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氷床の崩壊と海面上昇は,ボーリングの温暖化で14,600年前に起こりました
Pierre Deschamps1, Nicolas Durand, Edouard Bard
1CEREGE, UMR Aix-Marseille Université - CNRS - IRD - College de France, Technopole de l'Arbois, BP 80, 13545 Aix-en-Provence Cedex 4, France. deschamps@cerege.fr
Nature
|March 31, 2012
まとめ
最後の脱氷期は,14,650年から14,310年前の間,融水パルス1A (MWP-1A) と呼ばれる急速な海面上昇を特徴とした. 南半球の氷の融解に関連したこのイベントは,500年未満で海面が12メートル以上上昇した.
科学分野:
- パレオセアノグラフィーとパレオ気候学
- 氷床のダイナミクス
- 海水面再建工事について
背景:
- 過去の海平面記録は,気候変動に対する氷床の反応を理解するために不可欠です.
- この最後の脱氷期は,海面の大幅な変動によって特徴づけられ,その中には,急速に上昇した時期 (融水パルス1A,MWP-1A) が含まれていた.
- MWP-1Aのタイミング,規模,発生源については不確実性があり,急激な気候変動との関連を妨げています.
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