浙北地区两次强对流过程的闪电活动特征分析
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1.杭州市钱塘区气象局、中国气象局雄安大气边界层重点开放实验室、中国气象局气溶胶与云降水重点开放实验室;2.杭州市钱塘区气象局;3.中国气象局雄安大气边界层重点开放实验室、中国气象局气溶胶与云降水重点开放实验室、南通大学电气与自动化学院;4.杭州市钱塘区气象局、杭州城市气象联合实验室;5.无锡学院

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中国气象局雄安新区大气边界层重点开放实验室开放课题(2023LABL-B14),中国气象局气溶胶与云降水重点开放实验室开放课题(KDW2401),浙江省气象局青年项目(2024QN23)


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Analysis of Lightning Activity Characteristics in Two Severe Convective Events over Northern Zhejiang
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1.Qiantang District Meteorological Bureau of Hangzhou、ey Open Laboratory of Atmospheric Boundary Layer in Xiong&2.amp;3.#39;4.&5.an, China Meteorological Administration (CMA)、Key Laboratory for Aerosol–Cloud–Precipitation of China Meteorological Administration;6.Qiantang District Meteorological Bureau of Hangzhou;7.key Open Laboratory of Atmospheric Boundary Layer in Xiong&8.an, China Meteorological Administration (CMA)、Key Laboratory for Aerosol–Cloud–Precipitation of China Meteorological Administration、School of Electrical and Automation Engineering, Nantong University;9.Qiantang District Meteorological Bureau of Hangzhou、Hangzhou Urban Meteorology Joint Laboratory;10.Wuxi University

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Open Research Fund of the Key Open Laboratory of Atmospheric Boundary Layer of Xiong''an New Area, China Meteorological Administration (2023LABL-B14); Open Research Fund of the Key Open Laboratory of Aerosol and Cloud Precipitation, China Meteorological Administration (KDW2401);Youth Research Project of Zhejiang Meteorological Bureau (2024QN23)

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    摘要:

    利用浙江省三维闪电定位数据与杭州S波段多普勒天气雷达体扫资料,对比分析了2024年3月25日冰雹过程和8月20日暴雨过程的闪电活动特征及其与雷达参量的关联。结果表明:(1)两次过程的闪电活动均与强回波核心区保持良好的空间对应,但闪电类型构成差异显著,两次过程均以地闪(CG)为主,冰雹过程中云闪(IC)的相对占比更高,暴雨过程IC主要集中在对流最旺盛时段;(2)Spearman相关分析显示,闪电频数与雷达参量的最优相关参量因天气类型而异,冰雹过程中面积类参量(≥40 dBZ回波面积、≥55dBZ回波面积)相关性最突出,暴雨过程中回波顶高(ET)相关性最佳;(3)两次过程均展现出闪电预警指示信号,但表现形式不同,冰雹过程总闪频数跃增超前于首次降雹15~30 min,“闪电跳跃”特征明显,暴雨过程≥55dBZ回波面积峰值领先总闪频数峰值30 min,指示性更为突出;(4)两次过程的闪电电流分布存在明显差异:正地闪峰值电流在两次过程中分布相近,而负地闪峰值电流差异显著,暴雨过程中负地闪峰值电流整体偏强,中位数及高值事件比例均高于冰雹过程;此外,冰雹过程中负地闪峰值电流在降雹前后呈系统性下降,经Mann-Whitney U检验差异高度显著,可作为冰雹阶段转换的潜在电学指标。研究结果可为不同类型强对流天气的闪电临近预警策略优化提供参考依据。

    Abstract:

    Based on three-dimensional lightning location data from Zhejiang Province and volume scan data from the Hangzhou S-band Doppler weather radar, this study comparatively analyzes the lightning activity characteristics and their correlations with radar parameters during a hailstorm on March 25, 2024 and a rainstorm on August 20, 2024. The results show that: (1) Lightning activity in both events maintained good spatial correspondence with the intense echo core regions; however, the compositions of lightning types differed significantly. Both events were dominated by cloud-to-ground (CG) flashes, while the hailstorm exhibited higher absolute frequency and relative proportion of intra-cloud (IC) flashes. In the rainstorm, IC flashes were primarily concentrated during the most vigorous convective period. (2) Spearman correlation analysis reveals that the optimal radar parameter correlated with lightning frequency varies with weather type. For the hailstorm, areal parameters (≥40 dBZ echo area and ≥55 dBZ echo area) showed the most prominent correlations, whereas for the rainstorm, echo top height (ET) exhibited the best correlation. (3) Both events demonstrated lightning-based early warning indicators, albeit in different forms. In the hailstorm, a sharp surge in total lightning frequency preceded the first hailfall by 15–30 min, with a distinct "lightning jump" signature. In the rainstorm, the peak of ≥55 dBZ echo area led the peak of total lightning frequency by 30 min, presenting a more pronounced indicative signal. (4) The distributions of lightning peak current differed notably between the two events: positive CG peak currents exhibited similar distributions in both cases, while negative CG peak currents differed significantly. The rainstorm featured overall stronger negative CG peak currents, with higher median values and a greater proportion of high-amplitude events compared to the hailstorm. Furthermore, negative CG peak currents during the hailstorm showed a systematic decrease from the pre-hail to post-hail phase, with the difference being highly significant as confirmed by the Mann-Whitney U test, suggesting its potential as an electrical indicator for hail phase transitions. These findings provide a reference for optimizing lightning-based nowcasting strategies for different types of severe convective weather.

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  • 收稿日期:2026-03-19
  • 最后修改日期:2026-04-29
  • 录用日期:2026-04-29
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