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梅雨锋暴雨的Doppler雷达观测研究:中尺度对流回波系统的结构和特征
引用本文:杜秉玉,陈钟荣,张卫青.梅雨锋暴雨的Doppler雷达观测研究:中尺度对流回波系统的结构和特征[J].南京气象学院学报,1999(1).
作者姓名:杜秉玉  陈钟荣  张卫青
作者单位:南京气象学院电子信息科学系,南京气象学院计算机科学与技术系
摘    要:详细分析了1991年7月9日发生在江淮地区的一次梅雨锋大暴雨过程,研究了梅雨锋中尺度对流回波系统的形态、结构以及与它相伴随的中尺度天气系统,提出了梅雨锋内弱的低层辐合下暴雨对流回波的中尺度回波增强区(MEER)概念,并与台湾地区中尺度试验(TAMEX)中的梅雨锋暴雨研究结果作了比较

关 键 词:梅雨锋  暴雨  中尺度结构

A STUDY OF MEIYU FRONT STORM WITH DOPPLER RADAR OBSERVATIONS: STRUCTURE AND FEATURES OF A MESOSCALE CONVECTIVE ECHO SYSTEM
DU Bing yu,CHEN Zhong rong.A STUDY OF MEIYU FRONT STORM WITH DOPPLER RADAR OBSERVATIONS: STRUCTURE AND FEATURES OF A MESOSCALE CONVECTIVE ECHO SYSTEM[J].Journal of Nanjing Institute of Meteorology,1999(1).
Authors:DU Bing yu  CHEN Zhong rong
Abstract:The Meiyu frontal storm occurred on July 9, 1991 in the Jianghuai region has been analyzed in detail. The structure and features of the mesoscale convective echo system of the Meiyu front and the associated mesoscale weather systems have been studied. The concept of the mesoscale echo enhancing region in the convective storm region under the condition of weak low level convergence within the Meiyu front has been suggested. The results are compared with those from TAMEX in Taiwan.
Keywords:Meiyu front  heavy rain  mesoscale structure
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