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@@ -50,13 +50,15 @@ Rayleigh-Bénard convection involves fluid dynamics and thermodynamics, seen in
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  **Equation**:
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  While we solve equations in the frequency domain, the original time-domain problem is
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- ```math
 
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  \begin{align*}
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  \frac{\partial b}{\partial t} - \kappa\,\Delta b & = -u\nabla b\,,
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  \\
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  \frac{\partial u}{\partial t} - \nu\,\Delta u + \nabla p - b \vec{e}_z & = -u \nabla u\,,
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  \end{align*}
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- ```
 
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  where \\(\Delta = \nabla \cdot \nabla\\) is the spatial Laplacian, \\(b\\) is the buoyancy, \\(u = (u_x,u_y)\\) the (horizontal and vertical) velocity, and \\(p\\) is the pressure, \\(\vec{e}_z\\) is the unit vector in the vertical direction, with the additional constraints \\(\int p = 0\\) (pressure gauge).
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  The boundary conditions vertically are as follows:
 
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  **Equation**:
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  While we solve equations in the frequency domain, the original time-domain problem is
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+
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+ $$
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  \begin{align*}
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  \frac{\partial b}{\partial t} - \kappa\,\Delta b & = -u\nabla b\,,
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  \\
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  \frac{\partial u}{\partial t} - \nu\,\Delta u + \nabla p - b \vec{e}_z & = -u \nabla u\,,
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  \end{align*}
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+ $$
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+
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  where \\(\Delta = \nabla \cdot \nabla\\) is the spatial Laplacian, \\(b\\) is the buoyancy, \\(u = (u_x,u_y)\\) the (horizontal and vertical) velocity, and \\(p\\) is the pressure, \\(\vec{e}_z\\) is the unit vector in the vertical direction, with the additional constraints \\(\int p = 0\\) (pressure gauge).
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  The boundary conditions vertically are as follows: