Explanation:
Tropical deserts form due to a combination of factors, including subtropical high pressure (descending dry air), cold ocean currents (which stabilize the atmosphere), and rain shadow effects from nearby mountains.
Explanation:
A negative IOD (warmer waters in the eastern Indian Ocean) is generally associated with a weaker Southwest Monsoon and reduced rainfall in India.
Explanation:
Valley fog forms in mountain valleys due to temperature inversions, where cold, dense air settles in the valley, and radiation fog forms in the cooler air.
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