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Atmospheric Chemistry and Physics An interactive open-access journal of the European Geosciences Union
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Volume 13, issue 19
Atmos. Chem. Phys., 13, 10081-10094, 2013
https://doi.org/10.5194/acp-13-10081-2013
© Author(s) 2013. This work is distributed under
the Creative Commons Attribution 3.0 License.
Atmos. Chem. Phys., 13, 10081-10094, 2013
https://doi.org/10.5194/acp-13-10081-2013
© Author(s) 2013. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 14 Oct 2013

Research article | 14 Oct 2013

Expansion of global drylands under a warming climate

S. Feng2,1,* and Q. Fu3,1 S. Feng and Q. Fu
  • 1Key Laboratory of Western China's Environmental Systems & College of Atmospheric Sciences, Lanzhou University, China
  • 2School of Natural Resources, University of Nebraska-Lincoln, Lincoln, NE, USA
  • 3Department of Atmospheric Sciences, University of Washington, Seattle, WA, USA
  • *current address: Department of Geosciences, University of Arkansas, Fayetteville, AR, USA

Abstract. Global drylands encompassing hyper-arid, arid, semiarid, and dry subhumid areas cover about 41 percent of the earth's terrestrial surface and are home to more than a third of the world's population. By analyzing observations for 1948–2008 and climate model simulations for 1948–2100, we show that global drylands have expanded in the last sixty years and will continue to expand in the 21st~century. By the end of this century, the world's drylands (under a high greenhouse gas emission scenario) are projected to be 5.8 × 106 km2 (or 10%) larger than in the 1961–1990 climatology. The major expansion of arid regions will occur over southwest North America, the northern fringe of Africa, southern Africa, and Australia, while major expansions of semiarid regions will occur over the north side of the Mediterranean, southern Africa, and North and South America. The global dryland expansions will increase the population affected by water scarcity and land degradations.

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