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Geoscientific Model Development An interactive open-access journal of the European Geosciences Union
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Volume 10, issue 2
Geosci. Model Dev., 10, 1009–1031, 2017
https://doi.org/10.5194/gmd-10-1009-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.

Special issue: Nucleus for European Modelling of the Ocean - NEMO

Geosci. Model Dev., 10, 1009–1031, 2017
https://doi.org/10.5194/gmd-10-1009-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.

Model evaluation paper 03 Mar 2017

Model evaluation paper | 03 Mar 2017

Comparing sea ice, hydrography and circulation between NEMO3.6 LIM3 and LIM2

Petteri Uotila 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 Lorena Grabowski on behalf of the Authors (23 Dec 2016)  Author's response
ED: Referee Nomination & Report Request started (05 Jan 2017) by Anne Le Brocq
RR by Anonymous Referee #1 (11 Jan 2017)
ED: Publish subject to technical corrections (27 Jan 2017) by Anne Le Brocq
AR by Petteri Uotila on behalf of the Authors (08 Feb 2017)  Author's response    Manuscript
Publications Copernicus
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Short summary
We performed ocean model simulations with new and old sea-ice components. Sea ice improved in the new model compared to the earlier one due to better model physics. In the ocean, the largest differences are confined close to the surface within and near the sea-ice zone. The global ocean circulation slowly deviates between the simulations due to dissimilar sea ice in the deep water formation regions, such as the North Atlantic and Antarctic.
We performed ocean model simulations with new and old sea-ice components. Sea ice improved in...
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