Articles | Volume 10, issue 2
https://doi.org/10.5194/gmd-10-1009-2017
https://doi.org/10.5194/gmd-10-1009-2017
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, Doroteaciro Iovino, Martin Vancoppenolle, Mikko Lensu, and Clement Rousset

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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
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
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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.