Northern Hemisphere forcing of Southern Hemisphere climate during the last deglaciation

Feng He (), Jeremy D. Shakun, Peter U. Clark, Anders E. Carlson, Zhengyu Liu, Bette L. Otto-Bliesner and John E. Kutzbach
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Feng He: Center for Climatic Research, Nelson Institute for Environmental Studies, University of Wisconsin-Madison
Jeremy D. Shakun: Harvard University
Peter U. Clark: College of Earth, Ocean, and Atmospheric Sciences, Oregon State University
Anders E. Carlson: Center for Climatic Research, Nelson Institute for Environmental Studies, University of Wisconsin-Madison
Zhengyu Liu: Center for Climatic Research, Nelson Institute for Environmental Studies, University of Wisconsin-Madison
Bette L. Otto-Bliesner: National Center for Atmospheric Research
John E. Kutzbach: Center for Climatic Research, Nelson Institute for Environmental Studies, University of Wisconsin-Madison

Nature, 2013, vol. 494, issue 7435, 81-85

Abstract: Changes in ocean circulation are the most plausible explanation for the early Southern Hemisphere deglacial warming and its lead over Northern Hemisphere temperature.

Date: 2013
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DOI: 10.1038/nature11822

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