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气象:2026,52(9):1066-1078
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一次左移超级单体的双偏振雷达观测分析
彭恩翔,俞小鼎,钱学成,陈娟,张帆,孙素琴
(江西省吉安市气象局,吉安 343000; 气候变化风险与气象灾害防御江西省重点实验室,南昌 330096; 中国气象局气象干部培训学院,北京 100081; 江西省气象台,南昌 330096; 江西省赣州市气象局,赣州 341000)
Analysis of Dual-Polarization Radar Observation of a Left-Moving Supercell
PENG Enxiang,YU Xiaoding,QIAN Xuecheng,CHEN Juan,ZHANG Fan,SUN Suqin
(Ji’an Meteorological Office of Jiangxi Province, Ji’an 343000; Key Laboratory of Climate Change Risk and Meteorological Disaster Prevention of Jiangxi Province, Nanchang 330096; CMA Training Centre, Beijing 100081; Jiangxi Meteorological Observatory, Nanchang 330096; Ganzhou Meteorological Office of Jiangxi Province, Ganzhou 341000)
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投稿时间:2025-08-24    修订日期:2026-07-09
中文摘要: 2021年5月10日午后,江西中北部发生了一次罕见的由风暴分裂产生的左移超级单体过程。本文利用吉安CINRAD/SC双偏振雷达、高空与地面观测以及ERA5再分析资料,对此次过程的环境条件、风暴结构特征和动力机制进行了分析。结果表明:该左移超级单体形成于强对流有效位能(>3000 J·kg-1)和0~6 km强垂直风切变(>20 m·s-1)环境中,3.0~4.9 km垂直风切变矢量随高度逆时针旋转产生显著负水平涡度,是左移超级单体选择性加强的关键环境因素。成熟阶段风暴中高层呈现“双涡旋”结构,其中中层中反气旋对应前侧强上升气流区,中气旋位于后侧并与前侧下沉气流区(FFD)相伴,整体与经典右移风暴呈近似镜像对称。双偏振参量显示,风暴低层差分反射率因子(ZDR)大值区与强垂直风切变引起的粒子分选机制相关;中层ZDR环和ZDR柱分别指示中反气旋的强旋转和强上升运动。中反气旋的形成机制源于负水平涡度在强上升气流作用下倾斜为负垂直涡度;风暴左移则与FFD位置、南北涡旋强度差异引起的Magnus效应密切相关。本研究为深入理解中国地区左移超级单体的发生发展机制、风暴结构特征和微物理特征提供了参考。
Abstract:A rare left-moving supercell generated by storm splitting occurred in central and northern Jiangxi Province from 14:00 BT to 18:00 BT 10 May 2021. Using dual-polarization radar data from the Ji’an CINRAD/SC radar, upper-air and surface observations and ERA5 reanalysis data, this paper analyzes the environmental conditions, structural characteristics, and dynamic mechanisms of this event. The results show that the left-moving supercell was generated in an environment with high convective available potential energy (>3000 J·kg-1) and strong 0-6 km vertical wind shear (>20 m·s-1). The vertical wind shear vector of 3.0-4.9 km exhibited counterclockwise rotation with height, generating significant negative horizontal vorticity, which was a key factor for the selective intensification of the left-moving supercell. During its mature stage, the storm displayed a “dual-vortex” structure at mid-to-upper levels, with a mesoanticyclone located in the leading (northern) sector corresponding to a strong updraft, and a mesocyclone in the trailing (southern) sector associated with the forward-flank downdraft (FFD). Its overall appearance was approximately mirror-symmetrical to the structure of classic right-moving supercell. Dual-polarization parameters demonstrate that the large differential reflectivity factor (ZDR) zone in the lower levels was related to particle sorting under strong vertical wind shear, while the ZDR ring and ZDR column at mid-levels indicated strong rotation and updraft within the meso-anticyclone, respectively. The formation of the mesoanticyclone was attributed to the tilting of negative horizontal vorticity into negative vertical vorticity by the robust updraft. The leftward motion of the storm was closely related to the location of FFD and the Magnus effect resulting from the pressure gradient force induced by the asymmetry between the northern and southern vortices. This study provides a valuable case for understanding the development, structure, and microphysical characteristics of left-moving supercells in China.
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基金项目:中国气象局气象能力提升联合研究专项(23NLTSZ004)、江西省气象局气象科研项目(JX2022Y05、JX2022M11和JX2024RCM03)和吉安市生态气象重点实验室项目(2022JEM201)共同资助
引用文本:
彭恩翔,俞小鼎,钱学成,陈娟,张帆,孙素琴,2026.一次左移超级单体的双偏振雷达观测分析[J].气象,52(9):1066-1078.
PENG Enxiang,YU Xiaoding,QIAN Xuecheng,CHEN Juan,ZHANG Fan,SUN Suqin,2026.Analysis of Dual-Polarization Radar Observation of a Left-Moving Supercell[J].Meteor Mon,52(9):1066-1078.