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Vertical profiles of the horizontal wind speed and of the standard deviationof vertical wind speed from Large Eddy Simulations of a convectiveatmospheric boundary layer are compared to wind LIDAR measurements up to1400 m. Fair agreement regarding both types of profiles is observed onlywhen the simulated flow is driven by a both time- and height-dependentgeostrophic wind and a time-dependent surface heat flux. This underlines theimportance of mesoscale effects when the flow above the atmospheric surfacelayer is simulated with a computational fluid dynamics model

Comparison of Large Eddy Simulations of a convective boundary layer with wind LIDAR measurements