摘要
本文在前人工作的基础上,根据梯度风原理和大气热力学原理,采用了不同的物理量进行分析,对原划分的季风区域作了科学的合理的修正。分析结果使我们对季风的成因、季风天气的影响有了进一步的认识和了解,且对东亚季风和印度季风的性质差异也更清楚了。
In this article,a great amount of materials including different physical values of thermody-namics for atmosphere have been analysed in order to make a monsoon regionization on betterscientific basis.As a result,our understanding of the monsoon formation and its impacts onweather has been improved and the distinctions of East Asian monsoons from the Indian ones alsobecome clearer.