摘要
2010年7月19日午后塔额盆地出现了一场较强雹云天气过程。根据塔城雷达站监测回波资料,分析此次强单体雹云的结构、演变、移动和降雹特征,对此次冰雹云的类型、结构、特征及其演变趋势进行分析,并提出相应的雹云判识方法。
One strong hailstorm weather process happened in Tower frontal basin in the afternoon on July 19,2010.According to the echo data monitored from Tacheng Radar Station,the structure,changes,movement of single strong hail cloud and characteristics of hailstorms were expounded.The type,structure,characteristic and evolution trend of icy storm cloud were analyzed.Corresponding storm clouds were recognized.
出处
《安徽农业科学》
CAS
北大核心
2011年第12期7534-7535,共2页
Journal of Anhui Agricultural Sciences
关键词
强雹云
雷达回波
塔额盆地
Strong hailstorm
Radar echo
Tower frontal basin
