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《Chinese Journal of Atmospheric Sciences》 1992-01
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The Expressions for the Wind Profiles of Free Convective and Stable Boundary Layers and the Pumping Velocity at the Top of the Planetary Boundary Layer

Zhao Ming(Department of Atmospheric Sciences, Nanjing University, Nanjing, 210008)  
Based on recent studies of the turbulent transfer in free convective and stable boundary lay -ers , analytic expressions for wind profiles in these two cases are obtained , the profiles and boundary layer parameters are in agreement with observational characteristics . Furthermore, the analytic expressions for the pumping velocity at the top of the PBL and their relations to some parameters are also derived . The results show that the pumping velocity is connected with stratification and may be explained physically.
【Fund】: 国家自然科学基金
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【Co-citations】
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1 Zhao Ming(Department of Atmospheric Sciences, Nanjing University, Nanjing 210008);Effects of Boundary Layer Characteristic Parameters on the Vertical Velocity at the Top of Planetary Boundary Layer[J];Chinese Journal of Atmospheric Sciences;1994-04
2 Zhao Ming (Department of Atmospheric Sciences,Nanjing University,Nanjing 210093);A PBL Numerical Model Considering the Effects of Background Wind and Pressure Fields[J];SCIENTIA ATMOSPHERICA SINICA;1997-02
3 LI XING-SHENG (Academy of Meteorological Science, SMA, Beijing 100081, PRC)TANG CHENG-XIAN AND XU XIAO-JIN(Beijing Institute of Meteorology, Beijing 100081, PRC);A PARAMETERIZED STUDY ON THE LOCAL SIMILARITY THEORY IN THE STABLE BOUNDARY LAYER MODEL[J];中国科学B辑(英文版);1991-09
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1 ZHANG Qiang~{1, 2}, WANG Sheng~1 (1. Gansu Province Key Labortory of Arid Climate Change and Reducing Disaster, Institute of Arid Meteorology, China Meteorological Administration, Lanzhou Gansu 730020, China; 2. Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou Gansu 730000, China);Comparison of Atmospheric Characteristics of Near-Surface Layer between Oasis and Desert Background in Summer[J];Journal of Glaciology and Geocryology;2005-02
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