| Autor: |
Auclair JP; Institut des Sciences de la Terre (ISTerre), CNRS/Université Grenoble-Alpes, Saint-Martin d'Hères, 38400, France.; Department of Oceanography, Dalhousie University, Halifax, Nova Scotia, B3H 4R2, Canada., Dumont D; Institut des sciences de la mer de Rimouski, Université du Québec à Rimouski, Rimouski, Québec, G5L 3A1, Canada., Lemieux JF; Recherche en Prévision Numérique environnementale, Environnement et changement climatique Canada, Dorval, Québec, H9P 1J3, Canada., Ritchie H; Recherche en Prévision Numérique environnementale, Environnement et changement climatique Canada, Dorval, Québec, H9P 1J3, Canada. |
| Abstrakt: |
With the increasing resolution of operational forecasting models, the marginal ice zone (MIZ), the area where waves and sea ice interact, can now be better represented. However, the proper mechanics of wave propagation and attenuation in ice, and especially their influence on sea ice dynamics, still remain poorly understood and constrained in models. Observations have shown exponential wave energy decrease with distance in sea ice, particularly strong at higher frequencies. Some of this energy is transferred to the ice, breaking it into smaller floes and weakening it, as well as exerting a stress on the ice similar to winds and currents. In this article, we present a one-dimensional, fully integrated wave and ice model that has been developed to test different parameterizations of wave-ice interactions. The response of the ice cover to the wind and wave radiative stresses is investigated for a variety of wind, wave and ice conditions at different scales. Results of sensitivity analyses reveal the complex interplay between wave attenuation and rheological parameters and suggest that the compressive strength of the MIZ may be better represented by a Mohr-Coulomb parameterization with a nonlinear dependence on thickness. This article is part of the theme issue 'Theory, modelling and observations of marginal ice zone dynamics: multidisciplinary perspectives and outlooks'. |
