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投稿时间:2025-02-26 修订日期:2026-01-05
投稿时间:2025-02-26 修订日期:2026-01-05
中文摘要: 以2022年4月至2024年6月福州、厦门、龙岩双偏振雷达粒子分类产品、地闪定位数据为基础,遴选了有、无地闪发生的54个对流体样本,对样本发展过程中的霰粒子层厚度时序变化规律进行了研究。结果表明,有地闪发生的对流体在首次地闪初生时霰粒子层厚度至少达到2.26 km,无地闪发生的对流体在生命周期内霰粒子层厚度有95%样本小于2.2 km,在综合考虑地闪初生预报提前时间和准确率的条件下,提出采用霰粒子层厚度大于2 km作为福建省对流体地闪初生的预报指标,对其预报潜力进行了评价,计算得到样本TS评分为0.864,平均预报提前时间为28.13 min。以2022年6月14日福建省南部的4个对流体为例对上述预报指标进行了实例应用与分析,结果显示,该预报指标对4个对流体未来是否发生地闪均做出正确预报,地闪初生的预报提前时间为6 min。
中文关键词: 地闪初生,霰粒子,双偏振雷达,对流体
Abstract:Based on the dual-polarization radar particle classification products and cloud-to-ground lightning location data from Fuzhou, Xiamen and Longyan from April 2022 to June 2024, in this study we select 54 convective storm samples with or without cloud-to-ground lightning and investigate the temporal variation characteristics of graupel particle layer thickness during the developing processes of these samples. The results show that the graupel particle layer thickness of convective storms with cloud-to-ground lightning reaches at least 2.26 km at the initiation moment of the first cloud-to-ground lightning, while 95% of the samples without cloud-to-ground lightning, have graupel particle layer thickness less than 2.2 km throughout their lifecycles. Considering both the lead time and accuracy of cloud-to-ground lightning initiation forecasts, we propose to use a graupel particle layer thickness greater than 2 km as a forecast indicator for cloud-to-ground lightning initiation in Fujian Province. The forecast potential is evaluated, and the calculated TS score of the sample is 0.864 and the average forecast lead time is 28.13 min. Taking four convective storms on 14 June 2022 in southern Fujian Province as examples, the above-mentioned forecast indicators are applied and analyzed in these cases. The results show that the proposed forecast indicator can accurately forecast whether cloud-to-ground lightning will occur in the four convective storms, and the forecast lead time for cloud-to-ground lightning initiation is 6 min.
keywords: cloud-to-ground lightning initiation, graupel particle, dual-polarization radar, convective storm
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基金项目:福建省自然科学基金项目(2025J011224、2023J011335)、福建省自然科学基金社会发展引导性(重点)项目(2025Y0064)、福建省科技重大专项(2024YZ040025)、福建省气象局开放式气象科学研究基金项目(2023KJ04)和厦门市科技局自然科学基金项目(20241303)共同资助
引用文本:
张烨方,吴启树,李婷婷,冯真祯,刘冰,黄玲光,何清芳,廖廓,2026.福建对流体霰粒子层厚度特征与地闪初生关系研究[J].气象,52(3):337-347.
ZHANG Yefang,WU Qishu,LI Tingting,FENG Zhenzhen,LIU Bing,HUANG Lingguang,HE Qingfang,LIAO Kuo,2026.Relationship Between Graupel Particle Layer Thickness of Convective Storms and Cloud-to-Ground Lightning Initiation in Fujian Province[J].Meteor Mon,52(3):337-347.
张烨方,吴启树,李婷婷,冯真祯,刘冰,黄玲光,何清芳,廖廓,2026.福建对流体霰粒子层厚度特征与地闪初生关系研究[J].气象,52(3):337-347.
ZHANG Yefang,WU Qishu,LI Tingting,FENG Zhenzhen,LIU Bing,HUANG Lingguang,HE Qingfang,LIAO Kuo,2026.Relationship Between Graupel Particle Layer Thickness of Convective Storms and Cloud-to-Ground Lightning Initiation in Fujian Province[J].Meteor Mon,52(3):337-347.
