Damping of Regular Waves in Model Ice

M. Hartmann, R. V. B. U. Polach, Marco Klein
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引用次数: 3

Abstract

Wave characteristics change significantly when the waves propagate in a solid ice field. The damping of the incident waves due to the presence of the ice sheet has a significant impact on the modification of wave propagation and dispersion. In this study the interaction of waves with solid ice are investigated by means of model tests. The objective of the study is to measure wave and ice characteristics and analyze the data regarding wave damping and the change of wave parameters in model ice. The experiments were performed in the ice tank of the Hamburg ship model basin (HSVA) with a set of regular waves with varying wave number and steepness. The surface elevation of the waves is recorded by acoustic and motion capturing measurement devices. By comparing the measurements of the incident open water waves with the waves in ice, the change in terms of wave amplitude and dispersion due to the presence of ice is analyzed. It is shown that once the waves travels through the ice the angular frequency remains unchanged while the wave amplitude exponentially decays, with an increasing decay coefficient at smaller wave length. Furthermore, the dispersion relation in ice, represented by the measured angular frequency and wave number, is consistent with the theoretical dispersion relation.
模型冰中规则波的阻尼
当波在固体冰原中传播时,波的特性发生显著变化。由于冰盖的存在,入射波的阻尼对波的传播和频散的改变有重要的影响。本文通过模型试验研究了波浪与固体冰的相互作用。研究的目的是测量波浪和冰的特性,并分析模型冰中波浪阻尼和波浪参数变化的数据。在汉堡船模盆地(HSVA)的冰槽中,采用一组不同波数和陡度的规则波进行了实验。波的表面高度由声学和运动捕捉测量设备记录。通过对入射开阔水波和冰中波浪的测量结果进行比较,分析了冰存在时波浪振幅和频散的变化。结果表明,当波穿过冰时,角频率保持不变,而波幅呈指数衰减,在较小的波长处衰减系数增大。此外,以测量的角频率和波数表示的冰中的色散关系与理论色散关系一致。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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