A probabilistic analysis of climate variation during the period AD 1050–1800 refines available estimates of the influence of temperature change on the concentration of carbon dioxide in the atmosphere.
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References
Solomon, S. et al. (eds) Climate Change 2007: The Physical Basis (Cambridge Univ. Press, 2007).
Frank, D. C. et al. Nature 463, 527–530 (2010).
Friedlingstein, P. et al. J. Clim. 19, 3337–3353 (2006).
Denman, K. L. et al. in Climate Change 2007: The Physical Basis (eds Solomon, S. et al.) 499–587 (Cambridge Univ. Press, 2007).
Meehl, G. A. et al. in Climate Change 2007: The Physical Basis (eds Solomon, S. et al.) 747–845 (Cambridge Univ. Press, 2007).
Bertrand, C. et al. Tellus A 54, 221–244 (2002).
Pongratz, J. et al. Glob. Biogeochem. Cycles 23, GB4001 (2009).
Mann, M. E. et al. Science 326, 1256–1260 (2009).
Goosse, H. et al. J. Geophys. Res. doi:10.1029/2009JD012737 (in the press).
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Goosse, H. Degrees of climate feedback. Nature 463, 438–439 (2010). https://doi.org/10.1038/463438a
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DOI: https://doi.org/10.1038/463438a
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