首页|期刊导航|气象|福建对流体霰粒子层厚度特征与地闪初生关系研究

福建对流体霰粒子层厚度特征与地闪初生关系研究OA

Relationship Between Graupel Particle Layer Thickness of Convective Storms and Cloud-to-Ground Lightning Initiation in Fujian Province

中文摘要英文摘要

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.

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 re-sults 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 through-out 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 calcu-lated TS score of the sample is 0.864 and the average forecast lead time is 28.13 min.Taking four convec-tive storms on 14 June 2022 in southern Fujian Province as examples,the above-mentioned forecast indica-tors are applied and analyzed in these cases.The results show that the proposed forecast indicator can ac-curately forecast whether cloud-to-ground lightning will occur in the four convective storms,and the fore-cast lead time for cloud-to-ground lightning initiation is 6 min.

张烨方;吴启树;李婷婷;冯真祯;刘冰;黄玲光;何清芳;廖廓

福建省灾害天气重点实验室,福州 350001||中国气象局海峡灾害天气重点开放实验室,福州 350001福建省灾害天气重点实验室,福州 350001||中国气象局海峡灾害天气重点开放实验室,福州 350001||福建省气象台,福州 350001福建省气象台,福州 350001福建省灾害天气重点实验室,福州 350001||中国气象局海峡灾害天气重点开放实验室,福州 350001福建省灾害天气重点实验室,福州 350001||中国气象局海峡灾害天气重点开放实验室,福州 350001福建省灾害天气重点实验室,福州 350001||中国气象局海峡灾害天气重点开放实验室,福州 350001福建省灾害天气重点实验室,福州 350001||中国气象局海峡灾害天气重点开放实验室,福州 350001福建省灾害天气重点实验室,福州 350001||中国气象局海峡灾害天气重点开放实验室,福州 350001

天文与地球科学

地闪初生霰粒子双偏振雷达对流体

cloud-to-ground lightning initiationgraupel particledual-polarization radarconvective storm

《气象》 2026 (3)

337-347,11

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

10.7519/j.issn.1000-0526.2026.010501

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