diff --git "a/news_USW00013722.json" "b/news_USW00013722.json"
new file mode 100644--- /dev/null
+++ "b/news_USW00013722.json"
@@ -0,0 +1,1667 @@
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+        "2020-07-24 18:20:00",
+        "2020-07-28 16:35:00",
+        "2020-08-01 15:44:00",
+        "2020-08-04 09:49:00",
+        "2020-08-06 14:51:00",
+        "2020-08-14 21:30:00",
+        "2020-08-15 18:15:00",
+        "2020-08-31 23:59:00",
+        "2020-09-01 13:42:00",
+        "2020-09-25 19:25:00",
+        "2020-11-12 18:05:00",
+        "2020-12-24 21:09:00",
+        "2021-03-18 17:10:00",
+        "2021-03-27 17:09:00",
+        "2021-03-28 13:56:00",
+        "2021-04-09 16:13:00",
+        "2021-05-04 15:10:00",
+        "2021-05-07 13:24:00",
+        "2021-05-10 16:20:00",
+        "2021-05-29 17:36:00",
+        "2021-07-01 21:45:00",
+        "2021-07-08 16:32:00",
+        "2021-07-09 17:00:00",
+        "2021-07-17 21:13:00",
+        "2021-07-28 13:58:00",
+        "2021-08-01 06:28:00",
+        "2021-08-14 14:48:00",
+        "2021-08-20 19:28:00",
+        "2021-09-08 10:40:00",
+        "2021-09-09 13:15:00",
+        "2021-10-09 12:30:00",
+        "2021-10-25 20:12:00",
+        "2022-01-03 10:37:00",
+        "2022-03-07 20:55:00",
+        "2022-03-17 09:15:00",
+        "2022-03-31 14:50:00",
+        "2022-04-07 16:39:00",
+        "2022-04-26 15:15:00",
+        "2022-05-01 17:20:00",
+        "2022-05-03 15:14:00",
+        "2022-05-06 19:40:00",
+        "2022-05-07 17:31:00",
+        "2022-05-16 17:30:00",
+        "2022-05-19 23:48:00",
+        "2022-05-21 16:59:00",
+        "2022-05-22 17:12:00",
+        "2022-05-24 01:00:00",
+        "2022-05-27 18:00:00",
+        "2022-06-08 18:12:00",
+        "2022-06-16 16:52:00",
+        "2022-06-17 17:43:00",
+        "2022-07-05 18:05:00",
+        "2022-07-06 20:55:00",
+        "2022-07-07 18:26:00",
+        "2022-07-09 20:52:00",
+        "2022-07-13 22:12:00",
+        "2022-07-15 18:45:00",
+        "2022-07-16 14:49:00",
+        "2022-07-21 14:40:00",
+        "2022-07-24 16:07:00",
+        "2022-07-25 20:42:00",
+        "2022-07-26 14:17:00",
+        "2022-07-27 17:45:00",
+        "2022-07-29 19:34:00",
+        "2022-08-10 16:17:00",
+        "2022-08-11 18:20:00",
+        "2022-09-10 20:30:00",
+        "2022-09-12 18:39:00",
+        "2022-09-30 22:00:00",
+        "2022-10-17 17:46:00",
+        "2023-01-12 21:40:00",
+        "2023-03-02 04:51:00",
+        "2023-04-07 19:30:00",
+        "2023-04-14 15:22:00",
+        "2023-04-22 09:28:00",
+        "2023-04-30 14:35:00",
+        "2023-05-16 23:10:00",
+        "2023-06-16 16:46:00",
+        "2023-06-19 14:20:00",
+        "2023-06-23 19:00:00",
+        "2023-06-26 21:45:00",
+        "2023-06-30 23:59:00",
+        "2023-07-01 16:44:00",
+        "2023-07-05 13:34:00",
+        "2023-07-07 18:20:00",
+        "2023-07-08 17:50:00",
+        "2023-07-09 14:54:00",
+        "2023-07-14 07:30:00",
+        "2023-08-07 18:57:00",
+        "2023-08-15 16:25:00",
+        "2023-08-27 19:10:00",
+        "2023-08-29 20:15:00",
+        "2023-09-08 15:53:00",
+        "2023-09-09 16:10:00",
+        "2023-09-23 17:00:00",
+        "2023-12-10 15:38:00",
+        "2023-12-17 21:30:00"
+    ],
+    "NEWS": [
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 23.5615 km away, between 2003-02-22 12:10:00 and 2003-02-22 12:30:00. 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:   \nEvent Narrative: Numerous trees were blown down, some blocking roads. Trees were blown down. Trees were blown down.",
+        "The following events were reported: Hail. These occurred near station USW00013722, approximately 18.1137 km away, between 2003-04-26 17:40:00 and 2003-04-26 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:  \nEvent Narrative:",
+        "The following events were reported: Hail. These occurred near station USW00013722, approximately 38.4401 km away, between 2003-04-30 16:50:00 and 2003-04-30 16:50:00. 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: \nEvent Narrative:",
+        "The following events were reported: Hail. These occurred near station USW00013722, approximately 47.4002 km away, between 2003-05-10 18:20:00 and 2003-05-10 18:20:00. 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: \nEvent Narrative:",
+        "The following events were reported: Hail. These occurred near station USW00013722, approximately 46.713 km away, between 2003-07-09 18:58:00 and 2003-07-09 18:58:00. 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: \nEvent Narrative:",
+        "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00013722, approximately 36.7125 km away, between 2003-07-10 16:35:00 and 2003-07-10 17:45:00. The events included records with hailstones measuring 37.9375 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative:    \nEvent Narrative: Trees were blown down near New Hope Church Road and Headingham Blvd. Tobacco fields were damaged by large hail. Trees were blown down between Central Harnett High School and the Wake County line. Several trees were blown down.",
+        "The following events were reported: Hail. These occurred near station USW00013722, approximately 39.1678 km away, between 2003-07-18 21:15:00 and 2003-07-18 21:15:00. 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: \nEvent Narrative:",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 25.7924 km away, between 2003-07-22 18:40:00 and 2003-07-22 18:40:00. 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: \nEvent Narrative: Trees were blown down.",
+        "The following events were reported: Hail. These occurred near station USW00013722, approximately 39.1678 km away, between 2003-08-18 15:30:00 and 2003-08-18 15:30:00. 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: \nEvent Narrative:",
+        "The following events were reported: Hail. These occurred near station USW00013722, approximately 12.6857 km away, between 2003-08-22 13:54:00 and 2003-08-22 13:54:00. 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: \nEvent Narrative:",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 29.783 km away, between 2003-10-14 20:50:00 and 2003-10-14 21:44:00. 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:  \nEvent Narrative: Trees were blown down at the intersection of Highways 56 and 96. Several trees were blown down, some across roads.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 37.0943 km away, between 2003-11-19 11:08:00 and 2003-11-19 11:08:00. 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: \nEvent Narrative: Two trees were blown down onto powerlines along Highway 57 in Caldwell.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 14.5938 km away, between 2004-03-07 20:25:00 and 2004-03-07 20:25:00. The events included records with estimated wind gusts of 60.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: .\nEvent Narrative: Numerous trees and power lines were blown down on Yates Mill Road.",
+        "The following events were reported: Hail. These occurred near station USW00013722, approximately 24.4617 km away, between 2004-03-31 16:55:00 and 2004-03-31 20:50:00. 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:   \nEvent Narrative:",
+        "The following events were reported: Tornado. These occurred near station USW00013722, approximately 44.2774 km away, between 2004-05-02 16:15:00 and 2004-05-02 16:18:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: \nEvent Narrative: A tornado produced damage from Jackson Road to Christian Light Road to Cokesbury Road. Three homes had roof damage, and a tree fell on a mobile home. Several sheds and vehicles were also damaged. About 3 dozen large trees were blown down or snapped.",
+        "The following events were reported: Hail. These occurred near station USW00013722, approximately 29.5113 km away, between 2004-05-19 17:55:00 and 2004-05-19 17:55:00. 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: \nEvent Narrative:",
+        "The following events were reported: Hail. These occurred near station USW00013722, approximately 41.1278 km away, between 2004-05-23 17:00:00 and 2004-05-23 17:00:00. 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: \nEvent Narrative:",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 43.8573 km away, between 2004-06-04 13:00:00 and 2004-06-04 13:00:00. The events included records with estimated wind gusts of 60.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: \nEvent Narrative: Trees were blown down, shingles were blown off a roof, and a tin roof was blown off a car port near Highway 401.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 40.7556 km away, between 2004-06-10 19:10:00 and 2004-06-10 19:10:00. 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: \nEvent Narrative: Trees were blown down, one across Moncure-Pittsboro Road.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 30.0988 km away, between 2004-06-11 19:40:00 and 2004-06-11 21:10:00. 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:      \nEvent Narrative: Trees were blown down on Coal Mill Road and Sparger Road. Trees were blown across roads in the southern portion of the county. Trees were blown down on Highway 98. Trees were blown down on Rock Quarry Road and Jones Sausage Road. A barn was damaged, some homes had molding blown off, and trees were blown down. Trees were blown down on Brookhollow Road.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 46.1371 km away, between 2004-06-23 15:35:00 and 2004-06-23 15:35:00. 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: \nEvent Narrative: Trees were blown down along Highway 561.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 24.5557 km away, between 2004-07-12 18:04:00 and 2004-07-12 18:04:00. 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: \nEvent Narrative: Trees were blown down at the intersection of Timber and Woodland Roads.",
+        "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00013722, approximately 22.1952 km away, between 2004-07-14 20:00:00 and 2004-07-14 21:20:00. The events included records with hailstones measuring 17.293333333333333 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative:   \nEvent Narrative:  Trees were blown down.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 23.9026 km away, between 2004-07-29 16:45:00 and 2004-07-29 16:45:00. The events included records with estimated wind gusts of 60.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: \nEvent Narrative: Powerlines were blown down, a garage was destroyed, and a couple of cars were damaged along the 6700 block of Poole Road.",
+        "The following events were reported: Hail. These occurred near station USW00013722, approximately 34.3836 km away, between 2004-08-05 21:15:00 and 2004-08-05 21:15:00. 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: \nEvent Narrative:",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 14.5938 km away, between 2004-08-13 18:30:00 and 2004-08-13 18:30:00. 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: \nEvent Narrative: Trees were blown down on Glenwood Avenue.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 38.3856 km away, between 2004-08-17 18:30:00 and 2004-08-17 18:30:00. 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: \nEvent Narrative: Trees were blown down on the Highway 70 connector near Interstate 85.",
+        "The following events were reported: Flash Flood. These occurred near station USW00013722, approximately 27.8938 km away, between 2004-09-08 07:45:00 and 2004-09-08 12:00:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: \nEvent Narrative: Over 38 roads, mostly secondary and rural, had to be closed due to high water across the county.  A one-mile stretch of Meltonville Church Road was under three to four feet of water.  Some schools, including Wadesboro Elementary, sustained minor flood damage.  Brown Creek and Lanes Creek both overflowed their banks and flooded nearby roads.",
+        "The following events were reported: Thunderstorm Wind, Tornado. These occurred near station USW00013722, approximately 28.0902 km away, between 2004-09-17 11:55:00 and 2004-09-17 15:15:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative:       \nEvent Narrative: A tornado touched down briefly near Vass, blowing down trees and snapping power poles. A tornado touched down briefly on the west side of Pittsboro, blowing down several trees, which in turn knocked down several power lines. Trees were blown down north of Hillsborough on Keiger Road and McDades Road. Two trees were blown down. Trees were blown down in downtown Raleigh. Five small planes at the Raleigh-Durham Airport were damaged, with four of them sustaining significant damage.  The airport itself sustained structural damage, with parts of a roof blown off.  Several cars were damaged and several light poles were blown over.  Wind damage was reported along a line from Terminal A to Terminal C. Trees were blown down.",
+        "The following events were reported: Thunderstorm Wind, Tornado. These occurred near station USW00013722, approximately 17.9832 km away, between 2004-09-27 18:30:00 and 2004-09-28 04:20:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative:  \nEvent Narrative: Straight-line winds near Interstate 85 and Club Boulevard downed trees and blew over a fence along the back lot of the Starlight Drive-In.  One of the panels from the fence blew through a double-pane window at a residence across the street.  Minor roof damage, mostly missing shingles, occurred a other residences along the same block. A tornado touched down near the intersection of Holly Springs Road and Kildaire Farm Road.  Minor property damage occurred to a few mobile homes, and a few trees and power lines were blown down.  The tornado lifted briefly, and then touched down again on the north side of Apex were several large trees were blown down, especially near the intersection of Schiefflin Road and James road, and along Culvert Street.",
+        "The following events were reported: Hail. These occurred near station USW00013722, approximately 18.4041 km away, between 2004-10-03 21:45:00 and 2004-10-03 21:45:00. 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: \nEvent Narrative: Nickel sized hail was reported on Interstate 40 at Exit 278.",
+        "The following events were reported: Hail. These occurred near station USW00013722, approximately 48.0705 km away, between 2004-12-10 00:45:00 and 2004-12-10 00:45:00. 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: \nEvent Narrative:",
+        "The following events were reported: Thunderstorm Wind, Tornado. These occurred near station USW00013722, approximately 28.5517 km away, between 2005-01-14 04:15:00 and 2005-01-14 05:32:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative:    \nEvent Narrative: A large tree, approximately three feet in diameter, fell on a home in Cary off of Southeast Maynard Road. Scattered trees were blown down across the county. A tornado touched down in northeast Hillsborough along St. Mary's Road and damaged two properties.  The east wall of a home was almost completely blown out, and on an adjacent property a metal equipment shed was destroyed with some of the debris carried into nearby trees.  A small outbuilding was pushed a short distance off its foundation as well. A couple of small trees were blown down in northwest Durham near Interstate 85.",
+        "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00013722, approximately 29.9168 km away, between 2005-03-08 08:55:00 and 2005-03-08 10:00:00. The events included records with hailstones measuring 42.35 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative:     \nEvent Narrative:  A utility building was blown away in town.  Large trees were blown down on Ten Ten Road.  Homes were damaged in the Fairview area, north of Fuquay-Varina, with widespread reports of trees down and power outages.  Six to eight homes were damaged just southwest of Garner, with large pine and oak trees on houses.  Numerous trees were blown down on Senter Farm Road. Trees and power lines were blown down just west of Youngsville, on  Halifax Road, Pearces Road, and Ferrels Bridge Road. A tree fell through a mobile home on NC 231.  Near Knightdale, several large limbs were blown down. Trees and power lines were blown down on Shotwell Road near US 70.  A tree also fell on a house along Shotwell Road.  A barn was blown down and equipment was damaged on Cornwallis Road.  The old Champion building sustained roof damage.",
+        "The following events were reported: Hail. These occurred near station USW00013722, approximately 25.7536 km away, between 2005-03-28 07:10:00 and 2005-03-28 07:40:00. The events included records with hailstones measuring 1.97 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative:    \nEvent Narrative: 3.5 to 4 inch elongated hail reported at I-540 and Falls of Neuse Road.  3 inch hail reported at Strickland and Falls of Neuse Roads.  2 inch hail reported in Five Points.  Golf ball sized hail reported at Cameron Village, Atlantic and New Hope Church Roads, North Raleigh Community Hospital, Green and Lee Spring Roads, and Durant and Falls of Neuse Roads.  Ping pong ball sized hail reported on Wake Forest Road.  Quarter to half dollar sized hail reported on Highwoods Road. Hen egg sized hail reported on Lake Wheeler Road.  Quarter to half dollar sized hail reported in Fuquay Varina and at Highways 401 and 70 in Garner.",
+        "The following events were reported: Hail. These occurred near station USW00013722, approximately 15.8057 km away, between 2005-05-12 17:12:00 and 2005-05-12 17:12:00. 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: \nEvent Narrative: Reported at Interstate 440 and US 1 North.",
+        "The following events were reported: Hail. These occurred near station USW00013722, approximately 41.9065 km away, between 2005-05-19 14:05:00 and 2005-05-19 14:05:00. 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: \nEvent Narrative: Penny sized hail reported at exit 157 along Interstate 40.",
+        "The following events were reported: Flash Flood, Hail, Thunderstorm Wind. These occurred near station USW00013722, approximately 20.5019 km away, between 2005-06-07 14:35:00 and 2005-06-07 17:30:00. The events included records with hailstones measuring 35.964285714285715 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative:         \nEvent Narrative: One and a half feet of water covered the intersection of Falls of the Neuse and Spring Forest Roads.  The flood waters floated an SUV. Trees were blown down. Quarter sized hail was reported at the intersection of Sandy Forks and Falls of the Neuse Roads.  Numerous reports of dime sized hail elsewhere in Raleigh. Trees were blown down on power lines on Highway 55 and Carpenter Road. Five power poles were blown down with the wires still live, trapping thirteen people in eight different vehicles at Blue Ridge Road and Wade Avenue. Several inches of water covered the intersection of Falls of the Neuse and Spring Forest Roads.  Flood waters floated another vehicle, which blocked the intersection.  1.3 inches of rain fell in 20 minutes at Edwards Mill Road and Laurel Drive. Trees were blown down. Penny sized hail reported at the Durham Correctional Center. Trees were blown down near US Highway 1",
+        "The following events were reported: Flood. These occurred near station USW00013722, approximately 22.5798 km away, between 2005-06-12 17:30:00 and 2005-06-13 05:00:00. 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: Persistent, widespread heavy rain showers associated with moisture from tropical storm Arlene resulted in flooding across the southern mountains. County reported the Tuckaseegee was out of its banks in several locations, with several roads closed, including Shook Cove Rd, Dillard Rd, and North & South River Rd. As water was released from various dams along the river, the flooding persisted well after heavy rain ended across the area.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 39.6872 km away, between 2005-06-27 18:00:00 and 2005-06-27 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: \nEvent Narrative: Trees were blown down.",
+        "The following events were reported: Thunderstorm Wind, Tornado. These occurred near station USW00013722, approximately 29.2212 km away, between 2005-07-07 18:45:00 and 2005-07-07 20:10:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative:    \nEvent Narrative: A tornado touched down in Swann near the Harnett-Lee County Line. Several trees were blown down and twisted, and a few shingles were blown off of houses.  The tornado lifted and touched down intermittently as it traveled northeast, causing minor tree damage.  The tornado lifted after touching down a final time in Cokesbury. Trees were blown down on Old Smithfield Road. Trees were blown down. Several trees were blown down at Jordan Lake just north of US Highway 64.",
+        "The following events were reported: Hail. These occurred near station USW00013722, approximately 24.5557 km away, between 2005-07-13 15:55:00 and 2005-07-13 15:55:00. 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: \nEvent Narrative: Quarter size hail was reported at the corner of Aversboro and Timber Drives.",
+        "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00013722, approximately 27.5444 km away, between 2005-07-28 18:46:00 and 2005-07-28 21:35:00. The events included records with hailstones measuring 35.85 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative:          \nEvent Narrative: There were numerous reports of hail around the Pittsboro area.  Quarter size hail was reported at the intersection of Highways 902 and 87.  Several reports of dime to penny size hail were received as well. Numerous trees and powerlines were blown down along U.S. 15-501 near the Orange County line. Numerous trees were blown down on US Highway 64 East and Old Milburnie Road near the Neuse River. A trained spotter measured a 60 mph gust at Ten-Ten and Holland Church Roads as the gust front passed.  A gust of 57 mph was measured two minutes later.  Golfball size hail was reported in Research Triangle Park. Several large limbs were blown down on Highway 54 south of Durham.  Residents had to use chainsaws to cut the limbs in order to get out of their driveways. Trees were blown down. Trees were blown down. Trees were blown down in Clayton, and minor damage was sustained to a pickup truck.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 32.1485 km away, between 2005-08-05 15:55:00 and 2005-08-05 15:55:00. 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: \nEvent Narrative: Trees were blown down on Interstate 85 near mile marker 170.  Trees were also blown down north of the interstate on Willet Road.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 35.7495 km away, between 2005-09-20 20:15:00 and 2005-09-20 20:15:00. 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: \nEvent Narrative: Trees down on Hanks Chapel Road.",
+        "The following events were reported: Hail. These occurred near station USW00013722, approximately 34.7527 km away, between 2005-10-21 19:22:00 and 2005-10-21 19:22:00. 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: \nEvent Narrative:",
+        "The following events were reported: Hail. These occurred near station USW00013722, approximately 41.2902 km away, between 2005-10-21 19:28:00 and 2005-10-21 19:28:00. 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: \nEvent Narrative:",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 41.1278 km away, between 2006-01-13 23:00:00 and 2006-01-13 23:00:00. The events included records with estimated wind gusts of 60.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: \nEvent Narrative: Several trees down near Pittsboro at 1100 pm on River road and Hamlets Chapel Road.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 49.7626 km away, between 2006-01-13 23:00:00 and 2006-01-13 23:00:00. 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: 3 CHICKEN HOUSES DESTROYED.\nEvent Narrative:",
+        "The following events were reported: Hail. These occurred near station USW00013722, approximately 41.1278 km away, between 2006-04-03 08:15:00 and 2006-04-03 08:15:00. 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: \nEvent Narrative: Penny hail reported at intersection of Silk Hope and Gum Springs.",
+        "The following events were reported: Hail. These occurred near station USW00013722, approximately 19.4144 km away, between 2006-04-03 08:58:00 and 2006-04-03 08:58:00. 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: \nEvent Narrative: Penny size hail at intersection of of Buffalo and Forestville Road.",
+        "The following events were reported: Hail. These occurred near station USW00013722, approximately 28.522 km away, between 2006-04-03 09:19:00 and 2006-04-03 09:19:00. 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: \nEvent Narrative: Nickel size hail reported by highway 96.",
+        "The following events were reported: Hail. These occurred near station USW00013722, approximately 37.913 km away, between 2006-04-03 09:20:00 and 2006-04-03 09:20:00. 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: \nEvent Narrative: Penny size hail reported on highway 64 bypass at rolesville road exit.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 25.7924 km away, between 2006-04-03 18:21:00 and 2006-04-03 18:21:00. 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: \nEvent Narrative: TREES DOWN ALL ACROSS ORANGE COUNTY.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 17.622 km away, between 2006-04-03 18:30:00 and 2006-04-03 18:30:00. 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: \nEvent Narrative: TIN ROOFS TORN OFF A CARPORT AND BARN AND BLOWN 1000 TO 1500 FEET DOWNWIND. WELL HOUSE KNOCKED DOWN AND SHINGLES TORN OFF A HOME ON SHAW ROAD.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 49.1987 km away, between 2006-04-03 18:55:00 and 2006-04-03 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: \nEvent Narrative:",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 28.522 km away, between 2006-04-03 18:55:00 and 2006-04-03 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: \nEvent Narrative: ROLESVILLE POLICE OFFICER'S CAR ALMOST BLOWN OFF THE ROAD.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 25.3825 km away, between 2006-04-03 18:55:00 and 2006-04-03 18:55:00. 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: \nEvent Narrative:",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 21.819 km away, between 2006-04-03 18:57:00 and 2006-04-03 18:57:00. 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: \nEvent Narrative: TREE DOWN AND TREE LIMBS 4 TO 5 INCHES IN DIAMETER.",
+        "The following events were reported: Hail. These occurred near station USW00013722, approximately 36.8632 km away, between 2006-04-08 08:05:00 and 2006-04-08 08:05:00. The events included records with hailstones measuring 1.75 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: \nEvent Narrative: HIGHWAY 70 AT ORANGE HIGH SCHOOL.",
+        "The following events were reported: Hail. These occurred near station USW00013722, approximately 18.4041 km away, between 2006-04-08 08:12:00 and 2006-04-08 08:12:00. 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: \nEvent Narrative:",
+        "The following events were reported: Hail. These occurred near station USW00013722, approximately 31.8535 km away, between 2006-04-08 08:17:00 and 2006-04-08 08:17:00. 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: \nEvent Narrative: NORTHERN HIGH SCHOOL ON TOM WILKINSON ROAD.",
+        "The following events were reported: Hail. These occurred near station USW00013722, approximately 34.7246 km away, between 2006-04-08 08:30:00 and 2006-04-08 08:30:00. 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: \nEvent Narrative:",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 12.2152 km away, between 2006-04-17 14:25:00 and 2006-04-17 14:30:00. 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: \nEvent Narrative: TREE DOWN ON POWERLINES ON TRENTON ROAD.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 27.3987 km away, between 2006-04-17 14:35:00 and 2006-04-17 14:36:00. 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:  \nEvent Narrative: TREE DOWN ON POWERLINES AT 606 CURTIS DRIVE. TREE DOWN ON POWERLINES AT THE INTERSECTION OF WAGSTAFF AND PINEY GROVE WILBON ROAD.",
+        "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00013722, approximately 23.5426 km away, between 2006-04-22 11:30:00 and 2006-04-22 11:55:00. The events included records with hailstones measuring 33.82 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative:         \nEvent Narrative: TREES DOWN AT INTERSTATE 40 AND HARRISON AVE. EXIT. ONE TREE BLOCKED EASTBOUND ROAD RAMP. TREE DOWN ON POWER LINES AT INTERSECTION OF KENNEBEC AND HILLTOP ROADS. TREE DOWN ON POWER LINES AT THE BELTLINE AND POOLE ROAD. TREES DOWN NEAR JUNCTION OF HWY 50 AND HWY 42. QUARTER TO GOLF BALL SIZE HAIL REPORTED ON HWY 70 NEAR THE WHITE OAK SHOPPING CENTER. TREE LIMBS DOWN. TREE DOWN ON POWER LINES AT INTERSECTION OF STEWART ST. AND CARDINAL DR. NICKEL SIZE HAIL REPORTED BETWEEN I-540 AND EXIT 287 ON I-40. GOLF BALL SIZE HAIL AT THE INTERSECTION OF NEW BERN AND NEW HOPE ROAD.",
+        "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00013722, approximately 28.0115 km away, between 2006-04-22 12:05:00 and 2006-04-22 12:30:00. The events included records with hailstones measuring 37.72 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative:    \nEvent Narrative:  30 FT. MATURE TREE UPROOTED. SHINGLES AND GUTTER RIPPED OFF HOUSE NEAR MAGNOLIA RIDGE SUBDIVISION. SEVERAL TREES DOWN AND ROOF DAMAGE REPORTED NEAR THE INTERSECTION OF PEACH ORCHARD ROAD AND MAYS CROSSROADS ROAD. TREE DOWN ON POWER LINES AT LITCHFORD AND HARPS MILL ROAD.",
+        "The following events were reported: Hail. These occurred near station USW00013722, approximately 49.1987 km away, between 2006-04-22 12:20:00 and 2006-04-22 12:20:00. 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: \nEvent Narrative:",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 32.4448 km away, between 2006-04-25 20:50:00 and 2006-04-25 21:55:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative:        \nEvent Narrative: TREES DOWN. TREES DOWN ON US 1 NEAR THE CHATHAM AND LEE COUNTY LINE.  TREE DOWN ON HOLLY SPRING ROAD. THREE TREES DOWN AND ONE TREE DOWN ON HOUSE AT 204 MIDDLECREST DR. TREE DOWN BLOCKING HOLLY SPRINGS ROAD AT SUNSET RIDGE GOLF COURSE. 2 MILES SOUTH OF LAKE BENSON AT HOLLAND CHURCH RD. AND TEN TEN RD. TREES DOWN ON SEVEN PATHS RD.",
+        "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00013722, approximately 35.0005 km away, between 2006-05-14 13:45:00 and 2006-05-14 13:49:00. The events included records with hailstones measuring 17.375 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative:      \nEvent Narrative:   TREES DOWN NEAR THE INTERSECTION OF TEN TEN AND FANNY BROWN ROADS.  SEVERAL PINE TREES DOWN. REPORTED AT SUNSET LAKE ROAD.",
+        "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00013722, approximately 22.7254 km away, between 2006-05-14 13:55:00 and 2006-05-14 14:04:00. The events included records with hailstones measuring 6.666666666666667 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative:         \nEvent Narrative:  REPORTED AT PARK HAVEN LANE AND JOHNSTON STREET. REPORTED AT INTERSECTION OF TEN TEN AND BELLS LAKE ROAD. REPORTED NEAR HWY 401 AND WOODCREST ROAD. REPORTED AT SAUNDERS AND MAYWOOD STREET. TREE DOWN AT WAYNE NASH ROAD. REPORTED BETWEEN CREEDMOOR AND BUTNER AT HWY 56 AND ROGERS PLACE. REPORTED NEAR HWY 50.",
+        "The following events were reported: Hail. These occurred near station USW00013722, approximately 14.5938 km away, between 2006-05-14 14:07:00 and 2006-05-14 14:07:00. 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: \nEvent Narrative: REPORTED AT HODGE AND MINGO ROAD.",
+        "The following events were reported: Hail. These occurred near station USW00013722, approximately 29.5113 km away, between 2006-05-14 14:12:00 and 2006-05-14 14:12:00. The events included records with hailstones measuring 1.75 inches.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, Thunderstorm Wind. These occurred near station USW00013722, approximately 30.8983 km away, between 2006-05-14 14:40:00 and 2006-05-14 14:58:00. The events included records with hailstones measuring 13.345 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative:    \nEvent Narrative:  TREE DOWN ON A HOUSE WITH ROOF DAMAGE. REPORTED AT DUKE HOSPITAL.",
+        "The following events were reported: Hail. These occurred near station USW00013722, approximately 22.865 km away, between 2006-05-14 14:42:00 and 2006-05-14 14:42:00. 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: \nEvent Narrative:",
+        "The following events were reported: Hail. These occurred near station USW00013722, approximately 23.7894 km away, between 2006-05-14 15:15:00 and 2006-05-14 15:20:00. The events included records with hailstones measuring 0.9199999999999999 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative:   \nEvent Narrative: REPORTED IN WEST DURHAM NEAR DUKE HOSPITAL.",
+        "The following events were reported: Hail. These occurred near station USW00013722, approximately 31.108 km away, between 2006-05-14 16:20:00 and 2006-05-14 17:03:00. The events included records with hailstones measuring 1.21 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative:   \nEvent Narrative: REPORTED NEAR I-85 AND HWY 86. REPORTED ON CLUB BLVD. REPORTED ON HIGH ROCK ROAD NORTH OF EFLAND NEAR LEBENON CHRUCH ROAD.",
+        "The following events were reported: Tornado. These occurred near station USW00013722, approximately 17.8234 km away, between 2006-05-14 17:10:00 and 2006-05-14 17:10:00.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 USW00013722, approximately 21.4479 km away, between 2006-05-14 17:15:00 and 2006-05-14 17:28:00. The events included records with hailstones measuring 1.75 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative:   \nEvent Narrative: REPORTED NEAR THE INTERSECTION OF PURNELL AND NEW LIGHT ROAD. REPORTED AT ROLLING VIEW VARINA. REPORTED AT THE INTERSECTION OF STONEY HILL ROAD AND BUD MORRIS ROAD.",
+        "The following events were reported: Tornado. These occurred near station USW00013722, approximately 38.2929 km away, between 2006-05-14 17:43:00 and 2006-05-14 17:43:00.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, Thunderstorm Wind. These occurred near station USW00013722, approximately 15.4834 km away, between 2006-05-14 18:00:00 and 2006-05-14 18:04:00. The events included records with hailstones measuring 13.125 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative:    \nEvent Narrative: TREES DOWN NEAR BENNET.",
+        "The following events were reported: Hail. These occurred near station USW00013722, approximately 46.6936 km away, between 2006-05-14 19:20:00 and 2006-05-14 19:20:00. 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: \nEvent Narrative: HAIL IN COKESBURY.",
+        "The following events were reported: Hail. These occurred near station USW00013722, approximately 33.2574 km away, between 2006-05-15 21:45:00 and 2006-05-15 21:45:00. 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: \nEvent Narrative:",
+        "The following events were reported: Hail. These occurred near station USW00013722, approximately 12.2152 km away, between 2006-05-18 17:45:00 and 2006-05-18 17:45:00. 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: \nEvent Narrative:",
+        "The following events were reported: Hail. These occurred near station USW00013722, approximately 29.9178 km away, between 2006-05-18 17:50:00 and 2006-05-18 17:50:00. 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: \nEvent Narrative: REPORTED AT JORDAN LAKE.",
+        "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00013722, approximately 47.16 km away, between 2006-05-18 18:10:00 and 2006-05-18 18:41:00. The events included records with hailstones measuring 31.44 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative:  \nEvent Narrative: MEASURED WIND GUST OF 72 MPH AT THE JUNCTION OF HWY 210 AND I-40...EXIT 319 BY A SPOTTER WITH A WEATHER STATION.",
+        "The following events were reported: Hail. These occurred near station USW00013722, approximately 32.3952 km away, between 2006-05-20 18:59:00 and 2006-05-20 19:28:00. The events included records with hailstones measuring 1.0633333333333332 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative:      \nEvent Narrative: NEAR INTERSECTION OF OLD STAGE ROAD AND HWY 55. ALONG OLD STAGE ROAD. NEAR HOLLAND AND TEN TEN ROAD. NEAR JORDAN AND BRAT PENNY ROADS. REPORTED AT LAKE WHEELER AND ROUTE 401.",
+        "The following events were reported: Hail. These occurred near station USW00013722, approximately 38.8934 km away, between 2006-05-20 19:33:00 and 2006-05-20 19:35:00. 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:  \nEvent Narrative: REPORTED AT BARBOR MILL ROAD AND AMELIA CHURCH ROAD. NEAR 70 WEST AND SHOTWELL ROAD.",
+        "The following events were reported: Hail. These occurred near station USW00013722, approximately 39.1678 km away, between 2006-05-20 19:40:00 and 2006-05-20 19:40:00. 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: \nEvent Narrative: NEAR BOWLING ST. AND HWY 70.",
+        "The following events were reported: Hail. These occurred near station USW00013722, approximately 24.5557 km away, between 2006-05-20 21:23:00 and 2006-05-20 21:23:00. 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: \nEvent Narrative: REPORTED AT VITEX AND MALOS STREET.",
+        "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00013722, approximately 14.5114 km away, between 2006-05-25 16:25:00 and 2006-05-25 17:35:00. The events included records with hailstones measuring 25.4375 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative:    \nEvent Narrative:   TREES DOWN AT 7408 HARPSMILL ROAD IN NORTH RALEIGH. REPORTS OF SEVERAL TREES DOWN AT CARLTON AND PILGRIM DRIVE.",
+        "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00013722, approximately 13.171 km away, between 2006-05-25 17:38:00 and 2006-05-25 17:44:00. The events included records with hailstones measuring 33.625 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative:      \nEvent Narrative: POWER POLE AND LINES DOWN NEAR A PURE GAS STATION NEAR LOUISBURG ROAD SOUTH OF PERRY CREEK ROAD. PENNY SIZE HAIL AT GREENFIELD DRIVE. QUARTER SIZE HAIL AT FOX ROAD AND LOUISBURG ROAD. TREES DOWN NEAR FALLS OF THE NEUSE ROAD AND LITCHFORD ROAD. NUMEROUS TREES DOWN AT STRICKLAND ROAD AND FALLS OF THE NEUSE. SHINGLES OFF ROOF AT CHURCH OF CHRIST AND ACROSS THE STREET AT MT VERNON FALLS OF THE NEUSE CHURCH.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 10.4691 km away, between 2006-05-25 17:45:00 and 2006-05-25 17:45:00. 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: \nEvent Narrative: TREES AND POWER LINES DOWN ON HOUSE AT THE INTERSECTION OF CAPITAL BLVD. AND I-540.",
+        "The following events were reported: Hail. These occurred near station USW00013722, approximately 41.2902 km away, between 2006-05-26 18:45:00 and 2006-05-26 18:45:00. 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: \nEvent Narrative: PENNY SIZE HAIL REPORTED IN THE NORTHERN PART OF ZEBULON NEAR THE INTERSECTION OF WAKELON ST. AND NC HWY 96.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 40.3685 km away, between 2006-05-26 19:00:00 and 2006-05-26 19:00:00. 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: \nEvent Narrative: TREES AND FENCES BLOWN DOWN AT THE ORANGE COUNTY SPEEDWAY.",
+        "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00013722, approximately 37.1788 km away, between 2006-05-26 19:05:00 and 2006-05-26 19:10:00. The events included records with hailstones measuring 25.875 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative:    \nEvent Narrative:  TREES BLOWN DOWN.  TREE DOWN ACROSS STAGWELL ROAD.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 26.488 km away, between 2006-05-26 19:15:00 and 2006-05-26 19:15:00. 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: \nEvent Narrative: NUMEROUS TREES DOWN IN SOUTHERN GRANVILLE COUNTY.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 18.0595 km away, between 2006-05-26 19:59:00 and 2006-05-26 19:59:00. 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: \nEvent Narrative: SHINGLES BLOWN OFF ROOF AND MEASURED 57 MPH PEAK WIND GUST AT BUFFALO ROAD AND VALLEY STREAM DRIVE.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 22.8838 km away, between 2006-05-26 20:10:00 and 2006-05-26 20:10:00. 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: \nEvent Narrative: TREES AND POWER LINES DOWN.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 37.755 km away, between 2006-06-02 15:24:00 and 2006-06-02 15:24:00. 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: \nEvent Narrative: Roof blown off a mobile home near US 1.",
+        "The following events were reported: Hail. These occurred near station USW00013722, approximately 33.4452 km away, between 2006-06-06 14:30:00 and 2006-06-06 16:25:00. 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:      \nEvent Narrative: Reported near the US 1and NC highway 96 junction. Reported near US highway 64 and Beaver Creek Road. Reported 6 miles south of US highway 1. Reported near the intersection of US highway 64 and Rolesville Road.  Reported near the Interstate 85 and Interstate 40 split.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 40.1051 km away, between 2006-06-11 19:30:00 and 2006-06-11 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:   \nEvent Narrative: Several trees down along US highway 1 near exit 79. Numerous trees down throughout the city. Numerous trees down in Corinth and Moncure.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 38.8476 km away, between 2006-06-11 20:01:00 and 2006-06-11 20:05:00. 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:   \nEvent Narrative: Tree down on Atkins Road near the Wake County line. Automobile hit tree in the road. No injuries reported. Numerous trees down south of Holly Springs near the Wilbon area. Tree down on Cokesbury Road.",
+        "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00013722, approximately 34.6547 km away, between 2006-06-11 20:05:00 and 2006-06-11 20:15:00. The events included records with hailstones measuring 33.583333333333336 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative:   \nEvent Narrative: Penny size hail reported near US highway 401 and Ten Ten Road. Large trees down blocking Piney Grove-Wilbon Road. Trees down on Wyndham Place Drive off of Rawls Church Road.",
+        "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00013722, approximately 37.9872 km away, between 2006-06-11 20:25:00 and 2006-06-11 20:35:00. The events included records with hailstones measuring 19.166666666666668 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative:   \nEvent Narrative: Penny size hail in the town of Cleveland.  Reported on interstate 40 between exits 319 and 312.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 39.1678 km away, between 2006-06-21 12:50:00 and 2006-06-21 12:50:00. 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: \nEvent Narrative: Several trees down.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 21.5579 km away, between 2006-06-23 15:05:00 and 2006-06-23 15:25:00. 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:  \nEvent Narrative: Several trees snapped off at Hodge and Mingo Bluff Road. Trees down on Burlington Mill Road Between Capital Blvd and Ligon Mill Road.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 40.9697 km away, between 2006-06-23 16:00:00 and 2006-06-23 16:00:00. 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: \nEvent Narrative: Trees down in Moncure near Pittsboro Road and US highway 1.",
+        "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00013722, approximately 46.6337 km away, between 2006-07-03 18:30:00 and 2006-07-03 18:35:00. The events included records with hailstones measuring 33.626666666666665 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative:   \nEvent Narrative:  Trees down on South 5th Street. Numerous trees down blocking roads in the area of Buckhorn Road and West Ten Road.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 39.3499 km away, between 2006-07-14 16:18:00 and 2006-07-14 16:18:00. 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: \nEvent Narrative: Sever trees down on Coleman Road just north of Hillsborough.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 25.1784 km away, between 2006-07-19 13:00:00 and 2006-07-19 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:     \nEvent Narrative: Trees down at New Hill Holleman Road and Old US 1. Trees down on power lines...one of which caught fire. Report of trees down...blocking roads in Stem and Cornwall. Trees down on state road 56. Tree down blocking the road near the wake county line.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 42.457 km away, between 2006-07-19 15:25:00 and 2006-07-19 15:25:00. 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: \nEvent Narrative: Several trees down...one across the roadway.",
+        "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00013722, approximately 31.7543 km away, between 2006-07-27 12:55:00 and 2006-07-27 15:15:00. The events included records with hailstones measuring 35.964285714285715 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative:       \nEvent Narrative: Several trees down.  Several trees down. Large downed tree limb blocked traffice near the Lake Boone Trail Shopping Center.  Other large limbs reported down near the intersection of Wesern Blvd and Blue Ridge Road. Trees and large limbs reported down near Kipling. Trees down at Hilltop-Needmoore Road. Nickel to quarter sized hail covering the ground.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 24.5557 km away, between 2006-07-29 16:25:00 and 2006-07-29 16:25:00. 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: \nEvent Narrative: South of Garner near Interstate 40 reports of several trees down along the road.",
+        "The following events were reported: Hail. These occurred near station USW00013722, approximately 18.4041 km away, between 2006-08-07 15:36:00 and 2006-08-07 15:36:00. 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: \nEvent Narrative: Reported near Deerborn Drive and Club Road.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 35.9533 km away, between 2006-08-30 15:35:00 and 2006-08-30 15:55:00. 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:  \nEvent Narrative: Roof blown off a tractor barn off Moriah Road. A few trees reported down in northern Durham County.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 47.2693 km away, between 2006-08-30 16:00:00 and 2006-08-30 16:00:00. 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: \nEvent Narrative: A few trees down on HWY 56 and 158.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 43.9343 km away, between 2006-09-28 18:10:00 and 2006-09-28 18:10:00. 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: \nEvent Narrative: Several trees reported down north of Hillsborough.",
+        "The following events were reported: Flash Flood, Thunderstorm Wind. These occurred near station USW00013722, approximately 31.7311 km away, between 2006-11-16 04:50:00 and 2006-11-16 10:15:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A sharp cold front brought heavy rain and severe weather to the eastern  United States, including a deadly F3 in eastern NC. A sharp cold front brought heavy rain and severe weather to the eastern  United States, including a deadly F3 in eastern NC. A sharp cold front brought heavy rain and severe weather to the eastern  United States, including a deadly F3 in eastern NC. A sharp cold front brought heavy rain and severe weather to the eastern  United States, including a deadly F3 in eastern NC. A sharp cold front brought heavy rain and severe weather to the eastern  United States, including a deadly F3 in eastern NC.\nEvent Narrative: A 62 mph wind gust was recorded by a spotter using a mobile anemometer between Clayton and Archers Lodge. Durham Freeway was completed flooded near T.W. Alexander Drive. Two oak trees down on the state capital grounds. Tree down on Covered Bridge Road. Tree down on HWY 96.",
+        "The following events were reported: Heavy Rain. These occurred near station USW00013722, approximately 11.9121 km away, between 2006-11-22 09:15:00 and 2006-11-22 11:44:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Cyclogenesis spurred a developing surface cyclone which quickly occluded on November 20. Surface pressure gradient between this cyclone and a sprawling high stretching around its periphery from New England into the Deep South led to strong winds in the Carolinas. The cyclone deepened to a central pressure of 999 hPa before swinging westward into the Outer Banks of North Carolina on November 22. Storm total rainfall amounts averaged |2 to 4 inches across the WFO RAH forecast area. Cyclogenesis spurred a developing surface cyclone which quickly occluded on November 20. Surface pressure gradient between this cyclone and a sprawling high stretching around its periphery from New England into the Deep South led to strong winds in the Carolinas. The cyclone deepened to a central pressure of 999 hPa before swinging westward into the Outer Banks of North Carolina on November 22. Storm total rainfall amounts averaged |2 to 4 inches across the WFO RAH forecast area. Cyclogenesis spurred a developing surface cyclone which quickly occluded on November 20. Surface pressure gradient between this cyclone and a sprawling high stretching around its periphery from New England into the Deep South led to strong winds in the Carolinas. The cyclone deepened to a central pressure of 999 hPa before swinging westward into the Outer Banks of North Carolina on November 22. Storm total rainfall amounts averaged |2 to 4 inches across the WFO RAH forecast area.\nEvent Narrative: Crabtree Creek over flood stage at Old Wake Forest Road. Urban flooding reported on numerous city streets during the morning. Spotter reported Crabtree Creek at around 15 feet. Flooding was reported at Capital Bank and in Crabtree Valley Shopping Center.|",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 19.7384 km away, between 2007-03-02 04:54:00 and 2007-03-02 05:30:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: An area of low pressure formed ahead of a strong cold front and tracked along a warm front that extended across North Carolina. Strong kinematics from strong low-level jet and powerful 100kt 500mb jet resulted in scattered wind damage across central North Carolina. An area of low pressure formed ahead of a strong cold front and tracked along a warm front that extended across North Carolina. Strong kinematics from strong low-level jet and powerful 100kt 500mb jet resulted in scattered wind damage across central North Carolina.\nEvent Narrative:  Large tree down on NC HWY 42 near Johnston County line. NC HWY 42 blocked.",
+        "The following events were reported: Lightning. These occurred near station USW00013722, approximately 18.88 km away, between 2007-03-27 22:00:00 and 2007-03-27 22:00:00.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: Moderate to strong instability resulted from strong afternoon heating. Isolated thunderstorms developed across the northern piedmont along a weak surface boundary.\nEvent Narrative: Lightning struck an apartment complex and sparked a fire. There was no immediate information on the extent of the damage.",
+        "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00013722, approximately 35.1594 km away, between 2007-04-11 22:48:00 and 2007-04-11 23:15:00. 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: Thunderstorms developed overnight in a strong baroclinic zone as a coastal trough spread inland from southeast to northwest into central North Carolina...eroding A hybrid CAD event. An area of low pressure |developed along the coastal trough as a cold front approached from the west. Thunderstorms developed along the area of low pressure and in the warm and moist warm sector. Thunderstorms developed overnight in a strong baroclinic zone as a coastal trough spread inland from southeast to northwest into central North Carolina...eroding A hybrid CAD event. An area of low pressure |developed along the coastal trough as a cold front approached from the west. Thunderstorms developed along the area of low pressure and in the warm and moist warm sector.\nEvent Narrative: Quarter size hail on Whitehart Lane near the intersection of Ten-Ten Road and Grahm Newton Road. Tree blocking the road in McGees Crossroads area near HWY 210 and Raleigh road.",
+        "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00013722, approximately 32.7273 km away, between 2007-04-15 13:20:00 and 2007-04-15 17:50:00. The events included records with hailstones measuring 25.605 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Three rounds of severe weather struck Central North Carolina from the morning hours through the afternoon and into the evening. Widespread reports of damaging winds and large hail occurred with a rapidly intensifying surface low and attendant cold frontal passage. A powerful 70 knot low-level jet also aided in the initial round of severe storms. Thunderstorms re-developed in the late afternoon and evening hours as an amplifying upper level shortwave trough rotated across Central North Carolina. Three rounds of severe weather struck Central North Carolina from the morning hours through the afternoon and into the evening. Widespread reports of damaging winds and large hail occurred with a rapidly intensifying surface low and attendant cold frontal passage. A powerful 70 knot low-level jet also aided in the initial round of severe storms. Thunderstorms re-developed in the late afternoon and evening hours as an amplifying upper level shortwave trough rotated across Central North Carolina. Three rounds of severe weather struck Central North Carolina from the morning hours through the afternoon and into the evening. Widespread reports of damaging winds and large hail occurred with a rapidly intensifying surface low and attendant cold frontal passage. A powerful 70 knot low-level jet also aided in the initial round of severe storms. Thunderstorms re-developed in the late afternoon and evening hours as an amplifying upper level shortwave trough rotated across Central North Carolina. Three rounds of severe weather struck Central North Carolina from the morning hours through the afternoon and into the evening. Widespread reports of damaging winds and large hail occurred with a rapidly intensifying surface low and attendant cold frontal passage. A powerful 70 knot low-level jet also aided in the initial round of severe storms. Thunderstorms re-developed in the late afternoon and evening hours as an amplifying upper level shortwave trough rotated across Central North Carolina. Three rounds of severe weather struck Central North Carolina from the morning hours through the afternoon and into the evening. Widespread reports of damaging winds and large hail occurred with a rapidly intensifying surface low and attendant cold frontal passage. A powerful 70 knot low-level jet also aided in the initial round of severe storms. Thunderstorms re-developed in the late afternoon and evening hours as an amplifying upper level shortwave trough rotated across Central North Carolina. Three rounds of severe weather struck Central North Carolina from the morning hours through the afternoon and into the evening. Widespread reports of damaging winds and large hail occurred with a rapidly intensifying surface low and attendant cold frontal passage. A powerful 70 knot low-level jet also aided in the initial round of severe storms. Thunderstorms re-developed in the late afternoon and evening hours as an amplifying upper level shortwave trough rotated across Central North Carolina. Three rounds of severe weather struck Central North Carolina from the morning hours through the afternoon and into the evening. Widespread reports of damaging winds and large hail occurred with a rapidly intensifying surface low and attendant cold frontal passage. A powerful 70 knot low-level jet also aided in the initial round of severe storms. Thunderstorms re-developed in the late afternoon and evening hours as an amplifying upper level shortwave trough rotated across Central North Carolina. Three rounds of severe weather struck Central North Carolina from the morning hours through the afternoon and into the evening. Widespread reports of damaging winds and large hail occurred with a rapidly intensifying surface low and attendant cold frontal passage. A powerful 70 knot low-level jet also aided in the initial round of severe storms. Thunderstorms re-developed in the late afternoon and evening hours as an amplifying upper level shortwave trough rotated across Central North Carolina. Three rounds of severe weather struck Central North Carolina from the morning hours through the afternoon and into the evening. Widespread reports of damaging winds and large hail occurred with a rapidly intensifying surface low and attendant cold frontal passage. A powerful 70 knot low-level jet also aided in the initial round of severe storms. Thunderstorms re-developed in the late afternoon and evening hours as an amplifying upper level shortwave trough rotated across Central North Carolina. Three rounds of severe weather struck Central North Carolina from the morning hours through the afternoon and into the evening. Widespread reports of damaging winds and large hail occurred with a rapidly intensifying surface low and attendant cold frontal passage. A powerful 70 knot low-level jet also aided in the initial round of severe storms. Thunderstorms re-developed in the late afternoon and evening hours as an amplifying upper level shortwave trough rotated across Central North Carolina. Three rounds of severe weather struck Central North Carolina from the morning hours through the afternoon and into the evening. Widespread reports of damaging winds and large hail occurred with a rapidly intensifying surface low and attendant cold frontal passage. A powerful 70 knot low-level jet also aided in the initial round of severe storms. Thunderstorms re-developed in the late afternoon and evening hours as an amplifying upper level shortwave trough rotated across Central North Carolina. Three rounds of severe weather struck Central North Carolina from the morning hours through the afternoon and into the evening. Widespread reports of damaging winds and large hail occurred with a rapidly intensifying surface low and attendant cold frontal passage. A powerful 70 knot low-level jet also aided in the initial round of severe storms. Thunderstorms re-developed in the late afternoon and evening hours as an amplifying upper level shortwave trough rotated across Central North Carolina.\nEvent Narrative: A tree about 10 inchws in diameter tree was reported blown down near the intersection of Jordan and Sauls Rd. Several trees down just west of Fearrington. One tree fell on car. No injuries reported.  Two trees blown down on JJ Ranch Rd. Reported at Interstate 540 and Falls of the Neuse Rd. Reported on Lancashire Drive. Several trees down on roads. Quarter size hail reported between Angier and Fuquay-Varina.  Reported at the intersection of NC HWY 98 and Allen Rd. Off duty NWS Employee reported 55 to 60 mph winds on Guy Rd. Trees down on roads and power lines.",
+        "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00013722, approximately 30.349 km away, between 2007-05-09 16:03:00 and 2007-05-09 16:14:00. The events included records with hailstones measuring 17.166666666666668 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Pulse thunderstorms developed during peak afternoon heating as Subtropical Storm Andrea spun pumped warm and moist Atlantic moisture into the Carolinas. A mid-level shear axis associated with Andrea, helped the storms to become better organized. Pulse thunderstorms developed during peak afternoon heating as Subtropical Storm Andrea spun pumped warm and moist Atlantic moisture into the Carolinas. A mid-level shear axis associated with Andrea, helped the storms to become better organized. Pulse thunderstorms developed during peak afternoon heating as Subtropical Storm Andrea spun pumped warm and moist Atlantic moisture into the Carolinas. A mid-level shear axis associated with Andrea, helped the storms to become better organized.\nEvent Narrative:  Reported near the Durham county line. Several windows blown out along with minor roof damage to a business in downtown.",
+        "The following events were reported: Hail. These occurred near station USW00013722, approximately 33.1035 km away, between 2007-05-12 15:44:00 and 2007-05-12 15:54:00. 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: A weak surface wave developed along a pre-frontal trough that triggered pulse severe during max daytime heating. A weak surface wave developed along a pre-frontal trough that triggered pulse severe during max daytime heating. A weak surface wave developed along a pre-frontal trough that triggered pulse severe during max daytime heating.\nEvent Narrative:  Reported on East Lyon Station Rd. Reported near the intersection of HWY 15 and Sanders Rd.",
+        "The following events were reported: Hail. These occurred near station USW00013722, approximately 24.7805 km away, between 2007-05-29 17:40:00 and 2007-05-29 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: Showers and thunderstorms developed during peak time heating as a weak back-door cold front moved south into central North Carolina.\nEvent Narrative: Reported on Budsmith Road.",
+        "The following events were reported: Hail. These occurred near station USW00013722, approximately 39.4597 km away, between 2007-06-04 20:50:00 and 2007-06-04 20:50:00. The events included records with hailstones measuring 1.75 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Scattered thunderstorms developed during peak heating and continued into the evening hours as mid-level shortwave energy moved across the area.\nEvent Narrative: Golfball size hail was reported in the town of Caldwell.",
+        "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00013722, approximately 16.4582 km away, between 2007-06-09 19:10:00 and 2007-06-09 20:45:00. The events included records with hailstones measuring 28.18111111111111 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: An old outflow boundary from thunderstorms in Southern Virginia spawned severe thunderstorms across the central piedmont. An old outflow boundary from thunderstorms in Southern Virginia spawned severe thunderstorms across the central piedmont. An old outflow boundary from thunderstorms in Southern Virginia spawned severe thunderstorms across the central piedmont. An old outflow boundary from thunderstorms in Southern Virginia spawned severe thunderstorms across the central piedmont. An old outflow boundary from thunderstorms in Southern Virginia spawned severe thunderstorms across the central piedmont. An old outflow boundary from thunderstorms in Southern Virginia spawned severe thunderstorms across the central piedmont. An old outflow boundary from thunderstorms in Southern Virginia spawned severe thunderstorms across the central piedmont. An old outflow boundary from thunderstorms in Southern Virginia spawned severe thunderstorms across the central piedmont. An old outflow boundary from thunderstorms in Southern Virginia spawned severe thunderstorms across the central piedmont.\nEvent Narrative:  Penny size hail reported near Norwood Road and Mt. Vernon Church Road. Nickel size hail was reported along Interstate 40. A tree was reported down across Kemp Road. Several trees were reported down near the Stony Hills Area from 60 mph wind. Trees were reported down across Cornwallis Road. Trees were reported down across Carpenter Road.  Several trees were reported down along Old Erwin Road.",
+        "The following events were reported: Hail. These occurred near station USW00013722, approximately 20.0606 km away, between 2007-06-13 11:55:00 and 2007-06-13 12:20:00. 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: Mid and upper level impulses rotated southward in deep northerly flow|as a deep closed cyclone spun off the northeast coast. The pulse storms became severe during afternoon heating and quickly diminished with sunset. Mid and upper level impulses rotated southward in deep northerly flow|as a deep closed cyclone spun off the northeast coast. The pulse storms became severe during afternoon heating and quickly diminished with sunset.\nEvent Narrative: Penny size hail was reported at Knight's Play Golf Course on Ten Ten Road. Penny size hail was reported near the intersection of New Hope Church and Yates Mill Road near the Wake County line.",
+        "The following events were reported: Hail. These occurred near station USW00013722, approximately 40.585 km away, between 2007-06-22 16:21:00 and 2007-06-22 16:21:00. 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: Isolated thunderstorms developed during peak diurnal heating.\nEvent Narrative:",
+        "The following events were reported: Hail. These occurred near station USW00013722, approximately 46.8948 km away, between 2007-06-22 16:21:00 and 2007-06-22 16:21:00. 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: Afternoon heating resulted in a signle severe pulse thunderstorm over southern Franklin county.\nEvent Narrative:",
+        "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00013722, approximately 32.0054 km away, between 2007-06-29 12:25:00 and 2007-06-29 13:35:00. The events included records with hailstones measuring 21.25 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Strong daytime heating featuring temperatures in the mid 90s, resulted in |widespread convection. The strongest storms formed along the sea breeze boundary and lee side trough. Strong daytime heating featuring temperatures in the mid 90s, resulted in |widespread convection. The strongest storms formed along the sea breeze boundary and lee side trough. Strong daytime heating featuring temperatures in the mid 90s, resulted in |widespread convection. The strongest storms formed along the sea breeze boundary and lee side trough. Strong daytime heating featuring temperatures in the mid 90s, resulted in |widespread convection. The strongest storms formed along the sea breeze boundary and lee side trough. Strong daytime heating featuring temperatures in the mid 90s, resulted in |widespread convection. The strongest storms formed along the sea breeze boundary and lee side trough.\nEvent Narrative:   Penny size hail was reported on Route 50 just south of the Wake and Johnston County line. Penny size hail was reported on Durant Road. Several trees were blown down around Corinth.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 37.755 km away, between 2007-07-10 15:30:00 and 2007-07-10 15:30:00. 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: Scattered thunderstorms developed during strong daytime heating and along a weak low pressure trough.\nEvent Narrative: Several trees were reported blown down in the area.",
+        "The following events were reported: Lightning, Thunderstorm Wind. These occurred near station USW00013722, approximately 34.6872 km away, between 2007-07-11 16:10:00 and 2007-07-11 17:00:00.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 thunderstorms developed along a pre-frontal trough during peak  afternoon heating. Scattered thunderstorms developed along a pre-frontal trough during peak  afternoon heating. Scattered thunderstorms developed along a pre-frontal trough during peak  afternoon heating. Scattered thunderstorms developed along a pre-frontal trough during peak  afternoon heating. Scattered thunderstorms developed along a pre-frontal trough during peak  afternoon heating. Scattered thunderstorms developed along a pre-frontal trough during peak  afternoon heating.\nEvent Narrative: Several trees were blown down in southeastern portions of county. Several trees were blown down near the old brick plant along US Highway 1. Several trees were blown down along the exit ramp to US Highway 1 at exit 87. One tree was blown down in front of Holly Springs Elementary School. Several trees were blown down in the area. An unoccupied building in Youngsville was struck by lightning.",
+        "The following events were reported: Flash Flood, Hail, Thunderstorm Wind. These occurred near station USW00013722, approximately 15.9748 km away, between 2007-07-17 15:45:00 and 2007-07-18 00:59:00. The events included records with hailstones measuring 25.563 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Scattered thunderstorms initially developed during strong heating and then additional storms developed along numerous outflow boundaries. Thunderstorms persisted well into the evening as weak vorticity lobes |moved across the area from the southwest. Scattered thunderstorms initially developed during strong heating and then additional storms developed along numerous outflow boundaries. Thunderstorms persisted well into the evening as weak vorticity lobes |moved across the area from the southwest. Scattered thunderstorms initially developed during strong heating and then additional storms developed along numerous outflow boundaries. Thunderstorms persisted well into the evening as weak vorticity lobes |moved across the area from the southwest. Scattered thunderstorms initially developed during strong heating and then additional storms developed along numerous outflow boundaries. Thunderstorms persisted well into the evening as weak vorticity lobes |moved across the area from the southwest. Scattered thunderstorms initially developed during strong heating and then additional storms developed along numerous outflow boundaries. Thunderstorms persisted well into the evening as weak vorticity lobes |moved across the area from the southwest. Scattered thunderstorms initially developed during strong heating and then additional storms developed along numerous outflow boundaries. Thunderstorms persisted well into the evening as weak vorticity lobes |moved across the area from the southwest. Scattered thunderstorms initially developed during strong heating and then additional storms developed along numerous outflow boundaries. Thunderstorms persisted well into the evening as weak vorticity lobes |moved across the area from the southwest. Scattered thunderstorms initially developed during strong heating and then additional storms developed along numerous outflow boundaries. Thunderstorms persisted well into the evening as weak vorticity lobes |moved across the area from the southwest. Scattered thunderstorms initially developed during strong heating and then additional storms developed along numerous outflow boundaries. Thunderstorms persisted well into the evening as weak vorticity lobes |moved across the area from the southwest. Scattered thunderstorms initially developed during strong heating and then additional storms developed along numerous outflow boundaries. Thunderstorms persisted well into the evening as weak vorticity lobes |moved across the area from the southwest. Scattered thunderstorms initially developed during strong heating and then additional storms developed along numerous outflow boundaries. Thunderstorms persisted well into the evening as weak vorticity lobes |moved across the area from the southwest.\nEvent Narrative: Nickel size hail was reported near the intersection of Blue Ridge and Lake Boone Road. Penny size hail was reported in west Raleigh near North Carolina State University. Quarter size hail was reported on the campus of North Carolina State University. A trained spotter measured a 60 mph wind gust. Quarter size hail was reported at Wolf Village near the North Carolina State University Campus. Quarter size hail was reported at the National Weather Service office. Several trees were reported blown down in the area. One large tree was blown down on Western Boulevard near South Saunders Street. Trees and power lines were reported blown down on Morgan Street near Tryon Hill Drive. The tree crashed upon a house. There were no injuries reported. One tree was blown down in south Raleigh. TenTen Road between Kildaire Farm Road and Holly Springs Road was closed due to flooding.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 48.7212 km away, between 2007-07-19 17:45:00 and 2007-07-19 17:45:00. 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: An old outflow boundary from convection that fired in the higher terrain of the mountains redeveloped over the western piedmont. An old outflow boundary from convection that fired in the higher terrain of the mountains redeveloped over the western piedmont.\nEvent Narrative: One large tree was blown down across Mebane Oaks Road. Multiple trees were blown down on Mebane Oaks Road one mile south of Interstate of 85 between Old Hillsborough Road and Mebane Oaks Court.",
+        "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00013722, approximately 31.9755 km away, between 2007-07-27 12:39:00 and 2007-07-27 18:52:00. The events included records with hailstones measuring 10.678 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Relatively cool mid and upper level temperatures aloft associated with shortwave trough rotating around the upper low over the Great Lakes region |resulted in widespread convection during strong daytime heating. Relatively cool mid and upper level temperatures aloft associated with shortwave trough rotating around the upper low over the Great Lakes region |resulted in widespread convection during strong daytime heating. Relatively cool mid and upper level temperatures aloft associated with shortwave trough rotating around the upper low over the Great Lakes region |resulted in widespread convection during strong daytime heating. Relatively cool mid and upper level temperatures aloft associated with shortwave trough rotating around the upper low over the Great Lakes region |resulted in widespread convection during strong daytime heating. Relatively cool mid and upper level temperatures aloft associated with shortwave trough rotating around the upper low over the Great Lakes region |resulted in widespread convection during strong daytime heating.\nEvent Narrative:  Several trees were blown down near the intersection of Green Hill Road and Highway 56. Nickel size hail was reported along HWY 96 near Barham Siding Road. Nickel size hail was reported near the intersection of Mt. Gilead Road and Sugar Lake Road. Nickel size hail was reported near the intersection of Interstate 40 and NC Route 54.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 12.5823 km away, between 2007-08-09 19:30:00 and 2007-08-09 19:30:00. 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: Strong daytime heating featuring temperatures in the triple digits triggered scattered convection across Central NC.\nEvent Narrative: One tree was reported blown down and partially blocking traffic on Harrison Avenue near Reedy Creek. There were also several trees reported blown down on Weston Parkway. A metal gazebo was blown onto the porch of a residence in Cary. Finally, a shopping cart port was blown over, damaging  a car in the Harris Teeter parking lot at the intersection of Maynard and Harrison.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 15.698 km away, between 2007-08-10 17:10:00 and 2007-08-10 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: In the wake of an intense heat wave that shattered many high temperature records throughout the week, a surface trough moving southeast across the state sparked several severe thunderstorms.\nEvent Narrative: Several trees were blown down in Brentwood Park along Marsh Creek Road.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 33.6403 km away, between 2007-08-21 16:48:00 and 2007-08-21 18:50:00. The events included records with estimated wind gusts of 50.125 mph.The events resulted in 8 injuries and 0 fatalities. No significant property or crop damage was reported. \n\nEpisode Narrative: During the late afternoon and evening hours, the vorticity maximum associated with Erin\ufffd\ufffd\ufffds remnants served as a catalyst for organized thunderstorm development as it approached and eventually crossed the area. During the late afternoon and evening hours, the vorticity maximum associated with Erin\ufffd\ufffd\ufffds remnants served as a catalyst for organized thunderstorm development as it approached and eventually crossed the area. During the late afternoon and evening hours, the vorticity maximum associated with Erin\ufffd\ufffd\ufffds remnants served as a catalyst for organized thunderstorm development as it approached and eventually crossed the area. During the late afternoon and evening hours, the vorticity maximum associated with Erin\ufffd\ufffd\ufffds remnants served as a catalyst for organized thunderstorm development as it approached and eventually crossed the area. During the late afternoon and evening hours, the vorticity maximum associated with Erin\ufffd\ufffd\ufffds remnants served as a catalyst for organized thunderstorm development as it approached and eventually crossed the area. During the late afternoon and evening hours, the vorticity maximum associated with Erin\ufffd\ufffd\ufffds remnants served as a catalyst for organized thunderstorm development as it approached and eventually crossed the area. During the late afternoon and evening hours, the vorticity maximum associated with Erin\ufffd\ufffd\ufffds remnants served as a catalyst for organized thunderstorm development as it approached and eventually crossed the area. During the late afternoon and evening hours, the vorticity maximum associated with Erin\ufffd\ufffd\ufffds remnants served as a catalyst for organized thunderstorm development as it approached and eventually crossed the area. During the late afternoon and evening hours, the vorticity maximum associated with Erin\ufffd\ufffd\ufffds remnants served as a catalyst for organized thunderstorm development as it approached and eventually crossed the area. During the late afternoon and evening hours, the vorticity maximum associated with Erin\ufffd\ufffd\ufffds remnants served as a catalyst for organized thunderstorm development as it approached and eventually crossed the area. During the late afternoon and evening hours, the vorticity maximum associated with Erin\ufffd\ufffd\ufffds remnants served as a catalyst for organized thunderstorm development as it approached and eventually crossed the area. During the late afternoon and evening hours, the vorticity maximum associated with Erin\ufffd\ufffd\ufffds remnants served as a catalyst for organized thunderstorm development as it approached and eventually crossed the area. During the late afternoon and evening hours, the vorticity maximum associated with Erin\ufffd\ufffd\ufffds remnants served as a catalyst for organized thunderstorm development as it approached and eventually crossed the area. During the late afternoon and evening hours, the vorticity maximum associated with Erin\ufffd\ufffd\ufffds remnants served as a catalyst for organized thunderstorm development as it approached and eventually crossed the area. During the late afternoon and evening hours, the vorticity maximum associated with Erin\ufffd\ufffd\ufffds remnants served as a catalyst for organized thunderstorm development as it approached and eventually crossed the area. During the late afternoon and evening hours, the vorticity maximum associated with Erin\ufffd\ufffd\ufffds remnants served as a catalyst for organized thunderstorm development as it approached and eventually crossed the area.\nEvent Narrative: Multiple trees were blown down at the intersection Highway 70 and Amelia Church Road. A spotter reported several trees down at the Walnut Creek Amphitheatre. A roof was also blown off of an outdoor shelter at the amphitheatre. The public reported several large branches broken off of an Oak tree at the All-Star Mobile Home Park off of Lake Wheeler Road. One tree was blown down on Timber Drive near Highway 50. Three small trees were blown down. A trained spotter estimated a 60 to 70 mph wind gust at the intersection of Highways 50 and 210. One tree was blown down in Orange Grove near Dodsons Crossroads. Numerous trees were blown down throughout western portions of the county. Law enforcement reported one tree fell on a house in the city of Pittsboro. A stand of Oak trees were blown down east of Highways 98 and 501 near Five Points. One tree was blown down onto a house in Cary. Several trees were blown down near Hurdle Mills just north of the Orange County line. One tree was blown down on Chambers Road in Bahama. Multiple trees were blown down west of Oxford. Power utility poles were completely pulled out of the ground in the Starmount Subdivision at 2 different locations. Amateur radio reported that downed power lines were partially blocking  traffic on Old Stage Road. Numerous trees were blown down near Lillington, Kipling, and other locations in the area.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 43.0652 km away, between 2007-08-26 16:30:00 and 2007-08-26 16:30:00. 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: Scattered thunderstorms developed ahead of an approaching cold front during strong daytime heating. Weak deep layer shear resulted in slow moving to nearly stationary thunderstorms.\nEvent Narrative: One tree was blown down, blocking one lane of traffic on Raleigh Road near Coats Crossroads.",
+        "The following events were reported: Funnel Cloud, Lightning, Thunderstorm Wind, Tornado. These occurred near station USW00013722, approximately 36.8107 km away, between 2007-09-14 17:00:00 and 2007-09-14 18:50:00.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: On the afternoon and evening of September 14th, tropical moisture streamed north ahead of the remnants of Humberto. The environment over Central North Carolina became supportive for tornado development as a surface boundary stalled across the area. On the afternoon and evening of September 14th, tropical moisture streamed north ahead of the remnants of Humberto. The environment over Central North Carolina became supportive for tornado development as a surface boundary stalled across the area. On the afternoon and evening of September 14th, tropical moisture streamed north ahead of the remnants of Humberto. The environment over Central North Carolina became supportive for tornado development as a surface boundary stalled across the area. On the afternoon and evening of September 14th, tropical moisture streamed north ahead of the remnants of Humberto. The environment over Central North Carolina became supportive for tornado development as a surface boundary stalled across the area. On the afternoon and evening of September 14th, tropical moisture streamed north ahead of the remnants of Humberto. The environment over Central North Carolina became supportive for tornado development as a surface boundary stalled across the area. On the afternoon and evening of September 14th, tropical moisture streamed north ahead of the remnants of Humberto. The environment over Central North Carolina became supportive for tornado development as a surface boundary stalled across the area. On the afternoon and evening of September 14th, tropical moisture streamed north ahead of the remnants of Humberto. The environment over Central North Carolina became supportive for tornado development as a surface boundary stalled across the area. On the afternoon and evening of September 14th, tropical moisture streamed north ahead of the remnants of Humberto. The environment over Central North Carolina became supportive for tornado development as a surface boundary stalled across the area. On the afternoon and evening of September 14th, tropical moisture streamed north ahead of the remnants of Humberto. The environment over Central North Carolina became supportive for tornado development as a surface boundary stalled across the area. On the afternoon and evening of September 14th, tropical moisture streamed north ahead of the remnants of Humberto. The environment over Central North Carolina became supportive for tornado development as a surface boundary stalled across the area. On the afternoon and evening of September 14th, tropical moisture streamed north ahead of the remnants of Humberto. The environment over Central North Carolina became supportive for tornado development as a surface boundary stalled across the area.\nEvent Narrative: A tornado touch downed at Clayton Middle School on Guy Road. A second tornado touched down from the same thunderstorm near the Jordan community. Public reported a brief touch down of a tornado with debris just south of Garner near Lake Benson. Law enforcement reported a tornado and multiple trees down on Stephenson Road. A spotter reported a tree and limbs suspended on power lines on Academy Street. A trained spotter reported a tree down across Vance Street inside the city limits. Numerous funnel clouds were reported along Highway 42. Multiple reports of funnel clouds were reported by the public near Coats Crossroads. Widespread tree damage was reported on Old Hunneycut Road, Purfoy Road and Main Street. Several trees and a few power lines were blown down in the town if Ainger. A large tree fell onto the roof of a nursing home near the Five Points area causing significant damage. All of the residents had to be evacuated. A spotter reported a barn fire caused by lightning north of Clayton.",
+        "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00013722, approximately 32.6203 km away, between 2008-03-04 18:00:00 and 2008-03-04 23:35:00. The events included records with hailstones measuring 48.90384615384615 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Central North Carolina endured a one-two punch of severe weather as a well developed upper low and negatively tilted upper trough moved across the region. The first round of severe storms began in the afternoon as discrete storms developed well ahead of an organized squall line. Minor wind damage was reported, along with an isolated tornado. The second round of severe storms came later that evening, as the squall line swept through the state, producing widespread wind damage and another brief tornado touchdown. Central North Carolina endured a one-two punch of severe weather as a well developed upper low and negatively tilted upper trough moved across the region. The first round of severe storms began in the afternoon as discrete storms developed well ahead of an organized squall line. Minor wind damage was reported, along with an isolated tornado. The second round of severe storms came later that evening, as the squall line swept through the state, producing widespread wind damage and another brief tornado touchdown. Central North Carolina endured a one-two punch of severe weather as a well developed upper low and negatively tilted upper trough moved across the region. The first round of severe storms began in the afternoon as discrete storms developed well ahead of an organized squall line. Minor wind damage was reported, along with an isolated tornado. The second round of severe storms came later that evening, as the squall line swept through the state, producing widespread wind damage and another brief tornado touchdown. Central North Carolina endured a one-two punch of severe weather as a well developed upper low and negatively tilted upper trough moved across the region. The first round of severe storms began in the afternoon as discrete storms developed well ahead of an organized squall line. Minor wind damage was reported, along with an isolated tornado. The second round of severe storms came later that evening, as the squall line swept through the state, producing widespread wind damage and another brief tornado touchdown. Central North Carolina endured a one-two punch of severe weather as a well developed upper low and negatively tilted upper trough moved across the region. The first round of severe storms began in the afternoon as discrete storms developed well ahead of an organized squall line. Minor wind damage was reported, along with an isolated tornado. The second round of severe storms came later that evening, as the squall line swept through the state, producing widespread wind damage and another brief tornado touchdown. Central North Carolina endured a one-two punch of severe weather as a well developed upper low and negatively tilted upper trough moved across the region. The first round of severe storms began in the afternoon as discrete storms developed well ahead of an organized squall line. Minor wind damage was reported, along with an isolated tornado. The second round of severe storms came later that evening, as the squall line swept through the state, producing widespread wind damage and another brief tornado touchdown. Central North Carolina endured a one-two punch of severe weather as a well developed upper low and negatively tilted upper trough moved across the region. The first round of severe storms began in the afternoon as discrete storms developed well ahead of an organized squall line. Minor wind damage was reported, along with an isolated tornado. The second round of severe storms came later that evening, as the squall line swept through the state, producing widespread wind damage and another brief tornado touchdown. Central North Carolina endured a one-two punch of severe weather as a well developed upper low and negatively tilted upper trough moved across the region. The first round of severe storms began in the afternoon as discrete storms developed well ahead of an organized squall line. Minor wind damage was reported, along with an isolated tornado. The second round of severe storms came later that evening, as the squall line swept through the state, producing widespread wind damage and another brief tornado touchdown. Central North Carolina endured a one-two punch of severe weather as a well developed upper low and negatively tilted upper trough moved across the region. The first round of severe storms began in the afternoon as discrete storms developed well ahead of an organized squall line. Minor wind damage was reported, along with an isolated tornado. The second round of severe storms came later that evening, as the squall line swept through the state, producing widespread wind damage and another brief tornado touchdown. Central North Carolina endured a one-two punch of severe weather as a well developed upper low and negatively tilted upper trough moved across the region. The first round of severe storms began in the afternoon as discrete storms developed well ahead of an organized squall line. Minor wind damage was reported, along with an isolated tornado. The second round of severe storms came later that evening, as the squall line swept through the state, producing widespread wind damage and another brief tornado touchdown. Central North Carolina endured a one-two punch of severe weather as a well developed upper low and negatively tilted upper trough moved across the region. The first round of severe storms began in the afternoon as discrete storms developed well ahead of an organized squall line. Minor wind damage was reported, along with an isolated tornado. The second round of severe storms came later that evening, as the squall line swept through the state, producing widespread wind damage and another brief tornado touchdown. Central North Carolina endured a one-two punch of severe weather as a well developed upper low and negatively tilted upper trough moved across the region. The first round of severe storms began in the afternoon as discrete storms developed well ahead of an organized squall line. Minor wind damage was reported, along with an isolated tornado. The second round of severe storms came later that evening, as the squall line swept through the state, producing widespread wind damage and another brief tornado touchdown. Central North Carolina endured a one-two punch of severe weather as a well developed upper low and negatively tilted upper trough moved across the region. The first round of severe storms began in the afternoon as discrete storms developed well ahead of an organized squall line. Minor wind damage was reported, along with an isolated tornado. The second round of severe storms came later that evening, as the squall line swept through the state, producing widespread wind damage and another brief tornado touchdown.\nEvent Narrative: Numerous trees were blown down from Chapel hill, east to the Durham County line. Severe winds estimated between 60 to 70 mph, blew a tree down onto a home on Vickie Drive.  Numerous trees were reported blown down around Mebane. One tree was reported blown down, east-southeast of Rougemont. Trained spotter measured a 70 mph wind gust with widespread power outages reported. Trees were reported blown down across Pea Ridge Road in Pittsboro. Several trees were blown down along New Bern Avenue. A home sustained damaged when severe straight line damaging winds, estimated at 60 to 70 mph, blew a tree onto a home. One tree was reported blown down across P G Pearce Road. Three trees reported blown down just north of NC Highway 157 on NC Highway  57 near Caldwell. Trees were reported blown down in Rougemont. Penny size hail was reported near the city of Durham. Winds were also estimated at 60 mph.",
+        "The following events were reported: Hail. These occurred near station USW00013722, approximately 38.5484 km away, between 2008-04-20 14:56:00 and 2008-04-21 12:17:00. The events included records with hailstones measuring 1.1666666666666667 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Over the course of two day, several shortwave vorticity maxes rotated across the area as a closed upper low spun rotated through the region. Severe thunderstorms developed amidst steepening mid level lapse rates and peak afternoon heating. The severe storms resulted in mainly large hail, ranging from penny to golf ball size hail with an isolated flash flooding. Over the course of two day, several shortwave vorticity maxes rotated across the area as a closed upper low spun rotated through the region. Severe thunderstorms developed amidst steepening mid level lapse rates and peak afternoon heating. The severe storms resulted in mainly large hail, ranging from penny to golf ball size hail with an isolated flash flooding. Over the course of two day, several shortwave vorticity maxes rotated across the area as a closed upper low spun rotated through the region. Severe thunderstorms developed amidst steepening mid level lapse rates and peak afternoon heating. The severe storms resulted in mainly large hail, ranging from penny to golf ball size hail with an isolated flash flooding.\nEvent Narrative:  Penny size hail was reported near Sunset Lake Road and Holly Springs Road. Golf ball size hail was reported near the intersection of Highway 42 and Buckhorn Road.",
+        "The following events were reported: Flash Flood, Hail. These occurred near station USW00013722, approximately 24.6599 km away, between 2008-04-27 18:30:00 and 2008-04-27 22:30:00. 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 strong to severe convection developed during strong daytime heating and in advance of an approaching cold front. The severe storms produced penny size hail in the Triad. Scattered strong to severe convection developed during strong daytime heating and in advance of an approaching cold front. The severe storms produced penny size hail in the Triad. Scattered strong to severe convection developed during strong daytime heating and in advance of an approaching cold front. The severe storms produced penny size hail in the Triad.\nEvent Narrative: Penny size hail was reported near the intersection of Poplar Street and Anderson Street. Atlantic Avenue closed between Hodges and Millbrook roads due to high flood waters from Marsh Creek. A few vehicles had to be abandoned. Over three inches of rain fell between 645 pm and 1100 pm, with nearly 2.5 inches falling in the first hour alone. The heavy rainfall caused Marsh Creek to overflow, flooding south bound lanes of Capital Boulevard near the intersection of Brentwood Road. The softball field and walking trail in Brentwood Park also experienced flooding, with 4 to 5 feet of flowing water through the park.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 46.7367 km away, between 2008-05-08 20:35:00 and 2008-05-08 20:40:00. 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 strong upper level low moving east-northeast across Kentucky and Tennessee, triggered several instances of severe damaging winds and two  tornadoes across the Triad region in the northwest piedmont of North Carolina. A strong upper level low moving east-northeast across Kentucky and Tennessee, triggered several instances of severe damaging winds and two  tornadoes across the Triad region in the northwest piedmont of North Carolina.\nEvent Narrative: A tree was blown down onto George Sherman Road, Ben Thorpe Road, and Days Mill Road. One tree was blown down onto Kermit Duncan Road.",
+        "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00013722, approximately 27.026 km away, between 2008-05-09 22:50:00 and 2008-05-10 00:06:00. The events included records with hailstones measuring 4.418 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Strong thunderstorms developed east of the mountains as a strong mid level trough crossed the region. The storms intensified east of the mountains with a few long lived supercells producing numerous reports of golf ball size hail late into the evening hours. Strong thunderstorms developed east of the mountains as a strong mid level trough crossed the region. The storms intensified east of the mountains with a few long lived supercells producing numerous reports of golf ball size hail late into the evening hours. Strong thunderstorms developed east of the mountains as a strong mid level trough crossed the region. The storms intensified east of the mountains with a few long lived supercells producing numerous reports of golf ball size hail late into the evening hours. Strong thunderstorms developed east of the mountains as a strong mid level trough crossed the region. The storms intensified east of the mountains with a few long lived supercells producing numerous reports of golf ball size hail late into the evening hours. Strong thunderstorms developed east of the mountains as a strong mid level trough crossed the region. The storms intensified east of the mountains with a few long lived supercells producing numerous reports of golf ball size hail late into the evening hours. Strong thunderstorms developed east of the mountains as a strong mid level trough crossed the region. The storms intensified east of the mountains with a few long lived supercells producing numerous reports of golf ball size hail late into the evening hours. Strong thunderstorms developed east of the mountains as a strong mid level trough crossed the region. The storms intensified east of the mountains with a few long lived supercells producing numerous reports of golf ball size hail late into the evening hours. Strong thunderstorms developed east of the mountains as a strong mid level trough crossed the region. The storms intensified east of the mountains with a few long lived supercells producing numerous reports of golf ball size hail late into the evening hours. Strong thunderstorms developed east of the mountains as a strong mid level trough crossed the region. The storms intensified east of the mountains with a few long lived supercells producing numerous reports of golf ball size hail late into the evening hours. Strong thunderstorms developed east of the mountains as a strong mid level trough crossed the region. The storms intensified east of the mountains with a few long lived supercells producing numerous reports of golf ball size hail late into the evening hours. Strong thunderstorms developed east of the mountains as a strong mid level trough crossed the region. The storms intensified east of the mountains with a few long lived supercells producing numerous reports of golf ball size hail late into the evening hours. Strong thunderstorms developed east of the mountains as a strong mid level trough crossed the region. The storms intensified east of the mountains with a few long lived supercells producing numerous reports of golf ball size hail late into the evening hours. Strong thunderstorms developed east of the mountains as a strong mid level trough crossed the region. The storms intensified east of the mountains with a few long lived supercells producing numerous reports of golf ball size hail late into the evening hours. Strong thunderstorms developed east of the mountains as a strong mid level trough crossed the region. The storms intensified east of the mountains with a few long lived supercells producing numerous reports of golf ball size hail late into the evening hours. Strong thunderstorms developed east of the mountains as a strong mid level trough crossed the region. The storms intensified east of the mountains with a few long lived supercells producing numerous reports of golf ball size hail late into the evening hours.\nEvent Narrative: Ping-pong ball size hail was reported at the intersection of Davis Drive and Morrisville Parkway. Nickel size hail was reported near the intersection of Morrisville Parkway and Highway 55. Penny size hail was reported near the intersection of Castalia Drive and Old Apex Road.   Off duty National Weather Service Employee reported penny to nickel size hail.    Quarter size hail was reported on Arthur Minnis Road. Penny size hail was reported at the intersection of Allard and Lyon Roads.  Golf ball size hail was reported on Smith Level Road. Nickel size hail was reported at the intersection of Jenkins Carpenter and High House Road.",
+        "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00013722, approximately 30.4121 km away, between 2008-05-20 14:47:00 and 2008-05-20 16:57:00. The events included records with hailstones measuring 3.3264 inches.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 125000.0 and crop damage of 0.0. \n\nEpisode Narrative: Numerous thunderstorms developed across central North Carolina when a cold front and associated shortwave trough moved through central North Carolina during strong daytime heating. The severe storms produced widespread reports of large hail with only scattered thunderstorm wind damage. Numerous thunderstorms developed across central North Carolina when a cold front and associated shortwave trough moved through central North Carolina during strong daytime heating. The severe storms produced widespread reports of large hail with only scattered thunderstorm wind damage. Numerous thunderstorms developed across central North Carolina when a cold front and associated shortwave trough moved through central North Carolina during strong daytime heating. The severe storms produced widespread reports of large hail with only scattered thunderstorm wind damage. Numerous thunderstorms developed across central North Carolina when a cold front and associated shortwave trough moved through central North Carolina during strong daytime heating. The severe storms produced widespread reports of large hail with only scattered thunderstorm wind damage. Numerous thunderstorms developed across central North Carolina when a cold front and associated shortwave trough moved through central North Carolina during strong daytime heating. The severe storms produced widespread reports of large hail with only scattered thunderstorm wind damage. Numerous thunderstorms developed across central North Carolina when a cold front and associated shortwave trough moved through central North Carolina during strong daytime heating. The severe storms produced widespread reports of large hail with only scattered thunderstorm wind damage. Numerous thunderstorms developed across central North Carolina when a cold front and associated shortwave trough moved through central North Carolina during strong daytime heating. The severe storms produced widespread reports of large hail with only scattered thunderstorm wind damage. Numerous thunderstorms developed across central North Carolina when a cold front and associated shortwave trough moved through central North Carolina during strong daytime heating. The severe storms produced widespread reports of large hail with only scattered thunderstorm wind damage. Numerous thunderstorms developed across central North Carolina when a cold front and associated shortwave trough moved through central North Carolina during strong daytime heating. The severe storms produced widespread reports of large hail with only scattered thunderstorm wind damage. Numerous thunderstorms developed across central North Carolina when a cold front and associated shortwave trough moved through central North Carolina during strong daytime heating. The severe storms produced widespread reports of large hail with only scattered thunderstorm wind damage. Numerous thunderstorms developed across central North Carolina when a cold front and associated shortwave trough moved through central North Carolina during strong daytime heating. The severe storms produced widespread reports of large hail with only scattered thunderstorm wind damage. Numerous thunderstorms developed across central North Carolina when a cold front and associated shortwave trough moved through central North Carolina during strong daytime heating. The severe storms produced widespread reports of large hail with only scattered thunderstorm wind damage. Numerous thunderstorms developed across central North Carolina when a cold front and associated shortwave trough moved through central North Carolina during strong daytime heating. The severe storms produced widespread reports of large hail with only scattered thunderstorm wind damage. Numerous thunderstorms developed across central North Carolina when a cold front and associated shortwave trough moved through central North Carolina during strong daytime heating. The severe storms produced widespread reports of large hail with only scattered thunderstorm wind damage. Numerous thunderstorms developed across central North Carolina when a cold front and associated shortwave trough moved through central North Carolina during strong daytime heating. The severe storms produced widespread reports of large hail with only scattered thunderstorm wind damage. Numerous thunderstorms developed across central North Carolina when a cold front and associated shortwave trough moved through central North Carolina during strong daytime heating. The severe storms produced widespread reports of large hail with only scattered thunderstorm wind damage. Numerous thunderstorms developed across central North Carolina when a cold front and associated shortwave trough moved through central North Carolina during strong daytime heating. The severe storms produced widespread reports of large hail with only scattered thunderstorm wind damage. Numerous thunderstorms developed across central North Carolina when a cold front and associated shortwave trough moved through central North Carolina during strong daytime heating. The severe storms produced widespread reports of large hail with only scattered thunderstorm wind damage. Numerous thunderstorms developed across central North Carolina when a cold front and associated shortwave trough moved through central North Carolina during strong daytime heating. The severe storms produced widespread reports of large hail with only scattered thunderstorm wind damage. Numerous thunderstorms developed across central North Carolina when a cold front and associated shortwave trough moved through central North Carolina during strong daytime heating. The severe storms produced widespread reports of large hail with only scattered thunderstorm wind damage. Numerous thunderstorms developed across central North Carolina when a cold front and associated shortwave trough moved through central North Carolina during strong daytime heating. The severe storms produced widespread reports of large hail with only scattered thunderstorm wind damage. Numerous thunderstorms developed across central North Carolina when a cold front and associated shortwave trough moved through central North Carolina during strong daytime heating. The severe storms produced widespread reports of large hail with only scattered thunderstorm wind damage. Numerous thunderstorms developed across central North Carolina when a cold front and associated shortwave trough moved through central North Carolina during strong daytime heating. The severe storms produced widespread reports of large hail with only scattered thunderstorm wind damage. Numerous thunderstorms developed across central North Carolina when a cold front and associated shortwave trough moved through central North Carolina during strong daytime heating. The severe storms produced widespread reports of large hail with only scattered thunderstorm wind damage. Numerous thunderstorms developed across central North Carolina when a cold front and associated shortwave trough moved through central North Carolina during strong daytime heating. The severe storms produced widespread reports of large hail with only scattered thunderstorm wind damage.\nEvent Narrative:  Penny size hail reported at Churton and King Street. Penny size hail was reported near Cole Mill Road and Flemming Drive.   Nickel size hail was reported at the intersection of Schley Road and St. Marys Road.  Hail up to nickel size was reported on Mount Pleasant Church Road.   Penny size hail was reported near Spring Forest Road and Falls of the Neuse Road. Nickel size hail occurred 2 miles south of the Highway 56 and Highway 401 intersection.  Nickel size hail was reported in Holly Springs near Rouse Road. Penny size hail was reported near Cannon Gate Road and Tattenhall Drive.  Quarter size hail was reported at Highway 42 and Highway 50. Hail up to the size of pennies was reported at Norwood Road and Mount Vernon Church Road.   Quarter size hail covered the ground in Pittsboro. Quarter size hail occurred at Dwight Rowland Road and Highway 42. Nickel size hail was reported on Bells Lake Road. Quarter size hail occurred at the intersection of 2 Claude Road and Honeycutt Road. Emergency management reported 4 homes were damaged by falling trees in and to the north of Pittsboro. Numerous trees were blown down in a corridor from Pittsboro north and east to Ferrington. Several cars were damaged by falling trees with one person trapped in a vehicle just north of Pittsboro on NC Highway 87. Wind speeds were estimated to be near 70 mph.",
+        "The following events were reported: Hail. These occurred near station USW00013722, approximately 27.3945 km away, between 2008-05-31 16:32:00 and 2008-05-31 17:44:00. The events included records with hailstones measuring 1.1883333333333332 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Scattered thunderstorms developed along a lee side trough located over the Western Piedmont of North Carolina during the afternoon of May 31. Enough shear was in place to allow for the organization of severe thunderstorms, which primarily produced large hail across the northwest and northern Piedmont. Scattered thunderstorms developed along a lee side trough located over the Western Piedmont of North Carolina during the afternoon of May 31. Enough shear was in place to allow for the organization of severe thunderstorms, which primarily produced large hail across the northwest and northern Piedmont. Scattered thunderstorms developed along a lee side trough located over the Western Piedmont of North Carolina during the afternoon of May 31. Enough shear was in place to allow for the organization of severe thunderstorms, which primarily produced large hail across the northwest and northern Piedmont. Scattered thunderstorms developed along a lee side trough located over the Western Piedmont of North Carolina during the afternoon of May 31. Enough shear was in place to allow for the organization of severe thunderstorms, which primarily produced large hail across the northwest and northern Piedmont. Scattered thunderstorms developed along a lee side trough located over the Western Piedmont of North Carolina during the afternoon of May 31. Enough shear was in place to allow for the organization of severe thunderstorms, which primarily produced large hail across the northwest and northern Piedmont. Scattered thunderstorms developed along a lee side trough located over the Western Piedmont of North Carolina during the afternoon of May 31. Enough shear was in place to allow for the organization of severe thunderstorms, which primarily produced large hail across the northwest and northern Piedmont.\nEvent Narrative:  Quarter size hail was reported at Sandlewood Drive and Highway 501. Penny size hail was reported on Tom Oakley Road. Two waves of large hail occurred with a severe thunderstorm. The largest hail measured was close to ping pong ball sized. Half dollar size hail occurred on Denfield Road.",
+        "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00013722, approximately 20.9178 km away, between 2008-06-01 17:25:00 and 2008-06-01 18:26:00. The events included records with hailstones measuring 33.583333333333336 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Scattered thunderstorms developed in an unstable airmass and were focused along a surface trough in the vicinity of U.S. Highway 1. Some of the storms became severe, producing large hail and damaging winds. Scattered thunderstorms developed in an unstable airmass and were focused along a surface trough in the vicinity of U.S. Highway 1. Some of the storms became severe, producing large hail and damaging winds. Scattered thunderstorms developed in an unstable airmass and were focused along a surface trough in the vicinity of U.S. Highway 1. Some of the storms became severe, producing large hail and damaging winds. Scattered thunderstorms developed in an unstable airmass and were focused along a surface trough in the vicinity of U.S. Highway 1. Some of the storms became severe, producing large hail and damaging winds. Scattered thunderstorms developed in an unstable airmass and were focused along a surface trough in the vicinity of U.S. Highway 1. Some of the storms became severe, producing large hail and damaging winds. Scattered thunderstorms developed in an unstable airmass and were focused along a surface trough in the vicinity of U.S. Highway 1. Some of the storms became severe, producing large hail and damaging winds.\nEvent Narrative: Severe winds blew down large trees onto several homes on NC Highway 86. Penny size hail was reported on US Highway 70 near Linden Road. Large tree limbs were blown down onto Magnum Road. Numerous trees were reported down at the intersection of Norwood Road and Creedmoor Road. Straight line winds downed two large trees along Park Ridge Way. Penny size hail occurred at the intersection of Mitchell Mill Road and Forestville Road in the Wake Crossroads Area.",
+        "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00013722, approximately 33.8712 km away, between 2008-06-14 16:40:00 and 2008-06-14 18:09:00. The events included records with hailstones measuring 25.375 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Strong daytime heating fueled late afternoon convection as storms developed along a surface trough axis located across the central piedmont. Damaging thunderstorm wind gusts were frequently observed with the stronger cells with scattered reports of penny to nickel size hail. Strong daytime heating fueled late afternoon convection as storms developed along a surface trough axis located across the central piedmont. Damaging thunderstorm wind gusts were frequently observed with the stronger cells with scattered reports of penny to nickel size hail.\nEvent Narrative: One tree was blown down across Richardson Road near NC Highway 231. Penny size hail was reported near NC Highway 55 and South Salem Street.",
+        "The following events were reported: Hail. These occurred near station USW00013722, approximately 8.1923 km away, between 2008-06-21 16:00:00 and 2008-06-21 16:00:00. 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: Scattered showers and thunderstorms developed over Central North Carolina on the evening of June 21st. A few of the storms became severe and due to their slow motion isolated flash flooding was reported in western Wake County.\nEvent Narrative: Hail up to the size of pennies was reported at the intersection of Cary Parkway and Evans Road.",
+        "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00013722, approximately 33.8689 km away, between 2008-06-22 15:13:00 and 2008-06-22 15:40:00. The events included records with hailstones measuring 20.951999999999998 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: During the afternoon and evening hours of June 22nd, numerous showers and thunderstorms developed from the Triad east across the Triangle and sandhills. Due to the strength of the upper level disturbance and cold air aloft, nickel to golf ball size hail was reported. During the afternoon and evening hours of June 22nd, numerous showers and thunderstorms developed from the Triad east across the Triangle and sandhills. Due to the strength of the upper level disturbance and cold air aloft, nickel to golf ball size hail was reported. During the afternoon and evening hours of June 22nd, numerous showers and thunderstorms developed from the Triad east across the Triangle and sandhills. Due to the strength of the upper level disturbance and cold air aloft, nickel to golf ball size hail was reported. During the afternoon and evening hours of June 22nd, numerous showers and thunderstorms developed from the Triad east across the Triangle and sandhills. Due to the strength of the upper level disturbance and cold air aloft, nickel to golf ball size hail was reported. During the afternoon and evening hours of June 22nd, numerous showers and thunderstorms developed from the Triad east across the Triangle and sandhills. Due to the strength of the upper level disturbance and cold air aloft, nickel to golf ball size hail was reported.\nEvent Narrative: Numerous power lines were knocked down by high wind near Old Millstone Drive.  Nickel size hail was reported along Highway 86. Numerous trees were blown down across University Station Road, Old Highway 10, and New Hope Church Road. Quarter size hail was reported along Buckhorn Road.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 34.5487 km away, between 2008-06-23 17:40:00 and 2008-06-23 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: On the afternoon and evening of June 23rd isolated pulse severe thunderstorms developed over the eastern piedmont and northern coastal plain.\nEvent Narrative: A tree was reported blown down across Dairyland Road between Dodsons Crossroads and Rocky Ridge Road.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 15.7012 km away, between 2008-06-27 18:28:00 and 2008-06-27 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 few isolated severe thunderstorms developed across Central North Carolina along a weak front from near Winston Salem to Oxford and Halifax.\nEvent Narrative: A tree was blown down across the road at Winona Street near Falls of the Neuse Road.",
+        "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00013722, approximately 19.2763 km away, between 2008-06-29 18:22:00 and 2008-06-29 19:58:00. 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 line of thunderstorms, a few of which became severe, moved east across Central North Carolina from the Triad to the Triangle. These storms moving along a weak cold front produced a few areas of wind damage along with some hail. A line of thunderstorms, a few of which became severe, moved east across Central North Carolina from the Triad to the Triangle. These storms moving along a weak cold front produced a few areas of wind damage along with some hail. A line of thunderstorms, a few of which became severe, moved east across Central North Carolina from the Triad to the Triangle. These storms moving along a weak cold front produced a few areas of wind damage along with some hail. A line of thunderstorms, a few of which became severe, moved east across Central North Carolina from the Triad to the Triangle. These storms moving along a weak cold front produced a few areas of wind damage along with some hail.\nEvent Narrative: A tree was reported blown down into the intersection of Purnell Road and Bold Run Hill road. Penny size hail was reported near Highway 64 and Jordan Lake. Penny to nickel size hail was reported near the intersection of South Miami Boulevard and Alexander Drive. A tree was reported blown across the power lines and into the road at the intersection of Purnell Road and New Light Road.",
+        "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00013722, approximately 20.4411 km away, between 2008-07-04 19:52:00 and 2008-07-04 20:38:00. The events included records with hailstones measuring 40.176 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Organized convection rolled east off the mountains and foothills, into the Piedmont during the late afternoon and evening hours. The severe storms resulted in damaging thunderstorm winds from the Triad to the Triangle. Organized convection rolled east off the mountains and foothills, into the Piedmont during the late afternoon and evening hours. The severe storms resulted in damaging thunderstorm winds from the Triad to the Triangle. Organized convection rolled east off the mountains and foothills, into the Piedmont during the late afternoon and evening hours. The severe storms resulted in damaging thunderstorm winds from the Triad to the Triangle. Organized convection rolled east off the mountains and foothills, into the Piedmont during the late afternoon and evening hours. The severe storms resulted in damaging thunderstorm winds from the Triad to the Triangle. Organized convection rolled east off the mountains and foothills, into the Piedmont during the late afternoon and evening hours. The severe storms resulted in damaging thunderstorm winds from the Triad to the Triangle.\nEvent Narrative: Trees were blown down along Estes Drive and Hillsborough Road. Numerous trees were blown down on Green Hope School Road near Twila Road.|Some of the trees resulted in scattered power outages. Numerous trees were blown down along Perkins Road and off of Academy Road between Pincrest Road and Wrightwood Avenue. Nickel size hail was reported at South Miami Boulevard and US Highway 70. Trees were blown down on Pokomoke Road in West Franklinton.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 11.5325 km away, between 2008-07-05 15:33:00 and 2008-07-05 15:36:00. 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: Slow moving thunderstorms that developed along a stationary surface boundary caused flash flooding, several instances of damaging thunderstorm winds, and large quarter-size hail.\nEvent Narrative: Trees were blown down on Hope Valley Road and Waterford Valley Drive.",
+        "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00013722, approximately 17.2077 km away, between 2008-07-06 17:13:00 and 2008-07-06 17:23:00. The events included records with hailstones measuring 25.375 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Numerous thunderstorms developed in the moist and highly unstable airmass that was in place across central North Carolina. A measured thunderstorm wind gust of 72 mph highlighted the event, with only two reports of large hail up to the size of quarters. Numerous thunderstorms developed in the moist and highly unstable airmass that was in place across central North Carolina. A measured thunderstorm wind gust of 72 mph highlighted the event, with only two reports of large hail up to the size of quarters.\nEvent Narrative: Penny-size hail was reported on Tower Hamlet Drive. Power lines were blown down near the intersection of Person and Peace Streets.",
+        "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00013722, approximately 35.9801 km away, between 2008-07-08 18:54:00 and 2008-07-08 19:44:00. The events included records with hailstones measuring 30.326 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Widespread thunderstorms developed during peak heating as an upper level low transverse east across central North Carolina. The storms produced widespread thunderstorm wind damage and a few reports of large hail. As the severe event winded down, areas began to experience flash flooding from training thunderstorms. Widespread thunderstorms developed during peak heating as an upper level low transverse east across central North Carolina. The storms produced widespread thunderstorm wind damage and a few reports of large hail. As the severe event winded down, areas began to experience flash flooding from training thunderstorms. Widespread thunderstorms developed during peak heating as an upper level low transverse east across central North Carolina. The storms produced widespread thunderstorm wind damage and a few reports of large hail. As the severe event winded down, areas began to experience flash flooding from training thunderstorms. Widespread thunderstorms developed during peak heating as an upper level low transverse east across central North Carolina. The storms produced widespread thunderstorm wind damage and a few reports of large hail. As the severe event winded down, areas began to experience flash flooding from training thunderstorms. Widespread thunderstorms developed during peak heating as an upper level low transverse east across central North Carolina. The storms produced widespread thunderstorm wind damage and a few reports of large hail. As the severe event winded down, areas began to experience flash flooding from training thunderstorms.\nEvent Narrative: One tree was blown down across Brack Penny Road near NC-Highway 50 and 42. A trained spotter measured a 58 mph wind gust at the intersection of Holland Church Road and Feldmen Road. One tree was blown down on Lamont Norwood Road near Rockwood Lane. Two reports of penny to nickel-size hail near US Higway 401 and near the intersection of Chalybeate Springs Road and LaFayette Road.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 28.854 km away, between 2008-07-09 16:54:00 and 2008-07-09 18:38:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Strong convective developed along the higher terrain and in the lee of the  Appalachians during the afternoon. The storms and their associated outflow boundaries drifted east into the western and central piedmont, resulting in numerous reports of damaging thunderstorm wind gusts from the Triad to the Triangle. Strong convective developed along the higher terrain and in the lee of the  Appalachians during the afternoon. The storms and their associated outflow boundaries drifted east into the western and central piedmont, resulting in numerous reports of damaging thunderstorm wind gusts from the Triad to the Triangle. Strong convective developed along the higher terrain and in the lee of the  Appalachians during the afternoon. The storms and their associated outflow boundaries drifted east into the western and central piedmont, resulting in numerous reports of damaging thunderstorm wind gusts from the Triad to the Triangle. Strong convective developed along the higher terrain and in the lee of the  Appalachians during the afternoon. The storms and their associated outflow boundaries drifted east into the western and central piedmont, resulting in numerous reports of damaging thunderstorm wind gusts from the Triad to the Triangle. Strong convective developed along the higher terrain and in the lee of the  Appalachians during the afternoon. The storms and their associated outflow boundaries drifted east into the western and central piedmont, resulting in numerous reports of damaging thunderstorm wind gusts from the Triad to the Triangle.\nEvent Narrative: One tree was blown down across US Highway 15-501 near exit 106. One tree was blown down across Sanders Road near Belltown Road. A 68 mph wind gust was measured on Purnell Road. One tree was blown down across White Oak Road near the White Oak Shopping Center. Law enforcement reported downed trees on power-lines along NC-HWY 86 near Rocky Lane.",
+        "The following events were reported: Hail, Lightning, Thunderstorm Wind. These occurred near station USW00013722, approximately 40.6586 km away, between 2008-07-21 16:00:00 and 2008-07-22 18:30:00. The events included records with hailstones measuring 28.91142857142857 inches.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 180000.0 and crop damage of 0.0. \n\nEpisode Narrative: A very hot and humid airmass featuring afternoon temperatures in the middle to upper 90s resulted in a very buoyant airmass. A cluster of convection developed along a remnant MCS outflow boundary that transversed the area. Large hail up to the size of ping-pong balls was reported with widespread thunderstorm wind damage. The climax of the event was when minor injuries were reported when a tree fell onto a house in Hoke County, trapping 4 individual for more than an hour. A very hot and humid airmass featuring afternoon temperatures in the middle to upper 90s resulted in a very buoyant airmass. A cluster of convection developed along a remnant MCS outflow boundary that transversed the area. Large hail up to the size of ping-pong balls was reported with widespread thunderstorm wind damage. The climax of the event was when minor injuries were reported when a tree fell onto a house in Hoke County, trapping 4 individual for more than an hour. A very hot and humid airmass featuring afternoon temperatures in the middle to upper 90s resulted in a very buoyant airmass. A cluster of convection developed along a remnant MCS outflow boundary that transversed the area. Large hail up to the size of ping-pong balls was reported with widespread thunderstorm wind damage. The climax of the event was when minor injuries were reported when a tree fell onto a house in Hoke County, trapping 4 individual for more than an hour. A very hot and humid airmass featuring afternoon temperatures in the middle to upper 90s resulted in a very buoyant airmass. A cluster of convection developed along a remnant MCS outflow boundary that transversed the area. Large hail up to the size of ping-pong balls was reported with widespread thunderstorm wind damage. The climax of the event was when minor injuries were reported when a tree fell onto a house in Hoke County, trapping 4 individual for more than an hour. A very hot and humid airmass featuring afternoon temperatures in the middle to upper 90s resulted in a very buoyant airmass. A cluster of convection developed along a remnant MCS outflow boundary that transversed the area. Large hail up to the size of ping-pong balls was reported with widespread thunderstorm wind damage. The climax of the event was when minor injuries were reported when a tree fell onto a house in Hoke County, trapping 4 individual for more than an hour. A very hot and humid airmass featuring afternoon temperatures in the middle to upper 90s resulted in a very buoyant airmass. A cluster of convection developed along a remnant MCS outflow boundary that transversed the area. Large hail up to the size of ping-pong balls was reported with widespread thunderstorm wind damage. The climax of the event was when minor injuries were reported when a tree fell onto a house in Hoke County, trapping 4 individual for more than an hour. A very hot and humid airmass featuring afternoon temperatures in the middle to upper 90s resulted in a very buoyant airmass. A cluster of convection developed along a remnant MCS outflow boundary that transversed the area. Large hail up to the size of ping-pong balls was reported with widespread thunderstorm wind damage. The climax of the event was when minor injuries were reported when a tree fell onto a house in Hoke County, trapping 4 individual for more than an hour. A very hot and humid airmass featuring afternoon temperatures in the middle to upper 90s resulted in a very buoyant airmass. A cluster of convection developed along a remnant MCS outflow boundary that transversed the area. Large hail up to the size of ping-pong balls was reported with widespread thunderstorm wind damage. The climax of the event was when minor injuries were reported when a tree fell onto a house in Hoke County, trapping 4 individual for more than an hour.\nEvent Narrative: Nickel-size hail was reported at Covered Bridge Road and Coharie Drive. One tree was blown down at Somerset Place and Contender Drive. One tree was blown down on Old Milburnie Road.  KDTF AWOS at the Person County Airport, measured a 58 mph wind gust. Penny-size hail was reported on Interstate 540 near Highway 264. Trees were blown down on Corinth Road. A vacant house in the Buffalo Creek Subdivision of Zebulon caught on fire after it was hit by lightning. Another nearby home on Amsterdam Drive was also hit by lightning.",
+        "The following events were reported: Hail. These occurred near station USW00013722, approximately 46.2754 km away, between 2008-07-23 19:35:00 and 2008-07-23 19:35:00. 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: Pre-frontal convection broke out across central North Carolina early in the day, as a weak cold front approached from the west. Another round of storms developed late in the afternoon and evening with the approach of  the upper level trough. There were a few reports of penny-size hail and  minor thunderstorm wind damage.\nEvent Narrative:",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 25.1738 km away, between 2008-07-27 21:45:00 and 2008-07-27 22:11:00. 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: Scattered afternoon and late evening thunderstorms developed over the area. The combination of strong instability with steep low-level lapse rates produced large hail and damaging downbursts in the stronger storms.\nEvent Narrative: Several trees were blown down across southern portions of the county. Two trees were blown down on Oak Grove Church Road. Two additional trees were blown down on Martin Luther King Jr. Blvd and near the intersection of Caswell and Clayton Roads.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 33.9879 km away, between 2008-07-31 14:00:00 and 2008-07-31 15:10:00. 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: A linear convective cluster that initially formed along the Blue Ridge of North Carolina, intensified as it surged east through the area. Thunderstorm wind gust produced wind damage from the Triad to the coast. A linear convective cluster that initially formed along the Blue Ridge of North Carolina, intensified as it surged east through the area. Thunderstorm wind gust produced wind damage from the Triad to the coast. A linear convective cluster that initially formed along the Blue Ridge of North Carolina, intensified as it surged east through the area. Thunderstorm wind gust produced wind damage from the Triad to the coast.\nEvent Narrative: Several trees and power-lines were blown down on Joe Denton Road. One Pine tree was blown down across the road at the intersection of Old Guess Road and Rose of Sharon Road. One tree was blown down on Old Route 75.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 48.2867 km away, between 2008-08-02 13:00:00 and 2008-08-02 14:51:00. 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 moving into the Mid Atlantic and Northeast, skirted just north of central North Carolina on the afternoon of August 2nd. The trough passage was close enough to trigger scattered showers and thunderstorms during peak heating. Some of the storms became severe, producing large hail, damaging winds, and flash flooding across portions of the western Piedmont, the Sandhills, and the southern Coastal Plain of North Carolina. An upper level trough moving into the Mid Atlantic and Northeast, skirted just north of central North Carolina on the afternoon of August 2nd. The trough passage was close enough to trigger scattered showers and thunderstorms during peak heating. Some of the storms became severe, producing large hail, damaging winds, and flash flooding across portions of the western Piedmont, the Sandhills, and the southern Coastal Plain of North Carolina. An upper level trough moving into the Mid Atlantic and Northeast, skirted just north of central North Carolina on the afternoon of August 2nd. The trough passage was close enough to trigger scattered showers and thunderstorms during peak heating. Some of the storms became severe, producing large hail, damaging winds, and flash flooding across portions of the western Piedmont, the Sandhills, and the southern Coastal Plain of North Carolina.\nEvent Narrative: Several trees were blown down across the city of Mebane. A tree was blown down across the intersection of NC Highway 49 and 86. Straight line winds downed a tree through a house along NC Highway 96 north just to the northwest of Emit.",
+        "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00013722, approximately 30.8499 km away, between 2008-08-10 17:05:00 and 2008-08-10 17:25:00. 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 weak cold front and a potent upper level trough moved into an unstable airmass over central North Carolina during the evening of August 10th. Scattered showers and thunderstorms developed and some of them became severe. There were numerous reports of downed trees and up to quarter size hail. Torrential rains also caused flash flooding in Cumberland and Sampson counties during the early morning hours of August 11th. A weak cold front and a potent upper level trough moved into an unstable airmass over central North Carolina during the evening of August 10th. Scattered showers and thunderstorms developed and some of them became severe. There were numerous reports of downed trees and up to quarter size hail. Torrential rains also caused flash flooding in Cumberland and Sampson counties during the early morning hours of August 11th. A weak cold front and a potent upper level trough moved into an unstable airmass over central North Carolina during the evening of August 10th. Scattered showers and thunderstorms developed and some of them became severe. There were numerous reports of downed trees and up to quarter size hail. Torrential rains also caused flash flooding in Cumberland and Sampson counties during the early morning hours of August 11th.\nEvent Narrative: A tree was knocked down onto West Lyon Station Road. In addition, large limbs were downed along NC Highway 56. Nickel size hail was reported near Moores Mill Road and Highway 501. Just to the southwest, quarter size hail was reported at Bahama Road and Country Knoll Road. A severe thunderstorm knocked down trees onto Bahama Road.",
+        "The following events were reported: Lightning, Thunderstorm Wind. These occurred near station USW00013722, approximately 16.5671 km away, between 2008-08-15 14:55:00 and 2008-08-15 15:12:00.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 215000.0 and crop damage of 0.0. \n\nEpisode Narrative: During the afternoon of August 15th a few isolated severe thunderstorms developed along the piedmont trough resulting in wind damage and several home fires from lightning. During the afternoon of August 15th a few isolated severe thunderstorms developed along the piedmont trough resulting in wind damage and several home fires from lightning. During the afternoon of August 15th a few isolated severe thunderstorms developed along the piedmont trough resulting in wind damage and several home fires from lightning.\nEvent Narrative: Several trees were blown down at the intersection of Highway 64 and New Hill Road. Fire crews responded to a tree which fell onto a parked vehicle near Durant Road and Mount Vernon Church Road. The car was unoccupied at the time. Two homes struck by lightning in the Raleigh caught fire resulting in extensive damage to each home.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 18.2033 km away, between 2008-08-20 16:25:00 and 2008-08-20 16:25:00. 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: The passage of a weak cold front produce an isolated severe thunderstorm which affected the city of Raleigh in the early evening of August 20th.\nEvent Narrative: A large tree was snapped and fell across Ingram Drive at Brentwood Elementary School in Raleigh. Several other trees were downed in the vicinity of the school.",
+        "The following events were reported: Flash Flood, Tornado. These occurred near station USW00013722, approximately 32.1281 km away, between 2008-08-27 12:44:00 and 2008-08-28 01:45:00.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: The remnants of Hurricane Fay which made landfall along the Louisiana coast moved northeast across central North Carolina producing several weak tornadoes along with significant flash flooding. The remnants of Hurricane Fay which made landfall along the Louisiana coast moved northeast across central North Carolina producing several weak tornadoes along with significant flash flooding. The remnants of Hurricane Fay which made landfall along the Louisiana coast moved northeast across central North Carolina producing several weak tornadoes along with significant flash flooding. The remnants of Hurricane Fay which made landfall along the Louisiana coast moved northeast across central North Carolina producing several weak tornadoes along with significant flash flooding. The remnants of Hurricane Fay which made landfall along the Louisiana coast moved northeast across central North Carolina producing several weak tornadoes along with significant flash flooding.\nEvent Narrative: Numerous roads were closed due to flooding in the Durham area. Cabin Creek just north of Durham flooded several areas including Highway 501 between Smith Drive and Northern High School. The Ponds Dam overflowed near Tracey Trail Road and Highway 501. This caused extensive flooding of the Eden Lake subdivision. Several homes experienced up to two feet of water in them. Several roads in Bunter were closed due to flooding including West C street. Several roads in Fuquay Varina were flooded including Sunset lake Road. Local fire deparments and law enforcement reported a brief tornado touchdown near the intersection of Covered Bridge Road and Thanksgiving Road. Multiple trees were snapped and uprooted in the highly wooded area. Denny Store Road was flooded by over a foot of water and was closed by NCDOT.",
+        "The following events were reported: Flash Flood, Hail, Thunderstorm Wind. These occurred near station USW00013722, approximately 12.5048 km away, between 2008-08-30 18:25:00 and 2008-08-30 20:45:00. 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 moist and moderately unstable air mass over central North Carolina in conjunction with a weakening mid level disturbance triggered scattered thunderstorms across the northern Piedmont and Coastal Plain. A few of the storms became severe, causing flash flooding along with isolated wind damage and hail. A moist and moderately unstable air mass over central North Carolina in conjunction with a weakening mid level disturbance triggered scattered thunderstorms across the northern Piedmont and Coastal Plain. A few of the storms became severe, causing flash flooding along with isolated wind damage and hail. A moist and moderately unstable air mass over central North Carolina in conjunction with a weakening mid level disturbance triggered scattered thunderstorms across the northern Piedmont and Coastal Plain. A few of the storms became severe, causing flash flooding along with isolated wind damage and hail. A moist and moderately unstable air mass over central North Carolina in conjunction with a weakening mid level disturbance triggered scattered thunderstorms across the northern Piedmont and Coastal Plain. A few of the storms became severe, causing flash flooding along with isolated wind damage and hail.\nEvent Narrative:  Severe straight line winds knocked down several trees across Morrisville Carpenter Road near Davis Drive. Flooding was reported on South Saunders Street and Martin Luther King Boulevard in downtown Raleigh. A portion of Avent Ferry Road near North Carolina State University was also flooded. Flash flooding from heavy rain caused Morrisville Carpenter Road to be closed between Davis Drive and Town Hall Drive.",
+        "The following events were reported: Flash Flood. These occurred near station USW00013722, approximately 16.1488 km away, between 2008-09-06 00:30:00 and 2008-09-06 09:30:00.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 250000.0 and crop damage of 0.0. \n\nEpisode Narrative: During the early morning hours Tropical Storm Hanna made landfall near Myrtle Beach, South Carolina. The tropical storm tracked north into Central North Carolina from daybreak through noon tracking along Interstate 95. Peak wind gusts of 40 to 50 mph were recorded over the coastal plain and eastern piedmont. four to seven inches of rain which fell over the eastern piedmont resulted in flash flooding over large areas including the Triangle. During the early morning hours Tropical Storm Hanna made landfall near Myrtle Beach, South Carolina. The tropical storm tracked north into Central North Carolina from daybreak through noon tracking along Interstate 95. Peak wind gusts of 40 to 50 mph were recorded over the coastal plain and eastern piedmont. four to seven inches of rain which fell over the eastern piedmont resulted in flash flooding over large areas including the Triangle. During the early morning hours Tropical Storm Hanna made landfall near Myrtle Beach, South Carolina. The tropical storm tracked north into Central North Carolina from daybreak through noon tracking along Interstate 95. Peak wind gusts of 40 to 50 mph were recorded over the coastal plain and eastern piedmont. four to seven inches of rain which fell over the eastern piedmont resulted in flash flooding over large areas including the Triangle. During the early morning hours Tropical Storm Hanna made landfall near Myrtle Beach, South Carolina. The tropical storm tracked north into Central North Carolina from daybreak through noon tracking along Interstate 95. Peak wind gusts of 40 to 50 mph were recorded over the coastal plain and eastern piedmont. four to seven inches of rain which fell over the eastern piedmont resulted in flash flooding over large areas including the Triangle.\nEvent Narrative: Up to seven inches of rain caused flash flooding in many locations across Raleigh particularly along Crabtree Creek and other flood prone areas. A motorist was rescued from a vehicle after driving into a flooded underpass at Hillsborough Drive and Chapel Drive in west Raleigh.  Sullivan Drive between Dan Allen and Varsity Drive was closed due to flooding along with Avent Ferry Road at Trailwood Drive. Numerous Creeks across the region flooded low lying areas as well as some vehicles. Several roads were flooded east and south of Durham including Mineral Springs Road and Fletchers Chapel Road. In southwest Durham flood waters reached a few buildings at Durham Academy. Several roads north of Durham were closed due to flooding including Snowhill Road and Snow Valley Road. The intersection of Erwin Road and Mount Moriah Road was closed due to flooding. Flood waters also caused the evacuation of the Camelot Apartments at Estes Drive. A few vehicles were flooded in the area.",
+        "The following events were reported: Heavy Rain, Lightning. These occurred near station USW00013722, approximately 20.7278 km away, between 2008-12-11 12:05:00 and 2008-12-11 16:30:00.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 1500000.0 and crop damage of 0.0. \n\nEpisode Narrative: A powerful upper level disturbance with associated cold front pushed across the region the afternoon and evening of December 11. Over 2 inches of rain fell in many locations with several reports of minor urban flooding. One house was struck by lightning and burned to the ground. A powerful upper level disturbance with associated cold front pushed across the region the afternoon and evening of December 11. Over 2 inches of rain fell in many locations with several reports of minor urban flooding. One house was struck by lightning and burned to the ground.\nEvent Narrative: Law enforcement reported one foot of water over the road near the intersection of East Millbrook and Quail Hollow roads. Lightning struck a home in Chapel Hill and caught fire. The house burned to the ground when the lightning got into the gas lines of the home.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 37.0476 km away, between 2009-01-28 16:40:00 and 2009-01-28 16:40:00. 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 100000.0 and crop damage of 0.0. \n\nEpisode Narrative: A convective line of showers produced damaging wind gusts across|eastern North Carolina as a strong cold front moved east across the state.\nEvent Narrative: Damaging straight-line winds ripped the roof off the Sunday school building of Franklinton Baptist Church. A tree also fell on a vehicle in the church daycare parking lot.",
+        "The following events were reported: Tornado. These occurred near station USW00013722, approximately 48.4889 km away, between 2009-03-27 18:20:00 and 2009-03-27 18:21:00.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 0.0 and crop damage of 15000.0. \n\nEpisode Narrative: Low topped tornadic supercells developed along a stationary front located across the coastal plain region of North Carolina. The storms intensified as a shortwave trough moved northeast across the area, producing EF-1 damage in Cumberland County.\nEvent Narrative: Numerous trees were blown down and snapped in a wooded area behind an open field.",
+        "The following events were reported: Hail. These occurred near station USW00013722, approximately 45.9173 km away, between 2009-04-20 14:45:00 and 2009-04-20 15:30:00. The events included records with hailstones measuring 0.815 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Scattered to numerous showers and thunderstorms developed across the Central North Carolina as a cold front moved through the region. The|strongest cells developed across northern portions of the Piedmont and Coastal Plain. where hail as large as baseballs was reported in Granville County. Scattered to numerous showers and thunderstorms developed across the Central North Carolina as a cold front moved through the region. The|strongest cells developed across northern portions of the Piedmont and Coastal Plain. where hail as large as baseballs was reported in Granville County.\nEvent Narrative: Trained spotter reported nickel size hail in Efland near the intersection of High Rock Road and East Lebanon Road. Berea Fire Department reported penny size hail on Highway 158.",
+        "The following events were reported: Flash Flood, Flood, Hail, Thunderstorm Wind. These occurred near station USW00013722, approximately 15.6251 km away, between 2009-05-05 17:04:00 and 2009-05-05 19:30:00. The events included records with hailstones measuring 13.1575 inches. 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: Two tornadic supercells developed along a stalled warm front that extended across souther piedmont and coastal plain of North Carolina.|The cells produced 4 tornadoes in Johnston, Nash and Wilson counties. Two tornadic supercells developed along a stalled warm front that extended across souther piedmont and coastal plain of North Carolina.|The cells produced 4 tornadoes in Johnston, Nash and Wilson counties. Two tornadic supercells developed along a stalled warm front that extended across souther piedmont and coastal plain of North Carolina.|The cells produced 4 tornadoes in Johnston, Nash and Wilson counties. Two tornadic supercells developed along a stalled warm front that extended across souther piedmont and coastal plain of North Carolina.|The cells produced 4 tornadoes in Johnston, Nash and Wilson counties. Two tornadic supercells developed along a stalled warm front that extended across souther piedmont and coastal plain of North Carolina.|The cells produced 4 tornadoes in Johnston, Nash and Wilson counties. Two tornadic supercells developed along a stalled warm front that extended across souther piedmont and coastal plain of North Carolina.|The cells produced 4 tornadoes in Johnston, Nash and Wilson counties. Two tornadic supercells developed along a stalled warm front that extended across souther piedmont and coastal plain of North Carolina.|The cells produced 4 tornadoes in Johnston, Nash and Wilson counties. Two tornadic supercells developed along a stalled warm front that extended across souther piedmont and coastal plain of North Carolina.|The cells produced 4 tornadoes in Johnston, Nash and Wilson counties.\nEvent Narrative: Quarter sized hail was reported near Knightdale Boulevard and Village Squire Court. Trees were reported down on Jenks-Carpenter Road and Burgwin Wright Way. Penny sized hail was reported at the Morrisville Town Hall and Fire Department. Nickel sized hail was reported near Spring Forecast Road and Falls of Neuse Road. Flash flooding was reported at the Preston Wood Golf Course. Two to three feet of water was reported over Atlantic Avenue at Highwoods Boulevard. One vehicle was reported stalled in the flood waters. One foot of flowing water was reported across Capitol Boulevard at Old Buffaloe Road. One to two feet of water was reported standing in Medfield Subdivision.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 22.6703 km away, between 2009-05-09 17:00:00 and 2009-05-09 17:57:00. 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 cluster of storms developed across central North Carolina downstream of a shortwave trough located over eastern Tennessee. The severe storms produced widespread wind damage with only one report of severe hail. A cluster of storms developed across central North Carolina downstream of a shortwave trough located over eastern Tennessee. The severe storms produced widespread wind damage with only one report of severe hail. A cluster of storms developed across central North Carolina downstream of a shortwave trough located over eastern Tennessee. The severe storms produced widespread wind damage with only one report of severe hail. A cluster of storms developed across central North Carolina downstream of a shortwave trough located over eastern Tennessee. The severe storms produced widespread wind damage with only one report of severe hail. A cluster of storms developed across central North Carolina downstream of a shortwave trough located over eastern Tennessee. The severe storms produced widespread wind damage with only one report of severe hail. A cluster of storms developed across central North Carolina downstream of a shortwave trough located over eastern Tennessee. The severe storms produced widespread wind damage with only one report of severe hail. A cluster of storms developed across central North Carolina downstream of a shortwave trough located over eastern Tennessee. The severe storms produced widespread wind damage with only one report of severe hail. A cluster of storms developed across central North Carolina downstream of a shortwave trough located over eastern Tennessee. The severe storms produced widespread wind damage with only one report of severe hail. A cluster of storms developed across central North Carolina downstream of a shortwave trough located over eastern Tennessee. The severe storms produced widespread wind damage with only one report of severe hail. A cluster of storms developed across central North Carolina downstream of a shortwave trough located over eastern Tennessee. The severe storms produced widespread wind damage with only one report of severe hail. A cluster of storms developed across central North Carolina downstream of a shortwave trough located over eastern Tennessee. The severe storms produced widespread wind damage with only one report of severe hail. A cluster of storms developed across central North Carolina downstream of a shortwave trough located over eastern Tennessee. The severe storms produced widespread wind damage with only one report of severe hail. A cluster of storms developed across central North Carolina downstream of a shortwave trough located over eastern Tennessee. The severe storms produced widespread wind damage with only one report of severe hail. A cluster of storms developed across central North Carolina downstream of a shortwave trough located over eastern Tennessee. The severe storms produced widespread wind damage with only one report of severe hail. A cluster of storms developed across central North Carolina downstream of a shortwave trough located over eastern Tennessee. The severe storms produced widespread wind damage with only one report of severe hail. A cluster of storms developed across central North Carolina downstream of a shortwave trough located over eastern Tennessee. The severe storms produced widespread wind damage with only one report of severe hail. A cluster of storms developed across central North Carolina downstream of a shortwave trough located over eastern Tennessee. The severe storms produced widespread wind damage with only one report of severe hail. A cluster of storms developed across central North Carolina downstream of a shortwave trough located over eastern Tennessee. The severe storms produced widespread wind damage with only one report of severe hail.\nEvent Narrative: Trees and power lines were blown down on Legion Road. One tree 6 to 8 inches in diameter was blown down onto power lines on Martin Luther King Jr. Parkway near Roxboro Street. Several trees were blown down at White Cross Fire Department. One large tree was blown down and blocking traffic on Glendale Drive. Two trees were blown down at Angier Avenue and Discovery Road. Shingles were blown off the roof of a house at Highway 98 and South Miami Boulevard. Down tree blocking tracking on Creedmore Road, between Strickland and Bridgeport Roads. A six inch limb was blown down onto powerlines at Woodbury Drive and Hillcock Drive. One pine tree was blown down onto power lines near the intersection of Schely Road and New Sharon Church Road. Trees and power-lines were blown down inside the Raleigh city limits. |The down trees and power-lines resulted in scattered power outages and blocked traffic. One tree fell onto a house near the intersection of Method Road and Western Boulevard. Several trees were blown down across the Stage Coach Road and Farrington Road. Two downed trees were blocking traffic. The first downed tree was located near the intersection of Highway 401 and Spring Forest Road. The second downed tree was blocking south bound lanes on Leesville Road between West|Gate Road and Strickland Road. A 50 Foot tree was snapped off 7 feet from the base of tree along Cedar Creek Road. One large tree approximately 2 feet in diameter was snapped in half on Jenkins Road and Fullard Drive. Trees and power lines were blown down on Buckner Road and along Highway 64 around Pittsboro. A large tree and several power lines were blown down and blocking traffic|at Mebane Oaks Road and Bradshaw Quarry Road. Two trees were uprooted at Martin Luther King Jr. Parkway and Fayetteville Street. Fourteen inch diameter tree fell on a house at Chandler Court off of Becketts Ridge Drive.",
+        "The following events were reported: Hail. These occurred near station USW00013722, approximately 21.0807 km away, between 2009-06-02 16:02:00 and 2009-06-02 16:30:00. The events included records with hailstones measuring 1.1266666666666667 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A weak upper level disturbance over the area coupled with strong afternoon insolation produced isolated severe storms over central North Carolina. A weak upper level disturbance over the area coupled with strong afternoon insolation produced isolated severe storms over central North Carolina. A weak upper level disturbance over the area coupled with strong afternoon insolation produced isolated severe storms over central North Carolina.\nEvent Narrative: Quarter size hail was reported at the intersection of Roxboro Road and Lavender Road.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 38.7183 km away, between 2009-06-09 21:06:00 and 2009-06-09 22:00:00. 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: Initial storms developed along a surface trough axis across central and eastern portions of North Carolina. Additional thunderstorms then developed later in the afternoon and evening as a weak upper level shortwave trough moved east across the area.  There was widespread thunderstorm wind damage with the most significant damage concentrated |in the Triad. Flash flooding became a threat during the evening in the northeast coastal plain with several streets closed in Edgecombe and Halifax Counties. Initial storms developed along a surface trough axis across central and eastern portions of North Carolina. Additional thunderstorms then developed later in the afternoon and evening as a weak upper level shortwave trough moved east across the area.  There was widespread thunderstorm wind damage with the most significant damage concentrated |in the Triad. Flash flooding became a threat during the evening in the northeast coastal plain with several streets closed in Edgecombe and Halifax Counties.\nEvent Narrative: One tree was blown down along Highway 15-501. One tree was blown down across Orange Grove Road. There were other trees down in central portions of the county.",
+        "The following events were reported: Flash Flood. These occurred near station USW00013722, approximately 15.0729 km away, between 2009-06-16 05:34:00 and 2009-06-16 10:30:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Strong warm and moist air advection along the leading nose of a southerly low-level jet|and atop a stationary warm front in place across central North Carolina resulted in|heavy rainfall of 3 to 4 inches. The heaviest rainfall occurred over the Raleigh area |causing mainly urban and small stream flooding. Strong warm and moist air advection along the leading nose of a southerly low-level jet|and atop a stationary warm front in place across central North Carolina resulted in|heavy rainfall of 3 to 4 inches. The heaviest rainfall occurred over the Raleigh area |causing mainly urban and small stream flooding.\nEvent Narrative: Numerous roads closed due to flash flooding in and around Raleigh. Rescuers evacuated |15 to 20 occupants at the Southgate Community Center and surrounding apartments due to high flood waters from Walnut Creek. Rescue crews evacuated 60 occupants from the Brookhill Town House Apartments on Dana Drive due to high flood waters.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 19.4722 km away, between 2009-06-17 22:45:00 and 2009-06-17 22:45:00. 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: Storms developed along a stalled warm surface boundary late in the evening, persisting well into the overnight hours. Back-building thunderstorms resulted in flash flooding as 5 to 6 inches of rainfall fell over Randolph and northern Moore counties.\nEvent Narrative: A few trees were blown down near Fall Lakes blocking two roads in the area.",
+        "The following events were reported: Hail, Lightning, Thunderstorm Wind. These occurred near station USW00013722, approximately 20.9348 km away, between 2009-07-01 22:10:00 and 2009-07-01 22:46:00. The events included records with hailstones measuring 33.666666666666664 inches.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 8000.0 and crop damage of 0.0. \n\nEpisode Narrative: A strong upper level disturbance and attendant surface cold front combined to produce scattered showers and thunderstorms across the eastern half of central North Carolina. The unseasonably dry low levels of the atmosphere across central North Carolina created a favorable environment for any thunderstorms that developed to produce damaging winds. Many of the thunderstorms that developed became severe and produced damaging winds across the eastern half of central North Carolina. A strong upper level disturbance and attendant surface cold front combined to produce scattered showers and thunderstorms across the eastern half of central North Carolina. The unseasonably dry low levels of the atmosphere across central North Carolina created a favorable environment for any thunderstorms that developed to produce damaging winds. Many of the thunderstorms that developed became severe and produced damaging winds across the eastern half of central North Carolina. A strong upper level disturbance and attendant surface cold front combined to produce scattered showers and thunderstorms across the eastern half of central North Carolina. The unseasonably dry low levels of the atmosphere across central North Carolina created a favorable environment for any thunderstorms that developed to produce damaging winds. Many of the thunderstorms that developed became severe and produced damaging winds across the eastern half of central North Carolina. A strong upper level disturbance and attendant surface cold front combined to produce scattered showers and thunderstorms across the eastern half of central North Carolina. The unseasonably dry low levels of the atmosphere across central North Carolina created a favorable environment for any thunderstorms that developed to produce damaging winds. Many of the thunderstorms that developed became severe and produced damaging winds across the eastern half of central North Carolina.\nEvent Narrative: A tree was reported down on a house in the 400 block of North King Charles Road, in Raleigh, North Carolina. Quarter sized hail was reported in the Bedford Subdivison, near the intersection of Cardington Lane and Rogerson Street. Power lines were reported down on Van Buren Road, at North State Street. A town home fire was reported on Canvas Drive in Raleigh, North Carolina, which was caused by an apparent lightning strike that that ran in on the natural gas line. Damage to the town home was unknown.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 44.6728 km away, between 2009-07-12 18:05:00 and 2009-07-12 18:10:00. 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: Strong daytime heating featuring afternoon temperatures in the mid to upper 90s resulted in moderate instability across central North Carolina. Isolated convection|developed along a pre-frontal surface trough. Strong daytime heating featuring afternoon temperatures in the mid to upper 90s resulted in moderate instability across central North Carolina. Isolated convection|developed along a pre-frontal surface trough.\nEvent Narrative: Two trees were blown down along Route 157 near Hurdle Mills. Two trees were blown down near Moores Mill and Rassie Crabtree Roads.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 27.8649 km away, between 2009-07-17 13:07:00 and 2009-07-17 16:45:00. 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: Organized line segments and supercells produced widespread thunderstorm wind damage across central North Carolina as a strong upper shortwave trough and associated 50 to 60 knot mid-level jet streak spread into the area. Organized line segments and supercells produced widespread thunderstorm wind damage across central North Carolina as a strong upper shortwave trough and associated 50 to 60 knot mid-level jet streak spread into the area. Organized line segments and supercells produced widespread thunderstorm wind damage across central North Carolina as a strong upper shortwave trough and associated 50 to 60 knot mid-level jet streak spread into the area. Organized line segments and supercells produced widespread thunderstorm wind damage across central North Carolina as a strong upper shortwave trough and associated 50 to 60 knot mid-level jet streak spread into the area. Organized line segments and supercells produced widespread thunderstorm wind damage across central North Carolina as a strong upper shortwave trough and associated 50 to 60 knot mid-level jet streak spread into the area.\nEvent Narrative: One tree was blown down on Jones Street in downtown Raleigh. Two twenty-foot trees were uprooted at Edenton and McDowell Streets. One tree was blown down at the intersection of Hillsborough Street and Pullen Road. Numerous trees snapped along Highway 30 between Richardson Road and Corinth Holders Fire Station. Numerous trees were blown down and snapped along a one mile stretch along Highway 501 at Red Mountain Road to the intersection of Moores Mill Road.",
+        "The following events were reported: Hail. These occurred near station USW00013722, approximately 35.9881 km away, between 2009-07-20 15:55:00 and 2009-07-20 16:55:00. 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: A cluster of convection developed across central North Carolina as a large upper trough and upper jet translated east across the area. Large severe hail up to the size of golf ball was reported with thunderstorm wind damage responsible for structural damage to area homes in Moore County. A cluster of convection developed across central North Carolina as a large upper trough and upper jet translated east across the area. Large severe hail up to the size of golf ball was reported with thunderstorm wind damage responsible for structural damage to area homes in Moore County.\nEvent Narrative:",
+        "The following events were reported: Hail. These occurred near station USW00013722, approximately 45.7767 km away, between 2009-07-23 22:05:00 and 2009-07-23 22:05:00. 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: An upper level shortwave trough moved through the deep upper level trough over the Eastern United States and through central North Carolina on July 23, 2009, which helped to sharpen up a surface trough over central North Carolina and produce scattered showers and thunderstorms across the area. Some of these storms became severe and produced damaging winds and large hail to the size of quarters.\nEvent Narrative: Nickel sized hail was reported Indian Camp Road and Polenta Road.",
+        "The following events were reported: Hail. These occurred near station USW00013722, approximately 38.6385 km away, between 2009-07-25 16:25:00 and 2009-07-25 16:25:00. 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: Intense surface heating along with a surface trough across eastern portions of central North Carolina produced scattered showers and thunderstorms across the coastal plain of North Carolina. Some of these storms became severe and produced hail to the size of nickel and damaging winds. These storms also produced very heavy rain, and several reports of flash flooding.\nEvent Narrative: Nickel sized hail was reported at the intersection of North Carolina Highway 42 and Amelia Church Road.",
+        "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00013722, approximately 34.0528 km away, between 2009-07-27 15:15:00 and 2009-07-27 15:25:00. The events included records with hailstones measuring 36.916666666666664 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Several bands of strong to severe thunderstorms developed across central North Carolina as a a shortwave trough moved across the region. The severe threat quickly |transformed from a hail threat early in the event to a damaging wind episode as shortwave mid-level kinematics increased over the area. Several bands of strong to severe thunderstorms developed across central North Carolina as a a shortwave trough moved across the region. The severe threat quickly |transformed from a hail threat early in the event to a damaging wind episode as shortwave mid-level kinematics increased over the area. Several bands of strong to severe thunderstorms developed across central North Carolina as a a shortwave trough moved across the region. The severe threat quickly |transformed from a hail threat early in the event to a damaging wind episode as shortwave mid-level kinematics increased over the area.\nEvent Narrative:  Several trees were blown down along NC Highway 42 and Hill Top Road. Numerous trees were blown down along Old Stage Road, Panther Lake Road and Eddie Howard Road. One tree fell onto a car along Old Stage Road.",
+        "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00013722, approximately 16.5738 km away, between 2009-07-28 18:15:00 and 2009-07-28 19:30:00. The events included records with hailstones measuring 33.626666666666665 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A warm and moist atmosphere coupled with an lee side trough caused scattered showers and thunderstorms to develop across central North Carolina. As a MCS induced shortwave moved into the region from the west during the late afternoon and evening, some of the storms became severe and produced numerous reports of damaging winds and one report of hail. A warm and moist atmosphere coupled with an lee side trough caused scattered showers and thunderstorms to develop across central North Carolina. As a MCS induced shortwave moved into the region from the west during the late afternoon and evening, some of the storms became severe and produced numerous reports of damaging winds and one report of hail. A warm and moist atmosphere coupled with an lee side trough caused scattered showers and thunderstorms to develop across central North Carolina. As a MCS induced shortwave moved into the region from the west during the late afternoon and evening, some of the storms became severe and produced numerous reports of damaging winds and one report of hail.\nEvent Narrative: One tree was reported down at North Carolina Highway 98 and United States Highway 401. Nickel sized hail was reported at the corner of Glenwood Avenue and Ebenezer Church Road. A two in diameter tree was reported down at the intersection of Chapel Hill Road and West Maynard Road, along with an estimated wind gust of 70 mile per hour.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 13.0521 km away, between 2009-07-30 13:34:00 and 2009-07-30 13:34:00. 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: An upper level disturbance interacted with warm moist unstable atmosphere across central North Carolina and a lee side trough to produce scattered showers and thunderstorms. One of these thunderstorms became severe and produced wind damage in the town of Cary, NC.\nEvent Narrative: Trees were reported in the intersection of West Chatham Street and Southwest Maynard Road in Cary, North Carolina.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 30.4407 km away, between 2009-07-31 12:45:00 and 2009-07-31 13:20:00. 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 100000.0 and crop damage of 0.0. \n\nEpisode Narrative: A moist and unstable air mass was in place across central North Carolina as several bands of convection developed ahead of an upper trough and associated surface cold front. Across the coastal plain region, the sea breeze spread inland merging with  |with existing convection, and further enhancing the severe wind threat. A moist and unstable air mass was in place across central North Carolina as several bands of convection developed ahead of an upper trough and associated surface cold front. Across the coastal plain region, the sea breeze spread inland merging with  |with existing convection, and further enhancing the severe wind threat. A moist and unstable air mass was in place across central North Carolina as several bands of convection developed ahead of an upper trough and associated surface cold front. Across the coastal plain region, the sea breeze spread inland merging with  |with existing convection, and further enhancing the severe wind threat.\nEvent Narrative: One tree was blown down onto power-lines along Highway 55 and Springstone Drive. Several trees were blown down in the Clayton area. Several trees were blown down on homes along Skymont Drive.",
+        "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00013722, approximately 40.5138 km away, between 2009-08-05 12:48:00 and 2009-08-05 14:05:00. The events included records with hailstones measuring 13.1575 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A piedmont surface trough and approaching upper level shortwave produced numerous showers and thunderstorms in a warm moist unstable atmosphere across central North Carolina. Many of these thunderstorms became severe and produced heavy rain, damaging winds, and large hail. A piedmont surface trough and approaching upper level shortwave produced numerous showers and thunderstorms in a warm moist unstable atmosphere across central North Carolina. Many of these thunderstorms became severe and produced heavy rain, damaging winds, and large hail. A piedmont surface trough and approaching upper level shortwave produced numerous showers and thunderstorms in a warm moist unstable atmosphere across central North Carolina. Many of these thunderstorms became severe and produced heavy rain, damaging winds, and large hail. A piedmont surface trough and approaching upper level shortwave produced numerous showers and thunderstorms in a warm moist unstable atmosphere across central North Carolina. Many of these thunderstorms became severe and produced heavy rain, damaging winds, and large hail.\nEvent Narrative: Quarter sized hail was reported at the intersection of North Carolina Highway 42 and Christian Chapel Church Road. One tree was reported down across Lower River Road, near Moncure, North Carolina. Penny to nickel sized hail was reported at the intersection of Old Stage Road and Rock Service Station Road. Penny size hail was reported on Wilburn Road, near United States Highway 401.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 38.7052 km away, between 2009-08-11 16:08:00 and 2009-08-11 17:45:00. 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 5000.0 and crop damage of 0.0. \n\nEpisode Narrative: An approaching mid level trough and attendant cold front allowed warm moist air to filter into the region. Scattered showers developed across the foothills in the vicinity of a lee side trough, and moved eastward and across central North Carolina. Some of these storms became severe and produced numerous reports of damaging winds and one report of penny hail. An approaching mid level trough and attendant cold front allowed warm moist air to filter into the region. Scattered showers developed across the foothills in the vicinity of a lee side trough, and moved eastward and across central North Carolina. Some of these storms became severe and produced numerous reports of damaging winds and one report of penny hail. An approaching mid level trough and attendant cold front allowed warm moist air to filter into the region. Scattered showers developed across the foothills in the vicinity of a lee side trough, and moved eastward and across central North Carolina. Some of these storms became severe and produced numerous reports of damaging winds and one report of penny hail. An approaching mid level trough and attendant cold front allowed warm moist air to filter into the region. Scattered showers developed across the foothills in the vicinity of a lee side trough, and moved eastward and across central North Carolina. Some of these storms became severe and produced numerous reports of damaging winds and one report of penny hail. An approaching mid level trough and attendant cold front allowed warm moist air to filter into the region. Scattered showers developed across the foothills in the vicinity of a lee side trough, and moved eastward and across central North Carolina. Some of these storms became severe and produced numerous reports of damaging winds and one report of penny hail. An approaching mid level trough and attendant cold front allowed warm moist air to filter into the region. Scattered showers developed across the foothills in the vicinity of a lee side trough, and moved eastward and across central North Carolina. Some of these storms became severe and produced numerous reports of damaging winds and one report of penny hail. An approaching mid level trough and attendant cold front allowed warm moist air to filter into the region. Scattered showers developed across the foothills in the vicinity of a lee side trough, and moved eastward and across central North Carolina. Some of these storms became severe and produced numerous reports of damaging winds and one report of penny hail. An approaching mid level trough and attendant cold front allowed warm moist air to filter into the region. Scattered showers developed across the foothills in the vicinity of a lee side trough, and moved eastward and across central North Carolina. Some of these storms became severe and produced numerous reports of damaging winds and one report of penny hail. An approaching mid level trough and attendant cold front allowed warm moist air to filter into the region. Scattered showers developed across the foothills in the vicinity of a lee side trough, and moved eastward and across central North Carolina. Some of these storms became severe and produced numerous reports of damaging winds and one report of penny hail. An approaching mid level trough and attendant cold front allowed warm moist air to filter into the region. Scattered showers developed across the foothills in the vicinity of a lee side trough, and moved eastward and across central North Carolina. Some of these storms became severe and produced numerous reports of damaging winds and one report of penny hail.\nEvent Narrative: One tree was reported down across Old Route 75. Several trees were reported down in the town of Oxford, North Carolina. One tree was reported down on a car at United States Highway 401 and Bennett Perry Road. Numerous trees were reported down across Franklin County, North Carolina. One tree was reported down across Dobsons Crossroads at Dairyland Road. Numerous trees were reported down across Granville County. Several trees were reported down in the town of Bunn, North Carolina. One tree was reported down on Pembridge Lane at Long Acre Drive. One tree was reported down on Brassfield Road. Twelve inch diameter tree was reported down on Yarborough Road.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 13.1319 km away, between 2009-08-17 15:53:00 and 2009-08-17 15:53:00. 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: Isolated severe thunderstorms developed across central North Carolina as a weak upper level disturbance tracked across the area and interacted with a warm moist atmosphere.\nEvent Narrative: One tree was reported down on Western Boulevard and Hunt Club Lane.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 39.8543 km away, between 2009-08-22 10:35:00 and 2009-08-22 10:43:00. 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 deep mid/upper level trough propelled a cold front into central North Carolina, which sparked scattered showers and thunderstorms in a moist and unstable atmosphere. Some of these storms became severe and produced damaging winds. A deep mid/upper level trough propelled a cold front into central North Carolina, which sparked scattered showers and thunderstorms in a moist and unstable atmosphere. Some of these storms became severe and produced damaging winds.\nEvent Narrative: One tree was reported down across Walnut Grove Church Road at Wilkerson Road. One tree was reported down at the 4800 block of Orange Grove Road.",
+        "The following events were reported: Flash Flood. These occurred near station USW00013722, approximately 31.324 km away, between 2009-09-22 19:40:00 and 2009-09-23 01:00:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Locally heavy rainfall of 5 to 6 inches developed with the approach of an upper level shortwave and along a stalled surface trough. The heavy rainfall resulted in isolated flooding across southern Wake and northern Harnett county.\nEvent Narrative: A portion of Piney Grove Wilbon Road between Avent Ferry Road and NC Highway 42 was impassable due to flood waters.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 30.9353 km away, between 2009-09-28 17:15:00 and 2009-09-28 17:50:00. 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 strong cold front and powerful upper level trough swept across central North Carolina late in the afternoon into the early evening hours on September 28, 2009. A band of showers and thunderstorms formed as the cold front moved east of the mountains and into central North Carolina. Some of these storms became severe and produced damaging winds and hail to the size of nickels. A strong cold front and powerful upper level trough swept across central North Carolina late in the afternoon into the early evening hours on September 28, 2009. A band of showers and thunderstorms formed as the cold front moved east of the mountains and into central North Carolina. Some of these storms became severe and produced damaging winds and hail to the size of nickels. A strong cold front and powerful upper level trough swept across central North Carolina late in the afternoon into the early evening hours on September 28, 2009. A band of showers and thunderstorms formed as the cold front moved east of the mountains and into central North Carolina. Some of these storms became severe and produced damaging winds and hail to the size of nickels. A strong cold front and powerful upper level trough swept across central North Carolina late in the afternoon into the early evening hours on September 28, 2009. A band of showers and thunderstorms formed as the cold front moved east of the mountains and into central North Carolina. Some of these storms became severe and produced damaging winds and hail to the size of nickels.\nEvent Narrative: One tree was blown down across NC Highway 50 north of the Wake County line.|Other large limbs were also down in the area. One tree was reported down on Martin Luther King Boulevard and Critz Drive. One tree was reported down on Chestnut Ridge Church Road at Holmes Road. One tree was reported down at 3722 Old Greensboro Road.",
+        "The following events were reported: Flash Flood. These occurred near station USW00013722, approximately 18.8028 km away, between 2009-12-02 23:00:00 and 2009-12-03 02:00:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Deep boundary layer moisture transport of Gulf of Mexico and Atlantic moisture|ahead of an intense mid and upper level shortwave trough ejecting northeastward|across the deep south resulted in minor flooding as a swath of heavy rainfall of 2 to 3 inches fell across the central Piedmont. Deep boundary layer moisture transport of Gulf of Mexico and Atlantic moisture|ahead of an intense mid and upper level shortwave trough ejecting northeastward|across the deep south resulted in minor flooding as a swath of heavy rainfall of 2 to 3 inches fell across the central Piedmont. Deep boundary layer moisture transport of Gulf of Mexico and Atlantic moisture|ahead of an intense mid and upper level shortwave trough ejecting northeastward|across the deep south resulted in minor flooding as a swath of heavy rainfall of 2 to 3 inches fell across the central Piedmont. Deep boundary layer moisture transport of Gulf of Mexico and Atlantic moisture|ahead of an intense mid and upper level shortwave trough ejecting northeastward|across the deep south resulted in minor flooding as a swath of heavy rainfall of 2 to 3 inches fell across the central Piedmont. Deep boundary layer moisture transport of Gulf of Mexico and Atlantic moisture|ahead of an intense mid and upper level shortwave trough ejecting northeastward|across the deep south resulted in minor flooding as a swath of heavy rainfall of 2 to 3 inches fell across the central Piedmont. Deep boundary layer moisture transport of Gulf of Mexico and Atlantic moisture|ahead of an intense mid and upper level shortwave trough ejecting northeastward|across the deep south resulted in minor flooding as a swath of heavy rainfall of 2 to 3 inches fell across the central Piedmont.\nEvent Narrative: Avent Ferry Road and Gorman Street were closed due to two to three feet of flowing flood waters from local creek. The intersection of Hillsborough Street and Western Blvd. was closed due to flash flood waters. Minor flooding of Crabtree Creek over spilled into the lower level parking lot of Crabtree Creek Mall. Several streets inside the Franklinton city limits were closed due to flash flooding. Flash flooding was reported at Fletchers Chapel Road and Mineral Springs Road. Several feet of flood water was reported in several yards in Crenshaw Manor Subdivision from Richland Creek.",
+        "The following events were reported: Flash Flood, Thunderstorm Wind. These occurred near station USW00013722, approximately 25.6937 km away, between 2010-01-25 03:28:00 and 2010-01-25 06:15:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Heavy rain and severe thunderstorms overspread central North Carolina during the late evening hours of the 24th and into the overnight hours as a slow moving cold front approached from the west. Two to three inches of rain caused flash flooding across  the western and central Piedmont. A convective bow segment also produced localized thunderstorm wind damage in Johnston County. Heavy rain and severe thunderstorms overspread central North Carolina during the late evening hours of the 24th and into the overnight hours as a slow moving cold front approached from the west. Two to three inches of rain caused flash flooding across  the western and central Piedmont. A convective bow segment also produced localized thunderstorm wind damage in Johnston County. Heavy rain and severe thunderstorms overspread central North Carolina during the late evening hours of the 24th and into the overnight hours as a slow moving cold front approached from the west. Two to three inches of rain caused flash flooding across  the western and central Piedmont. A convective bow segment also produced localized thunderstorm wind damage in Johnston County. Heavy rain and severe thunderstorms overspread central North Carolina during the late evening hours of the 24th and into the overnight hours as a slow moving cold front approached from the west. Two to three inches of rain caused flash flooding across  the western and central Piedmont. A convective bow segment also produced localized thunderstorm wind damage in Johnston County.\nEvent Narrative: Flash flooding was reported on Old NC Highway 86 just north of Eubanks Road. Flash flooding was reported on Hillsborough Street near Gardner Street. Ramp from Dawson Street onto Western Boulevard was flooded. A vehicle was also stranded in the flood waters. Multiple trees were blown down on NC Highway 42 near Selma Road.",
+        "The following events were reported: Flood. These occurred near station USW00013722, approximately 43.2546 km away, between 2010-02-05 00:00:00 and 2010-02-06 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: Heavy rain falling across portions of Central North Carolina resulted in minor flooding across several counties along with a number of road closures.\nEvent Narrative: Heavy rain resulted in widespread minor flooding across the county. Several roads were closed due to flooding including the intersection of Covered Bridge Road and Buffalo Road.",
+        "The following events were reported: Flash Flood, Lightning, Thunderstorm Wind, Tornado. These occurred near station USW00013722, approximately 43.3462 km away, between 2010-03-28 22:55:00 and 2010-03-29 09:00:00.The events resulted in 0 injuries and 2 fatalities. The events caused property damage valued at 325000.0 and crop damage of 0.0. \n\nEpisode Narrative: Convection developed ahead of an amplified upper trough across the Tennessee Valley|while a strong southerly mid and upper level jet provided strong shear across the region. Tornadoes formed and track ahead of a developing surface low across Georgia and along a wedge front located across the western Piedmont of NC. Convection developed ahead of an amplified upper trough across the Tennessee Valley|while a strong southerly mid and upper level jet provided strong shear across the region. Tornadoes formed and track ahead of a developing surface low across Georgia and along a wedge front located across the western Piedmont of NC. Convection developed ahead of an amplified upper trough across the Tennessee Valley|while a strong southerly mid and upper level jet provided strong shear across the region. Tornadoes formed and track ahead of a developing surface low across Georgia and along a wedge front located across the western Piedmont of NC. Convection developed ahead of an amplified upper trough across the Tennessee Valley|while a strong southerly mid and upper level jet provided strong shear across the region. Tornadoes formed and track ahead of a developing surface low across Georgia and along a wedge front located across the western Piedmont of NC.\nEvent Narrative: Lightning struck three full sized pine trees where the runners then ripped through the electrical heating and air conditioning compressor behind the house before entering the home through its exterior receptacles. The electrical wiring through the home was completely destroyed. The lightning also severely damaged a full size SUV. Two teenagers drowned when their car hydroplaned, flipped and came to rest in a swollen swampy area. The vehicle was submerged. The passenger was found inside the car, with her seat belt on, while the driver's body was found by a water rescue team 150 feet away from the car. Five trees were blown down on Bushy Creek Road near Interstate 85. The tornado initially touched down as a EF0 with wind speeds rated 70 to 80 mph along Fire Tower Road near Moores Mill Road in extreme southwest Person County. The tornado then moved northeast crossing Helena-Moriah Road. Numerous trees were sheared off a quarter to halfway up. ||The tornado continued to move northeast where it struck a subdivision off Stoney Mountain Road.  Several trees were twisted off and uprooted. Two modular homes sustained damage when trees fell on them. The worst damage occurred as the tornado moved northeast across Medford Oakley Road. Numerous Pines and Hardwoods were snapped off and uprooted. A modular home was also moved off its foundation. The tornado reached EF1 strength here with estimated winds of 90 to 100 mph. ||The tornado then moved into a wooded area where it produced minor damage to an old barn before dissipating.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 41.5508 km away, between 2010-04-08 19:55:00 and 2010-04-08 20:00:00. 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: Scattered showers and thunderstorms developed over the North Carolina mountains and foothills during the afternoon before moving into the western Piedmont during the evening. The storms were focused along a strong low-level jet, in advance of an upper level trough and attendant surface cold front. A dry boundary layer featuring surface dewpoints in the 50s combined with steep lapse rates supported an increase wind threat.\nEvent Narrative: Two trees were reported blown down near the intersection of Brookhollow Road at  Lebanon Road and Highway 86 at Efland-Cedar Grove Road.",
+        "The following events were reported: Tornado. These occurred near station USW00013722, approximately 41.9056 km away, between 2010-04-25 18:59:00 and 2010-04-25 19:06:00.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 250000.0 and crop damage of 25000.0. \n\nEpisode Narrative: An isolated cell formed over Moore County in advance of a strong surface cold front in a high shear and moderate CAPE environment. The lone storm strengthened into a  super cell over central Wake County before it produced a weak EF0 tornado near Zebulon in eastern Wake County.\nEvent Narrative: The tornado initially touched down near Bell Street just west of Glaxo-Smith-Klein and the Zebulon municipal building. Both of these facilities experienced large fallen trees which damaged fencing but no structural damage occurred to any of the buildings. One oak tree at the municipal building was around 4 feet in diameter. The tornado moved east across Highway 96/North Arendell Avenue where it caused|minor damage to several businesses in the Triangle East Center. A McDonald's, Pizza Hut and other businesses in the shopping center experienced very minor damage. A four hundred pound condenser on the roof of the McDonald's was moved sideways. A couple of vehicles in the shopping center parking lot were moved about 10-15 feet and a number of vehicles had their windows shattered by debris from the tornado. Tornado wind speeds in the shopping center were around 70 mph. The tornado crossed Highway 64/264 near Shepards School Road traveling parallel to Highway 64/264 before crossing Old Bunn Road. Numerous trees were blown down and one shed was destroyed along Old Bunn Road. The strongest tornado damage was evident at 1311 Old Bunn Road where a home sustained a fair amount of minor roof damage when a carport collapsed and numerous outbuildings were destroyed by a combination of tornadic winds and falling trees. Winds in this area were estimated at  around 80 mph. After striking the residence on Old Bunn Road the tornado again crossed highway 64 eventually crossing Parks Village Road where another large hardwood fell destroying an outbuilding. The tornado then moved into a swampy area before crossing Highway 39 just north of the intersection of Highway 39 and Highway 97. Numerous trees at a residence on Highway 39 were uprooted or snapped. A|home in the area lost several shingles and some siding was damaged. Winds in this area were around 70 to 75 mph. The tornado moved into southern Franklin County for a short distance before lifting off the ground.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 49.6446 km away, between 2010-05-06 20:24:00 and 2010-05-06 20:24:00. 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: Isolated severe thunderstorms developed along a pre-frontal trough of low pressure during afternoon peak heating on May 06th.\nEvent Narrative: Multiple trees were reported down on Crawford Road in Mebane, NC.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 49.8169 km away, between 2010-05-15 23:05:00 and 2010-05-15 23:05:00. 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: Showers and Thunderstorms developed across portions of the North Carolina Mountains and Foothills and move east and into the North Carolina Piedmont and Sandhills in the late afternoon into the evening on May 15th. Some of these storms became strong to severe as an upper level disturbance tracked across the Western Piedmont and Western Sandhills producing damaging winds and large hail.\nEvent Narrative: Several trees were blown down just outside of Mebane, NC.",
+        "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00013722, approximately 40.9299 km away, between 2010-05-16 15:10:00 and 2010-05-16 15:40:00. The events included records with hailstones measuring 33.583333333333336 inches.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 30000.0 and crop damage of 0.0. \n\nEpisode Narrative: Strong to severe thunderstorms developed along a stalled surface front. A cell merger resulted in a strong wet microburst that resulted in extensive damage at a mobile home park in Hoke County. Strong to severe thunderstorms developed along a stalled surface front. A cell merger resulted in a strong wet microburst that resulted in extensive damage at a mobile home park in Hoke County. Strong to severe thunderstorms developed along a stalled surface front. A cell merger resulted in a strong wet microburst that resulted in extensive damage at a mobile home park in Hoke County.\nEvent Narrative: A tree fell onto a mobile home on Old Sanford Road causing significant damage. A roof of a livestock feed store was blown off by thunderstorm winds.",
+        "The following events were reported: Flash Flood, Thunderstorm Wind. These occurred near station USW00013722, approximately 24.7088 km away, between 2010-05-22 17:00:00 and 2010-05-22 20:00:00.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: Weak perturbation aloft rotated through the cyclonic flow across the region and interacted with a warm moist unstable atmosphere to produce scattered showers and thunderstorms. Some of these storms produced wind damage and flash flooding across portions of the Northern Piedmont of central North Carolina. Weak perturbation aloft rotated through the cyclonic flow across the region and interacted with a warm moist unstable atmosphere to produce scattered showers and thunderstorms. Some of these storms produced wind damage and flash flooding across portions of the Northern Piedmont of central North Carolina. Weak perturbation aloft rotated through the cyclonic flow across the region and interacted with a warm moist unstable atmosphere to produce scattered showers and thunderstorms. Some of these storms produced wind damage and flash flooding across portions of the Northern Piedmont of central North Carolina. Weak perturbation aloft rotated through the cyclonic flow across the region and interacted with a warm moist unstable atmosphere to produce scattered showers and thunderstorms. Some of these storms produced wind damage and flash flooding across portions of the Northern Piedmont of central North Carolina.\nEvent Narrative: Flooding was reported along Moores Mill Road. One tree was reported down at the intersection of Ellis Road and South Miami Boulevard. Flooding was reported at the intersection of Hurdle Mills Road and Charlie Monk Road. Multiple trees were reported down at the intersection of Olive Branch Road and Doc Nichols Road near the Oak Grove Community.",
+        "The following events were reported: Hail. These occurred near station USW00013722, approximately 24.6534 km away, between 2010-05-23 14:10:00 and 2010-05-23 17:16:00. The events included records with hailstones measuring 0.9166666666666666 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: An upper level disturbance crossed the area during peak heating and interacted with a warm moist unstable air mass which produced scattered to numerous showers and thunderstorms across central North Carolina. Some of these storms were severe and produced large hail and damaging winds. An upper level disturbance crossed the area during peak heating and interacted with a warm moist unstable air mass which produced scattered to numerous showers and thunderstorms across central North Carolina. Some of these storms were severe and produced large hail and damaging winds. An upper level disturbance crossed the area during peak heating and interacted with a warm moist unstable air mass which produced scattered to numerous showers and thunderstorms across central North Carolina. Some of these storms were severe and produced large hail and damaging winds.\nEvent Narrative: Penny sized hail was reported near the intersection of Yates Mill Pond Road and Woodard Lane. Quarter sized hail was reported near Barrys Cafe on Jones Franklin Road. The quarter hail lasted for 10 to 15 minutes. Nickel to quarter sized hail was reported along Belltown Road near Smith Road.",
+        "The following events were reported: Flash Flood, Hail, Lightning, Thunderstorm Wind. These occurred near station USW00013722, approximately 26.4405 km away, between 2010-05-28 20:50:00 and 2010-05-29 00:00:00. The events included records with hailstones measuring 37.74 inches.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 280000.0 and crop damage of 0.0. \n\nEpisode Narrative: A slow moving cold front dropped south and into central North Carolina on May 28th. Showers and thunderstorms developed ahead of the front across southern portions Virginia during the afternoon. Outflow from these showers and thunderstorms propagated southward and combined with convective outflows from convection that developed across portions of the foothills and mountains of North Carolina to produce widespread showers and thunderstorms. Some of these stomrs produced damaging wind gust. A slow moving cold front dropped south and into central North Carolina on May 28th. Showers and thunderstorms developed ahead of the front across southern portions Virginia during the afternoon. Outflow from these showers and thunderstorms propagated southward and combined with convective outflows from convection that developed across portions of the foothills and mountains of North Carolina to produce widespread showers and thunderstorms. Some of these stomrs produced damaging wind gust. A slow moving cold front dropped south and into central North Carolina on May 28th. Showers and thunderstorms developed ahead of the front across southern portions Virginia during the afternoon. Outflow from these showers and thunderstorms propagated southward and combined with convective outflows from convection that developed across portions of the foothills and mountains of North Carolina to produce widespread showers and thunderstorms. Some of these stomrs produced damaging wind gust. A slow moving cold front dropped south and into central North Carolina on May 28th. Showers and thunderstorms developed ahead of the front across southern portions Virginia during the afternoon. Outflow from these showers and thunderstorms propagated southward and combined with convective outflows from convection that developed across portions of the foothills and mountains of North Carolina to produce widespread showers and thunderstorms. Some of these stomrs produced damaging wind gust. A slow moving cold front dropped south and into central North Carolina on May 28th. Showers and thunderstorms developed ahead of the front across southern portions Virginia during the afternoon. Outflow from these showers and thunderstorms propagated southward and combined with convective outflows from convection that developed across portions of the foothills and mountains of North Carolina to produce widespread showers and thunderstorms. Some of these stomrs produced damaging wind gust. A slow moving cold front dropped south and into central North Carolina on May 28th. Showers and thunderstorms developed ahead of the front across southern portions Virginia during the afternoon. Outflow from these showers and thunderstorms propagated southward and combined with convective outflows from convection that developed across portions of the foothills and mountains of North Carolina to produce widespread showers and thunderstorms. Some of these stomrs produced damaging wind gust. A slow moving cold front dropped south and into central North Carolina on May 28th. Showers and thunderstorms developed ahead of the front across southern portions Virginia during the afternoon. Outflow from these showers and thunderstorms propagated southward and combined with convective outflows from convection that developed across portions of the foothills and mountains of North Carolina to produce widespread showers and thunderstorms. Some of these stomrs produced damaging wind gust. A slow moving cold front dropped south and into central North Carolina on May 28th. Showers and thunderstorms developed ahead of the front across southern portions Virginia during the afternoon. Outflow from these showers and thunderstorms propagated southward and combined with convective outflows from convection that developed across portions of the foothills and mountains of North Carolina to produce widespread showers and thunderstorms. Some of these stomrs produced damaging wind gust. A slow moving cold front dropped south and into central North Carolina on May 28th. Showers and thunderstorms developed ahead of the front across southern portions Virginia during the afternoon. Outflow from these showers and thunderstorms propagated southward and combined with convective outflows from convection that developed across portions of the foothills and mountains of North Carolina to produce widespread showers and thunderstorms. Some of these stomrs produced damaging wind gust. A slow moving cold front dropped south and into central North Carolina on May 28th. Showers and thunderstorms developed ahead of the front across southern portions Virginia during the afternoon. Outflow from these showers and thunderstorms propagated southward and combined with convective outflows from convection that developed across portions of the foothills and mountains of North Carolina to produce widespread showers and thunderstorms. Some of these stomrs produced damaging wind gust. A slow moving cold front dropped south and into central North Carolina on May 28th. Showers and thunderstorms developed ahead of the front across southern portions Virginia during the afternoon. Outflow from these showers and thunderstorms propagated southward and combined with convective outflows from convection that developed across portions of the foothills and mountains of North Carolina to produce widespread showers and thunderstorms. Some of these stomrs produced damaging wind gust. A slow moving cold front dropped south and into central North Carolina on May 28th. Showers and thunderstorms developed ahead of the front across southern portions Virginia during the afternoon. Outflow from these showers and thunderstorms propagated southward and combined with convective outflows from convection that developed across portions of the foothills and mountains of North Carolina to produce widespread showers and thunderstorms. Some of these stomrs produced damaging wind gust. A slow moving cold front dropped south and into central North Carolina on May 28th. Showers and thunderstorms developed ahead of the front across southern portions Virginia during the afternoon. Outflow from these showers and thunderstorms propagated southward and combined with convective outflows from convection that developed across portions of the foothills and mountains of North Carolina to produce widespread showers and thunderstorms. Some of these stomrs produced damaging wind gust. A slow moving cold front dropped south and into central North Carolina on May 28th. Showers and thunderstorms developed ahead of the front across southern portions Virginia during the afternoon. Outflow from these showers and thunderstorms propagated southward and combined with convective outflows from convection that developed across portions of the foothills and mountains of North Carolina to produce widespread showers and thunderstorms. Some of these stomrs produced damaging wind gust. A slow moving cold front dropped south and into central North Carolina on May 28th. Showers and thunderstorms developed ahead of the front across southern portions Virginia during the afternoon. Outflow from these showers and thunderstorms propagated southward and combined with convective outflows from convection that developed across portions of the foothills and mountains of North Carolina to produce widespread showers and thunderstorms. Some of these stomrs produced damaging wind gust. A slow moving cold front dropped south and into central North Carolina on May 28th. Showers and thunderstorms developed ahead of the front across southern portions Virginia during the afternoon. Outflow from these showers and thunderstorms propagated southward and combined with convective outflows from convection that developed across portions of the foothills and mountains of North Carolina to produce widespread showers and thunderstorms. Some of these stomrs produced damaging wind gust.\nEvent Narrative: One tree was reported down near the intersection of Massey Chapel and Fayetteville Road. Power was also out at this location after the storm. Power line was reported downed on Cole Mill Road near Kimball Drive.||. Several trees were reported down on Jones Ferry Road in North Chatham County. Numerous trees were reported down at 7800 Massey Chapel Road. Nickel sized hail was reported in Southern Wake County. A lightning strike caused an electrical failure at a pump station near Durham, North Carolina. The electrical failure allowed 18,000 gallons of sewage to spill into the Eno River. A two-story log cabin burned down on Lake Hart Trail in Brassfield, NC. A lightning strike caused the fire. Firefighters took seven hours to put out the blaze and used 200,000 gallons of water. Quarter sized hail was reported at 3719 United States Highway 70 near Hillsborough, NC. Quarter sized hail was reported near Hillsborough, NC. Several trees were reported down at Cheek Road and Hardee Street. Several trees were reported down at 1100 Taylor Street in Durham, NC. Several trees were reported down at 500 North Hyde Park Avenue in Durham, NC. Multiple trees were reported down throughout the county, with the great concentration across Hillsborough, NC. A housing development off Rhonda Road in Hillsborough, NC had damage to numerous cars and homes. Widespread flooding was reported throughout the city of Durham, NC, including roads closed, water coming up through manhole covers and trash cans floating in the street. Some roads which were reported to be flooded included; the intersection of Neal road and Wildberry Lane, the intersection of United States Highway 15/501 and Hillsborough Road, Hillandale Road and Carver Road. In addition, cars were reported to be floating near I-85 and the Durham freeway, Hillandale Road and Carver Road, and Morreene Steet. Flooding also collapsed a roof at an apartment complex off of Crest Street. Flash flooding was reported on Barber Mill Road at Government Road, and along Polenta Road at McLemore Road and Indian Camp Road. Several trees were reported down at the intersection of Moore Road and Cleveland Road.",
+        "The following events were reported: Flash Flood. These occurred near station USW00013722, approximately 11.6271 km away, between 2010-06-01 15:15:00 and 2010-06-01 15:45:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: An afternoon thunderstorm resulted in isolated urban flash flooding in Raleigh.\nEvent Narrative: A spotter reported 2 feet of water at the underpass on Hillsborough Street and Interstate 40. Traffic was stopped and the underpass was impassable.",
+        "The following events were reported: Lightning. These occurred near station USW00013722, approximately 29.6288 km away, between 2010-06-02 14:20:00 and 2010-06-02 14:40:00.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 1025000.0 and crop damage of 0.0. \n\nEpisode Narrative: Strong to severe slow moving storms and merging storms resulted in severe damaging winds and flash flooding across portions of Central North Carolina. Frequent to excessive lightning resulted in property damage across the area to homes and businesses. Strong to severe slow moving storms and merging storms resulted in severe damaging winds and flash flooding across portions of Central North Carolina. Frequent to excessive lightning resulted in property damage across the area to homes and businesses.\nEvent Narrative: A tree was hit by lightning, split and caught fire at the Devils Ridge Golf Course. Lightning struck a home on the corner of Wilbon Ridge Drive and Brackney Trail in Holly Springs. The home caught fire causing extensive damage.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 35.343 km away, between 2010-06-13 16:40:00 and 2010-06-13 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 1000.0 and crop damage of 0.0. \n\nEpisode Narrative: A weak cold front moving across area resulted in a line of severe storms which tracked across Central North Carolina resulting in wind damage from Roxboro and the Triangle to the Coastal Plain. A weak cold front moving across area resulted in a line of severe storms which tracked across Central North Carolina resulting in wind damage from Roxboro and the Triangle to the Coastal Plain.\nEvent Narrative: Several trees were blown down onto power lines in Knightdale. At least 400 residences were without power as a result of the downed trees. A large tree was reported blown down on the 400 block of Hunter Lane in Zebulon.",
+        "The following events were reported: Lightning. These occurred near station USW00013722, approximately 14.9106 km away, between 2010-06-15 18:10:00 and 2010-06-15 18:10:00.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: A broken line of thunderstorms, some which were severe, tracked east across the Northwest and Eastern Piedmont. The storms were associated with a weak upper level disturbance which combined with afternoon heating.\nEvent Narrative: Two houses, one on Bell Arthur Drive and the other on Cove Creek Drive were struck by lightning which resulted in large three alarm fires.",
+        "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00013722, approximately 23.9827 km away, between 2010-06-16 13:45:00 and 2010-06-16 13:45:00. 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 cluster of thunderstorms generated severe winds near Greensboro as well as Creedmoor. Frequent lightning caused damage to the runway at the Piedmont Triad International Airport. A cluster of thunderstorms generated severe winds near Greensboro as well as Creedmoor. Frequent lightning caused damage to the runway at the Piedmont Triad International Airport.\nEvent Narrative: Quarter size hail fell near the corner of Coley Road and Running Brook Road. Several trees were reported blown down across Dove Road.",
+        "The following events were reported: Lightning. These occurred near station USW00013722, approximately 14.5973 km away, between 2010-06-22 18:15:00 and 2010-06-22 18:15:00.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 125000.0 and crop damage of 0.0. \n\nEpisode Narrative: Strong insolation underneath an oppressive upper level heat ridge resulted in isolated|pulse severe convection.\nEvent Narrative: A single lightning strike to a large tree growing between two homes caused significant fire damage to the the attic and second floor bedrooms of the home at 102 and 104 Arthur Drive.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 28.8259 km away, between 2010-06-23 12:55:00 and 2010-06-23 16:05:00. 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 convectively induced shortwave aided by steep low-level lapse rates triggered scattered multicellular convection across central North Carolina. Widespread thunderstorm wind damage was reported in Durham and Orange Counties. A convectively induced shortwave aided by steep low-level lapse rates triggered scattered multicellular convection across central North Carolina. Widespread thunderstorm wind damage was reported in Durham and Orange Counties. A convectively induced shortwave aided by steep low-level lapse rates triggered scattered multicellular convection across central North Carolina. Widespread thunderstorm wind damage was reported in Durham and Orange Counties.\nEvent Narrative: Numerous trees down across the county. Numerous trees down across the county. One tree fell onto a home on Hillandale Road.  An estimated two thousand customers in southern Durham, including The Streets of Southpoint Mall. A tree was blown onto power lines at Amelia Church Road and Shotwell Road.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 45.2238 km away, between 2010-06-29 15:19:00 and 2010-06-29 15:19:00. 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: Showers and thunderstorms developed during the afternoon along a pre-frontal trough of low pressure in a moist and unstable atmosphere. Many of the thunderstorms became severe as a upper level disturbance tracked across the area, resulting in widespread wind damage.\nEvent Narrative: Power lines were reported down along North Carolina Highway 50 near North Carolina Highway 210.",
+        "The following events were reported: Lightning. These occurred near station USW00013722, approximately 37.3975 km away, between 2010-07-08 16:20:00 and 2010-07-08 16:20:00.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: An upper level low near Cape Hatteras drifted west towards eastern North Carolina during the afternoon and evening hours. Cyclonic flow around the low combined with a warm and moist airmass resulted in scattered convection across portion of central North Carolina.\nEvent Narrative: A house was struck by lightning at 1052 Ridge Drive in Clayton. Damage was sustained by the house when fire damaged the attic and then proceeded to spread to a bedroom.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 32.9541 km away, between 2010-07-13 19:10:00 and 2010-07-13 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 3000.0 and crop damage of 0.0. \n\nEpisode Narrative: Strong to severe storms developed across central North Carolina as an upper level trough moved through the region. The Triad also experienced minor flash flooding in which an indirect fatality occurred when a infant drowned in a flooded creek. Strong to severe storms developed across central North Carolina as an upper level trough moved through the region. The Triad also experienced minor flash flooding in which an indirect fatality occurred when a infant drowned in a flooded creek. Strong to severe storms developed across central North Carolina as an upper level trough moved through the region. The Triad also experienced minor flash flooding in which an indirect fatality occurred when a infant drowned in a flooded creek.\nEvent Narrative: Several trees were blown down along a swath from just west of Hillsborough to near Schley. Also, a roof was blown off of a barn south of Caldwell. Several trees were blown down across the city of Gorman. Several trees were blown down across the city of Mebane.",
+        "The following events were reported: Lightning. These occurred near station USW00013722, approximately 22.4652 km away, between 2010-07-16 19:44:00 and 2010-07-16 19:44:00.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 broken line of showers and thunderstorms developed across western North Carolina during the afternoon and then moved east across central and eastern North Carolina during the evening hours.\nEvent Narrative: A house was struck by lightning. The fire was contained to the attic where it burned the interior roof.",
+        "The following events were reported: Lightning, Thunderstorm Wind. These occurred near station USW00013722, approximately 33.5492 km away, between 2010-07-17 10:10:00 and 2010-07-17 15:20:00.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: Thunderstorms developed across Virginia and central North Carolina as a small long lived MCS crossed the central and southern Appalachians. Widespread wind damage was reported across northern and central portions of central North Carolina. Thunderstorms developed across Virginia and central North Carolina as a small long lived MCS crossed the central and southern Appalachians. Widespread wind damage was reported across northern and central portions of central North Carolina. Thunderstorms developed across Virginia and central North Carolina as a small long lived MCS crossed the central and southern Appalachians. Widespread wind damage was reported across northern and central portions of central North Carolina. Thunderstorms developed across Virginia and central North Carolina as a small long lived MCS crossed the central and southern Appalachians. Widespread wind damage was reported across northern and central portions of central North Carolina. Thunderstorms developed across Virginia and central North Carolina as a small long lived MCS crossed the central and southern Appalachians. Widespread wind damage was reported across northern and central portions of central North Carolina. Thunderstorms developed across Virginia and central North Carolina as a small long lived MCS crossed the central and southern Appalachians. Widespread wind damage was reported across northern and central portions of central North Carolina.\nEvent Narrative: A lightning strike caused a house fire at the 1100 Block of Oak Grove Drive. Lightning caused a fire to an unoccupied residence on the southeast side of Raleigh.|The fire started in the attic and smoldered for a time before igniting. Numerous trees were blown down along a swath extending from Burlington to Mebane. One tree fell onto a house at 2017 S Ashland Drive in Burlington. Additional property damage occurred in Mebane, when a tree fell onto a patrol car. Numerous trees were blown down along the swath extending from east of Mebane to Chapel Hill. A downed tree crashed through a home on Cornwalllis Road near the Cleveland area. Monetary damage was estimate. Several trees were blown down along Smith Lane just east of Angier in western Johnston County.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 21.8787 km away, between 2010-07-18 16:41:00 and 2010-07-18 16:41:00. 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 upper level disturbance moving across a moist and moderately unstable airmass in place across central North Carolina resulted in a couple of severe storms that produced severe thunderstorm winds in Vance and Orange Counties.\nEvent Narrative: A couple of trees were blown down along a swath extending from near Hillsborough to Chapel Hill.",
+        "The following events were reported: Lightning, Thunderstorm Wind. These occurred near station USW00013722, approximately 23.0368 km away, between 2010-07-20 16:45:00 and 2010-07-20 18:30:00.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: An upper level disturbance combined with strong afternoon heating to produce scattered strong to severe storms. Additional storms then developed along the numerous outflow boundaries. An upper level disturbance combined with strong afternoon heating to produce scattered strong to severe storms. Additional storms then developed along the numerous outflow boundaries. An upper level disturbance combined with strong afternoon heating to produce scattered strong to severe storms. Additional storms then developed along the numerous outflow boundaries. An upper level disturbance combined with strong afternoon heating to produce scattered strong to severe storms. Additional storms then developed along the numerous outflow boundaries. An upper level disturbance combined with strong afternoon heating to produce scattered strong to severe storms. Additional storms then developed along the numerous outflow boundaries. An upper level disturbance combined with strong afternoon heating to produce scattered strong to severe storms. Additional storms then developed along the numerous outflow boundaries. An upper level disturbance combined with strong afternoon heating to produce scattered strong to severe storms. Additional storms then developed along the numerous outflow boundaries.\nEvent Narrative: Several trees and power lines were blown down across a swath from near Teer to just west of Carrboro. Several trees were blown down along a swath from near Berea to near Oxford. Also, one tree was blown down onto a house on Linden Avenue near Oxford. Several trees were blown down along a swath from near Falls Lake to north Raleigh. Numerous trees were blown down along a swath from near Coats Crossroads to near Middlesex. A trained spotter measured a wind gust of 66 mph with a rooftop anemometer near Ebenezer Church Road and Glenwood Avenue. Also, a couple of trees were blown down a few miles east Raleigh Durham International Airport. A house located at 5219 Coffee Tree Road caught on fire due to a lightning strike. Part of the roof and attic were damaged by the flames. The monetary damage was estimated. A house located at 10408 Bedfordtown Drive caught on fire due to a lightning strike. The home suffered roof and water damage. Monetary damages were estimated.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 23.8423 km away, between 2010-07-25 20:33:00 and 2010-07-25 20:38:00. 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: In the midst of a mini heat wave, severe storms developed across central North Carolina as the southern end of an upper shortwave trough moved through the Mid-Atlantic region.\nEvent Narrative: Multiple trees were blown down along the swath. One tree along Open Air Camp Road fell onto a vehicle.",
+        "The following events were reported: Flash Flood, Lightning. These occurred near station USW00013722, approximately 25.8969 km away, between 2010-07-27 11:46:00 and 2010-07-27 15:30:00.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 very moist and moderately unstable airmass combined with a weak upper level disturbance to cause minor flash flooding and an isolated severe storm. A very moist and moderately unstable airmass combined with a weak upper level disturbance to cause minor flash flooding and an isolated severe storm. A very moist and moderately unstable airmass combined with a weak upper level disturbance to cause minor flash flooding and an isolated severe storm. A very moist and moderately unstable airmass combined with a weak upper level disturbance to cause minor flash flooding and an isolated severe storm.\nEvent Narrative: A house on Haddon Hall was struck by lightning. Smoke was coming from the home, although no fire was visible. The Beaver Creek bridge on Kelly Road near Olive Chapel Road is under water and the city had to close to the road. Farrel Road was covered by water and traffic had to be diverted. James Street between East Williams Street and South Hughes Street had to be closed for a half an hour due to flooding.",
+        "The following events were reported: Hail, Lightning, Thunderstorm Wind. These occurred near station USW00013722, approximately 27.0665 km away, between 2010-07-29 21:20:00 and 2010-07-29 22:45:00. The events included records with hailstones measuring 33.666666666666664 inches.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 303000.0 and crop damage of 0.0. \n\nEpisode Narrative: A line of strong to severe storms formed as a cold front moved into a very moist and moderately unstable air mass. A line of strong to severe storms formed as a cold front moved into a very moist and moderately unstable air mass. A line of strong to severe storms formed as a cold front moved into a very moist and moderately unstable air mass. A line of strong to severe storms formed as a cold front moved into a very moist and moderately unstable air mass. A line of strong to severe storms formed as a cold front moved into a very moist and moderately unstable air mass.\nEvent Narrative: Hail up to quarter size fell for 10 minutes near Harnett Central Road. Lightning struck a home on Vandemere Court causing damage to the chimney. Numerous trees were blown down along a swath from near Raleigh to near Fuquay Varina. Also, a tree was blown on to a house on Martin Street in Raleigh. A tree was blown down across Baptist Grove Road. Another tree was blown down across Kipling Road. A lightning strike caused a house fire at 4012 Gumleaf Dive. The majority of the attic and second floor was severely damaged.",
+        "The following events were reported: Flash Flood, Lightning, Thunderstorm Wind. These occurred near station USW00013722, approximately 25.1151 km away, between 2010-08-05 14:15:00 and 2010-08-05 20:44:00.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 instability and steep low-level lapse rates allowed scattered convection to initially develop along the lee side surface trough during the early afternoon. An outflow driven convective band then developed downstream of the initial convection and moved east across the area. The severe storms produced widespread thunderstorm wind damage and excessive cloud to ground lightning. Strong instability and steep low-level lapse rates allowed scattered convection to initially develop along the lee side surface trough during the early afternoon. An outflow driven convective band then developed downstream of the initial convection and moved east across the area. The severe storms produced widespread thunderstorm wind damage and excessive cloud to ground lightning. Strong instability and steep low-level lapse rates allowed scattered convection to initially develop along the lee side surface trough during the early afternoon. An outflow driven convective band then developed downstream of the initial convection and moved east across the area. The severe storms produced widespread thunderstorm wind damage and excessive cloud to ground lightning. Strong instability and steep low-level lapse rates allowed scattered convection to initially develop along the lee side surface trough during the early afternoon. An outflow driven convective band then developed downstream of the initial convection and moved east across the area. The severe storms produced widespread thunderstorm wind damage and excessive cloud to ground lightning. Strong instability and steep low-level lapse rates allowed scattered convection to initially develop along the lee side surface trough during the early afternoon. An outflow driven convective band then developed downstream of the initial convection and moved east across the area. The severe storms produced widespread thunderstorm wind damage and excessive cloud to ground lightning. Strong instability and steep low-level lapse rates allowed scattered convection to initially develop along the lee side surface trough during the early afternoon. An outflow driven convective band then developed downstream of the initial convection and moved east across the area. The severe storms produced widespread thunderstorm wind damage and excessive cloud to ground lightning. Strong instability and steep low-level lapse rates allowed scattered convection to initially develop along the lee side surface trough during the early afternoon. An outflow driven convective band then developed downstream of the initial convection and moved east across the area. The severe storms produced widespread thunderstorm wind damage and excessive cloud to ground lightning.\nEvent Narrative: A tree was blown down at NC Highway 86 and Walnut Grove Church Road. A couple of trees were blown down along Chapel Hill Road and Chapel Hill Street near Willard Street. One tree was blown down at the intersection of Milburnie Road and Shanta Drive. A tree was blown down at the intersection of Gorman Street and Thistledown Drive. Heavy thunderstorm rains forced the closing of eastbound Glenwood Avenue due to street flooding. Lightning blew a transformer on Snow Hill Road near Whispering Meadow Lane. Numerous trees down on a swatch extending from Graham to Mebane. The damage was most extensive in Mebane where down trees caused damage to two vehicles and two homes.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 31.797 km away, between 2010-08-11 22:23:00 and 2010-08-11 22:23:00. 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: Scattered severe thunderstorms developed as weak surface forcing associated with a lee side trough combined with a very unstable air mass. Isolated flash flooding was observed across the Triad as slow moving thunderstorms occurred in an extremely moist air mass.\nEvent Narrative: A couple of trees were blown down along Highway 96 just north of the Wake County border.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 21.0263 km away, between 2010-08-23 16:15:00 and 2010-08-23 16:15:00. 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 stalled frontal boundary provided enough surface convergence for the development of scattered strong storms and an isolated severe storm during peak heating.\nEvent Narrative: Multiple trees were blown down near and on the Hasentree Golf Course in Wake Forest.",
+        "The following events were reported: Flash Flood. These occurred near station USW00013722, approximately 28.6911 km away, between 2010-08-24 06:30:00 and 2010-08-24 10:50:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Multiple shortwave troughs rotating around an upper level low over Virginia resulted in heavy rainfall of 3 to 5 inches over the Triangle as slow moving showers and isolated thunderstorms persisted through the overnight and morning hours on the 24th. Multiple shortwave troughs rotating around an upper level low over Virginia resulted in heavy rainfall of 3 to 5 inches over the Triangle as slow moving showers and isolated thunderstorms persisted through the overnight and morning hours on the 24th.\nEvent Narrative: Heavy rainfall of 3 to 5 inches flooded several streets in the Raleigh area. Law enforcement reported that vehicle was stalled in 2 feet of flowing water over South Saunders Street at Interstate 40.  Law enforcement was forced to close several  sections of NC Highway 50 due to high flood waters. Heavy rainfall of 4 to 5 inches forced law enforcement to close several roads in the vicinity of Highway 70 and 42.",
+        "The following events were reported: Flash Flood. These occurred near station USW00013722, approximately 20.5722 km away, between 2010-09-30 05:45:00 and 2010-09-30 11:00:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A cold front stalled across across central and eastern portions of North Carolina on the 25th of September. In the mid and upper levels of the atmosphere, a closed low pressure was digging across western Tennessee. The slow moving upper low would cause a series of low pressure waves to ride along the stalled frontal zone, while also advecting copious amounts of tropical moisture into the region. Central North Carolina received 2 to 5 inches of widespread rainfall on the 26th, but because of ongoing severe drought conditions, no flooding occurred.  After a lull on the 27th and 28th, a second upper level low developed over western Tennessee once again. This acted to pull the stationary boundary and moisture conveyor back to the west, as well as pick up remnants of Tropical Storm Nicole. Central North Carolina saw an additional 3 to 6 inches on the 29th and 30th. The combined rainfall of 6 to 10 inches from the 26th through the 30th of September resulted in flashing flooding and minor river flooding. A cold front stalled across across central and eastern portions of North Carolina on the 25th of September. In the mid and upper levels of the atmosphere, a closed low pressure was digging across western Tennessee. The slow moving upper low would cause a series of low pressure waves to ride along the stalled frontal zone, while also advecting copious amounts of tropical moisture into the region. Central North Carolina received 2 to 5 inches of widespread rainfall on the 26th, but because of ongoing severe drought conditions, no flooding occurred.  After a lull on the 27th and 28th, a second upper level low developed over western Tennessee once again. This acted to pull the stationary boundary and moisture conveyor back to the west, as well as pick up remnants of Tropical Storm Nicole. Central North Carolina saw an additional 3 to 6 inches on the 29th and 30th. The combined rainfall of 6 to 10 inches from the 26th through the 30th of September resulted in flashing flooding and minor river flooding. A cold front stalled across across central and eastern portions of North Carolina on the 25th of September. In the mid and upper levels of the atmosphere, a closed low pressure was digging across western Tennessee. The slow moving upper low would cause a series of low pressure waves to ride along the stalled frontal zone, while also advecting copious amounts of tropical moisture into the region. Central North Carolina received 2 to 5 inches of widespread rainfall on the 26th, but because of ongoing severe drought conditions, no flooding occurred.  After a lull on the 27th and 28th, a second upper level low developed over western Tennessee once again. This acted to pull the stationary boundary and moisture conveyor back to the west, as well as pick up remnants of Tropical Storm Nicole. Central North Carolina saw an additional 3 to 6 inches on the 29th and 30th. The combined rainfall of 6 to 10 inches from the 26th through the 30th of September resulted in flashing flooding and minor river flooding.\nEvent Narrative: Heavy rainfall caused minor flooding of Crabtree Creek. Crabtree Creek crested at 12.69 feet. Sullivan Drive on the campus of North Carolina State University was closed due to flash flooding. High water was reported across road at Rock Service and Old Stage Roads.",
+        "The following events were reported: Tornado. These occurred near station USW00013722, approximately 48.992 km away, between 2010-10-27 16:30:00 and 2010-10-27 17:25:00.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 350000.0 and crop damage of 0.0. \n\nEpisode Narrative: Two supercell thunderstorms developed along a slow moving cold front in a high shear, low CAPE environment along the southern periphery of a strong upper vortex over the northern Great Lakes. These supercells produced 5 weak tornadoes across Person, Orange, Granville and Vance counties during the afternoon and evening. Two supercell thunderstorms developed along a slow moving cold front in a high shear, low CAPE environment along the southern periphery of a strong upper vortex over the northern Great Lakes. These supercells produced 5 weak tornadoes across Person, Orange, Granville and Vance counties during the afternoon and evening.\nEvent Narrative: A supercell thunderstorm produced a series of tornadoes across portions of Orange, Granville, and Vance counties in central North Carolina. The first tornado produced EF-1 damage with winds between 90 to 95 mph along Carr Store Road near Allie Mae Road in northern Orange County. At this location a church sustained significant damage, with two walls made of cinder blocks blown down. Numerous hard and soft wood trees were also snapped off and uprooted at this location. The tornado continued to track east northeast and damaged two homes along Pentecost Road. Both homes sustained roof damage, including a partially collapsed chimney. Two individuals were home at the time of the tornado and were not injured. Numerous trees where snapped off and uprooted at this location as well. Winds were estimated to range from 86 to 90 mph. The tornado weakened as it continued to track east north-east across Mcdade Store Road and Efland-Cedar Grove Road before lifting. Numerous trees were either damaged or downed during this area. A supercell thunderstorm moving northeast across Orange and Person counties had already produced a tornado near Cedar Grove in northern Orange County. This same storm produced a second tornado which touched down just east of Berea in Granville County. This EF-0 tornado tracked over 5 miles with a path width near 100 yards and winds of 80 to 85 mph. The tornado touched down north of Highway 158 near the intersection of Bob Daniel Road and Hebron Road. Numerous trees were uprooted and shingles were blown off houses. The tornado continued moving east-northeast partially removing the roof from a house on Hebron Road and destroying 2 sheds at 1657 Elam Currin Road. The tornado then crossed Pine Town Road where more minor damage to tin roofing and shingles was noted before crossing Graham-Hobgood Road. Numerous outbuildings were severely damaged along Joe Pruitt Road near its intersection with Graham-Hobgood Road. At least 2 outbuildings were destroyed and as many as 4 others suffered substantial damage. A single wide mobile home was shifted about 2 feet, however the tie downs and anchors held which kept the trailer from overturning. Winds in this area were rated around 80 to 85 mph based on the noted damage. The tornado then turned a little more to the northeast, crossing Bodie Currin Road causing minor roof damage to a residence at 2543 Bodie Currin Road. Numerous trees were blown down in this area and other homes suffered shingle and siding damage. The tornado then crossed Highway 96 lifting off the ground near the intersection of Cornwall Road and Sterl Carrington Road.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 33.6982 km away, between 2010-11-16 22:45:00 and 2010-11-17 00:37:00. 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 22000.0 and crop damage of 0.0. \n\nEpisode Narrative: A deepening surface low tracked northeast from middle Tennessee into the eastern Great Lakes, while the trailing attendant cold front moved east across North Carolina during the early morning of the 17th. A severe severe bow line segment raced east ahead of the cold front, producing widespread wind damage across central North Carolina. A deepening surface low tracked northeast from middle Tennessee into the eastern Great Lakes, while the trailing attendant cold front moved east across North Carolina during the early morning of the 17th. A severe severe bow line segment raced east ahead of the cold front, producing widespread wind damage across central North Carolina. A deepening surface low tracked northeast from middle Tennessee into the eastern Great Lakes, while the trailing attendant cold front moved east across North Carolina during the early morning of the 17th. A severe severe bow line segment raced east ahead of the cold front, producing widespread wind damage across central North Carolina. A deepening surface low tracked northeast from middle Tennessee into the eastern Great Lakes, while the trailing attendant cold front moved east across North Carolina during the early morning of the 17th. A severe severe bow line segment raced east ahead of the cold front, producing widespread wind damage across central North Carolina. A deepening surface low tracked northeast from middle Tennessee into the eastern Great Lakes, while the trailing attendant cold front moved east across North Carolina during the early morning of the 17th. A severe severe bow line segment raced east ahead of the cold front, producing widespread wind damage across central North Carolina. A deepening surface low tracked northeast from middle Tennessee into the eastern Great Lakes, while the trailing attendant cold front moved east across North Carolina during the early morning of the 17th. A severe severe bow line segment raced east ahead of the cold front, producing widespread wind damage across central North Carolina. A deepening surface low tracked northeast from middle Tennessee into the eastern Great Lakes, while the trailing attendant cold front moved east across North Carolina during the early morning of the 17th. A severe severe bow line segment raced east ahead of the cold front, producing widespread wind damage across central North Carolina. A deepening surface low tracked northeast from middle Tennessee into the eastern Great Lakes, while the trailing attendant cold front moved east across North Carolina during the early morning of the 17th. A severe severe bow line segment raced east ahead of the cold front, producing widespread wind damage across central North Carolina. A deepening surface low tracked northeast from middle Tennessee into the eastern Great Lakes, while the trailing attendant cold front moved east across North Carolina during the early morning of the 17th. A severe severe bow line segment raced east ahead of the cold front, producing widespread wind damage across central North Carolina. A deepening surface low tracked northeast from middle Tennessee into the eastern Great Lakes, while the trailing attendant cold front moved east across North Carolina during the early morning of the 17th. A severe severe bow line segment raced east ahead of the cold front, producing widespread wind damage across central North Carolina. A deepening surface low tracked northeast from middle Tennessee into the eastern Great Lakes, while the trailing attendant cold front moved east across North Carolina during the early morning of the 17th. A severe severe bow line segment raced east ahead of the cold front, producing widespread wind damage across central North Carolina. A deepening surface low tracked northeast from middle Tennessee into the eastern Great Lakes, while the trailing attendant cold front moved east across North Carolina during the early morning of the 17th. A severe severe bow line segment raced east ahead of the cold front, producing widespread wind damage across central North Carolina. A deepening surface low tracked northeast from middle Tennessee into the eastern Great Lakes, while the trailing attendant cold front moved east across North Carolina during the early morning of the 17th. A severe severe bow line segment raced east ahead of the cold front, producing widespread wind damage across central North Carolina. A deepening surface low tracked northeast from middle Tennessee into the eastern Great Lakes, while the trailing attendant cold front moved east across North Carolina during the early morning of the 17th. A severe severe bow line segment raced east ahead of the cold front, producing widespread wind damage across central North Carolina. A deepening surface low tracked northeast from middle Tennessee into the eastern Great Lakes, while the trailing attendant cold front moved east across North Carolina during the early morning of the 17th. A severe severe bow line segment raced east ahead of the cold front, producing widespread wind damage across central North Carolina. A deepening surface low tracked northeast from middle Tennessee into the eastern Great Lakes, while the trailing attendant cold front moved east across North Carolina during the early morning of the 17th. A severe severe bow line segment raced east ahead of the cold front, producing widespread wind damage across central North Carolina. A deepening surface low tracked northeast from middle Tennessee into the eastern Great Lakes, while the trailing attendant cold front moved east across North Carolina during the early morning of the 17th. A severe severe bow line segment raced east ahead of the cold front, producing widespread wind damage across central North Carolina. A deepening surface low tracked northeast from middle Tennessee into the eastern Great Lakes, while the trailing attendant cold front moved east across North Carolina during the early morning of the 17th. A severe severe bow line segment raced east ahead of the cold front, producing widespread wind damage across central North Carolina.\nEvent Narrative: One tree fell onto a house on Lee Road. The tree caused minor damage to dormer on roof. A large tree was blown down onto a power-line at 6345 Wimberly Road. One tree was blown down. Several trees were blown down along a swath from New Hill to near Garner. One tree was blown down on Athens Drive near Athens High School. Tree was blocking one lane on the road. A large tree was blown down at 3400 Poole Road. Several trees were blown down near Hedingham Golf Course. Several trees were blown down along NC Highway 96. One tree was blown down near the intersection of Highway 70 and White Oak Road in Garner. Several trees were blown down on Cheves Road in Bunn. Numerous trees were blown down across southern part of county. Several out buildiings were reported destroyed. One tree was blown down across Alston Avenue near the intersection of NC Highway 55 and NC Highway 147. Two trees were blown down on Ferbow Road and Cliffton Drive. One tree was blown down. One tree was blown down near the intersection of Pearces Road and Elm Walk Lane. Two trees were blown down. Numerous trees were blown down around Louisburg, especially near McKenzie Road and Shawnee Drive. A storage buildings was picked up and blown onto a mobile home. A telephone pole was also blown through the mobile home. Monetary damages were estimated.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 32.2632 km away, between 2010-12-01 03:40:00 and 2010-12-01 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: A line of thunderstorms along a slow moving cold front strengthened overnight as a powerful upper trough moved through the region. A convective bow line segment produced widespread wind damage across much of central North Carolina. A line of thunderstorms along a slow moving cold front strengthened overnight as a powerful upper trough moved through the region. A convective bow line segment produced widespread wind damage across much of central North Carolina.\nEvent Narrative: Two trees were blown down on Guess Road at New Sharon Road and near the intersection of NC Highway 751 and Highway 70. Several trees were blown down near Franklinton including downed trees on Tom Linum Road, Long Mill Road, and West River Road.",
+        "The following events were reported: Hail, Lightning. These occurred near station USW00013722, approximately 14.344 km away, between 2011-02-28 18:53:00 and 2011-02-28 19:10:00. The events included records with hailstones measuring 0.75 inches.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 bowing line segment developed ahead of a strong cold front approaching from the west. Despite very strong deep layer shear, marginal instability resulted in only sporadic |reports of wind damage across central North Carolina. A bowing line segment developed ahead of a strong cold front approaching from the west. Despite very strong deep layer shear, marginal instability resulted in only sporadic |reports of wind damage across central North Carolina. A bowing line segment developed ahead of a strong cold front approaching from the west. Despite very strong deep layer shear, marginal instability resulted in only sporadic |reports of wind damage across central North Carolina.\nEvent Narrative: Lightning struck a home and caused a fire above the garage at a home on Vermel Court. Property damage has been estimated. Lightning hit a chimney of a home, blasting the top off of it and damaging a closet upstairs.",
+        "The following events were reported: Thunderstorm Wind, Tornado. These occurred near station USW00013722, approximately 35.8265 km away, between 2011-03-06 17:10:00 and 2011-03-06 17:13:00.The events resulted in 1 injuries and 0 fatalities. The events caused property damage valued at 103000.0 and crop damage of 0.0. \n\nEpisode Narrative: Convection developed along and ahead of a cold front that moved across the state during the late afternoon and early evening hours. Two weak EF0 tornadoes developed across central North Carolina when a discrete cells along a couple of mesolows merged with the main convective band. Convection developed along and ahead of a cold front that moved across the state during the late afternoon and early evening hours. Two weak EF0 tornadoes developed across central North Carolina when a discrete cells along a couple of mesolows merged with the main convective band.\nEvent Narrative: A mobile home suffered shingle damage. A couple of trees were also blown down. A weak EF-0 tornado with winds between 70-75 mph touched down just northeast of downtown Rolesville along NC Highway 401 (Main St). The tornado tracked to the northeast for 2 miles along NC Highway 401 before crossing NC Highway 96 and then lifting. Numerous trees were snapped and buildings damaged from the 300 block to 700 block of Main Street. At 502 Main Street, shingles were torn from a home and the roof of the porch was lifted off. At 506 Main Street, a greenhouse was destroyed at the pure seed testing east facility. Several outbuildings at the facility also had their tin roofing removed. Continuing north on Main Street a carport was ripped from the side of a house at 708 Main Street. Two outbuilding were also destroyed on the property. A one story church at the intersection of Pulley Town Road experienced minor roof damage with numerous shingles ripped from the roof. Trees were blown down and outbuildings were damaged along NC Highway 401, from Pulley Town Road to Creek Pine Drive. A car was damaged by a large falling limb near Creek Pine Road. The tornado then crossed NC Highway 96 destroying another outbuilding. The tornado lifted off the ground shortly after crossing NC Highway 96. |An elderly man was injured from the tornado due to a house fire. Falling trees brought down power lines onto the house along Main Street near Pulley Town Road. The arcing power lines caused the house to catch fire. The elderly gentleman was transported to the hospital to be treated for smoke inhalation and burns.",
+        "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00013722, approximately 36.0537 km away, between 2011-03-23 18:14:00 and 2011-03-23 22:03:00. The events included records with hailstones measuring 37.75 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 cluster of thunderstorms moved eastward across the central and southern Appalachians and into central North Carolina during the afternoon hours of the 23rd.  Limited by marginal instability, the convective cluster produced small hail the size of pennies and scattered thunderstorm wind damage. A cluster of thunderstorms moved eastward across the central and southern Appalachians and into central North Carolina during the afternoon hours of the 23rd.  Limited by marginal instability, the convective cluster produced small hail the size of pennies and scattered thunderstorm wind damage. A cluster of thunderstorms moved eastward across the central and southern Appalachians and into central North Carolina during the afternoon hours of the 23rd.  Limited by marginal instability, the convective cluster produced small hail the size of pennies and scattered thunderstorm wind damage. A cluster of thunderstorms moved eastward across the central and southern Appalachians and into central North Carolina during the afternoon hours of the 23rd.  Limited by marginal instability, the convective cluster produced small hail the size of pennies and scattered thunderstorm wind damage.\nEvent Narrative: Hail the size of quarters was reported on Route 14 north of Wake Forest. One tree was blown down across the road near the corner of Hurdle Mills Road and Wheelers Church Road. One tree fell onto some power-lines near the intersection of Little River Church Road and Mary Hall Road. A large tree fell onto a home, damaging the garage and roof.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 30.8819 km away, between 2011-04-05 02:36:00 and 2011-04-05 08:40:00. 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 55000.0 and crop damage of 0.0. \n\nEpisode Narrative: With a strong cold front approaching the region from the west, a pre-frontal trough moved across the CWA during the overnight hours, resulting in an intense squall line tracking across the entire forecast area. This squall line caused widespread wind damage across all of central North Carolina. After a brief break in the precipitation, another line of severe storms with damaging winds developed along the cold front as it moved through the region during the mid morning hours. With a strong cold front approaching the region from the west, a pre-frontal trough moved across the CWA during the overnight hours, resulting in an intense squall line tracking across the entire forecast area. This squall line caused widespread wind damage across all of central North Carolina. After a brief break in the precipitation, another line of severe storms with damaging winds developed along the cold front as it moved through the region during the mid morning hours. With a strong cold front approaching the region from the west, a pre-frontal trough moved across the CWA during the overnight hours, resulting in an intense squall line tracking across the entire forecast area. This squall line caused widespread wind damage across all of central North Carolina. After a brief break in the precipitation, another line of severe storms with damaging winds developed along the cold front as it moved through the region during the mid morning hours. With a strong cold front approaching the region from the west, a pre-frontal trough moved across the CWA during the overnight hours, resulting in an intense squall line tracking across the entire forecast area. This squall line caused widespread wind damage across all of central North Carolina. After a brief break in the precipitation, another line of severe storms with damaging winds developed along the cold front as it moved through the region during the mid morning hours. With a strong cold front approaching the region from the west, a pre-frontal trough moved across the CWA during the overnight hours, resulting in an intense squall line tracking across the entire forecast area. This squall line caused widespread wind damage across all of central North Carolina. After a brief break in the precipitation, another line of severe storms with damaging winds developed along the cold front as it moved through the region during the mid morning hours.\nEvent Narrative: A couple of trees were blown down near the city of Durham, with one of the trees landing on a house. A few trees were blown down across Hwy 158 near Oxford. Numerous trees were blown down along a swath from just west of Apex to near Zebulon. One tree fell on a house near Cary and another tree fell through a mobile home near Garner. A couple of trees and power lines were blown down along a swath from Franklinton to just north of Louisburg. A tree was blown down in the Knightdale Estates area.",
+        "The following events were reported: Tornado. These occurred near station USW00013722, approximately 38.1183 km away, between 2011-04-16 13:56:00 and 2011-04-16 15:15:00.The events resulted in 103 injuries and 6 fatalities. The events caused property damage valued at 172075000.0 and crop damage of 0.0. \n\nEpisode Narrative: A strong storm system that had a history of producing deadly tornadoes across Oklahoma and the deep south on the 14th and 15th weakened as it crossed the southern Appalachians during the early morning hours of the 16th.  A squall line descended the Blue Ridge by the late morning hours, and rapidly intensified |as it moved east into the central Piedmont of North Carolina, with four long live tornadic supercells evolving from the linear convective segment. These tornadic supercells went on to produce 9 tornadoes in the Raleigh CWA, including 2 EF3s, and 4 EF2s. The tornadoes left 8 dead with approximately 275 injuries. A strong storm system that had a history of producing deadly tornadoes across Oklahoma and the deep south on the 14th and 15th weakened as it crossed the southern Appalachians during the early morning hours of the 16th.  A squall line descended the Blue Ridge by the late morning hours, and rapidly intensified |as it moved east into the central Piedmont of North Carolina, with four long live tornadic supercells evolving from the linear convective segment. These tornadic supercells went on to produce 9 tornadoes in the Raleigh CWA, including 2 EF3s, and 4 EF2s. The tornadoes left 8 dead with approximately 275 injuries. A strong storm system that had a history of producing deadly tornadoes across Oklahoma and the deep south on the 14th and 15th weakened as it crossed the southern Appalachians during the early morning hours of the 16th.  A squall line descended the Blue Ridge by the late morning hours, and rapidly intensified |as it moved east into the central Piedmont of North Carolina, with four long live tornadic supercells evolving from the linear convective segment. These tornadic supercells went on to produce 9 tornadoes in the Raleigh CWA, including 2 EF3s, and 4 EF2s. The tornadoes left 8 dead with approximately 275 injuries.\nEvent Narrative: The tornado exited Moore County and proceeded to strengthen to an EF1 as it moved into Lee County along Wildlife Road. The tornado blew a single wide trailer off its foundation, while also damaging the home home next door. The tornado continued to intensify to EF3 intensity along Lemon Springs Road striking the St. Andrews Subdivision. One fatality occurred when a tree fell onto a vehicle along Lemon Springs Road, crushing the driver. Numerous homes were completely destroyed and several two story homes had their upper floors removed. Wind speeds were estimated at 140 mph with a path length of over one quarter mile. Additional homes were blown off their foundations on Cemetery Drive. The tornado continued to produce major damage as it moved east along Cameron drive. The upper floor was blown off of two apartment buildings. The tornado then entered an industrial complex along Industrial Drive, where multiple steel constructed retail buildings were destroyed, in addition to 3 large warehouses at the static control facility. Winds In this area likely exceeded 160 mph. The tornado then destroyed the Tractor Supply Company, Big Lots and the Lowes Home Improvement Store along highway 421. Winds in this area were estimated around 140 mph. Two homes were blown off their foundations along Rice Road, north of NC Highway 42. Another fatality occurred along Poplar Spring Church Road when a mobile home was lifted off the ground and and then thrown into the woods and destroyed. In total,  457 homes were damaged with 116 homes being destroyed. Seventeen businesses were damaged as well. The tornado continued northeast along Avent Ferry Road, crossing into Chatham County, just east of Harris Lake. The tornado exited Lee County and move into extreme southeastern Chatham County, just south and east of Harris Lake. Only 2 homes sustained damage, with moderate|to major roof damage to one of the homes, when a tree crashed through it. The tornado exited Chatham County and entered southwest Wake County as an EF0. There was multiple tree and roof damage along Avent Ferry Road, southwest of Holly Springs. The tornado intensified to an EF1 with winds of 86 mph as it reached Fire Station Number Two and the Holly Glenn Subdivision before crossing highway 55 and tracking through the Remington subdivision.  The tornado continued to track northeastward and caused extensive tree damage and damage to numerous homes, mainly from fallen trees along Pierce Olive, Ten-Ten, Penny Road, and Yates Mill Pond roads, as wind speeds increased to around 100 mph. The tornado crossed Tryon Road, between Lake Wheeler Road and the Raleigh Golf Association Golf Course, before tracking northeast across the entire City of Raleigh, producing EF1 damage in a narrow swath between 50 to 100 yards. It crossed directly over Interstates 40-440, between exits 297 and 298 with damage on both sides of the interstate clearly visible. The tornado continued northeast across South Saunders Street, where 4 businesses were damaged. A body shop was completely destroyed when the roof was ripped off and the side walls collapsed. The tornado continued to snap hardwood trees and power-lines near Mount Hope Cemetery and nearby homes. The tornado weakened as it moved northeast towards Shaw University. Campus dormitories and the university student center had windows blown in with roof damage. The tornado moved northeast along the east side of the major high rise buildings in downtown Raleigh, downing hundreds of trees, many of which fell on houses. The historic Oakwood to Lion`s Park sections of town, including the historic Oakwood Cemetery were hardest hit. Also in the path of the tornado was Saint Augustine`s College, which sustained roof damage to every building on campus. The tornado continued to down trees on numerous homes as it crossed North King Charles Road to Yonkers Road, producing EF1 damage to several businesses.  The tornado crossed the 440 beltline for a second time, this time on the northeast side of downtown Raleigh near the intersections of Westinghouse and Brentwood roads, again causing damages to several businesses, including the Raleigh Iceplex. The tornado then strengthened to an EF2 with winds greater than 110 mph as it continued northeast producing extensive tree damage in a 100 to 200 yard wide path from Stony Brook Drive to Buffalo Road. Snapped trees crashed onto and through numerous homes all along the path. Four fatalities occurred when a large tree fell|onto a mobile home. Two other mobile homes were thrown 30 to 50 feet when the tie downs snapped from their anchor points with nearly all of the mobile homes in the Stony Brook mobile home park sustained some type of damage.  The EF2 tornado continued to move northeast across Buffalo Road, near the Cardinal Grove Subdivision. Several two story homes were completely destroyed with numerous other homes sustaining moderate to major damage. Damage consistent with an EF2 tornado continued with widespread damage in a 200 yard wide swath along Forestville road. A couple of mobile homes were destroyed and several two story homes suffered extensive roof damage, with continued numerous snapped trees falling on houses. The tornado weakened or lifted as it moved northeast towards Rolesville. Damage became very sporadic and isolated in nature as it neared the Franklin County line. In total, 2270 homes were damaged, including 67 homes that were destroyed, with another 184 homes experiencing major damage. There were also 34 businesses damaged.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 34.8819 km away, between 2011-04-27 12:10:00 and 2011-04-27 12:10:00. 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: Isolated to scattered storms developed across central North Carolina in strengthening southerly flow in advance of a strong cold front. A couple of the storms became severe across the Northern Piedmont and produce large hail and damaging winds.\nEvent Narrative: Several trees and power lines were reported down on Saint Mary's Road.",
+        "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00013722, approximately 31.2368 km away, between 2011-05-13 17:30:00 and 2011-05-14 00:45:00. The events included records with hailstones measuring 41.833333333333336 inches.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: Cold pool driven convection crossed the Appalachians and moved into a moderate unstable air mass in place across central North Carolina. Severe hail up to the size |of golf balls and wind damage from fallen trees were reported as the convective band moved through the area. Cold pool driven convection crossed the Appalachians and moved into a moderate unstable air mass in place across central North Carolina. Severe hail up to the size |of golf balls and wind damage from fallen trees were reported as the convective band moved through the area. Cold pool driven convection crossed the Appalachians and moved into a moderate unstable air mass in place across central North Carolina. Severe hail up to the size |of golf balls and wind damage from fallen trees were reported as the convective band moved through the area. Cold pool driven convection crossed the Appalachians and moved into a moderate unstable air mass in place across central North Carolina. Severe hail up to the size |of golf balls and wind damage from fallen trees were reported as the convective band moved through the area. Cold pool driven convection crossed the Appalachians and moved into a moderate unstable air mass in place across central North Carolina. Severe hail up to the size |of golf balls and wind damage from fallen trees were reported as the convective band moved through the area. Cold pool driven convection crossed the Appalachians and moved into a moderate unstable air mass in place across central North Carolina. Severe hail up to the size |of golf balls and wind damage from fallen trees were reported as the convective band moved through the area.\nEvent Narrative: One tree fell onto a truck along Wendell Road near Archer Lodge Road. Damages are estimated. One tree was blown down off Silk Hope Gum Springs Road. Two trees were blown down near the intersection of Durham and Hillsborough Road. Quarter size hail was reported at Brier Creek. A downed tree was blocking traffic on TW Alexander Drive. Trees and power-lines were blown down hear C.C. Andrews Road and Durham Road.",
+        "The following events were reported: Hail. These occurred near station USW00013722, approximately 16.0629 km away, between 2011-05-14 14:13:00 and 2011-05-14 14:14:00. 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: Widespread convection developed during the afternoon hours with the approach of a surface cold front and shortwave trough moving the region. A wet microburst produced widespread wind damage in Sampson County, with several storms producing|quarter size hail. Widespread convection developed during the afternoon hours with the approach of a surface cold front and shortwave trough moving the region. A wet microburst produced widespread wind damage in Sampson County, with several storms producing|quarter size hail.\nEvent Narrative:",
+        "The following events were reported: Flash Flood, Hail, Thunderstorm Wind. These occurred near station USW00013722, approximately 25.9543 km away, between 2011-05-27 11:15:00 and 2011-05-27 16:00:00. The events included records with hailstones measuring 16.153846153846153 inches.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: With moisten laden air in place, a series of upper level disturbances in advance of an upper level trough moving into the area from the Tennessee Vally produced heavy rainfall of 3 to 5 inches along with severe hail and and isolated thunderstorm wind damage. With moisten laden air in place, a series of upper level disturbances in advance of an upper level trough moving into the area from the Tennessee Vally produced heavy rainfall of 3 to 5 inches along with severe hail and and isolated thunderstorm wind damage. With moisten laden air in place, a series of upper level disturbances in advance of an upper level trough moving into the area from the Tennessee Vally produced heavy rainfall of 3 to 5 inches along with severe hail and and isolated thunderstorm wind damage. With moisten laden air in place, a series of upper level disturbances in advance of an upper level trough moving into the area from the Tennessee Vally produced heavy rainfall of 3 to 5 inches along with severe hail and and isolated thunderstorm wind damage. With moisten laden air in place, a series of upper level disturbances in advance of an upper level trough moving into the area from the Tennessee Vally produced heavy rainfall of 3 to 5 inches along with severe hail and and isolated thunderstorm wind damage. With moisten laden air in place, a series of upper level disturbances in advance of an upper level trough moving into the area from the Tennessee Vally produced heavy rainfall of 3 to 5 inches along with severe hail and and isolated thunderstorm wind damage. With moisten laden air in place, a series of upper level disturbances in advance of an upper level trough moving into the area from the Tennessee Vally produced heavy rainfall of 3 to 5 inches along with severe hail and and isolated thunderstorm wind damage. With moisten laden air in place, a series of upper level disturbances in advance of an upper level trough moving into the area from the Tennessee Vally produced heavy rainfall of 3 to 5 inches along with severe hail and and isolated thunderstorm wind damage. With moisten laden air in place, a series of upper level disturbances in advance of an upper level trough moving into the area from the Tennessee Vally produced heavy rainfall of 3 to 5 inches along with severe hail and and isolated thunderstorm wind damage. With moisten laden air in place, a series of upper level disturbances in advance of an upper level trough moving into the area from the Tennessee Vally produced heavy rainfall of 3 to 5 inches along with severe hail and and isolated thunderstorm wind damage. With moisten laden air in place, a series of upper level disturbances in advance of an upper level trough moving into the area from the Tennessee Vally produced heavy rainfall of 3 to 5 inches along with severe hail and and isolated thunderstorm wind damage. With moisten laden air in place, a series of upper level disturbances in advance of an upper level trough moving into the area from the Tennessee Vally produced heavy rainfall of 3 to 5 inches along with severe hail and and isolated thunderstorm wind damage. With moisten laden air in place, a series of upper level disturbances in advance of an upper level trough moving into the area from the Tennessee Vally produced heavy rainfall of 3 to 5 inches along with severe hail and and isolated thunderstorm wind damage. With moisten laden air in place, a series of upper level disturbances in advance of an upper level trough moving into the area from the Tennessee Vally produced heavy rainfall of 3 to 5 inches along with severe hail and and isolated thunderstorm wind damage. With moisten laden air in place, a series of upper level disturbances in advance of an upper level trough moving into the area from the Tennessee Vally produced heavy rainfall of 3 to 5 inches along with severe hail and and isolated thunderstorm wind damage. With moisten laden air in place, a series of upper level disturbances in advance of an upper level trough moving into the area from the Tennessee Vally produced heavy rainfall of 3 to 5 inches along with severe hail and and isolated thunderstorm wind damage. With moisten laden air in place, a series of upper level disturbances in advance of an upper level trough moving into the area from the Tennessee Vally produced heavy rainfall of 3 to 5 inches along with severe hail and and isolated thunderstorm wind damage.\nEvent Narrative:   A power pole was snapped and power-lines were blown down along the swath. The roof was torn off of an office building in Oxford. A tree was also blown down. A couple of trees were blown down. One tree fell onto a power line. Several power-lines were blown down across Chapel Hill. There were several reports of flooded roads within Pittsboro city limits, including West Salisbury and Hillsboro Streets. Several roads were flooded within the Durham city limits, including Sedwick Road and University Drive. Several roads were flooded within the Chapel Hill city limits, including West Franklin, Mallete, Estes, Greensboro and Randle streets.  Some vehicles stalled in the flood waters. Street flooding was reported at Holly Park Drive and Hillspring Lane.  Quarter to half dollar size hail lasted for several minutes at the intersection of Roxboro Street and Avondale Drive.",
+        "The following events were reported: Lightning, Thunderstorm Wind. These occurred near station USW00013722, approximately 22.5093 km away, between 2011-06-10 18:01:00 and 2011-06-10 22:09:00.The events resulted in 0 injuries and 1 fatalities. No significant property or crop damage was reported. \n\nEpisode Narrative: Scattered thunderstorms developed along an upper shear axis as strong daytime heating |resulted in moderate instability across the area. Scattered thunderstorms developed along an upper shear axis as strong daytime heating |resulted in moderate instability across the area. Scattered thunderstorms developed along an upper shear axis as strong daytime heating |resulted in moderate instability across the area.\nEvent Narrative: Several trees were blown down near the intersection of Old Creedmoor Road and Interstate 540. A 45 year old male died when he was struck by lightning while feeding his livestock. Severals trees were blown down along the swath extending from Bunn to Pilot.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 31.0995 km away, between 2011-06-11 17:38:00 and 2011-06-11 18:12:00. 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 strong to severe storms initially developed along the southern Appalachians, and moved eastward into the western Piedmont into an area of moderate instability. The severe storms produced mostly localized wet microburst.  Urban flash flooding also occurred in Greensboro as two to three inches of heavy rain fell over the city. Scattered strong to severe storms initially developed along the southern Appalachians, and moved eastward into the western Piedmont into an area of moderate instability. The severe storms produced mostly localized wet microburst.  Urban flash flooding also occurred in Greensboro as two to three inches of heavy rain fell over the city. Scattered strong to severe storms initially developed along the southern Appalachians, and moved eastward into the western Piedmont into an area of moderate instability. The severe storms produced mostly localized wet microburst.  Urban flash flooding also occurred in Greensboro as two to three inches of heavy rain fell over the city.\nEvent Narrative: Numerous trees were blown down across Orange County. Several trees were blown down in Hillsborough. Several trees were blown down along a swath extending just north of Pittsboro to just northeast of Fearrington.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 24.6705 km away, between 2011-06-18 17:05:00 and 2011-06-18 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 500.0 and crop damage of 0.0. \n\nEpisode Narrative: A linear mesoscale convective complex moved southeast, crossing the southern  Appalachians and into North Carolina during the afternoon of the 18th. Widespread thunderstorm wind damage was reported across western and central portions of the Piedmont as the line swept through the area. A linear mesoscale convective complex moved southeast, crossing the southern  Appalachians and into North Carolina during the afternoon of the 18th. Widespread thunderstorm wind damage was reported across western and central portions of the Piedmont as the line swept through the area. A linear mesoscale convective complex moved southeast, crossing the southern  Appalachians and into North Carolina during the afternoon of the 18th. Widespread thunderstorm wind damage was reported across western and central portions of the Piedmont as the line swept through the area. A linear mesoscale convective complex moved southeast, crossing the southern  Appalachians and into North Carolina during the afternoon of the 18th. Widespread thunderstorm wind damage was reported across western and central portions of the Piedmont as the line swept through the area.\nEvent Narrative: Several trees were blown down along the swath, including one down tree on White Cross Road. One tree also fell down on a shed. Monetary damages were estimated. Several trees were reported down in Chapel Hill. Several trees were blown down, with one tree down on a house. No other information was available. Several trees were blown down along a swath from John Mitchel Road to NC Highway 96.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 12.5221 km away, between 2011-06-20 00:20:00 and 2011-06-20 00:30:00. 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: Isolated thunderstorms developed across the central Piedmont and coastal plain as a weak upper level disturbance combined with a very moist and moderately unstable air mass. These storms resulted in hail up to the size of golf balls, as well as a couple of trees being blown down.\nEvent Narrative: A couple of trees were blown down along a swath from near Cary to near Raleigh. One tree fell on a house in Cary, but no damage information was available.",
+        "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00013722, approximately 32.6448 km away, between 2011-06-21 19:35:00 and 2011-06-21 20:05:00. 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: Strong to severe thunderstorms developed along the northern periphery of the strong upper level ridge as strong daytime heating resulted in moderate instability across the area. Severe hail ranging from quarter size to as large as golf ball size was reported along with numerous downed trees from thunderstorm wind gusts. Strong to severe thunderstorms developed along the northern periphery of the strong upper level ridge as strong daytime heating resulted in moderate instability across the area. Severe hail ranging from quarter size to as large as golf ball size was reported along with numerous downed trees from thunderstorm wind gusts. Strong to severe thunderstorms developed along the northern periphery of the strong upper level ridge as strong daytime heating resulted in moderate instability across the area. Severe hail ranging from quarter size to as large as golf ball size was reported along with numerous downed trees from thunderstorm wind gusts.\nEvent Narrative:   One tree was blown down along Rex Road.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 39.088 km away, between 2011-06-27 12:50:00 and 2011-06-27 13:55:00. The events included records with estimated wind gusts of 51.0 mph.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: With intense insolation and a weak surface trough across the forecast area, as well as an increasingly moist and unstable air mass, scattered severe storms developed across the region. Aided by an approaching mid level disturbance, these storms were able to persist through the evening hours. With intense insolation and a weak surface trough across the forecast area, as well as an increasingly moist and unstable air mass, scattered severe storms developed across the region. Aided by an approaching mid level disturbance, these storms were able to persist through the evening hours. With intense insolation and a weak surface trough across the forecast area, as well as an increasingly moist and unstable air mass, scattered severe storms developed across the region. Aided by an approaching mid level disturbance, these storms were able to persist through the evening hours. With intense insolation and a weak surface trough across the forecast area, as well as an increasingly moist and unstable air mass, scattered severe storms developed across the region. Aided by an approaching mid level disturbance, these storms were able to persist through the evening hours.\nEvent Narrative: A tree was blown down several miles southwest of Moncure. A trained spotter reported an estimated wind gust of 62 mph just southwest of Raleigh. Numerous trees were blown down along a swath from just southwest of Raleigh to just northeast of Raleigh. There was also a report of quarter size hail in northeast Raleigh. One tree was blown down several miles south of Wendell, near the intersection of Wendell Road and Salem Church Road. One tree was blown down a few miles north of Seminole at 2551 Buckhorn Road.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 26.9252 km away, between 2011-06-28 14:22:00 and 2011-06-28 15:36:00. 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: Intense heating coupled with a moist air mass to support strong to severe convection.|The strongest storms were focused along a pre-frontal trough and in advance of an upper level disturbance.  Widespread wind damage was reported across western and central portions of the Piedmont. Additionally, heavy rainfall of 3 to 4 inches resulted in flash flooding within urban areas in the Piedmont Triad. Intense heating coupled with a moist air mass to support strong to severe convection.|The strongest storms were focused along a pre-frontal trough and in advance of an upper level disturbance.  Widespread wind damage was reported across western and central portions of the Piedmont. Additionally, heavy rainfall of 3 to 4 inches resulted in flash flooding within urban areas in the Piedmont Triad. Intense heating coupled with a moist air mass to support strong to severe convection.|The strongest storms were focused along a pre-frontal trough and in advance of an upper level disturbance.  Widespread wind damage was reported across western and central portions of the Piedmont. Additionally, heavy rainfall of 3 to 4 inches resulted in flash flooding within urban areas in the Piedmont Triad. Intense heating coupled with a moist air mass to support strong to severe convection.|The strongest storms were focused along a pre-frontal trough and in advance of an upper level disturbance.  Widespread wind damage was reported across western and central portions of the Piedmont. Additionally, heavy rainfall of 3 to 4 inches resulted in flash flooding within urban areas in the Piedmont Triad.\nEvent Narrative: Multiple trees were blown down near Marthas Chapel Road and Farrington Point Road. Three down trees were partially blocking OKelly Chapel Road. Seven to ten trees were blown down near Old US 1 and Issac Drive. A nearby fence was also damaged. Multiple trees were blown down.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 22.7576 km away, between 2011-07-04 15:15:00 and 2011-07-04 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: Strong afternoon heating in advance of an approaching surface front and upper level trough fueled strong to severe thunderstorms across central North Carolina during the afternoon and evening of the 4th. Strong afternoon heating in advance of an approaching surface front and upper level trough fueled strong to severe thunderstorms across central North Carolina during the afternoon and evening of the 4th. Strong afternoon heating in advance of an approaching surface front and upper level trough fueled strong to severe thunderstorms across central North Carolina during the afternoon and evening of the 4th. Strong afternoon heating in advance of an approaching surface front and upper level trough fueled strong to severe thunderstorms across central North Carolina during the afternoon and evening of the 4th.\nEvent Narrative: Multiple trees were blown near Buckhorn and Chestnut Ridge Church Road. Trees were blown down near the intersection of Old Chapel Hill Road and Everwood Drive. Large pine tree fell down into a swimming pool near Cornwallis Road. Dozen of trees were blown down across southern portion of county.",
+        "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00013722, approximately 48.3787 km away, between 2011-07-06 18:41:00 and 2011-07-06 18:41:00. The events included records with hailstones measuring 28.5 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A moist air mass combined with an upper level trough over the region initially triggered scattered showers and thunderstorms across central North Carolina. Storms then quickly became driven by surface cold pool with numerous tree damage in Scotland and Hoke counties. A moist air mass combined with an upper level trough over the region initially triggered scattered showers and thunderstorms across central North Carolina. Storms then quickly became driven by surface cold pool with numerous tree damage in Scotland and Hoke counties.\nEvent Narrative:  Trained spotter measured a 65 mph wind gust in Surl.",
+        "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00013722, approximately 39.3157 km away, between 2011-07-13 15:25:00 and 2011-07-13 16:09:00. The events included records with hailstones measuring 41.791666666666664 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A disturbance aloft moving across central North Carolina and interacted with a warm moist and unstable atmosphere to produce damaging winds. A disturbance aloft moving across central North Carolina and interacted with a warm moist and unstable atmosphere to produce damaging winds. A disturbance aloft moving across central North Carolina and interacted with a warm moist and unstable atmosphere to produce damaging winds. A disturbance aloft moving across central North Carolina and interacted with a warm moist and unstable atmosphere to produce damaging winds. A disturbance aloft moving across central North Carolina and interacted with a warm moist and unstable atmosphere to produce damaging winds. A disturbance aloft moving across central North Carolina and interacted with a warm moist and unstable atmosphere to produce damaging winds.\nEvent Narrative: Penny sized hail was reported near Pilot, NC. One tree was reported down near the intersection of United States Highway 1 and Materials Drive. One tree was down at 1000 Moores Pond Road. One tree was reported down at Williams-White Road. One tree was reported down on Pearces Road. One tree was reported down on Moores Pond Road.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 35.7822 km away, between 2011-07-23 17:30:00 and 2011-07-23 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: A shortwave disturbance moved through the region as afternoon temperatures soared|into the triple digits, resulting in strong destabilization across central North Carolina.|Scattered thunderstorms produced wind damage across the area, with widespread wind damage reported in Johnston County, where one mobile home was destroyed. A shortwave disturbance moved through the region as afternoon temperatures soared|into the triple digits, resulting in strong destabilization across central North Carolina.|Scattered thunderstorms produced wind damage across the area, with widespread wind damage reported in Johnston County, where one mobile home was destroyed.\nEvent Narrative: Numerous large tree limbs were blown down. Multiple trees were blown down near Cornwallis Road and NC Highway 42.",
+        "The following events were reported: Flash Flood, Lightning, Thunderstorm Wind. These occurred near station USW00013722, approximately 18.7543 km away, between 2011-07-24 14:05:00 and 2011-07-24 17:40:00.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 cluster of shower and thunderstorms moved off the Appalachians and into central North Carolina during the afternoon. The severe storms produced thunderstorm wind damage across the Central Piedmont with minor structural damage to a couple of outdoor buildings. A cluster of shower and thunderstorms moved off the Appalachians and into central North Carolina during the afternoon. The severe storms produced thunderstorm wind damage across the Central Piedmont with minor structural damage to a couple of outdoor buildings. A cluster of shower and thunderstorms moved off the Appalachians and into central North Carolina during the afternoon. The severe storms produced thunderstorm wind damage across the Central Piedmont with minor structural damage to a couple of outdoor buildings. A cluster of shower and thunderstorms moved off the Appalachians and into central North Carolina during the afternoon. The severe storms produced thunderstorm wind damage across the Central Piedmont with minor structural damage to a couple of outdoor buildings. A cluster of shower and thunderstorms moved off the Appalachians and into central North Carolina during the afternoon. The severe storms produced thunderstorm wind damage across the Central Piedmont with minor structural damage to a couple of outdoor buildings.\nEvent Narrative: Severe thunderstorm wind gusts caused two sailboats to be flipped over at Bond Lake. Numerous trees were blown down, uprooted and snapped along a swath in Cary. Lightning started a house fire. Monetary damages were estimated. A stream was out of its bank near Bond Lake Park. Multiple trees and power-lines were blown along Highway 501 near the Durham and Person County line.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 34.0497 km away, between 2011-07-25 13:53:00 and 2011-07-25 16:30:00. 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: As a trailing short wave trough aloft moved across the region, a sharpening of the surface lee side trough occurred. With a very moist air mass and moderate instability also in place across the region, scattered severe thunderstorms were able to develop across the forecast area. As a trailing short wave trough aloft moved across the region, a sharpening of the surface lee side trough occurred. With a very moist air mass and moderate instability also in place across the region, scattered severe thunderstorms were able to develop across the forecast area. As a trailing short wave trough aloft moved across the region, a sharpening of the surface lee side trough occurred. With a very moist air mass and moderate instability also in place across the region, scattered severe thunderstorms were able to develop across the forecast area. As a trailing short wave trough aloft moved across the region, a sharpening of the surface lee side trough occurred. With a very moist air mass and moderate instability also in place across the region, scattered severe thunderstorms were able to develop across the forecast area. As a trailing short wave trough aloft moved across the region, a sharpening of the surface lee side trough occurred. With a very moist air mass and moderate instability also in place across the region, scattered severe thunderstorms were able to develop across the forecast area.\nEvent Narrative: A roof was blown off of an apartment building on Weymouth Street in Durham. (No monetary damage estimate was known.) Also, a couple of trees were blown down on Shannon Street near MLK Parkway in Durham. One tree was blown down on Mebane Oaks Road near Teer. A couple of trees were blown down along a swath from a few miles southwest of Garner to a few miles southeast of Garner. One tree was blown down near Efland. A couple of trees and power lines were blown down along a short swath just north of Flowers.",
+        "The following events were reported: Flash Flood. These occurred near station USW00013722, approximately 15.833 km away, between 2011-08-06 05:55:00 and 2011-08-06 10:59:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A very moist air mass was in place in the morning of the 6th as a band of convection in association with an MCV moved north over the area. Heavy rainfall of 3 to 4 inches fell over the central Piedmont, causing flash flooding in Wake and Nash Counties. By mid morning, a previously stall frontal zone lifted north over the area. As the MCV continued to move east, new convection developed and tracked northeastward, paralleling the surface front and weak surface low. A weak EF-0 and moved east for approximately 3 miles across southern Wilson County, where it caused minor damage to homes and a turkey farm. A very moist air mass was in place in the morning of the 6th as a band of convection in association with an MCV moved north over the area. Heavy rainfall of 3 to 4 inches fell over the central Piedmont, causing flash flooding in Wake and Nash Counties. By mid morning, a previously stall frontal zone lifted north over the area. As the MCV continued to move east, new convection developed and tracked northeastward, paralleling the surface front and weak surface low. A weak EF-0 and moved east for approximately 3 miles across southern Wilson County, where it caused minor damage to homes and a turkey farm. A very moist air mass was in place in the morning of the 6th as a band of convection in association with an MCV moved north over the area. Heavy rainfall of 3 to 4 inches fell over the central Piedmont, causing flash flooding in Wake and Nash Counties. By mid morning, a previously stall frontal zone lifted north over the area. As the MCV continued to move east, new convection developed and tracked northeastward, paralleling the surface front and weak surface low. A weak EF-0 and moved east for approximately 3 miles across southern Wilson County, where it caused minor damage to homes and a turkey farm.\nEvent Narrative: Pamlico Drive closed due to flash flooding. There were numerous reports of flooded road in North Raleigh. Several roads were closed including Craven Drive, Atlantic Avenue, Brentwood Road and Interstate 440 near Capital Boulevard. Numerous flooding was reported with flood waters infiltrating several businesses and residences. Eight people were displaced from a house at 320 Hill Street. Another 45 to 50 people at the Milner Hotel were taken to shelter. The lower units of the Capital Inn were also evacuated due to flood waters.  Monetary damages were unknown.",
+        "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00013722, approximately 36.4742 km away, between 2011-08-14 20:05:00 and 2011-08-14 22:01:00. The events included records with hailstones measuring 43.9375 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: An unseasonably strong amplifying upper level trough and attendant surface cold front moved east across the area during the afternoon. As the storms moved east off the higher terrain, they strengthened as the encountered moderate instability in place east of the mountains, producing widespread thunderstorm wind damage from the Triad to the Triangle. Hail ranging from quarter to golf ball size hail was reported, along with localized flash flooding. An unseasonably strong amplifying upper level trough and attendant surface cold front moved east across the area during the afternoon. As the storms moved east off the higher terrain, they strengthened as the encountered moderate instability in place east of the mountains, producing widespread thunderstorm wind damage from the Triad to the Triangle. Hail ranging from quarter to golf ball size hail was reported, along with localized flash flooding. An unseasonably strong amplifying upper level trough and attendant surface cold front moved east across the area during the afternoon. As the storms moved east off the higher terrain, they strengthened as the encountered moderate instability in place east of the mountains, producing widespread thunderstorm wind damage from the Triad to the Triangle. Hail ranging from quarter to golf ball size hail was reported, along with localized flash flooding. An unseasonably strong amplifying upper level trough and attendant surface cold front moved east across the area during the afternoon. As the storms moved east off the higher terrain, they strengthened as the encountered moderate instability in place east of the mountains, producing widespread thunderstorm wind damage from the Triad to the Triangle. Hail ranging from quarter to golf ball size hail was reported, along with localized flash flooding. An unseasonably strong amplifying upper level trough and attendant surface cold front moved east across the area during the afternoon. As the storms moved east off the higher terrain, they strengthened as the encountered moderate instability in place east of the mountains, producing widespread thunderstorm wind damage from the Triad to the Triangle. Hail ranging from quarter to golf ball size hail was reported, along with localized flash flooding. An unseasonably strong amplifying upper level trough and attendant surface cold front moved east across the area during the afternoon. As the storms moved east off the higher terrain, they strengthened as the encountered moderate instability in place east of the mountains, producing widespread thunderstorm wind damage from the Triad to the Triangle. Hail ranging from quarter to golf ball size hail was reported, along with localized flash flooding. An unseasonably strong amplifying upper level trough and attendant surface cold front moved east across the area during the afternoon. As the storms moved east off the higher terrain, they strengthened as the encountered moderate instability in place east of the mountains, producing widespread thunderstorm wind damage from the Triad to the Triangle. Hail ranging from quarter to golf ball size hail was reported, along with localized flash flooding. An unseasonably strong amplifying upper level trough and attendant surface cold front moved east across the area during the afternoon. As the storms moved east off the higher terrain, they strengthened as the encountered moderate instability in place east of the mountains, producing widespread thunderstorm wind damage from the Triad to the Triangle. Hail ranging from quarter to golf ball size hail was reported, along with localized flash flooding.\nEvent Narrative: One tree was blown down at the intersection of NC Highway 50 and NC Highway 201. One tree was blown down along NC Highway 210. One tree was blown down. One tree fell onto a house. No damage information was available. Numerous trees and power-lines were blown down across the county. Several trees were blown along a swath extending from Apex to west Raleigh, including down trees on N. Salem Street, Cary Parkway, Old Apex Road, West Skyhawk Drive, and  Harrison Avenue. Several trees were blown down in Franklinton.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 39.2816 km away, between 2011-08-21 15:50:00 and 2011-08-21 19:21:00. 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 vigorous shortwave enhanced a surface trough across the region and combined with strong instability and an increasingly moist air mass to produce scattered severe thunderstorms. Mostly wind damage occurred with these storms, although a couple of reports of one inch hail were received as well. Also, isolated flash flooding was observed, which resulted in a road closure and a few additional reports of minor street flooding were reported. A vigorous shortwave enhanced a surface trough across the region and combined with strong instability and an increasingly moist air mass to produce scattered severe thunderstorms. Mostly wind damage occurred with these storms, although a couple of reports of one inch hail were received as well. Also, isolated flash flooding was observed, which resulted in a road closure and a few additional reports of minor street flooding were reported. A vigorous shortwave enhanced a surface trough across the region and combined with strong instability and an increasingly moist air mass to produce scattered severe thunderstorms. Mostly wind damage occurred with these storms, although a couple of reports of one inch hail were received as well. Also, isolated flash flooding was observed, which resulted in a road closure and a few additional reports of minor street flooding were reported.\nEvent Narrative: A couple of trees were blown down along a swath from near Henderson to near Kittrell. A couple of trees were blown down along a mile long swath northwest of Pittsboro. A couple of trees were blown down along a swath from just west of Rolesville to several miles east of Rolesville.",
+        "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00013722, approximately 33.5114 km away, between 2011-08-29 15:26:00 and 2011-08-29 18:20:00. The events included records with hailstones measuring 32.25 inches.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 shortwave trough overspread a stalled surface front during peak heating. Scattered thunderstorms developed along the low-level baroclinic frontal zone, with the severe storms producing damaging thunderstorm wind gusts and quarter to half dollar size hail. A shortwave trough overspread a stalled surface front during peak heating. Scattered thunderstorms developed along the low-level baroclinic frontal zone, with the severe storms producing damaging thunderstorm wind gusts and quarter to half dollar size hail. A shortwave trough overspread a stalled surface front during peak heating. Scattered thunderstorms developed along the low-level baroclinic frontal zone, with the severe storms producing damaging thunderstorm wind gusts and quarter to half dollar size hail. A shortwave trough overspread a stalled surface front during peak heating. Scattered thunderstorms developed along the low-level baroclinic frontal zone, with the severe storms producing damaging thunderstorm wind gusts and quarter to half dollar size hail. A shortwave trough overspread a stalled surface front during peak heating. Scattered thunderstorms developed along the low-level baroclinic frontal zone, with the severe storms producing damaging thunderstorm wind gusts and quarter to half dollar size hail. A shortwave trough overspread a stalled surface front during peak heating. Scattered thunderstorms developed along the low-level baroclinic frontal zone, with the severe storms producing damaging thunderstorm wind gusts and quarter to half dollar size hail. A shortwave trough overspread a stalled surface front during peak heating. Scattered thunderstorms developed along the low-level baroclinic frontal zone, with the severe storms producing damaging thunderstorm wind gusts and quarter to half dollar size hail. A shortwave trough overspread a stalled surface front during peak heating. Scattered thunderstorms developed along the low-level baroclinic frontal zone, with the severe storms producing damaging thunderstorm wind gusts and quarter to half dollar size hail. A shortwave trough overspread a stalled surface front during peak heating. Scattered thunderstorms developed along the low-level baroclinic frontal zone, with the severe storms producing damaging thunderstorm wind gusts and quarter to half dollar size hail. A shortwave trough overspread a stalled surface front during peak heating. Scattered thunderstorms developed along the low-level baroclinic frontal zone, with the severe storms producing damaging thunderstorm wind gusts and quarter to half dollar size hail. A shortwave trough overspread a stalled surface front during peak heating. Scattered thunderstorms developed along the low-level baroclinic frontal zone, with the severe storms producing damaging thunderstorm wind gusts and quarter to half dollar size hail.\nEvent Narrative:  Several trees were blown down, including down trees near the intersection of Gus McGhee Road and Pearces Road.   One tree was blown down across Culbreth Road. Several trees were blown down along the swath, including a down tree onto a house on Johnny Burke Road and a down tree onto a vehicle on Moncure Pittsboro Road. Damages were estimated. Trees and power lines were blown down along Pea Ridge Road near the intersection of Cape Fear Drive and Woodhaven Drive. A couple of trees were blown down onto power-lines at the intersection of Creedmoor and Lynn Road and at the intersection of New Hope and Buffalo Roads.  Several trees were blown down. Numerous trees were blown down along the swath, including two trees blocking traffic on Turner Road. A tree was also reported to have fallen onto a house.",
+        "The following events were reported: Flash Flood, Thunderstorm Wind. These occurred near station USW00013722, approximately 31.5962 km away, between 2011-09-06 13:32:00 and 2011-09-06 23:30:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: As the remnants of Tropical Storm Lee tracked along a frontal zone that extended from the southern Appalachians into central Virginia, heavy rain and severe storms spread into central North Carolina. The initial severe weather threat, during the early morning hours, was tornadoes, due to the highly sheared environment associated with the former tropical cyclone. As the day progressed, and the remnant low of Lee continued to weaken, the severe weather threat transitioned to straight line winds, as instability increased with the heating of the day. As the remnants of Tropical Storm Lee tracked along a frontal zone that extended from the southern Appalachians into central Virginia, heavy rain and severe storms spread into central North Carolina. The initial severe weather threat, during the early morning hours, was tornadoes, due to the highly sheared environment associated with the former tropical cyclone. As the day progressed, and the remnant low of Lee continued to weaken, the severe weather threat transitioned to straight line winds, as instability increased with the heating of the day.\nEvent Narrative: Several tall pine trees were snapped by the wind. Multiple street closings due to high water were reported by law enforcement in Durham. The intersection of Berkely Street and Englewood Avenue was impassable due to flooding. Also, the intersection of Morrene Road and Tremont Drive was flooded. Indian Trail in Durham was closed due to rising water. High water also forced the closure of the intersection of North Alston Avenue and Juniper Street.",
+        "The following events were reported: Flash Flood. These occurred near station USW00013722, approximately 12.5184 km away, between 2011-09-21 20:50:00 and 2011-09-21 21:50:00.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 deep upper trough that extended from the upper Great Lakes to the Gulf of Mexico resulted in deep southwesterly flow across the region, allowing copious amounts of Gulf and Atlantic moisture to stream into the area. A disturbance in the southwesterly flow aloft triggered storms to develop over central North Carolina. Training of slow moving thunderstorms, with rainfall rates in excess of 2 inches per hour, caused flash flooding in Raleigh.\nEvent Narrative: Multiple roads were blocked across Raleigh due to flooding, including Blue Ridge Road at Western Boulevard, Hillsboro Street near the Chapel Hill Road split and Avent Ferry Road at Trailwood Drive. Also, a vehicle stalled in approximately 3 feet of water on Old Wake Forest Road, with another stalled vehicle on Millbrook Road at Hoyle Drive. Monetary damage was estimated.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 17.1044 km away, between 2011-09-28 01:53:00 and 2011-09-28 01:55:00. 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 stalled deep upper level low was centered over the southern Great Lakes Region,|with southwest flow aloft present downstream of the upper low over the Carolinas. |An MCV emerged from convection moving across South Carolina and Georgia and produced a bookend vortex that moved northward into the area overnight. The storm produced thunderstorm wind damage across three counties and a lone report of quarter size hail.\nEvent Narrative: Several trees were blown down in the downtown area. One tree fell onto a house on Pershing Road and another tree fell onto a roof at 1335 Courtland Road. Monetary damages were unknown.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 40.631 km away, between 2011-12-07 17:40:00 and 2011-12-07 17:45:00. 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 shallow line of storms developed along a cold front and in advance of an increasingly negative tilted trough as it moved across the southern Appalachians. Thunderstorm wind gusts of 50 to 60 mph resulted in scattered reported of down trees and power-lines. One person was injured when a tree crashed through a mobile home in Moore County. A shallow line of storms developed along a cold front and in advance of an increasingly negative tilted trough as it moved across the southern Appalachians. Thunderstorm wind gusts of 50 to 60 mph resulted in scattered reported of down trees and power-lines. One person was injured when a tree crashed through a mobile home in Moore County.\nEvent Narrative: One tree was blown down on Sam Moss Hayes Road. A down tree was blocking traffic on Lynn Bank Estates Road.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 24.4088 km away, between 2012-02-24 16:41:00 and 2012-02-24 17:45:00. 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: As very strong jet stream winds overspread the area, a line of storms in advance of an eastward moving cold front crossed the mountains and moved into the North Carolina Western Piedmont during the afternoon. The line went on to produce wind damage in the western Piedmont, before it weaken as it moved east into a more stable airmass in place across eastern North Carolina. As very strong jet stream winds overspread the area, a line of storms in advance of an eastward moving cold front crossed the mountains and moved into the North Carolina Western Piedmont during the afternoon. The line went on to produce wind damage in the western Piedmont, before it weaken as it moved east into a more stable airmass in place across eastern North Carolina. As very strong jet stream winds overspread the area, a line of storms in advance of an eastward moving cold front crossed the mountains and moved into the North Carolina Western Piedmont during the afternoon. The line went on to produce wind damage in the western Piedmont, before it weaken as it moved east into a more stable airmass in place across eastern North Carolina.\nEvent Narrative: Several trees were blown down from Hurdle Mills to the near Person-Orange County line. One tree was blown down between Western Blvd. and Hillsborough Street. Scattered trees and power-lines were blown down throughout the county.",
+        "The following events were reported: Hail, Lightning. These occurred near station USW00013722, approximately 28.6988 km away, between 2012-03-20 16:54:00 and 2012-03-20 22:33:00. The events included records with hailstones measuring 1.0 inches.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: With a mid level ridge to the west of the area and an upper low to the east, central North Carolina was dominated by northwesterly flow aloft. As a perturbation in this northwesterly flow aloft moved across the region, it combined with a moist air mass, steep mid level lapse rates and associated instability to produce isolated to scattered convection. A few of these storms became severe, producing quarter sized hail and some flash flooding. Also, these storms were prolific lightning producers and caused several house fires. With a mid level ridge to the west of the area and an upper low to the east, central North Carolina was dominated by northwesterly flow aloft. As a perturbation in this northwesterly flow aloft moved across the region, it combined with a moist air mass, steep mid level lapse rates and associated instability to produce isolated to scattered convection. A few of these storms became severe, producing quarter sized hail and some flash flooding. Also, these storms were prolific lightning producers and caused several house fires.\nEvent Narrative: Lightning struck a house causing a fire and resulting in $100,000 worth of damages. The damage was confined to the attic and the roof. Quarter size hail was reported along a swath from 4 miles west of Bunn to 3 miles west southwest of Bunn on Bob Richards Road.",
+        "The following events were reported: Hail. These occurred near station USW00013722, approximately 23.8794 km away, between 2012-03-24 18:00:00 and 2012-03-24 18:20:00. The events included records with hailstones measuring 1.125 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A strong upper level low approaching the region interacted with a weak frontal zone producing scattered convection across the area. With peak heating, instability increased across the region and with relatively low freezing levels, numerous reports of large hail accompanied the scattered convection that developed. There was also isolated wind damage. A strong upper level low approaching the region interacted with a weak frontal zone producing scattered convection across the area. With peak heating, instability increased across the region and with relatively low freezing levels, numerous reports of large hail accompanied the scattered convection that developed. There was also isolated wind damage.\nEvent Narrative: Quarter sized hail was reported along a swath from the city of Hillsborough to a couple of miles southeast of the city. Half dollar sized hail was reported near Durham.",
+        "The following events were reported: Hail. These occurred near station USW00013722, approximately 11.4806 km away, between 2012-03-31 22:48:00 and 2012-03-31 23:10:00. The events included records with hailstones measuring 1.75 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: As a shortwave trough advanced east across the area, convection developed along a stalled boundary near the North Carolina/Virginia border. An isolated storm moving from west to east became severe as it moved across Wake County, including the city of Raleigh. Numerous reports of hail ranging in size from quarter to golf ball were reported.\nEvent Narrative: Widespread reports of hail ranging in size from quarters to golf balls were received along a swath from Cary to Raleigh to several miles southwest of Raleigh.",
+        "The following events were reported: Hail. These occurred near station USW00013722, approximately 26.3859 km away, between 2012-05-01 17:15:00 and 2012-05-01 17:51:00. 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: An upper level disturbance tracked across portions of the Mid Atlantic Region and interacted with a moist and unstable low level air mass causing scattered showers and storms to develop across the Northern Piedmont of central North Carolina. Some of these storms became severe and produced damaging winds and large hail. An upper level disturbance tracked across portions of the Mid Atlantic Region and interacted with a moist and unstable low level air mass causing scattered showers and storms to develop across the Northern Piedmont of central North Carolina. Some of these storms became severe and produced damaging winds and large hail. An upper level disturbance tracked across portions of the Mid Atlantic Region and interacted with a moist and unstable low level air mass causing scattered showers and storms to develop across the Northern Piedmont of central North Carolina. Some of these storms became severe and produced damaging winds and large hail. An upper level disturbance tracked across portions of the Mid Atlantic Region and interacted with a moist and unstable low level air mass causing scattered showers and storms to develop across the Northern Piedmont of central North Carolina. Some of these storms became severe and produced damaging winds and large hail. An upper level disturbance tracked across portions of the Mid Atlantic Region and interacted with a moist and unstable low level air mass causing scattered showers and storms to develop across the Northern Piedmont of central North Carolina. Some of these storms became severe and produced damaging winds and large hail. An upper level disturbance tracked across portions of the Mid Atlantic Region and interacted with a moist and unstable low level air mass causing scattered showers and storms to develop across the Northern Piedmont of central North Carolina. Some of these storms became severe and produced damaging winds and large hail.\nEvent Narrative:  Quarter sized hail was reported covering the ground at Oak Forest Drive and Guess Road. Ping pong ball sized was reported covering the ground near Guess Road and Milton Road. Quarter size hail was reported at Cabin Branch Drive and Vintage Hill Parkway. Quarter size hail was reported at Barclay Drive and Smith Drive.",
+        "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00013722, approximately 34.077 km away, between 2012-05-04 17:27:00 and 2012-05-04 17:58:00. The events included records with hailstones measuring 25.375 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A mid level trough axis tracked across central NC and interacted with a moderately unstable atmosphere and produced scattered showers and thunderstorms. A few of these storms became severe along and east of the piedmont trough across the Coastal Plain and Northeast Piedmont. A mid level trough axis tracked across central NC and interacted with a moderately unstable atmosphere and produced scattered showers and thunderstorms. A few of these storms became severe along and east of the piedmont trough across the Coastal Plain and Northeast Piedmont.\nEvent Narrative:  One tree was reported down across a road near Covered Bridge Road.",
+        "The following events were reported: Hail. These occurred near station USW00013722, approximately 4.9062 km away, between 2012-05-05 13:37:00 and 2012-05-05 13:37:00. 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 crossed central North Carolina and interacted with a moderately unstable air mass. Scattered showers and thunderstorms developed along and in advance of the front. One thunderstorm became severe and caused damage to a house in Cumberland County, North Carolina.\nEvent Narrative:",
+        "The following events were reported: Lightning, Thunderstorm Wind. These occurred near station USW00013722, approximately 22.1372 km away, between 2012-05-09 14:47:00 and 2012-05-09 15:45:00.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 9500.0 and crop damage of 0.0. \n\nEpisode Narrative: A cold front moved into central North Carolina and interacted with an unstable air mass to produce scattered showers and thunderstorms. Some of these storms became strong to severe across portions of the Piedmont and Coastal Plain of central North Carolina. A cold front moved into central North Carolina and interacted with an unstable air mass to produce scattered showers and thunderstorms. Some of these storms became strong to severe across portions of the Piedmont and Coastal Plain of central North Carolina. A cold front moved into central North Carolina and interacted with an unstable air mass to produce scattered showers and thunderstorms. Some of these storms became strong to severe across portions of the Piedmont and Coastal Plain of central North Carolina. A cold front moved into central North Carolina and interacted with an unstable air mass to produce scattered showers and thunderstorms. Some of these storms became strong to severe across portions of the Piedmont and Coastal Plain of central North Carolina. A cold front moved into central North Carolina and interacted with an unstable air mass to produce scattered showers and thunderstorms. Some of these storms became strong to severe across portions of the Piedmont and Coastal Plain of central North Carolina. A cold front moved into central North Carolina and interacted with an unstable air mass to produce scattered showers and thunderstorms. Some of these storms became strong to severe across portions of the Piedmont and Coastal Plain of central North Carolina. A cold front moved into central North Carolina and interacted with an unstable air mass to produce scattered showers and thunderstorms. Some of these storms became strong to severe across portions of the Piedmont and Coastal Plain of central North Carolina. A cold front moved into central North Carolina and interacted with an unstable air mass to produce scattered showers and thunderstorms. Some of these storms became strong to severe across portions of the Piedmont and Coastal Plain of central North Carolina. A cold front moved into central North Carolina and interacted with an unstable air mass to produce scattered showers and thunderstorms. Some of these storms became strong to severe across portions of the Piedmont and Coastal Plain of central North Carolina. A cold front moved into central North Carolina and interacted with an unstable air mass to produce scattered showers and thunderstorms. Some of these storms became strong to severe across portions of the Piedmont and Coastal Plain of central North Carolina. A cold front moved into central North Carolina and interacted with an unstable air mass to produce scattered showers and thunderstorms. Some of these storms became strong to severe across portions of the Piedmont and Coastal Plain of central North Carolina.\nEvent Narrative: One 4 inch diameter tree was snapped in half and partially blocking Manning Drive. One tree was reported down near Timber Drive and North Carolina Highway 50. A house was struck by lightning and caught on fire on Canolder Street. Three trees were reported down near High Gate Drive and Hurdle Court. One tree was reported down near Old Oxford Road and Red Mill Road. One tree was reported down in the 100 Block of West Knox Street. A large oak tree was reported down at Jenks Carpenter and Fryar Creek Roads. Several small trees and branches were blown down or snapped on the Eagle Ridge Golf Course. A vending machine and patio furniture was also blown over. One tree was reported on a house at 1119 Ralph Drive. Several trees were reported down in Chapel Hill, North Carolina. One tree was reported down across the intersection of Orange Grove Road and Dairyland Road.",
+        "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00013722, approximately 45.7809 km away, between 2012-05-15 18:50:00 and 2012-05-15 18:59:00. The events included records with hailstones measuring 26.375 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A slow moving cold front moved across portions of central North Carolina along with a series of embedded shortwave troughs aloft in the broad cyclonic flow aloft to produce scattered showers and thunderstorms across the Eastern Piedmont and Coastal Plain. Some of these storms became severe and produced damaging wind gusts and large hail. A slow moving cold front moved across portions of central North Carolina along with a series of embedded shortwave troughs aloft in the broad cyclonic flow aloft to produce scattered showers and thunderstorms across the Eastern Piedmont and Coastal Plain. Some of these storms became severe and produced damaging wind gusts and large hail.\nEvent Narrative:  A Franklin County Airport employee reported that a thunderstorm wind gust, estimated up to 60 miles per hour, blew a parked aircraft off its pad and displaced it several feet away. The aircraft landed upright and no damage was noted to it.",
+        "The following events were reported: Hail. These occurred near station USW00013722, approximately 25.9436 km away, between 2012-05-17 15:35:00 and 2012-05-17 15:35:00. 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: Showers and thunderstorms developed along a weakening cold front and subtle shortwave trough aloft. One storm became strong and produced nickel size hail near Holly Springs, North Carolina.\nEvent Narrative: Nickel size hail was reported near the Sunset Ridge Neighborhood.",
+        "The following events were reported: Hail. These occurred near station USW00013722, approximately 20.337 km away, between 2012-05-22 16:34:00 and 2012-05-22 16:50:00. The events included records with hailstones measuring 0.875 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A deepening upper level trough coupled with a surface trough and warm moist low level air mass across central North Carolina caused scattered to numerous showers and thunderstorms to develop. Some of these storms became severe producing large hail and damaging winds, along with flash flooding. A deepening upper level trough coupled with a surface trough and warm moist low level air mass across central North Carolina caused scattered to numerous showers and thunderstorms to develop. Some of these storms became severe producing large hail and damaging winds, along with flash flooding.\nEvent Narrative: Penny sized hail was reported near Interstate 85 at mile marker 186. Quarter sized hail was reported covering the ground along Interstate 85 near mile marker 184.",
+        "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00013722, approximately 31.9761 km away, between 2012-05-23 14:38:00 and 2012-05-23 16:45:00. The events included records with hailstones measuring 6.919411764705882 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: Daytime heating combined with a deep area of low pressure aloft to produced scattered to numerous showers and thunderstorms. Some of these showers and storms became strong to severe and produced large hail and damaging winds. Daytime heating combined with a deep area of low pressure aloft to produced scattered to numerous showers and thunderstorms. Some of these showers and storms became strong to severe and produced large hail and damaging winds. Daytime heating combined with a deep area of low pressure aloft to produced scattered to numerous showers and thunderstorms. Some of these showers and storms became strong to severe and produced large hail and damaging winds. Daytime heating combined with a deep area of low pressure aloft to produced scattered to numerous showers and thunderstorms. Some of these showers and storms became strong to severe and produced large hail and damaging winds. Daytime heating combined with a deep area of low pressure aloft to produced scattered to numerous showers and thunderstorms. Some of these showers and storms became strong to severe and produced large hail and damaging winds. Daytime heating combined with a deep area of low pressure aloft to produced scattered to numerous showers and thunderstorms. Some of these showers and storms became strong to severe and produced large hail and damaging winds. Daytime heating combined with a deep area of low pressure aloft to produced scattered to numerous showers and thunderstorms. Some of these showers and storms became strong to severe and produced large hail and damaging winds. Daytime heating combined with a deep area of low pressure aloft to produced scattered to numerous showers and thunderstorms. Some of these showers and storms became strong to severe and produced large hail and damaging winds. Daytime heating combined with a deep area of low pressure aloft to produced scattered to numerous showers and thunderstorms. Some of these showers and storms became strong to severe and produced large hail and damaging winds. Daytime heating combined with a deep area of low pressure aloft to produced scattered to numerous showers and thunderstorms. Some of these showers and storms became strong to severe and produced large hail and damaging winds. Daytime heating combined with a deep area of low pressure aloft to produced scattered to numerous showers and thunderstorms. Some of these showers and storms became strong to severe and produced large hail and damaging winds. Daytime heating combined with a deep area of low pressure aloft to produced scattered to numerous showers and thunderstorms. Some of these showers and storms became strong to severe and produced large hail and damaging winds. Daytime heating combined with a deep area of low pressure aloft to produced scattered to numerous showers and thunderstorms. Some of these showers and storms became strong to severe and produced large hail and damaging winds. Daytime heating combined with a deep area of low pressure aloft to produced scattered to numerous showers and thunderstorms. Some of these showers and storms became strong to severe and produced large hail and damaging winds. Daytime heating combined with a deep area of low pressure aloft to produced scattered to numerous showers and thunderstorms. Some of these showers and storms became strong to severe and produced large hail and damaging winds. Daytime heating combined with a deep area of low pressure aloft to produced scattered to numerous showers and thunderstorms. Some of these showers and storms became strong to severe and produced large hail and damaging winds. Daytime heating combined with a deep area of low pressure aloft to produced scattered to numerous showers and thunderstorms. Some of these showers and storms became strong to severe and produced large hail and damaging winds.\nEvent Narrative:  Quarter size hail was reported near Interstate 40 at exit 319.  Golf ball size hail was reported near Tower Road at Guy Road.   Half dollar size hail was reported at the intersection of United States Highway 70 and Raynor Road. Half dollar size hail was reported near Business 70 at Jog Road. Nickel to quarter size hail was reported along Buffaloe Road. Quarter size hail was reported near Fox Road. Quarter size hail was reported at North Carolina Highway 98 and United States Highway 1.   Golf ball size hail was reported near Guy road. Some cars received minor hail damage from the hail. Quarter size hail was reported near Buffalo Mill Road. A flag pole was bent in half at Capital Boulevard and Burlington Mills Road. One tree was reported down across United States Highway 1 and Jenkins Road.",
+        "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00013722, approximately 40.5814 km away, between 2012-06-01 12:28:00 and 2012-06-01 15:44:00. The events included records with hailstones measuring 33.791666666666664 inches.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 140000.0 and crop damage of 0.0. \n\nEpisode Narrative: A broken band of storms developed across the Carolinas along a pre-frontal surface trough and in advance of a negative tilted upper trough and closed low over the southern Ohio Valley. Thunderstorm wind damage was extensive across central North Carolina with a few storms producing hail as large as golf balls. A broken band of storms developed across the Carolinas along a pre-frontal surface trough and in advance of a negative tilted upper trough and closed low over the southern Ohio Valley. Thunderstorm wind damage was extensive across central North Carolina with a few storms producing hail as large as golf balls. A broken band of storms developed across the Carolinas along a pre-frontal surface trough and in advance of a negative tilted upper trough and closed low over the southern Ohio Valley. Thunderstorm wind damage was extensive across central North Carolina with a few storms producing hail as large as golf balls. A broken band of storms developed across the Carolinas along a pre-frontal surface trough and in advance of a negative tilted upper trough and closed low over the southern Ohio Valley. Thunderstorm wind damage was extensive across central North Carolina with a few storms producing hail as large as golf balls. A broken band of storms developed across the Carolinas along a pre-frontal surface trough and in advance of a negative tilted upper trough and closed low over the southern Ohio Valley. Thunderstorm wind damage was extensive across central North Carolina with a few storms producing hail as large as golf balls. A broken band of storms developed across the Carolinas along a pre-frontal surface trough and in advance of a negative tilted upper trough and closed low over the southern Ohio Valley. Thunderstorm wind damage was extensive across central North Carolina with a few storms producing hail as large as golf balls.\nEvent Narrative: Law enforcement reported a downed tree onto a mobile home. Nearly a dozen trees were blown down and snapped in half. There was some moderate roof damage to several structures, including a smoke house. Numerous tree and large tree limbs were blown down inside the city limits of Mebane. One large oak tree with a base of more than 10 feet in diameter, fell onto a home. The home was a total loss. There were no injuries.   A trained spotter reported one tree blown down at Old Watkins and Forestville Roads.|A downed tree also fell across power lines along Highway 98.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 36.5992 km away, between 2012-06-29 21:55:00 and 2012-06-29 22:46:00. 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 25000.0 and crop damage of 0.0. \n\nEpisode Narrative: With much of the midwest and eastern United States experiencing a record breaking heat wave, a derecho, producing upwards of 90 mph winds, developed and moved across the Ohio Valley and into the Mid Atlantic, resulting in widespread damage and millions of power outages along its path. Triple digit heat across the region resulted in a very unstable atmosphere and with temperatures still in the upper 80s to lower 90s late into the evening, enough instability remained over the area and was able to sustain the derecho as it moved into the region. While central North Carolina only experienced the southern fringe of this powerful storm, widespread trees and power lines were blown down along a long swath of the forecast area, stretching from the Northern Piedmont to the Coastal Plain. With much of the midwest and eastern United States experiencing a record breaking heat wave, a derecho, producing upwards of 90 mph winds, developed and moved across the Ohio Valley and into the Mid Atlantic, resulting in widespread damage and millions of power outages along its path. Triple digit heat across the region resulted in a very unstable atmosphere and with temperatures still in the upper 80s to lower 90s late into the evening, enough instability remained over the area and was able to sustain the derecho as it moved into the region. While central North Carolina only experienced the southern fringe of this powerful storm, widespread trees and power lines were blown down along a long swath of the forecast area, stretching from the Northern Piedmont to the Coastal Plain. With much of the midwest and eastern United States experiencing a record breaking heat wave, a derecho, producing upwards of 90 mph winds, developed and moved across the Ohio Valley and into the Mid Atlantic, resulting in widespread damage and millions of power outages along its path. Triple digit heat across the region resulted in a very unstable atmosphere and with temperatures still in the upper 80s to lower 90s late into the evening, enough instability remained over the area and was able to sustain the derecho as it moved into the region. While central North Carolina only experienced the southern fringe of this powerful storm, widespread trees and power lines were blown down along a long swath of the forecast area, stretching from the Northern Piedmont to the Coastal Plain. With much of the midwest and eastern United States experiencing a record breaking heat wave, a derecho, producing upwards of 90 mph winds, developed and moved across the Ohio Valley and into the Mid Atlantic, resulting in widespread damage and millions of power outages along its path. Triple digit heat across the region resulted in a very unstable atmosphere and with temperatures still in the upper 80s to lower 90s late into the evening, enough instability remained over the area and was able to sustain the derecho as it moved into the region. While central North Carolina only experienced the southern fringe of this powerful storm, widespread trees and power lines were blown down along a long swath of the forecast area, stretching from the Northern Piedmont to the Coastal Plain. With much of the midwest and eastern United States experiencing a record breaking heat wave, a derecho, producing upwards of 90 mph winds, developed and moved across the Ohio Valley and into the Mid Atlantic, resulting in widespread damage and millions of power outages along its path. Triple digit heat across the region resulted in a very unstable atmosphere and with temperatures still in the upper 80s to lower 90s late into the evening, enough instability remained over the area and was able to sustain the derecho as it moved into the region. While central North Carolina only experienced the southern fringe of this powerful storm, widespread trees and power lines were blown down along a long swath of the forecast area, stretching from the Northern Piedmont to the Coastal Plain. With much of the midwest and eastern United States experiencing a record breaking heat wave, a derecho, producing upwards of 90 mph winds, developed and moved across the Ohio Valley and into the Mid Atlantic, resulting in widespread damage and millions of power outages along its path. Triple digit heat across the region resulted in a very unstable atmosphere and with temperatures still in the upper 80s to lower 90s late into the evening, enough instability remained over the area and was able to sustain the derecho as it moved into the region. While central North Carolina only experienced the southern fringe of this powerful storm, widespread trees and power lines were blown down along a long swath of the forecast area, stretching from the Northern Piedmont to the Coastal Plain.\nEvent Narrative: A large tree was snapped in half about 40 feet off the ground and numerous large limbs were blown down near Saxapahaw. Also, a roof was blown off of a carport in the same area. Numerous trees were blown down throughout the county, especially along a swath from Oxford to near Oak Hill. Numerous trees and power lines were blown down across the city of Durham, with one tree falling onto a van. One tree was blown down near Kittrell. Numerous trees were blown down throughout the county. A tree and several power lines were blown down along a swath from several miles south of Fuquay-Varina to several miles southwest of Angier.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 41.6198 km away, between 2012-06-30 22:10:00 and 2012-06-30 22:41:00. 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: In the midst of a heat wave that feature triple digit readings, isolated thunderstorms developed late in the day across the central Piedmont of North Carolina. In the midst of a heat wave that feature triple digit readings, isolated thunderstorms developed late in the day across the central Piedmont of North Carolina.\nEvent Narrative: Local law enforcement reported two downed trees on Buckhorn Road and Miller Road. Local law enforcement reported trees down near the intersections of Bason Road and Chris Street, Vickers Street and S. 8th Street, on S. 5th Street, and on Boswell Road.",
+        "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00013722, approximately 24.1338 km away, between 2012-07-01 13:38:00 and 2012-07-01 14:42:00. The events included records with hailstones measuring 10.983333333333333 inches.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 lee side surface trough interacted with a very unstable atmosphere and produced clusters of showers and thunderstorms. Some of these storms became severe and produce large hail and damaging winds across all of central North Carolina. A lee side surface trough interacted with a very unstable atmosphere and produced clusters of showers and thunderstorms. Some of these storms became severe and produce large hail and damaging winds across all of central North Carolina. A lee side surface trough interacted with a very unstable atmosphere and produced clusters of showers and thunderstorms. Some of these storms became severe and produce large hail and damaging winds across all of central North Carolina. A lee side surface trough interacted with a very unstable atmosphere and produced clusters of showers and thunderstorms. Some of these storms became severe and produce large hail and damaging winds across all of central North Carolina. A lee side surface trough interacted with a very unstable atmosphere and produced clusters of showers and thunderstorms. Some of these storms became severe and produce large hail and damaging winds across all of central North Carolina. A lee side surface trough interacted with a very unstable atmosphere and produced clusters of showers and thunderstorms. Some of these storms became severe and produce large hail and damaging winds across all of central North Carolina. A lee side surface trough interacted with a very unstable atmosphere and produced clusters of showers and thunderstorms. Some of these storms became severe and produce large hail and damaging winds across all of central North Carolina. A lee side surface trough interacted with a very unstable atmosphere and produced clusters of showers and thunderstorms. Some of these storms became severe and produce large hail and damaging winds across all of central North Carolina. A lee side surface trough interacted with a very unstable atmosphere and produced clusters of showers and thunderstorms. Some of these storms became severe and produce large hail and damaging winds across all of central North Carolina. A lee side surface trough interacted with a very unstable atmosphere and produced clusters of showers and thunderstorms. Some of these storms became severe and produce large hail and damaging winds across all of central North Carolina. A lee side surface trough interacted with a very unstable atmosphere and produced clusters of showers and thunderstorms. Some of these storms became severe and produce large hail and damaging winds across all of central North Carolina. A lee side surface trough interacted with a very unstable atmosphere and produced clusters of showers and thunderstorms. Some of these storms became severe and produce large hail and damaging winds across all of central North Carolina. A lee side surface trough interacted with a very unstable atmosphere and produced clusters of showers and thunderstorms. Some of these storms became severe and produce large hail and damaging winds across all of central North Carolina. A lee side surface trough interacted with a very unstable atmosphere and produced clusters of showers and thunderstorms. Some of these storms became severe and produce large hail and damaging winds across all of central North Carolina. A lee side surface trough interacted with a very unstable atmosphere and produced clusters of showers and thunderstorms. Some of these storms became severe and produce large hail and damaging winds across all of central North Carolina.\nEvent Narrative: One tree was reported down on North Carolina Highway 98.  Golf ball size hail was reported near the intersection of Season Drive and Six Forks Road.     Hail up to the size of quarters was reported covering I-540. A tree was uprooted and blown over onto a fence along Pulley Town Road.    Golf ball size hail was reported covering the ground. Quarter size hail was reported at Lennox Drive and Grovewood Drive. Numerous trees were reported down across Oxford, NC, including trees on houses along Coggeshall Street, Kearney Avenue, and College Street.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 19.2083 km away, between 2012-07-03 19:10:00 and 2012-07-03 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 4000.0 and crop damage of 0.0. \n\nEpisode Narrative: Intense surface heating and a moist and moderately unstable atmosphere allowed a few severe thunderstorms to develop. Intense surface heating and a moist and moderately unstable atmosphere allowed a few severe thunderstorms to develop. Intense surface heating and a moist and moderately unstable atmosphere allowed a few severe thunderstorms to develop. Intense surface heating and a moist and moderately unstable atmosphere allowed a few severe thunderstorms to develop. Intense surface heating and a moist and moderately unstable atmosphere allowed a few severe thunderstorms to develop.\nEvent Narrative: A couple of trees were reported down on Eva Mae Road. One tree was reported down across Lake Boone Trail at I-440. One tree was reported down at Van Dyke Avenue and Chamberlain Street. Powers lines were reported down near Brentwood Road and Atlantic Avenue. As a result 4500 customers lost power. Several trees were reported down on Johnson Pond Road.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 12.8181 km away, between 2012-07-04 15:25:00 and 2012-07-04 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 6000.0 and crop damage of 0.0. \n\nEpisode Narrative: Scattered showers and thunderstorms developed along a lee side trough across the Northeast Piedmont, Sandhills, and Coastal Plain. Some of these storms became severe and produced damaging winds and a few quarter sized hail reports as an upper level disturbance moved across the area in the late afternoon into the evening time frame. Scattered showers and thunderstorms developed along a lee side trough across the Northeast Piedmont, Sandhills, and Coastal Plain. Some of these storms became severe and produced damaging winds and a few quarter sized hail reports as an upper level disturbance moved across the area in the late afternoon into the evening time frame. Scattered showers and thunderstorms developed along a lee side trough across the Northeast Piedmont, Sandhills, and Coastal Plain. Some of these storms became severe and produced damaging winds and a few quarter sized hail reports as an upper level disturbance moved across the area in the late afternoon into the evening time frame. Scattered showers and thunderstorms developed along a lee side trough across the Northeast Piedmont, Sandhills, and Coastal Plain. Some of these storms became severe and produced damaging winds and a few quarter sized hail reports as an upper level disturbance moved across the area in the late afternoon into the evening time frame.\nEvent Narrative: One tree was reported down in the 4800 block of Yadkin Drive. Multiple trees were reported down, including one on a house. One tree was blown down at the corner of Vestavia Woods Drive and Hepworth Court. Power lines were reported down on Alleghany Drive.",
+        "The following events were reported: Lightning, Thunderstorm Wind. These occurred near station USW00013722, approximately 35.4063 km away, between 2012-07-05 12:55:00 and 2012-07-05 15:58:00.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: Intense heat combined with modest instability and a upper level disturbance which moved across the area allowed clusters of showers and storms to develop. Many of these storms became severe and produced damaging wind gusts. Intense heat combined with modest instability and a upper level disturbance which moved across the area allowed clusters of showers and storms to develop. Many of these storms became severe and produced damaging wind gusts. Intense heat combined with modest instability and a upper level disturbance which moved across the area allowed clusters of showers and storms to develop. Many of these storms became severe and produced damaging wind gusts. Intense heat combined with modest instability and a upper level disturbance which moved across the area allowed clusters of showers and storms to develop. Many of these storms became severe and produced damaging wind gusts. Intense heat combined with modest instability and a upper level disturbance which moved across the area allowed clusters of showers and storms to develop. Many of these storms became severe and produced damaging wind gusts. Intense heat combined with modest instability and a upper level disturbance which moved across the area allowed clusters of showers and storms to develop. Many of these storms became severe and produced damaging wind gusts. Intense heat combined with modest instability and a upper level disturbance which moved across the area allowed clusters of showers and storms to develop. Many of these storms became severe and produced damaging wind gusts. Intense heat combined with modest instability and a upper level disturbance which moved across the area allowed clusters of showers and storms to develop. Many of these storms became severe and produced damaging wind gusts. Intense heat combined with modest instability and a upper level disturbance which moved across the area allowed clusters of showers and storms to develop. Many of these storms became severe and produced damaging wind gusts. Intense heat combined with modest instability and a upper level disturbance which moved across the area allowed clusters of showers and storms to develop. Many of these storms became severe and produced damaging wind gusts. Intense heat combined with modest instability and a upper level disturbance which moved across the area allowed clusters of showers and storms to develop. Many of these storms became severe and produced damaging wind gusts. Intense heat combined with modest instability and a upper level disturbance which moved across the area allowed clusters of showers and storms to develop. Many of these storms became severe and produced damaging wind gusts. Intense heat combined with modest instability and a upper level disturbance which moved across the area allowed clusters of showers and storms to develop. Many of these storms became severe and produced damaging wind gusts. Intense heat combined with modest instability and a upper level disturbance which moved across the area allowed clusters of showers and storms to develop. Many of these storms became severe and produced damaging wind gusts. Intense heat combined with modest instability and a upper level disturbance which moved across the area allowed clusters of showers and storms to develop. Many of these storms became severe and produced damaging wind gusts. Intense heat combined with modest instability and a upper level disturbance which moved across the area allowed clusters of showers and storms to develop. Many of these storms became severe and produced damaging wind gusts. Intense heat combined with modest instability and a upper level disturbance which moved across the area allowed clusters of showers and storms to develop. Many of these storms became severe and produced damaging wind gusts.\nEvent Narrative: One tree was reported down on Cannady Road. Numerous trees were reported down near North Carolina Highway 57 and 157. Numerous trees were reported down along Kiger Road. Lightning struck a home on Poplar Drive. One tree was reported down at United States Highway 70A and Meadowlands Drive. A couple of trees were reported down on Walnut Grove Church Road near North Carolina Highway 86. One tree was blown down along Brassfield Church Road. One tree was reported down along Horseshoe Road. Several trees were reported down near Yates Mill Pond Road. One tree was reported down on Bertram Drive near Capital Boulevard. One large pine tree was blown over onto a truck. Two trees were reported down at a residence on Rock Cover Road. One tree was blown down along Old Goldston Road. One tree was blown into power lines along Old United States Highway 1. Multiple trees were reported down in the Bunn area. One large tree fell onto a car in the Brentmoor Apartment Complex near Capital Boulevard. Several trees were reported down along North Carolina 87 and Churchwood Lane, including two large uprooted pines. Power lines were also reported down in the area.",
+        "The following events were reported: Hail, Lightning, Thunderstorm Wind. These occurred near station USW00013722, approximately 18.1552 km away, between 2012-07-06 16:00:00 and 2012-07-06 16:35:00. The events included records with hailstones measuring 39.19444444444444 inches.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 12000.0 and crop damage of 0.0. \n\nEpisode Narrative: An upper level disturbance moved across central North Carolina and interacted with moderate to strong instability to trigger scattered showers and thunderstorms. Several of these storms became severe and produced damaging winds and a few isolated severe hail reports. An upper level disturbance moved across central North Carolina and interacted with moderate to strong instability to trigger scattered showers and thunderstorms. Several of these storms became severe and produced damaging winds and a few isolated severe hail reports. An upper level disturbance moved across central North Carolina and interacted with moderate to strong instability to trigger scattered showers and thunderstorms. Several of these storms became severe and produced damaging winds and a few isolated severe hail reports. An upper level disturbance moved across central North Carolina and interacted with moderate to strong instability to trigger scattered showers and thunderstorms. Several of these storms became severe and produced damaging winds and a few isolated severe hail reports. An upper level disturbance moved across central North Carolina and interacted with moderate to strong instability to trigger scattered showers and thunderstorms. Several of these storms became severe and produced damaging winds and a few isolated severe hail reports. An upper level disturbance moved across central North Carolina and interacted with moderate to strong instability to trigger scattered showers and thunderstorms. Several of these storms became severe and produced damaging winds and a few isolated severe hail reports. An upper level disturbance moved across central North Carolina and interacted with moderate to strong instability to trigger scattered showers and thunderstorms. Several of these storms became severe and produced damaging winds and a few isolated severe hail reports. An upper level disturbance moved across central North Carolina and interacted with moderate to strong instability to trigger scattered showers and thunderstorms. Several of these storms became severe and produced damaging winds and a few isolated severe hail reports. An upper level disturbance moved across central North Carolina and interacted with moderate to strong instability to trigger scattered showers and thunderstorms. Several of these storms became severe and produced damaging winds and a few isolated severe hail reports. An upper level disturbance moved across central North Carolina and interacted with moderate to strong instability to trigger scattered showers and thunderstorms. Several of these storms became severe and produced damaging winds and a few isolated severe hail reports. An upper level disturbance moved across central North Carolina and interacted with moderate to strong instability to trigger scattered showers and thunderstorms. Several of these storms became severe and produced damaging winds and a few isolated severe hail reports.\nEvent Narrative:   Three trees were reported down along Center Street between Satinwood Drive and Old Grove Lane. Power lines were reported down near United States Highway 1 and Ten Ten Road. One tree was reported down along United States Highway 64 Bypass near Zebulon. A large oak tree was reported down across Old Raleigh Road near the intersection with Buckingham Way. One tree was reported down at New Hope Church Road and Brentwood Road. One tree was reported down at Capital Boulevard and Calvary Drive. Two trees were reported down across Laurel Hollow Place. A fire at 1345 Legendary Lane was reported from a lightning strike. A fire was reported at 106 Carterwood Court, caused by a lightning strike.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 29.9786 km away, between 2012-07-09 13:51:00 and 2012-07-09 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 3500.0 and crop damage of 0.0. \n\nEpisode Narrative: Strong daytime heating resulted in moderate to strong destabilization across central North Carolina.  While initial convective started in proximity to a stalled surface boundary, convection quickly became dominated by convective outflow interaction and cell mergers that produced thunderstorm wind damage across the area with isolated flash flooding in Greensboro. Strong daytime heating resulted in moderate to strong destabilization across central North Carolina.  While initial convective started in proximity to a stalled surface boundary, convection quickly became dominated by convective outflow interaction and cell mergers that produced thunderstorm wind damage across the area with isolated flash flooding in Greensboro.\nEvent Narrative: One tree was blown down onto a power-line. A large limb was blown down onto a power-line which resulted in a blown transformer.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 27.0259 km away, between 2012-07-19 17:20:00 and 2012-07-19 17:20:00. 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: Another day of strong heating and a persistent Piedmont trough resulted in scattered afternoon/evening showers and thunderstorms. Several of the storms became severe, producing isolated wind damage.\nEvent Narrative: Two trees were blown down in Carrboro near Jones Ferry Road and Old Fayetteville Road, causing multiple power outages.",
+        "The following events were reported: Lightning, Thunderstorm Wind. These occurred near station USW00013722, approximately 41.4676 km away, between 2012-07-21 17:30:00 and 2012-07-21 19:15:00.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: With a nearly stationary front just to the north of central North Carolina and an approaching mid level trough/shear axis, scattered to numerous showers and thunderstorms developed during the afternoon/evening hours in a very moist and moderately unstable air mass. Several of these storms became severe, with damaging winds being the main issue, although one report of quarter sized hail was received. Also, some flash flooding occurred. With a nearly stationary front just to the north of central North Carolina and an approaching mid level trough/shear axis, scattered to numerous showers and thunderstorms developed during the afternoon/evening hours in a very moist and moderately unstable air mass. Several of these storms became severe, with damaging winds being the main issue, although one report of quarter sized hail was received. Also, some flash flooding occurred.\nEvent Narrative: Several trees were blown down along a swath from near Union Ridge to near Mebane. Lightning struck a home on Jamestown Road in Pittsboro causing a fire. The fire was contained to the attic. The home suffered fire damage in the attic and roof and some water damage was sustained to other parts of the house. Damage was estimated.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 26.7801 km away, between 2012-07-23 17:14:00 and 2012-07-23 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 11000.0 and crop damage of 0.0. \n\nEpisode Narrative: An upper level disturbance moved across central North Carolina during the late afternoon into the evening and interacted with a moist and unstable atmosphere to produce scattered showers and thunderstorms. Some of the thunderstorms became severe and produced damaging winds. An upper level disturbance moved across central North Carolina during the late afternoon into the evening and interacted with a moist and unstable atmosphere to produce scattered showers and thunderstorms. Some of the thunderstorms became severe and produced damaging winds. An upper level disturbance moved across central North Carolina during the late afternoon into the evening and interacted with a moist and unstable atmosphere to produce scattered showers and thunderstorms. Some of the thunderstorms became severe and produced damaging winds. An upper level disturbance moved across central North Carolina during the late afternoon into the evening and interacted with a moist and unstable atmosphere to produce scattered showers and thunderstorms. Some of the thunderstorms became severe and produced damaging winds. An upper level disturbance moved across central North Carolina during the late afternoon into the evening and interacted with a moist and unstable atmosphere to produce scattered showers and thunderstorms. Some of the thunderstorms became severe and produced damaging winds. An upper level disturbance moved across central North Carolina during the late afternoon into the evening and interacted with a moist and unstable atmosphere to produce scattered showers and thunderstorms. Some of the thunderstorms became severe and produced damaging winds.\nEvent Narrative: Several trees were reported down on power lines at 9319 North Roxboro Road. Two trees were reported down at McGees Crossroads. One tree was reported down across the intersection of Kittrell Drive and Cooleemee Drive. Several trees were reported down in the Lakeside Drive area. One tree was reported down on Grace Point Road. Seven trees were reported down in the Lake Jordan State Recreation area. One tree was reported to be down on a power line, with others down across roadways.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 22.7885 km away, between 2012-07-24 14:10:00 and 2012-07-24 14:55:00.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 64500.0 and crop damage of 0.0. \n\nEpisode Narrative: A very unstable airmass and deep dry sub cloud layer coupled with a disturbance which moved across the area during peak heating caused scattered to numerous showers and thunderstorms to develop in the afternoon into the evening. Many of these storms became severe and produces damaging wind gusts. A very unstable airmass and deep dry sub cloud layer coupled with a disturbance which moved across the area during peak heating caused scattered to numerous showers and thunderstorms to develop in the afternoon into the evening. Many of these storms became severe and produces damaging wind gusts. A very unstable airmass and deep dry sub cloud layer coupled with a disturbance which moved across the area during peak heating caused scattered to numerous showers and thunderstorms to develop in the afternoon into the evening. Many of these storms became severe and produces damaging wind gusts. A very unstable airmass and deep dry sub cloud layer coupled with a disturbance which moved across the area during peak heating caused scattered to numerous showers and thunderstorms to develop in the afternoon into the evening. Many of these storms became severe and produces damaging wind gusts. A very unstable airmass and deep dry sub cloud layer coupled with a disturbance which moved across the area during peak heating caused scattered to numerous showers and thunderstorms to develop in the afternoon into the evening. Many of these storms became severe and produces damaging wind gusts. A very unstable airmass and deep dry sub cloud layer coupled with a disturbance which moved across the area during peak heating caused scattered to numerous showers and thunderstorms to develop in the afternoon into the evening. Many of these storms became severe and produces damaging wind gusts. A very unstable airmass and deep dry sub cloud layer coupled with a disturbance which moved across the area during peak heating caused scattered to numerous showers and thunderstorms to develop in the afternoon into the evening. Many of these storms became severe and produces damaging wind gusts. A very unstable airmass and deep dry sub cloud layer coupled with a disturbance which moved across the area during peak heating caused scattered to numerous showers and thunderstorms to develop in the afternoon into the evening. Many of these storms became severe and produces damaging wind gusts. A very unstable airmass and deep dry sub cloud layer coupled with a disturbance which moved across the area during peak heating caused scattered to numerous showers and thunderstorms to develop in the afternoon into the evening. Many of these storms became severe and produces damaging wind gusts. A very unstable airmass and deep dry sub cloud layer coupled with a disturbance which moved across the area during peak heating caused scattered to numerous showers and thunderstorms to develop in the afternoon into the evening. Many of these storms became severe and produces damaging wind gusts. A very unstable airmass and deep dry sub cloud layer coupled with a disturbance which moved across the area during peak heating caused scattered to numerous showers and thunderstorms to develop in the afternoon into the evening. Many of these storms became severe and produces damaging wind gusts. A very unstable airmass and deep dry sub cloud layer coupled with a disturbance which moved across the area during peak heating caused scattered to numerous showers and thunderstorms to develop in the afternoon into the evening. Many of these storms became severe and produces damaging wind gusts. A very unstable airmass and deep dry sub cloud layer coupled with a disturbance which moved across the area during peak heating caused scattered to numerous showers and thunderstorms to develop in the afternoon into the evening. Many of these storms became severe and produces damaging wind gusts. A very unstable airmass and deep dry sub cloud layer coupled with a disturbance which moved across the area during peak heating caused scattered to numerous showers and thunderstorms to develop in the afternoon into the evening. Many of these storms became severe and produces damaging wind gusts. A very unstable airmass and deep dry sub cloud layer coupled with a disturbance which moved across the area during peak heating caused scattered to numerous showers and thunderstorms to develop in the afternoon into the evening. Many of these storms became severe and produces damaging wind gusts. A very unstable airmass and deep dry sub cloud layer coupled with a disturbance which moved across the area during peak heating caused scattered to numerous showers and thunderstorms to develop in the afternoon into the evening. Many of these storms became severe and produces damaging wind gusts. A very unstable airmass and deep dry sub cloud layer coupled with a disturbance which moved across the area during peak heating caused scattered to numerous showers and thunderstorms to develop in the afternoon into the evening. Many of these storms became severe and produces damaging wind gusts. A very unstable airmass and deep dry sub cloud layer coupled with a disturbance which moved across the area during peak heating caused scattered to numerous showers and thunderstorms to develop in the afternoon into the evening. Many of these storms became severe and produces damaging wind gusts. A very unstable airmass and deep dry sub cloud layer coupled with a disturbance which moved across the area during peak heating caused scattered to numerous showers and thunderstorms to develop in the afternoon into the evening. Many of these storms became severe and produces damaging wind gusts.\nEvent Narrative: One tree was blown down onto a car on South Columbia Street at UNC Chapel Hill. One adult and two high school students were inside the car at the time, but escaped without injuries. More than a dozen trees and power lines were reported down across the town of Chapel Hill. A tree fell on a car on Maiden Lane near North Carolina State University. One tree fell on a home in Apex, North Carolina causing damge to the home. One large tree was reported down on power lines near Old Greensboro Road. One tree was reported down on a fence along Gilmore Road. Several trees and power lines were reported down in Carrboro.  One tree was reported down on Leesville Road. One tree fell onto a truck near Hillsborough Street. One tree was reported down on I-440 near Glenwood Avenue. Multiple trees were reported down near I-40. One tree was reported down on Transylvania Avenue. One tree was reported down on Jones Family Road. One tree was reported down on White Oak Road. One tree was reported down on Ridge Road. Three trees were reported down at Smithfield Road and Grasshopper Road. Multiple trees were reported down along United States Highway 70 and 401 near Tryon Road. Two trees were reported down at 2552 River Road.",
+        "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00013722, approximately 39.8057 km away, between 2012-07-27 16:35:00 and 2012-07-27 18:40:00. The events included records with hailstones measuring 37.75 inches.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 313000.0 and crop damage of 0.0. \n\nEpisode Narrative: A band of strong to severe storms developed along a lee side trough and in advance of an amplifying long wave trough moving east over the Great Lakes. The line of storms produced scattered wind damage with one report of hail the size of quarters. A band of strong to severe storms developed along a lee side trough and in advance of an amplifying long wave trough moving east over the Great Lakes. The line of storms produced scattered wind damage with one report of hail the size of quarters. A band of strong to severe storms developed along a lee side trough and in advance of an amplifying long wave trough moving east over the Great Lakes. The line of storms produced scattered wind damage with one report of hail the size of quarters. A band of strong to severe storms developed along a lee side trough and in advance of an amplifying long wave trough moving east over the Great Lakes. The line of storms produced scattered wind damage with one report of hail the size of quarters.\nEvent Narrative: Numerous trees and power lines were blown down along a swath from near Elon College to Mebane. Mebane was especially hard hit, with damage to 15 structures and 9 vehicles. Several trees were blown down in the Louisburg area.  Several trees were blown down near Schley near the intersection of Breeze Road and Guess Road.",
+        "The following events were reported: Flash Flood, Thunderstorm Wind. These occurred near station USW00013722, approximately 22.9824 km away, between 2012-07-28 18:50:00 and 2012-07-28 23:00:00.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: Numerous thunderstorms in bands and clusters developed over central North Carolina |late in the afternoon and evening as a large scale trough amplified slowly over the region. The severe storms went on to produce damaging thunderstorm wind gusts with one report of isolated flash flooding. Numerous thunderstorms in bands and clusters developed over central North Carolina |late in the afternoon and evening as a large scale trough amplified slowly over the region. The severe storms went on to produce damaging thunderstorm wind gusts with one report of isolated flash flooding. Numerous thunderstorms in bands and clusters developed over central North Carolina |late in the afternoon and evening as a large scale trough amplified slowly over the region. The severe storms went on to produce damaging thunderstorm wind gusts with one report of isolated flash flooding. Numerous thunderstorms in bands and clusters developed over central North Carolina |late in the afternoon and evening as a large scale trough amplified slowly over the region. The severe storms went on to produce damaging thunderstorm wind gusts with one report of isolated flash flooding. Numerous thunderstorms in bands and clusters developed over central North Carolina |late in the afternoon and evening as a large scale trough amplified slowly over the region. The severe storms went on to produce damaging thunderstorm wind gusts with one report of isolated flash flooding. Numerous thunderstorms in bands and clusters developed over central North Carolina |late in the afternoon and evening as a large scale trough amplified slowly over the region. The severe storms went on to produce damaging thunderstorm wind gusts with one report of isolated flash flooding. Numerous thunderstorms in bands and clusters developed over central North Carolina |late in the afternoon and evening as a large scale trough amplified slowly over the region. The severe storms went on to produce damaging thunderstorm wind gusts with one report of isolated flash flooding. Numerous thunderstorms in bands and clusters developed over central North Carolina |late in the afternoon and evening as a large scale trough amplified slowly over the region. The severe storms went on to produce damaging thunderstorm wind gusts with one report of isolated flash flooding. Numerous thunderstorms in bands and clusters developed over central North Carolina |late in the afternoon and evening as a large scale trough amplified slowly over the region. The severe storms went on to produce damaging thunderstorm wind gusts with one report of isolated flash flooding. Numerous thunderstorms in bands and clusters developed over central North Carolina |late in the afternoon and evening as a large scale trough amplified slowly over the region. The severe storms went on to produce damaging thunderstorm wind gusts with one report of isolated flash flooding. Numerous thunderstorms in bands and clusters developed over central North Carolina |late in the afternoon and evening as a large scale trough amplified slowly over the region. The severe storms went on to produce damaging thunderstorm wind gusts with one report of isolated flash flooding.\nEvent Narrative: One tree was blown down. A couple of trees were blown down, with one down tree blocking Milton Road between Madden Avenue and Wendy Way. Two trees were blown down in the area. Tree blown down onto a house. No other information available. Several trees blown down on Marthas Chapel Road. A 66 mph wind gust was measure at the Raleigh-Durham International Airport. One tree was blown down. Two trees were blown along the swath, including one down tree near Buffaloe Road. Numerous trees were blown down throughout the county, especially west of Louisburg. Old Fearrington Road was closded due to flash flooding with area creek out of its banks. Several trees were blown along the swath.",
+        "The following events were reported: Flash Flood. These occurred near station USW00013722, approximately 16.9777 km away, between 2012-07-30 16:02:00 and 2012-07-30 16:25:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: With an upper level disturbance approaching from the northwest, convection initiated during peak heating along a stalled front draped across the Coastal Plain. With a very moist air mass in place (precipitable water values approaching 2 inches), these storms produced very heavy rain, even resulting in flash flooding across the Raleigh metro area.\nEvent Narrative: Flooding was reported at Atlantic Avenue and Hodges Street in northeast Raleigh. There was also flooding reported at Capital Boulevard and Hodges Street, with several lanes of traffic becoming impassible. An rainfall observer near these locations reported 2.25 inches of rain fell in 45 minutes.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 23.5209 km away, between 2012-08-01 16:12:00 and 2012-08-01 17:09:00. 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 mid/upper level through axis was located across western North Carolina. As a  disturbance aloft rotated through the base of the trough and eventually over our region in the southwesterly flow aloft, scattered showers and thunderstorms developed during the heating of the day, with a couple of the storms becoming severe in the moderately unstable air mass. A mid/upper level through axis was located across western North Carolina. As a  disturbance aloft rotated through the base of the trough and eventually over our region in the southwesterly flow aloft, scattered showers and thunderstorms developed during the heating of the day, with a couple of the storms becoming severe in the moderately unstable air mass.\nEvent Narrative: A couple of trees and power lines were blown down along a swath from near Falls Lake to near Wendell. A couple of trees were blown down around the Rolesville area.",
+        "The following events were reported: Hail. These occurred near station USW00013722, approximately 37.0476 km away, between 2012-08-02 14:41:00 and 2012-08-02 14:41:00. 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: With a broad area of troughing persisting across the East Coast, a strong vorticity center aloft and weak surface convergence combined with a moist and moderately unstable air mass and resulted in scattered showers and thunderstorms, mainly across the Coastal Plain. Numerous reports of wind damage and large hail were received, with flash flooding reported in the Fayetteville area.\nEvent Narrative: Quarter size hail was reported in Franklinton.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 31.7261 km away, between 2012-08-08 17:59:00 and 2012-08-08 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 750.0 and crop damage of 0.0. \n\nEpisode Narrative: Strong surface heating in advance of the passage of an upper level disturbance resulted in moderate destabilization across central North Carolina on the afternoon of the 8th. Storms developed quickly along the leading edge of lift associated with this upper level feature with three cluster of severe storms producing scattering wind damage across the area. Strong surface heating in advance of the passage of an upper level disturbance resulted in moderate destabilization across central North Carolina on the afternoon of the 8th. Storms developed quickly along the leading edge of lift associated with this upper level feature with three cluster of severe storms producing scattering wind damage across the area.\nEvent Narrative: A half dozen trees were blown down along the wind swath, including trees down onto power-lines on Pineview Drive in Wake Forest. One tree was blown down on Thanksgiving Fire Road.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 35.5013 km away, between 2012-09-02 20:15:00 and 2012-09-02 20:15:00. 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: Multicell clusters produced scattered thunderstorm wind damage during the afternoon and into the early evening hours on the second day of September.\nEvent Narrative: Downed tree blocking traffic at the intersection of Quail Roost Farm Road and N. Roxboro Road.",
+        "The following events were reported: Flash Flood, Thunderstorm Wind. These occurred near station USW00013722, approximately 27.3501 km away, between 2012-09-06 15:50:00 and 2012-09-06 18:14:00.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: An upper level disturbance and low level trough combined with a very moist air mass to produce scattered thunderstorms. Training of thunderstorms resulted in 2 to 3 inches of rainfall and minor flash flooding. Also, an isolated severe storm caused some minor wind damage. An upper level disturbance and low level trough combined with a very moist air mass to produce scattered thunderstorms. Training of thunderstorms resulted in 2 to 3 inches of rainfall and minor flash flooding. Also, an isolated severe storm caused some minor wind damage. An upper level disturbance and low level trough combined with a very moist air mass to produce scattered thunderstorms. Training of thunderstorms resulted in 2 to 3 inches of rainfall and minor flash flooding. Also, an isolated severe storm caused some minor wind damage.\nEvent Narrative: Several road closures due to flooding in the area, including Piney Mountain Road, MLK Jr. Boulevard, Carol Street, Hollow Street, Hillsborough Street, and Umstead Drive and Bradley Road. Power-lines were blown down at the intersection of Ranch Road and Little Creek Church Road. There were several road closures in the area due to flash flooding, including the intersection of Raleigh Boulevard and New Bern Avenue, Atlantic Avenue and Harrod Street, Peace Street and Wilmington Street, and Capital Boulevard near Wake Forest Road. There was also reports of vehicles stalled in flood waters.",
+        "The following events were reported: Flash Flood, Thunderstorm Wind. These occurred near station USW00013722, approximately 25.3917 km away, between 2012-09-08 16:45:00 and 2012-09-08 20:59:00.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 2250.0 and crop damage of 0.0. \n\nEpisode Narrative: A band of thunderstorms developed ahead of a cold front and produced scattered thunderstorm wind damage and isolated urban flooding from heavy rainfall of 1 to 2 inches. A band of thunderstorms developed ahead of a cold front and produced scattered thunderstorm wind damage and isolated urban flooding from heavy rainfall of 1 to 2 inches. A band of thunderstorms developed ahead of a cold front and produced scattered thunderstorm wind damage and isolated urban flooding from heavy rainfall of 1 to 2 inches. A band of thunderstorms developed ahead of a cold front and produced scattered thunderstorm wind damage and isolated urban flooding from heavy rainfall of 1 to 2 inches. A band of thunderstorms developed ahead of a cold front and produced scattered thunderstorm wind damage and isolated urban flooding from heavy rainfall of 1 to 2 inches.\nEvent Narrative: Several roads in the area were flooded, including Avent Ferry Road at Trailwood Road, Hillsborough Street near Chapel Hill Road, and Atlantic Avenue at Hodges Street. Water across the roadway at Atlantic Avenue and Hodges Street. A couple of trees and power-lines were blown down along Duke Street, Broad Street and near Avondale and Interstate 85. One tree was blown down on Castleberry Road near NC Highway 42. Another tree was reported down on some power-lines near Archer Lodge. A couple of trees were blown down with some trees down on power-lines.",
+        "The following events were reported: Flash Flood, Thunderstorm Wind, Tornado. These occurred near station USW00013722, approximately 38.6776 km away, between 2012-09-18 09:55:00 and 2012-09-18 16:00:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Multiple line segments of strong to severe storms developed over North Carolina as a compact but potent shortwave emanating from the gulf coast region and along the eastern flanks of a full latitude trough moved through the Carolinas.  The accompanying 50 to 60 knot mid level jet within a moist and unstable air mass produced scattered thunderstorm wind damage and an isolated EF-0 tornado near Zebulon. Multiple line segments of strong to severe storms developed over North Carolina as a compact but potent shortwave emanating from the gulf coast region and along the eastern flanks of a full latitude trough moved through the Carolinas.  The accompanying 50 to 60 knot mid level jet within a moist and unstable air mass produced scattered thunderstorm wind damage and an isolated EF-0 tornado near Zebulon. Multiple line segments of strong to severe storms developed over North Carolina as a compact but potent shortwave emanating from the gulf coast region and along the eastern flanks of a full latitude trough moved through the Carolinas.  The accompanying 50 to 60 knot mid level jet within a moist and unstable air mass produced scattered thunderstorm wind damage and an isolated EF-0 tornado near Zebulon. Multiple line segments of strong to severe storms developed over North Carolina as a compact but potent shortwave emanating from the gulf coast region and along the eastern flanks of a full latitude trough moved through the Carolinas.  The accompanying 50 to 60 knot mid level jet within a moist and unstable air mass produced scattered thunderstorm wind damage and an isolated EF-0 tornado near Zebulon. Multiple line segments of strong to severe storms developed over North Carolina as a compact but potent shortwave emanating from the gulf coast region and along the eastern flanks of a full latitude trough moved through the Carolinas.  The accompanying 50 to 60 knot mid level jet within a moist and unstable air mass produced scattered thunderstorm wind damage and an isolated EF-0 tornado near Zebulon. Multiple line segments of strong to severe storms developed over North Carolina as a compact but potent shortwave emanating from the gulf coast region and along the eastern flanks of a full latitude trough moved through the Carolinas.  The accompanying 50 to 60 knot mid level jet within a moist and unstable air mass produced scattered thunderstorm wind damage and an isolated EF-0 tornado near Zebulon.\nEvent Narrative: A 60-foot tree was topped off at about the 30-ffot level with large branches blown down. Several streets were flooded in the area including Six Forks Road, Wake Forest Road, and Atlantic Avenue and Interstate 440. A NWS damage survey found that a weak EF-0 tornado briefly touched down just west of the town of Zebulon. A well-defined damage path was found in a stand of trees of about one-half mile long and about 30 yards wide. Based on the type of trees affected and the magnitude of damage, the wind speeds are believed to have topped out at around 75 mph. No structural damage was found and there were no injuries or fatalities. A small cluster of trees were blown down at a private residence. Two trees were blown down at a private residence. Three trees were blown down.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 40.047 km away, between 2013-01-30 22:18:00 and 2013-01-30 23:00:00. 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 2500.0 and crop damage of 0.0. \n\nEpisode Narrative: Winds increased across central North Carolina ahead of a high amplitude trough aloft and a strong surface front. With an unseasonably warm and moist air mass in place, a squall line developed ahead of the approaching front, further enhancing the winds and causing wind damage. Winds increased across central North Carolina ahead of a high amplitude trough aloft and a strong surface front. With an unseasonably warm and moist air mass in place, a squall line developed ahead of the approaching front, further enhancing the winds and causing wind damage.\nEvent Narrative: Several trees and power lines were blown down along a swath from near Rougemont to near Surl. A 20 inch diameter tree was blown down and fell onto a home. The monetary damage was estimated.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 21.6058 km away, between 2013-04-19 17:27:00 and 2013-04-19 18:25:00.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 9500.0 and crop damage of 0.0. \n\nEpisode Narrative: Thunderstorms developed ahead of an approaching cold front, aided by a moderately unstable air mass and strong deep layer shear. These storms produced damaging wind gusts and hail up to half dollar size. Although several tornado warnings were issued for rotating storms, none were verified. As the cold front overtook these discrete cells, the primary threat became damaging wind gusts as it transitioned to a linear convective mode. Thunderstorms developed ahead of an approaching cold front, aided by a moderately unstable air mass and strong deep layer shear. These storms produced damaging wind gusts and hail up to half dollar size. Although several tornado warnings were issued for rotating storms, none were verified. As the cold front overtook these discrete cells, the primary threat became damaging wind gusts as it transitioned to a linear convective mode. Thunderstorms developed ahead of an approaching cold front, aided by a moderately unstable air mass and strong deep layer shear. These storms produced damaging wind gusts and hail up to half dollar size. Although several tornado warnings were issued for rotating storms, none were verified. As the cold front overtook these discrete cells, the primary threat became damaging wind gusts as it transitioned to a linear convective mode. Thunderstorms developed ahead of an approaching cold front, aided by a moderately unstable air mass and strong deep layer shear. These storms produced damaging wind gusts and hail up to half dollar size. Although several tornado warnings were issued for rotating storms, none were verified. As the cold front overtook these discrete cells, the primary threat became damaging wind gusts as it transitioned to a linear convective mode. Thunderstorms developed ahead of an approaching cold front, aided by a moderately unstable air mass and strong deep layer shear. These storms produced damaging wind gusts and hail up to half dollar size. Although several tornado warnings were issued for rotating storms, none were verified. As the cold front overtook these discrete cells, the primary threat became damaging wind gusts as it transitioned to a linear convective mode. Thunderstorms developed ahead of an approaching cold front, aided by a moderately unstable air mass and strong deep layer shear. These storms produced damaging wind gusts and hail up to half dollar size. Although several tornado warnings were issued for rotating storms, none were verified. As the cold front overtook these discrete cells, the primary threat became damaging wind gusts as it transitioned to a linear convective mode. Thunderstorms developed ahead of an approaching cold front, aided by a moderately unstable air mass and strong deep layer shear. These storms produced damaging wind gusts and hail up to half dollar size. Although several tornado warnings were issued for rotating storms, none were verified. As the cold front overtook these discrete cells, the primary threat became damaging wind gusts as it transitioned to a linear convective mode.\nEvent Narrative: The ASOS at the Raleigh Durham International Airport reported a peak wind gust of 59 mph. In addition, a trained spotter measured a 71 mph wind gust near the Interstate 540 on-ramp near Holly Springs 15 minutes earlier. One tree was blown down on Highway 64 near Jordan Lake, blocking one lane of traffic. Widespread trees and power lines were blown down along a swath from near Fuquay-Varina to Raleigh. In addition trees were reported to have fallen on 3 homes in the Apex and Cary areas (exact monetary damage is unknown). A couple of trees were blown down along a swath from several miles southwest of Bahama to near Bethesda, with one of the trees falling on the roof of a church (exact monetary damages are unknown). Multiple trees were blown down on Snow Hill Road several miles south of Bahama. Numerous trees and power lines were blown down in the town of Franklinton. Several trees were blown down near Clayton.",
+        "The following events were reported: Hail. These occurred near station USW00013722, approximately 47.575 km away, between 2013-05-08 18:40:00 and 2013-05-08 18:40:00. 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: Shortwave energy rotating around an upper level low located over Virginia and the District of Columbia triggered scattered showers and thunderstorms across central North Carolina. An isolated severe storm produced quarter-sized hail in Alamance County.\nEvent Narrative: Quarter size hail covering the ground.",
+        "The following events were reported: Flash Flood, Thunderstorm Wind. These occurred near station USW00013722, approximately 29.9038 km away, between 2013-06-07 05:38:00 and 2013-06-07 18:59:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Tropical Storm Andrea tracked northeast up the East Coast and through North Carolina on June 7th, bringing a swath of heavy rain of 3 to 6 inches across central and eastern portions of the area. This heavy rain resulted in numerous road closures and brought several small creeks and streams out of their banks. Tropical Storm Andrea tracked northeast up the East Coast and through North Carolina on June 7th, bringing a swath of heavy rain of 3 to 6 inches across central and eastern portions of the area. This heavy rain resulted in numerous road closures and brought several small creeks and streams out of their banks. Tropical Storm Andrea tracked northeast up the East Coast and through North Carolina on June 7th, bringing a swath of heavy rain of 3 to 6 inches across central and eastern portions of the area. This heavy rain resulted in numerous road closures and brought several small creeks and streams out of their banks. Tropical Storm Andrea tracked northeast up the East Coast and through North Carolina on June 7th, bringing a swath of heavy rain of 3 to 6 inches across central and eastern portions of the area. This heavy rain resulted in numerous road closures and brought several small creeks and streams out of their banks. Tropical Storm Andrea tracked northeast up the East Coast and through North Carolina on June 7th, bringing a swath of heavy rain of 3 to 6 inches across central and eastern portions of the area. This heavy rain resulted in numerous road closures and brought several small creeks and streams out of their banks. Tropical Storm Andrea tracked northeast up the East Coast and through North Carolina on June 7th, bringing a swath of heavy rain of 3 to 6 inches across central and eastern portions of the area. This heavy rain resulted in numerous road closures and brought several small creeks and streams out of their banks. Tropical Storm Andrea tracked northeast up the East Coast and through North Carolina on June 7th, bringing a swath of heavy rain of 3 to 6 inches across central and eastern portions of the area. This heavy rain resulted in numerous road closures and brought several small creeks and streams out of their banks. Tropical Storm Andrea tracked northeast up the East Coast and through North Carolina on June 7th, bringing a swath of heavy rain of 3 to 6 inches across central and eastern portions of the area. This heavy rain resulted in numerous road closures and brought several small creeks and streams out of their banks. Tropical Storm Andrea tracked northeast up the East Coast and through North Carolina on June 7th, bringing a swath of heavy rain of 3 to 6 inches across central and eastern portions of the area. This heavy rain resulted in numerous road closures and brought several small creeks and streams out of their banks. Tropical Storm Andrea tracked northeast up the East Coast and through North Carolina on June 7th, bringing a swath of heavy rain of 3 to 6 inches across central and eastern portions of the area. This heavy rain resulted in numerous road closures and brought several small creeks and streams out of their banks. Tropical Storm Andrea tracked northeast up the East Coast and through North Carolina on June 7th, bringing a swath of heavy rain of 3 to 6 inches across central and eastern portions of the area. This heavy rain resulted in numerous road closures and brought several small creeks and streams out of their banks. Tropical Storm Andrea tracked northeast up the East Coast and through North Carolina on June 7th, bringing a swath of heavy rain of 3 to 6 inches across central and eastern portions of the area. This heavy rain resulted in numerous road closures and brought several small creeks and streams out of their banks.\nEvent Narrative: Numerous road closures due to flash flooding including but not limited to Morrene Road, Junction Road at Holloway Street and Farrington Road at Old Chapel Hill Road. The 300 block of NC Highway 56 closed due to flooding. Balance Rock Road was closed due to flash flooding. Numerous roads were closed due to flooding including but not limited to Leesville Road, High House Road at Davis Road and Glenwood Avenue. Leesville Road was washed out near the 12300 Block. The fire department was also dispatched to assist with rescues from vehicles stranded in water. Piney Grove Wilbon Road was closed due to flash flooding near the intersections of Avent Ferry Road and Honeycutt Road.  Avent Ferry Road near Braxton Village was also closed due to flooding. Lake Boone Trail near Interstate 440 closed due to flash flooding. Dana Drive also closed due to flooding. Stadium Drive flooded due to nearby creek flowing out of its banks. Several trees were blown down near the 5500 Block of Highway 56. Trees blown down near the 600 Block of Otis Burrows Road. Road closed due to flooding at the intersection of Polena and Monroe. A car stalled in high water at a gas station on NC Highway 210. Crabtree Creek rose out of its bank causing flooding along Old Wake Forest Road, Highway 70 and Blue Ridge Road. Cars parked at the Crabtree Valley Mall had to be towed out of flood waters.",
+        "The following events were reported: Flash Flood, Thunderstorm Wind. These occurred near station USW00013722, approximately 29.9852 km away, between 2013-06-10 14:17:00 and 2013-06-10 19:20:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Persistent southwesterly flow aloft resulted in a warm, very moist and unstable air mass over the region. Weak disturbances in the flow aloft once again triggered afternoon showers and thunderstorm. However, an upper trough near the Ohio Valley resulted in slightly better forcing and shear over the area as it progressed eastward. This resulted in more convective coverage and also better storm organization. Numerous reports of wind damage were received with the storms. In addition, high moisture content and wet antecedent conditions resulted in some flash flooding. Persistent southwesterly flow aloft resulted in a warm, very moist and unstable air mass over the region. Weak disturbances in the flow aloft once again triggered afternoon showers and thunderstorm. However, an upper trough near the Ohio Valley resulted in slightly better forcing and shear over the area as it progressed eastward. This resulted in more convective coverage and also better storm organization. Numerous reports of wind damage were received with the storms. In addition, high moisture content and wet antecedent conditions resulted in some flash flooding.\nEvent Narrative: Several trees were blown down along Poole Road and Grasshopper Street in east Raleigh. Several roads were flooded in Clayton along US 70 Business.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 30.5143 km away, between 2013-06-13 15:54:00 and 2013-06-13 17:21:00.The events resulted in 0 injuries and 1 fatalities. The events caused property damage valued at 2018000.0 and crop damage of 0.0. \n\nEpisode Narrative: A ferocious line of strong to severe thunderstorms raced through central North Carolina|during the afternoon and into the early evening, uprooting trees and snapping power lines with straight-line wind gusts up to 80 mph. Damage was widespread with numerous trees falling on homes throughout the county warning area. The city of Albermarle, in Stanly County was hardest hit, with approximately 70 homes damaged and at least 3 injuries from trees crashing into and through homes and mobile homes. A University of North Carolina student   also died from injuries received when a large tree fell and landed on top of her on the sidewalk. A ferocious line of strong to severe thunderstorms raced through central North Carolina|during the afternoon and into the early evening, uprooting trees and snapping power lines with straight-line wind gusts up to 80 mph. Damage was widespread with numerous trees falling on homes throughout the county warning area. The city of Albermarle, in Stanly County was hardest hit, with approximately 70 homes damaged and at least 3 injuries from trees crashing into and through homes and mobile homes. A University of North Carolina student   also died from injuries received when a large tree fell and landed on top of her on the sidewalk. A ferocious line of strong to severe thunderstorms raced through central North Carolina|during the afternoon and into the early evening, uprooting trees and snapping power lines with straight-line wind gusts up to 80 mph. Damage was widespread with numerous trees falling on homes throughout the county warning area. The city of Albermarle, in Stanly County was hardest hit, with approximately 70 homes damaged and at least 3 injuries from trees crashing into and through homes and mobile homes. A University of North Carolina student   also died from injuries received when a large tree fell and landed on top of her on the sidewalk. A ferocious line of strong to severe thunderstorms raced through central North Carolina|during the afternoon and into the early evening, uprooting trees and snapping power lines with straight-line wind gusts up to 80 mph. Damage was widespread with numerous trees falling on homes throughout the county warning area. The city of Albermarle, in Stanly County was hardest hit, with approximately 70 homes damaged and at least 3 injuries from trees crashing into and through homes and mobile homes. A University of North Carolina student   also died from injuries received when a large tree fell and landed on top of her on the sidewalk. A ferocious line of strong to severe thunderstorms raced through central North Carolina|during the afternoon and into the early evening, uprooting trees and snapping power lines with straight-line wind gusts up to 80 mph. Damage was widespread with numerous trees falling on homes throughout the county warning area. The city of Albermarle, in Stanly County was hardest hit, with approximately 70 homes damaged and at least 3 injuries from trees crashing into and through homes and mobile homes. A University of North Carolina student   also died from injuries received when a large tree fell and landed on top of her on the sidewalk. A ferocious line of strong to severe thunderstorms raced through central North Carolina|during the afternoon and into the early evening, uprooting trees and snapping power lines with straight-line wind gusts up to 80 mph. Damage was widespread with numerous trees falling on homes throughout the county warning area. The city of Albermarle, in Stanly County was hardest hit, with approximately 70 homes damaged and at least 3 injuries from trees crashing into and through homes and mobile homes. A University of North Carolina student   also died from injuries received when a large tree fell and landed on top of her on the sidewalk. A ferocious line of strong to severe thunderstorms raced through central North Carolina|during the afternoon and into the early evening, uprooting trees and snapping power lines with straight-line wind gusts up to 80 mph. Damage was widespread with numerous trees falling on homes throughout the county warning area. The city of Albermarle, in Stanly County was hardest hit, with approximately 70 homes damaged and at least 3 injuries from trees crashing into and through homes and mobile homes. A University of North Carolina student   also died from injuries received when a large tree fell and landed on top of her on the sidewalk. A ferocious line of strong to severe thunderstorms raced through central North Carolina|during the afternoon and into the early evening, uprooting trees and snapping power lines with straight-line wind gusts up to 80 mph. Damage was widespread with numerous trees falling on homes throughout the county warning area. The city of Albermarle, in Stanly County was hardest hit, with approximately 70 homes damaged and at least 3 injuries from trees crashing into and through homes and mobile homes. A University of North Carolina student   also died from injuries received when a large tree fell and landed on top of her on the sidewalk. A ferocious line of strong to severe thunderstorms raced through central North Carolina|during the afternoon and into the early evening, uprooting trees and snapping power lines with straight-line wind gusts up to 80 mph. Damage was widespread with numerous trees falling on homes throughout the county warning area. The city of Albermarle, in Stanly County was hardest hit, with approximately 70 homes damaged and at least 3 injuries from trees crashing into and through homes and mobile homes. A University of North Carolina student   also died from injuries received when a large tree fell and landed on top of her on the sidewalk.\nEvent Narrative: Numerous trees were blown down across the road at Rawls Church Road and Kennebeck Road. A couple of other trees and power-lines  were also blown down along the wind swath. Amateur radio operators and trained spotters reported wind damage throughout the county with numerous trees and power-lines blown down. Some of the downed trees fell onto some homes including a tin roof blown off of an automotive dealership in Smithfield. Numerous trees and power-lines were blown down throughout the county. A large tree was blown down on the 300 Block of East Franklin Street killing a 20 year old female. Eight trees were blown down at the Central Regional Hospital in Butner. Numerous trees and power-lines were blown down along the swath.  The roof of a industrial carport at Pruitt Lumber Company in Louisburg collapsed. Numerous trees were blown down. Several trees fell onto some houses. The front porch of one of the homes was ripped off. Two utility poles were also blown down. Numerous trees were blown down along the wind swath and including in and around the Pittsboro area. Widespread trees and power-lines were blown down throughout the county. Some of the trees fell onto homes. Approximately 73,000 people in Wake County lost power.   In Raleigh, one large tree toppled onto the patio of NOFO at the Pig restaurant on Fairview Road.  There were no injuries. Monetary damages were estimated.",
+        "The following events were reported: Thunderstorm Wind, Tornado. These occurred near station USW00013722, approximately 29.2035 km away, between 2013-06-18 17:12:00 and 2013-06-18 17:34:00.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 150000.0 and crop damage of 0.0. \n\nEpisode Narrative: With a moderately unstable air mass in place, scattered to numerous showers and thunderstorms developed during the late afternoon and early evening hours as an upper level trough and associated cold front approached the region. Several reports of wind damage were received as some of the storms became severe. In addition, an MCV tracked east across north central North Carolina and enhanced the shear enough across the area to result in rotation in some of the storms. One of the storms produced an EF0 tornado near Louisburg in Franklin County that resulted in substantial tree damage and significant damage to several manufactured homes. With a moderately unstable air mass in place, scattered to numerous showers and thunderstorms developed during the late afternoon and early evening hours as an upper level trough and associated cold front approached the region. Several reports of wind damage were received as some of the storms became severe. In addition, an MCV tracked east across north central North Carolina and enhanced the shear enough across the area to result in rotation in some of the storms. One of the storms produced an EF0 tornado near Louisburg in Franklin County that resulted in substantial tree damage and significant damage to several manufactured homes.\nEvent Narrative: Multiple large oak trees were blown down at the Wakefield Plantation Gold Course. The National Weather Service confirmed that a tornado with a 1.25 mile damage path briefly touched down approximately 6 miles southeast of Youngsville in Franklin County, North Carolina. A significant area of tree damage was noted along Highway 401, near the intersection of Thompson Lane. The damage here consisted of a large stand of trees that had been blown down. The damage here suggested wind gusts with speeds of 80 mph. The most significant damage of this particular event was noted in the Wyndfield Neighborhood. The tornado reached its widest point at this location, reaching a maximum width of 150 yards. The damage at this location consisted of manufactured homes that experienced partial uplift of roofing material, shingle damage, and siding damage. In addition, dozens of hard and soft wood trees were blown down. The damage here suggested wind gusts with speeds of 85 mph. To the east-northeast of this location, the tornado path appeared to narrow as it approached Tarboro Road near the Harris Chapel Baptist Church. At this location, numerous headstones at an adjacent cemetery were blown over, and once again dozens of trees were noted to be blown down. The tornado appeared to cross Tarboro Road just south of the Braeburn subdivision. The damage pattern among the trees just east of Tarboro Road suggested that the tornado had lifted at this location. The damage at this location suggested wind gusts with speeds of 75 mph. In additon, straight-line wind damage immediately preceded and followed the time that the tornado was on the ground.",
+        "The following events were reported: Hail. These occurred near station USW00013722, approximately 40.5222 km away, between 2013-06-25 15:00:00 and 2013-06-25 15:26:00. The events included records with hailstones measuring 1.125 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Deep, moist southwesterly flow combined with strong insolation and weak disturbances aloft to produce scattered afternoon showers and thunderstorms. A lingering trough aloft resulted in slightly more than normal coverage for the day. Several storms became severe, producing wind damage and hail that ranged from the size of quarters to half dollars, with even one report of golf ball sized hail. Also, the very moist air mass and wet antecedent conditions resulted in some flash flooding. Deep, moist southwesterly flow combined with strong insolation and weak disturbances aloft to produce scattered afternoon showers and thunderstorms. A lingering trough aloft resulted in slightly more than normal coverage for the day. Several storms became severe, producing wind damage and hail that ranged from the size of quarters to half dollars, with even one report of golf ball sized hail. Also, the very moist air mass and wet antecedent conditions resulted in some flash flooding.\nEvent Narrative: Half dollar size hail occurred near Clayton and caused minor leaf damage. A mile long swath of quarter size hail occurred across southwest Clayton.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 46.0736 km away, between 2013-06-27 15:25:00 and 2013-06-27 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 500.0 and crop damage of 0.0. \n\nEpisode Narrative: Persistent east coast troughing combined with a warm and very moist air mass to produce scattered afternoon/evening showers and thunderstorms. A few of the storms resulted in isolated wind damage.\nEvent Narrative: Several trees and power lines were blown down along a swath from near Angier to Erwin.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 34.0353 km away, between 2013-06-28 16:45:00 and 2013-06-28 17:35:00. 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 2500.0 and crop damage of 0.0. \n\nEpisode Narrative: A very moist air mass and persistent troughing along the east coast lead to another round of scattered to numerous showers and thunderstorms. An increase in deep layer shear as an upper level disturbance tracked near the area lead to better organization of the convection and therefore numeorus storms became severe and produced damaging wind gusts. In addition, training storms with very heavy rain (2-3 inches) affected Stanly County and with already saturated soils from a very wet month, flash flooding occurred through the early morning hours of the 29th. In fact, several roads/bridges were washed out. A very moist air mass and persistent troughing along the east coast lead to another round of scattered to numerous showers and thunderstorms. An increase in deep layer shear as an upper level disturbance tracked near the area lead to better organization of the convection and therefore numeorus storms became severe and produced damaging wind gusts. In addition, training storms with very heavy rain (2-3 inches) affected Stanly County and with already saturated soils from a very wet month, flash flooding occurred through the early morning hours of the 29th. In fact, several roads/bridges were washed out. A very moist air mass and persistent troughing along the east coast lead to another round of scattered to numerous showers and thunderstorms. An increase in deep layer shear as an upper level disturbance tracked near the area lead to better organization of the convection and therefore numeorus storms became severe and produced damaging wind gusts. In addition, training storms with very heavy rain (2-3 inches) affected Stanly County and with already saturated soils from a very wet month, flash flooding occurred through the early morning hours of the 29th. In fact, several roads/bridges were washed out.\nEvent Narrative: A couple of trees and power lines were blown down along a swath from Youngsville to near Centerville. A few trees were blown down along a swath from near Goldston to near Bynum. A power pole, power lines and multiple trees were blown down along a swath from several miles west of Bahama to several miles northeast of Bahama.",
+        "The following events were reported: Flash Flood, Thunderstorm Wind. These occurred near station USW00013722, approximately 20.9839 km away, between 2013-06-30 03:45:00 and 2013-06-30 19:55:00.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 4112500.0 and crop damage of 0.0. \n\nEpisode Narrative: The forecast area remained sandwiched between an unseasonably deep trough aloft to the west and a ridge to the east. This resulted in a persistent very moist air mass and with soils already saturated, two rounds of heavy rain resulted in flash flooding, first in the early morning hours across Durham and Orange counties and later in the day across the same area, with additional flooding in Chatham, Anson and Stanly counties. Chapel Hill and Carrboro experienced the most significant flooding, with substantial property damage occurring. In addition, as afternoon destabilization occurred, a couple of storms became severe and produced some isolated wind damage. The forecast area remained sandwiched between an unseasonably deep trough aloft to the west and a ridge to the east. This resulted in a persistent very moist air mass and with soils already saturated, two rounds of heavy rain resulted in flash flooding, first in the early morning hours across Durham and Orange counties and later in the day across the same area, with additional flooding in Chatham, Anson and Stanly counties. Chapel Hill and Carrboro experienced the most significant flooding, with substantial property damage occurring. In addition, as afternoon destabilization occurred, a couple of storms became severe and produced some isolated wind damage. The forecast area remained sandwiched between an unseasonably deep trough aloft to the west and a ridge to the east. This resulted in a persistent very moist air mass and with soils already saturated, two rounds of heavy rain resulted in flash flooding, first in the early morning hours across Durham and Orange counties and later in the day across the same area, with additional flooding in Chatham, Anson and Stanly counties. Chapel Hill and Carrboro experienced the most significant flooding, with substantial property damage occurring. In addition, as afternoon destabilization occurred, a couple of storms became severe and produced some isolated wind damage. The forecast area remained sandwiched between an unseasonably deep trough aloft to the west and a ridge to the east. This resulted in a persistent very moist air mass and with soils already saturated, two rounds of heavy rain resulted in flash flooding, first in the early morning hours across Durham and Orange counties and later in the day across the same area, with additional flooding in Chatham, Anson and Stanly counties. Chapel Hill and Carrboro experienced the most significant flooding, with substantial property damage occurring. In addition, as afternoon destabilization occurred, a couple of storms became severe and produced some isolated wind damage. The forecast area remained sandwiched between an unseasonably deep trough aloft to the west and a ridge to the east. This resulted in a persistent very moist air mass and with soils already saturated, two rounds of heavy rain resulted in flash flooding, first in the early morning hours across Durham and Orange counties and later in the day across the same area, with additional flooding in Chatham, Anson and Stanly counties. Chapel Hill and Carrboro experienced the most significant flooding, with substantial property damage occurring. In addition, as afternoon destabilization occurred, a couple of storms became severe and produced some isolated wind damage. The forecast area remained sandwiched between an unseasonably deep trough aloft to the west and a ridge to the east. This resulted in a persistent very moist air mass and with soils already saturated, two rounds of heavy rain resulted in flash flooding, first in the early morning hours across Durham and Orange counties and later in the day across the same area, with additional flooding in Chatham, Anson and Stanly counties. Chapel Hill and Carrboro experienced the most significant flooding, with substantial property damage occurring. In addition, as afternoon destabilization occurred, a couple of storms became severe and produced some isolated wind damage. The forecast area remained sandwiched between an unseasonably deep trough aloft to the west and a ridge to the east. This resulted in a persistent very moist air mass and with soils already saturated, two rounds of heavy rain resulted in flash flooding, first in the early morning hours across Durham and Orange counties and later in the day across the same area, with additional flooding in Chatham, Anson and Stanly counties. Chapel Hill and Carrboro experienced the most significant flooding, with substantial property damage occurring. In addition, as afternoon destabilization occurred, a couple of storms became severe and produced some isolated wind damage. The forecast area remained sandwiched between an unseasonably deep trough aloft to the west and a ridge to the east. This resulted in a persistent very moist air mass and with soils already saturated, two rounds of heavy rain resulted in flash flooding, first in the early morning hours across Durham and Orange counties and later in the day across the same area, with additional flooding in Chatham, Anson and Stanly counties. Chapel Hill and Carrboro experienced the most significant flooding, with substantial property damage occurring. In addition, as afternoon destabilization occurred, a couple of storms became severe and produced some isolated wind damage.\nEvent Narrative: Heavy rain (4-5 inches) resulted in extensive flooding in the city of Chapel Hill. The first floor of the Town Hall flooded and may be closed for up to a year for repairs. Franklin Street saw widespread flooding, with water above the windows of cars in several locations and some businesses also being impacted. Several buildings on the University of North Carolina had water in them, including the bottom floor of Granville Tower. Another area of the city that experienced flooding was the East Gate Shopping Center, where water entered several businesses and stranded many cars in the parking lot. One hard hit residential areas was along Estes Drive near Highway 15-501, where the Camelot Village Condominiums experienced extensive flooding. In fact, 76 out of 116 units flooded. Another residential area that experienced flooding was the Airport Gardens Public Housing Neighborhood, where 18 out of the 26 units flooded. Due to the flooding, the county qualified for state and federal aid. Numerous streets in Chapel Hill were closed due to flooding, including Franklin Street at Estes Drive, which had 1-2 feet of water on it. In addition, high water began to encroach on the Camelot Village apartments that are located on Estes Street near Franklin Street. No damage was reported at this point. A few streets were closed due to flooding in Durham, including Pettigrew Street at Indiana Avenue and Liberty Street at Alston Avenue. Also, a couple of vehicles reportedly stalled at some of these locations. Monetary damage was unknown. A tree was blown down on the University of North Carolina campus, which damaged a couple of cars. Monetary damage was estimated. Several roads were closed in Durham due to flooding, including Highway 70 at Hinesley Road and Dover Road at Hope Valley Road. In addition, several cars stalled when water rose to their bumpers at Garrett Road and Old Chapel Hill Road. Monetary damages were estimated. Several roads in and just east of Pittsboro were closed due to flooding, including, but not limited to, Sanford Road, Mount Gilead Church Road near Sugar Lake Road, Thompson Street and Fire Tower Road. Several areas of Carrboro experienced flooding, including the Rocky Brook Mobile Home Park on Greensboro Street, where residents had to be evacuated due to high water. In fact, 20 out of 31 homes were eventually condemned. Several large limbs were blown down in the Durham area.",
+        "The following events were reported: Flash Flood. These occurred near station USW00013722, approximately 33.8442 km away, between 2013-07-08 18:05:00 and 2013-07-08 20:10:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: With a broad upper level trough over the area, diurnal destabilization combined with ample moisture to produce scattered showers and thunderstorms. A couple of these storms produced heavy rainfall amounts of 2-4 inches, which resulted in some flash flooding. With a broad upper level trough over the area, diurnal destabilization combined with ample moisture to produce scattered showers and thunderstorms. A couple of these storms produced heavy rainfall amounts of 2-4 inches, which resulted in some flash flooding.\nEvent Narrative: Dead Road was closed near Bunn Elementary Road due to high water. The road had to be closed at the intersection of Louisburg Road and Mitchell Mill Road due to high water.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 20.8643 km away, between 2013-07-09 14:34:00 and 2013-07-09 14:34:00. 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: Weak upper level disturbances moving within the weak cyclonic flow over the area combined with moist and unstable conditions to produce scattered afternoon/evening showers and thunderstorms. A couple of these storms resulted in some minor wind damage.\nEvent Narrative: A couple of trees and power lines were blown down near the intersection of Yates Mill Pond Road and Penny Road.",
+        "The following events were reported: Flash Flood. These occurred near station USW00013722, approximately 45.9072 km away, between 2013-07-12 14:30:00 and 2013-07-12 15:30:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: An amplifying upper level trough and a nearly stationary front across the Coastal Plain resulted in widespread showers and thunderstorms. Some isolated flash flooding occurred as a few of the storms were nearly stationary and antecedent ground conditions were already wet due to several days of rainfall.\nEvent Narrative: Interstate 40 had to be closed between exits 319 and 325 due to high water from approximately 3:30 to 4:30 pm.",
+        "The following events were reported: Hail. These occurred near station USW00013722, approximately 26.6819 km away, between 2013-07-16 19:05:00 and 2013-07-16 19:05:00. 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: Strong instability coupled with a weak surface trough across central North Carolina allowed scattered showers and storms to develop from the Northeast Piedmont and Northern Coastal Plain. Some of these storms became severe and produced severe hail and damaging wind gusts.\nEvent Narrative:",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 21.9338 km away, between 2013-07-24 16:40:00 and 2013-07-24 16:40:00. 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 to scattered showers and thunderstorms developed along a pre-frontal surface trough across central North Carolina... with moderate instability. A few of these storms became severe and produced damaging wind gusts across the northeast Piedmont and northern Coastal Plain.\nEvent Narrative: Trees and power lines were reported down at the intersection of Heatherfield Way and Southall Road.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 12.9834 km away, between 2013-08-03 18:19:00 and 2013-08-03 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: Showers and thunderstorms formed along and ahead of an approaching cold front. A few of these storm became strong to severe. One storm produced wind damage across western Wake County. Showers and thunderstorms formed along and ahead of an approaching cold front. A few of these storm became strong to severe. One storm produced wind damage across western Wake County.\nEvent Narrative: One tree was blown down in the road on East Cedar Street. One tree was reported down at Donaldson Drive and Hamilton Court.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 27.1251 km away, between 2013-08-10 16:10:00 and 2013-08-10 17:05:00. 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: Showers and thunderstorms developed across Virginia and sent an outflow southward into central North Carolina. With moderate to strong instability thunderstorms developed along this outflow. Several storms became severe across portions of the northern Piedmont and central and northern Coastal Plain of central North Carolina and produced damaging wind gusts. Showers and thunderstorms developed across Virginia and sent an outflow southward into central North Carolina. With moderate to strong instability thunderstorms developed along this outflow. Several storms became severe across portions of the northern Piedmont and central and northern Coastal Plain of central North Carolina and produced damaging wind gusts. Showers and thunderstorms developed across Virginia and sent an outflow southward into central North Carolina. With moderate to strong instability thunderstorms developed along this outflow. Several storms became severe across portions of the northern Piedmont and central and northern Coastal Plain of central North Carolina and produced damaging wind gusts. Showers and thunderstorms developed across Virginia and sent an outflow southward into central North Carolina. With moderate to strong instability thunderstorms developed along this outflow. Several storms became severe across portions of the northern Piedmont and central and northern Coastal Plain of central North Carolina and produced damaging wind gusts. Showers and thunderstorms developed across Virginia and sent an outflow southward into central North Carolina. With moderate to strong instability thunderstorms developed along this outflow. Several storms became severe across portions of the northern Piedmont and central and northern Coastal Plain of central North Carolina and produced damaging wind gusts.\nEvent Narrative: One tree was reported down near North Carolina highways 39 and 98. One tree was reported down on a power line near Carpenter Pond Road. One tree was reported down across the road at Brighton Road and Courtland Drive. One tree was reported down on a house near Southeast Cary Parkway. One tree was reported down on Williams Road near Old United States Highway 64.",
+        "The following events were reported: Flash Flood, Thunderstorm Wind. These occurred near station USW00013722, approximately 14.5678 km away, between 2013-09-01 17:15:00 and 2013-09-01 20:20:00.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 solid band of strong to severe showers and storms formed along an old outflow across north central NC on Sunday, September 1st, 2013. These storms became aligned roughly along I-40 and Highway 64, and tended to train repeatedly over the same areas. They knocked down trees, caused generally minor structural damage, produced flooding along|Crabtree Creek and generated a lot of CG lightning over a populated area. A solid band of strong to severe showers and storms formed along an old outflow across north central NC on Sunday, September 1st, 2013. These storms became aligned roughly along I-40 and Highway 64, and tended to train repeatedly over the same areas. They knocked down trees, caused generally minor structural damage, produced flooding along|Crabtree Creek and generated a lot of CG lightning over a populated area. A solid band of strong to severe showers and storms formed along an old outflow across north central NC on Sunday, September 1st, 2013. These storms became aligned roughly along I-40 and Highway 64, and tended to train repeatedly over the same areas. They knocked down trees, caused generally minor structural damage, produced flooding along|Crabtree Creek and generated a lot of CG lightning over a populated area. A solid band of strong to severe showers and storms formed along an old outflow across north central NC on Sunday, September 1st, 2013. These storms became aligned roughly along I-40 and Highway 64, and tended to train repeatedly over the same areas. They knocked down trees, caused generally minor structural damage, produced flooding along|Crabtree Creek and generated a lot of CG lightning over a populated area.\nEvent Narrative: Odyssey Drive was closed near the 1300 block due to two feet of water flowing across the road. A few trees were blown down along a several mile long swath across northwest Raleigh. Several trees were blown down near the intersection of New Hope Church Road and Mt. Hermon Church Road. The lower parking deck at Crabtree Valley Mall was flooded. Also, several roads were flooded, with numerous cars stranded, including Millbrook Road between Dixon Drive and Six Forks Road, New Falls of Neuse Road near Capital Boulevard and Creedmoor Road at Glenwood Avenue.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 37.1128 km away, between 2013-09-03 11:25:00 and 2013-09-03 11:25:00. 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 0.0 and crop damage of 3000.0. \n\nEpisode Narrative: The passage of an upper level disturbance within a very moist airmass in place across eastern North Carolina triggered scattered strong to severe thunderstorms.   The strongest of which resulted in downed trees and minor roof damage.\nEvent Narrative: Six large trees were blown down at the 4300 block of Zebulon Road.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 15.8232 km away, between 2014-01-11 13:40:00 and 2014-01-11 14:30:00.The events resulted in 4 injuries and 1 fatalities. The events caused property damage valued at 1356000.0 and crop damage of 0.0. \n\nEpisode Narrative: As a wedge front retreated northwestward into the western piedmont of North Carolina, modest warm sector destabilization via low-level warm advection and weak surface heating resulted in weak to moderate instability across central North Carolina. A line of strong to severe storms in advance of a strong mid-level trough approaching the Appalachians progressed eastward  across central North Carolina during the afternoon hours, producing a long swath of wind damage from Stanley County northeastward to Halifax County. The damage was most extensive across Wake County, with numerous uprooted and toppled trees across the Triangle, highlighted by a measured 86 mph wind gust at the Raleigh-Durham International.  Four people were injured from fallen trees or large tree limbs , including one fatality. As a wedge front retreated northwestward into the western piedmont of North Carolina, modest warm sector destabilization via low-level warm advection and weak surface heating resulted in weak to moderate instability across central North Carolina. A line of strong to severe storms in advance of a strong mid-level trough approaching the Appalachians progressed eastward  across central North Carolina during the afternoon hours, producing a long swath of wind damage from Stanley County northeastward to Halifax County. The damage was most extensive across Wake County, with numerous uprooted and toppled trees across the Triangle, highlighted by a measured 86 mph wind gust at the Raleigh-Durham International.  Four people were injured from fallen trees or large tree limbs , including one fatality. As a wedge front retreated northwestward into the western piedmont of North Carolina, modest warm sector destabilization via low-level warm advection and weak surface heating resulted in weak to moderate instability across central North Carolina. A line of strong to severe storms in advance of a strong mid-level trough approaching the Appalachians progressed eastward  across central North Carolina during the afternoon hours, producing a long swath of wind damage from Stanley County northeastward to Halifax County. The damage was most extensive across Wake County, with numerous uprooted and toppled trees across the Triangle, highlighted by a measured 86 mph wind gust at the Raleigh-Durham International.  Four people were injured from fallen trees or large tree limbs , including one fatality. As a wedge front retreated northwestward into the western piedmont of North Carolina, modest warm sector destabilization via low-level warm advection and weak surface heating resulted in weak to moderate instability across central North Carolina. A line of strong to severe storms in advance of a strong mid-level trough approaching the Appalachians progressed eastward  across central North Carolina during the afternoon hours, producing a long swath of wind damage from Stanley County northeastward to Halifax County. The damage was most extensive across Wake County, with numerous uprooted and toppled trees across the Triangle, highlighted by a measured 86 mph wind gust at the Raleigh-Durham International.  Four people were injured from fallen trees or large tree limbs , including one fatality. As a wedge front retreated northwestward into the western piedmont of North Carolina, modest warm sector destabilization via low-level warm advection and weak surface heating resulted in weak to moderate instability across central North Carolina. A line of strong to severe storms in advance of a strong mid-level trough approaching the Appalachians progressed eastward  across central North Carolina during the afternoon hours, producing a long swath of wind damage from Stanley County northeastward to Halifax County. The damage was most extensive across Wake County, with numerous uprooted and toppled trees across the Triangle, highlighted by a measured 86 mph wind gust at the Raleigh-Durham International.  Four people were injured from fallen trees or large tree limbs , including one fatality. As a wedge front retreated northwestward into the western piedmont of North Carolina, modest warm sector destabilization via low-level warm advection and weak surface heating resulted in weak to moderate instability across central North Carolina. A line of strong to severe storms in advance of a strong mid-level trough approaching the Appalachians progressed eastward  across central North Carolina during the afternoon hours, producing a long swath of wind damage from Stanley County northeastward to Halifax County. The damage was most extensive across Wake County, with numerous uprooted and toppled trees across the Triangle, highlighted by a measured 86 mph wind gust at the Raleigh-Durham International.  Four people were injured from fallen trees or large tree limbs , including one fatality. As a wedge front retreated northwestward into the western piedmont of North Carolina, modest warm sector destabilization via low-level warm advection and weak surface heating resulted in weak to moderate instability across central North Carolina. A line of strong to severe storms in advance of a strong mid-level trough approaching the Appalachians progressed eastward  across central North Carolina during the afternoon hours, producing a long swath of wind damage from Stanley County northeastward to Halifax County. The damage was most extensive across Wake County, with numerous uprooted and toppled trees across the Triangle, highlighted by a measured 86 mph wind gust at the Raleigh-Durham International.  Four people were injured from fallen trees or large tree limbs , including one fatality. As a wedge front retreated northwestward into the western piedmont of North Carolina, modest warm sector destabilization via low-level warm advection and weak surface heating resulted in weak to moderate instability across central North Carolina. A line of strong to severe storms in advance of a strong mid-level trough approaching the Appalachians progressed eastward  across central North Carolina during the afternoon hours, producing a long swath of wind damage from Stanley County northeastward to Halifax County. The damage was most extensive across Wake County, with numerous uprooted and toppled trees across the Triangle, highlighted by a measured 86 mph wind gust at the Raleigh-Durham International.  Four people were injured from fallen trees or large tree limbs , including one fatality.\nEvent Narrative: Numerous trees blown down throughout the county. A woman was killed when she and her husband and son were walking on Abbotts Creek Trail when a large tree limb and fell onto the family. The father son sustained minor injuries. A man struck by a fallen tree was breathing but was unconscious when emergency services arrived. He suffered multiple fractures and was taken to an area hospital. A tree fell on and seriously injured a man in the Wakefield area.  Trees and power-lines were blown down in the 800 block of Martin Luther King Blvd. In the Brier Creek area, a condominium complex under construction was damaged by the winds on Bruckhaus Street. Four units that had just been framed were blown over. Widespread trees down throughout the county, with damage primarily consisted of uprooted trees, with several cases of trees falling onto houses. Monetary damages were estimated.",
+        "The following events were reported: Lightning. These occurred near station USW00013722, approximately 32.4994 km away, between 2014-02-19 05:00:00 and 2014-02-19 05:00:00.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 cluster of sub-severe showers and thunderstorms moved through the area during the overnight hours. Lightning associated with the storms struck a house, resulting in minor damage.\nEvent Narrative: Officials said lightning struck the side of the home by the garage and traveled down the rain gutter, and into the sprinkler system in the yard.  Fire crews were able to quickly put out the blaze, which mainly damaged part of the garage.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 27.9379 km away, between 2014-02-21 10:23:00 and 2014-02-21 11:43:00. 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: An extensive QLCS developed ahead of a strong cold front. The QLCS raced eastward across the forecast area during the early to mid-morning hours on the 21st, exiting the coastal plain by the afternoon. The line produced scattered wind damage along the way, along with a brief EF-1 tornado touchdown near Grantham in Wayne County. An extensive QLCS developed ahead of a strong cold front. The QLCS raced eastward across the forecast area during the early to mid-morning hours on the 21st, exiting the coastal plain by the afternoon. The line produced scattered wind damage along the way, along with a brief EF-1 tornado touchdown near Grantham in Wayne County. An extensive QLCS developed ahead of a strong cold front. The QLCS raced eastward across the forecast area during the early to mid-morning hours on the 21st, exiting the coastal plain by the afternoon. The line produced scattered wind damage along the way, along with a brief EF-1 tornado touchdown near Grantham in Wayne County. An extensive QLCS developed ahead of a strong cold front. The QLCS raced eastward across the forecast area during the early to mid-morning hours on the 21st, exiting the coastal plain by the afternoon. The line produced scattered wind damage along the way, along with a brief EF-1 tornado touchdown near Grantham in Wayne County. An extensive QLCS developed ahead of a strong cold front. The QLCS raced eastward across the forecast area during the early to mid-morning hours on the 21st, exiting the coastal plain by the afternoon. The line produced scattered wind damage along the way, along with a brief EF-1 tornado touchdown near Grantham in Wayne County. An extensive QLCS developed ahead of a strong cold front. The QLCS raced eastward across the forecast area during the early to mid-morning hours on the 21st, exiting the coastal plain by the afternoon. The line produced scattered wind damage along the way, along with a brief EF-1 tornado touchdown near Grantham in Wayne County. An extensive QLCS developed ahead of a strong cold front. The QLCS raced eastward across the forecast area during the early to mid-morning hours on the 21st, exiting the coastal plain by the afternoon. The line produced scattered wind damage along the way, along with a brief EF-1 tornado touchdown near Grantham in Wayne County. An extensive QLCS developed ahead of a strong cold front. The QLCS raced eastward across the forecast area during the early to mid-morning hours on the 21st, exiting the coastal plain by the afternoon. The line produced scattered wind damage along the way, along with a brief EF-1 tornado touchdown near Grantham in Wayne County.\nEvent Narrative: One tree was blown down along NC Highway 96. One tree was blown down along Guess Road. One tree was blown down. Two trees were blown along Joe Peed Road. Large branches were blown dow along Six Forks Road. A large tree was blown down along Caistor Lane. One tree blown down along Walter Grissom Road. A large pine tree was blown along with other large limbs along Ellis Road near NC Highway 147.",
+        "The following events were reported: Flood. These occurred near station USW00013722, approximately 43.1492 km away, between 2014-03-07 11:25:00 and 2014-03-07 17:50:00. 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: In addition to a significant snow and ice storm for northern portions of the North Carolina Piedmont, the deepening coastal low also brought heavy rainfall of 2 to 4 inches to parts of the central and southern Piedmont that resulted in minor flooding during the morning and afternoon hours of the 7th. In addition to a significant snow and ice storm for northern portions of the North Carolina Piedmont, the deepening coastal low also brought heavy rainfall of 2 to 4 inches to parts of the central and southern Piedmont that resulted in minor flooding during the morning and afternoon hours of the 7th.\nEvent Narrative: Several small streams across southern Alamance County flooded. Flood water rising above bridge on Meadow Creek. Carver road closed due to flooding.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 15.6562 km away, between 2014-03-12 17:30:00 and 2014-03-12 17:58:00. The events included records with estimated wind gusts of 50.0 mph.The events resulted in 0 injuries and 1 fatalities. The events caused property damage valued at 8000.0 and crop damage of 0.0. \n\nEpisode Narrative: A line of thunderstorms, with damaging winds, affected the area as a strong cold front moved through during peak heating. Observed winds around 60 mph resulted in numerous trees and power lines being blown down. There was one fatality in Chapel Hill due to a tree falling on a vehicle. A line of thunderstorms, with damaging winds, affected the area as a strong cold front moved through during peak heating. Observed winds around 60 mph resulted in numerous trees and power lines being blown down. There was one fatality in Chapel Hill due to a tree falling on a vehicle. A line of thunderstorms, with damaging winds, affected the area as a strong cold front moved through during peak heating. Observed winds around 60 mph resulted in numerous trees and power lines being blown down. There was one fatality in Chapel Hill due to a tree falling on a vehicle.\nEvent Narrative: One tree was blown down along Highway 751 near the Durham County line. One tree was blown down near Old Raleigh Road and Shepards Vinyard Drive. Numerous trees, power lines and power poles were blown down from near Chapel Hill to near Parkwood. A 55-year old man was killed by a falling tree as he was standing on the back deck of his home on Roper Lane in Chapel Hill, North Carolina.",
+        "The following events were reported: Tornado. These occurred near station USW00013722, approximately 31.9727 km away, between 2014-03-29 19:57:00 and 2014-03-29 20:09:00.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: An isolated supercell developed ahead of a cold front as it moved through Central North Carolina in association with deepening low pressure system, as it tracked from the Mississippi River Valley northeast toward New England. The supercell produced multiple, but brief, weak tornado touchdowns. An isolated supercell developed ahead of a cold front as it moved through Central North Carolina in association with deepening low pressure system, as it tracked from the Mississippi River Valley northeast toward New England. The supercell produced multiple, but brief, weak tornado touchdowns.\nEvent Narrative: An EF0 tornado touched down and was on the ground for approximately one minute near the intersection of Old Stage Road and North Carolina Highway 42. Several trees were reported down in this area and a home sustained substantial shingle damage. An outbuilding was also picked up, moved 50 yards and destroyed in this location as well. A weak EF0 tornado occurred shortly after 9 pm at the intersection of Trebor Drive and Cross Pointe Lane. A residence sustained partial roof damage, a couple of windows were broken, and a couple of trees were blown down.",
+        "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00013722, approximately 32.9724 km away, between 2014-04-25 13:08:00 and 2014-04-25 16:35:00. The events included records with hailstones measuring 10.8 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Airmass became increasingly unstable as a warm front retreated northward during the morning hours, in advance of a compact but potent shortwave trough and associated surface cold front into the area from the west. Early in the event, discrete cells produced a weak EF-1 tornado touchdown in Halifax County along with severe hail ranging from quarter to golf ball size. As the storms progressed eastward into the coastal plain, they consolidated into a line and produced scattered wind damage before exiting the forecast area. Airmass became increasingly unstable as a warm front retreated northward during the morning hours, in advance of a compact but potent shortwave trough and associated surface cold front into the area from the west. Early in the event, discrete cells produced a weak EF-1 tornado touchdown in Halifax County along with severe hail ranging from quarter to golf ball size. As the storms progressed eastward into the coastal plain, they consolidated into a line and produced scattered wind damage before exiting the forecast area. Airmass became increasingly unstable as a warm front retreated northward during the morning hours, in advance of a compact but potent shortwave trough and associated surface cold front into the area from the west. Early in the event, discrete cells produced a weak EF-1 tornado touchdown in Halifax County along with severe hail ranging from quarter to golf ball size. As the storms progressed eastward into the coastal plain, they consolidated into a line and produced scattered wind damage before exiting the forecast area. Airmass became increasingly unstable as a warm front retreated northward during the morning hours, in advance of a compact but potent shortwave trough and associated surface cold front into the area from the west. Early in the event, discrete cells produced a weak EF-1 tornado touchdown in Halifax County along with severe hail ranging from quarter to golf ball size. As the storms progressed eastward into the coastal plain, they consolidated into a line and produced scattered wind damage before exiting the forecast area. Airmass became increasingly unstable as a warm front retreated northward during the morning hours, in advance of a compact but potent shortwave trough and associated surface cold front into the area from the west. Early in the event, discrete cells produced a weak EF-1 tornado touchdown in Halifax County along with severe hail ranging from quarter to golf ball size. As the storms progressed eastward into the coastal plain, they consolidated into a line and produced scattered wind damage before exiting the forecast area. Airmass became increasingly unstable as a warm front retreated northward during the morning hours, in advance of a compact but potent shortwave trough and associated surface cold front into the area from the west. Early in the event, discrete cells produced a weak EF-1 tornado touchdown in Halifax County along with severe hail ranging from quarter to golf ball size. As the storms progressed eastward into the coastal plain, they consolidated into a line and produced scattered wind damage before exiting the forecast area. Airmass became increasingly unstable as a warm front retreated northward during the morning hours, in advance of a compact but potent shortwave trough and associated surface cold front into the area from the west. Early in the event, discrete cells produced a weak EF-1 tornado touchdown in Halifax County along with severe hail ranging from quarter to golf ball size. As the storms progressed eastward into the coastal plain, they consolidated into a line and produced scattered wind damage before exiting the forecast area. Airmass became increasingly unstable as a warm front retreated northward during the morning hours, in advance of a compact but potent shortwave trough and associated surface cold front into the area from the west. Early in the event, discrete cells produced a weak EF-1 tornado touchdown in Halifax County along with severe hail ranging from quarter to golf ball size. As the storms progressed eastward into the coastal plain, they consolidated into a line and produced scattered wind damage before exiting the forecast area. Airmass became increasingly unstable as a warm front retreated northward during the morning hours, in advance of a compact but potent shortwave trough and associated surface cold front into the area from the west. Early in the event, discrete cells produced a weak EF-1 tornado touchdown in Halifax County along with severe hail ranging from quarter to golf ball size. As the storms progressed eastward into the coastal plain, they consolidated into a line and produced scattered wind damage before exiting the forecast area. Airmass became increasingly unstable as a warm front retreated northward during the morning hours, in advance of a compact but potent shortwave trough and associated surface cold front into the area from the west. Early in the event, discrete cells produced a weak EF-1 tornado touchdown in Halifax County along with severe hail ranging from quarter to golf ball size. As the storms progressed eastward into the coastal plain, they consolidated into a line and produced scattered wind damage before exiting the forecast area.\nEvent Narrative:   Quarter size hail reported at Fall Lake Recreation area. Quarter size hail reported near the intersection of NC Route 96 and NC Route 56.   Quarter size hail reported near Surl. Quarter size hail reported at Franklinton Highs School. Several trees down in the Youngsville area. Several trees down in the Louisburg area.",
+        "The following events were reported: Flash Flood, Thunderstorm Wind, Tornado. These occurred near station USW00013722, approximately 25.0514 km away, between 2014-05-15 16:05:00 and 2014-05-16 04:40:00.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 261000.0 and crop damage of 0.0. \n\nEpisode Narrative: Scattered convection impacted central North Carolina as a deep upper level trough and associated strong surface cold front approached and crossed the area. Strong moisture transport resulted in above normal precipitable water values and this, combined with the ultimate training of the storms, lead to flash flooding as many areas received 2-4 inches of rain, with isolated amounts up to 5-6 inches. In addition, some isolated wind damage occurred and as a secondary area of low pressure developed and tracked along the front, an isolated tornado formed. This EF1 tornado uprooted numerous trees, causing substantial property damage near Durham, North Carolina. Scattered convection impacted central North Carolina as a deep upper level trough and associated strong surface cold front approached and crossed the area. Strong moisture transport resulted in above normal precipitable water values and this, combined with the ultimate training of the storms, lead to flash flooding as many areas received 2-4 inches of rain, with isolated amounts up to 5-6 inches. In addition, some isolated wind damage occurred and as a secondary area of low pressure developed and tracked along the front, an isolated tornado formed. This EF1 tornado uprooted numerous trees, causing substantial property damage near Durham, North Carolina. Scattered convection impacted central North Carolina as a deep upper level trough and associated strong surface cold front approached and crossed the area. Strong moisture transport resulted in above normal precipitable water values and this, combined with the ultimate training of the storms, lead to flash flooding as many areas received 2-4 inches of rain, with isolated amounts up to 5-6 inches. In addition, some isolated wind damage occurred and as a secondary area of low pressure developed and tracked along the front, an isolated tornado formed. This EF1 tornado uprooted numerous trees, causing substantial property damage near Durham, North Carolina. Scattered convection impacted central North Carolina as a deep upper level trough and associated strong surface cold front approached and crossed the area. Strong moisture transport resulted in above normal precipitable water values and this, combined with the ultimate training of the storms, lead to flash flooding as many areas received 2-4 inches of rain, with isolated amounts up to 5-6 inches. In addition, some isolated wind damage occurred and as a secondary area of low pressure developed and tracked along the front, an isolated tornado formed. This EF1 tornado uprooted numerous trees, causing substantial property damage near Durham, North Carolina. Scattered convection impacted central North Carolina as a deep upper level trough and associated strong surface cold front approached and crossed the area. Strong moisture transport resulted in above normal precipitable water values and this, combined with the ultimate training of the storms, lead to flash flooding as many areas received 2-4 inches of rain, with isolated amounts up to 5-6 inches. In addition, some isolated wind damage occurred and as a secondary area of low pressure developed and tracked along the front, an isolated tornado formed. This EF1 tornado uprooted numerous trees, causing substantial property damage near Durham, North Carolina. Scattered convection impacted central North Carolina as a deep upper level trough and associated strong surface cold front approached and crossed the area. Strong moisture transport resulted in above normal precipitable water values and this, combined with the ultimate training of the storms, lead to flash flooding as many areas received 2-4 inches of rain, with isolated amounts up to 5-6 inches. In addition, some isolated wind damage occurred and as a secondary area of low pressure developed and tracked along the front, an isolated tornado formed. This EF1 tornado uprooted numerous trees, causing substantial property damage near Durham, North Carolina. Scattered convection impacted central North Carolina as a deep upper level trough and associated strong surface cold front approached and crossed the area. Strong moisture transport resulted in above normal precipitable water values and this, combined with the ultimate training of the storms, lead to flash flooding as many areas received 2-4 inches of rain, with isolated amounts up to 5-6 inches. In addition, some isolated wind damage occurred and as a secondary area of low pressure developed and tracked along the front, an isolated tornado formed. This EF1 tornado uprooted numerous trees, causing substantial property damage near Durham, North Carolina. Scattered convection impacted central North Carolina as a deep upper level trough and associated strong surface cold front approached and crossed the area. Strong moisture transport resulted in above normal precipitable water values and this, combined with the ultimate training of the storms, lead to flash flooding as many areas received 2-4 inches of rain, with isolated amounts up to 5-6 inches. In addition, some isolated wind damage occurred and as a secondary area of low pressure developed and tracked along the front, an isolated tornado formed. This EF1 tornado uprooted numerous trees, causing substantial property damage near Durham, North Carolina. Scattered convection impacted central North Carolina as a deep upper level trough and associated strong surface cold front approached and crossed the area. Strong moisture transport resulted in above normal precipitable water values and this, combined with the ultimate training of the storms, lead to flash flooding as many areas received 2-4 inches of rain, with isolated amounts up to 5-6 inches. In addition, some isolated wind damage occurred and as a secondary area of low pressure developed and tracked along the front, an isolated tornado formed. This EF1 tornado uprooted numerous trees, causing substantial property damage near Durham, North Carolina. Scattered convection impacted central North Carolina as a deep upper level trough and associated strong surface cold front approached and crossed the area. Strong moisture transport resulted in above normal precipitable water values and this, combined with the ultimate training of the storms, lead to flash flooding as many areas received 2-4 inches of rain, with isolated amounts up to 5-6 inches. In addition, some isolated wind damage occurred and as a secondary area of low pressure developed and tracked along the front, an isolated tornado formed. This EF1 tornado uprooted numerous trees, causing substantial property damage near Durham, North Carolina. Scattered convection impacted central North Carolina as a deep upper level trough and associated strong surface cold front approached and crossed the area. Strong moisture transport resulted in above normal precipitable water values and this, combined with the ultimate training of the storms, lead to flash flooding as many areas received 2-4 inches of rain, with isolated amounts up to 5-6 inches. In addition, some isolated wind damage occurred and as a secondary area of low pressure developed and tracked along the front, an isolated tornado formed. This EF1 tornado uprooted numerous trees, causing substantial property damage near Durham, North Carolina.\nEvent Narrative: A storm survey confirmed an EF-1 tornado near Durham. Damage consisted of dozens of snapped and uprooted trees and approximately 40 homes that experienced roof or other structural damage. Most of the damage to the homes was caused by falling trees and other debris. However, there were at least a half a dozen homes that experienced minor roof damage solely from the wind. In one case, a large oak tree was uprooted and fell onto a home, slicing through the roof and an exterior wall. Several roads were barricaded due to high water in the Timberlake area. There was minor damage to an outbuilding and a few trees were blown down south of Surl, near the Durham County line. Antioch Church Road at Lucy Garret Road was closed due to high water. Highway 55 near South Salem Street in Apex was closed due to high water. Observations indicated that 3-5 inches of rain fell throughout the county, with isolated amounts up to 6 inches. All but one lane of Glenwood Avenue had to be closed near Lynn Road due to high water. Observations indicated that 3-5 inches of rain fell throughout the county, with isolated amounts up to 6 inches. Odessy Road was closed near the intersection of Penrith Drive due to a creek coming out of its bank. Observations indicated that 2-4 inches of rain fell throughout the county, with isolated amounts up to 5 inches. Southall Road in Raleigh was closed due to heavy rain. Observations indicated that 2-4 inches of rain fell in a short period of time across this area. Bolin Creek was out of its banks, impacting Umstead Drive. In fact, the road was impassible and eventually had to be closed due to the flooding. In addition, some of the Camelot Village Apartments on Estes Drive (located near Bolin Creek) had to be evacuated. Observations indicated that 3-5 inches of rain fell throughout the county. An overflowing pond washed out a section of West Cornwallis Road near the intersection of Owls Wood Lane. Observations indicated that 3-5 inches of rain fell throughout the county. A foot of flowing water was impacting Atlantic Avenue near New Hope Road. Observations indicated that 3-5 inches of rain fell throughout the county, with isolated amounts up to 6 inches.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 27.9097 km away, between 2014-05-27 14:32:00 and 2014-05-27 15:43:00. 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: Scattered showers and storms developed along a lee/piedmont surface trough and subsequent outflow boundaries across central North Carolina during the afternoon and evening, aided by intense surface heating, moist low level air mass, and weak mid level disturbance crossing the area. Scattered showers and storms developed along a lee/piedmont surface trough and subsequent outflow boundaries across central North Carolina during the afternoon and evening, aided by intense surface heating, moist low level air mass, and weak mid level disturbance crossing the area. Scattered showers and storms developed along a lee/piedmont surface trough and subsequent outflow boundaries across central North Carolina during the afternoon and evening, aided by intense surface heating, moist low level air mass, and weak mid level disturbance crossing the area. Scattered showers and storms developed along a lee/piedmont surface trough and subsequent outflow boundaries across central North Carolina during the afternoon and evening, aided by intense surface heating, moist low level air mass, and weak mid level disturbance crossing the area.\nEvent Narrative: One tree was reported down on Oakland Drive. One tree was reported down at Fairview and Oberlin Road. Power lines were reported down near the intersection of Sertoma Road and Highway 54. One tree was reported down on a power line on Dallas Drive.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 16.221 km away, between 2014-06-04 14:42:00 and 2014-06-04 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: Weak disturbances aloft provided enough lift within a relatively moist and unstable air mass to result in scattered afternoon thunderstorms. One of the storms produced some minor wind damage near Durham and Raleigh. Weak disturbances aloft provided enough lift within a relatively moist and unstable air mass to result in scattered afternoon thunderstorms. One of the storms produced some minor wind damage near Durham and Raleigh.\nEvent Narrative: A power line was blown down at 3137 Fayetteville Street. Several trees and power lines were blown down along a swath from Raleigh to Wake Forest.",
+        "The following events were reported: Flash Flood, Hail, Thunderstorm Wind. These occurred near station USW00013722, approximately 26.788 km away, between 2014-06-11 12:55:00 and 2014-06-11 19:15:00. The events included records with hailstones measuring 43.875 inches.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 72000.0 and crop damage of 0.0. \n\nEpisode Narrative: As a upper level trough finally began to shift east, height falls aloft overspread the region, in addition several upper level disturbances affected the area. With the increased upper level forcing, fairly widespread convection developed across the area within the moderately unstable and moist air mass. Widespread trees were blown down, including several on homes and vehicles. Additionally, some large hail was observed. As a upper level trough finally began to shift east, height falls aloft overspread the region, in addition several upper level disturbances affected the area. With the increased upper level forcing, fairly widespread convection developed across the area within the moderately unstable and moist air mass. Widespread trees were blown down, including several on homes and vehicles. Additionally, some large hail was observed. As a upper level trough finally began to shift east, height falls aloft overspread the region, in addition several upper level disturbances affected the area. With the increased upper level forcing, fairly widespread convection developed across the area within the moderately unstable and moist air mass. Widespread trees were blown down, including several on homes and vehicles. Additionally, some large hail was observed. As a upper level trough finally began to shift east, height falls aloft overspread the region, in addition several upper level disturbances affected the area. With the increased upper level forcing, fairly widespread convection developed across the area within the moderately unstable and moist air mass. Widespread trees were blown down, including several on homes and vehicles. Additionally, some large hail was observed. As a upper level trough finally began to shift east, height falls aloft overspread the region, in addition several upper level disturbances affected the area. With the increased upper level forcing, fairly widespread convection developed across the area within the moderately unstable and moist air mass. Widespread trees were blown down, including several on homes and vehicles. Additionally, some large hail was observed. As a upper level trough finally began to shift east, height falls aloft overspread the region, in addition several upper level disturbances affected the area. With the increased upper level forcing, fairly widespread convection developed across the area within the moderately unstable and moist air mass. Widespread trees were blown down, including several on homes and vehicles. Additionally, some large hail was observed. As a upper level trough finally began to shift east, height falls aloft overspread the region, in addition several upper level disturbances affected the area. With the increased upper level forcing, fairly widespread convection developed across the area within the moderately unstable and moist air mass. Widespread trees were blown down, including several on homes and vehicles. Additionally, some large hail was observed. As a upper level trough finally began to shift east, height falls aloft overspread the region, in addition several upper level disturbances affected the area. With the increased upper level forcing, fairly widespread convection developed across the area within the moderately unstable and moist air mass. Widespread trees were blown down, including several on homes and vehicles. Additionally, some large hail was observed. As a upper level trough finally began to shift east, height falls aloft overspread the region, in addition several upper level disturbances affected the area. With the increased upper level forcing, fairly widespread convection developed across the area within the moderately unstable and moist air mass. Widespread trees were blown down, including several on homes and vehicles. Additionally, some large hail was observed.\nEvent Narrative: Numerous trees and power lines were blown down along a swath from several miles southwest of Clayton to several miles southwest of Princeton. In addition, crops were damaged near Princeton, as well as a few small barns. Also, shingles were blown off of a couple of homes. Monetary damages were unknown and were estimated. A couple of trees were blown down along a swath from near Youngsville to Franklinton. Several trees were blown down along a swath from near the Raleigh-Durham International Airport to near Falls Lake. In addition, one of trees fell onto a transformer in north Raleigh. Multiple trees were blown down along a swath from several miles west of Durham to near Bethesda. In addition, 2 homes had trees fall on them. Monetary damages were unknown and were estimated. The intersection of North Duke Street and North Gregson Street was flooded. Multiple trees were blown down near the Orange County Speedway. A couple of trees were blown down along a swath from near Pittsboro to near Jordan Lake. Quarter size hail was observed in Saxapahaw on Andover Road. Multiple trees were blown down within the city of Durham. In addition, 2 trees fell onto cars and 1 tree fell on a house. Monetary damages were unknown and were estimated.",
+        "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00013722, approximately 22.3908 km away, between 2014-06-19 15:39:00 and 2014-06-19 17:01:00. The events included records with hailstones measuring 39.111111111111114 inches.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 18500.0 and crop damage of 0.0. \n\nEpisode Narrative: Severe storms initially developed along a pre-frontal thermal trough in place across the western Piedmont of North Carolina during the early to mid afternoon hours. By the early evening, new storm development along a southward surging outflow boundary from a well defined multicell cluster over southeast Virginia produced thunderstorm wind damage and severe hail. Severe storms initially developed along a pre-frontal thermal trough in place across the western Piedmont of North Carolina during the early to mid afternoon hours. By the early evening, new storm development along a southward surging outflow boundary from a well defined multicell cluster over southeast Virginia produced thunderstorm wind damage and severe hail. Severe storms initially developed along a pre-frontal thermal trough in place across the western Piedmont of North Carolina during the early to mid afternoon hours. By the early evening, new storm development along a southward surging outflow boundary from a well defined multicell cluster over southeast Virginia produced thunderstorm wind damage and severe hail. Severe storms initially developed along a pre-frontal thermal trough in place across the western Piedmont of North Carolina during the early to mid afternoon hours. By the early evening, new storm development along a southward surging outflow boundary from a well defined multicell cluster over southeast Virginia produced thunderstorm wind damage and severe hail. Severe storms initially developed along a pre-frontal thermal trough in place across the western Piedmont of North Carolina during the early to mid afternoon hours. By the early evening, new storm development along a southward surging outflow boundary from a well defined multicell cluster over southeast Virginia produced thunderstorm wind damage and severe hail. Severe storms initially developed along a pre-frontal thermal trough in place across the western Piedmont of North Carolina during the early to mid afternoon hours. By the early evening, new storm development along a southward surging outflow boundary from a well defined multicell cluster over southeast Virginia produced thunderstorm wind damage and severe hail. Severe storms initially developed along a pre-frontal thermal trough in place across the western Piedmont of North Carolina during the early to mid afternoon hours. By the early evening, new storm development along a southward surging outflow boundary from a well defined multicell cluster over southeast Virginia produced thunderstorm wind damage and severe hail. Severe storms initially developed along a pre-frontal thermal trough in place across the western Piedmont of North Carolina during the early to mid afternoon hours. By the early evening, new storm development along a southward surging outflow boundary from a well defined multicell cluster over southeast Virginia produced thunderstorm wind damage and severe hail. Severe storms initially developed along a pre-frontal thermal trough in place across the western Piedmont of North Carolina during the early to mid afternoon hours. By the early evening, new storm development along a southward surging outflow boundary from a well defined multicell cluster over southeast Virginia produced thunderstorm wind damage and severe hail.\nEvent Narrative:  One tree was blown down at the intersection of Trent Drive and Erwin Road. Tree and powerlines were blown down onto a car at Dollar Avenue. Monetary damages were estimated. One tree was blown down near the intersection of Holloway Street and Joyland Street. Numerous trees were blown down across the county. One tree was blown down on London Bridge Court at Pembridge Lane. Large tree limb was blown down with damage to a fence near the intersection of Purnell and WoodLief Roads. Monetary  damages were estimated.  Numerous trees and powerlines were blown down west of Hillsborough.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 14.7391 km away, between 2014-07-03 12:45:00 and 2014-07-03 13:30:00. 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: The outer rain bands associated with Hurricane Arthur produced locally heavy rainfall of 3 to 4 inches and minor flooding across Edgecombe County. Additionally, an area of convection which developed well west of the circulation produced some isolated thunderstorm wind damage.\nEvent Narrative: A pine tree was snapped off at Hilltop Avenue and Circle Drive. An oak tree in Cary was also snapped in half.",
+        "The following events were reported: Flash Flood, Thunderstorm Wind. These occurred near station USW00013722, approximately 11.066 km away, between 2014-07-10 16:35:00 and 2014-07-10 19:00:00.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: Numerous showers and thunderstorms developed over eastern portions of central North Carolina ahead of a mid-level trough and associated surface cold front. Moderate instability in the presence of surface boundaries, descent shear and enhanced forcing for ascent under the right entrance region of the jet, resulted in a few isolated severe thunderstorms. Also, with precipitable water values of up to two inches, training thunderstorms resulted flash flooding. Numerous showers and thunderstorms developed over eastern portions of central North Carolina ahead of a mid-level trough and associated surface cold front. Moderate instability in the presence of surface boundaries, descent shear and enhanced forcing for ascent under the right entrance region of the jet, resulted in a few isolated severe thunderstorms. Also, with precipitable water values of up to two inches, training thunderstorms resulted flash flooding.\nEvent Narrative: A few trees were blown down along a swath from near Apex to just northwest of Raleigh. Numerous roads were flooded and impassable in downtown Raleigh. In addition, several water rescues were performed, including one on Hillsborough Street near Western Boulevard.",
+        "The following events were reported: Flash Flood, Thunderstorm Wind. These occurred near station USW00013722, approximately 18.6908 km away, between 2014-07-15 15:00:00 and 2014-07-15 19:15:00.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: Showers and thunderstorms developed along a pre-frontal trough, within a very moist and unstable air mass. Several of the storms produced damaging winds. In addition, the slow movement and training nature of some of the storms resulted in flash flooding. Showers and thunderstorms developed along a pre-frontal trough, within a very moist and unstable air mass. Several of the storms produced damaging winds. In addition, the slow movement and training nature of some of the storms resulted in flash flooding. Showers and thunderstorms developed along a pre-frontal trough, within a very moist and unstable air mass. Several of the storms produced damaging winds. In addition, the slow movement and training nature of some of the storms resulted in flash flooding. Showers and thunderstorms developed along a pre-frontal trough, within a very moist and unstable air mass. Several of the storms produced damaging winds. In addition, the slow movement and training nature of some of the storms resulted in flash flooding. Showers and thunderstorms developed along a pre-frontal trough, within a very moist and unstable air mass. Several of the storms produced damaging winds. In addition, the slow movement and training nature of some of the storms resulted in flash flooding.\nEvent Narrative: Several trees were blown down along a swath from near Apex to several miles southeast of Cary. Several roads became impassible across portions of western Wake County, as 3-4 inches of rain was observed. A pickup truck became stuck in high water at the intersection of Bowden Street and Chapel Hill Road. Numerous trees were blown down in and just south of Hillsborough. One tree fell on a home. The amount of damage to the home was unknown and monetary damages were estimated. Several trees and power lines were blown down along a swath from near Apex to near Purnell. A car became stranded at the intersection of Meriweather Driver and Carver Street. Barricades were placed at this location while the road was closed.",
+        "The following events were reported: Flash Flood. These occurred near station USW00013722, approximately 12.9619 km away, between 2014-07-21 11:15:00 and 2014-07-21 13:59:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Organized convection developed across central North Carolina in advance of a slow moving upper level trough stretching from the lower Ohio Valley south-southwestward into the lower Mississippi Valley. Locally heavily rainfall of two to three inches fell across the central Piedmont resulting in minor flooding across mostly urban areas. Organized convection developed across central North Carolina in advance of a slow moving upper level trough stretching from the lower Ohio Valley south-southwestward into the lower Mississippi Valley. Locally heavily rainfall of two to three inches fell across the central Piedmont resulting in minor flooding across mostly urban areas. Organized convection developed across central North Carolina in advance of a slow moving upper level trough stretching from the lower Ohio Valley south-southwestward into the lower Mississippi Valley. Locally heavily rainfall of two to three inches fell across the central Piedmont resulting in minor flooding across mostly urban areas. Organized convection developed across central North Carolina in advance of a slow moving upper level trough stretching from the lower Ohio Valley south-southwestward into the lower Mississippi Valley. Locally heavily rainfall of two to three inches fell across the central Piedmont resulting in minor flooding across mostly urban areas. Organized convection developed across central North Carolina in advance of a slow moving upper level trough stretching from the lower Ohio Valley south-southwestward into the lower Mississippi Valley. Locally heavily rainfall of two to three inches fell across the central Piedmont resulting in minor flooding across mostly urban areas.\nEvent Narrative: Dover Road and Woodridge Road closed due to flooding. Streets were flooding due to creeks overflowing at Legion Avenue and Chapel Hill Boulevard. Woodridge Road closed due to flooding. Morrisville Carpenter Road between Miller Road and Gratiot Road closed due to flooding. McCrimmon Parkway closed due to flooding between Church Street and NC Highway 54.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 25.6117 km away, between 2014-07-24 17:40:00 and 2014-07-24 18:30:00. 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 QLCS developed over southern Virginia along and ahead of a weak surface cold front and attendant shortwave trough moving into the area. The convective line produced scattered thunderstorm wind damage as it surged southeast into the northern Coastal Plain and eastern Piedmont of North Carolina. A QLCS developed over southern Virginia along and ahead of a weak surface cold front and attendant shortwave trough moving into the area. The convective line produced scattered thunderstorm wind damage as it surged southeast into the northern Coastal Plain and eastern Piedmont of North Carolina. A QLCS developed over southern Virginia along and ahead of a weak surface cold front and attendant shortwave trough moving into the area. The convective line produced scattered thunderstorm wind damage as it surged southeast into the northern Coastal Plain and eastern Piedmont of North Carolina. A QLCS developed over southern Virginia along and ahead of a weak surface cold front and attendant shortwave trough moving into the area. The convective line produced scattered thunderstorm wind damage as it surged southeast into the northern Coastal Plain and eastern Piedmont of North Carolina.\nEvent Narrative: A large tree limb was blown down near Dunhill Terrace. One tree was blown down. One tree was blown down with local power outages reported on Marshburn Road. Fire department was dispatched to remove a very large tree limb in the road.",
+        "The following events were reported: Flash Flood, Thunderstorm Wind. These occurred near station USW00013722, approximately 19.468 km away, between 2014-08-12 17:10:00 and 2014-08-13 03:30:00.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 2513000.0 and crop damage of 0.0. \n\nEpisode Narrative: A cluster of showers and storms develop across the triangle region of central North Carolina. A few of these storms became severe and produced damaging wind gusts. In addition, these storms produced heavy rain, resulting in significant flash flooding in Wake and Johnston Counties. A cluster of showers and storms develop across the triangle region of central North Carolina. A few of these storms became severe and produced damaging wind gusts. In addition, these storms produced heavy rain, resulting in significant flash flooding in Wake and Johnston Counties. A cluster of showers and storms develop across the triangle region of central North Carolina. A few of these storms became severe and produced damaging wind gusts. In addition, these storms produced heavy rain, resulting in significant flash flooding in Wake and Johnston Counties. A cluster of showers and storms develop across the triangle region of central North Carolina. A few of these storms became severe and produced damaging wind gusts. In addition, these storms produced heavy rain, resulting in significant flash flooding in Wake and Johnston Counties. A cluster of showers and storms develop across the triangle region of central North Carolina. A few of these storms became severe and produced damaging wind gusts. In addition, these storms produced heavy rain, resulting in significant flash flooding in Wake and Johnston Counties. A cluster of showers and storms develop across the triangle region of central North Carolina. A few of these storms became severe and produced damaging wind gusts. In addition, these storms produced heavy rain, resulting in significant flash flooding in Wake and Johnston Counties. A cluster of showers and storms develop across the triangle region of central North Carolina. A few of these storms became severe and produced damaging wind gusts. In addition, these storms produced heavy rain, resulting in significant flash flooding in Wake and Johnston Counties.\nEvent Narrative: Several cars were reported stuck in flood waters near the intersection of Highouse Road, with several water rescues preformed. Durham Drive at Gideon Creek Way were reported closed due to flash flooding. Lilly Atkins Road was closed to due flooding near Holly Springs Road. One tree was reported down on power lines near I-85 near mile marker 172. Four trees were reported down on Country Trail Road. Multiple businesses had to be evacuated from the 1600-1800 block of Capital Boulevard. As many as 71 people had to be rescued and evacuated from businesses in this area. In addition, at the nearby intersection of Atlantic Avenue and Old Louisburg Road cars were reported flooded and stuck in the flood waters. Another car was reported stranded in the flood waters nearby at the intersection of Atlantic Avenue and Hodges Street. Monetary damages were estimated to be around 2-3 million dollars. Numerous roads were reported closed in Clayton due to flooding.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 28.5788 km away, between 2014-08-18 18:50:00 and 2014-08-18 19:15:00. 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: A potent disturbance aloft tracked across the area during peak heating and allowed for the development of scattered strong to severe convection across central North Carolina. A potent disturbance aloft tracked across the area during peak heating and allowed for the development of scattered strong to severe convection across central North Carolina.\nEvent Narrative: Power lines were reported down at Tryon Road and Pink Acres Street. One tree was reported down on power lines on Flamingo Drive.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 16.1823 km away, between 2014-08-20 16:55:00 and 2014-08-20 18:00:00.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 37000.0 and crop damage of 0.0. \n\nEpisode Narrative: Isolated to locally scattered showers and storms developed during the afternoon in an environment conducive of enhanced wind gust potential. A few of the strongest storms became severe and produced damaging wind gusts across portions of Wake County, North Carolina, including at the Raleigh Durham International Airport. Isolated to locally scattered showers and storms developed during the afternoon in an environment conducive of enhanced wind gust potential. A few of the strongest storms became severe and produced damaging wind gusts across portions of Wake County, North Carolina, including at the Raleigh Durham International Airport. Isolated to locally scattered showers and storms developed during the afternoon in an environment conducive of enhanced wind gust potential. A few of the strongest storms became severe and produced damaging wind gusts across portions of Wake County, North Carolina, including at the Raleigh Durham International Airport. Isolated to locally scattered showers and storms developed during the afternoon in an environment conducive of enhanced wind gust potential. A few of the strongest storms became severe and produced damaging wind gusts across portions of Wake County, North Carolina, including at the Raleigh Durham International Airport. Isolated to locally scattered showers and storms developed during the afternoon in an environment conducive of enhanced wind gust potential. A few of the strongest storms became severe and produced damaging wind gusts across portions of Wake County, North Carolina, including at the Raleigh Durham International Airport.\nEvent Narrative: A tree was reported down on a power line near South Garner Park. Severe winds flipped over a super carivan aircraft and blew a large cargo container over an 8 foot fence into a car. One tree was blown down near the intersection of Timber Drive and Benson Road. A tree was blown down on a transmission line that feeds two substations near Mechanical Boulevard, which resulted in a large power outage affecting around 10,000 customers. A 50 knot wind gusts was reported at KRDU.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 22.5092 km away, between 2014-09-02 16:35:00 and 2014-09-02 16:35:00. 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: In the presence of steep low-level rates and in the vicinity of a sharpening pre-frontal surface trough, slow moving storms developed across the southern Piedmont and Sandhills during the afternoon and early evening.  Severe thunderstorm winds brought down several trees in Cumberland and Moore Counties.  Isolated flooding was also reported inside the Fayetteville city limits.\nEvent Narrative: Several trees were blown down along Lucky Drive, off of Ten Ten Road.",
+        "The following events were reported: Flash Flood. These occurred near station USW00013722, approximately 42.2076 km away, between 2014-09-08 18:20:00 and 2014-09-09 02:45:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Deep tropical moisture was in place across the region as a slow moving low pressure system tracked northeast across eastern North Carolina. A large swath of 5 to 8 inches of rain fell across the eastern Piedmont and coastal plain counties of North Carolina throughout the day and into the overnight hours. This heavy rainfall resulted in minor flooding and closed numerous roads across the area. The most severe flooding occurred in Warren County where as much as 9 inches fell that led to the collapse of two roads and resulted in minor injuries. Deep tropical moisture was in place across the region as a slow moving low pressure system tracked northeast across eastern North Carolina. A large swath of 5 to 8 inches of rain fell across the eastern Piedmont and coastal plain counties of North Carolina throughout the day and into the overnight hours. This heavy rainfall resulted in minor flooding and closed numerous roads across the area. The most severe flooding occurred in Warren County where as much as 9 inches fell that led to the collapse of two roads and resulted in minor injuries.\nEvent Narrative: Several roads were impassible and had to be closed near Coats Crossroads, including Polenta Road at Raleigh Road and Old Fairground Road near Zacks Mill Road. Several roads were impassible, including Government Road near Jack Road and Amelia Church Road near Shotwell Road.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 49.7894 km away, between 2015-01-04 15:45:00 and 2015-01-04 15:45:00. 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: Within a northward advancing warm sector, low top convection out of upstate South Carolina moved north into the area during the afternoon. One convective cluster produced isolated wind damage in Lee and Johnston Counties.\nEvent Narrative: Trees down near the intersection of North Carolina Highway 42 and Thanksgiving Fire Road.",
+        "The following events were reported: Hail. These occurred near station USW00013722, approximately 42.6591 km away, between 2015-04-08 18:55:00 and 2015-04-08 20:03:00. The events included records with hailstones measuring 1.75 inches.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 10000000.0 and crop damage of 0.0. \n\nEpisode Narrative: With a front draped across the area, an MCV tracked over the region. Given the unstable air mass in place, convection developed and several of the storms became severe. The main impact was very large hail up to the of hen eggs (around 2 inches). One of the storms did significant damage in Franklin county, with holes being put in several homes siding and windows and multiple car windshields being scattered. With a front draped across the area, an MCV tracked over the region. Given the unstable air mass in place, convection developed and several of the storms became severe. The main impact was very large hail up to the of hen eggs (around 2 inches). One of the storms did significant damage in Franklin county, with holes being put in several homes siding and windows and multiple car windshields being scattered. With a front draped across the area, an MCV tracked over the region. Given the unstable air mass in place, convection developed and several of the storms became severe. The main impact was very large hail up to the of hen eggs (around 2 inches). One of the storms did significant damage in Franklin county, with holes being put in several homes siding and windows and multiple car windshields being scattered.\nEvent Narrative: A swath of hail up to the size of hen eggs was reported from near Bunn to near Pilot. Multiple homes had holes in the siding and windows and multiple cars' windshields were scattered. Ping pong ball size hail was reported near the intersection of Charlie Grissom Road and Egypt Mountain Road just southwest of Kittrell. A swath of hail up to the size of golf balls was reported in and around Franklinton.",
+        "The following events were reported: Flash Flood, Lightning. These occurred near station USW00013722, approximately 23.0552 km away, between 2015-04-09 19:15:00 and 2015-04-09 20:50:00.The events resulted in 0 injuries and 1 fatalities. The events caused property damage valued at 25000.0 and crop damage of 0.0. \n\nEpisode Narrative: A northward retreating warm front served as the primary focus for convective development. Afternoon heating resulted in destabilization and several storms became severe, with large hail being the primary impact. Isolated flash flooding also occurred. These thunderstorms also had excessive lightning, which resulted in a fatality. A northward retreating warm front served as the primary focus for convective development. Afternoon heating resulted in destabilization and several storms became severe, with large hail being the primary impact. Isolated flash flooding also occurred. These thunderstorms also had excessive lightning, which resulted in a fatality. A northward retreating warm front served as the primary focus for convective development. Afternoon heating resulted in destabilization and several storms became severe, with large hail being the primary impact. Isolated flash flooding also occurred. These thunderstorms also had excessive lightning, which resulted in a fatality.\nEvent Narrative: Nine apartments were flooded, temporarily displacing several residents. Two cars became stranded in high water. A 28 year old male was struck and killed by lightning in the parking lot of a shopping center.",
+        "The following events were reported: Hail. These occurred near station USW00013722, approximately 41.3181 km away, between 2015-04-20 14:25:00 and 2015-04-20 15:45:00. 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: Scattered thunderstorms developed as a cold front approached the area during peak heating. Given the strong destabilization, many of these storms became severe and produced large hail. Scattered thunderstorms developed as a cold front approached the area during peak heating. Given the strong destabilization, many of these storms became severe and produced large hail.\nEvent Narrative: Quarter size hail reported just southwest of Pittsboro. Quarter size hail was reported by the public.",
+        "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00013722, approximately 28.2667 km away, between 2015-06-17 21:23:00 and 2015-06-17 23:35:00. The events included records with hailstones measuring 37.8125 inches.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 diffuse surface boundary helped trigger thunderstorms during the evening hours. Sufficient instability and shear allowed some of the storms to strengthen to severe limits, thus producing wind damage and large hail. A diffuse surface boundary helped trigger thunderstorms during the evening hours. Sufficient instability and shear allowed some of the storms to strengthen to severe limits, thus producing wind damage and large hail. A diffuse surface boundary helped trigger thunderstorms during the evening hours. Sufficient instability and shear allowed some of the storms to strengthen to severe limits, thus producing wind damage and large hail. A diffuse surface boundary helped trigger thunderstorms during the evening hours. Sufficient instability and shear allowed some of the storms to strengthen to severe limits, thus producing wind damage and large hail.\nEvent Narrative: Multiple trees were blown down across the roadway just south of Clayton. Several trees were blown down along a few mile swath in Cary. Also, one tree fell on a house in the 100 block of Honeysuckle Lane. Half dollar to quarter sized hail was reported along a swath from Cary to Raleigh. One tree and some power lines were blown down along a couple miles long swath extending through Angier.",
+        "The following events were reported: Flash Flood, Hail, Thunderstorm Wind. These occurred near station USW00013722, approximately 22.3347 km away, between 2015-06-18 18:59:00 and 2015-06-18 22:20:00. The events included records with hailstones measuring 33.666666666666664 inches.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 40000.0 and crop damage of 0.0. \n\nEpisode Narrative: Scattered thunderstorms developed in a very moist and moderately unstable air mass. Many of these storms became severe producing wind damage and large hail. In addition, some flash flooding occurred as the storms moved slowly. Scattered thunderstorms developed in a very moist and moderately unstable air mass. Many of these storms became severe producing wind damage and large hail. In addition, some flash flooding occurred as the storms moved slowly. Scattered thunderstorms developed in a very moist and moderately unstable air mass. Many of these storms became severe producing wind damage and large hail. In addition, some flash flooding occurred as the storms moved slowly. Scattered thunderstorms developed in a very moist and moderately unstable air mass. Many of these storms became severe producing wind damage and large hail. In addition, some flash flooding occurred as the storms moved slowly. Scattered thunderstorms developed in a very moist and moderately unstable air mass. Many of these storms became severe producing wind damage and large hail. In addition, some flash flooding occurred as the storms moved slowly. Scattered thunderstorms developed in a very moist and moderately unstable air mass. Many of these storms became severe producing wind damage and large hail. In addition, some flash flooding occurred as the storms moved slowly. Scattered thunderstorms developed in a very moist and moderately unstable air mass. Many of these storms became severe producing wind damage and large hail. In addition, some flash flooding occurred as the storms moved slowly.\nEvent Narrative: Quarter size hail was reported along a couple miles long swath across northwestern Raleigh. A couple of trees were blown down along a swath from a few miles northwest of Bunn to a couple of miles southeast of Bunn. One of the trees fell on a house on Dump Horton Road. Several trees and power lines were blown down along a swath from near Carrboro to near Chapel Hill. High was was reported on several roads in and around Morrisville, with one vehicle becoming stranded. Four cars were stuck in high water near Arendell Avenue and Highway 64. Also, a truck was stranded at Wendell Road exit ramp off Highway 64. Flooding was reported on Hillsboro Street at the railroad underpass. Avent Ferry Road at Trailwood Road was flooded.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 35.3532 km away, between 2015-06-20 18:09:00 and 2015-06-20 20:10:00. 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 42500.0 and crop damage of 0.0. \n\nEpisode Narrative: The remnants of Tropical Storm Bill moved across the Mid-Atlantic region, helping to produce scattered to numerous storms across the northern half of central North Carolina. Some of these storms became severe and produced wind damage. The remnants of Tropical Storm Bill moved across the Mid-Atlantic region, helping to produce scattered to numerous storms across the northern half of central North Carolina. Some of these storms became severe and produced wind damage. The remnants of Tropical Storm Bill moved across the Mid-Atlantic region, helping to produce scattered to numerous storms across the northern half of central North Carolina. Some of these storms became severe and produced wind damage. The remnants of Tropical Storm Bill moved across the Mid-Atlantic region, helping to produce scattered to numerous storms across the northern half of central North Carolina. Some of these storms became severe and produced wind damage.\nEvent Narrative: A large tree was reported down on a house. One tree was reported down near Mebane. One tree as reported down on a house and truck. A couple of trees were reported down on Timberlake Road near North Carolina Highway 56.",
+        "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00013722, approximately 26.9645 km away, between 2015-06-25 16:20:00 and 2015-06-25 20:32:00. The events included records with hailstones measuring 6.486111111111111 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A stalled cold front during the morning lifted northward in the afternoon. Several rounds of storms develop in the vicinity of the front. Some of the storms became severe and produced severe hail and damaging winds, along with localized flash flooding. A stalled cold front during the morning lifted northward in the afternoon. Several rounds of storms develop in the vicinity of the front. Some of the storms became severe and produced severe hail and damaging winds, along with localized flash flooding. A stalled cold front during the morning lifted northward in the afternoon. Several rounds of storms develop in the vicinity of the front. Some of the storms became severe and produced severe hail and damaging winds, along with localized flash flooding. A stalled cold front during the morning lifted northward in the afternoon. Several rounds of storms develop in the vicinity of the front. Some of the storms became severe and produced severe hail and damaging winds, along with localized flash flooding. A stalled cold front during the morning lifted northward in the afternoon. Several rounds of storms develop in the vicinity of the front. Some of the storms became severe and produced severe hail and damaging winds, along with localized flash flooding. A stalled cold front during the morning lifted northward in the afternoon. Several rounds of storms develop in the vicinity of the front. Some of the storms became severe and produced severe hail and damaging winds, along with localized flash flooding. A stalled cold front during the morning lifted northward in the afternoon. Several rounds of storms develop in the vicinity of the front. Some of the storms became severe and produced severe hail and damaging winds, along with localized flash flooding. A stalled cold front during the morning lifted northward in the afternoon. Several rounds of storms develop in the vicinity of the front. Some of the storms became severe and produced severe hail and damaging winds, along with localized flash flooding. A stalled cold front during the morning lifted northward in the afternoon. Several rounds of storms develop in the vicinity of the front. Some of the storms became severe and produced severe hail and damaging winds, along with localized flash flooding. A stalled cold front during the morning lifted northward in the afternoon. Several rounds of storms develop in the vicinity of the front. Some of the storms became severe and produced severe hail and damaging winds, along with localized flash flooding. A stalled cold front during the morning lifted northward in the afternoon. Several rounds of storms develop in the vicinity of the front. Some of the storms became severe and produced severe hail and damaging winds, along with localized flash flooding. A stalled cold front during the morning lifted northward in the afternoon. Several rounds of storms develop in the vicinity of the front. Some of the storms became severe and produced severe hail and damaging winds, along with localized flash flooding. A stalled cold front during the morning lifted northward in the afternoon. Several rounds of storms develop in the vicinity of the front. Some of the storms became severe and produced severe hail and damaging winds, along with localized flash flooding. A stalled cold front during the morning lifted northward in the afternoon. Several rounds of storms develop in the vicinity of the front. Some of the storms became severe and produced severe hail and damaging winds, along with localized flash flooding. A stalled cold front during the morning lifted northward in the afternoon. Several rounds of storms develop in the vicinity of the front. Some of the storms became severe and produced severe hail and damaging winds, along with localized flash flooding. A stalled cold front during the morning lifted northward in the afternoon. Several rounds of storms develop in the vicinity of the front. Some of the storms became severe and produced severe hail and damaging winds, along with localized flash flooding. A stalled cold front during the morning lifted northward in the afternoon. Several rounds of storms develop in the vicinity of the front. Some of the storms became severe and produced severe hail and damaging winds, along with localized flash flooding. A stalled cold front during the morning lifted northward in the afternoon. Several rounds of storms develop in the vicinity of the front. Some of the storms became severe and produced severe hail and damaging winds, along with localized flash flooding.\nEvent Narrative: Quarter size hail was reported. Quarter size hail was reported near Angier along North Carolina Highway 55. Quarter size hail was reported. Quarter size hail was reported. Quarter size hail was reported near the intersection of South Nash Street and Calvin Street. Quarter size hail was reported near Triple Creek Drive in Efland. Golf ball size hail was reported near Fordham Boulevard and East Franklin Street. Dime size hail was reported on Theford Road. Penny size hail was reported near Old Chapel Hill road and Garrett Road. Quarter size hail was reported near Taylor Hall Place. Quarter to half dollar size hail was reported on I-40 and North Carolina Highway 54. Quarter size hail was reported. One tree was blown down onto a home. No further information was available.   Tree was blown down across the road on Lannie Drive.  Quarter size hail was reported near Governor Scott Road.",
+        "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00013722, approximately 26.5569 km away, between 2015-06-26 15:00:00 and 2015-06-26 22:47:00. The events included records with hailstones measuring 37.75 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 pre-frontal trough served as a focus for convective development during the late afternoon and evening hours. Given the very moist and unstable air mass, many of the storms became severe, producing wind damage and large hail. A pre-frontal trough served as a focus for convective development during the late afternoon and evening hours. Given the very moist and unstable air mass, many of the storms became severe, producing wind damage and large hail. A pre-frontal trough served as a focus for convective development during the late afternoon and evening hours. Given the very moist and unstable air mass, many of the storms became severe, producing wind damage and large hail. A pre-frontal trough served as a focus for convective development during the late afternoon and evening hours. Given the very moist and unstable air mass, many of the storms became severe, producing wind damage and large hail.\nEvent Narrative: Several tress were blown down on Mal Weathers Road and Silver Farm Road. A pool was also blown over. Radar data strongly indicated a downburst. Quarter size hail was reported along a swath several miles west of Clayton to several miles south of Clayton. Several trees and power lines were blown down in Carrboro. Multiple trees were blown down along a swath that began several miles east of Chapel Hill and continued to Bethesda.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 37.572 km away, between 2015-06-27 17:05:00 and 2015-06-27 18:53:00. 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 5000.0 and crop damage of 0.0. \n\nEpisode Narrative: Scattered thunderstorms developed as an unseasonably strong mid level trough approached the region. With a prefrontal trough serving as a low level focus and a very moist and unstable air mass in place, many of the storms became severe, producing wind damage. In addition, a brief tornado spun up in Lee County. Scattered thunderstorms developed as an unseasonably strong mid level trough approached the region. With a prefrontal trough serving as a low level focus and a very moist and unstable air mass in place, many of the storms became severe, producing wind damage. In addition, a brief tornado spun up in Lee County. Scattered thunderstorms developed as an unseasonably strong mid level trough approached the region. With a prefrontal trough serving as a low level focus and a very moist and unstable air mass in place, many of the storms became severe, producing wind damage. In addition, a brief tornado spun up in Lee County.\nEvent Narrative: A tree was blown down on a mobile home in the New Hope Mobile Home Park. Several trees were blown down along a swath from near Coats Crossroads to near Benson. Multiple tress were blown down and were blocking one lane of Highway 42.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 26.4708 km away, between 2015-06-30 17:49:00 and 2015-06-30 18:38:00. 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: The persistent upper trough over the region was amplified as a strong vorticity maximum approached and crossed the region through the evening hours. With sufficient moisture, instability and shear, thunderstorms developed and organized into a broken line, which crossed most of the forecast area and produced widespread wind damage. The persistent upper trough over the region was amplified as a strong vorticity maximum approached and crossed the region through the evening hours. With sufficient moisture, instability and shear, thunderstorms developed and organized into a broken line, which crossed most of the forecast area and produced widespread wind damage.\nEvent Narrative: Numerous trees were blown down along a swath from near Carr to near Hillsborough. One tree fell on a car in the city of Hillsborough. Monetary damage was estimated. A couple of trees were blown down along a swath from near Creedmoor to several miles northeast of Creedmoor.",
+        "The following events were reported: Lightning, Thunderstorm Wind. These occurred near station USW00013722, approximately 37.2672 km away, between 2015-07-05 19:15:00 and 2015-07-05 21:00:00.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 35000.0 and crop damage of 0.0. \n\nEpisode Narrative: Several upper level disturbances crossed the area in the southwesterly flow aloft. These combined with a moist and unstable environment to produce scattered convection, with some of the storms becoming severe. One of the storms produced a microburst, resulting in multiple downed trees and some minor property damage. Several upper level disturbances crossed the area in the southwesterly flow aloft. These combined with a moist and unstable environment to produce scattered convection, with some of the storms becoming severe. One of the storms produced a microburst, resulting in multiple downed trees and some minor property damage. Several upper level disturbances crossed the area in the southwesterly flow aloft. These combined with a moist and unstable environment to produce scattered convection, with some of the storms becoming severe. One of the storms produced a microburst, resulting in multiple downed trees and some minor property damage. Several upper level disturbances crossed the area in the southwesterly flow aloft. These combined with a moist and unstable environment to produce scattered convection, with some of the storms becoming severe. One of the storms produced a microburst, resulting in multiple downed trees and some minor property damage.\nEvent Narrative: A lightning strike sparked a fire in the attic of 10 Kings Mount Court causing moderate structural damage. Monetary damage was estimated. A couple of trees were blown down near the intersection of Trail Ridge Drive and County Line Road. Multiple trees were blown down on Applewhite Road. Multiple trees were blown down, with some snapped and some uprooted. Also, some minor property damage was caused to a fence and a pool by falling trees. Photos and radar analysis confirmed that the cause of this wind damage was a microburst. Monetary damage was estimated.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 32.5314 km away, between 2015-07-08 20:31:00 and 2015-07-08 21:00:00. 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: With a nearly stationary front located just north of the North Carolina/Virginia state line, scattered thunderstorms developed within a marginally unstable air mass. In addition, a mid level shortwave approached and crossed the region during the evening hours, leading to an increase in convective coverage. Many of the storms became severe and produced wind damage. With a nearly stationary front located just north of the North Carolina/Virginia state line, scattered thunderstorms developed within a marginally unstable air mass. In addition, a mid level shortwave approached and crossed the region during the evening hours, leading to an increase in convective coverage. Many of the storms became severe and produced wind damage.\nEvent Narrative: Multiple trees were blown down on Lake Wheeler Road near Ten-Ten. A couple of trees were blown down in the road on Covered Bridge Road at O'Neil Street.",
+        "The following events were reported: Lightning, Thunderstorm Wind. These occurred near station USW00013722, approximately 29.2427 km away, between 2015-07-13 06:29:00 and 2015-07-13 06:40:00.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 32000.0 and crop damage of 0.0. \n\nEpisode Narrative: A series of mid level disturbances moved through central North Carolina, one in the morning into the early afternoon and another in the evening. These disturbances coupled with a very moist and unstable air mass allowed strong to severe storms to develop across the area, producing wind damage and large hail. A series of mid level disturbances moved through central North Carolina, one in the morning into the early afternoon and another in the evening. These disturbances coupled with a very moist and unstable air mass allowed strong to severe storms to develop across the area, producing wind damage and large hail. A series of mid level disturbances moved through central North Carolina, one in the morning into the early afternoon and another in the evening. These disturbances coupled with a very moist and unstable air mass allowed strong to severe storms to develop across the area, producing wind damage and large hail.\nEvent Narrative: A barn was struck by lightning and burned down near Meadowbrook Country Club. One tree was reported down on a house near Lake Benson. Trees were reported down near US Highway 401.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 38.2525 km away, between 2015-07-18 12:54:00 and 2015-07-18 14:25:00. 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 moving across the area during peak heating triggered a line of showers and thunderstorms, which produced numerous reports of wind damage. A shortwave moving across the area during peak heating triggered a line of showers and thunderstorms, which produced numerous reports of wind damage. A shortwave moving across the area during peak heating triggered a line of showers and thunderstorms, which produced numerous reports of wind damage.\nEvent Narrative: Several trees were blown down across the road at Highway 15S and Bryans Hill Road southwest of Oxford. A couple of trees were blown down along a swath from a few miles southwest of Franklinton (near Youngsville) to a couple of miles northeast of Franklinton. A couple of trees were blown down across the roadway.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 15.1586 km away, between 2015-07-19 14:54:00 and 2015-07-19 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 weak disturbance crossed the area in the northwesterly flow aloft. This coupled with a lee side trough across the region resulted in isolated to widely scattered showers and thunderstorms, with a few becoming severe and producing wind damage. A weak disturbance crossed the area in the northwesterly flow aloft. This coupled with a lee side trough across the region resulted in isolated to widely scattered showers and thunderstorms, with a few becoming severe and producing wind damage.\nEvent Narrative: A tree and several power lines were blown down along a short swath through Gorman. One tree was blown down at the intersection of Wade Avenue and Glenwood Avenue.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 15.7501 km away, between 2015-07-21 17:50:00 and 2015-07-21 18:21:00. 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: A trailing cold front moved into central North Carolina during the late afternoon into the evening triggering scattered thunderstorms in an unstable atmosphere. Some of these storms became severe and produced wind damage. A trailing cold front moved into central North Carolina during the late afternoon into the evening triggering scattered thunderstorms in an unstable atmosphere. Some of these storms became severe and produced wind damage. A trailing cold front moved into central North Carolina during the late afternoon into the evening triggering scattered thunderstorms in an unstable atmosphere. Some of these storms became severe and produced wind damage.\nEvent Narrative: Multiple trees were reported down in the Chapel Hill and Carrboro areas. A large tree was reported down across a pedestrian walkway. One tree was reported down on Vann Street.",
+        "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00013722, approximately 9.3853 km away, between 2015-07-23 09:25:00 and 2015-07-23 10:00:00. The events included records with hailstones measuring 33.583333333333336 inches.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 1000.0 and crop damage of 0.0. \n\nEpisode Narrative: An area of low pressure tracked along a stalled weak frontal boundary across southern portions of central North Carolina and produced scattered showers and storms. a few of the storms became severe and produced damaging winds and quarter size hail. An area of low pressure tracked along a stalled weak frontal boundary across southern portions of central North Carolina and produced scattered showers and storms. a few of the storms became severe and produced damaging winds and quarter size hail. An area of low pressure tracked along a stalled weak frontal boundary across southern portions of central North Carolina and produced scattered showers and storms. a few of the storms became severe and produced damaging winds and quarter size hail.\nEvent Narrative:  One tree was reported down near Saint Albans Drive and Wake Forest Road. A tree and power lines were reported down near Patterson Road.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 48.0229 km away, between 2015-08-11 16:33:00 and 2015-08-11 18:41:00. 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 3750.0 and crop damage of 0.0. \n\nEpisode Narrative: A broken line of showers and storms moved across the area during the afternoon into the evening. Some of these storms became severe and produced wind damage across the area. A broken line of showers and storms moved across the area during the afternoon into the evening. Some of these storms became severe and produced wind damage across the area. A broken line of showers and storms moved across the area during the afternoon into the evening. Some of these storms became severe and produced wind damage across the area. A broken line of showers and storms moved across the area during the afternoon into the evening. Some of these storms became severe and produced wind damage across the area.\nEvent Narrative: One tree was reported down at Union Grove Church Road. One tree was reported down at McCullock Loop Road. Power lines were reported down at Hurdle Mills Road. Trees were reported down near Covered Bridge Road.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 38.7786 km away, between 2015-09-10 16:18:00 and 2015-09-10 16:30:00. 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: Numerous thunderstorms developed ahead of an approaching cold front in a very moist and marginally unstable environment. A few of the storms became severe, with one storm blowing down several large trees.\nEvent Narrative: Several large trees were blown down along a swath between Newlin Road in Sutphin and River Road near Chicken Bridge Road north of Bynum.",
+        "The following events were reported: Flash Flood. These occurred near station USW00013722, approximately 19.5692 km away, between 2015-12-23 10:30:00 and 2015-12-23 18:00:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Deep southerly flow advected rich moisture into the forecast area as a deep trough remained situated west of the area. Precipitable water values were near record highs and 4-5 standard deviations above normal. This lead to moderate to heavy rainfall across the region, which had a flash flood watch in effect. Widespread 1-2 inches of rain occurred, with a few isolated areas receiving upwards of 3 inches. A couple locations experienced flash flooding. Deep southerly flow advected rich moisture into the forecast area as a deep trough remained situated west of the area. Precipitable water values were near record highs and 4-5 standard deviations above normal. This lead to moderate to heavy rainfall across the region, which had a flash flood watch in effect. Widespread 1-2 inches of rain occurred, with a few isolated areas receiving upwards of 3 inches. A couple locations experienced flash flooding.\nEvent Narrative: Twenty reports of high water were received across the city of Durham, from the late morning to early afternoon. This resulted in several street closings. Bolin Creek rose out of its banks and impacted areas near Estes Drive in Chapel Hill. During the morning hours, the fire department had to transport people off the flooded road. Later in the day, flooding became worse as more heavy rain fell.",
+        "The following events were reported: Flash Flood. These occurred near station USW00013722, approximately 22.5285 km away, between 2015-12-30 12:30:00 and 2015-12-30 18:00:00.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 triggered showers and a few isolated storms across the region. With an extremely moist air mass in place, moderate to heavy rain fell. Given the very saturated soils, flash flooding quickly developed. An approaching cold front triggered showers and a few isolated storms across the region. With an extremely moist air mass in place, moderate to heavy rain fell. Given the very saturated soils, flash flooding quickly developed. An approaching cold front triggered showers and a few isolated storms across the region. With an extremely moist air mass in place, moderate to heavy rain fell. Given the very saturated soils, flash flooding quickly developed. An approaching cold front triggered showers and a few isolated storms across the region. With an extremely moist air mass in place, moderate to heavy rain fell. Given the very saturated soils, flash flooding quickly developed. An approaching cold front triggered showers and a few isolated storms across the region. With an extremely moist air mass in place, moderate to heavy rain fell. Given the very saturated soils, flash flooding quickly developed.\nEvent Narrative: Nanas Restaurant on University Drive in Durham flooded. In addition, University Drive was impassible. Multiple roads were closed in the Chapel Hill and Carrboro area. In addition a home was reported to be flooded. Numerous roads were closed due to high water in southwest Orange County. Flooding caused minor damage to the Hillandale Road VA Clinic in Durham, where 1-2 inches of water got inside the building. In addition, high water signs were deployed across Durham. Several roads were flooded in downtown Raleigh. Several creeks were near or over their banks along NC 50.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 36.9866 km away, between 2017-03-01 20:20:00 and 2017-03-01 20:28:00. 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: Warm sector destabilization in advance of a strong cold front approaching from the west, allowed clusters and small lines of strong to severe thunderstorms to move east from the southern Appalachians during the afternoon, into the western and central Piedmont of  NC during the evening. The storms produced several quarter size hail swaths across |the western Piedmont, along with localized straight-line wind damage in Chatham County.\nEvent Narrative: Three trees reported blown down along the swath, including one down tree on Foxwood Trail.",
+        "The following events were reported: Hail. These occurred near station USW00013722, approximately 11.7371 km away, between 2017-04-06 06:35:00 and 2017-04-06 06:45:00. 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: On the early morning of April 6th, showers and thunderstorms moved into Central NC from the southwest. A few of the storms became severe as a result of strong dynamic forcing and steep lapse rates combined with the high surface dew points. The severe storms produced quarter size hail and a long swath of damaging winds.\nEvent Narrative: Dime to quarter size hail fell in Durham.",
+        "The following events were reported: Flash Flood. These occurred near station USW00013722, approximately 14.6459 km away, between 2017-04-25 00:45:00 and 2017-04-25 09:59:00.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 164000.0 and crop damage of 0.0. \n\nEpisode Narrative: A Flash Flood Watch was issued in advance of an abnormally deep upper level low moving over Central North Carolina. The trough became negatively tilted, pulling deep, moist air from the southwest into the region. The moist southwesterly flow overrunning a cold pool at the surface produced a prolonged period of moderate to heavy rain, which resulted in widespread areal flooding across the region. However, only isolated Flash Flooding occurred. A Flash Flood Watch was issued in advance of an abnormally deep upper level low moving over Central North Carolina. The trough became negatively tilted, pulling deep, moist air from the southwest into the region. The moist southwesterly flow overrunning a cold pool at the surface produced a prolonged period of moderate to heavy rain, which resulted in widespread areal flooding across the region. However, only isolated Flash Flooding occurred. A Flash Flood Watch was issued in advance of an abnormally deep upper level low moving over Central North Carolina. The trough became negatively tilted, pulling deep, moist air from the southwest into the region. The moist southwesterly flow overrunning a cold pool at the surface produced a prolonged period of moderate to heavy rain, which resulted in widespread areal flooding across the region. However, only isolated Flash Flooding occurred. A Flash Flood Watch was issued in advance of an abnormally deep upper level low moving over Central North Carolina. The trough became negatively tilted, pulling deep, moist air from the southwest into the region. The moist southwesterly flow overrunning a cold pool at the surface produced a prolonged period of moderate to heavy rain, which resulted in widespread areal flooding across the region. However, only isolated Flash Flooding occurred.\nEvent Narrative: Flash flooding resulted in a water rescue at the intersection of Johnson Pond Road and Bells Lake Road. Flash flooding resulted in a water rescue near the intersection of Ten-Ten Road and US-1. Lumley road was closed due to flash flooding between Interstate 540 and Brier Creek Parkway. Numerous roads were closed due to flash flooding along Crabtree Creek. Road closures included Atlantic Avenue at Hodges Street, Six Forks Road at Wake Forest Road and Creedmoor Road at Glenwood Avenue. Wycliff Road at Lake Boone Trail was also closed due to flooding.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 31.515 km away, between 2017-05-05 03:20:00 and 2017-05-05 04:51:00. 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 20000.0 and crop damage of 0.0. \n\nEpisode Narrative: A strong cold front moved across the region during the early morning hours of May 5th. Widespread Winds damage occurred in associated with the storms, along with one tornado in Granville County. A strong cold front moved across the region during the early morning hours of May 5th. Widespread Winds damage occurred in associated with the storms, along with one tornado in Granville County. A strong cold front moved across the region during the early morning hours of May 5th. Widespread Winds damage occurred in associated with the storms, along with one tornado in Granville County. A strong cold front moved across the region during the early morning hours of May 5th. Widespread Winds damage occurred in associated with the storms, along with one tornado in Granville County. A strong cold front moved across the region during the early morning hours of May 5th. Widespread Winds damage occurred in associated with the storms, along with one tornado in Granville County. A strong cold front moved across the region during the early morning hours of May 5th. Widespread Winds damage occurred in associated with the storms, along with one tornado in Granville County. A strong cold front moved across the region during the early morning hours of May 5th. Widespread Winds damage occurred in associated with the storms, along with one tornado in Granville County. A strong cold front moved across the region during the early morning hours of May 5th. Widespread Winds damage occurred in associated with the storms, along with one tornado in Granville County. A strong cold front moved across the region during the early morning hours of May 5th. Widespread Winds damage occurred in associated with the storms, along with one tornado in Granville County. A strong cold front moved across the region during the early morning hours of May 5th. Widespread Winds damage occurred in associated with the storms, along with one tornado in Granville County.\nEvent Narrative: One tree was reported down at White Cross Road and Old Greensboro Road. One tree was reported down at 4200 Brentwood. One tree was reported down at the intersection of Hopewell Drive and Pickett Road. A car crashed into a tree that was reported down on Garrett Road. One tree was reported down on Salem Road and Martin Luther King Junior Avenue. One tree was reported down on Manns Chapel Road. One tree and power lines were reported down on Lystra Road near Lystra Preserve Drive. A shed was destroyed off of Sam Adams Road near Highway 97. One tree was reported down on 24th Street. Power lines and one tree were reported down at the intersection of Helena-Moriah Road and Surl Mount Tizrah Road.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 19.1622 km away, between 2017-05-11 19:55:00 and 2017-05-11 21:05:00. 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 175000.0 and crop damage of 2000.0. \n\nEpisode Narrative: One severe cluster produced scattered wind damage along a northwest to southeast wind swath extending from Orange county to Johnston County. One severe cluster produced scattered wind damage along a northwest to southeast wind swath extending from Orange county to Johnston County. One severe cluster produced scattered wind damage along a northwest to southeast wind swath extending from Orange county to Johnston County. One severe cluster produced scattered wind damage along a northwest to southeast wind swath extending from Orange county to Johnston County. One severe cluster produced scattered wind damage along a northwest to southeast wind swath extending from Orange county to Johnston County. One severe cluster produced scattered wind damage along a northwest to southeast wind swath extending from Orange county to Johnston County. One severe cluster produced scattered wind damage along a northwest to southeast wind swath extending from Orange county to Johnston County. One severe cluster produced scattered wind damage along a northwest to southeast wind swath extending from Orange county to Johnston County. One severe cluster produced scattered wind damage along a northwest to southeast wind swath extending from Orange county to Johnston County. One severe cluster produced scattered wind damage along a northwest to southeast wind swath extending from Orange county to Johnston County. One severe cluster produced scattered wind damage along a northwest to southeast wind swath extending from Orange county to Johnston County. One severe cluster produced scattered wind damage along a northwest to southeast wind swath extending from Orange county to Johnston County. One severe cluster produced scattered wind damage along a northwest to southeast wind swath extending from Orange county to Johnston County. One severe cluster produced scattered wind damage along a northwest to southeast wind swath extending from Orange county to Johnston County. One severe cluster produced scattered wind damage along a northwest to southeast wind swath extending from Orange county to Johnston County.\nEvent Narrative: Approximately one dozen trees were blown down along Governor Burke Road, NC Highway 86 and New Hope Church Road. One tree was blown down and blocking the road on Pleasant Green Road at the Eno River Bridge. One tree was blown down near the 3200 Block of Rose of Sharon Road. One tree was blown down and was blocking the road at 104 Fox Ridge Road. One tree was blown down in a wooded area. One tree was blown down near the intersection of Cameron Blvd and Science Drive. A large tree fell and crashed into a home on Vickers Avenue. Monetary damages were estimated. One tree was blown near the intersection of Martin Luther King Jr Blvd and Stratford Lakes Drive. One tree was blown down and blocking the road near the intersection of Rock Creek Road and Timberlane Court. One tree was blown and blocking the road near the intersection of Durant Road and Falls of Neuse Road. One tree blown down onto power-lines at Anderson Drive and White Oak Road. Trees and power-lines blown down at Jarvis Street near Cameron Village. A large tree fell through the roof of a home in the Stonehenge Neighborhood. Monetary damages were estimated. One tree blown down on Mial Plantation Road. One tree was blown down at the 1900 block of Angier Avenue.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 30.2051 km away, between 2017-05-19 16:24:00 and 2017-05-19 16:42:00. 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: Ahead of a cold front approaching North Carolina, disturbances rotating around an upper level ridge off the Florida coast initiated deep convection in a moderately unstable airmass across southwestern Virginia and northwestern North Carolina. Ahead of a cold front approaching North Carolina, disturbances rotating around an upper level ridge off the Florida coast initiated deep convection in a moderately unstable airmass across southwestern Virginia and northwestern North Carolina.\nEvent Narrative: A couple of trees were blown down along a swath from northwest of Schley to just northeast of Hillsborough. Several trees were blown down on Old Oxford Road near Bahama.",
+        "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00013722, approximately 37.438 km away, between 2017-05-25 11:58:00 and 2017-05-25 16:45:00. The events included records with hailstones measuring 17.333333333333332 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: Numerous showers and thunderstorms developed in the wake of a surface cold front and ahead of an upper level trough approaching Central North Carolina. Increasing mid-level cold advection, steep low-level lapse rates and a strong mid-level jet resulted in a few of the thunderstorms becoming severe, producing large hail and isolated damaging winds. Numerous showers and thunderstorms developed in the wake of a surface cold front and ahead of an upper level trough approaching Central North Carolina. Increasing mid-level cold advection, steep low-level lapse rates and a strong mid-level jet resulted in a few of the thunderstorms becoming severe, producing large hail and isolated damaging winds. Numerous showers and thunderstorms developed in the wake of a surface cold front and ahead of an upper level trough approaching Central North Carolina. Increasing mid-level cold advection, steep low-level lapse rates and a strong mid-level jet resulted in a few of the thunderstorms becoming severe, producing large hail and isolated damaging winds.\nEvent Narrative: Hail up to the size of quarters was reported along a swath from Bunn to the campground at Lake Royale.  A tree was blown down onto power lines off Highway 70 in Hillsborough.",
+        "The following events were reported: Flash Flood, Thunderstorm Wind. These occurred near station USW00013722, approximately 28.775 km away, between 2017-06-16 18:13:00 and 2017-06-16 20:00:00.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 11250.0 and crop damage of 0.0. \n\nEpisode Narrative: A few loosely organized multicell convective clusters developed during the late afternoon and evening across the central Piedmont of North Carolina. The storms produced scattered thunderstorm wind damage and localized flash flooding. A few loosely organized multicell convective clusters developed during the late afternoon and evening across the central Piedmont of North Carolina. The storms produced scattered thunderstorm wind damage and localized flash flooding. A few loosely organized multicell convective clusters developed during the late afternoon and evening across the central Piedmont of North Carolina. The storms produced scattered thunderstorm wind damage and localized flash flooding. A few loosely organized multicell convective clusters developed during the late afternoon and evening across the central Piedmont of North Carolina. The storms produced scattered thunderstorm wind damage and localized flash flooding. A few loosely organized multicell convective clusters developed during the late afternoon and evening across the central Piedmont of North Carolina. The storms produced scattered thunderstorm wind damage and localized flash flooding. A few loosely organized multicell convective clusters developed during the late afternoon and evening across the central Piedmont of North Carolina. The storms produced scattered thunderstorm wind damage and localized flash flooding. A few loosely organized multicell convective clusters developed during the late afternoon and evening across the central Piedmont of North Carolina. The storms produced scattered thunderstorm wind damage and localized flash flooding. A few loosely organized multicell convective clusters developed during the late afternoon and evening across the central Piedmont of North Carolina. The storms produced scattered thunderstorm wind damage and localized flash flooding.\nEvent Narrative: Locally heavy rainfall of 2 to 3 inches flooded the right line of Interstate 40 near N. Harrison Avenue. Nearly a dozen trees and large branches were blown down in the Bahama area. There was also minor damage to an outbuilding. Monetary damages were estimated. Trees were blown down at the intersection of Martin Luther King Jr. Blvd and N. Estes Drive. Trees and power-lines were blown down near Fuquay Varina. A few trees were blown down, some on cars, at Nash Square Park in downtown Raleigh. Monetary damages were estimated. Several trees down in Youngsville, including along NC Highway 96. One tree was blown down across the west bound lane of NC Highway 56. One tree was blown down on Range Road.",
+        "The following events were reported: Flash Flood, Thunderstorm Wind. These occurred near station USW00013722, approximately 42.501 km away, between 2017-06-19 14:37:00 and 2017-06-20 02:10:00.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 14000.0 and crop damage of 0.0. \n\nEpisode Narrative: Multi-cellular convection developed ahead of an approaching cold front over Central North Carolina. A few thunderstorms became severe during the afternoon and evening, producing scattered wind damage. During the early morning hours of the 20th, the event morphed into more of a heavy rain and flash flooding threat, where isolated flash flooding developed within the convection ahead of the front. Multi-cellular convection developed ahead of an approaching cold front over Central North Carolina. A few thunderstorms became severe during the afternoon and evening, producing scattered wind damage. During the early morning hours of the 20th, the event morphed into more of a heavy rain and flash flooding threat, where isolated flash flooding developed within the convection ahead of the front. Multi-cellular convection developed ahead of an approaching cold front over Central North Carolina. A few thunderstorms became severe during the afternoon and evening, producing scattered wind damage. During the early morning hours of the 20th, the event morphed into more of a heavy rain and flash flooding threat, where isolated flash flooding developed within the convection ahead of the front. Multi-cellular convection developed ahead of an approaching cold front over Central North Carolina. A few thunderstorms became severe during the afternoon and evening, producing scattered wind damage. During the early morning hours of the 20th, the event morphed into more of a heavy rain and flash flooding threat, where isolated flash flooding developed within the convection ahead of the front.\nEvent Narrative: Heavy rain resulted in flash flooding on the south side of Hillsborough. A couple of roads were closed, including Dimmocks Mill Road at West Hill Avenue and Eno Street at Dimmocks Mill Road. A car became stranded in flood waters at the latter location. Several trees and a power line were blown down along a swath from the 1000 block of Old Stage Road near Angier to Abattoir Road near Coats. Several trees were blown down across northern Orange county, a few miles west-northwest of Schley. A couple of roads were closed due to flash flooding south-southeast of Mebane, including Ben Wilson Road near Bowman Road and the 2700 block of Mebane Oaks Road.",
+        "The following events were reported: Lightning, Thunderstorm Wind. These occurred near station USW00013722, approximately 36.1424 km away, between 2017-07-05 20:19:00 and 2017-07-05 20:35:00.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: Scattered severe storms, aided by propagation along cold pools and enhanced by any mergers of outflow produced scattered wind damage during the late afternoon and evening hours. Scattered severe storms, aided by propagation along cold pools and enhanced by any mergers of outflow produced scattered wind damage during the late afternoon and evening hours. Scattered severe storms, aided by propagation along cold pools and enhanced by any mergers of outflow produced scattered wind damage during the late afternoon and evening hours.\nEvent Narrative: Lightning struck a home, causing a fire on Quincy Cottage Road. Property damage was estimated. Three trees were blown down at the 1500 Block of Mt. Willing Road. One tree down near the intersection of Orange Grove Road and Dimmicks Mill Road.",
+        "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00013722, approximately 39.539 km away, between 2017-07-08 18:12:00 and 2017-07-08 19:50:00. The events included records with hailstones measuring 33.666666666666664 inches.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 5000.0 and crop damage of 0.0. \n\nEpisode Narrative: Scattered convection developed ahead of an approaching cold front in a warm, moist environment characterized by moderate instability and bulk shear. Several of the thunderstorms became severe as they progressed through Central North Carolina from west to east. Scattered convection developed ahead of an approaching cold front in a warm, moist environment characterized by moderate instability and bulk shear. Several of the thunderstorms became severe as they progressed through Central North Carolina from west to east. Scattered convection developed ahead of an approaching cold front in a warm, moist environment characterized by moderate instability and bulk shear. Several of the thunderstorms became severe as they progressed through Central North Carolina from west to east.\nEvent Narrative:  Two trees were blown down near the intersection of Wendell Boulevard and Wendell Falls Parkway. Both trees were approximately 12 inches in diameter, one was uprooted and the other was snapped. Three trees were blown down along a swath from 6 mile north of Coats Crossroads to 3 miles east of Benson. One of the trees was blown down onto power lines on Cleveland School Road.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 32.9001 km away, between 2017-07-13 17:01:00 and 2017-07-13 18:34:00. 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 11000.0 and crop damage of 0.0. \n\nEpisode Narrative: Scattered showers and thunderstorms developed in association with a weak surface trough in a warm, moist environment. A few isolated storms became severe, producing wind damage across several counties in Central North Carolina. Scattered showers and thunderstorms developed in association with a weak surface trough in a warm, moist environment. A few isolated storms became severe, producing wind damage across several counties in Central North Carolina.\nEvent Narrative: A couple of trees were blown down in northwest Orange County. Multiple large trees and several large branches were blown down along a swath between Falls Lake and Raleigh, resulting in damage to vehicles, as well as some roof and siding damage.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 36.3352 km away, between 2017-07-16 16:23:00 and 2017-07-16 16:28:00. 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: Showers and thunderstorms developed along and ahead of a stationary boundary over Central North Carolina. One thunderstorm became severe, producing isolated wind damage. Showers and thunderstorms developed along and ahead of a stationary boundary over Central North Carolina. One thunderstorm became severe, producing isolated wind damage.\nEvent Narrative: One tree was blown down near the intersection of Oakridge Duncan Road and NC Highway 42. One tree was blown down onto West Academy Street near Coley Farm Road.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 21.7496 km away, between 2017-07-23 16:45:00 and 2017-07-23 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 13000.0 and crop damage of 0.0. \n\nEpisode Narrative: Numerous showers and thunderstorms developed along differential heating boundaries in an abnormally hot and moderately unstable environment. Many of the thunderstorms became severe, producing widespread wind damage and isolated flash flooding. Numerous showers and thunderstorms developed along differential heating boundaries in an abnormally hot and moderately unstable environment. Many of the thunderstorms became severe, producing widespread wind damage and isolated flash flooding. Numerous showers and thunderstorms developed along differential heating boundaries in an abnormally hot and moderately unstable environment. Many of the thunderstorms became severe, producing widespread wind damage and isolated flash flooding.\nEvent Narrative: Several trees were blown down across southern Orange County, mainly south of Interstate 40. Several trees were blown down along a swath from Youngsville to Rolesville, including one large tree blown down across Highway 98 just northeast of Rolesville. Several trees were blown down along a swath from 4 miles northeast of the Raleigh-Durham International Airport to 2 miles northwest of Garner. Many of the trees fell across roadways, while one tree was blown down onto a fence.",
+        "The following events were reported: Hail. These occurred near station USW00013722, approximately 24.5325 km away, between 2017-07-28 17:30:00 and 2017-07-28 17:30:00. 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: Showers and thunderstorms developed ahead of a cold front approaching from the northwest. A couple of storms became severe and resulted in wind damage and large hail.\nEvent Narrative:",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 49.1263 km away, between 2017-08-17 15:30:00 and 2017-08-17 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 line of showers and thunderstorms associated with a short wave aloft moved through Central North Carolina in a moderately unstable environment. One storm produced a downburst, resulting in isolated wind damage.\nEvent Narrative: Several trees and a few large tree limbs were blown down along a swath through downtown Louisburg.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 30.8095 km away, between 2017-08-23 14:53:00 and 2017-08-23 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 10000.0 and crop damage of 0.0. \n\nEpisode Narrative: A strong cold front moved across central North Carolina during the evening into the overnight hours. Showers and storms developed in advance of the front along a prefrontal trough. Some of these storms became severe across eastern portions of central North Carolina, producing wind damage. One such report of damage resulted in an individual being injured from a large tree branch falling on a car, trapping and injuring the occupant.\nEvent Narrative: Trees were reported down near Rolesville and Zebulon.",
+        "The following events were reported: Flash Flood, Hail, Thunderstorm Wind. These occurred near station USW00013722, approximately 32.7474 km away, between 2017-09-01 15:45:00 and 2017-09-01 19:50:00. The events included records with hailstones measuring 28.61111111111111 inches.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 12017000.0 and crop damage of 0.0. \n\nEpisode Narrative: The remnants of Harvey increased the southwesterly flow over Central North Carolina as it moved northeastward through Tennessee and Kentucky. In the wake of the northward moving warm front, a cold front moved into and stalled over Central North Carolina providing lift in the strongly sheared, moist environment. The resulting thunderstorms became severe, producing damaging wind gusts, large hail and flash flooding. The remnants of Harvey increased the southwesterly flow over Central North Carolina as it moved northeastward through Tennessee and Kentucky. In the wake of the northward moving warm front, a cold front moved into and stalled over Central North Carolina providing lift in the strongly sheared, moist environment. The resulting thunderstorms became severe, producing damaging wind gusts, large hail and flash flooding. The remnants of Harvey increased the southwesterly flow over Central North Carolina as it moved northeastward through Tennessee and Kentucky. In the wake of the northward moving warm front, a cold front moved into and stalled over Central North Carolina providing lift in the strongly sheared, moist environment. The resulting thunderstorms became severe, producing damaging wind gusts, large hail and flash flooding. The remnants of Harvey increased the southwesterly flow over Central North Carolina as it moved northeastward through Tennessee and Kentucky. In the wake of the northward moving warm front, a cold front moved into and stalled over Central North Carolina providing lift in the strongly sheared, moist environment. The resulting thunderstorms became severe, producing damaging wind gusts, large hail and flash flooding. The remnants of Harvey increased the southwesterly flow over Central North Carolina as it moved northeastward through Tennessee and Kentucky. In the wake of the northward moving warm front, a cold front moved into and stalled over Central North Carolina providing lift in the strongly sheared, moist environment. The resulting thunderstorms became severe, producing damaging wind gusts, large hail and flash flooding. The remnants of Harvey increased the southwesterly flow over Central North Carolina as it moved northeastward through Tennessee and Kentucky. In the wake of the northward moving warm front, a cold front moved into and stalled over Central North Carolina providing lift in the strongly sheared, moist environment. The resulting thunderstorms became severe, producing damaging wind gusts, large hail and flash flooding. The remnants of Harvey increased the southwesterly flow over Central North Carolina as it moved northeastward through Tennessee and Kentucky. In the wake of the northward moving warm front, a cold front moved into and stalled over Central North Carolina providing lift in the strongly sheared, moist environment. The resulting thunderstorms became severe, producing damaging wind gusts, large hail and flash flooding. The remnants of Harvey increased the southwesterly flow over Central North Carolina as it moved northeastward through Tennessee and Kentucky. In the wake of the northward moving warm front, a cold front moved into and stalled over Central North Carolina providing lift in the strongly sheared, moist environment. The resulting thunderstorms became severe, producing damaging wind gusts, large hail and flash flooding. The remnants of Harvey increased the southwesterly flow over Central North Carolina as it moved northeastward through Tennessee and Kentucky. In the wake of the northward moving warm front, a cold front moved into and stalled over Central North Carolina providing lift in the strongly sheared, moist environment. The resulting thunderstorms became severe, producing damaging wind gusts, large hail and flash flooding. The remnants of Harvey increased the southwesterly flow over Central North Carolina as it moved northeastward through Tennessee and Kentucky. In the wake of the northward moving warm front, a cold front moved into and stalled over Central North Carolina providing lift in the strongly sheared, moist environment. The resulting thunderstorms became severe, producing damaging wind gusts, large hail and flash flooding. The remnants of Harvey increased the southwesterly flow over Central North Carolina as it moved northeastward through Tennessee and Kentucky. In the wake of the northward moving warm front, a cold front moved into and stalled over Central North Carolina providing lift in the strongly sheared, moist environment. The resulting thunderstorms became severe, producing damaging wind gusts, large hail and flash flooding.\nEvent Narrative: Heavy rain resulted in flash flooding on the US-1 Southbound ramp from NC-98. Numerous trees were blown down across northern portions of Harnett County. One tree was blown down onto Raws Church Road, blocking the road. One tree was blown down onto a roadway approximately 4 miles east-northeast of Angier. Multiple trees were blown down onto power lines and equipment. Multiple trees were blown down onto a power line and power equipment. Hail up to 1 inch in diameter fell on Feldman Drive south-southwest of Garner.  Heavy rain resulted in flash flooding in Clayton. The right lane of Route 70 near Champion Drive was impassable. A trained spotter 3 miles west of Clayton also measured 4.14 inches of rain in an hour and a half. Hail up to 2.75 inches fell across northern Harnett County. Property damage values have been estimated. Hail up to 2.75 inches in diameter fell along a swath from 2 miles west-southwest of Fuquay-Varina to 3 miles north of Angier. Multiple trees were also blown down along the swath. Damage estimates have been estimated.",
+        "The following events were reported: Flash Flood, Thunderstorm Wind, Tornado. These occurred near station USW00013722, approximately 32.1438 km away, between 2018-04-15 17:15:00 and 2018-04-15 22:15:00.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 167000.0 and crop damage of 0.0. \n\nEpisode Narrative: A strong upper low moved from Iowa across the Lower Great Lakes region, with a deep trough taking on a negative tilt while swinging into North Carolina. An associated strong cold front approached western North Carolina that afternoon and pushed east and east-northeast across central North Carolina on the night of the 15th. A strengthening and backing flow at all levels led to a surge of moisture into NC. Moderate instability, strong deep layer shear, and high low-level storm-relative helicity were also present. The result was a quasi-linear convective system with embedded mesovortices, which produced widespread severe weather, including a tornado in Greensboro, as it moved through North Carolina. A strong upper low moved from Iowa across the Lower Great Lakes region, with a deep trough taking on a negative tilt while swinging into North Carolina. An associated strong cold front approached western North Carolina that afternoon and pushed east and east-northeast across central North Carolina on the night of the 15th. A strengthening and backing flow at all levels led to a surge of moisture into NC. Moderate instability, strong deep layer shear, and high low-level storm-relative helicity were also present. The result was a quasi-linear convective system with embedded mesovortices, which produced widespread severe weather, including a tornado in Greensboro, as it moved through North Carolina. A strong upper low moved from Iowa across the Lower Great Lakes region, with a deep trough taking on a negative tilt while swinging into North Carolina. An associated strong cold front approached western North Carolina that afternoon and pushed east and east-northeast across central North Carolina on the night of the 15th. A strengthening and backing flow at all levels led to a surge of moisture into NC. Moderate instability, strong deep layer shear, and high low-level storm-relative helicity were also present. The result was a quasi-linear convective system with embedded mesovortices, which produced widespread severe weather, including a tornado in Greensboro, as it moved through North Carolina. A strong upper low moved from Iowa across the Lower Great Lakes region, with a deep trough taking on a negative tilt while swinging into North Carolina. An associated strong cold front approached western North Carolina that afternoon and pushed east and east-northeast across central North Carolina on the night of the 15th. A strengthening and backing flow at all levels led to a surge of moisture into NC. Moderate instability, strong deep layer shear, and high low-level storm-relative helicity were also present. The result was a quasi-linear convective system with embedded mesovortices, which produced widespread severe weather, including a tornado in Greensboro, as it moved through North Carolina. A strong upper low moved from Iowa across the Lower Great Lakes region, with a deep trough taking on a negative tilt while swinging into North Carolina. An associated strong cold front approached western North Carolina that afternoon and pushed east and east-northeast across central North Carolina on the night of the 15th. A strengthening and backing flow at all levels led to a surge of moisture into NC. Moderate instability, strong deep layer shear, and high low-level storm-relative helicity were also present. The result was a quasi-linear convective system with embedded mesovortices, which produced widespread severe weather, including a tornado in Greensboro, as it moved through North Carolina. A strong upper low moved from Iowa across the Lower Great Lakes region, with a deep trough taking on a negative tilt while swinging into North Carolina. An associated strong cold front approached western North Carolina that afternoon and pushed east and east-northeast across central North Carolina on the night of the 15th. A strengthening and backing flow at all levels led to a surge of moisture into NC. Moderate instability, strong deep layer shear, and high low-level storm-relative helicity were also present. The result was a quasi-linear convective system with embedded mesovortices, which produced widespread severe weather, including a tornado in Greensboro, as it moved through North Carolina. A strong upper low moved from Iowa across the Lower Great Lakes region, with a deep trough taking on a negative tilt while swinging into North Carolina. An associated strong cold front approached western North Carolina that afternoon and pushed east and east-northeast across central North Carolina on the night of the 15th. A strengthening and backing flow at all levels led to a surge of moisture into NC. Moderate instability, strong deep layer shear, and high low-level storm-relative helicity were also present. The result was a quasi-linear convective system with embedded mesovortices, which produced widespread severe weather, including a tornado in Greensboro, as it moved through North Carolina. A strong upper low moved from Iowa across the Lower Great Lakes region, with a deep trough taking on a negative tilt while swinging into North Carolina. An associated strong cold front approached western North Carolina that afternoon and pushed east and east-northeast across central North Carolina on the night of the 15th. A strengthening and backing flow at all levels led to a surge of moisture into NC. Moderate instability, strong deep layer shear, and high low-level storm-relative helicity were also present. The result was a quasi-linear convective system with embedded mesovortices, which produced widespread severe weather, including a tornado in Greensboro, as it moved through North Carolina. A strong upper low moved from Iowa across the Lower Great Lakes region, with a deep trough taking on a negative tilt while swinging into North Carolina. An associated strong cold front approached western North Carolina that afternoon and pushed east and east-northeast across central North Carolina on the night of the 15th. A strengthening and backing flow at all levels led to a surge of moisture into NC. Moderate instability, strong deep layer shear, and high low-level storm-relative helicity were also present. The result was a quasi-linear convective system with embedded mesovortices, which produced widespread severe weather, including a tornado in Greensboro, as it moved through North Carolina. A strong upper low moved from Iowa across the Lower Great Lakes region, with a deep trough taking on a negative tilt while swinging into North Carolina. An associated strong cold front approached western North Carolina that afternoon and pushed east and east-northeast across central North Carolina on the night of the 15th. A strengthening and backing flow at all levels led to a surge of moisture into NC. Moderate instability, strong deep layer shear, and high low-level storm-relative helicity were also present. The result was a quasi-linear convective system with embedded mesovortices, which produced widespread severe weather, including a tornado in Greensboro, as it moved through North Carolina. A strong upper low moved from Iowa across the Lower Great Lakes region, with a deep trough taking on a negative tilt while swinging into North Carolina. An associated strong cold front approached western North Carolina that afternoon and pushed east and east-northeast across central North Carolina on the night of the 15th. A strengthening and backing flow at all levels led to a surge of moisture into NC. Moderate instability, strong deep layer shear, and high low-level storm-relative helicity were also present. The result was a quasi-linear convective system with embedded mesovortices, which produced widespread severe weather, including a tornado in Greensboro, as it moved through North Carolina.\nEvent Narrative: One tree was blown down across Farrington Road. One tree was blown down across Thompson Avenue. One tree was blown down near the intersection of NC Highway 86 and Carr Store Road. One tree was blown down on River Forks Drive near NC-87. Several trees and power lines were blown down along a swath from Willow Springs to Rolesville. Flash Flooding cased the closure of several roads in the Durham area. An  EF-1  tornado briefly touched down approximately 5 miles north-northwest of Wendell, North Carolina on April 15, 2018.  | |The tornado touched down near Hals Farm Road, just off of Edgemont  |Road. The tornado tracked northward across an area consisting of a  |mixture of trees, a barn, and a few homes, before crossing Sadie  |Drive. The homes near the end of Sadie drive (near the cul-de-sac)  |sustained minor damage to siding and some loss/damage to shingles.  |Numerous trees were uprooted and several pine trees snapped off  |approximately 15 to 25 feet up. An apparent outbuilding was also  |destroyed at this location. The damage here was indicative of a weak  |tornado with approximate peak wind speeds of 87 MPH, or EF-1 on the  |Enhanced Fujita Scale.  | |The tornado continued tracking northward through a wooded area  |causing sporadic damage to trees. The tornado affected several homes  |along Woodie Drive, off of Riley Hill Road, with one sustaining  |significant damage from a tree falling through the roof of the home.  |The tornado then lifted near Riley Hill Road. One tree was blown down across West Poplar Road. Multiple trees were blown down in Hurdle Mills. Flash flooding was reported on Mangum Street at the Durham Freeway. Flash flooding was reported on United State highways 15 and 501 and along Gregson Street at Interstate 85.",
+        "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00013722, approximately 33.3074 km away, between 2018-05-10 16:25:00 and 2018-05-10 19:30:00. The events included records with hailstones measuring 30.65 inches.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: Central North Carolina was on the southern periphery of an increasingly sheared shortwave as it progressed eastward into New England and the Northeast United States. The attendant weak front crossed the area late in the afternoon and evening, with just enough CAPE/Shear to allow for loosely organized multi-cellular thunderstorms. Several of the storms produced severe wind gusts and large hail. Central North Carolina was on the southern periphery of an increasingly sheared shortwave as it progressed eastward into New England and the Northeast United States. The attendant weak front crossed the area late in the afternoon and evening, with just enough CAPE/Shear to allow for loosely organized multi-cellular thunderstorms. Several of the storms produced severe wind gusts and large hail. Central North Carolina was on the southern periphery of an increasingly sheared shortwave as it progressed eastward into New England and the Northeast United States. The attendant weak front crossed the area late in the afternoon and evening, with just enough CAPE/Shear to allow for loosely organized multi-cellular thunderstorms. Several of the storms produced severe wind gusts and large hail. Central North Carolina was on the southern periphery of an increasingly sheared shortwave as it progressed eastward into New England and the Northeast United States. The attendant weak front crossed the area late in the afternoon and evening, with just enough CAPE/Shear to allow for loosely organized multi-cellular thunderstorms. Several of the storms produced severe wind gusts and large hail. Central North Carolina was on the southern periphery of an increasingly sheared shortwave as it progressed eastward into New England and the Northeast United States. The attendant weak front crossed the area late in the afternoon and evening, with just enough CAPE/Shear to allow for loosely organized multi-cellular thunderstorms. Several of the storms produced severe wind gusts and large hail.\nEvent Narrative:  Ping pong ball size hail fell near the intersection of Rose Of Sharon Road and Golden Heather Drive and resulted in damage to vehicles and trees. Numerous trees were blown down within the community of Louisburg. Numerous trees were blown down along a swath from Siler City to Pittsboro. One tree was blown down in a cemetery near the intersection of Lake Wheeler Road and Inwood Road.",
+        "The following events were reported: Flash Flood, Hail, Thunderstorm Wind. These occurred near station USW00013722, approximately 21.8503 km away, between 2018-05-21 14:26:00 and 2018-05-22 01:40:00. The events included records with hailstones measuring 13.0625 inches.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 602000.0 and crop damage of 0.0. \n\nEpisode Narrative: An outflow-augmented back-door cold front, served as the foci for a slow northeast to southwest moving cluster of storms and torrential rainfall across the northern Piedmont and northern Coastal Plain counties. The heaviest rainfall of 3 to 5 inches fell across North Raleigh, which caused Crabtree Creek to flood. Multiple road closures were reported in northwest Raleigh and several cars were stranded in a flooded road. An outflow-augmented back-door cold front, served as the foci for a slow northeast to southwest moving cluster of storms and torrential rainfall across the northern Piedmont and northern Coastal Plain counties. The heaviest rainfall of 3 to 5 inches fell across North Raleigh, which caused Crabtree Creek to flood. Multiple road closures were reported in northwest Raleigh and several cars were stranded in a flooded road. An outflow-augmented back-door cold front, served as the foci for a slow northeast to southwest moving cluster of storms and torrential rainfall across the northern Piedmont and northern Coastal Plain counties. The heaviest rainfall of 3 to 5 inches fell across North Raleigh, which caused Crabtree Creek to flood. Multiple road closures were reported in northwest Raleigh and several cars were stranded in a flooded road. An outflow-augmented back-door cold front, served as the foci for a slow northeast to southwest moving cluster of storms and torrential rainfall across the northern Piedmont and northern Coastal Plain counties. The heaviest rainfall of 3 to 5 inches fell across North Raleigh, which caused Crabtree Creek to flood. Multiple road closures were reported in northwest Raleigh and several cars were stranded in a flooded road. An outflow-augmented back-door cold front, served as the foci for a slow northeast to southwest moving cluster of storms and torrential rainfall across the northern Piedmont and northern Coastal Plain counties. The heaviest rainfall of 3 to 5 inches fell across North Raleigh, which caused Crabtree Creek to flood. Multiple road closures were reported in northwest Raleigh and several cars were stranded in a flooded road.\nEvent Narrative: Dime sized hail reported at UNC Chapel Hill Medical Center.   Two trees were blown down along a swath from Sunrise Road to Greenwood Road in Chapel Hill. Several roads were closed in northwest Raleigh, many in the vicinity of Crabtree Valley Mall and Crabtree Creek, due to flash flooding. Newton Road near Six Forks Road washed out and collapsed. Several cars were stranded in flood water near the intersection of Leesville Road and Millbrook Road. Several cars were underwater at the Crabtree Valley Mall due to flooding along Crabtree Creek overflowing its banks into the parking garage.",
+        "The following events were reported: Hail. These occurred near station USW00013722, approximately 29.3121 km away, between 2018-05-23 15:40:00 and 2018-05-23 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 to numerous showers and thunderstorms developed in a moist and unstable air mass ahead of a slow moving cold front during the afternoon and evening. The strongest storms produced marginally severe hail, gusty winds and excessive lightning. Two slow moving, multi-cellular clusters of storms in the western Piedmont resulted in flash flooding when 2 to 3 inches of rain fell in less than an hour.\nEvent Narrative: Hail was reported at The Preserve Golf Club.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 17.6936 km away, between 2018-06-10 22:40:00 and 2018-06-10 23:25:00. 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 29000.0 and crop damage of 0.0. \n\nEpisode Narrative: Convection blossomed strongly near the intersection of a southward moving outflow boundary and a similar eastward moving boundary. The convection moved east along the boundary, with one cluster of storms becoming severe, producing a swath of wind damage from Orange county to Wake county. Convection blossomed strongly near the intersection of a southward moving outflow boundary and a similar eastward moving boundary. The convection moved east along the boundary, with one cluster of storms becoming severe, producing a swath of wind damage from Orange county to Wake county. Convection blossomed strongly near the intersection of a southward moving outflow boundary and a similar eastward moving boundary. The convection moved east along the boundary, with one cluster of storms becoming severe, producing a swath of wind damage from Orange county to Wake county. Convection blossomed strongly near the intersection of a southward moving outflow boundary and a similar eastward moving boundary. The convection moved east along the boundary, with one cluster of storms becoming severe, producing a swath of wind damage from Orange county to Wake county.\nEvent Narrative: Several trees were blown down along a swath from Carrboro to Chapel Hill. Two of the trees fell on residences, one at 123 Priestly Creek Drive and the other at 115 Bruton Drive. Power lines were blown down approximately 4 miles west-northwest of Durham. One tree was snapped by thunderstorm winds in a homeowner's yard along Monarch Way. A couple of trees were blown down along a swath from the Shinleaf Campground at Falls Lake to Old Highway 98.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 46.0813 km away, between 2018-06-11 16:06:00 and 2018-06-11 16:06:00. 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: Outflow from previous night's convection was stalled over the southeast third of NC, roughly from Camp Lejeune to Florence, SC. Meanwhile a surface cold front was drifting southward out of southern VA into NC. Thunderstorms erupted along this outflow by early afternoon. Outflows from these storms caused others to develop. The stronger cells produced quarter size hail along with isolated wind damage.\nEvent Narrative: Several trees were blown down along a 150 foot section of roadway on Olive Branch Road near Kipling Road.",
+        "The following events were reported: Lightning, Thunderstorm Wind. These occurred near station USW00013722, approximately 43.4153 km away, between 2018-06-20 16:01:00 and 2018-06-20 17:50:00.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 84000.0 and crop damage of 0.0. \n\nEpisode Narrative: Isolated pulse severe storms developed near the Piedmont trough at mid-afternoon. These storms formed into clusters as they moved east-southeast. The strongest and isolated severe storms affected Moore, Lee, Harnett, Johnston, Wilson, Franklin, Nash, and Edgecombe Counties. There were frequent CG strikes that affected Harnett, Johnston, and eastern Wake Counties as well, with some house fires reported. Isolated pulse severe storms developed near the Piedmont trough at mid-afternoon. These storms formed into clusters as they moved east-southeast. The strongest and isolated severe storms affected Moore, Lee, Harnett, Johnston, Wilson, Franklin, Nash, and Edgecombe Counties. There were frequent CG strikes that affected Harnett, Johnston, and eastern Wake Counties as well, with some house fires reported. Isolated pulse severe storms developed near the Piedmont trough at mid-afternoon. These storms formed into clusters as they moved east-southeast. The strongest and isolated severe storms affected Moore, Lee, Harnett, Johnston, Wilson, Franklin, Nash, and Edgecombe Counties. There were frequent CG strikes that affected Harnett, Johnston, and eastern Wake Counties as well, with some house fires reported. Isolated pulse severe storms developed near the Piedmont trough at mid-afternoon. These storms formed into clusters as they moved east-southeast. The strongest and isolated severe storms affected Moore, Lee, Harnett, Johnston, Wilson, Franklin, Nash, and Edgecombe Counties. There were frequent CG strikes that affected Harnett, Johnston, and eastern Wake Counties as well, with some house fires reported.\nEvent Narrative: Several trees were reported uprooted near Raven Rock State Park. Substantial crop damage was reported in the Bunn area due to severe winds and large hail. Lightning struck a home on Amberly Court and North Carolina Highway 50, resulting in a house fire. Lightning struck a home on off of Old Drug Store Road, resulting in a house fire.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 26.1487 km away, between 2018-06-24 14:45:00 and 2018-06-24 20:05:00. 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 9000.0 and crop damage of 0.0. \n\nEpisode Narrative: A boundary observed on radar late that morning was the focus for initial convective development around early afternoon across Harnett and western Johnston Counties. A mid level inversion capped the atmosphere initially across the western and northern Piedmont but this cap was broken around sunset, permitting isolated severe thunderstorms to develop between the Triad and the Triangle regions. A boundary observed on radar late that morning was the focus for initial convective development around early afternoon across Harnett and western Johnston Counties. A mid level inversion capped the atmosphere initially across the western and northern Piedmont but this cap was broken around sunset, permitting isolated severe thunderstorms to develop between the Triad and the Triangle regions. A boundary observed on radar late that morning was the focus for initial convective development around early afternoon across Harnett and western Johnston Counties. A mid level inversion capped the atmosphere initially across the western and northern Piedmont but this cap was broken around sunset, permitting isolated severe thunderstorms to develop between the Triad and the Triangle regions. A boundary observed on radar late that morning was the focus for initial convective development around early afternoon across Harnett and western Johnston Counties. A mid level inversion capped the atmosphere initially across the western and northern Piedmont but this cap was broken around sunset, permitting isolated severe thunderstorms to develop between the Triad and the Triangle regions.\nEvent Narrative: One tree was reported down on shoulder of Ballard Road. Several trees were reported down on roads, including Ruth Street, Redwood Road and Geer Street. One tree was reported down and blocking part of Highway 751. Trees were reported down on power lines.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 27.6764 km away, between 2018-07-04 18:17:00 and 2018-07-04 18:24:00. 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 weak westward moving mid level shear axis was a focus for the development of a broken band of showers and storms. A few of these storms became strong to severe and produced isolated wind damage. A weak westward moving mid level shear axis was a focus for the development of a broken band of showers and storms. A few of these storms became strong to severe and produced isolated wind damage. A weak westward moving mid level shear axis was a focus for the development of a broken band of showers and storms. A few of these storms became strong to severe and produced isolated wind damage. A weak westward moving mid level shear axis was a focus for the development of a broken band of showers and storms. A few of these storms became strong to severe and produced isolated wind damage.\nEvent Narrative: One tree was reported down along Erwin Road. One tree and a power line was reported down near the intersection of Dodson Crossroads and North Carolina Route 54. A couple of trees were reported down along North Carolina Route 54. One tree was reported down along Camille Court.",
+        "The following events were reported: Flash Flood, Lightning. These occurred near station USW00013722, approximately 9.5985 km away, between 2018-07-05 17:30:00 and 2018-07-05 19:30:00.The events resulted in 1 injuries and 0 fatalities. No significant property or crop damage was reported. \n\nEpisode Narrative: An inverted trough axis initiated early afternoon showers and storms along the NC coast which pushed inland thanks to weak onshore flow aloft. Aided and propagated by cold pool progression, a few of these storms became strong, producing heavy rainfall and flooding, along with frequent lightning strikes before dying off rapidly after sunset. An inverted trough axis initiated early afternoon showers and storms along the NC coast which pushed inland thanks to weak onshore flow aloft. Aided and propagated by cold pool progression, a few of these storms became strong, producing heavy rainfall and flooding, along with frequent lightning strikes before dying off rapidly after sunset.\nEvent Narrative: Chapel Hill Road was closed near the intersection of North Carolina Highway 54 due to flooding. A 74 year old male was struck by lightning and injured at the Fairfield Swim and Tennis Club. The individual was seeking shelter from the storm under a tree and under his umbrella. The tree was also damage and the umbrella was left in tatters.",
+        "The following events were reported: Flash Flood, Thunderstorm Wind. These occurred near station USW00013722, approximately 28.816 km away, between 2018-07-06 14:50:00 and 2018-07-06 16:50:00.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 39000.0 and crop damage of 0.0. \n\nEpisode Narrative: Storms initiated in split upper level flow along a prefrontal trough. Mean 850 MB to 300 MB winds were near calm at the time with storm propagation mainly cold pool driven. The primary impacts from these storms were gusty winds, resulting in trees down, and heavy rain. One storm did become anchored over Raleigh which prompted a flash flood warning. Storms initiated in split upper level flow along a prefrontal trough. Mean 850 MB to 300 MB winds were near calm at the time with storm propagation mainly cold pool driven. The primary impacts from these storms were gusty winds, resulting in trees down, and heavy rain. One storm did become anchored over Raleigh which prompted a flash flood warning. Storms initiated in split upper level flow along a prefrontal trough. Mean 850 MB to 300 MB winds were near calm at the time with storm propagation mainly cold pool driven. The primary impacts from these storms were gusty winds, resulting in trees down, and heavy rain. One storm did become anchored over Raleigh which prompted a flash flood warning. Storms initiated in split upper level flow along a prefrontal trough. Mean 850 MB to 300 MB winds were near calm at the time with storm propagation mainly cold pool driven. The primary impacts from these storms were gusty winds, resulting in trees down, and heavy rain. One storm did become anchored over Raleigh which prompted a flash flood warning. Storms initiated in split upper level flow along a prefrontal trough. Mean 850 MB to 300 MB winds were near calm at the time with storm propagation mainly cold pool driven. The primary impacts from these storms were gusty winds, resulting in trees down, and heavy rain. One storm did become anchored over Raleigh which prompted a flash flood warning. Storms initiated in split upper level flow along a prefrontal trough. Mean 850 MB to 300 MB winds were near calm at the time with storm propagation mainly cold pool driven. The primary impacts from these storms were gusty winds, resulting in trees down, and heavy rain. One storm did become anchored over Raleigh which prompted a flash flood warning. Storms initiated in split upper level flow along a prefrontal trough. Mean 850 MB to 300 MB winds were near calm at the time with storm propagation mainly cold pool driven. The primary impacts from these storms were gusty winds, resulting in trees down, and heavy rain. One storm did become anchored over Raleigh which prompted a flash flood warning. Storms initiated in split upper level flow along a prefrontal trough. Mean 850 MB to 300 MB winds were near calm at the time with storm propagation mainly cold pool driven. The primary impacts from these storms were gusty winds, resulting in trees down, and heavy rain. One storm did become anchored over Raleigh which prompted a flash flood warning. Storms initiated in split upper level flow along a prefrontal trough. Mean 850 MB to 300 MB winds were near calm at the time with storm propagation mainly cold pool driven. The primary impacts from these storms were gusty winds, resulting in trees down, and heavy rain. One storm did become anchored over Raleigh which prompted a flash flood warning. Storms initiated in split upper level flow along a prefrontal trough. Mean 850 MB to 300 MB winds were near calm at the time with storm propagation mainly cold pool driven. The primary impacts from these storms were gusty winds, resulting in trees down, and heavy rain. One storm did become anchored over Raleigh which prompted a flash flood warning.\nEvent Narrative: Trees were reported down on power lines. Trees were reported down on power lines. Numerous large tree limbs and four trees were reported down on Chambers Road near Highway 501. Multiple trees were reported down near the Durham Person County Line. Trees and power lines were reported down at the intersection of Moores Mill Road and Rassie Crabtree Road. Flooding was reported along North Raleigh Boulevard near Millbank Street, along with a car stuck in the flood waters, resulting in a water rescue. High water was reported on Peace Street and Capitol Boulevard. Atlantic Avenue at Hodges was closed due to flooding. A tree and power line were reported down at Elland Cedar Grove Road and Carr Store Road. A couple of trees were reported down on North Carolina Highway 86, one at Holman Drive and another on Highway 70.",
+        "The following events were reported: Flash Flood. These occurred near station USW00013722, approximately 25.6836 km away, between 2018-07-07 08:15:00 and 2018-07-07 13:00:00.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: The leading edge of cool air nosing down the coast caused widespread, mainly stratiform rain which was slow moving and producing rainfall rates greater than one inch per hour for several hours. The front nearly stalled across Wake County during the morning, with a heavy rain focus south of Raleigh down into northern Harnett county. Radar estimated fairly extensive 2 to 3.35 inches of rainfall. This resulted in a couple of flash flooding reports. The leading edge of cool air nosing down the coast caused widespread, mainly stratiform rain which was slow moving and producing rainfall rates greater than one inch per hour for several hours. The front nearly stalled across Wake County during the morning, with a heavy rain focus south of Raleigh down into northern Harnett county. Radar estimated fairly extensive 2 to 3.35 inches of rainfall. This resulted in a couple of flash flooding reports.\nEvent Narrative: Banks Road and Ten Ten Road were reported to be flooded. Flash Flooding was reported along Gideon Creek Way near the intersection of Durham Drive. One vehicle became stalled in the flood waters, prompting a water rescue.",
+        "The following events were reported: Flash Flood. These occurred near station USW00013722, approximately 49.2243 km away, between 2018-07-17 20:43:00 and 2018-07-17 21:45:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A slow moving cold front lagged over West Virginia and Virginia through late afternoon, with a prefrontal trough over central NC. Scattered clusters of storms developed during the mid afternoon, with a couple becoming severe and producing wind damage, along with one producing flash flooding.\nEvent Narrative: Flooding was reported at 401 North at Christian Light Road.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 36.3306 km away, between 2018-07-21 22:06:00 and 2018-07-21 22:50:00. 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: Multiple disturbances rotating around an upper-level low across the Ohio Valley produced multiple clusters of showers and storms across central NC during the late evening and  overnight hours. Convection congealed into an MCS-like complex and pushed east during the overnight hours which produced some isolated wind damage and pockets of heavy rainfall which produced flash flooding. Multiple disturbances rotating around an upper-level low across the Ohio Valley produced multiple clusters of showers and storms across central NC during the late evening and  overnight hours. Convection congealed into an MCS-like complex and pushed east during the overnight hours which produced some isolated wind damage and pockets of heavy rainfall which produced flash flooding. Multiple disturbances rotating around an upper-level low across the Ohio Valley produced multiple clusters of showers and storms across central NC during the late evening and  overnight hours. Convection congealed into an MCS-like complex and pushed east during the overnight hours which produced some isolated wind damage and pockets of heavy rainfall which produced flash flooding. Multiple disturbances rotating around an upper-level low across the Ohio Valley produced multiple clusters of showers and storms across central NC during the late evening and  overnight hours. Convection congealed into an MCS-like complex and pushed east during the overnight hours which produced some isolated wind damage and pockets of heavy rainfall which produced flash flooding.\nEvent Narrative: Trees were reported down along Kennebec Church Road. Multiple trees were blown down near NC Highway 42. One tree was reported down near the intersection of Fanny Brown Road and Banks Road. One tree was blown down near the intersection of Washington and Wall Streets.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 31.1424 km away, between 2018-07-22 20:05:00 and 2018-07-22 20:42:00. 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 stationary surface low over western North Carolina, and a pair of outflow modulated fronts over North Carolina and Virginia, were overspread by perturbed south southwesterly flow around an anomalous mid to upper low over the Ohio Valley. Loosely organized multi clusters resulted, with accompanying marginally severe hail, wind damage, and isolated flooding. A stationary surface low over western North Carolina, and a pair of outflow modulated fronts over North Carolina and Virginia, were overspread by perturbed south southwesterly flow around an anomalous mid to upper low over the Ohio Valley. Loosely organized multi clusters resulted, with accompanying marginally severe hail, wind damage, and isolated flooding.\nEvent Narrative: Trees were reported down on Green Street. Multiple trees and power lines were reported down near the intersection of Surl Mount Tirzah Road and Helena Moriah Road.",
+        "The following events were reported: Lightning, Thunderstorm Wind. These occurred near station USW00013722, approximately 35.8303 km away, between 2018-07-28 13:30:00 and 2018-07-28 17:58:00.The events resulted in 1 injuries and 1 fatalities. The events caused property damage valued at 2000.0 and crop damage of 0.0. \n\nEpisode Narrative: A quasi-stationary front, bisecting central NC, provided a focus point for scattered to numerous showers and thunderstorms. Thanks to a moist and unstable airmass, a few of these storms breached the severe limit, resulting in isolated wind damage, and localized flash flooding. A quasi-stationary front, bisecting central NC, provided a focus point for scattered to numerous showers and thunderstorms. Thanks to a moist and unstable airmass, a few of these storms breached the severe limit, resulting in isolated wind damage, and localized flash flooding. A quasi-stationary front, bisecting central NC, provided a focus point for scattered to numerous showers and thunderstorms. Thanks to a moist and unstable airmass, a few of these storms breached the severe limit, resulting in isolated wind damage, and localized flash flooding. A quasi-stationary front, bisecting central NC, provided a focus point for scattered to numerous showers and thunderstorms. Thanks to a moist and unstable airmass, a few of these storms breached the severe limit, resulting in isolated wind damage, and localized flash flooding. A quasi-stationary front, bisecting central NC, provided a focus point for scattered to numerous showers and thunderstorms. Thanks to a moist and unstable airmass, a few of these storms breached the severe limit, resulting in isolated wind damage, and localized flash flooding.\nEvent Narrative: A 41 year old male was struck by lightning and was taken to the hospital to be treated for his injuries.   The victim subsequently passed away from his injuries. Tree down across roadway at Wendell Boulevard and Industrial Drive. Tree reported down on power-line at Wendell Boulevard and Rolesville Road. One tree was blown down along Wendell Boulevard and N Oakwood Avenue. Numerous trees and power-lines were blown down throughout the city limits of Wendell.",
+        "The following events were reported: Flash Flood, Thunderstorm Wind. These occurred near station USW00013722, approximately 25.5328 km away, between 2018-08-02 14:12:00 and 2018-08-02 17:25:00.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 113000.0 and crop damage of 0.0. \n\nEpisode Narrative: Heavy rain showers and thunderstorms developed over central NC in association with a series of disturbances moving through the long wave trough aloft. Deep moist advection and unidirectional flow through the atmosphere resulted in training of heavy rain and thunderstorms. Saturated antecedent conditions contributed to the flash flooding that occurred as a result of the training storms. A cluster of storms became severe during the afternoon, resulting in sporadic downed trees and power lines while other marginally severe storms resulted in numerous downed trees and power lines due to saturated ground. Heavy rain showers and thunderstorms developed over central NC in association with a series of disturbances moving through the long wave trough aloft. Deep moist advection and unidirectional flow through the atmosphere resulted in training of heavy rain and thunderstorms. Saturated antecedent conditions contributed to the flash flooding that occurred as a result of the training storms. A cluster of storms became severe during the afternoon, resulting in sporadic downed trees and power lines while other marginally severe storms resulted in numerous downed trees and power lines due to saturated ground. Heavy rain showers and thunderstorms developed over central NC in association with a series of disturbances moving through the long wave trough aloft. Deep moist advection and unidirectional flow through the atmosphere resulted in training of heavy rain and thunderstorms. Saturated antecedent conditions contributed to the flash flooding that occurred as a result of the training storms. A cluster of storms became severe during the afternoon, resulting in sporadic downed trees and power lines while other marginally severe storms resulted in numerous downed trees and power lines due to saturated ground. Heavy rain showers and thunderstorms developed over central NC in association with a series of disturbances moving through the long wave trough aloft. Deep moist advection and unidirectional flow through the atmosphere resulted in training of heavy rain and thunderstorms. Saturated antecedent conditions contributed to the flash flooding that occurred as a result of the training storms. A cluster of storms became severe during the afternoon, resulting in sporadic downed trees and power lines while other marginally severe storms resulted in numerous downed trees and power lines due to saturated ground. Heavy rain showers and thunderstorms developed over central NC in association with a series of disturbances moving through the long wave trough aloft. Deep moist advection and unidirectional flow through the atmosphere resulted in training of heavy rain and thunderstorms. Saturated antecedent conditions contributed to the flash flooding that occurred as a result of the training storms. A cluster of storms became severe during the afternoon, resulting in sporadic downed trees and power lines while other marginally severe storms resulted in numerous downed trees and power lines due to saturated ground.\nEvent Narrative: Heavy rainfall resulted in flash flooding throughout the the Pittsboro business district. Several streets were closed due to flash flooding throughout the city of Durham, including sections of Roxboro Street and Lumley Road. Several trees were blown down along a swath through Apex, including one on a car along Olive Chapel Road. A couple of trees were blown down along a swath from Sugar Lake Road to near the intersection of Bynum Road and Hearne Road. One tree was blown down at the intersection of South Roxboro Street and Vistawood Way.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 21.8886 km away, between 2018-08-03 14:12:00 and 2018-08-03 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 1500.0 and crop damage of 0.0. \n\nEpisode Narrative: A persistent plume of tropical moisture and embedded perturbations aloft triggered clusters of convection with torrential downpours. Since the wind field was fairly unidirectional, training cells lead to locally excessive rainfall and flash flooding, along with isolated wind damage. A persistent plume of tropical moisture and embedded perturbations aloft triggered clusters of convection with torrential downpours. Since the wind field was fairly unidirectional, training cells lead to locally excessive rainfall and flash flooding, along with isolated wind damage. A persistent plume of tropical moisture and embedded perturbations aloft triggered clusters of convection with torrential downpours. Since the wind field was fairly unidirectional, training cells lead to locally excessive rainfall and flash flooding, along with isolated wind damage. A persistent plume of tropical moisture and embedded perturbations aloft triggered clusters of convection with torrential downpours. Since the wind field was fairly unidirectional, training cells lead to locally excessive rainfall and flash flooding, along with isolated wind damage. A persistent plume of tropical moisture and embedded perturbations aloft triggered clusters of convection with torrential downpours. Since the wind field was fairly unidirectional, training cells lead to locally excessive rainfall and flash flooding, along with isolated wind damage.\nEvent Narrative: Power lines were reported down in the 3800 block of Air Park Road. One tree was reported down on Optimist Farm Road at Bostian Drive. One tree was reported down at Slater Road and Carrington Mill Boulevard. One tree was reported down at New Bern Avenue and King William Road. One tree was reported down at Hodge Road and Knightdale Boulevard.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 48.2183 km away, between 2018-08-06 15:18:00 and 2018-08-06 15:18:00. 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 1500.0 and crop damage of 0.0. \n\nEpisode Narrative: Showers and thunderstorms developed along a lee side surface trough across central North Carolina. The storms intensified as a weak mid level shortwave disturbance approached the area from the west in the late afternoon and early evening hours. Some of these storms became severe and produced wind damage.\nEvent Narrative: Two trees were reported down at the intersection of Highway 210 and Berea Chruch Road.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 39.4336 km away, between 2018-08-07 19:00:00 and 2018-08-07 19:59:00. 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 5000.0 and crop damage of 0.0. \n\nEpisode Narrative: Thunderstorms developed along a lee trough axis and were further enhanced by a sea breeze moving inland. Some of these storms became strong to severe producing wind damage. Thunderstorms developed along a lee trough axis and were further enhanced by a sea breeze moving inland. Some of these storms became strong to severe producing wind damage. Thunderstorms developed along a lee trough axis and were further enhanced by a sea breeze moving inland. Some of these storms became strong to severe producing wind damage.\nEvent Narrative: One tree was reported down at Saint Marys Road and Miller Road. One tree was reported down on East King Street and South Cameron Street. The tree downed power lines. A tree was reported down on Hillsboro Street.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 35.2254 km away, between 2018-08-08 16:09:00 and 2018-08-08 17:43:00. 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 remnant MCV helped to initiate a broken band of thunderstorms that moved east  across central North Carolina during the afternoon and late evening hours. The band of storms organized into a fairly large bowing cluster as it crossed the area, downing numerous trees across Central NC. A remnant MCV helped to initiate a broken band of thunderstorms that moved east  across central North Carolina during the afternoon and late evening hours. The band of storms organized into a fairly large bowing cluster as it crossed the area, downing numerous trees across Central NC. A remnant MCV helped to initiate a broken band of thunderstorms that moved east  across central North Carolina during the afternoon and late evening hours. The band of storms organized into a fairly large bowing cluster as it crossed the area, downing numerous trees across Central NC. A remnant MCV helped to initiate a broken band of thunderstorms that moved east  across central North Carolina during the afternoon and late evening hours. The band of storms organized into a fairly large bowing cluster as it crossed the area, downing numerous trees across Central NC. A remnant MCV helped to initiate a broken band of thunderstorms that moved east  across central North Carolina during the afternoon and late evening hours. The band of storms organized into a fairly large bowing cluster as it crossed the area, downing numerous trees across Central NC.\nEvent Narrative: One down tree was blocking the intersection at NC Highway 87 and Chicken Bridge Road. Trees were reported down on power-lines near the intersection of Holly Springs Road and Sunset Lake Road. One tree and power-line was blown down near the intersection of Chapel Hill Road and Vesson Avenue. One tree was blown down near the intersection of Old Hillsborough Road and Longleadf Pine Place. A tree and power-line were blown down at 300 Tinnin Road.",
+        "The following events were reported: Lightning. These occurred near station USW00013722, approximately 45.8917 km away, between 2018-08-18 20:00:00 and 2018-08-18 20:00:00.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: Prefrontal convection developed over central North Carolina during the late evening in a warm and unstable atmosphere. Several of the storms produced wind damage, with one report of flash flooding.\nEvent Narrative: Lightning struck a home on Regal Crest Drive, causing it to catch Fire.",
+        "The following events were reported: Flash Flood, Thunderstorm Wind. These occurred near station USW00013722, approximately 16.9724 km away, between 2018-08-19 22:53:00 and 2018-08-20 02:29:00.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: A meso-scale boundary along the North Carolina-Virginia state line sparked a complex of slow moving convection that produced 4 to 5 inches of rain and isolated flash flooding across Person County. This complex then moved southward into the Triangle region around midnight, where it produced another 3 to 4 inch swath of rain over the Raleigh-Durham Metro area. This heavy rainfall led to numerous reports of flash flooding within the Raleigh urban area, with multiple water rescues. Additionally, with saturated soils, the thunderstorms also produced scattered wind damage across the Raleigh metro. A meso-scale boundary along the North Carolina-Virginia state line sparked a complex of slow moving convection that produced 4 to 5 inches of rain and isolated flash flooding across Person County. This complex then moved southward into the Triangle region around midnight, where it produced another 3 to 4 inch swath of rain over the Raleigh-Durham Metro area. This heavy rainfall led to numerous reports of flash flooding within the Raleigh urban area, with multiple water rescues. Additionally, with saturated soils, the thunderstorms also produced scattered wind damage across the Raleigh metro. A meso-scale boundary along the North Carolina-Virginia state line sparked a complex of slow moving convection that produced 4 to 5 inches of rain and isolated flash flooding across Person County. This complex then moved southward into the Triangle region around midnight, where it produced another 3 to 4 inch swath of rain over the Raleigh-Durham Metro area. This heavy rainfall led to numerous reports of flash flooding within the Raleigh urban area, with multiple water rescues. Additionally, with saturated soils, the thunderstorms also produced scattered wind damage across the Raleigh metro. A meso-scale boundary along the North Carolina-Virginia state line sparked a complex of slow moving convection that produced 4 to 5 inches of rain and isolated flash flooding across Person County. This complex then moved southward into the Triangle region around midnight, where it produced another 3 to 4 inch swath of rain over the Raleigh-Durham Metro area. This heavy rainfall led to numerous reports of flash flooding within the Raleigh urban area, with multiple water rescues. Additionally, with saturated soils, the thunderstorms also produced scattered wind damage across the Raleigh metro. A meso-scale boundary along the North Carolina-Virginia state line sparked a complex of slow moving convection that produced 4 to 5 inches of rain and isolated flash flooding across Person County. This complex then moved southward into the Triangle region around midnight, where it produced another 3 to 4 inch swath of rain over the Raleigh-Durham Metro area. This heavy rainfall led to numerous reports of flash flooding within the Raleigh urban area, with multiple water rescues. Additionally, with saturated soils, the thunderstorms also produced scattered wind damage across the Raleigh metro. A meso-scale boundary along the North Carolina-Virginia state line sparked a complex of slow moving convection that produced 4 to 5 inches of rain and isolated flash flooding across Person County. This complex then moved southward into the Triangle region around midnight, where it produced another 3 to 4 inch swath of rain over the Raleigh-Durham Metro area. This heavy rainfall led to numerous reports of flash flooding within the Raleigh urban area, with multiple water rescues. Additionally, with saturated soils, the thunderstorms also produced scattered wind damage across the Raleigh metro. A meso-scale boundary along the North Carolina-Virginia state line sparked a complex of slow moving convection that produced 4 to 5 inches of rain and isolated flash flooding across Person County. This complex then moved southward into the Triangle region around midnight, where it produced another 3 to 4 inch swath of rain over the Raleigh-Durham Metro area. This heavy rainfall led to numerous reports of flash flooding within the Raleigh urban area, with multiple water rescues. Additionally, with saturated soils, the thunderstorms also produced scattered wind damage across the Raleigh metro. A meso-scale boundary along the North Carolina-Virginia state line sparked a complex of slow moving convection that produced 4 to 5 inches of rain and isolated flash flooding across Person County. This complex then moved southward into the Triangle region around midnight, where it produced another 3 to 4 inch swath of rain over the Raleigh-Durham Metro area. This heavy rainfall led to numerous reports of flash flooding within the Raleigh urban area, with multiple water rescues. Additionally, with saturated soils, the thunderstorms also produced scattered wind damage across the Raleigh metro. A meso-scale boundary along the North Carolina-Virginia state line sparked a complex of slow moving convection that produced 4 to 5 inches of rain and isolated flash flooding across Person County. This complex then moved southward into the Triangle region around midnight, where it produced another 3 to 4 inch swath of rain over the Raleigh-Durham Metro area. This heavy rainfall led to numerous reports of flash flooding within the Raleigh urban area, with multiple water rescues. Additionally, with saturated soils, the thunderstorms also produced scattered wind damage across the Raleigh metro. A meso-scale boundary along the North Carolina-Virginia state line sparked a complex of slow moving convection that produced 4 to 5 inches of rain and isolated flash flooding across Person County. This complex then moved southward into the Triangle region around midnight, where it produced another 3 to 4 inch swath of rain over the Raleigh-Durham Metro area. This heavy rainfall led to numerous reports of flash flooding within the Raleigh urban area, with multiple water rescues. Additionally, with saturated soils, the thunderstorms also produced scattered wind damage across the Raleigh metro. A meso-scale boundary along the North Carolina-Virginia state line sparked a complex of slow moving convection that produced 4 to 5 inches of rain and isolated flash flooding across Person County. This complex then moved southward into the Triangle region around midnight, where it produced another 3 to 4 inch swath of rain over the Raleigh-Durham Metro area. This heavy rainfall led to numerous reports of flash flooding within the Raleigh urban area, with multiple water rescues. Additionally, with saturated soils, the thunderstorms also produced scattered wind damage across the Raleigh metro. A meso-scale boundary along the North Carolina-Virginia state line sparked a complex of slow moving convection that produced 4 to 5 inches of rain and isolated flash flooding across Person County. This complex then moved southward into the Triangle region around midnight, where it produced another 3 to 4 inch swath of rain over the Raleigh-Durham Metro area. This heavy rainfall led to numerous reports of flash flooding within the Raleigh urban area, with multiple water rescues. Additionally, with saturated soils, the thunderstorms also produced scattered wind damage across the Raleigh metro. A meso-scale boundary along the North Carolina-Virginia state line sparked a complex of slow moving convection that produced 4 to 5 inches of rain and isolated flash flooding across Person County. This complex then moved southward into the Triangle region around midnight, where it produced another 3 to 4 inch swath of rain over the Raleigh-Durham Metro area. This heavy rainfall led to numerous reports of flash flooding within the Raleigh urban area, with multiple water rescues. Additionally, with saturated soils, the thunderstorms also produced scattered wind damage across the Raleigh metro.\nEvent Narrative: Multiple water rescues reported in Raleigh, including at 3415 Aventy Ferry Road and 3600 Lake Boone Trail. Multiple water rescues reported across the city, including at E. Millbrook Road, Six Forks Road, Atlantic Avenue, Hodges Street, and I-440 W at Glenwood Avenue. Water rescues were conducted as multiple vehicles were submerged in over 4 feet of water on Wake Forest Road near Georgetown Road. Water rescue conducted at Capital Boulevard and Old Wake Forest Road. There were several reports of flooded roadways in the area, including at Jones Ferry Road, NC-Highway 54 at Old Fayetteville Road, and Old Greensboro Road. Three trees were blown down along a wind swath extending from Trenton Road to Spring Forest Road. One tree was blown down on I-440 at Lake Boone Trail. One tree was blown down on Court and Noble Street. One tree was blown down on Penny Road and Hunter Hollow Road. One tree was blown down on Blaney Franks Road and Penny Road. Water rescue conducted on Capital Boulevard, underneath the Wake Forest Road Bridge. |Capital Boulevard was closed in both directions. Water rescued was conducted at S. Wilmington Street and City Farm Road. Outbound Capital Blvd before Peace Street closed due to high water.",
+        "The following events were reported: Flash Flood, Flood. These occurred near station USW00013722, approximately 34.686 km away, between 2018-09-14 11:45:00 and 2018-09-24 19:40:00. The flood was caused by Heavy Rain / Tropical System. Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 55271310.0 and crop damage of 75030000.0. \n\nEpisode Narrative: A ridge of high pressure over eastern North America stalled Florence's forward motion a few miles off the southeast North Carolina coast on September 13th. Hurricane Florence made landfall near Wrightsville Beach early on Saturday September 15, and weakened further as it moved slowly inland.  Despite making landfall as a weakened|Category 1 hurricane, Florence still produced 40 to 70 mph wind gusts, enough wind speed to uproot trees and cause widespread power outages throughout the Carolinas.  As the storm moved inland, from September 15 to 17,  heavy rain of 10 to 25 inches  caused widespread inland flooding, inundating cities such as Fayetteville, Smithfield, Goldsboro, Durham, and Chapel Hill, and causing major river flooding on main-stem rivers such as the Neuse, Cape Fear, and Little River. Most major roads and highways in the area experienced some flooding, with large stretches of I-40 and I-95 remaining impassable for days after the storm had passed. The storm also spawned tornadoes in several places along its path. There were 3 direct and 6 indirect deaths attributed to the storm with in the WFO RAH CWA. A ridge of high pressure over eastern North America stalled Florence's forward motion a few miles off the southeast North Carolina coast on September 13th. Hurricane Florence made landfall near Wrightsville Beach early on Saturday September 15, and weakened further as it moved slowly inland.  Despite making landfall as a weakened|Category 1 hurricane, Florence still produced 40 to 70 mph wind gusts, enough wind speed to uproot trees and cause widespread power outages throughout the Carolinas.  As the storm moved inland, from September 15 to 17,  heavy rain of 10 to 25 inches  caused widespread inland flooding, inundating cities such as Fayetteville, Smithfield, Goldsboro, Durham, and Chapel Hill, and causing major river flooding on main-stem rivers such as the Neuse, Cape Fear, and Little River. Most major roads and highways in the area experienced some flooding, with large stretches of I-40 and I-95 remaining impassable for days after the storm had passed. The storm also spawned tornadoes in several places along its path. There were 3 direct and 6 indirect deaths attributed to the storm with in the WFO RAH CWA. A ridge of high pressure over eastern North America stalled Florence's forward motion a few miles off the southeast North Carolina coast on September 13th. Hurricane Florence made landfall near Wrightsville Beach early on Saturday September 15, and weakened further as it moved slowly inland.  Despite making landfall as a weakened|Category 1 hurricane, Florence still produced 40 to 70 mph wind gusts, enough wind speed to uproot trees and cause widespread power outages throughout the Carolinas.  As the storm moved inland, from September 15 to 17,  heavy rain of 10 to 25 inches  caused widespread inland flooding, inundating cities such as Fayetteville, Smithfield, Goldsboro, Durham, and Chapel Hill, and causing major river flooding on main-stem rivers such as the Neuse, Cape Fear, and Little River. Most major roads and highways in the area experienced some flooding, with large stretches of I-40 and I-95 remaining impassable for days after the storm had passed. The storm also spawned tornadoes in several places along its path. There were 3 direct and 6 indirect deaths attributed to the storm with in the WFO RAH CWA. A ridge of high pressure over eastern North America stalled Florence's forward motion a few miles off the southeast North Carolina coast on September 13th. Hurricane Florence made landfall near Wrightsville Beach early on Saturday September 15, and weakened further as it moved slowly inland.  Despite making landfall as a weakened|Category 1 hurricane, Florence still produced 40 to 70 mph wind gusts, enough wind speed to uproot trees and cause widespread power outages throughout the Carolinas.  As the storm moved inland, from September 15 to 17,  heavy rain of 10 to 25 inches  caused widespread inland flooding, inundating cities such as Fayetteville, Smithfield, Goldsboro, Durham, and Chapel Hill, and causing major river flooding on main-stem rivers such as the Neuse, Cape Fear, and Little River. Most major roads and highways in the area experienced some flooding, with large stretches of I-40 and I-95 remaining impassable for days after the storm had passed. The storm also spawned tornadoes in several places along its path. There were 3 direct and 6 indirect deaths attributed to the storm with in the WFO RAH CWA. A ridge of high pressure over eastern North America stalled Florence's forward motion a few miles off the southeast North Carolina coast on September 13th. Hurricane Florence made landfall near Wrightsville Beach early on Saturday September 15, and weakened further as it moved slowly inland.  Despite making landfall as a weakened|Category 1 hurricane, Florence still produced 40 to 70 mph wind gusts, enough wind speed to uproot trees and cause widespread power outages throughout the Carolinas.  As the storm moved inland, from September 15 to 17,  heavy rain of 10 to 25 inches  caused widespread inland flooding, inundating cities such as Fayetteville, Smithfield, Goldsboro, Durham, and Chapel Hill, and causing major river flooding on main-stem rivers such as the Neuse, Cape Fear, and Little River. Most major roads and highways in the area experienced some flooding, with large stretches of I-40 and I-95 remaining impassable for days after the storm had passed. The storm also spawned tornadoes in several places along its path. There were 3 direct and 6 indirect deaths attributed to the storm with in the WFO RAH CWA. A ridge of high pressure over eastern North America stalled Florence's forward motion a few miles off the southeast North Carolina coast on September 13th. Hurricane Florence made landfall near Wrightsville Beach early on Saturday September 15, and weakened further as it moved slowly inland.  Despite making landfall as a weakened|Category 1 hurricane, Florence still produced 40 to 70 mph wind gusts, enough wind speed to uproot trees and cause widespread power outages throughout the Carolinas.  As the storm moved inland, from September 15 to 17,  heavy rain of 10 to 25 inches  caused widespread inland flooding, inundating cities such as Fayetteville, Smithfield, Goldsboro, Durham, and Chapel Hill, and causing major river flooding on main-stem rivers such as the Neuse, Cape Fear, and Little River. Most major roads and highways in the area experienced some flooding, with large stretches of I-40 and I-95 remaining impassable for days after the storm had passed. The storm also spawned tornadoes in several places along its path. There were 3 direct and 6 indirect deaths attributed to the storm with in the WFO RAH CWA. A ridge of high pressure over eastern North America stalled Florence's forward motion a few miles off the southeast North Carolina coast on September 13th. Hurricane Florence made landfall near Wrightsville Beach early on Saturday September 15, and weakened further as it moved slowly inland.  Despite making landfall as a weakened|Category 1 hurricane, Florence still produced 40 to 70 mph wind gusts, enough wind speed to uproot trees and cause widespread power outages throughout the Carolinas.  As the storm moved inland, from September 15 to 17,  heavy rain of 10 to 25 inches  caused widespread inland flooding, inundating cities such as Fayetteville, Smithfield, Goldsboro, Durham, and Chapel Hill, and causing major river flooding on main-stem rivers such as the Neuse, Cape Fear, and Little River. Most major roads and highways in the area experienced some flooding, with large stretches of I-40 and I-95 remaining impassable for days after the storm had passed. The storm also spawned tornadoes in several places along its path. There were 3 direct and 6 indirect deaths attributed to the storm with in the WFO RAH CWA. A ridge of high pressure over eastern North America stalled Florence's forward motion a few miles off the southeast North Carolina coast on September 13th. Hurricane Florence made landfall near Wrightsville Beach early on Saturday September 15, and weakened further as it moved slowly inland.  Despite making landfall as a weakened|Category 1 hurricane, Florence still produced 40 to 70 mph wind gusts, enough wind speed to uproot trees and cause widespread power outages throughout the Carolinas.  As the storm moved inland, from September 15 to 17,  heavy rain of 10 to 25 inches  caused widespread inland flooding, inundating cities such as Fayetteville, Smithfield, Goldsboro, Durham, and Chapel Hill, and causing major river flooding on main-stem rivers such as the Neuse, Cape Fear, and Little River. Most major roads and highways in the area experienced some flooding, with large stretches of I-40 and I-95 remaining impassable for days after the storm had passed. The storm also spawned tornadoes in several places along its path. There were 3 direct and 6 indirect deaths attributed to the storm with in the WFO RAH CWA. A ridge of high pressure over eastern North America stalled Florence's forward motion a few miles off the southeast North Carolina coast on September 13th. Hurricane Florence made landfall near Wrightsville Beach early on Saturday September 15, and weakened further as it moved slowly inland.  Despite making landfall as a weakened|Category 1 hurricane, Florence still produced 40 to 70 mph wind gusts, enough wind speed to uproot trees and cause widespread power outages throughout the Carolinas.  As the storm moved inland, from September 15 to 17,  heavy rain of 10 to 25 inches  caused widespread inland flooding, inundating cities such as Fayetteville, Smithfield, Goldsboro, Durham, and Chapel Hill, and causing major river flooding on main-stem rivers such as the Neuse, Cape Fear, and Little River. Most major roads and highways in the area experienced some flooding, with large stretches of I-40 and I-95 remaining impassable for days after the storm had passed. The storm also spawned tornadoes in several places along its path. There were 3 direct and 6 indirect deaths attributed to the storm with in the WFO RAH CWA. A ridge of high pressure over eastern North America stalled Florence's forward motion a few miles off the southeast North Carolina coast on September 13th. Hurricane Florence made landfall near Wrightsville Beach early on Saturday September 15, and weakened further as it moved slowly inland.  Despite making landfall as a weakened|Category 1 hurricane, Florence still produced 40 to 70 mph wind gusts, enough wind speed to uproot trees and cause widespread power outages throughout the Carolinas.  As the storm moved inland, from September 15 to 17,  heavy rain of 10 to 25 inches  caused widespread inland flooding, inundating cities such as Fayetteville, Smithfield, Goldsboro, Durham, and Chapel Hill, and causing major river flooding on main-stem rivers such as the Neuse, Cape Fear, and Little River. Most major roads and highways in the area experienced some flooding, with large stretches of I-40 and I-95 remaining impassable for days after the storm had passed. The storm also spawned tornadoes in several places along its path. There were 3 direct and 6 indirect deaths attributed to the storm with in the WFO RAH CWA. A ridge of high pressure over eastern North America stalled Florence's forward motion a few miles off the southeast North Carolina coast on September 13th. Hurricane Florence made landfall near Wrightsville Beach early on Saturday September 15, and weakened further as it moved slowly inland.  Despite making landfall as a weakened|Category 1 hurricane, Florence still produced 40 to 70 mph wind gusts, enough wind speed to uproot trees and cause widespread power outages throughout the Carolinas.  As the storm moved inland, from September 15 to 17,  heavy rain of 10 to 25 inches  caused widespread inland flooding, inundating cities such as Fayetteville, Smithfield, Goldsboro, Durham, and Chapel Hill, and causing major river flooding on main-stem rivers such as the Neuse, Cape Fear, and Little River. Most major roads and highways in the area experienced some flooding, with large stretches of I-40 and I-95 remaining impassable for days after the storm had passed. The storm also spawned tornadoes in several places along its path. There were 3 direct and 6 indirect deaths attributed to the storm with in the WFO RAH CWA. A ridge of high pressure over eastern North America stalled Florence's forward motion a few miles off the southeast North Carolina coast on September 13th. Hurricane Florence made landfall near Wrightsville Beach early on Saturday September 15, and weakened further as it moved slowly inland.  Despite making landfall as a weakened|Category 1 hurricane, Florence still produced 40 to 70 mph wind gusts, enough wind speed to uproot trees and cause widespread power outages throughout the Carolinas.  As the storm moved inland, from September 15 to 17,  heavy rain of 10 to 25 inches  caused widespread inland flooding, inundating cities such as Fayetteville, Smithfield, Goldsboro, Durham, and Chapel Hill, and causing major river flooding on main-stem rivers such as the Neuse, Cape Fear, and Little River. Most major roads and highways in the area experienced some flooding, with large stretches of I-40 and I-95 remaining impassable for days after the storm had passed. The storm also spawned tornadoes in several places along its path. There were 3 direct and 6 indirect deaths attributed to the storm with in the WFO RAH CWA. A ridge of high pressure over eastern North America stalled Florence's forward motion a few miles off the southeast North Carolina coast on September 13th. Hurricane Florence made landfall near Wrightsville Beach early on Saturday September 15, and weakened further as it moved slowly inland.  Despite making landfall as a weakened|Category 1 hurricane, Florence still produced 40 to 70 mph wind gusts, enough wind speed to uproot trees and cause widespread power outages throughout the Carolinas.  As the storm moved inland, from September 15 to 17,  heavy rain of 10 to 25 inches  caused widespread inland flooding, inundating cities such as Fayetteville, Smithfield, Goldsboro, Durham, and Chapel Hill, and causing major river flooding on main-stem rivers such as the Neuse, Cape Fear, and Little River. Most major roads and highways in the area experienced some flooding, with large stretches of I-40 and I-95 remaining impassable for days after the storm had passed. The storm also spawned tornadoes in several places along its path. There were 3 direct and 6 indirect deaths attributed to the storm with in the WFO RAH CWA.\nEvent Narrative: Heavy rainfall of 6 to 12 inches flooded numerous roads across the county. Many of the roads are impassable. This list includes but is not limited to Jones Ferry Road Bridge at Uuniversity Lake, Eastgate Crossing and University Place parking lots in Chapel Hill.  Whitfield road is washed out at Foxridge road. Torrential rainfall of 6 to 10 inches caused widespread flooding across the county, which caused flooding along the Eno River and other creeks and streams throughout the county. Additionally, water held in Jordan Lake from rainfall in its headwaters resulted in flooding along the lake into far southeast portions of the county. Flooding damaged approximately 276 structures throughout the county, destroying 1 and resulting in $26.4 million in property damage. Numerous roads were closed due to flooding. Numerous homes and businesses were flooded as well. While final losses on crops are not yet tallied, estimates around $5 million or more are possible. Flash flooding from heavy rainfall of 5 to 8 inches closed several roads across the county. Heavy rainfall of 8 to 12 inches flooded numerous roads across the county. Many of the roads are impassable. This list includes but is not limited to Durham-Chapel Hill Boulevard split, Westgate Drive at Durham-Chapel Hill Boulevard, Rippling Stream at 200 Seven Oaks Road and Old Farm neighborhood in northern Durham. Heavy rainfall of 8 to 12 inches flooded numerous roads across the county. Several roads in are impassable due to flash flooding. This list includes but is not limited to U.S. 15-501 south at the Deep River, Morris Road between Parker Herndon Road and U.S. 15-501, Corinth Road between old U.S. 1 and Moncure Flatwood Road, Chatham Church Road at the bridge over the Rocky River, and R. Jordan Road near Rosser Road. Torrential rainfall of 8 to 10 inches caused widespread flooding across the county, which caused flooding along the creeks and other tributaries of the Neuse River Basin. Water being held in both Lake Jordan and Falls Lake resulted in flooding along the lake perimeters. Flooding caused over $20 million in crop damages. Numerous streets and roads were flooded. Final property damage estimates are still be tallied, but estimates of $5 to $10 million or more are possible. Torrential rainfall of 6 to 10 inches caused widespread flooding across the county. Additional rainfall upstream caused moderate flooding along the Haw River near Haw River. Flooding damaged approximately 202 structures throughout the county, resulting in over $1.07 million in property damage. Numerous roads were closed due to flooding. Numerous homes and businesses were flooded as well. While final losses on crops are not yet tallied, estimates around $5 million are possible. Torrential rainfall of 10 to 15 inches caused widespread flooding across the county. Additional rainfall upstream caused moderate flooding along the Eno River near Enon. Additionally, water held in Jordan Lake from rainfall in its headwaters resulted in flooding along the lake into portions of the county, which lingered for several days. Flooding damaged approximately 638 structures throughout the county, destroying 4 and resulting in $11.05 million in property damage. Numerous roads were closed due to flooding. Numerous homes and businesses were flooded as well. While final losses on crops are not yet tallied, estimates around $5 million are possible. Torrential rainfall of 8 to 15 inches caused widespread flash flooding across the county. The heavy rains caused flash flooding on several creeks, especially across southern portions of the county.  Numerous roads throughout the county were closed, due to flooding, including portions of Interstate 95,  NC-Highway 242, NC-Highway 96, and US-Highway 701. Several roads washed out across the county, including  Stevens Chapel Road, near Princeton. Numerous homes and businesses were flooded as well. Torrential rainfall of 8 to 15 inches caused widespread flash flooding across the county. The heavy rains caused several creeks to over-spill their banks.  Numerous roads throughout the county were closed, due to flooding, including portions of Interstate 95, between Fayetteville and Dunn and Highways 301 and 401, near Dunn.  Numerous homes and businesses were flooded as well. Torrential rainfall of 10 to 15 inches caused widespread flooding across the county. Additional rainfall upstream caused minor flooding along the Neuse River at Clayton and the Little River near Princeton and moderate flooding along the Neuse River at Smithfield. Flooding damaged approximately 221 structures throughout the county, resulting in over $1.3 million in property damage, and $30 million in crop damage. Numerous streets and roads were reported flooded. Torrential rainfall of 10 to 15 inches caused widespread flooding across the county. Additional rainfall upstream caused major flooding along the Deep River near Moncure and along the Haw River near Bynum. Flooding damaged approximately 107 structures throughout the county, destroying 3, resulting in approximately $6.33 million in property damage and and at least $20 million in crop damage. Numerous roads were closed due to flooding. Numerous homes and businesses were flooded as well. Torrential rainfall of 10 to 15 inches caused widespread flash flooding across the county. Additional heavy rainfall upstream caused moderate flooding along the Deep River near Moncure. Flooding damaged approximately 210 structures throughout the county, destroying 13 and resulting in over $5.4 million in property damage and over $20 million in crop damage. Numerous streets and roads were reported flooded.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 43.5498 km away, between 2018-09-17 15:15:00 and 2018-09-17 15:30:00. 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: As remnants of Florence lifted north of the area, scattered thunderstorms developed during the afternoon due to strong differential heating within the pronounced mid-level dry slot, east of the center of the circulation. Two thunderstorms produced some scattered thunderstorm wind damage, along with some isolated flash flooding due to the  wet antecedent conditions. As remnants of Florence lifted north of the area, scattered thunderstorms developed during the afternoon due to strong differential heating within the pronounced mid-level dry slot, east of the center of the circulation. Two thunderstorms produced some scattered thunderstorm wind damage, along with some isolated flash flooding due to the  wet antecedent conditions.\nEvent Narrative: Two trees blown down in the area. Several trees blown down south of Rougemont.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 26.625 km away, between 2018-09-27 18:55:00 and 2018-09-27 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 2500.0 and crop damage of 0.0. \n\nEpisode Narrative: Isolated severe storms developed ahead of a cold front during the late afternoon in a moist and unstable air mass. A more organized comma head and trailing line of storms moved into the area mid to late evening. Some of the storms produced wind damage across portions of the area. Isolated severe storms developed ahead of a cold front during the late afternoon in a moist and unstable air mass. A more organized comma head and trailing line of storms moved into the area mid to late evening. Some of the storms produced wind damage across portions of the area.\nEvent Narrative: One tree was reported down blocking the entrance to Shanley Drive near Edgemont Road. Trees were reported down on power lines near South Wilmington Street.",
+        "The following events were reported: Flash Flood. These occurred near station USW00013722, approximately 27.8425 km away, between 2018-10-11 13:48:00 and 2018-10-12 00:40:00.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 125000.0 and crop damage of 0.0. \n\nEpisode Narrative: Tropical Storm Michael moved through North Carolina on Thursday, October 11th.  Michael brought heavy rain and strong damaging winds to central North Carolina. While heavy rainfall of 3 to 6 inches produced minor flash flooding across the area, it was high wind gusts of 40 to 60 mph that caused the biggest problems, knocking down score of  trees, leading to blocked roadways and thousands without power. Tropical Storm Michael moved through North Carolina on Thursday, October 11th.  Michael brought heavy rain and strong damaging winds to central North Carolina. While heavy rainfall of 3 to 6 inches produced minor flash flooding across the area, it was high wind gusts of 40 to 60 mph that caused the biggest problems, knocking down score of  trees, leading to blocked roadways and thousands without power. Tropical Storm Michael moved through North Carolina on Thursday, October 11th.  Michael brought heavy rain and strong damaging winds to central North Carolina. While heavy rainfall of 3 to 6 inches produced minor flash flooding across the area, it was high wind gusts of 40 to 60 mph that caused the biggest problems, knocking down score of  trees, leading to blocked roadways and thousands without power.\nEvent Narrative: Heavy rainfall of 3 to 5 inches across the county resulted in several road closures due to flash flooding. Capital Boulevard between West Lane Street and West Peace Street and the intersection of Highway 264 and Gannon Avenue both had to be closed due to flooding. Additionally, Crabtree Creek came out of its banks at Old Wake Forest Road. Heavy rainfall of 2 to 5 inches flooded multiple roads across the county. Heavy rainfall of 2 to 4 inches flooded several roads across the southern half of the county, most of which were in the Creedmoor area.",
+        "The following events were reported: Flash Flood. These occurred near station USW00013722, approximately 25.333 km away, between 2018-11-12 21:10:00 and 2018-11-13 05:20:00.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 strong low pressure system lifted northeastward into central North Carolina ahead of a strong cold front approaching from the west. There was fairly substantial lift over the region thanks to a strengthening low level jet and increasing diffluence aloft supplied by a 140 to 150 knot jet streaking northeastward across the OH Valley. All that combined with precipatable water values in the 1.5 -1.7 inch range set the stage for flash flooding across portions of central North Carolina. A strong low pressure system lifted northeastward into central North Carolina ahead of a strong cold front approaching from the west. There was fairly substantial lift over the region thanks to a strengthening low level jet and increasing diffluence aloft supplied by a 140 to 150 knot jet streaking northeastward across the OH Valley. All that combined with precipatable water values in the 1.5 -1.7 inch range set the stage for flash flooding across portions of central North Carolina.\nEvent Narrative: Heavy rain resulted in flash flooding throughout the city of Chapel Hill. Multiple roads were flooded, including Umstead Road, Estes Drive, Cleland Road and Old Mason Farm Road. Heavy rainfall resulted in flash flooding along the New Light Creek in northern Wake County. Water from the New Light Creek was flowing over bridge on Mangum Dairy Road, making the road impassable.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 28.9277 km away, between 2019-04-08 16:20:00 and 2019-04-08 18:57:00. The events included records with estimated wind gusts of 50.25 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 shortwave in the flow aloft approaching central NC from the southwest resulted in  backing low to mid level winds. The backing winds enhanced the low level shear and advected warm moist air into central NC. The resultant moderately unstable  |atmosphere lead to the development of numerous showers and thunderstorms. Due to the presence of the available shear and instability, several storms became severe, producing damaging winds. A shortwave in the flow aloft approaching central NC from the southwest resulted in  backing low to mid level winds. The backing winds enhanced the low level shear and advected warm moist air into central NC. The resultant moderately unstable  |atmosphere lead to the development of numerous showers and thunderstorms. Due to the presence of the available shear and instability, several storms became severe, producing damaging winds. A shortwave in the flow aloft approaching central NC from the southwest resulted in  backing low to mid level winds. The backing winds enhanced the low level shear and advected warm moist air into central NC. The resultant moderately unstable  |atmosphere lead to the development of numerous showers and thunderstorms. Due to the presence of the available shear and instability, several storms became severe, producing damaging winds. A shortwave in the flow aloft approaching central NC from the southwest resulted in  backing low to mid level winds. The backing winds enhanced the low level shear and advected warm moist air into central NC. The resultant moderately unstable  |atmosphere lead to the development of numerous showers and thunderstorms. Due to the presence of the available shear and instability, several storms became severe, producing damaging winds. A shortwave in the flow aloft approaching central NC from the southwest resulted in  backing low to mid level winds. The backing winds enhanced the low level shear and advected warm moist air into central NC. The resultant moderately unstable  |atmosphere lead to the development of numerous showers and thunderstorms. Due to the presence of the available shear and instability, several storms became severe, producing damaging winds. A shortwave in the flow aloft approaching central NC from the southwest resulted in  backing low to mid level winds. The backing winds enhanced the low level shear and advected warm moist air into central NC. The resultant moderately unstable  |atmosphere lead to the development of numerous showers and thunderstorms. Due to the presence of the available shear and instability, several storms became severe, producing damaging winds. A shortwave in the flow aloft approaching central NC from the southwest resulted in  backing low to mid level winds. The backing winds enhanced the low level shear and advected warm moist air into central NC. The resultant moderately unstable  |atmosphere lead to the development of numerous showers and thunderstorms. Due to the presence of the available shear and instability, several storms became severe, producing damaging winds. A shortwave in the flow aloft approaching central NC from the southwest resulted in  backing low to mid level winds. The backing winds enhanced the low level shear and advected warm moist air into central NC. The resultant moderately unstable  |atmosphere lead to the development of numerous showers and thunderstorms. Due to the presence of the available shear and instability, several storms became severe, producing damaging winds.\nEvent Narrative: Wind gusts to 60 miles per hour were reported in Angier. Some small limbs were blown down as a result of the gusts. Five trees were blown down along a swath from 3600 Darroch Road in Lillington to the intersection of Highway 27 South and Delma Grimes Road in Grove Township. A couple of the trees fell onto power lines. One tree was blown down near the intersection of Fayetteville Street and Buxton Drive. One tree was blown down into the back yard of a residence on Peninsula Forest Place in Cary. One tree was blown down near the intersection of Strickland Road and Cold Springs Road in North Raleigh. A 60 foot tall tree fell onto a residence in Cary. Multiple trees were blown down in the Willow Springs and Benson areas, including one tree near the intersection of Steel Bridge Road and Benson Hardee Road. One tree was blown down across the railroad tracks near West Front Street in Clayton.",
+        "The following events were reported: Flash Flood, Thunderstorm Wind, Tornado. These occurred near station USW00013722, approximately 28.9866 km away, between 2019-04-12 16:28:00 and 2019-04-12 20:25:00.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 52000.0 and crop damage of 0.0. \n\nEpisode Narrative: Enhanced southerly flow advected warm, moist air into the region ahead of a diving shortwave trough and attendant cold front. This resulted in sufficient moisture, strong shear and marginal instability to produce a line of showers and strong thunderstorms. These storms produced scattered wind damage, localized flash flooding and a brief tornado as they moved through central North Carolina. Enhanced southerly flow advected warm, moist air into the region ahead of a diving shortwave trough and attendant cold front. This resulted in sufficient moisture, strong shear and marginal instability to produce a line of showers and strong thunderstorms. These storms produced scattered wind damage, localized flash flooding and a brief tornado as they moved through central North Carolina. Enhanced southerly flow advected warm, moist air into the region ahead of a diving shortwave trough and attendant cold front. This resulted in sufficient moisture, strong shear and marginal instability to produce a line of showers and strong thunderstorms. These storms produced scattered wind damage, localized flash flooding and a brief tornado as they moved through central North Carolina. Enhanced southerly flow advected warm, moist air into the region ahead of a diving shortwave trough and attendant cold front. This resulted in sufficient moisture, strong shear and marginal instability to produce a line of showers and strong thunderstorms. These storms produced scattered wind damage, localized flash flooding and a brief tornado as they moved through central North Carolina. Enhanced southerly flow advected warm, moist air into the region ahead of a diving shortwave trough and attendant cold front. This resulted in sufficient moisture, strong shear and marginal instability to produce a line of showers and strong thunderstorms. These storms produced scattered wind damage, localized flash flooding and a brief tornado as they moved through central North Carolina. Enhanced southerly flow advected warm, moist air into the region ahead of a diving shortwave trough and attendant cold front. This resulted in sufficient moisture, strong shear and marginal instability to produce a line of showers and strong thunderstorms. These storms produced scattered wind damage, localized flash flooding and a brief tornado as they moved through central North Carolina.\nEvent Narrative: Multiple roads were closed due to flash flooding near Durham. Hillandale Road at Sprunt Avenue, Morreene Road at American Drive and Hillandale Road at Peppertree Street were all closed due to flooding. A car became stranded in flood waters near the intersection of Belleavue Avenue and Hillsborough Road. A few trees were blown down along Mt Carmel Church Road. A few trees were blown down along Virginia Drive. One tree was blown down on Beaver Creek Road near Old US 1 Highway. Power lines and a power pole were blown down along Buckhorn-Duncan Road. An EF0 tornado touched down just south of Raven Rock State Park, crossed Hicks Road and moved north-northeast through the park. The tornado then crossed the Cape Fear River, exited the park and lifted just before reaching Cokesbury Road. The tornado remained on the ground for approximately 4 minutes and traveled 4.9 miles. This tornado produced minor intermittent tree damage in the form of uprooted and snapped hardwood trees.",
+        "The following events were reported: Flash Flood. These occurred near station USW00013722, approximately 32.3792 km away, between 2019-04-13 12:45:00 and 2019-04-13 17:10:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A series of upper-level disturbances moved northeast across a stationary cold front situated over central NC in a moist and unstable atmosphere. The resulting heavy showers and thunderstorms across the northern Piedmont combined with saturated antecedent conditions produced flash flooding across the region. Multiple roads were closed due to flash flooding, and one road partially collapsed. A series of upper-level disturbances moved northeast across a stationary cold front situated over central NC in a moist and unstable atmosphere. The resulting heavy showers and thunderstorms across the northern Piedmont combined with saturated antecedent conditions produced flash flooding across the region. Multiple roads were closed due to flash flooding, and one road partially collapsed.\nEvent Narrative: The Eno River near South Church Street in Hillsborough came out of its banks, threatening the riverwalk. The 300 block of Johnson Mill Road was closed due to flooding.",
+        "The following events were reported: Flash Flood, Thunderstorm Wind. These occurred near station USW00013722, approximately 16.1784 km away, between 2019-04-14 23:48:00 and 2019-04-15 01:40:00.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: An initial round of convection developed in the wake of a northwestward propagating warm front as the atmosphere became increasingly moist and unstable during the afternoon. There was a brief lull in convective activity during the evening hours. Large scale forcing for ascent increased over central North Carolina through the overnight hours, downstream of a slightly positively tilted synoptic trough. An approaching quasi-linear convective system moved through the area overnight, producing widespread wind damage, isolated flash flooding and a weak tornado. An initial round of convection developed in the wake of a northwestward propagating warm front as the atmosphere became increasingly moist and unstable during the afternoon. There was a brief lull in convective activity during the evening hours. Large scale forcing for ascent increased over central North Carolina through the overnight hours, downstream of a slightly positively tilted synoptic trough. An approaching quasi-linear convective system moved through the area overnight, producing widespread wind damage, isolated flash flooding and a weak tornado. An initial round of convection developed in the wake of a northwestward propagating warm front as the atmosphere became increasingly moist and unstable during the afternoon. There was a brief lull in convective activity during the evening hours. Large scale forcing for ascent increased over central North Carolina through the overnight hours, downstream of a slightly positively tilted synoptic trough. An approaching quasi-linear convective system moved through the area overnight, producing widespread wind damage, isolated flash flooding and a weak tornado.\nEvent Narrative: A few trees were blown down in the Raleigh area, one on the 2600 block of Western Boulevard, one on power lines on Ward Road near Glenridge Drive and one on Seabrook Road near Frinks Street. Numerous trees were blown down along a swath from the intersection of Lake Wheeler Road and Inwood Drive to near the intersection of Six Forks Road and Barrett Drive, just inside the beltline. Heavy rain resulted in flash flooding along several roadways in Raleigh. The flooded intersections included West Peace Street and Capital Boulevard, Glenwood Avenue and West Peace Street, and Atlantic Avenue and Hodges Street.",
+        "The following events were reported: Thunderstorm Wind, Tornado. These occurred near station USW00013722, approximately 32.1573 km away, between 2019-04-19 10:01:00 and 2019-04-19 16:25:00.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 2029000.0 and crop damage of 0.0. \n\nEpisode Narrative: A deepening upper-level trough, which featured a strong polar jet ejecting northeast atop an eastward advancing cold front, brought severe thunderstorms that produced|7 tornadoes and widespread damaging straight-line winds across central NC. The strongest tornado of the day in North Carolina formed in southwestern Orange County and reached EF-2 strength as it neared Hillsborough. Along its path estimated at 12 miles long and a maximum of 600 yards wide, the roof and exterior walls of one home were reported as completely destroyed. A deepening upper-level trough, which featured a strong polar jet ejecting northeast atop an eastward advancing cold front, brought severe thunderstorms that produced|7 tornadoes and widespread damaging straight-line winds across central NC. The strongest tornado of the day in North Carolina formed in southwestern Orange County and reached EF-2 strength as it neared Hillsborough. Along its path estimated at 12 miles long and a maximum of 600 yards wide, the roof and exterior walls of one home were reported as completely destroyed. A deepening upper-level trough, which featured a strong polar jet ejecting northeast atop an eastward advancing cold front, brought severe thunderstorms that produced|7 tornadoes and widespread damaging straight-line winds across central NC. The strongest tornado of the day in North Carolina formed in southwestern Orange County and reached EF-2 strength as it neared Hillsborough. Along its path estimated at 12 miles long and a maximum of 600 yards wide, the roof and exterior walls of one home were reported as completely destroyed. A deepening upper-level trough, which featured a strong polar jet ejecting northeast atop an eastward advancing cold front, brought severe thunderstorms that produced|7 tornadoes and widespread damaging straight-line winds across central NC. The strongest tornado of the day in North Carolina formed in southwestern Orange County and reached EF-2 strength as it neared Hillsborough. Along its path estimated at 12 miles long and a maximum of 600 yards wide, the roof and exterior walls of one home were reported as completely destroyed. A deepening upper-level trough, which featured a strong polar jet ejecting northeast atop an eastward advancing cold front, brought severe thunderstorms that produced|7 tornadoes and widespread damaging straight-line winds across central NC. The strongest tornado of the day in North Carolina formed in southwestern Orange County and reached EF-2 strength as it neared Hillsborough. Along its path estimated at 12 miles long and a maximum of 600 yards wide, the roof and exterior walls of one home were reported as completely destroyed. A deepening upper-level trough, which featured a strong polar jet ejecting northeast atop an eastward advancing cold front, brought severe thunderstorms that produced|7 tornadoes and widespread damaging straight-line winds across central NC. The strongest tornado of the day in North Carolina formed in southwestern Orange County and reached EF-2 strength as it neared Hillsborough. Along its path estimated at 12 miles long and a maximum of 600 yards wide, the roof and exterior walls of one home were reported as completely destroyed. A deepening upper-level trough, which featured a strong polar jet ejecting northeast atop an eastward advancing cold front, brought severe thunderstorms that produced|7 tornadoes and widespread damaging straight-line winds across central NC. The strongest tornado of the day in North Carolina formed in southwestern Orange County and reached EF-2 strength as it neared Hillsborough. Along its path estimated at 12 miles long and a maximum of 600 yards wide, the roof and exterior walls of one home were reported as completely destroyed. A deepening upper-level trough, which featured a strong polar jet ejecting northeast atop an eastward advancing cold front, brought severe thunderstorms that produced|7 tornadoes and widespread damaging straight-line winds across central NC. The strongest tornado of the day in North Carolina formed in southwestern Orange County and reached EF-2 strength as it neared Hillsborough. Along its path estimated at 12 miles long and a maximum of 600 yards wide, the roof and exterior walls of one home were reported as completely destroyed. A deepening upper-level trough, which featured a strong polar jet ejecting northeast atop an eastward advancing cold front, brought severe thunderstorms that produced|7 tornadoes and widespread damaging straight-line winds across central NC. The strongest tornado of the day in North Carolina formed in southwestern Orange County and reached EF-2 strength as it neared Hillsborough. Along its path estimated at 12 miles long and a maximum of 600 yards wide, the roof and exterior walls of one home were reported as completely destroyed. A deepening upper-level trough, which featured a strong polar jet ejecting northeast atop an eastward advancing cold front, brought severe thunderstorms that produced|7 tornadoes and widespread damaging straight-line winds across central NC. The strongest tornado of the day in North Carolina formed in southwestern Orange County and reached EF-2 strength as it neared Hillsborough. Along its path estimated at 12 miles long and a maximum of 600 yards wide, the roof and exterior walls of one home were reported as completely destroyed. A deepening upper-level trough, which featured a strong polar jet ejecting northeast atop an eastward advancing cold front, brought severe thunderstorms that produced|7 tornadoes and widespread damaging straight-line winds across central NC. The strongest tornado of the day in North Carolina formed in southwestern Orange County and reached EF-2 strength as it neared Hillsborough. Along its path estimated at 12 miles long and a maximum of 600 yards wide, the roof and exterior walls of one home were reported as completely destroyed. A deepening upper-level trough, which featured a strong polar jet ejecting northeast atop an eastward advancing cold front, brought severe thunderstorms that produced|7 tornadoes and widespread damaging straight-line winds across central NC. The strongest tornado of the day in North Carolina formed in southwestern Orange County and reached EF-2 strength as it neared Hillsborough. Along its path estimated at 12 miles long and a maximum of 600 yards wide, the roof and exterior walls of one home were reported as completely destroyed. A deepening upper-level trough, which featured a strong polar jet ejecting northeast atop an eastward advancing cold front, brought severe thunderstorms that produced|7 tornadoes and widespread damaging straight-line winds across central NC. The strongest tornado of the day in North Carolina formed in southwestern Orange County and reached EF-2 strength as it neared Hillsborough. Along its path estimated at 12 miles long and a maximum of 600 yards wide, the roof and exterior walls of one home were reported as completely destroyed. A deepening upper-level trough, which featured a strong polar jet ejecting northeast atop an eastward advancing cold front, brought severe thunderstorms that produced|7 tornadoes and widespread damaging straight-line winds across central NC. The strongest tornado of the day in North Carolina formed in southwestern Orange County and reached EF-2 strength as it neared Hillsborough. Along its path estimated at 12 miles long and a maximum of 600 yards wide, the roof and exterior walls of one home were reported as completely destroyed. A deepening upper-level trough, which featured a strong polar jet ejecting northeast atop an eastward advancing cold front, brought severe thunderstorms that produced|7 tornadoes and widespread damaging straight-line winds across central NC. The strongest tornado of the day in North Carolina formed in southwestern Orange County and reached EF-2 strength as it neared Hillsborough. Along its path estimated at 12 miles long and a maximum of 600 yards wide, the roof and exterior walls of one home were reported as completely destroyed. A deepening upper-level trough, which featured a strong polar jet ejecting northeast atop an eastward advancing cold front, brought severe thunderstorms that produced|7 tornadoes and widespread damaging straight-line winds across central NC. The strongest tornado of the day in North Carolina formed in southwestern Orange County and reached EF-2 strength as it neared Hillsborough. Along its path estimated at 12 miles long and a maximum of 600 yards wide, the roof and exterior walls of one home were reported as completely destroyed. A deepening upper-level trough, which featured a strong polar jet ejecting northeast atop an eastward advancing cold front, brought severe thunderstorms that produced|7 tornadoes and widespread damaging straight-line winds across central NC. The strongest tornado of the day in North Carolina formed in southwestern Orange County and reached EF-2 strength as it neared Hillsborough. Along its path estimated at 12 miles long and a maximum of 600 yards wide, the roof and exterior walls of one home were reported as completely destroyed. A deepening upper-level trough, which featured a strong polar jet ejecting northeast atop an eastward advancing cold front, brought severe thunderstorms that produced|7 tornadoes and widespread damaging straight-line winds across central NC. The strongest tornado of the day in North Carolina formed in southwestern Orange County and reached EF-2 strength as it neared Hillsborough. Along its path estimated at 12 miles long and a maximum of 600 yards wide, the roof and exterior walls of one home were reported as completely destroyed.\nEvent Narrative: Media reported downed tree onto a vehicle resulting in a cracked windshield. Large trees blown down onto car. Monetary damages were estimated. Several trees down in the Holly Springs, including downed trees along Holly Springs Road, Richardson Road, Optimist Road, and Avent Ferry Road. Numerous trees down in the Pittsboro area. Trees and power-lines blown down along Dodsons Cross Roads. One large tree fell through a fence. Tress were reported down near Dairyland Road. A 50 ft. tree fell down across the road. Several trees blown down along a swath extending from Charlie Grissom Road to |S. Garnett Street in Henderson. Tree down on power-lines at 454 S. Chavis Strett. Power-line was blown down at 526 Peach Orchard Road. Multiple trees were reported down, some snapped off, near Old Crews Road. A tree was reported down at Guy Road and Amelia Church Road. A tornado initially touched down in the White Cross area and Leslie Drive area of southwest Orange County. Considerable tree damage occurred in this area, including the snapping and splitting of healthy large-trunk trees.  Subsequent damage to vehicles and homes occurred as the trees fell.  Given the magnitude and nature of the damage, wind speeds were estimated at 110 mph.  The tornado then tracked north-northeast eventually crossing Dodsons Cross Road, Dairlyland Road, Arthur Minnis Road, and Borland Roads, all while producing similar tree damage.  The tornado finally began to lift and/or dissipate near Hillsborough just north of I-40 near exit 261, but not before producing considerable damage to several homes just south of exit 261.  The roof and several exterior walls of one home were completely destroyed.  Damage at this location was estimated at 115 mph, making this tornado a low-end EF-2 on the EF scale. One tree was blown down near the intersection of Hight and Fairport Road. Several power-lines also reported down in Oxford. Trees were reported down. Power-lines reported down at S. Lombard Street and Regency Park Drive. Power-lines were blown down near the intersection of Mack Todd Road and Black Love Road.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 45.1665 km away, between 2019-04-26 14:53:00 and 2019-04-26 15:02:00. 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 potent upper level trough swung through the region accompanied by a 120 knot upper level jet and strong surface cold front. The boundary layer was sufficiently warm and moist ahead of the front to result in marginal instability during the afternoon, largely confined to eastern portions of central North Carolina. A scattered line of thunderstorms developed ahead of the front as it moved through the area. One storm became severe, producing wind damage in Wilson and Edgecombe counties.\nEvent Narrative: Two trees were blown down in Johnston county, one near the intersection of Smith Road and Water Oak Drive and the other at 3030 Highway 42 East near the Neuse Colony Subdivision in Clayton.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 33.3826 km away, between 2019-05-04 19:15:00 and 2019-05-04 19:23:00. The events included records with estimated wind gusts of 50.0 mph.The events resulted in 1 injuries and 1 fatalities. The events caused property damage valued at 10000.0 and crop damage of 0.0. \n\nEpisode Narrative: Several multi-cellular clusters moved across the area during the late afternoon and evening. Multiple clusters produced wind damage as they moved through the area in a moist and unstable environment. Several multi-cellular clusters moved across the area during the late afternoon and evening. Multiple clusters produced wind damage as they moved through the area in a moist and unstable environment. Several multi-cellular clusters moved across the area during the late afternoon and evening. Multiple clusters produced wind damage as they moved through the area in a moist and unstable environment.\nEvent Narrative: One tree was reported down near the intersection of Avent Ferry Road and Bartley Holleman Road. One tree was reported down on a vehicle near the intersection of Jackpot Lane and Walter Myatt Road, with one person reported injured. One tree was reported down near the intersection of Old Stage Road and Fanny Brown Road.",
+        "The following events were reported: Hail, Thunderstorm Wind, Tornado. These occurred near station USW00013722, approximately 24.9623 km away, between 2019-05-13 08:54:00 and 2019-05-13 13:10:00. The events included records with hailstones measuring 5.323333333333333 inches.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 101250000.0 and crop damage of 0.0. \n\nEpisode Narrative: A southward moving cold front interacted with a rather unstable air mass for mid to late morning into the early afternoon across the area and allowed for the development of an isolated cluster of thunderstorms across the central Piedmont and central Coastal Plain of central North Carolina. The cluster of thunderstorms become severe and produced wind damage, very large hail and a EF-2 tornado as shortwave disturbance moved across the area allowing the convection to quickly intensify. A southward moving cold front interacted with a rather unstable air mass for mid to late morning into the early afternoon across the area and allowed for the development of an isolated cluster of thunderstorms across the central Piedmont and central Coastal Plain of central North Carolina. The cluster of thunderstorms become severe and produced wind damage, very large hail and a EF-2 tornado as shortwave disturbance moved across the area allowing the convection to quickly intensify. A southward moving cold front interacted with a rather unstable air mass for mid to late morning into the early afternoon across the area and allowed for the development of an isolated cluster of thunderstorms across the central Piedmont and central Coastal Plain of central North Carolina. The cluster of thunderstorms become severe and produced wind damage, very large hail and a EF-2 tornado as shortwave disturbance moved across the area allowing the convection to quickly intensify. A southward moving cold front interacted with a rather unstable air mass for mid to late morning into the early afternoon across the area and allowed for the development of an isolated cluster of thunderstorms across the central Piedmont and central Coastal Plain of central North Carolina. The cluster of thunderstorms become severe and produced wind damage, very large hail and a EF-2 tornado as shortwave disturbance moved across the area allowing the convection to quickly intensify. A southward moving cold front interacted with a rather unstable air mass for mid to late morning into the early afternoon across the area and allowed for the development of an isolated cluster of thunderstorms across the central Piedmont and central Coastal Plain of central North Carolina. The cluster of thunderstorms become severe and produced wind damage, very large hail and a EF-2 tornado as shortwave disturbance moved across the area allowing the convection to quickly intensify. A southward moving cold front interacted with a rather unstable air mass for mid to late morning into the early afternoon across the area and allowed for the development of an isolated cluster of thunderstorms across the central Piedmont and central Coastal Plain of central North Carolina. The cluster of thunderstorms become severe and produced wind damage, very large hail and a EF-2 tornado as shortwave disturbance moved across the area allowing the convection to quickly intensify. A southward moving cold front interacted with a rather unstable air mass for mid to late morning into the early afternoon across the area and allowed for the development of an isolated cluster of thunderstorms across the central Piedmont and central Coastal Plain of central North Carolina. The cluster of thunderstorms become severe and produced wind damage, very large hail and a EF-2 tornado as shortwave disturbance moved across the area allowing the convection to quickly intensify. A southward moving cold front interacted with a rather unstable air mass for mid to late morning into the early afternoon across the area and allowed for the development of an isolated cluster of thunderstorms across the central Piedmont and central Coastal Plain of central North Carolina. The cluster of thunderstorms become severe and produced wind damage, very large hail and a EF-2 tornado as shortwave disturbance moved across the area allowing the convection to quickly intensify. A southward moving cold front interacted with a rather unstable air mass for mid to late morning into the early afternoon across the area and allowed for the development of an isolated cluster of thunderstorms across the central Piedmont and central Coastal Plain of central North Carolina. The cluster of thunderstorms become severe and produced wind damage, very large hail and a EF-2 tornado as shortwave disturbance moved across the area allowing the convection to quickly intensify. A southward moving cold front interacted with a rather unstable air mass for mid to late morning into the early afternoon across the area and allowed for the development of an isolated cluster of thunderstorms across the central Piedmont and central Coastal Plain of central North Carolina. The cluster of thunderstorms become severe and produced wind damage, very large hail and a EF-2 tornado as shortwave disturbance moved across the area allowing the convection to quickly intensify. A southward moving cold front interacted with a rather unstable air mass for mid to late morning into the early afternoon across the area and allowed for the development of an isolated cluster of thunderstorms across the central Piedmont and central Coastal Plain of central North Carolina. The cluster of thunderstorms become severe and produced wind damage, very large hail and a EF-2 tornado as shortwave disturbance moved across the area allowing the convection to quickly intensify. A southward moving cold front interacted with a rather unstable air mass for mid to late morning into the early afternoon across the area and allowed for the development of an isolated cluster of thunderstorms across the central Piedmont and central Coastal Plain of central North Carolina. The cluster of thunderstorms become severe and produced wind damage, very large hail and a EF-2 tornado as shortwave disturbance moved across the area allowing the convection to quickly intensify. A southward moving cold front interacted with a rather unstable air mass for mid to late morning into the early afternoon across the area and allowed for the development of an isolated cluster of thunderstorms across the central Piedmont and central Coastal Plain of central North Carolina. The cluster of thunderstorms become severe and produced wind damage, very large hail and a EF-2 tornado as shortwave disturbance moved across the area allowing the convection to quickly intensify. A southward moving cold front interacted with a rather unstable air mass for mid to late morning into the early afternoon across the area and allowed for the development of an isolated cluster of thunderstorms across the central Piedmont and central Coastal Plain of central North Carolina. The cluster of thunderstorms become severe and produced wind damage, very large hail and a EF-2 tornado as shortwave disturbance moved across the area allowing the convection to quickly intensify.\nEvent Narrative: A supercell thunderstorm tracked across portions of southern Wake County into central Johnston County. The thunderstorm produced hail ranging from golf ball size to baseball size hail. The hail caused extensive damage to homes, cars, buildings and businesses in its path. Several car dealerships has substantial damage done to cars on their lots and many homeowners had broken winds and significant roof and siding damage.   Nickel size hail was reported at Creedmoor Road and West Millbrook Road.  One inch hail was reported at Piermont Drive.     The tornado initially touched down just west of Rolesville Road  |near Tink's Place in eastern Wake County. The tornado initially  |produced widespread EF-1 damage with sporadic EF-2 damage noted on |Weathers Road. Along the path to Weathers Road, numerous trees  |were either uprooted or snapped and mangled together, consistent  |with EF-1 damage.  | |At Weathers Road, structural damage was noted as a single family  |home had its exterior walls collapsed. Several metal farm  |buildings were also completely destroyed and strewn about a field. |Sheet metal was wrapped around a nearby tree. An RV was flipped  |over numerous times landing crushed in an open field. In  |addition, another home had the windows blown out with roof damage. |It was in this area that EF-2 damage was determined. | |The tornado continued tracking east and crossed Edgemont Road just  |north of HWY 264/64, then crossing HWY 264/64 where numerous trees  |were downed and snapped. Generally EF-1 damage was noted here.  | |The tornado then moved east into Zebulon along and near Highway  |97 (West Gannon Avenue) where numerous trees snapped and uprooted. |It continued east of Zebulon, crossing HWY 264/64 again, and going |just north of the Five County Stadium. Generally EF-0 and EF-1  |damage was noted here. The Tink's Place tornado continued into western Nash County and then crossed into Nash County, where damage was  observed on Brantley Road. Most of the damage consisted of trees being snapped and uprooted, with structural damage to an open-air  |farm outhouse. Just east on Massey Road, one newly constructed  home suffered roof damage, with roof trusses severely damaged. Shingles had not been completed on the home yet, therefore this damage was considered EF-1 level. Also on Massey Road, a modular home suffered roof and wall damage, while two farm outhouses were severely damaged. The tornado then tracked east along Nade Road causing more uprooted and snapped trees. A home along Nade Road also lost its chimney with a cinderblock outhouse suffering complete roof failure. | |Finally, the tornado began to weaken as it crossed the woods east of Hoyt Road, and it eventually lifted just east of Winters Road. One tree was reported down on a power line near Moore Mountain Road. Two inch diameter hail damaged cars, shingles and broke windows a couple miles southeast of Williams Crossroads.",
+        "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00013722, approximately 22.7338 km away, between 2019-05-31 16:10:00 and 2019-05-31 19:18:00. The events included records with hailstones measuring 8.86076923076923 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A vigorous shortwave trough and associated cold front moved across the area an interacted with a moist and unstable air mass to produce scattered storms. Multiple storms produced large hail and damaging wind across the area. A vigorous shortwave trough and associated cold front moved across the area an interacted with a moist and unstable air mass to produce scattered storms. Multiple storms produced large hail and damaging wind across the area. A vigorous shortwave trough and associated cold front moved across the area an interacted with a moist and unstable air mass to produce scattered storms. Multiple storms produced large hail and damaging wind across the area. A vigorous shortwave trough and associated cold front moved across the area an interacted with a moist and unstable air mass to produce scattered storms. Multiple storms produced large hail and damaging wind across the area. A vigorous shortwave trough and associated cold front moved across the area an interacted with a moist and unstable air mass to produce scattered storms. Multiple storms produced large hail and damaging wind across the area. A vigorous shortwave trough and associated cold front moved across the area an interacted with a moist and unstable air mass to produce scattered storms. Multiple storms produced large hail and damaging wind across the area. A vigorous shortwave trough and associated cold front moved across the area an interacted with a moist and unstable air mass to produce scattered storms. Multiple storms produced large hail and damaging wind across the area. A vigorous shortwave trough and associated cold front moved across the area an interacted with a moist and unstable air mass to produce scattered storms. Multiple storms produced large hail and damaging wind across the area. A vigorous shortwave trough and associated cold front moved across the area an interacted with a moist and unstable air mass to produce scattered storms. Multiple storms produced large hail and damaging wind across the area. A vigorous shortwave trough and associated cold front moved across the area an interacted with a moist and unstable air mass to produce scattered storms. Multiple storms produced large hail and damaging wind across the area. A vigorous shortwave trough and associated cold front moved across the area an interacted with a moist and unstable air mass to produce scattered storms. Multiple storms produced large hail and damaging wind across the area. A vigorous shortwave trough and associated cold front moved across the area an interacted with a moist and unstable air mass to produce scattered storms. Multiple storms produced large hail and damaging wind across the area. A vigorous shortwave trough and associated cold front moved across the area an interacted with a moist and unstable air mass to produce scattered storms. Multiple storms produced large hail and damaging wind across the area. A vigorous shortwave trough and associated cold front moved across the area an interacted with a moist and unstable air mass to produce scattered storms. Multiple storms produced large hail and damaging wind across the area. A vigorous shortwave trough and associated cold front moved across the area an interacted with a moist and unstable air mass to produce scattered storms. Multiple storms produced large hail and damaging wind across the area. A vigorous shortwave trough and associated cold front moved across the area an interacted with a moist and unstable air mass to produce scattered storms. Multiple storms produced large hail and damaging wind across the area. A vigorous shortwave trough and associated cold front moved across the area an interacted with a moist and unstable air mass to produce scattered storms. Multiple storms produced large hail and damaging wind across the area. A vigorous shortwave trough and associated cold front moved across the area an interacted with a moist and unstable air mass to produce scattered storms. Multiple storms produced large hail and damaging wind across the area. A vigorous shortwave trough and associated cold front moved across the area an interacted with a moist and unstable air mass to produce scattered storms. Multiple storms produced large hail and damaging wind across the area. A vigorous shortwave trough and associated cold front moved across the area an interacted with a moist and unstable air mass to produce scattered storms. Multiple storms produced large hail and damaging wind across the area. A vigorous shortwave trough and associated cold front moved across the area an interacted with a moist and unstable air mass to produce scattered storms. Multiple storms produced large hail and damaging wind across the area. A vigorous shortwave trough and associated cold front moved across the area an interacted with a moist and unstable air mass to produce scattered storms. Multiple storms produced large hail and damaging wind across the area. A vigorous shortwave trough and associated cold front moved across the area an interacted with a moist and unstable air mass to produce scattered storms. Multiple storms produced large hail and damaging wind across the area. A vigorous shortwave trough and associated cold front moved across the area an interacted with a moist and unstable air mass to produce scattered storms. Multiple storms produced large hail and damaging wind across the area. A vigorous shortwave trough and associated cold front moved across the area an interacted with a moist and unstable air mass to produce scattered storms. Multiple storms produced large hail and damaging wind across the area. A vigorous shortwave trough and associated cold front moved across the area an interacted with a moist and unstable air mass to produce scattered storms. Multiple storms produced large hail and damaging wind across the area.\nEvent Narrative:  Two inch diameter size hail was reported at Hunter Street and Highway 55.  Quarter size hail was reported near Russel Road.   Quarter size hail was reported near the intersection of Boxwood Court and Farmington Woods Drive. Ping Pong size hail was reported at Hillcrest Road and Lakeview Drive.   Dime to quarter size hail was reported near Avent Ferry Road and Tryon Road.       Penny size hail was reported at the intersection of Louisburg Road and Fox Road.  Quarter sized hail was reported along Stallings Road. A tree was reported down on Bluffridge Drive. A tree was reported down on Farnham Court. One tree was reported down near Pagan Road. One tree was reported down on Western Boulevard. Quarter size hail was reported on Zion Church Road. Half dollar to ping pong size hail was reported near the intersection of Olive Chapel Road and Winecott Drive.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 42.6668 km away, between 2019-06-05 15:20:00 and 2019-06-05 15:20:00. 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 severe storms developed across central and eastern portions of central North Carolina during the afternoon into the early evening hours in a warm, moist and unstable environment. Several storms in the line became severe and produced damaging winds and large hail.\nEvent Narrative: A large tree was reported down.",
+        "The following events were reported: Flash Flood. These occurred near station USW00013722, approximately 34.33 km away, between 2019-06-08 10:24:00 and 2019-06-08 14:30:00.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 stalled front over the region interacting with a very moist and slightly unstable atmosphere resulted in slow moving thunderstorms across central NC.  Two swaths of   |heavy rainfall of 3 to 5 inches over Cumberland County, northeastern Wake County and southern Franklin County, produced minor flash flooding. A stalled front over the region interacting with a very moist and slightly unstable atmosphere resulted in slow moving thunderstorms across central NC.  Two swaths of   |heavy rainfall of 3 to 5 inches over Cumberland County, northeastern Wake County and southern Franklin County, produced minor flash flooding. A stalled front over the region interacting with a very moist and slightly unstable atmosphere resulted in slow moving thunderstorms across central NC.  Two swaths of   |heavy rainfall of 3 to 5 inches over Cumberland County, northeastern Wake County and southern Franklin County, produced minor flash flooding. A stalled front over the region interacting with a very moist and slightly unstable atmosphere resulted in slow moving thunderstorms across central NC.  Two swaths of   |heavy rainfall of 3 to 5 inches over Cumberland County, northeastern Wake County and southern Franklin County, produced minor flash flooding.\nEvent Narrative: Multiple road closures due to flooding reported in Youngsville. Multiple road closures due to flooding reported in Franklinton. Severeral road closures due to flooding in the Rolesville area including Rogers Road, Mitchell Mill Road and Oscar Barham Road. Heavy rainfall of 7.30 INCHES over spilled the dam. Footbridge over the spill way was washed away.",
+        "The following events were reported: Flash Flood. These occurred near station USW00013722, approximately 28.1732 km away, between 2019-06-18 23:11:00 and 2019-06-19 00:38:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A line of training thunderstorms developed in a weakly sheared low level confluent zone. Moisture advection and convergence were maximized in that region as well. As a result, locally heavy rainfall produced by the thunderstorms produced some isolated flash flooding in northern Durham County.\nEvent Narrative: Bahama Road near Ball Road was closed due to flash flooding. The Department of Transportation also reported that North Roxboro Street near John Jones Road was impassable due to flooding.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 32.4581 km away, between 2019-06-20 13:51:00 and 2019-06-20 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 73000.0 and crop damage of 0.0. \n\nEpisode Narrative: A line of storms developed to the northwest of central North Carolina during the early afternoon associated with a strong mid level disturbance and associated cold front. The storms moved into central NC and interacted with a warm and unstable atmosphere and intensified and increased in coverage. A large percentage of the storms became severe and produced wind damage across central North Carolina. A line of storms developed to the northwest of central North Carolina during the early afternoon associated with a strong mid level disturbance and associated cold front. The storms moved into central NC and interacted with a warm and unstable atmosphere and intensified and increased in coverage. A large percentage of the storms became severe and produced wind damage across central North Carolina. A line of storms developed to the northwest of central North Carolina during the early afternoon associated with a strong mid level disturbance and associated cold front. The storms moved into central NC and interacted with a warm and unstable atmosphere and intensified and increased in coverage. A large percentage of the storms became severe and produced wind damage across central North Carolina. A line of storms developed to the northwest of central North Carolina during the early afternoon associated with a strong mid level disturbance and associated cold front. The storms moved into central NC and interacted with a warm and unstable atmosphere and intensified and increased in coverage. A large percentage of the storms became severe and produced wind damage across central North Carolina. A line of storms developed to the northwest of central North Carolina during the early afternoon associated with a strong mid level disturbance and associated cold front. The storms moved into central NC and interacted with a warm and unstable atmosphere and intensified and increased in coverage. A large percentage of the storms became severe and produced wind damage across central North Carolina. A line of storms developed to the northwest of central North Carolina during the early afternoon associated with a strong mid level disturbance and associated cold front. The storms moved into central NC and interacted with a warm and unstable atmosphere and intensified and increased in coverage. A large percentage of the storms became severe and produced wind damage across central North Carolina. A line of storms developed to the northwest of central North Carolina during the early afternoon associated with a strong mid level disturbance and associated cold front. The storms moved into central NC and interacted with a warm and unstable atmosphere and intensified and increased in coverage. A large percentage of the storms became severe and produced wind damage across central North Carolina. A line of storms developed to the northwest of central North Carolina during the early afternoon associated with a strong mid level disturbance and associated cold front. The storms moved into central NC and interacted with a warm and unstable atmosphere and intensified and increased in coverage. A large percentage of the storms became severe and produced wind damage across central North Carolina. A line of storms developed to the northwest of central North Carolina during the early afternoon associated with a strong mid level disturbance and associated cold front. The storms moved into central NC and interacted with a warm and unstable atmosphere and intensified and increased in coverage. A large percentage of the storms became severe and produced wind damage across central North Carolina. A line of storms developed to the northwest of central North Carolina during the early afternoon associated with a strong mid level disturbance and associated cold front. The storms moved into central NC and interacted with a warm and unstable atmosphere and intensified and increased in coverage. A large percentage of the storms became severe and produced wind damage across central North Carolina. A line of storms developed to the northwest of central North Carolina during the early afternoon associated with a strong mid level disturbance and associated cold front. The storms moved into central NC and interacted with a warm and unstable atmosphere and intensified and increased in coverage. A large percentage of the storms became severe and produced wind damage across central North Carolina. A line of storms developed to the northwest of central North Carolina during the early afternoon associated with a strong mid level disturbance and associated cold front. The storms moved into central NC and interacted with a warm and unstable atmosphere and intensified and increased in coverage. A large percentage of the storms became severe and produced wind damage across central North Carolina.\nEvent Narrative: A few trees were reported down near the intersection of Old Milburnie Road and Knightdale Boulevard. An 11 inch diameter tree was reported uprooted and across Shore Drive in Garner. One tree was reported down along Vandora Springs Road between North Hall Boulevard and Miriam Avenue. Two trees were reported down on Deep River Road near United States Highway 1. A tree was reported down on a house south of Hurdle Mills. A large tree was reported down on a hours on Chambers Loop Road near Riverbend Way. One tree was reported down on a house in the 1100 block of Chambers Loop Road. Power lines were reported down along East Franklin Street near the intersection with Plant Road. A large tree was reported down near the intersection of Bradshaw Quarry Road and Vernon Road. Multiple trees were reported down in downtown Durham. One tree was reported down on a house in Chapel Hill. Multiple trees were reported down from Butner to Creedmoor.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 20.6697 km away, between 2019-06-30 16:23:00 and 2019-06-30 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 175000.0 and crop damage of 0.0. \n\nEpisode Narrative: Isolated pulse severe storms developed during the late afternoon into early evenings in an environment characterized by a deep dry sub cloud layer with moderate instability, which yielded enhanced destructive downburst winds across portions of the Piedmont of central North Carolina. Isolated pulse severe storms developed during the late afternoon into early evenings in an environment characterized by a deep dry sub cloud layer with moderate instability, which yielded enhanced destructive downburst winds across portions of the Piedmont of central North Carolina. Isolated pulse severe storms developed during the late afternoon into early evenings in an environment characterized by a deep dry sub cloud layer with moderate instability, which yielded enhanced destructive downburst winds across portions of the Piedmont of central North Carolina. Isolated pulse severe storms developed during the late afternoon into early evenings in an environment characterized by a deep dry sub cloud layer with moderate instability, which yielded enhanced destructive downburst winds across portions of the Piedmont of central North Carolina. Isolated pulse severe storms developed during the late afternoon into early evenings in an environment characterized by a deep dry sub cloud layer with moderate instability, which yielded enhanced destructive downburst winds across portions of the Piedmont of central North Carolina. Isolated pulse severe storms developed during the late afternoon into early evenings in an environment characterized by a deep dry sub cloud layer with moderate instability, which yielded enhanced destructive downburst winds across portions of the Piedmont of central North Carolina.\nEvent Narrative: Multiple trees were reported down on White Oak Road off of Anderson Drive. A large tree was reported snapped off and fell on power lines and a car at Beechridge Road and Breeze Road. A tree and power lines were reported down on a car with a person inside at Drewry Lane and Anderson Drive. Two large trees were reported down along Poole Road near the intersection with Beverly Drive. One tree was approximately three feed in diameter and was uprooted alongside the westbound side of the road. The other tree was about two feet in diameter and was blown down. A tree that was two feet in diameter was uprooted and fell on a home at Beverly Drive and Bromley Street. Another tree that was two and a half feet in diameter was down across Bromley Street near Beverly Drive and fell into two power lines, which brought them down. Trees were reported down on power lines along Old United States Highway 70 near Pine Hollow Road.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 30.2413 km away, between 2019-07-04 13:00:00 and 2019-07-04 16:02:00. 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 77000.0 and crop damage of 0.0. \n\nEpisode Narrative: Scattered showers and thunderstorms developed across central North Carolina, primarily along differential heating boundaries, during peak heating as the moist atmosphere became moderately unstable. Several storms became severe, producing wind damage and isolated flash flooding. Scattered showers and thunderstorms developed across central North Carolina, primarily along differential heating boundaries, during peak heating as the moist atmosphere became moderately unstable. Several storms became severe, producing wind damage and isolated flash flooding. Scattered showers and thunderstorms developed across central North Carolina, primarily along differential heating boundaries, during peak heating as the moist atmosphere became moderately unstable. Several storms became severe, producing wind damage and isolated flash flooding. Scattered showers and thunderstorms developed across central North Carolina, primarily along differential heating boundaries, during peak heating as the moist atmosphere became moderately unstable. Several storms became severe, producing wind damage and isolated flash flooding.\nEvent Narrative: Several trees and power lines were blown down along a swath from Duncan to Holly Springs resulting in numerous power outages. Dime size hail also fell in Holly Springs. One tree was blown down onto a residence along Dacian Avenue in Durham. A lightning strike also resulted in a house fire near the 100 block of Presidents Drive. Numerous trees were blown down as a result of a downburst near the Cedar Grove area. A few of the trees damaged structures, including a house, a barn and several small outbuildings. A couple of trees were blown down along a swath from the intersection of Branch Road and Farmdale Road to the intersection of Bethlehem Road and Grasshopper Road, between Clayton and Knightdale.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 20.9452 km away, between 2019-07-11 18:13:00 and 2019-07-11 18:18:00. 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 4000.0 and crop damage of 0.0. \n\nEpisode Narrative: A line of showers and thunderstorms developed ahead of a cold front as it moved through central North Carolina. A few of the storms became severe, producing damaging winds. Persistent, training storms overnight produced heavy rain and resulted in localized flash flooding in the cities of Goldsboro and Smithfield. A line of showers and thunderstorms developed ahead of a cold front as it moved through central North Carolina. A few of the storms became severe, producing damaging winds. Persistent, training storms overnight produced heavy rain and resulted in localized flash flooding in the cities of Goldsboro and Smithfield.\nEvent Narrative: Power lines were blown down on Strickland Road, just west of Creedmoor Road. Multiple trees and tree limbs were blown down onto power lines near the intersection of White Oak Road and Hicks Road.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 7.9994 km away, between 2019-07-16 13:33:00 and 2019-07-16 13:33:00. 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 showers and thunderstorms developed along subtle surface boundaries within an environment of moderate instability, very poor shear and high Downdraft CAPE. One storm became severe, producing a microburst that resulted in isolated wind damage.\nEvent Narrative: A few trees were blown down in the Oak Park Community.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 44.0755 km away, between 2019-07-17 16:31:00 and 2019-07-17 23:00:00. 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 69000.0 and crop damage of 0.0. \n\nEpisode Narrative: Scattered showers and thunderstorms developed ahead of a surface front, containing the weak remnants of Barry, associated with a mid level trough as it moved into the central and southern Appalachians. A wet atmosphere with moderate instability and good low level lapse rates increased the chances for strong downbursts. A couple of storms became severe, producing downburst that resulted in scattered wind damage across Johnston county. Scattered showers and thunderstorms developed ahead of a surface front, containing the weak remnants of Barry, associated with a mid level trough as it moved into the central and southern Appalachians. A wet atmosphere with moderate instability and good low level lapse rates increased the chances for strong downbursts. A couple of storms became severe, producing downburst that resulted in scattered wind damage across Johnston county. Scattered showers and thunderstorms developed ahead of a surface front, containing the weak remnants of Barry, associated with a mid level trough as it moved into the central and southern Appalachians. A wet atmosphere with moderate instability and good low level lapse rates increased the chances for strong downbursts. A couple of storms became severe, producing downburst that resulted in scattered wind damage across Johnston county. Scattered showers and thunderstorms developed ahead of a surface front, containing the weak remnants of Barry, associated with a mid level trough as it moved into the central and southern Appalachians. A wet atmosphere with moderate instability and good low level lapse rates increased the chances for strong downbursts. A couple of storms became severe, producing downburst that resulted in scattered wind damage across Johnston county. Scattered showers and thunderstorms developed ahead of a surface front, containing the weak remnants of Barry, associated with a mid level trough as it moved into the central and southern Appalachians. A wet atmosphere with moderate instability and good low level lapse rates increased the chances for strong downbursts. A couple of storms became severe, producing downburst that resulted in scattered wind damage across Johnston county.\nEvent Narrative: A couple of trees were blown down near Coats Crossroads, one on NC-50 near Old Lee Road and the other on Interstate 40 at mile marker 317. A couple of trees were blown down between Coats Crossroads and Clayton, one at 93 Spaniel Lane and the other on Cleveland Road near North Shiloh Road. Numerous trees were blown down along Cleveland Road. At least six trees damaged structures on Hazelnut Lane, Brazil Nut Lane and Lee Trace Drive. Multiple trees were blown down onto power lines near the intersection of Twin Acres Road and Knights Bridge Drive. Several trees were blown down along a swath from 159 Strickland Road to Wilson's Mills Road. Multiple trees were blown down onto power lines. Additionally, the roof of a shed was blown off on Steel Bridge Road.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 38.4044 km away, between 2019-07-22 16:33:00 and 2019-07-22 19:42:00. 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: Severe thunderstorms developed across central NC, in advance of an amplifying upper level trough and attendant cold front moving into the region. A high DCAPE environment supported isolated to scattered wind damage with the strongest storm cells. Severe thunderstorms developed across central NC, in advance of an amplifying upper level trough and attendant cold front moving into the region. A high DCAPE environment supported isolated to scattered wind damage with the strongest storm cells. Severe thunderstorms developed across central NC, in advance of an amplifying upper level trough and attendant cold front moving into the region. A high DCAPE environment supported isolated to scattered wind damage with the strongest storm cells. Severe thunderstorms developed across central NC, in advance of an amplifying upper level trough and attendant cold front moving into the region. A high DCAPE environment supported isolated to scattered wind damage with the strongest storm cells. Severe thunderstorms developed across central NC, in advance of an amplifying upper level trough and attendant cold front moving into the region. A high DCAPE environment supported isolated to scattered wind damage with the strongest storm cells.\nEvent Narrative: Large tree limb fell onto power-lines, damaging the power pole. One tree reported down. Multiple trees and power-lines were reported down in the Timberlake area. Power-lines reported down along  NC Highway 56. Power-lines down in roadway.",
+        "The following events were reported: Thunderstorm Wind, Tornado. These occurred near station USW00013722, approximately 35.3053 km away, between 2019-07-23 13:00:00 and 2019-07-23 14:01:00.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: A cold front overtook a preceding outflow boundary and pre-frontal surface trough that was in place across central NC. Convection along the southward moving cold front organized into a QLCS as it intercepted the axis of strong diabatic heating and instability south of the front. Along with swaths of wind damage, two weak, short-lived tornadoes developed along the line. A cold front overtook a preceding outflow boundary and pre-frontal surface trough that was in place across central NC. Convection along the southward moving cold front organized into a QLCS as it intercepted the axis of strong diabatic heating and instability south of the front. Along with swaths of wind damage, two weak, short-lived tornadoes developed along the line. A cold front overtook a preceding outflow boundary and pre-frontal surface trough that was in place across central NC. Convection along the southward moving cold front organized into a QLCS as it intercepted the axis of strong diabatic heating and instability south of the front. Along with swaths of wind damage, two weak, short-lived tornadoes developed along the line. A cold front overtook a preceding outflow boundary and pre-frontal surface trough that was in place across central NC. Convection along the southward moving cold front organized into a QLCS as it intercepted the axis of strong diabatic heating and instability south of the front. Along with swaths of wind damage, two weak, short-lived tornadoes developed along the line.\nEvent Narrative: Several trees blown down along a wind swath, including downed trees on Badders Road, U.S. Highway 1, and Lower Moncure Road. Downed tree on power-lines at Highway 55 near W. Holly Springs Road. A brief tornado touched down in the community of Willow Springs. The damage consisted of  a combination of snapped and uprooted trees, minor siding damage to one home, and numerous fences blown down. Damage indicators suggested wind speeds of 75 to 85 mph. A brief tornado touched down in the Cleveland area, near the intersection of Cornwallis Road and Justin Drive and lifted near the intersection of Goldfield Drive and Justin Drive. Damage observed included minor shingle on several homes, numerous softwood trees snapped, and lawn furniture tossed a substantial distance. Damage indicators were consistent consistent with maximum wind speeds of 85 to 90 mph.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 19.6082 km away, between 2019-08-01 13:48:00 and 2019-08-01 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 10000.0 and crop damage of 0.0. \n\nEpisode Narrative: Scattered showers and thunderstorms developed in a moist, unstable environment during peak heating. Storms initially fired along differential heating boundaries, transitioning into multi-cell clusters with time. Several of the storms produced localized wind damage across central North Carolina. Scattered showers and thunderstorms developed in a moist, unstable environment during peak heating. Storms initially fired along differential heating boundaries, transitioning into multi-cell clusters with time. Several of the storms produced localized wind damage across central North Carolina.\nEvent Narrative: Two trees were blown down on Ward Road near Patrick Road, resulting in power outages. A tree also fell onto utility equipment near the intersection of East Whitaker Mill Road and Wake Forest Road. Several trees were blown down along Friar Tuck Road, a few of which damaged power lines and a fence.",
+        "The following events were reported: Flash Flood. These occurred near station USW00013722, approximately 13.3591 km away, between 2019-08-02 19:40:00 and 2019-08-02 21:55:00.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 few isolated thunderstorms developed along a stalled surface boundary in a very moist, slightly unstable environment. One nearly stationary storm developed over Wake County near the towns of Apex and Cary, resulting in flash flooding.\nEvent Narrative: Numerous roads were flooded throughout Apex and Cary. A weather observer measured 5.29 inches of rainfall near the intersection of Highway 55 and Highway 64. Flooded roads include; Jenks Road at West Williams Street, Highway 64 at West Williams Street, Olive Chapel Road near Pearson Farms, Kelly Road near Highway 64, High House Road between Cary Parkway and Davis Drive, James Jackson Avenue near Darrington Drive, and Cary Parkway at West High Street.",
+        "The following events were reported: Flash Flood. These occurred near station USW00013722, approximately 9.0306 km away, between 2019-08-05 15:45:00 and 2019-08-05 16:30:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A clusters of showers and storms moved across portions of the eastern Piedmont and Coastal Plain of central North Carolina during the late afternoon and early evening in a warm, moist and unstable atmosphere. Some of the clusters produced very heavy rainfall, which resulted in localized flash flooding. A clusters of showers and storms moved across portions of the eastern Piedmont and Coastal Plain of central North Carolina during the late afternoon and early evening in a warm, moist and unstable atmosphere. Some of the clusters produced very heavy rainfall, which resulted in localized flash flooding.\nEvent Narrative: Flash Flooding was reported near the intersection of Glenwood Avenue and Kodiak Drive. Flash flooding was reported on portions of Two Creeks Road between Lake Pine Drive and Cary Parkway.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 24.8711 km away, between 2019-08-07 23:10:00 and 2019-08-08 00:12:00. 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 18000.0 and crop damage of 0.0. \n\nEpisode Narrative: Scattered showers and thunderstorms developed across central North Carolina in a moderately unstable environment ahead of an approaching cold front. A strengthening mid-level shortwave increased shear in the low and middle layers of the atmosphere and resulted in strong low-level lapse rates. Consequently, several of the storms that developed during the afternoon and evening hours became severe, producing locally severe damaging wind gusts. Scattered showers and thunderstorms developed across central North Carolina in a moderately unstable environment ahead of an approaching cold front. A strengthening mid-level shortwave increased shear in the low and middle layers of the atmosphere and resulted in strong low-level lapse rates. Consequently, several of the storms that developed during the afternoon and evening hours became severe, producing locally severe damaging wind gusts. Scattered showers and thunderstorms developed across central North Carolina in a moderately unstable environment ahead of an approaching cold front. A strengthening mid-level shortwave increased shear in the low and middle layers of the atmosphere and resulted in strong low-level lapse rates. Consequently, several of the storms that developed during the afternoon and evening hours became severe, producing locally severe damaging wind gusts. Scattered showers and thunderstorms developed across central North Carolina in a moderately unstable environment ahead of an approaching cold front. A strengthening mid-level shortwave increased shear in the low and middle layers of the atmosphere and resulted in strong low-level lapse rates. Consequently, several of the storms that developed during the afternoon and evening hours became severe, producing locally severe damaging wind gusts. Scattered showers and thunderstorms developed across central North Carolina in a moderately unstable environment ahead of an approaching cold front. A strengthening mid-level shortwave increased shear in the low and middle layers of the atmosphere and resulted in strong low-level lapse rates. Consequently, several of the storms that developed during the afternoon and evening hours became severe, producing locally severe damaging wind gusts. Scattered showers and thunderstorms developed across central North Carolina in a moderately unstable environment ahead of an approaching cold front. A strengthening mid-level shortwave increased shear in the low and middle layers of the atmosphere and resulted in strong low-level lapse rates. Consequently, several of the storms that developed during the afternoon and evening hours became severe, producing locally severe damaging wind gusts.\nEvent Narrative: Several trees were blown down along US-70 between Garner and Clayton. One tree was blown down onto power lines near the intersection of Bethlehem Road and Interstate 87, resulting in power outages. One tree was blown down onto a residence at 113 Lucky Ribbon Lane in Twelve Oaks. One tree was blown down onto power lines and blocking both lanes of Kelly Road near the intersection with Apex Barbecue Road. Several trees and power lines were blown down along Kelly Road, three of which were near the intersection with Holland Road. A couple of trees were blown down along a swath parallel to Holly Springs Road from the intersection of Ten Ten Road and Megawood Court to the intersection of Holly Springs Road and Birkhaven Drive.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 40.172 km away, between 2019-08-13 14:59:00 and 2019-08-13 17:32:00. 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 18000.0 and crop damage of 0.0. \n\nEpisode Narrative: Scattered showers and thunderstorms developed along the remnant outflow of a mesoscale convective complex as it moved into central North Carolina ahead of an approaching cold front. Several storms became severe, producing localized wind damage. Scattered showers and thunderstorms developed along the remnant outflow of a mesoscale convective complex as it moved into central North Carolina ahead of an approaching cold front. Several storms became severe, producing localized wind damage. Scattered showers and thunderstorms developed along the remnant outflow of a mesoscale convective complex as it moved into central North Carolina ahead of an approaching cold front. Several storms became severe, producing localized wind damage.\nEvent Narrative: Several trees were blown down across roadways and onto power lines in and around the town of Franklinton. Power lines were blown down along Guy Road in Clayton. Several trees were blown down along a swath from Bushy Fork to Surl. One tree was blown down on Newton Pleasant Loop Road near Hesters Store Road. One tree was blown down on Thee Hester Road off Highway 158. Three trees were blown down near the intersection of Helena-Moriah Road and Malone Road. One final tree was blown down at Dink Ashley Road and River Oaks Parkway. Additionally, a power pole at Shiloh Church Road and Highway 501 was struck by lightning, splitting it in half and downing power lines onto the road.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 40.863 km away, between 2019-08-15 20:29:00 and 2019-08-15 20:40:00. 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 5000.0 and crop damage of 0.0. \n\nEpisode Narrative: Scattered late afternoon and evening showers and thunderstorms developed along a slow moving surface trough across eastern portions of central North Carolina in an unstable atmosphere. Some of the storms became severe and produced wind damage, including widespread wind damage around Benson, North Carolina. Scattered late afternoon and evening showers and thunderstorms developed along a slow moving surface trough across eastern portions of central North Carolina in an unstable atmosphere. Some of the storms became severe and produced wind damage, including widespread wind damage around Benson, North Carolina. Scattered late afternoon and evening showers and thunderstorms developed along a slow moving surface trough across eastern portions of central North Carolina in an unstable atmosphere. Some of the storms became severe and produced wind damage, including widespread wind damage around Benson, North Carolina.\nEvent Narrative: Trees were reported down on power lines along Highway 15 near May Farm Road. Multiple trees were reported down off of Moncure Pittsboro Road. One tree was reported down on John Robert Headen Road.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 47.6782 km away, between 2019-08-17 17:00:00 and 2019-08-17 17:00:00. 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 5000.0 and crop damage of 0.0. \n\nEpisode Narrative: A broken line of showers and storms, associated with a mid level disturbance, moved across central North Carolina during the afternoon. A few of the stronger storms produced wind damage across the northern Piedmont.\nEvent Narrative: Trees were reported down on power lines.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 23.1128 km away, between 2019-08-19 15:23:00 and 2019-08-19 16:00:00. 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 7000.0 and crop damage of 0.0. \n\nEpisode Narrative: Scattered to numerous showers and thunderstorms developed in a very warm, moist and unstable environment. Several thunderstorms became severe, producing scattered wind damage, isolated flash flooding and hail. Scattered to numerous showers and thunderstorms developed in a very warm, moist and unstable environment. Several thunderstorms became severe, producing scattered wind damage, isolated flash flooding and hail.\nEvent Narrative: Several trees were blown down across the city of Raleigh. The locations include one tree on Cabarrus Street near South East Street, one tree on Dorothea Drive near South Saunders Street, one tree at Woodburn Road near Hillsborough Street, and multiple trees in Dorothea Dix Park. Additionally, A dime-sized hail and a wind gust of 56 mph were reported at the National Weather Service office. A power line was blown down on Knightdale Boulevard near Rose of Sharon Road, causing major power outages.",
+        "The following events were reported: Lightning, Thunderstorm Wind. These occurred near station USW00013722, approximately 31.1873 km away, between 2019-08-21 17:57:00 and 2019-08-21 18:04:00.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 6500.0 and crop damage of 0.0. \n\nEpisode Narrative: Scattered afternoon showers and thunderstorms developed in the North Carolina and Virginia mountains and moved southeastward and developed into a line and moved into the northwest Piedmont of central North Carolina. The line of storms produced multiple reports of wind damage across the northwest Piedmont. Scattered afternoon showers and thunderstorms developed in the North Carolina and Virginia mountains and moved southeastward and developed into a line and moved into the northwest Piedmont of central North Carolina. The line of storms produced multiple reports of wind damage across the northwest Piedmont.\nEvent Narrative: A large tree was reported down on the 100 block of North Cameron Street. Lightning struck a traffic light box at the intersection of Homestead Road and Seawell School Road.",
+        "The following events were reported: Lightning, Thunderstorm Wind. These occurred near station USW00013722, approximately 26.6959 km away, between 2019-08-22 14:09:00 and 2019-08-22 18:30:00.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 106500.0 and crop damage of 0.0. \n\nEpisode Narrative: Multiple multi-cellular clusters of showers and storms moved across central North Carolina during the afternoon and evening. The strongest clusters produced wind damage and measured wind gust above 58 miles per hour. Multiple multi-cellular clusters of showers and storms moved across central North Carolina during the afternoon and evening. The strongest clusters produced wind damage and measured wind gust above 58 miles per hour. Multiple multi-cellular clusters of showers and storms moved across central North Carolina during the afternoon and evening. The strongest clusters produced wind damage and measured wind gust above 58 miles per hour. Multiple multi-cellular clusters of showers and storms moved across central North Carolina during the afternoon and evening. The strongest clusters produced wind damage and measured wind gust above 58 miles per hour. Multiple multi-cellular clusters of showers and storms moved across central North Carolina during the afternoon and evening. The strongest clusters produced wind damage and measured wind gust above 58 miles per hour. Multiple multi-cellular clusters of showers and storms moved across central North Carolina during the afternoon and evening. The strongest clusters produced wind damage and measured wind gust above 58 miles per hour. Multiple multi-cellular clusters of showers and storms moved across central North Carolina during the afternoon and evening. The strongest clusters produced wind damage and measured wind gust above 58 miles per hour.\nEvent Narrative: Two homes were struck by lightning near 7900 Mitchell Mill Road. Trees were reported down on power lines near the intersection of Highway 401 and Tarboro Road. Multiple trees and power lines were reported down in Pittsboro. Trees were reported down on power lines near the intersection of Fairview Road and Cambridge Road. A large tree was reported down at Brentwood Road and Julian Drive. Trees were reported down on power lines in Stony Hill. One tree was reported down on a vehicle at the 3100 block of Rogers Road.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 29.5279 km away, between 2019-10-31 18:40:00 and 2019-10-31 19:49:00. 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 52500.0 and crop damage of 0.0. \n\nEpisode Narrative: A line of strong to severe storms, in advance of a strong cold front, moved across central North Carolina during the late afternoon into evening. This resulted in numerous reports wind damage across western and northern portions of central North Carolina. A line of strong to severe storms, in advance of a strong cold front, moved across central North Carolina during the late afternoon into evening. This resulted in numerous reports wind damage across western and northern portions of central North Carolina. A line of strong to severe storms, in advance of a strong cold front, moved across central North Carolina during the late afternoon into evening. This resulted in numerous reports wind damage across western and northern portions of central North Carolina. A line of strong to severe storms, in advance of a strong cold front, moved across central North Carolina during the late afternoon into evening. This resulted in numerous reports wind damage across western and northern portions of central North Carolina. A line of strong to severe storms, in advance of a strong cold front, moved across central North Carolina during the late afternoon into evening. This resulted in numerous reports wind damage across western and northern portions of central North Carolina. A line of strong to severe storms, in advance of a strong cold front, moved across central North Carolina during the late afternoon into evening. This resulted in numerous reports wind damage across western and northern portions of central North Carolina. A line of strong to severe storms, in advance of a strong cold front, moved across central North Carolina during the late afternoon into evening. This resulted in numerous reports wind damage across western and northern portions of central North Carolina. A line of strong to severe storms, in advance of a strong cold front, moved across central North Carolina during the late afternoon into evening. This resulted in numerous reports wind damage across western and northern portions of central North Carolina.\nEvent Narrative: Trees were reported down on power lines on Highway 70. One tree was reported dwon on Dick Holeman Road. One tree was reported down on a mobile home on Mount Herman Church Road near Pleasant Green Road. One tree was reported down near the intersection of Leon Street and North Duke Street. Multiple trees were reported down on power lines near the intersection of Guess Road and Latta Road. Multiple tree were reported down across the county. One tree was reported down along Walters Road. A couple of trees were reported down near Lake Wheeler Road.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 23.0519 km away, between 2020-01-12 00:14:00 and 2020-01-12 00:24:00. 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 22500.0 and crop damage of 0.0. \n\nEpisode Narrative: A potent shortwave disturbance aloft and associated cold front allowed for the development of a damaging line of showers and storms. The prefrontal line moved across the area during the late evening and into the early morning hours, producing lots of wind damage. A potent shortwave disturbance aloft and associated cold front allowed for the development of a damaging line of showers and storms. The prefrontal line moved across the area during the late evening and into the early morning hours, producing lots of wind damage. A potent shortwave disturbance aloft and associated cold front allowed for the development of a damaging line of showers and storms. The prefrontal line moved across the area during the late evening and into the early morning hours, producing lots of wind damage.\nEvent Narrative: A tree was reported down on power lines near the intersection of Saddle Seat Drive at Western Boulevard. Trees were reported down on power lines near the intersection of Buck Jones Road at Norman Place. Trees were reported down on power lines along Price Hocutt Road.",
+        "The following events were reported: Flash Flood, Hail, Thunderstorm Wind. These occurred near station USW00013722, approximately 27.5221 km away, between 2020-02-06 12:40:00 and 2020-02-07 08:45:00. The events included records with hailstones measuring 42.47115384615385 inches.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 467000.0 and crop damage of 0.0. \n\nEpisode Narrative: A strong upper-level trough tracked eastward across North Carolina from the Gulf Coast states and brought heavy rain and severe weather. A warm front produced heavy rain and flash flooding along with the first round of severe weather during the early to mid afternoon. An assoiciated cold front and surface wave moved across the area during the mid to late afternoon and evening. This is when a line of strong to severe thunderstorms raced across the area, producing widespread damaging wind gusts. There were many reports of downed trees and power lines. A bow echo produced 80 to 100 mph straight line winds near Enfield and near Bunn, which snapped and uprooted trees and resulted in minor to moderate damage to numerous structures. In addition, two EF1 tornadoes were confirmed, one in Randolph County and one in Stanly County. A strong upper-level trough tracked eastward across North Carolina from the Gulf Coast states and brought heavy rain and severe weather. A warm front produced heavy rain and flash flooding along with the first round of severe weather during the early to mid afternoon. An assoiciated cold front and surface wave moved across the area during the mid to late afternoon and evening. This is when a line of strong to severe thunderstorms raced across the area, producing widespread damaging wind gusts. There were many reports of downed trees and power lines. A bow echo produced 80 to 100 mph straight line winds near Enfield and near Bunn, which snapped and uprooted trees and resulted in minor to moderate damage to numerous structures. In addition, two EF1 tornadoes were confirmed, one in Randolph County and one in Stanly County. A strong upper-level trough tracked eastward across North Carolina from the Gulf Coast states and brought heavy rain and severe weather. A warm front produced heavy rain and flash flooding along with the first round of severe weather during the early to mid afternoon. An assoiciated cold front and surface wave moved across the area during the mid to late afternoon and evening. This is when a line of strong to severe thunderstorms raced across the area, producing widespread damaging wind gusts. There were many reports of downed trees and power lines. A bow echo produced 80 to 100 mph straight line winds near Enfield and near Bunn, which snapped and uprooted trees and resulted in minor to moderate damage to numerous structures. In addition, two EF1 tornadoes were confirmed, one in Randolph County and one in Stanly County. A strong upper-level trough tracked eastward across North Carolina from the Gulf Coast states and brought heavy rain and severe weather. A warm front produced heavy rain and flash flooding along with the first round of severe weather during the early to mid afternoon. An assoiciated cold front and surface wave moved across the area during the mid to late afternoon and evening. This is when a line of strong to severe thunderstorms raced across the area, producing widespread damaging wind gusts. There were many reports of downed trees and power lines. A bow echo produced 80 to 100 mph straight line winds near Enfield and near Bunn, which snapped and uprooted trees and resulted in minor to moderate damage to numerous structures. In addition, two EF1 tornadoes were confirmed, one in Randolph County and one in Stanly County. A strong upper-level trough tracked eastward across North Carolina from the Gulf Coast states and brought heavy rain and severe weather. A warm front produced heavy rain and flash flooding along with the first round of severe weather during the early to mid afternoon. An assoiciated cold front and surface wave moved across the area during the mid to late afternoon and evening. This is when a line of strong to severe thunderstorms raced across the area, producing widespread damaging wind gusts. There were many reports of downed trees and power lines. A bow echo produced 80 to 100 mph straight line winds near Enfield and near Bunn, which snapped and uprooted trees and resulted in minor to moderate damage to numerous structures. In addition, two EF1 tornadoes were confirmed, one in Randolph County and one in Stanly County. A strong upper-level trough tracked eastward across North Carolina from the Gulf Coast states and brought heavy rain and severe weather. A warm front produced heavy rain and flash flooding along with the first round of severe weather during the early to mid afternoon. An assoiciated cold front and surface wave moved across the area during the mid to late afternoon and evening. This is when a line of strong to severe thunderstorms raced across the area, producing widespread damaging wind gusts. There were many reports of downed trees and power lines. A bow echo produced 80 to 100 mph straight line winds near Enfield and near Bunn, which snapped and uprooted trees and resulted in minor to moderate damage to numerous structures. In addition, two EF1 tornadoes were confirmed, one in Randolph County and one in Stanly County. A strong upper-level trough tracked eastward across North Carolina from the Gulf Coast states and brought heavy rain and severe weather. A warm front produced heavy rain and flash flooding along with the first round of severe weather during the early to mid afternoon. An assoiciated cold front and surface wave moved across the area during the mid to late afternoon and evening. This is when a line of strong to severe thunderstorms raced across the area, producing widespread damaging wind gusts. There were many reports of downed trees and power lines. A bow echo produced 80 to 100 mph straight line winds near Enfield and near Bunn, which snapped and uprooted trees and resulted in minor to moderate damage to numerous structures. In addition, two EF1 tornadoes were confirmed, one in Randolph County and one in Stanly County. A strong upper-level trough tracked eastward across North Carolina from the Gulf Coast states and brought heavy rain and severe weather. A warm front produced heavy rain and flash flooding along with the first round of severe weather during the early to mid afternoon. An assoiciated cold front and surface wave moved across the area during the mid to late afternoon and evening. This is when a line of strong to severe thunderstorms raced across the area, producing widespread damaging wind gusts. There were many reports of downed trees and power lines. A bow echo produced 80 to 100 mph straight line winds near Enfield and near Bunn, which snapped and uprooted trees and resulted in minor to moderate damage to numerous structures. In addition, two EF1 tornadoes were confirmed, one in Randolph County and one in Stanly County. A strong upper-level trough tracked eastward across North Carolina from the Gulf Coast states and brought heavy rain and severe weather. A warm front produced heavy rain and flash flooding along with the first round of severe weather during the early to mid afternoon. An assoiciated cold front and surface wave moved across the area during the mid to late afternoon and evening. This is when a line of strong to severe thunderstorms raced across the area, producing widespread damaging wind gusts. There were many reports of downed trees and power lines. A bow echo produced 80 to 100 mph straight line winds near Enfield and near Bunn, which snapped and uprooted trees and resulted in minor to moderate damage to numerous structures. In addition, two EF1 tornadoes were confirmed, one in Randolph County and one in Stanly County. A strong upper-level trough tracked eastward across North Carolina from the Gulf Coast states and brought heavy rain and severe weather. A warm front produced heavy rain and flash flooding along with the first round of severe weather during the early to mid afternoon. An assoiciated cold front and surface wave moved across the area during the mid to late afternoon and evening. This is when a line of strong to severe thunderstorms raced across the area, producing widespread damaging wind gusts. There were many reports of downed trees and power lines. A bow echo produced 80 to 100 mph straight line winds near Enfield and near Bunn, which snapped and uprooted trees and resulted in minor to moderate damage to numerous structures. In addition, two EF1 tornadoes were confirmed, one in Randolph County and one in Stanly County. A strong upper-level trough tracked eastward across North Carolina from the Gulf Coast states and brought heavy rain and severe weather. A warm front produced heavy rain and flash flooding along with the first round of severe weather during the early to mid afternoon. An assoiciated cold front and surface wave moved across the area during the mid to late afternoon and evening. This is when a line of strong to severe thunderstorms raced across the area, producing widespread damaging wind gusts. There were many reports of downed trees and power lines. A bow echo produced 80 to 100 mph straight line winds near Enfield and near Bunn, which snapped and uprooted trees and resulted in minor to moderate damage to numerous structures. In addition, two EF1 tornadoes were confirmed, one in Randolph County and one in Stanly County. A strong upper-level trough tracked eastward across North Carolina from the Gulf Coast states and brought heavy rain and severe weather. A warm front produced heavy rain and flash flooding along with the first round of severe weather during the early to mid afternoon. An assoiciated cold front and surface wave moved across the area during the mid to late afternoon and evening. This is when a line of strong to severe thunderstorms raced across the area, producing widespread damaging wind gusts. There were many reports of downed trees and power lines. A bow echo produced 80 to 100 mph straight line winds near Enfield and near Bunn, which snapped and uprooted trees and resulted in minor to moderate damage to numerous structures. In addition, two EF1 tornadoes were confirmed, one in Randolph County and one in Stanly County. A strong upper-level trough tracked eastward across North Carolina from the Gulf Coast states and brought heavy rain and severe weather. A warm front produced heavy rain and flash flooding along with the first round of severe weather during the early to mid afternoon. An assoiciated cold front and surface wave moved across the area during the mid to late afternoon and evening. This is when a line of strong to severe thunderstorms raced across the area, producing widespread damaging wind gusts. There were many reports of downed trees and power lines. A bow echo produced 80 to 100 mph straight line winds near Enfield and near Bunn, which snapped and uprooted trees and resulted in minor to moderate damage to numerous structures. In addition, two EF1 tornadoes were confirmed, one in Randolph County and one in Stanly County. A strong upper-level trough tracked eastward across North Carolina from the Gulf Coast states and brought heavy rain and severe weather. A warm front produced heavy rain and flash flooding along with the first round of severe weather during the early to mid afternoon. An assoiciated cold front and surface wave moved across the area during the mid to late afternoon and evening. This is when a line of strong to severe thunderstorms raced across the area, producing widespread damaging wind gusts. There were many reports of downed trees and power lines. A bow echo produced 80 to 100 mph straight line winds near Enfield and near Bunn, which snapped and uprooted trees and resulted in minor to moderate damage to numerous structures. In addition, two EF1 tornadoes were confirmed, one in Randolph County and one in Stanly County. A strong upper-level trough tracked eastward across North Carolina from the Gulf Coast states and brought heavy rain and severe weather. A warm front produced heavy rain and flash flooding along with the first round of severe weather during the early to mid afternoon. An assoiciated cold front and surface wave moved across the area during the mid to late afternoon and evening. This is when a line of strong to severe thunderstorms raced across the area, producing widespread damaging wind gusts. There were many reports of downed trees and power lines. A bow echo produced 80 to 100 mph straight line winds near Enfield and near Bunn, which snapped and uprooted trees and resulted in minor to moderate damage to numerous structures. In addition, two EF1 tornadoes were confirmed, one in Randolph County and one in Stanly County. A strong upper-level trough tracked eastward across North Carolina from the Gulf Coast states and brought heavy rain and severe weather. A warm front produced heavy rain and flash flooding along with the first round of severe weather during the early to mid afternoon. An assoiciated cold front and surface wave moved across the area during the mid to late afternoon and evening. This is when a line of strong to severe thunderstorms raced across the area, producing widespread damaging wind gusts. There were many reports of downed trees and power lines. A bow echo produced 80 to 100 mph straight line winds near Enfield and near Bunn, which snapped and uprooted trees and resulted in minor to moderate damage to numerous structures. In addition, two EF1 tornadoes were confirmed, one in Randolph County and one in Stanly County. A strong upper-level trough tracked eastward across North Carolina from the Gulf Coast states and brought heavy rain and severe weather. A warm front produced heavy rain and flash flooding along with the first round of severe weather during the early to mid afternoon. An assoiciated cold front and surface wave moved across the area during the mid to late afternoon and evening. This is when a line of strong to severe thunderstorms raced across the area, producing widespread damaging wind gusts. There were many reports of downed trees and power lines. A bow echo produced 80 to 100 mph straight line winds near Enfield and near Bunn, which snapped and uprooted trees and resulted in minor to moderate damage to numerous structures. In addition, two EF1 tornadoes were confirmed, one in Randolph County and one in Stanly County. A strong upper-level trough tracked eastward across North Carolina from the Gulf Coast states and brought heavy rain and severe weather. A warm front produced heavy rain and flash flooding along with the first round of severe weather during the early to mid afternoon. An assoiciated cold front and surface wave moved across the area during the mid to late afternoon and evening. This is when a line of strong to severe thunderstorms raced across the area, producing widespread damaging wind gusts. There were many reports of downed trees and power lines. A bow echo produced 80 to 100 mph straight line winds near Enfield and near Bunn, which snapped and uprooted trees and resulted in minor to moderate damage to numerous structures. In addition, two EF1 tornadoes were confirmed, one in Randolph County and one in Stanly County. A strong upper-level trough tracked eastward across North Carolina from the Gulf Coast states and brought heavy rain and severe weather. A warm front produced heavy rain and flash flooding along with the first round of severe weather during the early to mid afternoon. An assoiciated cold front and surface wave moved across the area during the mid to late afternoon and evening. This is when a line of strong to severe thunderstorms raced across the area, producing widespread damaging wind gusts. There were many reports of downed trees and power lines. A bow echo produced 80 to 100 mph straight line winds near Enfield and near Bunn, which snapped and uprooted trees and resulted in minor to moderate damage to numerous structures. In addition, two EF1 tornadoes were confirmed, one in Randolph County and one in Stanly County. A strong upper-level trough tracked eastward across North Carolina from the Gulf Coast states and brought heavy rain and severe weather. A warm front produced heavy rain and flash flooding along with the first round of severe weather during the early to mid afternoon. An assoiciated cold front and surface wave moved across the area during the mid to late afternoon and evening. This is when a line of strong to severe thunderstorms raced across the area, producing widespread damaging wind gusts. There were many reports of downed trees and power lines. A bow echo produced 80 to 100 mph straight line winds near Enfield and near Bunn, which snapped and uprooted trees and resulted in minor to moderate damage to numerous structures. In addition, two EF1 tornadoes were confirmed, one in Randolph County and one in Stanly County. A strong upper-level trough tracked eastward across North Carolina from the Gulf Coast states and brought heavy rain and severe weather. A warm front produced heavy rain and flash flooding along with the first round of severe weather during the early to mid afternoon. An assoiciated cold front and surface wave moved across the area during the mid to late afternoon and evening. This is when a line of strong to severe thunderstorms raced across the area, producing widespread damaging wind gusts. There were many reports of downed trees and power lines. A bow echo produced 80 to 100 mph straight line winds near Enfield and near Bunn, which snapped and uprooted trees and resulted in minor to moderate damage to numerous structures. In addition, two EF1 tornadoes were confirmed, one in Randolph County and one in Stanly County. A strong upper-level trough tracked eastward across North Carolina from the Gulf Coast states and brought heavy rain and severe weather. A warm front produced heavy rain and flash flooding along with the first round of severe weather during the early to mid afternoon. An assoiciated cold front and surface wave moved across the area during the mid to late afternoon and evening. This is when a line of strong to severe thunderstorms raced across the area, producing widespread damaging wind gusts. There were many reports of downed trees and power lines. A bow echo produced 80 to 100 mph straight line winds near Enfield and near Bunn, which snapped and uprooted trees and resulted in minor to moderate damage to numerous structures. In addition, two EF1 tornadoes were confirmed, one in Randolph County and one in Stanly County. A strong upper-level trough tracked eastward across North Carolina from the Gulf Coast states and brought heavy rain and severe weather. A warm front produced heavy rain and flash flooding along with the first round of severe weather during the early to mid afternoon. An assoiciated cold front and surface wave moved across the area during the mid to late afternoon and evening. This is when a line of strong to severe thunderstorms raced across the area, producing widespread damaging wind gusts. There were many reports of downed trees and power lines. A bow echo produced 80 to 100 mph straight line winds near Enfield and near Bunn, which snapped and uprooted trees and resulted in minor to moderate damage to numerous structures. In addition, two EF1 tornadoes were confirmed, one in Randolph County and one in Stanly County. A strong upper-level trough tracked eastward across North Carolina from the Gulf Coast states and brought heavy rain and severe weather. A warm front produced heavy rain and flash flooding along with the first round of severe weather during the early to mid afternoon. An assoiciated cold front and surface wave moved across the area during the mid to late afternoon and evening. This is when a line of strong to severe thunderstorms raced across the area, producing widespread damaging wind gusts. There were many reports of downed trees and power lines. A bow echo produced 80 to 100 mph straight line winds near Enfield and near Bunn, which snapped and uprooted trees and resulted in minor to moderate damage to numerous structures. In addition, two EF1 tornadoes were confirmed, one in Randolph County and one in Stanly County. A strong upper-level trough tracked eastward across North Carolina from the Gulf Coast states and brought heavy rain and severe weather. A warm front produced heavy rain and flash flooding along with the first round of severe weather during the early to mid afternoon. An assoiciated cold front and surface wave moved across the area during the mid to late afternoon and evening. This is when a line of strong to severe thunderstorms raced across the area, producing widespread damaging wind gusts. There were many reports of downed trees and power lines. A bow echo produced 80 to 100 mph straight line winds near Enfield and near Bunn, which snapped and uprooted trees and resulted in minor to moderate damage to numerous structures. In addition, two EF1 tornadoes were confirmed, one in Randolph County and one in Stanly County. A strong upper-level trough tracked eastward across North Carolina from the Gulf Coast states and brought heavy rain and severe weather. A warm front produced heavy rain and flash flooding along with the first round of severe weather during the early to mid afternoon. An assoiciated cold front and surface wave moved across the area during the mid to late afternoon and evening. This is when a line of strong to severe thunderstorms raced across the area, producing widespread damaging wind gusts. There were many reports of downed trees and power lines. A bow echo produced 80 to 100 mph straight line winds near Enfield and near Bunn, which snapped and uprooted trees and resulted in minor to moderate damage to numerous structures. In addition, two EF1 tornadoes were confirmed, one in Randolph County and one in Stanly County. A strong upper-level trough tracked eastward across North Carolina from the Gulf Coast states and brought heavy rain and severe weather. A warm front produced heavy rain and flash flooding along with the first round of severe weather during the early to mid afternoon. An assoiciated cold front and surface wave moved across the area during the mid to late afternoon and evening. This is when a line of strong to severe thunderstorms raced across the area, producing widespread damaging wind gusts. There were many reports of downed trees and power lines. A bow echo produced 80 to 100 mph straight line winds near Enfield and near Bunn, which snapped and uprooted trees and resulted in minor to moderate damage to numerous structures. In addition, two EF1 tornadoes were confirmed, one in Randolph County and one in Stanly County. A strong upper-level trough tracked eastward across North Carolina from the Gulf Coast states and brought heavy rain and severe weather. A warm front produced heavy rain and flash flooding along with the first round of severe weather during the early to mid afternoon. An assoiciated cold front and surface wave moved across the area during the mid to late afternoon and evening. This is when a line of strong to severe thunderstorms raced across the area, producing widespread damaging wind gusts. There were many reports of downed trees and power lines. A bow echo produced 80 to 100 mph straight line winds near Enfield and near Bunn, which snapped and uprooted trees and resulted in minor to moderate damage to numerous structures. In addition, two EF1 tornadoes were confirmed, one in Randolph County and one in Stanly County. A strong upper-level trough tracked eastward across North Carolina from the Gulf Coast states and brought heavy rain and severe weather. A warm front produced heavy rain and flash flooding along with the first round of severe weather during the early to mid afternoon. An assoiciated cold front and surface wave moved across the area during the mid to late afternoon and evening. This is when a line of strong to severe thunderstorms raced across the area, producing widespread damaging wind gusts. There were many reports of downed trees and power lines. A bow echo produced 80 to 100 mph straight line winds near Enfield and near Bunn, which snapped and uprooted trees and resulted in minor to moderate damage to numerous structures. In addition, two EF1 tornadoes were confirmed, one in Randolph County and one in Stanly County.\nEvent Narrative: Two foot in diameter trees were report down near the intersection of Barham Siding Road and Zebulon Road. Numerous large trees were reported down in and around Vandemere Court and Selfridge Court and Coldstream Court. Structural damage was reported to several warehouses, including several air conditioning units getting ripped off from the buildings. Power poles were reported snapped near the intersection of Lake Wheeler Road and Tryon Road. Several trees were reported down in the Summerfield North Subdivision. Glenwood Avenue was reported flooded due to high water near the Five Points area.  A swath of damage was reported east of Rolesville near Pulley Town Road and continued eastward to near the Wake and Franklin County Line. Numerous pines trees were reported down or snapped off, barns and outbuildings were tossed or destroyed, and damage to fencing. Trees were reported down on power lines near the 4400 block of Zebulon Road. Multiple trees were reported down on Castalia Drive. Power lines were reported down near the intersection of Mitchell Mill Road and Highway 96. A large tree was reported down off of Rooksley court. Several trees were reported down off of Mc Wilder Road. Several trees were reported down near Hillsborough. Numerous trees were reported down across Alamance County. Two trees were reported down near Moncure. Numerous trees were reported down on power lines near Moncure. Numerous trees were reported down on power lines along Mount Carmel Church Road. Several trees were reported down near Bynum Ridge Road. Quarter size hail was reported at Wellington Court.   One tree was reported down near the intersection of Forestville Road and Burlington Mills Road. A backyard playground set was reported to be picked up and tossed around 45 feet. This destroyed the playground set. Numerous trees were reported down on power lines along Mount Carmel Church Road. Crabtree Creek at Old Wake Forecast Road crested above flood stage at 14.18 feet. One tree was reported down near the intersection of South Franklin Street and Holding Road. One tree was reported down across a driveway along Wait Street. A couple of road were reported flooded in the town of Holly Springs, including Old Holly Springs Apex Road at the Little Branch Bridge and along Rex Road in between People Road and Avent Ferry Road.",
+        "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00013722, approximately 32.9123 km away, between 2020-04-08 16:57:00 and 2020-04-08 19:07:00. The events included records with hailstones measuring 14.285454545454543 inches.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: The combination of warm moist air and the passage of a mid level disturbance from the northwest produced multiple clusters and line segments of strong to severe storms moving across northern portions of central North Carolina during the late afternoon into the evening. The storms produced multiple reports of wind damage, large hail and one measured wind gusts of 58 mile per hour. The combination of warm moist air and the passage of a mid level disturbance from the northwest produced multiple clusters and line segments of strong to severe storms moving across northern portions of central North Carolina during the late afternoon into the evening. The storms produced multiple reports of wind damage, large hail and one measured wind gusts of 58 mile per hour. The combination of warm moist air and the passage of a mid level disturbance from the northwest produced multiple clusters and line segments of strong to severe storms moving across northern portions of central North Carolina during the late afternoon into the evening. The storms produced multiple reports of wind damage, large hail and one measured wind gusts of 58 mile per hour. The combination of warm moist air and the passage of a mid level disturbance from the northwest produced multiple clusters and line segments of strong to severe storms moving across northern portions of central North Carolina during the late afternoon into the evening. The storms produced multiple reports of wind damage, large hail and one measured wind gusts of 58 mile per hour. The combination of warm moist air and the passage of a mid level disturbance from the northwest produced multiple clusters and line segments of strong to severe storms moving across northern portions of central North Carolina during the late afternoon into the evening. The storms produced multiple reports of wind damage, large hail and one measured wind gusts of 58 mile per hour. The combination of warm moist air and the passage of a mid level disturbance from the northwest produced multiple clusters and line segments of strong to severe storms moving across northern portions of central North Carolina during the late afternoon into the evening. The storms produced multiple reports of wind damage, large hail and one measured wind gusts of 58 mile per hour. The combination of warm moist air and the passage of a mid level disturbance from the northwest produced multiple clusters and line segments of strong to severe storms moving across northern portions of central North Carolina during the late afternoon into the evening. The storms produced multiple reports of wind damage, large hail and one measured wind gusts of 58 mile per hour. The combination of warm moist air and the passage of a mid level disturbance from the northwest produced multiple clusters and line segments of strong to severe storms moving across northern portions of central North Carolina during the late afternoon into the evening. The storms produced multiple reports of wind damage, large hail and one measured wind gusts of 58 mile per hour. The combination of warm moist air and the passage of a mid level disturbance from the northwest produced multiple clusters and line segments of strong to severe storms moving across northern portions of central North Carolina during the late afternoon into the evening. The storms produced multiple reports of wind damage, large hail and one measured wind gusts of 58 mile per hour. The combination of warm moist air and the passage of a mid level disturbance from the northwest produced multiple clusters and line segments of strong to severe storms moving across northern portions of central North Carolina during the late afternoon into the evening. The storms produced multiple reports of wind damage, large hail and one measured wind gusts of 58 mile per hour. The combination of warm moist air and the passage of a mid level disturbance from the northwest produced multiple clusters and line segments of strong to severe storms moving across northern portions of central North Carolina during the late afternoon into the evening. The storms produced multiple reports of wind damage, large hail and one measured wind gusts of 58 mile per hour.\nEvent Narrative:  Quarter size hail was reported at North Carolina Highway 56 and Birch Drive.   Nickel size hail was reported at Rogers Road and Highway 401.  Nickel to quarter size hail was reported at Rogers Lane and New Bern Avenue. Nickel size hail was reported near the interchange of Interstate 40 and North Carolina Highway 42. One tree was reported down in the 2200 block of Clay Long Road. One tree was reported down on Hopkins Trace Lane. Two trees were reported down behind a residence near Rogers Lane and New Bern Avenue.",
+        "The following events were reported: Thunderstorm Wind, Tornado. These occurred near station USW00013722, approximately 31.6738 km away, between 2020-04-13 05:25:00 and 2020-04-13 06:55:00.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 786500.0 and crop damage of 0.0. \n\nEpisode Narrative: Multiple clusters of strong to severe storms moved across central North Carolina in advance of a strong cold front during the morning hours. The storms caused numerous reports of wind damages, including multiple measured wind gusts in excess of 58 miles per hour. Some of the trees fell on homes causing significant damage and one fatality in Davidson County. Three tornadoes touch down during the early morning hours, resulting in numerous trees snapped and uprooted and structural damage. Multiple clusters of strong to severe storms moved across central North Carolina in advance of a strong cold front during the morning hours. The storms caused numerous reports of wind damages, including multiple measured wind gusts in excess of 58 miles per hour. Some of the trees fell on homes causing significant damage and one fatality in Davidson County. Three tornadoes touch down during the early morning hours, resulting in numerous trees snapped and uprooted and structural damage. Multiple clusters of strong to severe storms moved across central North Carolina in advance of a strong cold front during the morning hours. The storms caused numerous reports of wind damages, including multiple measured wind gusts in excess of 58 miles per hour. Some of the trees fell on homes causing significant damage and one fatality in Davidson County. Three tornadoes touch down during the early morning hours, resulting in numerous trees snapped and uprooted and structural damage. Multiple clusters of strong to severe storms moved across central North Carolina in advance of a strong cold front during the morning hours. The storms caused numerous reports of wind damages, including multiple measured wind gusts in excess of 58 miles per hour. Some of the trees fell on homes causing significant damage and one fatality in Davidson County. Three tornadoes touch down during the early morning hours, resulting in numerous trees snapped and uprooted and structural damage. Multiple clusters of strong to severe storms moved across central North Carolina in advance of a strong cold front during the morning hours. The storms caused numerous reports of wind damages, including multiple measured wind gusts in excess of 58 miles per hour. Some of the trees fell on homes causing significant damage and one fatality in Davidson County. Three tornadoes touch down during the early morning hours, resulting in numerous trees snapped and uprooted and structural damage. Multiple clusters of strong to severe storms moved across central North Carolina in advance of a strong cold front during the morning hours. The storms caused numerous reports of wind damages, including multiple measured wind gusts in excess of 58 miles per hour. Some of the trees fell on homes causing significant damage and one fatality in Davidson County. Three tornadoes touch down during the early morning hours, resulting in numerous trees snapped and uprooted and structural damage. Multiple clusters of strong to severe storms moved across central North Carolina in advance of a strong cold front during the morning hours. The storms caused numerous reports of wind damages, including multiple measured wind gusts in excess of 58 miles per hour. Some of the trees fell on homes causing significant damage and one fatality in Davidson County. Three tornadoes touch down during the early morning hours, resulting in numerous trees snapped and uprooted and structural damage. Multiple clusters of strong to severe storms moved across central North Carolina in advance of a strong cold front during the morning hours. The storms caused numerous reports of wind damages, including multiple measured wind gusts in excess of 58 miles per hour. Some of the trees fell on homes causing significant damage and one fatality in Davidson County. Three tornadoes touch down during the early morning hours, resulting in numerous trees snapped and uprooted and structural damage. Multiple clusters of strong to severe storms moved across central North Carolina in advance of a strong cold front during the morning hours. The storms caused numerous reports of wind damages, including multiple measured wind gusts in excess of 58 miles per hour. Some of the trees fell on homes causing significant damage and one fatality in Davidson County. Three tornadoes touch down during the early morning hours, resulting in numerous trees snapped and uprooted and structural damage. Multiple clusters of strong to severe storms moved across central North Carolina in advance of a strong cold front during the morning hours. The storms caused numerous reports of wind damages, including multiple measured wind gusts in excess of 58 miles per hour. Some of the trees fell on homes causing significant damage and one fatality in Davidson County. Three tornadoes touch down during the early morning hours, resulting in numerous trees snapped and uprooted and structural damage. Multiple clusters of strong to severe storms moved across central North Carolina in advance of a strong cold front during the morning hours. The storms caused numerous reports of wind damages, including multiple measured wind gusts in excess of 58 miles per hour. Some of the trees fell on homes causing significant damage and one fatality in Davidson County. Three tornadoes touch down during the early morning hours, resulting in numerous trees snapped and uprooted and structural damage. Multiple clusters of strong to severe storms moved across central North Carolina in advance of a strong cold front during the morning hours. The storms caused numerous reports of wind damages, including multiple measured wind gusts in excess of 58 miles per hour. Some of the trees fell on homes causing significant damage and one fatality in Davidson County. Three tornadoes touch down during the early morning hours, resulting in numerous trees snapped and uprooted and structural damage. Multiple clusters of strong to severe storms moved across central North Carolina in advance of a strong cold front during the morning hours. The storms caused numerous reports of wind damages, including multiple measured wind gusts in excess of 58 miles per hour. Some of the trees fell on homes causing significant damage and one fatality in Davidson County. Three tornadoes touch down during the early morning hours, resulting in numerous trees snapped and uprooted and structural damage. Multiple clusters of strong to severe storms moved across central North Carolina in advance of a strong cold front during the morning hours. The storms caused numerous reports of wind damages, including multiple measured wind gusts in excess of 58 miles per hour. Some of the trees fell on homes causing significant damage and one fatality in Davidson County. Three tornadoes touch down during the early morning hours, resulting in numerous trees snapped and uprooted and structural damage. Multiple clusters of strong to severe storms moved across central North Carolina in advance of a strong cold front during the morning hours. The storms caused numerous reports of wind damages, including multiple measured wind gusts in excess of 58 miles per hour. Some of the trees fell on homes causing significant damage and one fatality in Davidson County. Three tornadoes touch down during the early morning hours, resulting in numerous trees snapped and uprooted and structural damage. Multiple clusters of strong to severe storms moved across central North Carolina in advance of a strong cold front during the morning hours. The storms caused numerous reports of wind damages, including multiple measured wind gusts in excess of 58 miles per hour. Some of the trees fell on homes causing significant damage and one fatality in Davidson County. Three tornadoes touch down during the early morning hours, resulting in numerous trees snapped and uprooted and structural damage. Multiple clusters of strong to severe storms moved across central North Carolina in advance of a strong cold front during the morning hours. The storms caused numerous reports of wind damages, including multiple measured wind gusts in excess of 58 miles per hour. Some of the trees fell on homes causing significant damage and one fatality in Davidson County. Three tornadoes touch down during the early morning hours, resulting in numerous trees snapped and uprooted and structural damage. Multiple clusters of strong to severe storms moved across central North Carolina in advance of a strong cold front during the morning hours. The storms caused numerous reports of wind damages, including multiple measured wind gusts in excess of 58 miles per hour. Some of the trees fell on homes causing significant damage and one fatality in Davidson County. Three tornadoes touch down during the early morning hours, resulting in numerous trees snapped and uprooted and structural damage. Multiple clusters of strong to severe storms moved across central North Carolina in advance of a strong cold front during the morning hours. The storms caused numerous reports of wind damages, including multiple measured wind gusts in excess of 58 miles per hour. Some of the trees fell on homes causing significant damage and one fatality in Davidson County. Three tornadoes touch down during the early morning hours, resulting in numerous trees snapped and uprooted and structural damage. Multiple clusters of strong to severe storms moved across central North Carolina in advance of a strong cold front during the morning hours. The storms caused numerous reports of wind damages, including multiple measured wind gusts in excess of 58 miles per hour. Some of the trees fell on homes causing significant damage and one fatality in Davidson County. Three tornadoes touch down during the early morning hours, resulting in numerous trees snapped and uprooted and structural damage.\nEvent Narrative: Trees were reported down on a mobile home, causing significant damage near Calloway Drive. Trees were reported down on power lines near the intersection of North Carolina Highway 57 and Guess Road. One tree was reported down near Old Graham Road. A tree was reported down near Manns Chapel Road. A power pole was snapped off on Ode Turner Road. Trees were reported down near the intersection of United States Highway 70 and Lawrence Road. Pine trees were uprooted near Bivins Road. Trees were reported down near Interstate 85 and Glenn School Road. Severe wind gusts reported at the Lake Wheeler econet station. Trees were reported down near Jack Clement Road. Numerous trees were reported down along Lake Wheeler Raod, between Simpkins Road and Optimist Farm Road. Trees were reported down and covering the road at West Garner Road and Yeargan Road. A tree was reported down on a mobile home near the intersection of Lake Wheeler Road and Simpkins Road. Trees, power poles, and power lines were reported down near the intersection of Oxford Road and White Oak Road. One tree was reported down on a home in the 4800 block of Fayetteville Road, trapping two individuals inside. One tree was reported down along United States Highway 401 near Interstate 40. Numerous large tree branches and damage to roof panels were reported near Quarry Road. Trees were reported down on power lines near the intersection of Raleigh Street and Martin Luther King Junior Avenue. An EF-1 tornado with maximum wind speeds of 110 mph touched down near a sawmill business 4 miles southwest of Saxahapaw. The tornado then did considerable damage to buildings and structures on the sawmill property. The tornado continued on the  ground toward the northeast for another 4 to 5 miles before lifting one mile east of Saxahapaw, and produced substantial tree and structural damage along the path. The damage consisted of both uprooted and snapped soft and hardwood trees. Numerous homes were damaged by both falling trees and direct wind damage. Several homes had  |considerable roof damage and roof cover loss, including one home in which the entire roof was lifted off the home. Finally, numerous outbuildings, sheds, and garages were completely destroyed. Numerous trees were reported down near North Carolina Highway 42.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 14.277 km away, between 2020-04-26 18:45:00 and 2020-04-26 19:30:00. 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 51500.0 and crop damage of 0.0. \n\nEpisode Narrative: Showers and thunderstorms developed along a stalled boundary across central North Carolina during the afternoon and evening as a positivity tilted mid to upper level trough approached the area from the northwest. Some of the storms became severe and produced damaging winds. Showers and thunderstorms developed along a stalled boundary across central North Carolina during the afternoon and evening as a positivity tilted mid to upper level trough approached the area from the northwest. Some of the storms became severe and produced damaging winds. Showers and thunderstorms developed along a stalled boundary across central North Carolina during the afternoon and evening as a positivity tilted mid to upper level trough approached the area from the northwest. Some of the storms became severe and produced damaging winds. Showers and thunderstorms developed along a stalled boundary across central North Carolina during the afternoon and evening as a positivity tilted mid to upper level trough approached the area from the northwest. Some of the storms became severe and produced damaging winds. Showers and thunderstorms developed along a stalled boundary across central North Carolina during the afternoon and evening as a positivity tilted mid to upper level trough approached the area from the northwest. Some of the storms became severe and produced damaging winds. Showers and thunderstorms developed along a stalled boundary across central North Carolina during the afternoon and evening as a positivity tilted mid to upper level trough approached the area from the northwest. Some of the storms became severe and produced damaging winds.\nEvent Narrative: A tree fell on a house along Monterey Valley Drive. One tree was reported down on Barton Street. One tree was reported down near a parking lot at the Raleigh Durham International Airport. One tree was reported down along Cheek Road. A tree was reported down on a house near the intersection of Simtree Court and Darfield Drive. Two trees were reported down on power lines at the intersection of Ghoston Road and New Light Road.",
+        "The following events were reported: Flash Flood, Thunderstorm Wind. These occurred near station USW00013722, approximately 25.022 km away, between 2020-06-11 18:00:00 and 2020-06-11 20:20:00.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: An approaching cold front initiated scattered thunderstorms across Virginia and North Carolina during the afternoon and evening. The convection initially developed across the northern Piedmont and then back built to the west as the overall line of storms moved south. Isolated wet downbursts and some storm organization resulted in reports of trees down. The slow moving nature of the storms combined with their back-building nature also resulted in some flash flooding. An approaching cold front initiated scattered thunderstorms across Virginia and North Carolina during the afternoon and evening. The convection initially developed across the northern Piedmont and then back built to the west as the overall line of storms moved south. Isolated wet downbursts and some storm organization resulted in reports of trees down. The slow moving nature of the storms combined with their back-building nature also resulted in some flash flooding. An approaching cold front initiated scattered thunderstorms across Virginia and North Carolina during the afternoon and evening. The convection initially developed across the northern Piedmont and then back built to the west as the overall line of storms moved south. Isolated wet downbursts and some storm organization resulted in reports of trees down. The slow moving nature of the storms combined with their back-building nature also resulted in some flash flooding. An approaching cold front initiated scattered thunderstorms across Virginia and North Carolina during the afternoon and evening. The convection initially developed across the northern Piedmont and then back built to the west as the overall line of storms moved south. Isolated wet downbursts and some storm organization resulted in reports of trees down. The slow moving nature of the storms combined with their back-building nature also resulted in some flash flooding. An approaching cold front initiated scattered thunderstorms across Virginia and North Carolina during the afternoon and evening. The convection initially developed across the northern Piedmont and then back built to the west as the overall line of storms moved south. Isolated wet downbursts and some storm organization resulted in reports of trees down. The slow moving nature of the storms combined with their back-building nature also resulted in some flash flooding. An approaching cold front initiated scattered thunderstorms across Virginia and North Carolina during the afternoon and evening. The convection initially developed across the northern Piedmont and then back built to the west as the overall line of storms moved south. Isolated wet downbursts and some storm organization resulted in reports of trees down. The slow moving nature of the storms combined with their back-building nature also resulted in some flash flooding. An approaching cold front initiated scattered thunderstorms across Virginia and North Carolina during the afternoon and evening. The convection initially developed across the northern Piedmont and then back built to the west as the overall line of storms moved south. Isolated wet downbursts and some storm organization resulted in reports of trees down. The slow moving nature of the storms combined with their back-building nature also resulted in some flash flooding. An approaching cold front initiated scattered thunderstorms across Virginia and North Carolina during the afternoon and evening. The convection initially developed across the northern Piedmont and then back built to the west as the overall line of storms moved south. Isolated wet downbursts and some storm organization resulted in reports of trees down. The slow moving nature of the storms combined with their back-building nature also resulted in some flash flooding.\nEvent Narrative: One tree was reported down on power lines in downtown Durham. Multiple trees were reported down in Chapel Hill. Flash flooding was reported on Highway 86 in Hillsborough. Redwood Road was flooded at the interchange with Interstate 85. Flash flooding was reported on Umstead Road at Riverdale Road. Multiple locations along Infinity Road were impassable. Flash flooding was reported on Redding Lane. Power poles were reported down near Tuscarora Drive.",
+        "The following events were reported: Flood. These occurred near station USW00013722, approximately 49.7265 km away, between 2020-06-17 11:44:00 and 2020-06-17 14:44:00. 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: A slow moving upper-level low combined with a surge of warmer and more moist air that moved over a cooler air mass near the surface produced multiple rounds of rain, showers, and thunderstorms across the Coastal Plain and the northeast Piedmont of North Carolina during the morning hours. Widespread rain fell across the area during the previous day or two saturating the soil and raising stream and creek levels. A narrow corridor of heavy rain moved across this area overnight and during the morning hours and produced the flash flooding. Several locations reported between 5 and 6 inches of rain. Many roads were flooded, with at least one water rescue and some roads damaged.\nEvent Narrative: High water flooded Geranium Lane from Long Creek.",
+        "The following events were reported: Hail. These occurred near station USW00013722, approximately 25.5637 km away, between 2020-06-19 15:38:00 and 2020-06-19 15:38:00. 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: Cyclonic, perturbed flow related to a weakening mid and upper level low centered over Ohio and Pennsylvania supported the development of numerous, mainly multi-cellular storms that produced  sub-severe hail and flash flooding. Storms became anchor or backbuild on outflow mergers, which resulted in flash flooding. Cyclonic, perturbed flow related to a weakening mid and upper level low centered over Ohio and Pennsylvania supported the development of numerous, mainly multi-cellular storms that produced  sub-severe hail and flash flooding. Storms became anchor or backbuild on outflow mergers, which resulted in flash flooding.\nEvent Narrative:  Penny sized hail was reported near Interstate 540 and Business Highway 64.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 25.5499 km away, between 2020-06-28 15:50:00 and 2020-06-28 15:50:00. The events included records with estimated wind gusts of 50.0 mph.The events resulted in 0 injuries and 1 fatalities. The events caused property damage valued at 50000.0 and crop damage of 0.0. \n\nEpisode Narrative: Multiple mid to upper level disturbances moving through the region triggered scattered showers and thunderstorms. One cluster of storms moved across the northern Piedmont counties, knocking down a few trees in Burlington, including one tree down onto a home. The same cluster of storms continued to move east across Orange County where an isolated tree crashed through a mobile home and caused a fatality.\nEvent Narrative: One tree fell on a mobile home in the 1200 block of Martin Luther King Boulevard, resulting in a fatality.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 38.4737 km away, between 2020-06-30 14:30:00 and 2020-06-30 17:32:00. 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 35000.0 and crop damage of 0.0. \n\nEpisode Narrative: Multiple outflow boundaries triggered scattered thunderstorms across central North Carolina during the afternoon and evening resulting in a few pulse severe storms. Multiple outflow boundaries triggered scattered thunderstorms across central North Carolina during the afternoon and evening resulting in a few pulse severe storms. Multiple outflow boundaries triggered scattered thunderstorms across central North Carolina during the afternoon and evening resulting in a few pulse severe storms. Multiple outflow boundaries triggered scattered thunderstorms across central North Carolina during the afternoon and evening resulting in a few pulse severe storms.\nEvent Narrative: A tree fell on a car and power lines were reported down near Eagle Rock Road and Old Battle Bridge. Multiple trees were reported down on Ed Brooks Road. Multiple tree were reported down on Moores Mill Road. A tree was reported down near Central Avenue.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 14.8886 km away, between 2020-07-05 12:54:00 and 2020-07-05 12:54:00. 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: Isolated to scattered showers and storms developed in a weak stationary front in a warm and unstable air mass during the afternoon into the evening across central North Carolina. Some of these storms became severe and produced localized wind damage.\nEvent Narrative: A tree was reported down on a house and power lines were reported down near North Miami Boulevard.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 27.3354 km away, between 2020-07-13 18:55:00 and 2020-07-13 18:55:00. 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: Showers and thunderstorms developed along a northwestward retreating surface boundary in a warm, unstable air mass. The storms continued to develop along outflow boundaries from earlier storms and persisted into the evening. Several storms became severe, producing scattered wind damage and marginally severe hail.\nEvent Narrative: One tree was reported down on power lines near Johnson Pond Road.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 33.7448 km away, between 2020-07-18 14:40:00 and 2020-07-18 14:59:00. 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 20000.0 and crop damage of 0.0. \n\nEpisode Narrative: Several clusters of strong to severe storms developed during the late afternoon and evening in a hot and unstable summer time environment. A few of these storms became severe and produced wind damage and lots of lightning. Several clusters of strong to severe storms developed during the late afternoon and evening in a hot and unstable summer time environment. A few of these storms became severe and produced wind damage and lots of lightning. Several clusters of strong to severe storms developed during the late afternoon and evening in a hot and unstable summer time environment. A few of these storms became severe and produced wind damage and lots of lightning. Several clusters of strong to severe storms developed during the late afternoon and evening in a hot and unstable summer time environment. A few of these storms became severe and produced wind damage and lots of lightning.\nEvent Narrative: A tree was reported down along Three Sisters Road. A tree was reported down on Edgemont Road. Multiple trees and power lines were reported down along Knightdale Boulevard. A tree was reported down on Dunn Road.",
+        "The following events were reported: Lightning, Thunderstorm Wind. These occurred near station USW00013722, approximately 36.9131 km away, between 2020-07-23 13:43:00 and 2020-07-23 17:44:00.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: Convection initiated over the North Carolina mountains and foothills by midday and then spread east into the North Carolina Piedmont during early to mid afternoon. The first storms of the day produced some damaging downbursts with convection then becoming outflow dominated. By the late early evening, the combination of slow moving and training convection resulted in isolated flash flooding. Convection initiated over the North Carolina mountains and foothills by midday and then spread east into the North Carolina Piedmont during early to mid afternoon. The first storms of the day produced some damaging downbursts with convection then becoming outflow dominated. By the late early evening, the combination of slow moving and training convection resulted in isolated flash flooding. Convection initiated over the North Carolina mountains and foothills by midday and then spread east into the North Carolina Piedmont during early to mid afternoon. The first storms of the day produced some damaging downbursts with convection then becoming outflow dominated. By the late early evening, the combination of slow moving and training convection resulted in isolated flash flooding. Convection initiated over the North Carolina mountains and foothills by midday and then spread east into the North Carolina Piedmont during early to mid afternoon. The first storms of the day produced some damaging downbursts with convection then becoming outflow dominated. By the late early evening, the combination of slow moving and training convection resulted in isolated flash flooding. Convection initiated over the North Carolina mountains and foothills by midday and then spread east into the North Carolina Piedmont during early to mid afternoon. The first storms of the day produced some damaging downbursts with convection then becoming outflow dominated. By the late early evening, the combination of slow moving and training convection resulted in isolated flash flooding. Convection initiated over the North Carolina mountains and foothills by midday and then spread east into the North Carolina Piedmont during early to mid afternoon. The first storms of the day produced some damaging downbursts with convection then becoming outflow dominated. By the late early evening, the combination of slow moving and training convection resulted in isolated flash flooding. Convection initiated over the North Carolina mountains and foothills by midday and then spread east into the North Carolina Piedmont during early to mid afternoon. The first storms of the day produced some damaging downbursts with convection then becoming outflow dominated. By the late early evening, the combination of slow moving and training convection resulted in isolated flash flooding.\nEvent Narrative:  Lightning struck a house near Lake Wheeler Road and Penny Road. Trees and power lines were reported down on Highway 96 and Riley Hill Road. One tree was reported down on Pippin Road. Power lines were reported down at Pippin Road and Zebulon Road. Multiple trees were reported at the Eagle Ridge Gulf Club. Trees and power lines were reported down on Shepard School Road.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 11.8892 km away, between 2020-07-24 18:20:00 and 2020-07-24 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 3000.0 and crop damage of 0.0. \n\nEpisode Narrative: Scattered showers and thunderstorms produced several wet microbursts during the afternoon and evening in an environment that was characterized by high CAPE and low shear. This resulted in several reports of wind damage across the Sandhills and portions of the Piedmont.\nEvent Narrative: Three trees were reported down in the vicinity of Old Apex Road and Howland Avenue.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 17.3886 km away, between 2020-07-28 16:35:00 and 2020-07-28 16:35:00. 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: Precipitable water values near 2 inches, high temperatures in the 90s and an upper-level wave moving across the area helped to develop widespread showers and thunderstorms across central North Carolina. Colliding outflow boundaries continued storm development throughout the afternoon and evening hours. MLCAPE of 1500-3000 J/kg and low shear created pulse-type, slow moving storms. This resulted in multiple reports of wind damage.\nEvent Narrative: One tree was reported down on a car in a parking lot near Atlantic Avenue and Harrod Street.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 48.4772 km away, between 2020-08-01 15:34:00 and 2020-08-01 15:44:00. 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 cluster of strong to severe storms developed along multiple outflows across portions the Sandhills and Coastal Plain of central North Carolina in a moist and unstable atmosphere. A few of the storms became severe and produced damaging winds gusts in Johnston County. A cluster of strong to severe storms developed along multiple outflows across portions the Sandhills and Coastal Plain of central North Carolina in a moist and unstable atmosphere. A few of the storms became severe and produced damaging winds gusts in Johnston County.\nEvent Narrative: A large tree was reported down at North Carolina Highway 231 and Richardson Road. One tree was reported down at North Carolina Highway 96 and Covered Bridge Road.",
+        "The following events were reported: Flash Flood, Heavy Rain. These occurred near station USW00013722, approximately 31.444 km away, between 2020-08-04 01:27:00 and 2020-08-04 09:49:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Hurricane Isaias made landfall in southeast North Carolina, then moved north through coastal North Carolina. Significant rain fell across the Coastal Plain, Sandhills and eastern Piedmont of North Carolina as Isaias moved northward through the state along with gusty winds up to 50 to 60 miles per hour. Isaias produced two to five inches of rain across much of eastern NC, resulting in flash flooding, as well as minor flooding along the Neuse River. Hurricane Isaias made landfall in southeast North Carolina, then moved north through coastal North Carolina. Significant rain fell across the Coastal Plain, Sandhills and eastern Piedmont of North Carolina as Isaias moved northward through the state along with gusty winds up to 50 to 60 miles per hour. Isaias produced two to five inches of rain across much of eastern NC, resulting in flash flooding, as well as minor flooding along the Neuse River. Hurricane Isaias made landfall in southeast North Carolina, then moved north through coastal North Carolina. Significant rain fell across the Coastal Plain, Sandhills and eastern Piedmont of North Carolina as Isaias moved northward through the state along with gusty winds up to 50 to 60 miles per hour. Isaias produced two to five inches of rain across much of eastern NC, resulting in flash flooding, as well as minor flooding along the Neuse River. Hurricane Isaias made landfall in southeast North Carolina, then moved north through coastal North Carolina. Significant rain fell across the Coastal Plain, Sandhills and eastern Piedmont of North Carolina as Isaias moved northward through the state along with gusty winds up to 50 to 60 miles per hour. Isaias produced two to five inches of rain across much of eastern NC, resulting in flash flooding, as well as minor flooding along the Neuse River. Hurricane Isaias made landfall in southeast North Carolina, then moved north through coastal North Carolina. Significant rain fell across the Coastal Plain, Sandhills and eastern Piedmont of North Carolina as Isaias moved northward through the state along with gusty winds up to 50 to 60 miles per hour. Isaias produced two to five inches of rain across much of eastern NC, resulting in flash flooding, as well as minor flooding along the Neuse River. Hurricane Isaias made landfall in southeast North Carolina, then moved north through coastal North Carolina. Significant rain fell across the Coastal Plain, Sandhills and eastern Piedmont of North Carolina as Isaias moved northward through the state along with gusty winds up to 50 to 60 miles per hour. Isaias produced two to five inches of rain across much of eastern NC, resulting in flash flooding, as well as minor flooding along the Neuse River. Hurricane Isaias made landfall in southeast North Carolina, then moved north through coastal North Carolina. Significant rain fell across the Coastal Plain, Sandhills and eastern Piedmont of North Carolina as Isaias moved northward through the state along with gusty winds up to 50 to 60 miles per hour. Isaias produced two to five inches of rain across much of eastern NC, resulting in flash flooding, as well as minor flooding along the Neuse River. Hurricane Isaias made landfall in southeast North Carolina, then moved north through coastal North Carolina. Significant rain fell across the Coastal Plain, Sandhills and eastern Piedmont of North Carolina as Isaias moved northward through the state along with gusty winds up to 50 to 60 miles per hour. Isaias produced two to five inches of rain across much of eastern NC, resulting in flash flooding, as well as minor flooding along the Neuse River. Hurricane Isaias made landfall in southeast North Carolina, then moved north through coastal North Carolina. Significant rain fell across the Coastal Plain, Sandhills and eastern Piedmont of North Carolina as Isaias moved northward through the state along with gusty winds up to 50 to 60 miles per hour. Isaias produced two to five inches of rain across much of eastern NC, resulting in flash flooding, as well as minor flooding along the Neuse River. Hurricane Isaias made landfall in southeast North Carolina, then moved north through coastal North Carolina. Significant rain fell across the Coastal Plain, Sandhills and eastern Piedmont of North Carolina as Isaias moved northward through the state along with gusty winds up to 50 to 60 miles per hour. Isaias produced two to five inches of rain across much of eastern NC, resulting in flash flooding, as well as minor flooding along the Neuse River. Hurricane Isaias made landfall in southeast North Carolina, then moved north through coastal North Carolina. Significant rain fell across the Coastal Plain, Sandhills and eastern Piedmont of North Carolina as Isaias moved northward through the state along with gusty winds up to 50 to 60 miles per hour. Isaias produced two to five inches of rain across much of eastern NC, resulting in flash flooding, as well as minor flooding along the Neuse River. Hurricane Isaias made landfall in southeast North Carolina, then moved north through coastal North Carolina. Significant rain fell across the Coastal Plain, Sandhills and eastern Piedmont of North Carolina as Isaias moved northward through the state along with gusty winds up to 50 to 60 miles per hour. Isaias produced two to five inches of rain across much of eastern NC, resulting in flash flooding, as well as minor flooding along the Neuse River. Hurricane Isaias made landfall in southeast North Carolina, then moved north through coastal North Carolina. Significant rain fell across the Coastal Plain, Sandhills and eastern Piedmont of North Carolina as Isaias moved northward through the state along with gusty winds up to 50 to 60 miles per hour. Isaias produced two to five inches of rain across much of eastern NC, resulting in flash flooding, as well as minor flooding along the Neuse River. Hurricane Isaias made landfall in southeast North Carolina, then moved north through coastal North Carolina. Significant rain fell across the Coastal Plain, Sandhills and eastern Piedmont of North Carolina as Isaias moved northward through the state along with gusty winds up to 50 to 60 miles per hour. Isaias produced two to five inches of rain across much of eastern NC, resulting in flash flooding, as well as minor flooding along the Neuse River. Hurricane Isaias made landfall in southeast North Carolina, then moved north through coastal North Carolina. Significant rain fell across the Coastal Plain, Sandhills and eastern Piedmont of North Carolina as Isaias moved northward through the state along with gusty winds up to 50 to 60 miles per hour. Isaias produced two to five inches of rain across much of eastern NC, resulting in flash flooding, as well as minor flooding along the Neuse River. Hurricane Isaias made landfall in southeast North Carolina, then moved north through coastal North Carolina. Significant rain fell across the Coastal Plain, Sandhills and eastern Piedmont of North Carolina as Isaias moved northward through the state along with gusty winds up to 50 to 60 miles per hour. Isaias produced two to five inches of rain across much of eastern NC, resulting in flash flooding, as well as minor flooding along the Neuse River. Hurricane Isaias made landfall in southeast North Carolina, then moved north through coastal North Carolina. Significant rain fell across the Coastal Plain, Sandhills and eastern Piedmont of North Carolina as Isaias moved northward through the state along with gusty winds up to 50 to 60 miles per hour. Isaias produced two to five inches of rain across much of eastern NC, resulting in flash flooding, as well as minor flooding along the Neuse River. Hurricane Isaias made landfall in southeast North Carolina, then moved north through coastal North Carolina. Significant rain fell across the Coastal Plain, Sandhills and eastern Piedmont of North Carolina as Isaias moved northward through the state along with gusty winds up to 50 to 60 miles per hour. Isaias produced two to five inches of rain across much of eastern NC, resulting in flash flooding, as well as minor flooding along the Neuse River. Hurricane Isaias made landfall in southeast North Carolina, then moved north through coastal North Carolina. Significant rain fell across the Coastal Plain, Sandhills and eastern Piedmont of North Carolina as Isaias moved northward through the state along with gusty winds up to 50 to 60 miles per hour. Isaias produced two to five inches of rain across much of eastern NC, resulting in flash flooding, as well as minor flooding along the Neuse River. Hurricane Isaias made landfall in southeast North Carolina, then moved north through coastal North Carolina. Significant rain fell across the Coastal Plain, Sandhills and eastern Piedmont of North Carolina as Isaias moved northward through the state along with gusty winds up to 50 to 60 miles per hour. Isaias produced two to five inches of rain across much of eastern NC, resulting in flash flooding, as well as minor flooding along the Neuse River. Hurricane Isaias made landfall in southeast North Carolina, then moved north through coastal North Carolina. Significant rain fell across the Coastal Plain, Sandhills and eastern Piedmont of North Carolina as Isaias moved northward through the state along with gusty winds up to 50 to 60 miles per hour. Isaias produced two to five inches of rain across much of eastern NC, resulting in flash flooding, as well as minor flooding along the Neuse River. Hurricane Isaias made landfall in southeast North Carolina, then moved north through coastal North Carolina. Significant rain fell across the Coastal Plain, Sandhills and eastern Piedmont of North Carolina as Isaias moved northward through the state along with gusty winds up to 50 to 60 miles per hour. Isaias produced two to five inches of rain across much of eastern NC, resulting in flash flooding, as well as minor flooding along the Neuse River. Hurricane Isaias made landfall in southeast North Carolina, then moved north through coastal North Carolina. Significant rain fell across the Coastal Plain, Sandhills and eastern Piedmont of North Carolina as Isaias moved northward through the state along with gusty winds up to 50 to 60 miles per hour. Isaias produced two to five inches of rain across much of eastern NC, resulting in flash flooding, as well as minor flooding along the Neuse River. Hurricane Isaias made landfall in southeast North Carolina, then moved north through coastal North Carolina. Significant rain fell across the Coastal Plain, Sandhills and eastern Piedmont of North Carolina as Isaias moved northward through the state along with gusty winds up to 50 to 60 miles per hour. Isaias produced two to five inches of rain across much of eastern NC, resulting in flash flooding, as well as minor flooding along the Neuse River. Hurricane Isaias made landfall in southeast North Carolina, then moved north through coastal North Carolina. Significant rain fell across the Coastal Plain, Sandhills and eastern Piedmont of North Carolina as Isaias moved northward through the state along with gusty winds up to 50 to 60 miles per hour. Isaias produced two to five inches of rain across much of eastern NC, resulting in flash flooding, as well as minor flooding along the Neuse River. Hurricane Isaias made landfall in southeast North Carolina, then moved north through coastal North Carolina. Significant rain fell across the Coastal Plain, Sandhills and eastern Piedmont of North Carolina as Isaias moved northward through the state along with gusty winds up to 50 to 60 miles per hour. Isaias produced two to five inches of rain across much of eastern NC, resulting in flash flooding, as well as minor flooding along the Neuse River. Hurricane Isaias made landfall in southeast North Carolina, then moved north through coastal North Carolina. Significant rain fell across the Coastal Plain, Sandhills and eastern Piedmont of North Carolina as Isaias moved northward through the state along with gusty winds up to 50 to 60 miles per hour. Isaias produced two to five inches of rain across much of eastern NC, resulting in flash flooding, as well as minor flooding along the Neuse River. Hurricane Isaias made landfall in southeast North Carolina, then moved north through coastal North Carolina. Significant rain fell across the Coastal Plain, Sandhills and eastern Piedmont of North Carolina as Isaias moved northward through the state along with gusty winds up to 50 to 60 miles per hour. Isaias produced two to five inches of rain across much of eastern NC, resulting in flash flooding, as well as minor flooding along the Neuse River. Hurricane Isaias made landfall in southeast North Carolina, then moved north through coastal North Carolina. Significant rain fell across the Coastal Plain, Sandhills and eastern Piedmont of North Carolina as Isaias moved northward through the state along with gusty winds up to 50 to 60 miles per hour. Isaias produced two to five inches of rain across much of eastern NC, resulting in flash flooding, as well as minor flooding along the Neuse River. Hurricane Isaias made landfall in southeast North Carolina, then moved north through coastal North Carolina. Significant rain fell across the Coastal Plain, Sandhills and eastern Piedmont of North Carolina as Isaias moved northward through the state along with gusty winds up to 50 to 60 miles per hour. Isaias produced two to five inches of rain across much of eastern NC, resulting in flash flooding, as well as minor flooding along the Neuse River. Hurricane Isaias made landfall in southeast North Carolina, then moved north through coastal North Carolina. Significant rain fell across the Coastal Plain, Sandhills and eastern Piedmont of North Carolina as Isaias moved northward through the state along with gusty winds up to 50 to 60 miles per hour. Isaias produced two to five inches of rain across much of eastern NC, resulting in flash flooding, as well as minor flooding along the Neuse River.\nEvent Narrative: Storm total rainfall for Tropical Cyclone Isaias was 3.93 inches. Storm total rainfall for Tropical Cyclone Isaias was 3.26 inches. Storm total rainfall for Tropical Cyclone Isaias was 3.90 inches. Storm total rainfall for Tropical Cyclone Isaias was 3.56 inches. Storm total rainfall for Tropical Cyclone Isaias was 3.78 inches. River gage WSSN7 on Walnut Creek at South State Street rose above flood stage and came out of its banks. Also, at least one road was closed due to flash flooding in Holly Springs. Rainfall totals exceeded 4 inches in some locations across Wake County. Storm total rainfall for Tropical Cyclone Isaias was 5.06 inches. Storm total rainfall for Tropical Cyclone Isaias was 3.12 inches. Storm total rainfall for Tropical Cyclone Isaias was 3.12 inches. Storm total rainfall for Tropical Cyclone Isaias was 3.86 inches. Storm total rainfall for Tropical Cyclone Isaias was 4.06 inches. A rainfall total of 4.01 inches was recorded in Raleigh, most of which fell between 8 PM Monday and 5 AM Tuesday. Storm total rainfall for Tropical Cyclone Isaias was 3.70 inches. Storm total rainfall for Tropical Cyclone Isaias was 3.35 inches. Storm total rainfall for Tropical Cyclone Isaias was 3.00 inches. Storm total rainfall for Tropical Cyclone Isaias was 3.00 inches. Storm total rainfall for Tropical Cyclone Isaias was 3.31 inches. Storm total rainfall for Tropical Cyclone Isaias was 3.02 inches. Storm total rainfall for Tropical Cyclone Isaias was 3.26 inches. Storm total rainfall for Tropical Cyclone Isaias was 3.17 inches. Storm total rainfall for Tropical Cyclone Isaias was 3.17 inches. Storm total rainfall for Tropical Cyclone Isaias was 3.53 inches. Storm total rainfall for Tropical Cyclone Isaias was 3.73 inches. Storm total rainfall for Tropical Cyclone Isaias was 3.80 inches. Storm total rainfall for Tropical Cyclone Isaias was 4.00 inches. Storm total rainfall for Tropical Cyclone Isaias was 3.73 inches. Storm total rainfall for Tropical Cyclone Isaias was 3.13 inches. Storm total rainfall for Tropical Cyclone Isaias was 3.67 inches. Storm total rainfall for Tropical Cyclone Isaias was 3.29 inches. Storm total rainfall for Tropical Cyclone Isaias was 3.79 inches. Storm total rainfall for Tropical Cyclone Isaias was 3.28 inches.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 39.1275 km away, between 2020-08-06 14:51:00 and 2020-08-06 14:51:00. 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 5000.0 and crop damage of 0.0. \n\nEpisode Narrative: Aided by large scale ascent ahead of a broad midlevel trough centered over the Tennessee Valley, multicellular convection produced some isolated wind damage across central North Carolina, along with some heavy rain and flash flooding. Aided by large scale ascent ahead of a broad midlevel trough centered over the Tennessee Valley, multicellular convection produced some isolated wind damage across central North Carolina, along with some heavy rain and flash flooding.\nEvent Narrative: One tree was reported down on power lines along North Carolina Highway 97 near Little River Park. One tree was reported down near the intersection of Riley Hilll Road and Jack Mitchell Road.",
+        "The following events were reported: Flash Flood. These occurred near station USW00013722, approximately 21.8593 km away, between 2020-08-14 20:45:00 and 2020-08-14 21:30:00.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: Scattered showers and thunderstorms developed along a southward sinking outflow boundary in a very moist atmosphere, characterized by a weak westerly steering flow. This resulted in training showers and storms producing heavy rainfall. This resulted in several reports of flash flooding across the Piedmont of central North Carolina. Scattered showers and thunderstorms developed along a southward sinking outflow boundary in a very moist atmosphere, characterized by a weak westerly steering flow. This resulted in training showers and storms producing heavy rainfall. This resulted in several reports of flash flooding across the Piedmont of central North Carolina. Scattered showers and thunderstorms developed along a southward sinking outflow boundary in a very moist atmosphere, characterized by a weak westerly steering flow. This resulted in training showers and storms producing heavy rainfall. This resulted in several reports of flash flooding across the Piedmont of central North Carolina. Scattered showers and thunderstorms developed along a southward sinking outflow boundary in a very moist atmosphere, characterized by a weak westerly steering flow. This resulted in training showers and storms producing heavy rainfall. This resulted in several reports of flash flooding across the Piedmont of central North Carolina.\nEvent Narrative: Flash flooding closed the intersection of New Hope Church Road and Atlantic Avenue. Vehicles were reported stuck in flood waters at the intersection of North Market Street and Craftsman Drive. An individual was rescued from flood waters near North Hills Drive. Flash flooding was reported at Morphus Bridge Road and Corbin Road.",
+        "The following events were reported: Flash Flood, Heavy Rain. These occurred near station USW00013722, approximately 29.2393 km away, between 2020-08-15 14:30:00 and 2020-08-15 18:15:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Training thunderstorms along a stalled front bisecting central North Carolina produced pockets of 3 to 6 inches of rain across Wake, Franklin and Harnett counties. Numerous roads were flooded across Harnett and Franklin counties from the storms. Training thunderstorms along a stalled front bisecting central North Carolina produced pockets of 3 to 6 inches of rain across Wake, Franklin and Harnett counties. Numerous roads were flooded across Harnett and Franklin counties from the storms. Training thunderstorms along a stalled front bisecting central North Carolina produced pockets of 3 to 6 inches of rain across Wake, Franklin and Harnett counties. Numerous roads were flooded across Harnett and Franklin counties from the storms. Training thunderstorms along a stalled front bisecting central North Carolina produced pockets of 3 to 6 inches of rain across Wake, Franklin and Harnett counties. Numerous roads were flooded across Harnett and Franklin counties from the storms. Training thunderstorms along a stalled front bisecting central North Carolina produced pockets of 3 to 6 inches of rain across Wake, Franklin and Harnett counties. Numerous roads were flooded across Harnett and Franklin counties from the storms.\nEvent Narrative: Numerous roads were reported closed due to flooding in and around Louisburg. Flash flooding was reported at Wall Road and Harris Road. Flash flooding was reported near the intersection of Knightdale Boulevard and Hodge Road. Storm total rain was 3.29 inches. Storm total rain was 2.55 inches.",
+        "The following events were reported: Flash Flood. These occurred near station USW00013722, approximately 29.845 km away, between 2020-08-31 15:35:00 and 2020-08-31 23:59:00.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 60000.0 and crop damage of 0.0. \n\nEpisode Narrative: Warm moist air lifted along a wavy stationary front. This combined with slow moving and merging thunderstorms resulted in heavy rain and flash flooding, including a dam break in Johnston County and two fatalities. Warm moist air lifted along a wavy stationary front. This combined with slow moving and merging thunderstorms resulted in heavy rain and flash flooding, including a dam break in Johnston County and two fatalities. Warm moist air lifted along a wavy stationary front. This combined with slow moving and merging thunderstorms resulted in heavy rain and flash flooding, including a dam break in Johnston County and two fatalities. Warm moist air lifted along a wavy stationary front. This combined with slow moving and merging thunderstorms resulted in heavy rain and flash flooding, including a dam break in Johnston County and two fatalities. Warm moist air lifted along a wavy stationary front. This combined with slow moving and merging thunderstorms resulted in heavy rain and flash flooding, including a dam break in Johnston County and two fatalities. Warm moist air lifted along a wavy stationary front. This combined with slow moving and merging thunderstorms resulted in heavy rain and flash flooding, including a dam break in Johnston County and two fatalities. Warm moist air lifted along a wavy stationary front. This combined with slow moving and merging thunderstorms resulted in heavy rain and flash flooding, including a dam break in Johnston County and two fatalities. Warm moist air lifted along a wavy stationary front. This combined with slow moving and merging thunderstorms resulted in heavy rain and flash flooding, including a dam break in Johnston County and two fatalities. Warm moist air lifted along a wavy stationary front. This combined with slow moving and merging thunderstorms resulted in heavy rain and flash flooding, including a dam break in Johnston County and two fatalities. Warm moist air lifted along a wavy stationary front. This combined with slow moving and merging thunderstorms resulted in heavy rain and flash flooding, including a dam break in Johnston County and two fatalities. Warm moist air lifted along a wavy stationary front. This combined with slow moving and merging thunderstorms resulted in heavy rain and flash flooding, including a dam break in Johnston County and two fatalities.\nEvent Narrative: Flash Flooding closed North Carolina Highway 55 near Ennis Road. Flash flooding was reported on Kay Lane. Flash flooding was reported on North Carolina Highway 210. Flash flooding was reported down Old Buies Creek Road. Flash flooding was reported on Honeycutt Drive. Flash flooding was reported near Sanders Road, where a water rescue occurred. Flash flooding was reported on North Wilmington Street at Polk Street, where flood waters went into the first floor of a building. Flash flooding was reported near West Millbrook Road and Leesville road. Flash flooding was reported at East Lawson Street. Flash flooding was reported near North Carolina Highway 147 and Ellis Road. Flash Flooding was reported near Fayetteville Street.",
+        "The following events were reported: Flash Flood, Heavy Rain. These occurred near station USW00013722, approximately 26.0275 km away, between 2020-09-01 00:00:00 and 2020-09-01 13:42:00.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: Flash flooding that originated on August 31st continued across portions of the northeast Piedmont and central Coastal Plain of central North Carolina during the early morning hours of September 1st. Rainfall amounts of up to 11 inches were reported across this area, resulting in lingering flash flooding. Flash flooding that originated on August 31st continued across portions of the northeast Piedmont and central Coastal Plain of central North Carolina during the early morning hours of September 1st. Rainfall amounts of up to 11 inches were reported across this area, resulting in lingering flash flooding. Flash flooding that originated on August 31st continued across portions of the northeast Piedmont and central Coastal Plain of central North Carolina during the early morning hours of September 1st. Rainfall amounts of up to 11 inches were reported across this area, resulting in lingering flash flooding. Flash flooding that originated on August 31st continued across portions of the northeast Piedmont and central Coastal Plain of central North Carolina during the early morning hours of September 1st. Rainfall amounts of up to 11 inches were reported across this area, resulting in lingering flash flooding. Flash flooding that originated on August 31st continued across portions of the northeast Piedmont and central Coastal Plain of central North Carolina during the early morning hours of September 1st. Rainfall amounts of up to 11 inches were reported across this area, resulting in lingering flash flooding. Flash flooding that originated on August 31st continued across portions of the northeast Piedmont and central Coastal Plain of central North Carolina during the early morning hours of September 1st. Rainfall amounts of up to 11 inches were reported across this area, resulting in lingering flash flooding. Flash flooding that originated on August 31st continued across portions of the northeast Piedmont and central Coastal Plain of central North Carolina during the early morning hours of September 1st. Rainfall amounts of up to 11 inches were reported across this area, resulting in lingering flash flooding. Flash flooding that originated on August 31st continued across portions of the northeast Piedmont and central Coastal Plain of central North Carolina during the early morning hours of September 1st. Rainfall amounts of up to 11 inches were reported across this area, resulting in lingering flash flooding. Flash flooding that originated on August 31st continued across portions of the northeast Piedmont and central Coastal Plain of central North Carolina during the early morning hours of September 1st. Rainfall amounts of up to 11 inches were reported across this area, resulting in lingering flash flooding.\nEvent Narrative: Storm total rainfall of 2.74 inches was reported. Storm total rainfall of 4.17 inches was reported. Storm total rainfall of 4.14 inches was reported. Crabtree Creek at Old Wake Forecast Road flooded due to heavy rain. Flash flooding was reported along and near Crabtree Creek in Raleigh, which resulted in multiple cars stranded in flood waters. Storm total rainfall of 4.60 inches was reported. Storm total rainfall of 5.93 inches was reported. Storm total rainfall of 5.23 inches was reported. Storm total rainfall of 3.84 inches was reported.",
+        "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00013722, approximately 13.717 km away, between 2020-09-25 18:45:00 and 2020-09-25 19:25:00. The events included records with hailstones measuring 2.9642857142857144 inches.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: The remnant low from Tropical Cyclone Beta was moving from north Alabama into Georgia, along a warm frontal zone across South Carolina and south-central North Carolina to the northern Outer Banks. Meanwhile, a mid level shortwave trough was tracking eastward across southwestern Virginia. Convection began to increase in a broad band just south of central North Carolina, and it was from this that two distinct cells started accelerating to the north-northeastward, with the leftmost cell eventually becoming dominant and intensifying over northeast Lee County as it move to the of the surface boundary. It produced a swath of large hail across western Wake County before starting to weaken over far northwest Wake County. The remnant low from Tropical Cyclone Beta was moving from north Alabama into Georgia, along a warm frontal zone across South Carolina and south-central North Carolina to the northern Outer Banks. Meanwhile, a mid level shortwave trough was tracking eastward across southwestern Virginia. Convection began to increase in a broad band just south of central North Carolina, and it was from this that two distinct cells started accelerating to the north-northeastward, with the leftmost cell eventually becoming dominant and intensifying over northeast Lee County as it move to the of the surface boundary. It produced a swath of large hail across western Wake County before starting to weaken over far northwest Wake County. The remnant low from Tropical Cyclone Beta was moving from north Alabama into Georgia, along a warm frontal zone across South Carolina and south-central North Carolina to the northern Outer Banks. Meanwhile, a mid level shortwave trough was tracking eastward across southwestern Virginia. Convection began to increase in a broad band just south of central North Carolina, and it was from this that two distinct cells started accelerating to the north-northeastward, with the leftmost cell eventually becoming dominant and intensifying over northeast Lee County as it move to the of the surface boundary. It produced a swath of large hail across western Wake County before starting to weaken over far northwest Wake County. The remnant low from Tropical Cyclone Beta was moving from north Alabama into Georgia, along a warm frontal zone across South Carolina and south-central North Carolina to the northern Outer Banks. Meanwhile, a mid level shortwave trough was tracking eastward across southwestern Virginia. Convection began to increase in a broad band just south of central North Carolina, and it was from this that two distinct cells started accelerating to the north-northeastward, with the leftmost cell eventually becoming dominant and intensifying over northeast Lee County as it move to the of the surface boundary. It produced a swath of large hail across western Wake County before starting to weaken over far northwest Wake County. The remnant low from Tropical Cyclone Beta was moving from north Alabama into Georgia, along a warm frontal zone across South Carolina and south-central North Carolina to the northern Outer Banks. Meanwhile, a mid level shortwave trough was tracking eastward across southwestern Virginia. Convection began to increase in a broad band just south of central North Carolina, and it was from this that two distinct cells started accelerating to the north-northeastward, with the leftmost cell eventually becoming dominant and intensifying over northeast Lee County as it move to the of the surface boundary. It produced a swath of large hail across western Wake County before starting to weaken over far northwest Wake County. The remnant low from Tropical Cyclone Beta was moving from north Alabama into Georgia, along a warm frontal zone across South Carolina and south-central North Carolina to the northern Outer Banks. Meanwhile, a mid level shortwave trough was tracking eastward across southwestern Virginia. Convection began to increase in a broad band just south of central North Carolina, and it was from this that two distinct cells started accelerating to the north-northeastward, with the leftmost cell eventually becoming dominant and intensifying over northeast Lee County as it move to the of the surface boundary. It produced a swath of large hail across western Wake County before starting to weaken over far northwest Wake County. The remnant low from Tropical Cyclone Beta was moving from north Alabama into Georgia, along a warm frontal zone across South Carolina and south-central North Carolina to the northern Outer Banks. Meanwhile, a mid level shortwave trough was tracking eastward across southwestern Virginia. Convection began to increase in a broad band just south of central North Carolina, and it was from this that two distinct cells started accelerating to the north-northeastward, with the leftmost cell eventually becoming dominant and intensifying over northeast Lee County as it move to the of the surface boundary. It produced a swath of large hail across western Wake County before starting to weaken over far northwest Wake County. The remnant low from Tropical Cyclone Beta was moving from north Alabama into Georgia, along a warm frontal zone across South Carolina and south-central North Carolina to the northern Outer Banks. Meanwhile, a mid level shortwave trough was tracking eastward across southwestern Virginia. Convection began to increase in a broad band just south of central North Carolina, and it was from this that two distinct cells started accelerating to the north-northeastward, with the leftmost cell eventually becoming dominant and intensifying over northeast Lee County as it move to the of the surface boundary. It produced a swath of large hail across western Wake County before starting to weaken over far northwest Wake County. The remnant low from Tropical Cyclone Beta was moving from north Alabama into Georgia, along a warm frontal zone across South Carolina and south-central North Carolina to the northern Outer Banks. Meanwhile, a mid level shortwave trough was tracking eastward across southwestern Virginia. Convection began to increase in a broad band just south of central North Carolina, and it was from this that two distinct cells started accelerating to the north-northeastward, with the leftmost cell eventually becoming dominant and intensifying over northeast Lee County as it move to the of the surface boundary. It produced a swath of large hail across western Wake County before starting to weaken over far northwest Wake County. The remnant low from Tropical Cyclone Beta was moving from north Alabama into Georgia, along a warm frontal zone across South Carolina and south-central North Carolina to the northern Outer Banks. Meanwhile, a mid level shortwave trough was tracking eastward across southwestern Virginia. Convection began to increase in a broad band just south of central North Carolina, and it was from this that two distinct cells started accelerating to the north-northeastward, with the leftmost cell eventually becoming dominant and intensifying over northeast Lee County as it move to the of the surface boundary. It produced a swath of large hail across western Wake County before starting to weaken over far northwest Wake County. The remnant low from Tropical Cyclone Beta was moving from north Alabama into Georgia, along a warm frontal zone across South Carolina and south-central North Carolina to the northern Outer Banks. Meanwhile, a mid level shortwave trough was tracking eastward across southwestern Virginia. Convection began to increase in a broad band just south of central North Carolina, and it was from this that two distinct cells started accelerating to the north-northeastward, with the leftmost cell eventually becoming dominant and intensifying over northeast Lee County as it move to the of the surface boundary. It produced a swath of large hail across western Wake County before starting to weaken over far northwest Wake County. The remnant low from Tropical Cyclone Beta was moving from north Alabama into Georgia, along a warm frontal zone across South Carolina and south-central North Carolina to the northern Outer Banks. Meanwhile, a mid level shortwave trough was tracking eastward across southwestern Virginia. Convection began to increase in a broad band just south of central North Carolina, and it was from this that two distinct cells started accelerating to the north-northeastward, with the leftmost cell eventually becoming dominant and intensifying over northeast Lee County as it move to the of the surface boundary. It produced a swath of large hail across western Wake County before starting to weaken over far northwest Wake County. The remnant low from Tropical Cyclone Beta was moving from north Alabama into Georgia, along a warm frontal zone across South Carolina and south-central North Carolina to the northern Outer Banks. Meanwhile, a mid level shortwave trough was tracking eastward across southwestern Virginia. Convection began to increase in a broad band just south of central North Carolina, and it was from this that two distinct cells started accelerating to the north-northeastward, with the leftmost cell eventually becoming dominant and intensifying over northeast Lee County as it move to the of the surface boundary. It produced a swath of large hail across western Wake County before starting to weaken over far northwest Wake County. The remnant low from Tropical Cyclone Beta was moving from north Alabama into Georgia, along a warm frontal zone across South Carolina and south-central North Carolina to the northern Outer Banks. Meanwhile, a mid level shortwave trough was tracking eastward across southwestern Virginia. Convection began to increase in a broad band just south of central North Carolina, and it was from this that two distinct cells started accelerating to the north-northeastward, with the leftmost cell eventually becoming dominant and intensifying over northeast Lee County as it move to the of the surface boundary. It produced a swath of large hail across western Wake County before starting to weaken over far northwest Wake County. The remnant low from Tropical Cyclone Beta was moving from north Alabama into Georgia, along a warm frontal zone across South Carolina and south-central North Carolina to the northern Outer Banks. Meanwhile, a mid level shortwave trough was tracking eastward across southwestern Virginia. Convection began to increase in a broad band just south of central North Carolina, and it was from this that two distinct cells started accelerating to the north-northeastward, with the leftmost cell eventually becoming dominant and intensifying over northeast Lee County as it move to the of the surface boundary. It produced a swath of large hail across western Wake County before starting to weaken over far northwest Wake County. The remnant low from Tropical Cyclone Beta was moving from north Alabama into Georgia, along a warm frontal zone across South Carolina and south-central North Carolina to the northern Outer Banks. Meanwhile, a mid level shortwave trough was tracking eastward across southwestern Virginia. Convection began to increase in a broad band just south of central North Carolina, and it was from this that two distinct cells started accelerating to the north-northeastward, with the leftmost cell eventually becoming dominant and intensifying over northeast Lee County as it move to the of the surface boundary. It produced a swath of large hail across western Wake County before starting to weaken over far northwest Wake County. The remnant low from Tropical Cyclone Beta was moving from north Alabama into Georgia, along a warm frontal zone across South Carolina and south-central North Carolina to the northern Outer Banks. Meanwhile, a mid level shortwave trough was tracking eastward across southwestern Virginia. Convection began to increase in a broad band just south of central North Carolina, and it was from this that two distinct cells started accelerating to the north-northeastward, with the leftmost cell eventually becoming dominant and intensifying over northeast Lee County as it move to the of the surface boundary. It produced a swath of large hail across western Wake County before starting to weaken over far northwest Wake County. The remnant low from Tropical Cyclone Beta was moving from north Alabama into Georgia, along a warm frontal zone across South Carolina and south-central North Carolina to the northern Outer Banks. Meanwhile, a mid level shortwave trough was tracking eastward across southwestern Virginia. Convection began to increase in a broad band just south of central North Carolina, and it was from this that two distinct cells started accelerating to the north-northeastward, with the leftmost cell eventually becoming dominant and intensifying over northeast Lee County as it move to the of the surface boundary. It produced a swath of large hail across western Wake County before starting to weaken over far northwest Wake County. The remnant low from Tropical Cyclone Beta was moving from north Alabama into Georgia, along a warm frontal zone across South Carolina and south-central North Carolina to the northern Outer Banks. Meanwhile, a mid level shortwave trough was tracking eastward across southwestern Virginia. Convection began to increase in a broad band just south of central North Carolina, and it was from this that two distinct cells started accelerating to the north-northeastward, with the leftmost cell eventually becoming dominant and intensifying over northeast Lee County as it move to the of the surface boundary. It produced a swath of large hail across western Wake County before starting to weaken over far northwest Wake County. The remnant low from Tropical Cyclone Beta was moving from north Alabama into Georgia, along a warm frontal zone across South Carolina and south-central North Carolina to the northern Outer Banks. Meanwhile, a mid level shortwave trough was tracking eastward across southwestern Virginia. Convection began to increase in a broad band just south of central North Carolina, and it was from this that two distinct cells started accelerating to the north-northeastward, with the leftmost cell eventually becoming dominant and intensifying over northeast Lee County as it move to the of the surface boundary. It produced a swath of large hail across western Wake County before starting to weaken over far northwest Wake County. The remnant low from Tropical Cyclone Beta was moving from north Alabama into Georgia, along a warm frontal zone across South Carolina and south-central North Carolina to the northern Outer Banks. Meanwhile, a mid level shortwave trough was tracking eastward across southwestern Virginia. Convection began to increase in a broad band just south of central North Carolina, and it was from this that two distinct cells started accelerating to the north-northeastward, with the leftmost cell eventually becoming dominant and intensifying over northeast Lee County as it move to the of the surface boundary. It produced a swath of large hail across western Wake County before starting to weaken over far northwest Wake County. The remnant low from Tropical Cyclone Beta was moving from north Alabama into Georgia, along a warm frontal zone across South Carolina and south-central North Carolina to the northern Outer Banks. Meanwhile, a mid level shortwave trough was tracking eastward across southwestern Virginia. Convection began to increase in a broad band just south of central North Carolina, and it was from this that two distinct cells started accelerating to the north-northeastward, with the leftmost cell eventually becoming dominant and intensifying over northeast Lee County as it move to the of the surface boundary. It produced a swath of large hail across western Wake County before starting to weaken over far northwest Wake County. The remnant low from Tropical Cyclone Beta was moving from north Alabama into Georgia, along a warm frontal zone across South Carolina and south-central North Carolina to the northern Outer Banks. Meanwhile, a mid level shortwave trough was tracking eastward across southwestern Virginia. Convection began to increase in a broad band just south of central North Carolina, and it was from this that two distinct cells started accelerating to the north-northeastward, with the leftmost cell eventually becoming dominant and intensifying over northeast Lee County as it move to the of the surface boundary. It produced a swath of large hail across western Wake County before starting to weaken over far northwest Wake County. The remnant low from Tropical Cyclone Beta was moving from north Alabama into Georgia, along a warm frontal zone across South Carolina and south-central North Carolina to the northern Outer Banks. Meanwhile, a mid level shortwave trough was tracking eastward across southwestern Virginia. Convection began to increase in a broad band just south of central North Carolina, and it was from this that two distinct cells started accelerating to the north-northeastward, with the leftmost cell eventually becoming dominant and intensifying over northeast Lee County as it move to the of the surface boundary. It produced a swath of large hail across western Wake County before starting to weaken over far northwest Wake County. The remnant low from Tropical Cyclone Beta was moving from north Alabama into Georgia, along a warm frontal zone across South Carolina and south-central North Carolina to the northern Outer Banks. Meanwhile, a mid level shortwave trough was tracking eastward across southwestern Virginia. Convection began to increase in a broad band just south of central North Carolina, and it was from this that two distinct cells started accelerating to the north-northeastward, with the leftmost cell eventually becoming dominant and intensifying over northeast Lee County as it move to the of the surface boundary. It produced a swath of large hail across western Wake County before starting to weaken over far northwest Wake County. The remnant low from Tropical Cyclone Beta was moving from north Alabama into Georgia, along a warm frontal zone across South Carolina and south-central North Carolina to the northern Outer Banks. Meanwhile, a mid level shortwave trough was tracking eastward across southwestern Virginia. Convection began to increase in a broad band just south of central North Carolina, and it was from this that two distinct cells started accelerating to the north-northeastward, with the leftmost cell eventually becoming dominant and intensifying over northeast Lee County as it move to the of the surface boundary. It produced a swath of large hail across western Wake County before starting to weaken over far northwest Wake County. The remnant low from Tropical Cyclone Beta was moving from north Alabama into Georgia, along a warm frontal zone across South Carolina and south-central North Carolina to the northern Outer Banks. Meanwhile, a mid level shortwave trough was tracking eastward across southwestern Virginia. Convection began to increase in a broad band just south of central North Carolina, and it was from this that two distinct cells started accelerating to the north-northeastward, with the leftmost cell eventually becoming dominant and intensifying over northeast Lee County as it move to the of the surface boundary. It produced a swath of large hail across western Wake County before starting to weaken over far northwest Wake County. The remnant low from Tropical Cyclone Beta was moving from north Alabama into Georgia, along a warm frontal zone across South Carolina and south-central North Carolina to the northern Outer Banks. Meanwhile, a mid level shortwave trough was tracking eastward across southwestern Virginia. Convection began to increase in a broad band just south of central North Carolina, and it was from this that two distinct cells started accelerating to the north-northeastward, with the leftmost cell eventually becoming dominant and intensifying over northeast Lee County as it move to the of the surface boundary. It produced a swath of large hail across western Wake County before starting to weaken over far northwest Wake County.\nEvent Narrative:   Two inch diameter hail was reported near the intersection of Highway 55 and Indian Wells Road.             Multiple trees were reported down near the intersection of Leesville Road and Crestmont Drive.",
+        "The following events were reported: Flash Flood. These occurred near station USW00013722, approximately 27.2869 km away, between 2020-11-12 10:30:00 and 2020-11-12 18:05:00.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: Moisture from Tropical Storm Eta was drawn northward into the Mid Atlantic during the day of Wednesday November 11th. Meanwhile, a slow moving cold front approached the area and made its way through central North Carolina during the day Thursday, resulting in widespread showers and isolated thunderstorms. Rainfall totals were generally in the 4 to 6 inches range, although some spots near Rocky Mount saw close to 10 inches of rain by the time the event drew to a close. This resulted in numerous flooded road, including one death resulting from the flash flooding. One thunderstorm also caused some localized storm damage in Sampson County. Moisture from Tropical Storm Eta was drawn northward into the Mid Atlantic during the day of Wednesday November 11th. Meanwhile, a slow moving cold front approached the area and made its way through central North Carolina during the day Thursday, resulting in widespread showers and isolated thunderstorms. Rainfall totals were generally in the 4 to 6 inches range, although some spots near Rocky Mount saw close to 10 inches of rain by the time the event drew to a close. This resulted in numerous flooded road, including one death resulting from the flash flooding. One thunderstorm also caused some localized storm damage in Sampson County. Moisture from Tropical Storm Eta was drawn northward into the Mid Atlantic during the day of Wednesday November 11th. Meanwhile, a slow moving cold front approached the area and made its way through central North Carolina during the day Thursday, resulting in widespread showers and isolated thunderstorms. Rainfall totals were generally in the 4 to 6 inches range, although some spots near Rocky Mount saw close to 10 inches of rain by the time the event drew to a close. This resulted in numerous flooded road, including one death resulting from the flash flooding. One thunderstorm also caused some localized storm damage in Sampson County. Moisture from Tropical Storm Eta was drawn northward into the Mid Atlantic during the day of Wednesday November 11th. Meanwhile, a slow moving cold front approached the area and made its way through central North Carolina during the day Thursday, resulting in widespread showers and isolated thunderstorms. Rainfall totals were generally in the 4 to 6 inches range, although some spots near Rocky Mount saw close to 10 inches of rain by the time the event drew to a close. This resulted in numerous flooded road, including one death resulting from the flash flooding. One thunderstorm also caused some localized storm damage in Sampson County. Moisture from Tropical Storm Eta was drawn northward into the Mid Atlantic during the day of Wednesday November 11th. Meanwhile, a slow moving cold front approached the area and made its way through central North Carolina during the day Thursday, resulting in widespread showers and isolated thunderstorms. Rainfall totals were generally in the 4 to 6 inches range, although some spots near Rocky Mount saw close to 10 inches of rain by the time the event drew to a close. This resulted in numerous flooded road, including one death resulting from the flash flooding. One thunderstorm also caused some localized storm damage in Sampson County. Moisture from Tropical Storm Eta was drawn northward into the Mid Atlantic during the day of Wednesday November 11th. Meanwhile, a slow moving cold front approached the area and made its way through central North Carolina during the day Thursday, resulting in widespread showers and isolated thunderstorms. Rainfall totals were generally in the 4 to 6 inches range, although some spots near Rocky Mount saw close to 10 inches of rain by the time the event drew to a close. This resulted in numerous flooded road, including one death resulting from the flash flooding. One thunderstorm also caused some localized storm damage in Sampson County. Moisture from Tropical Storm Eta was drawn northward into the Mid Atlantic during the day of Wednesday November 11th. Meanwhile, a slow moving cold front approached the area and made its way through central North Carolina during the day Thursday, resulting in widespread showers and isolated thunderstorms. Rainfall totals were generally in the 4 to 6 inches range, although some spots near Rocky Mount saw close to 10 inches of rain by the time the event drew to a close. This resulted in numerous flooded road, including one death resulting from the flash flooding. One thunderstorm also caused some localized storm damage in Sampson County. Moisture from Tropical Storm Eta was drawn northward into the Mid Atlantic during the day of Wednesday November 11th. Meanwhile, a slow moving cold front approached the area and made its way through central North Carolina during the day Thursday, resulting in widespread showers and isolated thunderstorms. Rainfall totals were generally in the 4 to 6 inches range, although some spots near Rocky Mount saw close to 10 inches of rain by the time the event drew to a close. This resulted in numerous flooded road, including one death resulting from the flash flooding. One thunderstorm also caused some localized storm damage in Sampson County. Moisture from Tropical Storm Eta was drawn northward into the Mid Atlantic during the day of Wednesday November 11th. Meanwhile, a slow moving cold front approached the area and made its way through central North Carolina during the day Thursday, resulting in widespread showers and isolated thunderstorms. Rainfall totals were generally in the 4 to 6 inches range, although some spots near Rocky Mount saw close to 10 inches of rain by the time the event drew to a close. This resulted in numerous flooded road, including one death resulting from the flash flooding. One thunderstorm also caused some localized storm damage in Sampson County. Moisture from Tropical Storm Eta was drawn northward into the Mid Atlantic during the day of Wednesday November 11th. Meanwhile, a slow moving cold front approached the area and made its way through central North Carolina during the day Thursday, resulting in widespread showers and isolated thunderstorms. Rainfall totals were generally in the 4 to 6 inches range, although some spots near Rocky Mount saw close to 10 inches of rain by the time the event drew to a close. This resulted in numerous flooded road, including one death resulting from the flash flooding. One thunderstorm also caused some localized storm damage in Sampson County.\nEvent Narrative: Flash flooding was reported along Fountain Drive, where Walnut Creek had overflowed it\ufffd\ufffd\ufffds banks. Flash flooding was reported along Holly Springs New Hill Road near Cedar Wren Lane. Flash flooding was reported near the intersection of North Carolina Highway 98 and Moores Pond Road. Flash flooding was reported along Rex Road, between Avent Ferry Road and Cass Holt Road. Flash flooding was reported at the intersection of Wade Nash Road and Piney Grove Road. Flash flooding was reported along Duncan Cook Road near Buckhorn Duncan Road. Flash flooding was reported along Crabtree Creek at Old Wake Forest Road. Flash flooding was reported along Snow Hill Road between Snow Valley Road and Infinity Road. Flash flooding was reported in the 5700 Lord Granville Way, where a child drowned in the flood waters. Flash flooding and a water rescue were reported in the 12,000 block of Holly Springs New Hill Road.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 37.6582 km away, between 2020-12-24 21:09:00 and 2020-12-24 21:09:00. 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 line of showers and isolated thunderstorms intensified as it moved eastward across central North Carolina as an associated strong cold front moved across the area. As the line of convection moved across eastern portions of the area the line produced strong to damaging winds, resulting in some localized wind damage.\nEvent Narrative: Several trees were reported down along United States Highway 70, near Shortwell Road.",
+        "The following events were reported: Tornado. These occurred near station USW00013722, approximately 49.9788 km away, between 2021-03-18 17:04:00 and 2021-03-18 17:10:00.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 150000.0 and crop damage of 0.0. \n\nEpisode Narrative: A mid level trough approached central North Carolina from the west and moved across the area during the afternoon and evening. This helped spark a round of late day showers and thunderstorms, some of which produced severe weather across the central Piedmont along a cold air damming surface boundary. Several tornadic storms occurred along and north of Interstate 85 during the late afternoon hours along the aforementioned boundary.\nEvent Narrative: An EF-1 tornado tracked across portions of northern Orange County, with an estimated maximum wind gusts of around 100 miles per hour. The storm initially produced straight line wind damage across eastern Alamance County before producing more widespread tornado damage in Orange County a few minutes later. The tornado snapped off and downed numerous trees and power lines along the path, along with blowing a roof off a house near Pentecost Road.",
+        "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00013722, approximately 25.7881 km away, between 2021-03-27 15:02:00 and 2021-03-27 17:09:00. The events included records with hailstones measuring 25.5 inches.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 7500.0 and crop damage of 0.0. \n\nEpisode Narrative: Thunderstorms initially over middle and eastern Tennesse during the morning moved to the east of the Appalachians during the the afternoon, where they intercepted an east/west-oriented quasi-stationary front over central and eastern North Carolina. The storms intensified, while scattered supercells developed immediately preceding them, and tracked all generally eastward along and in the vicinity of the front. Some of the storms become strong to severe and produced large hail up to the size of a golf ball and damaging wind. Thunderstorms initially over middle and eastern Tennesse during the morning moved to the east of the Appalachians during the the afternoon, where they intercepted an east/west-oriented quasi-stationary front over central and eastern North Carolina. The storms intensified, while scattered supercells developed immediately preceding them, and tracked all generally eastward along and in the vicinity of the front. Some of the storms become strong to severe and produced large hail up to the size of a golf ball and damaging wind. Thunderstorms initially over middle and eastern Tennesse during the morning moved to the east of the Appalachians during the the afternoon, where they intercepted an east/west-oriented quasi-stationary front over central and eastern North Carolina. The storms intensified, while scattered supercells developed immediately preceding them, and tracked all generally eastward along and in the vicinity of the front. Some of the storms become strong to severe and produced large hail up to the size of a golf ball and damaging wind. Thunderstorms initially over middle and eastern Tennesse during the morning moved to the east of the Appalachians during the the afternoon, where they intercepted an east/west-oriented quasi-stationary front over central and eastern North Carolina. The storms intensified, while scattered supercells developed immediately preceding them, and tracked all generally eastward along and in the vicinity of the front. Some of the storms become strong to severe and produced large hail up to the size of a golf ball and damaging wind.\nEvent Narrative: Quarter size hail was reported near exit 326 on United States Highway 70. Trees were reported down near Lakemount Drive and Northwood Drive. A few trees were reported down at the Occoneechee Golf Course.",
+        "The following events were reported: Hail. These occurred near station USW00013722, approximately 25.8531 km away, between 2021-03-28 13:56:00 and 2021-03-28 13:56:00. 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 line of showers and embedded thunderstorms in the morning hours of March 28th over eastern Tennessee and western North Carolina pushed eastward ahead of a strong cold front. These storms intensified during the afternoon hours across portions of central North Carolina, producing several reports of trees down and quarter size hail.\nEvent Narrative: Penny sized hail reported at the intersection of Wescott Ridge Drive and Danagher Court.",
+        "The following events were reported: Hail. These occurred near station USW00013722, approximately 46.3613 km away, between 2021-04-09 15:36:00 and 2021-04-09 16:13:00. 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: A warm front draped across the region helped trigger scattered to numerous thunderstorms, some of which become severe across the Piedmont and northern Coastal Plain and produced hail up to the size of golf balls and isolated wind damage. A warm front draped across the region helped trigger scattered to numerous thunderstorms, some of which become severe across the Piedmont and northern Coastal Plain and produced hail up to the size of golf balls and isolated wind damage. A warm front draped across the region helped trigger scattered to numerous thunderstorms, some of which become severe across the Piedmont and northern Coastal Plain and produced hail up to the size of golf balls and isolated wind damage.\nEvent Narrative:",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 30.0387 km away, between 2021-05-04 14:25:00 and 2021-05-04 15:10:00. 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 1500.0 and crop damage of 0.0. \n\nEpisode Narrative: Showers and storms developed across the central Piedmont during the mid afternoon hours in a moist and unstable atmosphere. Several storms became severe and produced damaging wind gust and large hail. Showers and storms developed across the central Piedmont during the mid afternoon hours in a moist and unstable atmosphere. Several storms became severe and produced damaging wind gust and large hail. Showers and storms developed across the central Piedmont during the mid afternoon hours in a moist and unstable atmosphere. Several storms became severe and produced damaging wind gust and large hail. Showers and storms developed across the central Piedmont during the mid afternoon hours in a moist and unstable atmosphere. Several storms became severe and produced damaging wind gust and large hail. Showers and storms developed across the central Piedmont during the mid afternoon hours in a moist and unstable atmosphere. Several storms became severe and produced damaging wind gust and large hail.\nEvent Narrative: A tree was reported down at Highland Farm Road and Kenion Road. A tree was reported down on BPW Club Road in Carrboro. A tree was reported down near Linden Road. Two trees were reported down Chapel Hill. A tree was reported down in the 7000 block of North Carolina Highway 86.",
+        "The following events were reported: Hail. These occurred near station USW00013722, approximately 39.4758 km away, between 2021-05-07 13:24:00 and 2021-05-07 13:24:00. 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 weak area of low pressure tracked east across central and eastern North Carolina in the early morning hours and moved off toward the North Carolina coast by the afternoon. This low pressure formed along a cold front over the western Appalachians and Ohio Valley. Scattered showers and storms developed across central North Carolina in the morning, with the strongest storms over Moore County. These strong storms produced a swath of hail reports from three quarters of an inch to an inch across Moore, Johnston, Harnett, and Cumberland Counties as the storms tracked east-southeast toward the North Carolina coast. In the afternoon, additional scattered showers and storms developed along the cold front and largely only produced small to sub-severe hail.\nEvent Narrative: Three quarter inch hail was reported near the intersection of Castanea Road and Chestnut Ridge Church Road.",
+        "The following events were reported: Hail, Thunderstorm Wind, Tornado. These occurred near station USW00013722, approximately 37.0727 km away, between 2021-05-10 15:46:00 and 2021-05-10 16:20:00. The events included records with hailstones measuring 33.666666666666664 inches.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 140000.0 and crop damage of 0.0. \n\nEpisode Narrative: Scattered strong to severe storms formed just ahead of a cold front which moved into northern and western portions of central North Carolina during the early afternoon, before pushing southeast through central North Carolina through mid evening. Several of the storms produced damaging winds and large hail. The strongest supercell produced an |EF-1 tornado in southern portions of Alamance County. Scattered strong to severe storms formed just ahead of a cold front which moved into northern and western portions of central North Carolina during the early afternoon, before pushing southeast through central North Carolina through mid evening. Several of the storms produced damaging winds and large hail. The strongest supercell produced an |EF-1 tornado in southern portions of Alamance County. Scattered strong to severe storms formed just ahead of a cold front which moved into northern and western portions of central North Carolina during the early afternoon, before pushing southeast through central North Carolina through mid evening. Several of the storms produced damaging winds and large hail. The strongest supercell produced an |EF-1 tornado in southern portions of Alamance County. Scattered strong to severe storms formed just ahead of a cold front which moved into northern and western portions of central North Carolina during the early afternoon, before pushing southeast through central North Carolina through mid evening. Several of the storms produced damaging winds and large hail. The strongest supercell produced an |EF-1 tornado in southern portions of Alamance County. Scattered strong to severe storms formed just ahead of a cold front which moved into northern and western portions of central North Carolina during the early afternoon, before pushing southeast through central North Carolina through mid evening. Several of the storms produced damaging winds and large hail. The strongest supercell produced an |EF-1 tornado in southern portions of Alamance County. Scattered strong to severe storms formed just ahead of a cold front which moved into northern and western portions of central North Carolina during the early afternoon, before pushing southeast through central North Carolina through mid evening. Several of the storms produced damaging winds and large hail. The strongest supercell produced an |EF-1 tornado in southern portions of Alamance County. Scattered strong to severe storms formed just ahead of a cold front which moved into northern and western portions of central North Carolina during the early afternoon, before pushing southeast through central North Carolina through mid evening. Several of the storms produced damaging winds and large hail. The strongest supercell produced an |EF-1 tornado in southern portions of Alamance County.\nEvent Narrative: Trees were reported down on Crawford Dairy Road. A large tree was reported down on a home along Lamont Norwood Road near Tobacco Road. Trees were reported down on Linden Close Road. Trees were reported down on Manns Chapel Road near Great Ridge Parkway.   A supercell thunderstorm moved through southern portions of Alamance County, producing wind damage across the southern portion of the county. While there were several areas of damage consistent with straight line winds, damage to numerous trees and several structures along Greensboro Chapel Hill Rd near the town of Sutphin |were consistent with that of an EF-1 tornado. The tornado was on the ground for approximately 2 minutes and traveled a length of 1.25 |miles before lifting to the west of Stockard Rd.",
+        "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00013722, approximately 46.1211 km away, between 2021-05-29 15:43:00 and 2021-05-29 17:36:00. The events included records with hailstones measuring 37.75 inches.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 17500.0 and crop damage of 0.0. \n\nEpisode Narrative: A strong cold front arrived into central North Carolina during the late morning and afternoon. High temperatures reached 80 to 90 degrees at most locations. The cold front was associated with a large upper-level trough that was approaching the Mid-Atlantic states from the upper Midwest. The cold front pushed cool and stable air south and undercut the warm and humid air aloft, helping generate scattered thunderstorms. A few of these storms produced some wind damage and large hail. The severity of the storms diminished after sunset. A strong cold front arrived into central North Carolina during the late morning and afternoon. High temperatures reached 80 to 90 degrees at most locations. The cold front was associated with a large upper-level trough that was approaching the Mid-Atlantic states from the upper Midwest. The cold front pushed cool and stable air south and undercut the warm and humid air aloft, helping generate scattered thunderstorms. A few of these storms produced some wind damage and large hail. The severity of the storms diminished after sunset. A strong cold front arrived into central North Carolina during the late morning and afternoon. High temperatures reached 80 to 90 degrees at most locations. The cold front was associated with a large upper-level trough that was approaching the Mid-Atlantic states from the upper Midwest. The cold front pushed cool and stable air south and undercut the warm and humid air aloft, helping generate scattered thunderstorms. A few of these storms produced some wind damage and large hail. The severity of the storms diminished after sunset. A strong cold front arrived into central North Carolina during the late morning and afternoon. High temperatures reached 80 to 90 degrees at most locations. The cold front was associated with a large upper-level trough that was approaching the Mid-Atlantic states from the upper Midwest. The cold front pushed cool and stable air south and undercut the warm and humid air aloft, helping generate scattered thunderstorms. A few of these storms produced some wind damage and large hail. The severity of the storms diminished after sunset.\nEvent Narrative: A trained spotter reported quarter size hail near the town of Angier, at the intersection of Pondview Lane and Mabry Road. Several trees were reported down near the intersection of North Carolina highway 210 and North Carolina highway 50 North. Trees were reported down near the intersection of Old Mill Drive and Wiggins Road. An emergency manager reported a metal roof was blown off of a barn due to damaging straight line winds.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 27.263 km away, between 2021-07-01 20:43:00 and 2021-07-01 21:45:00. 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 15000.0 and crop damage of 0.0. \n\nEpisode Narrative: An unstable air mass was present across central North Carolina in the afternoon and evening of July 1. An approaching cold front, along with a large upper-level trough, were present across Virginia and North Carolina. Scattered thunderstorms developed over central South Carolina and moved northeast into North Carolina. These storms merged into a line of storms that produced widespread strong winds that downed numerous trees in central North Carolina. An unstable air mass was present across central North Carolina in the afternoon and evening of July 1. An approaching cold front, along with a large upper-level trough, were present across Virginia and North Carolina. Scattered thunderstorms developed over central South Carolina and moved northeast into North Carolina. These storms merged into a line of storms that produced widespread strong winds that downed numerous trees in central North Carolina. An unstable air mass was present across central North Carolina in the afternoon and evening of July 1. An approaching cold front, along with a large upper-level trough, were present across Virginia and North Carolina. Scattered thunderstorms developed over central South Carolina and moved northeast into North Carolina. These storms merged into a line of storms that produced widespread strong winds that downed numerous trees in central North Carolina. An unstable air mass was present across central North Carolina in the afternoon and evening of July 1. An approaching cold front, along with a large upper-level trough, were present across Virginia and North Carolina. Scattered thunderstorms developed over central South Carolina and moved northeast into North Carolina. These storms merged into a line of storms that produced widespread strong winds that downed numerous trees in central North Carolina. An unstable air mass was present across central North Carolina in the afternoon and evening of July 1. An approaching cold front, along with a large upper-level trough, were present across Virginia and North Carolina. Scattered thunderstorms developed over central South Carolina and moved northeast into North Carolina. These storms merged into a line of storms that produced widespread strong winds that downed numerous trees in central North Carolina. An unstable air mass was present across central North Carolina in the afternoon and evening of July 1. An approaching cold front, along with a large upper-level trough, were present across Virginia and North Carolina. Scattered thunderstorms developed over central South Carolina and moved northeast into North Carolina. These storms merged into a line of storms that produced widespread strong winds that downed numerous trees in central North Carolina. An unstable air mass was present across central North Carolina in the afternoon and evening of July 1. An approaching cold front, along with a large upper-level trough, were present across Virginia and North Carolina. Scattered thunderstorms developed over central South Carolina and moved northeast into North Carolina. These storms merged into a line of storms that produced widespread strong winds that downed numerous trees in central North Carolina.\nEvent Narrative: A tree was reported down near the intersection of Fieldcrest Ln and Parker Mill Trail. Trees fell down on a house on Pearson Street in Apex. A tree fell down on power lines near the intersection of Jackson-King Road and White Memorial Church Rd. One tree fell down near the intersection of Old Horseman Trail and Kemp Rd. A tree fell down across the roadway of Stony Hill Rd. One tree fell down near the intersection of Johnson Mill Rd and Lowell Rd. Trees fell down on power lines near the intersection of Old Franklinton Rd and Suitts Store Rd.",
+        "The following events were reported: Flash Flood. These occurred near station USW00013722, approximately 25.9123 km away, between 2021-07-08 15:32:00 and 2021-07-08 16:32:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Tropical Storm Elsa moved through central North Carolina during the daytime hours of Thursday, July 8. Widespread rainfall ranging from 2-5 inches affected areas along Highway US-1, with lesser amounts across the Coastal Plain and only a few tenths of an inch around the Greensboro and Winston-Salem areas. A few storms produced transient circulations capable of producing tornadoes. One report of flash flooding occurred as a result of Elsa.\nEvent Narrative: The intersection of Purnell Rd and Jackson Rd in Wake Forest was closed briefly due to flash flooding.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 30.0831 km away, between 2021-07-09 15:00:00 and 2021-07-09 17:00:00. 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: Plentiful moisture and a couple of weak surface troughs lingered over central North Carolina after the passage of tropical storm Elsa. Saturated ground was present as a result of two to five inches of rain over the eastern Piedmont into Virginia. Storms developed over the northwest foothills early in the afternoon and tracked east into the early evening hours over central North Carolina. Most storms were marginally severe but some reports included trees down across portions of the region. Antecedent soil conditions likely aided some of the downed trees. Plentiful moisture and a couple of weak surface troughs lingered over central North Carolina after the passage of tropical storm Elsa. Saturated ground was present as a result of two to five inches of rain over the eastern Piedmont into Virginia. Storms developed over the northwest foothills early in the afternoon and tracked east into the early evening hours over central North Carolina. Most storms were marginally severe but some reports included trees down across portions of the region. Antecedent soil conditions likely aided some of the downed trees. Plentiful moisture and a couple of weak surface troughs lingered over central North Carolina after the passage of tropical storm Elsa. Saturated ground was present as a result of two to five inches of rain over the eastern Piedmont into Virginia. Storms developed over the northwest foothills early in the afternoon and tracked east into the early evening hours over central North Carolina. Most storms were marginally severe but some reports included trees down across portions of the region. Antecedent soil conditions likely aided some of the downed trees. Plentiful moisture and a couple of weak surface troughs lingered over central North Carolina after the passage of tropical storm Elsa. Saturated ground was present as a result of two to five inches of rain over the eastern Piedmont into Virginia. Storms developed over the northwest foothills early in the afternoon and tracked east into the early evening hours over central North Carolina. Most storms were marginally severe but some reports included trees down across portions of the region. Antecedent soil conditions likely aided some of the downed trees. Plentiful moisture and a couple of weak surface troughs lingered over central North Carolina after the passage of tropical storm Elsa. Saturated ground was present as a result of two to five inches of rain over the eastern Piedmont into Virginia. Storms developed over the northwest foothills early in the afternoon and tracked east into the early evening hours over central North Carolina. Most storms were marginally severe but some reports included trees down across portions of the region. Antecedent soil conditions likely aided some of the downed trees. Plentiful moisture and a couple of weak surface troughs lingered over central North Carolina after the passage of tropical storm Elsa. Saturated ground was present as a result of two to five inches of rain over the eastern Piedmont into Virginia. Storms developed over the northwest foothills early in the afternoon and tracked east into the early evening hours over central North Carolina. Most storms were marginally severe but some reports included trees down across portions of the region. Antecedent soil conditions likely aided some of the downed trees. Plentiful moisture and a couple of weak surface troughs lingered over central North Carolina after the passage of tropical storm Elsa. Saturated ground was present as a result of two to five inches of rain over the eastern Piedmont into Virginia. Storms developed over the northwest foothills early in the afternoon and tracked east into the early evening hours over central North Carolina. Most storms were marginally severe but some reports included trees down across portions of the region. Antecedent soil conditions likely aided some of the downed trees. Plentiful moisture and a couple of weak surface troughs lingered over central North Carolina after the passage of tropical storm Elsa. Saturated ground was present as a result of two to five inches of rain over the eastern Piedmont into Virginia. Storms developed over the northwest foothills early in the afternoon and tracked east into the early evening hours over central North Carolina. Most storms were marginally severe but some reports included trees down across portions of the region. Antecedent soil conditions likely aided some of the downed trees. Plentiful moisture and a couple of weak surface troughs lingered over central North Carolina after the passage of tropical storm Elsa. Saturated ground was present as a result of two to five inches of rain over the eastern Piedmont into Virginia. Storms developed over the northwest foothills early in the afternoon and tracked east into the early evening hours over central North Carolina. Most storms were marginally severe but some reports included trees down across portions of the region. Antecedent soil conditions likely aided some of the downed trees. Plentiful moisture and a couple of weak surface troughs lingered over central North Carolina after the passage of tropical storm Elsa. Saturated ground was present as a result of two to five inches of rain over the eastern Piedmont into Virginia. Storms developed over the northwest foothills early in the afternoon and tracked east into the early evening hours over central North Carolina. Most storms were marginally severe but some reports included trees down across portions of the region. Antecedent soil conditions likely aided some of the downed trees.\nEvent Narrative: One tree was reported down on Trollingwood Lane. One tree was reported down on the roadway near the intersection of U.S. Highway 64 and Alex Cockman Rd. One tree fell near the intersection of Crawford Dairy Rd and Old Greensboro Rd in Chapel Hill. One tree fell on the roadway near the intersection of Old Graham Rd and Chapel Ridge Dr. Three trees fell down near the intersection of Garrett Rd and King Charles Rd. One tree fell down near the intersection of Lorilane Dr and Westbrook Dr in Carrboro. Two trees fell down at Falls Lake near Durham Rd. One tree fell down near the intersection of Sanders Rd and west Watson Rd. A power outage from downed power lines occurred near the intersection of Kildaire Farm Rd and Ten Ten Rd. One tree fell on a power line near the intersection of Seaforth Rd and Forest Ln.",
+        "The following events were reported: Lightning, Thunderstorm Wind. These occurred near station USW00013722, approximately 40.1565 km away, between 2021-07-17 15:25:00 and 2021-07-17 21:13:00.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 approaching cold front west and northwest of the Appalachian mountains tracked east into central North Carolina. A pre-frontal trough ahead of the cold front forced showers and thunderstorms during the evening hours, with several damaging wind reports and one lightning related house fire. An approaching cold front west and northwest of the Appalachian mountains tracked east into central North Carolina. A pre-frontal trough ahead of the cold front forced showers and thunderstorms during the evening hours, with several damaging wind reports and one lightning related house fire. An approaching cold front west and northwest of the Appalachian mountains tracked east into central North Carolina. A pre-frontal trough ahead of the cold front forced showers and thunderstorms during the evening hours, with several damaging wind reports and one lightning related house fire. An approaching cold front west and northwest of the Appalachian mountains tracked east into central North Carolina. A pre-frontal trough ahead of the cold front forced showers and thunderstorms during the evening hours, with several damaging wind reports and one lightning related house fire. An approaching cold front west and northwest of the Appalachian mountains tracked east into central North Carolina. A pre-frontal trough ahead of the cold front forced showers and thunderstorms during the evening hours, with several damaging wind reports and one lightning related house fire. An approaching cold front west and northwest of the Appalachian mountains tracked east into central North Carolina. A pre-frontal trough ahead of the cold front forced showers and thunderstorms during the evening hours, with several damaging wind reports and one lightning related house fire. An approaching cold front west and northwest of the Appalachian mountains tracked east into central North Carolina. A pre-frontal trough ahead of the cold front forced showers and thunderstorms during the evening hours, with several damaging wind reports and one lightning related house fire.\nEvent Narrative: An emergency manager reported a house was struck by lightning, causing a structure fire. One tree fell down near the intersection of Hassel St and Tryon St. One tree fell down near the intersection of North Carolina Highway 57 and Guess Rd. Power lines were down across the roadway at the intersection of Terry Rd and St. Mary's Rd. A tree fell down near the intersection of Ned Moore Rd and Windy Creek Cir. A tree fell down near the intersection of Dick Holeman Rd and Forest View Dr. Law enforcement reported multiple trees down near the intersection of Dick Holeman Rd and Durham Rd.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 39.166 km away, between 2021-07-28 13:30:00 and 2021-07-28 13:58:00. 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 10000.0 and crop damage of 0.0. \n\nEpisode Narrative: An upper-level and surface trough pushed from northwest to southeast across portions of central and eastern North Carolina during the afternoon and evening hours of July 28. A line of showers and storms formed along and east of the trough axis, resulting in some isolated damaging wind gusts across portions of the area. An upper-level and surface trough pushed from northwest to southeast across portions of central and eastern North Carolina during the afternoon and evening hours of July 28. A line of showers and storms formed along and east of the trough axis, resulting in some isolated damaging wind gusts across portions of the area.\nEvent Narrative: Broadcast Media reported trees and power lines down near Oakridge Duncan Rd. Fire department reported power lines down at the intersection of Oakridge River Road and Avery Spence Rd.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 45.7643 km away, between 2021-08-01 06:28:00 and 2021-08-01 06:28:00. 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: Showers and thunderstorms developed during the early to mid afternoon along a stationary front draped across central North Carolina from northeast to southwest. A very moist and unstable airmass was in place south of the stationary front. This combined with an unseasonably strong mid/upper level trough over the are resulted in a deep layer shear profile favorable for multicellular clusters and even a few supercells. Thus, as the showers and storms developed they quickly developed into clusters of storms with embedded supercells. Multiple storms/clusters became severe and produced wind damaging and large hail.\nEvent Narrative: One tree was reported down at the intersection of Pine Meadow Lane and Fieldsview Road.",
+        "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00013722, approximately 16.4588 km away, between 2021-08-14 13:35:00 and 2021-08-14 14:48:00. The events included records with hailstones measuring 33.64 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Scattered to numerous showers and thunderstorms developed along a pre-frontal trough in a very hot and unstable environment over the North Carolina Piedmont. Weak steering flow combined with the unstable environment resulted in both slow moving showers and thunderstorms and strong downdrafts, with new thunderstorms developing along the subsequent outflow boundaries. The storms produced damaging winds and isolated large hail and flash flooding. Scattered to numerous showers and thunderstorms developed along a pre-frontal trough in a very hot and unstable environment over the North Carolina Piedmont. Weak steering flow combined with the unstable environment resulted in both slow moving showers and thunderstorms and strong downdrafts, with new thunderstorms developing along the subsequent outflow boundaries. The storms produced damaging winds and isolated large hail and flash flooding. Scattered to numerous showers and thunderstorms developed along a pre-frontal trough in a very hot and unstable environment over the North Carolina Piedmont. Weak steering flow combined with the unstable environment resulted in both slow moving showers and thunderstorms and strong downdrafts, with new thunderstorms developing along the subsequent outflow boundaries. The storms produced damaging winds and isolated large hail and flash flooding. Scattered to numerous showers and thunderstorms developed along a pre-frontal trough in a very hot and unstable environment over the North Carolina Piedmont. Weak steering flow combined with the unstable environment resulted in both slow moving showers and thunderstorms and strong downdrafts, with new thunderstorms developing along the subsequent outflow boundaries. The storms produced damaging winds and isolated large hail and flash flooding. Scattered to numerous showers and thunderstorms developed along a pre-frontal trough in a very hot and unstable environment over the North Carolina Piedmont. Weak steering flow combined with the unstable environment resulted in both slow moving showers and thunderstorms and strong downdrafts, with new thunderstorms developing along the subsequent outflow boundaries. The storms produced damaging winds and isolated large hail and flash flooding. Scattered to numerous showers and thunderstorms developed along a pre-frontal trough in a very hot and unstable environment over the North Carolina Piedmont. Weak steering flow combined with the unstable environment resulted in both slow moving showers and thunderstorms and strong downdrafts, with new thunderstorms developing along the subsequent outflow boundaries. The storms produced damaging winds and isolated large hail and flash flooding. Scattered to numerous showers and thunderstorms developed along a pre-frontal trough in a very hot and unstable environment over the North Carolina Piedmont. Weak steering flow combined with the unstable environment resulted in both slow moving showers and thunderstorms and strong downdrafts, with new thunderstorms developing along the subsequent outflow boundaries. The storms produced damaging winds and isolated large hail and flash flooding. Scattered to numerous showers and thunderstorms developed along a pre-frontal trough in a very hot and unstable environment over the North Carolina Piedmont. Weak steering flow combined with the unstable environment resulted in both slow moving showers and thunderstorms and strong downdrafts, with new thunderstorms developing along the subsequent outflow boundaries. The storms produced damaging winds and isolated large hail and flash flooding. Scattered to numerous showers and thunderstorms developed along a pre-frontal trough in a very hot and unstable environment over the North Carolina Piedmont. Weak steering flow combined with the unstable environment resulted in both slow moving showers and thunderstorms and strong downdrafts, with new thunderstorms developing along the subsequent outflow boundaries. The storms produced damaging winds and isolated large hail and flash flooding.\nEvent Narrative: The public reported nickel size hail near Cary Parkway and Holly Springs Road. The public reported up to quarter size hail at the Raleigh Durham International Airport. A large tree was reported down near the intersection of Avent Ferry Road and Center Hill Drive. The road was closed between Center Hill Drive and New Hill Holleman Road. The public reported nickel size hail in north Raleigh near Falls Lake. A tree was reported down along Melvin Arnold Road. A tree was reported down near the intersection of Norwood Road and Mount Vernon Church Road. A tree was reported down near the intersection of Fall Line Court and Old Creedmoor Road. A tree was reported down near the intersection of North Falls Drive and Creedmoor Road. A tree was reported down at Highway 64 West near Zebulon.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 43.2667 km away, between 2021-08-20 15:03:00 and 2021-08-20 19:28:00. 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 stationary frontal boundary was draped from northeast to southwest across central North Carolina. A series of mid-level disturbances tracked along the front to produce scattered to numerous showers and thunderstorms in the late afternoon into the late evening hours. Some of the storms produced downed trees with localized strong storms in a favorable moist environment. A stationary frontal boundary was draped from northeast to southwest across central North Carolina. A series of mid-level disturbances tracked along the front to produce scattered to numerous showers and thunderstorms in the late afternoon into the late evening hours. Some of the storms produced downed trees with localized strong storms in a favorable moist environment. A stationary frontal boundary was draped from northeast to southwest across central North Carolina. A series of mid-level disturbances tracked along the front to produce scattered to numerous showers and thunderstorms in the late afternoon into the late evening hours. Some of the storms produced downed trees with localized strong storms in a favorable moist environment. A stationary frontal boundary was draped from northeast to southwest across central North Carolina. A series of mid-level disturbances tracked along the front to produce scattered to numerous showers and thunderstorms in the late afternoon into the late evening hours. Some of the storms produced downed trees with localized strong storms in a favorable moist environment.\nEvent Narrative: One tree was reported down across the roadway near the intersection of Loop Road and Covered Bridge Road. Multiple trees down near the intersection of North Carolina Highway 42 East and Glen Laurel Road. A large tree was reported down near the intersection of Chestnut Ridge Church Road and Castanea Road. A tree fell on power lines near the intersection of Payne Road and Brevard Road. The power lines also fell on a car.",
+        "The following events were reported: Lightning. These occurred near station USW00013722, approximately 18.88 km away, between 2021-09-08 10:40:00 and 2021-09-08 10:40:00.The events resulted in 3 injuries and 0 fatalities. No significant property or crop damage was reported. \n\nEpisode Narrative: A cluster of showers and storms producing heavy rain develop across Warren County in central North Carolina along a slow moving mid level disturbance in advance of a slow moving cold front. The heavy rain produced a couple of reports fo flash flooding across Warren County.\nEvent Narrative: Three men were injured by lightning at an apartment complex along Broad Street.",
+        "The following events were reported: Flash Flood. These occurred near station USW00013722, approximately 14.5096 km away, between 2021-09-09 10:34:00 and 2021-09-09 13:15:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A band of slow moving showers and thunderstorms producing heavy rain along a slow moving cold front and produced flash flooding across Wake County in central North Carolina. A band of slow moving showers and thunderstorms producing heavy rain along a slow moving cold front and produced flash flooding across Wake County in central North Carolina.\nEvent Narrative: Flash flooding was reported in the 2300 block of Atlantic Avenue, where a water rescue occurred. Flash flooding closed multiple westbound lanes of Interstate 440.",
+        "The following events were reported: Flash Flood, Heavy Rain. These occurred near station USW00013722, approximately 14.9123 km away, between 2021-10-09 06:30:00 and 2021-10-09 12:30:00.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 250000.0 and crop damage of 0.0. \n\nEpisode Narrative: The combination of high moisture content air and a slow moving negatively tilted upper trough, along with a boundary stalled across the area resulted in areas of very heavy rain during the morning into the afternoon. Some of the areas of heavy rain produced flash flooding across portions of the central Piedmont and central Coastal Plain of central North Carolina. The combination of high moisture content air and a slow moving negatively tilted upper trough, along with a boundary stalled across the area resulted in areas of very heavy rain during the morning into the afternoon. Some of the areas of heavy rain produced flash flooding across portions of the central Piedmont and central Coastal Plain of central North Carolina. The combination of high moisture content air and a slow moving negatively tilted upper trough, along with a boundary stalled across the area resulted in areas of very heavy rain during the morning into the afternoon. Some of the areas of heavy rain produced flash flooding across portions of the central Piedmont and central Coastal Plain of central North Carolina. The combination of high moisture content air and a slow moving negatively tilted upper trough, along with a boundary stalled across the area resulted in areas of very heavy rain during the morning into the afternoon. Some of the areas of heavy rain produced flash flooding across portions of the central Piedmont and central Coastal Plain of central North Carolina. The combination of high moisture content air and a slow moving negatively tilted upper trough, along with a boundary stalled across the area resulted in areas of very heavy rain during the morning into the afternoon. Some of the areas of heavy rain produced flash flooding across portions of the central Piedmont and central Coastal Plain of central North Carolina. The combination of high moisture content air and a slow moving negatively tilted upper trough, along with a boundary stalled across the area resulted in areas of very heavy rain during the morning into the afternoon. Some of the areas of heavy rain produced flash flooding across portions of the central Piedmont and central Coastal Plain of central North Carolina.\nEvent Narrative: Flash flooding was reported near the intersection of Westgate Road and Fast Park Drive, where Sycamore Creek runs under Fast Park Drive. Numerous cars were stalled in the flood waters at this location. Flash flooding was reported along Holly Springs New Hill Road between Cedar Wren Lane and Cateswood Court, do to flash flooding along White Oak Creek. Campbell Road was closed near Holly Springs Road due to flash flooding. A trained spotter reported 6.04 inches of rain in the 100 block of Tower Hamlet Drive. Flash flooding was reported near the 5200 block of Dana Drive, where apartments were flooding. The lower parking deck at Crabtree Valley Mall was flooded do to flash flooding near Crabtree Creek.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 23.8093 km away, between 2021-10-25 19:55:00 and 2021-10-25 20:12:00. 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 2500.0 and crop damage of 0.0. \n\nEpisode Narrative: A line of strong to severe storms moved across the northern Piedmont of central North Carolina during the evening in advance of a strong cold front, resulting in several reports of wind damage. A line of strong to severe storms moved across the northern Piedmont of central North Carolina during the evening in advance of a strong cold front, resulting in several reports of wind damage. A line of strong to severe storms moved across the northern Piedmont of central North Carolina during the evening in advance of a strong cold front, resulting in several reports of wind damage.\nEvent Narrative: Power lines were reported down near the intersection of Range Road and Cassam Road. One tree was reported down near the intersection of Range Road and Hampton Road. One tree was reported down near the intersection of Leesville Road and Doc Nichols Road.",
+        "The following events were reported: Flash Flood, Heavy Rain, Thunderstorm Wind. These occurred near station USW00013722, approximately 20.3999 km away, between 2022-01-03 06:16:00 and 2022-01-03 10:37:00.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 strong upper level low moved from the Midwest into the Mid Atlantic from January 2nd into the 3rd. Strong storms to isolated severe storms preceded the arrival of the low along with a broad area of 2 to 4 inches of rain along United States Highway 1 corridor, producing flooding around the Triangle region of central North Carolina. Strong sustained gradient winds were felt over much of the area, with numerous gusts of 35 to 50 miles per hour. As the low moved through the area, rain mixed with and changed to snow with several inches of snow reported across portions of the northwest and far northern Piedmont. A strong upper level low moved from the Midwest into the Mid Atlantic from January 2nd into the 3rd. Strong storms to isolated severe storms preceded the arrival of the low along with a broad area of 2 to 4 inches of rain along United States Highway 1 corridor, producing flooding around the Triangle region of central North Carolina. Strong sustained gradient winds were felt over much of the area, with numerous gusts of 35 to 50 miles per hour. As the low moved through the area, rain mixed with and changed to snow with several inches of snow reported across portions of the northwest and far northern Piedmont. A strong upper level low moved from the Midwest into the Mid Atlantic from January 2nd into the 3rd. Strong storms to isolated severe storms preceded the arrival of the low along with a broad area of 2 to 4 inches of rain along United States Highway 1 corridor, producing flooding around the Triangle region of central North Carolina. Strong sustained gradient winds were felt over much of the area, with numerous gusts of 35 to 50 miles per hour. As the low moved through the area, rain mixed with and changed to snow with several inches of snow reported across portions of the northwest and far northern Piedmont. A strong upper level low moved from the Midwest into the Mid Atlantic from January 2nd into the 3rd. Strong storms to isolated severe storms preceded the arrival of the low along with a broad area of 2 to 4 inches of rain along United States Highway 1 corridor, producing flooding around the Triangle region of central North Carolina. Strong sustained gradient winds were felt over much of the area, with numerous gusts of 35 to 50 miles per hour. As the low moved through the area, rain mixed with and changed to snow with several inches of snow reported across portions of the northwest and far northern Piedmont. A strong upper level low moved from the Midwest into the Mid Atlantic from January 2nd into the 3rd. Strong storms to isolated severe storms preceded the arrival of the low along with a broad area of 2 to 4 inches of rain along United States Highway 1 corridor, producing flooding around the Triangle region of central North Carolina. Strong sustained gradient winds were felt over much of the area, with numerous gusts of 35 to 50 miles per hour. As the low moved through the area, rain mixed with and changed to snow with several inches of snow reported across portions of the northwest and far northern Piedmont. A strong upper level low moved from the Midwest into the Mid Atlantic from January 2nd into the 3rd. Strong storms to isolated severe storms preceded the arrival of the low along with a broad area of 2 to 4 inches of rain along United States Highway 1 corridor, producing flooding around the Triangle region of central North Carolina. Strong sustained gradient winds were felt over much of the area, with numerous gusts of 35 to 50 miles per hour. As the low moved through the area, rain mixed with and changed to snow with several inches of snow reported across portions of the northwest and far northern Piedmont. A strong upper level low moved from the Midwest into the Mid Atlantic from January 2nd into the 3rd. Strong storms to isolated severe storms preceded the arrival of the low along with a broad area of 2 to 4 inches of rain along United States Highway 1 corridor, producing flooding around the Triangle region of central North Carolina. Strong sustained gradient winds were felt over much of the area, with numerous gusts of 35 to 50 miles per hour. As the low moved through the area, rain mixed with and changed to snow with several inches of snow reported across portions of the northwest and far northern Piedmont. A strong upper level low moved from the Midwest into the Mid Atlantic from January 2nd into the 3rd. Strong storms to isolated severe storms preceded the arrival of the low along with a broad area of 2 to 4 inches of rain along United States Highway 1 corridor, producing flooding around the Triangle region of central North Carolina. Strong sustained gradient winds were felt over much of the area, with numerous gusts of 35 to 50 miles per hour. As the low moved through the area, rain mixed with and changed to snow with several inches of snow reported across portions of the northwest and far northern Piedmont. A strong upper level low moved from the Midwest into the Mid Atlantic from January 2nd into the 3rd. Strong storms to isolated severe storms preceded the arrival of the low along with a broad area of 2 to 4 inches of rain along United States Highway 1 corridor, producing flooding around the Triangle region of central North Carolina. Strong sustained gradient winds were felt over much of the area, with numerous gusts of 35 to 50 miles per hour. As the low moved through the area, rain mixed with and changed to snow with several inches of snow reported across portions of the northwest and far northern Piedmont. A strong upper level low moved from the Midwest into the Mid Atlantic from January 2nd into the 3rd. Strong storms to isolated severe storms preceded the arrival of the low along with a broad area of 2 to 4 inches of rain along United States Highway 1 corridor, producing flooding around the Triangle region of central North Carolina. Strong sustained gradient winds were felt over much of the area, with numerous gusts of 35 to 50 miles per hour. As the low moved through the area, rain mixed with and changed to snow with several inches of snow reported across portions of the northwest and far northern Piedmont. A strong upper level low moved from the Midwest into the Mid Atlantic from January 2nd into the 3rd. Strong storms to isolated severe storms preceded the arrival of the low along with a broad area of 2 to 4 inches of rain along United States Highway 1 corridor, producing flooding around the Triangle region of central North Carolina. Strong sustained gradient winds were felt over much of the area, with numerous gusts of 35 to 50 miles per hour. As the low moved through the area, rain mixed with and changed to snow with several inches of snow reported across portions of the northwest and far northern Piedmont.\nEvent Narrative: Flash flooding was reported along Umstead Drive in between Pritchard Avenue and Martin Luther King Junior Boulevard. Flash flooding was reported on I-40 at exit 291. Flash flooding was reported along Highway 1 in northern Wake County. Flash flooding was reported along eastbound lanes of I-40, near the Highway 751 exit. A car was stranded in the flood water at this location as well. Flash flooding was reported underneath the I-440 overpass along Western Boulevard. Storm total rainfall of 3.02 inches was reported near Spring Forest Road Park. Flash flooding was reported along he entrance ramp to Western Boulevard. Flash flooding was reported along I-440, just to the east of the Pool Road exit. One tree was reported down along Johnston Pond Road. Flash flooding was reported along Old Mason Farm Road. Flash flooding was reported at Oakwood drive at Cleland Drive.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 30.4046 km away, between 2022-03-07 20:41:00 and 2022-03-07 20:55:00. 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 tracked east-southeast from the Ohio Valley into the southeastern United States late in the evening on the 7th of March. Ahead of the front, weak instability was met by strong deep-layer shear for isolated to scattered showers and storms. A line of showers and storms tracked from the Northwest Piedmont in the early evening into the Northern Coastal Plain by late evening. Most of the storms were sub-severe, though a strong cell developed in the northern part of the line, producing some damaging wind reports in Granville and Franklin Counties. A cold front tracked east-southeast from the Ohio Valley into the southeastern United States late in the evening on the 7th of March. Ahead of the front, weak instability was met by strong deep-layer shear for isolated to scattered showers and storms. A line of showers and storms tracked from the Northwest Piedmont in the early evening into the Northern Coastal Plain by late evening. Most of the storms were sub-severe, though a strong cell developed in the northern part of the line, producing some damaging wind reports in Granville and Franklin Counties. A cold front tracked east-southeast from the Ohio Valley into the southeastern United States late in the evening on the 7th of March. Ahead of the front, weak instability was met by strong deep-layer shear for isolated to scattered showers and storms. A line of showers and storms tracked from the Northwest Piedmont in the early evening into the Northern Coastal Plain by late evening. Most of the storms were sub-severe, though a strong cell developed in the northern part of the line, producing some damaging wind reports in Granville and Franklin Counties.\nEvent Narrative: A state official reported a tree down near Butner, NC. Powerlines and power poles were reported down near the intersection of Hayes Road and Bennett Road in Creedmoor. A tree was reported down near the intersection of Cedar Creek Road and Lane Store Road. The tree was blocking the roadway.",
+        "The following events were reported: Flash Flood. These occurred near station USW00013722, approximately 17.6031 km away, between 2022-03-17 07:15:00 and 2022-03-17 09:15:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A strong mid-level trough of low pressure over Georgia tracked northeast into the Carolinas early on the morning of the 17th of March. At the surface, a surface low tracked northeast along the eastern Piedmont and Coastal Plain during the early morning hours. A warm front also was tied to the system. This area of low pressure provided deep lift and moisture for periods of widespread rain and some heavier storms capable of flash flooding. There was one report of flash flooding in Wake County in the morning of the 17th.\nEvent Narrative: The onramp from South Dawson Street to Martin Luther King Jr. Boulevard was closed due to flash flooding.",
+        "The following events were reported: Thunderstorm Wind, Tornado. These occurred near station USW00013722, approximately 5.1904 km away, between 2022-03-31 12:50:00 and 2022-03-31 14:50:00.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 115000.0 and crop damage of 0.0. \n\nEpisode Narrative: A pre-frontal band of showers and isolated thunderstorms moved into a marginally unstable but highly sheared environment leading to a couple of tornadoes, namely in Anson into Stanly counties and just west of the Raleigh Durham International Airport from Research Triangle Park into southeast Durham County. A pre-frontal band of showers and isolated thunderstorms moved into a marginally unstable but highly sheared environment leading to a couple of tornadoes, namely in Anson into Stanly counties and just west of the Raleigh Durham International Airport from Research Triangle Park into southeast Durham County.\nEvent Narrative: A brief and fast moving EF-1 tornado touched down and began uprooting and snapping numerous trees near Shilo Glenn Drive near the Wake and Durham County line in southern Durham County. In addition, an HVAC unit was dislodged and flipped over on the roof of a warehouse building before quickly dissipating. Several trees were uprooted and damage was noted to a fence along near North Carolina Highway 540 and Slater Road.",
+        "The following events were reported: Lightning, Thunderstorm Wind. These occurred near station USW00013722, approximately 42.3831 km away, between 2022-04-07 15:15:00 and 2022-04-07 16:39:00.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: A warm, moist, and unstable air mass ahead of an approaching cold and deep mid to upper level trough allowed for the development of showers and thunderstorms across eastern portions of the area. Several supercelll thunderstorms formed, resulting in large hail and damaging straight line winds. A warm, moist, and unstable air mass ahead of an approaching cold and deep mid to upper level trough allowed for the development of showers and thunderstorms across eastern portions of the area. Several supercelll thunderstorms formed, resulting in large hail and damaging straight line winds. A warm, moist, and unstable air mass ahead of an approaching cold and deep mid to upper level trough allowed for the development of showers and thunderstorms across eastern portions of the area. Several supercelll thunderstorms formed, resulting in large hail and damaging straight line winds. A warm, moist, and unstable air mass ahead of an approaching cold and deep mid to upper level trough allowed for the development of showers and thunderstorms across eastern portions of the area. Several supercelll thunderstorms formed, resulting in large hail and damaging straight line winds.\nEvent Narrative: A tree was reported down near I-40. A tree was reported down near the North Carolina Highway 42 and I-40 interchange. A house was struck by lightning, causing a fire, along Covered Bridge Road. A pine tree was reported down on Chamblee Road.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 25.0891 km away, between 2022-04-26 14:18:00 and 2022-04-26 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 92500.0 and crop damage of 0.0. \n\nEpisode Narrative: A cold front crossed the mountains during the late morning then moved into the Foothills by around noon. A line of showers and thunderstorms developed along an outflow out ahead of the front in a moist and unstable airmass over the southwest Piedmont of central North Carolina and spread quickly east across the area during the afternoon into the early evening. Numerous trees were downed by wind gusts in the stronger storms. A cold front crossed the mountains during the late morning then moved into the Foothills by around noon. A line of showers and thunderstorms developed along an outflow out ahead of the front in a moist and unstable airmass over the southwest Piedmont of central North Carolina and spread quickly east across the area during the afternoon into the early evening. Numerous trees were downed by wind gusts in the stronger storms. A cold front crossed the mountains during the late morning then moved into the Foothills by around noon. A line of showers and thunderstorms developed along an outflow out ahead of the front in a moist and unstable airmass over the southwest Piedmont of central North Carolina and spread quickly east across the area during the afternoon into the early evening. Numerous trees were downed by wind gusts in the stronger storms. A cold front crossed the mountains during the late morning then moved into the Foothills by around noon. A line of showers and thunderstorms developed along an outflow out ahead of the front in a moist and unstable airmass over the southwest Piedmont of central North Carolina and spread quickly east across the area during the afternoon into the early evening. Numerous trees were downed by wind gusts in the stronger storms. A cold front crossed the mountains during the late morning then moved into the Foothills by around noon. A line of showers and thunderstorms developed along an outflow out ahead of the front in a moist and unstable airmass over the southwest Piedmont of central North Carolina and spread quickly east across the area during the afternoon into the early evening. Numerous trees were downed by wind gusts in the stronger storms. A cold front crossed the mountains during the late morning then moved into the Foothills by around noon. A line of showers and thunderstorms developed along an outflow out ahead of the front in a moist and unstable airmass over the southwest Piedmont of central North Carolina and spread quickly east across the area during the afternoon into the early evening. Numerous trees were downed by wind gusts in the stronger storms. A cold front crossed the mountains during the late morning then moved into the Foothills by around noon. A line of showers and thunderstorms developed along an outflow out ahead of the front in a moist and unstable airmass over the southwest Piedmont of central North Carolina and spread quickly east across the area during the afternoon into the early evening. Numerous trees were downed by wind gusts in the stronger storms. A cold front crossed the mountains during the late morning then moved into the Foothills by around noon. A line of showers and thunderstorms developed along an outflow out ahead of the front in a moist and unstable airmass over the southwest Piedmont of central North Carolina and spread quickly east across the area during the afternoon into the early evening. Numerous trees were downed by wind gusts in the stronger storms. A cold front crossed the mountains during the late morning then moved into the Foothills by around noon. A line of showers and thunderstorms developed along an outflow out ahead of the front in a moist and unstable airmass over the southwest Piedmont of central North Carolina and spread quickly east across the area during the afternoon into the early evening. Numerous trees were downed by wind gusts in the stronger storms. A cold front crossed the mountains during the late morning then moved into the Foothills by around noon. A line of showers and thunderstorms developed along an outflow out ahead of the front in a moist and unstable airmass over the southwest Piedmont of central North Carolina and spread quickly east across the area during the afternoon into the early evening. Numerous trees were downed by wind gusts in the stronger storms. A cold front crossed the mountains during the late morning then moved into the Foothills by around noon. A line of showers and thunderstorms developed along an outflow out ahead of the front in a moist and unstable airmass over the southwest Piedmont of central North Carolina and spread quickly east across the area during the afternoon into the early evening. Numerous trees were downed by wind gusts in the stronger storms.\nEvent Narrative: A tree was reported down along United States Highway 15/501. A tree was reported down on a house near Harkey Lane. Power lines were reported down across Wimberly Road. A tree was reported down near the intersection of Dick Holeman Road and Ned Moore Road. A tree was reported down along Harrison Ridge road near Woodcross Way. A tree was reported down across Hester Road. Trees and power lines were reported down along Birch Drive. A large tree was reported down on Louisburg Road. Multiple trees were reported down on Doc Nichols Road. A large tree was reported down at near Nazareth Street and Crusader Drive. An apartment building near the intersection of North Smithfield Road and Aragon Drive sustained damage to the roof and shingles blown off.",
+        "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00013722, approximately 35.568 km away, between 2022-05-01 16:08:00 and 2022-05-01 17:20:00. The events included records with hailstones measuring 30.4 inches.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 15000.0 and crop damage of 0.0. \n\nEpisode Narrative: A weak frontal zone sat and wavered generally west to east across North Carolina. A mid level perturbation along with daytime heating spawned loosely organized thunderstorms, starting in the Triad region around in the mid to late afternoon and growing upscale and expanding across the Piedmont with an east-southeastward motion. Some of the strongest storms became severe and produced damaging wind gusts and large hail. Storms became outflow dominant and weakened as they headed into eastern portions of central North Carolina. A weak frontal zone sat and wavered generally west to east across North Carolina. A mid level perturbation along with daytime heating spawned loosely organized thunderstorms, starting in the Triad region around in the mid to late afternoon and growing upscale and expanding across the Piedmont with an east-southeastward motion. Some of the strongest storms became severe and produced damaging wind gusts and large hail. Storms became outflow dominant and weakened as they headed into eastern portions of central North Carolina. A weak frontal zone sat and wavered generally west to east across North Carolina. A mid level perturbation along with daytime heating spawned loosely organized thunderstorms, starting in the Triad region around in the mid to late afternoon and growing upscale and expanding across the Piedmont with an east-southeastward motion. Some of the strongest storms became severe and produced damaging wind gusts and large hail. Storms became outflow dominant and weakened as they headed into eastern portions of central North Carolina. A weak frontal zone sat and wavered generally west to east across North Carolina. A mid level perturbation along with daytime heating spawned loosely organized thunderstorms, starting in the Triad region around in the mid to late afternoon and growing upscale and expanding across the Piedmont with an east-southeastward motion. Some of the strongest storms became severe and produced damaging wind gusts and large hail. Storms became outflow dominant and weakened as they headed into eastern portions of central North Carolina. A weak frontal zone sat and wavered generally west to east across North Carolina. A mid level perturbation along with daytime heating spawned loosely organized thunderstorms, starting in the Triad region around in the mid to late afternoon and growing upscale and expanding across the Piedmont with an east-southeastward motion. Some of the strongest storms became severe and produced damaging wind gusts and large hail. Storms became outflow dominant and weakened as they headed into eastern portions of central North Carolina.\nEvent Narrative: Quarter size hail was reported near Efland - Cedar Grove Road and McGown Creek Road. A tree fell on powerlines near the intersection of Fayetteville Street and West Street in Pittsboro. A power outage was caused by objects coming in contact with power lines in Corinth, near the intersection of NC Highway 42 and Buckhorn Rd. A power outage was caused by fallen trees damaging the power equipment, near the intersection of Infinity Rd and Seterra Bend in Durham. Quarter size hail was reported near Holly Springs, near the intersection of Avent Ferry Rd and Buckhorn Duncan Rd.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 36.6284 km away, between 2022-05-03 15:14:00 and 2022-05-03 15:14:00. 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 stalled frontal zone was located over northeastern North Carolina and south-central Virginia during the day, while a lee surface trough was present over the Foothills of western North Carolina. A mid-level perturbation along with daytime heating led to the development of isolated to widely scattered showers and storms, starting over the western and central Piedmont in the mid to late afternoon, growing upscale into a line of storms and expanding into the Sandhills and southern Coastal Plain by the late afternoon and evening hours. Some of the stronger storms became severe and produced damaging winds and large hail. The storms moved east toward the coast and dissipated by late evening with the loss of daytime heating.\nEvent Narrative: Multiple trees reported down in the town of Fuquay-Varina, near the intersection of Howard Rd and Wagstaff Rd.",
+        "The following events were reported: Hail, Lightning, Thunderstorm Wind, Tornado. These occurred near station USW00013722, approximately 17.7054 km away, between 2022-05-06 14:21:00 and 2022-05-06 19:40:00. The events included records with hailstones measuring 32.95454545454545 inches.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 262000.0 and crop damage of 0.0. \n\nEpisode Narrative: Strong southerly flow lifted a warm front through central North Carolina Friday afternoon, triggering multiple rounds of severe and tornadic storms producing a radar confirmed tornado near the Orange/Alamance County line and hail up to golf ball size over the southern Piedmont and Sandhills. Numerous wind reports were also noted across the Sandhills and the Northwest and Northeast Piedmont. Strong southerly flow lifted a warm front through central North Carolina Friday afternoon, triggering multiple rounds of severe and tornadic storms producing a radar confirmed tornado near the Orange/Alamance County line and hail up to golf ball size over the southern Piedmont and Sandhills. Numerous wind reports were also noted across the Sandhills and the Northwest and Northeast Piedmont. Strong southerly flow lifted a warm front through central North Carolina Friday afternoon, triggering multiple rounds of severe and tornadic storms producing a radar confirmed tornado near the Orange/Alamance County line and hail up to golf ball size over the southern Piedmont and Sandhills. Numerous wind reports were also noted across the Sandhills and the Northwest and Northeast Piedmont. Strong southerly flow lifted a warm front through central North Carolina Friday afternoon, triggering multiple rounds of severe and tornadic storms producing a radar confirmed tornado near the Orange/Alamance County line and hail up to golf ball size over the southern Piedmont and Sandhills. Numerous wind reports were also noted across the Sandhills and the Northwest and Northeast Piedmont. Strong southerly flow lifted a warm front through central North Carolina Friday afternoon, triggering multiple rounds of severe and tornadic storms producing a radar confirmed tornado near the Orange/Alamance County line and hail up to golf ball size over the southern Piedmont and Sandhills. Numerous wind reports were also noted across the Sandhills and the Northwest and Northeast Piedmont. Strong southerly flow lifted a warm front through central North Carolina Friday afternoon, triggering multiple rounds of severe and tornadic storms producing a radar confirmed tornado near the Orange/Alamance County line and hail up to golf ball size over the southern Piedmont and Sandhills. Numerous wind reports were also noted across the Sandhills and the Northwest and Northeast Piedmont. Strong southerly flow lifted a warm front through central North Carolina Friday afternoon, triggering multiple rounds of severe and tornadic storms producing a radar confirmed tornado near the Orange/Alamance County line and hail up to golf ball size over the southern Piedmont and Sandhills. Numerous wind reports were also noted across the Sandhills and the Northwest and Northeast Piedmont. Strong southerly flow lifted a warm front through central North Carolina Friday afternoon, triggering multiple rounds of severe and tornadic storms producing a radar confirmed tornado near the Orange/Alamance County line and hail up to golf ball size over the southern Piedmont and Sandhills. Numerous wind reports were also noted across the Sandhills and the Northwest and Northeast Piedmont. Strong southerly flow lifted a warm front through central North Carolina Friday afternoon, triggering multiple rounds of severe and tornadic storms producing a radar confirmed tornado near the Orange/Alamance County line and hail up to golf ball size over the southern Piedmont and Sandhills. Numerous wind reports were also noted across the Sandhills and the Northwest and Northeast Piedmont. Strong southerly flow lifted a warm front through central North Carolina Friday afternoon, triggering multiple rounds of severe and tornadic storms producing a radar confirmed tornado near the Orange/Alamance County line and hail up to golf ball size over the southern Piedmont and Sandhills. Numerous wind reports were also noted across the Sandhills and the Northwest and Northeast Piedmont. Strong southerly flow lifted a warm front through central North Carolina Friday afternoon, triggering multiple rounds of severe and tornadic storms producing a radar confirmed tornado near the Orange/Alamance County line and hail up to golf ball size over the southern Piedmont and Sandhills. Numerous wind reports were also noted across the Sandhills and the Northwest and Northeast Piedmont. Strong southerly flow lifted a warm front through central North Carolina Friday afternoon, triggering multiple rounds of severe and tornadic storms producing a radar confirmed tornado near the Orange/Alamance County line and hail up to golf ball size over the southern Piedmont and Sandhills. Numerous wind reports were also noted across the Sandhills and the Northwest and Northeast Piedmont. Strong southerly flow lifted a warm front through central North Carolina Friday afternoon, triggering multiple rounds of severe and tornadic storms producing a radar confirmed tornado near the Orange/Alamance County line and hail up to golf ball size over the southern Piedmont and Sandhills. Numerous wind reports were also noted across the Sandhills and the Northwest and Northeast Piedmont.\nEvent Narrative: Trees were reported down near Fearrington near the intersection of E Camden and E Madison. Quarter size hail reported near Apex at the intersection of Apex Barbeque Rd and Kelly Rd. The wind observation at Raleigh-Durham International airport measured a peak wind of 55 kts. There were multiple reports of quarter size hail in the town of Morrisville. One report was near the intersection of Singer Way and Rope Walk Ct. A trained spotter measured half dollar size hail near the town of cary, at the intersection of Castalia Dr and Old Apex Rd. A large tree was reported down near the Raleigh-Durham International Airport, blocking the road, near the intersection of Airport Blvd and Cedar Fork Dr. A trained spotter estimated half dollar size hail at the Raleigh-Durham International Airport, near the intersection of Airport Blvd and Cedar Fork Dr. A house fire was reported when there was frequent lighting from thunderstorms. No injuries were reported. Multiple trees were reported down near Falls Lake, near the intersection of Six Forks Rd and Mt Vernon Church Rd. Numerous power outages were reported east of Angier caused by downed trees, near the intersection of Old Stage Rd N and Piney Grove Rd. Multiple trees were reported down near Pittsboro, near the intersection of Mt. Gilead Church Rd and Bartlett Dr. The wind observation at Raleigh-Durham International Airport reported a second wind gust to 61 mph due to a severe thunderstorm. A tornado touched down two miles east of Mebane at 5:08 PM EDT. Damage at this location consisted of a brick wall of a large manufacturing facility that was blown over. The tornado then continued to move approximately 3.6 miles to the northeast before lifting and dissipating at 5:15 PM EDT.  Along the track, damage consisted of mostly uprooted hardwood trees and snapped softwood or pine trees. In several cases, the trees fell onto homes, which resulted in damage to the homes. At least one detached garage was completely destroyed and its roof and walls were scattered in nearly all directions. At this location, the damage path width was at its widest, measuring nearly 400 yards wide. Tree damage became more widely scattered and less intense approximately 4 miles northeast of Mebane, where the tornado subsequently lifted.",
+        "The following events were reported: Flash Flood. These occurred near station USW00013722, approximately 15.6719 km away, between 2022-05-07 16:05:00 and 2022-05-07 17:31:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A upper-level low pressure system near West Virginia led to the development of afternoon and evening showers with some embedded thunderstorms over the Piedmont. One strong storm in Wake County led to an isolated flash flood. The showers and storms weakened by late evening as the trough moved east.\nEvent Narrative: Several hours of heavy rain led to flooding near Pullen Park, as the Rocky Branch river gage in Raleigh reached minor flood stage.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 32.8852 km away, between 2022-05-16 16:31:00 and 2022-05-16 17:30:00. 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 moist and unstable airmass within a warm and moist airmass spawned multiple rounds of strong to severe storms consisting of sub-severe hail and severe straight line wind gusts. The first round of storms was initiated by a weak convergence axis over the Sandhills, as well as a pre-frontal trough over the northwest Piedmont. The second round of storms was mainly focused by a trailing cold front that cleared central North Carolina by late evening. A moist and unstable airmass within a warm and moist airmass spawned multiple rounds of strong to severe storms consisting of sub-severe hail and severe straight line wind gusts. The first round of storms was initiated by a weak convergence axis over the Sandhills, as well as a pre-frontal trough over the northwest Piedmont. The second round of storms was mainly focused by a trailing cold front that cleared central North Carolina by late evening. A moist and unstable airmass within a warm and moist airmass spawned multiple rounds of strong to severe storms consisting of sub-severe hail and severe straight line wind gusts. The first round of storms was initiated by a weak convergence axis over the Sandhills, as well as a pre-frontal trough over the northwest Piedmont. The second round of storms was mainly focused by a trailing cold front that cleared central North Carolina by late evening. A moist and unstable airmass within a warm and moist airmass spawned multiple rounds of strong to severe storms consisting of sub-severe hail and severe straight line wind gusts. The first round of storms was initiated by a weak convergence axis over the Sandhills, as well as a pre-frontal trough over the northwest Piedmont. The second round of storms was mainly focused by a trailing cold front that cleared central North Carolina by late evening. A moist and unstable airmass within a warm and moist airmass spawned multiple rounds of strong to severe storms consisting of sub-severe hail and severe straight line wind gusts. The first round of storms was initiated by a weak convergence axis over the Sandhills, as well as a pre-frontal trough over the northwest Piedmont. The second round of storms was mainly focused by a trailing cold front that cleared central North Carolina by late evening. A moist and unstable airmass within a warm and moist airmass spawned multiple rounds of strong to severe storms consisting of sub-severe hail and severe straight line wind gusts. The first round of storms was initiated by a weak convergence axis over the Sandhills, as well as a pre-frontal trough over the northwest Piedmont. The second round of storms was mainly focused by a trailing cold front that cleared central North Carolina by late evening. A moist and unstable airmass within a warm and moist airmass spawned multiple rounds of strong to severe storms consisting of sub-severe hail and severe straight line wind gusts. The first round of storms was initiated by a weak convergence axis over the Sandhills, as well as a pre-frontal trough over the northwest Piedmont. The second round of storms was mainly focused by a trailing cold front that cleared central North Carolina by late evening.\nEvent Narrative: Multiple trees were reported down near the intersection of Amherst Creek Dr and Cedar Branch Ct. Power outages centered around the town of New Hill caused by downed trees caused damage to equipment. Damage was estimated near the intersection of Old US Highway 1 and New Hill Holleman Rd. A tree was reported down near the intersection of Holly Mountain Rd and Stargate Rd near Holly Springs. A power outage was caused by downed trees, causing damage to equipment. The damage was near the intersection of N Rotary St and W Sycamore St. A tree was reported down near the intersection of North Pine Street and Nowell Street in the town of Wendell. A power outage was caused by downed trees on power equipment. Damage was near the intersection of Brookwood Dr and Parkway Dr. Multiple trees were reported down near the intersection of Ocean Dr and Sonny Rd.",
+        "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00013722, approximately 26.4705 km away, between 2022-05-19 22:05:00 and 2022-05-19 23:48:00. The events included records with hailstones measuring 37.75 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Initial thunderstorms on the evening of the 19th of May developed along a stationary front and mid-level impulse over the northern North Carolina Piedmont in the mid to late evening hours, producing mostly hail initially. The storms grew upscale and congealed into several thunderstorm clusters that produced both severe hail and damaging wind gusts as the storm complex propagated east-southeast across the central Piedmont and into the Coastal Plain. The storms weakened after midnight. Initial thunderstorms on the evening of the 19th of May developed along a stationary front and mid-level impulse over the northern North Carolina Piedmont in the mid to late evening hours, producing mostly hail initially. The storms grew upscale and congealed into several thunderstorm clusters that produced both severe hail and damaging wind gusts as the storm complex propagated east-southeast across the central Piedmont and into the Coastal Plain. The storms weakened after midnight. Initial thunderstorms on the evening of the 19th of May developed along a stationary front and mid-level impulse over the northern North Carolina Piedmont in the mid to late evening hours, producing mostly hail initially. The storms grew upscale and congealed into several thunderstorm clusters that produced both severe hail and damaging wind gusts as the storm complex propagated east-southeast across the central Piedmont and into the Coastal Plain. The storms weakened after midnight. Initial thunderstorms on the evening of the 19th of May developed along a stationary front and mid-level impulse over the northern North Carolina Piedmont in the mid to late evening hours, producing mostly hail initially. The storms grew upscale and congealed into several thunderstorm clusters that produced both severe hail and damaging wind gusts as the storm complex propagated east-southeast across the central Piedmont and into the Coastal Plain. The storms weakened after midnight. Initial thunderstorms on the evening of the 19th of May developed along a stationary front and mid-level impulse over the northern North Carolina Piedmont in the mid to late evening hours, producing mostly hail initially. The storms grew upscale and congealed into several thunderstorm clusters that produced both severe hail and damaging wind gusts as the storm complex propagated east-southeast across the central Piedmont and into the Coastal Plain. The storms weakened after midnight. Initial thunderstorms on the evening of the 19th of May developed along a stationary front and mid-level impulse over the northern North Carolina Piedmont in the mid to late evening hours, producing mostly hail initially. The storms grew upscale and congealed into several thunderstorm clusters that produced both severe hail and damaging wind gusts as the storm complex propagated east-southeast across the central Piedmont and into the Coastal Plain. The storms weakened after midnight. Initial thunderstorms on the evening of the 19th of May developed along a stationary front and mid-level impulse over the northern North Carolina Piedmont in the mid to late evening hours, producing mostly hail initially. The storms grew upscale and congealed into several thunderstorm clusters that produced both severe hail and damaging wind gusts as the storm complex propagated east-southeast across the central Piedmont and into the Coastal Plain. The storms weakened after midnight. Initial thunderstorms on the evening of the 19th of May developed along a stationary front and mid-level impulse over the northern North Carolina Piedmont in the mid to late evening hours, producing mostly hail initially. The storms grew upscale and congealed into several thunderstorm clusters that produced both severe hail and damaging wind gusts as the storm complex propagated east-southeast across the central Piedmont and into the Coastal Plain. The storms weakened after midnight. Initial thunderstorms on the evening of the 19th of May developed along a stationary front and mid-level impulse over the northern North Carolina Piedmont in the mid to late evening hours, producing mostly hail initially. The storms grew upscale and congealed into several thunderstorm clusters that produced both severe hail and damaging wind gusts as the storm complex propagated east-southeast across the central Piedmont and into the Coastal Plain. The storms weakened after midnight. Initial thunderstorms on the evening of the 19th of May developed along a stationary front and mid-level impulse over the northern North Carolina Piedmont in the mid to late evening hours, producing mostly hail initially. The storms grew upscale and congealed into several thunderstorm clusters that produced both severe hail and damaging wind gusts as the storm complex propagated east-southeast across the central Piedmont and into the Coastal Plain. The storms weakened after midnight. Initial thunderstorms on the evening of the 19th of May developed along a stationary front and mid-level impulse over the northern North Carolina Piedmont in the mid to late evening hours, producing mostly hail initially. The storms grew upscale and congealed into several thunderstorm clusters that produced both severe hail and damaging wind gusts as the storm complex propagated east-southeast across the central Piedmont and into the Coastal Plain. The storms weakened after midnight. Initial thunderstorms on the evening of the 19th of May developed along a stationary front and mid-level impulse over the northern North Carolina Piedmont in the mid to late evening hours, producing mostly hail initially. The storms grew upscale and congealed into several thunderstorm clusters that produced both severe hail and damaging wind gusts as the storm complex propagated east-southeast across the central Piedmont and into the Coastal Plain. The storms weakened after midnight.\nEvent Narrative: A tree was reported down at the intersection of Pritchard Ave and Umstead Dr in the town of Chapel Hill. A tree was reported down near the intersection of Calvin St and Fern St in Durham. A tree was reported down near Bynum at the intersection of Old Graham Rd and The Parks Dr. Trees were reported down near the intersection of Avent Ferry Rd and Athens Dr in Raleigh. Quarter size hail reported near the intersection of Humie Olive Rd and Butterfinger Ln in the town of New Hill. Blaney Franks Road at Tucker Drive was closed due to multiple trees down. Multiple trees were reported down near the intersection of Blaney Franks Rd and Old Sorrell Rd. A large tree was down, blocking both lanes of Ten-Ten Rd at S Mountain Dr near Raleigh. Numerous trees were reported down in the town of Garner. Public reported quarter inch hail near the intersection of Key Biscayne Ct and Locke Woods Rd. A tree fell on a residence near the intersection of Ses Dr and Garrison Ave in Clayton. Quarter inch hail reported near the intersection of Woodtrestle Way and Coalyard Dr east of Garner.",
+        "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00013722, approximately 17.1623 km away, between 2022-05-21 16:07:00 and 2022-05-21 16:59:00. The events included records with hailstones measuring 17.293333333333333 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A weak shortwave trough in the southwest flow at mid-levels initiated showers and thunderstorms over Georgia and South Carolina during the early afternoon hours.  These storms propagated into the southern and western Piedmont of central North Carolina by mid-afternoon, while additional storms developed into the central Piedmont and Coastal Plain and moved north toward Virginia during the evening hours. Many of the storms produced small hail and damaging winds, while a few storms produced one inch hail. A weak shortwave trough in the southwest flow at mid-levels initiated showers and thunderstorms over Georgia and South Carolina during the early afternoon hours.  These storms propagated into the southern and western Piedmont of central North Carolina by mid-afternoon, while additional storms developed into the central Piedmont and Coastal Plain and moved north toward Virginia during the evening hours. Many of the storms produced small hail and damaging winds, while a few storms produced one inch hail. A weak shortwave trough in the southwest flow at mid-levels initiated showers and thunderstorms over Georgia and South Carolina during the early afternoon hours.  These storms propagated into the southern and western Piedmont of central North Carolina by mid-afternoon, while additional storms developed into the central Piedmont and Coastal Plain and moved north toward Virginia during the evening hours. Many of the storms produced small hail and damaging winds, while a few storms produced one inch hail.\nEvent Narrative: Nickel size hail was reported by a trained spotter near the intersection of Green Level Church Road and Cary Glen Blvd. Quarter size hail reported near the intersection of Airport Blvd and McCrimmon Parkway. Multiple trees were reported down near Smithfield Rd and Interstate 87 in Knightdale.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 45.7348 km away, between 2022-05-22 17:12:00 and 2022-05-22 17:12:00. 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 trough over the North Carolina mountains, as well as a mid-level disturbance moving northeast out of Georgia and South Carolina, led to development of isolated to scattered showers and storms by the late afternoon and evening. Storms over the western Piedmont moved east-southeast, while storms tied to the disturbance tracked east-northeast into the Sandhills and Coastal Plain. All the storm activity was ahead of a southward moving cold front. One storm reached severe limits, produced a downed tree in Johnston County. Most storms died out after midnight.\nEvent Narrative: A tree was reported down near the intersection of Earpsboro Rd and Route 96 in Linwood.",
+        "The following events were reported: Flash Flood, Lightning, Thunderstorm Wind, Tornado. These occurred near station USW00013722, approximately 29.6364 km away, between 2022-05-23 14:25:00 and 2022-05-24 01:00:00.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 210000.0 and crop damage of 0.0. \n\nEpisode Narrative: A stalled surface boundary across the central North Carolina was the focal point for shower and thunderstorm development. Primary impacts were in the form of gusty winds and small hail. Several tornado warnings were issued, although most of the damage was from straight line winds. Moderate flooding due to two rounds of short-lived but heavy rainfall was observed in Alamance, Orange, and Wake counties. Storm activity largely waned after midnight. A stalled surface boundary across the central North Carolina was the focal point for shower and thunderstorm development. Primary impacts were in the form of gusty winds and small hail. Several tornado warnings were issued, although most of the damage was from straight line winds. Moderate flooding due to two rounds of short-lived but heavy rainfall was observed in Alamance, Orange, and Wake counties. Storm activity largely waned after midnight. A stalled surface boundary across the central North Carolina was the focal point for shower and thunderstorm development. Primary impacts were in the form of gusty winds and small hail. Several tornado warnings were issued, although most of the damage was from straight line winds. Moderate flooding due to two rounds of short-lived but heavy rainfall was observed in Alamance, Orange, and Wake counties. Storm activity largely waned after midnight. A stalled surface boundary across the central North Carolina was the focal point for shower and thunderstorm development. Primary impacts were in the form of gusty winds and small hail. Several tornado warnings were issued, although most of the damage was from straight line winds. Moderate flooding due to two rounds of short-lived but heavy rainfall was observed in Alamance, Orange, and Wake counties. Storm activity largely waned after midnight. A stalled surface boundary across the central North Carolina was the focal point for shower and thunderstorm development. Primary impacts were in the form of gusty winds and small hail. Several tornado warnings were issued, although most of the damage was from straight line winds. Moderate flooding due to two rounds of short-lived but heavy rainfall was observed in Alamance, Orange, and Wake counties. Storm activity largely waned after midnight. A stalled surface boundary across the central North Carolina was the focal point for shower and thunderstorm development. Primary impacts were in the form of gusty winds and small hail. Several tornado warnings were issued, although most of the damage was from straight line winds. Moderate flooding due to two rounds of short-lived but heavy rainfall was observed in Alamance, Orange, and Wake counties. Storm activity largely waned after midnight. A stalled surface boundary across the central North Carolina was the focal point for shower and thunderstorm development. Primary impacts were in the form of gusty winds and small hail. Several tornado warnings were issued, although most of the damage was from straight line winds. Moderate flooding due to two rounds of short-lived but heavy rainfall was observed in Alamance, Orange, and Wake counties. Storm activity largely waned after midnight. A stalled surface boundary across the central North Carolina was the focal point for shower and thunderstorm development. Primary impacts were in the form of gusty winds and small hail. Several tornado warnings were issued, although most of the damage was from straight line winds. Moderate flooding due to two rounds of short-lived but heavy rainfall was observed in Alamance, Orange, and Wake counties. Storm activity largely waned after midnight. A stalled surface boundary across the central North Carolina was the focal point for shower and thunderstorm development. Primary impacts were in the form of gusty winds and small hail. Several tornado warnings were issued, although most of the damage was from straight line winds. Moderate flooding due to two rounds of short-lived but heavy rainfall was observed in Alamance, Orange, and Wake counties. Storm activity largely waned after midnight. A stalled surface boundary across the central North Carolina was the focal point for shower and thunderstorm development. Primary impacts were in the form of gusty winds and small hail. Several tornado warnings were issued, although most of the damage was from straight line winds. Moderate flooding due to two rounds of short-lived but heavy rainfall was observed in Alamance, Orange, and Wake counties. Storm activity largely waned after midnight. A stalled surface boundary across the central North Carolina was the focal point for shower and thunderstorm development. Primary impacts were in the form of gusty winds and small hail. Several tornado warnings were issued, although most of the damage was from straight line winds. Moderate flooding due to two rounds of short-lived but heavy rainfall was observed in Alamance, Orange, and Wake counties. Storm activity largely waned after midnight. A stalled surface boundary across the central North Carolina was the focal point for shower and thunderstorm development. Primary impacts were in the form of gusty winds and small hail. Several tornado warnings were issued, although most of the damage was from straight line winds. Moderate flooding due to two rounds of short-lived but heavy rainfall was observed in Alamance, Orange, and Wake counties. Storm activity largely waned after midnight. A stalled surface boundary across the central North Carolina was the focal point for shower and thunderstorm development. Primary impacts were in the form of gusty winds and small hail. Several tornado warnings were issued, although most of the damage was from straight line winds. Moderate flooding due to two rounds of short-lived but heavy rainfall was observed in Alamance, Orange, and Wake counties. Storm activity largely waned after midnight. A stalled surface boundary across the central North Carolina was the focal point for shower and thunderstorm development. Primary impacts were in the form of gusty winds and small hail. Several tornado warnings were issued, although most of the damage was from straight line winds. Moderate flooding due to two rounds of short-lived but heavy rainfall was observed in Alamance, Orange, and Wake counties. Storm activity largely waned after midnight. A stalled surface boundary across the central North Carolina was the focal point for shower and thunderstorm development. Primary impacts were in the form of gusty winds and small hail. Several tornado warnings were issued, although most of the damage was from straight line winds. Moderate flooding due to two rounds of short-lived but heavy rainfall was observed in Alamance, Orange, and Wake counties. Storm activity largely waned after midnight. A stalled surface boundary across the central North Carolina was the focal point for shower and thunderstorm development. Primary impacts were in the form of gusty winds and small hail. Several tornado warnings were issued, although most of the damage was from straight line winds. Moderate flooding due to two rounds of short-lived but heavy rainfall was observed in Alamance, Orange, and Wake counties. Storm activity largely waned after midnight.\nEvent Narrative: Trees and power lines were reported down near the intersection of Deep River Rd and Cedar Lake Rd near the town of Moncure. A tree was reported down near the intersection of Efland-Cedar Grove Rd and US Highway 70 W in Efland. A tree was reported down at North Carolina Highway 54 W and Stanford Rd near the town of Oaks. A structural fire was presumed to be caused by lightning in the town of Efland, near the intersection of Forrest Ave and Brookhollow Rd. Downed trees fell on power equipment and power lines in the town of Corinth, near the intersection of Dickens Rd and Route 42. Numerous trees were snapped along S Miami Blvd near Laurel Dr in Bethesda. Trees were reported down in the Northgate Park Neighborhood north of Downtown Durham, near the intersection of W Lavender Ave and Glendale Ave. Emergency managers reported numerous trees down throughout much of Durham County, including downed trees on homes. Downed trees fell on power lines in Clayton near the intersection of Summer Pl Ct and Loop Rd. Downed trees fell on power equipment, causing power outages near the intersection of Boyce Mill Rd and Old Creedmoor Rd. Flooding due to heavy rain along US-70 in Hillsborough led to closures from Holiday Park Dr to Lawrence Rd. A tree fell on power lines near the intersection of Fontana Dr and Loop Rd near the town of Flowers. Numerous trees and power lines were reported down throughout Franklin County, with some damage near the intersection of Warner Winn Rd and Dyking Rd. An automated creek gage along Walnut Creek near the intersection of southeast Maynard Rd and East Chatham St was above flood stage. Flash flooding due to heavy rainfall was reported at Wolf Creek Circle in Raleigh. A very brief EF-0 tornado, with estimated maximum wind speeds of 85 mph, touched down during the late afternoon on Monday, May 23, 2022, just northeast of the City of Durham, Durham County North Carolina. The touchdown, which occurred at treetop level, first occurred along Glenbrook Dr, De Mille St, Hinson Dr, Waring St, Da Vinci St, and several of the surrounding streets. The tornado then lifted and briefly touched down again at treetop level along Colonial Heights Dr and Thompson Rd, before lifting and finally dissipating. ||Since the rotary winds never actually touched the ground and remained at treetop level, the direct damage was confined to trees and resulted in numerous uprooted and snapped trees. Subsequent damage occurred to several homes when the uprooted and |snapped trees fell on them. While surveying the damage, a resident of the affected area showed the surveyor video that was captured as the damaging was occurring. This video showed a funnel cloud extending down to, but not below the treetop or tree canopy level, thus resulting in the heavy damage to numerous trees in the affected area, and subsequent structural damage.",
+        "The following events were reported: Flash Flood, Thunderstorm Wind. These occurred near station USW00013722, approximately 30.3477 km away, between 2022-05-27 07:34:00 and 2022-05-27 18:00:00.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: Two rounds of severe weather moved through central NC on the 27th of May tied to a deep upper-level low pressure system over the Mid-Mississippi and Ohio Valleys and an approaching cold front from the Tennessee Valley. The first round of storms was focused along a low-level moisture transport axis in the morning, producing strong straight line winds across the northern half of central North Carolina, along with flash flooding concerns over the western Piedmont and urban areas in the northeast Piedmont. The second round of storms formed along a pre-frontal convergence axis in the afternoon and early evening, stretching from Granville to Scotland County. A cluster of storms organized into a storm complex, which produced local flooding over the Sandhills into southern Wake County and a strong mesocyclone over the Raleigh metro area. Two rounds of severe weather moved through central NC on the 27th of May tied to a deep upper-level low pressure system over the Mid-Mississippi and Ohio Valleys and an approaching cold front from the Tennessee Valley. The first round of storms was focused along a low-level moisture transport axis in the morning, producing strong straight line winds across the northern half of central North Carolina, along with flash flooding concerns over the western Piedmont and urban areas in the northeast Piedmont. The second round of storms formed along a pre-frontal convergence axis in the afternoon and early evening, stretching from Granville to Scotland County. A cluster of storms organized into a storm complex, which produced local flooding over the Sandhills into southern Wake County and a strong mesocyclone over the Raleigh metro area. Two rounds of severe weather moved through central NC on the 27th of May tied to a deep upper-level low pressure system over the Mid-Mississippi and Ohio Valleys and an approaching cold front from the Tennessee Valley. The first round of storms was focused along a low-level moisture transport axis in the morning, producing strong straight line winds across the northern half of central North Carolina, along with flash flooding concerns over the western Piedmont and urban areas in the northeast Piedmont. The second round of storms formed along a pre-frontal convergence axis in the afternoon and early evening, stretching from Granville to Scotland County. A cluster of storms organized into a storm complex, which produced local flooding over the Sandhills into southern Wake County and a strong mesocyclone over the Raleigh metro area. Two rounds of severe weather moved through central NC on the 27th of May tied to a deep upper-level low pressure system over the Mid-Mississippi and Ohio Valleys and an approaching cold front from the Tennessee Valley. The first round of storms was focused along a low-level moisture transport axis in the morning, producing strong straight line winds across the northern half of central North Carolina, along with flash flooding concerns over the western Piedmont and urban areas in the northeast Piedmont. The second round of storms formed along a pre-frontal convergence axis in the afternoon and early evening, stretching from Granville to Scotland County. A cluster of storms organized into a storm complex, which produced local flooding over the Sandhills into southern Wake County and a strong mesocyclone over the Raleigh metro area. Two rounds of severe weather moved through central NC on the 27th of May tied to a deep upper-level low pressure system over the Mid-Mississippi and Ohio Valleys and an approaching cold front from the Tennessee Valley. The first round of storms was focused along a low-level moisture transport axis in the morning, producing strong straight line winds across the northern half of central North Carolina, along with flash flooding concerns over the western Piedmont and urban areas in the northeast Piedmont. The second round of storms formed along a pre-frontal convergence axis in the afternoon and early evening, stretching from Granville to Scotland County. A cluster of storms organized into a storm complex, which produced local flooding over the Sandhills into southern Wake County and a strong mesocyclone over the Raleigh metro area. Two rounds of severe weather moved through central NC on the 27th of May tied to a deep upper-level low pressure system over the Mid-Mississippi and Ohio Valleys and an approaching cold front from the Tennessee Valley. The first round of storms was focused along a low-level moisture transport axis in the morning, producing strong straight line winds across the northern half of central North Carolina, along with flash flooding concerns over the western Piedmont and urban areas in the northeast Piedmont. The second round of storms formed along a pre-frontal convergence axis in the afternoon and early evening, stretching from Granville to Scotland County. A cluster of storms organized into a storm complex, which produced local flooding over the Sandhills into southern Wake County and a strong mesocyclone over the Raleigh metro area. Two rounds of severe weather moved through central NC on the 27th of May tied to a deep upper-level low pressure system over the Mid-Mississippi and Ohio Valleys and an approaching cold front from the Tennessee Valley. The first round of storms was focused along a low-level moisture transport axis in the morning, producing strong straight line winds across the northern half of central North Carolina, along with flash flooding concerns over the western Piedmont and urban areas in the northeast Piedmont. The second round of storms formed along a pre-frontal convergence axis in the afternoon and early evening, stretching from Granville to Scotland County. A cluster of storms organized into a storm complex, which produced local flooding over the Sandhills into southern Wake County and a strong mesocyclone over the Raleigh metro area. Two rounds of severe weather moved through central NC on the 27th of May tied to a deep upper-level low pressure system over the Mid-Mississippi and Ohio Valleys and an approaching cold front from the Tennessee Valley. The first round of storms was focused along a low-level moisture transport axis in the morning, producing strong straight line winds across the northern half of central North Carolina, along with flash flooding concerns over the western Piedmont and urban areas in the northeast Piedmont. The second round of storms formed along a pre-frontal convergence axis in the afternoon and early evening, stretching from Granville to Scotland County. A cluster of storms organized into a storm complex, which produced local flooding over the Sandhills into southern Wake County and a strong mesocyclone over the Raleigh metro area. Two rounds of severe weather moved through central NC on the 27th of May tied to a deep upper-level low pressure system over the Mid-Mississippi and Ohio Valleys and an approaching cold front from the Tennessee Valley. The first round of storms was focused along a low-level moisture transport axis in the morning, producing strong straight line winds across the northern half of central North Carolina, along with flash flooding concerns over the western Piedmont and urban areas in the northeast Piedmont. The second round of storms formed along a pre-frontal convergence axis in the afternoon and early evening, stretching from Granville to Scotland County. A cluster of storms organized into a storm complex, which produced local flooding over the Sandhills into southern Wake County and a strong mesocyclone over the Raleigh metro area. Two rounds of severe weather moved through central NC on the 27th of May tied to a deep upper-level low pressure system over the Mid-Mississippi and Ohio Valleys and an approaching cold front from the Tennessee Valley. The first round of storms was focused along a low-level moisture transport axis in the morning, producing strong straight line winds across the northern half of central North Carolina, along with flash flooding concerns over the western Piedmont and urban areas in the northeast Piedmont. The second round of storms formed along a pre-frontal convergence axis in the afternoon and early evening, stretching from Granville to Scotland County. A cluster of storms organized into a storm complex, which produced local flooding over the Sandhills into southern Wake County and a strong mesocyclone over the Raleigh metro area. Two rounds of severe weather moved through central NC on the 27th of May tied to a deep upper-level low pressure system over the Mid-Mississippi and Ohio Valleys and an approaching cold front from the Tennessee Valley. The first round of storms was focused along a low-level moisture transport axis in the morning, producing strong straight line winds across the northern half of central North Carolina, along with flash flooding concerns over the western Piedmont and urban areas in the northeast Piedmont. The second round of storms formed along a pre-frontal convergence axis in the afternoon and early evening, stretching from Granville to Scotland County. A cluster of storms organized into a storm complex, which produced local flooding over the Sandhills into southern Wake County and a strong mesocyclone over the Raleigh metro area. Two rounds of severe weather moved through central NC on the 27th of May tied to a deep upper-level low pressure system over the Mid-Mississippi and Ohio Valleys and an approaching cold front from the Tennessee Valley. The first round of storms was focused along a low-level moisture transport axis in the morning, producing strong straight line winds across the northern half of central North Carolina, along with flash flooding concerns over the western Piedmont and urban areas in the northeast Piedmont. The second round of storms formed along a pre-frontal convergence axis in the afternoon and early evening, stretching from Granville to Scotland County. A cluster of storms organized into a storm complex, which produced local flooding over the Sandhills into southern Wake County and a strong mesocyclone over the Raleigh metro area. Two rounds of severe weather moved through central NC on the 27th of May tied to a deep upper-level low pressure system over the Mid-Mississippi and Ohio Valleys and an approaching cold front from the Tennessee Valley. The first round of storms was focused along a low-level moisture transport axis in the morning, producing strong straight line winds across the northern half of central North Carolina, along with flash flooding concerns over the western Piedmont and urban areas in the northeast Piedmont. The second round of storms formed along a pre-frontal convergence axis in the afternoon and early evening, stretching from Granville to Scotland County. A cluster of storms organized into a storm complex, which produced local flooding over the Sandhills into southern Wake County and a strong mesocyclone over the Raleigh metro area. Two rounds of severe weather moved through central NC on the 27th of May tied to a deep upper-level low pressure system over the Mid-Mississippi and Ohio Valleys and an approaching cold front from the Tennessee Valley. The first round of storms was focused along a low-level moisture transport axis in the morning, producing strong straight line winds across the northern half of central North Carolina, along with flash flooding concerns over the western Piedmont and urban areas in the northeast Piedmont. The second round of storms formed along a pre-frontal convergence axis in the afternoon and early evening, stretching from Granville to Scotland County. A cluster of storms organized into a storm complex, which produced local flooding over the Sandhills into southern Wake County and a strong mesocyclone over the Raleigh metro area. Two rounds of severe weather moved through central NC on the 27th of May tied to a deep upper-level low pressure system over the Mid-Mississippi and Ohio Valleys and an approaching cold front from the Tennessee Valley. The first round of storms was focused along a low-level moisture transport axis in the morning, producing strong straight line winds across the northern half of central North Carolina, along with flash flooding concerns over the western Piedmont and urban areas in the northeast Piedmont. The second round of storms formed along a pre-frontal convergence axis in the afternoon and early evening, stretching from Granville to Scotland County. A cluster of storms organized into a storm complex, which produced local flooding over the Sandhills into southern Wake County and a strong mesocyclone over the Raleigh metro area.\nEvent Narrative: A tree was reported down in Chapel Hill at the intersection of South Columbia St and Old Pittsboro Rd. A large tree was reported down near the intersection of Fordham Blvd and Willow Dr in Chapel Hill. Traffic lights were out along Fordham Blvd between Willow Dr and Raleigh Rd in Chapel Hill, caused by downed trees. A tree was reported down in the town of Efland at the intersection of Cedar Grove Rd and Lebanon Rd. A tree was reported down on the roadway, blocking both lanes, at the intersection of Jim Latta Rd and Welch Whitfield Rd. Four trees were reported down near the Person/Durham County line, at the intersection of Moores Mill Rd and Bowen Rd. An extremely large tree crashed onto a house on Red Mill Rd. Additional trees were reported down along Red Mill Rd near I-85. Power outages were caused by downed trees north of Creedmoor near Hester Rd. A large tree fell down on a vehicle near the Raleigh-Durham International Airport. A tree fell on a home near the intersection of Aaron Dr and Dandridge Dr near Garner. Power outages were caused by fallen trees damaging equipment near the intersection of Barwell Rd and Rock Quarry Rd. Two trees fell down near the intersection of Main St and Hollingsworth St near Bunn. One tree was on a resident's fence. Law enforcement reported road and lane closures due to flash flooding near the intersection of Avent Ferry Rd and Center Hill Dr. Flooding was also reported nearby along Bartley Holleman Rd. A tree was reported down near Fearrington at the intersection of Lystra Rd and Governors Dr. A tree was reported down 7 miles west of Pittsboro at the intersection of Hadley Mill Rd and Jay Shambley Rd.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 28.5578 km away, between 2022-06-08 17:29:00 and 2022-06-08 18:12:00. 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 31000.0 and crop damage of 0.0. \n\nEpisode Narrative: Deep moist advection combined with a pre-frontal trough and mid-level shortwave to result in scattered showers and thunderstorms across central North Carolina in the afternoon and evening. The most intense storms with damaging winds were over portions of the northern Piedmont and Sandhills. Deep moist advection combined with a pre-frontal trough and mid-level shortwave to result in scattered showers and thunderstorms across central North Carolina in the afternoon and evening. The most intense storms with damaging winds were over portions of the northern Piedmont and Sandhills. Deep moist advection combined with a pre-frontal trough and mid-level shortwave to result in scattered showers and thunderstorms across central North Carolina in the afternoon and evening. The most intense storms with damaging winds were over portions of the northern Piedmont and Sandhills. Deep moist advection combined with a pre-frontal trough and mid-level shortwave to result in scattered showers and thunderstorms across central North Carolina in the afternoon and evening. The most intense storms with damaging winds were over portions of the northern Piedmont and Sandhills.\nEvent Narrative: Trees were reported down on power lines along Hammond Road and Chapanoke Road. Trees were reported down on power lines along Homestead Road near Stratford Drive. A tree was reported down on Lochwood Court in Chapel Hill. Trees were reported down on power lines near the intersection of North Carolina Highway 42 and Rollins Mill Road.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 23.5426 km away, between 2022-06-16 15:53:00 and 2022-06-16 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 23500.0 and crop damage of 0.0. \n\nEpisode Narrative: An occluded front interacted with a hot and humid air mass to produce a cluster of showers and thunderstorms that moved east across central North Carolina during the afternoon and evening. These storms resulted in widespread wind damage across roughly the western half of the region. There was also a report of flash flooding in Stanly County. An occluded front interacted with a hot and humid air mass to produce a cluster of showers and thunderstorms that moved east across central North Carolina during the afternoon and evening. These storms resulted in widespread wind damage across roughly the western half of the region. There was also a report of flash flooding in Stanly County. An occluded front interacted with a hot and humid air mass to produce a cluster of showers and thunderstorms that moved east across central North Carolina during the afternoon and evening. These storms resulted in widespread wind damage across roughly the western half of the region. There was also a report of flash flooding in Stanly County. An occluded front interacted with a hot and humid air mass to produce a cluster of showers and thunderstorms that moved east across central North Carolina during the afternoon and evening. These storms resulted in widespread wind damage across roughly the western half of the region. There was also a report of flash flooding in Stanly County. An occluded front interacted with a hot and humid air mass to produce a cluster of showers and thunderstorms that moved east across central North Carolina during the afternoon and evening. These storms resulted in widespread wind damage across roughly the western half of the region. There was also a report of flash flooding in Stanly County. An occluded front interacted with a hot and humid air mass to produce a cluster of showers and thunderstorms that moved east across central North Carolina during the afternoon and evening. These storms resulted in widespread wind damage across roughly the western half of the region. There was also a report of flash flooding in Stanly County. An occluded front interacted with a hot and humid air mass to produce a cluster of showers and thunderstorms that moved east across central North Carolina during the afternoon and evening. These storms resulted in widespread wind damage across roughly the western half of the region. There was also a report of flash flooding in Stanly County. An occluded front interacted with a hot and humid air mass to produce a cluster of showers and thunderstorms that moved east across central North Carolina during the afternoon and evening. These storms resulted in widespread wind damage across roughly the western half of the region. There was also a report of flash flooding in Stanly County. An occluded front interacted with a hot and humid air mass to produce a cluster of showers and thunderstorms that moved east across central North Carolina during the afternoon and evening. These storms resulted in widespread wind damage across roughly the western half of the region. There was also a report of flash flooding in Stanly County.\nEvent Narrative: A tree was reported down at Renfrow Road and Parkland Road. A tree was reported down at the 1000 block of South Person Street in downtown Raleigh. A tree was reported down at Lake Wheeler Road and South Saunders Street in Raleigh. Fallen trees caused power outages in downtown Pittsboro as well as to the north and west. A tree fell on a car, damaging it, in the Jordan Lake area. A power line was reported down at the 2000 block of Poole Road. A tree was reported down at South State Street and Interstate 40 in Raleigh. A tree was reported down at Cross Link Road and Hadley Road. A tree was reported down at the 700 block of Belmont Drive in Raleigh.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 31.7849 km away, between 2022-06-17 16:31:00 and 2022-06-17 17:43:00.The events resulted in 1 injuries and 1 fatalities. The events caused property damage valued at 230000.0 and crop damage of 0.0. \n\nEpisode Narrative: A complex of showers and thunderstorms moved across central North Carolina during the late afternoon and evening. The line produced numerous damaging wind gusts along with marginally severe hail. One fatality occurred as the line moved through Franklin County, as a tree fell on and killed a person who was outside. A complex of showers and thunderstorms moved across central North Carolina during the late afternoon and evening. The line produced numerous damaging wind gusts along with marginally severe hail. One fatality occurred as the line moved through Franklin County, as a tree fell on and killed a person who was outside. A complex of showers and thunderstorms moved across central North Carolina during the late afternoon and evening. The line produced numerous damaging wind gusts along with marginally severe hail. One fatality occurred as the line moved through Franklin County, as a tree fell on and killed a person who was outside. A complex of showers and thunderstorms moved across central North Carolina during the late afternoon and evening. The line produced numerous damaging wind gusts along with marginally severe hail. One fatality occurred as the line moved through Franklin County, as a tree fell on and killed a person who was outside. A complex of showers and thunderstorms moved across central North Carolina during the late afternoon and evening. The line produced numerous damaging wind gusts along with marginally severe hail. One fatality occurred as the line moved through Franklin County, as a tree fell on and killed a person who was outside. A complex of showers and thunderstorms moved across central North Carolina during the late afternoon and evening. The line produced numerous damaging wind gusts along with marginally severe hail. One fatality occurred as the line moved through Franklin County, as a tree fell on and killed a person who was outside. A complex of showers and thunderstorms moved across central North Carolina during the late afternoon and evening. The line produced numerous damaging wind gusts along with marginally severe hail. One fatality occurred as the line moved through Franklin County, as a tree fell on and killed a person who was outside. A complex of showers and thunderstorms moved across central North Carolina during the late afternoon and evening. The line produced numerous damaging wind gusts along with marginally severe hail. One fatality occurred as the line moved through Franklin County, as a tree fell on and killed a person who was outside. A complex of showers and thunderstorms moved across central North Carolina during the late afternoon and evening. The line produced numerous damaging wind gusts along with marginally severe hail. One fatality occurred as the line moved through Franklin County, as a tree fell on and killed a person who was outside. A complex of showers and thunderstorms moved across central North Carolina during the late afternoon and evening. The line produced numerous damaging wind gusts along with marginally severe hail. One fatality occurred as the line moved through Franklin County, as a tree fell on and killed a person who was outside. A complex of showers and thunderstorms moved across central North Carolina during the late afternoon and evening. The line produced numerous damaging wind gusts along with marginally severe hail. One fatality occurred as the line moved through Franklin County, as a tree fell on and killed a person who was outside. A complex of showers and thunderstorms moved across central North Carolina during the late afternoon and evening. The line produced numerous damaging wind gusts along with marginally severe hail. One fatality occurred as the line moved through Franklin County, as a tree fell on and killed a person who was outside. A complex of showers and thunderstorms moved across central North Carolina during the late afternoon and evening. The line produced numerous damaging wind gusts along with marginally severe hail. One fatality occurred as the line moved through Franklin County, as a tree fell on and killed a person who was outside. A complex of showers and thunderstorms moved across central North Carolina during the late afternoon and evening. The line produced numerous damaging wind gusts along with marginally severe hail. One fatality occurred as the line moved through Franklin County, as a tree fell on and killed a person who was outside. A complex of showers and thunderstorms moved across central North Carolina during the late afternoon and evening. The line produced numerous damaging wind gusts along with marginally severe hail. One fatality occurred as the line moved through Franklin County, as a tree fell on and killed a person who was outside. A complex of showers and thunderstorms moved across central North Carolina during the late afternoon and evening. The line produced numerous damaging wind gusts along with marginally severe hail. One fatality occurred as the line moved through Franklin County, as a tree fell on and killed a person who was outside. A complex of showers and thunderstorms moved across central North Carolina during the late afternoon and evening. The line produced numerous damaging wind gusts along with marginally severe hail. One fatality occurred as the line moved through Franklin County, as a tree fell on and killed a person who was outside. A complex of showers and thunderstorms moved across central North Carolina during the late afternoon and evening. The line produced numerous damaging wind gusts along with marginally severe hail. One fatality occurred as the line moved through Franklin County, as a tree fell on and killed a person who was outside. A complex of showers and thunderstorms moved across central North Carolina during the late afternoon and evening. The line produced numerous damaging wind gusts along with marginally severe hail. One fatality occurred as the line moved through Franklin County, as a tree fell on and killed a person who was outside.\nEvent Narrative: A tree fell on a car with a person inside. A 55 knot gust was measured on the roof of Duke University Hospital. A tree fell on an apartment building off of First Street. Heavy damage was reported to the roof of a house along East Center Street. A tree fell on a residence along Alpha Drive. A tree fell on a garage on Pervis Road. A mobile home was damaged by severe wind gusts near Franklinton. A tree fell on a retirement community building in Garner. There were two mobile homes damaged near Louisburg. A tree was reported down along Mill Creek Road. A tree fell blocking the left lane on Interstate 85 near mile marker 196. A tree fell across the street near Kingswood Drive. A tree fell and killed a man outside of a mobile home along Cleghorns One Drive near Youngsville. A very large tree was reported down across Blaney Bluffs Lane near Lake Wheeler. Multiple trees were reported down along Interstate 85/40 near Exit 157. Many trees were reported down across the southern portions of the county, including Butner and Creedmoor. A tree fell on a car along Wild Wood Forest Drive. Extensive trees were reported down causing power outages across southern Wake County. Some of the hardest hit locations were around Fuquay-Varina, Garner, and Apex. A large tree and power lines were reported down along Garner Road.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 43.7252 km away, between 2022-07-05 17:43:00 and 2022-07-05 18:05:00. 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 10000.0 and crop damage of 0.0. \n\nEpisode Narrative: A warm front draped from the Great Lakes into the Ohio Valley led to morning showers and thunderstorms across the Ohio Valley early in the day. These showers and storms continued to progress southward toward central North Carolina in the evening hours, especially across the northwest, central, and southern Piedmont. The storms did not completely clear the area until the early overnight hours, as storms by then moved into South Carolina. There were numerous reports of trees and power lines down across Guilford, Forsyth, and Davidson Counties, as well as wind damage reports over Granville, Person, and Franklin Counties. Isolated flash flooding also occurred in parts of Forsyth County. A warm front draped from the Great Lakes into the Ohio Valley led to morning showers and thunderstorms across the Ohio Valley early in the day. These showers and storms continued to progress southward toward central North Carolina in the evening hours, especially across the northwest, central, and southern Piedmont. The storms did not completely clear the area until the early overnight hours, as storms by then moved into South Carolina. There were numerous reports of trees and power lines down across Guilford, Forsyth, and Davidson Counties, as well as wind damage reports over Granville, Person, and Franklin Counties. Isolated flash flooding also occurred in parts of Forsyth County.\nEvent Narrative: Power outages along Hatchers Run were caused by fallen trees damaging power equipment. Power outages near the intersection of Ballard Pruitt Rd and Barefoots Way were caused by fallen trees damaging power equipment.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 33.3004 km away, between 2022-07-06 17:45:00 and 2022-07-06 20:55:00. 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 1015000.0 and crop damage of 0.0. \n\nEpisode Narrative: Morning thunderstorms over the Ohio Valley, as well as a surface trough over the western Piedmont, led to several boundaries where afternoon and evening thunderstorms formed across central North Carolina. The storms formed over the western Piedmont and over Virginia, tracking into the central and eastern Piedmont and Coastal Plain in the mid to late-evening hours. The storms reached the far eastern portions of North Carolina in the early overnight hours. Numerous trees and wind damage was reported as a result of these thunderstorms. Morning thunderstorms over the Ohio Valley, as well as a surface trough over the western Piedmont, led to several boundaries where afternoon and evening thunderstorms formed across central North Carolina. The storms formed over the western Piedmont and over Virginia, tracking into the central and eastern Piedmont and Coastal Plain in the mid to late-evening hours. The storms reached the far eastern portions of North Carolina in the early overnight hours. Numerous trees and wind damage was reported as a result of these thunderstorms. Morning thunderstorms over the Ohio Valley, as well as a surface trough over the western Piedmont, led to several boundaries where afternoon and evening thunderstorms formed across central North Carolina. The storms formed over the western Piedmont and over Virginia, tracking into the central and eastern Piedmont and Coastal Plain in the mid to late-evening hours. The storms reached the far eastern portions of North Carolina in the early overnight hours. Numerous trees and wind damage was reported as a result of these thunderstorms. Morning thunderstorms over the Ohio Valley, as well as a surface trough over the western Piedmont, led to several boundaries where afternoon and evening thunderstorms formed across central North Carolina. The storms formed over the western Piedmont and over Virginia, tracking into the central and eastern Piedmont and Coastal Plain in the mid to late-evening hours. The storms reached the far eastern portions of North Carolina in the early overnight hours. Numerous trees and wind damage was reported as a result of these thunderstorms. Morning thunderstorms over the Ohio Valley, as well as a surface trough over the western Piedmont, led to several boundaries where afternoon and evening thunderstorms formed across central North Carolina. The storms formed over the western Piedmont and over Virginia, tracking into the central and eastern Piedmont and Coastal Plain in the mid to late-evening hours. The storms reached the far eastern portions of North Carolina in the early overnight hours. Numerous trees and wind damage was reported as a result of these thunderstorms. Morning thunderstorms over the Ohio Valley, as well as a surface trough over the western Piedmont, led to several boundaries where afternoon and evening thunderstorms formed across central North Carolina. The storms formed over the western Piedmont and over Virginia, tracking into the central and eastern Piedmont and Coastal Plain in the mid to late-evening hours. The storms reached the far eastern portions of North Carolina in the early overnight hours. Numerous trees and wind damage was reported as a result of these thunderstorms. Morning thunderstorms over the Ohio Valley, as well as a surface trough over the western Piedmont, led to several boundaries where afternoon and evening thunderstorms formed across central North Carolina. The storms formed over the western Piedmont and over Virginia, tracking into the central and eastern Piedmont and Coastal Plain in the mid to late-evening hours. The storms reached the far eastern portions of North Carolina in the early overnight hours. Numerous trees and wind damage was reported as a result of these thunderstorms. Morning thunderstorms over the Ohio Valley, as well as a surface trough over the western Piedmont, led to several boundaries where afternoon and evening thunderstorms formed across central North Carolina. The storms formed over the western Piedmont and over Virginia, tracking into the central and eastern Piedmont and Coastal Plain in the mid to late-evening hours. The storms reached the far eastern portions of North Carolina in the early overnight hours. Numerous trees and wind damage was reported as a result of these thunderstorms. Morning thunderstorms over the Ohio Valley, as well as a surface trough over the western Piedmont, led to several boundaries where afternoon and evening thunderstorms formed across central North Carolina. The storms formed over the western Piedmont and over Virginia, tracking into the central and eastern Piedmont and Coastal Plain in the mid to late-evening hours. The storms reached the far eastern portions of North Carolina in the early overnight hours. Numerous trees and wind damage was reported as a result of these thunderstorms.\nEvent Narrative: Trees were reported down near the intersection of Labrador Dr and Pintail Ct. Trees were reported down near the intersection of McGrath Way and Old Milburnie Rd. Multiple trees were reported down near the intersection of Hurdle Mills Rd and Etzold Painter Rd in the Hurdle Mills area. Power outages were caused by fallen trees damaging power equipment near the intersection of Bunting Dr and Vailwood Ct. Trees were reported down near the intersection of Old Crews Rd and Labrador Dr. A tree fell on a home near the intersection of Jackson Oaks Ct and Old Crews Rd. A tree was reported down near the intersection of Highway 97 and Brantley Rd. Minor structural damage was reported on a house near the intersection of Old Crews Rd and Buffaloe Rd. There was significant damage to various aircraft at the Triangle North Executive Airport, including a glider belonging to the Franklin Composite Squadron of the Civil Air Patrol. A few hangers were also damaged.",
+        "The following events were reported: Flash Flood, Thunderstorm Wind. These occurred near station USW00013722, approximately 27.2725 km away, between 2022-07-07 16:20:00 and 2022-07-07 18:26:00.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: A stalled frontal boundary to the north from the Mid-Mississippi Valley into the Ohio Valley and northern Virginia led to early morning storms north of the Carolinas. This led to numerous surface boundaries that aided thunderstorms to form along the Piedmont in the mid to late-afternoon hours. These storms tracked east-southeast in the evening to early overnight hours into the Sandhills and Coastal Plain. Many of the storms produced thunderstorm wind damage and a few also produced flash flooding. A stalled frontal boundary to the north from the Mid-Mississippi Valley into the Ohio Valley and northern Virginia led to early morning storms north of the Carolinas. This led to numerous surface boundaries that aided thunderstorms to form along the Piedmont in the mid to late-afternoon hours. These storms tracked east-southeast in the evening to early overnight hours into the Sandhills and Coastal Plain. Many of the storms produced thunderstorm wind damage and a few also produced flash flooding. A stalled frontal boundary to the north from the Mid-Mississippi Valley into the Ohio Valley and northern Virginia led to early morning storms north of the Carolinas. This led to numerous surface boundaries that aided thunderstorms to form along the Piedmont in the mid to late-afternoon hours. These storms tracked east-southeast in the evening to early overnight hours into the Sandhills and Coastal Plain. Many of the storms produced thunderstorm wind damage and a few also produced flash flooding. A stalled frontal boundary to the north from the Mid-Mississippi Valley into the Ohio Valley and northern Virginia led to early morning storms north of the Carolinas. This led to numerous surface boundaries that aided thunderstorms to form along the Piedmont in the mid to late-afternoon hours. These storms tracked east-southeast in the evening to early overnight hours into the Sandhills and Coastal Plain. Many of the storms produced thunderstorm wind damage and a few also produced flash flooding. A stalled frontal boundary to the north from the Mid-Mississippi Valley into the Ohio Valley and northern Virginia led to early morning storms north of the Carolinas. This led to numerous surface boundaries that aided thunderstorms to form along the Piedmont in the mid to late-afternoon hours. These storms tracked east-southeast in the evening to early overnight hours into the Sandhills and Coastal Plain. Many of the storms produced thunderstorm wind damage and a few also produced flash flooding. A stalled frontal boundary to the north from the Mid-Mississippi Valley into the Ohio Valley and northern Virginia led to early morning storms north of the Carolinas. This led to numerous surface boundaries that aided thunderstorms to form along the Piedmont in the mid to late-afternoon hours. These storms tracked east-southeast in the evening to early overnight hours into the Sandhills and Coastal Plain. Many of the storms produced thunderstorm wind damage and a few also produced flash flooding. A stalled frontal boundary to the north from the Mid-Mississippi Valley into the Ohio Valley and northern Virginia led to early morning storms north of the Carolinas. This led to numerous surface boundaries that aided thunderstorms to form along the Piedmont in the mid to late-afternoon hours. These storms tracked east-southeast in the evening to early overnight hours into the Sandhills and Coastal Plain. Many of the storms produced thunderstorm wind damage and a few also produced flash flooding. A stalled frontal boundary to the north from the Mid-Mississippi Valley into the Ohio Valley and northern Virginia led to early morning storms north of the Carolinas. This led to numerous surface boundaries that aided thunderstorms to form along the Piedmont in the mid to late-afternoon hours. These storms tracked east-southeast in the evening to early overnight hours into the Sandhills and Coastal Plain. Many of the storms produced thunderstorm wind damage and a few also produced flash flooding.\nEvent Narrative: One tree was blown down near the intersection of White Daisies Ct and Brookshadow Dr. A tree fell down, blocking the roadway near the intersection of York Rd and Canterbury Rd in Raleigh. A tree fell on a house, causing at least a partial structure collapse. This was near the intersection of West Barnes St and Ridgecrest Dr. Fallen trees damaged power equipment and resulted in roughly three thousand power outages in and around the intersection of Auburn Knightdale Rd and Battle Bridge Rd. Fallen trees damaged power equipment, resulting in two thousand power outages in and around the intersection of Amos St and Boling St. Numerous trees and power lines were reported down in the town of Clayton, near the intersection of East Horne St and Barbour St. A tree was reported down in the Glenwood Village area, near the intersection of Glenwood Ave and Granville Dr. Power outages were also reported in the area. Broadcast Media reported West Johnson Street was flooded in downtown Raleigh. A taxi also stalled and became partially submerged in floodwaters at the Raleigh Union Station.",
+        "The following events were reported: Flash Flood. These occurred near station USW00013722, approximately 22.4249 km away, between 2022-07-09 17:49:00 and 2022-07-09 20:52:00.The events resulted in 1 injuries and 0 fatalities. The events caused property damage valued at 151500.0 and crop damage of 0.0. \n\nEpisode Narrative: A very warm and humid air mass south of an approaching backdoor front combined with passing mid level disturbances within a broad mid-level trough to produce widespread showers and storms. Very high moisture, deeply warm low levels, and slow storm motion produced high rainfall rates and flash flooding, ranging from nuisance flooding in most places to road closures in Chapel Hill, Durham, and Wake county. Isolated damaging winds were also reported in Sampson County. A very warm and humid air mass south of an approaching backdoor front combined with passing mid level disturbances within a broad mid-level trough to produce widespread showers and storms. Very high moisture, deeply warm low levels, and slow storm motion produced high rainfall rates and flash flooding, ranging from nuisance flooding in most places to road closures in Chapel Hill, Durham, and Wake county. Isolated damaging winds were also reported in Sampson County. A very warm and humid air mass south of an approaching backdoor front combined with passing mid level disturbances within a broad mid-level trough to produce widespread showers and storms. Very high moisture, deeply warm low levels, and slow storm motion produced high rainfall rates and flash flooding, ranging from nuisance flooding in most places to road closures in Chapel Hill, Durham, and Wake county. Isolated damaging winds were also reported in Sampson County. A very warm and humid air mass south of an approaching backdoor front combined with passing mid level disturbances within a broad mid-level trough to produce widespread showers and storms. Very high moisture, deeply warm low levels, and slow storm motion produced high rainfall rates and flash flooding, ranging from nuisance flooding in most places to road closures in Chapel Hill, Durham, and Wake county. Isolated damaging winds were also reported in Sampson County. A very warm and humid air mass south of an approaching backdoor front combined with passing mid level disturbances within a broad mid-level trough to produce widespread showers and storms. Very high moisture, deeply warm low levels, and slow storm motion produced high rainfall rates and flash flooding, ranging from nuisance flooding in most places to road closures in Chapel Hill, Durham, and Wake county. Isolated damaging winds were also reported in Sampson County. A very warm and humid air mass south of an approaching backdoor front combined with passing mid level disturbances within a broad mid-level trough to produce widespread showers and storms. Very high moisture, deeply warm low levels, and slow storm motion produced high rainfall rates and flash flooding, ranging from nuisance flooding in most places to road closures in Chapel Hill, Durham, and Wake county. Isolated damaging winds were also reported in Sampson County.\nEvent Narrative: Old Falls of Neuse Rd and Riverside Dr was flooded with debris in the roadway. Flooded was reported near the intersection of NC Highway 147 (Durham Freeway) and Fulton St. The left lane of Interstate 400 West was flooded near Glenwood Ave. The Knightdale Fire Department conducted fifteen to twenty water rescues along Knightdale Blvd in the town of Knightdale. Multiple boats were used to conduct a water rescue along Countrywood Ln to rescue a woman on top of a vehicle in the water of the washed-out road. A car was partially flooded near the intersection of Ephesus Church Rd and Fordham Blvd in Chapel Hill.",
+        "The following events were reported: Flash Flood. These occurred near station USW00013722, approximately 21.801 km away, between 2022-07-13 19:17:00 and 2022-07-13 22:12:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A mid-level disturbance and surface trough draped from western North Carolina into south-central Virginia led to development of scattered to numerous showers and thunderstorms across the northwest Piedmont in the late afternoon. These storms tracked east-southeast during the mid to late-evening hours, tapering off by late evening. The storms over Orange and Durham Counties produced flash flooding around Chapel Hill and Durham. A mid-level disturbance and surface trough draped from western North Carolina into south-central Virginia led to development of scattered to numerous showers and thunderstorms across the northwest Piedmont in the late afternoon. These storms tracked east-southeast during the mid to late-evening hours, tapering off by late evening. The storms over Orange and Durham Counties produced flash flooding around Chapel Hill and Durham. A mid-level disturbance and surface trough draped from western North Carolina into south-central Virginia led to development of scattered to numerous showers and thunderstorms across the northwest Piedmont in the late afternoon. These storms tracked east-southeast during the mid to late-evening hours, tapering off by late evening. The storms over Orange and Durham Counties produced flash flooding around Chapel Hill and Durham. A mid-level disturbance and surface trough draped from western North Carolina into south-central Virginia led to development of scattered to numerous showers and thunderstorms across the northwest Piedmont in the late afternoon. These storms tracked east-southeast during the mid to late-evening hours, tapering off by late evening. The storms over Orange and Durham Counties produced flash flooding around Chapel Hill and Durham. A mid-level disturbance and surface trough draped from western North Carolina into south-central Virginia led to development of scattered to numerous showers and thunderstorms across the northwest Piedmont in the late afternoon. These storms tracked east-southeast during the mid to late-evening hours, tapering off by late evening. The storms over Orange and Durham Counties produced flash flooding around Chapel Hill and Durham.\nEvent Narrative: Flash flooding was reported along Fordham Blvd between south Estes Dr and Ephesus Church Rd. Flash flooding was reported on West Franklin St between Kenan St and Mallette St. Flash flooding was reported near the intersection of Martin Luther King Jr. Blvd and Estes Dr. Flash flooding was reported near the intersection of Butler St and Farrington Rd. Flash flooding was reported near the intersection of Old Chapel Hill Rd and Garrett Rd.",
+        "The following events were reported: Flash Flood. These occurred near station USW00013722, approximately 6.467 km away, between 2022-07-15 16:45:00 and 2022-07-15 18:45:00.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 85000.0 and crop damage of 0.0. \n\nEpisode Narrative: A mid-level disturbance coupled to a cold front draped along the western Piedmont triggered scattered afternoon and evening thunderstorms across the southern to northeastern Piedmont. These storms produced several reports of flash flooding in Wake and Cumberland Counties. No storms reached severe limits and the storm activity tapered off across central North Carolina by late evening. A mid-level disturbance coupled to a cold front draped along the western Piedmont triggered scattered afternoon and evening thunderstorms across the southern to northeastern Piedmont. These storms produced several reports of flash flooding in Wake and Cumberland Counties. No storms reached severe limits and the storm activity tapered off across central North Carolina by late evening. A mid-level disturbance coupled to a cold front draped along the western Piedmont triggered scattered afternoon and evening thunderstorms across the southern to northeastern Piedmont. These storms produced several reports of flash flooding in Wake and Cumberland Counties. No storms reached severe limits and the storm activity tapered off across central North Carolina by late evening. A mid-level disturbance coupled to a cold front draped along the western Piedmont triggered scattered afternoon and evening thunderstorms across the southern to northeastern Piedmont. These storms produced several reports of flash flooding in Wake and Cumberland Counties. No storms reached severe limits and the storm activity tapered off across central North Carolina by late evening. A mid-level disturbance coupled to a cold front draped along the western Piedmont triggered scattered afternoon and evening thunderstorms across the southern to northeastern Piedmont. These storms produced several reports of flash flooding in Wake and Cumberland Counties. No storms reached severe limits and the storm activity tapered off across central North Carolina by late evening. A mid-level disturbance coupled to a cold front draped along the western Piedmont triggered scattered afternoon and evening thunderstorms across the southern to northeastern Piedmont. These storms produced several reports of flash flooding in Wake and Cumberland Counties. No storms reached severe limits and the storm activity tapered off across central North Carolina by late evening. A mid-level disturbance coupled to a cold front draped along the western Piedmont triggered scattered afternoon and evening thunderstorms across the southern to northeastern Piedmont. These storms produced several reports of flash flooding in Wake and Cumberland Counties. No storms reached severe limits and the storm activity tapered off across central North Carolina by late evening.\nEvent Narrative: A car was submerged in flood waters near the intersection of Lynn Rd and Glenwood Ave. A car was submerged in flood waters near the intersection of Leesville Rd and West Millbrook Rd. A car was submerged in flood waters near the 8600 block of Glenwood Ave. A car was submerged in flood waters near the intersection of Alexander Dr and Glenwood Ave. A mudslide caused by flash flooding closed Duraleigh Rd at Weaver Dr. A car was in flood waters near the intersection of Lynn Rd and Glenwood Ave. Flooding closed several lanes on Glenwood Ave near Crabtree Valley Mall in Raleigh.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 47.8206 km away, between 2022-07-16 14:49:00 and 2022-07-16 14:49:00. 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: A mid-level trough across the Mid-Atlantic region tracked east-southeast by the late afternoon and evening, reaching the Virginia coast by late in the evening around midnight. A Piedmont trough along with the mid-level disturbance led to isolated to scattered showers and storms across the region, several of which produced damaging winds over the northern Piedmont, as well as one instance of flash flooding.\nEvent Narrative: A tree was reported down near the intersection of Mill Creek Rd and Lee St.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 35.1498 km away, between 2022-07-21 14:22:00 and 2022-07-21 14:40:00. 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 line of thunderstorms moved eastward through central North Carolina during the early afternoon hours, within an increasingly warm, moist environment ahead of a surface trough and southward moving cold front. Several of the storms produced damaging wind gusts as they moved through the Triad toward the Triangle of central North Carolina in the evening hours. A line of thunderstorms moved eastward through central North Carolina during the early afternoon hours, within an increasingly warm, moist environment ahead of a surface trough and southward moving cold front. Several of the storms produced damaging wind gusts as they moved through the Triad toward the Triangle of central North Carolina in the evening hours.\nEvent Narrative: One tree was reported down near the intersection of east Green St and south Main St in Franklinton. One tree was reported down near the intersection of North Carolina Highway 96 and Old Franklinton Rd near Wilton.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 26.614 km away, between 2022-07-24 16:00:00 and 2022-07-24 16:07:00. 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: Under the influence of the North Atlantic subtropical high, classic summer time storms developed within an environment conducive to microbursts. Isolated reports of wind damage occurred within close proximity to the strongest downdrafts, especially across the central Piedmont. Under the influence of the North Atlantic subtropical high, classic summer time storms developed within an environment conducive to microbursts. Isolated reports of wind damage occurred within close proximity to the strongest downdrafts, especially across the central Piedmont.\nEvent Narrative: Multiple trees were reported down northeast of Pittsboro, near the intersection of Redbud and Poplar Lane. Multiple trees were reported down in the King Charles area, near the intersection of North King Charles Rd and Brighton Rd east of Raleigh.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 36.3778 km away, between 2022-07-25 20:23:00 and 2022-07-25 20:42:00. 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 surface lee trough over the Foothills of western North Carolina and the northwest Piedmont of central North Carolina led to the development of scattered afternoon and evening severe storms. Several of the storms produced wind damage and resultant downed trees and power lines. Storm activity waned by the late evening hours. A surface lee trough over the Foothills of western North Carolina and the northwest Piedmont of central North Carolina led to the development of scattered afternoon and evening severe storms. Several of the storms produced wind damage and resultant downed trees and power lines. Storm activity waned by the late evening hours.\nEvent Narrative: Trees were reported down on power lines near the intersection of Keel Boat Lane and Royal Street. Power outages were reported from fallen trees and limbs near the intersection of Old Stage Road and Stone Home Lane.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 18.9191 km away, between 2022-07-26 13:24:00 and 2022-07-26 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 25000.0 and crop damage of 0.0. \n\nEpisode Narrative: A mid to upper-level disturbance was present along the Mid-Mississippi and Ohio Valleys, with a frontal boundary oriented west to east over Kentucky into Virginia. The frontal boundary remained to the north during the event, but subtle surface boundaries with high instability and moisture across central NC and the mid-level disturbance led to scattered to numerous showers and storms forming around midday, peaking in the late-afternoon to early evening and tapering off by the late-evening hours. Several storms produced downed trees across the Piedmont of central NC. A mid to upper-level disturbance was present along the Mid-Mississippi and Ohio Valleys, with a frontal boundary oriented west to east over Kentucky into Virginia. The frontal boundary remained to the north during the event, but subtle surface boundaries with high instability and moisture across central NC and the mid-level disturbance led to scattered to numerous showers and storms forming around midday, peaking in the late-afternoon to early evening and tapering off by the late-evening hours. Several storms produced downed trees across the Piedmont of central NC. A mid to upper-level disturbance was present along the Mid-Mississippi and Ohio Valleys, with a frontal boundary oriented west to east over Kentucky into Virginia. The frontal boundary remained to the north during the event, but subtle surface boundaries with high instability and moisture across central NC and the mid-level disturbance led to scattered to numerous showers and storms forming around midday, peaking in the late-afternoon to early evening and tapering off by the late-evening hours. Several storms produced downed trees across the Piedmont of central NC.\nEvent Narrative: A large tree caused a downed power pole and snapped power poles, producing several power outages near the intersection of Willow Drive and Conner Drive. Trees were reported down on power lines along Ebenezer Church Road near Umstead State Park. Multiple trees were reported down on utility company equipment, leading to at least two thousand power outages near Auburn along the intersection of Battle Bridge Road and Offshore Drive.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 33.5152 km away, between 2022-07-27 17:43:00 and 2022-07-27 17:45:00. 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 10000.0 and crop damage of 0.0. \n\nEpisode Narrative: Central North Carolina was under a mid-level ridge of high pressure over the southeastern US, while the stronger mid-level flow was over the Mississippi Valley into the Mid-Atlantic states. While there was no defined surface boundary, isolated/scattered storms developed in the mid to late afternoon across the area. Another round of more widespread showers and storms tracked from south-central Virginia into the central North Carolina Piedmont and Coastal Plain in the mid to late-evening hours. Several of the storms produced downed trees and resultant power outages. Central North Carolina was under a mid-level ridge of high pressure over the southeastern US, while the stronger mid-level flow was over the Mississippi Valley into the Mid-Atlantic states. While there was no defined surface boundary, isolated/scattered storms developed in the mid to late afternoon across the area. Another round of more widespread showers and storms tracked from south-central Virginia into the central North Carolina Piedmont and Coastal Plain in the mid to late-evening hours. Several of the storms produced downed trees and resultant power outages.\nEvent Narrative: Trees were reported down on powerlines near the intersection of Pocomoke Road and Fred Wilder Road. Trees were reported down on powerlines near the intersection of US Highway 1 North and Cleghorns 2 Drive in Youngsville.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 14.7082 km away, between 2022-07-29 19:34:00 and 2022-07-29 19:34:00. 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 mid-level disturbance tracked east across the Midwest and Ohio Valley during the afternoon and evening. This disturbance allowed a cold front across Missouri, Illinois, and Indiana to approach central North Carolina during the evening and overnight. Ahead of the front, strong surface heating with a moist atmosphere, as well as a Piedmont trough, allowed isolated to scattered thunderstorms to develop in the late afternoon and evening across the western Piedmont, tracking east into the Sandhills and Coastal Plain overnight. A few of the storms led to downed trees and power lines.\nEvent Narrative: Power outages were caused by fallen trees near the intersection of Ortega Road and Windsor Place.",
+        "The following events were reported: Lightning, Thunderstorm Wind. These occurred near station USW00013722, approximately 20.5281 km away, between 2022-08-10 16:06:00 and 2022-08-10 16:17:00.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 35000.0 and crop damage of 0.0. \n\nEpisode Narrative: A weak disturbance moved into and across the area and interacted with hot and humid air mass over central North Carolina, which led to clusters of strong to severe thunderstorms moving across the Piedmont. This resulted in multiple reports of wind damage. A weak disturbance moved into and across the area and interacted with hot and humid air mass over central North Carolina, which led to clusters of strong to severe thunderstorms moving across the Piedmont. This resulted in multiple reports of wind damage.\nEvent Narrative: A tree fell on a car near West Garner Road and Cedar Lane. Lightning struck a house near Hunting Ride Road.",
+        "The following events were reported: Flash Flood, Thunderstorm Wind. These occurred near station USW00013722, approximately 15.6648 km away, between 2022-08-11 17:58:00 and 2022-08-11 18:20:00.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 cluster of showers and thunderstorms developed along a slow moving cold front across the central Piedmont of central North Carolina. A few of the storms became strong to severe and produced damaging wind gusts and flash flooding across Wake County. A cluster of showers and thunderstorms developed along a slow moving cold front across the central Piedmont of central North Carolina. A few of the storms became strong to severe and produced damaging wind gusts and flash flooding across Wake County. A cluster of showers and thunderstorms developed along a slow moving cold front across the central Piedmont of central North Carolina. A few of the storms became strong to severe and produced damaging wind gusts and flash flooding across Wake County. A cluster of showers and thunderstorms developed along a slow moving cold front across the central Piedmont of central North Carolina. A few of the storms became strong to severe and produced damaging wind gusts and flash flooding across Wake County.\nEvent Narrative: Trees were reported down on power lines near the intersection of Strother Road and Garrett Road. Trees were reported down on power lines along Southall Road near Buffaloe Road. Flash flooding was reported along Glenwood Avenue at I-440. Flash flooding was reported along Atlantic Avenue at Hodges Street and Capital Boulevard.",
+        "The following events were reported: Flash Flood. These occurred near station USW00013722, approximately 35.9033 km away, between 2022-09-10 18:25:00 and 2022-09-10 20:30:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A tropical airmass interacted with a stalled frontal zone across portions of the southern Coatal Plain and eastern Sandhills of central North Carolina, producing heavy rain from numerous showers and storms. Flash flooding was reported in these areas, where the heaviest rain fell.\nEvent Narrative: Flash flooding was reported near the intersection of North Carolina Highway 42 and I-40.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 31.9018 km away, between 2022-09-12 14:55:00 and 2022-09-12 18:39:00. 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 15000.0 and crop damage of 0.0. \n\nEpisode Narrative: Scattered showers and thunderstorms developed along and in advance of a cold front across central North Carolina during the afternoon into the early evening hours in a moist and unstable atmosphere. Some of the storms across the western Piedmont became severe and produced damaging winds. Scattered showers and thunderstorms developed along and in advance of a cold front across central North Carolina during the afternoon into the early evening hours in a moist and unstable atmosphere. Some of the storms across the western Piedmont became severe and produced damaging winds. Scattered showers and thunderstorms developed along and in advance of a cold front across central North Carolina during the afternoon into the early evening hours in a moist and unstable atmosphere. Some of the storms across the western Piedmont became severe and produced damaging winds. Scattered showers and thunderstorms developed along and in advance of a cold front across central North Carolina during the afternoon into the early evening hours in a moist and unstable atmosphere. Some of the storms across the western Piedmont became severe and produced damaging winds.\nEvent Narrative: A tree was reported down at the intersection of Schely Road and Mincey Road. Trees were reported down near United States Highway 501. Trees were reported down near Ball Road. Trees and power lines were reported down near Fayetteville Road.",
+        "The following events were reported: Flash Flood. These occurred near station USW00013722, approximately 16.2251 km away, between 2022-09-30 20:05:00 and 2022-09-30 22:00:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: Hurricane Ian made landfall along the South Carolina coast near Georgetown during the early afternoon hours of September 30, 2022. Widespread wind gusts over tropical storm force and heavy rainfall occurred across much of central North Carolina through the afternoon and evening hours. There were numerous reports of wind damage and power outages as a result of the storm. Hurricane Ian made landfall along the South Carolina coast near Georgetown during the early afternoon hours of September 30, 2022. Widespread wind gusts over tropical storm force and heavy rainfall occurred across much of central North Carolina through the afternoon and evening hours. There were numerous reports of wind damage and power outages as a result of the storm. Hurricane Ian made landfall along the South Carolina coast near Georgetown during the early afternoon hours of September 30, 2022. Widespread wind gusts over tropical storm force and heavy rainfall occurred across much of central North Carolina through the afternoon and evening hours. There were numerous reports of wind damage and power outages as a result of the storm.\nEvent Narrative: Flashing flooding was reported near United States Highway 501 and Stadium Drive. Flash flooding was reporte along Walnut Creek at Rose Lane. Flash Flooding was reported along Crabtree Creek greenway near Morrisville.",
+        "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00013722, approximately 24.3378 km away, between 2022-10-17 17:24:00 and 2022-10-17 17:46:00. The events included records with hailstones measuring 25.5625 inches.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 deep trough across the eastern United States helped propel a strong cold front across central North Carolina during the late afternoon into the evening hours of October 17th. The strong dynamics and deep layer shear allowed for the development of a broken band of showers and storms along and ahead of the front. A couple of the storms became severe and produced large hail and damaging wind gusts. A deep trough across the eastern United States helped propel a strong cold front across central North Carolina during the late afternoon into the evening hours of October 17th. The strong dynamics and deep layer shear allowed for the development of a broken band of showers and storms along and ahead of the front. A couple of the storms became severe and produced large hail and damaging wind gusts. A deep trough across the eastern United States helped propel a strong cold front across central North Carolina during the late afternoon into the evening hours of October 17th. The strong dynamics and deep layer shear allowed for the development of a broken band of showers and storms along and ahead of the front. A couple of the storms became severe and produced large hail and damaging wind gusts. A deep trough across the eastern United States helped propel a strong cold front across central North Carolina during the late afternoon into the evening hours of October 17th. The strong dynamics and deep layer shear allowed for the development of a broken band of showers and storms along and ahead of the front. A couple of the storms became severe and produced large hail and damaging wind gusts.\nEvent Narrative: Half dollar size hail was reported near the intersection of Hillsborough Road and Britton Drive.  A tree was reported down near the intersection of Lawrence Road and Jack Franklin Road. A tree fell on a car along Red Mill Road, near I-85.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 29.9211 km away, between 2023-01-12 20:23:00 and 2023-01-12 21:40:00. 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 50000.0 and crop damage of 0.0. \n\nEpisode Narrative: Showers and thunderstorms developed along a prefrontal trough across the southern Appalachians and Carolinas during the afternoon into the evening in a weakly unstable airmass. However, strengthening southerly low level flow of 50kts along with strong flow aloft resulted in strong deep layer shear, helping to organize the convection into clusters/lines of storms. Some of the storms in the clusters produced damaging winds as they moved across the Piedmont of central North Carolina. Showers and thunderstorms developed along a prefrontal trough across the southern Appalachians and Carolinas during the afternoon into the evening in a weakly unstable airmass. However, strengthening southerly low level flow of 50kts along with strong flow aloft resulted in strong deep layer shear, helping to organize the convection into clusters/lines of storms. Some of the storms in the clusters produced damaging winds as they moved across the Piedmont of central North Carolina. Showers and thunderstorms developed along a prefrontal trough across the southern Appalachians and Carolinas during the afternoon into the evening in a weakly unstable airmass. However, strengthening southerly low level flow of 50kts along with strong flow aloft resulted in strong deep layer shear, helping to organize the convection into clusters/lines of storms. Some of the storms in the clusters produced damaging winds as they moved across the Piedmont of central North Carolina. Showers and thunderstorms developed along a prefrontal trough across the southern Appalachians and Carolinas during the afternoon into the evening in a weakly unstable airmass. However, strengthening southerly low level flow of 50kts along with strong flow aloft resulted in strong deep layer shear, helping to organize the convection into clusters/lines of storms. Some of the storms in the clusters produced damaging winds as they moved across the Piedmont of central North Carolina.\nEvent Narrative: Trees were reported down across the southern half of the county. A roof was blown off a building near the intersection of North Lasalle Street and Hillsborough Road. A tree was reported down on Smithfield Road near the Wake-Johnston County line. Two trees were reported down on a power line near the intersection of Highway 98 and United States Highway 401.",
+        "The following events were reported: Lightning. These occurred near station USW00013722, approximately 38.0479 km away, between 2023-03-02 04:05:00 and 2023-03-02 04:51:00.Thankfully, no injuries or fatalities were reported. The events caused property damage valued at 200000.0 and crop damage of 0.0. \n\nEpisode Narrative: An area of rain with embedded thunderstorms developed across the central North Carolina during the early morning hours of March 2nd in the area of a stalled surface front. While the thunderstorms remained below severe limits a couple of homes were struck by lighting, resulting in significant damage to the homes. An area of rain with embedded thunderstorms developed across the central North Carolina during the early morning hours of March 2nd in the area of a stalled surface front. While the thunderstorms remained below severe limits a couple of homes were struck by lighting, resulting in significant damage to the homes.\nEvent Narrative: A home was reported on fire from a lightning strike along Walnut Cove Drive. A home was reported on fire from a lightning strike on Marcellus Way.",
+        "The following events were reported: Flash Flood, Flood, Lightning. These occurred near station USW00013722, approximately 29.345 km away, between 2023-04-07 06:00:00 and 2023-04-07 19:30:00. The flood was caused by Heavy Rain. 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: A strong cold front resulted in the development of slow-moving thunderstorms with very heavy rain across portions of the Triangle. This resulted in multiple road and highway closures, particularly around Fuquay-Varina. A strong cold front resulted in the development of slow-moving thunderstorms with very heavy rain across portions of the Triangle. This resulted in multiple road and highway closures, particularly around Fuquay-Varina. A strong cold front resulted in the development of slow-moving thunderstorms with very heavy rain across portions of the Triangle. This resulted in multiple road and highway closures, particularly around Fuquay-Varina. A strong cold front resulted in the development of slow-moving thunderstorms with very heavy rain across portions of the Triangle. This resulted in multiple road and highway closures, particularly around Fuquay-Varina. A strong cold front resulted in the development of slow-moving thunderstorms with very heavy rain across portions of the Triangle. This resulted in multiple road and highway closures, particularly around Fuquay-Varina. A strong cold front resulted in the development of slow-moving thunderstorms with very heavy rain across portions of the Triangle. This resulted in multiple road and highway closures, particularly around Fuquay-Varina.\nEvent Narrative: A house fire was reported due to a lightning strike, which burned the attic. A roadway was closed near the intersection of North Carolina Highway 55 and North Carolina Highway 42. A flooded roadway was reported near Brookside Drive in Fuquay-Varina. A road closure was reported near the intersection of Holland Road and Mayfair Wood Road. South Estes Drive near Fordham Boulevard was flooded due to heavy rain from earlier in the day. Flooding was reported along Cleland Drive between Oakwood Drive and Kendall Drive from heavy rain earlier in the day.",
+        "The following events were reported: Hail. These occurred near station USW00013722, approximately 21.5405 km away, between 2023-04-14 14:26:00 and 2023-04-14 15:22:00. The events included records with hailstones measuring 1.1944444444444444 inches.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A warm front lifted through the area during the afternoon hours. Scattered showers and thunderstorms developed along the front, triggering several clusters of severe thunderstorms. A warm front lifted through the area during the afternoon hours. Scattered showers and thunderstorms developed along the front, triggering several clusters of severe thunderstorms. A warm front lifted through the area during the afternoon hours. Scattered showers and thunderstorms developed along the front, triggering several clusters of severe thunderstorms. A warm front lifted through the area during the afternoon hours. Scattered showers and thunderstorms developed along the front, triggering several clusters of severe thunderstorms. A warm front lifted through the area during the afternoon hours. Scattered showers and thunderstorms developed along the front, triggering several clusters of severe thunderstorms. A warm front lifted through the area during the afternoon hours. Scattered showers and thunderstorms developed along the front, triggering several clusters of severe thunderstorms. A warm front lifted through the area during the afternoon hours. Scattered showers and thunderstorms developed along the front, triggering several clusters of severe thunderstorms. A warm front lifted through the area during the afternoon hours. Scattered showers and thunderstorms developed along the front, triggering several clusters of severe thunderstorms. A warm front lifted through the area during the afternoon hours. Scattered showers and thunderstorms developed along the front, triggering several clusters of severe thunderstorms.\nEvent Narrative: Quarter size hail was reported along River Forks Road.    Quarter size hail was reported on Whistling Quail Run.  Quarter size hail was reported near Boxcar Way.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 43.2742 km away, between 2023-04-22 09:28:00 and 2023-04-22 09:28:00. 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: An upper low over the western Great Lakes and associated surface cold front over the Appalachians produced two rounds of showers and thunderstorms across the region. The first round of storms in the morning produced isolated wind damage along the I-85 corridor from the Triad eastward to Alamance and Orange Counties. Following a break in the storms around mid-day, a second round of storms develop immediately ahead of the cold front, producing additional wind damage across the Sandhills into the southern Coastal Plain. An upper low over the western Great Lakes and associated surface cold front over the Appalachians produced two rounds of showers and thunderstorms across the region. The first round of storms in the morning produced isolated wind damage along the I-85 corridor from the Triad eastward to Alamance and Orange Counties. Following a break in the storms around mid-day, a second round of storms develop immediately ahead of the cold front, producing additional wind damage across the Sandhills into the southern Coastal Plain.\nEvent Narrative: One tree was reported down near the intersection of Old Greensboro Road and Crawford Dairy Road. One tree was reported down on Compton Road.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 32.5957 km away, between 2023-04-30 13:50:00 and 2023-04-30 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 7500.0 and crop damage of 0.0. \n\nEpisode Narrative: A sub 1000 millibar surface low tracked through NC during the early afternoon hours. Showers and thunderstorms developed along a retreating warm front, causing numerous reports of downed trees and wind damage. Some portions of Wilson County saw significant tree damage with the storms as they moved through the area. A sub 1000 millibar surface low tracked through NC during the early afternoon hours. Showers and thunderstorms developed along a retreating warm front, causing numerous reports of downed trees and wind damage. Some portions of Wilson County saw significant tree damage with the storms as they moved through the area.\nEvent Narrative: Multiple trees were reported down at Caryle Road. Several trees were reported down on trails across Blue Jay Point County Park.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 37.4524 km away, between 2023-05-16 22:12:00 and 2023-05-16 23:10:00. 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 50000.0 and crop damage of 0.0. \n\nEpisode Narrative: A surface cold front approaching from the north northwest in the afternoon was associated with a nearly west to east mid level shear axis streaking through the base of a large mid level trough whose low was centered over northern Quebec. Southwest flow ahead of this front drew in warm air and 60s dew points into the area, and this combined with strengthening mid level flow and upper divergence produced sufficient support for the development of numerous severe thunderstorms. A surface cold front approaching from the north northwest in the afternoon was associated with a nearly west to east mid level shear axis streaking through the base of a large mid level trough whose low was centered over northern Quebec. Southwest flow ahead of this front drew in warm air and 60s dew points into the area, and this combined with strengthening mid level flow and upper divergence produced sufficient support for the development of numerous severe thunderstorms. A surface cold front approaching from the north northwest in the afternoon was associated with a nearly west to east mid level shear axis streaking through the base of a large mid level trough whose low was centered over northern Quebec. Southwest flow ahead of this front drew in warm air and 60s dew points into the area, and this combined with strengthening mid level flow and upper divergence produced sufficient support for the development of numerous severe thunderstorms. A surface cold front approaching from the north northwest in the afternoon was associated with a nearly west to east mid level shear axis streaking through the base of a large mid level trough whose low was centered over northern Quebec. Southwest flow ahead of this front drew in warm air and 60s dew points into the area, and this combined with strengthening mid level flow and upper divergence produced sufficient support for the development of numerous severe thunderstorms.\nEvent Narrative: A tree fell on an unoccupied house near Covered Bridge Road and Aldean Drive. A tree was reported down in the intersection of Medlin Road and Windless Trail. One tree was reported down near the intersection of Archer Lodge Road and Buffalo Road. Multiple trees were reported down on power lines.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 29.4674 km away, between 2023-06-16 16:00:00 and 2023-06-16 16:46:00. 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 15000.0 and crop damage of 0.0. \n\nEpisode Narrative: An approaching cold front from the Ohio Valley led to the development of scattered showers and thunderstorms across central NC in the late-afternoon and early evening hours. Several of the storms became severe, with reports of damaging winds across the northeast Piedmont. An approaching cold front from the Ohio Valley led to the development of scattered showers and thunderstorms across central NC in the late-afternoon and early evening hours. Several of the storms became severe, with reports of damaging winds across the northeast Piedmont. An approaching cold front from the Ohio Valley led to the development of scattered showers and thunderstorms across central NC in the late-afternoon and early evening hours. Several of the storms became severe, with reports of damaging winds across the northeast Piedmont.\nEvent Narrative: Power outages were reported due to fallen trees near the intersection of Carriage Tour Lane and Hometown Dr. Franklin County emergency management reports several trees down on cars, as well as wind damage producing a damaged shed and playground equipment, near the intersection of Cricketwood Lane and Spencers Gate Dr. Several trees were reported down in the towns of Efland, Mebane, and Hillsborough areas. This included a tree down on a car in Hillsborough, a tree down on a mobile home in Efland, and another tree down on the roof of a business in Efland.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 17.4702 km away, between 2023-06-19 14:09:00 and 2023-06-19 14:20:00. 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 15000.0 and crop damage of 0.0. \n\nEpisode Narrative: A slow moving area of low pressure west of the mountains brought abundant moisture into the Carolinas. Showers and thunderstorms developed across western and central North Carolina during the afternoon hours, producing numerous reports of downed trees and power lines. Training thunderstorms also produced minor flooding in the Greensboro area. A slow moving area of low pressure west of the mountains brought abundant moisture into the Carolinas. Showers and thunderstorms developed across western and central North Carolina during the afternoon hours, producing numerous reports of downed trees and power lines. Training thunderstorms also produced minor flooding in the Greensboro area. A slow moving area of low pressure west of the mountains brought abundant moisture into the Carolinas. Showers and thunderstorms developed across western and central North Carolina during the afternoon hours, producing numerous reports of downed trees and power lines. Training thunderstorms also produced minor flooding in the Greensboro area. A slow moving area of low pressure west of the mountains brought abundant moisture into the Carolinas. Showers and thunderstorms developed across western and central North Carolina during the afternoon hours, producing numerous reports of downed trees and power lines. Training thunderstorms also produced minor flooding in the Greensboro area. A slow moving area of low pressure west of the mountains brought abundant moisture into the Carolinas. Showers and thunderstorms developed across western and central North Carolina during the afternoon hours, producing numerous reports of downed trees and power lines. Training thunderstorms also produced minor flooding in the Greensboro area.\nEvent Narrative: A tree was reported down on power lines, resulting in power outages around the intersection of Willowdale Dr and Driftwood Dr. A tree fell on power lines, resulting in power outages around Monticello Ave. A tree was reported down near the 1000 block of Leon St, destroying a bus stop shelter. A tree was reported down at the intersection of Cole Mill Rd and Medford Rd. A tree was reported down near the intersection of Academy Rd and Duke University Rd.",
+        "The following events were reported: Flash Flood, Thunderstorm Wind. These occurred near station USW00013722, approximately 25.2764 km away, between 2023-06-23 16:52:00 and 2023-06-23 19:00:00.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 stalled frontal boundary remained in place across the central North Carolina Piedmont. A line of showers and storms tracked east-southeast and resulted in flash flooding across Orange County. A few trees were also reported down across the county. A stalled frontal boundary remained in place across the central North Carolina Piedmont. A line of showers and storms tracked east-southeast and resulted in flash flooding across Orange County. A few trees were also reported down across the county. A stalled frontal boundary remained in place across the central North Carolina Piedmont. A line of showers and storms tracked east-southeast and resulted in flash flooding across Orange County. A few trees were also reported down across the county. A stalled frontal boundary remained in place across the central North Carolina Piedmont. A line of showers and storms tracked east-southeast and resulted in flash flooding across Orange County. A few trees were also reported down across the county. A stalled frontal boundary remained in place across the central North Carolina Piedmont. A line of showers and storms tracked east-southeast and resulted in flash flooding across Orange County. A few trees were also reported down across the county. A stalled frontal boundary remained in place across the central North Carolina Piedmont. A line of showers and storms tracked east-southeast and resulted in flash flooding across Orange County. A few trees were also reported down across the county.\nEvent Narrative: The road was flooded near the intersection of Willow Dr and S Estes Dr. Flooding was reported along Fordham Blvd near Willow Dr. A few trees were reported down near the intersection of Westminster Dr and Martin Luther King Jr. Blvd. A few hundred people were without power due to fallen trees on power equipment. This was around the intersection of Old Oxford Rd and Oxford Hills Dr. Flooding was reported along Grove St in Chapel Hill. A flooded road was reported near the intersection of White Cross Rd and Old Greensboro Rd.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 19.7626 km away, between 2023-06-26 21:15:00 and 2023-06-26 21:45:00. 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 42500.0 and crop damage of 0.0. \n\nEpisode Narrative: A cold front interacted with a moist and unstable air mass to result in numerous showers and storms across central North Carolina. A few discrete cells first developed during the evening in the northwest Piedmont, resulting in reports of one to two inch hail there. Once the storms consolidated into a line farther south and east, they transitioned into more of a damaging wind event in the late evening and early overnight hours, with numerous reports of trees and power lines down in parts of the northeast Piedmont, Sandhills, and Coastal Plain. There were also many reports of flash flooding in Cumberland County, including Fayetteville. A cold front interacted with a moist and unstable air mass to result in numerous showers and storms across central North Carolina. A few discrete cells first developed during the evening in the northwest Piedmont, resulting in reports of one to two inch hail there. Once the storms consolidated into a line farther south and east, they transitioned into more of a damaging wind event in the late evening and early overnight hours, with numerous reports of trees and power lines down in parts of the northeast Piedmont, Sandhills, and Coastal Plain. There were also many reports of flash flooding in Cumberland County, including Fayetteville. A cold front interacted with a moist and unstable air mass to result in numerous showers and storms across central North Carolina. A few discrete cells first developed during the evening in the northwest Piedmont, resulting in reports of one to two inch hail there. Once the storms consolidated into a line farther south and east, they transitioned into more of a damaging wind event in the late evening and early overnight hours, with numerous reports of trees and power lines down in parts of the northeast Piedmont, Sandhills, and Coastal Plain. There were also many reports of flash flooding in Cumberland County, including Fayetteville. A cold front interacted with a moist and unstable air mass to result in numerous showers and storms across central North Carolina. A few discrete cells first developed during the evening in the northwest Piedmont, resulting in reports of one to two inch hail there. Once the storms consolidated into a line farther south and east, they transitioned into more of a damaging wind event in the late evening and early overnight hours, with numerous reports of trees and power lines down in parts of the northeast Piedmont, Sandhills, and Coastal Plain. There were also many reports of flash flooding in Cumberland County, including Fayetteville.\nEvent Narrative: A tree was reported down on power lines at Moon Meadow Lane. Trees were reported down on power lines. Trees were reported down on utility equipment. A tree landed on the roof of a house in Cary, causing the roof to collapse.",
+        "The following events were reported: Flash Flood, Thunderstorm Wind. These occurred near station USW00013722, approximately 22.0635 km away, between 2023-06-30 20:45:00 and 2023-06-30 23:59:00.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 weak surface trough was present across portions of the Piedmont of central North Carolina in an otherwise high pressure regime. Isolated to scattered showers and storms developed in the late afternoon to early evening over the western Piedmont, tracking east and south over the central Piedmont and Sandhills during the late evening and overnight hours. A few of the storms became severe in Chatham and Orange Counties, along with flash flooding over Durham. A weak surface trough was present across portions of the Piedmont of central North Carolina in an otherwise high pressure regime. Isolated to scattered showers and storms developed in the late afternoon to early evening over the western Piedmont, tracking east and south over the central Piedmont and Sandhills during the late evening and overnight hours. A few of the storms became severe in Chatham and Orange Counties, along with flash flooding over Durham. A weak surface trough was present across portions of the Piedmont of central North Carolina in an otherwise high pressure regime. Isolated to scattered showers and storms developed in the late afternoon to early evening over the western Piedmont, tracking east and south over the central Piedmont and Sandhills during the late evening and overnight hours. A few of the storms became severe in Chatham and Orange Counties, along with flash flooding over Durham. A weak surface trough was present across portions of the Piedmont of central North Carolina in an otherwise high pressure regime. Isolated to scattered showers and storms developed in the late afternoon to early evening over the western Piedmont, tracking east and south over the central Piedmont and Sandhills during the late evening and overnight hours. A few of the storms became severe in Chatham and Orange Counties, along with flash flooding over Durham. A weak surface trough was present across portions of the Piedmont of central North Carolina in an otherwise high pressure regime. Isolated to scattered showers and storms developed in the late afternoon to early evening over the western Piedmont, tracking east and south over the central Piedmont and Sandhills during the late evening and overnight hours. A few of the storms became severe in Chatham and Orange Counties, along with flash flooding over Durham. A weak surface trough was present across portions of the Piedmont of central North Carolina in an otherwise high pressure regime. Isolated to scattered showers and storms developed in the late afternoon to early evening over the western Piedmont, tracking east and south over the central Piedmont and Sandhills during the late evening and overnight hours. A few of the storms became severe in Chatham and Orange Counties, along with flash flooding over Durham. A weak surface trough was present across portions of the Piedmont of central North Carolina in an otherwise high pressure regime. Isolated to scattered showers and storms developed in the late afternoon to early evening over the western Piedmont, tracking east and south over the central Piedmont and Sandhills during the late evening and overnight hours. A few of the storms became severe in Chatham and Orange Counties, along with flash flooding over Durham.\nEvent Narrative: The city of Durham reported high water and numerous vehicles stranded. The USGS river gauge on Third Fork Creek at Martin Luther King Jr Parkway in Durham reached moderate flood stage. Cars were reported stranded in flooded roadways near the intersection of Fayetteville St and East Pilot St. Several reports of trees down in the area near the intersection of Settle St and Village Park Dr. Power outages were also reported. Trees were reported down, resulting in power outages near the intersection of Big Woods Rd and Jack Bennett Rd. Trees were reported down, resulting in power outages near the intersection of Mt Zion Rd and Moncure Pittsboro Rd. Emergency management reported multiple trees down, along with damage to a car and a non-residential building/structure along Mangum Ct.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 36.3236 km away, between 2023-07-01 16:06:00 and 2023-07-01 16:44:00. 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: An area of showers and thunderstorms developed over southwestern Virginia and intensified as they moved southeast into North Carolina. The line of showers and thunderstorms tracked east-southeast across the central North Carolina Piedmont and into the Sandhills, producing numerous damaging wind reports. An area of showers and thunderstorms developed over southwestern Virginia and intensified as they moved southeast into North Carolina. The line of showers and thunderstorms tracked east-southeast across the central North Carolina Piedmont and into the Sandhills, producing numerous damaging wind reports. An area of showers and thunderstorms developed over southwestern Virginia and intensified as they moved southeast into North Carolina. The line of showers and thunderstorms tracked east-southeast across the central North Carolina Piedmont and into the Sandhills, producing numerous damaging wind reports. An area of showers and thunderstorms developed over southwestern Virginia and intensified as they moved southeast into North Carolina. The line of showers and thunderstorms tracked east-southeast across the central North Carolina Piedmont and into the Sandhills, producing numerous damaging wind reports.\nEvent Narrative: An emergency manager reported a tree down across the roadway near the intersection of Dairyland Rd and Triple Crown Dr. A tree was reported down near the intersection of Moncure Pittsboro Rd and Highway US-1. An emergency manager reported a tree was down across the roadway near the 2100 block of Moorefields Rd in Efland. A large tree was reported down on powerlines near the intersection of Katie Lane and North Carolina Highway 54.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 40.2541 km away, between 2023-07-05 13:34:00 and 2023-07-05 13:34:00. 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: Showers and thunderstorms developed during the late afternoon over the central/eastern Piedmont and central Coastal Plain. The storms then drifted southward over the Sandhills and southern Piedmont by the evening and overnight.\nEvent Narrative: A tree was reported down at Old Stage Rd and Pete Fish Rd.",
+        "The following events were reported: Hail, Lightning, Thunderstorm Wind. These occurred near station USW00013722, approximately 27.3525 km away, between 2023-07-07 16:28:00 and 2023-07-07 18:20:00. The events included records with hailstones measuring 30.45 inches.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 Piedmont trough was the focus of initially isolated thunderstorms during the mid afternoon. The storms formed over the eastern Piedmont, then became more clustered as they moved southeast and south through portions of Edgecombe, Wilson, Franklin, Wake, Wilson, Nash, Wayne, Harnett, Johnston, and Sampson Counties. A Piedmont trough was the focus of initially isolated thunderstorms during the mid afternoon. The storms formed over the eastern Piedmont, then became more clustered as they moved southeast and south through portions of Edgecombe, Wilson, Franklin, Wake, Wilson, Nash, Wayne, Harnett, Johnston, and Sampson Counties. A Piedmont trough was the focus of initially isolated thunderstorms during the mid afternoon. The storms formed over the eastern Piedmont, then became more clustered as they moved southeast and south through portions of Edgecombe, Wilson, Franklin, Wake, Wilson, Nash, Wayne, Harnett, Johnston, and Sampson Counties. A Piedmont trough was the focus of initially isolated thunderstorms during the mid afternoon. The storms formed over the eastern Piedmont, then became more clustered as they moved southeast and south through portions of Edgecombe, Wilson, Franklin, Wake, Wilson, Nash, Wayne, Harnett, Johnston, and Sampson Counties. A Piedmont trough was the focus of initially isolated thunderstorms during the mid afternoon. The storms formed over the eastern Piedmont, then became more clustered as they moved southeast and south through portions of Edgecombe, Wilson, Franklin, Wake, Wilson, Nash, Wayne, Harnett, Johnston, and Sampson Counties. A Piedmont trough was the focus of initially isolated thunderstorms during the mid afternoon. The storms formed over the eastern Piedmont, then became more clustered as they moved southeast and south through portions of Edgecombe, Wilson, Franklin, Wake, Wilson, Nash, Wayne, Harnett, Johnston, and Sampson Counties.\nEvent Narrative: Fallen trees resulted in downed power lines near the intersection of Holland Rd and Purfoy Rd. Fallen trees resulted in downed power lines near the intersection of Ebenezer Church Rd and Westgate Rd. Lightning struck a home near the intersection of Bucksport Ln and Boothbay Ct. Public reported 1.25 inch hail near the intersection of Powell Dr and England Ave. A tree was reported down near the intersection of Knights Bridge Dr and Twin Acres Rd. A trained spotter reported quarter inch hail along Sherron Hill Ln.",
+        "The following events were reported: Flash Flood. These occurred near station USW00013722, approximately 15.7356 km away, between 2023-07-08 16:17:00 and 2023-07-08 17:50:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A surface trough over the central North Carolina Piedmont coupled with an upper trough led to scattered thunderstorm development that eventually merged into a line of showers and thunderstorms over the northwest Piedmont. These storms tracked east into the Triangle, Sandhills, and Coastal Plain by late in the evening hours, weakening with eastward extent into the overnight hours. Flash flooding was reported in Alamance and Wake counties. A surface trough over the central North Carolina Piedmont coupled with an upper trough led to scattered thunderstorm development that eventually merged into a line of showers and thunderstorms over the northwest Piedmont. These storms tracked east into the Triangle, Sandhills, and Coastal Plain by late in the evening hours, weakening with eastward extent into the overnight hours. Flash flooding was reported in Alamance and Wake counties.\nEvent Narrative: Flooding was reported at Interstate 440 and Western Blvd in Raleigh. Flooding was reported on Atlantic Ave between Highwoods Blvd and Millbrook Rd.",
+        "The following events were reported: Flash Flood, Thunderstorm Wind. These occurred near station USW00013722, approximately 28.6373 km away, between 2023-07-09 11:43:00 and 2023-07-09 14:54:00.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: A southward moving cold front from the Ohio Valley led to the development of a line of showers and thunderstorms that tracking from the northwest Piedmont in the late-morning hours into the Coastal Plain of central North Carolina by mid to late afternoon. Numerous reports of damaging winds and flash flooding were reported throughout central North Carolina. A southward moving cold front from the Ohio Valley led to the development of a line of showers and thunderstorms that tracking from the northwest Piedmont in the late-morning hours into the Coastal Plain of central North Carolina by mid to late afternoon. Numerous reports of damaging winds and flash flooding were reported throughout central North Carolina. A southward moving cold front from the Ohio Valley led to the development of a line of showers and thunderstorms that tracking from the northwest Piedmont in the late-morning hours into the Coastal Plain of central North Carolina by mid to late afternoon. Numerous reports of damaging winds and flash flooding were reported throughout central North Carolina. A southward moving cold front from the Ohio Valley led to the development of a line of showers and thunderstorms that tracking from the northwest Piedmont in the late-morning hours into the Coastal Plain of central North Carolina by mid to late afternoon. Numerous reports of damaging winds and flash flooding were reported throughout central North Carolina. A southward moving cold front from the Ohio Valley led to the development of a line of showers and thunderstorms that tracking from the northwest Piedmont in the late-morning hours into the Coastal Plain of central North Carolina by mid to late afternoon. Numerous reports of damaging winds and flash flooding were reported throughout central North Carolina. A southward moving cold front from the Ohio Valley led to the development of a line of showers and thunderstorms that tracking from the northwest Piedmont in the late-morning hours into the Coastal Plain of central North Carolina by mid to late afternoon. Numerous reports of damaging winds and flash flooding were reported throughout central North Carolina. A southward moving cold front from the Ohio Valley led to the development of a line of showers and thunderstorms that tracking from the northwest Piedmont in the late-morning hours into the Coastal Plain of central North Carolina by mid to late afternoon. Numerous reports of damaging winds and flash flooding were reported throughout central North Carolina. A southward moving cold front from the Ohio Valley led to the development of a line of showers and thunderstorms that tracking from the northwest Piedmont in the late-morning hours into the Coastal Plain of central North Carolina by mid to late afternoon. Numerous reports of damaging winds and flash flooding were reported throughout central North Carolina. A southward moving cold front from the Ohio Valley led to the development of a line of showers and thunderstorms that tracking from the northwest Piedmont in the late-morning hours into the Coastal Plain of central North Carolina by mid to late afternoon. Numerous reports of damaging winds and flash flooding were reported throughout central North Carolina. A southward moving cold front from the Ohio Valley led to the development of a line of showers and thunderstorms that tracking from the northwest Piedmont in the late-morning hours into the Coastal Plain of central North Carolina by mid to late afternoon. Numerous reports of damaging winds and flash flooding were reported throughout central North Carolina. A southward moving cold front from the Ohio Valley led to the development of a line of showers and thunderstorms that tracking from the northwest Piedmont in the late-morning hours into the Coastal Plain of central North Carolina by mid to late afternoon. Numerous reports of damaging winds and flash flooding were reported throughout central North Carolina. A southward moving cold front from the Ohio Valley led to the development of a line of showers and thunderstorms that tracking from the northwest Piedmont in the late-morning hours into the Coastal Plain of central North Carolina by mid to late afternoon. Numerous reports of damaging winds and flash flooding were reported throughout central North Carolina. A southward moving cold front from the Ohio Valley led to the development of a line of showers and thunderstorms that tracking from the northwest Piedmont in the late-morning hours into the Coastal Plain of central North Carolina by mid to late afternoon. Numerous reports of damaging winds and flash flooding were reported throughout central North Carolina. A southward moving cold front from the Ohio Valley led to the development of a line of showers and thunderstorms that tracking from the northwest Piedmont in the late-morning hours into the Coastal Plain of central North Carolina by mid to late afternoon. Numerous reports of damaging winds and flash flooding were reported throughout central North Carolina. A southward moving cold front from the Ohio Valley led to the development of a line of showers and thunderstorms that tracking from the northwest Piedmont in the late-morning hours into the Coastal Plain of central North Carolina by mid to late afternoon. Numerous reports of damaging winds and flash flooding were reported throughout central North Carolina. A southward moving cold front from the Ohio Valley led to the development of a line of showers and thunderstorms that tracking from the northwest Piedmont in the late-morning hours into the Coastal Plain of central North Carolina by mid to late afternoon. Numerous reports of damaging winds and flash flooding were reported throughout central North Carolina.\nEvent Narrative: A tree was reported down along Triple Creek Dr north of Efland. Two trees were reported down along Efland Cedar Grove Rd. A tree was reported down near the intersection of Mill Creek Rd and Lonesome Rd. Multiple trees were reported down on the property located along Eno Cemetery Rd. Power outages were reported due to fallen trees on powerlines near the intersection of Jackson Rd and Christian Light Rd. Trees were reported down, resulting in power outages, near the intersection of Hillsborough Rd and Old Springs Rd. Hundreds of power outages were reported due to downed trees on powerlines near the intersection of Old Farrington Rd and Whippoorwill Ln. Power outages were reported due to fallen trees on powerlines near the intersection of Poyner Rd and Burcliff Pl. Power outages were reported due to fallen trees on powerlines near the intersection of Landingham Dr and Lautenberg Ln. Power outages were reported due to fallen trees on powerlines near the intersection of New Bern Ave and Dickens Dr. Hillsborough St at William Moore Dr was closed due to flooding. Trees fell on power lines and resulted in hundreds of power outages near the intersection of NC Highway 87 and W Salisbury St. Flooding near W Franklin St and Semart Dr led to road closures. Flash flooding led to flooding along Hillsborough St near Chapel Hill Rd. The intersection of Melbourne Rd and Aukland Dr was closed due to flash flooding. A large tree fell on power lines near the intersection of Mills St and Wake Forest Rd in Raleigh.",
+        "The following events were reported: Flash Flood. These occurred near station USW00013722, approximately 32.4637 km away, between 2023-07-14 05:45:00 and 2023-07-14 07:30:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A few surface boundaries, from upstream thunderstorms over Virginia and the North Carolina Foothills during the afternoon and evening on the 13th of July, converged upon and focused thunderstorm development over central North Carolina, as they settled generally southward throughout the morning through evening hours on the 14th. Damaging wind gusts and flash flooding resulted from a combination of slow-moving showers and thunderstorms. A few surface boundaries, from upstream thunderstorms over Virginia and the North Carolina Foothills during the afternoon and evening on the 13th of July, converged upon and focused thunderstorm development over central North Carolina, as they settled generally southward throughout the morning through evening hours on the 14th. Damaging wind gusts and flash flooding resulted from a combination of slow-moving showers and thunderstorms. A few surface boundaries, from upstream thunderstorms over Virginia and the North Carolina Foothills during the afternoon and evening on the 13th of July, converged upon and focused thunderstorm development over central North Carolina, as they settled generally southward throughout the morning through evening hours on the 14th. Damaging wind gusts and flash flooding resulted from a combination of slow-moving showers and thunderstorms.\nEvent Narrative: Several feet of water was reported over the roadway near the intersection of Chatham Church Rd and Johnny Shaw Rd. The road was impassable. The roadway was closed near the intersection of Rodinson Ln and Woodland Church Rd due to high water. Water was covering the bridge with debris in the roadway near the intersection of Mangum Dairy Rd and Brayer Hill Path.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 28.6685 km away, between 2023-08-07 17:55:00 and 2023-08-07 18:57:00. 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 57500.0 and crop damage of 0.0. \n\nEpisode Narrative: A shortwave trough approached from the west ahead of a cold front. Forcing from this trough and adequate bulk wind shear combined with strong surface heating and instability to result in a line of severe storms that initially developed over the North Carolina mountains. The line then pushed east across central North Carolina in the late afternoon and early evening, resulting in widespread straight-line wind damage. A shortwave trough approached from the west ahead of a cold front. Forcing from this trough and adequate bulk wind shear combined with strong surface heating and instability to result in a line of severe storms that initially developed over the North Carolina mountains. The line then pushed east across central North Carolina in the late afternoon and early evening, resulting in widespread straight-line wind damage. A shortwave trough approached from the west ahead of a cold front. Forcing from this trough and adequate bulk wind shear combined with strong surface heating and instability to result in a line of severe storms that initially developed over the North Carolina mountains. The line then pushed east across central North Carolina in the late afternoon and early evening, resulting in widespread straight-line wind damage. A shortwave trough approached from the west ahead of a cold front. Forcing from this trough and adequate bulk wind shear combined with strong surface heating and instability to result in a line of severe storms that initially developed over the North Carolina mountains. The line then pushed east across central North Carolina in the late afternoon and early evening, resulting in widespread straight-line wind damage. A shortwave trough approached from the west ahead of a cold front. Forcing from this trough and adequate bulk wind shear combined with strong surface heating and instability to result in a line of severe storms that initially developed over the North Carolina mountains. The line then pushed east across central North Carolina in the late afternoon and early evening, resulting in widespread straight-line wind damage. A shortwave trough approached from the west ahead of a cold front. Forcing from this trough and adequate bulk wind shear combined with strong surface heating and instability to result in a line of severe storms that initially developed over the North Carolina mountains. The line then pushed east across central North Carolina in the late afternoon and early evening, resulting in widespread straight-line wind damage.\nEvent Narrative: Trees and power lines were down at Launis Street and Circle Drive. Several thousand power outages were reported due to trees down on power equipment. A tree was blocking a portion of Bass Lake Road near Goosehaven Lane. A 20 foot pine tree and power lines were down at Simpkins Road and Race Track Road. A power pole and power line were down at 4400 Wake Forest Road. A tree was down on a house.",
+        "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00013722, approximately 26.9634 km away, between 2023-08-15 13:20:00 and 2023-08-15 16:25:00. The events included records with hailstones measuring 45.526315789473685 inches.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 trough and associated cold front interacted with a very hot and humid air mass to result in widespread showers and storms across much of central North Carolina in the afternoon and early evening. With adequate wind shear, some of the storms were severe, and they consolidated into a line as they pushed east. There were numerous reports of wind damage across the Piedmont and northern and central Coastal Plain, along with several reports of large hail. One fatality occurred in Durham where a tree fell on a woman's vehicle. A trough and associated cold front interacted with a very hot and humid air mass to result in widespread showers and storms across much of central North Carolina in the afternoon and early evening. With adequate wind shear, some of the storms were severe, and they consolidated into a line as they pushed east. There were numerous reports of wind damage across the Piedmont and northern and central Coastal Plain, along with several reports of large hail. One fatality occurred in Durham where a tree fell on a woman's vehicle. A trough and associated cold front interacted with a very hot and humid air mass to result in widespread showers and storms across much of central North Carolina in the afternoon and early evening. With adequate wind shear, some of the storms were severe, and they consolidated into a line as they pushed east. There were numerous reports of wind damage across the Piedmont and northern and central Coastal Plain, along with several reports of large hail. One fatality occurred in Durham where a tree fell on a woman's vehicle. A trough and associated cold front interacted with a very hot and humid air mass to result in widespread showers and storms across much of central North Carolina in the afternoon and early evening. With adequate wind shear, some of the storms were severe, and they consolidated into a line as they pushed east. There were numerous reports of wind damage across the Piedmont and northern and central Coastal Plain, along with several reports of large hail. One fatality occurred in Durham where a tree fell on a woman's vehicle. A trough and associated cold front interacted with a very hot and humid air mass to result in widespread showers and storms across much of central North Carolina in the afternoon and early evening. With adequate wind shear, some of the storms were severe, and they consolidated into a line as they pushed east. There were numerous reports of wind damage across the Piedmont and northern and central Coastal Plain, along with several reports of large hail. One fatality occurred in Durham where a tree fell on a woman's vehicle. A trough and associated cold front interacted with a very hot and humid air mass to result in widespread showers and storms across much of central North Carolina in the afternoon and early evening. With adequate wind shear, some of the storms were severe, and they consolidated into a line as they pushed east. There were numerous reports of wind damage across the Piedmont and northern and central Coastal Plain, along with several reports of large hail. One fatality occurred in Durham where a tree fell on a woman's vehicle. A trough and associated cold front interacted with a very hot and humid air mass to result in widespread showers and storms across much of central North Carolina in the afternoon and early evening. With adequate wind shear, some of the storms were severe, and they consolidated into a line as they pushed east. There were numerous reports of wind damage across the Piedmont and northern and central Coastal Plain, along with several reports of large hail. One fatality occurred in Durham where a tree fell on a woman's vehicle. A trough and associated cold front interacted with a very hot and humid air mass to result in widespread showers and storms across much of central North Carolina in the afternoon and early evening. With adequate wind shear, some of the storms were severe, and they consolidated into a line as they pushed east. There were numerous reports of wind damage across the Piedmont and northern and central Coastal Plain, along with several reports of large hail. One fatality occurred in Durham where a tree fell on a woman's vehicle. A trough and associated cold front interacted with a very hot and humid air mass to result in widespread showers and storms across much of central North Carolina in the afternoon and early evening. With adequate wind shear, some of the storms were severe, and they consolidated into a line as they pushed east. There were numerous reports of wind damage across the Piedmont and northern and central Coastal Plain, along with several reports of large hail. One fatality occurred in Durham where a tree fell on a woman's vehicle. A trough and associated cold front interacted with a very hot and humid air mass to result in widespread showers and storms across much of central North Carolina in the afternoon and early evening. With adequate wind shear, some of the storms were severe, and they consolidated into a line as they pushed east. There were numerous reports of wind damage across the Piedmont and northern and central Coastal Plain, along with several reports of large hail. One fatality occurred in Durham where a tree fell on a woman's vehicle. A trough and associated cold front interacted with a very hot and humid air mass to result in widespread showers and storms across much of central North Carolina in the afternoon and early evening. With adequate wind shear, some of the storms were severe, and they consolidated into a line as they pushed east. There were numerous reports of wind damage across the Piedmont and northern and central Coastal Plain, along with several reports of large hail. One fatality occurred in Durham where a tree fell on a woman's vehicle. A trough and associated cold front interacted with a very hot and humid air mass to result in widespread showers and storms across much of central North Carolina in the afternoon and early evening. With adequate wind shear, some of the storms were severe, and they consolidated into a line as they pushed east. There were numerous reports of wind damage across the Piedmont and northern and central Coastal Plain, along with several reports of large hail. One fatality occurred in Durham where a tree fell on a woman's vehicle. A trough and associated cold front interacted with a very hot and humid air mass to result in widespread showers and storms across much of central North Carolina in the afternoon and early evening. With adequate wind shear, some of the storms were severe, and they consolidated into a line as they pushed east. There were numerous reports of wind damage across the Piedmont and northern and central Coastal Plain, along with several reports of large hail. One fatality occurred in Durham where a tree fell on a woman's vehicle. A trough and associated cold front interacted with a very hot and humid air mass to result in widespread showers and storms across much of central North Carolina in the afternoon and early evening. With adequate wind shear, some of the storms were severe, and they consolidated into a line as they pushed east. There were numerous reports of wind damage across the Piedmont and northern and central Coastal Plain, along with several reports of large hail. One fatality occurred in Durham where a tree fell on a woman's vehicle. A trough and associated cold front interacted with a very hot and humid air mass to result in widespread showers and storms across much of central North Carolina in the afternoon and early evening. With adequate wind shear, some of the storms were severe, and they consolidated into a line as they pushed east. There were numerous reports of wind damage across the Piedmont and northern and central Coastal Plain, along with several reports of large hail. One fatality occurred in Durham where a tree fell on a woman's vehicle. A trough and associated cold front interacted with a very hot and humid air mass to result in widespread showers and storms across much of central North Carolina in the afternoon and early evening. With adequate wind shear, some of the storms were severe, and they consolidated into a line as they pushed east. There were numerous reports of wind damage across the Piedmont and northern and central Coastal Plain, along with several reports of large hail. One fatality occurred in Durham where a tree fell on a woman's vehicle. A trough and associated cold front interacted with a very hot and humid air mass to result in widespread showers and storms across much of central North Carolina in the afternoon and early evening. With adequate wind shear, some of the storms were severe, and they consolidated into a line as they pushed east. There were numerous reports of wind damage across the Piedmont and northern and central Coastal Plain, along with several reports of large hail. One fatality occurred in Durham where a tree fell on a woman's vehicle. A trough and associated cold front interacted with a very hot and humid air mass to result in widespread showers and storms across much of central North Carolina in the afternoon and early evening. With adequate wind shear, some of the storms were severe, and they consolidated into a line as they pushed east. There were numerous reports of wind damage across the Piedmont and northern and central Coastal Plain, along with several reports of large hail. One fatality occurred in Durham where a tree fell on a woman's vehicle. A trough and associated cold front interacted with a very hot and humid air mass to result in widespread showers and storms across much of central North Carolina in the afternoon and early evening. With adequate wind shear, some of the storms were severe, and they consolidated into a line as they pushed east. There were numerous reports of wind damage across the Piedmont and northern and central Coastal Plain, along with several reports of large hail. One fatality occurred in Durham where a tree fell on a woman's vehicle.\nEvent Narrative: There were several downed trees across Johnston County. The worst damage was seen from Jackson King Road to Four Oaks and locations south. Numerous trees were down across a widespread area in Franklin County. A tree was down at North Carolina Highway 96 and Pocomoke Road. There was a fatality from a tree falling onto a vehicle at Anderson Street and Morehead Avenue. Numerous trees were down in the Maplewood Cemetery area. A large tree was down. Wind damage resulted in a broken crossing arm at a railroad crossing. Trees were down in the area. A tree was reported down on Holland Road at Judd Road. A tree was reported down at Purnell Road and Holly Forest Drive.   A large tree was blown down. Trees and tree limbs were down blocking the road. Multiple trees were reported down at Creedmoor Road and Old Weaver Trail. Several trees were down blocking the road at Park Avenue and Hampton Lane. This gust was measured on the Duke Hospital helipad. Two pine trees were down in a parking lot. Two trees were down on North Carolina Highway 98 in the vicinity of Woodcrest Street.",
+        "The following events were reported: Thunderstorm Wind. These occurred near station USW00013722, approximately 29.3183 km away, between 2023-08-27 19:10:00 and 2023-08-27 19:10:00. 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 25000.0 and crop damage of 0.0. \n\nEpisode Narrative: A weak stationary front and upper disturbance interacted with a very moist and unstable air mass to result in scattered showers and storms across central North Carolina in the afternoon and evening. A tree fell on a house in Chatham County, and flash flooding was reported in Albemarle.\nEvent Narrative: A tree was reported down on a house along Windstone Road near Village Way.",
+        "The following events were reported: Flash Flood. These occurred near station USW00013722, approximately 46.7719 km away, between 2023-08-29 20:15:00 and 2023-08-29 20:15:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: A stalled front interacted with a moist and unstable air mass to result in showers and storms across central North Carolina. There were several reports of flash flooding in Stanly and Franklin counties during the evening. A stalled front interacted with a moist and unstable air mass to result in showers and storms across central North Carolina. There were several reports of flash flooding in Stanly and Franklin counties during the evening.\nEvent Narrative: Bennette Perry Road was closed near Springfield Lane due to flooding. Flash flooding was reported on North Carolina Highway 39 at Louisburg Road.",
+        "The following events were reported: Hail, Thunderstorm Wind. These occurred near station USW00013722, approximately 18.9376 km away, between 2023-09-08 14:45:00 and 2023-09-08 15:53:00. The events included records with hailstones measuring 43.4 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 trough over the southern Appalachians combined with a surface trough over the eastern Piedmont and an inland penetrating sea breeze to produce scattered showers and thunderstorms over the eastern Sandhills, Coastal Plain, and eastern Piedmont. Several of the storms produced damaging winds and hail along and east of the US-1 Corridor. An upper-level trough over the southern Appalachians combined with a surface trough over the eastern Piedmont and an inland penetrating sea breeze to produce scattered showers and thunderstorms over the eastern Sandhills, Coastal Plain, and eastern Piedmont. Several of the storms produced damaging winds and hail along and east of the US-1 Corridor. An upper-level trough over the southern Appalachians combined with a surface trough over the eastern Piedmont and an inland penetrating sea breeze to produce scattered showers and thunderstorms over the eastern Sandhills, Coastal Plain, and eastern Piedmont. Several of the storms produced damaging winds and hail along and east of the US-1 Corridor. An upper-level trough over the southern Appalachians combined with a surface trough over the eastern Piedmont and an inland penetrating sea breeze to produce scattered showers and thunderstorms over the eastern Sandhills, Coastal Plain, and eastern Piedmont. Several of the storms produced damaging winds and hail along and east of the US-1 Corridor. An upper-level trough over the southern Appalachians combined with a surface trough over the eastern Piedmont and an inland penetrating sea breeze to produce scattered showers and thunderstorms over the eastern Sandhills, Coastal Plain, and eastern Piedmont. Several of the storms produced damaging winds and hail along and east of the US-1 Corridor.\nEvent Narrative: Power outages were reported due to fallen trees on power equipment near the intersection of Dwight Rowland Road and Kennebec Road. Power outages were reported due to fallen trees on power lines near the intersection of Holloman Road and Page Road.   Trees were down at Oakland Avenue and Englewood Avenue.",
+        "The following events were reported: Flash Flood, Thunderstorm Wind. These occurred near station USW00013722, approximately 14.1147 km away, between 2023-09-09 09:10:00 and 2023-09-09 16:10:00.Thankfully, no injuries or fatalities were reported. No significant property or crop damage was reported. \n\nEpisode Narrative: An upper-level trough over the Tennessee valley and a stalled frontal boundary over western North Carolina and Virginia combined with a surface trough over the Coastal Plain of central North Carolina brought several rounds of showers and thunderstorms. Flash flooding and damaging winds were reported in Wake, Halifax, and Forsyth counties. An upper-level trough over the Tennessee valley and a stalled frontal boundary over western North Carolina and Virginia combined with a surface trough over the Coastal Plain of central North Carolina brought several rounds of showers and thunderstorms. Flash flooding and damaging winds were reported in Wake, Halifax, and Forsyth counties. An upper-level trough over the Tennessee valley and a stalled frontal boundary over western North Carolina and Virginia combined with a surface trough over the Coastal Plain of central North Carolina brought several rounds of showers and thunderstorms. Flash flooding and damaging winds were reported in Wake, Halifax, and Forsyth counties. An upper-level trough over the Tennessee valley and a stalled frontal boundary over western North Carolina and Virginia combined with a surface trough over the Coastal Plain of central North Carolina brought several rounds of showers and thunderstorms. Flash flooding and damaging winds were reported in Wake, Halifax, and Forsyth counties. An upper-level trough over the Tennessee valley and a stalled frontal boundary over western North Carolina and Virginia combined with a surface trough over the Coastal Plain of central North Carolina brought several rounds of showers and thunderstorms. Flash flooding and damaging winds were reported in Wake, Halifax, and Forsyth counties. An upper-level trough over the Tennessee valley and a stalled frontal boundary over western North Carolina and Virginia combined with a surface trough over the Coastal Plain of central North Carolina brought several rounds of showers and thunderstorms. Flash flooding and damaging winds were reported in Wake, Halifax, and Forsyth counties.\nEvent Narrative: Flooding was reported along US Highway 1 at Walnut St. Flooding was reported near the intersection of Walker St and Walnut St. The city of Raleigh reported flooding along Hillsborough St at Western under the railroad. The Crabtree creek greenway in Morrisville reached minor flood stage. The flood stage peaked at 9.45 feet. The Walnut creek gage along southeast Maynard Rd in Cary reached minor flood stage, peaking at 3.72 feet. One tree was reported down near the intersection of Tody Goodwin Rd and New Hill Olive Chapel Rd in Apex.",
+        "The following events were reported: Flash Flood, Heavy Rain. These occurred near station USW00013722, approximately 18.4456 km away, between 2023-09-23 11:25:00 and 2023-09-23 17:00:00.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: Tropical Storm Ophelia made landfall across southeastern North Carolina. Ophelia tracked north-northwest into the northern Coastal Plain of central North Carolina by midday, then into eastern Virginia by the early evening hours. Widespread rainfall to the north and west of Ophelia led to numerous flash flood reports in Wake, Wilson, and Halifax Counties during the morning and early afternoon hours. Tropical Storm Ophelia made landfall across southeastern North Carolina. Ophelia tracked north-northwest into the northern Coastal Plain of central North Carolina by midday, then into eastern Virginia by the early evening hours. Widespread rainfall to the north and west of Ophelia led to numerous flash flood reports in Wake, Wilson, and Halifax Counties during the morning and early afternoon hours. Tropical Storm Ophelia made landfall across southeastern North Carolina. Ophelia tracked north-northwest into the northern Coastal Plain of central North Carolina by midday, then into eastern Virginia by the early evening hours. Widespread rainfall to the north and west of Ophelia led to numerous flash flood reports in Wake, Wilson, and Halifax Counties during the morning and early afternoon hours. Tropical Storm Ophelia made landfall across southeastern North Carolina. Ophelia tracked north-northwest into the northern Coastal Plain of central North Carolina by midday, then into eastern Virginia by the early evening hours. Widespread rainfall to the north and west of Ophelia led to numerous flash flood reports in Wake, Wilson, and Halifax Counties during the morning and early afternoon hours. Tropical Storm Ophelia made landfall across southeastern North Carolina. Ophelia tracked north-northwest into the northern Coastal Plain of central North Carolina by midday, then into eastern Virginia by the early evening hours. Widespread rainfall to the north and west of Ophelia led to numerous flash flood reports in Wake, Wilson, and Halifax Counties during the morning and early afternoon hours. Tropical Storm Ophelia made landfall across southeastern North Carolina. Ophelia tracked north-northwest into the northern Coastal Plain of central North Carolina by midday, then into eastern Virginia by the early evening hours. Widespread rainfall to the north and west of Ophelia led to numerous flash flood reports in Wake, Wilson, and Halifax Counties during the morning and early afternoon hours. Tropical Storm Ophelia made landfall across southeastern North Carolina. Ophelia tracked north-northwest into the northern Coastal Plain of central North Carolina by midday, then into eastern Virginia by the early evening hours. Widespread rainfall to the north and west of Ophelia led to numerous flash flood reports in Wake, Wilson, and Halifax Counties during the morning and early afternoon hours. Tropical Storm Ophelia made landfall across southeastern North Carolina. Ophelia tracked north-northwest into the northern Coastal Plain of central North Carolina by midday, then into eastern Virginia by the early evening hours. Widespread rainfall to the north and west of Ophelia led to numerous flash flood reports in Wake, Wilson, and Halifax Counties during the morning and early afternoon hours.\nEvent Narrative: Floodwaters were on the road at Wake Forest Road and Bland Road, making it passable only in one lane. Floodwaters resulted in a road closure and stranded cars at United States Highway 401 and Fox Road. Floodwaters caused a road closure at Poole Road and Barwell Road. Flooding was reported at Lynn Road and Grove Barton Road. One lane was open, but the rest were closed. A total rainfall of 3.66 inches was measured in Raleigh. A total rainfall of 3.64 inches was measured in Garner. A total rainfall of 3.54 inches was measured at Garner. A total rainfall of 3.48 inches was measured at the Lake Wheeler Road Field Lab ECONet station in Raleigh.",
+        "The following events were reported: Thunderstorm Wind, Tornado. These occurred near station USW00013722, approximately 16.8129 km away, between 2023-12-10 12:28:00 and 2023-12-10 15:38:00.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 strong upper level trough and cold front moved across the Carolinas, triggering multiple rounds of showers and thunderstorms. A cluster of stronger storms moved northeast across the eastern North Carolina Piedmont, producing a Tornado in Wake County and damaging winds across the northeast Piedmont and Coastal Plain. A strong upper level trough and cold front moved across the Carolinas, triggering multiple rounds of showers and thunderstorms. A cluster of stronger storms moved northeast across the eastern North Carolina Piedmont, producing a Tornado in Wake County and damaging winds across the northeast Piedmont and Coastal Plain.\nEvent Narrative: Trees and powerlines were reported down near the intersection of Glen Forest Dr and Tanglewood Dr. An EF-1 tornado touched down near Old Stage Road at approximately 12:28 PM EST. The tornado was on the ground for 4 minutes and tracked east-northeastward for approximately 1.9 miles before lifting near United States Highway 70 along 7th Avenue.|Most of the damage was associated with snapped and uprooted trees, and some subsequent building damage due to trees falling on several structures. There we no injuries or fatalities.",
+        "The following events were reported: Flood. These occurred near station USW00013722, approximately 20.3488 km away, between 2023-12-17 17:00:00 and 2023-12-17 21:30:00. 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 intense area of low pressure developed in the northeastern Gulf of Mexico and then moved northeast along and near the Carolina coastline before moving off the Virginia Capes and into the western Atlantic. This storm system dumped an average of 2 to 5 inches of rain across central North Carolina over a 12 to 18 hour period that resulted in areas of flash flooding and eventual river flooding. In addition, a burst of strong wind gusts spread across the Sandhills and southern Piedmont producing area of wind damage and an isolated cluster of thunderstorms produced damaging winds in the southern Coastal Plain. An intense area of low pressure developed in the northeastern Gulf of Mexico and then moved northeast along and near the Carolina coastline before moving off the Virginia Capes and into the western Atlantic. This storm system dumped an average of 2 to 5 inches of rain across central North Carolina over a 12 to 18 hour period that resulted in areas of flash flooding and eventual river flooding. In addition, a burst of strong wind gusts spread across the Sandhills and southern Piedmont producing area of wind damage and an isolated cluster of thunderstorms produced damaging winds in the southern Coastal Plain.\nEvent Narrative: Rose Lane at Walnut Creek was closed due to flooding. Flooding was reported at the intersection of Capital Blvd and Calvary Dr."
+    ]
+}
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