Drive and Wilkens Avenue. Southbound MD-166 South Rolling Road was closed due to fallen trees between Wilkens Avenue and Highfields Drive. A tree blew down onto wires in the 6200 block of Gilston Park Road. A tree blew down onto a house in the 1000 block of Marleigh Cirlce. A tree blew down onto a house along Coniston Road. A tree blew down near the intersection of Old Court Road and Ruxton Road. Many large trees were blown down near the intersection of West Joppa Road and Bellona Avenue. A tree blew down onto a house in the 2200 block of Stryker Court. A tree blew down onto two vehicles in the 2300 block of Chetwood Circle. A tree blew down onto a house in the 600 block of Sherwood Road. A tree blew down onto a house in the 3100 block of Baker Street.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 37.9145 km away, between 2021-07-09 15:00:00 and 2021-07-09 16:10:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 5000.0 and crop damage of 0.0. \n\nEpisode Narrative: Scattered thunderstorms produced several instances of wind damage during the afternoon hours, mainly over central and southern Maryland. Scattered thunderstorms produced several instances of wind damage during the afternoon hours, mainly over central and southern Maryland.\nEvent Narrative: Trees blew down onto wires causing a fire near the intersection of MD-27 Ridge Road and Windsor Forest Road. Tree damage was reported near Londontowne and Edgewater, including a tree that fell onto a fence near the intersection of Bishop Road and Londontown Road.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 34.9616 km away, between 2021-07-09 15:55:00 and 2021-07-09 16:32:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Scattered thunderstorms produced gusty winds over portions of the tidal Potomac River and the Chesapeake Bay. Scattered thunderstorms produced gusty winds over portions of the tidal Potomac River and the Chesapeake Bay. Scattered thunderstorms produced gusty winds over portions of the tidal Potomac River and the Chesapeake Bay. Scattered thunderstorms produced gusty winds over portions of the tidal Potomac River and the Chesapeake Bay.\nEvent Narrative: A wind gust of 38 knots (44 MPH) was measured by the AWOS at Lee Airport (KANP). Wind gusts of 34 knots (39 MPH) were measured by a buoy near Saunders Point Lighthouse. A wind gust of 47 knots (54 MPH) was measured by a mesonet near Galesville. A thunderstorm produced an estimated wind gust to 34 knots (39 MPH) near a buoy near Thomas Point.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 47.2407 km away, between 2021-07-12 17:45:00 and 2021-07-12 18:45:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 2000.0 and crop damage of 0.0. \n\nEpisode Narrative: Scattered thunderstorms produced several instances of wind damage across northern Maryland, eastern West Virginia and northwestern Virginia. Scattered thunderstorms produced several instances of wind damage across northern Maryland, eastern West Virginia and northwestern Virginia.\nEvent Narrative: A tree blew down across the roadway near the intersection of Pocock Road and Ebenezer Road. A tree blew down near the intersection of Laurel Bush Road and Burgh Westra Way.", "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00093721, approximately 27.9451 km away, between 2021-07-17 12:45:00 and 2021-07-17 15:10:00. The events included records with hailstones measuring 50.083333333333336 inches.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 628000.0 and crop damage of 0.0. \n\nEpisode Narrative: Showers and thunderstorms produced scattered instances of wind damage during the afternoon and early evening hours. Showers and thunderstorms produced scattered instances of wind damage during the afternoon and early evening hours. Showers and thunderstorms produced scattered instances of wind damage during the afternoon and early evening hours. Showers and thunderstorms produced scattered instances of wind damage during the afternoon and early evening hours. Showers and thunderstorms produced scattered instances of wind damage during the afternoon and early evening hours. Showers and thunderstorms produced scattered instances of wind damage during the afternoon and early evening hours. Showers and thunderstorms produced scattered instances of wind damage during the afternoon and early evening hours. Showers and thunderstorms produced scattered instances of wind damage during the afternoon and early evening hours. Showers and thunderstorms produced scattered instances of wind damage during the afternoon and early evening hours. Showers and thunderstorms produced scattered instances of wind damage during the afternoon and early evening hours. Showers and thunderstorms produced scattered instances of wind damage during the afternoon and early evening hours. Showers and thunderstorms produced scattered instances of wind damage during the afternoon and early evening hours.\nEvent Narrative: Multiple trees blew down near the Liberty Reservoir. A tree blew down on Oakland Mills Road near MD-26 Liberty Road. A tree blew down onto a vehicle near the intersection of Clearfield Circle and Tally Ho Road. A tree blew down on MD-25 Falls Road at MD-131 West Seminary Avenue. Trees blew down on MD-133 Old Court Road near MD-25 Falls Road. Multiple trees blew down in Cockeysville. Multiple trees blew down in and around Long Green. Trees blew down in Parkville. Quarter size hail was reported near Rosedale. A tree blew down on Bushey Road near MD-854 Old Washington Road. Two large trees fell onto an apartment building on Garden Drive causing significant structural damage. A tree blew down on Delaware Avenue. A tree blew down onto a mobile home on Beachwood Avenue near Bletzer Road. Trees and wires blew down on eastbound US-40 Pulaski Highway at Chesaco Avenue. Three trees blew down on Saffa Drive. Trees and wires blew down on westbound MD-150 Eastern Avenue at Diamond Point Road, on MD-150 Eastern Boulevard at Old Eastern Avenue, and on eastbound MD-151 North Point Boulevard prior to I-695 Baltimore Beltway. Trees blew down on I-695 Baltimore Beltway Outer Loop at Exit 42/MD-151 North Point Boulevard. Several trees blew down in the Glen Burnie area, including a tree that blew down into the roadway at the intersection of Arundel Corporation Road and Morris Hill Avenue. A couple of trees and wires blew down leading to the road being blocked near the intersection of MD-650 New Hampshire Avenue and Brighton Dam Road.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 21.3484 km away, between 2021-07-17 14:46:00 and 2021-07-17 17:00:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Thunderstorms produced scattered instances of gusty winds during the afternoon and evening hours. Thunderstorms produced scattered instances of gusty winds during the afternoon and evening hours. Thunderstorms produced scattered instances of gusty winds during the afternoon and evening hours. Thunderstorms produced scattered instances of gusty winds during the afternoon and evening hours. Thunderstorms produced scattered instances of gusty winds during the afternoon and evening hours. Thunderstorms produced scattered instances of gusty winds during the afternoon and evening hours. Thunderstorms produced scattered instances of gusty winds during the afternoon and evening hours. Thunderstorms produced scattered instances of gusty winds during the afternoon and evening hours.\nEvent Narrative: A thunderstorm produced an estimated wind gust to 34 knots (39 MPH) near a buoy in Baltimore Inner Harbor. A wind gust of 39 knots (45 MPH) was measured by a mesonet in Essex adjacent to the upper Chesapeake Bay. A wind gust of 37 knots (43 MPH) was measured by the AWOS at Martin State Airport (KMTN). A thunderstorm produced estimated wind gusts to 34 knots (39 MPH) near a mesonet on Colonial Beach Road adjacent to the upper Chesapeake Bay. Wind gusts of up to 42 knots (48 MPH) were measured by a buoy near Francis Scott Key Bridge. A wind gust of 38 knots (44 MPH) was measured by a mesonet at Bayside Beach. A wind gust of 34 knots (39 MPH) was measured by a mesonet in Fells Point adjacent to Baltimore Inner Harbor. Wind gusts of up to 37 knots (43 MPH) were measured by a buoy near Tolchester Beach.", "The following events were reported: Flash Flood, Flood. These occurred near station USW00093721, approximately 21.0685 km away, between 2021-07-17 14:58:00 and 2021-07-17 19:30:00. The flood was caused by Heavy Rain. Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Showers and thunderstorms produced scattered instances of flooding and flash flooding across northeastern Maryland. Showers and thunderstorms produced scattered instances of flooding and flash flooding across northeastern Maryland. Showers and thunderstorms produced scattered instances of flooding and flash flooding across northeastern Maryland. Showers and thunderstorms produced scattered instances of flooding and flash flooding across northeastern Maryland. Showers and thunderstorms produced scattered instances of flooding and flash flooding across northeastern Maryland. Showers and thunderstorms produced scattered instances of flooding and flash flooding across northeastern Maryland. Showers and thunderstorms produced scattered instances of flooding and flash flooding across northeastern Maryland. Showers and thunderstorms produced scattered instances of flooding and flash flooding across northeastern Maryland. Showers and thunderstorms produced scattered instances of flooding and flash flooding across northeastern Maryland. Showers and thunderstorms produced scattered instances of flooding and flash flooding across northeastern Maryland. Showers and thunderstorms produced scattered instances of flooding and flash flooding across northeastern Maryland.\nEvent Narrative: Several water rescues via boat occurred on East Pulaski Highway. Route 7 near Hamilton Avenue was closed due to flooding. The roadway was flooded at the corner of Cheseco Avenue and Philadelphia Road. Emergency Management reported multiple road closures due to ongoing flooding. Northpoint Boulevard near Charlesmont Road was closed due to flooding. Two vehicles were stranded in water along Erdman Avenue near Ashland Avenue. A vehicle was under water at Route 40 near Pulaski Tire. Sollers Point Road near Louth Road was closed due to high water. There were reports off vehicles filling up with water at the corner of Franklin Avenue. A part of Route 695 was closed near exit 38 due to high water. A vehicle was stuck in high water on Chesnut Street.", "The following events were reported: Lightning, Thunderstorm Wind. These occurred near station USW00093721, approximately 37.7864 km away, between 2021-07-21 13:05:00 and 2021-07-21 13:11:00.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 3500.0 and crop damage of 0.0. \n\nEpisode Narrative: Several thunderstorms ahead of a cold front produced widely scattered instances of wind damage. Several thunderstorms ahead of a cold front produced widely scattered instances of wind damage.\nEvent Narrative: A lightning strike broke a branch that fell onto wires causing a small fire in the 14400 block of MD-25 Falls Road. A tree blew down on southbound MD-25 Falls Road at Geist Road. A tree blew down near the intersection of Beaver Dam Road and Warren Road.", "The following events were reported: Thunderstorm Wind, Tornado. These occurred near station USW00093721, approximately 18.517 km away, between 2021-07-29 15:20:00 and 2021-07-29 16:23:00.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 67000.0 and crop damage of 0.0. \n\nEpisode Narrative: Supercell thunderstorms produced large hail, damaging wind and a tornado during the afternoon hours. The hardest hit areas were near Columbia, Maryland, and near Falmouth, Virginia. Supercell thunderstorms produced large hail, damaging wind and a tornado during the afternoon hours. The hardest hit areas were near Columbia, Maryland, and near Falmouth, Virginia. Supercell thunderstorms produced large hail, damaging wind and a tornado during the afternoon hours. The hardest hit areas were near Columbia, Maryland, and near Falmouth, Virginia. Supercell thunderstorms produced large hail, damaging wind and a tornado during the afternoon hours. The hardest hit areas were near Columbia, Maryland, and near Falmouth, Virginia. Supercell thunderstorms produced large hail, damaging wind and a tornado during the afternoon hours. The hardest hit areas were near Columbia, Maryland, and near Falmouth, Virginia. Supercell thunderstorms produced large hail, damaging wind and a tornado during the afternoon hours. The hardest hit areas were near Columbia, Maryland, and near Falmouth, Virginia. Supercell thunderstorms produced large hail, damaging wind and a tornado during the afternoon hours. The hardest hit areas were near Columbia, Maryland, and near Falmouth, Virginia.\nEvent Narrative: Tree damage was reported near Reese, including a tree that blew down on Arnold Road near Poole Road. Tree damage was reported near Gaither and Woodstock, including a tree that blew down near the intersection of Gaither Road and Forsythe Road. A tree and light pole were damaged near Woodstock. Trees blew down on westbound US-40 Baltimore National Pike at Bethany Lane. A tree blew down near the intersection of Green Mountain Circle and Painted Cup. A tree blew down near the intersection of Governor Warfield Parkway and Little Patuxent Parkway. Several trees blew down and heavy metal barrels were flipped over near the intersection of Dorsey Road and Arundel Avenue. A wind gust of 54 knots (62 MPH) was measured by the ASOS at Baltimore-Washington International Thurgood Marshall Airport (KBWI). A brief EF0 tornado touched down at the Snowden Square shopping mall. Damage was limited to a quarter-mile path, and peak wind gusts were estimated to have been around 70 mph.||Initial tree damage was noted in front of the Goodwill store where two ornamental trees were snapped at their base. Small branch and leaf litter was noted as the tornado passed over the open parking lot towards a BJs store. As the tornado passed over a BJ`s store and tire center, a section of the wall facade, estimated about 50 feet by 20 feet, was removed. The affected wall was on the opposite side from the direction of storm motion. An employee at the tire center noted that nearby shopping carts were lofted and then rapidly blown to the north. The store manager noted the time of the incident from a video taken in the store shortly after it happened. That time matched the time that a tight tornadic circulation with hook echo was noted right over the shopping center by the nearby TBWI terminal doppler weather radar. TBWI|radar had a good view of the event, and was just 10 miles away and sampling only 600 feet off the ground over the shopping center.||Final damage was noted to two more mid-sized trees at the end of Snowden Square Drive. Large branches were snapped off and thrown in multiple directions, north to southeast. Trash and debris was also noted to have been blown to the southeast into an adjacent field. No further damage was noted past this point.", "The following events were reported: Waterspout. These occurred near station USW00093721, approximately 44.0837 km away, between 2021-08-01 05:55:00 and 2021-08-01 06:05:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Several waterspouts were reported over the Chesapeake Bay in the morning, with localized gusty winds over the upper tidal Potomac River in the evening.\nEvent Narrative: A few waterspouts were spotted offshore of Deale, one with a spray ring.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 32.5033 km away, between 2021-08-09 17:51:00 and 2021-08-09 17:51:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 2000.0 and crop damage of 0.0. \n\nEpisode Narrative: A cluster of thunderstorms produced a few downbursts from Northeast DC into nearby adjacent metro Maryland and over southeastern Anne Arundel County.\nEvent Narrative: Several trees blew down northwest of Galesville, including near the intersection of MD-2 Solomons Island Road and Mill Swamp Road.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 28.9748 km away, between 2021-08-10 17:30:00 and 2021-08-10 17:52:00. The events included records with estimated wind gusts of 52.5 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 17000.0 and crop damage of 0.0. \n\nEpisode Narrative: A lee pressure trough ignited thunderstorms in a strongly unstable environment. The strongest thunderstorms produced severe downbursts and sporadic hail. A lee pressure trough ignited thunderstorms in a strongly unstable environment. The strongest thunderstorms produced severe downbursts and sporadic hail.\nEvent Narrative: Trees blew down on I-695 Baltimore Beltway Inner Loop at Exit 22/Greenspring Avenue. About a dozen other trees, branches and wires were reported blown down between Pikesville and Towson. Multiple trees blew down near the intersection of Harwood Road and Lankford Road.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 26.6184 km away, between 2021-08-10 17:45:00 and 2021-08-10 18:12:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A lee pressure trough ignited thunderstorms in a strongly unstable environment. The strongest thunderstorms produced severe downbursts and sporadic hail. A lee pressure trough ignited thunderstorms in a strongly unstable environment. The strongest thunderstorms produced severe downbursts and sporadic hail. A lee pressure trough ignited thunderstorms in a strongly unstable environment. The strongest thunderstorms produced severe downbursts and sporadic hail. A lee pressure trough ignited thunderstorms in a strongly unstable environment. The strongest thunderstorms produced severe downbursts and sporadic hail. A lee pressure trough ignited thunderstorms in a strongly unstable environment. The strongest thunderstorms produced severe downbursts and sporadic hail. A lee pressure trough ignited thunderstorms in a strongly unstable environment. The strongest thunderstorms produced severe downbursts and sporadic hail. A lee pressure trough ignited thunderstorms in a strongly unstable environment. The strongest thunderstorms produced severe downbursts and sporadic hail.\nEvent Narrative: A thunderstorm produced an estimated wind gust to 34 knots (39 MPH) near the ASOS at the U.S. Naval Academy adjacent to the Chesapeake Bay. A thunderstorm produced an estimated wind gust to 34 knots (39 MPH) near a buoy near Greenbury Point. A wind gust of 40 knots (46 MPH) was measured by a buoy near Thomas Point. A thunderstorm produced an estimated wind gust to 34 knots (39 MPH) near a buoy near Saunders Point Light. Wind gusts of up to 40 knots (46 MPH) were measured by a buoy near Hart Miller Island. A wind gust of 35 knots (40 MPH) was measured by a mesonet at the Maryland Science Center adjacent to Baltimore Inner Harbor. Wind gusts of up to 36 knots (41 MPH) were measured by a mesonet at Oriole Park at Camden Yards adjacent to Baltimore Inner Harbor.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 31.5059 km away, between 2021-08-11 16:00:00 and 2021-08-11 16:50:00. The events included records with estimated wind gusts of 47.5 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 8000.0 and crop damage of 0.0. \n\nEpisode Narrative: A lee pressure trough and weak cold front combined to ignite numerous thunderstorms in a strongly unstable environment. The strongest thunderstorms produced severe wind gusts and sporadic hail. A lee pressure trough and weak cold front combined to ignite numerous thunderstorms in a strongly unstable environment. The strongest thunderstorms produced severe wind gusts and sporadic hail. A lee pressure trough and weak cold front combined to ignite numerous thunderstorms in a strongly unstable environment. The strongest thunderstorms produced severe wind gusts and sporadic hail. A lee pressure trough and weak cold front combined to ignite numerous thunderstorms in a strongly unstable environment. The strongest thunderstorms produced severe wind gusts and sporadic hail.\nEvent Narrative: A tree was reported down on Cuba Road near Western Run Road. Wires blew down in the 7000 block of Bridgewood Drive. A tree blew down onto power lines in the 11000 block of Raphel Road. A large tree limb blew down onto wires causing a fire in the 10000 block of Gunridge Circle. A tree blew down onto power lines in the 11000 block of MD-150 Eastern Avenue.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 28.1106 km away, between 2021-08-11 16:42:00 and 2021-08-11 17:30:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A lee pressure trough and weak cold front combined to ignite numerous thunderstorms in a strongly unstable environment. The strongest thunderstorms produced severe wind gusts and sporadic hail. A lee pressure trough and weak cold front combined to ignite numerous thunderstorms in a strongly unstable environment. The strongest thunderstorms produced severe wind gusts and sporadic hail. A lee pressure trough and weak cold front combined to ignite numerous thunderstorms in a strongly unstable environment. The strongest thunderstorms produced severe wind gusts and sporadic hail. A lee pressure trough and weak cold front combined to ignite numerous thunderstorms in a strongly unstable environment. The strongest thunderstorms produced severe wind gusts and sporadic hail. A lee pressure trough and weak cold front combined to ignite numerous thunderstorms in a strongly unstable environment. The strongest thunderstorms produced severe wind gusts and sporadic hail. A lee pressure trough and weak cold front combined to ignite numerous thunderstorms in a strongly unstable environment. The strongest thunderstorms produced severe wind gusts and sporadic hail. A lee pressure trough and weak cold front combined to ignite numerous thunderstorms in a strongly unstable environment. The strongest thunderstorms produced severe wind gusts and sporadic hail.\nEvent Narrative: Wind gusts of up to 42 knots (48 MPH) were measured by a buoy near Francis Scott Key Bridge. A thunderstorm produced an estimated wind gust to 34 knots (39 MPH) near a buoy in Baltimore Inner Harbor. A thunderstorm produced estimated wind gusts to 34 knots (39 MPH) near a buoy near Hart Miller Island. Wind gusts of up to 36 knots (41 MPH) were measured by a buoy near Tolchester Beach. A thunderstorm produced an estimated wind gust to 34 knots (39 MPH) near the ASOS at the U.S. Naval Academy adjacent to the Chesapeake Bay. A wind gust of 40 knots (46 MPH) was measured by a buoy near Thomas Point. A wind gust of 45 knots (52 MPH) was measured by a buoy near Saunders Point Light.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 32.9748 km away, between 2021-08-13 15:37:00 and 2021-08-13 17:20:00. The events included records with estimated wind gusts of 52.142857142857146 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 565000.0 and crop damage of 0.0. \n\nEpisode Narrative: A cold front intersected an extremely unstable airmass. The result was numerous strong to severe thunderstorms containing damaging wind gusts and some hail. A cold front intersected an extremely unstable airmass. The result was numerous strong to severe thunderstorms containing damaging wind gusts and some hail. A cold front intersected an extremely unstable airmass. The result was numerous strong to severe thunderstorms containing damaging wind gusts and some hail. A cold front intersected an extremely unstable airmass. The result was numerous strong to severe thunderstorms containing damaging wind gusts and some hail. A cold front intersected an extremely unstable airmass. The result was numerous strong to severe thunderstorms containing damaging wind gusts and some hail. A cold front intersected an extremely unstable airmass. The result was numerous strong to severe thunderstorms containing damaging wind gusts and some hail. A cold front intersected an extremely unstable airmass. The result was numerous strong to severe thunderstorms containing damaging wind gusts and some hail. A cold front intersected an extremely unstable airmass. The result was numerous strong to severe thunderstorms containing damaging wind gusts and some hail. A cold front intersected an extremely unstable airmass. The result was numerous strong to severe thunderstorms containing damaging wind gusts and some hail. A cold front intersected an extremely unstable airmass. The result was numerous strong to severe thunderstorms containing damaging wind gusts and some hail. A cold front intersected an extremely unstable airmass. The result was numerous strong to severe thunderstorms containing damaging wind gusts and some hail. A cold front intersected an extremely unstable airmass. The result was numerous strong to severe thunderstorms containing damaging wind gusts and some hail. A cold front intersected an extremely unstable airmass. The result was numerous strong to severe thunderstorms containing damaging wind gusts and some hail. A cold front intersected an extremely unstable airmass. The result was numerous strong to severe thunderstorms containing damaging wind gusts and some hail.\nEvent Narrative: Trees blew down on MD-94 Woodbine Road near Annapolis Rock Road. Numerous trees blew down in the Woodbine area. Numerous trees blew down in the Dayton and Glenwood area. Trees blew down near the intersection of McNeal Road and Union Chapel Road. Trees blew down near the intersection of Gared Road and Sharp Road. Numerous trees blew down in the West Friendship area. Trees blew down near the intersection of US-40 Baltimore National Pike and MD-144 Frederick Road. A large tree blew down near the intersection of Ten Oaks Road and Green Bridge Road. Trees blew down on MD-99 Old Frederick Road near Taylor Farm Road. Several trees blew down in the Columbia area. A tree blew down on Launcelot Lane. Two trees blew down near the intersection of Broken Lane Parkway and Patuxent Woods Drive. A tree blew down on Hess Road near MD-146 Jarresttsville Pike. Several trees and power lines blew down in and around Bel Air. Power lines blew down in the 300 block of Baltimore Pike. A tree blew down near the intersection of Jade Drive and Emerald Drive. Trees blew down on southbound MD-197 near Race Track Road. A tree blew down in the 1400 block of Hollingsworth Road. A branch blew down onto wires causing a fire in the 3000 block of Clayton Road. Wires blew down near the intersection of MD-424 Davidsonville Road and MD-214 Central Avenue. Trees blew down on MD-468 Muddy Creek Road near MD-255 Galesville Road. A few hundred trees blew down throughout the City of Baltimore. A large tree and several branches were blown down near the intersection of Biltmore Avenue and Pinkey Road. Several trees blew down in and around Fallston. Trees blew down near the intersection of MD-152 Fallston Road and Carrs Mill Road. A tree blew down on MD-152 Fallston Road near Rochelle Drive. A tree blew down near the intersection of Durham Road and Bellechase Road. A tree blew down in the 2800 block of Pleasantville Road.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 24.2023 km away, between 2021-08-13 16:09:00 and 2021-08-13 17:40:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front intersected an extremely unstable airmass. The result was numerous strong to severe thunderstorms containing damaging wind gusts and some hail. A cold front intersected an extremely unstable airmass. The result was numerous strong to severe thunderstorms containing damaging wind gusts and some hail. A cold front intersected an extremely unstable airmass. The result was numerous strong to severe thunderstorms containing damaging wind gusts and some hail. A cold front intersected an extremely unstable airmass. The result was numerous strong to severe thunderstorms containing damaging wind gusts and some hail. A cold front intersected an extremely unstable airmass. The result was numerous strong to severe thunderstorms containing damaging wind gusts and some hail. A cold front intersected an extremely unstable airmass. The result was numerous strong to severe thunderstorms containing damaging wind gusts and some hail. A cold front intersected an extremely unstable airmass. The result was numerous strong to severe thunderstorms containing damaging wind gusts and some hail. A cold front intersected an extremely unstable airmass. The result was numerous strong to severe thunderstorms containing damaging wind gusts and some hail. A cold front intersected an extremely unstable airmass. The result was numerous strong to severe thunderstorms containing damaging wind gusts and some hail. A cold front intersected an extremely unstable airmass. The result was numerous strong to severe thunderstorms containing damaging wind gusts and some hail. A cold front intersected an extremely unstable airmass. The result was numerous strong to severe thunderstorms containing damaging wind gusts and some hail. A cold front intersected an extremely unstable airmass. The result was numerous strong to severe thunderstorms containing damaging wind gusts and some hail. A cold front intersected an extremely unstable airmass. The result was numerous strong to severe thunderstorms containing damaging wind gusts and some hail.\nEvent Narrative: Wind gusts of up to 39 knots (45 MPH) were measured by a buoy near Francis Scott Key Bridge. A wind gust of 37 knots (43 MPH) was measured by a mesonet at Oriole Park at Camden Yards adjacent to Baltimore Inner Harbor. A thunderstorm produced an estimated wind gust to 34 knots (39 MPH) near a mesonet at Hampstead Hill Academy adjacent to Baltimore Inner Harbor. A wind gust of 38 k nots (44 MPH) was measured by a mesonet on I-695 Francis Scott Key Bridge. Wind gusts of up to 35 knots (40 MPH) were measured by a buoy in Baltimore Inner Harbor. A wind gust of 38 knots (44 MPH) was measured by a mesonet at Oriole Park at Camden Yards adjacent to Baltimore Inner Harbor. A thunderstorm produced an estimated wind gust to 34 knots (39 MPH) near a buoy near Hart Miller Island. A thunderstorm produced an estimated wind gust to 34 knots (39 MPH) near a buoy near Greenbury Point. Wind gusts of up to 36 knots (41 MPH) were measured by a mesonet on the US-50/US-301 Chesapeake Bay Bridge. Wind gusts of up to 38 knots (44 MPH) were measured by a buoy near Saunders Point Light. A thunderstorm produced an estimated wind gust to 34 knots (39 MPH) near a buoy near Tolly Point. A wind gust of 46 knots (53 MPH) was measured by a buoy near Thomas Point. A wind gust of 42 knots (48 MPH) was measured by a buoy near Saunders Point Light.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 27.8504 km away, between 2021-08-14 23:03:00 and 2021-08-14 23:03:00. The events included records with measured wind gusts of 41.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Thunderstorms ignited along a stalled front and produced several instances of wind damage.\nEvent Narrative: A wind gust of 41 knots (47 MPH) was measured by a mesonet on the US-50/US-301 Chesapeake Bay Bridge.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 37.5484 km away, between 2021-08-26 16:30:00 and 2021-08-26 16:30:00. The events included records with estimated wind gusts of 45.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 500.0 and crop damage of 0.0. \n\nEpisode Narrative: Isolated severe thunderstorms produced a few instances of wind damage over central and western Maryland.\nEvent Narrative: A few branches about two inches in diameter blew down along Blenheim Road North.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 30.458 km away, between 2021-08-27 15:40:00 and 2021-08-27 17:35:00. The events included records with estimated wind gusts of 49.285714285714285 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 19000.0 and crop damage of 0.0. \n\nEpisode Narrative: Showers and thunderstorms developed ahead of a pressure trough, with several turning severe. Considerable wind damage was noted in suburban Maryland. Showers and thunderstorms developed ahead of a pressure trough, with several turning severe. Considerable wind damage was noted in suburban Maryland. Showers and thunderstorms developed ahead of a pressure trough, with several turning severe. Considerable wind damage was noted in suburban Maryland. Showers and thunderstorms developed ahead of a pressure trough, with several turning severe. Considerable wind damage was noted in suburban Maryland. Showers and thunderstorms developed ahead of a pressure trough, with several turning severe. Considerable wind damage was noted in suburban Maryland. Showers and thunderstorms developed ahead of a pressure trough, with several turning severe. Considerable wind damage was noted in suburban Maryland. Showers and thunderstorms developed ahead of a pressure trough, with several turning severe. Considerable wind damage was noted in suburban Maryland.\nEvent Narrative: Trees and wires blew down in Millersville, including along I-97 between Exits 12 and 14. Trees and wires blew down in Herald Harbor. A tree blew down in Belvedere Park. Trees blew down on westbound US-50/US-301 prior to Exit 32/MD-908 Oceanic Drive. A tree and wires blew down on MD-137 Mount Carmel Road near Cedar Grove Road. A tree blew down on MD-138 Monkton Road near Piney Woods Road. Trees blew down in Forest Hill, including near the intersection of MD-152 Fallston Road and Fox Meadow Court, and in the 1800 block of Parkwood Drive. A tree blew down in the 100 block of Reckford Road.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 28.4913 km away, between 2021-08-27 16:06:00 and 2021-08-27 18:13:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Thunderstorms developed along and ahead of a pressure trough, producing gusty winds over portions of the tidal Potomac River and Chesapeake Bay. Thunderstorms developed along and ahead of a pressure trough, producing gusty winds over portions of the tidal Potomac River and Chesapeake Bay. Thunderstorms developed along and ahead of a pressure trough, producing gusty winds over portions of the tidal Potomac River and Chesapeake Bay. Thunderstorms developed along and ahead of a pressure trough, producing gusty winds over portions of the tidal Potomac River and Chesapeake Bay. Thunderstorms developed along and ahead of a pressure trough, producing gusty winds over portions of the tidal Potomac River and Chesapeake Bay. Thunderstorms developed along and ahead of a pressure trough, producing gusty winds over portions of the tidal Potomac River and Chesapeake Bay. Thunderstorms developed along and ahead of a pressure trough, producing gusty winds over portions of the tidal Potomac River and Chesapeake Bay. Thunderstorms developed along and ahead of a pressure trough, producing gusty winds over portions of the tidal Potomac River and Chesapeake Bay. Thunderstorms developed along and ahead of a pressure trough, producing gusty winds over portions of the tidal Potomac River and Chesapeake Bay. Thunderstorms developed along and ahead of a pressure trough, producing gusty winds over portions of the tidal Potomac River and Chesapeake Bay. Thunderstorms developed along and ahead of a pressure trough, producing gusty winds over portions of the tidal Potomac River and Chesapeake Bay.\nEvent Narrative: Wind gusts of up to 39 knots (45 MPH) were measured by a buoy near Francis Scott Key Bridge. Wind gusts of up to 44 knots (51 MPH) were measured by a mesonet on I-695 Francis Scott Key Bridge. A wind gust of 36 knots (41 MPH) was measured by the ASOS at the U.S. Naval Academy in Annapolis adjacent to the Chesapeake Bay. A thunderstorm produced an estimated wind gust to 34 knots (39 MPH) near a buoy near Annapolis. A wind gust of 34 knots (39 MPH) was measured by a buoy near Greenbury Point. A wind gust of 49 knots (56 MPH) was measured by a buoy near Annapolis. A thunderstorm produced an estimated wind gust to 34 knots (39 MPH) near a mesonet on the US-50/US-301 Chesapeake Bay Bridge. A wind gust of 34 knots (39 MPH) was measured by a mesonet on Thomas Point Road adjacent to the Chesapeake Bay. A wind gust of 43 knots (49 MPH) was measured by a buoy near Thomas Point. A thunderstorm produced an estimated wind gust to 34 knots (39 MPH) near a buoy near Tolly Point. A wind gust of 36 knots (41 MPH) was measured by a mesonet on the US-50/US-301 Chesapeake Bay Bridge.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 38.2874 km away, between 2021-08-27 18:23:00 and 2021-08-27 18:23:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A hot and humid air mass remained in place over the mid-Atlantic on August 27. A slow moving cold front began dropping southward into the region during the afternoon. This helped scattered to widespread convection develop in a strongly unstable air mass. Shear was weak over the region, but thanks to the strong instability, a number of storms became strong to severe with a threat for damaging downburst winds, in addition to locally heavy rain. Convection continued into the late evening hours before gradually waning in coverage as instability was lost.\nEvent Narrative: A tree fell into a residence on Cloverfields Dr. No injuries were reported.", "The following events were reported: Thunderstorm Wind, Tornado. These occurred near station USW00093721, approximately 24.1471 km away, between 2021-09-01 03:55:00 and 2021-09-01 14:10:00.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 65000.0 and crop damage of 0.0. \n\nEpisode Narrative: The remnants of Ida produced two tornadoes and sporadic straight line wind damage. The remnants of Ida produced two tornadoes and sporadic straight line wind damage. The remnants of Ida produced two tornadoes and sporadic straight line wind damage. The remnants of Ida produced two tornadoes and sporadic straight line wind damage. The remnants of Ida produced two tornadoes and sporadic straight line wind damage. The remnants of Ida produced two tornadoes and sporadic straight line wind damage. The remnants of Ida produced two tornadoes and sporadic straight line wind damage.\nEvent Narrative: Multiple large trees blew down with a few snapped near the top in northeastern Anne Arundel County (near Green Haven and Riverdale). The remnants of Ida produced one of the strongest tornadoes in the past decade of Maryland's history. Only four other EF2 or stronger tornadoes have occurred in the state in the past 10 years.||On Wednesday afternoon, a tornado that peaked in intensity with winds estimated at 125 mph traveled northeast along a path through Anne Arundel County and the City of Annapolis. It not only snapped numerous trees, but also produced significant structural damage to homes, businesses, and a school. Fortunately, there were no injuries reported, even though it tracked through a heavily populated area. Several eyewitnesses to the event reported getting the NWS Tornado Warning through their cell phone in advance, and sheltering in response to the warning.||From the NWS storm survey, the first damage noted, and recorded touchdown point was in Owensville, Maryland, in southern Anne Arundel County, near the intersection of Sudley Road and Owensville Road. This included a large limb from a tree top over Sudley Road and several portions of large cedar trees snapped along Owensville Road. The tornado moved northeast across rural southern Anne Arundel County before crossing Mill Swamp Road. Here, about a quarter of a mile east of the intersection with Dove Farm Road, dozens of trees and large branches were snapped and uprooted in a path from southwest to northeast as far as you could see in either direction from the road. While the dominant direction of the tree damage was being blown down to the north or northeast, there were trees downed in multiple directions, and many were topped.||The tornado intensified further as it moved into the South River Colony community. Dozens of trees were downed along the easternmost portions of Monarch Drive. Homes near the intersection of Monarch Drive and Red Admiral Court were particularly hard hit by some of the strongest winds of the entire tornado path. Several had significant portions of their roof damaged or removed, and one home in the middle of the track was unroofed entirely. One resident in this area reported seeing the tornado as it approached. The tornado then crossed South River Golf Links before moving into a campus of school buildings that includes South River High School and the Center of Applied Technology South. There it damaged the upper parts of the football field grandstands and concessions stand, damaged the roof, and caused cosmetic damage to some of the upper portions of the Center of Applied Technology South. The schools were left structurally sound, and the staff and some students that were there were able to shelter without injury.||The tornado crossed Central Avenue around 2:11 PM and moved into Edgewater. Here it crossed the communities of Woodland Beach, Londontowne, and Edgewater Park. Dozens of trees and large branches were snapped, and portions of 5 to 10 roofs were noted to have been damaged. One home near the intersection of Millstone Drive and Oakwood Road had only damaged roof trusses remaining of its roof.||The tornado crossed the South River and moved through western portions of the City of Annapolis at peak intensity with winds estimated at 125 mph at 2:20 PM. Several trees were snapped along the path as it crossed Aris T. Allen Boulevard just east of the Annapolis Harbour Center shopping area. It crossed Forest Drive at the intersection of Parole Street. Several homes there sustained roof damage, and one home was unroofed entirely. As it crossed the area near the intersection of West Street and Lee Street, the most substantial structural damage was noted. A large warehouse building had the winds enter the south side of the building and blow out a large portion of the west side cinder block wall. The roof with large metal trusses was largely removed. A fast food restaurant had its sign entirely removed from its post. Another commercial building had its roof removed, significant upper portions of the cinder block building removed, and its large commercial sign post blown over. A strip mall across the street had its windows blown out and flat roof damaged. All the telephone poles and attached wires along this stretch of West Street were downed. Another commercial building had its windows blown out. Several eyewitnesses saw the tornado as it passed.||Additional residential roof damage occurred as the tornado moved north over Bowman Court. From here, the tornado crossed into the community of Admiral Heights. Affected were areas along Halsey Road and adjacent Cedar Park Road. Here, the wind did not directly cause any structural damage, but about a dozen trees were snapped. That included one large, healthy tree about two and a half feet in diameter. The tornado crossed Weems Creek and Rowe Boulevard, and then snapped several trees along Riverview Avenue.||Finally, the tornado crossed US Route 50/301 a few hundred yards west of the Severn River Bridge, snapping trees on both sides of the highway. The final damage noted occurred at the end of Acorn Drive at the last residential property that sits on the shore of the Severn River. Several trees were snapped here. The tornado dissipated here, or as it crossed the Severn River. The survey team was not able to find any damage north of the Severn River, and video evidence from social media indicates the funnel dissipated here. Trees blew down on southbound MD-10 Arundel Expressway at MD-710 East Ordnance Road. A NWS storm survey team determined that aN EF-0 tornado occurred near Edgemere in Baltimore County, Maryland, on Wednesday afternoon, September 1, 2021. This tornado produced scattered minor tree damage across an approximate 6.7 mile path. This tornado was produced by the same supercell that produced the Anne Arundel County/Annapolis tornado roughly a half hour prior.||The first damage noted was near Fort Howard Park where there were broken tree branches and a hardwood tree snapped. As the tornado progressed to the northeast, hardwood and softwood trees were snapped and uprooted along Fort Howard Park Road. The tornado continued its northeast trek through North Point State Park where more broken tree branches and softwood trees were found snapped. Sporadic damage continued throughout the park before the tornado crossed the Black River.||As the tornado moved northeast over Rocky Point, leaf debris and small branches covered Rocky Point Golf Course. The northeast track continued just west of Browns Creek where hardwood trees were sheared on the tree line and tree branches were broken. The last of the damage was found near Holly Beach. A tree was reported down on eastbound I-695 Baltimore Beltway Inner Loop at Exit 27A/MD-146 Dulaney Valley Road. A tree blew down near the intersection of Cold Bottom Road/Stringtown Road and Yeoho Road. A tree was reported down on MD-150 Eastern Avenue in Bowleys Quarters.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 14.2666 km away, between 2021-09-01 04:00:00 and 2021-09-01 04:00:00. The events included records with measured wind gusts of 43.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: The remnants of Ida produced gusty winds and tornadoes near the tidal Potomac River and Chesapeake Bay.\nEvent Narrative: A wind gust of 43 knots (49 MPH) was measured by a buoy near the I-695 Francis Scott Key Bridge.", "The following events were reported: Flood. These occurred near station USW00093721, approximately 20.3872 km away, between 2021-09-01 04:09:00 and 2021-09-02 00:45:00. The flood was caused by Heavy Rain. Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: The remnants of Ida produced widespread flooding along with instances of flash flooding across the area. Tropical moisture infiltrated the area and there were moderate amounts of instability as well. This combined with the lift provided from the remnants of Ida led to heavy rainfall during this time. Rainfall amounts averaged around 1-3 near and east of Interstate 95, with amounts around 4 to 8 inches across portions of northern and central Maryland. Excess runoff from the heavy rainfall led to river flooding as well. The remnants of Ida produced widespread flooding along with instances of flash flooding across the area. Tropical moisture infiltrated the area and there were moderate amounts of instability as well. This combined with the lift provided from the remnants of Ida led to heavy rainfall during this time. Rainfall amounts averaged around 1-3 near and east of Interstate 95, with amounts around 4 to 8 inches across portions of northern and central Maryland. Excess runoff from the heavy rainfall led to river flooding as well. The remnants of Ida produced widespread flooding along with instances of flash flooding across the area. Tropical moisture infiltrated the area and there were moderate amounts of instability as well. This combined with the lift provided from the remnants of Ida led to heavy rainfall during this time. Rainfall amounts averaged around 1-3 near and east of Interstate 95, with amounts around 4 to 8 inches across portions of northern and central Maryland. Excess runoff from the heavy rainfall led to river flooding as well. The remnants of Ida produced widespread flooding along with instances of flash flooding across the area. Tropical moisture infiltrated the area and there were moderate amounts of instability as well. This combined with the lift provided from the remnants of Ida led to heavy rainfall during this time. Rainfall amounts averaged around 1-3 near and east of Interstate 95, with amounts around 4 to 8 inches across portions of northern and central Maryland. Excess runoff from the heavy rainfall led to river flooding as well. The remnants of Ida produced widespread flooding along with instances of flash flooding across the area. Tropical moisture infiltrated the area and there were moderate amounts of instability as well. This combined with the lift provided from the remnants of Ida led to heavy rainfall during this time. Rainfall amounts averaged around 1-3 near and east of Interstate 95, with amounts around 4 to 8 inches across portions of northern and central Maryland. Excess runoff from the heavy rainfall led to river flooding as well. The remnants of Ida produced widespread flooding along with instances of flash flooding across the area. Tropical moisture infiltrated the area and there were moderate amounts of instability as well. This combined with the lift provided from the remnants of Ida led to heavy rainfall during this time. Rainfall amounts averaged around 1-3 near and east of Interstate 95, with amounts around 4 to 8 inches across portions of northern and central Maryland. Excess runoff from the heavy rainfall led to river flooding as well. The remnants of Ida produced widespread flooding along with instances of flash flooding across the area. Tropical moisture infiltrated the area and there were moderate amounts of instability as well. This combined with the lift provided from the remnants of Ida led to heavy rainfall during this time. Rainfall amounts averaged around 1-3 near and east of Interstate 95, with amounts around 4 to 8 inches across portions of northern and central Maryland. Excess runoff from the heavy rainfall led to river flooding as well. The remnants of Ida produced widespread flooding along with instances of flash flooding across the area. Tropical moisture infiltrated the area and there were moderate amounts of instability as well. This combined with the lift provided from the remnants of Ida led to heavy rainfall during this time. Rainfall amounts averaged around 1-3 near and east of Interstate 95, with amounts around 4 to 8 inches across portions of northern and central Maryland. Excess runoff from the heavy rainfall led to river flooding as well.\nEvent Narrative: Multiple roads flooded in Fells Point. Flooding reported at North Point Boulevard and Kane Street. Flooding reported in the 2900 block of Liberty Parkway. Water rescue near Brock Bridge Road and Laurel-Bowie Road. The on ramp from MD-2 southbound onto I-695 was closed due to flooding. Flooding reported at Pine Street and Chestnut Street. The water level rose above flood stage of 7 feet, cresting at 7.90 feet on September 1st at 8:40 PM EST. Portions of Upper Glencoe Road and Lower Glencoe Road were flooded. The water level along the Middle River rose above flood stage, cresting at 11.02 feet on September 1st at 2:42 PM EST.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 28.3818 km away, between 2021-09-16 16:13:00 and 2021-09-16 16:18:00. The events included records with measured wind gusts of 34.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A thunderstorm produced gusty winds over the upper Chesapeake Bay.\nEvent Narrative: Wind gusts of up to 34 knots were measured by a buoy near Hart Miller Island.", "The following events were reported: Flood. These occurred near station USW00093721, approximately 44.3922 km away, between 2021-09-16 19:00:00 and 2021-09-16 21:00:00. The flood was caused by Heavy Rain. Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A light flow aloft along with an unstable atmosphere led to slow moving showers and thunderstorms. Heavy amounts of rain led to instances of flooding.\nEvent Narrative: Twin Arch Road in Mount Airy closed due to high water.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 21.0711 km away, between 2021-09-22 13:30:00 and 2021-09-22 17:50:00. The events included records with estimated wind gusts of 49.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 15000.0 and crop damage of 0.0. \n\nEpisode Narrative: Several showers and thunderstorms in a strong low-level wind shear environment produced damaging wind gusts. Several showers and thunderstorms in a strong low-level wind shear environment produced damaging wind gusts. Several showers and thunderstorms in a strong low-level wind shear environment produced damaging wind gusts. Several showers and thunderstorms in a strong low-level wind shear environment produced damaging wind gusts. Several showers and thunderstorms in a strong low-level wind shear environment produced damaging wind gusts.\nEvent Narrative: Several trees, large branches, and wires blew down in Severn, including near the intersection of MD-174 Reece Road and New Disney Road. A tree blew down near the intersection of Broken Timber Way/Five Fingers Way and Summer Hollow Lane. A tree blew down in the 3000 block of Toll House Road. A tree blew down on westbound US-40 Baltimore National Pike prior to Bethany Lane/Centennial Lane. A tree blew down on westbound I-70 at Exit 87A/US-29 Columbia Pike. Trees blew down near Woodstock, including in the 1500 block of Grooms Lane. Trees blew down near Arbutus, including onto westbound I-695 Baltimore Beltway Inner Loop near MD-372 Wilkens Avenue. A tree was reported down in the 2900 block of Shepperd Road.", "The following events were reported: Flood. These occurred near station USW00093721, approximately 31.8748 km away, between 2021-09-23 06:30:00 and 2021-09-23 16:56:00. The flood was caused by Heavy Rain. Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A slow moving cold front approached the area on the 22nd before passing through on the 23rd. A deep southerly flow allowed for tropical moisture to move into the area ahead of the boundary. This led to heavy rainfall as the cold front approached, and several instances of flooding along with isolated instances of flash flooding occurred. A slow moving cold front approached the area on the 22nd before passing through on the 23rd. A deep southerly flow allowed for tropical moisture to move into the area ahead of the boundary. This led to heavy rainfall as the cold front approached, and several instances of flooding along with isolated instances of flash flooding occurred. A slow moving cold front approached the area on the 22nd before passing through on the 23rd. A deep southerly flow allowed for tropical moisture to move into the area ahead of the boundary. This led to heavy rainfall as the cold front approached, and several instances of flooding along with isolated instances of flash flooding occurred. A slow moving cold front approached the area on the 22nd before passing through on the 23rd. A deep southerly flow allowed for tropical moisture to move into the area ahead of the boundary. This led to heavy rainfall as the cold front approached, and several instances of flooding along with isolated instances of flash flooding occurred. A slow moving cold front approached the area on the 22nd before passing through on the 23rd. A deep southerly flow allowed for tropical moisture to move into the area ahead of the boundary. This led to heavy rainfall as the cold front approached, and several instances of flooding along with isolated instances of flash flooding occurred. A slow moving cold front approached the area on the 22nd before passing through on the 23rd. A deep southerly flow allowed for tropical moisture to move into the area ahead of the boundary. This led to heavy rainfall as the cold front approached, and several instances of flooding along with isolated instances of flash flooding occurred. A slow moving cold front approached the area on the 22nd before passing through on the 23rd. A deep southerly flow allowed for tropical moisture to move into the area ahead of the boundary. This led to heavy rainfall as the cold front approached, and several instances of flooding along with isolated instances of flash flooding occurred. A slow moving cold front approached the area on the 22nd before passing through on the 23rd. A deep southerly flow allowed for tropical moisture to move into the area ahead of the boundary. This led to heavy rainfall as the cold front approached, and several instances of flooding along with isolated instances of flash flooding occurred. A slow moving cold front approached the area on the 22nd before passing through on the 23rd. A deep southerly flow allowed for tropical moisture to move into the area ahead of the boundary. This led to heavy rainfall as the cold front approached, and several instances of flooding along with isolated instances of flash flooding occurred. A slow moving cold front approached the area on the 22nd before passing through on the 23rd. A deep southerly flow allowed for tropical moisture to move into the area ahead of the boundary. This led to heavy rainfall as the cold front approached, and several instances of flooding along with isolated instances of flash flooding occurred. A slow moving cold front approached the area on the 22nd before passing through on the 23rd. A deep southerly flow allowed for tropical moisture to move into the area ahead of the boundary. This led to heavy rainfall as the cold front approached, and several instances of flooding along with isolated instances of flash flooding occurred.\nEvent Narrative: The stream gauge on Gunpowder Falls at Glencoe reached flood stage. Grace Road was closed due to flooding near Alice Avenue. MD-7 Philadelphia Road is closed due to flooding near MD-136 Calvary Road. The stream gauge on the Patuxent River at Unity reached flood stage. Old Battle Grove Road was closed due to flooding near North Point Road. About a half dozen roads closed for high water. Several roads were blocked by high water in Mount Airy . Several roads were blocked by high water in Winfield . The water level rose above flood stage of 7 feet, cresting at 7.46 feet on September 23rd at 12:00 PM EST. Portions of Upper Glencoe Road and Lower Glencoe Road were flooded. The water level rose above flood stage along the Patuxent River in Unity, cresting at 8.54 feet at 11:25 AM EST on the 23rd. The parking lot for the Patuxent River State Park at Maryland Route 97 was flooded. The water level rose above flood stage, cresting at 16.39 feet at 3:35 PM EST on the 23rd. Water covered a portion of River Road in the Patapsco Valley State Park. Large portions of the park were flooded near the playground off Gunn Road.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 42.6407 km away, between 2021-09-23 07:00:00 and 2021-09-23 07:05:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 5000.0 and crop damage of 0.0. \n\nEpisode Narrative: A line of showers and thunderstorms produced widely scattered wind damage over northeastern Maryland. A line of showers and thunderstorms produced widely scattered wind damage over northeastern Maryland.\nEvent Narrative: Several large trees and branches were blown down near Cockeysville, including near Beaver Dam Road. A tree and wires blew down near the intersection of Wesley Chapel Road and McComas Road.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 36.8319 km away, between 2021-09-23 07:25:00 and 2021-09-23 07:25:00. The events included records with measured wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Several showers and thunderstorms produced gusty winds during the morning hours.\nEvent Narrative: A wind gust of 50 knots (58 MPH) was measured by a buoy near Saunders Point Light.", "The following events were reported: Flash Flood. These occurred near station USW00093721, approximately 47.0304 km away, between 2021-09-23 09:05:00 and 2021-09-23 11:30:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Thunderstorms produced locally heavy rain in northeastern Maryland on the morning of September 23. Rainfall totals were as high as 3 to 5 inches. Thunderstorms produced locally heavy rain in northeastern Maryland on the morning of September 23. Rainfall totals were as high as 3 to 5 inches.\nEvent Narrative: A vehicle was stranded in flood waters at the intersection of Main Street and Melvin Avenue in Queenstown, leading to a water rescue. Maryland Route 298 was closed near Fairlee due to flooding.", "The following events were reported: Marine Thunderstorm Wind, Waterspout. These occurred near station USW00093721, approximately 30.526 km away, between 2021-10-16 13:36:00 and 2021-10-16 15:34:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A strong cold front produced a line of showers resulting in brief-gale force winds and a couple of waterspouts. A strong cold front produced a line of showers resulting in brief-gale force winds and a couple of waterspouts. A strong cold front produced a line of showers resulting in brief-gale force winds and a couple of waterspouts. A strong cold front produced a line of showers resulting in brief-gale force winds and a couple of waterspouts. A strong cold front produced a line of showers resulting in brief-gale force winds and a couple of waterspouts. A strong cold front produced a line of showers resulting in brief-gale force winds and a couple of waterspouts. A strong cold front produced a line of showers resulting in brief-gale force winds and a couple of waterspouts. A strong cold front produced a line of showers resulting in brief-gale force winds and a couple of waterspouts. A strong cold front produced a line of showers resulting in brief-gale force winds and a couple of waterspouts. A strong cold front produced a line of showers resulting in brief-gale force winds and a couple of waterspouts. A strong cold front produced a line of showers resulting in brief-gale force winds and a couple of waterspouts. A strong cold front produced a line of showers resulting in brief-gale force winds and a couple of waterspouts. A strong cold front produced a line of showers resulting in brief-gale force winds and a couple of waterspouts.\nEvent Narrative: A wind gust of 34 knots (39 MPH) was measured by the ASOS at the United States Naval Academy in Annapolis (KNAK) adjacent to the Chesapeake Bay. A squall produced an estimated wind gust to 34 knots (39 MPH) near the NOS sensor near Annapolis (APAM2). A squall produced estimated wind gusts to 34 knots (39 MPH) near the Greenbury Point WeatherFlow sensor (XGBY). Several pictures and videos from social media showed two spray rings from waterspouts just south of the US-50/US-301 Chesapeake Bay Bridge. A squall produced estimated wind gusts to 34 knots (39 MPH) near the Tolchester Beach NOS sensor (TCBM2). A squall produced estimated wind gusts to 34 knots (39 MPH) near the Tolly Point WeatherFlow sensor (XTOL). A squall produced an estimated wind gust to 34 knots (39 MPH) near the ASOS at the United States Naval Academy in Annapolis (KNAK) adjacent to the Chesapeake Bay. A wind gust of 36 knots (41 MPH) was measured by the Kent Island WeatherFlow sensor (XKNT). A wind gust of 36 knots (41 MPH) was measured by the Thomas Point NOS sensor (TPLM2). A squall produced an estimated wind gust to 34 knots (39 MPH) near a mesonet on the eastbound span of the US-50/US-301 Chesapeake Bay Bridge (MD066). A wind gust of 34 knots (39 MPH) was measured by a mesonet on the eastbound span of the US-50/US-301 Chesapeake Bay Bridge (MD066). A wind gust of 36 knots (41 MPH) was measured by one of the I-695 Francis Scott Key Bridge NOS sensors (FSNM2). A squall produced estimated wind gusts to 34 knots (39 MPH) near the Annapolis CBIBS sensor (44063).", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 34.2713 km away, between 2021-10-25 16:33:00 and 2021-10-25 17:35:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A strong area of low pressure produced several bands of showers and thunderstorms resulting in brief, gusty winds. A strong area of low pressure produced several bands of showers and thunderstorms resulting in brief, gusty winds. A strong area of low pressure produced several bands of showers and thunderstorms resulting in brief, gusty winds. A strong area of low pressure produced several bands of showers and thunderstorms resulting in brief, gusty winds. A strong area of low pressure produced several bands of showers and thunderstorms resulting in brief, gusty winds. A strong area of low pressure produced several bands of showers and thunderstorms resulting in brief, gusty winds. A strong area of low pressure produced several bands of showers and thunderstorms resulting in brief, gusty winds.\nEvent Narrative: A line of thunderstorms produced an estimated wind gust to 34 knots (39 MPH) near the Saunders Point Light/Mayo-Triton Beach WeatherFlow sensor (WFMTR). A wind gust of 37 knots (43 MPH) was measured by the Kent Island WeatherFlow sensor (XKNT). A wind gust of 36 knots (41 MPH) was measured by the Thomas Point NOS sensor (TPLM2). Wind gusts of up to 45 knots (52 MPH) were measured by the Hart Miller WeatherFlow sensor (XHRT). A line of thunderstorms produced an estimated wind gust to 34 knots (39 MPH) near the AWOS at Martin State Airport (KMTN) adjacent to the Chesapeake Bay. A line of thunderstorms produced an estimated wind gust to 34 knots (39 MPH) near the AWOS at the Weide Army Helicopter Pad (KEDG) adjacent to the Chesapeake Bay. A wind gust of 34 knots (39 MPH) was measured by a mesonet at the US-50/US-301 Chesapeake Bay Bridge (MD066) over the Chesapeake Bay.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 37.4149 km away, between 2021-10-25 17:45:00 and 2021-10-25 17:50:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 4000.0 and crop damage of 0.0. \n\nEpisode Narrative: A strong low pressure system spawned a few bands of thunderstorms that resulted in widely scattered wind damage. A strong low pressure system spawned a few bands of thunderstorms that resulted in widely scattered wind damage.\nEvent Narrative: Two trees blew down near the intersection of Deer Park Road and Ivy Mill Road. A tree and wires blew down in the 2500 block of Whitt Road.", "The following events were reported: Flood. These occurred near station USW00093721, approximately 23.0896 km away, between 2021-10-29 16:36:00 and 2021-10-29 22:51:00. The flood was caused by Heavy Rain. Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Slow moving low pressure and its associated warm front caused rain to overspread the area. Subtropical moisture was wrapped into this system, which led to instances of heavy rain and flooding. Slow moving low pressure and its associated warm front caused rain to overspread the area. Subtropical moisture was wrapped into this system, which led to instances of heavy rain and flooding. Slow moving low pressure and its associated warm front caused rain to overspread the area. Subtropical moisture was wrapped into this system, which led to instances of heavy rain and flooding.\nEvent Narrative: The water level along the Patuxent River at Elkridge rose above the flood stage of 16.0 feet, cresting at 16.43 feet at 4:45 PM EST on the 29th. Hammonds Ferry Road was flooded and closed at the Patapsco River. Backwater flooding lead to the closure of Furnace Avenue in Elkridge. The water level along the Little Patuxent River at Savage rose above the flood stage of 10.0 feet, cresting at 11.06 feet at 7:45 PM EST on the 29th. The riverside trail was flooded and water approached fields off of Bald Eagle Drive and Brock Ridge Road. High water was over Park Beach Road at Clubhouse Road.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 32.5618 km away, between 2021-11-12 05:12:00 and 2021-11-12 06:56:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A strong cold front produced squalls that resulted in gale-force wind gusts. A strong cold front produced squalls that resulted in gale-force wind gusts. A strong cold front produced squalls that resulted in gale-force wind gusts. A strong cold front produced squalls that resulted in gale-force wind gusts. A strong cold front produced squalls that resulted in gale-force wind gusts. A strong cold front produced squalls that resulted in gale-force wind gusts. A strong cold front produced squalls that resulted in gale-force wind gusts. A strong cold front produced squalls that resulted in gale-force wind gusts. A strong cold front produced squalls that resulted in gale-force wind gusts. A strong cold front produced squalls that resulted in gale-force wind gusts. A strong cold front produced squalls that resulted in gale-force wind gusts.\nEvent Narrative: A wind gust of 47 knots (54 MPH) was measured by a mesonet on the US-50/US-301 Chesapeake Bay Bridge (MD066). A squall produced an estimated wind gust to 34 knots (39 MPH) near the Saunders Point Light/Mayo-Triton Beach WeatherFlow sensor (WFMTR). A wind gust of 44 knots (51 MPH) was measured by a mesonet on the US-50/US-301 Chesapeake Bay Bridge (MD065). Wind gusts of up to 39 knots (45 MPH) were measured by the Tolly Point WeatherFlow sensor (XTOL). A squall produced estimated wind gusts to 34 knots (39 MPH) near the Greenbury Point WeatherFlow sensor (XGBY). Wind gusts of up to 34 knots (39 MPH) were measured by the Hart Miller Island WeatherFlow sensor (XHRT). A squall produced estimated wind gusts to 34 knots (39 MPH) near the Annapolis CBIBS sensor (44063). A squall produced an estimated wind gust to 34 knots (39 MPH) near the AWOS at Martin State Airport (KMTN) adjacent to the upper Chesapeake Bay. A wind gust of 36 knots (41 MPH) was measured by the Greenbury Point Weatherflow sensor (XGBY). A wind gust of 36 knots (41 MPH) was measured by the Thomas Point NOS sensor (TPLM2). A wind gust of 35 knots (40 MPH) was measured by the Kent Island WeatherFlow sensor (XKNT).", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 32.7717 km away, between 2021-11-13 12:22:00 and 2021-11-13 13:35:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A strong cold front produced squalls that resulted in gale-force wind gusts. A strong cold front produced squalls that resulted in gale-force wind gusts. A strong cold front produced squalls that resulted in gale-force wind gusts. A strong cold front produced squalls that resulted in gale-force wind gusts. A strong cold front produced squalls that resulted in gale-force wind gusts. A strong cold front produced squalls that resulted in gale-force wind gusts. A strong cold front produced squalls that resulted in gale-force wind gusts. A strong cold front produced squalls that resulted in gale-force wind gusts. A strong cold front produced squalls that resulted in gale-force wind gusts. A strong cold front produced squalls that resulted in gale-force wind gusts. A strong cold front produced squalls that resulted in gale-force wind gusts. A strong cold front produced squalls that resulted in gale-force wind gusts.\nEvent Narrative: Wind gusts of up to 38 knots (44 MPH) were measured by the Greenbury Point WeatherFlow sensor (XGBY). A squall produced estimated wind gusts to 34 knots (39 MPH) near the Tolly Point WeatherFlow sensor (XTOL). A squall produced an estimated wind gust to 34 knots (39 MPH) near the Sandy Point WeatherFlow sensor (XSPT). A wind gust of 48 knots (55 MPH) was measured by a mesonet on the US-50/US-301 Chesapeake Bay Bridge (MD066). A squall produced estimated wind gusts to 34 knots (39 MPH) near the Saunders Point Light/Mayo-Triton Beach WeatherFlow sensor (WFMTR). Wind gusts of up to 37 knots (43 MPH) were measured by a mesonet on the US-50/US-301 Chesapeake Bay Bridge (MD065). A wind gust of 34 knots (39 MPH) was measured by the ASOS at the U.S. Naval Academy in Annapolis (KNAK) adjacent to the Chesapeake Bay. A squall produced an estimated wind gust to 34 knots (39 MPH) near the Kent Island WeatherFlow sensor (XKNT). Wind gusts of 34 knots (39 MPH) were measured by the Tolchester Beach NOS sensor (TCBM2). A squall produced an estimated wind gust to 34 knots (39 MPH) near the Thomas Point NOS sensor (TPLM2). Wind gusts of up to 36 knots (41 MPH) were measured by the Hart Miller Island WeatherFlow sensor (XHRT). A wind gust of 36 knots (42 MPH) was measured by a mesonet on the US-50/US-301 Chesapeake Bay Bridge (MD066).", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 24.9094 km away, between 2021-11-18 18:54:00 and 2021-11-18 20:28:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A strong cold front produced squalls that resulted in gale- to storm-force wind gusts. A strong cold front produced squalls that resulted in gale- to storm-force wind gusts. A strong cold front produced squalls that resulted in gale- to storm-force wind gusts. A strong cold front produced squalls that resulted in gale- to storm-force wind gusts. A strong cold front produced squalls that resulted in gale- to storm-force wind gusts. A strong cold front produced squalls that resulted in gale- to storm-force wind gusts. A strong cold front produced squalls that resulted in gale- to storm-force wind gusts. A strong cold front produced squalls that resulted in gale- to storm-force wind gusts. A strong cold front produced squalls that resulted in gale- to storm-force wind gusts. A strong cold front produced squalls that resulted in gale- to storm-force wind gusts. A strong cold front produced squalls that resulted in gale- to storm-force wind gusts. A strong cold front produced squalls that resulted in gale- to storm-force wind gusts. A strong cold front produced squalls that resulted in gale- to storm-force wind gusts.\nEvent Narrative: A squall produced an estimated wind gust to 35 knots (40 MPH) near a mesonet in Shady Side (FW8079) adjacent to the Chesapeake Bay. Wind gusts of up to 40 knots (46 MPH) were measured by the Hart Miller Island Weatherflow sensor (XHRT). A squall produced an estimated wind gust to 34 knots (39 MPH) near a mesonet in Patterson Park (KMDBALTI126) adjacent to the tidal Patapsco River. A squall produced an estimated wind gust to 34 knots (39 MPH) near a mesonet at the Maryland Science Center (BLMRE) adjacent to the tidal Patapsco River. A wind gust of 41 knots (47 MPH) was measured by a mesonet on the US-50/US-301 Chesapeake Bay Bridge (MD066). A squall produced an estimated wind gust to 34 knots (39 MPH) near the Tolly Point WeatherFlow sensor (XTOL). A squall produced an estimated wind gust to 34 knots (39 MPH) near the Greenbury Point WeatherFlow sensor (XGBY). A squall produced estimated wind gusts to 34 knots (39 MPH) near the Annapolis CBIBS sensor (44063). A squall produced an estimated wind gust to 34 knots (39 MPH) near the Hart Miller Island WeatherFlow sensor (XHRT). A squall produced an estimated wind gust to 34 knots (39 MPH) near the Tolly Point WeatherFlow sensor (XTOL). A squall produced an estimated wind gust to 34 knots (39 MPH) near one of NOS sensors near the I-695 Francis Scott Key Bridge (FSNM2). A wind gust of 36 knots (41 MPH) was measured by one of the NOS sensors near the I-695 Francis Scott Key Bridge (FSNM2). A squall produced estimated wind gusts to 34 knots (39 MPH) near one of NOS sensors near the I-695 Francis Scott Key Bridge (FSKM2).", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 27.8255 km away, between 2021-12-06 19:00:00 and 2021-12-06 20:02:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A strong cold front produced squalls with gale and brief storm force winds. A strong cold front produced squalls with gale and brief storm force winds. A strong cold front produced squalls with gale and brief storm force winds. A strong cold front produced squalls with gale and brief storm force winds. A strong cold front produced squalls with gale and brief storm force winds. A strong cold front produced squalls with gale and brief storm force winds. A strong cold front produced squalls with gale and brief storm force winds. A strong cold front produced squalls with gale and brief storm force winds. A strong cold front produced squalls with gale and brief storm force winds. A strong cold front produced squalls with gale and brief storm force winds.\nEvent Narrative: Wind gusts of up to 44 knots (51 MPH) was measured by one of the NOS sensors at the I-695 Francis Scott Key Bridge (FSNM2). A wind gust of 37 knots (43 MPH) was measured by a mesonet at Oriole Park at Camden Yards (BLTPC) adjacent to the tidal Patapsco River. Wind gusts of up to 34 knots (39 MPH) were measured by the Hart Miller Island WeatherFlow sensor (XHRT). A squall produced estimated wind gusts to 34 knots (39 MPH) near one of the NOS sensors at the I-695 Francis Scott Key Bridge (FSKM2). A squall produced estimated wind gusts to 48 knots (55 MPH) near a mesonet on the eastbound span of the US-50/US-301 Chesapeake Bay Bridge (MD066). A wind gust of 36 knots (41 MPH) was measured by the Saunders Point Light/Mayo-Triton Beach WxFlow sensor (WFMTR). A squall produced estimated wind gusts to 34 knots (39 MPH) near the Greenbury Point WeatherFlow sensor (XGBY). Wind gusts of up to 36 knots (41 MPH) were measured by the Tolly Point WeatherFlow sensor (XTOL). A wind gust of 38 knots (44 MPH) was measured by the Thomas Point NOS sensor (TPLM2). Wind gusts of up to 36 knots (41 MPH) were measured by a mesonet in Galesville (EW0112) adjacent to the Chesapeake Bay.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 28.8795 km away, between 2021-12-11 20:54:00 and 2021-12-11 21:45:00. The events included records with measured wind gusts of 42.285714285714285 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A strong cold front produced squalls that resulted in gale to near storm force wind gusts. A strong cold front produced squalls that resulted in gale to near storm force wind gusts. A strong cold front produced squalls that resulted in gale to near storm force wind gusts. A strong cold front produced squalls that resulted in gale to near storm force wind gusts. A strong cold front produced squalls that resulted in gale to near storm force wind gusts. A strong cold front produced squalls that resulted in gale to near storm force wind gusts. A strong cold front produced squalls that resulted in gale to near storm force wind gusts.\nEvent Narrative: Wind gusts to 39 knots (45 MPH) were measured by one of the NOS sensors on the I-695 Francis Scott Key Bridge (FSNM2). A wind gust of 41 knots (47 MPH) was measured by the Hart Miller Island WeatherFlow sensor (XHRT). A wind gust of 34 knots (39 MPH) was measured by the ASOS at the United States Naval Academy in Annapolis (KNAK) adjacent to the Chesapeake Bay. Wind gusts of up to 47 knots (54 MPH) were measured by the Annapolis CBIBS sensor (44063). A wind gust of 46 knots (53 MPH) was measured by the Thomas Point NOS sensor (TPLM2). Wind gusts of up to 42 knots (48 MPH) were measured by the Tolly Point WeatherFlow sensor (XTOL). Wind gusts of up to 47 knots (54 MPH) were measured by the Greenbury Point WeatherFlow sensor (XGBY).", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 29.1965 km away, between 2022-01-01 20:54:00 and 2022-01-01 21:23:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A squall produced gale-force wind gusts over portions of the Chesapeake Bay during the evening hours. A squall produced gale-force wind gusts over portions of the Chesapeake Bay during the evening hours. A squall produced gale-force wind gusts over portions of the Chesapeake Bay during the evening hours. A squall produced gale-force wind gusts over portions of the Chesapeake Bay during the evening hours.\nEvent Narrative: A squall produced an estimated wind gust to 34 knots (39 MPH) near the NOS sensor at the I-695 Francis Scott Key Bridge (FSKM2). A wind gust of 38 knots (44 MPH) was measured by the Hart Miller WeatherFlow sensor (XHRT). A wind gust of 42 knots (48 MPH) was measured by the Tolchester Beach NOS sensor (TCBM2). A wind gust of 36 knots (41 mph) was measured by a mesonet on the westbound span of the US-50/US-301 Chesapeake Bay Bridge (MD065).", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 35.9257 km away, between 2022-03-07 20:14:00 and 2022-03-07 20:35:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 5000.0 and crop damage of 0.0. \n\nEpisode Narrative: A strong cold front produced a line of low-topped showers and squalls that resulted in isolated severe wind gusts and tree and power line damage. A strong cold front produced a line of low-topped showers and squalls that resulted in isolated severe wind gusts and tree and power line damage.\nEvent Narrative: A few trees blew down in the Reisterstown/Owings Mills area. A tree blew down on Ridgelawn Road. A tree blew down on Rosewood Lane. A tree blew down on Deer Lodge Court. A couple of trees blew down in the Fallston/Perry Hall area. A tree blew down on Fork Road. A tree blew down on Bauer Avenue.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 28.6555 km away, between 2022-03-07 20:46:00 and 2022-03-07 20:46:00. The events included records with estimated wind gusts of 48.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A strong cold front produced a squall that resulted in brief storm-force winds over the upper Chesapeake Bay.\nEvent Narrative: A squall produced an estimated wind gust to 48 knots (55 MPH) near the AWOS at Martin State Airport (KMTN) adjacent to the upper Chesapeake Bay.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 29.7019 km away, between 2022-03-12 07:00:00 and 2022-03-12 07:55:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A strong cold front and wave of low pressure produced a squall that resulted in a sudden onset of gale- to storm-force winds. A strong cold front and wave of low pressure produced a squall that resulted in a sudden onset of gale- to storm-force winds. A strong cold front and wave of low pressure produced a squall that resulted in a sudden onset of gale- to storm-force winds. A strong cold front and wave of low pressure produced a squall that resulted in a sudden onset of gale- to storm-force winds. A strong cold front and wave of low pressure produced a squall that resulted in a sudden onset of gale- to storm-force winds. A strong cold front and wave of low pressure produced a squall that resulted in a sudden onset of gale- to storm-force winds. A strong cold front and wave of low pressure produced a squall that resulted in a sudden onset of gale- to storm-force winds. A strong cold front and wave of low pressure produced a squall that resulted in a sudden onset of gale- to storm-force winds. A strong cold front and wave of low pressure produced a squall that resulted in a sudden onset of gale- to storm-force winds. A strong cold front and wave of low pressure produced a squall that resulted in a sudden onset of gale- to storm-force winds. A strong cold front and wave of low pressure produced a squall that resulted in a sudden onset of gale- to storm-force winds. A strong cold front and wave of low pressure produced a squall that resulted in a sudden onset of gale- to storm-force winds. A strong cold front and wave of low pressure produced a squall that resulted in a sudden onset of gale- to storm-force winds. A strong cold front and wave of low pressure produced a squall that resulted in a sudden onset of gale- to storm-force winds. A strong cold front and wave of low pressure produced a squall that resulted in a sudden onset of gale- to storm-force winds. A strong cold front and wave of low pressure produced a squall that resulted in a sudden onset of gale- to storm-force winds. A strong cold front and wave of low pressure produced a squall that resulted in a sudden onset of gale- to storm-force winds. A strong cold front and wave of low pressure produced a squall that resulted in a sudden onset of gale- to storm-force winds. A strong cold front and wave of low pressure produced a squall that resulted in a sudden onset of gale- to storm-force winds. A strong cold front and wave of low pressure produced a squall that resulted in a sudden onset of gale- to storm-force winds. A strong cold front and wave of low pressure produced a squall that resulted in a sudden onset of gale- to storm-force winds.\nEvent Narrative: A squall resulted in a sudden onset of gale-force winds at the Baltimore/Fort McHenry NOS sensor (BLTM2). A squall resulted in a sudden onset of gale-force winds at the Seneca Creek WeatherFlow sensor. A squall resulted in a sudden onset of gale-force winds at the Hart Miller WeatherFlow sensor (XHRT). A squall resulted in a sudden onset of gale-force winds at the I-695 Francis Scott Key Bridge NOS sensor (FSKM2). A squall resulted in a sudden onset of gale-force winds at Oriole Park at Camden Yards (BLTPC) adjacent to the tidal Patapsco River. A squall resulted in a sudden onset of gale-force winds at Lakeland Elementary and Middle School (BLTLK) adjacent to the tidal Patapsco River. A squall resulted in a sudden onset of gale-force winds at the Tolly Point WeatherFlow sensor (XTOL). A squall resulted in a sudden onset of gale-force winds at the Saunders Point Light/Mayo-Triton Beach WxFlow sensor. A squall resulted in a sudden onset of gale-force winds at the Maryland Science Center (BLMRE) adjacent to the tidal Patapsco River. A squall resulted in a sudden onset of gale-force winds at the Greenbury Point WeatherFlow sensor (XGBY). A squall resulted in a sudden onset of gale-force winds at Bayside Beach on the Chesapeake Bay. A squall resulted in a sudden onset of gale-force winds at the Annapolis NOS sensor (APAM2). A squall resulted in a sudden onset of gale-force winds at the Annapolis CBIBS sensor (44063). A squall resulted in a sudden onset of gale-force winds at the ASOS at the U.S. Naval Academy in Annapolis (KNAK) adjacent to the Chesapeake Bay. A squall resulted in a sudden onset of gale-force winds on Salthouse Cove Lane adjacent to the tidal Chester River. A squall resulted in a sudden onset of gale-force winds at the Kent Island WeatherFlow sensor (XKNT). A squall resulted in a sudden onset of gale-force winds at Otto Beach House adjacent to the Chesapeake Bay. A squall resulted in a sudden onset of gale-force winds at the Tolchester Beach NOS sensor (TCBM2). A squall resulted in a sudden onset of gale-force winds at the Thomas Point NOS sensor (TPLM2). A squall resulted in a sudden onset of gale-force winds at Crab Alley Bay adjacent to Eastern Bay. A squall resulted in a sudden onset of gale-force winds at the AWOS at Bay Bridge Airport in Stevensville (KW29) adjacent to the Chesapeake Bay.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 27.9748 km away, between 2022-04-14 15:00:00 and 2022-04-14 16:06:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A strong cold front produced squalls and thunderstorms that resulted in gale-force winds over portions of the Chesapeake Bay and tidal Potomac River during the afternoon and evening hours. A strong cold front produced squalls and thunderstorms that resulted in gale-force winds over portions of the Chesapeake Bay and tidal Potomac River during the afternoon and evening hours. A strong cold front produced squalls and thunderstorms that resulted in gale-force winds over portions of the Chesapeake Bay and tidal Potomac River during the afternoon and evening hours. A strong cold front produced squalls and thunderstorms that resulted in gale-force winds over portions of the Chesapeake Bay and tidal Potomac River during the afternoon and evening hours. A strong cold front produced squalls and thunderstorms that resulted in gale-force winds over portions of the Chesapeake Bay and tidal Potomac River during the afternoon and evening hours. A strong cold front produced squalls and thunderstorms that resulted in gale-force winds over portions of the Chesapeake Bay and tidal Potomac River during the afternoon and evening hours. A strong cold front produced squalls and thunderstorms that resulted in gale-force winds over portions of the Chesapeake Bay and tidal Potomac River during the afternoon and evening hours. A strong cold front produced squalls and thunderstorms that resulted in gale-force winds over portions of the Chesapeake Bay and tidal Potomac River during the afternoon and evening hours. A strong cold front produced squalls and thunderstorms that resulted in gale-force winds over portions of the Chesapeake Bay and tidal Potomac River during the afternoon and evening hours. A strong cold front produced squalls and thunderstorms that resulted in gale-force winds over portions of the Chesapeake Bay and tidal Potomac River during the afternoon and evening hours. A strong cold front produced squalls and thunderstorms that resulted in gale-force winds over portions of the Chesapeake Bay and tidal Potomac River during the afternoon and evening hours. A strong cold front produced squalls and thunderstorms that resulted in gale-force winds over portions of the Chesapeake Bay and tidal Potomac River during the afternoon and evening hours. A strong cold front produced squalls and thunderstorms that resulted in gale-force winds over portions of the Chesapeake Bay and tidal Potomac River during the afternoon and evening hours. A strong cold front produced squalls and thunderstorms that resulted in gale-force winds over portions of the Chesapeake Bay and tidal Potomac River during the afternoon and evening hours. A strong cold front produced squalls and thunderstorms that resulted in gale-force winds over portions of the Chesapeake Bay and tidal Potomac River during the afternoon and evening hours. A strong cold front produced squalls and thunderstorms that resulted in gale-force winds over portions of the Chesapeake Bay and tidal Potomac River during the afternoon and evening hours. A strong cold front produced squalls and thunderstorms that resulted in gale-force winds over portions of the Chesapeake Bay and tidal Potomac River during the afternoon and evening hours. A strong cold front produced squalls and thunderstorms that resulted in gale-force winds over portions of the Chesapeake Bay and tidal Potomac River during the afternoon and evening hours. A strong cold front produced squalls and thunderstorms that resulted in gale-force winds over portions of the Chesapeake Bay and tidal Potomac River during the afternoon and evening hours. A strong cold front produced squalls and thunderstorms that resulted in gale-force winds over portions of the Chesapeake Bay and tidal Potomac River during the afternoon and evening hours.\nEvent Narrative: A wind gust of 34 knots (39 MPH) was measured by a mesonet at the Maryland Science Center (BLMRE) adjacent to the tidal Patapsco River. A squall produced an estimated wind gust to 34 knots (39 MPH) near the Fort McHenry NOS sensor (BLTM2). Wind gusts of up to 36 knots (41 MPH) were measured by the I-695 Francis Scott Key Bridge NOS sensor (FSKM2). A squall produced estimated wind gusts to 34 knots (39 MPH) near a mesonet at Hampstead Hill Academy (BLMHH) adjacent to the tidal Patapsco River. A squall produced an estimated wind gust to 34 knots (39 MPH) near a mesonet at Lakeland Elementary and Middle School (BLTLK) adjacent to the tidal Patapsco River. Wind gusts of up to 44 knots (51 MPH) were measured by the Hart Miller WeatherFlow sensor (XHRT). Wind gusts of up to 39 knots (45 MPH) were measured by the Seneca Creek WeatherFlow sensor. A wind gust of 35 knots (40 MPH) was measured by the ASOS at the United States Naval Academy in Annapolis (KNAK) adjacent to the Chesapeake Bay. Wind gusts of up to 34 knots (39 MPH) were measured by the Saunders Point Light WeatherFlow sensor. A wind gust of 34 knots (39 MPH) was measured by the Annapolis NOS sensor (APAM2). Wind gusts of up to 41 knots (47 MPH) were measured by the Annapolis CBIBS sensor (44063). A squall produced estimated wind gusts to 34 knots (39 MPH) near the Sandy Point WeatherFlow sensor (XSPT). Wind gusts of up to 39 knots (45 MPH) were measured by the Greenbury Point WeatherFlow sensor (XGBY). Wind gusts of up to 42 knots (48 MPH) were measured by a mesonet on Thomas Point Road. A wind gust of 47 knots (54 MPH) was measured by the Thomas Point NOS sensor (TPLM2). A wind gust of 37 knots (43 MPH) was measured by the Tolly Point WeatherFlow sensor (XTOL). A squall produced an estimated wind gust to 34 knots (39 MPH) at a mesonet on Bayside Beach on the Chesapeake Bay. A squall produced an estimated wind gust to 34 knots (39 MPH) near the AWOS at Bay Bridge Airport in Stevensville (KW29) adjacent to the Chesapeake Bay. A wind gust of 34 knots (39 MPH) was measured by the Kent Island WeatherFlow sensor (XKNT). A squall produced an estimated wind gust to 34 knots (39 MPH) at Crab Alley Bay adjacent to Eastern Bay.", "The following events were reported: Flood. These occurred near station USW00093721, approximately 33.0714 km away, between 2022-05-07 03:30:00 and 2022-05-07 09:00:00. The flood was caused by Heavy Rain. Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A line of thunderstorms crossing a warm front caused several instances of flooding across MD on May 6th into May 7th. Residual river flooding continued through May 9th due to excessive runoff. A line of thunderstorms crossing a warm front caused several instances of flooding across MD on May 6th into May 7th. Residual river flooding continued through May 9th due to excessive runoff.\nEvent Narrative: Flooding occurred on Zion Rd. at the Hawlings River. Flooding occurred along Brighton Dam Rd. at the Hawlings River crossing. Water rescue reported around 6 AM.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 34.3885 km away, between 2022-05-22 15:50:00 and 2022-05-22 18:37:00. The events included records with estimated wind gusts of 51.42857142857143 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 17000.0 and crop damage of 0.0. \n\nEpisode Narrative: A strong cold front produced multiple rounds of strong to severe thunderstorms resulting in isolated large hail and scattered wind damage. A strong cold front produced multiple rounds of strong to severe thunderstorms resulting in isolated large hail and scattered wind damage. A strong cold front produced multiple rounds of strong to severe thunderstorms resulting in isolated large hail and scattered wind damage. A strong cold front produced multiple rounds of strong to severe thunderstorms resulting in isolated large hail and scattered wind damage. A strong cold front produced multiple rounds of strong to severe thunderstorms resulting in isolated large hail and scattered wind damage. A strong cold front produced multiple rounds of strong to severe thunderstorms resulting in isolated large hail and scattered wind damage. A strong cold front produced multiple rounds of strong to severe thunderstorms resulting in isolated large hail and scattered wind damage.\nEvent Narrative: Numerous trees, large tree limbs, and wires blew down near Brookeville and Roxbury Mills. A large tree blew down in the 21000 block of MD-97 Georgia Avenue. A tree blew down near the intersection of MD-97 Georgia Avenue and MD-650 New Hampshire Avenue. A tree blew down onto a car near the intersection of MD-650 New Hampshire Avenue and Brighton Knolls Drive. A tree blew down on MD-650 Damascus Road north of MD-108 Laytsonville Road. Trees blew down near the intersection of MD-25 Falls Road and Miller Road. Tree damage was reported near Towson and Pikesville. Large trees blew down in the 8400 block of Greenspring Avenue. Trees blew down on northbound MD-133 Old Court Road prior to MD-25 Falls Road. Tree damage was reported in Glen Arm, including a tree that blew down in the 13000 block of Manor Road. A tree blew down in the 2200 block of Connolly Road. Tree damage was reported in Kingsville, including a tree that blew down blocking the roadway. Tree damage was reported near Silver Spring, including a tree that blew down in the 17000 block of Pinebrook Drive.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 30.8879 km away, between 2022-05-22 16:42:00 and 2022-05-22 19:42:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Multiple lines of thunderstorms produced gale- to storm-force winds over much of the tidal Potomac River and portions of the Chesapeake Bay. Multiple lines of thunderstorms produced gale- to storm-force winds over much of the tidal Potomac River and portions of the Chesapeake Bay. Multiple lines of thunderstorms produced gale- to storm-force winds over much of the tidal Potomac River and portions of the Chesapeake Bay. Multiple lines of thunderstorms produced gale- to storm-force winds over much of the tidal Potomac River and portions of the Chesapeake Bay. Multiple lines of thunderstorms produced gale- to storm-force winds over much of the tidal Potomac River and portions of the Chesapeake Bay. Multiple lines of thunderstorms produced gale- to storm-force winds over much of the tidal Potomac River and portions of the Chesapeake Bay.\nEvent Narrative: A squall produced an estimated wind gust to 34 knots (39 MPH) near the Annapolis CBIBS sensor (44063). Wind gusts of up to 36 knots (41 MPH) were measured by the Tolly Point WeatherFlow sensor (XTOL). A squall produced an estimated wind gust to 34 knots (39 MPH) near the Greenbury Point WeatherFlow sensor (XGBY). A wind gust of 41 knots (47 MPH) was measured by the Thomas Point NOS sensor (TPLM2). A squall produced an estimated wind gust to 34 knots (39 MPH) near the I-695 Francis Scott Key Bridge NOS sensor (FSKM2). A squall produced an estimated wind gust to 34 knots (39 MPH) near the Kent Island WeatherFlow sensor (XKNT).", "The following events were reported: Thunderstorm Wind, Tornado. These occurred near station USW00093721, approximately 30.6332 km away, between 2022-05-27 11:22:00 and 2022-05-27 12:23:00.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 205000.0 and crop damage of 0.0. \n\nEpisode Narrative: Multiple rounds of severe thunderstorms spawned by a strong cold front produced hail, scattered damaging wind gusts, and a couple of tornadoes. Multiple rounds of severe thunderstorms spawned by a strong cold front produced hail, scattered damaging wind gusts, and a couple of tornadoes. Multiple rounds of severe thunderstorms spawned by a strong cold front produced hail, scattered damaging wind gusts, and a couple of tornadoes. Multiple rounds of severe thunderstorms spawned by a strong cold front produced hail, scattered damaging wind gusts, and a couple of tornadoes.\nEvent Narrative: An EF-0 tornado with winds estimated at 80 MPH briefly touched down in Montgomery County, MD, in the town of Olney on the afternoon of Friday, May 27, 2022.||The tornado damage path started at the 3600 block of Toddsbury Lane, where large limbs were downed, with limbs blown to the southeast and north, damaging vehicles parked in the driveway of a residence. The tornado lifted before doing concentrated damage at the end of Toddsbury Lane in and around the cul de sac.||Approximately 12-15 trees were uprooted and snapped in and around this cul de sac. Some of these were uprooted with a diameter of two feet, falling along a walking path located between the cul de sac and Queen Elizabeth Drive. The trees produced damage on both automobiles and on the rear of residences along Queen Elizabeth Drive. Drone footage provided by the Montgomery County Office of Emergency Management and Homeland Security confirmed the linear damage path, along with other trees that were topped in the vicinity of the path.||Eyewitness accounts noted a swirling of debris on the Toddsbury Lane cul de sac. Radar analysis depicted a velocity couplet by KLWX WSR-88D in Sterling, Virginia, that was colocated with the area sustaining damage. Winds were estimated to be 80 MPH due to the snapping and uprooting of both hardwood and softwood trees in the damage path. Tree damage was reported near Ellicott City, including a tree that blew down onto wires in the unit block of Oella Avenue. Tree damage was reported near Long Green, including a tree that blew down onto wires near the intersection of Glen Arm Road East and Hooper Lane. Tree damage was reported near Fallston, with several tree limbs blown down in the area.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 36.0833 km away, between 2022-05-27 12:11:00 and 2022-05-27 20:52:00. The events included records with measured wind gusts of 36.6 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Multiple rounds of thunderstorms produced strong to severe wind gusts over the tidal Potomac River and Chesapeake Bay. Multiple rounds of thunderstorms produced strong to severe wind gusts over the tidal Potomac River and Chesapeake Bay. Multiple rounds of thunderstorms produced strong to severe wind gusts over the tidal Potomac River and Chesapeake Bay. Multiple rounds of thunderstorms produced strong to severe wind gusts over the tidal Potomac River and Chesapeake Bay. Multiple rounds of thunderstorms produced strong to severe wind gusts over the tidal Potomac River and Chesapeake Bay.\nEvent Narrative: A wind gust of 34 knots (39 MPH) was measured by the Saunders Point Light WeatherFlow sensor. Wind gusts of up to 40 knots (46 MPH) were measured by the Kent Island WeatherFlow sensor (XKNT). A wind gust of 39 knots (45 MPH) was measured by the Hart Miller WeatherFlow sensor (XHRT). A wind gust of 36 knots (41 MPH) was measured by the Tolchester Beach NOS sensor (TCBM2). A wind gust of 34 knots (39 MPH) was measured by the Thomas Point NOS sensor (TPLM2).", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 38.4788 km away, between 2022-05-27 12:35:00 and 2022-05-27 12:35:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A frontal system affected much of the mid-Atlantic on May 27. Following a warm frontal passage and ahead of a cold front, a weakly to moderately unstable and moderate to strongly sheared environment developed. As frontal forcing increased, scattered to widespread convective development occurred across the region, with messy, mixed mode storm structures dominating. While the messy storm mode and only somewhat favorable environmental conditions limited the coverage of severe weather, some storms did become strong to severe, producing instances of damaging wind. Convection gradually departed the region during the evening hours.\nEvent Narrative: A few trees were downed in the Rock Hall and Tolchester area. Time estimated from radar.", "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00093721, approximately 18.6282 km away, between 2022-06-02 12:29:00 and 2022-06-02 13:42:00. The events included records with hailstones measuring 28.0 inches.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 20000.0 and crop damage of 0.0. \n\nEpisode Narrative: Scattered to numerous showers and thunderstorms produced isolated instances of large hail and wind damage. Scattered to numerous showers and thunderstorms produced isolated instances of large hail and wind damage.\nEvent Narrative: Quarter size hail was reported in Crofton. About a dozen trees and large tree limbs blew down between Crownsville and Herold Harbor, including two trees that blew down onto houses.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 36.2509 km away, between 2022-06-02 14:21:00 and 2022-06-02 16:24:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Strong to severe thunderstorms produced gusty winds over the tidal Potomac River and Chesapeake Bay. Strong to severe thunderstorms produced gusty winds over the tidal Potomac River and Chesapeake Bay. Strong to severe thunderstorms produced gusty winds over the tidal Potomac River and Chesapeake Bay. Strong to severe thunderstorms produced gusty winds over the tidal Potomac River and Chesapeake Bay. Strong to severe thunderstorms produced gusty winds over the tidal Potomac River and Chesapeake Bay. Strong to severe thunderstorms produced gusty winds over the tidal Potomac River and Chesapeake Bay. Strong to severe thunderstorms produced gusty winds over the tidal Potomac River and Chesapeake Bay. Strong to severe thunderstorms produced gusty winds over the tidal Potomac River and Chesapeake Bay. Strong to severe thunderstorms produced gusty winds over the tidal Potomac River and Chesapeake Bay. Strong to severe thunderstorms produced gusty winds over the tidal Potomac River and Chesapeake Bay.\nEvent Narrative: Wind gusts of up to 42 knots (48 MPH) were measured by the Saunders Point Light WeatherFlow sensor. A squall produced an estimated wind gust to 34 knots (39 MPH) near the Annapolis CBIBS sensor (44063). A squall produced an estimated wind gust to 34 knots (39 MPH) near the Greenbury Point WeatherFlow sensor (XGBY). A squall produced an estimated wind gust to 34 knots (39 MPH) near the Tolly Point WeatherFlow sensor (XTOL). A wind gust of 36 knots (41 MPH) was measured by the Kent Island WeatherFlow sensor (XKNT). A wind gust of 50 knots (58 MPH) was measured by the Thomas Point NOS sensor (TPLM2). A squall produced an estimated wind gust to 34 knots (39 MPH) at Otto Beach House adjacent to the Chesapeake Bay. A squall produced an estimated wind gust to 34 knots (39 MPH) on Beach Side Drive adjacent to the Chesapeake Bay. A wind gust of 42 knots (48 MPH) was measured by the Tolly Point WeatherFlow sensor (XTOL). A wind gust of 38 knots (44 MPH) was measured by a mesonet on Thomas Point Road adjacent to the Chesapeake Bay.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 24.0569 km away, between 2022-06-08 17:45:00 and 2022-06-08 21:41:00. The events included records with estimated wind gusts of 53.125 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 1030000.0 and crop damage of 0.0. \n\nEpisode Narrative: A cold front spawned numerous thunderstorms resulting in scattered instances of damaging wind, some large hail, and a tornado. A cold front spawned numerous thunderstorms resulting in scattered instances of damaging wind, some large hail, and a tornado. A cold front spawned numerous thunderstorms resulting in scattered instances of damaging wind, some large hail, and a tornado. A cold front spawned numerous thunderstorms resulting in scattered instances of damaging wind, some large hail, and a tornado. A cold front spawned numerous thunderstorms resulting in scattered instances of damaging wind, some large hail, and a tornado. A cold front spawned numerous thunderstorms resulting in scattered instances of damaging wind, some large hail, and a tornado. A cold front spawned numerous thunderstorms resulting in scattered instances of damaging wind, some large hail, and a tornado. A cold front spawned numerous thunderstorms resulting in scattered instances of damaging wind, some large hail, and a tornado.\nEvent Narrative: Tree damage was reported near Historic Ellicott City. A tree blew down near the intersection of Ellicott Mills Drive and Burgess Mill Way. A tree blew down near the intersection of Sylvan Lane and Church Road. A tree blew down on US-40 Baltimore National Pike near Tyson Road. A tree blew down near the intersection of New Cut Road and College Avenue. Tree damage was reported near Finksburg, including trees that blew down near the intersection of Hughes Road and MD-91 Gamber Road. Hundreds of trees and wires blew down in Columbia, along with minor shingle and siding damage to about a dozen homes. A tree blew down in the 6700 block of Carlinda Avenue. A 12-inch tree limb blew down onto Cradlerock Way. A tree blew down in the 6200 block of Star Path. Trees blew down on Quiet Hours, Overheart Lane, Tinted Hill, and Setting Star. Multiple trees and large tree limbs over 10 inches in diameter blew down near the intersection of Broken Land Parkway and Stevens Forest Road, and onto a residence on Commodore Court. A tree blew down near the intersection of Old Columbia Road and Riverwood Drive. Trees blew down on northbound US-29 Columbia Pike near Exit 21A/MD-108 Old Annapolis Road. A tree blew down near the intersection of Sandchain Road and Cobbler Court. A tree branch punctured the ceiling of a home with other trees and large branches snapped in the 6500 block of Fruitgift Place. Tree damage was reported between Laytonsville and Germantown. A tree blew down near the intersection of Hawkins Creamery Road and MD-108 Laytonsville Road. A tree blew down near the intersection of MD-27 Ridge Road and Diamondback Drive. Two trees and large tree limbs blew down along I-70 near Marriotsville. A few trees and large tree limbs blew down on the Kendall Ridge Path Bike Loop east of Steel Flower Path. A large tree blew down onto a house in the 5900 block of Prince Georges Street. Numerous large tree limbs were snapped and a flag pole was bent in the 1600 block of Cliff Drive.", "The following events were reported: Flash Flood, Flood. These occurred near station USW00093721, approximately 13.0575 km away, between 2022-06-08 18:45:00 and 2022-06-09 03:15:00. The flood was caused by Heavy Rain. Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Multiple rounds of thunderstorms produced locally heavy rainfall that led to instances of flooding and flash flooding. Multiple rounds of thunderstorms produced locally heavy rainfall that led to instances of flooding and flash flooding. Multiple rounds of thunderstorms produced locally heavy rainfall that led to instances of flooding and flash flooding. Multiple rounds of thunderstorms produced locally heavy rainfall that led to instances of flooding and flash flooding. Multiple rounds of thunderstorms produced locally heavy rainfall that led to instances of flooding and flash flooding. Multiple rounds of thunderstorms produced locally heavy rainfall that led to instances of flooding and flash flooding. Multiple rounds of thunderstorms produced locally heavy rainfall that led to instances of flooding and flash flooding. Multiple rounds of thunderstorms produced locally heavy rainfall that led to instances of flooding and flash flooding.\nEvent Narrative: Two creeks were flowing across Lime Kiln Road near Holly Manor Way. Tiger Branch was out of its banks and flowing into parking lots off of Main Street in Ellicott City. There were reports of multiple cars stuck in flood waters in the city of Catonsville. There reports of multiple roads in the area closed due to flooding around Elkridge, per the Howard County Police Department. Multiple roads were closed around the city of Columbia, per the Howard County Police Department. The gauge along the Patapsco River at Elkridge rose above flood stage, cresting at 16.52 feet at 10:05 PM EST. Hammonds Ferry Road was flooded along the Patapsco River. Backwater flooding likely led to the closure of Furnace Avenue in Elkridge. The Little Patuxent River near Savage exceeded flood stage, cresting at 11.58 feet at 12:15 AM on the 9th of June. The riverside trail was flooded. Water approached the fields off of Bald Eagle Drive and water also approached Brock Bridge Road. There were reports of multiple cars stuck in flood waters in Gwynn Oak.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 35.6734 km away, between 2022-06-08 20:13:00 and 2022-06-08 22:12:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Multiple rounds of thunderstorms produced gale to storm force winds over the tidal Potomac River and Chesapeake Bay. Multiple rounds of thunderstorms produced gale to storm force winds over the tidal Potomac River and Chesapeake Bay. Multiple rounds of thunderstorms produced gale to storm force winds over the tidal Potomac River and Chesapeake Bay. Multiple rounds of thunderstorms produced gale to storm force winds over the tidal Potomac River and Chesapeake Bay. Multiple rounds of thunderstorms produced gale to storm force winds over the tidal Potomac River and Chesapeake Bay. Multiple rounds of thunderstorms produced gale to storm force winds over the tidal Potomac River and Chesapeake Bay. Multiple rounds of thunderstorms produced gale to storm force winds over the tidal Potomac River and Chesapeake Bay. Multiple rounds of thunderstorms produced gale to storm force winds over the tidal Potomac River and Chesapeake Bay.\nEvent Narrative: A squall produced an estimated wind gust to 34 knots (39 MPH) near the Thomas Point NOS sensor (TPLM2). A wind gust of 35 knots (40 MPH) was measured by the Saunders Point Light WeatherFlow sensor. A wind gust of 40 knots (46 MPH) was measured by the Tolly Point WeatherFlow sensor (XTOL). A wind gust of 64 knots (74 MPH) was measured by the Saunders Point Light WeatherFlow sensor. A wind gust of 35 knots (40 MPH) was measured by the Thomas Point NOS sensor (TPLM2). A wind gust of 37 knots (43 MPH) was measured by the Tolly Point WeatherFlow sensor (XTOL). A wind gust of 38 knots (44 MPH) was measured by the Kent Island WeatherFlow sensor (XKNT). A squall produced an estimated wind gust to 34 knots (39 MPH) near the Annapolis CBIBS sensor (44063).", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 34.0586 km away, between 2022-06-14 06:24:00 and 2022-06-14 06:48:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Thunderstorms produced localized gale force winds over the upper Chesapeake Bay. Thunderstorms produced localized gale force winds over the upper Chesapeake Bay. Thunderstorms produced localized gale force winds over the upper Chesapeake Bay. Thunderstorms produced localized gale force winds over the upper Chesapeake Bay. Thunderstorms produced localized gale force winds over the upper Chesapeake Bay. Thunderstorms produced localized gale force winds over the upper Chesapeake Bay. Thunderstorms produced localized gale force winds over the upper Chesapeake Bay.\nEvent Narrative: A squall produced an estimated wind gust to 34 knots (39 MPH) near the Annapolis CBIBS sensor (44063). Wind gusts of up to 38 knots (44 MPH) were measured by the Greenbury Point WeatherFlow sensor (XGBY). A wind gust of 38 knots (44 MPH) was measured by the Tolly Point WeatherFlow sensor (XTOL). A squall produced an estimated wind gust to 34 knots (39 MPH) near the Thomas Point NOS sensor (TPML2). A wind gust of 40 knots (46 MPH) was measured by the Kent Island WeatherFlow sensor (XKNT). A wind gust of 41 knots (47 MPH) was measured by the Saunders Point Light WeatherFlow sensor. A squall produced an estimated wind gust to 34 knots (39 MPH) near the Sandy Point WeatherFlow sensor (XSPT).", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 31.1793 km away, between 2022-07-01 13:50:00 and 2022-07-01 14:08:00. The events included records with estimated wind gusts of 45.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 3000.0 and crop damage of 0.0. \n\nEpisode Narrative: Several pulse to loosely organized multicell thunderstorms produced localized wind damage. Several pulse to loosely organized multicell thunderstorms produced localized wind damage.\nEvent Narrative: A tree was reported down on MD-128 Butler Road. Trees blew down off of Folly Quarter Road near Carroll Mill Road.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 21.6278 km away, between 2022-07-02 18:50:00 and 2022-07-02 20:40:00. The events included records with estimated wind gusts of 47.5 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 3000.0 and crop damage of 0.0. \n\nEpisode Narrative: A few severe thunderstorms produced several instances of wind damage ahead of a cold front during the afternoon and evening hours. A few severe thunderstorms produced several instances of wind damage ahead of a cold front during the afternoon and evening hours.\nEvent Narrative: Trees blew down along MD-108 Ashton Road between Mink Hollow Road and MD-650 New Hampshire Avenue. Several branches blew down near downtown Baltimore.", "The following events were reported: Flash Flood, Flood. These occurred near station USW00093721, approximately 23.441 km away, between 2022-07-02 19:43:00 and 2022-07-02 21:58:00. The flood was caused by Heavy Rain. Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front dropped down from the north, causing showers and thunderstorms to develop. The storm motion was nearly parallel to the boundary, causing some storms to train over the same area. This led to instances of flooding and flash flooding. A cold front dropped down from the north, causing showers and thunderstorms to develop. The storm motion was nearly parallel to the boundary, causing some storms to train over the same area. This led to instances of flooding and flash flooding. A cold front dropped down from the north, causing showers and thunderstorms to develop. The storm motion was nearly parallel to the boundary, causing some storms to train over the same area. This led to instances of flooding and flash flooding. A cold front dropped down from the north, causing showers and thunderstorms to develop. The storm motion was nearly parallel to the boundary, causing some storms to train over the same area. This led to instances of flooding and flash flooding. A cold front dropped down from the north, causing showers and thunderstorms to develop. The storm motion was nearly parallel to the boundary, causing some storms to train over the same area. This led to instances of flooding and flash flooding. A cold front dropped down from the north, causing showers and thunderstorms to develop. The storm motion was nearly parallel to the boundary, causing some storms to train over the same area. This led to instances of flooding and flash flooding.\nEvent Narrative: The road was flooded around Colborne Road. Water was over the curbs along Fulton Avenue. A water rescue was reported on Wise Avenue. A water rescue was reported on Route 40 in White Marsh due to high water. A water rescue was reported along Honeygo Boulevard due to high water. The water level along Whitemarsh Run rapidly reached minor flood stage, cresting at 11.88 feet at 9:25 PM EST on the 2nd of July. The water level fell below flood stage at 10:55 PM EST. ||Water covered the parking lots near the stream, particularly near the Town Center Court.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 35.1449 km away, between 2022-07-02 20:02:00 and 2022-07-02 23:57:00. The events included records with measured wind gusts of 37.2 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A few thunderstorms produced several instances of gale force winds ahead of a cold front during the afternoon and evening hours. A few thunderstorms produced several instances of gale force winds ahead of a cold front during the afternoon and evening hours. A few thunderstorms produced several instances of gale force winds ahead of a cold front during the afternoon and evening hours. A few thunderstorms produced several instances of gale force winds ahead of a cold front during the afternoon and evening hours. A few thunderstorms produced several instances of gale force winds ahead of a cold front during the afternoon and evening hours.\nEvent Narrative: A wind gust of 35 knots (40 MPH) was measured by the Seneca Creek WeatherFlow sensor. Winds of up to 36 knots (41 MPH) were measured by a mesonet on the eastbound span on the US-50/US-301 Chesapeake Bay Bridge (MD066). A wind gust of 35 knots (40 MPH) was measured by a mesonet on the US-50/US-301 Kent Narrows Bridge adjacent to the tidal Chester River. A wind gust of 34 knots (39 MPH) was measured by the Thomas Point NOS sensor (TPLM2). Wind gusts of up to 46 knots (53 MPH) were measured by the ASOS at the U.S. Naval Academy in Annapolis (KNAK) adjacent to the Chesapeake Bay.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 32.6752 km away, between 2022-07-05 15:42:00 and 2022-07-06 01:51:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A few thunderstorms produced sporadic gale force winds near a stalled warm front. A few thunderstorms produced sporadic gale force winds near a stalled warm front. A few thunderstorms produced sporadic gale force winds near a stalled warm front.\nEvent Narrative: A wind gust of 35 knots (40 MPH) was measured by the Seneca Creek WeatherFlow sensor. A wind gust of 36 knots (41 MPH) was measured by the Greenbury Point WeatherFlow sensor (XGBY). A squall produced an estimated wind gust to 34 knots (39 MPH) near the Thomas Point NOS sensor (TPLM2).", "The following events were reported: Thunderstorm Wind, Tornado. These occurred near station USW00093721, approximately 30.827 km away, between 2022-07-05 16:31:00 and 2022-07-05 16:57:00.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 257000.0 and crop damage of 0.0. \n\nEpisode Narrative: A few thunderstorms, including an isolated supercell, produced sporadic wind damage and a couple of tornadoes along a stalled warm front. A few thunderstorms, including an isolated supercell, produced sporadic wind damage and a couple of tornadoes along a stalled warm front. A few thunderstorms, including an isolated supercell, produced sporadic wind damage and a couple of tornadoes along a stalled warm front. A few thunderstorms, including an isolated supercell, produced sporadic wind damage and a couple of tornadoes along a stalled warm front.\nEvent Narrative: A supercell thunderstorm spawned a brief EF1 tornado just north of Bowie, MD in Prince Georges County late on Tuesday afternoon July 5th, 2022, between 5:31 and 5:34 PM EDT. This supercell spawned along the Howard/Montgomery County line as a result of a remnant mesoscale convective vortex moving through the region which had moved through the Ohio Valley earlier in the day. It evolved into a cluster of cells initially before splitting off into an individual supercell that would develop rotation as it moved out of southeastern Montgomery County into northwestern Prince Georges County. The tornado caused extensive tree damage in the Somerset subdivision just north of Bowie, MD. There was also one instance where a tree had fallen on top of a residence near the intersection of Stafford Lane near Saber Lane. However, there were several other trees down in the area outside of the more concentrated tornadic damage, particularly along Buckingham Drive perpendicular to White Marsh Branch. At this location along Buckingham Drive, trees fell upon power lines, snapping several supporting utility poles. The tornado initially touched down around Tarragon Lane and tracked eastward over the Bowie High School Annex before tracking into the Somerset subdivision, where the majority of the damage was observed. The tornado would then lift just before reaching southern portions of Whitemarsh Park. Trees blew down between MD-2 and Muddy Creek Road east of HopScratch Farms. Trees blew down off of Owensville Road northwest of Galesville. A supercell thunderstorm spawned a brief tornado just north of Harwood, Maryland (4 miles southwest of Londontowne) in Anne Arundel County late Tuesday afternoon July 5th, 2022, between 5:55 and 5:56 PM EDT. This supercell originally developed along the Howard/Montgomery County line as a result of a remnant mesoscale convective vortex (MCV) moving through the region which had moved through the Ohio Valley earlier in the day. It evolved into a cluster of cells initially before splitting off into an individual supercell that would develop rotation as it moved out of southeastern Montgomery County into northwestern Prince Georges County. The cell dropped a tornado earlier in the afternoon near Bowie, and would then cycle to produce the second tornado in Harwood. A broadcast media partner provided video and eyewitness evidence of a brief spin-up tornado while located at the intersection of Birdsville Road and MD-2 Solomons Island Road. This individual noted that the tornado was located just to their north in an open field and was on the ground for about one minute.", "The following events were reported: Flood. These occurred near station USW00093721, approximately 7.2677 km away, between 2022-07-07 01:30:00 and 2022-07-07 03:30:00. The flood was caused by Heavy Rain. Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Heavy rainfall from thunderstorms led to isolated instances of flooding.\nEvent Narrative: Several roads were partially blocked briefly by high standing water near Glen Burnie, Odenton, and Pasadena.", "The following events were reported: Flood. These occurred near station USW00093721, approximately 29.6014 km away, between 2022-07-09 09:09:00 and 2022-07-09 12:09:00. The flood was caused by Heavy Rain. Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A weak cold front slowly moved through the area later on the 8th into the 9th. A wave of low pressure tracked along the front, passing through the area during that time. Plenty of moisture ahead of the boundary along with moderate instability led to areas of heavy rainfall. The slower storm motion and training storms led to areas of flooding and flash flooding.\nEvent Narrative: Brick Church Road was closed due go high water.", "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00093721, approximately 34.1997 km away, between 2022-07-12 15:20:00 and 2022-07-12 17:45:00. The events included records with hailstones measuring 54.57142857142857 inches.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 724000.0 and crop damage of 0.0. \n\nEpisode Narrative: An outbreak of significant severe weather occurred during the afternoon and evening hours of Tuesday, July 12th, 2022. An unseasonably strong cold front interacted with a high instability airmass to result in several bowing lines of thunderstorms, which maintained their organization and intensity due to strong atmospheric wind shear. Swaths of widespread damaging winds were observed, much of which was considerable. A couple of tornadoes were also confirmed, along with some significant hail. A wind gust of over 100 MPH was measured in one of the most powerful storms over eastern West Virginia. An outbreak of significant severe weather occurred during the afternoon and evening hours of Tuesday, July 12th, 2022. An unseasonably strong cold front interacted with a high instability airmass to result in several bowing lines of thunderstorms, which maintained their organization and intensity due to strong atmospheric wind shear. Swaths of widespread damaging winds were observed, much of which was considerable. A couple of tornadoes were also confirmed, along with some significant hail. A wind gust of over 100 MPH was measured in one of the most powerful storms over eastern West Virginia. An outbreak of significant severe weather occurred during the afternoon and evening hours of Tuesday, July 12th, 2022. An unseasonably strong cold front interacted with a high instability airmass to result in several bowing lines of thunderstorms, which maintained their organization and intensity due to strong atmospheric wind shear. Swaths of widespread damaging winds were observed, much of which was considerable. A couple of tornadoes were also confirmed, along with some significant hail. A wind gust of over 100 MPH was measured in one of the most powerful storms over eastern West Virginia. An outbreak of significant severe weather occurred during the afternoon and evening hours of Tuesday, July 12th, 2022. An unseasonably strong cold front interacted with a high instability airmass to result in several bowing lines of thunderstorms, which maintained their organization and intensity due to strong atmospheric wind shear. Swaths of widespread damaging winds were observed, much of which was considerable. A couple of tornadoes were also confirmed, along with some significant hail. A wind gust of over 100 MPH was measured in one of the most powerful storms over eastern West Virginia. An outbreak of significant severe weather occurred during the afternoon and evening hours of Tuesday, July 12th, 2022. An unseasonably strong cold front interacted with a high instability airmass to result in several bowing lines of thunderstorms, which maintained their organization and intensity due to strong atmospheric wind shear. Swaths of widespread damaging winds were observed, much of which was considerable. A couple of tornadoes were also confirmed, along with some significant hail. A wind gust of over 100 MPH was measured in one of the most powerful storms over eastern West Virginia. An outbreak of significant severe weather occurred during the afternoon and evening hours of Tuesday, July 12th, 2022. An unseasonably strong cold front interacted with a high instability airmass to result in several bowing lines of thunderstorms, which maintained their organization and intensity due to strong atmospheric wind shear. Swaths of widespread damaging winds were observed, much of which was considerable. A couple of tornadoes were also confirmed, along with some significant hail. A wind gust of over 100 MPH was measured in one of the most powerful storms over eastern West Virginia. An outbreak of significant severe weather occurred during the afternoon and evening hours of Tuesday, July 12th, 2022. An unseasonably strong cold front interacted with a high instability airmass to result in several bowing lines of thunderstorms, which maintained their organization and intensity due to strong atmospheric wind shear. Swaths of widespread damaging winds were observed, much of which was considerable. A couple of tornadoes were also confirmed, along with some significant hail. A wind gust of over 100 MPH was measured in one of the most powerful storms over eastern West Virginia. An outbreak of significant severe weather occurred during the afternoon and evening hours of Tuesday, July 12th, 2022. An unseasonably strong cold front interacted with a high instability airmass to result in several bowing lines of thunderstorms, which maintained their organization and intensity due to strong atmospheric wind shear. Swaths of widespread damaging winds were observed, much of which was considerable. A couple of tornadoes were also confirmed, along with some significant hail. A wind gust of over 100 MPH was measured in one of the most powerful storms over eastern West Virginia. An outbreak of significant severe weather occurred during the afternoon and evening hours of Tuesday, July 12th, 2022. An unseasonably strong cold front interacted with a high instability airmass to result in several bowing lines of thunderstorms, which maintained their organization and intensity due to strong atmospheric wind shear. Swaths of widespread damaging winds were observed, much of which was considerable. A couple of tornadoes were also confirmed, along with some significant hail. A wind gust of over 100 MPH was measured in one of the most powerful storms over eastern West Virginia. An outbreak of significant severe weather occurred during the afternoon and evening hours of Tuesday, July 12th, 2022. An unseasonably strong cold front interacted with a high instability airmass to result in several bowing lines of thunderstorms, which maintained their organization and intensity due to strong atmospheric wind shear. Swaths of widespread damaging winds were observed, much of which was considerable. A couple of tornadoes were also confirmed, along with some significant hail. A wind gust of over 100 MPH was measured in one of the most powerful storms over eastern West Virginia. An outbreak of significant severe weather occurred during the afternoon and evening hours of Tuesday, July 12th, 2022. An unseasonably strong cold front interacted with a high instability airmass to result in several bowing lines of thunderstorms, which maintained their organization and intensity due to strong atmospheric wind shear. Swaths of widespread damaging winds were observed, much of which was considerable. A couple of tornadoes were also confirmed, along with some significant hail. A wind gust of over 100 MPH was measured in one of the most powerful storms over eastern West Virginia. An outbreak of significant severe weather occurred during the afternoon and evening hours of Tuesday, July 12th, 2022. An unseasonably strong cold front interacted with a high instability airmass to result in several bowing lines of thunderstorms, which maintained their organization and intensity due to strong atmospheric wind shear. Swaths of widespread damaging winds were observed, much of which was considerable. A couple of tornadoes were also confirmed, along with some significant hail. A wind gust of over 100 MPH was measured in one of the most powerful storms over eastern West Virginia. An outbreak of significant severe weather occurred during the afternoon and evening hours of Tuesday, July 12th, 2022. An unseasonably strong cold front interacted with a high instability airmass to result in several bowing lines of thunderstorms, which maintained their organization and intensity due to strong atmospheric wind shear. Swaths of widespread damaging winds were observed, much of which was considerable. A couple of tornadoes were also confirmed, along with some significant hail. A wind gust of over 100 MPH was measured in one of the most powerful storms over eastern West Virginia. An outbreak of significant severe weather occurred during the afternoon and evening hours of Tuesday, July 12th, 2022. An unseasonably strong cold front interacted with a high instability airmass to result in several bowing lines of thunderstorms, which maintained their organization and intensity due to strong atmospheric wind shear. Swaths of widespread damaging winds were observed, much of which was considerable. A couple of tornadoes were also confirmed, along with some significant hail. A wind gust of over 100 MPH was measured in one of the most powerful storms over eastern West Virginia. An outbreak of significant severe weather occurred during the afternoon and evening hours of Tuesday, July 12th, 2022. An unseasonably strong cold front interacted with a high instability airmass to result in several bowing lines of thunderstorms, which maintained their organization and intensity due to strong atmospheric wind shear. Swaths of widespread damaging winds were observed, much of which was considerable. A couple of tornadoes were also confirmed, along with some significant hail. A wind gust of over 100 MPH was measured in one of the most powerful storms over eastern West Virginia. An outbreak of significant severe weather occurred during the afternoon and evening hours of Tuesday, July 12th, 2022. An unseasonably strong cold front interacted with a high instability airmass to result in several bowing lines of thunderstorms, which maintained their organization and intensity due to strong atmospheric wind shear. Swaths of widespread damaging winds were observed, much of which was considerable. A couple of tornadoes were also confirmed, along with some significant hail. A wind gust of over 100 MPH was measured in one of the most powerful storms over eastern West Virginia. An outbreak of significant severe weather occurred during the afternoon and evening hours of Tuesday, July 12th, 2022. An unseasonably strong cold front interacted with a high instability airmass to result in several bowing lines of thunderstorms, which maintained their organization and intensity due to strong atmospheric wind shear. Swaths of widespread damaging winds were observed, much of which was considerable. A couple of tornadoes were also confirmed, along with some significant hail. A wind gust of over 100 MPH was measured in one of the most powerful storms over eastern West Virginia. An outbreak of significant severe weather occurred during the afternoon and evening hours of Tuesday, July 12th, 2022. An unseasonably strong cold front interacted with a high instability airmass to result in several bowing lines of thunderstorms, which maintained their organization and intensity due to strong atmospheric wind shear. Swaths of widespread damaging winds were observed, much of which was considerable. A couple of tornadoes were also confirmed, along with some significant hail. A wind gust of over 100 MPH was measured in one of the most powerful storms over eastern West Virginia. An outbreak of significant severe weather occurred during the afternoon and evening hours of Tuesday, July 12th, 2022. An unseasonably strong cold front interacted with a high instability airmass to result in several bowing lines of thunderstorms, which maintained their organization and intensity due to strong atmospheric wind shear. Swaths of widespread damaging winds were observed, much of which was considerable. A couple of tornadoes were also confirmed, along with some significant hail. A wind gust of over 100 MPH was measured in one of the most powerful storms over eastern West Virginia. An outbreak of significant severe weather occurred during the afternoon and evening hours of Tuesday, July 12th, 2022. An unseasonably strong cold front interacted with a high instability airmass to result in several bowing lines of thunderstorms, which maintained their organization and intensity due to strong atmospheric wind shear. Swaths of widespread damaging winds were observed, much of which was considerable. A couple of tornadoes were also confirmed, along with some significant hail. A wind gust of over 100 MPH was measured in one of the most powerful storms over eastern West Virginia. An outbreak of significant severe weather occurred during the afternoon and evening hours of Tuesday, July 12th, 2022. An unseasonably strong cold front interacted with a high instability airmass to result in several bowing lines of thunderstorms, which maintained their organization and intensity due to strong atmospheric wind shear. Swaths of widespread damaging winds were observed, much of which was considerable. A couple of tornadoes were also confirmed, along with some significant hail. A wind gust of over 100 MPH was measured in one of the most powerful storms over eastern West Virginia.\nEvent Narrative: Multiple trees blew down in the 200 block of Morningstar Way. Multiple trees blew down along Lees Mill Road near Aspen Run. Roofing was partially blown off the roof of a bank and numerous trees and wires blew down in Upperco. Numerous trees blew down around Cockeysville. Approximately 10 trees blew down along Phoenix Road. Numerous trees and power lines blew down along Paper Mill Road. Numerous trees were snapped and uprooted in the Monkton, Sparks, and Hereford areas nearby, including along Blenheim Road North. Numerous trees and wires blew down near Pleasant Furnace, including along MD-147 Harford Road near Reckford Road. Several large trees blew down in the 11000 block of MD-147 Harford Road. Numerous trees were uprooted and snapped near Fallston and Darlington, including near Carrs Mill Road, and along a five-mile stretch of Putnam Road near Fallston to just south of Darlington. Quarter size hail was reported near Jarrettsville and Fallston. Numerous trees blew down in the Abingdon area. A tree snapped at a residence on Merrick Way. A tree blew through the windshield of a vehicle near the intersection of MD-943 Emmorton Road and Holly Wreath Drive. Trees blew down on MD-140 Baltimore Boulevard just east of the intersection with Dede Road. Several large trees and tree limbs blew down in the 4700 block of MD-32 Sykesville Road. Multiple trees blew down near the intersection of Majestic Lane and Milan Way. Two large trees blew down near the intersection of MD-197 Laurel Bowie Road and Old Chapel Road. Numerous trees blew down around Davidsonville, including at least one onto a house. MD-424 Davidsonville Road was blocked by downed trees near Bell Branch Road. Trees also blew down nearby along US-50/US-301 John Hanson Highway and MD-450 Defense Highway. Several trees blew down in Harwood. Several trees and wires blew down in the 2000 block of MD-424 Davidsonville Road. A large tree blew down onto a house in the 2000 block of Swann Way. Power lines blew down in the 2000 block of Rutland Road. A tree blew down onto the roof of a house in the 900 block of Bramleigh Lane. Tree damage was reported near Belvedere Heights, including in the 900 block of Blue Fox Way. Tree damage was reported near Annapolis, including on MD-665 Aris T. Allen Boulevard/Forest Drive near Chinquapin Road. Several trees blew down around Highland Beach.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 32.7389 km away, between 2022-07-12 15:59:00 and 2022-07-12 17:54:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Several severe lines of thunderstorms produced gale to storm force winds ahead of a strong cold front. Several severe lines of thunderstorms produced gale to storm force winds ahead of a strong cold front. Several severe lines of thunderstorms produced gale to storm force winds ahead of a strong cold front. Several severe lines of thunderstorms produced gale to storm force winds ahead of a strong cold front. Several severe lines of thunderstorms produced gale to storm force winds ahead of a strong cold front. Several severe lines of thunderstorms produced gale to storm force winds ahead of a strong cold front.\nEvent Narrative: A squall produced an estimated wind gust to 34 knots (39 MPH) near the AWOS at Martin State Airport (KMTN) adjacent to the Chesapeake Bay. A wind gust of 35 knots (40 MPH) was measured by the ASOS at the U.S. Naval Academy in Annapolis (KNAK) adjacent to the Chesapeake Bay. Wind gusts of up to 41 knots (47 MPH) were measured by the Greenbury Point WeatherFlow sensor (XGBY). Wind gusts of up to 34 knots (39 MPH) were measured by the Tolly Point WeatherFlow sensor (XTOL). A wind gust of 37 knots (43 MPH) was measured by the Saunders Point Light WeatherFlow sensor. A wind gust of 37 knots (43 MPH) was measured by the Kent Island WeatherFlow sensor (XKNT).", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 23.2316 km away, between 2022-07-16 13:51:00 and 2022-07-16 16:05:00. The events included records with estimated wind gusts of 53.75 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 53000.0 and crop damage of 0.0. \n\nEpisode Narrative: Several thunderstorms produced localized wind damage ahead of a weak cold front. Several thunderstorms produced localized wind damage ahead of a weak cold front. Several thunderstorms produced localized wind damage ahead of a weak cold front. Several thunderstorms produced localized wind damage ahead of a weak cold front.\nEvent Narrative: Several trees and wires blew down in the Pikesville area. Wires blew down in the 8200 block of Anita Road. A tree and wires blew down near the intersection of MD-25 Falls Road and Ivy Brook Farm Court. Wires blew down near the intersection of MD-25 Falls Road and Timothy Road. Trees blew down on MD-32 Patuxent Freeway near MD-3 Crain Highway. Trees blew down on MD-3 Crain Highway near Riedel Road. Trees blew down onto wires bringing down a pole on River Road in Herald Harbor. Trees blew down near the intersection of MD-178 Generals Highway and Honeysuckle Lane. Numerous trees blew down blocking roadways between Edgewater and Harwood. Fifteen trees blew down at a residence in Davidsonville.", "The following events were reported: Flash Flood, Flood. These occurred near station USW00093721, approximately 23.4733 km away, between 2022-07-16 15:40:00 and 2022-07-16 22:15:00. The flood was caused by Heavy Rain. Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: An upper-level trough was overhead while a weak boundary was stalled nearby. Plenty of moisture around high pressure over the Atlantic led to the development of showers and thunderstorms. With slower storm motion, this led to instances of flooding and flash flooding. An upper-level trough was overhead while a weak boundary was stalled nearby. Plenty of moisture around high pressure over the Atlantic led to the development of showers and thunderstorms. With slower storm motion, this led to instances of flooding and flash flooding. An upper-level trough was overhead while a weak boundary was stalled nearby. Plenty of moisture around high pressure over the Atlantic led to the development of showers and thunderstorms. With slower storm motion, this led to instances of flooding and flash flooding. An upper-level trough was overhead while a weak boundary was stalled nearby. Plenty of moisture around high pressure over the Atlantic led to the development of showers and thunderstorms. With slower storm motion, this led to instances of flooding and flash flooding. An upper-level trough was overhead while a weak boundary was stalled nearby. Plenty of moisture around high pressure over the Atlantic led to the development of showers and thunderstorms. With slower storm motion, this led to instances of flooding and flash flooding. An upper-level trough was overhead while a weak boundary was stalled nearby. Plenty of moisture around high pressure over the Atlantic led to the development of showers and thunderstorms. With slower storm motion, this led to instances of flooding and flash flooding. An upper-level trough was overhead while a weak boundary was stalled nearby. Plenty of moisture around high pressure over the Atlantic led to the development of showers and thunderstorms. With slower storm motion, this led to instances of flooding and flash flooding. An upper-level trough was overhead while a weak boundary was stalled nearby. Plenty of moisture around high pressure over the Atlantic led to the development of showers and thunderstorms. With slower storm motion, this led to instances of flooding and flash flooding. An upper-level trough was overhead while a weak boundary was stalled nearby. Plenty of moisture around high pressure over the Atlantic led to the development of showers and thunderstorms. With slower storm motion, this led to instances of flooding and flash flooding.\nEvent Narrative: Defense Highway near Huntwood Drive was flooded due to high water. Several roads were blocked by high, swift water near Crofton. Several creeks were out of their banks flowing across roadways. Several roads were blocked by high, swift water near Crownsville. Several creeks were out of their banks flowing across roadways. Several roads were blocked by high water in the Edgewater area. MD-214 Central AVenue was closed due to swift moving water. Beards Creek was out of its banks. A vehicle became stranded when attempting to drive into high water at Beards Creek on MD-214 Central Avenue. Several instances of flooding were reported in northern and central Baltimore City. Flooding was reported on MD-253 May Road and Shore Drive. Flooding reported on MD-214 central Avenue near Brick Church/Beards Point Road. Flooding blocked several lanes of MD-193 Greenbelt Road near MD-564 Lanham Severn Road.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 36.9103 km away, between 2022-07-16 16:20:00 and 2022-07-16 18:25:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Several thunderstorms produced localized gusty winds ahead of a weak cold front. Several thunderstorms produced localized gusty winds ahead of a weak cold front.\nEvent Narrative: Wind gusts of up to 41 knots (47 MPH) were measured by a mesonet on Thomas Point Road adjacent to the Chesapeake Bay. A squall produced an estimated wind gust to 34 knots (39 MPH) near a mesonet on Frederick Avenue adjacent to the Chesapeake Bay.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 39.0005 km away, between 2022-07-18 14:45:00 and 2022-07-18 15:59:00. The events included records with estimated wind gusts of 51.81818181818182 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 33000.0 and crop damage of 0.0. \n\nEpisode Narrative: Several bands of thunderstorms containing damaging winds developed along a cold front. Several bands of thunderstorms containing damaging winds developed along a cold front. Several bands of thunderstorms containing damaging winds developed along a cold front. Several bands of thunderstorms containing damaging winds developed along a cold front. Several bands of thunderstorms containing damaging winds developed along a cold front. Several bands of thunderstorms containing damaging winds developed along a cold front. Several bands of thunderstorms containing damaging winds developed along a cold front. Several bands of thunderstorms containing damaging winds developed along a cold front. Several bands of thunderstorms containing damaging winds developed along a cold front. Several bands of thunderstorms containing damaging winds developed along a cold front. Several bands of thunderstorms containing damaging winds developed along a cold front.\nEvent Narrative: Trees blew down on westbound I-70 Baltimore National Pike between Mile Marker 68.0 and Exit 62/MD-75 Green Valley Road. Large tree limbs blew down, a gutter was blown off, and fencing blew down at a residence in the 7200 block of Honeybush Drive. A tree blew down in the 7400 block of Watersville Road. Tree damage was reported near Winfield, including a tree that blew down onto wires in the 3700 block of Baker Road. Trees blew down near the intersection of MD-97 Washington Road and MD-26 Liberty Road. A tree blew down in the 200 block of West Old Liberty Road. Tree damage was reported near Gamber, including a tree that blew down in the 4200 block of London Bridge Road. Tree damage was reported near McDonogh, including a tree that blew down onto power lines in the 300 block of Garrison Forest Road. A large tree two feet in diameter and numerous large tree limbs blew down near the intersection of International Circle and International Drive. Trees blew down north of Cockeysville, including one onto three cars on Dove Creek Way. Tree damage was reported near Parkville, including a tree that blew down onto wires near the intersection of Opal Road and Garnet Road. Tree damage was reported northwest of Abingdon, including a tree that blew down near the intersection of South Tollgate Road and Singer Road. Tree damage was reported southeast of Pleasant Furnace, including a tree that blew down on Jerusalem Road near Valley Brook Drive.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 36.438 km away, between 2022-07-18 16:00:00 and 2022-07-18 18:15:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Several bands of thunderstorms containing gusty winds developed along a cold front. Several bands of thunderstorms containing gusty winds developed along a cold front. Several bands of thunderstorms containing gusty winds developed along a cold front. Several bands of thunderstorms containing gusty winds developed along a cold front. Several bands of thunderstorms containing gusty winds developed along a cold front.\nEvent Narrative: A squall produced an estimated wind gust to 34 knots (39 MPH) near the I-695 Francis Scott Key Bridge NOS sensor (FSKM2). A squall produced estimated wind gusts to 34 knots (39 MPH) near the Seneca Creek WeatherFlow sensor. A squall produced an estimated wind gust to 34 knots (39 MPH) near the Tolchester Beach NOS sensor (TCBM2). Wind gusts of up to 39 knots (45 MPH) were measured by a mesonet on Indian Field Court adjacent to the Chesapeake Bay. Wind gusts of up to 55 knots (63 MPH) was measured by a mesonet on Salthouse Cove Lane adjacent to the tidal Chester River.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 49.971 km away, between 2022-07-18 18:10:00 and 2022-07-18 18:20:00. The events included records with measured wind gusts of 57.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A storm moved into the eastern shore of Maryland and produced strong winds and some wind damage. A storm moved into the eastern shore of Maryland and produced strong winds and some wind damage.\nEvent Narrative: Salthouse Cove Lane mesonet reports 64 mph gust. WeatherFlow station. Time of gust given in report. Salthouse Cove Lane gusted to 67 mph. Time given in report. WeatherFlow mesonet station.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 35.8332 km away, between 2022-07-21 16:50:00 and 2022-07-21 17:00:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A couple of thunderstorms produced sporadic instances of gusty winds when a surface trough interacted with the bay breeze. A couple of thunderstorms produced sporadic instances of gusty winds when a surface trough interacted with the bay breeze. A couple of thunderstorms produced sporadic instances of gusty winds when a surface trough interacted with the bay breeze.\nEvent Narrative: Wind gusts of up to 39 knots (45 MPH) were measured by the Saunders Point Light WeatherFlow sensor. A squall produced an estimated wind gust to 34 knots (39 MPH) near the Tolly Point WeatherFlow sensor (XTOL). Wind gusts of up to 40 knots (46 MPH) were measured by the Thomas Point NOS sensor (TPLM2).", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 14.6299 km away, between 2022-07-23 19:24:00 and 2022-07-23 19:24:00. The events included records with estimated wind gusts of 37.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front sparked showers and thunderstorms, some of which resulted in gusty winds near Baltimore Inner Harbor and the tidal Potomac River.\nEvent Narrative: A squall produced estimated wind gusts up to 37 knots near one of the I-695 Francis Scott Key Bridge NOS sensor (FSNM2).", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 35.083 km away, between 2022-07-28 19:42:00 and 2022-07-28 19:55:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A few thunderstorms produced localized gusty winds over the area waterways. A few thunderstorms produced localized gusty winds over the area waterways. A few thunderstorms produced localized gusty winds over the area waterways.\nEvent Narrative: A wind gust of 34 knots (39 MPH) was measured by the Tolchester Beach NOS sensor (TCBM2). A wind gust of 36 knots (41 MPH) was measured by the Greenbury Point WeatherFlow sensor (XGBY). A squall produced an estimated wind gust to 34 knots (39 MPH) near the Thomas Point NOS sensor (TPLM2).", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 33.4301 km away, between 2022-08-02 14:29:00 and 2022-08-02 14:29:00. The events included records with estimated wind gusts of 34.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: An isolated thunderstorm produced gusty winds over the middle Chesapeake Bay and tidal Choptank River.\nEvent Narrative: A squall produced an estimated wind gust to 34 knots (39 MPH) near the Tolly Point WeatherFlow sensor (XTOL).", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 28.3189 km away, between 2022-08-04 16:05:00 and 2022-08-04 16:05:00. The events included records with estimated wind gusts of 39.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 1000.0 and crop damage of 0.0. \n\nEpisode Narrative: A surface trough ignited numerous showers and thunderstorms that resulted in scattered instances of damaging wind gusts and sporadic large hail.\nEvent Narrative: Power lines were reported down along VA-600 Campbell Road near VA-686 Paddock Wood Road.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 28.0598 km away, between 2022-08-04 16:30:00 and 2022-08-04 19:00:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Strong to severe thunderstorms produced numerous instances of gale to storm force winds over the area waterways. Strong to severe thunderstorms produced numerous instances of gale to storm force winds over the area waterways. Strong to severe thunderstorms produced numerous instances of gale to storm force winds over the area waterways. Strong to severe thunderstorms produced numerous instances of gale to storm force winds over the area waterways. Strong to severe thunderstorms produced numerous instances of gale to storm force winds over the area waterways. Strong to severe thunderstorms produced numerous instances of gale to storm force winds over the area waterways. Strong to severe thunderstorms produced numerous instances of gale to storm force winds over the area waterways. Strong to severe thunderstorms produced numerous instances of gale to storm force winds over the area waterways. Strong to severe thunderstorms produced numerous instances of gale to storm force winds over the area waterways. Strong to severe thunderstorms produced numerous instances of gale to storm force winds over the area waterways. Strong to severe thunderstorms produced numerous instances of gale to storm force winds over the area waterways. Strong to severe thunderstorms produced numerous instances of gale to storm force winds over the area waterways. Strong to severe thunderstorms produced numerous instances of gale to storm force winds over the area waterways. Strong to severe thunderstorms produced numerous instances of gale to storm force winds over the area waterways. Strong to severe thunderstorms produced numerous instances of gale to storm force winds over the area waterways. Strong to severe thunderstorms produced numerous instances of gale to storm force winds over the area waterways. Strong to severe thunderstorms produced numerous instances of gale to storm force winds over the area waterways. Strong to severe thunderstorms produced numerous instances of gale to storm force winds over the area waterways. Strong to severe thunderstorms produced numerous instances of gale to storm force winds over the area waterways. Strong to severe thunderstorms produced numerous instances of gale to storm force winds over the area waterways. Strong to severe thunderstorms produced numerous instances of gale to storm force winds over the area waterways. Strong to severe thunderstorms produced numerous instances of gale to storm force winds over the area waterways. Strong to severe thunderstorms produced numerous instances of gale to storm force winds over the area waterways.\nEvent Narrative: Wind gusts of up to 53 knots (61 MPH) were measured by the Hart Miller WeatherFlow sensor (XHRT). Wind gusts of up to 54 knots (62 MPH) were measured by the Seneca Creek WeatherFlow sensor. Wind gusts of up to 53 knots (61 MPH) were measured by the Tolchester Beach NOS sensor (TCBM2). A squall produced estimated wind gusts to 34 knots (39 MPH) near the Annapolis NOS sensor (APAM2). A squall produced estimated wind gusts to 34 knots (39 MPH) near the Annapolis CBIBS sensor (44063). A wind gust of 35 knots (40 MPH) was measured by a mesonet near Cape Saint Claire (EW5391). Wind gusts of up to 45 knots (52 MPH) were meausred by the Greenbury Point WeatherFlow sensor (XGBY). Wind gusts of up to 42 knots (48 MPH) were measured by a mesonet on the eastbound span of the US-50/US-301 Chesapeake Bay Bridge (MD066). Wind gusts of up to 41 knots (47 MPH) were measured by the Tolly Point WeatherFlow sensor (XTOL). Winds of up to 47 knots (54 MPH) were measured by a mesonet on the westbound span of the US-50/US-301 Chesapeake Bay Bridge (MD067). Wind gusts of up to 34 knots (39 MPH) were measured by the Kent Island WeatherFlow sensor (XKNT). A squall produced an estimated wind gust to 34 knots (39 MPH) near the Sandy Point WeatherFlow sensor (XSPT). Wind gusts of up to 49 knots (56 MPH) were measured by the Baltimore NOS sensor (BLTM2). Wind gusts of up to 45 knots (52 MPH) were measured by the Saunders Point Light WeatherFlow sensor. Wind gusts of up to 40 knots (46 MPH) were measured by a mesonet at Otto Beach House adjacent to the Chesapeake Bay and Eastern Bay. A wind gust of 36 knots (41 MPH) was measured by the Thomas Point NOS sensor (TPLM2). A wind gust of 42 knots (48 MPH) was measured by a mesonet at Crab Alley Bay adjacent to Eastern Bay. A squall produced an estimated wind gust to 34 knots (39 MPH) near a mesonet at Hampstead Hill Academy (BLMHH) adjacent to the tidal Patapsco River. Wind gusts of up to 43 knots (50 MPH) were measured by a mesonet in Baltimore (GW1324) adjacent to the tidal Patapsco River. A squall produced an estimated wind gust to 34 knots (39 MPH) near a mesonet at Morrell Park School (BLTIM) adjacent to the tidal Patapsco River. Wind gusts of up to 43 knots (49 MPH) were measured by one of the I-695 Francis Scott Key Bridge NOS sensors (FSKM2). Wind gusts of up to 58 knots (67 MPH) were measured by a mesonet on the I-695 Francis Scott Key Bridge (MD120). Wind gusts of 34 knots (39 MPH) were meausred by one of the I-695 Francis Scott Key Bridge NOS sensors (FSNM2).", "The following events were reported: Lightning, Thunderstorm Wind. These occurred near station USW00093721, approximately 27.6733 km away, between 2022-08-04 16:43:00 and 2022-08-04 18:26:00.The events resulted in 0 injuries and 1 fatalities. The events caused property damage valued at 114000.0 and crop damage of 0.0. \n\nEpisode Narrative: A surface trough ignited numerous showers and thunderstorms that resulted in scattered instances of damaging wind gusts and sporadic large hail. A surface trough ignited numerous showers and thunderstorms that resulted in scattered instances of damaging wind gusts and sporadic large hail. A surface trough ignited numerous showers and thunderstorms that resulted in scattered instances of damaging wind gusts and sporadic large hail. A surface trough ignited numerous showers and thunderstorms that resulted in scattered instances of damaging wind gusts and sporadic large hail. A surface trough ignited numerous showers and thunderstorms that resulted in scattered instances of damaging wind gusts and sporadic large hail. A surface trough ignited numerous showers and thunderstorms that resulted in scattered instances of damaging wind gusts and sporadic large hail. A surface trough ignited numerous showers and thunderstorms that resulted in scattered instances of damaging wind gusts and sporadic large hail. A surface trough ignited numerous showers and thunderstorms that resulted in scattered instances of damaging wind gusts and sporadic large hail. A surface trough ignited numerous showers and thunderstorms that resulted in scattered instances of damaging wind gusts and sporadic large hail. A surface trough ignited numerous showers and thunderstorms that resulted in scattered instances of damaging wind gusts and sporadic large hail. A surface trough ignited numerous showers and thunderstorms that resulted in scattered instances of damaging wind gusts and sporadic large hail. A surface trough ignited numerous showers and thunderstorms that resulted in scattered instances of damaging wind gusts and sporadic large hail. A surface trough ignited numerous showers and thunderstorms that resulted in scattered instances of damaging wind gusts and sporadic large hail. A surface trough ignited numerous showers and thunderstorms that resulted in scattered instances of damaging wind gusts and sporadic large hail.\nEvent Narrative: Multiple trees blew down along MD-2 Solomons Island Road. Several dozen trees blew down across the eastern part of the City of Baltimore. Trees blew down near the Royal Farms on Snowden River Parkway in Columbia. A large tree, tree limbs, and wires blew down in the 22800 block of Howard Chapel Road. Trees blew down in Jessup, including one that blocked all lanes of southbound MD-295. Tree damage was reported near Gamber, Sykesville, and Eldersburg. A tree blew down blocking the road in the 4500 block of Cherry Tree Lane. A tree blew down in the 500 block of Klees Mill Road. A tree blew down near the intersection of Gibbons Road and Bartholow Road. Several trees blew down across the western part of the City of Baltimore. A contracter was killed when they were struck by lightning while doing work in the 8800 block of Walther Boulevard. Trees blew down on westbound US-40 Baltimore National Pike near US-29 Columbia Pike. Trees blew down southeast of Eldersburg, including one onto a car in the 6400 block of Cornwall Drive. A tree was reported down blocking the roadway near the intersection of Deer Park Road and Louisville Road. Trees blew down on MD-145 Sweet Air Road near Greene Road. Multiple trees blew down in the Jarrettsville area. Trees blew down along MD-648 Baltimore Annapolis Boulevard near Asquithoaks Lane.", "The following events were reported: Flash Flood, Flood. These occurred near station USW00093721, approximately 13.6069 km away, between 2022-08-04 17:25:00 and 2022-08-05 03:00:00. The flood was caused by Heavy Rain. Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Numerous showers and thunderstorms developed during the afternoon and evening of the 4th. Slow storm movement led to some instances of flooding and flash flooding. Numerous showers and thunderstorms developed during the afternoon and evening of the 4th. Slow storm movement led to some instances of flooding and flash flooding. Numerous showers and thunderstorms developed during the afternoon and evening of the 4th. Slow storm movement led to some instances of flooding and flash flooding. Numerous showers and thunderstorms developed during the afternoon and evening of the 4th. Slow storm movement led to some instances of flooding and flash flooding. Numerous showers and thunderstorms developed during the afternoon and evening of the 4th. Slow storm movement led to some instances of flooding and flash flooding.\nEvent Narrative: Twelve inches of flowing water was over the roadway at the intersection of E Ostend Street and Light Street. A car was stranded in high water along the intersection of Monroe Street and Washington Boulevard. There were multiple reports of flooded roadways in the southeastern portion of Baltimore City. There were numerous streets flooded in the city of Baltimore. The worst was in the eastern portion of the city. The 911 Center reported numerous roads still closed due to flooding.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 44.4297 km away, between 2022-08-04 17:55:00 and 2022-08-04 18:00:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Clusters of thunderstorms moved into Delmarva from the west causing scattered wind damage across the eastern shore. Clusters of thunderstorms moved into Delmarva from the west causing scattered wind damage across the eastern shore. Clusters of thunderstorms moved into Delmarva from the west causing scattered wind damage across the eastern shore.\nEvent Narrative: MD 298 north/south at St. James Newtown Road closed due to trees/debris on road. Time estimated from radar. Trees down on Earl Nicholson Road, with partial road closure. Time estimated from radar. Rock hall Road east/west at Heaven Court closed due to trees/debris on roadway. Time estimated from radar.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 10.942 km away, between 2022-08-05 16:45:00 and 2022-08-05 17:30:00. The events included records with estimated wind gusts of 51.5 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 30000.0 and crop damage of 0.0. \n\nEpisode Narrative: A few thunderstorms produced locally damaging winds ahead of a pressure trough. A few thunderstorms produced locally damaging winds ahead of a pressure trough. A few thunderstorms produced locally damaging winds ahead of a pressure trough. A few thunderstorms produced locally damaging winds ahead of a pressure trough.\nEvent Narrative: Several trees blew down near Jessup. Trees blew down on northbound MD-295 Baltimore-Washington Parkway at MD-175 Annapolis Road. Trees blew down on northbound MD-295 Baltimore-Washington Parkway near MD-100 Paul T. Pitcher Memorial Highway. Trees blew down on northbound MD-295 Baltimore-Washington Parkway near Ridge Road. Trees blew down near the intersection of MD-2 Governor Ritchie Highway and Shelly Road. Several trees blew down between Owings Mills and Reisterstown. A tree blew down onto a house in the 400 block of Main Street in Reisterstown. Trees blew down on MD-140 Reisterstown Road near Pleasant Ridge Drive, including one onto a moving vehicle. Trees blew down near the intersection of MD-129 Park Heights Avenue and Old Court Road.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 31.1672 km away, between 2022-08-05 17:15:00 and 2022-08-05 19:37:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Thunderstorms ahead of a cold front produced numerous instances of gale to storm force winds over area waterways. Thunderstorms ahead of a cold front produced numerous instances of gale to storm force winds over area waterways. Thunderstorms ahead of a cold front produced numerous instances of gale to storm force winds over area waterways. Thunderstorms ahead of a cold front produced numerous instances of gale to storm force winds over area waterways. Thunderstorms ahead of a cold front produced numerous instances of gale to storm force winds over area waterways. Thunderstorms ahead of a cold front produced numerous instances of gale to storm force winds over area waterways. Thunderstorms ahead of a cold front produced numerous instances of gale to storm force winds over area waterways. Thunderstorms ahead of a cold front produced numerous instances of gale to storm force winds over area waterways. Thunderstorms ahead of a cold front produced numerous instances of gale to storm force winds over area waterways. Thunderstorms ahead of a cold front produced numerous instances of gale to storm force winds over area waterways. Thunderstorms ahead of a cold front produced numerous instances of gale to storm force winds over area waterways. Thunderstorms ahead of a cold front produced numerous instances of gale to storm force winds over area waterways. Thunderstorms ahead of a cold front produced numerous instances of gale to storm force winds over area waterways. Thunderstorms ahead of a cold front produced numerous instances of gale to storm force winds over area waterways.\nEvent Narrative: A wind gust of 40 knots (46 MPH) was measured by a mesonet at the Maryland Science Center (BLMRE) adjacent to the tidal Patapsco River. A squall produced an estimated wind gust to 34 knots (39 MPH) near a mesonet at Lakeland Elementary and Middle School (BLTLK) adjacent to the tidal Patapsco River. Wind gusts of up to 38 knots (43 MPH) were measured by the Saunders Point Light WeatherFlow sensor. Wind gusts of up to 51 knots (59 MPH) were measured by the Thomas Point NOS sensor (TPLM2). Wind gusts of up to 35 knots (40 MPH) were measured by the Kent Island WeatherFlow sensor (XKNT). Wind gusts of up to 42 knots (48 MPH) were measured by the Tolly Point WeatherFlow sensor (XTOL). A squall produced estimated wind gusts to 34 knots (39 MPH) near a mesonet on Thomas Point Road adjacent to the Chesapeake Bay. Wind gusts of up to 35 knots (40 MPH) were measured by the Greenbury Point WeatherFlow sensor (XGBY). A squall produced estimated wind gusts to 34 knots (39 MPH) near the Annapolis CBIBS sensor (44063). Wind gusts of up to 47 knots (54 MPH) were measured by a mesonet on the westbound span of the US-50/US-301 Chesapeake Bay Bridge (MD065). Winds of up to 44 knots (51 MPH) were measured by a mesonet on the eastbound span of the US-50/US-301 Chesapeake Bay Bridge (MD066). Wind gusts of up to 40 knots (46 MPH) was measured by the Sandy Point WeatherFlow sensor (XSPT). A squall produced an estimated wind gust to 34 knots (39 MPH) near a mesonet at Crab Alley Bay adjacent to Eastern Bay. A wind gust of 37 knots (43 MPH) was measured by a mesonet at Saint Mary's Elementary School in Annapolis (ANNAS) adjacent to the Chesapeake Bay.", "The following events were reported: Flash Flood, Flood. These occurred near station USW00093721, approximately 15.6409 km away, between 2022-08-05 18:00:00 and 2022-08-05 20:00:00. The flood was caused by Heavy Rain. Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Isolated instances of flooding and flash flooding occurred due to slow moving thunderstorms around Baltimore. Isolated instances of flooding and flash flooding occurred due to slow moving thunderstorms around Baltimore.\nEvent Narrative: Street flooding was reported along Boston Street near Fleet Street. Flooding was reported along the Intersection of Orleans Street and North Lakewood Avenue.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 31.4817 km away, between 2022-08-08 13:42:00 and 2022-08-08 16:39:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A couple thunderstorms produced gusty winds over the middle Chesapeake Bay. A couple thunderstorms produced gusty winds over the middle Chesapeake Bay. A couple thunderstorms produced gusty winds over the middle Chesapeake Bay. A couple thunderstorms produced gusty winds over the middle Chesapeake Bay. A couple thunderstorms produced gusty winds over the middle Chesapeake Bay. A couple thunderstorms produced gusty winds over the middle Chesapeake Bay. A couple thunderstorms produced gusty winds over the middle Chesapeake Bay.\nEvent Narrative: Wind gusts of up to 36 knots (41 MPH) were measured by the ASOS at the U.S. Naval Academy in Annapolis (KNAK) adjacent to the Chesapeake Bay. Wind gusts of up to 37 knots (43 MPH) were measured by the Annapolis NOS sensor (APAM2). A wind gust of 37 knots (43 MPH) was measured by the Greenbury Point WeatherFlow sensor (XGBY). A wind gust of 41 knots (47 MPH) was measured by a mesonet on the eastbound span of the US-50/US-301 Chesapeake Bay Bridge (MD066). A squall produced an estimated wind gust to 34 knots (39 MPH) near the ASOS at the U.S. Naval Academy in Annapolis (KNAK) adjacent to the Chesapeake Bay. Wind gusts of up to 38 knots (44 MPH) were measured by the Tolly Point WeatherFlow sensor (XTOL). A wind gust of 37 knots (43 MPH) was measured by the Kent Island WeatherFlow sensor (XKNT).", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 31.651 km away, between 2022-08-09 15:49:00 and 2022-08-09 21:00:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A few strong thunderstorms produced gale force winds over the upper Chesapeake Bay area. A few strong thunderstorms produced gale force winds over the upper Chesapeake Bay area. A few strong thunderstorms produced gale force winds over the upper Chesapeake Bay area. A few strong thunderstorms produced gale force winds over the upper Chesapeake Bay area. A few strong thunderstorms produced gale force winds over the upper Chesapeake Bay area. A few strong thunderstorms produced gale force winds over the upper Chesapeake Bay area. A few strong thunderstorms produced gale force winds over the upper Chesapeake Bay area. A few strong thunderstorms produced gale force winds over the upper Chesapeake Bay area. A few strong thunderstorms produced gale force winds over the upper Chesapeake Bay area.\nEvent Narrative: Wind gusts of up to 35 knots (40 MPH) were measured by the Tolly Point WeatherFlow sensor (XTOL). A squall produced an estimated wind gust to 34 knots (39 MPH) near the Thomas Point NOS sensor (TPLM2). A squall produced estimated winds to 34 knots (39 MPH) near a mesonet on the eastbound span of the US-50/US-301 Chesapeake Bay Bridge (MD066). A squall produced an estimated wind gust to 34 knots (39 MPH) near a mesonet on the I-695 Francis Scott Key Bridge (MD120). A wind gust of 34 knots (39 MPH) was measured by the AWOS at Martin State Airport (KMTN) adjacent to the Chesapeake Bay. Wind gusts of up to 34 knots (39 MPH) were measured by the Hart Miller WeatherFlow sensor (XHRT). A squall produced estimated wind gusts of up to 34 knots (39 MPH) near the Seneca Creek WeatherFlow sensor. Wind gusts of up to 36 knots (41 MPH) were measured by the Tolchester Beach NOS sensor (TCBM2). A squall produced estimated wind gusts to 34 knots (39 MPH) near a mesonet on North Bayview Avenue adjacent to the Chesapeake Bay.", "The following events were reported: Flash Flood, Flood. These occurred near station USW00093721, approximately 19.0739 km away, between 2022-08-10 16:35:00 and 2022-08-10 19:30:00. The flood was caused by Heavy Rain. Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A weak boundary remained overhead while anomalous amounts of moisture remained in place along with moderate instability. Thunderstorms caused heavy rainfall, and with a slow storm motion this led to instances of flooding and flash flooding. A weak boundary remained overhead while anomalous amounts of moisture remained in place along with moderate instability. Thunderstorms caused heavy rainfall, and with a slow storm motion this led to instances of flooding and flash flooding. A weak boundary remained overhead while anomalous amounts of moisture remained in place along with moderate instability. Thunderstorms caused heavy rainfall, and with a slow storm motion this led to instances of flooding and flash flooding. A weak boundary remained overhead while anomalous amounts of moisture remained in place along with moderate instability. Thunderstorms caused heavy rainfall, and with a slow storm motion this led to instances of flooding and flash flooding.\nEvent Narrative: The Baltimore-Washington Parkway northbound was closed due to high water flowing across the road. Multiple water rescues were reported in Glen Dale. Numerous Roads were closed due to high water near Lanham Severn Road along Folly Branch Creek. Numerous roads were closed from Crofton to the Prince George County Line due to high water.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 19.3799 km away, between 2022-08-10 16:38:00 and 2022-08-10 16:55:00. The events included records with estimated wind gusts of 51.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 20000.0 and crop damage of 0.0. \n\nEpisode Narrative: An approaching cold front caused numerous thunderstorms, several of which became strong to marginally severe producing sporadic wind damage. An approaching cold front caused numerous thunderstorms, several of which became strong to marginally severe producing sporadic wind damage. An approaching cold front caused numerous thunderstorms, several of which became strong to marginally severe producing sporadic wind damage. An approaching cold front caused numerous thunderstorms, several of which became strong to marginally severe producing sporadic wind damage.\nEvent Narrative: Trees blew down near the intersection of MD-424 Davidsonville Road and MD-450 Defense Highway. At least half a dozen trees blew down along MD-450 Defense Highway near Crownsville near the intersection with Huntwood Drive. Trees blew down on MD-214 Central Avenue near Rolling Road. Several trees blew down on the south side of Glen Burnie.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 33.1364 km away, between 2022-08-10 17:00:00 and 2022-08-10 17:23:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: An approaching cold front caused numerous thunderstorms that produced numerous gale force wind gusts over area waterways. An approaching cold front caused numerous thunderstorms that produced numerous gale force wind gusts over area waterways. An approaching cold front caused numerous thunderstorms that produced numerous gale force wind gusts over area waterways. An approaching cold front caused numerous thunderstorms that produced numerous gale force wind gusts over area waterways. An approaching cold front caused numerous thunderstorms that produced numerous gale force wind gusts over area waterways. An approaching cold front caused numerous thunderstorms that produced numerous gale force wind gusts over area waterways. An approaching cold front caused numerous thunderstorms that produced numerous gale force wind gusts over area waterways. An approaching cold front caused numerous thunderstorms that produced numerous gale force wind gusts over area waterways. An approaching cold front caused numerous thunderstorms that produced numerous gale force wind gusts over area waterways.\nEvent Narrative: A wind gust of 34 knots (39 MPH) was measured by the ASOS at the U.S. Naval Academy in Annapolis (KNAK) adjacent to the Chesapeake Bay. Wind gusts of up to 36 knots (41 MPH) were measured by the Saunders Point Light WeatherFlow sensor. Wind gusts of up to 39 knots (45 MPH) were measured by the Greenbury Point WeatherFlow sensor (XGBY). Wind gusts of up to 41 knots (47 MPH) were measured by a mesonet on the eastbound span of the US-50/US-301 Chesapeake Bay Bridge (MD066). Wind gusts of up to 37 knots (43 MPH) were measured by a mesonet on Thomas Point Road adjacent to the Chesapeake Bay. A squall produced an estimated wind gust to 34 knots (39 MPH) near the Annapolis CBIBS sensor (44063). Wind gusts of up to 38 knots (44 MPH) were measured by a mesonet on the westbound span of the US-50/US-301 Chesapeake Bay Bridge (MD065). Wind gusts of up to 38 knots (44 MPH) were measured by the Tolly Point WeatherFlow sensor (XTOL). A wind gust of 36 knots (41 MPH) was measured by the Thomas Point NOS sensor (TPLM2).", "The following events were reported: Marine Hail. These occurred near station USW00093721, approximately 8.1148 km away, between 2022-08-17 16:07:00 and 2022-08-17 16:07:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A couple of thunderstorms produced gusty winds and hail over and near area waterways, particularly Baltimore Inner Harbor and the tidal Patapsco River during the afternoon.\nEvent Narrative: Penny size hail was reported in the unit block of Fourteenth Avenue adjacent to the tidal Patapsco River.", "The following events were reported: Flash Flood, Flood. These occurred near station USW00093721, approximately 42.6401 km away, between 2022-08-21 22:04:00 and 2022-08-22 19:27:00. The flood was caused by Heavy Rain. Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Showers and thunderstorms developed near a boundary during the afternoon and evening of the 21st as well as the 22nd. Anomalous moisture was present, and the storm motion was slow which led to areas of flooding and flash flooding. Showers and thunderstorms developed near a boundary during the afternoon and evening of the 21st as well as the 22nd. Anomalous moisture was present, and the storm motion was slow which led to areas of flooding and flash flooding. Showers and thunderstorms developed near a boundary during the afternoon and evening of the 21st as well as the 22nd. Anomalous moisture was present, and the storm motion was slow which led to areas of flooding and flash flooding. Showers and thunderstorms developed near a boundary during the afternoon and evening of the 21st as well as the 22nd. Anomalous moisture was present, and the storm motion was slow which led to areas of flooding and flash flooding. Showers and thunderstorms developed near a boundary during the afternoon and evening of the 21st as well as the 22nd. Anomalous moisture was present, and the storm motion was slow which led to areas of flooding and flash flooding. Showers and thunderstorms developed near a boundary during the afternoon and evening of the 21st as well as the 22nd. Anomalous moisture was present, and the storm motion was slow which led to areas of flooding and flash flooding. Showers and thunderstorms developed near a boundary during the afternoon and evening of the 21st as well as the 22nd. Anomalous moisture was present, and the storm motion was slow which led to areas of flooding and flash flooding. Showers and thunderstorms developed near a boundary during the afternoon and evening of the 21st as well as the 22nd. Anomalous moisture was present, and the storm motion was slow which led to areas of flooding and flash flooding. Showers and thunderstorms developed near a boundary during the afternoon and evening of the 21st as well as the 22nd. Anomalous moisture was present, and the storm motion was slow which led to areas of flooding and flash flooding. Showers and thunderstorms developed near a boundary during the afternoon and evening of the 21st as well as the 22nd. Anomalous moisture was present, and the storm motion was slow which led to areas of flooding and flash flooding. Showers and thunderstorms developed near a boundary during the afternoon and evening of the 21st as well as the 22nd. Anomalous moisture was present, and the storm motion was slow which led to areas of flooding and flash flooding.\nEvent Narrative: The 500 Block of Old Joppa Road was close due to flooding. Joppa Farm Road was closed due to flooding near Doncaster Road. About three feet of standing water was located around the 2300 Block of Belair Road. US-1 near Reckord Road was closed due to water flowing over the road. Route 7 was closed due to water flowing over the road. There was a water rescue for a vehicle stuck in flowing water near the 1500 Block of Charlestown Drive. I-95 Northbound lane was closed at Exit 75 MD-152 Mountain Road due to high water. A vehicle was stuck in high water near the 900 Block of Joppa Road. Portions of the eastbound and westbound lanes of MD-7 were closed between MD-24 and and Fashion Way due to high water. High standing water was on the road where Route 165 and Furnace Road meet. Harford Road near the Baltimore County line was closed due to flooding.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 24.7887 km away, between 2022-08-30 15:33:00 and 2022-08-30 16:50:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A low-topped line of showers and thunderstorms produced gusty winds over area waterways. A low-topped line of showers and thunderstorms produced gusty winds over area waterways. A low-topped line of showers and thunderstorms produced gusty winds over area waterways. A low-topped line of showers and thunderstorms produced gusty winds over area waterways. A low-topped line of showers and thunderstorms produced gusty winds over area waterways. A low-topped line of showers and thunderstorms produced gusty winds over area waterways. A low-topped line of showers and thunderstorms produced gusty winds over area waterways.\nEvent Narrative: A wind gust of 34 knots (39 MPH) was measured by a mesonet at Hampstead Hill Academy (BLMHH) adjacent to the tidal Patapsco River. A wind gust of 36 knots (41 MPH) was measured by a mesonet at the Maryland Science Center (BLMRE) adjacent to the tidal Patapsco River. Wind gusts of up to 35 knots (40 MPH) were measured by one of the I-695 Francis Scott Key Bridge NOS sensors (FSKM2). Wind gusts of up to 43 knots (50 MPH) were measured by a mesonet on the I-695 Francis Scott Key Bridge (MD120). Wind gusts of up to 34 knots (39 MPH) were measured by the Tolchester Beach NOS sensor (TCBM2). A wind gust of 35 knots (40 MPH) was measured by a mesonet on the westbound span of the US-50/US-301 Chesapeake Bay Bridge (MD065). A squall produced an estimated wind gust to 34 knots (39 MPH) near a mesonet on the US-50/US-301 Kent Narrows Bridge (MD040) between the tidal Chester River and Eastern Bay.", "The following events were reported: Flash Flood, Flood. These occurred near station USW00093721, approximately 30.6381 km away, between 2022-09-12 15:16:00 and 2022-09-12 19:18:00. The flood was caused by Heavy Rain. Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A slow moving cold front caused showers and thunderstorms that led to instances of flooding and flash flooding. A slow moving cold front caused showers and thunderstorms that led to instances of flooding and flash flooding. A slow moving cold front caused showers and thunderstorms that led to instances of flooding and flash flooding. A slow moving cold front caused showers and thunderstorms that led to instances of flooding and flash flooding.\nEvent Narrative: The road was closed at Gwynnbrook Avenue at Gwynn Falls with up to three feet of standing water in the road. The road was closed due to high water along the 12000 Block of Dulaney Valley Road. The roadway was impassable due to high water near the intersection of Cherry Hill Road and Reisterstown Road. The road was closed near the intersection of Ruxton Road and Circle Road due to high water.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 33.5438 km away, between 2022-10-17 16:50:00 and 2022-10-17 16:50:00. The events included records with estimated wind gusts of 34.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A squall produced localized gale force wind gusts near the US-50/US-301 Chesapeake Bay Bridge.\nEvent Narrative: A squall produced an estimated wind gust to 34 knots (39 MPH) near a mesonet on the westbound span on the US-50/US-301 Chesapeake Bay Bridge (MD065).", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 26.3134 km away, between 2022-11-30 15:48:00 and 2022-11-30 16:24:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front produced a line of squalls that resulted in a sudden onset of gale force winds over the upper Chesapeake Bay. A cold front produced a line of squalls that resulted in a sudden onset of gale force winds over the upper Chesapeake Bay. A cold front produced a line of squalls that resulted in a sudden onset of gale force winds over the upper Chesapeake Bay. A cold front produced a line of squalls that resulted in a sudden onset of gale force winds over the upper Chesapeake Bay.\nEvent Narrative: A squall produced an estimated wind gust to 34 knots (39 MPH) near the I-695 Francis Scott Key Bridge NOS sensor (FSKM2). A squall produced an estimated wind gust to 34 knots (39 MPH) near the ASOS at the U.S. Naval Academy in Annapolis (KNAK) adjacent to the Chesapeake Bay. A wind gust of 35 knots (40 MPH) was measured by the Greenbury Point WeatherFlow sensor (XGBY). A squall produced an estimated wind gust to 34 knots (39 MPH) near the Tolly Point WeatherFlow sensor (XTOL).", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 35.2599 km away, between 2023-01-13 06:36:00 and 2023-01-13 06:54:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front produced a squall that resulted in several gale-force wind gusts. A cold front produced a squall that resulted in several gale-force wind gusts. A cold front produced a squall that resulted in several gale-force wind gusts. A cold front produced a squall that resulted in several gale-force wind gusts.\nEvent Narrative: A wind gust of 41 knots (47 MPH) was measured by the Annapolis CBIBS sensor (44063). Wind gusts of up to 42 knots (48 MPH) were measured by a mesonet on Thomas Point Road adjacent to the Chesapeake Bay. A squall produced an estimated wind gust to 34 knots (39 MPH) near the Thomas Point NOS sensor (TPLM2). A squall produced an estimated wind gust to 34 knots (39 MPH) near the Tolchester Beach NOS sensor (TCBM2).", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 35.6533 km away, between 2023-02-03 06:41:00 and 2023-02-03 07:42:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front caused a squall that resulted in several gale-force wind gusts. A cold front caused a squall that resulted in several gale-force wind gusts. A cold front caused a squall that resulted in several gale-force wind gusts.\nEvent Narrative: A wind gust of 40 knots (46 MPH) was measured by the Seneca Creek WeatherFlow sensor. A squall produced an estimated wind gust to 34 knots (39 MPH) near the Tolchester Beach NOS sensor (TCBM2). A wind gust of 35 knots (40 MPH) was measured by the Saunders Point Light WeatherFlow sensor.", "The following events were reported: Hail. These occurred near station USW00093721, approximately 39.9941 km away, between 2023-04-01 17:20:00 and 2023-04-01 17:20:00. The events included records with hailstones measuring 1.0 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A line of thunderstorms developed along a strong cold front near and east of I-95 from northeastern to southern Maryland. An embedded supercell spawned an EF-1 tornado over Cecil County, and there were numerous instances of wind damage as a result of straight-line winds of up to around 70 MPH.\nEvent Narrative: Quarter size hail was reported in Jacksonville.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 38.0509 km away, between 2023-04-01 18:15:00 and 2023-04-01 18:15:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A strong cold front approached the region, with a line of strong showers and thunderstorms developing out ahead of the front. Storms produced damaging winds and small to medium sized hail in Maryland. A strong cold front approached the region, with a line of strong showers and thunderstorms developing out ahead of the front. Storms produced damaging winds and small to medium sized hail in Maryland.\nEvent Narrative: Huntingfield Point measured a wind gust to 60 MPH. Report of a tree blown down into a house. Time estimated from radar.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 37.3739 km away, between 2023-04-01 18:25:00 and 2023-04-01 18:25:00. The events included records with measured wind gusts of 34.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A strong cold front resulted in several clusters of thunderstorms that produced strong winds and hail over area waterways.\nEvent Narrative: A wind gust of 34 knots (39 MPH) was measured by the AWOS at Bay Bridge Airport in Stevensville (KW29) adjacent to the Chesapeake Bay.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 36.9916 km away, between 2023-04-06 17:44:00 and 2023-04-06 17:44:00. The events included records with measured wind gusts of 37.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front spawned several thunderstorms that resulted in up to near hurricane force wind gusts over area waterways.\nEvent Narrative: A wind gust of 37 knots (43 MPH) was measured by the Thomas Point NOS sensor (TPLM2).", "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00093721, approximately 29.7806 km away, between 2023-04-15 12:36:00 and 2023-04-15 15:05:00. The events included records with hailstones measuring 25.625 inches.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 1000.0 and crop damage of 0.0. \n\nEpisode Narrative: A few thunderstorms under an upper-level low produced localized marginally severe hail. A few thunderstorms under an upper-level low produced localized marginally severe hail.\nEvent Narrative: Hail up to half dollar size was reported in Reisterstown. Tree damage was reported near Riva, including a tree that blew down near the intersection of Governor Bridge Road and Blackberry Lane.", "The following events were reported: Thunderstorm Wind, Tornado. These occurred near station USW00093721, approximately 28.0597 km away, between 2023-04-22 13:36:00 and 2023-04-22 14:35:00.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 1077000.0 and crop damage of 0.0. \n\nEpisode Narrative: A strong cold front produced a line of thunderstorms that resulted in widely scattered damaging straight-line wind gusts and a couple tornadoes. A strong cold front produced a line of thunderstorms that resulted in widely scattered damaging straight-line wind gusts and a couple tornadoes. A strong cold front produced a line of thunderstorms that resulted in widely scattered damaging straight-line wind gusts and a couple tornadoes. A strong cold front produced a line of thunderstorms that resulted in widely scattered damaging straight-line wind gusts and a couple tornadoes. A strong cold front produced a line of thunderstorms that resulted in widely scattered damaging straight-line wind gusts and a couple tornadoes. A strong cold front produced a line of thunderstorms that resulted in widely scattered damaging straight-line wind gusts and a couple tornadoes. A strong cold front produced a line of thunderstorms that resulted in widely scattered damaging straight-line wind gusts and a couple tornadoes. A strong cold front produced a line of thunderstorms that resulted in widely scattered damaging straight-line wind gusts and a couple tornadoes. A strong cold front produced a line of thunderstorms that resulted in widely scattered damaging straight-line wind gusts and a couple tornadoes. A strong cold front produced a line of thunderstorms that resulted in widely scattered damaging straight-line wind gusts and a couple tornadoes. A strong cold front produced a line of thunderstorms that resulted in widely scattered damaging straight-line wind gusts and a couple tornadoes. A strong cold front produced a line of thunderstorms that resulted in widely scattered damaging straight-line wind gusts and a couple tornadoes. A strong cold front produced a line of thunderstorms that resulted in widely scattered damaging straight-line wind gusts and a couple tornadoes. A strong cold front produced a line of thunderstorms that resulted in widely scattered damaging straight-line wind gusts and a couple tornadoes. A strong cold front produced a line of thunderstorms that resulted in widely scattered damaging straight-line wind gusts and a couple tornadoes.\nEvent Narrative: A line of severe thunderstorms produced an EF0 tornado along its leading edge as it passed over Fork, Fallston and western Bel Air Maryland on the mid-afternoon of Saturday April 22nd. The tornado was on the ground intermittently for eight minutes, but it produced a fair amount of tree damage along its nearly 7 mile path. Wind gusts where it caused noted damage were estimated 70 to 75 miles per hour along its path.||The tornado touched down in Fork Maryland in northeastern Baltimore County, about a mile from the border with Harford County. There it downed a tree which knocked down power poles and lines near the intersection of Sunshine Avenue and Harford Road. A line of severe thunderstorms produced an EF0 tornado along its leading edge as it passed over Fork, Fallston and western Bel Air Maryland on the mid-afternoon of Saturday April 22nd. The tornado was on the ground intermittently for eight minutes, but it produced a fair amount of tree damage along its nearly 7 mile path. Wind gusts where it caused noted damage were estimated 70 to 75 miles per hour along its path.||It strengthened slightly as it crossed the border into Harford County. There was numerous large branches snapped and downed power lines along Reckord Road as the tornado traveled along it. There were also 4 large trees snapped in the 400 block of Reckord Road.||The tornado continued northeast and produced similar damage to many trees with large branches snapped mainly off the upper parts of trees, with a few falling on homes and vehicles. Affected properties included those along Old Fallston Road, Watervale Road, Waters Avenue, Red Pump Road, Fox Den Road, and Vale Road. About 10 trees and large branches were down in a wooded park near the intersection of Red Pump Road and Vale Road in multiple directions. Two eyewitnesses reported seeing the rotating funnel as it passed. Another reported debris swiftly rotating up off the ground and tops of trees being spun in circles.||The final significant large branch damage noted was about a quarter mile southwest of the intersection of state route 24 and Red Pump Road, along Marywood Drive. A tree blew down onto power lines near the intersection of East Wheel Road and Cedar Lane. Tree damage was reported near Columbia, including a tree that blew down in the 9400 block of North Penfield Road. Several trees blew down in Crofton, including a large tree that blew down near Reidel Road. A tree blew down onto power lines in the 2700 block of Old Kays Mill Road. Trees blew down in the 200 block of West Baltimore Street. Tree damage was reported southeast of Hampstead, including a tree that blew down along Mount Zion Road. Large tree branches snapped along East Baltimore Street near Commerce Street/Holliday Street. A tree blew down onto a house in the 700 block of Seminary Drive. Trees blew down on South Washington Street. Trees blew down near the intersection of US-1 Belair Road and Clifton Park Terrace. Trees blew down in the 4200 block of Furley Avenue. Tree damage was reported near Hampton, including a tree that blew down on MD-131 East Seminary Avenue. Several shingles blew off a roof, a trampoline was tosseed into a fence, and trees and a power pole were blown down.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 28.7138 km away, between 2023-04-22 14:05:00 and 2023-04-22 14:42:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front produced strong to severe thunderstorms resulting in gusty winds over area waterways. A cold front produced strong to severe thunderstorms resulting in gusty winds over area waterways. A cold front produced strong to severe thunderstorms resulting in gusty winds over area waterways. A cold front produced strong to severe thunderstorms resulting in gusty winds over area waterways. A cold front produced strong to severe thunderstorms resulting in gusty winds over area waterways. A cold front produced strong to severe thunderstorms resulting in gusty winds over area waterways. A cold front produced strong to severe thunderstorms resulting in gusty winds over area waterways. A cold front produced strong to severe thunderstorms resulting in gusty winds over area waterways.\nEvent Narrative: A wind gust of 37 knots (43 MPH) was measured by a mesonet at Hampstead Hill Academy (BLMHH) adjacent to the tidal Patapsco River. A wind gust of 37 knots (43 MPH) was measured by a mesonet at Maryland Science Center (BLMRE) adjacent to the tidal Patapsco River. A thunderstorm produced an estimated wind gust to 34 knots (39 MPH) near the Saunders Point Light WeatherFlow sensor (XMTR). A thunderstorm produced an estimated wind gust to 34 knots (39 MPH) near the Thomas Point NOS sensor (TPLM2). A thunderstorm produced an estimated wind gust to 34 knots (39 MPH) near a mesonet on Breezy Point Court adjacent to the Chesapeake Bay. A thunderstorm produced an estimated wind gust to 34 knots (39 MPH) near the Hart Miller WeatherFlow sensor (XHRT). Wind gusts of up to 38 knots (44 MPH) were measured by the Seneca Creek WeatherFlow sensor (XSNC). A thunderstorm produced an estimated wind gust to 34 knots (39 MPH) near the Tolchester Beach NOS sensor (TCBM2).", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 35.259 km away, between 2023-05-03 17:39:00 and 2023-05-03 18:25:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Showers around an upper-level low produced several gale-force wind gusts. Showers around an upper-level low produced several gale-force wind gusts. Showers around an upper-level low produced several gale-force wind gusts. Showers around an upper-level low produced several gale-force wind gusts. Showers around an upper-level low produced several gale-force wind gusts. Showers around an upper-level low produced several gale-force wind gusts. Showers around an upper-level low produced several gale-force wind gusts. Showers around an upper-level low produced several gale-force wind gusts. Showers around an upper-level low produced several gale-force wind gusts. Showers around an upper-level low produced several gale-force wind gusts.\nEvent Narrative: A squall produced an estimated wind gust to 34 knots (39 MPH) near the ASOS at the Annapolis U.S. Naval Academy (KNAK) adjacent to the Chesapeake Bay. A squall produced estimated wind gusts to 34 knots (39 MPH) near the Annapolis NOS sensor (APAM2). Wind gusts of up to 37 knots (43 MPH) were measured by the Greenbury Point WeatherFlow sensor (XGBY). Wind gusts of up to 39 knots (45 MPH) were measured by the Annapolis CBIBS sensor (44063). A wind gust of 37 knots (43 MPH) was measured by the Thomas Point NOS sensor (TPLM2). A squall produced an estimated wind gust to 34 knots (39 MPH) near the Saunders Point Light WeatherFlow sensor (XMTR). A wind gust of 34 knots (39 MPH) was measured by a mesonet at WPL Pier 31 (MD068). A squall produced an estimated wind gust to 34 knots (39 MPH) near a mesonet on Beach Side Drive adjacent to the Chesapeake Bay. A squall produced an estimated wind gust to 34 knots (39 MPH) near a mesonet at Crab Alley Bay adjacent to Eastern Bay. A wind gust of 34 knots (39 MPH) was measured by a mesonet at Huntingfield Point adjacent to the tidal Chester River.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 27.535 km away, between 2023-06-09 15:44:00 and 2023-06-09 15:49:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A few showers and thunderstorms produced gale-force wind gusts sporadically over upper portions of the Chesapeake Bay. A few showers and thunderstorms produced gale-force wind gusts sporadically over upper portions of the Chesapeake Bay.\nEvent Narrative: A squall produced an estimated wind gust to 34 knots (39 MPH) near a mesonet at Annapolis Sailing School (KMDANNAP2625). A wind gust of 35 knots (40 MPH) was measured by a personal weather station at Persimmon Point (KMDANNAP2658).", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 24.9331 km away, between 2023-06-12 17:48:00 and 2023-06-12 18:00:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A line of showers and a few thunderstorms produced sporadic gale-force winds over portions of the Chesapeake Bay and the tidal Potomac River. A line of showers and a few thunderstorms produced sporadic gale-force winds over portions of the Chesapeake Bay and the tidal Potomac River. A line of showers and a few thunderstorms produced sporadic gale-force winds over portions of the Chesapeake Bay and the tidal Potomac River.\nEvent Narrative: A squall produced an estimated wind gust to 34 knots (39 MPH) near one of the NOS sensors near the I-695 Francis Scott Key Bridge (FSNM2). A wind gust of 34 knots (39 MPH) was measured by a mesonet at Annapolis Sailing School (KMDANNAP2625). A thunderstorm produced an estimated wind gust to 34 knots (39 MPH) near the Annapolis CBIBS sensor (44063).", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 28.4539 km away, between 2023-06-16 09:42:00 and 2023-06-16 10:34:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Several thunderstorms produced sporadic gale-force winds. Several thunderstorms produced sporadic gale-force winds. Several thunderstorms produced sporadic gale-force winds. Several thunderstorms produced sporadic gale-force winds. Several thunderstorms produced sporadic gale-force winds. Several thunderstorms produced sporadic gale-force winds. Several thunderstorms produced sporadic gale-force winds. Several thunderstorms produced sporadic gale-force winds.\nEvent Narrative: A thunderstorm produced estimated wind gusts to 34 knots (39 MPH) near the I-695 Francis Scott Key Bridge NOS sensor (FSKM2). A thunderstorm produced an estimated wind gust to 34 knots (39 MPH) near the AWOS at Martin State Airport (KMTN) adjacent to the Chesapeake Bay. A wind gust of 34 knots (39 MPH) was measured by the Seneca Creek WeatherFlow sensor (XSNC). A thunderstorm produced an estimated wind gust to 34 knots (39 MPH) near the Hart Miller WeatherFlow sensor (XHRT). Wind gusts of up to 39 knots (45 MPH) were measured by a personal weather station at Persimmon Point (KMDANNAP2658). A thunderstorm produced estimated wind gusts to 34 knots (39 MPH) near a Tempest station on River Bay Road adjacent to the Chesapeake Bay. Wind gusts of up to 36 knots (41 MPH) were measured by the Tolchester Beach NOS sensor (TCBM2). A wind gust of 34 knots (39 MPH) was measured by a personal weather station at Love Point (KMDSTEVE52).", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 30.5771 km away, between 2023-06-26 17:20:00 and 2023-06-26 20:04:00. The events included records with estimated wind gusts of 53.5 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 51000.0 and crop damage of 0.0. \n\nEpisode Narrative: Several clusters of thunderstorms produced widely scattered wind damage ahead of a slow-moving cold front. Several clusters of thunderstorms produced widely scattered wind damage ahead of a slow-moving cold front. Several clusters of thunderstorms produced widely scattered wind damage ahead of a slow-moving cold front. Several clusters of thunderstorms produced widely scattered wind damage ahead of a slow-moving cold front.\nEvent Narrative: Tree damage was reported near Pikesville, including a tree that blew down onto an apartment building and damaged the roof in the 6000 block of Sanzo Road. Tree damage was reported northwest of Towson, including a tree that blew down onto a car near the intersection of Joppa Road and Bellona Avenue. There were about two dozen reports of trees and wires down near and east-northeast of Towson. Tree damage was reported in Abingdon, including near the intersection of Abingdon Road and Federal Lane.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 13.8716 km away, between 2023-06-26 18:24:00 and 2023-06-26 20:30:00. The events included records with measured wind gusts of 39.5 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Clusters of thunderstorms produced gale-force wind gusts over area waterways ahead of a slow-moving cold front. Clusters of thunderstorms produced gale-force wind gusts over area waterways ahead of a slow-moving cold front.\nEvent Narrative: A wind gust of 34 knots (39 MPH) was measured by the I-695 Francis Scott Key Bridge NOS sensor (FSKM2). A wind gust of 45 knots (52 MPH) was measured by a mesonet at the Maryland Science Center (BLMRE) adjacent to the tidal Patapsco River.", "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00093721, approximately 22.3934 km away, between 2023-06-27 14:09:00 and 2023-06-27 15:12:00. The events included records with hailstones measuring 9.583333333333334 inches.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 3000.0 and crop damage of 0.0. \n\nEpisode Narrative: A couple bands of showers and thunderstorms produced localized wind damage and hail ahead of a weakening cold front. A couple bands of showers and thunderstorms produced localized wind damage and hail ahead of a weakening cold front. A couple bands of showers and thunderstorms produced localized wind damage and hail ahead of a weakening cold front. A couple bands of showers and thunderstorms produced localized wind damage and hail ahead of a weakening cold front. A couple bands of showers and thunderstorms produced localized wind damage and hail ahead of a weakening cold front. A couple bands of showers and thunderstorms produced localized wind damage and hail ahead of a weakening cold front.\nEvent Narrative: Hail of up to ping pong ball size was reported near Odenton. Trees blew down blocking a couple of roadways in Odenton. Quarter size hail was reported in Crofton. Quarter size hail was reported near Fullerton. Quarter size hail was reported in Birdsville. Quarter size hail was reported in Middle River.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 30.9834 km away, between 2023-06-27 14:49:00 and 2023-06-27 15:29:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Multiple bands of thunderstorms produced gale to near storm-force wind gusts over area waterways during the mid to late afternoon and early evening hours. Multiple bands of thunderstorms produced gale to near storm-force wind gusts over area waterways during the mid to late afternoon and early evening hours. Multiple bands of thunderstorms produced gale to near storm-force wind gusts over area waterways during the mid to late afternoon and early evening hours. Multiple bands of thunderstorms produced gale to near storm-force wind gusts over area waterways during the mid to late afternoon and early evening hours. Multiple bands of thunderstorms produced gale to near storm-force wind gusts over area waterways during the mid to late afternoon and early evening hours. Multiple bands of thunderstorms produced gale to near storm-force wind gusts over area waterways during the mid to late afternoon and early evening hours. Multiple bands of thunderstorms produced gale to near storm-force wind gusts over area waterways during the mid to late afternoon and early evening hours. Multiple bands of thunderstorms produced gale to near storm-force wind gusts over area waterways during the mid to late afternoon and early evening hours. Multiple bands of thunderstorms produced gale to near storm-force wind gusts over area waterways during the mid to late afternoon and early evening hours. Multiple bands of thunderstorms produced gale to near storm-force wind gusts over area waterways during the mid to late afternoon and early evening hours. Multiple bands of thunderstorms produced gale to near storm-force wind gusts over area waterways during the mid to late afternoon and early evening hours. Multiple bands of thunderstorms produced gale to near storm-force wind gusts over area waterways during the mid to late afternoon and early evening hours.\nEvent Narrative: A wind gust of 36 knots (41 MPH) was measured by the Seneca Creek WeatherFlow sensor (XSNC). Wind gusts of up to 47 knots (54 MPH) were measured by the Saunders Point Light WeatherFlow sensor (XMTR). A wind gust of 36 knots (41 MPH) was measured by a Tempest station on Thomas Point Road adjacent to the Chesapeake Bay. A wind gust of 45 knots (52 MPH) was measured by the Thomas Point NOS sensor (TPLM2). A thunderstorm produced estimated wind gusts to 34 knots (39 MPH) near a personal weather station at Goose Point (KMDSTEVE82). A wind gust of 36 knots (41 MPH) was measured by a personal weather station at Annapolis Sailing School (KMDANNAP2625). A wind gust of 37 knots (43 MPH) was measured by a personal weather station at Canton - Baltimore Water Taxi (KMDBALTI181). Wind gusts of up to 37 knots (43 MPH) were measured by a mesonet at Hampstead Hill Academy (BLMHH) adjacent to the tidal Patapsco River. A thunderstorm produced an estimated wind gust to 34 knots (39 MPH) near the Annapolis CBIBS sensor (44063). Wind gusts of up to 38 knots (44 MPH) were measured by a mesonet at WPL Pier 31 (MD068). Wind gusts of up to 38 knots (44 MPH) were measured by the Greenbury Point WeatherFlow sensor (XGBY). A thunderstorm produced an estimated wind gust to 34 knots (39 MPH) near the Tolly Point WeatherFlow sensor (XTOL).", "The following events were reported: Flash Flood. These occurred near station USW00093721, approximately 16.6522 km away, between 2023-06-27 15:20:00 and 2023-06-27 17:00:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front triggered showers and thunderstorms. Some thunderstorms trained over the same areas, resulting in isolated instances of flooding and flash flooding around Baltimore.\nEvent Narrative: A vehicle was stalled in standing water along US-40 Pulaski Highway near East Monument Street. Another vehicle was stalled in standing water along MD-173 West Patapsco Avenue near MD-2 Potee Street. North Lakewood Avenue was closed due to flooding in the 700 block and South Hanover Street was also closed due to flooding.", "The following events were reported: Lightning, Thunderstorm Wind. These occurred near station USW00093721, approximately 13.9728 km away, between 2023-06-30 15:33:00 and 2023-06-30 15:45:00.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 38000.0 and crop damage of 0.0. \n\nEpisode Narrative: A line of thunderstorms produced localized wind damage over eastern Howard County. A line of thunderstorms produced localized wind damage over eastern Howard County. A line of thunderstorms produced localized wind damage over eastern Howard County. A line of thunderstorms produced localized wind damage over eastern Howard County. A line of thunderstorms produced localized wind damage over eastern Howard County.\nEvent Narrative: Several trees and branches blew down near Simpsonville, including in the 6000 block of Lochridge Road, and in the 10000 block of Green View Way. Several trees and light poles blew down on Broken Land Parkway between Hickory Ridge Road and US-29 Columbia Pike. A tree and branches blew down near the intersection of Overheart Lane and Pressed Gentian. Trees and wires blew down near the intersection of US-1 Washington Boulevard and Kit Kat Road. Lightning struck a house in the 6300 block of Sandchain Road causing a fire along the roof line.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 23.2219 km away, between 2023-06-30 16:19:00 and 2023-06-30 16:39:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A line of thunderstorms produced localized gale-force wind gusts near Baltimore Harbor and portions of the upper Chesapeake Bay. A line of thunderstorms produced localized gale-force wind gusts near Baltimore Harbor and portions of the upper Chesapeake Bay. A line of thunderstorms produced localized gale-force wind gusts near Baltimore Harbor and portions of the upper Chesapeake Bay.\nEvent Narrative: A thunderstorm produced estimated wind gusts to 34 knots (39 MPH) near a personal weather station at Canton - Baltimore Water Taxi (KMDBALTI181). A wind gust of 35 knots (40 MPH) was measured by a personal weather station at Persimmon Point (KMDANNAP2658). A thunderstorm produced an estimated wind gust to 34 knots (39 MPH) near a mesonet at the intersection of MD-43 White Marsh Boulevard and MD-150 Eastern Boulevard (MD063) adjacent to the Chesapeake Bay.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 20.7 km away, between 2023-07-02 17:32:00 and 2023-07-02 18:28:00. The events included records with estimated wind gusts of 54.6 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 77000.0 and crop damage of 0.0. \n\nEpisode Narrative: A couple of severe thunderstorms initiated off the bay breeze near and to the south of Baltimore. Meanwhile, a couple of isolated thunderstorms produced sporadic wind damage further west in the vicinity of a lee pressure trough. A couple of severe thunderstorms initiated off the bay breeze near and to the south of Baltimore. Meanwhile, a couple of isolated thunderstorms produced sporadic wind damage further west in the vicinity of a lee pressure trough. A couple of severe thunderstorms initiated off the bay breeze near and to the south of Baltimore. Meanwhile, a couple of isolated thunderstorms produced sporadic wind damage further west in the vicinity of a lee pressure trough. A couple of severe thunderstorms initiated off the bay breeze near and to the south of Baltimore. Meanwhile, a couple of isolated thunderstorms produced sporadic wind damage further west in the vicinity of a lee pressure trough. A couple of severe thunderstorms initiated off the bay breeze near and to the south of Baltimore. Meanwhile, a couple of isolated thunderstorms produced sporadic wind damage further west in the vicinity of a lee pressure trough.\nEvent Narrative: Two trees blew down in the Cylburn neighborhood. Wind damage was reported near Parkville, including a large tree that blew down onto power lines snapping a power pole in the 8300 block of MD-542 Loch Raven Boulevard. Wind damage was reported northwest of Parkville, including a large tree that blew down onto power lines snapping a power pole in the 8500 block of Pleasant Plains Road. There were at least five calls for numerous trees blown down throughout Pasadena. Numerous trees blew down between Lake Shore and Arcadia.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 26.0518 km away, between 2023-07-02 17:48:00 and 2023-07-02 19:01:00. The events included records with measured wind gusts of 36.666666666666664 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A couple of thunderstorms initiated off the bay breeze near and to the south of Baltimore. A couple of thunderstorms initiated off the bay breeze near and to the south of Baltimore. A couple of thunderstorms initiated off the bay breeze near and to the south of Baltimore. A couple of thunderstorms initiated off the bay breeze near and to the south of Baltimore. A couple of thunderstorms initiated off the bay breeze near and to the south of Baltimore. A couple of thunderstorms initiated off the bay breeze near and to the south of Baltimore.\nEvent Narrative: A wind gust of 34 knots (39 MPH) was measured by the I-695 Francis Scott Key Bridge NOS sensor (FSKM2). A wind gust of 34 knots (39 MPH) was measured by a mesonet one mile north of Belvedere Heights adjacent to the Chesapeake Bay. A wind gust of 34 knots (39 MPH) was measured by a mesonet one mile north of Cape Saint Claire adjacent to the Chesapeake Bay. A wind gust of 38 knots (44 MPH) was measured by a buoy five miles southeast of Cape Saint Claire. A wind gust of 42 knots (48 MPH) was measured by a mesonet seven miles east-southeast of Gibson Island adjacent to the Chesapeake Bay and tidal Chester River. A wind gust of 38 knots (44 MPH) was measured by a buoy four miles south-southeast of Cape Saint Claire.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 31.8645 km away, between 2023-07-03 18:19:00 and 2023-07-03 18:40:00. The events included records with estimated wind gusts of 52.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 40000.0 and crop damage of 0.0. \n\nEpisode Narrative: A cold front sparked a few lines of thunderstorms. These thunderstorms produced localized wind damage, most notably over northeastern Maryland during the early evening hours. A cold front sparked a few lines of thunderstorms. These thunderstorms produced localized wind damage, most notably over northeastern Maryland during the early evening hours. A cold front sparked a few lines of thunderstorms. These thunderstorms produced localized wind damage, most notably over northeastern Maryland during the early evening hours. A cold front sparked a few lines of thunderstorms. These thunderstorms produced localized wind damage, most notably over northeastern Maryland during the early evening hours. A cold front sparked a few lines of thunderstorms. These thunderstorms produced localized wind damage, most notably over northeastern Maryland during the early evening hours. A cold front sparked a few lines of thunderstorms. These thunderstorms produced localized wind damage, most notably over northeastern Maryland during the early evening hours.\nEvent Narrative: A few trees blew down in Towson. Tree damage was reported southwest of Long Green, including a tree that blew down near the intersection of Morgan Mill Road and Loch Raven Drive. Tree damage was reported northeast of Perry Hall, including a tree that blew down near the intersection of US-1 Belair Road and Miller Road. Tree damage was reported northwest of Kingsville, including a tree that blew down near the intersection of Sunshine Avenue and MD-147 Harford Road. A tree and numerous branches also blew down nearby on Mount Vista Road near Glen Arm Road. Tree damage was reported near Hampton, including a tree that blew down onto a house in the 1900 block of Haverhill Road. Tree damage was reported in Carney, including a tree that blew down and took down a utility pole at the intersection of Glen Arm Road and Cromwell Bridge Road.", "The following events were reported: Flash Flood, Flood. These occurred near station USW00093721, approximately 35.9344 km away, between 2023-07-03 22:28:00 and 2023-07-04 00:33:00. The flood was caused by Heavy Rain. Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Showers and thunderstorms developed ahead of a weak boundary. A few areas received multiple rounds of storms, resulting in isolated instances of flash flooding and flooding. Showers and thunderstorms developed ahead of a weak boundary. A few areas received multiple rounds of storms, resulting in isolated instances of flash flooding and flooding. Showers and thunderstorms developed ahead of a weak boundary. A few areas received multiple rounds of storms, resulting in isolated instances of flash flooding and flooding. Showers and thunderstorms developed ahead of a weak boundary. A few areas received multiple rounds of storms, resulting in isolated instances of flash flooding and flooding. Showers and thunderstorms developed ahead of a weak boundary. A few areas received multiple rounds of storms, resulting in isolated instances of flash flooding and flooding. Showers and thunderstorms developed ahead of a weak boundary. A few areas received multiple rounds of storms, resulting in isolated instances of flash flooding and flooding.\nEvent Narrative: A swift water rescue was needed between Route 40 and Route 7. Three cars were stranded with water flowing across the road 6 to 12 inches deep. I-95 was partially closed northbound due to standing water between mile markers 72 and 75. Edgewood Road was closed at Route 40 due to high water. The water level rose above 6 feet along the HoneyGo Run in White Marsh. At 6 feet, water begins to flow behind a business on Ebenezer Road. The water level along White Marsh Run at White Marsh rose rapidly above the flood stage of 11 feet, cresting at 12.44 feet at 11:20 PM EST. Water covered the parking lots near the stream, particularly near the Town Center Court. Water was likely flowing and about 1 to 2 feet deep. Two cars were stuck in a flooded roadway near the 9100 Block of Snyder Lane.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 44.2672 km away, between 2023-07-06 13:10:00 and 2023-07-06 13:10:00. The events included records with estimated wind gusts of 52.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 5000.0 and crop damage of 0.0. \n\nEpisode Narrative: Unstable air along a pressure trough well ahead of a cold front over the Ohio River Valley sparked scattered thunderstorms during the afternoon and evening hours. Localized wind damage was reported in northern Maryland, and a considerably severe thunderstorm affected parts of the central Shenandoah Valley in Virginia.\nEvent Narrative: Several trees and branches blew down near Watersville, including near the intersection of Flag Marsh Road and Watersville Road, Watersville Road and Gillis Falls Road, and Gillis Ford Road and John Pickett Road.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 32.4959 km away, between 2023-07-07 10:59:00 and 2023-07-07 12:03:00. The events included records with estimated wind gusts of 52.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 7000.0 and crop damage of 0.0. \n\nEpisode Narrative: A pressure trough sparked several thunderstorms during the afternoon and evening hours, a few of which produced localized wind damage east of the Blue Ridge and Catoctin Mountains. A pressure trough sparked several thunderstorms during the afternoon and evening hours, a few of which produced localized wind damage east of the Blue Ridge and Catoctin Mountains.\nEvent Narrative: Tree damage was reported near Scaggsville, including a large tree that blew down in the 10600 block of Delfield Court. A large tree and multiple large tree limbs blew down in the 1900 block of Parkwood Drive.", "The following events were reported: Flood. These occurred near station USW00093721, approximately 25.2537 km away, between 2023-07-07 13:04:00 and 2023-07-07 15:04:00. The flood was caused by Heavy Rain. Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front passed through the area on the 7th, leading to a few showers and thunderstorms. Some thunderstorms caused heavy rainfall in a short period of time that led to an instance of flooding.\nEvent Narrative: Ruxton Road was closed at Circle Road due to high water.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 46.9837 km away, between 2023-07-09 14:16:00 and 2023-07-09 14:17:00. The events included records with estimated wind gusts of 52.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 3000.0 and crop damage of 0.0. \n\nEpisode Narrative: A cluster of thunderstorms produced several instances of wind damage across northern Maryland near and east of Interstate 81. A cluster of thunderstorms produced several instances of wind damage across northern Maryland near and east of Interstate 81.\nEvent Narrative: Tree damage was reported north-northwest of Fallston, including a tree that blew down in the 2100 block of Putnam Road. Wind damage was reported west-southwest of Jarrettsville, including wires that blew down in the 3000 block of Houcks Road.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 30.5829 km away, between 2023-07-21 01:09:00 and 2023-07-21 03:29:00. The events included records with estimated wind gusts of 52.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 7000.0 and crop damage of 0.0. \n\nEpisode Narrative: A line of thunderstorms (Mesoscale Convective Complex, MCS) that developed over the Midwest moved across northern Maryland and eastern West Virginia producing localized wind damage overnight. The event was noteworthy due to its timing. A line of thunderstorms (Mesoscale Convective Complex, MCS) that developed over the Midwest moved across northern Maryland and eastern West Virginia producing localized wind damage overnight. The event was noteworthy due to its timing.\nEvent Narrative: Several trees blew down in the Eldersburg/Sykesville area, including on Emerald Lane, Cherry Tree Road, and Nicodemus Road. Several large tree limbs and wires blew down near Annapolis, including in the 2000 block of South Haven Road.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 33.0055 km away, between 2023-07-21 03:36:00 and 2023-07-21 03:56:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A line of thunderstorms (Mesoscale Convective Complex, MCS) that developed over the Midwest moved across the waters during the early morning hours. The event was noteworthy due to its timing. A line of thunderstorms (Mesoscale Convective Complex, MCS) that developed over the Midwest moved across the waters during the early morning hours. The event was noteworthy due to its timing. A line of thunderstorms (Mesoscale Convective Complex, MCS) that developed over the Midwest moved across the waters during the early morning hours. The event was noteworthy due to its timing. A line of thunderstorms (Mesoscale Convective Complex, MCS) that developed over the Midwest moved across the waters during the early morning hours. The event was noteworthy due to its timing. A line of thunderstorms (Mesoscale Convective Complex, MCS) that developed over the Midwest moved across the waters during the early morning hours. The event was noteworthy due to its timing. A line of thunderstorms (Mesoscale Convective Complex, MCS) that developed over the Midwest moved across the waters during the early morning hours. The event was noteworthy due to its timing. A line of thunderstorms (Mesoscale Convective Complex, MCS) that developed over the Midwest moved across the waters during the early morning hours. The event was noteworthy due to its timing. A line of thunderstorms (Mesoscale Convective Complex, MCS) that developed over the Midwest moved across the waters during the early morning hours. The event was noteworthy due to its timing. A line of thunderstorms (Mesoscale Convective Complex, MCS) that developed over the Midwest moved across the waters during the early morning hours. The event was noteworthy due to its timing.\nEvent Narrative: A squall produced estimated wind gusts to 34 knots (39 MPH) near the Annapolis NOS sensor (APAM2). A squall produced estimated wind gusts of up to 34 knots (39 MPH) near a mesonet at WPL Pier 31 (MD068). Wind gusts of up to 36 knots (41 MPH) were measured by the ASOS at the Annapolis U.S. Naval Academy (KNAK) adjacent to the Chesapeake Bay. Wind gusts of up to 44 knots (51 MPH) were measured by the Tolly Point WeatherFlow sensor (XTOL). A squall produced an estimated wind gust to 34 knots (39 MPH) near the Annapolis CBIBS sensor (44063). A squall produced estimated wind gusts to 34 knots (39 MPH) near the Saunders Point Light WeatherFlow sensor (XMTR). A wind gust of 39 knots (45 MPH) was measured by a mesonet in Galesville (EW0112) adjacent to the Chesapeake Bay. A wind gust of 35 knots (40 MPH) was measured by the Thomas Point NOS sensor (TPLM2). A squall produced estimated wind gusts to 34 knots (39 MPH) near the Greenbury Point WeatherFlow sensor (XGBY).", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 32.4071 km away, between 2023-07-25 11:12:00 and 2023-07-25 13:14:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Remnant outflow from convection the day before over the Midwest combined with a lee pressure trough resulted in scattered to numerous showers and thunderstorms. Several produced localized gale- to storm-force winds over area waterways. Remnant outflow from convection the day before over the Midwest combined with a lee pressure trough resulted in scattered to numerous showers and thunderstorms. Several produced localized gale- to storm-force winds over area waterways. Remnant outflow from convection the day before over the Midwest combined with a lee pressure trough resulted in scattered to numerous showers and thunderstorms. Several produced localized gale- to storm-force winds over area waterways. Remnant outflow from convection the day before over the Midwest combined with a lee pressure trough resulted in scattered to numerous showers and thunderstorms. Several produced localized gale- to storm-force winds over area waterways.\nEvent Narrative: Wind gusts of up to 35 knots (40 MPH) were measured by the I-695 Francis Scott Key Bridge NOS sensor (FSKM2). A thunderstorm produced an estimated wind gust to 34 knots (39 MPH) near a mesonet at WPL Pier 31 (MD068). Wind gusts of up to 36 knots (41 MPH) were measured by the Saunders Point Light WeatherFlow sensor (XMTR). A wind gust of 35 knots (40 MPH) was measured by a mesonet on the US-50 Kent Narrows Bridge (MD040).", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 21.8371 km away, between 2023-07-25 11:30:00 and 2023-07-25 11:30:00. The events included records with estimated wind gusts of 52.0 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 10000.0 and crop damage of 0.0. \n\nEpisode Narrative: Remnant outflow from convection the day before over the Midwest combined with a lee pressure trough resulted in scattered to numerous showers and thunderstorms. Several produced localized wind damage and some hail.\nEvent Narrative: There were several reports of trees, branches and wires blown down in the Edgemere area.", "The following events were reported: Flash Flood. These occurred near station USW00093721, approximately 21.7062 km away, between 2023-07-25 12:30:00 and 2023-07-25 13:15:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A weak cold front passed through, but with plenty of moisture and weaker flow aloft, some slow moving storms produced instances of flooding and flash flooding around Baltimore County. A weak cold front passed through, but with plenty of moisture and weaker flow aloft, some slow moving storms produced instances of flooding and flash flooding around Baltimore County. A weak cold front passed through, but with plenty of moisture and weaker flow aloft, some slow moving storms produced instances of flooding and flash flooding around Baltimore County. A weak cold front passed through, but with plenty of moisture and weaker flow aloft, some slow moving storms produced instances of flooding and flash flooding around Baltimore County.\nEvent Narrative: At least 6 inches of water was flowing across the 2300 block o Ruth Avenue, with cars unable to drive on the roadway. North Point Road was closed to due to water flowing over the road near Wood Avenue. Lodge Forest Road near North Point Road was closed due to flowing water. Ruth avenue was closed near Sparrows Point Road due to flowing water.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 44.1644 km away, between 2023-07-25 13:14:00 and 2023-07-25 13:14:00. The events included records with measured wind gusts of 51.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A strong mid-level shortwave trough moved into a very moist and unstable environment, with scattered strong to severe thunderstorms developing. Thunderstorms produced damaging winds across parts of Maryland.\nEvent Narrative: Wunderground station kmdsteve76 measured a 59.3 MPH gust.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 36.9715 km away, between 2023-07-28 17:40:00 and 2023-07-28 19:24:00. The events included records with estimated wind gusts of 58.94117647058823 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 5544000.0 and crop damage of 0.0. \n\nEpisode Narrative: A subtle remnant disturbance from prior day's convection over the Midwest amplified a pre-existing lee pressure trough, igniting numerous thunderstorms. Given the excessive hot, humid, and unstable environment, these thunderstorms were able to organize into clusters and lines despite a lack of stronger wind shear. A subtle remnant disturbance from prior day's convection over the Midwest amplified a pre-existing lee pressure trough, igniting numerous thunderstorms. Given the excessive hot, humid, and unstable environment, these thunderstorms were able to organize into clusters and lines despite a lack of stronger wind shear. A subtle remnant disturbance from prior day's convection over the Midwest amplified a pre-existing lee pressure trough, igniting numerous thunderstorms. Given the excessive hot, humid, and unstable environment, these thunderstorms were able to organize into clusters and lines despite a lack of stronger wind shear. A subtle remnant disturbance from prior day's convection over the Midwest amplified a pre-existing lee pressure trough, igniting numerous thunderstorms. Given the excessive hot, humid, and unstable environment, these thunderstorms were able to organize into clusters and lines despite a lack of stronger wind shear. A subtle remnant disturbance from prior day's convection over the Midwest amplified a pre-existing lee pressure trough, igniting numerous thunderstorms. Given the excessive hot, humid, and unstable environment, these thunderstorms were able to organize into clusters and lines despite a lack of stronger wind shear. A subtle remnant disturbance from prior day's convection over the Midwest amplified a pre-existing lee pressure trough, igniting numerous thunderstorms. Given the excessive hot, humid, and unstable environment, these thunderstorms were able to organize into clusters and lines despite a lack of stronger wind shear. A subtle remnant disturbance from prior day's convection over the Midwest amplified a pre-existing lee pressure trough, igniting numerous thunderstorms. Given the excessive hot, humid, and unstable environment, these thunderstorms were able to organize into clusters and lines despite a lack of stronger wind shear. A subtle remnant disturbance from prior day's convection over the Midwest amplified a pre-existing lee pressure trough, igniting numerous thunderstorms. Given the excessive hot, humid, and unstable environment, these thunderstorms were able to organize into clusters and lines despite a lack of stronger wind shear. A subtle remnant disturbance from prior day's convection over the Midwest amplified a pre-existing lee pressure trough, igniting numerous thunderstorms. Given the excessive hot, humid, and unstable environment, these thunderstorms were able to organize into clusters and lines despite a lack of stronger wind shear. A subtle remnant disturbance from prior day's convection over the Midwest amplified a pre-existing lee pressure trough, igniting numerous thunderstorms. Given the excessive hot, humid, and unstable environment, these thunderstorms were able to organize into clusters and lines despite a lack of stronger wind shear. A subtle remnant disturbance from prior day's convection over the Midwest amplified a pre-existing lee pressure trough, igniting numerous thunderstorms. Given the excessive hot, humid, and unstable environment, these thunderstorms were able to organize into clusters and lines despite a lack of stronger wind shear. A subtle remnant disturbance from prior day's convection over the Midwest amplified a pre-existing lee pressure trough, igniting numerous thunderstorms. Given the excessive hot, humid, and unstable environment, these thunderstorms were able to organize into clusters and lines despite a lack of stronger wind shear. A subtle remnant disturbance from prior day's convection over the Midwest amplified a pre-existing lee pressure trough, igniting numerous thunderstorms. Given the excessive hot, humid, and unstable environment, these thunderstorms were able to organize into clusters and lines despite a lack of stronger wind shear. A subtle remnant disturbance from prior day's convection over the Midwest amplified a pre-existing lee pressure trough, igniting numerous thunderstorms. Given the excessive hot, humid, and unstable environment, these thunderstorms were able to organize into clusters and lines despite a lack of stronger wind shear. A subtle remnant disturbance from prior day's convection over the Midwest amplified a pre-existing lee pressure trough, igniting numerous thunderstorms. Given the excessive hot, humid, and unstable environment, these thunderstorms were able to organize into clusters and lines despite a lack of stronger wind shear. A subtle remnant disturbance from prior day's convection over the Midwest amplified a pre-existing lee pressure trough, igniting numerous thunderstorms. Given the excessive hot, humid, and unstable environment, these thunderstorms were able to organize into clusters and lines despite a lack of stronger wind shear. A subtle remnant disturbance from prior day's convection over the Midwest amplified a pre-existing lee pressure trough, igniting numerous thunderstorms. Given the excessive hot, humid, and unstable environment, these thunderstorms were able to organize into clusters and lines despite a lack of stronger wind shear.\nEvent Narrative: Trees and branches blew down on MD-295 Baltimore-Washington Parkway near MD-197 Laurel-Bowie Road. Hundreds of trees blew down around Reisterstown, including many onto houses and cars. Several trees and wires blew down in central Howard County, including along Carroll Mill Road near Folly Quarter Road where trees fell onto wires cracking a pole. Hundreds of trees blew down west of Cockeysville. Numerous trees blew down along MD-25 Falls Road near Shawan Road. Trees blew down on southbound I-83 near Exit 18/MD-943 Warren Road. Numerous trees blew down along MD-25 Falls Road near Greenway Road. Trees blew down on I-83 near Exit 24/Belfast Road. Trees blew down along MD-146 Dulaney Valley Road between MD-131 East Seminary Avenue and Valley Court Road. Hundreds of trees blew down around Pikesville, Garrison, Chestnut Ridge, and Brooklandville blocking numerous roads. Many trees fell onto houses and cars. There were several calls for trees, branches, and wires blown down in the City of Baltimore. Dozens of trees and wires blew down around Fallston and Baldwin, including trees onto houses in the 2800 block of Green Road. Numerous trees blew down along MD-27 Ridge Road near and north of West Falls Road. Trees blew down along MD-26 Liberty Road near Woodbine Road. Trees blew down near Marston and New Windsor, including a large tree that blew down blocking Sams Creek Road in the 2700 block. Trees and wires blew down onto MD-27 Ridge Road. Numerous trees and wires blew down around Winfield. Numerous trees blew down in the 600 block of Conaway Lane. Numerous trees blew down around Kingsville and Pleasant Furnace, including one onto a car in the 800 block of Petem Road. Dozens of trees, branches and wires blew down around Bel Air. Numerous trees, branches, and wires blew down around Joppa. There were a couple dozen reports of trees and wires blown down in the Mount Airy area.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 26.4759 km away, between 2023-07-28 18:36:00 and 2023-07-28 20:35:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A subtle remnant disturbance from prior day's convection over the Midwest amplified a pre-existing lee pressure trough, igniting numerous thunderstorms. Given the excessive hot, humid, and unstable environment, these thunderstorms were able to organize into clusters and lines despite a lack of stronger wind shear. A subtle remnant disturbance from prior day's convection over the Midwest amplified a pre-existing lee pressure trough, igniting numerous thunderstorms. Given the excessive hot, humid, and unstable environment, these thunderstorms were able to organize into clusters and lines despite a lack of stronger wind shear. A subtle remnant disturbance from prior day's convection over the Midwest amplified a pre-existing lee pressure trough, igniting numerous thunderstorms. Given the excessive hot, humid, and unstable environment, these thunderstorms were able to organize into clusters and lines despite a lack of stronger wind shear. A subtle remnant disturbance from prior day's convection over the Midwest amplified a pre-existing lee pressure trough, igniting numerous thunderstorms. Given the excessive hot, humid, and unstable environment, these thunderstorms were able to organize into clusters and lines despite a lack of stronger wind shear. A subtle remnant disturbance from prior day's convection over the Midwest amplified a pre-existing lee pressure trough, igniting numerous thunderstorms. Given the excessive hot, humid, and unstable environment, these thunderstorms were able to organize into clusters and lines despite a lack of stronger wind shear. A subtle remnant disturbance from prior day's convection over the Midwest amplified a pre-existing lee pressure trough, igniting numerous thunderstorms. Given the excessive hot, humid, and unstable environment, these thunderstorms were able to organize into clusters and lines despite a lack of stronger wind shear. A subtle remnant disturbance from prior day's convection over the Midwest amplified a pre-existing lee pressure trough, igniting numerous thunderstorms. Given the excessive hot, humid, and unstable environment, these thunderstorms were able to organize into clusters and lines despite a lack of stronger wind shear. A subtle remnant disturbance from prior day's convection over the Midwest amplified a pre-existing lee pressure trough, igniting numerous thunderstorms. Given the excessive hot, humid, and unstable environment, these thunderstorms were able to organize into clusters and lines despite a lack of stronger wind shear. A subtle remnant disturbance from prior day's convection over the Midwest amplified a pre-existing lee pressure trough, igniting numerous thunderstorms. Given the excessive hot, humid, and unstable environment, these thunderstorms were able to organize into clusters and lines despite a lack of stronger wind shear. A subtle remnant disturbance from prior day's convection over the Midwest amplified a pre-existing lee pressure trough, igniting numerous thunderstorms. Given the excessive hot, humid, and unstable environment, these thunderstorms were able to organize into clusters and lines despite a lack of stronger wind shear. A subtle remnant disturbance from prior day's convection over the Midwest amplified a pre-existing lee pressure trough, igniting numerous thunderstorms. Given the excessive hot, humid, and unstable environment, these thunderstorms were able to organize into clusters and lines despite a lack of stronger wind shear. A subtle remnant disturbance from prior day's convection over the Midwest amplified a pre-existing lee pressure trough, igniting numerous thunderstorms. Given the excessive hot, humid, and unstable environment, these thunderstorms were able to organize into clusters and lines despite a lack of stronger wind shear. A subtle remnant disturbance from prior day's convection over the Midwest amplified a pre-existing lee pressure trough, igniting numerous thunderstorms. Given the excessive hot, humid, and unstable environment, these thunderstorms were able to organize into clusters and lines despite a lack of stronger wind shear. A subtle remnant disturbance from prior day's convection over the Midwest amplified a pre-existing lee pressure trough, igniting numerous thunderstorms. Given the excessive hot, humid, and unstable environment, these thunderstorms were able to organize into clusters and lines despite a lack of stronger wind shear. A subtle remnant disturbance from prior day's convection over the Midwest amplified a pre-existing lee pressure trough, igniting numerous thunderstorms. Given the excessive hot, humid, and unstable environment, these thunderstorms were able to organize into clusters and lines despite a lack of stronger wind shear. A subtle remnant disturbance from prior day's convection over the Midwest amplified a pre-existing lee pressure trough, igniting numerous thunderstorms. Given the excessive hot, humid, and unstable environment, these thunderstorms were able to organize into clusters and lines despite a lack of stronger wind shear. A subtle remnant disturbance from prior day's convection over the Midwest amplified a pre-existing lee pressure trough, igniting numerous thunderstorms. Given the excessive hot, humid, and unstable environment, these thunderstorms were able to organize into clusters and lines despite a lack of stronger wind shear. A subtle remnant disturbance from prior day's convection over the Midwest amplified a pre-existing lee pressure trough, igniting numerous thunderstorms. Given the excessive hot, humid, and unstable environment, these thunderstorms were able to organize into clusters and lines despite a lack of stronger wind shear. A subtle remnant disturbance from prior day's convection over the Midwest amplified a pre-existing lee pressure trough, igniting numerous thunderstorms. Given the excessive hot, humid, and unstable environment, these thunderstorms were able to organize into clusters and lines despite a lack of stronger wind shear.\nEvent Narrative: Wind gusts of up to 40 knots (46 MPH) were measured by the Hart Miller WeatherFlow sensor (XHRT). A wind gust of 39 knots (45 MPH) was measured by a mesonet at the intersection of MD-43 White Marsh Boulevard and MD-150 Eastern Boulevard (MD063) adjacent to the Chesapeake Bay. A wind gust of 40 knots (46 MPH) was measured by a mesonet at Baltimore Tower (MSI05) adjacent to the tidal Patapsco River. A thunderstorm produced an estimated wind gust to 34 knots (39 MPH) near a mesonet at Hampstead Hill Academy (BLMHH) adjacent to the tidal Patapsco River. A wind gust of 35 knots (40 MPH) was measured by a mesonet at the Maryland Science Center (BLMRE) adjacent to the tidal Patapsco River. Wind gusts of up to 48 knots (55 MPH) were measured by a personal weather station at Persimmon Point (KMDANNAP2658) adjacent to the Chesapeake Bay. Wind gusts of up to 43 knots (49 MPH) were measured by the Tolchester Beach NOS sensor (TCBM2). A thunderstorm produced an estimated wind gust to 34 knots (39 MPH) near a Tempest station on North Bayview Avenue adjacent to the Chesapeake Bay. Wind gusts of up to 49 knots (56 MPH) were measured by a Tempest station at Huntingfield Point adjacent to the tidal Chester River. A thunderstorm produced an estimated wind gust to 34 knots (39 MPH) near the Thomas Point NOS sensor (TPLM2). A thunderstorm produced an estimated wind gust to 34 knots (39 MPH) near a personal weather station at Annapolis Sailing School (KMDANNAP2625) adjacent to the Chesapeake Bay. Wind gusts of up to 43 knots (49 MPH) were measured by the Tolly Point WeatherFlow sensor (XTOL). A thunderstorm produced an estimated wind gust to 34 knots (39 MPH) near the Greenbury Point WeatherFlow sensor (XGBY). A thunderstorm produced an estimated wind gust to 34 knots (39 MPH) near a Tempest station on Thomas Point Road adjacent to the Chesapeake Bay. Wind gusts of up to 46 knots (53 MPH) were measured by the I-695 Francis Scott Key Bridge Northeast Tower NOS sensor (FSNM2). Wind gusts of up to 38 knots (44 MPH) were measured by a personal weather station at Canton - Baltimore Water Taxi (KMDBALTI181). Wind gusts of up to 39 knots (45 MPH) were measured by the Seneca Creek WeatherFlow sensor (XSNC). Wind gusts of up to 42 knots (48 MPH) were measured by the I-695 Francis Scott Key Bridge NOS sensor (FSKM2). A thunderstorm produced an estimated wind gust to 34 knots (39 MPH) near a personal weather station at Persimmon Point (KMDANNAP2658) adjacent to the Chesapeake Bay.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 39.8141 km away, between 2023-07-28 20:36:00 and 2023-07-28 20:43:00. The events included records with estimated wind gusts of 50.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A shortwave and weak frontal boundary over the area resulted in showers and thunderstorms developing. A few storms became severe, producing damaging wind gusts. A shortwave and weak frontal boundary over the area resulted in showers and thunderstorms developing. A few storms became severe, producing damaging wind gusts.\nEvent Narrative: Tree down in Stevensville per 911 call center. Time estimated from radar. Multiple large tree branches down. picture provided via social media.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 29.5014 km away, between 2023-07-29 15:04:00 and 2023-07-29 16:00:00.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 1645000.0 and crop damage of 0.0. \n\nEpisode Narrative: A strong cold front intersected a very hot, humid, and unstable airmass across the Mid-Atlantic shortly after peak heating. Aided by dynamics and moderately strong shear from an approaching upper-level trough, the front spawned bands of thunderstorms that produced considerable wind damage particularly in the I-95 corridor. Some areas saw the worst thunderstorm-driven wind speeds and damage since the derecho in June 2012, though the area affected by the highest magnitude of winds was not nearly as large. A strong cold front intersected a very hot, humid, and unstable airmass across the Mid-Atlantic shortly after peak heating. Aided by dynamics and moderately strong shear from an approaching upper-level trough, the front spawned bands of thunderstorms that produced considerable wind damage particularly in the I-95 corridor. Some areas saw the worst thunderstorm-driven wind speeds and damage since the derecho in June 2012, though the area affected by the highest magnitude of winds was not nearly as large. A strong cold front intersected a very hot, humid, and unstable airmass across the Mid-Atlantic shortly after peak heating. Aided by dynamics and moderately strong shear from an approaching upper-level trough, the front spawned bands of thunderstorms that produced considerable wind damage particularly in the I-95 corridor. Some areas saw the worst thunderstorm-driven wind speeds and damage since the derecho in June 2012, though the area affected by the highest magnitude of winds was not nearly as large. A strong cold front intersected a very hot, humid, and unstable airmass across the Mid-Atlantic shortly after peak heating. Aided by dynamics and moderately strong shear from an approaching upper-level trough, the front spawned bands of thunderstorms that produced considerable wind damage particularly in the I-95 corridor. Some areas saw the worst thunderstorm-driven wind speeds and damage since the derecho in June 2012, though the area affected by the highest magnitude of winds was not nearly as large. A strong cold front intersected a very hot, humid, and unstable airmass across the Mid-Atlantic shortly after peak heating. Aided by dynamics and moderately strong shear from an approaching upper-level trough, the front spawned bands of thunderstorms that produced considerable wind damage particularly in the I-95 corridor. Some areas saw the worst thunderstorm-driven wind speeds and damage since the derecho in June 2012, though the area affected by the highest magnitude of winds was not nearly as large. A strong cold front intersected a very hot, humid, and unstable airmass across the Mid-Atlantic shortly after peak heating. Aided by dynamics and moderately strong shear from an approaching upper-level trough, the front spawned bands of thunderstorms that produced considerable wind damage particularly in the I-95 corridor. Some areas saw the worst thunderstorm-driven wind speeds and damage since the derecho in June 2012, though the area affected by the highest magnitude of winds was not nearly as large. A strong cold front intersected a very hot, humid, and unstable airmass across the Mid-Atlantic shortly after peak heating. Aided by dynamics and moderately strong shear from an approaching upper-level trough, the front spawned bands of thunderstorms that produced considerable wind damage particularly in the I-95 corridor. Some areas saw the worst thunderstorm-driven wind speeds and damage since the derecho in June 2012, though the area affected by the highest magnitude of winds was not nearly as large. A strong cold front intersected a very hot, humid, and unstable airmass across the Mid-Atlantic shortly after peak heating. Aided by dynamics and moderately strong shear from an approaching upper-level trough, the front spawned bands of thunderstorms that produced considerable wind damage particularly in the I-95 corridor. Some areas saw the worst thunderstorm-driven wind speeds and damage since the derecho in June 2012, though the area affected by the highest magnitude of winds was not nearly as large. A strong cold front intersected a very hot, humid, and unstable airmass across the Mid-Atlantic shortly after peak heating. Aided by dynamics and moderately strong shear from an approaching upper-level trough, the front spawned bands of thunderstorms that produced considerable wind damage particularly in the I-95 corridor. Some areas saw the worst thunderstorm-driven wind speeds and damage since the derecho in June 2012, though the area affected by the highest magnitude of winds was not nearly as large. A strong cold front intersected a very hot, humid, and unstable airmass across the Mid-Atlantic shortly after peak heating. Aided by dynamics and moderately strong shear from an approaching upper-level trough, the front spawned bands of thunderstorms that produced considerable wind damage particularly in the I-95 corridor. Some areas saw the worst thunderstorm-driven wind speeds and damage since the derecho in June 2012, though the area affected by the highest magnitude of winds was not nearly as large.\nEvent Narrative: Trees and wires blew down on MD-138 Shepperd Road between Monkton Road and Wesley Chapel Road. Several trees blew down in and near Columbia, including along Harpers Farm Road, Cedar Lane, and Homewood Road. Dozens of large trees and branches blew down between Jessup and Savage. Numerous trees blew down on northbound US-1 Washington Boulevard at Corridor Road. Numerous large trees and branches blew down on Vollmerhausen Road between the Little Patuxent River and Savage Guilford Road, and along Foundry Street. Trees blew down on US-1 Washington Boulevard at Whiskey Bottom Road. Trees blew down on southbound US-29 Columbia Pike at Exit 21A/southbound MD-108 Clarksville Pike. Trees blew down on MD-175 Rouse Parkway/Little Patuxent Parkway at US-29 Columbia Pike. Trees blew down on US-1 Belair Road at New Cut Road. A wind gust of 50 knots (58 MPH) was measured by a mesonet at Kenilworth Elementary School (BOWIE). Numerous trees and large branches blew down in the area, including near the intersection of MD-197 Laurel-Bowie Road and Old Chapel Road. Trees blew down on Madelay Lane at Melody Turn, and Marn Street at Moylan Street. Dozens of trees, branches and wires blew down in the Edgewood area, including several onto cars and houses. Trees blew down on US-40 Pulaski Highway at Abingdon Road. Numerous trees blew down on MD-450 Defense Highway at Pebblebrook Court, MD-424 Davidsonville Road at US-50 John Hanson Highway, and MD-178 Generals Highway prior to Herald Harbor Road. Trees blew down in Olney, including on Gainford Court, and near the intersection of MD-108 Olney Sandy Spring Road past Prince Philip Drive.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 34.1659 km away, between 2023-07-29 15:48:00 and 2023-07-29 17:00:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A strong cold front intersected a very hot, humid, and unstable airmass across the Mid-Atlantic shortly after peak heating. Aided by dynamics and moderately strong shear from an approaching upper-level trough, the front spawned bands of thunderstorms that produced up to storm-force winds over area waterways. A strong cold front intersected a very hot, humid, and unstable airmass across the Mid-Atlantic shortly after peak heating. Aided by dynamics and moderately strong shear from an approaching upper-level trough, the front spawned bands of thunderstorms that produced up to storm-force winds over area waterways. A strong cold front intersected a very hot, humid, and unstable airmass across the Mid-Atlantic shortly after peak heating. Aided by dynamics and moderately strong shear from an approaching upper-level trough, the front spawned bands of thunderstorms that produced up to storm-force winds over area waterways. A strong cold front intersected a very hot, humid, and unstable airmass across the Mid-Atlantic shortly after peak heating. Aided by dynamics and moderately strong shear from an approaching upper-level trough, the front spawned bands of thunderstorms that produced up to storm-force winds over area waterways. A strong cold front intersected a very hot, humid, and unstable airmass across the Mid-Atlantic shortly after peak heating. Aided by dynamics and moderately strong shear from an approaching upper-level trough, the front spawned bands of thunderstorms that produced up to storm-force winds over area waterways. A strong cold front intersected a very hot, humid, and unstable airmass across the Mid-Atlantic shortly after peak heating. Aided by dynamics and moderately strong shear from an approaching upper-level trough, the front spawned bands of thunderstorms that produced up to storm-force winds over area waterways. A strong cold front intersected a very hot, humid, and unstable airmass across the Mid-Atlantic shortly after peak heating. Aided by dynamics and moderately strong shear from an approaching upper-level trough, the front spawned bands of thunderstorms that produced up to storm-force winds over area waterways. A strong cold front intersected a very hot, humid, and unstable airmass across the Mid-Atlantic shortly after peak heating. Aided by dynamics and moderately strong shear from an approaching upper-level trough, the front spawned bands of thunderstorms that produced up to storm-force winds over area waterways. A strong cold front intersected a very hot, humid, and unstable airmass across the Mid-Atlantic shortly after peak heating. Aided by dynamics and moderately strong shear from an approaching upper-level trough, the front spawned bands of thunderstorms that produced up to storm-force winds over area waterways. A strong cold front intersected a very hot, humid, and unstable airmass across the Mid-Atlantic shortly after peak heating. Aided by dynamics and moderately strong shear from an approaching upper-level trough, the front spawned bands of thunderstorms that produced up to storm-force winds over area waterways. A strong cold front intersected a very hot, humid, and unstable airmass across the Mid-Atlantic shortly after peak heating. Aided by dynamics and moderately strong shear from an approaching upper-level trough, the front spawned bands of thunderstorms that produced up to storm-force winds over area waterways. A strong cold front intersected a very hot, humid, and unstable airmass across the Mid-Atlantic shortly after peak heating. Aided by dynamics and moderately strong shear from an approaching upper-level trough, the front spawned bands of thunderstorms that produced up to storm-force winds over area waterways. A strong cold front intersected a very hot, humid, and unstable airmass across the Mid-Atlantic shortly after peak heating. Aided by dynamics and moderately strong shear from an approaching upper-level trough, the front spawned bands of thunderstorms that produced up to storm-force winds over area waterways. A strong cold front intersected a very hot, humid, and unstable airmass across the Mid-Atlantic shortly after peak heating. Aided by dynamics and moderately strong shear from an approaching upper-level trough, the front spawned bands of thunderstorms that produced up to storm-force winds over area waterways. A strong cold front intersected a very hot, humid, and unstable airmass across the Mid-Atlantic shortly after peak heating. Aided by dynamics and moderately strong shear from an approaching upper-level trough, the front spawned bands of thunderstorms that produced up to storm-force winds over area waterways. A strong cold front intersected a very hot, humid, and unstable airmass across the Mid-Atlantic shortly after peak heating. Aided by dynamics and moderately strong shear from an approaching upper-level trough, the front spawned bands of thunderstorms that produced up to storm-force winds over area waterways. A strong cold front intersected a very hot, humid, and unstable airmass across the Mid-Atlantic shortly after peak heating. Aided by dynamics and moderately strong shear from an approaching upper-level trough, the front spawned bands of thunderstorms that produced up to storm-force winds over area waterways. A strong cold front intersected a very hot, humid, and unstable airmass across the Mid-Atlantic shortly after peak heating. Aided by dynamics and moderately strong shear from an approaching upper-level trough, the front spawned bands of thunderstorms that produced up to storm-force winds over area waterways. A strong cold front intersected a very hot, humid, and unstable airmass across the Mid-Atlantic shortly after peak heating. Aided by dynamics and moderately strong shear from an approaching upper-level trough, the front spawned bands of thunderstorms that produced up to storm-force winds over area waterways. A strong cold front intersected a very hot, humid, and unstable airmass across the Mid-Atlantic shortly after peak heating. Aided by dynamics and moderately strong shear from an approaching upper-level trough, the front spawned bands of thunderstorms that produced up to storm-force winds over area waterways. A strong cold front intersected a very hot, humid, and unstable airmass across the Mid-Atlantic shortly after peak heating. Aided by dynamics and moderately strong shear from an approaching upper-level trough, the front spawned bands of thunderstorms that produced up to storm-force winds over area waterways. A strong cold front intersected a very hot, humid, and unstable airmass across the Mid-Atlantic shortly after peak heating. Aided by dynamics and moderately strong shear from an approaching upper-level trough, the front spawned bands of thunderstorms that produced up to storm-force winds over area waterways. A strong cold front intersected a very hot, humid, and unstable airmass across the Mid-Atlantic shortly after peak heating. Aided by dynamics and moderately strong shear from an approaching upper-level trough, the front spawned bands of thunderstorms that produced up to storm-force winds over area waterways. A strong cold front intersected a very hot, humid, and unstable airmass across the Mid-Atlantic shortly after peak heating. Aided by dynamics and moderately strong shear from an approaching upper-level trough, the front spawned bands of thunderstorms that produced up to storm-force winds over area waterways. A strong cold front intersected a very hot, humid, and unstable airmass across the Mid-Atlantic shortly after peak heating. Aided by dynamics and moderately strong shear from an approaching upper-level trough, the front spawned bands of thunderstorms that produced up to storm-force winds over area waterways. A strong cold front intersected a very hot, humid, and unstable airmass across the Mid-Atlantic shortly after peak heating. Aided by dynamics and moderately strong shear from an approaching upper-level trough, the front spawned bands of thunderstorms that produced up to storm-force winds over area waterways. A strong cold front intersected a very hot, humid, and unstable airmass across the Mid-Atlantic shortly after peak heating. Aided by dynamics and moderately strong shear from an approaching upper-level trough, the front spawned bands of thunderstorms that produced up to storm-force winds over area waterways. A strong cold front intersected a very hot, humid, and unstable airmass across the Mid-Atlantic shortly after peak heating. Aided by dynamics and moderately strong shear from an approaching upper-level trough, the front spawned bands of thunderstorms that produced up to storm-force winds over area waterways. A strong cold front intersected a very hot, humid, and unstable airmass across the Mid-Atlantic shortly after peak heating. Aided by dynamics and moderately strong shear from an approaching upper-level trough, the front spawned bands of thunderstorms that produced up to storm-force winds over area waterways. A strong cold front intersected a very hot, humid, and unstable airmass across the Mid-Atlantic shortly after peak heating. Aided by dynamics and moderately strong shear from an approaching upper-level trough, the front spawned bands of thunderstorms that produced up to storm-force winds over area waterways. A strong cold front intersected a very hot, humid, and unstable airmass across the Mid-Atlantic shortly after peak heating. Aided by dynamics and moderately strong shear from an approaching upper-level trough, the front spawned bands of thunderstorms that produced up to storm-force winds over area waterways. A strong cold front intersected a very hot, humid, and unstable airmass across the Mid-Atlantic shortly after peak heating. Aided by dynamics and moderately strong shear from an approaching upper-level trough, the front spawned bands of thunderstorms that produced up to storm-force winds over area waterways. A strong cold front intersected a very hot, humid, and unstable airmass across the Mid-Atlantic shortly after peak heating. Aided by dynamics and moderately strong shear from an approaching upper-level trough, the front spawned bands of thunderstorms that produced up to storm-force winds over area waterways. A strong cold front intersected a very hot, humid, and unstable airmass across the Mid-Atlantic shortly after peak heating. Aided by dynamics and moderately strong shear from an approaching upper-level trough, the front spawned bands of thunderstorms that produced up to storm-force winds over area waterways. A strong cold front intersected a very hot, humid, and unstable airmass across the Mid-Atlantic shortly after peak heating. Aided by dynamics and moderately strong shear from an approaching upper-level trough, the front spawned bands of thunderstorms that produced up to storm-force winds over area waterways. A strong cold front intersected a very hot, humid, and unstable airmass across the Mid-Atlantic shortly after peak heating. Aided by dynamics and moderately strong shear from an approaching upper-level trough, the front spawned bands of thunderstorms that produced up to storm-force winds over area waterways. A strong cold front intersected a very hot, humid, and unstable airmass across the Mid-Atlantic shortly after peak heating. Aided by dynamics and moderately strong shear from an approaching upper-level trough, the front spawned bands of thunderstorms that produced up to storm-force winds over area waterways. A strong cold front intersected a very hot, humid, and unstable airmass across the Mid-Atlantic shortly after peak heating. Aided by dynamics and moderately strong shear from an approaching upper-level trough, the front spawned bands of thunderstorms that produced up to storm-force winds over area waterways.\nEvent Narrative: Wind gusts of up to 37 knots (43 MPH) were measured by the Annapolis CBIBS sensor (44063). Wind gusts of up to 43 knots (49 MPH) were measured by the Greenbury Point WeatherFlow sensor (XGBY). Wind gusts of up to 53 knots (61 MPH) were measured by the Saunders Point Light WeatherFlow sensor (XMTR). Wind gusts of up to 44 knots (51 MPH) were measured by the Tolly Point WeatherFlow sensor (XTOL). A wind gust of 35 knots (40 MPH) was measured by a personal weather station at Persimmon Point (KMDANNAP2658). Wind gusts of up to 49 knots (56 MPH) were measured by a personal weather station at Annapolis Sailing School (KMDANNAP2625). Wind gusts of up to 41 knots (47 MPH) were measured by a personal weather station on Ramsgate Drive (KMDANNAP2704) adjacent to the Chesapeake Bay. Wind gusts of up to 41 knots (47 MPH) were measured by a personal weather station at Curtis Point (KMDSHADY19) adjacent to the Chesapeake Bay. A thunderstorm produced an estimated wind gust to 34 knots (39 MPH) near a Tempest station on Wainwright Beach. Wind gusts of up to 43 knots (49 MPH) were measured by a Tempest station on Thomas Point Road adjacent to the Chesapeake Bay. A wind gust of 37 knots (43 MPH) was measured by a personal weather station at Love Point (KMDSTEVE52) adjacent to the Chesapeake Bay. A wind gust of 41 knots (47 MPH) was measured by the AWOS at Bay Bridge Airport (KW29) adjacent to the Chesapeake Bay. Wind gusts of up to 41 knots (47 MPH) were measured by the I-695 Francis Scott Key Bridge NOS sensor (FSKM2). Wind gusts of up to 37 knots (43 MPH) were measured by a Tempest station on Frederick Avenue adjacent to the Chesapeake Bay. A thunderstorm produced an estimated wind gust to 34 knots (39 MPH) near a mesonet at Saint Mary's Elementary School (ANNAS). A wind gust of 58 knots (67 MPH) was measured by the Thomas Point NOS sensor (TPLM2). A wind gust of 49 knots (56 MPH) was measured by a mesonet at WPL Pier 31 (MD068). A thunderstorm produced an estimated wind gust to 34 knots (39 MPH) near the Sandy Point WeatherFlow sensor (XSPT). Wind gusts of up to 44 knots (51 MPH) were measured by a personal weather station at Marling Farms (KMDCHEST20) adjacent to Eastern Bay. Wind gusts of up to 57 knots (66 MPH) were measured by a Tempest station on Beach Side Drive adjacent to the Chesapeake Bay. Wind gusts of up to 42 knots (48 MPH) were measured by a personal weather station at Canton - Baltimore Water Taxi (KMDBALTI181). A thunderstorm produced an estimated wind gust to 34 knots (39 MPH) near a mesonet at the Maryland Science Center (BLMRE) adjacent to the tidal Patapsco River. A thunderstorm produced an estimated wind gust to 34 knots (39 MPH) near the AWOS at Martin State Airport (KMTN) adjacent to the Chesapeake Bay. A wind gust of 34 knots (39 MPH) was measured by the I-695 Francis Scott Key Bridge Northeast Tower NOS sensor (FSNM2). Wind gusts of up 39 knots (45 MPH) were measured by the Kent Island WeatherFlow sensor (XKNT). Wind gusts of up to 39 knots (45 MPH) were measured by a personal weather station (Lighthouse View, KMDSTEVE73) adjacent to the Chesapeake Bay. Wind gusts of up to 43 knots (49 MPH) were measured by a personal weather station at Cove Creek (KMDSTEVE97) adjacent to the Chesapeake Bay. Wind gusts of up to 34 knots (39 MPH) were measured by a mesonet at Prospect Bay adjacent to Eastern Bay. A thunderstorm produced an estimated wind gust to 34 knots (39 MPH) near the AWOS at Weide (KEDG) adjacent to the Chesapeake Bay. Wind gusts of up to 42 knots (48 MPH) were measured by the Hart Miller WeatherFlow sensor (XHRT). A wind gust of 40 knots (46 MPH) was measured by the Seneca Creek WeatherFlow sensor (XSNC). A wind gust of 34 knots (39 MPH) was measured by the ASOS at the U.S. Naval Academy in Annapolis (KNAK) adjacent to the Chesapeake Bay. A thunderstorm produced an estimated wind gust to 34 knots (39 MPH) near a personal weather station at Holly Farm Beach (KMDESSEX50) adjacent to the Chesapeake Bay. Wind gusts of up to 61 knots (70 MPH) were measured by a personal weather station at Northwest Creek (KMDSTEVE76) adjacent to the Chesapeake Bay. A thunderstorm produced an estimated wind gust to 34 knots (39 MPH) near a personal weather station (Kratz Weather Station, KMDSTEVE113) adjacent to the Chesapeake Bay. A thunderstorm produced an estimated wind gust to 34 knots (39 MPH) near a Tempest station on Beach Side Drive adjacent to the Chesapeake Bay. Wind gusts of up to 43 knots (49 MPH) were measured by a mesonet at Crab Alley Bay adjacent to Eastern Bay. A wind gust of 38 knots (44 MPH) was measured by a mesonet on the US-50 Kent Narrows Bridge (MD040).", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 42.4903 km away, between 2023-07-29 16:19:00 and 2023-07-29 16:30:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A strong cold front moved through, with widespread showers and thunderstorms moving through. Some severe storms produced damaging wind gusts. A strong cold front moved through, with widespread showers and thunderstorms moving through. Some severe storms produced damaging wind gusts. A strong cold front moved through, with widespread showers and thunderstorms moving through. Some severe storms produced damaging wind gusts. A strong cold front moved through, with widespread showers and thunderstorms moving through. Some severe storms produced damaging wind gusts. A strong cold front moved through, with widespread showers and thunderstorms moving through. Some severe storms produced damaging wind gusts.\nEvent Narrative: Tree down at Kent Island High School. Time estimated from radar. Wunderground Station kmdsteve76. Time given in report. WxFlow gauge at Beach Side Drive. Time given in report. Wunderground station kmdsteve76. Time given in report. WxFlow gauge at Beach Side Drive. Time given in report.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 32.6376 km away, between 2023-08-07 15:57:00 and 2023-08-07 17:17:00. The events included records with estimated wind gusts of 54.916666666666664 mph.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 406000.0 and crop damage of 0.0. \n\nEpisode Narrative: A strong cold front, driven by an unusually strong upper-level trough and wind shear, interacted with a hot, humid, and unstable airmass over the Mid-Atlantic. This pattern resulted in the formation of lines of thunderstorms and several supercells. The most widespread and significant wind damage was noted over northern Maryland, although pockets of considerable wind damage were noted over portions of northwestern Virginia and eastern West Virginia. Somewhat atypical for the Mid-Atlantic is late summer was the number of large hail reports, with multiple instances of giant hail noted. A strong cold front, driven by an unusually strong upper-level trough and wind shear, interacted with a hot, humid, and unstable airmass over the Mid-Atlantic. This pattern resulted in the formation of lines of thunderstorms and several supercells. The most widespread and significant wind damage was noted over northern Maryland, although pockets of considerable wind damage were noted over portions of northwestern Virginia and eastern West Virginia. Somewhat atypical for the Mid-Atlantic is late summer was the number of large hail reports, with multiple instances of giant hail noted. A strong cold front, driven by an unusually strong upper-level trough and wind shear, interacted with a hot, humid, and unstable airmass over the Mid-Atlantic. This pattern resulted in the formation of lines of thunderstorms and several supercells. The most widespread and significant wind damage was noted over northern Maryland, although pockets of considerable wind damage were noted over portions of northwestern Virginia and eastern West Virginia. Somewhat atypical for the Mid-Atlantic is late summer was the number of large hail reports, with multiple instances of giant hail noted. A strong cold front, driven by an unusually strong upper-level trough and wind shear, interacted with a hot, humid, and unstable airmass over the Mid-Atlantic. This pattern resulted in the formation of lines of thunderstorms and several supercells. The most widespread and significant wind damage was noted over northern Maryland, although pockets of considerable wind damage were noted over portions of northwestern Virginia and eastern West Virginia. Somewhat atypical for the Mid-Atlantic is late summer was the number of large hail reports, with multiple instances of giant hail noted. A strong cold front, driven by an unusually strong upper-level trough and wind shear, interacted with a hot, humid, and unstable airmass over the Mid-Atlantic. This pattern resulted in the formation of lines of thunderstorms and several supercells. The most widespread and significant wind damage was noted over northern Maryland, although pockets of considerable wind damage were noted over portions of northwestern Virginia and eastern West Virginia. Somewhat atypical for the Mid-Atlantic is late summer was the number of large hail reports, with multiple instances of giant hail noted. A strong cold front, driven by an unusually strong upper-level trough and wind shear, interacted with a hot, humid, and unstable airmass over the Mid-Atlantic. This pattern resulted in the formation of lines of thunderstorms and several supercells. The most widespread and significant wind damage was noted over northern Maryland, although pockets of considerable wind damage were noted over portions of northwestern Virginia and eastern West Virginia. Somewhat atypical for the Mid-Atlantic is late summer was the number of large hail reports, with multiple instances of giant hail noted. A strong cold front, driven by an unusually strong upper-level trough and wind shear, interacted with a hot, humid, and unstable airmass over the Mid-Atlantic. This pattern resulted in the formation of lines of thunderstorms and several supercells. The most widespread and significant wind damage was noted over northern Maryland, although pockets of considerable wind damage were noted over portions of northwestern Virginia and eastern West Virginia. Somewhat atypical for the Mid-Atlantic is late summer was the number of large hail reports, with multiple instances of giant hail noted. A strong cold front, driven by an unusually strong upper-level trough and wind shear, interacted with a hot, humid, and unstable airmass over the Mid-Atlantic. This pattern resulted in the formation of lines of thunderstorms and several supercells. The most widespread and significant wind damage was noted over northern Maryland, although pockets of considerable wind damage were noted over portions of northwestern Virginia and eastern West Virginia. Somewhat atypical for the Mid-Atlantic is late summer was the number of large hail reports, with multiple instances of giant hail noted. A strong cold front, driven by an unusually strong upper-level trough and wind shear, interacted with a hot, humid, and unstable airmass over the Mid-Atlantic. This pattern resulted in the formation of lines of thunderstorms and several supercells. The most widespread and significant wind damage was noted over northern Maryland, although pockets of considerable wind damage were noted over portions of northwestern Virginia and eastern West Virginia. Somewhat atypical for the Mid-Atlantic is late summer was the number of large hail reports, with multiple instances of giant hail noted. A strong cold front, driven by an unusually strong upper-level trough and wind shear, interacted with a hot, humid, and unstable airmass over the Mid-Atlantic. This pattern resulted in the formation of lines of thunderstorms and several supercells. The most widespread and significant wind damage was noted over northern Maryland, although pockets of considerable wind damage were noted over portions of northwestern Virginia and eastern West Virginia. Somewhat atypical for the Mid-Atlantic is late summer was the number of large hail reports, with multiple instances of giant hail noted. A strong cold front, driven by an unusually strong upper-level trough and wind shear, interacted with a hot, humid, and unstable airmass over the Mid-Atlantic. This pattern resulted in the formation of lines of thunderstorms and several supercells. The most widespread and significant wind damage was noted over northern Maryland, although pockets of considerable wind damage were noted over portions of northwestern Virginia and eastern West Virginia. Somewhat atypical for the Mid-Atlantic is late summer was the number of large hail reports, with multiple instances of giant hail noted. A strong cold front, driven by an unusually strong upper-level trough and wind shear, interacted with a hot, humid, and unstable airmass over the Mid-Atlantic. This pattern resulted in the formation of lines of thunderstorms and several supercells. The most widespread and significant wind damage was noted over northern Maryland, although pockets of considerable wind damage were noted over portions of northwestern Virginia and eastern West Virginia. Somewhat atypical for the Mid-Atlantic is late summer was the number of large hail reports, with multiple instances of giant hail noted.\nEvent Narrative: Trees blew down near Carroll Community College. Several trees blew down along MD-97 Old Washington Road at the Carroll/Howard County line. Trees blew down across MD-144 Frederick Road near MD-97 Roxbury Mills Road. Dozens of trees, branches and wires blew down around Eldersburg, blocking several roads for up to a day. Dozens of trees blew down in Glenwood and Lisbon. Numerous trees blew down in Sykesville, including at least one onto a house. Dozens of trees, branches and wires blew down in the Finksburg area. Trees blew down on MD-26 Liberty Road to the west of Lyons Mill Road. A large tree blew down onto a structure in the 12300 block of Timber Grove Road. Several trees blew down near the intersection of McDonogh Road and Winands Road. A tree blew down onto a structure in the 1300 block of Sudvale Road. Trees and power lines blew down around Davidsonville.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 28.1238 km away, between 2023-08-07 16:39:00 and 2023-08-07 18:05:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A strong cold front, driven by an unusually strong upper-level trough and wind shear, interacted with a hot, humid, and unstable airmass over the Mid-Atlantic. This pattern resulted in the formation of lines of thunderstorms and several supercells. The most widespread and significant wind damage was noted over northern Maryland, although pockets of considerable wind damage were noted over portions of northwestern Virginia and eastern West Virginia. Somewhat atypical for the Mid-Atlantic is late summer was the number of large hail reports, with multiple instances of giant hail noted. A strong cold front, driven by an unusually strong upper-level trough and wind shear, interacted with a hot, humid, and unstable airmass over the Mid-Atlantic. This pattern resulted in the formation of lines of thunderstorms and several supercells. The most widespread and significant wind damage was noted over northern Maryland, although pockets of considerable wind damage were noted over portions of northwestern Virginia and eastern West Virginia. Somewhat atypical for the Mid-Atlantic is late summer was the number of large hail reports, with multiple instances of giant hail noted. A strong cold front, driven by an unusually strong upper-level trough and wind shear, interacted with a hot, humid, and unstable airmass over the Mid-Atlantic. This pattern resulted in the formation of lines of thunderstorms and several supercells. The most widespread and significant wind damage was noted over northern Maryland, although pockets of considerable wind damage were noted over portions of northwestern Virginia and eastern West Virginia. Somewhat atypical for the Mid-Atlantic is late summer was the number of large hail reports, with multiple instances of giant hail noted. A strong cold front, driven by an unusually strong upper-level trough and wind shear, interacted with a hot, humid, and unstable airmass over the Mid-Atlantic. This pattern resulted in the formation of lines of thunderstorms and several supercells. The most widespread and significant wind damage was noted over northern Maryland, although pockets of considerable wind damage were noted over portions of northwestern Virginia and eastern West Virginia. Somewhat atypical for the Mid-Atlantic is late summer was the number of large hail reports, with multiple instances of giant hail noted. A strong cold front, driven by an unusually strong upper-level trough and wind shear, interacted with a hot, humid, and unstable airmass over the Mid-Atlantic. This pattern resulted in the formation of lines of thunderstorms and several supercells. The most widespread and significant wind damage was noted over northern Maryland, although pockets of considerable wind damage were noted over portions of northwestern Virginia and eastern West Virginia. Somewhat atypical for the Mid-Atlantic is late summer was the number of large hail reports, with multiple instances of giant hail noted. A strong cold front, driven by an unusually strong upper-level trough and wind shear, interacted with a hot, humid, and unstable airmass over the Mid-Atlantic. This pattern resulted in the formation of lines of thunderstorms and several supercells. The most widespread and significant wind damage was noted over northern Maryland, although pockets of considerable wind damage were noted over portions of northwestern Virginia and eastern West Virginia. Somewhat atypical for the Mid-Atlantic is late summer was the number of large hail reports, with multiple instances of giant hail noted. A strong cold front, driven by an unusually strong upper-level trough and wind shear, interacted with a hot, humid, and unstable airmass over the Mid-Atlantic. This pattern resulted in the formation of lines of thunderstorms and several supercells. The most widespread and significant wind damage was noted over northern Maryland, although pockets of considerable wind damage were noted over portions of northwestern Virginia and eastern West Virginia. Somewhat atypical for the Mid-Atlantic is late summer was the number of large hail reports, with multiple instances of giant hail noted. A strong cold front, driven by an unusually strong upper-level trough and wind shear, interacted with a hot, humid, and unstable airmass over the Mid-Atlantic. This pattern resulted in the formation of lines of thunderstorms and several supercells. The most widespread and significant wind damage was noted over northern Maryland, although pockets of considerable wind damage were noted over portions of northwestern Virginia and eastern West Virginia. Somewhat atypical for the Mid-Atlantic is late summer was the number of large hail reports, with multiple instances of giant hail noted. A strong cold front, driven by an unusually strong upper-level trough and wind shear, interacted with a hot, humid, and unstable airmass over the Mid-Atlantic. This pattern resulted in the formation of lines of thunderstorms and several supercells. The most widespread and significant wind damage was noted over northern Maryland, although pockets of considerable wind damage were noted over portions of northwestern Virginia and eastern West Virginia. Somewhat atypical for the Mid-Atlantic is late summer was the number of large hail reports, with multiple instances of giant hail noted. A strong cold front, driven by an unusually strong upper-level trough and wind shear, interacted with a hot, humid, and unstable airmass over the Mid-Atlantic. This pattern resulted in the formation of lines of thunderstorms and several supercells. The most widespread and significant wind damage was noted over northern Maryland, although pockets of considerable wind damage were noted over portions of northwestern Virginia and eastern West Virginia. Somewhat atypical for the Mid-Atlantic is late summer was the number of large hail reports, with multiple instances of giant hail noted. A strong cold front, driven by an unusually strong upper-level trough and wind shear, interacted with a hot, humid, and unstable airmass over the Mid-Atlantic. This pattern resulted in the formation of lines of thunderstorms and several supercells. The most widespread and significant wind damage was noted over northern Maryland, although pockets of considerable wind damage were noted over portions of northwestern Virginia and eastern West Virginia. Somewhat atypical for the Mid-Atlantic is late summer was the number of large hail reports, with multiple instances of giant hail noted. A strong cold front, driven by an unusually strong upper-level trough and wind shear, interacted with a hot, humid, and unstable airmass over the Mid-Atlantic. This pattern resulted in the formation of lines of thunderstorms and several supercells. The most widespread and significant wind damage was noted over northern Maryland, although pockets of considerable wind damage were noted over portions of northwestern Virginia and eastern West Virginia. Somewhat atypical for the Mid-Atlantic is late summer was the number of large hail reports, with multiple instances of giant hail noted. A strong cold front, driven by an unusually strong upper-level trough and wind shear, interacted with a hot, humid, and unstable airmass over the Mid-Atlantic. This pattern resulted in the formation of lines of thunderstorms and several supercells. The most widespread and significant wind damage was noted over northern Maryland, although pockets of considerable wind damage were noted over portions of northwestern Virginia and eastern West Virginia. Somewhat atypical for the Mid-Atlantic is late summer was the number of large hail reports, with multiple instances of giant hail noted. A strong cold front, driven by an unusually strong upper-level trough and wind shear, interacted with a hot, humid, and unstable airmass over the Mid-Atlantic. This pattern resulted in the formation of lines of thunderstorms and several supercells. The most widespread and significant wind damage was noted over northern Maryland, although pockets of considerable wind damage were noted over portions of northwestern Virginia and eastern West Virginia. Somewhat atypical for the Mid-Atlantic is late summer was the number of large hail reports, with multiple instances of giant hail noted. A strong cold front, driven by an unusually strong upper-level trough and wind shear, interacted with a hot, humid, and unstable airmass over the Mid-Atlantic. This pattern resulted in the formation of lines of thunderstorms and several supercells. The most widespread and significant wind damage was noted over northern Maryland, although pockets of considerable wind damage were noted over portions of northwestern Virginia and eastern West Virginia. Somewhat atypical for the Mid-Atlantic is late summer was the number of large hail reports, with multiple instances of giant hail noted. A strong cold front, driven by an unusually strong upper-level trough and wind shear, interacted with a hot, humid, and unstable airmass over the Mid-Atlantic. This pattern resulted in the formation of lines of thunderstorms and several supercells. The most widespread and significant wind damage was noted over northern Maryland, although pockets of considerable wind damage were noted over portions of northwestern Virginia and eastern West Virginia. Somewhat atypical for the Mid-Atlantic is late summer was the number of large hail reports, with multiple instances of giant hail noted.\nEvent Narrative: Wind gusts of up to 44 knots (51 MPH) were measured by a Tempest station on East Randall Street adjacent to the tidal Patapsco River. A wind gust of 37 knots (43 MPH) was measured by a mesonet at Baltimore Tower (MSI05) adjacent to the Patapsco River. A thunderstorm produced estimated wind gusts to 34 knots (39 MPH) near the I-695 Francis Scott Key Bridge NOS sensor (FSKM2). Wind gusts of up to 49 knots (56 MPH) were measured by the Hart Miller WeatherFlow sensor (XHRT). A thunderstorm produced estimated wind gusts to 34 knots (39 MPH) near a mesonet near Annapolis (EW5391) adjacent to the Chesapeake Bay. Wind gusts of up to 36 knots (41 MPH) were measured by the ASOS at the U.S. Naval Academy in Annapolis (KNAK) adjacent to the Chesapeake Bay. Wind gusts of up to 38 knots (44 MPH) were measured by the Greenbury Point WeatherFlow sensor (XGBY). Wind gusts of up to 42 knots (48 MPH) were measured by a mesonet at WPL Pier 31 (MD068). A wind gust of 36 knots (42 MPH) was measured by the Annapolis NOS sensor (APAM2). Wind gusts of up to 35 knots (40 MPH) were measured by the Tolly Point WeatherFlow sensor (XTOL). Wind gusts of up to 39 knots (45 MPH) were measured by a Tempest station at Huntingfield Point adjacent to the tidal Chester River. A thunderstorm produced estimated wind gusts to 34 knots (39 MPH) near the Sandy Point WeatherFlow sensor (XSPT). A thunderstorm produced an estimated wind gust to 34 knots (39 MPH) near a mesonet at Crab Alley Bay adjacent to Eastern Bay. A wind gust of 43 knots (50 MPH) was measured by a mesonet at the intersection of MD-43 White Marsh Boulevard and MD-150 Eastern Boulevard (MD063) adjacent to the Chesapeake Bay. Wind gusts of up to 39 knots (45 MPH) were measured by the Seneca Creek WeatherFlow sensor (XSNC). A wind gust of 45 knots (52 MPH) was measured by the AWOS at Martin State Airport (KMTN) adjacent to the Chesapeake Bay.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 40.0175 km away, between 2023-08-14 16:30:00 and 2023-08-14 17:35:00. The events included records with estimated wind gusts of 34.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A few clusters of thunderstorms developed ahead of an approaching cold front in an excessively humid environment during the afternoon hours. A few clusters of thunderstorms developed ahead of an approaching cold front in an excessively humid environment during the afternoon hours. A few clusters of thunderstorms developed ahead of an approaching cold front in an excessively humid environment during the afternoon hours. A few clusters of thunderstorms developed ahead of an approaching cold front in an excessively humid environment during the afternoon hours. A few clusters of thunderstorms developed ahead of an approaching cold front in an excessively humid environment during the afternoon hours.\nEvent Narrative: A thunderstorm produced an estimated wind gust to 34 knots (39 MPH) near the Thomas Point NOS sensor (TPLM2). A thunderstorm produced an estimated wind gust to 34 knots (39 MPH) near the AWOS at Bay Bridge Airport (KW29) adjacent to the Chesapeake Bay. A thunderstorm produced an estimated wind gust to 34 knots (39 MPH) near a mesonet at Crab Alley Bay adjacent to Eastern Bay. A thunderstorm produced an estimated wind gust to 34 knots (39 MPH) near a Tempest station at Huntingfield Point adjacent to the tidal Chester River. A thunderstorm produced an estimated wind gust to 34 knots (39 MPH) near the AWOS at Weide (KEDG) adjacent to the Chesapeake Bay.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 33.882 km away, between 2023-08-15 14:25:00 and 2023-08-15 14:55:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Lines of thunderstorms developed along a stalling cold front resulting in gusty winds and a waterspout over the Chesapeake Bay and tidal Potomac River. Lines of thunderstorms developed along a stalling cold front resulting in gusty winds and a waterspout over the Chesapeake Bay and tidal Potomac River. Lines of thunderstorms developed along a stalling cold front resulting in gusty winds and a waterspout over the Chesapeake Bay and tidal Potomac River. Lines of thunderstorms developed along a stalling cold front resulting in gusty winds and a waterspout over the Chesapeake Bay and tidal Potomac River. Lines of thunderstorms developed along a stalling cold front resulting in gusty winds and a waterspout over the Chesapeake Bay and tidal Potomac River.\nEvent Narrative: A thunderstorm produced an estimated wind gust to 34 knots (39 MPH) near a Tempest station on River Bay Road adjacent to the Chesapeake Bay. Wind gusts of up to 35 knots (40 MPH) were measured by a Tempest station at Huntingfield Point adjacent to the tidal Chester River. Wind gusts of up to 38 knots (43 MPH) were measured by a personal weather station at Love Point (KMDSTEVE52) adjacent to the Chesapeake Bay and tidal Chester River. A thunderstorm produced an estimated wind gust to 34 knots (39 MPH) near a mesonet on the westbound span of the US-50/US-301 Chesapeake Bay Bridge (MD065). A thunderstorm produced an estimated wind gust to 34 knots (39 MPH) near the Thomas Point NOS sensor (TPLM2).", "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00093721, approximately 33.2836 km away, between 2023-09-07 13:35:00 and 2023-09-08 03:23:00. The events included records with hailstones measuring 36.416666666666664 inches.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 13000.0 and crop damage of 0.0. \n\nEpisode Narrative: Numerous showers and thunderstorms developed along a lee pressure trough after several days of late season heat. Several of these storms turned severe, producing both damaging wind gusts and large hail. Numerous showers and thunderstorms developed along a lee pressure trough after several days of late season heat. Several of these storms turned severe, producing both damaging wind gusts and large hail. Numerous showers and thunderstorms developed along a lee pressure trough after several days of late season heat. Several of these storms turned severe, producing both damaging wind gusts and large hail. Numerous showers and thunderstorms developed along a lee pressure trough after several days of late season heat. Several of these storms turned severe, producing both damaging wind gusts and large hail. Numerous showers and thunderstorms developed along a lee pressure trough after several days of late season heat. Several of these storms turned severe, producing both damaging wind gusts and large hail. Numerous showers and thunderstorms developed along a lee pressure trough after several days of late season heat. Several of these storms turned severe, producing both damaging wind gusts and large hail.\nEvent Narrative: Multiple trees blew down in the Severna Park area. Trees and wires blew down on MD-27 Ridge Road at Penn Shop Road. Trees blew down along Woodbine Road and White Rock Road. Hail of up to ping pong ball size was reported in the Mount Washington area of Baltimore City. Quarter size hail was reported in Towson. Trees blew down between Bynum and Bel Air, including near the intersection of High Point Road and MD-23 East-West Highway.", "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00093721, approximately 28.1791 km away, between 2023-09-08 18:29:00 and 2023-09-08 19:09:00. The events included records with hailstones measuring 41.75 inches.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 168000.0 and crop damage of 0.0. \n\nEpisode Narrative: An approaching cold front ignited scattered to numerous showers and strong to severe thunderstorms as it intersected an unseasonably hot and humid airmass. Several storms turned severe, with a few producing considerable wind damage and hail. An approaching cold front ignited scattered to numerous showers and strong to severe thunderstorms as it intersected an unseasonably hot and humid airmass. Several storms turned severe, with a few producing considerable wind damage and hail. An approaching cold front ignited scattered to numerous showers and strong to severe thunderstorms as it intersected an unseasonably hot and humid airmass. Several storms turned severe, with a few producing considerable wind damage and hail. An approaching cold front ignited scattered to numerous showers and strong to severe thunderstorms as it intersected an unseasonably hot and humid airmass. Several storms turned severe, with a few producing considerable wind damage and hail. An approaching cold front ignited scattered to numerous showers and strong to severe thunderstorms as it intersected an unseasonably hot and humid airmass. Several storms turned severe, with a few producing considerable wind damage and hail. An approaching cold front ignited scattered to numerous showers and strong to severe thunderstorms as it intersected an unseasonably hot and humid airmass. Several storms turned severe, with a few producing considerable wind damage and hail. An approaching cold front ignited scattered to numerous showers and strong to severe thunderstorms as it intersected an unseasonably hot and humid airmass. Several storms turned severe, with a few producing considerable wind damage and hail. An approaching cold front ignited scattered to numerous showers and strong to severe thunderstorms as it intersected an unseasonably hot and humid airmass. Several storms turned severe, with a few producing considerable wind damage and hail.\nEvent Narrative: Numerous trees blew down blocking MD-140 Reisterstown Road near Woodholme Avenue. There were multiple reports of trees blown down northwest of Cockeysville toward Butler. Multiple trees blew down on MD-144 Frederick Road and Fairgrounds Road. Trees blew down on eastbound I-70 Baltimore National Pike between mile markers 82.0 and 83.0. There were multiple reports of large hail around quarter size in West Friendship. A wind gust of 59 knots (68 MPH) was measured by a personal weather station near Randallstown (KMDWOODS5). Dozens of trees, wires, and large branches blew down in the Randallstown, Windsor Mill, and Woodlawn area. A roof caved in on the north side of Woodlawn. Quarter size hail was reported in Cockeysville.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 28.8433 km away, between 2023-09-08 22:13:00 and 2023-09-08 23:04:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: An approaching cold front ignited scattered to numerous showers and strong to severe thunderstorms as it intersected an unseasonably hot and humid airmass. Several storms produced strong winds over area waterways. An approaching cold front ignited scattered to numerous showers and strong to severe thunderstorms as it intersected an unseasonably hot and humid airmass. Several storms produced strong winds over area waterways. An approaching cold front ignited scattered to numerous showers and strong to severe thunderstorms as it intersected an unseasonably hot and humid airmass. Several storms produced strong winds over area waterways. An approaching cold front ignited scattered to numerous showers and strong to severe thunderstorms as it intersected an unseasonably hot and humid airmass. Several storms produced strong winds over area waterways.\nEvent Narrative: A thunderstorm produced an estimated wind gust to 34 knots (39 MPH) near a mesonet on the I-695 Francis Scott Key Bridge (MD120). Wind gusts of up to 36 knots (42 MPH) were measured by a mesonet on the westbound span of the US-50/US-301 Chesapeake Bay Bridge (MD065). Wind gusts of up to 42 knots (48 MPH) were measured by the Tolly Point WeatherFlow sensor (XTOL). A thunderstorm produced an estimated wind gust to 34 knots (39 MPH) near a mesonet on the eastbound span of the US-50/US-301 Chesapeake Bay Bridge (MD066).", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 36.0814 km away, between 2023-09-09 16:32:00 and 2023-09-09 16:49:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front stalling over the Mid-Atlantic ignited several thunderstorms that produced gusty winds over area waterways. A cold front stalling over the Mid-Atlantic ignited several thunderstorms that produced gusty winds over area waterways. A cold front stalling over the Mid-Atlantic ignited several thunderstorms that produced gusty winds over area waterways. A cold front stalling over the Mid-Atlantic ignited several thunderstorms that produced gusty winds over area waterways.\nEvent Narrative: A wind gust of 37 knots (43 MPH) was measured by the Thomas Point NOS sensor (TPLM2). A wind gust of 34 knots (39 MPH) was measured by the Kent Island WeatherFlow sensor (XKNT). A thunderstorm produced an estimated wind gust to 34 knots (39 MPH) near a mesonet on the westbound span of the US-50/US-301 Chesapeake Bay Bridge (MD065). Wind gusts of up to 35 knots (40 MPH) were measured by a mesonet on the eastbound span of the US-50/US-301 Chesapeake Bay Bridge (MD066).", "The following events were reported: Flash Flood, Flood. These occurred near station USW00093721, approximately 20.5625 km away, between 2023-09-12 22:00:00 and 2023-09-13 00:35:00. The flood was caused by Heavy Rain. Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 500000.0 and crop damage of 0.0. \n\nEpisode Narrative: A slow moving cold front moved into the area during the evening of the 12th into the overnight and early morning hours of the 13th. Moisture pooling ahead of the cold front caused instability to increase in addition to added atmospheric moisture. Showers and thunderstorms developed, and some trained over the same areas resulting in instances of flooding and flash flooding. Central and northeastern Maryland were the areas hardest hit, where moisture and instability was highest. A slow moving cold front moved into the area during the evening of the 12th into the overnight and early morning hours of the 13th. Moisture pooling ahead of the cold front caused instability to increase in addition to added atmospheric moisture. Showers and thunderstorms developed, and some trained over the same areas resulting in instances of flooding and flash flooding. Central and northeastern Maryland were the areas hardest hit, where moisture and instability was highest. A slow moving cold front moved into the area during the evening of the 12th into the overnight and early morning hours of the 13th. Moisture pooling ahead of the cold front caused instability to increase in addition to added atmospheric moisture. Showers and thunderstorms developed, and some trained over the same areas resulting in instances of flooding and flash flooding. Central and northeastern Maryland were the areas hardest hit, where moisture and instability was highest. A slow moving cold front moved into the area during the evening of the 12th into the overnight and early morning hours of the 13th. Moisture pooling ahead of the cold front caused instability to increase in addition to added atmospheric moisture. Showers and thunderstorms developed, and some trained over the same areas resulting in instances of flooding and flash flooding. Central and northeastern Maryland were the areas hardest hit, where moisture and instability was highest. A slow moving cold front moved into the area during the evening of the 12th into the overnight and early morning hours of the 13th. Moisture pooling ahead of the cold front caused instability to increase in addition to added atmospheric moisture. Showers and thunderstorms developed, and some trained over the same areas resulting in instances of flooding and flash flooding. Central and northeastern Maryland were the areas hardest hit, where moisture and instability was highest. A slow moving cold front moved into the area during the evening of the 12th into the overnight and early morning hours of the 13th. Moisture pooling ahead of the cold front caused instability to increase in addition to added atmospheric moisture. Showers and thunderstorms developed, and some trained over the same areas resulting in instances of flooding and flash flooding. Central and northeastern Maryland were the areas hardest hit, where moisture and instability was highest. A slow moving cold front moved into the area during the evening of the 12th into the overnight and early morning hours of the 13th. Moisture pooling ahead of the cold front caused instability to increase in addition to added atmospheric moisture. Showers and thunderstorms developed, and some trained over the same areas resulting in instances of flooding and flash flooding. Central and northeastern Maryland were the areas hardest hit, where moisture and instability was highest. A slow moving cold front moved into the area during the evening of the 12th into the overnight and early morning hours of the 13th. Moisture pooling ahead of the cold front caused instability to increase in addition to added atmospheric moisture. Showers and thunderstorms developed, and some trained over the same areas resulting in instances of flooding and flash flooding. Central and northeastern Maryland were the areas hardest hit, where moisture and instability was highest. A slow moving cold front moved into the area during the evening of the 12th into the overnight and early morning hours of the 13th. Moisture pooling ahead of the cold front caused instability to increase in addition to added atmospheric moisture. Showers and thunderstorms developed, and some trained over the same areas resulting in instances of flooding and flash flooding. Central and northeastern Maryland were the areas hardest hit, where moisture and instability was highest. A slow moving cold front moved into the area during the evening of the 12th into the overnight and early morning hours of the 13th. Moisture pooling ahead of the cold front caused instability to increase in addition to added atmospheric moisture. Showers and thunderstorms developed, and some trained over the same areas resulting in instances of flooding and flash flooding. Central and northeastern Maryland were the areas hardest hit, where moisture and instability was highest. A slow moving cold front moved into the area during the evening of the 12th into the overnight and early morning hours of the 13th. Moisture pooling ahead of the cold front caused instability to increase in addition to added atmospheric moisture. Showers and thunderstorms developed, and some trained over the same areas resulting in instances of flooding and flash flooding. Central and northeastern Maryland were the areas hardest hit, where moisture and instability was highest. A slow moving cold front moved into the area during the evening of the 12th into the overnight and early morning hours of the 13th. Moisture pooling ahead of the cold front caused instability to increase in addition to added atmospheric moisture. Showers and thunderstorms developed, and some trained over the same areas resulting in instances of flooding and flash flooding. Central and northeastern Maryland were the areas hardest hit, where moisture and instability was highest. A slow moving cold front moved into the area during the evening of the 12th into the overnight and early morning hours of the 13th. Moisture pooling ahead of the cold front caused instability to increase in addition to added atmospheric moisture. Showers and thunderstorms developed, and some trained over the same areas resulting in instances of flooding and flash flooding. Central and northeastern Maryland were the areas hardest hit, where moisture and instability was highest. A slow moving cold front moved into the area during the evening of the 12th into the overnight and early morning hours of the 13th. Moisture pooling ahead of the cold front caused instability to increase in addition to added atmospheric moisture. Showers and thunderstorms developed, and some trained over the same areas resulting in instances of flooding and flash flooding. Central and northeastern Maryland were the areas hardest hit, where moisture and instability was highest.\nEvent Narrative: Vehicles were stranded in high water along Wabash Avenue in northwest Baltimore City. Water was flowing at least wheel deep on the roads. The water level rapidly rose above the flood stage of 13 feet along Gwynns Falls at Washington Boulevard. At 13 feet, Beach drive is flooded in several places and both the Riley Springs Trailbridge and Rapids Footbridge are completely covered by water. Vehicles were stranded in high water in Arbutus due to flowing water. Vehicles were stranded in flowing high water in Pikesville. Occupied vehicles were in floodwater due to heavy rainfall. There were occupied vehicles stranded in floodwater at Loch Raven Boulevard. There were occupied vehicles in floodwater at the intersection of Oakleigh Road and Redwood Avenue. An occupied vehicle was stuck in flood water at Buckingham Road and Liberty Road. The water level rapidly rose above flood stage of 11 feet along the Whitemarsh Run at White Marsh. At 11 feet, water covers the parking lots near the stream, particularly near the Town Center Court. The water fell below flood stage at 12:55 AM EST. US 29 was closed at Fairland Road due to high water. Roads were closed due to flowing water around Essex. Flood waters entered businesses along Gladstone Avenue and Wyndhurst Avenue due to Stony Creek flowing out of its banks. The fire department reported dozens of water rescues around the city of Baltimore along with Jones Falls flowing out of its banks. The fire department reported dozens of water rescues around the city of Baltimore along with Jones Falls flowing out of its banks.", "The following events were reported: Marine Thunderstorm Wind. These occurred near station USW00093721, approximately 28.4249 km away, between 2023-09-12 22:20:00 and 2023-09-12 23:40:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front produced a few thunderstorms resulting in gusty winds over area waterways, especially over the northern Chesapeake Bay. A cold front produced a few thunderstorms resulting in gusty winds over area waterways, especially over the northern Chesapeake Bay. A cold front produced a few thunderstorms resulting in gusty winds over area waterways, especially over the northern Chesapeake Bay. A cold front produced a few thunderstorms resulting in gusty winds over area waterways, especially over the northern Chesapeake Bay. A cold front produced a few thunderstorms resulting in gusty winds over area waterways, especially over the northern Chesapeake Bay. A cold front produced a few thunderstorms resulting in gusty winds over area waterways, especially over the northern Chesapeake Bay. A cold front produced a few thunderstorms resulting in gusty winds over area waterways, especially over the northern Chesapeake Bay. A cold front produced a few thunderstorms resulting in gusty winds over area waterways, especially over the northern Chesapeake Bay. A cold front produced a few thunderstorms resulting in gusty winds over area waterways, especially over the northern Chesapeake Bay. A cold front produced a few thunderstorms resulting in gusty winds over area waterways, especially over the northern Chesapeake Bay. A cold front produced a few thunderstorms resulting in gusty winds over area waterways, especially over the northern Chesapeake Bay. A cold front produced a few thunderstorms resulting in gusty winds over area waterways, especially over the northern Chesapeake Bay. A cold front produced a few thunderstorms resulting in gusty winds over area waterways, especially over the northern Chesapeake Bay. A cold front produced a few thunderstorms resulting in gusty winds over area waterways, especially over the northern Chesapeake Bay. A cold front produced a few thunderstorms resulting in gusty winds over area waterways, especially over the northern Chesapeake Bay. A cold front produced a few thunderstorms resulting in gusty winds over area waterways, especially over the northern Chesapeake Bay. A cold front produced a few thunderstorms resulting in gusty winds over area waterways, especially over the northern Chesapeake Bay. A cold front produced a few thunderstorms resulting in gusty winds over area waterways, especially over the northern Chesapeake Bay. A cold front produced a few thunderstorms resulting in gusty winds over area waterways, especially over the northern Chesapeake Bay. A cold front produced a few thunderstorms resulting in gusty winds over area waterways, especially over the northern Chesapeake Bay.\nEvent Narrative: A wind gust of 35 knots (40 MPH) was measured by a Tempest station on Todd Point Lane adjacent to the Chesapeake Bay. A thunderstorm produced an estimated wind gust to 34 knots (39 MPH) near a Tempest station on Race Street adjacent to the tidal Patapsco River. A wind gust of 37 knots (43 MPH) was measured by a mesonet at the Maryland Science Center (BLMRE) adjacent to the tidal Patapsco River. A wind gust of 40 knots (46 MPH) was measured by a Tempest station on South Eaton Street adjacent to the tidal Patapsco River. A wind gust of 37 knots (43 MPH) was measured by the Thomas Point NOS sensor (TPLM2). A wind gust of 38 knots (44 MPH) was measured by a personal weather station on East Randall Street (KMDBALTI365) adjacent to the tidal Patapsco River. Wind gusts of up to 40 knots (46 MPH) were measured by a Tempest station on East Randall Street adjacent to the tidal Patapsco River. A thunderstorm produced an estimated wind gust to 34 knots (39 MPH) near the Kent Island WeatherFlow sensor (XKNT). A wind gust of 34 knots (39 MPH) was measured by a Tempest station on South Ann Street adjacent to the tidal Patapsco River. A thunderstorm produced an estimated wind gust to 34 knots (39 MPH) near a Tempest station on Beach Side Drive adjacent to the Chesapeake Bay. A wind gust of 40 knots (46 MPH) was measured by a Tempest station on Todd Point Lane adjacent to the Chesapeake Bay. Wind gusts of up to 39 knots (45 MPH) were measured by a personal weather station at Bowleys Marina House (KMDMIDDL129) adjacent to the Chesapeake Bay. Wind gusts of up to 39 knots (45 MPH) were measured by a personal weather station at Bowleys Quarters Fuel Dock (KMDMIDDL42) adjacent to the Chesapeake Bay. A thunderstorm produced an estimated wind gust to 34 knots (39 MPH) near a mesonet on the eastbound span of the US-50/US-301 Chesapeake Bay Bridge (MD066). Wind gusts of up to 45 knots (52 MPH) were measured by a personal weather station at Marling Farms (KMDCHEST20) adjacent to Eastern Bay. A thunderstorm produced an estimated wind gust to 34 knots (39 MPH) near the Patapsco CBIBS sensor (44043). A thunderstorm produced estimated wind gusts to 34 knots (39 MPH) near the Hart Miller WeatherFlow sensor (XHRT). A thunderstorm produced an estimated wind gust to 34 knots (39 MPH) near a personal weather station between Kent Narrows and Grasonville (KMDGRASO34) adjacent to the tidal Chester River and Eastern Bay. A wind gust of 45 knots (52 MPH) was measured by a mesonet at Crab Alley Bay adjacent to Eastern Bay. A wind gust of 35 knots (40 MPH) was measured by a Tempest station at Huntingfield Point.", "The following events were reported: Thunderstorm Wind. These occurred near station USW00093721, approximately 30.781 km away, between 2023-09-12 23:00:00 and 2023-09-12 23:08:00.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 10000.0 and crop damage of 0.0. \n\nEpisode Narrative: A cold front produced a few severe thunderstorms generally near and east of I-95 in Maryland. A cold front produced a few severe thunderstorms generally near and east of I-95 in Maryland.\nEvent Narrative: Several large trees, branches, and wires blew down at the intersection of Ebenezer Road and Meyers Lane. A wind gust of 54 knots (62 MPH) was measured by the AWOS at Martin State Airport (KMTN).", "The following events were reported: Flood. These occurred near station USW00093721, approximately 25.1962 km away, between 2023-12-18 00:50:00 and 2023-12-18 10:15:00. The flood was caused by Heavy Rain. Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: An area of low pressure moved along the Atlantic seaboard bringing widespread rainfall amounts of 1.5 to 4 inches. This resulted in numerous creeks, streams, and rivers reaching minor to moderate flood stage. Numerous roads were closed in areas as well. An area of low pressure moved along the Atlantic seaboard bringing widespread rainfall amounts of 1.5 to 4 inches. This resulted in numerous creeks, streams, and rivers reaching minor to moderate flood stage. Numerous roads were closed in areas as well. An area of low pressure moved along the Atlantic seaboard bringing widespread rainfall amounts of 1.5 to 4 inches. This resulted in numerous creeks, streams, and rivers reaching minor to moderate flood stage. Numerous roads were closed in areas as well.\nEvent Narrative: Beaverdam Run at Cockeysville hit minor flood stage (1:00 AM) and crested at 9.62 feet before coming below minor flood stage by 4:45 AM. Portions of Upper Glencoe Road and Lower Glencoe Road were flooded. Little Patuxent River in Howard County reached minor flooding at 1:40 AM, eventually cresting at 12.27 feet before falling below minor flood stage around 10:15 AM. Hawlings River flooded on Brighton Dam Road resulting in road closure and 1 water rescue.", "The following events were reported: Flood. These occurred near station USW00093721, approximately 43.7218 km away, between 2023-12-28 00:15:00 and 2023-12-28 04:15:00. The flood was caused by Heavy Rain. Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: An area of low pressure moved along the Atlantic seaboard bringing widespread rainfall amounts of 1.5 to 2.5 inches. This resulted in a few road closures.\nEvent Narrative: Vehicle stuck in floodwaters on Winters Run Road. Road has also been closed due to high water." ] }