Temperature plays a crucial role in controlling monsoon winds by creating differential heating between land and ocean. During summer, the land heats up faster than the surrounding water, leading to lower pressure over the land and higher pressure over the ocean. This pressure difference drives moist air from the ocean toward the land, resulting in the characteristic heavy rains of the monsoon season. Conversely, during winter, the land cools down more rapidly, reversing the pressure dynamics and leading to dry conditions.
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