Changeset 11433 for NEMO/trunk/doc/latex/NEMO
- Timestamp:
- 2019-08-12T21:44:18+02:00 (5 years ago)
- Location:
- NEMO/trunk/doc/latex/NEMO/main
- Files:
-
- 3 edited
Legend:
- Unmodified
- Added
- Removed
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NEMO/trunk/doc/latex/NEMO/main/definitions.tex
r11176 r11433 1 %% Engine ( folder name)1 %% Engine (subfolder name) 2 2 \def \engine{NEMO} 3 3 4 %% Title (variable name already use by 'titling' pkg) 4 %% Title and cover page settings 5 \def \spacetop{ \vspace*{1.85cm} } 5 6 \def \heading{NEMO ocean engine} 7 \def \subheading{} 8 \def \spacedown{ \vspace*{0.75cm } } 9 \def \authorswidth{ 0.3\linewidth} 10 \def \rulelenght{270pt} 11 \def \abstractwidth{0.6\linewidth} 6 12 7 %% Authors (thanks will apply to the second author) 8 \def \firstauthor{Gurvan Madec~} 9 \def \secondauthor{NEMO System Team} 13 %% Color for document (frontpage banner, links and chapter boxes) 14 \def \setcolor{ \definecolor{manualcolor}{cmyk}{1, .60, 0, .40} } 10 15 11 16 %% IPSL publication number -
NEMO/trunk/doc/latex/NEMO/main/foreword.tex
r11176 r11433 1 % ================================================================ 2 % Foreword 3 % ================================================================ 4 \chapter*{Foreword} 1 %% ================================================================ 2 %% Abstract 3 %% ================================================================ 5 4 6 The ocean engine of NEMO (Nucleus for European Modelling of the Ocean) is a primitive equation model adapted to 7 regional and global ocean circulation problems. 8 It is intended to be a flexible tool for studying the ocean and its interactions with the others components of 9 the earth climate system over a wide range of space and time scales. 5 %% Common part between NEMO-SI3-TOP 6 \NEMO\ (``Nucleus for European Modelling of the Ocean'') is a framework of ocean-related engines. 7 It is intended to be a flexible tool for studying the ocean dynamics and thermodynamics (``blue ocean''), 8 as well as its interactions with the components of the Earth climate system over 9 a wide range of space and time scales. 10 Within \NEMO, the ocean engine is interfaced with a sea-ice model (\SIcube\ or 11 \href{http://github.com/CICE-Consortium/CICE}{CICE}), 12 passive tracers and biogeochemical models (\TOP) and, 13 via the \href{http://portal.enes.org/oasis}{OASIS} coupler, 14 with several atmospheric general circulation models. 15 It also supports two-way grid embedding by means of the \href{http://agrif.imag.fr}{AGRIF} software. 10 16 17 %% Specific part 18 The primitive equation model is adapted to regional and global ocean circulation problems down to 19 kilometric scale. 11 20 Prognostic variables are the three-dimensional velocity field, a non-linear sea surface height, 12 21 the \textit{Conservative} Temperature and the \textit{Absolute} Salinity. 13 In the horizontal direction, the model uses a curvilinear orthogonal grid and in the vertical direction, 14 a full or partial step $z$-coordinate, or $s$-coordinate, or a mixture of the two. 22 In the horizontal direction, the model uses a curvilinear orthogonal grid and 23 in the vertical direction, a full or partial step $z$-coordinate, or $s$-coordinate, or 24 a mixture of the two. 15 25 The distribution of variables is a three-dimensional Arakawa C-type grid. 16 Various physical choices are available to describe ocean physics, including TKE, and GLS vertical physics. 17 18 Within NEMO, the ocean is interfaced with a sea-ice model (SI$^3$) 19 %or \href{https://github.com/CICE-Consortium/CICE}{CICE}), 20 passive tracer and biogeochemical models (TOP-PISCES) and, 21 via the \href{https://portal.enes.org/oasis}{OASIS} coupler, with several atmospheric general circulation models. 22 It also support two-way grid embedding via the \href{http://agrif.imag.fr}{AGRIF} software. 26 Various physical choices are available to describe ocean physics, 27 so as various HPC functionalities to improve performances. -
NEMO/trunk/doc/latex/NEMO/main/thanks.tex
r11212 r11433 1 J\'{e}r\^{o}me Chanut, 2 Silvia Mocavero 1 %Romain Bourdall\'{e}-Badie 2 %\orcid{0000-0002-8742-3289} \\ 3 %Mike Bell \\ 4 %J\'{e}r\^{o}me Chanut \\ 5 %Emanuela Clementi 6 %\orcid{0000-0002-5752-1849} \\ 7 %Andrew Coward 8 %\orcid{0000-0002-0456-129X} \\ 9 %Massimiliano Drudi 10 %\orcid{0000-0002-9951-740X} \\ 11 %Christian \'{E}th\'{e} \\ 12 %Doroteaciro Iovino 13 %\orcid{0000-0001-5132-7255} \\ 14 %Dan Lea \\ 15 %Claire L\'{e}vy 16 %\orcid{0000-0003-2518-6692} \\ 17 %Gurvan Madec 18 %\orcid{0000-0002-6447-4198} \\ 19 %Nicolas Martin \\ 20 %S\'{e}bastien Masson 21 %\orcid{0000-0002-1694-8117} \\ 22 %Pierre Mathiot \\ 23 %Silvia Mocavero 24 %\orcid{0000-0002-6309-8282} \\ 25 %Simon M\"{u}ller \\ 26 %George Nurser \\ 27 %Guillaume Samson 28 %\orcid{0000-0001-7481-6369} \\ 29 %Dave Storkey 30 31 \orcid{0000-0002-8742-3289} Romain Bourdall\'{e}-Badie \\ 32 Mike Bell \\ 33 J\'{e}r\^{o}me Chanut \\ 34 \orcid{0000-0002-5752-1849} Emanuela Clementi \\ 35 \orcid{0000-0002-0456-129X} Andrew Coward \\ 36 \orcid{0000-0002-9951-740X} Massimiliano Drudi \\ 37 Christian \'{E}th\'{e} \\ 38 \orcid{0000-0001-5132-7255} Doroteaciro Iovino \\ 39 Dan Lea \\ 40 \orcid{0000-0003-2518-6692} Claire L\'{e}vy \\ 41 \orcid{0000-0002-6447-4198} Gurvan Madec \\ 42 Nicolas Martin \\ 43 \orcid{0000-0002-1694-8117} S\'{e}bastien Masson \\ 44 Pierre Mathiot \\ 45 \orcid{0000-0002-6309-8282} Silvia Mocavero \\ 46 Simon M\"{u}ller \\ 47 George Nurser \\ 48 \orcid{0000-0001-7481-6369} Guillaume Samson \\ 49 Dave Storkey
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