https://hal.inria.fr/hal-01413010v2Kazantsev, EugeneEugeneKazantsevAIRSEA - Mathematics and computing applied to oceanic and atmospheric flows - Inria Grenoble - Rhône-Alpes - Inria - Institut National de Recherche en Informatique et en Automatique - Grenoble INP - Institut polytechnique de Grenoble - Grenoble Institute of Technology - UGA [2016-2019] - Université Grenoble Alpes [2016-2019] - LJK - Laboratoire Jean Kuntzmann - Grenoble INP - Institut polytechnique de Grenoble - Grenoble Institute of Technology - Inria - Institut National de Recherche en Informatique et en Automatique - CNRS - Centre National de la Recherche Scientifique - UGA [2016-2019] - Université Grenoble Alpes [2016-2019]Parameterizing subgrid scale eddy effects in a shallow water modelHAL CCSD2017Shallow waterSubgrid scalesBackscattering Viscous flowTurbulent flowShallow water model[PHYS.PHYS.PHYS-AO-PH] Physics [physics]/Physics [physics]/Atmospheric and Oceanic Physics [physics.ao-ph][MATH.MATH-MP] Mathematics [math]/Mathematical Physics [math-ph]Kazantsev, Eugene2017-12-18 14:37:522023-03-24 14:53:052017-12-18 16:42:50enPreprints, Working Papers, ...https://hal.inria.fr/hal-01413010v1application/pdf2Basing on the maximum entropy production principle, the influence of subgrid scales on the flow is presented as the harmonic dissipation accompanied by the backscattering of the dissipated energy. This parametrization is tested on the shallow water model in a square box. The closure problem is analyzed basing on the balance between the dissipation of energy and its backscattering. Results of this model on the coarse resolution grid are compared with the reference simulation at four times higher resolution. It is shown that the mean flow is correctly recovered, as well as variability properties, such as eddy kinetic energy fields and its spectrum.