摘要
本文指出,大气环流的明显的季节变化(如入梅、出梅和冬季环流的建立等),是通过一次长波斜压不稳定发展向下游传播的中期过程来具体实现的。
In this paper,it is shown that the notable seasonal changes of atmosphere circulation,such as the begining and the end of Mai-yu and the establishment of the winter circulation,were achieved with a medium-range process in which there is the propagation of the development of long wave baroclinic instability down stream.
作者
缪锦海
Miao jin-hai(Department of Geophysics,Beijing University)
出处
《气象学报》
1980年第3期269-276,共8页
Acta Meteorologica Sinica
