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.
机构:
Chinese Acad Meteorol Sci, State Key Lab Severe Weather, Beijing 100081, Peoples R ChinaChinese Acad Meteorol Sci, State Key Lab Severe Weather, Beijing 100081, Peoples R China
Xu, Hongxiong
Wang, Minzhong
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Chinese Acad Meteorol Sci, State Key Lab Severe Weather, Beijing 100081, Peoples R China
China Meteorol Adm, Inst Desert Meteorol, Urumqi 830002, Peoples R China
Taklimakan Desert Atmospher Environm Observat Exp, Tazhong 841000, Peoples R ChinaChinese Acad Meteorol Sci, State Key Lab Severe Weather, Beijing 100081, Peoples R China
Wang, Minzhong
Wang, Yinjun
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Chinese Acad Meteorol Sci, State Key Lab Severe Weather, Beijing 100081, Peoples R ChinaChinese Acad Meteorol Sci, State Key Lab Severe Weather, Beijing 100081, Peoples R China
Wang, Yinjun
Cai, Wenyue
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Chinese Acad Meteorol Sci, State Key Lab Severe Weather, Beijing 100081, Peoples R China
China Meteorol Adm, Natl Climate Ctr, Beijing 100081, Peoples R ChinaChinese Acad Meteorol Sci, State Key Lab Severe Weather, Beijing 100081, Peoples R China