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Updated: Aug 9, 2025

Evolution of Staircase Structures in Diffusive Convection
Published on: September 5, 2018
在Thwaites冰川接地线附近的异质融化
B E Schmidt1,2, P Washam3,4, P E D Davis5
1Department of Astronomy, Cornell University, Ithaca, NY, USA. britneys@cornell.edu.
由于温暖的海洋水融化了它的冰架, 这项研究揭示了依赖斜率的融化在接地线上是冰的损失的主要驱动因素.
科学领域:
- 冰川学
- 海洋学
- 气候科学
背景情况:
- 对于西南极冰盖的稳定性至关重要.
- 它的接地线很容易受到海洋变暖的影响,
- 最近冰的加速和退却表明冰正在流失.
研究的目的:
- 为了研究Thwaites冰川冰架融化的机制.
- 了解海洋变暖对冰川退缩的影响.
- 量化冰架次层的融化速度.
主要方法:
- 在Thwaites东部冰架 (TEIS) 进行水下车辆观测.
- 数据从接地线收集到海边3公里.
- 测量冰层地形,海洋温度和融化模式.
主要成果:
- 从2011年到2020年观察到持续的接地线退缩.
- 在冰洞中存在温暖的海洋水 (>2°C以上).
- 在的冰坡和露台上增强融化,在平面上抑制融化.
结论:
- 这种依赖斜率的融化极大地影响了冰基的形状.
- 这种融化机制是对Thwaites冰川海洋变暖的关键反应.
- 了解这些过程对于预测未来的冰损失至关重要.
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