Explanation:
A positive IOD (warmer waters in the western Indian Ocean) is generally associated with a stronger Southwest Monsoon and good rainfall in India.
Explanation:
Subtropical high-pressure belts are located at approximately 30° North and South latitude. These are regions of sinking air, creating arid and semi-arid climates such as deserts.
Explanation:
Rain shadow deserts form when mountains block moisture-laden winds from reaching the leeward side. As air rises over the mountains, it cools and releases precipitation on the windward side, leaving the leeward side dry.
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