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一次由海风锋激发的下击暴流天气过程分析

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利用珠海市地面自动站观测资料、MICAPS资料和横琴X波段双偏振相控阵雷达资料,对珠海市一次由海风锋激发的下击暴流天气过程进行分析,结果表明:(1)该次下击暴流过程发生前,大气层结呈现"上干下湿"结构,温度垂直递减率大,CAPE大,环境条件有利于雷雨大风天气发生;(2)该次伴随下击暴流的强对流系统主要由珠海东部沿岸形成的海风锋触发,并伴有中气旋出现;(3)下击暴流发生前,处于低层反射率大值期,X波段相控雷达可以清晰观测到强反射率因子下降、中层径向速度辐合、近地面气流辐散等现象.
Analysis of a Downburst Process Triggered by a Sea Breeze Front
Using the data of surface automatic weather stations in Zhuhai,MICAPS and an X-band du-al-polarization phased-array radar at Hengqin,Zhuhai,this paper analyzed a weather process of downburst triggered by a sea breeze front.The results are shown as follows.1)Prior to the downburst,the atmosphere was structured such that it was dry in the upper level but moist in the low level,with large vertical gradients of temperature and CAPE and favorable environmental conditions for thunderstorms to take place.2)A se-vere convective system accompanying this downburst was mainly triggered by a sea breeze front formed over the eastern coast of Zhuhai and a mesocyclone was also present.3)Before the onset of the downburst,the lower level of the atmosphere was in the period of large reflectivity such that the X-band dual-polarization phased-array radar clearly captured the falling of strong reflectivity factor,the convergence of mid-level ra-dial velocity and the divergence of near-surface airflows.

synopticsdownburstsea breeze frontmesocycloneX-band dual-polarization phased-ar-ray radar

王世强、黄菲、詹棠、张金清、李伟明

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珠海市公共气象服务中心,广东珠海 519000

珠海市国家观象台,广东珠海 519000

天气学 下击暴流 海风锋 中气旋 相控阵雷达

广东省气象局科学技术研究面上项目

GRMC2019M47

2024

广东气象
广东省气象学会

广东气象

影响因子:1.013
ISSN:1007-6190
年,卷(期):2024.46(1)
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