A new approach for simulating the paleo-evolution of the Northern Hemisphere ice sheets

Banderas, Rubén; Alvarez-Solas, Jorge; Robinson, Alexander; Montoya, Marisa

doi:https://doi.org/10.5194/gmd-11-2299-2018

Articles | Volume 11, issue 6

https://doi.org/10.5194/gmd-11-2299-2018

© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.

https://doi.org/10.5194/gmd-11-2299-2018

© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.

Articles | Volume 11, issue 6

Model experiment description paper

|

19 Jun 2018

Model experiment description paper |

| 19 Jun 2018

A new approach for simulating the paleo-evolution of the Northern Hemisphere ice sheets

Rubén Banderas, Jorge Alvarez-Solas, Alexander Robinson, and Marisa Montoya

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Final revised paper (published on 19 Jun 2018)
Supplement to the final revised paper
Preprint (discussion started on 31 Jul 2017)
Supplement to the preprint

Interactive discussion

Status: closed

AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment

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- Supplement

RC1: 'Review of Banderas et al', Anonymous Referee #1, 22 Aug 2017
RC2: 'Review statement of the manuscript “A new approach for simulating the paleo-evolution of the Northern Hemisphere ice sheets” by Banderas et al.', Anonymous Referee #2, 26 Nov 2017
AC1: 'Reply to referee's comments', Rubén Banderas , 17 Jan 2018

Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision

AR by Rubén Banderas on behalf of the Authors (21 Jan 2018) Author's response Manuscript

ED: Referee Nomination & Report Request started (06 Mar 2018) by Philippe Huybrechts

RR by Anonymous Referee #2 (07 Mar 2018)

RR by Anonymous Referee #1 (16 Mar 2018)

ED: Publish subject to technical corrections (26 Apr 2018) by Philippe Huybrechts

Short summary

Here we present a new approach to force ice-sheet models offline, which accounts for a more realistic treatment of millennial-scale climate variability as compared to the existing methods. Our results reveal that an incorrect representation of the characteristic pattern of millennial-scale climate variability within the climate forcing not only affects NH ice-volume variations at millennial timescales but has consequences for glacial–interglacial ice-volume changes too.