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在最后一次除冰期期间,海洋和大气中的同步百年突然事件
Tianyu Chen1, Laura F Robinson2, Andrea Burke3
1Bristol Isotope Group, School of Earth Sciences, University of Bristol, Bristol, UK. tc14502@bristol.ac.uk.
概括
海洋循环的变化导致了上一次脱冰期间大气二氧化碳的快速增加. 来自深海珊瑚的放射性碳数据揭示了两个与更强大的大西洋循环有关的"超越"事件,影响了气候变化.
科学领域:
- 古气候学 古气候学
- 海洋学 海洋学 海洋学
- 气候科学 气候科学
背景情况:
- 南极冰芯显示,在最后一次脱冰过程 (18,00011,000年前) 中,二氧化碳迅速增加.
- 了解海洋循环的作用需要高分辨率的海洋记录.
研究的目的:
- 为了研究海洋循环和大气二氧化碳在最后一次脱冰期间的变化之间的联系.
- 为了确定海洋循环变化的时间和性质.
主要方法:
- 在赤道大西洋和德雷克海峡的深海珊瑚的放射性碳测年.
- 在过去的25,000年里,与的约会对年龄进行了准确的控制.
主要成果:
- 检测到两个显著的放射性碳转移,与百年CO2上升的14.8k和11.7k年前相吻合.
- 这些变化表明短暂 (<500年) 的海洋循环"超越"事件.
- 大西洋南部翻转循环在这些事件中比现在更强.
结论:
- 海洋循环和百年气候事件在最后一次脱冰期间紧密联系在一起.
- 有证据表明,海洋循环动态在气候突然变化中起着重要作用.
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