Condensation pressure: Difference between revisions
From Glossary of Meteorology
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<div class="definition"><div class="short_definition">(''Also called'' adiabatic saturation pressure, adiabatic condensation pressure.) The [[pressure]] at which a [[parcel]] of moist unsaturated air expanded [[dry-adiabatically]] reaches [[saturation]].</div><br/> <div class="paragraph"><br/>''See'' [[condensation temperature]], [[lifting condensation level]].</div><br/> </div> | <div class="definition"><div class="short_definition">(''Also called'' adiabatic saturation pressure, adiabatic condensation pressure.) The [[pressure]] at which a [[parcel]] of moist unsaturated air expanded [[dry-adiabatic process|dry-adiabatically]] reaches [[saturation]].</div><br/> <div class="paragraph"><br/>''See'' [[condensation temperature]], [[lifting condensation level]].</div><br/> </div> | ||
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Latest revision as of 15:40, 25 April 2012
condensation pressure[edit | edit source]
(Also called adiabatic saturation pressure, adiabatic condensation pressure.) The pressure at which a parcel of moist unsaturated air expanded dry-adiabatically reaches saturation.
