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气象:2008,34(10):50-59
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一次中-β尺度局地大暴雨对流系统的雷达回波特征
(福建省龙岩市气象局, 364000)
CINRAD Radar Echo Features of a Mesoscale-β Local Heavy Rainfall Convective System
(Longyan Meteorological Office, Fujian Province 364000)
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投稿时间:2008-03-05    修订日期:2008-04-30
中文摘要: 利用新一代天气雷达产品对2006年6月18日永定一次中-β尺度大暴雨对流系统的雷达回波 特征进行分析,探讨短时大暴雨的回波特征。结果表明:有利的大尺度环流、充足的水汽条 件和较强的上升运动是产生强降水有利的天气背景。新一代天气雷达资料分析表明,强降 水是由局地发展的对流回波加强合并产生的;中低层冷平流的入侵触发了强对流的产生,对 流单体有明显的典型的液态强降水系统特征;逆风区及良好的垂直运动使对流单体发展加强 ,强降水区域尺度较大,与回波移向一致产生“列车效应”,同时系统移动较慢,导致了强 降水的持续。
中文关键词: 液态强降水  逆风区  列车效应
Abstract:Radar echo feature of a heavy rainfall event is discussed on the basis of analyz ing NEXRAD products during the mesoscale -β heavy rainfall convective system e vent in June 18th, 2006 occurred in Yongding City. Conclusion is drawn as follow s: large scale circulation, ample water vapor and stronger ascending movement ar e advantageous weather background of severe rainfall. The results of show that severe rainfall is led by local convective echoes strengthening a nd integrating; lower middle layer cold advection triggers the strong convectio n. And convective cells show typical features of severe precipitation system. Co nverse wind region and good vertical movement strengthens the development of con vective cells. The server larger scale rainfall area moves along the same direc tion as echoes do, which cause so called “train domino effect". Furthermore, s ystem moves slowly, which helps severe rainfall continue.
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冯晋勤,童以长,罗小金,2008.一次中-β尺度局地大暴雨对流系统的雷达回波特征[J].气象,34(10):50-59.
Feng Jinqin,Tong Yichang,Luo Xiaojin,2008.CINRAD Radar Echo Features of a Mesoscale-β Local Heavy Rainfall Convective System[J].Meteor Mon,34(10):50-59.