Moist Adiabatic Processes
Moist Adiabatic Processes is a thermodynamic process describing the behavior of saturated air parcels undergoing vertical displacement in the atmosphere, wherein temperature changes occur without external heat exchange but include latent heat release from condensation, distinguishing it from dry adiabatic processes by its dependence on moisture content and lower lapse rate.
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Saturated Adiabatic Processes
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Rik Leemans, Wolfgang Crämer · Helmholtz-Zentrum für Polar-und Meeresforschung (Alfred-Wegener-Institut) · 1991 · 656 citations · Full text
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NSF National Center for Atmospheric Research, United States
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NSF National Center for Atmospheric Research
Boulder, United States
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Massachusetts Institute of Technology
Cambridge, United States
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Colorado State University
Fort Collins, United States
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Centre National de la Recherche Scientifique
Paris, France
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University of Arizona
Tucson, United States
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University of Michigan
Ann Arbor, United States
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University of Washington
Seattle, United States
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NOAA Geophysical Fluid Dynamics Laboratory
Princeton, United States
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