Anafront: Difference between revisions

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Revision as of 16:25, 26 January 2012



anafront[edit | edit source]

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.


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

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