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2010年吉林省3次暴雪天气对比分析和落区探讨
引用本文:魏婷婷,郭维,刘晓东.2010年吉林省3次暴雪天气对比分析和落区探讨[J].安徽农业科学,2010,38(29):16347-16352.
作者姓名:魏婷婷  郭维  刘晓东
作者单位:1. 吉林省四平市气象台,吉林四平,136000
2. 吉林省气象局,吉林长春,130062
摘    要:利用NCEP再分析资料结合Micaps资料,对吉林省2010年冬末春初的3次区域性暴雪天气过程的形成机理及落区进行了对比分析。结果表明:3次暴雪过程均发生在有利的大尺度环流背景下,过程1为冷锋型暴雪;过程2为倒槽北上型暴雪;过程3为回流型暴雪。暴雪在吉林省的落区与系统来向、地形作用、水汽与动力大值中心重合区域、湿舌以及θse高能舌等都具有一定关系。

关 键 词:暴雪  形成机理  急流  回流

Comparative Analysis and Falling Area Study of Three Snow Storms in Jilin Province in 2010
WEI Ting-ting et al.Comparative Analysis and Falling Area Study of Three Snow Storms in Jilin Province in 2010[J].Journal of Anhui Agricultural Sciences,2010,38(29):16347-16352.
Authors:WEI Ting-ting
Institution:WEI Ting-ting et al(Siping Meteorological station,Sipiug,Jilin 136000)
Abstract:Based on NCEP reanalysis data and Micaps data,the formation mechanism and falling area of the three regional snow storms which occurred by the end of winter and the beginning of spring in 2010 in Jilin Province was comparatively analyzed.The results showed that the three snow storms were occurred in the favorable large-scale circulation background.Process one was classified as cold front type.Process two was classified as northward inverted trough type.Process three was classified as returnning flow type.Th...
Keywords:Snow storm  Formation mechanism  Jet current  Returning flow  
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