冰流床的摩擦阻力有规律的模式,通过表面数据的反转来观察
Olga V Sergienko1, Richard C A Hindmarsh
1Program in Atmospheric and Oceanic Sciences, Princeton University, 201 Forrestal Road. Princeton, NJ 08540, USA.
概括
研究南极洲的松岛和Thwaites冰川揭示了高基底剪压的肋状模式. 亚冰川水可能会影响这些模式,可能会影响接地线.
科学领域:
- 冰川学的冰川学
- 南极冰盖的动态 南极冰盖的动态
- 地质物理学 地质物理学
背景情况:
- 快速流动的冰川和冰流对于南极洲的冰排放至关重要.
- 松岛和Thwaites冰川正在以加速的速度失去质量.
- 冰的排放是由冰床接口的条件控制的.
研究的目的:
- 为了计算松岛和Thwaites冰川下面的基底剪切应力分布.
- 调查控制冰块排放速度的因素.
主要方法:
- 使用了高分辨率数据集.
- 应用了一个标准的反向方法来计算基底剪切应力.
- 分析了基底剪切应力和液压潜力之间的关系.
主要成果:
- 确定了非常高的基底剪切应力的肋状模式.
- 在更大的零基底剪压区域内观察到这些高压力区域.
- 发现了高切割应力与液压潜力的高梯度的配色.
结论:
- 亚冰川水可能会控制高基底剪切压力肋骨的演变.
- 在接地线附近的基底电阻的变化可能受到亚冰川水的影响.
- 这种机制可能导致接地线迁移.
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