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.
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Acknowledgements
S.R. and M.C. acknowledge discussions with S. Joussaume, A. Broccoli and others at the European Science Foundation's Research Conference on Paleoclimate Modelling and Analysis, in Castelvecchio Pascoli. We received comments on the manuscript from E. Bard; D. Smart critically read the manuscript. This work was supported by the European Union's Environment and Climate programme.
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Ganopolski, A., Rahmstorf, S., Petoukhov, V. et al. Simulation of modern and glacial climates with a coupled global model of intermediate complexity. Nature 391, 351–356 (1998). https://doi.org/10.1038/34839
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DOI: https://doi.org/10.1038/34839
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