Spectral code setup for a stratified Ekman boundary layer. The solver is parallelized in the spanwise direction. The time marching is performed using a third-order RK method. The spatial derivatives are performed using second-order central finite differences in the vertical direction and with a pseudo-spectral method in the horizontal directions.
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Spectral code to solve a stratified Ekman boundary layer. A canonical setup to study atmospheric turbulence where the influence of the Earth rotation and the nocturnal surface cooling is included.
jortizta/ekman_bl
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Spectral code to solve a stratified Ekman boundary layer. A canonical setup to study atmospheric turbulence where the influence of the Earth rotation and the nocturnal surface cooling is included.
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