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在海洋 - 大气 - 冰层系统模型中,冰川气候的不稳定性
Andreas Schmittner1, Masakazu Yoshimori, Andrew J Weaver
1School of Earth and Ocean Sciences, University of Victoria, Post Office Box 3055, Victoria, BC V8W 3P6, Canada. andreas@ocean.seos.uvic.ca
概括
在冰川时期,大西洋洋流和冰盖之间的水文相互作用导致了突然的变暖事件. 这项研究解释了在最后一个冰河时代观察到的气候变化.
科学领域:
- 古气候学 古气候学
- 气候动力学 气候动力学
- 海洋学 海洋学 海洋学
背景情况:
- 过去1万年 (全新世纪) 的气候稳定,与冰川时期不同.
- 北大西洋冰川在寒冷 (阶段) 和温暖 (阶段间) 阶段之间经历了显著的气候变化.
研究的目的:
- 研究冰盖与海洋相互作用在冰川时期引发气候突然变化的作用.
- 了解限制温暖间期和破坏海洋循环稳定的机制.
主要方法:
- 利用气候建模研究来模拟相互作用.
- 专注于大西洋的热环流 (THC) 和大陆冰盖.
主要成果:
- 冰盖和大西洋THC之间的水文相互作用可以引发突然变暖事件.
- 这些相互作用限制了阶段间循环模式的持续时间.
- 在冰川条件下,THC对这些相互作用更敏感.
结论:
- 冰盖-海洋水文反提供了突然冰川变暖的机制.
- 这些反解释了在冰川时期观察到的气候变化增加.
- 这项研究强调了大西洋THC对冰川边界条件的敏感性.
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