贵州省三都 1 次强降雹天气的 X 波段雷达特征
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1.贵州省三都水族自治县气象局;2.贵州省黔南布依族苗族自治州气象局;3.贵州省荔波县气象局

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2024年州县联合科研基金项目


Characteristics of X-band Radar During a Severe Hail Event in Sandu County of Guizhou Province
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1.Sandu Shui Meteorological Station of Guizhou Province;2.Qiannan Buyi and Miao Autonomous Prefecture Meteorological Office of Guizhou Province

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    摘要:

    【目的】为探究 X 波段双偏振多普勒天气雷达在三都水族自治县(简称三都县)强对流天气监测预警中的本地化应用价值,以 2024 年 4 月 16 日三都县强降雹过程为研究对象,基于常规气象观测、ERA5 再分析数据及三都县 X 波段双偏振多普勒天气雷达数据,系统揭示该过程的成因机制与雷达回波特征。【结果】1) 此次强降雹发生在 500 hPa 高空槽前、700 hPa 西南急流、850 hPa 切变线与地面辐合线的协同环流背景下;热力、动力诊断显示,强对流发展阶段的整层强上升运动以及“低层辐合、高层辐散 ”配置为对流维持提供必要条件,降雹阶段强垂直风切变维持风暴倾斜结构,延长降雹时间。2) 雷达回波呈现典型超级单体特征,钩状回波、入流缺口与深厚中气旋结构是强降雹的关键雷达标志。3) 大冰雹诊断的核心偏振参量包括:组合反射率 CR > 50 dBz 降至地面、差分反射率因子 Z DR ≈0 dB 、相关系数 CC < 0 . 8 及差分相移率因子 KDP 介于 0 . 15 ~ 1 . 1 ( °)/km;不同高度 ZDR 与 CC 的演变可反映冰雹粒子微物理增长过程,低层出现 ZDR 柱、Z DR 柱高度下降及 CC < 0 . 8 区域水平扩展可作为降雹先兆信号。【结论】研究结果为 X 波段雷达在三都县的本地化运用提供科学依据。

    Abstract:

    Abstract: To explore the localized application value of the X-band dual-polarization Doppler weather radar in monitoring and early warning of severe convective weather in Sandu Shuizu Autonomous County ( hereinafter referred to as Sandu County) , this study focuses on the severe hailstorm event in Sandu County on April 16 , 2024 and systematically clarifies the formation mechanism and radar echo characteristics of the event by using conventional meteorological observation data , ERA5 reanalysis data and data from the local X-band dual-polarization Doppler weather radar. The results are as follows : ( 1 ) The severe hailstorm occurred under the synergistic circulation of the pre-500 hPa upper trough , 700 hPa southwest jet , 850 hPa shear line , and surface convergence line . Thermodynamic and dynamic diagnosis shows that in the stage of severe convection development , the strong whole-layer ascending motion and the " low-level convergence with upper-level divergence " configuration provided essential conditions for sustaining convection . Then , during the hailstorm stage , the strong vertical wind shear maintained the tilted storm structure , extending the lasting time of the hailstorm. (2) The radar echo presented typical features of super cells , with hook echo , inflow notch and deep meso-cyclone being the key radar indicators for the severe hailstorm. (3 ) The core polarization parameters for large-size hail diagnosis are as follows: composite reflectivity (CR) > 50 dBz reaching the ground , differential reflectivity factor (Z DR ) ≈0 dB , correlation coefficient (CC) < 0 . 8 , and specific differential phase factor (KDP ) ranging from 0 . 15 to 1 . 1 °/km. The evolution of ZDR and CC at different heights can reflect the microphysical growth of hail particles . In other words , the emergence of a low- level Z DR column , the descent of the Z DR column height , and the horizontal expansion of the CC < 0 . 8 area can serve as precursory signals for hailstorms . These research findings can be used as a scientific basis for the localized application of the X-band radar in Sandu County.

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兰鸿侠,冯正艳,龙宇芸,等.贵州省三都 1 次强降雹天气的 X 波段雷达特征[J].山地气象学报,2026,50(1):58-66.

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  • 收稿日期:2025-06-30
  • 最后修改日期:2025-11-04
  • 录用日期:2025-11-13
  • 在线发布日期: 2026-03-10
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