| 青藏高原近地面层微气象学特征 |
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| 引用本文： | Liu Huizhi,Zhang Hongsheng,Bian Lin＇gen,Chen Jiayi,Zhou Mingyu,Xu Xiangde,Li Shiming,Zhao Yijun.青藏高原近地面层微气象学特征[J].大气科学进展,2002,19(1):73-88. |
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| 作者姓名： | Liu Huizhi Zhang Hongsheng Bian Lin＇gen Chen Jiayi Zhou Mingyu Xu Xiangde Li Shiming Zhao Yijun |
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| 作者单位： | Liu Huizhi 1，Zhang Hongsheng 2，Bian Lingen 3 Chen Jiayi 2. Zhou Mingyu 4，Xu Xiangde 3 Li Shiming4 and Zhao Yijun 1 1LAPC，Institute of Atmospheric Physics，Chinese Academy of Sciences，Beijing 100029 2 Department of Geophysics，Peking University，Beiji |
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| 基金项目： | This study was supported by the NKBRSF 61999043404 and the Program TIPEX. and partly supported by the Program KZCX2-204 of the C |
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| 摘 要： | 利用1998年5月-7月在改则、当雄和昌都三测站获得的近地面层气象要素变化的观测资料，分析了青藏高原近地面层风速、温度和湿度日变化特征及廓线规律，发现高原近地面层微气象学特征具有自己的特点；同时还讨论了高原近地面层白天出现的逆湿现象。
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| 关 键 词： | 气象要素日变化 廓线 青藏高原 近地面层 风速 温度 湿度 |
| 收稿时间： | 26 February 2001 |
Characteristics of micrometeorology in the surface layer in the Tibetan Plateau |
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| Liu?Huizhi,Zhang?Hongsheng,Bian?Lin’gen,Chen?Jiayi,Zhou?Mingyu,Xu?Xiangde,Li?Shiming,Zhao?Yijun.Characteristics of micrometeorology in the surface layer in the Tibetan Plateau[J].Advances in Atmospheric Sciences,2002,19(1):73-88. |
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| Authors: | Liu Huizhi Zhang Hongsheng Bian Lin’gen Chen Jiayi Zhou Mingyu Xu Xiangde Li Shiming Zhao Yijun |
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| Institution: | 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 |
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| 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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| Keywords: | Diurnal variation of meteorological element Vertical profile Tibetan Plateau |
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