Wave attenuation by sea ice turbulence

The dissipation of wave energy in the marginal ice zone is often attributed to wave scattering and the dissipative mechanisms associated with the ice layer. In this study we present observations indicating that turbulence generated by the differential velocity between the sea ice cover and the orbit...

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Published in:Geophysical Research Letters
Main Authors: Voermans, J. J., Babanin, A. V., Thomson, J., Smith, M. M., Shen, Hayley H.
Other Authors: Nanyang Environment and Water Research Institute
Format: Article in Journal/Newspaper
Language:English
Published: 2019
Subjects:
Online Access:http://hdl.handle.net/10220/49673
https://doi.org/10.1029/2019GL082945
id ftnanyangtu:oai:dr.ntu.edu.sg:10220/49673
record_format openpolar
spelling ftnanyangtu:oai:dr.ntu.edu.sg:10220/49673 2023-05-15T18:17:08+02:00 Wave attenuation by sea ice turbulence Voermans, J. J. Babanin, A. V. Thomson, J. Smith, M. M. Shen, Hayley H. Nanyang Environment and Water Research Institute 2019 8 p. http://hdl.handle.net/10220/49673 https://doi.org/10.1029/2019GL082945 en eng Geophysical Research Letters Voermans, J. J., Babanin, A. V., Thomson, J., Smith, M. M., & Shen, H. H. (2019). Wave attenuation by sea ice turbulence. Geophysical Research Letters, 46(12), 6796-6803. doi:10.1029/2019GL082945 0094-8276 http://hdl.handle.net/10220/49673 http://dx.doi.org/10.1029/2019GL082945 © 2019 American Geophysical Union. All rights reserved. This paper was published in Geophysical Research Letters and is made available with permission of American Geophysical Union. Wave Attenuation Sea Ice Turbulence Engineering::Environmental engineering Journal Article 2019 ftnanyangtu https://doi.org/10.1029/2019GL082945 2019-08-23T00:05:29Z The dissipation of wave energy in the marginal ice zone is often attributed to wave scattering and the dissipative mechanisms associated with the ice layer. In this study we present observations indicating that turbulence generated by the differential velocity between the sea ice cover and the orbital wave motion may be an important dissipative mechanism of wave energy. Through field measurements of under‐ice turbulence dissipation rates in pancake and frazil ice, it is shown that turbulence‐induced wave attenuation coefficients are in agreement with observed wave attenuation in the marginal ice zone. The results suggest that the turbulence‐induced attenuation rates can be parameterized by the characteristic wave properties and a coefficient. The coefficient is determined by the ice layer properties. Published version Article in Journal/Newspaper Sea ice DR-NTU (Digital Repository at Nanyang Technological University, Singapore) Pancake ENVELOPE(-55.815,-55.815,52.600,52.600) Geophysical Research Letters 46 12 6796 6803
institution Open Polar
collection DR-NTU (Digital Repository at Nanyang Technological University, Singapore)
op_collection_id ftnanyangtu
language English
topic Wave Attenuation
Sea Ice Turbulence
Engineering::Environmental engineering
spellingShingle Wave Attenuation
Sea Ice Turbulence
Engineering::Environmental engineering
Voermans, J. J.
Babanin, A. V.
Thomson, J.
Smith, M. M.
Shen, Hayley H.
Wave attenuation by sea ice turbulence
topic_facet Wave Attenuation
Sea Ice Turbulence
Engineering::Environmental engineering
description The dissipation of wave energy in the marginal ice zone is often attributed to wave scattering and the dissipative mechanisms associated with the ice layer. In this study we present observations indicating that turbulence generated by the differential velocity between the sea ice cover and the orbital wave motion may be an important dissipative mechanism of wave energy. Through field measurements of under‐ice turbulence dissipation rates in pancake and frazil ice, it is shown that turbulence‐induced wave attenuation coefficients are in agreement with observed wave attenuation in the marginal ice zone. The results suggest that the turbulence‐induced attenuation rates can be parameterized by the characteristic wave properties and a coefficient. The coefficient is determined by the ice layer properties. Published version
author2 Nanyang Environment and Water Research Institute
format Article in Journal/Newspaper
author Voermans, J. J.
Babanin, A. V.
Thomson, J.
Smith, M. M.
Shen, Hayley H.
author_facet Voermans, J. J.
Babanin, A. V.
Thomson, J.
Smith, M. M.
Shen, Hayley H.
author_sort Voermans, J. J.
title Wave attenuation by sea ice turbulence
title_short Wave attenuation by sea ice turbulence
title_full Wave attenuation by sea ice turbulence
title_fullStr Wave attenuation by sea ice turbulence
title_full_unstemmed Wave attenuation by sea ice turbulence
title_sort wave attenuation by sea ice turbulence
publishDate 2019
url http://hdl.handle.net/10220/49673
https://doi.org/10.1029/2019GL082945
long_lat ENVELOPE(-55.815,-55.815,52.600,52.600)
geographic Pancake
geographic_facet Pancake
genre Sea ice
genre_facet Sea ice
op_relation Geophysical Research Letters
Voermans, J. J., Babanin, A. V., Thomson, J., Smith, M. M., & Shen, H. H. (2019). Wave attenuation by sea ice turbulence. Geophysical Research Letters, 46(12), 6796-6803. doi:10.1029/2019GL082945
0094-8276
http://hdl.handle.net/10220/49673
http://dx.doi.org/10.1029/2019GL082945
op_rights © 2019 American Geophysical Union. All rights reserved. This paper was published in Geophysical Research Letters and is made available with permission of American Geophysical Union.
op_doi https://doi.org/10.1029/2019GL082945
container_title Geophysical Research Letters
container_volume 46
container_issue 12
container_start_page 6796
op_container_end_page 6803
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