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Effective resolution in ocean models

Patrick Marchesiello 1 Yves Soufflet 1 Xavier Capet 2 Julien Jouanno 3 Florian Lemarié 4 
2 PEPS - Processus de couplage à Petite Echelle, Ecosystèmes et Prédateurs Supérieurs
LOCEAN - Laboratoire d'Océanographie et du Climat : Expérimentations et Approches Numériques
3 OLVAC - Océan du Large et Variabilité Climatique
LEGOS - Laboratoire d'études en Géophysique et océanographie spatiales
4 MOISE - Modelling, Observations, Identification for Environmental Sciences
Inria Grenoble - Rhône-Alpes, LJK - Laboratoire Jean Kuntzmann, Grenoble INP - Institut polytechnique de Grenoble - Grenoble Institute of Technology
Abstract : The increase of model resolution naturally leads to the representation of a wider energy spectrum. As a result, in recent years, the understanding of oceanic submesoscale dynamics has significantly improved. Also, the ubiquity of upper ocean frontal dynamics driving a direct energy cascade is now acknowledged. In the forward cascade framework, numerical and physical closures are more consistent in principle, but dissipation in submesoscale models remains dominated by numerical constraints rather than physical ones. Therefore, effective resolution can be defined by its numerical dissipation range, which is a function of the model numerical filters (assuming that dispersive numerical modes are efficiently removed). The COMODO project gathers the whole French ocean modeling community in order to assess current nu- merical methods and guide the development of future models. Within this framework, we present an idealized ACC-type Jet case, which provides a controllable test of a model capacity at resolving submesoscale dynamics. We compare analyses performed on simulations from two models, ROMS and NEMO, at different mesh sizes (from 20 to 1 km). Through a spectral decomposition of kinetic energy and its budget terms, we identify the characteristics of turbulent cascade, numerical dissipation, and effective resolution. It shows that numerical dissipation appears in different parts of a model, especially in spatial advection-diffusion schemes for momentum equations (KE dissipation) and tracer equations (APE dissipation) and in the time stepping algorithms.
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Contributor : Florian Lemarié Connect in order to contact the contributor
Submitted on : Thursday, September 11, 2014 - 9:53:51 AM
Last modification on : Wednesday, November 16, 2022 - 11:46:08 AM
Long-term archiving on: : Friday, December 12, 2014 - 10:18:43 AM


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  • HAL Id : hal-01062950, version 1


Patrick Marchesiello, Yves Soufflet, Xavier Capet, Julien Jouanno, Florian Lemarié. Effective resolution in ocean models. EGU General Assembly 2014, Apr 2014, Vienna, Austria. 2014. ⟨hal-01062950⟩



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