海洋腔调节的转变逆转了西南极洲接地线的退缩在末期的全新纪
Daniel P Lowry1, Holly K Han2,3, Nicholas R Golledge4
1Department of Surface Geosciences, GNS Science, Lower Hutt, New Zealand. d.lowry@gns.cri.nz.
Nature communications
|April 23, 2024
概括
西南极冰盖的接地线因海洋变化而逆转,而不仅仅是静态反弹. 这表明未来对子冰架海洋循环变化的敏感性.
科学领域:
- 古气候学 古气候学
- 冰川学的冰川学
- 地球系统科学 地球系统科学
背景情况:
- 地质和建模证据表明,在全新纪期间,西南极冰盖 (WAIS) 的Siple海岸上出现了显著的接地线撤退和重新推进.
- 这种基线逆转在历史上被归因于静态反弹和区域气候变化.
研究的目的:
- 调查西普尔海岸接地线逆转的主要驱动因素.
- 在过去的冰盖动态中区分海洋热强迫和冰川静态调整 (GIA) 的作用.
主要方法:
- 利用了一个代理信息集的冰盖模型模拟.
- 整合了不同的海洋热力强迫场景.
- 进行了全球冰川静态调整 (GIA) 建模和结合冰盖-GIA模拟.
主要成果:
- 结果强烈表明,从温暖到寒冷的海洋腔系统的转变是接地线逆转的最可能原因.
- 研究人员发现,冰冰静态调整 (GIA) 调节了冰盖对海洋强迫反应的速度.
- 这项研究强调了海洋变化和冰盖行为之间的相互联系.
结论:
- 西普尔海岸的接地线逆转主要是由海洋学变化驱动的.
- 冰冰静态调整在调节冰盖反应速度方面发挥着至关重要的作用.
- 西普尔海岸接地线对子冰架海洋循环的未来变化具有显著的敏感性,这对海平面上升预测有影响.
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