暴雨灾害2024,Vol.43Issue(3) :332-341.DOI:10.12406/byzh.2023-165

南岭地区一次高架雷暴冰雹过程双偏振特征分析

Dual polarization characteristics of an elevated thunderstorm hail event in the Nanling region

袁韬 唐明晖 陈伟 冯盼盼 杨湘婧 汤宇
暴雨灾害2024,Vol.43Issue(3) :332-341.DOI:10.12406/byzh.2023-165

南岭地区一次高架雷暴冰雹过程双偏振特征分析

Dual polarization characteristics of an elevated thunderstorm hail event in the Nanling region

袁韬 1唐明晖 2陈伟 3冯盼盼 4杨湘婧 3汤宇5
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作者信息

  • 1. 湖南省郴州市气象局,郴州 423000;气象防灾减灾湖南重点实验室,长沙 410118
  • 2. 湖南省气象台,长沙 410118;气象防灾减灾湖南重点实验室,长沙 410118
  • 3. 湖南省郴州市气象局,郴州 423000
  • 4. 湖南省湘西自治州气象局,吉首 416000
  • 5. 湖南省气象灾害防御技术中心,长沙 410053
  • 折叠

摘要

2023年3月22-23日南岭地区郴州发生了一次高架雷暴冰雹过程,降雹范围广、冰雹直径达20mm,在高架对流中鲜见.为增强对此类冰雹过程的预报预警能力,利用常规气象观测数据、SA波段双偏振雷达产品,对此次过程的天气形势、双偏振雷达回波特征进行分析,结果表明:(1)此次过程发生在地面锋线北侧冷区内,属于典型的高架雷暴,降雹落区位于地面锋面北侧140 km处,20 mm直径大冰雹由超级单体风暴造成.(2)导致郴州南部出现大冰雹的风暴可分为初生、发展跃增、降雹、减弱消亡阶段.风暴发展跃增阶段的强回波中心迅速增高且垂直累积液态水含量(VIL)跃增,差分反射率因子(ZDR)柱伸至0℃层以上4~5 km,上升气流强劲,有利于冰雹发展;降雹阶段强回波中心迅速降低,弱回波区(WER)消失,ZDR柱高度明显下降,下降融化的冰雹表现为ZDR和差分传播相移率(KDP)向着地面方向逐渐增大,KDP足位置与降雹落区对应较好.(3)大冰雹的三体散射(TBSS)特征表现为根部ZDR值较大,随着径向距离增加,ZDR值迅速减小,相关系数(CC)明显偏低;大冰雹的旁瓣回波特征表现为低ZDR、低CC,以上双偏振特征为大冰雹预警的关键关注点.

Abstract

An elevated thunderstorm hail event occurred in Chenzhou and its vicinity in the Nanling region during March 22-23,2023.A wide range of hail with diameters reaching up to 20 mm was reported,which was rare in elevated convection.In order to enhance the capabili-ty of forecasting and early warning of such hail events,this paper uses conventional meteorological observation data and SA-band dual-polar-ization radar products to analyze its weather conditions and dual-polarization radar echo characteristics.The results are as follows.(1)This event occurred in the cold area on the north side of the surface front,which was a typical elevated thunderstorm process.The hail-falling ar-ea was located 140 km to the north side of the surface front,and the large hail of 20 mm in diameter was caused by a supercell storm.(2)The storms that caused large hail in southern Chenzhou can be divided into four stages,which are the initial stage,the rapid development stage,the hail-falling stage,and the weakening stage.During the rapid development stage,the strong echo center increases rapidly and the vertical cumulative liquid water content(VIL)increases sharply.The differential reflectivity(ZDR)column extends to 4~5km above the 0 ℃ layer.A stronger updraft provides favorable conditions for hail development.During the hail-falling stage,with the rapid decrease of the strong echo center,the weak echo region(WER)disappears,and the height of the ZDR column decreases significantly.The values of ZDR and specific dif-ferential phase(KDR)gradually increase as the melting hail falls toward the ground.While the footprints of KDR correspond well with the hail-falling region.(3)The three-body scattering(TBSS)characteristics of large hail showed that the ZDR value at the root was large,which then decreased rapidly with the increase of radial distance,and the cross-correlation coefficient(CC)was significantly low.The sidelobal echo features of large hail indicate a low ZDR and low CC signature.These dual polarization features are key concerns for the large hail warning.

关键词

高架雷暴/双偏振雷达/南岭/三体散射/ZDR柱

Key words

elevated thunderstorm/dual polarization radar/Nanling region/TBSS/ZDR column

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基金项目

湖南省自然科学基金重大项目(2021JC0009)

湖南省气象局重点课题(2022)(XQKJ22A003)

出版年

2024
暴雨灾害
中国气象局武汉暴雨研究所

暴雨灾害

CSTPCD
影响因子:1.533
ISSN:1004-9045
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