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大西洋化推动了最近北极的加强,颠覆了循环
Marius Årthun1, Ailin Brakstad1, Jakob Dörr1
1Geophysical Institute, University of Bergen, and Bjerknes Centre for Climate Research, Bergen, Norway.
Science advances
|July 11, 2025
概括
大西洋变暖的水域正在将北冰洋的循环转向极地,增强北极内部的密集水形成. 这加强了北极翻转循环,保持了稳定的密集水运输到大西洋南部翻转循环,尽管气候变化.
科学领域:
- 海洋学 海洋学 海洋学
- 气候科学 气候科学
- 北极研究研究北极研究
背景情况:
- 北极洋对于通过大西洋南部翻转循环 (AMOC) 的全球海洋循环至关重要.
- 快速的北极气候变化引发了关于北冰洋翻转循环的稳定性的问题.
- 大西洋化,即温暖的大西洋水域的涌入,正在改变北极的条件.
研究的目的:
- 为了调查大西洋化对北冰洋翻转循环的影响.
- 为了确定密度较高的水源地区在北极地区的变化.
- 评估北方翻转循环在气候变化下的弹性.
主要方法:
- 使用了高分辨率的海洋再分析数据集.
- 与观察数据相符的重新分析结果.
- 从1993年到2020年分析了水质转换和循环模式的变化.
主要成果:
- 由于大西洋化,在密集的水源地区观察到极向转移.
- 记录了北冰洋内的增强的地表水质量转变.
- 发现北极的变化补偿了北欧海的变化减少.
- 检测到北冰洋的强化颠覆循环.
结论:
- 北极洋翻转的循环已经显示出对气候变化的弹性.
- 大西洋化导致了密集水形成的极向转移.
- 保持密集溢出水的稳定运输到AMOC的下肢.
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