Anafront: Difference between revisions

From Glossary of Meteorology
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|Meaning=A [[front]] at which the warm air is ascending the [[frontal surface]] up to high altitudes.
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|Explanation=With anafronts, [[precipitation]] may occur to the rear of the front and is sometimes associated  with [[cyclogenesis]]. <br/>''Compare'' [[katafront]].
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== anafront ==
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<div class="definition"><div class="short_definition">A [[front]] at which the warm air is ascending the [[frontal surface]] up to high altitudes.</div><br/> <div class="paragraph">With anafronts, [[precipitation]] may occur to the rear of the front and is sometimes associated  with [[cyclogenesis]]. <br/>''Compare'' [[katafront]].</div><br/> </div>
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Latest revision as of 22:26, 27 March 2024

A front at which the warm air is ascending the frontal surface up to high altitudes.

With anafronts, precipitation may occur to the rear of the front and is sometimes associated with cyclogenesis.
Compare katafront.

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