Articles | Volume 14, issue 12
https://doi.org/10.5194/cp-14-2071-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/cp-14-2071-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
21 Dec 2018
Research article |
| 21 Dec 2018
| 21 Dec 2018
Climate evolution across the Mid-Brunhes Transition
Department of Geography and Earth and Environmental Sciences, Emory and Henry College, Emory, VA 24327, USA
College of Earth, Ocean, and Atmospheric Sciences, Oregon State University, Corvallis, OR 97331, USA
Peter U. Clark
College of Earth, Ocean, and Atmospheric Sciences, Oregon State University, Corvallis, OR 97331, USA
Nicholas S. Bill
College of Earth, Ocean, and Atmospheric Sciences, Oregon State University, Corvallis, OR 97331, USA
Department of Geoscience, University of Wisconsin – Madison, Madison, WI 53706, USA
Center for Climatic Research, Nelson Institute for Environmental Studies, University of Wisconsin – Madison, Madison, WI 53706, USA
Nicklas G. Pisias
College of Earth, Ocean, and Atmospheric Sciences, Oregon State University, Corvallis, OR 97331, USA
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Short summary
Multiple components of the global climate system record a transition ~ 430 ka from lower- to higher-amplitude glacial cycles. Statistical analyses of globally distributed climate proxies show that a sequence of events including persistent Asian summer monsoons, weak glaciation, and reorganization of water masses preceded the transition to higher interglacial values for temperature, atmospheric greenhouse gases, and sea level.
Multiple components of the global climate system record a transition ~ 430 ka from lower- to...
