Floe Size Effect on Wave‐Ice Interactions: Possible Effects, Implementation in Wave Model, and Evaluation. Issue 7 (10th July 2018)

• Record Type: Journal Article
• Authors: Boutin, Guillaume; Ardhuin, Fabrice; Dumont, Dany; Sévigny, Caroline; Girard‐Ardhuin, Fanny; Accensi, Mickael
• Is Part Of: Journal of geophysical research. Volume 123:Issue 7(2018)
• Page Start: 4779
• Page End: 4805
• Publication Date: 2018-07-10
• Subjects: sea ice -- floes -- spectral wave model; Oceanography -- Periodicals; 551.4605
• DOI: 10.1029/2017JC013622
• Languages: English
• ISSNs: 2169-9275

Abstract

Abstract: Wind waves may play an important role in the evolution of sea ice. That role is largely determined by how fast the ice layer dissipates the wave energy. The transition from a continuous layer of ice to a series of broken floes is expected to have a strong impact on the several attenuation processes. Here we explore the possible effects of basal friction, scattering, and dissipation within the ice layer. The ice is treated as a single layer that can be fractured in many floes. Dissipation associated with ice flexure is evaluated using an anelastic linear dissipation and a cubic inelastic viscous dissipation. Tests aiming to reproduce a Marginal Ice Zone are used to discuss the effects of each process separately. Attenuation is exponential for friction and scattering. Scattering produces an increase in the wave height near the ice edge and broadens the wave directional spectrum, especially for short‐period waves. The nonlinear inelastic dissipation is larger for larger wave heights as long as the ice is not broken. These effects are combined in a realistic simulation of an ice break‐up event observed south of Svalbard in 2010. The recorded rapid shift from a strong attenuation to little attenuation when the ice is broken is only reproduced when using a nonlinear dissipation that vanishes when the ice is broken. A preliminary pan‐Arctic test of these different parameterizations suggests that inelastic dissipation alone is not enough and requires its combination with basal friction. Key Points: A spectral wave model with effects of sea ice floe size is presented Ice breakup is combined with three attenuations processes Model wave heights for a break‐up event reproduce observations in Svalbard