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桂林一次强下击暴流成因分析
引用本文:李彩玲,蔡康龙,黄先香,植江玲,陈志芳,麦文强. 桂林一次强下击暴流成因分析[J]. 气象, 2021, 47(2): 242-252
作者姓名:李彩玲  蔡康龙  黄先香  植江玲  陈志芳  麦文强
作者单位:广东省佛山市气象局/佛山市龙卷风研究中心,佛山528315;广东省佛山市气象局/佛山市龙卷风研究中心,佛山528315;中国气象科学研究院灾害天气国家重点实验室,北京100081
基金项目:广东省科技厅社会发展科技协同创新体系建设专项(2019B020208015);灾害天气国家重点实验室开放课题(2020LASW-A03,2018LASW-B18);佛山市气象局科技项目(201906)共同资助。
摘    要:2019年3月21日广西桂林市临桂区发生一次极端大风天气过程(以下简称"3·21"临桂大风),当日21:13临桂观测站记录最大阵风风速为60.3 m·s-1(17级).通过风灾现场调查判断这是强度为EF2级的微下击暴流过程.应用常规观测资料以及加密自动气象站、探空、多普勒雷达等资料,分析了"3·21"临桂大风的环流背景...

关 键 词:下击暴流  低层径向速度辐散  中层径向辐合  中气旋  下降的反射率因子核心

Cause Analysis of a Severe Downburst in Guilin
LI Cailing,CAI Kanglong,HUANG Xianxiang,ZHI Jiangling,CHEN Zhifang,MAI Wenqiang. Cause Analysis of a Severe Downburst in Guilin[J]. Meteorological Monthly, 2021, 47(2): 242-252
Authors:LI Cailing  CAI Kanglong  HUANG Xianxiang  ZHI Jiangling  CHEN Zhifang  MAI Wenqiang
Affiliation:(Foshan Tornado Research Center/Foshan Meteorological Office of Guangdong Province,Foshan 528315;State Key Laboratory of Severe Weather,Chinese Academy of Meteorological Sciences,Beijing 100081)
Abstract:An extreme gale event,hereinafter referred to as“3.21 Lingui gale event”,occurred in Lingui,Guangxi on 21 March 2019.Maximum gust of 60.3 m·s-1(Grade 17)was recorded at the Lingui Station at 21:13 BT.Based on the results of the wind damage survey with video and meteorological data,this paper shows that the serious wind damage was caused by a severe microburst.Using the data from conventional meteorological observations,dense automatic weather station,radiosonde,Doppler weather radar,this paper analyzes the environmental conditions and influencing systems of the“3.21 Lingui gale event”.Results are that the“3.21 Lingui gale event”occurred under some favorable conditions such as active low-level warm and humid air flow,mid-level significant dry layer and strong low-level vertical wind shear.The event was triggered by the surface mesoscale convergence line and the southward cold front.The“3.21 Lingui gale event”was caused by the merging of two supercells into one supercell.Before the downburst occurred,the supercell developed to the most powerful stage.The maximum reflectivity core height(HGT)exceeded 6 km.There was a medium intensity of the mesocyclone accompanied by the(mid-altitude radial convergence,MARC)value of 36 m·s-1.When the downbursts occurred,reflectivity factor began to weaken,the height of storm top dropped and HGT dropped.When HGT dropped sharply,the scanned volume interval dropped by 3.5 km,and the extreme gale of Grade 17 occurred.At this time,the low-level 0.5°elevation was observed in the high-altitude area of the cyclone,with a high radial divergence value of 27 m·s-1.The mesocyclone had the strongest wind shear strengthening,the bottom height rapidly dropped to less than 1 km,and so on.In addition,the occurrence of downburst was closely related to the dragging effect of extreme severe precipitation and hail.Usually,when the minutely rainfall is higher than 3 mm,wind force is higher than Grade 12;when the minutely rainfall is higher than 6 mm,the extreme gale of Grade 17 occurs.
Keywords:downburst  low-level radial velocity divergence  mid-altitude radial convergence(MARC)  mesocyclone  drop of reflectivity factor core
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