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深圳市前汛期西风带大暴雨天气形势特征
引用本文:谢小敏,王明洁,胡娟.深圳市前汛期西风带大暴雨天气形势特征[J].广东气象,2010,32(3):9-11,16.
作者姓名:谢小敏  王明洁  胡娟
作者单位:深圳市气象局,广东深圳,518001
摘    要:对1978~2008年深圳市前汛期西风带大暴雨期间的500、850 hPa和地面环流形势进行统计分析,发现深圳市前汛期大暴雨过程多由西风带系统引起,占总数的77%。4~6月均可出现大暴雨,6月份最多,4月份次多,5月份最少。深圳前汛期西风带系统大暴雨过程按天气形势特征分为锋面低槽和暖区两类,其中锋面低槽类又分东北低涡(低槽)型和西南低涡型。

关 键 词:气候学  前汛期西风带  大暴雨  深圳市

Characteristics Analysis of Synoptic Situation on Heavy Rainstorms induced by Westerlies in First Flood Season in Shenzhen
XIE Xiao-min,WANG Ming-jie,HU Juan.Characteristics Analysis of Synoptic Situation on Heavy Rainstorms induced by Westerlies in First Flood Season in Shenzhen[J].Journal of Guangdong Meteorology,2010,32(3):9-11,16.
Authors:XIE Xiao-min  WANG Ming-jie  HU Juan
Institution:(Shenzhen meteorological bureau, Shenzhen 518001, China)
Abstract:Through statistical analysis on the weather situation at the levels of 500hPa,850hPa and ground during heavy rainstorm events in first flood season of Shenzhen from 1978 to 2008 ,it is revealed that 77% heavy rainstorms were induced by weather systems in westerly belt in first flood season in Shenzhen. Heavy rainstorms can occur from April to June,in which June take the largest proportion, then April followed by May. Heavy rainstorm processes can be classified as Type frontal trough and Type warm -sector vortex, and Type frontal trough can be further divided into northeast vortex (trough) and southeast vortex.
Keywords:climatology  westerly belt in first flood season  heavy rainstorm  shenzhen
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