Articles | Volume 7, issue 2
https://doi.org/10.5194/esd-7-419-2016
https://doi.org/10.5194/esd-7-419-2016
Research article
 | 
28 Apr 2016
Research article |  | 28 Apr 2016

Are there multiple scaling regimes in Holocene temperature records?

Tine Nilsen, Kristoffer Rypdal, and Hege-Beate Fredriksen

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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
AR by Tine Nilsen on behalf of the Authors (27 Oct 2015)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (27 Oct 2015) by Gerrit Lohmann
RR by Anonymous Referee #3 (29 Oct 2015)
RR by Shaun Lovejoy (09 Nov 2015)
ED: Reconsider after major revisions (23 Nov 2015) by Gerrit Lohmann
AR by Svenja Lange on behalf of the Authors (04 Dec 2015)  Author's response
ED: Referee Nomination & Report Request started (04 Dec 2015) by Gerrit Lohmann
RR by Shaun Lovejoy (22 Dec 2015)
ED: Reconsider after major revisions (26 Feb 2016) by Gerrit Lohmann
AR by Tine Nilsen on behalf of the Authors (21 Mar 2016)  Author's response    Manuscript
ED: Publish as is (18 Apr 2016) by Gerrit Lohmann
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Short summary
In this article it is discussed how temperature variability on centennial timescales and longer can be described in a simplistic way. By analysing the scaling in late Holocene temperature reconstructions and longer temperature records from Greenland and Antarctic ice cores, we find that the choice of model depends heavily on the data material and timescale one chooses to emphasize. Ignoring data beyond the Holocene seems plausible when predicting temperature, but not for other purposes.
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