Abrupt climate changes during the last glacial period affected most of the Northern Hemisphere. Greenland ice core data suggest that for the penultimate abrupt warming event, climate change was nearly synchronous at high and low latitudes.
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References
Johnsen, S. J. et al. Nature 359, 311–313 (1992).
Wolff, E. W., Chappellaz, J., Blunier, T., Rasmussen, S. O. & Svensson, A. Quat. Sci. Rev. 29, 2828–2838 (2010).
Rosen, J. L. et al. Nature Geosci. 7, 459–463 (2014).
Barker, S. et al. Science 334, 347–351 (2011).
Blunier, T. et al. Nature 394, 739–743 (1998).
Severinghaus, J. P. & Brook, E. J. Science 286, 930–934 (1999).
Baumgartner, M. et al. Biogeosciences 9, 3961–3977 (2012).
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Wolff, E. Climate in phase. Nature Geosci 7, 397–398 (2014). https://doi.org/10.1038/ngeo2165
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DOI: https://doi.org/10.1038/ngeo2165