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Geoscientific Model Development An interactive open-access journal of the European Geosciences Union
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Volume 9, issue 8
Geosci. Model Dev., 9, 2665-2684, 2016
https://doi.org/10.5194/gmd-9-2665-2016
© Author(s) 2016. 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., 9, 2665-2684, 2016
https://doi.org/10.5194/gmd-9-2665-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.

Model evaluation paper 12 Aug 2016

Model evaluation paper | 12 Aug 2016

A 1/16° eddying simulation of the global NEMO sea-ice–ocean system

Doroteaciro Iovino et al.
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Bernie, D., Guilyardi, E., Madec, G., Slingo, J. M., and Woolnough, S. J.: Impact of resolving the diurnal cycle in an ocean–atmosphere GCM. Part 1: a diurnally forced OGCM, Clim. Dynam., 29, 575–590, 2007.
Blanke, B. and Delecluse, P.: Variability of the tropical Atlantic Ocean simulated by a general circulation model with two different mixed layer physics, J. Phys. Oceanogr., 23, 1363–1388, 1993.
Bonjean, F. and Lagerloef, G. S. E.: Diagnostic model and analysis of the surface currents in the tropical Pacific Ocean, J. Phys. Oceanogr., 32, 2938–2954, 2002.
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An 11-year simulation of a global eddying ocean (1/16) configuration is presented. Model performance is evaluated against observations and a twin 1/4 configuration. The model realistically represents the variability at upper and intermediate depths, the position and strength of the surface circulation, and exchanges of mass through key passages. Sea ice properties are close to satellite observations. This simulation constitutes the groundwork for future applications to short range ocean forecasting.
An 11-year simulation of a global eddying ocean (1/16) configuration is presented. Model...
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