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Research Article

State-dependent climate sensitivity in past warm climates and its implications for future climate projections

Rodrigo Caballero and Matthew Huber
PNAS August 27, 2013 110 (35) 14162-14167; https://doi.org/10.1073/pnas.1303365110
Rodrigo Caballero
aDepartment of Meteorology and Bolin Centre for Climate Research, Stockholm University, 10691 Stockholm, Sweden; and
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Matthew Huber
bPurdue Climate Change Research Center and Department of Earth, Atmospheric, and Planetary Sciences, Purdue University, West Lafayette, IN 47907
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  • For correspondence: huberm@purdue.edu
  1. Edited by Kerry A. Emanuel, Massachusetts Institute of Technology, Cambridge, MA, and approved July 10, 2013 (received for review February 22, 2013)

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Abstract

Projections of future climate depend critically on refined estimates of climate sensitivity. Recent progress in temperature proxies dramatically increases the magnitude of warming reconstructed from early Paleogene greenhouse climates and demands a close examination of the forcing and feedback mechanisms that maintained this warmth and the broad dynamic range that these paleoclimate records attest to. Here, we show that several complementary resolutions to these questions are possible in the context of model simulations using modern and early Paleogene configurations. We find that (i) changes in boundary conditions representative of slow “Earth system” feedbacks play an important role in maintaining elevated early Paleogene temperatures, (ii) radiative forcing by carbon dioxide deviates significantly from pure logarithmic behavior at concentrations relevant for simulation of the early Paleogene, and (iii) fast or “Charney” climate sensitivity in this model increases sharply as the climate warms. Thus, increased forcing and increased slow and fast sensitivity can all play a substantial role in maintaining early Paleogene warmth. This poses an equifinality problem: The same climate can be maintained by a different mix of these ingredients; however, at present, the mix cannot be constrained directly from climate proxy data. The implications of strongly state-dependent fast sensitivity reach far beyond the early Paleogene. The study of past warm climates may not narrow uncertainty in future climate projections in coming centuries because fast climate sensitivity may itself be state-dependent, but proxies and models are both consistent with significant increases in fast sensitivity with increasing temperature.

  • superrotation
  • hyperthermal

Footnotes

  • ↵1To whom correspondence should be addressed. E-mail: huberm{at}purdue.edu.
  • Author contributions: R.C. and M.H. designed research, performed research, and wrote the paper.

  • The authors declare no conflict of interest.

  • This article is a PNAS Direct Submission.

  • See Commentary on page 14118.

  • This article contains supporting information online at www.pnas.org/lookup/suppl/doi:10.1073/pnas.1303365110/-/DCSupplemental.

Freely available online through the PNAS open access option.

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State-dependent climate sensitivity
Rodrigo Caballero, Matthew Huber
Proceedings of the National Academy of Sciences Aug 2013, 110 (35) 14162-14167; DOI: 10.1073/pnas.1303365110

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State-dependent climate sensitivity
Rodrigo Caballero, Matthew Huber
Proceedings of the National Academy of Sciences Aug 2013, 110 (35) 14162-14167; DOI: 10.1073/pnas.1303365110
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