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最後の氷河間期における氷の量と海面

A Dutton1, K Lambeck

  • 1Research School of Earth Sciences, The Australian National University, 1 Mills Road, Canberra, ACT 0200, Australia. adutton@ufl.edu

Science (New York, N.Y.)
|July 17, 2012
PubMed
まとめ

世界の海水位は,最後の氷河間期に大幅に上昇し,気候変化に対する氷床の感受性が高かったことを示しています. これは,わずかな温暖化でさえ,海面の大幅な上昇を引き起こす可能性があることを示唆しています.

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