| HAL : hal-00409281, version 1 |
| DOI : 10.1016/j.csr.2007.01.023 |
| Fiche détaillée | Récupérer au format |
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| Continental Shelf Research 27, 9 (2007) 1317-1343 |
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| Resolution issues in numerical models of oceanic and coastal circulation |
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| David A. Greenberg 1Frédéric Dupont 2 |
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| (2007) |
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| The baroclinic and barotropic properties of ocean processes vary on many scales. These scales are determined by various factors such as the variations in coastline and bottom topography, the forcing meteorology, the latitudinal dependence of the Coriolis force, and the Rossby radius of deformation among others. In this paper we attempt to qualify and quantify scales of these processes, with particular attention to the horizontal resolution necessary to accurately reproduce physical processes in numerical ocean models. We also discuss approaches taken in nesting or down-scaling from global /basin- scale models to regional-scale or shelf-scale models. Finally we offer comments on how vertical resolution affects the representation of stratification in these numerical models. (c) 2007 Elsevier Ltd. All rights reserved. |
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| 1 : | Fisheries and Oceans Canada |
| Bedford Institute of Oceanography | |
| 2 : | Québec-Océan |
| Université Laval | |
| 3 : | Laboratoire d'études en Géophysique et océanographie spatiales (LEGOS) |
| CNRS : UMR5566 – Institut de recherche pour le développement [IRD] – CNES – Observatoire Midi-Pyrénées – INSU – Université Paul Sabatier [UPS] - Toulouse III | |
| 4 : | Dartmouth College |
| Dartmouth College | |
| 5 : | University of North Carolina at Chapel Hill |
| North Carolina State University | |
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| ECOLA |
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| Numerical ocean – Model – Resolution – Finite difference – Finite element – Coastline – Assimilation – Open boundary conditions – Topography |
| hal-00409281, version 1 | |
| http://hal.archives-ouvertes.fr/hal-00409281 | |
| oai:hal.archives-ouvertes.fr:hal-00409281 | |
| Contributeur : Le Gos | |
| Soumis le : Jeudi 6 Août 2009, 16:41:50 | |
| Dernière modification le : Jeudi 10 Janvier 2013, 19:03:45 | |