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.
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).
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Dokken, T., Nisancioglu, K. Fresh angle on the polar seesaw. Nature 430, 842–843 (2004). https://doi.org/10.1038/430842a
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DOI: https://doi.org/10.1038/430842a
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