在格陵兰 - 苏格兰山脊上观测和建模的溢出稳定性
Steffen M Olsen1, Bogi Hansen, Detlef Quadfasel
1Danish Meteorological Institute, Lyngbyvej 100, 2100 Copenhagen, Denmark. smo@dmi.dk
Nature
|September 27, 2008
概括
与气候变化预测相反,从北欧海到大西洋的冷水溢出没有显著的趋势. 这项研究分析了法罗银行1948-2005年的道溢出数据.
科学领域:
- 海洋学 海洋学 海洋学
- 气候科学 气候科学
背景情况:
- 格陵兰岛-苏格兰山脊促进了北欧海洋从北欧海洋涌入大西洋的冷,密集的水流.
- 这种溢出对北大西洋深水形成和大西洋南部翻转循环 (AMOC) 至关重要.
- 气候变化预测表明AMOC的潜在削弱.
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