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dry adiabatic lapse rate

A Dictionary of Ecology | 2004 | 269 words | Copyright

dry adiabatic lapse rate The rate at which dry (i.e. unsaturated) air cools when rising adiabatically through the atmosphere as a result of the utilization of energy in expansion. It is 9.8°C/km. See also instability; saturated adiabatic lapse rate; and stability.

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MICHAEL ALLABY. "dry adiabatic lapse rate." A Dictionary of Ecology. 2004. Encyclopedia.com. 28 May. 2012 <http://www.encyclopedia.com>.

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