Sensitivity of a global sea ice model to the treatment of ice thermodynamics and dynamics
The sensitivity of a global thermodynamic-dynamic sea ice model coupled to a one-dimensional upper ocean model to degradations of the model physics is investigated. A single set of parameter values is employed to simultaneously simulate the Arctic and Antarctic ice regimes. A control run carried out...
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American Geophysical Union
1997
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Online Access: | http://hdl.handle.net/2078.1/129428 |
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ftunistlouisbrus:oai:dial.uclouvain.be:boreal:129428 2024-05-12T07:55:55+00:00 Sensitivity of a global sea ice model to the treatment of ice thermodynamics and dynamics Fichefet, Thierry Morales Maqueda, M.A. UCL - SST/ELI/ELIC - Earth & Climate 1997 http://hdl.handle.net/2078.1/129428 eng eng American Geophysical Union boreal:129428 http://hdl.handle.net/2078.1/129428 urn:ISSN:0148-0227 urn:EISSN:2156-2202 info:eu-repo/semantics/restrictedAccess Journal of Geophysical Research, Vol. 102, no.12, p. 12609-12646 (1997) dynamics global model sea ice sensitivity thermodynamics CISM : CECI 1443 info:eu-repo/semantics/article 1997 ftunistlouisbrus 2024-04-18T18:00:45Z The sensitivity of a global thermodynamic-dynamic sea ice model coupled to a one-dimensional upper ocean model to degradations of the model physics is investigated. A single set of parameter values is employed to simultaneously simulate the Arctic and Antarctic ice regimes. A control run carried out with the model demonstrates that it does reasonably well in simulating the seasonal waxing and waning of both ice packs. The sensitivity study focuses on physical processes pertaining to (1) the vertical growth and decay of sea ice, (2) the lateral growth and decay of sea ice, and (3) the sea ice dynamics. A total of nine sensitivity experiments have been performed. It appears that the thermal inertia of the snow-ice system is negligible in the Antarctic but not in the Arctic. It is also found that the inclusion of a prognostic snow layer and of a scheme of snow ice formation is important for sea ice modeling in the Southern Hemisphere. Furthermore, results suggest that the thermodynamic effect of the subgrid-scale snow and ice thickness distributions, the existence of open water areas within the ice cover, and the ice motion play a crucial role in determining the seasonal behavior of both ice packs. Article in Journal/Newspaper Antarc* Antarctic Arctic Sea ice DIAL@USL-B (Université Saint-Louis, Bruxelles) Antarctic Arctic The Antarctic |
institution |
Open Polar |
collection |
DIAL@USL-B (Université Saint-Louis, Bruxelles) |
op_collection_id |
ftunistlouisbrus |
language |
English |
topic |
dynamics global model sea ice sensitivity thermodynamics CISM : CECI 1443 |
spellingShingle |
dynamics global model sea ice sensitivity thermodynamics CISM : CECI 1443 Fichefet, Thierry Morales Maqueda, M.A. Sensitivity of a global sea ice model to the treatment of ice thermodynamics and dynamics |
topic_facet |
dynamics global model sea ice sensitivity thermodynamics CISM : CECI 1443 |
description |
The sensitivity of a global thermodynamic-dynamic sea ice model coupled to a one-dimensional upper ocean model to degradations of the model physics is investigated. A single set of parameter values is employed to simultaneously simulate the Arctic and Antarctic ice regimes. A control run carried out with the model demonstrates that it does reasonably well in simulating the seasonal waxing and waning of both ice packs. The sensitivity study focuses on physical processes pertaining to (1) the vertical growth and decay of sea ice, (2) the lateral growth and decay of sea ice, and (3) the sea ice dynamics. A total of nine sensitivity experiments have been performed. It appears that the thermal inertia of the snow-ice system is negligible in the Antarctic but not in the Arctic. It is also found that the inclusion of a prognostic snow layer and of a scheme of snow ice formation is important for sea ice modeling in the Southern Hemisphere. Furthermore, results suggest that the thermodynamic effect of the subgrid-scale snow and ice thickness distributions, the existence of open water areas within the ice cover, and the ice motion play a crucial role in determining the seasonal behavior of both ice packs. |
author2 |
UCL - SST/ELI/ELIC - Earth & Climate |
format |
Article in Journal/Newspaper |
author |
Fichefet, Thierry Morales Maqueda, M.A. |
author_facet |
Fichefet, Thierry Morales Maqueda, M.A. |
author_sort |
Fichefet, Thierry |
title |
Sensitivity of a global sea ice model to the treatment of ice thermodynamics and dynamics |
title_short |
Sensitivity of a global sea ice model to the treatment of ice thermodynamics and dynamics |
title_full |
Sensitivity of a global sea ice model to the treatment of ice thermodynamics and dynamics |
title_fullStr |
Sensitivity of a global sea ice model to the treatment of ice thermodynamics and dynamics |
title_full_unstemmed |
Sensitivity of a global sea ice model to the treatment of ice thermodynamics and dynamics |
title_sort |
sensitivity of a global sea ice model to the treatment of ice thermodynamics and dynamics |
publisher |
American Geophysical Union |
publishDate |
1997 |
url |
http://hdl.handle.net/2078.1/129428 |
geographic |
Antarctic Arctic The Antarctic |
geographic_facet |
Antarctic Arctic The Antarctic |
genre |
Antarc* Antarctic Arctic Sea ice |
genre_facet |
Antarc* Antarctic Arctic Sea ice |
op_source |
Journal of Geophysical Research, Vol. 102, no.12, p. 12609-12646 (1997) |
op_relation |
boreal:129428 http://hdl.handle.net/2078.1/129428 urn:ISSN:0148-0227 urn:EISSN:2156-2202 |
op_rights |
info:eu-repo/semantics/restrictedAccess |
_version_ |
1798835806763220992 |