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中国地区闪电和对流层上部NOx的时空分布特征及其相关性分析

郭凤霞 陈聪

大气科学2012,Vol.36Issue(4):713-721,9.
大气科学2012,Vol.36Issue(4):713-721,9.DOI:10.3878/j.issn.1006-9895.2011.11129

中国地区闪电和对流层上部NOx的时空分布特征及其相关性分析

Comparison of Lightning Activity and NOx Distribution in the Upper Troposphere in China

郭凤霞 1陈聪2

作者信息

  • 1. 南京信息工程大学气象灾害省部共建教育部重点实验室,南京210044
  • 2. 南京信息工程大学中国气象局大气物理与大气环境重点开放实验室,南京210044
  • 折叠

摘要

Abstract

In order to understand the contribution of lightning to the abundance of NOx in the upper troposphere,the characteristics of spatial and temporal distribution of NOx in the upper troposphere and lightning in China,and the relationships between them are analyzed in this paper.The lightning data (from April 1995 to December 2005) and the NOx data (from October 1991 to November 2005) are obtained from the Global Hydrology Resource Center (GHRC),USA and the Halogen Occupation Experiment (HALOE) boarded on the Upper Atmosphere Research Satellite (UARS),respectively.It is found that lightning activities are in very good agreement with NOx volume mixing ratio in seasonal variations,annual variations,and spatial variations.The results prove that lightning is an important source of NOx in the upper troposphere.The height of the extreme value of NO is at about 350 hPa,while that of NO2 is at about 250 hPa.Intra-cloud lightning-generated NO is the main reason for the extreme value,the NO will oxidize into NO2 during the transmission process,and NO2 will be transported to higher height through the thunderstorms.Strong convective is helpful to transport NOx to the upper troposphere,while NOx generated by human activities can hardly do this.Therefore,in the area that more lightnings occur,the extreme value is bigger and its height is higher.

关键词

闪电/NOx/对流层上部

Key words

lightning, NOx, upper troposphere

分类

天文与地球科学

引用本文复制引用

郭凤霞,陈聪..中国地区闪电和对流层上部NOx的时空分布特征及其相关性分析[J].大气科学,2012,36(4):713-721,9.

基金项目

公益性行业科研专项GYHY200806014,南京信息工程大学校基金20080319,江苏省气象灾害重点实验室开放课题KLME1004,中国气象科学研究院基本科研业务费专项资金2010Z004和江苏高校优势学科建设工程资助项目(PAPD) (PAPD)

大气科学

OA北大核心CSCDCSTPCD

1006-9895

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