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Assessment of a NEMO-based downscaling experiment for the North-Western Mediterranean region: Impacts on the Northern Current and comparison with ADCP data and altimetry products
Institution:1. Department of Food Science, Faculty of Science, University of Copenhagen, Rolighedsvej 30, 1958 Frederiksberg C, Denmark;2. Department of Veterinary Disease Biology, Faculty of Health and Medical Sciences, University of Copenhagen, Ridebanevej 9, 1870 Frederiksberg C, Denmark;1. Université Bordeaux, CNRS, EPOC, UMR 5805, F-33120 Arcachon, France;2. Université Paris 6, CNRS, LECOB, UMR 8222, F-66650 Banyuls-sur-Mer, France;3. Centre d''Estudis Avançats de Blanes, Consejo Superior de Investigaciones Científicas, Carrer d''accés a la Cala Sant Francesc 14, F-17300 Blanes, Spain;4. Université d''Aix-Marseille, OSU-Institut Pythéas IMBE Station marine d''Endoume, Chemin de la Batterie des Lions, F- 13007 Marseille, France;5. Marine Ecology Laboratory, University of Crete, Vasilika Vouton, Heraklion 70013, Crete, Greece;6. Hellenic Centre for Marine Research, Athens Sounio, Anavyssos Attiki 19013, Greece
Abstract:The aim of this paper is to assess the impact of numerical resolution on the simulation of the circulation in the North-Western Mediterranean Sea by comparing two realistic model configurations of 1/64° and 1/16°, the low resolution configuration (LRC) being also used at the high resolution configuration (HRC) open boundaries. The study mainly focuses on the Northern Current (NC), the major feature of the regional circulation in the area, influencing important processes such as meanders giving birth to eddies and NC intrusions on the shelf, strongly conditioning the interactions between coastal and off-shore waters. Both configurations use the NEMO code with the LRC covering the entire Mediterranean basin and the HRC being restricted to the North-Western Mediterranean Sea. The two numerical configurations are assessed by using hull-mounted ADCP data and geostrophic velocities derived from AVISO altimetry at key locations along the NC path. The two configurations develop a different solution regarding the current dynamics but both indicate an important variability of the NC position along its general path. The LRC simulations systematically exhibit a NC shifted too far off the coast and also spuriously displaced seaward along the Gulf of Lions shelf edge while high resolution simulations better fit the remote and in situ observations. In addition, the HRC is able to simulate more realistic coastal features such as a confined coastal jet in good agreement with the ADCP measurements. As satisfactory agreement is reached with the various observations used at different space and time scales, the development of this NEMO high resolution configuration stands as a promising experiment for various process studies or operational oriented applications.
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