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Geoscientific Model Development An interactive open-access journal of the European Geosciences Union
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Volume 11, issue 2
Geosci. Model Dev., 11, 521-540, 2018
https://doi.org/10.5194/gmd-11-521-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 3.0 License.
Geosci. Model Dev., 11, 521-540, 2018
https://doi.org/10.5194/gmd-11-521-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 3.0 License.

Model description paper 06 Feb 2018

Model description paper | 06 Feb 2018

An axisymmetric non-hydrostatic model for double-diffusive water systems

Koen Hilgersom 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 Koen Hilgersom on behalf of the Authors (31 Mar 2017)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (07 May 2017) by Ignacio Pisso
RR by Anonymous Referee #1 (12 May 2017)
RR by Anonymous Referee #2 (02 Jun 2017)
ED: Reconsider after major revisions (18 Jun 2017) by Ignacio Pisso
AR by Lorena Grabowski on behalf of the Authors (01 Sep 2017)  Author's response
ED: Referee Nomination & Report Request started (28 Sep 2017) by Ignacio Pisso
RR by Anonymous Referee #2 (08 Oct 2017)
ED: Publish subject to minor revisions (Editor review) (09 Oct 2017) by Ignacio Pisso
AR by Koen Hilgersom on behalf of the Authors (26 Oct 2017)  Author's response    Manuscript
ED: Publish as is (18 Dec 2017) by Ignacio Pisso
Publications Copernicus
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Short summary
This study models the local inflow of groundwater at the bottom of a stream with large density gradients between the groundwater and surface water. Modelling salt and heat transport in a water body is very challenging, as it requires large computation times. Due to the circular local groundwater inflow and a negligible stream discharge, we assume axisymmetry around the inflow, which is easily implemented in an existing model, largely reduces the computation times, and still performs accurately.
This study models the local inflow of groundwater at the bottom of a stream with large density...
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