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北大西洋循环和最后一次冰河时期的气候突然变化
L G Henry1, J F McManus2, W B Curry3
1Lamont-Doherty Earth Observatory (LDEO), Columbia University, Palisades, NY 10964, USA. lhenry@ldeo.columbia.edu.
概括
海洋循环的变化导致了最后一个冰河时期的快速气候变化. 降低大西洋翻转循环与寒冷时期相吻合,而更强的循环带来了变暖,凸显了海洋在冰川气候突然变化中的关键作用.
科学领域:
- 古气候学
- 海洋学
- 气候科学
背景情况:
- 最后一个冰河时代的特点是快速的,异步的气候波动的起源尚未解决.
- 海洋热传输变化可能导致这些气候变化,特别是在海洋同位素阶段3 (25-60万年前).
研究的目的:
- 研究海洋循环在海洋同位素第三阶段突然的冰川气候变化中的作用.
- 重建北大西洋的高分辨率气候和海洋循环动态.
主要方法:
- 对北大西洋深层沉积物的分析.
- 采用高分辨率的替代物:/ (Pa/Th) 用于动态追踪和表层 δ(13) C 用于深水质的识别.
主要成果:
- 在每一个凉爽的北方季节中都观察到大西洋翻转循环的减少.
- 在哈德逊海峡的冰山排放过程中,流量减少最为显著.
- 北部地区的急剧变暖事件随之而来,
结论:
- 提供了海洋在突然的冰川气候变化中的持续和核心作用的直接证据.
- 将北大西洋循环动态与最后一个冰河时代的快速气候变化联系起来.
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