Making sense of palaeoclimate sensitivity

E. J. Rohling*, A. Sluijs, H. A. Dijkstra, P. Köhler, R. S.W. Van De Wal, A. S. Von Der Heydt, D. J. Beerling, A. Berger, P. K. Bijl, M. Crucifix, R. Deconto, S. S. Drijfhout, A. Fedorov, G. L. Foster, A. Ganopolski, J. Hansen, B. Hönisch, H. Hooghiemstra, M. Huber, P. HuybersR. Knutti, D. W. Lea, L. J. Lourens, D. Lunt, V. Masson-Demotte, M. Medina-Elizalde, B. Otto-Bliesner, M. Pagani, H. Pälike, H. Renssen, D. L. Royer, M. Siddall, P. Valdes, J. C. Zachos, R. E. Zeebe

*Corresponding author for this work

    Research output: Contribution to journalArticlepeer-review

    242 Citations (Scopus)

    Abstract

    Many palaeoclimate studies have quantified pre-anthropogenic climate change to calculate climate sensitivity (equilibrium temperature change in response to radiative forcing change), but a lack of consistent methodologies produces a wide range of estimates and hinders comparability of results. Here we present a stricter approach, to improve intercomparison of palaeoclimate sensitivity estimates in a manner compatible with equilibrium projections for future climate change. Over the past 65 million years, this reveals a climate sensitivity (in K W-1 m 2) of 0.3-1.9 or 0.6-1.3 at 95% or 68% probability, respectively. The latter implies a warming of 2.2-4.8 K per doubling of atmospheric CO2, which agrees with IPCC estimates.

    Original languageEnglish
    Pages (from-to)683-691
    Number of pages9
    JournalNature
    Volume491
    Issue number7426
    DOIs
    Publication statusPublished - 29 Nov 2012

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