Polynyas in a high-resolution dynamic-thermodynamic sea ice model and their parameterization using flux models

This paper presents an analysis of the solutions for a steady state latent heat polynya generated by an applied wind stress acting over a semi-enclosed channel using: (a) a dynamic-thermodynamic sea ice model, and (b) a steady state flux model. We examine what processes in the sea ice model are resp...

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Main Authors: Bjornsson, H., Willmott, A.J., Mysak, L.A., Morales Maqueda, M.A.
Format: Article in Journal/Newspaper
Language:English
Published: Abingdon : Taylor and Francis Ltd. 2001
Subjects:
Online Access:https://oa.tib.eu/renate/handle/123456789/5354
https://doi.org/10.34657/3983
id fttibhannoverren:oai:oa.tib.eu:123456789/5354
record_format openpolar
spelling fttibhannoverren:oai:oa.tib.eu:123456789/5354 2023-07-30T04:02:01+02:00 Polynyas in a high-resolution dynamic-thermodynamic sea ice model and their parameterization using flux models Bjornsson, H. Willmott, A.J. Mysak, L.A. Morales Maqueda, M.A. 2001 application/pdf text/plain; charset=utf-8 https://oa.tib.eu/renate/handle/123456789/5354 https://doi.org/10.34657/3983 eng eng Abingdon : Taylor and Francis Ltd. ISSN:0280-6495 DOI:https://doi.org/10.3402/tellusa.v53i2.12184 https://oa.tib.eu/renate/handle/123456789/5354 https://doi.org/10.34657/3983 CC BY 4.0 Unported https://creativecommons.org/licenses/by/4.0/ frei zugänglich Tellus, Series A: Dynamic Meteorology and Oceanography 53 (2001), Nr. 2 flux measurement latent heat flux parameterization polynya sea ice thermodynamics Arctic Ocean ddc:550 status-type:publishedVersion doc-type:article doc-type:Text 2001 fttibhannoverren https://doi.org/10.34657/398310.3402/tellusa.v53i2.12184 2023-07-10T16:19:43Z This paper presents an analysis of the solutions for a steady state latent heat polynya generated by an applied wind stress acting over a semi-enclosed channel using: (a) a dynamic-thermodynamic sea ice model, and (b) a steady state flux model. We examine what processes in the sea ice model are responsible for the maintenance of the polynya and how sensitive the results are to the choice of rheological parameters. We find that when the ice is driven onshore by an applied wind stress, a consolidated ice pack forms downwind of a zone of strong convergence in the ice velocities. The build-up of internal stresses within the consolidated ice pack becomes a crucial factor in the formation of this zone and results in a distinct polynya edge. Furthermore, within the ice pack the across-channel ice velocity varies with the across-channel distance. It is demonstrated that provided this velocity is well represented, the steady state polynya flux model solutions are in close agreement with those of the sea ice model. Experiments with the sea ice model also show that the polynya shape and area are insensitive to (a) the sea ice rheology; (b) the imposition of either free- slip or no-slip boundary conditions. These findings are used in the development of a simplified model of the consolidated ice pack dynamics, the output of which is then compared with the sea ice model results. Finally, we discuss the relevance of this study for the modelling of the North Water Polynya in northern Baffin Bay. Article in Journal/Newspaper Arctic Arctic Ocean Baffin Bay Baffin Bay Baffin ice pack Sea ice Renate - Repositorium für Naturwissenschaften und Technik (TIB Hannover) Arctic Arctic Ocean Baffin Bay
institution Open Polar
collection Renate - Repositorium für Naturwissenschaften und Technik (TIB Hannover)
op_collection_id fttibhannoverren
language English
topic flux measurement
latent heat flux
parameterization
polynya
sea ice
thermodynamics
Arctic Ocean
ddc:550
spellingShingle flux measurement
latent heat flux
parameterization
polynya
sea ice
thermodynamics
Arctic Ocean
ddc:550
Bjornsson, H.
Willmott, A.J.
Mysak, L.A.
Morales Maqueda, M.A.
Polynyas in a high-resolution dynamic-thermodynamic sea ice model and their parameterization using flux models
topic_facet flux measurement
latent heat flux
parameterization
polynya
sea ice
thermodynamics
Arctic Ocean
ddc:550
description This paper presents an analysis of the solutions for a steady state latent heat polynya generated by an applied wind stress acting over a semi-enclosed channel using: (a) a dynamic-thermodynamic sea ice model, and (b) a steady state flux model. We examine what processes in the sea ice model are responsible for the maintenance of the polynya and how sensitive the results are to the choice of rheological parameters. We find that when the ice is driven onshore by an applied wind stress, a consolidated ice pack forms downwind of a zone of strong convergence in the ice velocities. The build-up of internal stresses within the consolidated ice pack becomes a crucial factor in the formation of this zone and results in a distinct polynya edge. Furthermore, within the ice pack the across-channel ice velocity varies with the across-channel distance. It is demonstrated that provided this velocity is well represented, the steady state polynya flux model solutions are in close agreement with those of the sea ice model. Experiments with the sea ice model also show that the polynya shape and area are insensitive to (a) the sea ice rheology; (b) the imposition of either free- slip or no-slip boundary conditions. These findings are used in the development of a simplified model of the consolidated ice pack dynamics, the output of which is then compared with the sea ice model results. Finally, we discuss the relevance of this study for the modelling of the North Water Polynya in northern Baffin Bay.
format Article in Journal/Newspaper
author Bjornsson, H.
Willmott, A.J.
Mysak, L.A.
Morales Maqueda, M.A.
author_facet Bjornsson, H.
Willmott, A.J.
Mysak, L.A.
Morales Maqueda, M.A.
author_sort Bjornsson, H.
title Polynyas in a high-resolution dynamic-thermodynamic sea ice model and their parameterization using flux models
title_short Polynyas in a high-resolution dynamic-thermodynamic sea ice model and their parameterization using flux models
title_full Polynyas in a high-resolution dynamic-thermodynamic sea ice model and their parameterization using flux models
title_fullStr Polynyas in a high-resolution dynamic-thermodynamic sea ice model and their parameterization using flux models
title_full_unstemmed Polynyas in a high-resolution dynamic-thermodynamic sea ice model and their parameterization using flux models
title_sort polynyas in a high-resolution dynamic-thermodynamic sea ice model and their parameterization using flux models
publisher Abingdon : Taylor and Francis Ltd.
publishDate 2001
url https://oa.tib.eu/renate/handle/123456789/5354
https://doi.org/10.34657/3983
geographic Arctic
Arctic Ocean
Baffin Bay
geographic_facet Arctic
Arctic Ocean
Baffin Bay
genre Arctic
Arctic Ocean
Baffin Bay
Baffin Bay
Baffin
ice pack
Sea ice
genre_facet Arctic
Arctic Ocean
Baffin Bay
Baffin Bay
Baffin
ice pack
Sea ice
op_source Tellus, Series A: Dynamic Meteorology and Oceanography 53 (2001), Nr. 2
op_relation ISSN:0280-6495
DOI:https://doi.org/10.3402/tellusa.v53i2.12184
https://oa.tib.eu/renate/handle/123456789/5354
https://doi.org/10.34657/3983
op_rights CC BY 4.0 Unported
https://creativecommons.org/licenses/by/4.0/
frei zugänglich
op_doi https://doi.org/10.34657/398310.3402/tellusa.v53i2.12184
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