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Ocean circulation in a warming climate

Author

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  • J. R. Toggweiler

    (J. R. Toggweiler is at the Geophysical Fluid Dynamics Laboratory, National Oceanic and Atmospheric Administration, Princeton, New Jersey 08542, USA.)

  • Joellen Russell

    (University of Arizona, Tucson, Arizona 85721, USA.)

Abstract

Climate models predict that the ocean's circulation will weaken in response to global warming, but the warming at the end of the last ice age suggests a different outcome.

Suggested Citation

  • J. R. Toggweiler & Joellen Russell, 2008. "Ocean circulation in a warming climate," Nature, Nature, vol. 451(7176), pages 286-288, January.
    • Handle: RePEc:nat:nature:v:451:y:2008:i:7176:d:10.1038_nature06590
    DOI: 10.1038/nature06590
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    Cited by:

    1. Fernando Taboada & Ricardo Anadón, 2012. "Patterns of change in sea surface temperature in the North Atlantic during the last three decades: beyond mean trends," Climatic Change, Springer, vol. 115(2), pages 419-431, November.
    2. Michael E. Weber & Nicholas R. Golledge & Chris J. Fogwill & Chris S. M. Turney & Zoë A. Thomas, 2021. "Decadal-scale onset and termination of Antarctic ice-mass loss during the last deglaciation," Nature Communications, Nature, vol. 12(1), pages 1-13, December.

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