Ocean Circulation: Its Effects on Seasonal Sea-Ice Simulations

A diagnostic ice-ocean model of the Arctic, Greenland, and Norwegian seas is constructed and used to examine the role of ocean circulation in seasonal sea-ice simulations. The model includes lateral ice motion and three-dimensional ocean circulation. The ocean portion of the model is weakly forced b...

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Bibliographic Details
Published in:Science
Main Authors: Hibler, W. D., Bryan, Kirk
Format: Article in Journal/Newspaper
Language:English
Published: American Association for the Advancement of Science (AAAS) 1984
Subjects:
Online Access:http://dx.doi.org/10.1126/science.224.4648.489
https://www.science.org/doi/pdf/10.1126/science.224.4648.489
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spelling craaas:10.1126/science.224.4648.489 2024-06-09T07:43:52+00:00 Ocean Circulation: Its Effects on Seasonal Sea-Ice Simulations Hibler, W. D. Bryan, Kirk 1984 http://dx.doi.org/10.1126/science.224.4648.489 https://www.science.org/doi/pdf/10.1126/science.224.4648.489 en eng American Association for the Advancement of Science (AAAS) Science volume 224, issue 4648, page 489-492 ISSN 0036-8075 1095-9203 journal-article 1984 craaas https://doi.org/10.1126/science.224.4648.489 2024-05-16T12:54:24Z A diagnostic ice-ocean model of the Arctic, Greenland, and Norwegian seas is constructed and used to examine the role of ocean circulation in seasonal sea-ice simulations. The model includes lateral ice motion and three-dimensional ocean circulation. The ocean portion of the model is weakly forced by observed temperature and salinity data. Simulation results show that including modeled ocean circulation in seasonal sea-ice simulations substantially improves the predicted ice drift and ice margin location. Simulations that do not include lateral ocean movement predict a much less realistic ice edge. Article in Journal/Newspaper Arctic Greenland Sea ice AAAS Resource Center (American Association for the Advancement of Science) Arctic Greenland Science 224 4648 489 492
institution Open Polar
collection AAAS Resource Center (American Association for the Advancement of Science)
op_collection_id craaas
language English
description A diagnostic ice-ocean model of the Arctic, Greenland, and Norwegian seas is constructed and used to examine the role of ocean circulation in seasonal sea-ice simulations. The model includes lateral ice motion and three-dimensional ocean circulation. The ocean portion of the model is weakly forced by observed temperature and salinity data. Simulation results show that including modeled ocean circulation in seasonal sea-ice simulations substantially improves the predicted ice drift and ice margin location. Simulations that do not include lateral ocean movement predict a much less realistic ice edge.
format Article in Journal/Newspaper
author Hibler, W. D.
Bryan, Kirk
spellingShingle Hibler, W. D.
Bryan, Kirk
Ocean Circulation: Its Effects on Seasonal Sea-Ice Simulations
author_facet Hibler, W. D.
Bryan, Kirk
author_sort Hibler, W. D.
title Ocean Circulation: Its Effects on Seasonal Sea-Ice Simulations
title_short Ocean Circulation: Its Effects on Seasonal Sea-Ice Simulations
title_full Ocean Circulation: Its Effects on Seasonal Sea-Ice Simulations
title_fullStr Ocean Circulation: Its Effects on Seasonal Sea-Ice Simulations
title_full_unstemmed Ocean Circulation: Its Effects on Seasonal Sea-Ice Simulations
title_sort ocean circulation: its effects on seasonal sea-ice simulations
publisher American Association for the Advancement of Science (AAAS)
publishDate 1984
url http://dx.doi.org/10.1126/science.224.4648.489
https://www.science.org/doi/pdf/10.1126/science.224.4648.489
geographic Arctic
Greenland
geographic_facet Arctic
Greenland
genre Arctic
Greenland
Sea ice
genre_facet Arctic
Greenland
Sea ice
op_source Science
volume 224, issue 4648, page 489-492
ISSN 0036-8075 1095-9203
op_doi https://doi.org/10.1126/science.224.4648.489
container_title Science
container_volume 224
container_issue 4648
container_start_page 489
op_container_end_page 492
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