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Global warming preceded by increasing carbon dioxide concentrations during the last deglaciation

Author

Listed:
  • Jeremy D. Shakun

    (Harvard University
    Lamont-Doherty Earth Observatory, Columbia University)

  • Peter U. Clark

    (College of Earth, Ocean, and Atmospheric Sciences, Oregon State University)

  • Feng He

    (Center for Climatic Research, University of Wisconsin)

  • Shaun A. Marcott

    (College of Earth, Ocean, and Atmospheric Sciences, Oregon State University)

  • Alan C. Mix

    (College of Earth, Ocean, and Atmospheric Sciences, Oregon State University)

  • Zhengyu Liu

    (Center for Climatic Research, University of Wisconsin
    University of Wisconsin
    Laboratory for Ocean-Atmosphere Studies, Peking University)

  • Bette Otto-Bliesner

    (National Center for Atmospheric Research)

  • Andreas Schmittner

    (College of Earth, Ocean, and Atmospheric Sciences, Oregon State University)

  • Edouard Bard

    (CEREGE, Collège de France, CNRS-Université Aix-Marseille, Europole de l’Arbois, 13545 Aix-en-Provence, France)

Abstract

The covariation of carbon dioxide (CO2) concentration and temperature in Antarctic ice-core records suggests a close link between CO2 and climate during the Pleistocene ice ages. The role and relative importance of CO2 in producing these climate changes remains unclear, however, in part because the ice-core deuterium record reflects local rather than global temperature. Here we construct a record of global surface temperature from 80 proxy records and show that temperature is correlated with and generally lags CO2 during the last (that is, the most recent) deglaciation. Differences between the respective temperature changes of the Northern Hemisphere and Southern Hemisphere parallel variations in the strength of the Atlantic meridional overturning circulation recorded in marine sediments. These observations, together with transient global climate model simulations, support the conclusion that an antiphased hemispheric temperature response to ocean circulation changes superimposed on globally in-phase warming driven by increasing CO2 concentrations is an explanation for much of the temperature change at the end of the most recent ice age.

Suggested Citation

  • Jeremy D. Shakun & Peter U. Clark & Feng He & Shaun A. Marcott & Alan C. Mix & Zhengyu Liu & Bette Otto-Bliesner & Andreas Schmittner & Edouard Bard, 2012. "Global warming preceded by increasing carbon dioxide concentrations during the last deglaciation," Nature, Nature, vol. 484(7392), pages 49-54, April.
    • Handle: RePEc:nat:nature:v:484:y:2012:i:7392:d:10.1038_nature10915
    DOI: 10.1038/nature10915
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    13. Carolyn W. Snyder, 2019. "Revised estimates of paleoclimate sensitivity over the past 800,000 years," Climatic Change, Springer, vol. 156(1), pages 121-138, September.
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    15. Hongfei Wang & Zhipeng Yu & Jie Zhou & Chengming Li & Ananthanarasimhan Jayanarasimhan & Xiqiang Zhao & Hao Zhang, 2023. "A Scientometric Review of CO 2 Electroreduction Research from 2005 to 2022," Energies, MDPI, vol. 16(2), pages 1-21, January.
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    19. David Stern & Robert Kaufmann, 2014. "Anthropogenic and natural causes of climate change," Climatic Change, Springer, vol. 122(1), pages 257-269, January.
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