摘要
本文论证熵平衡方程可用来判断大气中对流和降水的发生,非线性热力学理论中的超熵产生可用来判断天气系统的产生.
This paper proves that the entropy equilibrium equation can be used to diagnose the generation of the convection and precipitation in the atmosphere, and that the excess entropy production in the non-linear thermodynamical theory can be used to diagnose the generation of weather systems.
出处
《大气科学》
CSCD
北大核心
1992年第1期84-91,共8页
Chinese Journal of Atmospheric Sciences
关键词
耗散结构
大气
熵平衡方程
对流运动
降水
Dissipative structure
Entropy equilibrium equation
Excess entropy production
Convective motion.
