Nonlinear simulation of wave group attenuation due to scattering in broken floe fields
Boyang Xu, Philippe Guyenne

TL;DR
This study uses nonlinear simulations to analyze how ocean waves are attenuated by scattering in fragmented sea ice, revealing frequency-dependent behaviors and the importance of nonlinear interactions, with results aligning with Arctic field observations.
Contribution
It introduces a nonlinear simulation framework for wave-ice interactions that captures complex scattering effects and explains the roll-over phenomenon observed in Arctic experiments.
Findings
Wave attenuation increases with frequency.
Non-monotonic attenuation near a specific frequency.
Nonlinear interactions are crucial for the roll-over effect.
Abstract
Direct phase-resolved simulations are performed to investigate the propagation and scattering of nonlinear ocean waves in fragmented sea ice. The numerical model solves the full time-dependent equations for nonlinear potential flow coupled with a nonlinear thin-plate representation of the ice cover, and neglects dissipative processes. The two-dimensional setting with incident wave groups on deep water is considered, in view of applications to wave attenuation along transects of the marginal ice zone. A spatially-varying weight is assigned to the surface pressure so that irregular distributions of ice floes can be directly specified in the physical domain. For various wave regimes and floe configurations, a local wave spectrum across the ice field is computed and then least-squares fitted to extract a spatial attenuation rate as a function of wave frequency. A general increase with…
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