S-2010 is an ocean model developed by the SIROCCO system team (CNRS & Toulouse University). Physical frame: Boussinesq Hydrostatic, free surface. Horizontal Grid: C curvilinear. Vertical grid: sigma generalized. Numerical method: finite differences + energy conserving (Marsaleix et al 2008). Time stepping scheme: Leap Frog + LP/FD filters (Marsaleix et al, 2012). PGF: Pressure Jacobian (Marsaleix et al, 2009). EOS: TEOS10 (Marsaleix et al, 2011). Lateral boundaries: (Marsaleix et al, 2006).
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March 2012:

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  Prévisions sur la Méditerranée nord-occidentale

Campagne CASCADE (Pour en savoir plus)

Ces prévisions sont réalisées avec le modèle SYMPHONIE. Elles utilisent le forçage aux frontières océaniques du modèle de prévision de Mediterranée (Mediterranean ocean Forecasting System, http://gnoo.bo.ingv.it/mfs/). En surface le modèle est forcé par les prévisions du European Centre for Medium-Range Weather Forecasts. Les débits des fleuves sont fournies par la Compagnie Nationale du Rhone et par la base Hydroreel du Ministère de l'Ecologie et du Développement Durable.

Jour J : / Jour J+1 / Jour J+2 / Jour J+3 / Jour J+4 / Jour J+5

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prevision maps
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  • Aygues-Mortes vertical section
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  • Agde vertical section
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  • Leucate vertical section
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  • Canet vertical section
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  • Across canyon heads vertical section
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  • Along Cap de Creus canyon axis vertical section
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  • Across Cap de Creus canyon (600m) vertical section
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  • Across Cap de Creus canyon (1000m) vertical section
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  • Across the deep convection area (L) vertical section
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  • Across the deep convection area (M) vertical section
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  DOWNLOAD the last SYMPHONIE release

REAL TIME FORECAST in North-Western Mediterranean (CASCADE projet)

REAL TIME FORECAST of the Pacific coast of Japan
PhD proposition: Budget of biogenic elements on the Gulf of Lion shelf and offshore transport. More details

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Energy transfers in internal tide generation, propagation and dissipation in the deep ocean
Floor J.W., Auclair F., Marsaleix P., 2011 Ocean Modelling

The energy transfers associated with internal tide (IT) generation by a semi-diurnal surface tidal wave impinging on a supercritical meridionally uniform deep ocean ridge on the f-plane, and subsequent IT-propagation are analysed using the Boussinesq, free-surface, terrain-following ocean model Symphonie. The energy diagnostics are explicitly based on the numerical formulation of the governing equations, permitting a globally conservative, high-precision analysis of all physical and numerical/artificial energy transfers in a sub-domain with open lateral boundaries.
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