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Climate of the Past An interactive open-access journal of the European Geosciences Union
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Volume 12, issue 8
Clim. Past, 12, 1635–1644, 2016
https://doi.org/10.5194/cp-12-1635-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
Clim. Past, 12, 1635–1644, 2016
https://doi.org/10.5194/cp-12-1635-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 11 Aug 2016

Research article | 11 Aug 2016

Reconstructing geographical boundary conditions for palaeoclimate modelling during the Cenozoic

Michiel Baatsen 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 (12 Feb 2016) by André Paul
AR by Michiel Baatsen on behalf of the Authors (24 Mar 2016)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (31 Mar 2016) by André Paul
RR by Dietmar Müller (13 Apr 2016)
ED: Publish subject to minor revisions (review by Editor) (13 May 2016) by André Paul
AR by Michiel Baatsen on behalf of the Authors (30 May 2016)  Author's response    Manuscript
ED: Publish subject to minor revisions (review by Editor) (15 Jun 2016) by André Paul
AR by Michiel Baatsen on behalf of the Authors (20 Jun 2016)  Author's response    Manuscript
ED: Publish as is (23 Jun 2016) by André Paul
Publications Copernicus
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Short summary
One of the major difficulties in modelling palaeoclimate is constricting the boundary conditions, causing significant discrepancies between different studies. Here, a new method is presented to automate much of the process of generating the necessary geographical reconstructions. The latter can be made using various rotational frameworks and topography/bathymetry input, allowing for easy inter-comparisons and the incorporation of the latest insights from geoscientific research.
One of the major difficulties in modelling palaeoclimate is constricting the boundary...
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