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在最后一次冰川过渡期间的全球平均海洋温度
Bernhard Bereiter1,2,3, Sarah Shackleton1, Daniel Baggenstos1,2
1Scripps Institution of Oceanography, University of California San Diego, La Jolla, California 92037, USA.
Nature
|January 5, 2018
概括
海洋温度在最后一个冰川过渡期间显著上升. 这项研究利用冰核的高贵气体重建了全球海洋温度变化超过1万年.
科学领域:
- 古气候学
- 海洋学
- 气候科学
背景情况:
- 关于海洋温度对气候变化的长期反应的数据有限.
- 海洋在长期吸收人为热量的作用仍然不确定.
研究的目的:
- 通过高精度和时间分辨率重建过去的全球海洋温度.
- 调查海洋温度,南极温度和大气二氧化碳水平之间的关系.
- 分析地球气候历史中的突然变暖事件.
主要方法:
- 在冰核中保存的贵重气体用于古气候重建.
- 开发了一种用于估计全球海洋温度的新方法.
- 与南极温度和大气二氧化碳记录相关的海洋温度数据.
主要成果:
- 全球海洋温度从2万到1万年前增加了2.57±0.24°C.
- 海洋温度与南极温度密切相关,与大气二氧化碳相比没有领先或滞后.
- 鉴定了年轻干旱时期的700年变暖事件, 超过了现代海洋吸收热量的估计.
结论:
- 南半球气候显著影响全球气候趋势.
- 冰核中的高贵气体分析为全球海洋温度重建提供了强有力的方法.
- 过去海洋的突然变暖事件是显著的,
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