Wave dispersion and dissipation in landfast ice: Comparison of observations against models
Abstract. 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 independent...
Published in: | The Cryosphere |
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Main Authors: | , , , , , , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
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Copernicus Publications under license by EGU – European Geosciences Union GmbH
2022
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Online Access: | http://hdl.handle.net/10852/92354 http://urn.nb.no/URN:NBN:no-94895 https://doi.org/10.5194/tc-15-5557-2021 |
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ftoslouniv:oai:www.duo.uio.no:10852/92354 |
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Open Polar |
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Universitet i Oslo: Digitale utgivelser ved UiO (DUO) |
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ftoslouniv |
language |
English |
description |
Abstract. 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 that the attenuation of long waves is weaker in comparison to short waves, but their dependence on wave energy is stronger. Further studies are required to measure the spatial variability of wave attenuation and measure turbulence underneath the ice independently of observations of wave attenuation to confirm our interpretation of the results. |
format |
Article in Journal/Newspaper |
author |
Voermans, Joey Liu, Qingxiang Marchenko, Aleksey Rabault, Jean Filchuk, Kirill Ryzhov, Ivan Heil, Petra Waseda, Takuji Nose, Takehiko Kodaira, Tsubasa Li, Jingkai Babanin, Alexander V. |
spellingShingle |
Voermans, Joey Liu, Qingxiang Marchenko, Aleksey Rabault, Jean Filchuk, Kirill Ryzhov, Ivan Heil, Petra Waseda, Takuji Nose, Takehiko Kodaira, Tsubasa Li, Jingkai Babanin, Alexander V. Wave dispersion and dissipation in landfast ice: Comparison of observations against models |
author_facet |
Voermans, Joey Liu, Qingxiang Marchenko, Aleksey Rabault, Jean Filchuk, Kirill Ryzhov, Ivan Heil, Petra Waseda, Takuji Nose, Takehiko Kodaira, Tsubasa Li, Jingkai Babanin, Alexander V. |
author_sort |
Voermans, Joey |
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 under license by EGU – European Geosciences Union GmbH |
publishDate |
2022 |
url |
http://hdl.handle.net/10852/92354 http://urn.nb.no/URN:NBN:no-94895 https://doi.org/10.5194/tc-15-5557-2021 |
geographic |
Antarctic Arctic |
geographic_facet |
Antarctic Arctic |
genre |
Antarc* Antarctic Arctic Sea ice The Cryosphere |
genre_facet |
Antarc* Antarctic Arctic Sea ice The Cryosphere |
op_source |
1994-0416 |
op_relation |
NFR/280625 http://urn.nb.no/URN:NBN:no-94895 Voermans, Joey Liu, Qingxiang Marchenko, Aleksey Rabault, Jean Filchuk, Kirill Ryzhov, Ivan Heil, Petra Waseda, Takuji Nose, Takehiko Kodaira, Tsubasa Li, Jingkai Babanin, Alexander V. . Wave dispersion and dissipation in landfast ice: Comparison of observations against models. The Cryosphere. 2021, 15(12), 5557-5575 http://hdl.handle.net/10852/92354 1991022 info:ofi/fmt:kev:mtx:ctx&ctx_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.jtitle=The Cryosphere&rft.volume=15&rft.spage=5557&rft.date=2021 The Cryosphere 15 12 5557 5575 https://doi.org/10.5194/tc-15-5557-2021 URN:NBN:no-94895 Fulltext https://www.duo.uio.no/bitstream/handle/10852/92354/1/tc-15-5557-2021.pdf |
op_rights |
Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/ |
op_rightsnorm |
CC-BY |
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 |
_version_ |
1766106408838758400 |
spelling |
ftoslouniv:oai:www.duo.uio.no:10852/92354 2023-05-15T13:38:27+02:00 Wave dispersion and dissipation in landfast ice: Comparison of observations against models Voermans, Joey Liu, Qingxiang Marchenko, Aleksey Rabault, Jean Filchuk, Kirill Ryzhov, Ivan Heil, Petra Waseda, Takuji Nose, Takehiko Kodaira, Tsubasa Li, Jingkai Babanin, Alexander V. 2022-01-27T10:22:15Z http://hdl.handle.net/10852/92354 http://urn.nb.no/URN:NBN:no-94895 https://doi.org/10.5194/tc-15-5557-2021 EN eng Copernicus Publications under license by EGU – European Geosciences Union GmbH NFR/280625 http://urn.nb.no/URN:NBN:no-94895 Voermans, Joey Liu, Qingxiang Marchenko, Aleksey Rabault, Jean Filchuk, Kirill Ryzhov, Ivan Heil, Petra Waseda, Takuji Nose, Takehiko Kodaira, Tsubasa Li, Jingkai Babanin, Alexander V. . Wave dispersion and dissipation in landfast ice: Comparison of observations against models. The Cryosphere. 2021, 15(12), 5557-5575 http://hdl.handle.net/10852/92354 1991022 info:ofi/fmt:kev:mtx:ctx&ctx_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.jtitle=The Cryosphere&rft.volume=15&rft.spage=5557&rft.date=2021 The Cryosphere 15 12 5557 5575 https://doi.org/10.5194/tc-15-5557-2021 URN:NBN:no-94895 Fulltext https://www.duo.uio.no/bitstream/handle/10852/92354/1/tc-15-5557-2021.pdf Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/ CC-BY 1994-0416 Journal article Tidsskriftartikkel Peer reviewed PublishedVersion 2022 ftoslouniv https://doi.org/10.5194/tc-15-5557-2021 2022-03-16T23:33:52Z Abstract. 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 that the attenuation of long waves is weaker in comparison to short waves, but their dependence on wave energy is stronger. Further studies are required to measure the spatial variability of wave attenuation and measure turbulence underneath the ice independently of observations of wave attenuation to confirm our interpretation of the results. Article in Journal/Newspaper Antarc* Antarctic Arctic Sea ice The Cryosphere Universitet i Oslo: Digitale utgivelser ved UiO (DUO) Antarctic Arctic The Cryosphere 15 12 5557 5575 |