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在东部Thwaites冰川接地区抑制基底融化
Peter E D Davis1, Keith W Nicholls2, David M Holland3,4
1British Antarctic Survey, Cambridge, UK. petvis@bas.ac.uk.
Nature
|February 15, 2023
概括
温暖的海洋水正在融化.
科学领域:
- 冰川学
- 海洋学
- 南极研究
背景情况:
- 斯威特斯冰川是一个快速变化的南极冰洋系统.
- 在海平面下方的内陆岩层使其易受不可逆转的冰损失和全球海平面上升的影响.
- 对于预测冰的消失至关重要.
研究的目的:
- 在Thwaites东部冰架 (TEIS) 的接地区域调查海洋条件和基底融化.
- 评估当前模型在预测基底融化速率方面的准确性.
主要方法:
- 使用热水钻孔的观测结果.
- 分析了水柱温度,稳定性,电流速度和密度分层.
主要成果:
- 在TEIS接地区域观察到温暖,高度稳定的水柱,温度高于现场点.
- 发现低流速和强密度分层显著限制了冰基层的热混合,抑制了基底融化.
- 证明目前的冰架基底融化模型无法复制观察到的融化速度.
结论:
- 尽管海洋温度较高,但由于热量混合有限,TEIS的基础化被抑制.
- 海平面预测的正规模型可能无法准确地反映Thwaites冰川的融化过程.
- 即使基底融速率很小,也可能发生快速且不稳定的接地线退缩.
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