Articles | Volume 11, issue 5
https://doi.org/10.5194/tc-11-2117-2017
https://doi.org/10.5194/tc-11-2117-2017
Research article
 | 
07 Sep 2017
Research article |  | 07 Sep 2017

Wave–ice interactions in the neXtSIM sea-ice model

Timothy D. Williams, Pierre Rampal, and Sylvain Bouillon

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Revised manuscript accepted for TC
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Cited articles

Ardhuin, F., Sutherland, P., Doble, M., and Wadhams, P.: Ocean waves across the Arctic: Attenuation due to dissipation dominates over scattering for periods longer than 19s., Geophys. Res. Lett., 43, 5775–5783, https://doi.org/10.1002/2016GL068204, 2016.
Ardhuin, F., Stopa, J., Chapron, B., Collard, F., Smith, M., Thomson, J., Doble, M., Blomquist, B., Persson, O., Collins, III, C. O., and Wadhams, P.: Measuring ocean waves in sea ice using SAR imagery: A quasi-deterministic approach evaluated with Sentinel-1 and in situ data, Remote Sens. Environ., 189, 211–222, https://doi.org/10.1016/j.rse.2016.11.024, 2017.
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Bennetts, L. G. and Squire, V. A.: On the calculation of an attenuation coefficient for transects of ice-covered ocean, Proc. Roy. Soc. Lond. A, 468, 136–162, https://doi.org/10.1098/rspa.2011.0155, 2012.
Bennetts, L. G., O'Farrell, S., and Uotila, P.: Brief communication: Impacts of ocean-wave-induced breakup of Antarctic sea ice via thermodynamics in a stand-alone version of the CICE sea-ice model, The Cryosphere, 11, 1035–1040, https://doi.org/10.5194/tc-11-1035-2017, 2017.
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Short summary
As the Arctic sea ice extent drops, more ship traffic seeks to take advantage of this, and a need for better wave and sea ice forecasts arises. One aspect of this is the location of the sea ice edge. The waves here can be quite large, but they die away as they travel into the ice. This causes momentum to be transferred from the waves to the ice, causing ice drift. However, our study found that the effect of the wind drag had more impact on the ice edge position than the waves.