摘要
任何地点的降水量可能来自地球的任何地点的水分蒸发。为了定量描述大气中的这种水分循环的复杂过程,我们引入了两个概念性的工具:大气水分辐合函数和大气水分辐散函数,并且建立了用它们描述大气水分循环的方程组。
The precipitation at any place of the world may come from any water evaporation that happened at any part of the globe. In order to describe the complicated process of the water circulation in the atmosphere quantitatively, two conceptual tools, the water convergent function and the water divergent function in the atmosphere, are introduced; and an equation system, which can be used to describe the water circulation in the atmosphere, has been found.
出处
《高原气象》
CSCD
北大核心
2006年第2期190-194,共5页
Plateau Meteorology
基金
科技部科技公益研究专项(2004DIB3J118)资助
关键词
大气水分循环
大气水分循环方程
Atmospheric water circulation
Atmospheric water circulation equation