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Simulation of modern and glacial climates with a coupled global model of intermediate complexity

Author

Listed:
  • Andrey Ganopolski

    (Potsdam Institute for Climate Impact Research (PIK))

  • Stefan Rahmstorf

    (Potsdam Institute for Climate Impact Research (PIK))

  • Vladimir Petoukhov

    (Potsdam Institute for Climate Impact Research (PIK))

  • Martin Claussen

    (Potsdam Institute for Climate Impact Research (PIK))

Abstract

A global coupled ocean–atmosphere model of intermediate complexity is used to simulate the equilibrium climate of both today and the Last Glacial Maximum, around 21,000 years ago. The model successfully predicts the atmospheric and oceanic circulations, temperature distribution, hydrological cycle and sea-ice cover of both periods without using ‘flux adjustments’. Changes in oceanic circulation, particularly in the Atlantic Ocean, play an important role in glacial cooling.

Suggested Citation

  • Andrey Ganopolski & Stefan Rahmstorf & Vladimir Petoukhov & Martin Claussen, 1998. "Simulation of modern and glacial climates with a coupled global model of intermediate complexity," Nature, Nature, vol. 391(6665), pages 351-356, January.
    • Handle: RePEc:nat:nature:v:391:y:1998:i:6665:d:10.1038_34839
    DOI: 10.1038/34839
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    Cited by:

    1. Megan Ceronsky & David Anthoff & Cameron Hepburn & Richard S.J. Tol, 2005. "Checking The Price Tag On Catastrophe: The Social Cost Of Carbon Under Non-Linear Climate Response," Working Papers FNU-87, Research unit Sustainability and Global Change, Hamburg University, revised Aug 2005.

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