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桂东南“6.28”大暴雨触发机制分析

黄永森 林宝婷

气象研究与应用2012,Vol.33Issue(1):10-12,I0001,4.
气象研究与应用2012,Vol.33Issue(1):10-12,I0001,4.

桂东南“6.28”大暴雨触发机制分析

Trigger Mechanism of “6.28” Heavy Rain in Southeastern Guangxi

黄永森 1林宝婷1

作者信息

  • 1. 广西玉林市气象局,玉林537000
  • 折叠

摘要

Abstract

Basing the heavy rain on June 27-29 in Yulin City,the dynamic mechanism was analyzed.The results show that: The heavy rain occurs in the strong meridional circulation of two slots and two ridges.The plateau trough moving eastward provides storms a favorable dynamic condition.On 850hpa,the shear line fast moving southward triggers local instability energy releasing.The coupling of low-level strong convergence and high-level strong divergence is conducive to the development of vertical velocity and MCS.The heavy precipitation occurs in the most productive periods of MCS development.

关键词

大暴雨/中尺度对流系统MCS/动力机制

Key words

heavy rain/mesoscale convective systems/dynamic mechanism

分类

天文与地球科学

引用本文复制引用

黄永森,林宝婷..桂东南“6.28”大暴雨触发机制分析[J].气象研究与应用,2012,33(1):10-12,I0001,4.

气象研究与应用

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