摘要
用ECMWF提供的1982年7月1—31日逐日2.5°×2.5°网格资料,分析了江淮梅雨过程高低层流函数与势函数场的演变及其相互作用,并讨论了梅雨前后东亚季风的变化。
In this paper, the interaction between the velocity potential X and stream function ψ fields and the change of summer monsoon over the East-Asia in a Mei-Yu process from July 1 to July 31 1982 were discussed by using the daily data (2. 5°×癤2. 5° of the ECMWF , and significant results were obtained.
出处
《热带气象学报》
CSCD
1993年第4期364-369,共6页
Journal of Tropical Meteorology
基金
国家自然科学基金资助项目
关键词
梅雨
流函数
势函数
降水
Mei-Yu Velocity potential function Χ Stream function ψ
