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《Plateau Meteorology》 2008-03
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The Air Flow Structure and Characteristic of CINRAD-Products in a Long-Life Storm

DIAO Xiu-guang1,YANG Xiao-xia1,ZHU Jun-jian1,WANG Jun2,HUANG Xiu-shao1(1.Shandong Province Meteorological Observatory,Jinan 250031,China2.Shandong Research Institute of Meteorology,Jinan 250031,China)  
Using the soundingdata,vorticity,surface temperature,wind vector and Jinan-CINRAD/SA products such as reflectivity,base velocity,mesocyclone and VIL in a long-life severe hailstorm in west Shandong Province on 24 June 2004,the stormstructurewas analysed.The results show that there was cyclonic-convergenceat low level.The updraft was sustained by a strong cold air pool near the surface in the back of storm,an upshear tiltingmain-updraft was built in the front of storm.The double-vortex flow pattern,which can resistthe environmentalairflow,was built form mid to mid-high levels.The storm was hard to be blown away by environmental airflow,and persisted long time.The storm had the characteristicsof supercell storm,and accompanied with mesocyclones.The \!Three-Body Scatter Spike"-TBSS was detected at mid-high levels of the storm,and it precededthe largest surface hailfall by 10~15minutes.Hailfall lasted 10~20minutes after the disappearanceof the TBSS.
【Fund】: 国家自然科学基金项目(40575012);; 山东省气象局科学技术研究项目(2006sdqxg11)共同资助
【CateGory Index】: P425
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