摘要
使用南京气象学院的Ｄｏｐｐｌｅｒ雷达资料分析了１９９１年７月９日的江淮梅雨锋大暴雨过程。结果表明：当天的大暴雨与边界层中尺度涡旋系统活动密切相关，同时揭示了暴雨区大气低层的气流垂直结构特征。
The rain gush associated with the Jiang Huai Mei yu front occurred on July 9,1991, was observed with the Doppler radar in Nanjing Institute of Meteorology. The analysis of the data has shown in this paper that the rain gush was closely related with the activity of the mesoscale vortex system in the boundary layer. The vertical structure features of air flow in the lower atmosphere in the region are also revealed.
出处
《南京气象学院学报》
CSCD
1998年第2期201-207,共7页
Journal of Nanjing Institute of Meteorology
