刘烈霜, 刘贵萍, 刘开宇, 张媛. 一次下击暴流个例的诊断分析〖DM)〗[J]. 云南大学学报(自然科学版), 2012, 34(S1): 33-38.
引用本文: 刘烈霜, 刘贵萍, 刘开宇, 张媛. 一次下击暴流个例的诊断分析〖DM)〗[J]. 云南大学学报(自然科学版), 2012, 34(S1): 33-38.
1.Atmospheric and Oceanic Sciences,Department of Physics,Peking University,Beijing 100871,China; 2.Guizhou Air Traffic Control Bureau of CAAC,Guiyang 550012,China[J]. Journal of Yunnan University: Natural Sciences Edition, 2012, 34(S1): 33-38.
Citation: 1.Atmospheric and Oceanic Sciences,Department of Physics,Peking University,Beijing 100871,China; 2.Guizhou Air Traffic Control Bureau of CAAC,Guiyang 550012,China[J]. Journal of Yunnan University: Natural Sciences Edition, 2012, 34(S1): 33-38.

一次下击暴流个例的诊断分析〖DM)〗

1.Atmospheric and Oceanic Sciences,Department of Physics,Peking University,Beijing 100871,China; 2.Guizhou Air Traffic Control Bureau of CAAC,Guiyang 550012,China

  • 摘要: 通过对2011年10月13日贵阳机场一次突发性大风强降水天气的分析,表明:此次过程是一次明显的小尺度对流单体引起的下击暴流个例.虽无有利的天气尺度影响系统,但地面小尺度辐合触发了过程对流的发展;低层辐合、中高层强辐散产生的大气补偿抽吸效应使得上升运动加强,对流单体发展迅速.但缺少天气尺度系统的动力支持,对流被抑制,单体也快速崩塌,下沉运动出现后迅速占据主导,强烈的下降气流随降水冲击到地面,从而造成下击暴流.

     

    Abstract: By analysing a suddenly strong winds and rainfall weather event which happened on October 13th,2011,Guiyang airport,the results indicated that the process is a clear downburst event.Although no favorable synoptic scale weather systems,but the ground small scale convergence system triggered the development of convection process,strong divergence in the middle to high-level inhibited the development of convective cells' height .Low level convergence,upper level divergence generated effect of atmospheric compensation,and which strengthened the upward motion,convective cells developed rapidly.But lack of support of synoptic scale systems,convection was inhibited,the convective cells collapsed rapidly also.When the strong downdraft with precipitation strike to the ground,then resulted in the downburst.

     

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