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Investigating Lightning Characteristics through a Supercell Storm by Comprehensive Coordinated Observations over North China

Investigating Lightning Characteristics through a Supercell Storm by Comprehensive Coordinated Observations over North China

作     者:Dongxia LIU Xiushu QIE Yichen CHEN Zhuling SUN Shanfeng YUAN Dongxia LIU;Xiushu QIE;Yichen CHEN;Zhuling SUN;Shanfeng YUAN

作者机构:Key Laboratory of Middle Atmosphere and Global Environment Observation(LAGEO)Institute of Atmospheric PhysicsChina Academy ScienceBeijing 100029China State Key Laboratory of Severe WeatherChinese Academy of Meteorological SciencesBeijing 100081China Beijing Weather Modification OfficeBeijing 100089China 

出 版 物:《Advances in Atmospheric Sciences》 (大气科学进展(英文版))

年 卷 期:2020年第37卷第8期

页      面:861-872页

核心收录:

学科分类:07[理学] 070601[理学-气象学] 0706[理学-大气科学] 

基  金:supported by the National Natural Science Foundation of China(Grant Nos.41875007 and 41630425) the Special Fund for Meteorology-Scientific Research in the Public Interest(Grant No.GYHY201506004) the 2018 Open Research Program of the State Key Laboratory of Severe Weather(Grant No.2018LASWB06) 

主  题:lightning supercell Beijing Lightning Network charge structure 

摘      要:Electrical characteristics of an isolated supercell storm observed on 13 June 2014 over Beijing were investigated using lightning data obtained from the Beijing Lightning Network,radar reflectivity,and hydrometeor retrievals during the 6-h *** cloud-to-ground(+CG)lightning took a high percentage of CG *** and during a hail event,+CG lightning was more frequent than negative cloud-to-ground(-CG)lightning,except that+CG lightning took a high percentage at the beginning and in the dissipating *** the hail event ended,-CG lightning dominated and reached its maximum *** analysis of hydrometeors retrieved by X-band polarimetric radar revealed that the discharge concentrated in the convective region with graupel particles and hailstones,whereas graupel,snow and ice crystals in the stratiform *** radiation sources were located mainly in the convective region,some of which were distributed along a gradient of radar reflectivity from the convective region to the stratiform *** indication is that the supercell demonstrated an inverted tripole charge structure before the hail event,which converted to a normal tripole structure after the hail event.

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