温带冰的线性粘性流
Collin M Schohn1, Neal R Iverson1, Lucas K Zoet2
1Department of Geological and Atmospheric Sciences, Iowa State University, Ames, IA, USA.
概括
温带冰川表现为线性粘性物质,而不是以前所认为的非线性. 基于剪切变形实验的这一发现影响了海平面上升的预测.
科学领域:
- 冰川学
- 冰的物理
- 气候科学
背景情况:
- 对于预测海平面上升至关重要.
- 目前的模型通常依赖于格伦的流量定律,假设非线性冰粘度 (n=3-4).
- 温的冰在粒边上含有液态水,影响其机械行为.
研究的目的:
- 在现实的压力和水分含量条件下研究温带冰川的浮动行为.
- 为了确定温带冰变形的应变速率指数 (n).
- 评估观察到的冰粘度对冰盖建模的影响.
主要方法:
- 在温带冰川上进行大规模的剪切变形实验.
- 冰川床和冰流边缘相关的范围内的液态水含量和应力.
- 分析了应力和应变率之间的关系以确定粘度指数 (n).
主要成果:
- 在测试条件下,温带冰川表现出线性粘性行为 (n ≈1.0).
- 这与格伦的流量定律所假定的非线性粘度 (n=3-4) 形成鲜明对比.
- 观察到的线性归因于在谷物边界的扩散压力化和重新结.
结论:
- 温带冰的线性粘性挑战了现有的冰流模型.
- 这一发现可能有助于稳定冰盖应对气候变化的预测.
- 修订后的模型包含了线性粘度,可以改善海平面上升的预测.
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