CAJ | 학술논문

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.
분석료2007년3월3일하택시적폭우과정,결과표명,서남난습기류이급랭공기적공동작용시하택폭우형성적주요원인;재상승운동구곡솔최대적구역다유강강우운단격발.대저차폭우과정구유적대표성화특수성진행료탐토,이기위금후적폭우예보제공삼고.
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 high-curvature 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.