Short episodes of warming and cooling occurred throughout the last glaciation. An innovative modelling study indicates that ocean-circulation changes produced much of the causative variation in greenhouse gases.
References
EPICA Community Members. Nature 444, 195–198 (2006).
Schmittner, A. & Galbraith, E. D. Nature 456, 373–376 (2008).
Flückiger, J. et al. Glob. Biogeochem. Cycles doi:10.1029/2003GB002122 (2004).
Huber, C. et al. Earth Planet. Sci. Lett. 243, 504–519 (2006).
Flückiger, J. et al. Clim. Dyn. 31, 633–645 (2008).
Stocker, T. F. & Johnsen, S. J. Paleoceanography doi:10.1029/2003PA000920 (2003).
Levermann, A., Schewe, J. & Montoya, M. Geophys. Res. Lett. doi:10.1029/2007GL030255 (2007).
Gruber, N. & Galloway, J. N. Nature 451, 293–296 (2008).
Timmermann, A. et al. J. Clim. 20, 4899–4919 (2007).
Dällenbach, A. et al. Geophys. Res. Lett. 27, 1005–1008 (2000).
Sowers, T., Alley, R. B. & Jubenville, J. Science 301, 945–948 (2003).
Fischer, H. et al. Nature 452, 864–867 (2008).
Flückiger, J. et al. Science 285, 227–230 (1999).
North GRIP Members. Nature 431, 147–151 (2004).
Author information
Authors and Affiliations
Rights and permissions
About this article
Cite this article
Stocker, T., Schilt, A. Greenhouse-gas fingerprints. Nature 456, 331–333 (2008). https://doi.org/10.1038/456331a
Published:
Issue Date:
DOI: https://doi.org/10.1038/456331a
- Springer Nature Limited