相关实验视频
Updated: Jul 12, 2026

07:55
Flexural Rigidity Measurements of Biopolymers Using Gliding Assays
Published on: November 9, 2012
在北极大洋,由内部波束所迫使的冰曲折是北极大洋的波束
概括
北极海洋的内部波浪导致了冰的显著屈曲,通过倾斜计和应变计测量. 这项研究量化了冰的数量.
科学领域:
- 海洋学 海洋学 海洋学
- 北极研究研究北极研究
- 地质物理学 地质物理学
背景情况:
- 内部波是海洋混合和能量转移的重要驱动因素.
- 北极海冰的动态对于气候调节至关重要.
- 在耶尔马克高原附近观察到日间内部钻孔.
研究的目的:
- 为了测量北极海冰的折 flexure.
- 量化内部波对海冰的影响.
- 为了将冰的曲率与波浪特征相关联.
主要方法:
- 在北极海冰上部署倾斜计和应变计.
- 测量冰的倾斜,应变,垂直速度和表面移位.
- 冰的测量与地下火岩位移和当前数据的比较.
主要成果:
- 记录了36微辐射的振荡式冰倾斜.
- 这种倾斜对应于每秒16微米的表面垂直速度和3.5毫米的表面位移.
- 测量了3×10(-7) 的冰压,显示了曲,这与波浪强迫相一致.
结论:
- 充满活力的内部波浪可以在北极海冰中引起可测量的屈曲.
- 观察到的冰曲线与内部孔的动态相一致.
- 这项研究提供了内部波和海冰之间的相互作用的直接证据.
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