Ocean Sci. Discuss., 10, 83-151, 2013
www.ocean-sci-discuss.net/10/83/2013/
doi:10.5194/osd-10-83-2013
© Author(s) 2013. This work is distributed
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Review Status
This discussion paper has been under review for the journal Ocean Science (OS). Please refer to the corresponding final paper in OS.
NEMO on the shelf: assessment of the Iberia-Biscay-Ireland configuration
C. Maraldi1,*, J. Chanut2, B. Levier2, N. Ayoub1, P. De Mey1, G. Reffray2, F. Lyard1, S. Cailleau2, M. Drévillon2, E. A. Fanjul3, M. G. Sotillo3, and P. Marsaleix4
1Laboratoire d'études en géophysique et océanographie spatiales (LEGOS), UMR 5566, CNRS – Université de Toulouse, 14 Avenue Edouard Belin, 31400 Toulouse, France
2Mercator-Océan, Parc Technologique du Canal, 8–10 rue Hermès, 31520 Ramonville Saint Agne, France
3Puertos del Estado, Avda. del Partenón, 10 – 28042 Madrid, Spain
4Laboratoire d'Aérologie/CNRS/Université de Toulouse, 14 avenue Edouard Belin, 31400 Toulouse, France
*now at: Service Hydrographique et Océanographique de la Marine, Toulouse, France

Abstract. The Iberia-Biscay-Ireland (IBI) system serves one of the 7 MyOcean "Monitoring and Forecasting Centres". A high resolution simulation covering the IBI region is set-up over July 2007–February 2009. The NEMO (Nucleus for European Modelling of the Ocean) model is used with a 1/36° horizontal resolution and 50 z-levels in the vertical. New developments have been incorporated in NEMO to make it suitable to open- as well as coastal-ocean modelling. In this paper, we pursue three main objectives: (1) give an overview of the model configuration used for the simulations; (2) give a broad-brush account of one particular aspect of this work, namely consistency verification; this type of validation is conducted upstream of the implementation of the system before it is used for production and routinely validated; it is meant to guide model development in identifying gross deficiencies in the modelling of several key physical processes; (3) show that such a regional modelling system has potential as a complement to patchy observations (an integrated approach) to give information on non-observed physical quantities and to provide links between observations by identifying broader-scale patterns and processes. We concentrate on the year 2008. We first provide domain-wide consistency verification results in terms of barotropic tides, transports, sea surface temperature and stratification. We then focus on two dynamical sub-regions: the Celtic shelves and the Bay of Biscay slope and deep regions. The model-data consistency is checked for variables and processes such as tidal currents, tidal fronts, internal tides, residual elevation. We also examine the representation in the model of a seasonal pattern of the Bay of Biscay circulation: the warm extension of the Iberian Poleward Current along the northern Spanish coast (Navidad event) in winter 2007–2008.

Citation: Maraldi, C., Chanut, J., Levier, B., Ayoub, N., De Mey, P., Reffray, G., Lyard, F., Cailleau, S., Drévillon, M., Fanjul, E. A., Sotillo, M. G., and Marsaleix, P.: NEMO on the shelf: assessment of the Iberia-Biscay-Ireland configuration, Ocean Sci. Discuss., 10, 83-151, doi:10.5194/osd-10-83-2013, 2013.
 
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