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云下部正电荷区与负地闪预击穿过程

张义军 孟青 吕伟涛 马明 郑栋 Paul R. Krehbiel

气象学报2008,Vol.66Issue(2):274-282,9.
气象学报2008,Vol.66Issue(2):274-282,9.

云下部正电荷区与负地闪预击穿过程

Positive charge region in lower part of thunderstorm and preliminary breakdown process of negative cloud-to-ground lightning.

张义军 1孟青 2吕伟涛 1马明 2郑栋 1Paul R. Krehbiel2

作者信息

  • 1. 中国气象科学研究院雷电物理与防护工程实验室,北京,100081
  • 2. 中国气象科学研究院灾害天气国家重点实验室,北京,100081
  • 折叠

摘要

Abstract

A new lightning locating technology, called Lightning Mapping Array (LMA), has been developed. The system takes the advantage of GPS technology to measure the times of arrival (TOA) of lightning impulsive VHF radiation events at each remote location. The temporal and 3-D spatial development processes of lightning are described by measurements of the system with high time resolution (50 ns) and space precision (50-100 m). The charge structures in thunderstorms and the relationship between the charge structure and lightning discharge processes are revealed. The temporal and spatial characteristics of preliminary breakdown process in negative cloud-to-ground(CG) lightning discharges are analyzed based on the data of lightning VHF radiation events. The effect of the positive charge region in the lower part of thunderstorms on the occurrence of negative CG lightning discharge is discussed. The results indicate that the preliminary breakdown process with longer lasting time of negative CG lightning discharges is an intracloud discharge process between the negative and positive charge regions located in the lower and middle parts of thunderstorms respectively. It initiated from the negative charge region in the middle part and propagated downward. After entered the positive charge region in the lower part, the lightning channel developed horizontally. The characteristics of preliminary breakdown process are consistent with that of inverted intracloud lightning discharges. The stepped leaders were initiated by the K type breakdown which occurred in the last stage of the preliminary breakdown process and penetrated downward through the positive charge region. The existence of positive charge region in the lower part of thunderstorms is the reason why there is a preliminary breakdown process with longer lasting time in thunderstorms before the first return stroke of negative CG lightning discharges take place.

关键词

地闪/正电荷区'预击穿过程

Key words

Cloud-to-ground lightning/Positive charge region/Preliminary breakdown process

分类

天文与地球科学

引用本文复制引用

张义军,孟青,吕伟涛,马明,郑栋,Paul R. Krehbiel..云下部正电荷区与负地闪预击穿过程[J].气象学报,2008,66(2):274-282,9.

基金项目

国家自然科学基金项目(40475002)和国家重大基础研究项目课题(2004CB418306). (40475002)

气象学报

OA北大核心CSCDCSTPCD

0577-6619

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