摘要
对１９９５年６月３０日—７月１日华北高空冷涡的强降水过程作了详细分析，探讨了冷涡演变的物理量场分布特征及其云系变化与降水的对应关系，为日常业务预报提供了一些启示。
An analysis on upper cold vortex that caused heavy rain in North China from 30 June to 1 July 1995 is presented.The physics field features and cloud system development of cold vortex corresponding to precipitation are discussed.The results are referential for routine operational prediction.
出处
《气象》
CSCD
北大核心
1997年第9期50-53,共4页
Meteorological Monthly
关键词
冷涡
涡度
冷锋
副冷锋
华北地区
cold vortex positive vorticity area cold front secondary cold front
