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《Chinese Journal of Atmospheric Sciences》 2007-06
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An Analysis on the Southwest Vortex and Its Environment Fields during Heavy Rainfall in Eastern Sichuan Province and Chongqing in September 2004

ZHAO Si-Xiong 1 and FU Shen-Ming 1,2 1 Institute of Atmospheric Physics,Chinese Academy of Sciences,Beijing 1000292 Graduate University of Chinese Academy of Sciences,Beijing 100049  
Based on the 6-hour-interval reanalysis data with 1.0°×1.0° resolution from NCEP/NCAR,station observational data and so on,the environment fields and the influencing systems of the heavy rainfall during 2-8 September 2004 are analyzed.The results show that there are 3 stages during the heavy rainfall,and there exist two main rainy influencing systems in the first and third stages,the main rainy influencing system is the low level shear lines;in the second stage,the southwest vortex,which is the low pressure or vortex to the east of the Tibetan Plateau in the lower troposphere,is the main rainy influencing system,and in the second stage,both the precipitation and the range of rainfall reach the maxima.In earlier stage,the southwest vortex is a meso-β-scale system,then it develops,and its diameter reaches 200-500 km,which belongs to the mesoα-scale system.It appears at 0000 UTC 4 September and disappears at 0600 UTC 6 September.It lasts 54 hours.In this paper,the heavy rainfall related to the southwest vortex is studied,and results indicate that the special terrain of eastern Sichuan,the trough at 500 hPa and the vortex at 700 hPa in the lower troposphere could be all favorable conditions contributing to the formation and maintenance of the southwest vortex;there are twenty rainy clusters during the heavy rainfall;it implies that mesoscale system is the direct influencing system;the result of the moisture budget computation shows that the water vapor could come from the low-latitude tropical region.
【Fund】: 国家重点基础研究发展规划项目2004CB418301;; 国家自然科学基金资助项目40405008
【CateGory Index】: P447
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