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Deep Heating

Global warming is popularly viewed only as an atmospheric process, when, as shown by marine temperature records covering the last several decades, most heat uptake occurs in the ocean. How did subsurface ocean temperatures vary during past warm and cold intervals? Rosenthal et al. (p. 617) present a temperature record of western equatorial Pacific subsurface and intermediate water masses over the past 10,000 years that shows that heat content varied in step with both northern and southern high-latitude oceans. The findings support the view that the Holocene Thermal Maximum, the Medieval Warm Period, and the Little Ice Age were global events, and they provide a long-term perspective for evaluating the role of ocean heat content in various warming scenarios for the future.

Abstract

Observed increases in ocean heat content (OHC) and temperature are robust indicators of global warming during the past several decades. We used high-resolution proxy records from sediment cores to extend these observations in the Pacific 10,000 years beyond the instrumental record. We show that water masses linked to North Pacific and Antarctic intermediate waters were warmer by 2.1 ± 0.4°C and 1.5 ± 0.4°C, respectively, during the middle Holocene Thermal Maximum than over the past century. Both water masses were ~0.9°C warmer during the Medieval Warm period than during the Little Ice Age and ~0.65° warmer than in recent decades. Although documented changes in global surface temperatures during the Holocene and Common era are relatively small, the concomitant changes in OHC are large.
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Supplementary Material

Summary

Supplementary Text
Figs. S1 to S8
Tables S1 to S3
References
Database S1

Resources

File (database.s1.xlsx)
File (rosenthal.sm.pdf)
File (rosenthal.sm.revision.1.pdf)

References and Notes

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Published In

Science
Volume 342Issue 61581 November 2013
Pages: 617 - 621

History

Received: 21 May 2013
Accepted: 30 September 2013

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Authors

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Yair Rosenthal* [email protected]
Institute for Marine and Coastal Sciences and Department of Earth and Planetary Sciences, Rutgers University, 71 Dudley Road, New Brunswick, NJ 08901, USA.
Braddock K. Linsley
Lamont-Doherty Earth Observatory of Columbia University, Palisades, NY 10964, USA.
Delia W. Oppo
Department of Geology and Geophysics, Woods Hole Oceanographic Institution, Woods Hole, MA 02543, USA.

Notes

*Corresponding author. E-mail: [email protected]

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Science
Volume 342|Issue 6158
1 November 2013
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Received:21 May 2013
Accepted:30 September 2013
Published in print:1 November 2013
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