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Evolution of Staircase Structures in Diffusive Convection
Published on: September 5, 2018
在最后的冰川最大期,大西洋深水的逆流
César Negre1, Rainer Zahn, Alexander L Thomas
1Institut de Ciència i Tecnologia Ambientals (ICTA), Universitat Autònoma de Barcelona, 08193 Bellaterra, Spain. cesar@negre.us
Nature
|November 5, 2010
概括
大西洋南部翻转循环 (MOC) 可能在最后的冰川最大期逆转,深水从南大洋流向北,与今天的模式不同.
科学领域:
- 古海洋学是古海洋学.
- 气候科学 气候科学
- 海洋学 海洋学 海洋学
背景情况:
- 大西洋南部翻转循环 (MOC) 对全球气候至关重要,重新分配热量并通风深海.
- 过去的MOC行为,特别是在最后的冰川最大期,是有争议的,有来自代理人的相互矛盾的证据.
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