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南极冰的动态被北半球海平面强迫放大
Natalya Gomez1, Michael E Weber2, Peter U Clark3,4
1Department of Earth and Planetary Sciences, McGill University, Montreal, Quebec, Canada. natalya.gomez@mcgill.ca.
Nature
|November 26, 2020
概括
北半球海平面变化放大了南极冰盖 (AIS) 的动态. 这种半球间的相互作用导致冰化过程中AIS体积增加,并在脱冰过程中增加了回退和质量损失.
科学领域:
- 古气候学
- 冰川学
- 海平面研究
背景情况:
- 北半球的冰流影响全球海平面,可能影响南极冰层 (AIS).
- 之前的模型表明由于海平面强迫而导致AIS接地线的退缩,但复杂的相互作用没有完全被捕捉到.
- 在最后一次脱冰期间,AIS的千年变化支持外部海平面强迫.
研究的目的:
- 调查南极冰盖 (AIS) 由于北半球海平面强迫而增强的动态.
- 模拟影响AIS接地线行为的复杂半球间相互作用.
- 将模拟的AIS行为与地质重建和古气候数据相协调.
主要方法:
- 冰盖模型与全球海平面模型的结合.
- 在北半球不同海平面强迫场景下模拟AIS动态.
- 将模型输出与AIS范围和海平面变化的地质证据进行比较.
主要成果:
- 北半球海平面强迫显著放大了AIS的动态.
- 半球间的相互作用导致了冰川时期的增强接地线和质量增长.
- 北半球海平面的快速上升导致了早些时候的接地线退缩和脱冰过程中的质量损失,导致了千年级的变化.
结论:
- 这项研究证实北半球海平面强迫在调节AIS行为中起着至关重要的作用.
- 这些半球间的相互作用使我们对过去的冰河周期和南极冰盖的演变有了更深入的了解.
- 发现与地质记录一致, 支持半球之间的复杂相互作用驱动冰盖变化.
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