During the last glacial period, climatic variation in the Northern and Southern Hemispheres was evidently linked. Modelling work points to freshwater discharge into the North Atlantic as a driving factor.
This is a preview of subscription content, access via your institution
Access options
Subscribe to this journal
Receive 51 print issues and online access
$199.00 per year
only $3.90 per issue
Buy this article
- Purchase on SpringerLink
- Instant access to full article PDF
Prices may be subject to local taxes which are calculated during checkout
References
Knutti, R., Flückiger, J., Stocker, T. F. & Timmermann, A. Nature 430, 851–856 (2004).
Blunier, T. et al. Nature 394, 739–743 (1998).
Broecker, W. S. Paleoceanography 13, 119–121 (1998).
Crowley, T. J. Paleoceanography 7, 489–497 (1992).
Stocker, T. F. Science 282, 61–62 (1998).
Steig, E. J. & Alley, R. B. Ann. Glaciol. 35, 451–456 (2002).
Schmittner, A. et al. Quat. Sci. Rev. 22, 659–671 (2003).
Stocker, T. F. & Johnsen, S. J. Paleoceanography 18, doi:0.1029/2003PA000920 (2003).
Hinnov, L. A. et al. Quat. Sci. Rev. 21, 1213–1228 (2002).
Toggweiler, J. R. & Samuels, B. Deep-Sea Res. I 42, 477–500 (1995).
Knorr, G. & Lohmann, G. Nature 424, 532–536 (2003).
Weaver, A. J. et al. Science 299, 1709–1713 (2003).
Ninnemann, U. S. & Charles, C. D. Earth Planet. Sci. Lett. 201, 383–396 (2002).
Peeters, F. J. C. et al. Nature 430, 661–665 (2004).
Dokken, T. M. & Jansen, E. Nature 401, 458–461 (1999).
Author information
Authors and Affiliations
Rights and permissions
About this article
Cite this article
Dokken, T., Nisancioglu, K. Fresh angle on the polar seesaw. Nature 430, 842–843 (2004). https://doi.org/10.1038/430842a
Published:
Issue Date:
DOI: https://doi.org/10.1038/430842a