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Cirrocumulus castellanus : ウィキペディア英語版 | Cirrocumulus castellanus
Cirrocumulus castellanus is a type of cirrocumulus cloud. The name ''cirrocumulus catellanus'' is derived from Latin, meaning "of a castle".〔(【引用サイトリンク】url=http://latinlexicon.org/definition.php?p1=1002184 )〕 These clouds appear as round turrets that are rising from either a lowered line or sheet of clouds. Cirrocumulus castellanus is an indicator of atmospheric instability at the level of the cloud. The clouds form when condensation occurs in the base cloud, causing latent heating to occur. This causes air to rise from the base cloud, and if the air ascends into conditionally unstable air, cirrocumulus castellanus will form. ==See also==
*List of cloud types
抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)』 ■ウィキペディアで「Cirrocumulus castellanus」の詳細全文を読む
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