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襄阳一次强雷暴过程的雷达回波与地闪特征分析

Radar echoes and cloud-to-ground lightning characteristics of a strong thunderstorm in Xiangyang

  • 摘要: 利用湖北省闪电定位仪、新一代天气雷达资料并结合常规气象观测等资料,对2011 年7 月24 日下午出现在湖北襄阳的一次强雷暴天气过程进行了分析。该过程的两个强风暴分别产生了冰雹和雷雨大风(后期强降水),重点分析了两个强风暴系统生命期雷达回波和闪电(地闪)特征。结果表明: 产生冰雹的强风暴是一个孤立的超级单体,降雹发生在超级单体成熟阶段;产生雷雨大风和强降水的强风暴是一个弓状回波,雷雨大风发生在弓状回波顶部,强降水回波成片状且移速较慢;两个风暴的地闪演变特征及闪电在风暴生命史各阶段分布的位置不同。

     

    Abstract: Based on lightning monitoring and warning network, Doppler radar data and conventional meteorological observational data, the strong thunderstorm occurred in Xiangyang, Hubei province on 24 July 2011 is analyzed. Two strong storms of the thunderstorm process produced hail and thunderstorm gale (later heavy precipitation happened) respectively, and the emphasis is on the analysis of radar echoes and cloud-to-ground lightning characteristics during their lifetimes. The results show that the strong storm which produced hail is an isolated supercell, and the hail happened in the maturity stage of the supercell. The strong storm generating thunderstorm gale and heavy precipitation isa bow echo. The thunderstorm gale happened at the top of the echo, and the heavy precipitation echo is flaky and its moving speed is slow. The cloud-to-ground lighting develpment characteristics and lightning distributing locations of the two thunderstorms are different in each stage of life history.

     

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