Articles | Volume 11, issue 1
Earth Syst. Dynam., 11, 281–289, 2020
https://doi.org/10.5194/esd-11-281-2020
Earth Syst. Dynam., 11, 281–289, 2020
https://doi.org/10.5194/esd-11-281-2020

Research article 17 Mar 2020

Research article | 17 Mar 2020

π-theorem generalization of the ice-age theory

Mikhail Y. Verbitsky and Michel Crucifix

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AR: Author's response | RR: Referee report | ED: Editor decision
ED: Reconsider after major revisions (10 Jan 2020) by Gabriele Messori
AR by Mikhail Verbitsky on behalf of the Authors (11 Jan 2020)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (15 Jan 2020) by Gabriele Messori
RR by Anonymous Referee #3 (17 Jan 2020)
RR by Anonymous Referee #1 (26 Jan 2020)
RR by Anonymous Referee #2 (30 Jan 2020)
ED: Publish subject to minor revisions (review by editor) (31 Jan 2020) by Gabriele Messori
AR by Mikhail Verbitsky on behalf of the Authors (03 Feb 2020)  Author's response    Manuscript
ED: Publish as is (11 Feb 2020) by Gabriele Messori
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Short summary
Using the central theorem of dimensional analysis, the π theorem, we show that the relationship between the amplitude and duration of glacial cycles is governed by a property of scale invariance that does not depend on the physical nature of the underlying positive and negative feedbacks incorporated by the system. It thus turns out to be one of the most fundamental properties of the Pleistocene climate.
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