Snow stage: Difference between revisions
From Glossary of Meteorology
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<div class="definition"><div class="short_definition">Part of an obsolete conceptual [[model]] of [[air parcel]] ascent referring to conditions under which the [[condensation level]] is at a [[temperature]] below [[freezing]] and it is assumed that all condensed [[vapor]] immediately freezes.</div><br/> <div class="paragraph">Other portions of the ascent were described as the [[dry stage]], the [[rain stage]], and the [[hail stage.]]</div><br/> </div> | <div class="definition"><div class="short_definition">Part of an obsolete conceptual [[model]] of [[air parcel]] ascent referring to conditions under which the [[condensation level]] is at a [[temperature]] below [[freezing]] and it is assumed that all condensed [[vapor]] immediately freezes.</div><br/> <div class="paragraph">Other portions of the ascent were described as the [[dry stage]], the [[rain stage]], and the [[hail stage|hail stage.]]</div><br/> </div> | ||
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Latest revision as of 17:54, 25 April 2012
snow stage
Part of an obsolete conceptual model of air parcel ascent referring to conditions under which the condensation level is at a temperature below freezing and it is assumed that all condensed vapor immediately freezes.