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一次伴随冰雹的超级单体风暴特征
引用本文:江玉华,刘娟,何跃,赵大军,王欢,翟丹华.一次伴随冰雹的超级单体风暴特征[J].气象科技,2011,39(2):172-181.
作者姓名:江玉华  刘娟  何跃  赵大军  王欢  翟丹华
作者单位:1. 中国气象科学研究院灾害天气国家重点实验室,北京,100081;重庆市气象台,重庆,401147
2. 安徽省阜阳市气象局,阜阳,236001
3. 重庆市气象台,重庆,401147
4. 解放军93762部队气象台,北京,102100
基金项目:灾害天气国家重点实验室基金(2008LASWB08)课题、国家自然科学基金“超级单体风暴三维结构和流场研究”(40575012)资助
摘    要:利用中国气象监测网实测资料、重庆西部多普勒天气雷达资料及NCEP/NCAR 6 h间隔1°×1°再分析资料,对2008年6月5日发生在重庆市中部的大风冰雹天气过程进行了天气背景、物理量、雷达回波和云图特征分析.研究表明:大气中显著的水平风切变和垂直风切变及晴空太阳辐射对地面的不均匀加热都有利于诱生涡度;从北部高层向南侵...

关 键 词:冰雹  物理量诊断  超级单体  强风暴  预报
收稿时间:2009/12/16 0:00:00
修稿时间:2010/2/21 0:00:00

Characteristics of a Super Cell Storm with Hail
Jiang Yuhu,Liu Juan,He Yue,Zhao Dajun,Wang Huan and Zai Danhua.Characteristics of a Super Cell Storm with Hail[J].Meteorological Science and Technology,2011,39(2):172-181.
Authors:Jiang Yuhu  Liu Juan  He Yue  Zhao Dajun  Wang Huan and Zai Danhua
Institution:1 State Key Laboratory of Severe Weather, Chinese Academy of Meteorological Sciences, Beijing 100081; 2 Chongqing Municipal Meteorological Bureau, Chongqing 401147;Anhui Fuyang Meteorological Bureau, Anhui Province, Fuyang 236001;Chongqing Municipal Meteorological Bureau, Chongqing 401147;Unite 93762 of PLA, Beijing 102100;Chongqing Municipal Meteorological Bureau, Chongqing 401147;Chongqing Municipal Meteorological Bureau, Chongqing 401147
Abstract:A hail event with a gale occurred on 5 June 2008 is analyzed from the aspects of the synoptic circulation background,physical quantities,and the characteristics of radar echoes and cloud pictures by means of observational data from the Meteorological Observation Network of China,Doppler weather radar data from the western Chongqing,and NCEP/NCAR 1°×1° reanalysis data.It is demonstrated that the vertical and horizontal wind shear and the clear sky solar radiation,which resulted in uneven surface heating,were apt to the vorticity genesis.The dry-cold air in the upper troposphere intruded into the lower layer favored the maintenance of convective instability,and the increasing of specific humidity and CAPE in the lower troposphere was essential to the development of the convective storm.The high potential vorticity(greater than 1 PVU) contributed to the genesis and development of the super-cell storm(meso-cyclone).The features of a super-cell storm can be found,such as the strong overhanging echo core,false echo,meso-cyclone,weak echo and echo wall,large echo intensity gradient,etc.,and there existed the cumulonimbus plume and up-rushing cloud top in the visible satellite imagery(VIS).Some forecast clues are concluded for super-cell storms.
Keywords:hail  physical quantity diagnosis  super-cell feature  severe storm  forecast  
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