Articles | Volume 13, issue 9
Clim. Past, 13, 1081–1095, 2017
https://doi.org/10.5194/cp-13-1081-2017
Clim. Past, 13, 1081–1095, 2017
https://doi.org/10.5194/cp-13-1081-2017

Research article 01 Sep 2017

Research article | 01 Sep 2017

Oceanic response to changes in the WAIS and astronomical forcing during the MIS31 superinterglacial

Flavio Justino et al.

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Interactive discussion

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 (22 Mar 2017) by Erin McClymont
AR by Flavio Justino on behalf of the Authors (10 May 2017)  Author's response    Manuscript
ED: Reconsider after major revisions (23 May 2017) by Erin McClymont
AR by Flavio Justino on behalf of the Authors (04 Jul 2017)  Author's response    Manuscript
ED: Publish subject to technical corrections (19 Jul 2017) by Erin McClymont
AR by Flavio Justino on behalf of the Authors (28 Jul 2017)  Author's response    Manuscript
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Short summary
These modeling results have enormous implications for paleoreconstructions of the MIS31 climate that assume overall ice-free conditions in the vicinity of the Antarctic continent. Since these reconstructions may depict dominant signals in a particular time interval and locale, they cannot be assumed to geographically represent large-scale domains, and their ability to reproduce long-term environmental conditions should be considered with care.