Orographic fog: Difference between revisions
From Glossary of Meteorology
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<div class="definition"><div class="short_definition">[[Fog]] formed as [[moist air]] blows up a mountain slope and becomes saturated.</div><br/> <div class="paragraph">Flow can result from large-scale upslope winds or thermally forced upslope ([[anabatic]]) winds. <br/>''See'' [[anabatic wind]], [[orographic cloud]].</div><br/> </div> | <div class="definition"><div class="short_definition">[[fog|Fog]] formed as [[moist air]] blows up a mountain slope and becomes saturated.</div><br/> <div class="paragraph">Flow can result from large-scale upslope winds or thermally forced upslope ([[anabatic]]) winds. <br/>''See'' [[anabatic wind]], [[orographic cloud]].</div><br/> </div> | ||
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Latest revision as of 16:33, 25 April 2012
orographic fog
Flow can result from large-scale upslope winds or thermally forced upslope (anabatic) winds.
See anabatic wind, orographic cloud.
See anabatic wind, orographic cloud.
