Ocean response to greenhouse warming

Changes in surface air temperature resulting from a doubling in atmospheric carbon dioxide drive changes in ocean circulation. Results from an ocean general circulation model project a global mean sea level rise from thermal expansion alone to be 19cm in 50 years. Regional values, however, can vary:...

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Published in:Nature
Main Authors: Mikolajewicz, U., Santer , B., Maier-Reimer, E.
Format: Article in Journal/Newspaper
Language:English
Published: 1990
Subjects:
Online Access:http://hdl.handle.net/21.11116/0000-0000-F7F6-4
http://hdl.handle.net/21.11116/0000-0000-F7F8-2
http://hdl.handle.net/21.11116/0000-0000-F7F9-1
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spelling ftpubman:oai:pure.mpg.de:item_2566456 2023-08-20T04:08:16+02:00 Ocean response to greenhouse warming Mikolajewicz, U. Santer , B. Maier-Reimer, E. 1990 application/pdf http://hdl.handle.net/21.11116/0000-0000-F7F6-4 http://hdl.handle.net/21.11116/0000-0000-F7F8-2 http://hdl.handle.net/21.11116/0000-0000-F7F9-1 eng eng info:eu-repo/semantics/altIdentifier/doi/10.1038/345589a0 http://hdl.handle.net/21.11116/0000-0000-F7F6-4 http://hdl.handle.net/21.11116/0000-0000-F7F8-2 http://hdl.handle.net/21.11116/0000-0000-F7F9-1 info:eu-repo/semantics/openAccess Nature Report / Max-Planck-Institut für Meteorologie info:eu-repo/semantics/article 1990 ftpubman https://doi.org/10.1038/345589a0 2023-08-01T22:35:43Z Changes in surface air temperature resulting from a doubling in atmospheric carbon dioxide drive changes in ocean circulation. Results from an ocean general circulation model project a global mean sea level rise from thermal expansion alone to be 19cm in 50 years. Regional values, however, can vary: a rise of 40cm is projected in the North Atlantic (owing to reduction of deep-water formation), whereas the level of the Ross Sea actually falls through changes in ocean circulation. Article in Journal/Newspaper North Atlantic Ross Sea Max Planck Society: MPG.PuRe Ross Sea Nature 345 6276 589 593
institution Open Polar
collection Max Planck Society: MPG.PuRe
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language English
description Changes in surface air temperature resulting from a doubling in atmospheric carbon dioxide drive changes in ocean circulation. Results from an ocean general circulation model project a global mean sea level rise from thermal expansion alone to be 19cm in 50 years. Regional values, however, can vary: a rise of 40cm is projected in the North Atlantic (owing to reduction of deep-water formation), whereas the level of the Ross Sea actually falls through changes in ocean circulation.
format Article in Journal/Newspaper
author Mikolajewicz, U.
Santer , B.
Maier-Reimer, E.
spellingShingle Mikolajewicz, U.
Santer , B.
Maier-Reimer, E.
Ocean response to greenhouse warming
author_facet Mikolajewicz, U.
Santer , B.
Maier-Reimer, E.
author_sort Mikolajewicz, U.
title Ocean response to greenhouse warming
title_short Ocean response to greenhouse warming
title_full Ocean response to greenhouse warming
title_fullStr Ocean response to greenhouse warming
title_full_unstemmed Ocean response to greenhouse warming
title_sort ocean response to greenhouse warming
publishDate 1990
url http://hdl.handle.net/21.11116/0000-0000-F7F6-4
http://hdl.handle.net/21.11116/0000-0000-F7F8-2
http://hdl.handle.net/21.11116/0000-0000-F7F9-1
geographic Ross Sea
geographic_facet Ross Sea
genre North Atlantic
Ross Sea
genre_facet North Atlantic
Ross Sea
op_source Nature
Report / Max-Planck-Institut für Meteorologie
op_relation info:eu-repo/semantics/altIdentifier/doi/10.1038/345589a0
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op_rights info:eu-repo/semantics/openAccess
op_doi https://doi.org/10.1038/345589a0
container_title Nature
container_volume 345
container_issue 6276
container_start_page 589
op_container_end_page 593
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