ラブラドール海における異常なコンベクションと,過去150年の大西洋の転覆
David J R Thornalley1,2, Delia W Oppo3, Pablo Ortega4
1Department of Geography, University College London, London, UK. d.thornalley@cantab.net.
Nature
|April 13, 2018
まとめ
過去150年間,大西洋南極の転覆循環 (AMOC) は,氷の融解と淡水の流入により,異常に弱くなっています. 最近の変動は,この非典型的,弱まった状態で起こります.
科学分野:
- 古代海洋学
- 気候科学
- 海洋学
背景:
- アトランティック・メリディアン・オーバーターニング・サーキュレーション (AMOC) は,地球温暖化と炭素循環に不可欠です.
- 最近の観測は,AMOCの弱まる傾向を示しています.
- 限られた過去のデータは,長期のAMOCの変動性を理解することを妨げています.
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