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Ocean response to greenhouse warming

Nature volume 345, pages 589–593 (1990)Cite this article

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.

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Authors and Affiliations

  1. Max-Planck Institut für Meteorologie, Bundesstrasse 55, D-2000, Hamburg, 13, FRG

    Uwe Mikolajewicz, Benjamin D. Santer & Ernst Maier-Reimer

Authors
  1. Uwe Mikolajewicz
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  2. Benjamin D. Santer
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  3. Ernst Maier-Reimer
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Mikolajewicz, U., Santer, B. & Maier-Reimer, E. Ocean response to greenhouse warming. Nature 345, 589–593 (1990). https://doi.org/10.1038/345589a0

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