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Southern Hemisphere climate variability forced by Northern Hemisphere ice-sheet topography

Jones, T. R., Roberts, W. H. G., Steig, E. J., Cuffey, K. M., Markle, B. R., White, J. W. C.·2018·Nature
DOI 10.1038/nature24669
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  • This cold event, concurrent with Heinrich event 1, may also imply a regional response of the Cordilleran Ice Sheet to hemispheric changes in climate during the last deglaciation.

    “This cold event, concurrent with Heinrich event 1 (Figure 4), may also imply a regional response of the Cordilleran Ice Sheet to hemispheric changes in climate during the last deglaciation (Jones et al., 2018).”

    From Retreat of the Western Cordilleran Ice Sheet Margin During the Last Deglaciation (2018) · cites this paper as Jones et al., 2018

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Metadata

Authors
Jones, T. R., Roberts, W. H. G., Steig, E. J., Cuffey, K. M., Markle, B. R., & White, J. W. C.
Venue
Nature
Publisher
Springer Science and Business Media LLC
Published
2018-02
Volume
554
Issue
7692
Pages
351-355
ISSN
  • 0028-0836
  • 1476-4687
DOI
10.1038/nature24669
Cited by
57
References
0
Language
en
Licence
www.springer.com/tdm (tdm)

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