Experimental evidence for a universal threshold characterizing wave-induced sea ice break-up
Waves can drastically transform a sea ice cover by inducing break-up over vast distances in the course of a few hours. However, relatively few detailed studies have described this phenomenon in a quantitative manner, and the process of sea ice break-up by waves needs to be further parameterized and...
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2020
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ftunivtasmania:oai:eprints.utas.edu.au:40552 2023-05-15T18:16:06+02:00 Experimental evidence for a universal threshold characterizing wave-induced sea ice break-up Voermans, JJ Rabault, J Filchuk, K Ryzhov, I Heil, P Marchenko, A Collins, CO Dabboor, M Sutherland, G Babanin, AV 2020 application/pdf https://eprints.utas.edu.au/40552/ https://eprints.utas.edu.au/40552/1/143580%20-%20Experimental%20evidence%20for%20a%20universal%20threshold%20characterizing%20wave-induced.pdf en eng Copernicus GmbH https://eprints.utas.edu.au/40552/1/143580%20-%20Experimental%20evidence%20for%20a%20universal%20threshold%20characterizing%20wave-induced.pdf Voermans, JJ, Rabault, J, Filchuk, K, Ryzhov, I, Heil, P, Marchenko, A, Collins, CO, Dabboor, M, Sutherland, G and Babanin, AV 2020 , 'Experimental evidence for a universal threshold characterizing wave-induced sea ice break-up' , Cryosphere, vol. 14, no. 11 , pp. 4265-4278 , doi:10.5194/tc-14-4265-2020 <http://dx.doi.org/10.5194/tc-14-4265-2020>. sea ice waves sea ice break up forecasting Article PeerReviewed 2020 ftunivtasmania https://doi.org/10.5194/tc-14-4265-2020 2022-01-24T23:18:21Z Waves can drastically transform a sea ice cover by inducing break-up over vast distances in the course of a few hours. However, relatively few detailed studies have described this phenomenon in a quantitative manner, and the process of sea ice break-up by waves needs to be further parameterized and verified before it can be reliably included in forecasting models. In the present work, we discuss sea ice break-up parameterization and demonstrate the existence of an observational threshold separating breaking and non-breaking cases. This threshold is based on information from two recent field campaigns, supplemented with existing observations of sea ice break-up. The data used cover a wide range of scales, from laboratory-grown sea ice to polar field observations. Remarkably, we show that both field and laboratory observations tend to converge to a single quantitative threshold at which the wave-induced sea ice breakup takes place, which opens a promising avenue for robust parametrization in operational forecasting models. Article in Journal/Newspaper Sea ice University of Tasmania: UTas ePrints The Cryosphere 14 11 4265 4278 |
institution |
Open Polar |
collection |
University of Tasmania: UTas ePrints |
op_collection_id |
ftunivtasmania |
language |
English |
topic |
sea ice waves sea ice break up forecasting |
spellingShingle |
sea ice waves sea ice break up forecasting Voermans, JJ Rabault, J Filchuk, K Ryzhov, I Heil, P Marchenko, A Collins, CO Dabboor, M Sutherland, G Babanin, AV Experimental evidence for a universal threshold characterizing wave-induced sea ice break-up |
topic_facet |
sea ice waves sea ice break up forecasting |
description |
Waves can drastically transform a sea ice cover by inducing break-up over vast distances in the course of a few hours. However, relatively few detailed studies have described this phenomenon in a quantitative manner, and the process of sea ice break-up by waves needs to be further parameterized and verified before it can be reliably included in forecasting models. In the present work, we discuss sea ice break-up parameterization and demonstrate the existence of an observational threshold separating breaking and non-breaking cases. This threshold is based on information from two recent field campaigns, supplemented with existing observations of sea ice break-up. The data used cover a wide range of scales, from laboratory-grown sea ice to polar field observations. Remarkably, we show that both field and laboratory observations tend to converge to a single quantitative threshold at which the wave-induced sea ice breakup takes place, which opens a promising avenue for robust parametrization in operational forecasting models. |
format |
Article in Journal/Newspaper |
author |
Voermans, JJ Rabault, J Filchuk, K Ryzhov, I Heil, P Marchenko, A Collins, CO Dabboor, M Sutherland, G Babanin, AV |
author_facet |
Voermans, JJ Rabault, J Filchuk, K Ryzhov, I Heil, P Marchenko, A Collins, CO Dabboor, M Sutherland, G Babanin, AV |
author_sort |
Voermans, JJ |
title |
Experimental evidence for a universal threshold characterizing wave-induced sea ice break-up |
title_short |
Experimental evidence for a universal threshold characterizing wave-induced sea ice break-up |
title_full |
Experimental evidence for a universal threshold characterizing wave-induced sea ice break-up |
title_fullStr |
Experimental evidence for a universal threshold characterizing wave-induced sea ice break-up |
title_full_unstemmed |
Experimental evidence for a universal threshold characterizing wave-induced sea ice break-up |
title_sort |
experimental evidence for a universal threshold characterizing wave-induced sea ice break-up |
publisher |
Copernicus GmbH |
publishDate |
2020 |
url |
https://eprints.utas.edu.au/40552/ https://eprints.utas.edu.au/40552/1/143580%20-%20Experimental%20evidence%20for%20a%20universal%20threshold%20characterizing%20wave-induced.pdf |
genre |
Sea ice |
genre_facet |
Sea ice |
op_relation |
https://eprints.utas.edu.au/40552/1/143580%20-%20Experimental%20evidence%20for%20a%20universal%20threshold%20characterizing%20wave-induced.pdf Voermans, JJ, Rabault, J, Filchuk, K, Ryzhov, I, Heil, P, Marchenko, A, Collins, CO, Dabboor, M, Sutherland, G and Babanin, AV 2020 , 'Experimental evidence for a universal threshold characterizing wave-induced sea ice break-up' , Cryosphere, vol. 14, no. 11 , pp. 4265-4278 , doi:10.5194/tc-14-4265-2020 <http://dx.doi.org/10.5194/tc-14-4265-2020>. |
op_doi |
https://doi.org/10.5194/tc-14-4265-2020 |
container_title |
The Cryosphere |
container_volume |
14 |
container_issue |
11 |
container_start_page |
4265 |
op_container_end_page |
4278 |
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1766189537712668672 |