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Cited by 95

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Geobiological constraints on Earth system sensitivity to CO2 during the Cretaceous and Cenozoic

ROYER, D. L., PAGANI, M., BEERLING, D. J.·2012·Geobiology
DOI 10.1111/j.1472-4669.2012.00320.x
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Abstract

Earth system climate sensitivity (ESS) is the long‐term (>10 3 year) response of global surface temperature to doubled CO 2 that integrates fast and slow climate feedbacks. ESS has energy policy implications because global temperatures are not expected to decline appreciably for at least 10 3 year, even if anthropogenic greenhouse gas emissions drop to zero. We report provisional ESS estimates of 3 °C or higher for some of the Cretaceous and Cenozoic based on paleo‐reconstructions of CO 2 and temperature. These estimates are generally higher than climate sensitivities simulated from global climate models for the same ancient periods (approximately 3 °C). Climate models probably do not capture the full suite of positive climate feedbacks that amplify global temperatures during some globally warm periods, as well as other characteristic features of warm climates such as low meridional temperature gradients. These absent feedbacks may be related to clouds, trace greenhouse gases (GHGs), seasonal snow cover, and/or vegetation, especially in polar regions. Better characterization and quantification of these feedbacks is a priority given the current accumulation of atmospheric GHGs.

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Metadata

Authors
ROYER, D. L., PAGANI, M., & BEERLING, D. J.
Venue
Geobiology
Publisher
Wiley
Published
2012-02-22
Volume
10
Issue
4
Pages
298-310
ISSN
  • 1472-4677
  • 1472-4669
DOI
10.1111/j.1472-4669.2012.00320.x
Cited by
95
References
4
Language
en
Licence
onlinelibrary.wiley.com/termsAndConditions#vor (vor)

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