极地南大洋的脱冰分层
François Fripiat1,2, Daniel M Sigman3, Xuyuan E Ai2,3
1Department of Geosciences, Environment and Society, Université Libre de Bruxelles, Brussels 1050, Belgium.
概括
南极冰盖的融水影响了南洋流和全球气候. 这项研究揭示了南极融水如何加强海洋分层,影响深海通风,并可能在脱冰过程中推动双极气候变化.
科学领域:
- 古海洋学是古海洋学.
- 气候科学 气候科学
- 冰川学的冰川学
背景情况:
- 北方冰盖的融水影响大西洋循环,但南极冰盖对南洋翻转的影响还未得到充分研究.
- 南洋对于全球海洋通风和气候调节至关重要.
研究的目的:
- 调查南极冰盖 (AIS) 融化水对南洋在脱冰过程中颠覆循环的影响.
- 了解南极融水在深海通风和全球气候动态中的作用.
主要方法:
- 用二原子结合的同位素分析来重建过去的海洋条件.
- 整合古海洋学数据与现有的融水排放重建和气候模型模拟.
主要成果:
- 在降冰过程中,AIS融化增加了极地南极洋的密度分层.
- 淡水输入削弱了南大洋的下层翻转细胞,同时加强了上层细胞.
- 最强的分层是与北大西洋深水形成重新开始之前的Bølling-Allerød时期相吻合.
结论:
- 开放的南极海洋,不仅仅是极地,直接通风深海.
- 淡水驱动的分层和风驱动的上升增加了海洋流的重定向,加深了全球的火山岩.
- 两半球的极地海洋清新可能有助于脱冰期间的"双极摇摆"气候事件.
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