罗恩冰原经历了最后一个冰河间
Eric W Wolff1, Robert Mulvaney2, Mackenzie M Grieman3
1Department of Earth Sciences, University of Cambridge, Cambridge, UK. ew428@cam.ac.uk.
Nature
|January 29, 2025
概括
在最后的冰河间期,西南极冰层 (WAIS) 可能在很大程度上保持完整,与一些海平面上升模型相反. 这一发现影响了未来的海平面预测,
科学领域:
- 古气候学
- 冰川学
- 海平面研究
背景情况:
- 西南极冰盖 (WAIS) 对过去海平面上升的贡献是不确定的.
- 最后一个冰河间时期 (LIG) 的海平面更高,这意味着南极冰块的损失很大.
- 南极洲和南大洋的温暖LIG条件类似于未来的气候预测.
研究的目的:
- 重建WAIS及其冰架的LIG范围.
- 提供LIG冰盖行为的观测约束.
- 重新评估LIG的海平面贡献和未来海平面上升的预测.
主要方法:
- 分析 Skytrain 冰上升的海盐数据.
- 来自同一冰核的水同位素数据的解释.
- 与现有的古气候模型和数据进行比较.
主要成果:
- 罗恩冰架在LIG的大部分地区都存在.
- WAIS的退缩发生了,但可能不是完全失去冰架的程度.
- 观察到的LIG WAIS范围与预测极大冰损失的模型不一致.
结论:
- 在LIG WAIS比某些模型更稳定.
- 需要重新评估LIG海平面预算部分.
- 未来极端海平面上升预测的观测基础受到削弱.
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