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

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 their re...

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Bibliographic Details
Published in:Geophysical Research Letters
Main Authors: Ardhuin, Fabrice, Sutherland, Peter, Doble, Martin, Wadhams, Peter
Format: Article in Journal/Newspaper
Language:English
Published: Amer Geophysical Union 2016
Subjects:
Online Access:https://archimer.ifremer.fr/doc/00333/44455/44127.pdf
https://doi.org/10.1002/2016GL068204
https://archimer.ifremer.fr/doc/00333/44455/