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贵州南部一次突发性大暴雨的中尺度分析
引用本文:毛冬艳,钱传海,乔林,陈涛,吴秋霞.贵州南部一次突发性大暴雨的中尺度分析[J].南京气象学院学报,2007,30(5):601-609.
作者姓名:毛冬艳  钱传海  乔林  陈涛  吴秋霞
作者单位:1. 国家气象中心,北京,100081
2. 中国气象科学研究院,灾害天气国家重点实验室,北京,100081
基金项目:国家自然科学基金 , 科技部社会公益研究项目
摘    要:利用地面加密观测资料、贵州自动站雨量资料、FY-2C卫星红外辐射亮度温度(tbb)资料等,对2006年6月12日夜间贵州南部突发性大暴雨过程进行了中尺度分析.结果表明:具有类似于MCC(Mesoscale Convective Complex)特征的中尺度对流云团的发生发展及其缓慢东移是造成此次大暴雨的直接原因.对流层中低层大量的水汽输送和对流有效位能的积累为大暴雨的形成提供了有利的环境条件,中高层弱冷空气入侵使偏南暖湿气流被迫抬升、地面中尺度低压和辐合线的形成是暴雨发生的可能触发机制.中尺度天气系统具有低层辐合、高层辐散的高、低空配置,暴雨区南、北两侧的正、反垂直环流构成了中尺度次级环流圈的垂直结构特征.

关 键 词:突发性大暴雨  中尺度分析  中尺度对流复合体  贵州  南部  突发性大暴雨  中尺度分析  South  of  Guizhou  Heavy  Rain  Analysis  结构特征  次级环流  构成  垂直环流  雨区  配置  高层辐散  低层辐合  中尺度天气系统  机制  触发  辐合线  中尺度低压
文章编号:1000-2022(2007)05-0601-09
修稿时间:2006-10-10

Mesoscale Analysis of a Heavy Rain in the South of Guizhou
MAO Dong-yan,QIAN Chuan-hai,QIAO Lin,CHEN Tao,WU Qiu-xia.Mesoscale Analysis of a Heavy Rain in the South of Guizhou[J].Journal of Nanjing Institute of Meteorology,2007,30(5):601-609.
Authors:MAO Dong-yan  QIAN Chuan-hai  QIAO Lin  CHEN Tao  WU Qiu-xia
Institution:1. National Meteorological Center,Beijing 100081 ,China; 2. State Key Laboratory of Severe Weather,Chinese Academy of Meteorological Sciences,Beijing 100081 ,China
Abstract:A mesoscale analysis for the heavy rain at night on 12 June 2006 in Guizhou Province is performed using the surface intensified observation,rainfall of automatic weather stations,FY-2C satellite tbb,etc.Results indicate that the mesoscale convective cloud clusters and their slowly moving are the direct reason for the heavy rain.Rich water vapour transport and the accumulation of CAPE(Convective Available Potential Energy) in the mid-and low-levels provide the favorable environmental conditions for the occurrence of the heavy rain,which is probably triggered by the lifting of warm and humid airflow forced by the intrusion of weak cold air from high-and mid-levels,and the formation of mesoscale low and mesoscale convergence line.Mesoscale weather systems have the features of convergence in the low level and divergence in the high level and the vertical structure of mesoscale secondary circulations.
Keywords:heavy rain  mesoscale analysis  mesoscale convective complex
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