Changeset 6140 for trunk/DOC/TexFiles/Chapters/Abstracts_Foreword.tex
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- 2015-12-21T12:35:23+01:00 (8 years ago)
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trunk/DOC/TexFiles/Chapters/Abstracts_Foreword.tex
r3294 r6140 13 13 be a flexible tool for studying the ocean and its interactions with the others components of 14 14 the earth climate system over a wide range of space and time scales. 15 Prognostic variables are the three-dimensional velocity field, a linear16 or non-linear sea surface height, the temperature and the salinity. In the horizontal direction,17 the model uses a curvilinear orthogonal grid and in the vertical direction, a full or partial step18 $z$-coordinate, or $s$-coordinate, or a mixture of the two. The distribution of variables is a19 three-dimensional Arakawa C-type grid. Various physical choices are available to describe20 ocean physics, including TKE, GLS and KPP vertical physics. Within NEMO, the ocean is21 interfaced with a sea-ice model (LIM v2 and v3), passive tracer and biogeochemical models (TOP)22 and, via the OASIS coupler, with several atmospheric general circulation models. It also23 support two-way grid embedding via the AGRIF software.15 Prognostic variables are the three-dimensional velocity field, a non-linear sea surface height, 16 the \textit{Conservative} Temperature and the \textit{Absolut} Salinity. 17 In the horizontal direction, the model uses a curvilinear orthogonal grid and in the vertical direction, 18 a full or partial step $z$-coordinate, or $s$-coordinate, or a mixture of the two. 19 The distribution of variables is a three-dimensional Arakawa C-type grid. 20 Various physical choices are available to describe ocean physics, including TKE, and GLS vertical physics. 21 Within NEMO, the ocean is interfaced with a sea-ice model (LIM or CICE), passive tracer and 22 biogeochemical models (TOP) and, via the OASIS coupler, with several atmospheric general circulation models. 23 It also support two-way grid embedding via the AGRIF software. 24 24 25 25 % ================================================================ … … 31 31 interactions avec les autres composantes du syst\`{e}me climatique terrestre. 32 32 Les variables pronostiques sont le champ tridimensionnel de vitesse, une hauteur de la mer 33 lin\'{e}aire ou non, la temperature et la salinit\'{e}.33 lin\'{e}aire, la Ttemperature Conservative et la Salinit\'{e} Absolue. 34 34 La distribution des variables se fait sur une grille C d'Arakawa tridimensionnelle utilisant une 35 35 coordonn\'{e}e verticale $z$ \`{a} niveaux entiers ou partiels, ou une coordonn\'{e}e s, ou encore 36 36 une combinaison des deux. Diff\'{e}rents choix sont propos\'{e}s pour d\'{e}crire la physique 37 oc\'{e}anique, incluant notamment des physiques verticales TKE , GLS et KPP. A travers l'infrastructure38 NEMO, l'oc\'{e}an est interfac\'{e} avec des mod\`{e}les de glace de mer , de biog\'{e}ochimie39 et de traceurs passifs, et, via le coupleur OASIS, \`{a} plusieurs mod\`{e}les de circulation40 g\'{e}n\'{e}rale atmosph\'{e}rique. Il supporte \'{e}galement l'embo\^{i}tement interactif de41 maillages via le logiciel AGRIF.37 oc\'{e}anique, incluant notamment des physiques verticales TKE et GLS. A travers l'infrastructure 38 NEMO, l'oc\'{e}an est interfac\'{e} avec des mod\`{e}les de glace de mer (LIM ou CICE), 39 de biog\'{e}ochimie marine et de traceurs passifs, et, via le coupleur OASIS, \`{a} plusieurs 40 mod\`{e}les de circulation g\'{e}n\'{e}rale atmosph\'{e}rique. 41 Il supporte \'{e}galement l'embo\^{i}tement interactif de maillages via le logiciel AGRIF. 42 42 } 43 43
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