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东莞一次强对流天气的X波段相控阵雷达特征

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利用X波段相控阵雷达等资料分析了 2023年4月21日在广州南部和东莞发生的一次混合型强对流天气过程,结果发现:(1)该过程由海上北抬的暖式切变线触发,具有低空暖平流强迫和中等垂直风切变等有利条件,导致冰雹、短时强降水、下击暴流等强对流现象;(2)雷达观测到雨雹混合物具有高基本反射率、低差分反射率、低相关系数等特征;(3)雷达捕捉到普通降雹单体风暴,其CC谷和ZDR柱反映了暖湿气流在前侧抬升到过冷冻层形成大冰晶,在中心附近下降时融化成大雨滴或外包水膜的雨雹混合物;(4)降水的拖曳作用和冰雹融化下降导致了下击暴流的形成,雷达显示了近地层的辐散速度对特征;(5)相控阵雷达能监测到下击暴流形成前雷暴的反射率因子核和风暴顶高度下降等变化特征.
Characteristics of an X-band Phased Array Radar for a Severe Convective Weather in Dongguan
The data of an X-band phased array radar was used to analyze the process of a mixed-type severe convective weather that took place in southern Guangzhou and Dongguan on April 21,2023.The re-sults are shown as follows.(1)Triggered by a warm shear moving north from the sea,the weather of interest had favorable conditions of low-level warm advection forcing and moderate vertical wind shear,causing se-vere convection of hails,short-range intense rains and downbursts.(2)As detected by the radar,the mix-ture of rain and hail was characterized by high basic reflectivity,low differential reflectivity and low correla-tion coefficient.(3)The radar captured an ordinary hail cell storm,whose CC valley and ZDR column reflec-ted that warm and humid air currents lifted at the front edge to the super-cooled layer to form large-sized ice crystals,which descended near the storm center and melted to large-sized rain droplets or a mixture of rain and hail that was covered by a film of water.(4)For the formation of the downbursts,which resulted from the dragging effect of rain and the descent of melting hail,the radar displayed the features of diverging veloc-ity pairs at the near-surface layer.(5)The phased array radar was able to observe such pre-downburst varia-tions as the core of the storm reflectivity factor and the descent of storm top height.

synopticsphased array radarhaildownburstshort-range intense rainDongguan

冼星河、蔡奕萍、李婵珠、张玮

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东莞市气象局,广东东莞 523000

天气学 相控阵雷达 冰雹 下击暴流 短时强降水 东莞市

广东省气象局科研项目

GRMC2021Q20

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(4)