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desert climate

Also known as: BW climate, arid climate

Quick Summary

A desert climate is characterized by a severe lack of available moisture for plants, resulting from an imbalance between precipitation and evapotranspiration. This aridity is often exacerbated by low humidity, high temperatures, and wind. Most deserts are located in subtropical regions, typically between 15° and 30° latitude, under descending dry air masses associated with subtropical high-pressure cells.123

While often pictured as sandy and hot, deserts can also be cold. Precipitation is minimal, often less than 10 inches (250 mm) annually, and can be highly unreliable, with years passing without rain in some areas. Despite the harsh conditions, deserts support unique ecosystems with specially adapted plants and animals. Desertification, the degradation of land in arid areas, is an ongoing environmental concern.1345

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