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Atmospheric Science

Can climate feel the pressure?

Science12 Jun 2015Vol 348, Issue 6240pp. 1210-1211DOI: 10.1126/science.aac5264

Abstract

Atmospheric carbon dioxide (CO2) concentrations are widely held to be the main driver of climate change through the Phanerozoic (the past 541 million years), with warm intervals corresponding to high CO2 concentrations and cold intervals having low CO2 concentrations (1) (see the figure). However, paleoclimate models often cannot match proxy estimates of temperature and precipitation unless unrealistic CO2 concentrations are prescribed (2, 3). The solution may come from an unexpected direction: atmospheric oxygen (O2), which is not a greenhouse gas and thus provides no direct greenhouse forcing. On page 1238 of this issue, Poulsen et al. (4) report model results that identify O2 as an important climate driver through its contribution to total atmospheric pressure.
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References

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Science
Volume 348 | Issue 6240
12 June 2015

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Published in print: 12 June 2015

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Daniel J. Peppe
Terrestrial Paleoclimatology Research Group, Department of Geology, Baylor University, Waco, TX 76706, USA.
Dana L. Royer
Department of Earth and Environmental Sciences, Wesleyan University, Middletown, CT 06459, USA.

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Cited by
  1. Earth’s Climate System, Paris Climate Agreement: Beacon of Hope, (1-50), (2017).https://doi.org/10.1007/978-3-319-46939-3_1
    Crossref
  2. CO2 and temperature decoupling at the million-year scale during the Cretaceous Greenhouse, Scientific Reports, 7, 1, (2017).https://doi.org/10.1038/s41598-017-08234-0
    Crossref
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