非线性波冰相互作用的数值研究

M. Hartmann, R. V. B. U. Polach, S. Ehlers, N. Hoffmann, M. Onorato, Marco Klein
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引用次数: 0

摘要

本文研究了水平冰下非线性波冰相互作用的基本问题,重点研究了波的非线性传播和频散问题。因此,进行数值研究以从理论上验证非线性是否发生在水平冰下,以及这是否会导致远离冰缘的强烈波浪事件,以便为观测到的真实世界的冰破裂提供解释。因此,本文将研究波浪与冰的非线性相互作用以及冰的特性对这种相互作用的影响。在非线性Schrödinger方程(NLSE)框架下,对固体冰下的非线性波传播进行了直接数值模拟。应用Peregrine呼吸解来表示非线性波群的NLSE的精确解。这种非线性波群的应用是为了验证冰盖下发生的非线性波-波相互作用。对于模拟装置中波浪和冰参数的定义,采用了上述参数研究的结果。分析了波冰非线性相互作用和波传播的相关特性。通过假设物理一致性方面的约束,可以缩小NLSE模拟的参数范围。本研究的范围是为了更好地了解观测水平冰下非线性波效应所需的冰况。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Numerical Study on Nonlinear Wave-Ice-Interaction
This paper investigates the fundamental question of nonlinear wave-ice interaction under level ice focusing on nonlinear wave propagation and dispersion of waves. Therefore, numerical investigations are performed to verify theoretically if nonlinearity takes place under level ice and if this can lead to intense wave events far away from the ice edge in order to provide an explanation for observed real-world ice break-ups. Therefore, nonlinear wave-ice interaction as well as the impact of the ice characteristics on this interaction will be investigated. The direct numerical simulations of the nonlinear wave propagation under solid ice are performed within the Nonlinear Schrödinger Equation (NLSE) framework. The Peregrine breather solution is applied to represent exact solutions of the NLSE for a nonlinear wave group. The application of such a nonlinear wave group is predestined for the verification of occurring nonlinear wave-wave interaction below the ice sheet. For the definition of wave and ice parameters in the simulation setup, the results of the presented parameter study are used. The parameters are analyzed regarding relevant characteristics of nonlinear wave-ice interaction and wave propagation. By assuming constraints with respect to physical consistency, the parameter range for the NLSE simulations can be narrowed. The scope of this investigation is to provide a better understanding of the ice conditions required to observe nonlinear wave effects under level ice.
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