%0 Journal Article
%T The Observational Analysis of Atmospheric Boundary Layer Structure in East Part and Downstream of Tibetan Plateau<br>青藏高原东部及下游地区冬季边界层的观测分析
%A JIANG Xing-wen
%A LI Yue-qing
%A WANG Xin
%A ZHAO Xing-bing
%A HE Guang-bi
%A <br>蒋兴文
%A 李跃清
%A 王鑫
%A 赵兴炳
%A 何光碧
%J 高原气象
%D 2009
%I 
%X The atmospheric boundary layer(ABL) structure in east part and downstream of Tibetan Plateau(TP) was investigated utilizing the intensifying radiosonde data in December 2007.The results indicate that there is a surface-based temperature inversion layer(SBTIL) with an average heights of 500 m at nighttime,and a mixed layer(ML) with the heights of 2000 m in east part of TP in winter.The water vapor and wind speed were well mixed in the ML,and there is a deeply humidity inversion layer(HIL) when the ML was mat...
%K Tibetan Plateau
%K Sichuan basin
%K Atmospheric boundary layer
%K Inversion layer<br>青藏高原
%K 四川盆地
%K 边界层
%K 逆温层
%U http://www.alljournals.cn/get_abstract_url.aspx?pcid=E62459D214FD64A3C8082E4ED1ABABED5711027BBBDDD35B&cid=28A2F569B2458C17&jid=FCD959CAD9EF92C38C4323B51D54F3DB&aid=BED69DC80EB6E798B0CC056BABB1A5E2&yid=DE12191FBD62783C&vid=D3E34374A0D77D7F&iid=E158A972A605785F&sid=9409F3EB075DCD5B&eid=1CBB73E9593E8833&journal_id=1000-0534&journal_name=高原气象&referenced_num=3&reference_num=23