Articles | Volume 10, issue 2
Earth Syst. Dynam., 10, 333–345, 2019
https://doi.org/10.5194/esd-10-333-2019
Earth Syst. Dynam., 10, 333–345, 2019
https://doi.org/10.5194/esd-10-333-2019

Research article 14 Jun 2019

Research article | 14 Jun 2019

Including the efficacy of land ice changes in deriving climate sensitivity from paleodata

Lennert B. Stap et al.

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Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
ED: Reconsider after major revisions (10 Mar 2019) by Daniel Kirk-Davidoff
AR by Lennert Stap on behalf of the Authors (14 Mar 2019)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (15 Mar 2019) by Daniel Kirk-Davidoff
RR by Anonymous Referee #1 (01 Apr 2019)
RR by Anonymous Referee #2 (10 Apr 2019)
ED: Publish subject to minor revisions (review by editor) (29 Apr 2019) by Daniel Kirk-Davidoff
AR by Lennert Stap on behalf of the Authors (09 May 2019)  Author's response    Manuscript
ED: Publish subject to technical corrections (27 May 2019) by Daniel Kirk-Davidoff
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Short summary
Processes causing the same global-average radiative forcing might lead to different global temperature changes. We expand the theoretical framework by which we calculate paleoclimate sensitivity with an efficacy factor. Applying the revised approach to radiative forcing caused by CO2 and land ice albedo perturbations, inferred from data of the past 800 000 years, gives a new paleo-based estimate of climate sensitivity.
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