Wave dispersion and dissipation in landfast ice: comparison of observations against models
Observations of wave dissipation and dispersion in sea ice are a necessity for the development and validation of wave–ice interaction models. As the composition of the ice layer can be extremely complex, most models treat the ice layer as a continuum with effective, rather than independently measura...
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ftdoajarticles:oai:doaj.org/article:9b683629e61a49c8ae3b6a883c6f6968 2023-05-15T13:46:10+02:00 Wave dispersion and dissipation in landfast ice: comparison of observations against models J. J. Voermans Q. Liu A. Marchenko J. Rabault K. Filchuk I. Ryzhov P. Heil T. Waseda T. Nose T. Kodaira J. Li A. V. Babanin 2021-12-01T00:00:00Z https://doi.org/10.5194/tc-15-5557-2021 https://doaj.org/article/9b683629e61a49c8ae3b6a883c6f6968 EN eng Copernicus Publications https://tc.copernicus.org/articles/15/5557/2021/tc-15-5557-2021.pdf https://doaj.org/toc/1994-0416 https://doaj.org/toc/1994-0424 doi:10.5194/tc-15-5557-2021 1994-0416 1994-0424 https://doaj.org/article/9b683629e61a49c8ae3b6a883c6f6968 The Cryosphere, Vol 15, Pp 5557-5575 (2021) Environmental sciences GE1-350 Geology QE1-996.5 article 2021 ftdoajarticles https://doi.org/10.5194/tc-15-5557-2021 2022-12-31T05:44:37Z Observations of wave dissipation and dispersion in sea ice are a necessity for the development and validation of wave–ice interaction models. As the composition of the ice layer can be extremely complex, most models treat the ice layer as a continuum with effective, rather than independently measurable, properties. While this provides opportunities to fit the model to observations, it also obscures our understanding of the wave–ice interactive processes; in particular, it hinders our ability to identify under which environmental conditions these processes are of significance. Here, we aimed to reduce the number of free variables available by studying wave dissipation in landfast ice. That is, in continuous sea ice, such as landfast ice, the effective properties of the continuum ice layer should revert to the material properties of the ice. We present observations of wave dispersion and dissipation from a field experiment on landfast ice in the Arctic and Antarctic. Independent laboratory measurements were performed on sea ice cores from a neighboring fjord in the Arctic to estimate the ice viscosity. Results show that the dispersion of waves in landfast ice is well described by theory of a thin elastic plate, and such observations could provide an estimate of the elastic modulus of the ice. Observations of wave dissipation in landfast ice are about an order of magnitude larger than in ice floes and broken ice. Comparison of our observations against models suggests that wave dissipation is attributed to the viscous dissipation within the ice layer for short waves only, whereas turbulence generated through the interactions between the ice and waves is the most likely process for the dissipation of wave energy for long periods. The separation between short and long waves in this context is expected to be determined by the ice thickness through its influence on the lengthening of short waves. Through the comparison of the estimated wave attenuation rates with distance from the landfast ice edge, our results suggest ... Article in Journal/Newspaper Antarc* Antarctic Arctic Sea ice The Cryosphere Directory of Open Access Journals: DOAJ Articles Arctic Antarctic The Cryosphere 15 12 5557 5575 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
Environmental sciences GE1-350 Geology QE1-996.5 |
spellingShingle |
Environmental sciences GE1-350 Geology QE1-996.5 J. J. Voermans Q. Liu A. Marchenko J. Rabault K. Filchuk I. Ryzhov P. Heil T. Waseda T. Nose T. Kodaira J. Li A. V. Babanin Wave dispersion and dissipation in landfast ice: comparison of observations against models |
topic_facet |
Environmental sciences GE1-350 Geology QE1-996.5 |
description |
Observations of wave dissipation and dispersion in sea ice are a necessity for the development and validation of wave–ice interaction models. As the composition of the ice layer can be extremely complex, most models treat the ice layer as a continuum with effective, rather than independently measurable, properties. While this provides opportunities to fit the model to observations, it also obscures our understanding of the wave–ice interactive processes; in particular, it hinders our ability to identify under which environmental conditions these processes are of significance. Here, we aimed to reduce the number of free variables available by studying wave dissipation in landfast ice. That is, in continuous sea ice, such as landfast ice, the effective properties of the continuum ice layer should revert to the material properties of the ice. We present observations of wave dispersion and dissipation from a field experiment on landfast ice in the Arctic and Antarctic. Independent laboratory measurements were performed on sea ice cores from a neighboring fjord in the Arctic to estimate the ice viscosity. Results show that the dispersion of waves in landfast ice is well described by theory of a thin elastic plate, and such observations could provide an estimate of the elastic modulus of the ice. Observations of wave dissipation in landfast ice are about an order of magnitude larger than in ice floes and broken ice. Comparison of our observations against models suggests that wave dissipation is attributed to the viscous dissipation within the ice layer for short waves only, whereas turbulence generated through the interactions between the ice and waves is the most likely process for the dissipation of wave energy for long periods. The separation between short and long waves in this context is expected to be determined by the ice thickness through its influence on the lengthening of short waves. Through the comparison of the estimated wave attenuation rates with distance from the landfast ice edge, our results suggest ... |
format |
Article in Journal/Newspaper |
author |
J. J. Voermans Q. Liu A. Marchenko J. Rabault K. Filchuk I. Ryzhov P. Heil T. Waseda T. Nose T. Kodaira J. Li A. V. Babanin |
author_facet |
J. J. Voermans Q. Liu A. Marchenko J. Rabault K. Filchuk I. Ryzhov P. Heil T. Waseda T. Nose T. Kodaira J. Li A. V. Babanin |
author_sort |
J. J. Voermans |
title |
Wave dispersion and dissipation in landfast ice: comparison of observations against models |
title_short |
Wave dispersion and dissipation in landfast ice: comparison of observations against models |
title_full |
Wave dispersion and dissipation in landfast ice: comparison of observations against models |
title_fullStr |
Wave dispersion and dissipation in landfast ice: comparison of observations against models |
title_full_unstemmed |
Wave dispersion and dissipation in landfast ice: comparison of observations against models |
title_sort |
wave dispersion and dissipation in landfast ice: comparison of observations against models |
publisher |
Copernicus Publications |
publishDate |
2021 |
url |
https://doi.org/10.5194/tc-15-5557-2021 https://doaj.org/article/9b683629e61a49c8ae3b6a883c6f6968 |
geographic |
Arctic Antarctic |
geographic_facet |
Arctic Antarctic |
genre |
Antarc* Antarctic Arctic Sea ice The Cryosphere |
genre_facet |
Antarc* Antarctic Arctic Sea ice The Cryosphere |
op_source |
The Cryosphere, Vol 15, Pp 5557-5575 (2021) |
op_relation |
https://tc.copernicus.org/articles/15/5557/2021/tc-15-5557-2021.pdf https://doaj.org/toc/1994-0416 https://doaj.org/toc/1994-0424 doi:10.5194/tc-15-5557-2021 1994-0416 1994-0424 https://doaj.org/article/9b683629e61a49c8ae3b6a883c6f6968 |
op_doi |
https://doi.org/10.5194/tc-15-5557-2021 |
container_title |
The Cryosphere |
container_volume |
15 |
container_issue |
12 |
container_start_page |
5557 |
op_container_end_page |
5575 |
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1766237953797914624 |