摘要
利用一个带有地形的二层均质流体模式,引入参数化形式的积云对流加热反馈,研究了重力惯性波的不稳定增长及传播,得到并讨论了一些接近天气实际情况的结果。
In this paper, a two-layer homogeneous fluid model with the terrain considered is used. And a parameterized feedback of cumulus convection heating is introduced. After the study of the unstable development and propagation of inertia-gravitational wave, some results similar to the actual weather cases are obtained and discussed.
出处
《热带气象》
CSCD
1991年第1期8-15,共8页
