Northern Hemisphere forcing of Southern Hemisphere climate during the last deglaciation

被引：0
|
作者：
Feng He
Jeremy D. Shakun
Peter U. Clark
Anders E. Carlson
Zhengyu Liu
Bette L. Otto-Bliesner
John E. Kutzbach
机构：
[1] Center for Climatic Research,Department of Earth and Planetary Sciences
[2] Nelson Institute for Environmental Studies,Department of Geoscience
[3] University of Wisconsin-Madison,Department of Atmospheric and Oceanic Sciences
[4] Harvard University,Climate and Global Dynamics Division
[5] College of Earth,undefined
[6] Ocean,undefined
[7] and Atmospheric Sciences,undefined
[8] Oregon State University,undefined
[9] University of Wisconsin-Madison,undefined
[10] University of Wisconsin-Madison,undefined
[11] National Center for Atmospheric Research,undefined
来源：
Nature | 2013年 / 494卷
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摘要：
Changes in ocean circulation are the most plausible explanation for the early Southern Hemisphere deglacial warming and its lead over Northern Hemisphere temperature.
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页码：81 / 85
页数：4
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