Which desert results from the Himalayas blocking moisture?

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The Gobi Desert results from the Himalayas blocking moisture due to a meteorological phenomenon known as the rain shadow effect. As moist air masses travel from the ocean towards the land, they encounter the towering heights of the Himalayas. When these air masses rise over the mountains, they cool and lose moisture in the form of precipitation. By the time the air descends on the other side of the Himalayas, it is much drier, leading to arid conditions found in the Gobi Desert.

This geographic situation creates limited vegetation and low rainfall in the Gobi, contributing to its classification as a desert. The location and elevation of the Himalayas play a significant role in shaping the climate in this region, creating the distinct arid environment of the Gobi. Other deserts listed are influenced by different geographical and climatic conditions, which do not involve the blocking of moisture by the Himalayas specifically.

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