在格陵兰岛的冰块上同时发生叠加的冰形成和融化水流动
Andrew Tedstone1,2, Horst Machguth3, Nicole Clerx3,4
1Department of Geosciences, University of Fribourg, Fribourg, Switzerland. andrew.tedstone@unil.ch.
Nature communications
|May 14, 2025
概括
格陵兰冰盖板块上叠加的冰形成重新结了大多数在流水极限附近的融化水. 这些板块对于了解冰盖水文和未来海平面上升至关重要.
科学领域:
- 冰川学的冰川学
- 气候科学 气候科学
- 水文学的水文学
背景情况:
- 在格陵兰冰盖上形成了河流和泥沼地,特别是在积累区存在冰块的地方.
- 在这些冰块上,融化水流动和保持之间的平衡还不太清楚.
研究的目的:
- 测量在可见流水极限附近的冰块上叠加的冰形成.
- 在这些地区量化融水的保留和重新结过程.
主要方法:
- 对叠加冰形成的现场测量.
- 热传导模型. 热传导模型.
- 雷达观测秋季潮湿的情况.
主要成果:
- 叠加的冰量取决于接近地表水和地表斜率,表明在重新结之前的横向融水流.
- 在2022年,65%的叠加冰在夏季形成,35%在秋季形成.
- 总体而言,在可见流量极限附近的融化水中,有84%重新结.
- 据估计,在2017-2022年期间,全球约有56亿的融水在冰块上重新结.
结论:
- 冰块在上冰层水文网络中充当了重要的重新结区.
- 这些地区正日益成为表面流失的重要区域,影响冰盖质量平衡.
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