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Determination of the Drag Coefficient over the Tibetan Plateau
作者姓名:Li Guoping  Duan Tingyang  Wan Jun  Gong Yuanf  Shigenori Haginoy  Chen Longxun  Li Weiliang
作者单位:Chengdu Institute of Meteorology,Chengdu 610041,Chengdu Institute of Meteorology,Chengdu 610041,Chengdu Institute of Meteorology,Chengdu 610041,Chengdu Institute of Meteorology,Chengdu 610041,Meteorological Research Institute,Japan Meteorological Agency,Chinese Academy of Meteorological Sciences,Beijing 100081,Chinese Academy of Meteorological Sciences,Beijing 100081
摘    要:In this paper,a preliminary study is given on the drag (i.e.bulk transfer for momentum) coefficient,on the basis of data from four sets of AWS in Tibet during the first observational year from July 1993 to July 1994 according to China Japan Asian Monsoon Cooperative Research Program.The results show that the drag coefficient over the Tibetan Plateau is 3.3 to 4.4×103.In addition,monthly and diurnal variations of drag coefficient and the relationship among the drag coefficients and the bulk Richardson number,surface roughness length and wind speed at 10 m height are discussed in detail.


Determination of the Drag Coefficient over the Tibetan Plateau
Li Guoping,Duan Tingyang,Wan Jun,Gong Yuanf,Shigenori Haginoy,Chen Longxun,Li Weiliang.Determination of the Drag Coefficient over the Tibetan Plateau[J].Advances in Atmospheric Sciences,1996,13(4):511-518.
Authors:Li Guoping  Duan Tingyang  Wan Jun  Gong Yuanfa  Shigenori Haginoya  Chen Longxun  Li Weiliang
Institution:Chengdu Institute of Meteorology, Chengdu 610041,Chengdu Institute of Meteorology, Chengdu 610041,Chengdu Institute of Meteorology, Chengdu 610041,Chengdu Institute of Meteorology, Chengdu 610041,Meteorological Research Institute, Japan Meteorological Agency,Chinese Academy of Meteorological Sciences, Beijing 100081,Chinese Academy of Meteorological Sciences, Beijing 100081
Abstract:In this paper, a preliminary study is given on the drag (i.e. bulk transfer for momentum) coefficient, on the basis of data from four sets of AWS in Tibet during the first observational year from July 1993 to July 1994 according to China-Japan Asian Monsoon Cooperative Research Program. The results show that the drag coefficient over the Tibetan Plateau is 3.3 to 4.4 × 10-3. In addition, monthly and diurnal variations of drag coefficient and the relation-ship among the drag coefficients and the bulk Richardson number, surface roughness length and wind speed at 10 m height are discussed in detail.
Keywords:Drag coefficient  Roughness length  Bulk Richardson number  Similarity formulation
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