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《Chinese Journal of Atmospheric Sciences》 2008-02
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Cloud-to-Ground Lightning Characteristics of Hail Clouds in Shandong Province

FENG Gui-Li1,2,QIE Xiu-Shu3,and WU Shu-Jun 41 Cold and Arid Regions Environmental and Engineering Research Institute,Chinese Academy of Sciences,Lanzhou 7300002 Shandong Institute of Meteorological Sciences,Jinan 2500313 Institute of Atmospheric Physics,Chinese Academy of Sciences,Beijing 1000294 Binzhou Meteorological Bureau,Binzhou 256612  
There are usually intensive electrification and active discharges in severe hailstorms because of strong updraft and abundant ice particles and supercooled water content.Although a lot of researchers have analyzed the lightning activities in hailstorms and many useful results have been achieved,the evolution of lightning activities and its relations with hail-falling in hailstorms are not quite clear up to now.In order to help to understand the lightning characteristics in hailstorms and the application of lightning information to the warning of severe convective weather,the cloud-to-ground(CG) lightning activities of hailstorms occurring in Shandong Province are studied in this paper.The CG flashes were observed by Shandong Lightning Detection Network(SLDN),which consists of 10 sensors covering all over the Shandong Province.Firstly,the characteristics of CG lightning polarity,spatial and temporal distribution of ten hailstorms are analyzed statistically.The results show that the mean proportion of positive CG lightning accounting for total CG lightning is 57.39%,which is much higher than the local climatic normal rate by 13.48%.The hail-falling is often reported in the region of dense positive CG lightning.Sometimes hailstone appears slightly at right flank of the dense CG lightning region.There is a distinct intensive increase in CG flash rate in the quickly developing period of hail cloud,while the rapid reduction in CG flash rate occurs at the dissipating stage.The hailstone falling corresponds to an active positive flash period,and the increase of positive CG flash rate is generally accompanied with a decrease of negative CG flash rate.The peak negative CG flash rate usually occurs 0 to 20 minutes earlier than hailstone falling,but the peak positive CG flash rate usually is late or simultaneous for the occurrence of hailstones.When the polarity of CG lightning changes,it often indicates the advent of severe weather such as hail,strong wind and heavy precipitation.Secondly,using the advantage of TRMM LIS being able to detect total lightning,i.e.intracloud(IC) and CG lightning,the ratios of IC lightning to CG lightning in hailstorms are compared with those in common thunderstorms.The analysis discloses that both the ratio of IC to CG lightning and IC flash density in hailstorms are far bigger than those in the thunderstorms.This is mainly caused by elevated charge structures associated with strong updrafts.These features are likely useful for hailstorms forecasting.At last,the reasons of high percentage of positive CG lightning in hailstorms are discussed,and it is speculated that inverted tripole charge structure is likely leading to high ratio of positive CG lightning in hailstorms.
【Fund】: 中国科学院知识创新工程重要方向项目KZCX2-YW-206;; 国家自然科学基金资助项目40505001、40325013;; 山东省气象局基金2005sdqxj01
【CateGory Index】: P426.5;P427.32
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