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Geoscientific Model Development An interactive open-access journal of the European Geosciences Union
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Volume 11, issue 10
Geosci. Model Dev., 11, 4291-4316, 2018
https://doi.org/10.5194/gmd-11-4291-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
Geosci. Model Dev., 11, 4291-4316, 2018
https://doi.org/10.5194/gmd-11-4291-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.

Development and technical paper 19 Oct 2018

Development and technical paper | 19 Oct 2018

Dynamic hydrological discharge modelling for coupled climate model simulations of the last glacial cycle: the MPI-DynamicHD model version 3.0

Thomas Riddick et al.
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Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
Printer-friendly Version - Printer-friendly version Supplement - Supplement
Peer review completion
AR: Author's response | RR: Referee report | ED: Editor decision
AR by Thomas Riddick on behalf of the Authors (03 Aug 2018)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (03 Sep 2018) by Olivier Marti
RR by Lev Tarasov (19 Sep 2018)
RR by Dai Yamazaki (19 Sep 2018)
ED: Publish subject to technical corrections (24 Sep 2018) by Olivier Marti
AR by Thomas Riddick on behalf of the Authors (01 Oct 2018)  Author's response    Manuscript
Publications Copernicus
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Short summary
During the Last Glacial Maximum, many rivers were blocked by the presence of large ice sheets and thus found new routes to the sea. This resulted in changes in the pattern of freshwater discharge into the oceans and thus would have significantly affected ocean circulation. Also, rivers found routes across the vast exposed continental shelves to the lower coastlines of that time. We propose a model for such changes in river routing suitable for use in wider models of the last glacial cycle.
During the Last Glacial Maximum, many rivers were blocked by the presence of large ice sheets...
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