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

T. R. Jones (), W. H. G. Roberts, E. J. Steig, K. M. Cuffey, B. R. Markle and J. W. C. White
Additional contact information
T. R. Jones: Institute of Arctic and Alpine Research, University of Colorado
W. H. G. Roberts: Bristol Research Initiative for the Dynamic Global Environment and Bristol Glaciology Centre, School of Geographical Sciences, University of Bristol
E. J. Steig: University of Washington
K. M. Cuffey: University of California
B. R. Markle: University of Washington
J. W. C. White: University of Colorado

Nature, 2018, vol. 554, issue 7692, 351-355

Abstract: An Antarctic ice core reveals that, during the last ice age, the topography of Northern Hemisphere ice sheets shifted tropical Pacific convection eastward, increasing climate variability in the high southern latitudes.

Date: 2018
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DOI: 10.1038/nature24669

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