摘要
分析了2007年3月3日菏泽市的暴雨过程,结果表明,西南暖湿气流以及冷空气的共同作用是菏泽暴雨形成的主要原因;在上升运动区曲率最大的区域多有强降雨云团激发。对这次暴雨过程具有的代表性和特殊性进行了探讨,以期为今后的暴雨预报提供参考。
The course of storm of Heze City in March 3rd, 2007 was analyzed. The results showed that the effects of southwest warm-wet airflow and the freezing air were the main reason of the formation of rainstorm in Heze City. Torrential rains cloud was always motivated in highcurvature areas of ascending motion areas. At the same time, the representativeness and particularity of the rainstorm was discussed, so as to provide reference for the future forecast of rainstorm.
出处
《安徽农业科学》
CAS
北大核心
2010年第3期1329-1331,1374,共4页
Journal of Anhui Agricultural Sciences
关键词
初春暴雨
成因分析
地面气旋
Rainstorm in the early spring
Cause analysis
Surface cyclone
