Trade winds are global wind belts, not local winds. Chinook, Loo, and Sirocco are local or regional winds. Trade winds are part of the Earth's global circulation and blow from the subtropics towards the equator.
Explanation:
The Malabar Coast (Kerala) receives high rainfall due to the orographic effect of the Western Ghats, the Southwest Monsoon, and convection.
Explanation:
The leeward side of the Western Ghats receives low rainfall due to the rain shadow effect, creating semi-arid conditions in the Deccan Plateau.
Explanation:
During a La Niña event, the Walker Circulation strengthens as the trade winds intensify, pushing warm water further westward in the Pacific. This often results in heavy rainfall in Southeast Asia and Australia.
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