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广西南宁一次"龙舟水"暴雨空报事件对流生消成因分析

周琰 翟丽萍 张丁丁 樊盛 黄卓帆 李渝平 李紫甜 潘杰丽 黄增俊

气象2024,Vol.50Issue(8):941-952,12.
气象2024,Vol.50Issue(8):941-952,12.DOI:10.7519/j.issn.1000-0526.2024.071001

广西南宁一次"龙舟水"暴雨空报事件对流生消成因分析

Causes for Convection Generation and Dissipation in an Unsuccessful"Dragon Boat Water"Rainstorm Prediction Event in Nanning of Guangxi

周琰 1翟丽萍 2张丁丁 1樊盛 2黄卓帆 1李渝平 1李紫甜 1潘杰丽 1黄增俊3

作者信息

  • 1. 南宁市气象局,南宁 530029
  • 2. 广西壮族自治区气象台,南宁 530022
  • 3. 广西南宁市邕宁区气象局,邕宁 530200
  • 折叠

摘要

Abstract

On June 13,2022,a large-scale regional rainstorm event occurred in Guangxi.During this period,a rainstorm false alarm was issued for the downtown area of Nanning.The echo attenuated in the north side of Nanning City,maintained in the east side and developed in the south side,which made the process com-plicated.This article investigates the causes for the generation and dissipation of the convection during this event by utilizing various observational data and ERA5 reanalysis data.The results are as follows.The circulation background of this process was the typical heavy rainfall circulation and ambient condition in the first rainy season in Guangxi.However,under the combined influence of synoptic-scale cold advection and storm cold pool,the cold air quickly moved over Nanning City,and the outflow boundary formed by the storm in the north side of Nanning moved away from the storm parent body.Meanwhile,the low-level wa-ter vapor transport in the front of the storm moved eastward,resulting in poor thermodynamic and dynam-ic conditions,leading to the attenuation and dissipation of echoes in the north side of Nanning City.In the east side of Nanning City,the outflow boundary of the storm was next to the storm parent body during its advancing,and the lower layer ahead of the storm kept the southwest jet stream so that the storm was strengthened or sustained by continuous convective cells triggered along the outflow boundary.There was a low-level high temperature and high humidity environment in the south side of Nanning,which was con-ducive to the reconstruction or enhancement of convective available potential energy.Based on the above,a conceptual model of the evolution mechanism of convection generation and dissipation in this process has been built,and with it,the short-time and nowcasting forecasts can be supplemented and corrected by ana-lyzing the evolution of cold pool,outflow boundary and ambient conditions.

关键词

暴雨空报/对流生消/冷平流/冷池/出流边界

Key words

rainstorm false alarm/convection generation and dissipation/cold advection/cold pool/out-flow boundary

分类

天文与地球科学

引用本文复制引用

周琰,翟丽萍,张丁丁,樊盛,黄卓帆,李渝平,李紫甜,潘杰丽,黄增俊..广西南宁一次"龙舟水"暴雨空报事件对流生消成因分析[J].气象,2024,50(8):941-952,12.

基金项目

中国气象局复盘总结专项项目(FPZJ2024-098)、广西气象科研计划指令性项目(桂气科2023ZL08、桂气科2024ZL08)、广西气象科研计划面上项目(桂气科2023M15)和广西气象科研计划青年人才培养项目(桂气科2023QN09)共同资助 (FPZJ2024-098)

气象

OA北大核心CSTPCD

1000-0526

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