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《Chinese Journal of Geophysics》 2002-06
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THE CHARACTERISTICS OF THE PROFILES FOR WIND,TEMPERATURE AND HUMIDITY IN THE BAROCLINIC CONVECTIVE BOUNDARY LAYER ONXIZANG PLATEAU

ZHOU MING-YU 1) QIAN FEN-LAN 1)CHEN ZHI 1) LI SHI-MING SU LI-RONG 1) XU XIANG-DE 2)CHEN LIAN-SHOU 2)LIU JI-CHENG 3)ZHAXI DUNZHU 4) 1) National Center for Marine Environmental Forecasts,Beijing 100081,China2) Chinese Academy of Meteorological Sciences,Beijing 100081,China3) Department of Geophysics,Peking University,Beijing 100871,China4) Tibetan Institute of Meteorological Sciences,Lhasa 850000,China  
The characteristics of the profiles for wind,temperature and humidity in the baroclinic convective boundary layer on Xizang plateau were analyzed and discussed based on the observed data of Damxung boundary layer station and the radiosounding data at Lhasa,Gerze and Wuhan during the second field experiment of atmospheric sciences on Xizang plateau. The results illustrate that the convective boundary layer at daytime on the plateau could be developed strongly with a height of 2200m,which is distinctly higher than that over plain and ocean in middle latitude. The temperature profile in the plateau convective boundary layer has the well mixed characteristics,while the maximum value of humidity appears sometimes at certain level in the humidity profile. The budget analyses of heat and water vapour in the plateau convective boundary layer shows that the horizontal advection has important effect on the structures of boundary layer. There exists the wind shear in the vertical distribution of the average wind speed in the convective boundary layer. The baroclinity formed by the horizontal temperature gradient is the main reason for the formation of the wind shear.
【Fund】: 国家自然科学基金资助项目 (4 0 0 75 0 0 1 );; 国家攀登B项目 (TIPEX);; 国家 973项目 (G1 9990 43 5 0 3 ) .
【CateGory Index】: P434
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