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《Plateau Meteorology》 2008-03
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Mechanism Analysis of a Severe Hailstorm Process in Guangxi

SUN Ying1-3,SHOU Shao-wen2,SHEN Xin-yong2,LIU Ze-jun3,XIONG Wen-bing4(1.Guilin Meteorological Bureau,Guilin 541001,China;2.Jiangsu Key Laboratory of Meteorological Disaster,Nanjing University of Information Science and Technology,Nanjing 2100044,China;3.Guangxi Institute of Meteorological Disaster Mitigation,Guilin 530022,China;4.Guangxi Meteorological Science and Technique Service Center,Guilin 530022,China)  
Based onthe NCEP reanalyzed data,MM5 numerical simulation data and the Doppler radarproducts,a severehailstormprocess occurred in north of Guangxi Province of China on April 9~10,2006 was analyzed.The results indicatethat the dry and warm lids existed previously to the severe convection process is favorable to storing of the convective available potential energy(CAPE).The increase of verticalwind shear promoted the exchanges of the upper and lower levels to unveilthe dry and warm lids,to triggerthe convection.The downward transportion of the potential vorticityof upper level cause the lower level vorticitychanges,and lead to the convergenceof lower level and divergenceof upper level,it keeps and strengthens the strong convection.The severe convection storm center is located above 500 hPa,there is a weak echo on the lower level.Storm center ascended incline and whirl clockwisefrom lower level to upper level.
【Fund】: 国家自然科学基金项目(40405009 40575022 40205008);; 江苏省气象局科技开发项目(200406);; 江苏省气象灾害重点实验室项目(KLME050201);; 国家重点基础研究发展规划项目(2004CB418301);; 江苏省自然科学基金项目(BK2005141);; 广西气象局重点攻关项目(QK200603)共同资助
【CateGory Index】: P458.121.2
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