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Sensitivity analysis of a viscoelastic parameterization for gravity wave dispersion in ice covered seas

机译:冰川覆盖海域重力波散射的粘弹性参数化敏感性分析

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Viscoelastic parameterization has been proposed for modeling gravity wave propagation under various ice covers. The resulting dispersion relation predicts wave speed change and attenuation, both depend on the viscoelastic parameters. Through direct measurements of wave characteristics, these parameters may be inversely determined. To effectively use an inverse method, the present study employs ANOVA to perform a sensitivity analysis on the dispersion relation. Two dispersion models are examined. Both models have qualitatively similar sensitivity to their parameters, but different parameterization. The statistical results show that the change of wave speed is most strongly dependent on the elasticity parameter, while attenuation is most strongly dependent on the wave period. The sensitivity analysis provides additional information. For example, for high frequency waves strong interactions exist between wave period, ice thickness, and viscoelastic parameters, which result in uncertainties to the inversely determined parameters. For low frequency waves, the viscoelastic parameters may be determined from attenuation data alone. If in addition the ice cover is thick and rigid, the accuracy of ice thickness is not crucial to the inversely determined elastic parameter. These findings are tested and validated using a field data set. The method presented in this study may be used to test other viscoelastic models. (C) 2015 Elsevier B.V. All rights reserved.
机译:已经提出了粘弹性参数化来模拟重力波在各种冰盖下的传播。所得的色散关系预测波速的变化和衰减,这都取决于粘弹性参数。通过直接测量波浪特征,可以反过来确定这些参数。为了有效地使用逆方法,本研究采用方差分析对色散关系进行敏感性分析。检查了两个色散模型。两种模型在质量上都对它们的参数敏感,但是参数设置不同。统计结果表明,波速的变化最大程度地取决于弹性参数,而衰减最大程度地取决于波周期。敏感性分析提供了其他信息。例如,对于高频波,波周期,冰厚度和粘弹性参数之间存在很强的相互作用,这导致了反确定参数的不确定性。对于低频波,可以仅从衰减数据确定粘弹性参数。另外,如果冰盖是厚且刚性的,则冰厚度的精度对于反确定的弹性参数不是至关重要的。这些发现是使用现场数据集进行测试和验证的。本研究中介绍的方法可用于测试其他粘弹性模型。 (C)2015 Elsevier B.V.保留所有权利。

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