Articles | Volume 3, issue 2
https://doi.org/10.5194/gmd-3-377-2010
https://doi.org/10.5194/gmd-3-377-2010
25 Aug 2010
 | 25 Aug 2010

The mechanism behind internally generated centennial-to-millennial scale climate variability in an earth system model of intermediate complexity

T. Friedrich, A. Timmermann, L. Menviel, O. Elison Timm, A. Mouchet, and D. M. Roche

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Cited articles

Aeberhardt, M., Blatter, M., and Stocker, T. F.: Variability on the century timescale and regime changes in a stochastically forced zonally averaged ocean-atmosphere model, Geophys. Res. Lett., 27(9), 1303-1306, https://doi.org/10.1029/1999GL011103, 2000.
Alley, R. B., Anandakrishnan, S., and Jung, P.: Stochastic Resonance in the North Atlantic, Paleoceanography, 16, 190–198, 2001.
Broecker, W. S.: Paleocean circulation during the last deglaciation: A bipolar seesaw?, Paleoceanography, 13, 119–121, 1998.
Broecker, W. S., Bond, G., and Klas, M.: A salt oscillator in the glacial Atlantic? 1. The concept, Paleoceanography, 5, 469–477, 1990.
Brovkin, V., Ganopolski, A., and Svirezhev, Y.: A continuous climate-vegetation classification for use in climate-biosphere studies, Ecol. Model., 101, 251–261, 1997.
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