一次超级单体风暴长时间维持的双偏振特征和机制分析

李海俊 ,  金米娜 ,  徐渊 ,  李婕 ,  周安平 ,  陈娟

暴雨灾害 ›› 2026, Vol. 45 ›› Issue (3) : 361 -372.

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暴雨灾害 ›› 2026, Vol. 45 ›› Issue (3) : 361 -372. DOI: 10.12406/byzh.2025-090

一次超级单体风暴长时间维持的双偏振特征和机制分析

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Analysis of dual-polarization characteristics and mechanisms of a supercell storm with long-term maintenance

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摘要

2025 年 3 月 3 日 00:00 (北京时,下同) 到 07:00,江南北部一个超级单体风暴生命史达 7 h,突出特征是不断发生合并和分裂,厘清这一特征与超级单体风暴长时间维持的关系,有利于提高对长生命超级单体风暴的认识。基于地面和高空观测、双偏振雷达、风廓线雷达等资料,使用 ROSE2.1 和 PyDDA 软件对雷达基数据处理后,结合云桥量化分析其双偏振特征和维持机制,并给出此类风暴天气的预报关注重点。结果表明:(1) 此次超级单体风暴后侧存在短线状风暴并不断向前伸出云桥与超级单体风暴合并,表现为 0 ℃ 层以上差分反射率因子 (ZDR) 柱和差分传播相移率 (KDP) 柱水平宽度加大,且 KDP 柱高度更高。(2) 超级单体风暴合并的同时伴随自上而下迅速分裂,分裂后南部单体承接中气旋,且中气旋半径显著减小,强烈拉伸作用使上升运动突增。(3) 超级单体风暴后侧小单体沿移向的切向合并显著加强了其南侧的上升运动。超级单体风暴南侧分裂出的单体快速发展,替代原超级单体风暴,如此迭代的若干次分裂、合并过程,是其维持长生命史的主要机制。(4) 预报业务中,在强垂直风切变环境下,超级单体风暴后侧有雷暴向前合并,出现云桥,伴随超级单体风暴自身分裂,尤其需关注超级单体风暴长时间维持的可能性。

Abstract

From 00:00 BT to 07:00 BT on March 3, 2025, a supercell in northern Jiangnan persisted for 7 hours, with recurrent merging and splitting as its prominent feature. Elucidating how these behaviors contribute to its prolonged duration can improve the understanding of long-lived supercell storms. Based on surface and upper-air observation data, dual-polarization radar data, and wind profiler radar data, the radar base data were processed using ROSE 2.1 and PyDDA software. The dual-polarization characteristics and maintenance mechanisms of the storm are analyzed quantitatively in combination with cloud bridges. Finally, the key points for forecasting such storm weather are presented. The results are as follows. (1) A short linear storm existed at the rear of the supercell and continuously extended cloud bridges forward to merge with the supercell. This merging process was characterized by an increase in the horizontal width of the differential reflectivity factor (ZDR) column and specific differential phase (KDP) column above the 0 °C level, along with a higher height of the KDP column. (2) Concurrently with the merger, the supercell split rapidly from top to bottom. After splitting, the southern cell inherited the mesocyclone, and the radius of the mesocyclone decreased significantly; the strong stretching effect led to a sudden increase in upward motion. (3) The tangential merger of small cells at the rear of the supercell (along the storm’s moving direction) significantly enhanced the upward motion on the supercell’s southern side. The cells that split from the southern side of the supercell developed rapidly and replaced the original supercell. Such a repeated iterative process of multiple splits and mergers is the main mechanism underlying the supercell’s long lifespan. (4) In operational forecasting, under an environment with strong vertical wind shear, if thunderstorms at the rear of a supercell merge forward with the supercell (accompanied by cloud bridge formation) and the supercell itself splits, special attention should be paid to the possibility of the supercell maintaining for a long duration.

关键词

超级单体风暴 / 中气旋 / 维持机制 / 分裂 / 合并 / 双偏振雷达

Key words

supercell storm / mesocyclone / maintenance mechanism / split / merger / dual-polarization radar

引用本文

引用格式 ▾
李海俊,金米娜,徐渊,李婕,周安平,陈娟. 一次超级单体风暴长时间维持的双偏振特征和机制分析[J]. 暴雨灾害, 2026, 45(3): 361-372 DOI:10.12406/byzh.2025-090

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参考文献

[1]

陈云辉,许爱华,许彬,等. 2019.江西一次极端雷暴大风过程的中尺度特征与成因分析[J].暴雨灾害,38(2):126-134.

[2]

Chen Y H, Xu A H, Xu B, et al. 2019. Analysis on mesoscale characteristics and causes of an extreme thunderstorm gale event in Jiangxi [J].Torrential Rain and Disasters,38(2):126-134 (in Chinese). doi:10.3969/j.issn.1004−9045.2019.02.004

[3]

陈瑞敏,赵孝伟,于海磊,等. 2021.一次长生命史超级单体风暴的雷达观测特征[J].暴雨灾害,40(4):419-429.

[4]

Chen R M, Zhao X W, Yu H L, et al. 2021. Characteristics of a supercell storm with long life cycle based on analysis of weather radar data [J].Torrential Rain and Disasters,40(4):419-429 (in Chinese). doi:10.3969/j.issn.1004−9045.2021.04.010

[5]

戴建华,陶岚,丁杨,等. 2012.一次罕见飑前强降雹超级单体风暴特征分析[J].气象学报,70(4):609-627.

[6]

Dai J H, Tao L, Ding Y, et al. 2012. Case analysis of a large hail-producing severe supercell ahead of a squall line [J].Acta Meteorologica Sinica,70(4):609-627(in Chinese). doi:10.11676/qxxb2012.050

[7]

刁秀广,杨传凤,张骞,等. 2021.二次长寿命超级单体风暴参数与 ZDR 柱演变特征分析[J].高原气象,40(3):580-589.

[8]

Diao X G, Yang C F, Zhang Q, et al. 2021. Analysis on the evolution characteristics of storm parameters and ZDR column for two long life supercells [J].Plateau Meteorology,40(3):580-589 (in Chinese). doi:10.7522/j.issn.1000−0534.2020.00034

[9]

付丹红,郭学良. 2007.积云并合在强对流系统形成中的作用[J].大气科学,31(4):635-644.

[10]

Fu D H, Guo X L. 2007. The role of cumulus merger in a severe mesoscale convective system [J].Chinese Journal of Atmospheric Sciences,31(4):635-644 (in Chinese). doi: 10.3878/j.issn.1006−9895.2007.04.08

[11]

黄勇,冯妍,翟菁. 2016.对流云合并的国内外研究进展[J].暴雨灾害,35(1):91-96.

[12]

Huang Y, Feng Y, Zhai J. 2016. A review of convective cloud merger studies [J].Torrential Rain and Disasters,35(1):91-96 (in Chinese). doi:10.3969/j.issn.1004−9045.2016.01.013

[13]

金米娜,陈云辉,许爱华,等. 2013. 2013 年 3 月 19 日江西省冰雹天气成因分析[J].暴雨灾害,32(2):158-166.

[14]

Jin M N, Chen Y H, Xu A H, et al. 2013. Cause analysis of a hail event occurred in Jiangxi on 19 March 2013 [J].Torrential Rain and Disasters,32(2):158-166 (in Chinese). doi:10.3969/j.issn.1004−9045.2013.02.009

[15]

李海俊,吴静,李婕,等. 2025. ROSE2.1 南昌雷达 2021-2023 年定量降水估测产品检验评估[J].沙漠与绿洲气象,19(3):147-156.

[16]

Li H J, Wu J, Li J, et al. 2025. Assessment of ROSE2.1 quantitative precipitation estimation product from Nanchang radar during 2021 ― 2023 [J].Desert and Oasis Meteorology,19(3):147-156 (in Chinese). doi:10.12057/j.issn.1002−0799.2402.04001

[17]

李淑璠,王秀明,刘屹靖,等. 2025.江西南昌“3.31”极端大风成因分析[J].大气科学,49(3):609-628.

[18]

Li S F, Wang X M, Liu Y J, et al. 2025. Analysis on the causes of the extreme winds on march 31, 2024, in Nanchang, Jiangxi province [J].Chinese Journal of Atmospheric Sciences,49(3):609-628 (in Chinese). doi:10.3878/j.issn.1006−9895.2503.24089

[19]

毛倩,龙凌云,刘埙勋,等. 2024.ROSE2.1 产品在黔东南一次冰雹天气过程中的应用检验[J].山地气象学报,48(4):24-32.

[20]

Mao Q, Long L Y, Liu X X, et al. 2024. Application verification of ROSE2.1 products in hail process in the southeast of Guizhou Province [J].Journal of Mountain Meteorology,48(4):24-32 (in Chinese). doi:10.3969/j.issn.1003−6598.2024.04.004

[21]

唐明晖,陈龙,陈鹤,等. 2023.基于双偏振雷达资料的洞庭湖区一次强对流过程的分阶段特征分析[J].暴雨灾害,42(6):692-703.

[22]

Tang M H, Chen L, Chen H, et al. 2023. Staged characteristics analysis of a severe convection over the Dongting Lake area based on dual-polarization Doppler weather radar data [J].Torrential Rain and Disasters,42(6):692-703 (in Chinese). doi:10.12406/byzh.2022−170

[23]

王秀明,汤欢,俞小鼎,等. 2025.超级单体风暴研究进展[J].气象学报,83(3):813-832.

[24]

Wang X M, Tang H, Yu X D, et al. 2025. Advances in research on supercell storms [J].Acta Meteorologica Sinica,83(3):813-832 (in Chinese). doi:10.11676/qxxb2025.20240156

[25]

王福侠,薛学武,杨吕玉慈,等. 2024.一次长生命史超级单体风暴双偏振参量结构及演变特征[J].气象,50(10):1216-1230.

[26]

Wang F X, Xue X W, Yang L Y C, et al. 2024. Dual-polarization parameter structure and evolution characteristics of a long-life supercell storm [J].Meteorological Monthly,50(10):1216-1230 (in Chinese). doi:10.7519/j.issn.1000−0526.2024.031801

[27]

王福侠,俞小鼎,闫雪瑾. 2014.一次超级单体分裂过程的雷达回波特征分析[J].气象学报,72(1):152-167.

[28]

Wang F X, Yu X D, Yan X J. 2014. Analysis of the splitting processes of the supercell storms based on the Doppler weather radar data [J].Acta Meteorologica Sinica,72(1):152-167 (in Chinese). doi:10.11676/qxxb2014.010

[29]

许爱华,孙继松,许东蓓,等. 2014.中国中东部强对流天气的天气形势分类和基本要素配置特征[J].气象,40(4):400-411.

[30]

Xu A H, Sun J S, Xu D B, et al. 2014. Basic synoptic situation classification and element character of severe convection in China [J].Meteorological Monthly,40(4):400-411 (in Chinese). doi:10.7519/j.issn.1000−0526.2014.04.002

[31]

易笑园,孙晓磊,张义军,等. 2017.雷暴单体合并进行中雷达回波参数演变及闪电活动的特征分析[J].气象学报,75(6):981-995.

[32]

Yi X Y, Sun X L, Zhang Y J, et al. 2017. Evolution of radar parameters and lightning activity during thunderstorm cells merging [J].Acta Meteorologica Sinica,75(6):981-995 (in Chinese). doi:10.11676/qxxb2017.073

[33]

袁韬,唐明晖,陈伟,等. 2024.南岭地区一次高架雷暴冰雹过程双偏振特征分析[J].暴雨灾害,43(3):332-341.

[34]

Yuan T, Tang M H, Chen W, et al. 2024. Dual polarization characteristics of an elevated thunderstorm hail event in the Nanling region [J].Torrential Rain and Disasters,43(3):332-341(in Chinese). doi:10.12406/byzh.2023−165

[35]

俞小鼎,王秀明,李万莉,等. 2020.雷暴与强对流临近预报[M].北京:气象出版社:125-157.

[36]

Yu X D, Wang X M, Li W L, et al. 2020. The nowcasting on thunderstorms and severe convection [M]. Beijing:Meteorological Press: 125-157 (in Chinese)

[37]

俞小鼎,姚秀萍,熊廷南,等. 2006. 多普勒天气雷达原理与业务应用[M].北京:气象出版社:125-157.

[38]

Yu X D, Yao X P, Xiong T N, et al. 2006. Principles and operational applications of doppler weather radar [M]. Beijing:Meteorological Press: 163-169 (in Chinese)

[39]

郑媛媛,俞小鼎,方翀,等. 2004.一次典型超级单体风暴的多普勒天气雷达观测分析[J].气象学报,62(3):317-328.

[40]

Zheng Y Y, Yu X D, Fang C, et al. 2004. Analysis of a strong classic supercell storm with Doppler weather radar data [J].Acta Meteorologica Sinica,62(3):317-328 (in Chinese). doi:10.3321/j.issn:0577−6619.2004.03.006

[41]

Browning K A. 1962. Cellular structure of convective storms [J].Australian Meteorological Magazine,91(1085):341-350. doi:10.1016/j.atmosres.2019.04.015

[42]

Bringi V N, Burrows D A, Menon S M. 1991. Multiparameter radar and aircraft study of raindrop spectral evolution in warm-based clouds [J].Journal of Applied Meteorology And Climatology,30(6):853-880. doi:10.1175/1520−0450(1991)030<0853:MRAASO>2.0.CO

[43]

Jackson R, Collis S, Lang T, et al. 2020. PyDDA: A pythonic direct data assimilation framework for wind retrievals [J].Journal of Open Research Software,8(1). doi:10.5334/jors.264

[44]

Kumjian M R, Khain A P, Benmoshe N, et al. 2014. The anatomy and physics of ZDR columns: investigating a polarimetric radarsignature with a spectral bin microphysical model [J].Journal of Applied Meteorology and Climatology,53(7):1820-1843. doi:10.1175/JAMC−D−13−0354.1

[45]

Wang X M, Zheng Y G, Fan L M, et al. 2023. The key mesoscale systems and mesoscale vortices of the Henan extreme precipitation in 2021 [J].Sustainability,15(6). doi:10.3390/su15064875

[46]

Yu X D, Wang X M, Zhao J, et al. 2012. Investigation of supercells in China: environmental and storm characteristie [C]//Psocedings of the 26th Conference on Severe Local Storms. Nashville: American Meteorological Society

基金资助

江西省气象局创新团队项目(JXCX202304)

中国气象局面上项目(CXFZ2025J027)

江西省重点研发计划项目(20243BBH81005)

江西省气象局重点项目(JX2021Z01, JX2021Z09)

江西省气象局人才培养面上专项(JX2024RCM03)

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