Changeset 6808 for branches/NERC/dev_r5549_BDY_ZEROGRAD/DOC/TexFiles/Chapters/Abstracts_Foreword.tex

Timestamp:

2016-07-19T10:38:35+02:00 (8 years ago)

Author:

jamesharle

Message:

merge with trunk@6232 for consistency with SSB code

File:

• branches/NERC/dev_r5549_BDY_ZEROGRAD/DOC/TexFiles/Chapters/Abstracts_Foreword.tex (modified) (2 diffs)

branches/NERC/dev_r5549_BDY_ZEROGRAD/DOC/TexFiles/Chapters/Abstracts_Foreword.tex

@@ -13 +13 @@
 be a flexible tool for studying the ocean and its interactions with the others components of 
 the earth climate system over a wide range of space and time scales. 
-Prognostic variables are the three-dimensional velocity field, a linear 
-or non-linear sea surface height, the temperature and the salinity. In the horizontal direction, 
-the model uses a curvilinear orthogonal grid and in the vertical direction, a full or partial step 
-$z$-coordinate, or $s$-coordinate, or a mixture of the two. The distribution of variables is a 
-three-dimensional Arakawa C-type grid. Various physical choices are available to describe 
-ocean physics, including TKE, GLS and KPP vertical physics. Within NEMO, the ocean is 
-interfaced with a sea-ice model (LIM v2 and v3), passive tracer and biogeochemical models (TOP) 
-and, via the OASIS coupler, with several atmospheric general circulation models. It also 
-support two-way grid embedding via the AGRIF software.
+Prognostic variables are the three-dimensional velocity field, a non-linear sea surface height, 
+the \textit{Conservative} Temperature and the \textit{Absolut} Salinity. 
+In the horizontal direction, the model uses a curvilinear orthogonal grid and in the vertical direction, 
+a full or partial step $z$-coordinate, or $s$-coordinate, or a mixture of the two. 
+The distribution of variables is a three-dimensional Arakawa C-type grid. 
+Various physical choices are available to describe ocean physics, including TKE, and GLS vertical physics. 
+Within NEMO, the ocean is interfaced with a sea-ice model (LIM or CICE), passive tracer and 
+biogeochemical models (TOP) and, via the OASIS coupler, with several atmospheric general circulation models. 
+It also support two-way grid embedding via the AGRIF software.
 
 % ================================================================
@@ -31 +31 @@
 interactions avec les autres composantes du syst\`{e}me climatique terrestre. 
 Les variables pronostiques sont le champ tridimensionnel de vitesse, une hauteur de la mer 
-lin\'{e}aire ou non, la temperature et la salinit\'{e}. 
+lin\'{e}aire, la Ttemperature Conservative et la Salinit\'{e} Absolue. 
 La distribution des variables se fait sur une grille C d'Arakawa tridimensionnelle utilisant une 
 coordonn\'{e}e verticale $z$ \`{a} niveaux entiers ou partiels, ou une coordonn\'{e}e s, ou encore 
 une combinaison des deux. Diff\'{e}rents choix sont propos\'{e}s pour d\'{e}crire la physique 
-oc\'{e}anique, incluant notamment des physiques verticales TKE, GLS et KPP. A travers l'infrastructure 
-NEMO, l'oc\'{e}an est interfac\'{e} avec des mod\`{e}les de glace de mer, de biog\'{e}ochimie 
-et de traceurs passifs, et, via le coupleur OASIS, \`{a} plusieurs mod\`{e}les de circulation 
-g\'{e}n\'{e}rale atmosph\'{e}rique. Il supporte \'{e}galement l'embo\^{i}tement interactif de 
-maillages via le logiciel AGRIF.
+oc\'{e}anique, incluant notamment des physiques verticales TKE et GLS. A travers l'infrastructure 
+NEMO, l'oc\'{e}an est interfac\'{e} avec des mod\`{e}les de glace de mer (LIM ou CICE), 
+de biog\'{e}ochimie marine et de traceurs passifs, et, via le coupleur OASIS, \`{a} plusieurs 
+mod\`{e}les de circulation g\'{e}n\'{e}rale atmosph\'{e}rique. 
+Il supporte \'{e}galement l'embo\^{i}tement interactif de maillages via le logiciel AGRIF.
 }