Droxtal: Difference between revisions
From Glossary of Meteorology
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<div class="definition"><div class="short_definition">A tiny [[ice]] particle, about 10–20 μm in diameter, formed by direct [[freezing]] of [[supercooled water]] droplets with little growth directly from the [[vapor]].</div><br/> <div class="paragraph">The term combines the words [[drop]] and [[crystal]]. Droxtals cause most of the [[visibility]] reduction in [[ice fog]].</div><br/> </div> | <div class="definition"><div class="short_definition">A tiny [[ice]] particle, about 10–20 μm in diameter, formed by direct [[freezing]] of [[supercooled water|supercooled water]] droplets with little growth directly from the [[vapor]].</div><br/> <div class="paragraph">The term combines the words [[drop]] and [[crystal]]. Droxtals cause most of the [[visibility]] reduction in [[ice fog]].</div><br/> </div> | ||
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Latest revision as of 15:50, 25 April 2012
droxtal
A tiny ice particle, about 10–20 μm in diameter, formed by direct freezing of supercooled water droplets with little growth directly from the vapor.
The term combines the words drop and crystal. Droxtals cause most of the visibility reduction in ice fog.
