Importance of ice-ocean interactions for the global ocean circulation: A model study
Numerical experiments are conducted with a coarse-resolution global ice-ocean model in order to determine to what degree the sea ice-ocean exchanges of heat, salt/freshwater, and momentum control the general circulation of the world ocean on long timescales. These experiments reveal that the formati...
Published in: | Journal of Geophysical Research: Oceans |
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Amer Geophysical Union
1999
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Online Access: | http://hdl.handle.net/2078.1/44125 https://doi.org/10.1029/1999JC900215 |
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ftunivlouvain:oai:dial.uclouvain.be:boreal:44125 2024-05-19T07:30:43+00:00 Importance of ice-ocean interactions for the global ocean circulation: A model study Goosse, Hugues Fichefet, Thierry UCL - SC/PHYS - Département de physique UCL - SST/ELI/ELIC - Earth & Climate 1999 http://hdl.handle.net/2078.1/44125 https://doi.org/10.1029/1999JC900215 eng eng Amer Geophysical Union boreal:44125 http://hdl.handle.net/2078.1/44125 doi:10.1029/1999JC900215 urn:ISSN:0148-0227 Journal of Geophysical Research, Vol. 104, no. C10, p. 23337-23355 (1999) info:eu-repo/semantics/article 1999 ftunivlouvain https://doi.org/10.1029/1999JC900215 2024-04-24T01:48:21Z Numerical experiments are conducted with a coarse-resolution global ice-ocean model in order to determine to what degree the sea ice-ocean exchanges of heat, salt/freshwater, and momentum control the general circulation of the world ocean on long timescales. These experiments reveal that the formation of North Atlantic Deep Water (NADW) in the model results from the strong heat losses that occur at the oceanic surface in the high-latitude North Atlantic. The large-scale ice-ocean interactions have nearly no influence on this process. In particular, neglecting the freshwater flux associated with the southward ice transport at Fram Strait does not impact seriously on the salinity of the Greenland and Norwegian Seas. At equilibrium the absence of this freshwater flux is balanced by an enhanced oceanic freshwater transport from the Arctic. Furthermore, it appears that the model NADW formation does not critically depend on the media (ice or ocean) transporting the freshwater. Besides, both the salt/freshwater and heat exchanges between sea ice and ocean are crucial in the Southern Ocean for the deep water production, properties, and export. The large amount of brine released during ice formation on the model Antarctic continental shelf leads to very high salinities there. The resulting dense shelf waters are then transported toward great depths after some mixing with ambient waters, finally forming the Antarctic Bottom Water body. On the other hand, the net ice melting associated with ice convergence in some areas, such as the southwestern Pacific, stabilizes the water column and forbids deep mixing in these regions. Furthermore, the contact with the ice imposes that the polar surface waters must be maintained very close to their freezing point temperature. Our results suggest that this process takes an important part in increasing the density of the Antarctic Bottom Water. We also show that the modifications of the stress at the ocean surface induced by the internal ice stress have only a regional effect. Article in Journal/Newspaper Antarc* Antarctic Arctic Fram Strait Greenland NADW North Atlantic Deep Water North Atlantic Sea ice Southern Ocean DIAL@UCLouvain (Université catholique de Louvain) Journal of Geophysical Research: Oceans 104 C10 23337 23355 |
institution |
Open Polar |
collection |
DIAL@UCLouvain (Université catholique de Louvain) |
op_collection_id |
ftunivlouvain |
language |
English |
description |
Numerical experiments are conducted with a coarse-resolution global ice-ocean model in order to determine to what degree the sea ice-ocean exchanges of heat, salt/freshwater, and momentum control the general circulation of the world ocean on long timescales. These experiments reveal that the formation of North Atlantic Deep Water (NADW) in the model results from the strong heat losses that occur at the oceanic surface in the high-latitude North Atlantic. The large-scale ice-ocean interactions have nearly no influence on this process. In particular, neglecting the freshwater flux associated with the southward ice transport at Fram Strait does not impact seriously on the salinity of the Greenland and Norwegian Seas. At equilibrium the absence of this freshwater flux is balanced by an enhanced oceanic freshwater transport from the Arctic. Furthermore, it appears that the model NADW formation does not critically depend on the media (ice or ocean) transporting the freshwater. Besides, both the salt/freshwater and heat exchanges between sea ice and ocean are crucial in the Southern Ocean for the deep water production, properties, and export. The large amount of brine released during ice formation on the model Antarctic continental shelf leads to very high salinities there. The resulting dense shelf waters are then transported toward great depths after some mixing with ambient waters, finally forming the Antarctic Bottom Water body. On the other hand, the net ice melting associated with ice convergence in some areas, such as the southwestern Pacific, stabilizes the water column and forbids deep mixing in these regions. Furthermore, the contact with the ice imposes that the polar surface waters must be maintained very close to their freezing point temperature. Our results suggest that this process takes an important part in increasing the density of the Antarctic Bottom Water. We also show that the modifications of the stress at the ocean surface induced by the internal ice stress have only a regional effect. |
author2 |
UCL - SC/PHYS - Département de physique UCL - SST/ELI/ELIC - Earth & Climate |
format |
Article in Journal/Newspaper |
author |
Goosse, Hugues Fichefet, Thierry |
spellingShingle |
Goosse, Hugues Fichefet, Thierry Importance of ice-ocean interactions for the global ocean circulation: A model study |
author_facet |
Goosse, Hugues Fichefet, Thierry |
author_sort |
Goosse, Hugues |
title |
Importance of ice-ocean interactions for the global ocean circulation: A model study |
title_short |
Importance of ice-ocean interactions for the global ocean circulation: A model study |
title_full |
Importance of ice-ocean interactions for the global ocean circulation: A model study |
title_fullStr |
Importance of ice-ocean interactions for the global ocean circulation: A model study |
title_full_unstemmed |
Importance of ice-ocean interactions for the global ocean circulation: A model study |
title_sort |
importance of ice-ocean interactions for the global ocean circulation: a model study |
publisher |
Amer Geophysical Union |
publishDate |
1999 |
url |
http://hdl.handle.net/2078.1/44125 https://doi.org/10.1029/1999JC900215 |
genre |
Antarc* Antarctic Arctic Fram Strait Greenland NADW North Atlantic Deep Water North Atlantic Sea ice Southern Ocean |
genre_facet |
Antarc* Antarctic Arctic Fram Strait Greenland NADW North Atlantic Deep Water North Atlantic Sea ice Southern Ocean |
op_source |
Journal of Geophysical Research, Vol. 104, no. C10, p. 23337-23355 (1999) |
op_relation |
boreal:44125 http://hdl.handle.net/2078.1/44125 doi:10.1029/1999JC900215 urn:ISSN:0148-0227 |
op_doi |
https://doi.org/10.1029/1999JC900215 |
container_title |
Journal of Geophysical Research: Oceans |
container_volume |
104 |
container_issue |
C10 |
container_start_page |
23337 |
op_container_end_page |
23355 |
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1799488852639875072 |