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A Reconstruction of Regional and Global Temperature for the Past 11,300 Years

Science
8 Mar 2013
Vol 339, Issue 6124
pp. 1198-1201

Exceptional Now

The climate has been warming since the industrial revolution, but how warm is climate now compared with the rest of the Holocene? Marcott et al. (p. 1198) constructed a record of global mean surface temperature for more than the last 11,000 years, using a variety of land- and marine-based proxy data from all around the world. The pattern of temperatures shows a rise as the world emerged from the last deglaciation, warm conditions until the middle of the Holocene, and a cooling trend over the next 5000 years that culminated around 200 years ago in the Little Ice Age. Temperatures have risen steadily since then, leaving us now with a global temperature higher than those during 90% of the entire Holocene.

Abstract

Surface temperature reconstructions of the past 1500 years suggest that recent warming is unprecedented in that time. Here we provide a broader perspective by reconstructing regional and global temperature anomalies for the past 11,300 years from 73 globally distributed records. Early Holocene (10,000 to 5000 years ago) warmth is followed by ~0.7°C cooling through the middle to late Holocene (<5000 years ago), culminating in the coolest temperatures of the Holocene during the Little Ice Age, about 200 years ago. This cooling is largely associated with ~2°C change in the North Atlantic. Current global temperatures of the past decade have not yet exceeded peak interglacial values but are warmer than during ~75% of the Holocene temperature history. Intergovernmental Panel on Climate Change model projections for 2100 exceed the full distribution of Holocene temperature under all plausible greenhouse gas emission scenarios.

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File (marcott.sm.database.s1.xlsx)
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References and Notes

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Information & Authors

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Published In

BERJAYA
Science
Volume 339 | Issue 6124
8 March 2013

Submission history

Received: 27 July 2012
Accepted: 4 January 2013
Published in print: 8 March 2013

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Acknowledgments

We thank J. Alder, T. Bauska, E. Brook, C. Buizert, V. Ersek, S. Hostetler, P. Huybers, N. Pisias, J. Rosen, G. Schmidt, A. Schmittner, M. Tingley, and our reviewers for invaluable insight and helpful discussion. The data sets provided by T. Barrows, J.-H. Kim, Y. Kubota, I. Larocque, G. Leduc, M. McGlone, T. Rodrigues, C. Rühlemann, J. Sachs, R. Schneider, H. Seppä, J. Tierney, M. Yamamoto, B. Vinther, and C. Waelbrock, as well as the data sets compiled from the National Oceanic and Atmospheric Administration Climate Data Center and PANGAEA databases, made this research possible. Funding for this work was provided by the NSF Paleoclimate Program for the Paleovar Project.

Authors

Affiliations

Shaun A. Marcott
College of Earth, Ocean, and Atmospheric Sciences, Oregon State University, Corvallis, OR 97331, USA.
Jeremy D. Shakun
Department of Earth and Planetary Sciences, Harvard University, Cambridge, MA 02138, USA.
Peter U. Clark
College of Earth, Ocean, and Atmospheric Sciences, Oregon State University, Corvallis, OR 97331, USA.
Alan C. Mix
College of Earth, Ocean, and Atmospheric Sciences, Oregon State University, Corvallis, OR 97331, USA.

Notes

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To whom correspondence should be addressed. E-mail: [email protected]

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