Ocean response to greenhouse warming

Mikolajewicz, Uwe, Santer, Benjamin D. and Maier-Reimer, Ernst (1990) Ocean response to greenhouse warming. Nature, 345 (6276). pp. 589-593. ISSN 0028-0836

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Abstract

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.

Item Type: Article
Uncontrolled Keywords: general ,/dk/atira/pure/subjectarea/asjc/1000
Faculty \ School: Faculty of Science > School of Environmental Sciences
Related URLs:
Depositing User: LivePure Connector
Date Deposited: 23 Mar 2026 10:30
Last Modified: 23 Mar 2026 10:30
URI: https://ueaeprints.uea.ac.uk/id/eprint/102549
DOI: 10.1038/345589a0

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