グリーンランド - スコットランド山脈の横断の溢出の観測およびモデルの安定性
Steffen M Olsen1, Bogi Hansen, Detlef Quadfasel
1Danish Meteorological Institute, Lyngbyvej 100, 2100 Copenhagen, Denmark. smo@dmi.dk
Nature
|September 27, 2008
まとめ
北欧海から大西洋への冷水溢出は,気候変動の予測に反して,大きな傾向を示していない. この研究では,1948年から2005年にかけてのフェロー・バンク・チャネル・オーバーフローデータを分析した.
科学分野:
- 海洋学 海洋学 海洋学
- 気候科学 気候科学
背景:
- グリーンランド・スコットランド・リッジは,北欧の海から大西洋に冷たい,密度の高い水の流れを容易にする.
- このオーバーフローは北大西洋の深水形成と大西洋南極転覆循環 (AMOC) に極めて重要です.
- 気候変動の予測は,AMOCの潜在的弱体化を示唆している.
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