Wet-bulb potential temperature: Difference between revisions
From Glossary of Meteorology
imported>Perlwikibot (Created page with " {{TermHeader}} {{TermSearch}} <div class="termentry"> <div class="term"> == wet-bulb potential temperature == </div> <div class="definition"><div class="short_definiti...") |
imported>Perlwikibot No edit summary |
||
Line 9: | Line 9: | ||
</div> | </div> | ||
<div class="definition"><div class="short_definition">( | <div class="definition"><div class="short_definition">(''Also called'' pseudo wet-bulb potential temperature.) The [[temperature]] an [[air parcel]] would have if cooled from its initial state adiabatically to [[saturation]], and thence brought to 1000 mb by a [[moist-adiabatic process]].</div><br/> <div class="paragraph">This temperature is conservative with respect to reversible adiabatic changes.</div><br/> </div> | ||
</div> | </div> | ||
Latest revision as of 15:28, 20 February 2012
wet-bulb potential temperature
(Also called pseudo wet-bulb potential temperature.) The temperature an air parcel would have if cooled from its initial state adiabatically to saturation, and thence brought to 1000 mb by a moist-adiabatic process.
This temperature is conservative with respect to reversible adiabatic changes.