Winds whose direction is reversed from one season to the other are called the
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The winds whose direction is reversed from one season to another are called monsoons. Monsoons are characterized by seasonal reversal of wind direction, which are caused by differential heating and cooling of land and water surfaces. During summer, the land gets heated more than the ocean, causing a low-pressure zone over the land and high-pressure zone over the ocean, which leads to moisture-laden winds blowing from the ocean towards the land. In winter, the opposite occurs due to the reversal of the pressure gradient, causing the dry winds to blow from the land towards the ocean. This phenomenon is most commonly observed in South and Southeast Asia.