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鹰潭一次雷暴大风"天衍"雷达产品特征分析

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文章利用MICAPS天气图资料、地面自动气象站资料和"天衍"雷达拼图等资料,采用天气图、统计方法、回波图像、回波廓线等分析方法,对2024-03-25鹰潭雷暴大风天气过程进行分析.结果表明:"3.25"鹰潭雷暴大风天气过程是由500 hPa高空槽、850 hPa切变线、850hPa急流及地面冷锋共同作用造成的;强对流回波在地面冷锋东移南压的过程中被触发,并沿着地面冷锋的移动方向移动;飑线形强对流回波造成鹰潭出现大片雷暴大风,由于回波移动较快,影响时间短,此次过程未造成鹰潭出现强降水.这次过程提示在预警预报中要时刻紧盯上游实况及对流回波移向,为雷暴大风天气的预报预警增加提前量.
Analysis of the characteristics of"Tianyan"radar product for a thunderstorm in Yingtan
This paper uses MICAPS weather map data,ground automatic meteorological station data,and"Tianyan"radar mosaic data,and uses analysis methods such as weather map analysis,statistical methods,echo images,and echo profiles to analyze the process of the 2024-03-25 Yingtan thunderstorm.The results show that the process of the"3.25"Yingtan thunderstorm is caused by the combined action of a 500 hPa high trough,850 hPa shear line,850 hPa jet stream,and a ground cold front.The strong convective echo was triggered during the process of the ground cold front moving eastward and southward,and moved along the direction of the ground cold front movement.The squall shaped strong convective echo caused a large area of thunderstorms in Yingtan.Due to the fast movement of the echo and the short impact time,this process did not cause heavy precipitation in Yingtan.This process reminds us to always keep an eye on the upstream situation and the direction of convective echoes in early warning and forecasting,in order to increase the amount of advance for forecast ans early waring of thunderstorms and strong winds.

Yingtanthunderstorms"Tianyan"radar mosaic productecho characteristics

刘强

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鹰潭市气象局,鹰潭 335001

鹰潭 雷暴大风 "天衍"雷达拼图产品 回波特征

国家自然科学基金面上项目吉安市生态气象重点实验室江西省气象局青年人才科研项目

419750012021JEM211JX2022Q01

2024

气象水文海洋仪器
中国仪器仪表学会 气象水文海洋仪器分会 长春气象仪器研究所

气象水文海洋仪器

影响因子:0.307
ISSN:1006-009X
年,卷(期):2024.41(3)