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重庆"5·6"强对流过程诊断分析

任思衡 秦牧原 王春明 陈锋立 卢强

安徽农业科学2011,Vol.39Issue(15):9093-9098,9108,7.
安徽农业科学2011,Vol.39Issue(15):9093-9098,9108,7.

重庆"5·6"强对流过程诊断分析

The Diagnosis Analysis of “5·6” Strong Convention in Chongqing

任思衡 1秦牧原 2王春明 3陈锋立 1卢强1

作者信息

  • 1. 解放军理工大学气象学院,江苏南京,211101
  • 2. 96167部队,福建永安,366000
  • 3. 南疆军区气象室,新疆喀什,844200
  • 折叠

摘要

Abstract

One strong convective process occurred in Chongqing province in the morning on May 6. 2010. The strong convective storm caused thundderstorms ,hailstorms and gale.The conventional weather observations, the data of Doppler radar and the 1°x 1°re-analysis data of NCEP were used to analyze the event. the result indcated that the warm tongue at 850 hPa and cold air at 700 hPa were the circulation background of the strong convective storm. The low energy tongue located above high energy tongue caused atmospheric convective instability,the air convergence and rising motion produced by mesoscale occlusion front and low prssure trough at the 975 hPa triggered convective instable enegy released so as to produce strong convective storm; the positive vortex corresponded to the convergence area. The convergence in the lower layer and divergence in the upper layer were conductive to the generation and development of strong convection; there was strong vertical wind shear in 850 - 200 hPa, especially strong vertical shear in the lower and higner layer and mild change in the middle layer, which was conductive to the development and maintenance of strong convection; radar echao analysis suggested that supercell form caused hailstorm in Chongqing.

关键词

强对流/诊断分析/垂直风切变/触发机制/中尺度锢囚锋

Key words

strong convectoion/ Diagnosis analysis/ Vertical wind shear/ Trigger mechanism/ Mesoscale occlusion front

分类

天文与地球科学

引用本文复制引用

任思衡,秦牧原,王春明,陈锋立,卢强..重庆"5·6"强对流过程诊断分析[J].安徽农业科学,2011,39(15):9093-9098,9108,7.

安徽农业科学

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