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南洋の起源は,脱氷期間の大西洋熱ハリン循環の再開のためである

Gregor Knorr1, Gerrit Lohmann

  • 1Institut für Meteorologie, Universität Hamburg, Bundesstrasse 55, 20146 Hamburg, Germany. gregor.knorr@dkrz.de

Nature
|August 2, 2003
PubMed
まとめ

南洋の温暖化は,融水ではなく,脱氷の間に大西洋循環の強化を開始しました. この発見は,北半球と南半球の気候変化を調和させ,氷河期間の状態への帰還を説明しています.

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