How the monsoon works, and why India's climate varies so dramatically across its regions.
The monsoon arises from differential heating between the Indian landmass (heats up faster in summer) and the surrounding Indian Ocean, creating a low-pressure zone over land that draws in moisture-laden winds from the sea. The monsoon typically arrives at the Kerala coast around 1 June and gradually advances across the country.
Rainfall is highly uneven β areas like Mawsynram and Cherrapunji in Meghalaya receive some of the highest rainfall in the world due to orographic effects (moist winds forced upward by the hills), while regions like western Rajasthan remain arid, lying in the "rain shadow" or receiving winds that have already lost most of their moisture.
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