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A seasonally reversing wind, often referred to as a monsoon, is a wind pattern that changes direction with the seasons, typically influenced by shifts in temperature and pressure between land and ocean. During the summer, these winds usually blow from the ocean to land, bringing moisture and rainfall, while in winter, they reverse direction, blowing from land to ocean, leading to drier conditions. This phenomenon is most commonly associated with regions in South Asia and parts of Africa, where it significantly impacts local climate and agriculture.

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