S. Handayani
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引用次数: 18

摘要

陆地和水的不同加热和冷却在印度大陆上产生了低压,而周围的海洋则经历了相对较高的压力。夏季在恒河平原上空的热带辐合带(ITCZ)的位置变化(这是赤道槽,通常位于赤道5°N左右)。在季风季节,它也被称为季风槽。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Monsoon
The differential heating and cooling of land and water creates a low pressure on the landmass of India while the seas around experience comparatively high pressure. The shift of the position of Inter Tropical Convergence Zone (ITCZ) in summer, over the Ganga plain (this is the equatorial trough normally positioned about 5°N of the equator. It is also known as the monsoon-trough during the monsoon season).
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