Journal cover Journal topic
Geoscientific Model Development An interactive open-access journal of the European Geosciences Union
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
Comparing sea ice, hydrography and circulation between NEMO3.6 LIM3 and LIM2
Petteri Uotila et al.
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Interactive discussionStatus: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
Printer-friendly Version - Printer-friendly version      Supplement - Supplement
 
SC1: 'Executive Editor Comment on "On the influence of sea-ice physics in multi-decadal ocean-ice hindcasts"', Astrid Kerkweg, 22 Aug 2016 Printer-friendly Version 
AC1: 'Author response', Petteri Uotila, 22 Dec 2016 Printer-friendly Version 
 
RC1: 'Review: 'On the influence of sea-ice physics in multi-decadal ocean-ice hindcast' by P. Uotila et al.', Anonymous Referee #1, 21 Sep 2016 Printer-friendly Version 
AC3: 'Author response', Petteri Uotila, 22 Dec 2016 Printer-friendly Version Supplement 
 
RC2: 'Review of "On the influence of sea-ice physics in multi-decadal ocean-ice hindcasts" by Petteri Uotila et al.', Anonymous Referee #2, 02 Nov 2016 Printer-friendly Version 
AC2: 'Author response', Petteri Uotila, 22 Dec 2016 Printer-friendly Version 
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
CC BY 4.0
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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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