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一次中天山暴雨天气的诊断分析
引用本文:刘春风,徐欢,柳宏英,李新燕,周立伟.一次中天山暴雨天气的诊断分析[J].新疆气象,2009,3(4):17-21.
作者姓名:刘春风  徐欢  柳宏英  李新燕  周立伟
作者单位:昌吉州气象局,新疆,昌吉,831100 
基金项目:自治区人影科研(昌吉州人工影响天气作业条件预报、判断和识别技术的研究课题)基金 
摘    要:利用常规气象资料、T213物理量、风云2c红外云图及多普勒雷达探测资料,对2008年7月25日17时-26日08时发生在中天山的暴雨天气过程进行了特征分析。结果表明:此次暴雨过程由天气尺度的冷锋暴雨云团造成,暴雨落区出现在高空西南急流轴南侧,各测站的短时强降水由冷锋暴雨云团中的中尺度雨团所致。

关 键 词:中天山  暴雨  诊断分析

A Diagnostic Analysis of Heavy Rain in Mid-Tianshan Mountain
LIU Chun-feng,XU Huan,LIU Hong-ying,LI Xin-yan and ZHOU Li-wei.A Diagnostic Analysis of Heavy Rain in Mid-Tianshan Mountain[J].Bimonthly of Xinjiang Meteorology,2009,3(4):17-21.
Authors:LIU Chun-feng  XU Huan  LIU Hong-ying  LI Xin-yan and ZHOU Li-wei
Institution:(Changji Meteorological Bureau, Changji 831100, China)
Abstract:In this paper, the evolution of a heavy rain over the Mid-Tianshan Mountain of Xinjiang from 17:00 on 25 July to 08:00 on 26 July 2008 was analyzed by using the observations, T213 simulations, Fengyun-2C infrared images and Doppler radar echo. The result shows that the synoptic scale cold front cloud caused this heavy rain. The heavy rainfall center appeared in the southern of Southwest jet axis. The short-term heavy rainfall in each station was all resulted by mesoscale rain cluster of cold front rain cloud.
Keywords:Mid-Tianshan Mountain  heavy rain  diagnostic analysis
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