Possible maintaining mechanism of cl

Possible maintaining mechanism of climatological atmospheric quasi-biweekly oscillation around Sumatra

There are convective activities over the maritime continent during a whole year, especially over Sumatra, a vigorous center of convection due to the blocking of the surface topography[1]. Many researchers have pointed out that the first commencement of the monsoonal convection over Indo-China peninsula is the result of the northward propagation of tropical convection over Sumatra along the "land bridge"[2-5], emphasizing the importance of the convective activities over Sumatra in the process of Asian summer monsoon (ASM) onset.

作 者： WEN Min ZHANG Renhe   作者单位： State Key Laboratory of Severe Weather, Chinese Academy of Meteorological Sciences, Beijing 100081, China  刊 名： 科学通报（英文版）  SCI 英文刊名： CHINESE SCIENCE BULLETIN  年，卷(期)： 2005 50(10)  分类号： P4  关键词：  

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