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《Chinese Journal of Atmospheric Sciences》 2004-01
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Heavy Rainfalls in South China and Related Circulation during HUAMEX Period

Chen Hong, and Zhao Sixiong (Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029)  
During HUAMEX period of 1998, six heavy rainfalls occurred in South China. In this paper, diagnostic study and numerical simulation have been conducted. The conclusions are the followings: 1)The heavy rainfalls during HUAMEX period were the result of the interaction between middle and lower latitude systems. Except the influence of tropical summer monsoon, cold air from middle and higher latitudes also played an important role in the rainfall. 2)The eight rainfall processes were related with the activity of fronts. In each case, the front corresponds to the frontogenetical area, the heavy rainfall occurred near the front or during front passage or in the warm sector ahead of front. 3)Computations showed that, Q 1 and Q 2 contributed significantly to these rainfall processes at the area of South China, and the convective condensation heating resulted from columns convection also played an important role in rainfall. 4)Heavy rainfalls in South China associated closely with monsoon circulation. During pre-rainy season in 1998, the southwest current associated with South China Sea monsoon moved northwards several times, rainfall processes had a direct relationship with these activities. 5)The moisture source areas of these rainfall processes have been analyzed; it should be noticed that not only the Bay of Bengal, but also the South China Sea and the West Pacific were the important moisture source areas. 6)The analysis of the cloud systems indicated that the meso-β scale convective cloud clusters provided very favorable conditions to the occurrence of heavy rainfall.
【Fund】: 国家重点基础研究规划项目G1 9980 40 90 8;; 国家科技部攀登专项 95 专 0 3;; 国家自然科学基金资助项目4973 5 1 80资助
【CateGory Index】: P458.121.1
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