# Changeset 10442 for NEMO/trunk/doc/latex/NEMO/subfiles/chap_CONFIG.tex

Ignore:
Timestamp:
2018-12-21T15:18:38+01:00 (22 months ago)
Message:

Front page edition, cleaning in custom LaTeX commands and add index for single subfile compilation

• Use \thanks storing cmd to refer to the ST members list for 2018 in an footnote on the cover page
• NEMO and Fortran in small capitals
• Removing of unused or underused custom cmds, move local cmds to their respective .tex file
• Addition of new ones (\zstar, \ztilde, \sstar, \stilde, \ie, \eg, \fortran, \fninety)
• Fonts for indexed items: italic font for files (modules and .nc files), preformat for code (CPP keys, routines names and namelists content)
File:
1 edited

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Unmodified
 r10414 the 3x3 domain is imposed over the whole domain; \item[(3)] a call to \rou{lbc\_lnk} is systematically done when reading input data ($i.e.$ in \mdl{iom}); a call to \rou{lbc\_lnk} is systematically done when reading input data (\ie in \mdl{iom}); \item[(3)] a simplified \rou{stp} routine is used (\rou{stp\_c1d}, see \mdl{step\_c1d} module) in which \protect\label{fig:MISC_ORCA_msh} ORCA mesh conception. The departure from an isotropic Mercator grid start poleward of 20\degN. The departure from an isotropic Mercator grid start poleward of 20\deg{N}. The two "north pole" are the foci of a series of embedded ellipses (blue curves) which are determined analytically and form the i-lines of the ORCA mesh (pseudo latitudes). \textit{Bottom}: ratio of anisotropy ($e_1 / e_2$) for ORCA 0.5\deg ~mesh. South of 20\degN a Mercator grid is used ($e_1 = e_2$) so that the anisotropy ratio is 1. Poleward of 20\degN, the two "north pole" introduce a weak anisotropy over the ocean areas ($< 1.2$) except in South of 20\deg{N} a Mercator grid is used ($e_1 = e_2$) so that the anisotropy ratio is 1. Poleward of 20\deg{N}, the two "north pole" introduce a weak anisotropy over the ocean areas ($< 1.2$) except in vicinity of Victoria Island (Canadian Arctic Archipelago). } %>>>>>>>>>>>>>>>>>>>>>>>>>>>> The method is applied to Mercator grid ($i.e.$ same zonal and meridional grid spacing) poleward of 20\degN, The method is applied to Mercator grid (\ie same zonal and meridional grid spacing) poleward of 20\deg{N}, so that the Equator is a mesh line, which provides a better numerical solution for equatorial dynamics. The choice of the series of embedded ellipses (position of the foci and variation of the ellipses) For ORCA\_R1 and R025, setting the configuration key to 75 allows to use 75 vertical levels, otherwise 46 are used. In the other ORCA configurations, 31 levels are used (see \autoref{tab:orca_zgr} \sfcomment{HERE I need to put new table for ORCA2 values} and \autoref{fig:zgr}). (see \autoref{tab:orca_zgr} %\sfcomment{HERE I need to put new table for ORCA2 values} and \autoref{fig:zgr}). Only the ORCA\_R2 is provided with all its input files in the \NEMO distribution. and their contribution to the large scale circulation. The domain geometry is a closed rectangular basin on the $\beta$-plane centred at $\sim$ 30\degN and The domain geometry is a closed rectangular basin on the $\beta$-plane centred at $\sim$ 30\deg{N} and rotated by 45\deg, 3180~km long, 2120~km wide and 4~km deep (\autoref{fig:MISC_strait_hand}). The domain is bounded by vertical walls and by a flat bottom. The circulation is forced by analytical profiles of wind and buoyancy fluxes. The applied forcings vary seasonally in a sinusoidal manner between winter and summer extrema \citep{Levy_al_OM10}. The wind stress is zonal and its curl changes sign at 22\degN and 36\degN. The wind stress is zonal and its curl changes sign at 22\deg{N} and 36\deg{N}. It forces a subpolar gyre in the north, a subtropical gyre in the wider part of the domain and a small recirculation gyre in the southern corner. \biblio \pindex \end{document}