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The global spatial distribution of deserts primarily results from climatic factors, particularly the patterns of atmospheric circulation. Deserts are commonly found at approximately 30 degrees latitude, where descending air from high-pressure systems leads to arid conditions. Additionally, the rain shadow effect occurs when mountain ranges block moist air, causing dry regions on the leeward side. Lastly, cold ocean currents can contribute to desert formation by cooling coastal air and reducing humidity.

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