西

L G Henry1, J F McManus2, W B Curry3

  • 1Lamont-Doherty Earth Observatory (LDEO), Columbia University, Palisades, NY 10964, USA. lhenry@ldeo.columbia.edu.

Science (New York, N.Y.)
|July 2, 2016
PubMed
まとめ

海洋循環の変化は 最後の氷河期に 急速な気候変動を引き起こしました 大西洋の転覆循環の減少は 寒冷期と一致し 循環の強化は 温暖化をもたらし 氷河期の急激な気候変動における 海の重要な役割を強調しました

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