Vertical profiles of the horizontal wind speed and of the standard deviation of vertical wind speed from Large Eddy Simulations of a convective atmospheric boundary layer are compared to wind LIDAR measurements up to 1400 m. Fair agreement regarding both types of profiles is observed only when the simulated flow is driven by a both time- and height-dependent geostrophic wind and a time-dependent surface heat flux. This underlines the importance of mesoscale effects when the flow above the atmospheric surface layer is simulated with a computational fluid dynamics model.
|Journal||Advances in Science and Research|
|Publication status||Published - 2012|
|Event||11th European Meteorological Society Annual Meeting and 10th European Conference on Applications Meteorology - Berlin, Germany|
Duration: 12 Sep 2011 → 16 Sep 2011
|Conference||11th European Meteorological Society Annual Meeting and 10th European Conference on Applications Meteorology|
|Period||12/09/2011 → 16/09/2011|