Wave Attenuation Through an Arctic Marginal Ice Zone on 12 October 2015: 2. Numerical Modeling of Waves and Associated Ice Breakup-Reference-Cited by-同舟云学术

Wave Attenuation Through an Arctic Marginal Ice Zone on 12 October 2015: 2. Numerical Modeling of Waves and Associated Ice Breakup

Published:2018-08 Issue:8 Volume:123 Page:5652-5668
ISSN:2169-9275
Container-title:Journal of Geophysical Research: Oceans
language:en
Short-container-title:J. Geophys. Res. Oceans

Author:

Ardhuin Fabrice¹^ORCID,Boutin Guillaume¹^ORCID,Stopa Justin¹^ORCID,Girard‐Ardhuin Fanny¹^ORCID,Melsheimer Christian²,Thomson Jim³^ORCID,Kohout Alison⁴,Doble Martin⁵^ORCID,Wadhams Peter⁶^ORCID

Affiliation:

1. Univ. Brest, CNRS, IRD, Ifremer, Laboratoire d'Océanographie Physique et Spatiale, IUEM Brest France

2. Institute of Environmental Physics, University of Bremen Bremen Germany

3. Applied Physics Laboratory University of Washington, Seattle Washington USA

4. National Institute of Water and Atmospheric Research Christchurch New Zealand

5. PolarScientific Ltd. Appin UK

6. Cambridge Polar Consultants Ltd. Cambridge UK

Funder

Office of Naval Research

Centre National d’Etudes Spatiales

Publisher

American Geophysical Union (AGU)

Subject

Earth and Planetary Sciences (miscellaneous),Space and Planetary Science,Geochemistry and Petrology,Geophysics,Oceanography

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1002/2018JC013784

Reference56 articles.

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3. Small-scale open ocean currents have large effects on wind wave heights

4. Semiempirical Dissipation Source Functions for Ocean Waves. Part I: Definition, Calibration, and Validation

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

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