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《Plateau Meteorology》 2006-04
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Diagnostic Analysis of a Heavy Snowstorm Processe in Lower Latitude Plateau of China

ZHANG Teng-fei~1, LU Ya-bin~2, ZHANG Jie~2, PU Gui-ming~2(1.Yunnan Lightning Study and Protection Center,Kunming 650034,China;2.Meteorological Observatoryof Yunnan Province,Kunming 650034,China)  
Using the conventional meteorological data,the various variable fields,the satellite and the Doppler radar echo images,the heavy snow process on February 7,2004 has been analyzed.The results show when the Xinjiang upper trough oriented in NE-SW direction changes its orientation into N-S direction and moves eastward,the cold air from the north diffuses continually southward,accumulates and intensifies in the boundaries among Sichuan,Guizhou and Yunnan,makes the Kunmin stationary front to intensify,move westward and affect the mid-Yunnan province.Meanwhile the satellite images also show that the cloud area of the southern brauch trough in India intensies,moves eastward and merges with the forementioned strong stationary front cloud area,so the moderat-heavy snow storm occur in mid- and east-Yunnan.Because of the function of the relief,there is light rain in west Yunnan mostly.Southwest wind enhancement,water vapour flux increase,ascending motion enhancement and water vapour convergence in upper level arouse the heavy snow process in central and east Yunnan.In the meantime the cold and warm advections and the southwest jet in upper level are the main characters of the heavy snow in the Doppler radar velocity fields.This further substantiates that the water vapor condition brought by southwest airflow is very important to snowfall in lower latitude plateau.
【Fund】: 云南省“十五”攻关项目(2001NG43);; 云南省气象局2003年青年基金项目共同资助
【CateGory Index】: P426.634
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