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ボーリング・アレルード以前の急激な温暖化と深海の循環の変化
Nivedita Thiagarajan1, Adam V Subhas1, John R Southon2
1Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, California 91125, USA.
Nature
|July 4, 2014
まとめ
深海の熱放出は北半球の急激な温暖化を引き起こし,大西洋循環は最後の脱氷期中に再開した. この発見は,過去の気候ダイナミクスと海洋気候のフィードバックに関する私たちの理解を再構築します.
科学分野:
- パレオセアノグラフィー
- 気候科学 気候科学
- 海洋地質学 海洋地質学
背景:
- 最後の脱氷は,北半球の温暖化や海洋循環の変化を含む急速な気候変動を特徴づけたが,その原因については議論が続いている.
- Bølling-Allerødの温暖化と大西洋南部転覆循環 (AMOC) の再起動は重要なイベントですが,そのトリガーは完全に理解されていません.
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