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Analysis of Tidal Deformations of Land Fast Ice in Shallow Arctic Fjord

机译:浅层北极峡湾陆上快速冰的潮汐变形分析

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The paper is devoted to the investigation of ice deformations and ice stresses build up in shore line zone of Sveasundet in Svea Bay of the Van Mijen Fjord in Spitsbergen. Two field surveys were performed in 2011 and 2012 for the monitoring of ice deformations induced by semidiurnal tides. A Leica Total Station and Laser Scanner Riegl VZ-1000 were used in the field measurements. Significant deflections of the ice surface from the horizontal plane were detected at low tide phases. Measurements of ice stresses near the shoreline indicated their semidiurnal oscillations with maximal onshore stresses at high tide. Mathematical model and numerical simulations were performed to explain the buildup and concentration of the ice stresses near narrow tips of the shoreline.
机译:这篇论文致力于调查斯匹次卑尔根范米延峡湾斯韦亚湾斯韦阿松德海岸岸线区的冰变形和冰应力。 2011年和2012年进行了两次野外调查,以监测半日潮引起的冰变形。现场测量中使用了徕卡全站仪和激光扫描仪Riegl VZ-1000。在退潮阶段,检测到冰面相对于水平面的明显偏斜。海岸线附近的冰应力测量表明,在涨潮时它们的半日振荡和最大的陆上应力。进行了数学模型和数值模拟,以解释海岸线狭窄尖端附近冰应力的累积和集中。

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