Inter-Tropical Convergence Zone (ITCZ)
The area where the trade winds from the Northern and Southern Hemisphere meet is known as the Intertropical Convergence Zone, or ITCZ. The equator’s warm water and bright sun heat the air in the ITCZ, increasing humidity and giving it a buoyant quality. As the air rises and cools, moisture that has accumulated in a seemingly endless cycle of thunderstorms is released. The wet and dry seasons in the tropics are caused by seasonal variations in the location of the ITCZ, which have a considerable impact on rainfall in many tropical countries. A catastrophic drought or flooding in the surrounding areas can be brought on by changes in the ITCZ over time.
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During the monsoon season, India’s climate is hot and muggy, similar to that of South and Southeast Asia. Two of the four seasons that exist in the Indian subcontinent are monsoon seasons. Those are Season of the Southwest Monsoon and The Monsoon Season in the North-East.
The Arabic term mausin or the Malayan word monsin, both of which indicate season, are the origins of the name monsoon. Seasonal winds (rhythmic wind movements) (periodic winds) that change direction with the seasons are known as monsoons. A seasonal wind pattern known as the monsoon moves from the sea to land in the summer and from the land to the sea in the winter. According to some academics, monsoon winds are significant land and sea breezes.
Inter-Tropical Convergence Zone (ITCZ) is one of the important facts to understand the mechanism of the monsoons.
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