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Science (New York, N.Y.)
|April 1, 1977
PubMed
まとめ

デボン島の氷の核の溶けた層は,1925年以来の温暖化傾向を明らかにし,北極の氷河と海氷に影響を与えています. この古気候データは,より暖かい夏が,北西経路の探検のような歴史的探検に影響を与えたことを示唆しています.

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