摘要
通过对2003年7月8日发生在长江中游的一场大暴雨进行中尺度分析,初步研究了暴雨的形成及发展过程,总结了暴雨的产生与中小尺度系统的关系,着重阐述了低空急流在暴雨形成中的作用,以及在低空急流左侧强正涡度中心附近形成中尺度涡旋,激发暴雨云团等。
By mesoanalysis of a precipitation that occurred in the middle reaches of the Changjiang River, 8th Jul. in 2003, the formation and development of the event, its relation with the meso-microscale system are studied, it is emphasized that the low-level jet would cause favorable thermodynamic, moisture and dynamic conditions for the heavy rainfall in the middle reaches of the Changjiang River and that the mesoscale vortex formed in the left of the low-level jet would stimulate strong convective clouds and cause the heavy rain.
出处
《气象》
CSCD
北大核心
2005年第9期24-29,共6页
Meteorological Monthly
基金
科技部公益研究项目"我国南方致洪暴雨预测预警系统研究"
