Difference between revisions of "Warm cloud"

From Glossary of Meteorology
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<div class="definition"><div class="short_definition">Cloud that is only in the liquid [[phase]]; levels are not present with [[temperature]] below  0&deg;C (32&deg;F); no [[ice]] is present.</div><br/> <div class="paragraph">Any [[precipitation]] will originate from droplet [[coalescence]]. It is not to be confused with clouds  extending to levels with temperature below 0&deg;C; here, precipitation may form from the ice phase  but could form by the warm cloud coalescence process.</div><br/> </div>
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<div class="definition"><div class="short_definition">Cloud that is only in the liquid [[phase]]; levels are not present with [[temperature]] below  0&#x000b0;C (32&#x000b0;F); no [[ice]] is present.</div><br/> <div class="paragraph">Any [[precipitation]] will originate from droplet [[coalescence]]. It is not to be confused with clouds  extending to levels with temperature below 0&#x000b0;C; here, precipitation may form from the ice phase  but could form by the warm cloud coalescence process.</div><br/> </div>
 
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Latest revision as of 15:26, 20 February 2012



warm cloud

Cloud that is only in the liquid phase; levels are not present with temperature below 0°C (32°F); no ice is present.

Any precipitation will originate from droplet coalescence. It is not to be confused with clouds extending to levels with temperature below 0°C; here, precipitation may form from the ice phase but could form by the warm cloud coalescence process.