Interhemispheric Ice-Sheet Synchronicity During the Last Glacial Maximum

Author:

Weber Michael E.1,Clark Peter U.2,Ricken Werner1,Mitrovica Jerry X.3,Hostetler Steven W.4,Kuhn Gerhard5

Affiliation:

1. Institute of Geology and Mineralogy, University of Cologne, Zuelpicher Strasse 49a, 50674 Cologne, Germany.

2. College of Earth, Ocean, and Atmospheric Sciences, Oregon State University, Corvallis, OR 97331, USA.

3. Department of Earth and Planetary Sciences, Harvard University, Cambridge, MA 02138, USA.

4. U.S. Geological Survey, College of Earth, Ocean, and Atmospheric Sciences, Oregon State University, Corvallis, OR 97331, USA.

5. Alfred Wegener Institute for Polar and Marine Research, Helmholtz Association, Am Alten Hafen 26, 27568 Bremerhaven, Germany.

Abstract

Part of the East Antarctic Ice Sheet advanced and retreated in synchrony with Northern Hemispheric ice sheets.

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

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