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南极洲和北大西洋的同步气候变化
1E. J. Steig, J. W. C. White, S. J. Lehman, Institute of Arctic and Alpine Research, University of Colorado, Boulder, CO 80309, USA. E. J. Brook, Department of Geology, Washington State University, Vancouver, WA 98686, USA. C. M. Sucher, Gradua.
概括
南极冰芯揭示了与北半球同步的气候变化,挑战了以前关于异步半球对突然气候变化事件的反应的概念.
科学领域:
- 古气候学 古气候学
- 冰川学的冰川学
- 海洋学 海洋学 海洋学
背景情况:
- 格陵兰岛的冰芯显示了10万年来气候的突然变化.
- 北大西洋深海核心证实了千年气候变化与海洋热环流之间的联系.
研究的目的:
- 为了调查南极气候记录,寻找北大西洋主要气候事件的证据.
- 为了比较南极的气候反应与北半球的气候反应.
主要方法:
- 来自泰勒圆顶的冰芯的分析,罗斯海西部,南极洲.
- 南极气候数据与现有的格陵兰岛和北大西洋记录进行比较.
主要成果:
- 泰勒圆顶冰芯记录了两个主要的北大西洋事件:冰河期末的变暖和波林/艾勒罗德-年轻德利亚斯振荡.
- 这种同步记录与在其他南极冰芯中观察到的异步反应形成鲜明对比.
结论:
- 北大西洋地区的突然气候变化反映在西南极洲.
- 这表明南极半球之间的气候系统比以前的一些南极记录所表明的更为结合.
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