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影响"05.06.25"长江流域暴雨的西南低涡特征
引用本文:王晓芳,廖移山,闵爱荣,崔春光.影响"05.06.25"长江流域暴雨的西南低涡特征[J].高原气象,2007,26(1):197-205.
作者姓名:王晓芳  廖移山  闵爱荣  崔春光
作者单位:中国气象局,武汉暴雨研究所,湖北,武汉,430074
基金项目:湖北省自然科学基金 , 中国气象局武汉暴雨研究所资助项目
摘    要:利用NCEP逐日再分析值资料,分析了影响2005年6月25日长江流域暴雨过程的西南低涡结构特征及其移动发展机制。结果表明:25日移出川东影响长江中游的西南低涡是一个显著不对称的斜压系统,其发展过程中始终伴随着强盛的西南低空急流;低涡移动过程中非地转平衡性很强,高层正涡度平流和低层暖平流的共同作用,是低涡移动过程中周围大气维持较大的非热成风涡度,从而造成低涡区域上空强上升运动的重要原因。

关 键 词:西南涡  低空急流  非地转平衡  非热成风涡度
文章编号:1000-0534(2007)01-0197-09
修稿时间:2006-03-132006-07-25

Characteristics of Southwest Vortex of Influencing "05.06.25" Yangtze River Rainstorm
WANG Xiao-fang,LIAO Yi-shan,MIN Ai-rong,CUI Chun-guang.Characteristics of Southwest Vortex of Influencing "05.06.25" Yangtze River Rainstorm[J].Plateau Meteorology,2007,26(1):197-205.
Authors:WANG Xiao-fang  LIAO Yi-shan  MIN Ai-rong  CUI Chun-guang
Institution:Wuhan Institute of Heavy Rain, China Meteorological Administration, Wuhan 430074, China
Abstract:Using the NCEP reanalysed daily data,we analysed the structure and developing mechanism of the southwest low vortex affecting the heavy rain along the Yangtze River valley on 25 June,2005.The results indicated that the southwest low vortex was a prominent baroclinic system,and there was keeping the strong southwest lower jet in the southeast position of the moving low vortex.There were non-geostrophic balance in the low vortex area,the effects of the vorticity advection in upper level and the temperature advection in low level were the importance reason of maintaining the big non-thermal-wind vorticity,so caused strong ascending motion in the area of the low vortex.
Keywords:Southwest vortex  Lower layer jet  Non-geostrophic balance  Non-thermal-wind vorticity
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