Numerical modification of atmospheric models to include the feedback of oceanic currents on air-sea fluxes in ocean-atmosphere coupled models

Florian Lemarié 1
1 AIRSEA - Mathematics and computing applied to oceanic and atmospheric flows
Inria Grenoble - Rhône-Alpes, LJK - Laboratoire Jean Kuntzmann, UJF - Université Joseph Fourier - Grenoble 1, INPG - Institut National Polytechnique de Grenoble
Abstract : In this note we present the modification to bring to an atmospheric model to account for relative winds (i.e. the difference between the near-surface winds and the oceanic currents) instead of absolute winds in the computation of air-sea fluxes. Because of the implicit treatment of the bottom boundary condition in most atmospheric models the use of relative winds involves a modification of both the surface layer parameterization and the tridiagonal matrix for vertical turbulent diffusion.
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Rapport
[Technical Report] RT-0464, INRIA Grenoble - Rhône-Alpes; Laboratoire Jean Kuntzmann; Universite de Grenoble I - Joseph Fourier; INRIA. 2015
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https://hal.inria.fr/hal-01184711
Contributeur : Florian Lemarié <>
Soumis le : lundi 17 août 2015 - 14:25:08
Dernière modification le : mercredi 11 avril 2018 - 01:59:00
Document(s) archivé(s) le : mercredi 18 novembre 2015 - 12:10:32

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Florian Lemarié. Numerical modification of atmospheric models to include the feedback of oceanic currents on air-sea fluxes in ocean-atmosphere coupled models. [Technical Report] RT-0464, INRIA Grenoble - Rhône-Alpes; Laboratoire Jean Kuntzmann; Universite de Grenoble I - Joseph Fourier; INRIA. 2015. 〈hal-01184711〉

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