首页 | 本学科首页   官方微博 | 高级检索  
     检索      

2010年7月19日安阳暴雨过程诊断分析
引用本文:王安俊.2010年7月19日安阳暴雨过程诊断分析[J].河南科学,2011,29(9):1076-1080.
作者姓名:王安俊
作者单位:商丘市气象局,河南商丘,476000
摘    要:利用天气图资料、物理量场、卫星云图、雷达回波等气象资料,对2010年7月19日安阳区域一次典型暴雨天气过程进行分析,进而对我市区域性暴雨天气过程的特征进行总结,得出以下结论:①造成此次区域性暴雨的主要影响系统是西太平洋副热带高压及其西北侧的西风带低槽和西南低涡,属于典型的北槽南涡型暴雨天气类型.低槽引导西南低涡东北上,...

关 键 词:暴雨  分析  天气图  物理量场  卫星云图  雷达回波

A Diagnostic Analysis of Rainstorm Process in Anyang on July 19th 2010
Wang Anjun.A Diagnostic Analysis of Rainstorm Process in Anyang on July 19th 2010[J].Henan Science,2011,29(9):1076-1080.
Authors:Wang Anjun
Institution:Wang Anjun(Shangqiu Meteorological Bureau,Shangqiu 476000,Henan China)
Abstract:By using of weather maps material,physical fields,such as satellite image,radar meteorology,for July 19th 2010 at Anyang region a typical rainstorm weather process analysis,then for zhuhai’s regional rainstorm weather process features summarized can reach the following conclusion:①By the regional the main influence system is heavy and west of the western Pacific subtropical high of wetting weakeed low slots and southwest vortex.Low groove guide,southwest vortex northeast,trough the cold air and the apparent northeast and southwest vortex of subtropical high level warm-moist air southwest edge of outer common effect convergence,caused anyang re-emergence heavy rain process.②Strong and not produce precipitation in Tbb valuable center point,but in the nearby produced with dense,within the isoline.This is due to lowest,Tbb genting supreme,right now is often the most exuberant cloud body development stage,and not only the strongest,precipitation in genting gradually declined,the precipitation to reach the strongest.③Look from radar rainfall from southwest to northeast echo generally moving,echo intensity 48 dBz maximum.
Keywords:rainstorm  analysis  weather map  physical field  satellite cloud picture  radar echo  
本文献已被 CNKI 维普 万方数据 等数据库收录!
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号