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《Chinese Journal of Atmospheric Sciences》 2007-01
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A Numerical Study of the Charge Structure in Thunderstorm in Nagqu Area of the Qinghai-Xizang Plateau

GUO Feng-Xia,ZHANG Yi-Jun,and YAN Mu-HongCold and Arid Regions Environmental and Engineering Research Institute,Chinese Academy of Sciences,Lanzhou 730000  
Due to Nagqu's unique geographical situation,dominated by large plateaus,valleys and basins which average altitudes are 4-5 km MSL,the thundercloud activity in the Qinghai-Xizang Plateau is particular.The characteristics of soundings in two thunderstorm days in Nagqu are analyzed.As the altitude of Nagqu is about 4.5 km MSL,the average surface temperature is 15.7℃,which is lower than Chinese inland plateau and littoral.The thickness between 0℃ and-20℃ levels is about 2.93 km.The average heights of cloud-base and top are 5.7 km and(12.2 km) MSL,respectively.On the average,CAPE(convective available potential energy) is critical instability(0-1000 J/kg).The mean relative humidities in the middle and upper levels are 62.1% and 43.5%,respectively.The high humidity and dynamic force can provide the favorable conditions for the formation of line storms or MCSs.The characteristics of charge structure in thunderstorm of Nagqu are analyzed by using the three-dimensional dynamic-electrification coupled model.This model only includes inductive and non-inductive charging mechanisms.Two thunderstorms are simulated.The result shows that the charge region under the temperature reversal is limited,because the surface temperature is lower in Nagqu.The mean duration of solid particles in strong updraft is longer than in weak updraft.Collision probability between big and small particles is increased in strong updraft,so it is easy to form tripole charge structure.The centers of specific water content of big and small particles are separated early in weak updraft.The small particle in the upper layer and big particle in the lower layer hardly take part in charge activity,so main positive charge region and LPCC(lower positive charge center) is small.On the average,LPCC is located in downdraft,while main positive charge region is located in updraft.Main negative charge region is distributed about zero vertical velocity.It is easy to form several alternate negative and positive charge layers in strong updraft.
【Fund】: 国家自然科学基金资助项目40575002;; 中国科学院西部之光项目“西北地区人工增雨防雹减灾关键理论与技术研究”;; 国家自然科学基金资助项目40605002
【CateGory Index】: P427
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8 Zhang Yijun Liu Xinsheng Xiao Qingfu (Lanzhou Institute of Plateau Atmospheric Physics,Chinese Academy of Sciences,Lanzhou Gansu 730000);A ANALYSIS OF CHARACTERISTICS OF THUNDERSTORM AND ARTIFICIALLY TRIGGERED LIGHTNING IN THE NORTH AND SOUTH OF CHINA[J];PLATEAU METEOROLOGY;1997-02
9 WANG Shi-gong1 YANG De-bao1 LI La-ping1HUANG Jian-guo1 QI Bin2( 1 Department of Atmospheric Sciences, Lanzhou University,Lanzhou,Gansu 730000)( 2 Environmental Monitoring Station of Lanzhou,Lanzhou,Gansu 730000);COLD-FRONT ACTIVITIES AND ITSINFLUENCE ON AIR POLLUTION ATURBAN DISTRICTS OF LANZHOUIN COLD HALF YEAR[J];PLATEAU METEOROLOGY;1998-02
10 Liu Xinsheng Guo Changming Wang Caiwei Yan Muhong(Lanzhou Institute of Plateau Atmospheric Physics, Academia Sinica);THE SURFACE ELECTROSTATIC FIELD-CHANGE PRODUCED BY LIGHTNING FLASHES AND THE LOWER POSITIVE CHARGE LAYER OF THE THUNDERSTORM[J];Acta Meteorologica Sinica;1987-04
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