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Flaw lead : ウィキペディア英語版
Flaw lead
Flaw lead is an oceanographic term for a waterway opening between pack ice and fast ice.〔(【引用サイトリンク】title=Lead )〕 Flaw lead occurs annually at the time when central pack ice drifts from coastal ice, thereby creating the flaw. The process begins in autumn. Flaw leads can have interconnected polynyas. The Canadian government's Circumpolar Flaw Lead System Study, through the University of Manitoba examines the physical changes and their effects on biological processes with flaw leads.
A similar opening ("lead") can exist between pack ice and the shore, referred to as a shore lead.〔

==References==


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「Flaw lead」の詳細全文を読む



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