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Evaporation

Atmospheric Science:

Evaporation

This article has been reviewed by the following Topic Editor: Kevin Vranes

Evaporation can be defined as the process where liquid water, or any other liquid, is transformed into a gaseous state. In terms of water, evaporation requires that the humidity of the atmosphere be less than the evaporating surface (at 100% relative humidity there is no more evaporation). The evaporation process requires an input of energy from the environment. For example, the evaporation of one gram of water requires 600 calories of heat energy. The reverse process, a transformation from gas to liquid, is referred to as condensation. Condensation releases energy to the environment.

Citation

Michael Pidwirny (Lead Author);Kevin Vranes (Topic Editor) "Evaporation". In: Encyclopedia of Earth. Eds. Cutler J. Cleveland (Washington, D.C.: Environmental Information Coalition, National Council for Science and the Environment). [First published in the Encyclopedia of Earth March 12, 2007; Last revised Date May 22, 2011; Retrieved June 19, 2013 <http://www.eoearth.org/article/Evaporation?topic=49479>

The Author

Michael Pidwirny Michael Pidwirny studied Physical Geography at the University of Winnipeg and the University of Manitoba. He received his PhD from the Simon Fraser University in Burnaby, British Columbia in 1994. He currently is an Associate Professor of Physical Geography at the University of British Columbia, Okanagan Campus. Pidwirny’s research interests include climate change, the influence of land-use change on biodiversity, and the use of technology in education. He publishes regularly in encyclop ... (Full Bio)

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