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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American Association for the Advancement of Science (AAAS)
1984
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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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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 |
_version_ |
1801372701502210048 |