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闵颖, 孙绩华, 王曼, 朱莉, 王治国, 杨倩媛. 2022: 静止锋东退背景下云南文山“4.28”局地强风暴过程分析. 暴雨灾害, 41(2): 151-157. DOI: 10.3969/j.issn.1004-9045.2022.02.005
引用本文: 闵颖, 孙绩华, 王曼, 朱莉, 王治国, 杨倩媛. 2022: 静止锋东退背景下云南文山“4.28”局地强风暴过程分析. 暴雨灾害, 41(2): 151-157. DOI: 10.3969/j.issn.1004-9045.2022.02.005
MIN Ying, SUN Jihua, WANG Man, ZHU Li, WANG Zhiguo, YANG Qianyuan. 2022: Analysis of"4.28"sever local storm caused stationary front of Wenshan in Yunnan Province. Torrential Rain and Disasters, 41(2): 151-157. DOI: 10.3969/j.issn.1004-9045.2022.02.005
Citation: MIN Ying, SUN Jihua, WANG Man, ZHU Li, WANG Zhiguo, YANG Qianyuan. 2022: Analysis of"4.28"sever local storm caused stationary front of Wenshan in Yunnan Province. Torrential Rain and Disasters, 41(2): 151-157. DOI: 10.3969/j.issn.1004-9045.2022.02.005

静止锋东退背景下云南文山“4.28”局地强风暴过程分析

Analysis of"4.28"sever local storm caused stationary front of Wenshan in Yunnan Province

  • 摘要: 利用常规观测资料、ERA5资料、加密自动站资料、卫星云图资料和天气雷达资料,对2021年4月28日午后出现在文山市的一次局地强风暴过程进行分析。结果表明:(1) 此次过程发生在静止锋东退减弱和副热带高压西进北抬的天气尺度背景下,中等以上强度垂直风切变、层结不稳定和大的对流有效位能为风暴的发生提供了有利的环境条件。(2) 静止锋形成的地面辐合线与地形的共同作用触发对流生成,雷暴高压出流边界与环境风形成的地面辐合线对风暴的加强有重要作用。(3) 局地强风暴过程是由单单体风暴产生的:雷达回波具有倾斜结构、前侧“V”型缺口、旁瓣回波、反射率因子质心快速下降以及VIL值跃增等特征,这些特征对监测和预警冰雹有一定的指示作用。

     

    Abstract: Based on data from conventional observations, ERA5, intensive automatic weather stations, satellite cloud images and weather radar, a sever local storm in Wenshan on 28 April 2021 was analyzed. The results are as follows. (1) This event took place under the synoptic condition of the weaken stationary front and the strong subtropical high. Several factors, such as moderate vertical wind shear, unstable stratification and large convective available potential energy, provided favorable environmental conditions for the occurrence of storm. (2) The combined action of the surface convergence line formed by the stationary front and terrain triggered the generation of convection. The ground convergence line formed by outflow boundary of thunderstorm high and ambient wind played an important role in strengthening the storm. (3) The severe local storm was caused by single-cell storm. Radar echoes had characteristics of inclined structure, hook echo, sidelobe echo, rapid declines of the core of reflectivity factor and jumped VIL. The characteristics had a certain indication in monitoring and warning of hail.

     

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