Experimental evidence for a universal threshold characterizing wave-induced sea ice break-up

<p>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 parameter...

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Main Authors: J. J. Voermans, J. Rabault, K. Filchuk, I. Ryzhov, P. Heil, A. Marchenko, C. O. Collins III, M. Dabboor, G. Sutherland, A. V. Babanin
Format: Article
Language:English
Published: Copernicus Publications 2020-11-01
Series:The Cryosphere
Online Access:https://tc.copernicus.org/articles/14/4265/2020/tc-14-4265-2020.pdf
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author J. J. Voermans
J. Rabault
J. Rabault
K. Filchuk
I. Ryzhov
P. Heil
A. Marchenko
C. O. Collins III
M. Dabboor
G. Sutherland
A. V. Babanin
A. V. Babanin
author_facet J. J. Voermans
J. Rabault
J. Rabault
K. Filchuk
I. Ryzhov
P. Heil
A. Marchenko
C. O. Collins III
M. Dabboor
G. Sutherland
A. V. Babanin
A. V. Babanin
author_sort J. J. Voermans
collection DOAJ
description <p>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 break-up takes place, which opens a promising avenue for robust parametrization in operational forecasting models.</p>
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spelling doaj.art-576d43e2ea154040b439e213843886e02022-12-21T22:09:50ZengCopernicus PublicationsThe Cryosphere1994-04161994-04242020-11-01144265427810.5194/tc-14-4265-2020Experimental evidence for a universal threshold characterizing wave-induced sea ice break-upJ. J. Voermans0J. Rabault1J. Rabault2K. Filchuk3I. Ryzhov4P. Heil5A. Marchenko6C. O. Collins III7M. Dabboor8G. Sutherland9A. V. Babanin10A. V. Babanin11Department of Infrastructure Engineering, University of Melbourne, Parkville, AustraliaNorwegian Meteorological Institute, Oslo, NorwayDepartment of Mathematics, University of Oslo, Oslo, NorwayArctic and Antarctic Research Institute (AARI), St. Petersburg, Russian FederationArctic and Antarctic Research Institute (AARI), St. Petersburg, Russian FederationAustralian Antarctic Division and Australian Antarctic Program Partnership, University of Tasmania, Hobart, AustraliaThe University Centre in Svalbard, Longyearbyen, NorwayCoastal and Hydraulics Laboratory, U.S. Army Engineering Research and Development Center, Duck, North Carolina, USAScience and Technology Branch, Environment and Climate Change Canada, Dorval, CanadaEnvironmental Numerical Prediction Research, Environment and Climate Change Canada, Dorval, CanadaDepartment of Infrastructure Engineering, University of Melbourne, Parkville, AustraliaLaboratory for Regional Oceanography and Numerical Modeling, National Laboratory for Marine Science and Technology, Qingdao, China<p>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 break-up takes place, which opens a promising avenue for robust parametrization in operational forecasting models.</p>https://tc.copernicus.org/articles/14/4265/2020/tc-14-4265-2020.pdf
spellingShingle J. J. Voermans
J. Rabault
J. Rabault
K. Filchuk
I. Ryzhov
P. Heil
A. Marchenko
C. O. Collins III
M. Dabboor
G. Sutherland
A. V. Babanin
A. V. Babanin
Experimental evidence for a universal threshold characterizing wave-induced sea ice break-up
The Cryosphere
title 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_short 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
url https://tc.copernicus.org/articles/14/4265/2020/tc-14-4265-2020.pdf
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