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大西洋深海循环在最后一个冰川开始时突然减弱
Yuxin Zhou1,2,3,4, Jerry F McManus5,6, Celeste T Pallone5,6,7
1Lamont-Doherty Earth Observatory of Columbia University, Palisades, NY, USA. xiaoxin.yo@gmail.com.
Nature communications
|August 14, 2025
概括
研究人员发现了在最后一个冰川开始 (LGI) 期间,大西洋南部翻转循环 (AMOC) 减弱的证据. 这项研究强调了海洋循环.
科学领域:
- 古气候学和海洋学
- 季度气候动态 四季度气候动态
背景情况:
- 降冰和冰川开始是关键的气候转型,但冰川开始的理解较少.
- 大西洋南部翻转循环 (AMOC) 在最后一次脱冰期间发生了变化,模型表明在最后一次冰川开始 (LGI) 时出现了减弱,但证据不确定.
研究的目的:
- 调查LGI (113-119万年前) 期间AMOC变化的证据.
- 了解海洋循环在轨道强迫气候变化和大气二氧化碳变化中的作用.
主要方法:
- 分析了三种- (Pa/Th) 同位素记录.
- 使用来自北大西洋西部和中部的古海洋学代理来重建AMOC强度.
主要成果:
- 在LGI检测到AMOC的突然减弱.
- 重建的AMOC减弱幅度很大,接近但没有达到海因里希事件中断的严重程度.
结论:
- LGI是一个突然的时期,轨道迫使海洋循环变化.
- 在气候转型期间,海洋过程在引发大气二氧化碳变化方面发挥着至关重要的作用.
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