Anafront: Difference between revisions
From Glossary of Meteorology
m (Rewrite with Template:Term and clean up) |
m (Rewrite with Template:Term and clean up) |
||
| Line 3: | Line 3: | ||
|Definitions={{Definition | |Definitions={{Definition | ||
|Num=1 | |Num=1 | ||
|Meaning= | |Meaning=A [[front]] at which the warm air is ascending the [[frontal surface]] up to high altitudes. | ||
A [[front]] at which the warm air is ascending the [[frontal surface]] up to high altitudes. | |Explanation=With anafronts, [[precipitation]] may occur to the rear of the front and is sometimes associated with [[cyclogenesis]]. <br/>''Compare'' [[katafront]]. | ||
}} | }} | ||
}} | }} | ||
Latest revision as of 21:21, 13 January 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.
