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A desert is a landscape or region that receives an extremely low amount of precipitation, less than enough to support growth of most plants. Deserts are defined as areas with an average annual precipitation of less than 250 millimetres (10 in) per year,[1][2] or as areas where more water is lost by evapotranspiration than falls as precipitation.[3] In the Köppen climate classification system, deserts are classed as BWh (hot desert) or BWk (temperate desert). In the Thornthwaite climate classification system, deserts would be classified as arid megathermal climates.[4][5]

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  1. "What is a desert?". Pubs.usgs.gov. http://pubs.usgs.gov/gip/deserts/what/. Retrieved 2010-10-16. 
  2. According to What is a desert?, the 250 mm threshold definition is attributed to Peveril Meigs.
  3. "desert". Encyclopædia Britannica online. http://www.britannica.com/eb/article-70815/desert. Retrieved 2008-02-09. 
  4. Fredlund, D.G.; Rahardjo, H. (1993) (PDF). Soil Mechanics for Unsaturated Soils. Wiley-Interscience. ISBN 978-0471850083. http://www.soilvision.com/subdomains/unsaturatedsoil.com/Docs/chapter1UST.pdf. Retrieved 2008-05-21. 
  5. Glossary of Meteorology. Megathermal Climate. Retrieved on 2008-05-21.
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