Ocean waves across the Arctic: Attenuation due to dissipation dominates over scattering for periods longer than 19 s

Abstract The poorly understood attenuation of surface waves in sea ice is generally attributed to the combination of scattering and dissipation. Scattering and dissipation have very different effects on the directional and temporal distribution of wave energy, making it possible to better understand...

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Bibliographic Details
Main Authors: Fabrice Ardhuin, Peter Sutherland, Martin Doble, Peter Wadhams
Format: Article
Language:English
Published: Wiley 2016-06-01
Series:Geophysical Research Letters
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Online Access:https://doi.org/10.1002/2016GL068204
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