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Characteristics of Micrometeorology in the Surface Layer in the Tibetan Plateau


doi: 10.1007/s00376-002-0035-7

  • The data of the meteorological elements in the surface layer have been analyzed which were obtained during the IOP of TIPEX fiom May to July 1998 in Gerze, Damxung and Qamdo. The characteristics of the diurnal variations and the vertical profiles of the wind velocity, temperature and humidity in the surface layer have been investigated. Some interesting results have been obtained. The moisture inversion phenomena occured during the daytime in the surface layer have also been discussed.
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Manuscript History

Manuscript received: 10 January 2002
Manuscript revised: 10 January 2002
通讯作者: 陈斌, bchen63@163.com
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Characteristics of Micrometeorology in the Surface Layer in the Tibetan Plateau

  • 1. LAPC, Institute of Atmospheric Ph ysies, Chinese Academy of Sciences, Beijing 100029,Department ofGeophysics, Peking University, Beijing 100871,Chinese Aeademy of Meteorological Sciences, Beijing 100081,Department ofGeophysics, Peking University, Beijing 100871,The National Center of Marine Environmental Forecast, Beijing 100081,Chinese Aeademy of Meteorological Sciences, Beijing 100081,The National Center of Marine Environmental Forecast, Beijing 100081,LAPC, Institute of Atmospheric Ph ysies, Chinese Academy of Sciences, Beijing 100029

Abstract: The data of the meteorological elements in the surface layer have been analyzed which were obtained during the IOP of TIPEX fiom May to July 1998 in Gerze, Damxung and Qamdo. The characteristics of the diurnal variations and the vertical profiles of the wind velocity, temperature and humidity in the surface layer have been investigated. Some interesting results have been obtained. The moisture inversion phenomena occured during the daytime in the surface layer have also been discussed.

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