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在最后一个间冰期期间的冰量和海平面
1Research School of Earth Sciences, The Australian National University, 1 Mills Road, Canberra, ACT 0200, Australia. adutton@ufl.edu
概括
全球海平面在最后一个冰河间时期显著上升,这表明冰盖对气候变化的敏感性更大. 这表明,即使是微小的变暖也可能导致海平面大幅上升.
科学领域:
- 古气候学 古气候学
- 冰川学的冰川学
- 海平面研究的研究.
背景情况:
- 在最后一个冰河间时期 (大约125,000年前),海平面大幅上升.
- 在此期间,人们对西南极洲冰盖动态一直感兴趣.
- 地理多样化的地点显示了海平面峰值观测的变化.
研究的目的:
- 为了评估最近的冰河间海平面观测.
- 提供一个内部一致的珊瑚U-Th年龄数据库.
- 评估海平面数据在静态建模和地平面学证据的背景下.
主要方法:
- 珊瑚U-Th年龄的汇编.
- 同静态建模. 静态建模.
- 分析地平线图证据. 分析地平线图证据.
主要成果:
- 全球海平面高于当前水平5.5至9米.
- 与今天相比,在格陵兰岛和南极洲的冰盖较小.
- 海平面对辐射强迫变化具有很高的敏感性.
结论:
- 西南极洲的冰盖在最后一个冰河间时期可能并没有完全崩.
- 过去的海平面上升表明,冰盖对气候强迫的反应很大.
- 了解过去的海平面变化对于预测未来的冰盖行为和海平面上升至关重要.
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