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青藏高原东北侧雷电气候特征

黄涛 王让会 王润元

南京信息工程大学学报2012,Vol.4Issue(2):151-156,6.
南京信息工程大学学报2012,Vol.4Issue(2):151-156,6.

青藏高原东北侧雷电气候特征

Analysis on thunderstorm and lightning climate characteristics in the northeast side of Qinghai-Tibet Plateau

黄涛 1王让会 2王润元1

作者信息

  • 1. 南京信息工程大学环境科学与工程学院,南京,210044
  • 2. 中国气象局西北区域气候中心,兰州,730020
  • 折叠

摘要

Abstract

By using the thunderstorm observation data from 1980 to 2010 of Linxia station in the northeast side of Qinghai-Tibet Plateau and the lightning data from 2006 to 2010 in the middle area of Gansu, thunderstorm and lightning characteristics such as inter-annual variation, annual variation, diurnal variation, directions of first thunderstorm , cloud-to-ground lightning density, etc were analyzed. The results of this paper found the formation characteristics of thunderstorm and lightning:the thunderstorms and lightning mainly happened in the summer and afternoon; the cloud-to-ground lightning density is higher than the average densities in China. This research will be useful to prevention and mitigation of disasters.

关键词

青藏高原东北侧/雷电/气候特征

Key words

northeastern side of Qinghai-Tibet Plateau/ thunderstorm and lightning/ climate characteristic

分类

天文与地球科学

引用本文复制引用

黄涛,王让会,王润元..青藏高原东北侧雷电气候特征[J].南京信息工程大学学报,2012,4(2):151-156,6.

基金项目

中国气象局干旱气象研究基金(IAM201001) (IAM201001)

国家重点基础研究发展规划项目(2006CB705809) (2006CB705809)

南京信息工程大学学报

OACSTPCD

1674-7070

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