海洋变暖推动了南极半岛西部海洋终结冰川的快速动态激活
Benjamin J Wallis1, Anna E Hogg2, Michael P Meredith3
1School of Earth and Environment, University of Leeds, Leeds, UK. eebjwa@leeds.ac.uk.
Nature communications
|November 28, 2023
概括
南极冰川的快速变化,包括速度的增加和冰架的崩,是由温暖的海洋水的入侵驱动的. 这突出了南极半岛的特点.
科学领域:
- 冰川学和海洋学
- 气候变化研究 气候变化研究
- 南极研究南极研究.
背景情况:
- 冰的动态是南极冰盖质量损失的主要驱动因素.
- 了解冰洋相互作用对于预测冰盖行为和海平面上升至关重要.
- 南极半岛对气候变化特别敏感.
研究的目的:
- 为了调查南极洲快速冰的动态变化的原因和时间表.
- 分析海洋学条件对冰川稳定性的影响.
- 评估南极冰川对海洋强迫的敏感性.
主要方法:
- 利用卫星观测来监测冰的速度,冰的排放和前线的撤退.
- 分析了海洋温度异常和浴度数据.
- 将卡德曼冰川的变化与邻近的冰川 (Funk和Lever) 的变化进行比较.
主要成果:
- 卡德曼冰川在2018-2019年间经历了94%的速度增加和显著的冰架崩.
- 冰流量每年增加了0.52 Gt,分娩前线撤退8公里.
- 一个400米深的通道允许温暖的海洋水到达卡德曼冰川,引发了动态失衡,而边缘保护了附近的冰川.
结论:
- 温暖的海洋水入侵可以迅速破坏南极冰川的稳定,增加冰的排放.
- 这些发现强调了南极半岛对海洋学变化的脆弱性.
- 这项研究突出了由于未来气候变化而加速冰损失的可能性.
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