Application of a Numerical Sea Ice Model to the East Greenland Area
A dynamic-thermodynamic sea ice model which employs a viscous-plastic constitutive law has been applied to East Greenland area. The model is run on a 40-km spatial scale at 1/4-day time steps for a 60-day period with forcing data beginning on 1 October 1979. Results tend to verify that the model pre...
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ftdtic:ADA120659 2023-05-15T16:03:38+02:00 Application of a Numerical Sea Ice Model to the East Greenland Area Tucker,Walter B , III COLD REGIONS RESEARCH AND ENGINEERING LAB HANOVER NH 1982-08 text/html http://www.dtic.mil/docs/citations/ADA120659 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA120659 en eng http://www.dtic.mil/docs/citations/ADA120659 APPROVED FOR PUBLIC RELEASE DTIC AND NTIS Physical and Dynamic Oceanography Snow Ice and Permafrost *SEA ICE VELOCITY OCEAN CURRENTS DYNAMICS THERMODYNAMICS GROWTH(GENERAL) WIND MOTION MATHEMATICAL PREDICTION OCEAN MODELS GREENLAND SEA Text 1982 ftdtic 2016-02-20T21:20:55Z A dynamic-thermodynamic sea ice model which employs a viscous-plastic constitutive law has been applied to East Greenland area. The model is run on a 40-km spatial scale at 1/4-day time steps for a 60-day period with forcing data beginning on 1 October 1979. Results tend to verify that the model predicts reasonable thicknesses and velocities within the ice margin. Thermodynamic ice growth produces excessive ice extent, however, probably due to inadequate parameterization of oceanic heat flux. Ice velocities near the free ice edge are also not well simulated, and preliminary investigations attribute this to an improper wind field in this area. A simulation which neglects ice strength, effectively damping ice interaciton with itself and allowing no resistance to deformation, produces excessive ice drift toward the coast and results in unrealistic nearshore thickness. A dynamics-only simulation produced reasonable results, including a more realistic ice extent, but the need for proper thermodynamics is also apparent. Other simulations verify that ice import from the Artic Basin, and ice transport due to winds and currents, were also important components in the model studies. Text East Greenland Greenland Greenland Sea Ice permafrost Sea ice Defense Technical Information Center: DTIC Technical Reports database Greenland |
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Open Polar |
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Defense Technical Information Center: DTIC Technical Reports database |
op_collection_id |
ftdtic |
language |
English |
topic |
Physical and Dynamic Oceanography Snow Ice and Permafrost *SEA ICE VELOCITY OCEAN CURRENTS DYNAMICS THERMODYNAMICS GROWTH(GENERAL) WIND MOTION MATHEMATICAL PREDICTION OCEAN MODELS GREENLAND SEA |
spellingShingle |
Physical and Dynamic Oceanography Snow Ice and Permafrost *SEA ICE VELOCITY OCEAN CURRENTS DYNAMICS THERMODYNAMICS GROWTH(GENERAL) WIND MOTION MATHEMATICAL PREDICTION OCEAN MODELS GREENLAND SEA Tucker,Walter B , III Application of a Numerical Sea Ice Model to the East Greenland Area |
topic_facet |
Physical and Dynamic Oceanography Snow Ice and Permafrost *SEA ICE VELOCITY OCEAN CURRENTS DYNAMICS THERMODYNAMICS GROWTH(GENERAL) WIND MOTION MATHEMATICAL PREDICTION OCEAN MODELS GREENLAND SEA |
description |
A dynamic-thermodynamic sea ice model which employs a viscous-plastic constitutive law has been applied to East Greenland area. The model is run on a 40-km spatial scale at 1/4-day time steps for a 60-day period with forcing data beginning on 1 October 1979. Results tend to verify that the model predicts reasonable thicknesses and velocities within the ice margin. Thermodynamic ice growth produces excessive ice extent, however, probably due to inadequate parameterization of oceanic heat flux. Ice velocities near the free ice edge are also not well simulated, and preliminary investigations attribute this to an improper wind field in this area. A simulation which neglects ice strength, effectively damping ice interaciton with itself and allowing no resistance to deformation, produces excessive ice drift toward the coast and results in unrealistic nearshore thickness. A dynamics-only simulation produced reasonable results, including a more realistic ice extent, but the need for proper thermodynamics is also apparent. Other simulations verify that ice import from the Artic Basin, and ice transport due to winds and currents, were also important components in the model studies. |
author2 |
COLD REGIONS RESEARCH AND ENGINEERING LAB HANOVER NH |
format |
Text |
author |
Tucker,Walter B , III |
author_facet |
Tucker,Walter B , III |
author_sort |
Tucker,Walter B , III |
title |
Application of a Numerical Sea Ice Model to the East Greenland Area |
title_short |
Application of a Numerical Sea Ice Model to the East Greenland Area |
title_full |
Application of a Numerical Sea Ice Model to the East Greenland Area |
title_fullStr |
Application of a Numerical Sea Ice Model to the East Greenland Area |
title_full_unstemmed |
Application of a Numerical Sea Ice Model to the East Greenland Area |
title_sort |
application of a numerical sea ice model to the east greenland area |
publishDate |
1982 |
url |
http://www.dtic.mil/docs/citations/ADA120659 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA120659 |
geographic |
Greenland |
geographic_facet |
Greenland |
genre |
East Greenland Greenland Greenland Sea Ice permafrost Sea ice |
genre_facet |
East Greenland Greenland Greenland Sea Ice permafrost Sea ice |
op_source |
DTIC AND NTIS |
op_relation |
http://www.dtic.mil/docs/citations/ADA120659 |
op_rights |
APPROVED FOR PUBLIC RELEASE |
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1766399331436331008 |