19,000年前の海面の急速な上昇とその世界的な影響
Peter U Clark1, A Marshall McCabe, Alan C Mix
1Department of Geosciences, Oregon State University, Corvallis, OR 97331, USA. clarkp@geo.oregonstate.edu
まとめ
19,000年前,北半球の氷床から発生した海面上昇または融水パルスが顕著でした. この現象により北大西洋は冷却され,熱帯と南半球は温暖化しました.
科学分野:
- 古代気候学 (paleoclimatology) とは,古代気候学 (paleoclimatology) とは,古代気候学 (paleoclimatology) とは,古代気候学 (paleoclimatology) とは,古代気候学 (paleoclimatology) とは
- 海洋学 海洋学とは
- 氷河学 氷河学とは
背景:
- 脱氷期における海面の変化と気候の動態は,地球の気候システムを理解する上で極めて重要です.
- 北半球の氷床が突然の気候変化に果たす役割については,さらなる調査が必要である.
研究 の 目的:
- 現在より約1万9000年前の急激な海面上昇のタイミングと発生源を調査する (B.P. ) を実施する.
- この融水パルスに対する世界的な気候反応を駆動するメカニズムを解明する.
主な方法:
- アイルランド海流域からの証拠の分析.
- 北大西洋の深水形成と海洋温度を含む気候記録の調査.
主要な成果:
- 証拠は,海面の急激な上昇 (融水パルス) が19,000 B.P.年に起こったことを支持しています. アイルランド海流域に存在する.
- 北大西洋の深水形成の減少と北大西洋の冷却は,融水パルスと一致しました.
- 熱帯の大西洋,太平洋,南半球で同時に温暖化が発生した.
結論:
- 融水パルスは北半球の氷床から発生した可能性が高い.
- この研究は,氷河解凍の気候シグナルを世界的に拡散するメカニズムを特定し,北半球の冷却と南半球の温暖化を説明する.
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