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Jiang Jixi;Xiang Xukang;Fan Meizhu(National Satellite Meteorological Center, Beijing 100081 )  
By using GMS-4 hourly IR stretched digital data from June through August 1991, all293 severe Mesoscale Convective Systems (s-MCSs) Over Tibetan Plateau were investigatedand analysed. The results show that those s-MCSs had larger frequency and more typicalfeatures of meso-β scale system in its life cycle, size and intensity ; their initiation and development was mainly derived from the thermotopographic effect; their movement basicallyconsorted with the mean flow between 300 and 200 hpa, and few of them moved away fromTibetan Plateau.
【Fund】: 高原试验研究预研项目
【CateGory Index】: P432.1
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