Condensation temperature: Difference between revisions
From Glossary of Meteorology
imported>Perlwikibot No edit summary |
imported>Perlwikibot No edit summary |
||
| Line 9: | Line 9: | ||
</div> | </div> | ||
<div class="definition"><div class="short_definition">(''Also called'' adiabatic saturation temperature, adiabatic condensation temperature, saturation temperature.) The [[temperature]] at which a [[parcel]] of moist unsaturated air expanded [[dry-adiabatically]] reaches [[saturation]].</div><br/> <div class="paragraph"><br/>''See'' [[condensation pressure]], [[lifting condensation level]].</div><br/> </div> | <div class="definition"><div class="short_definition">(''Also called'' adiabatic saturation temperature, adiabatic condensation temperature, saturation temperature.) The [[temperature]] at which a [[parcel]] of moist unsaturated air expanded [[dry-adiabatic process|dry-adiabatically]] reaches [[saturation]].</div><br/> <div class="paragraph"><br/>''See'' [[condensation pressure]], [[lifting condensation level]].</div><br/> </div> | ||
</div> | </div> | ||
Latest revision as of 15:40, 25 April 2012
condensation temperature[edit | edit source]
(Also called adiabatic saturation temperature, adiabatic condensation temperature, saturation temperature.) The temperature at which a parcel of moist unsaturated air expanded dry-adiabatically reaches saturation.
