Effects of Wave-Induced Sea Ice Break-Up and Mixing in a High-Resolution Coupled Ice-Ocean Model

Arctic sea ice plays a vital role in modulating the global climate. In the most recent decades, the rapid decline of the Arctic summer sea ice cover has exposed increasing areas of ice-free ocean, with sufficient fetch for waves to develop. This has highlighted the complex and not well-understood na...

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Main Authors: Junde Li, Alexander V. Babanin, Qingxiang Liu, Joey J. Voermans, Petra Heil, Youmin Tang
Format: Article
Language:English
Published: MDPI AG 2021-03-01
Series:Journal of Marine Science and Engineering
Subjects:
Online Access:https://www.mdpi.com/2077-1312/9/4/365
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author Junde Li
Alexander V. Babanin
Qingxiang Liu
Joey J. Voermans
Petra Heil
Youmin Tang
author_facet Junde Li
Alexander V. Babanin
Qingxiang Liu
Joey J. Voermans
Petra Heil
Youmin Tang
author_sort Junde Li
collection DOAJ
description Arctic sea ice plays a vital role in modulating the global climate. In the most recent decades, the rapid decline of the Arctic summer sea ice cover has exposed increasing areas of ice-free ocean, with sufficient fetch for waves to develop. This has highlighted the complex and not well-understood nature of wave-ice interactions, requiring modeling effort. Here, we introduce two independent parameterizations in a high-resolution coupled ice-ocean model to investigate the effects of wave-induced sea ice break-up (through albedo change) and mixing on the Arctic sea ice simulation. Our results show that wave-induced sea ice break-up leads to increases in sea ice concentration and thickness in the Bering Sea, the Baffin Sea and the Barents Sea during the ice growth season, but accelerates the sea ice melt in the Chukchi Sea and the East Siberian Sea in summer. Further, wave-induced mixing can decelerate the sea ice formation in winter and the sea ice melt in summer by exchanging the heat fluxes between the surface and subsurface layer. As our baseline model underestimates sea ice cover in winter and produces more sea ice in summer, wave-induced sea ice break-up plays a positive role in improving the sea ice simulation. This study provides two independent parameterizations to directly include the wave effects into the sea ice models, with important implications for the future sea ice model development.
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spelling doaj.art-e94b4a4d98c940298c9ada4abac15cce2023-11-21T13:19:26ZengMDPI AGJournal of Marine Science and Engineering2077-13122021-03-019436510.3390/jmse9040365Effects of Wave-Induced Sea Ice Break-Up and Mixing in a High-Resolution Coupled Ice-Ocean ModelJunde Li0Alexander V. Babanin1Qingxiang Liu2Joey J. Voermans3Petra Heil4Youmin Tang5Department of Infrastructure Engineering, University of Melbourne, Melbourne, VIC 3010, AustraliaDepartment of Infrastructure Engineering, University of Melbourne, Melbourne, VIC 3010, AustraliaDepartment of Infrastructure Engineering, University of Melbourne, Melbourne, VIC 3010, AustraliaDepartment of Infrastructure Engineering, University of Melbourne, Melbourne, VIC 3010, AustraliaAustralian Antarctica Division and Australian Antarctic Programme Partnership, University of Tasmania, Hobart, TAS 7001, AustraliaEnvironmental Science and Engineering, University of Northern British Columbia, Prince George, BC V2N 4Z9, CanadaArctic sea ice plays a vital role in modulating the global climate. In the most recent decades, the rapid decline of the Arctic summer sea ice cover has exposed increasing areas of ice-free ocean, with sufficient fetch for waves to develop. This has highlighted the complex and not well-understood nature of wave-ice interactions, requiring modeling effort. Here, we introduce two independent parameterizations in a high-resolution coupled ice-ocean model to investigate the effects of wave-induced sea ice break-up (through albedo change) and mixing on the Arctic sea ice simulation. Our results show that wave-induced sea ice break-up leads to increases in sea ice concentration and thickness in the Bering Sea, the Baffin Sea and the Barents Sea during the ice growth season, but accelerates the sea ice melt in the Chukchi Sea and the East Siberian Sea in summer. Further, wave-induced mixing can decelerate the sea ice formation in winter and the sea ice melt in summer by exchanging the heat fluxes between the surface and subsurface layer. As our baseline model underestimates sea ice cover in winter and produces more sea ice in summer, wave-induced sea ice break-up plays a positive role in improving the sea ice simulation. This study provides two independent parameterizations to directly include the wave effects into the sea ice models, with important implications for the future sea ice model development.https://www.mdpi.com/2077-1312/9/4/365wave-induced sea ice break-upwave-induced mixingice-ocean coupled model
spellingShingle Junde Li
Alexander V. Babanin
Qingxiang Liu
Joey J. Voermans
Petra Heil
Youmin Tang
Effects of Wave-Induced Sea Ice Break-Up and Mixing in a High-Resolution Coupled Ice-Ocean Model
Journal of Marine Science and Engineering
wave-induced sea ice break-up
wave-induced mixing
ice-ocean coupled model
title Effects of Wave-Induced Sea Ice Break-Up and Mixing in a High-Resolution Coupled Ice-Ocean Model
title_full Effects of Wave-Induced Sea Ice Break-Up and Mixing in a High-Resolution Coupled Ice-Ocean Model
title_fullStr Effects of Wave-Induced Sea Ice Break-Up and Mixing in a High-Resolution Coupled Ice-Ocean Model
title_full_unstemmed Effects of Wave-Induced Sea Ice Break-Up and Mixing in a High-Resolution Coupled Ice-Ocean Model
title_short Effects of Wave-Induced Sea Ice Break-Up and Mixing in a High-Resolution Coupled Ice-Ocean Model
title_sort effects of wave induced sea ice break up and mixing in a high resolution coupled ice ocean model
topic wave-induced sea ice break-up
wave-induced mixing
ice-ocean coupled model
url https://www.mdpi.com/2077-1312/9/4/365
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