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saturation-adiabatic process |
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saturation-adiabatic process [‚sach·ə′rā·shən ¦ad·ē·ə¦bad·ik ′prä·səs] (meteorology) An adiabatic process in which the air is maintained at saturation by the evaporation or condensation of water substance, the latent heat being supplied by or to the air respectively; the ascent of cloudy air, for example, is often assumed to be such a process. How to thank TFD for its existence? Tell a friend about us, add a link to this page, add the site to iGoogle, or visit webmaster's page for free fun content. |
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