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Earth's major deserts are primarily located in regions where dry air descends, such as the subtropics, due to the Hadley cell circulation. Additionally, the presence of cold ocean currents can inhibit moisture-laden winds, contributing to arid conditions. Geographic features, like mountain ranges, can also create rain shadows, where one side receives ample precipitation while the other remains dry. Lastly, high-pressure systems often dominate these areas, leading to clear skies and minimal rainfall.

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