Pancake ice: Difference between revisions

From Glossary of Meteorology
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|Meaning=Roughly circular accumulations of [[frazil ice]], usually less than about 3 m in diameter,  with raised rims caused by collisions.
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|Explanation=This form of [[ice]] is common in the Antarctic. Pancake ice may develop from [[grease ice]] or  [[shuga]].
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== pancake ice ==
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<div class="definition"><div class="short_definition">Roughly circular accumulations of [[frazil ice]], usually less than about 3 m in diameter,  with raised rims caused by collisions.</div><br/> <div class="paragraph">This form of [[ice]] is common in the Antarctic. Pancake ice may develop from [[grease ice]] or  [[shuga]].</div><br/> </div>
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Latest revision as of 01:54, 29 March 2024

Roughly circular accumulations of frazil ice, usually less than about 3 m in diameter, with raised rims caused by collisions.

This form of ice is common in the Antarctic. Pancake ice may develop from grease ice or shuga.

Roughly circular accumulations of frazil ice, usually less than about 3 m in diameter, with raised rims caused by collisions.

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