气象与减灾研究2024,Vol.47Issue(3) :173-183.DOI:10.12013/qxyjzyj2024-022

苏南地区一次冷涡背景下的短时强降水成因及中尺度特征

Mechanism and Mesoscale Characteristics of an Extreme Short-Term Heavy Rainfall Event under Cold Vortex Background in Southern Jiangsu

张盛曦 禹梁玉 顾荣直
气象与减灾研究2024,Vol.47Issue(3) :173-183.DOI:10.12013/qxyjzyj2024-022

苏南地区一次冷涡背景下的短时强降水成因及中尺度特征

Mechanism and Mesoscale Characteristics of an Extreme Short-Term Heavy Rainfall Event under Cold Vortex Background in Southern Jiangsu

张盛曦 1禹梁玉 2顾荣直2
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作者信息

  • 1. 宜兴市气象局,江苏无锡 214206
  • 2. 江苏省气象台,江苏南京 210041
  • 折叠

摘要

利用自动站、多普勒天气雷达、风廓线等观测资料以及ERA5再分析资料,对2023年8月17日苏南地区一次冷涡南落背景下的极端短时强降水过程进行分析,揭示其成因机理及中尺度演变特征.结果表明:1)此次极端短时强降水过程属于冷涡后部西北气流型对流天气,快速南下的冷涡及其后部的强盛西北气流为强对流系统的发展提供了不稳定层结条件.2)较高的对流有效位能、较厚的暖云层、近地面层大比湿区是形成极端短时强降水的关键环境因子,超过50 kg/m2的整层大气可降水量、近地面层南北向风向的辐合及东西向风速的辐合共同为强降水的产生提供了水汽和初始动力条件.3)苏南地区存在大陆性强对流型和热带海洋型两种类型的强降水回波,"列车效应"和"合并作用"共同造成了单点极端强降水的"双峰"结构,以及局部地区回波呈现类似超级单体风暴的结构特征.4)强降水发生前,高层北风动量的下传改变了中层的风向和风速,同时近地层东北风速的快速增强,两者的共同作用加大了垂直风切变,使层结的不稳定性增强.

Abstract

Based on data from automatic station,Doppler weather radar,wind profiler,and ERA5 reanalysis data,an extreme short-term heavy rainfall event under the background of a southward-moving cold vortex in southern Jiangsu on August 17,2023 was analyzed,and its formation mechanism and mesoscale evolution characteristics were revealed.The results showed that:1)This extreme short-term heavy rainfall event was classified as convective weather type of the northwest flow in the back of cold vortex,with the cold vortex moving southward rapidly and the strong northwest flow in the back of the vortex providing unstable stratification conditions for the development of convection.2)High Convective Available Potential Energy(CAPE),a thick warm cloud layer,and a large specific humidity area near the surface layer were the key environmental factors for the formation of extreme short-term heavy rainfall.The total precipitable water exceeding 50 kg/m2,along with the wind direction convergence in north-south direction and wind speed convergence in east-west direction near the surface layer jointly provided favorable water vapor and initial dynamic conditions for the generation of heavy rainfall.3)Two types of strong pre-cipitation echoes were observed in southern Jiangsu:continental strong convection and tropical maritime convection.The"train effect"and"merging effect"jointly led to the"double-peak"structure of extreme single-point heavy rainfall,while some local-ized echoes showed characteristics similar to a supcrccll storm structure.4)Prior to the occurrence of heavy rainfall,the down-ward propagation of momentum from the high-level north winds changed the direction and speed of winds in the mid-levels,while the northeast wind speed near the surface increased rapidly.The combined effects of the two factors intensified the verti-cal wind shear,thereby enhancing the instability of stratification.

关键词

短时强降水/冷涡/大气可降水量/成因机理/中尺度演变

Key words

short-term heavy rainfall/cold vortex/total precipitable water/formation mechanism/mesoscale evolution

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出版年

2024
气象与减灾研究
江西省气象学会

气象与减灾研究

影响因子:0.881
ISSN:1007-9033
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