Ignore:
Timestamp:
2018-12-21T15:18:38+01:00 (22 months ago)
Author:
nicolasmartin
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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  • NEMO/trunk/doc/latex/NEMO/subfiles/chap_CONFIG.tex

    r10414 r10442  
    6565  the 3x3 domain is imposed over the whole domain; 
    6666\item[(3)] 
    67   a call to \rou{lbc\_lnk} is systematically done when reading input data ($i.e.$ in \mdl{iom}); 
     67  a call to \rou{lbc\_lnk} is systematically done when reading input data (\ie in \mdl{iom}); 
    6868\item[(3)] 
    6969  a simplified \rou{stp} routine is used (\rou{stp\_c1d}, see \mdl{step\_c1d} module) in which 
     
    103103      \protect\label{fig:MISC_ORCA_msh} 
    104104      ORCA mesh conception. 
    105       The departure from an isotropic Mercator grid start poleward of 20\degN. 
     105      The departure from an isotropic Mercator grid start poleward of 20\deg{N}. 
    106106      The two "north pole" are the foci of a series of embedded ellipses (blue curves) which 
    107107      are determined analytically and form the i-lines of the ORCA mesh (pseudo latitudes). 
     
    138138      \textit{Bottom}: ratio of anisotropy ($e_1 / e_2$) 
    139139      for ORCA 0.5\deg ~mesh. 
    140       South of 20\degN a Mercator grid is used ($e_1 = e_2$) so that the anisotropy ratio is 1. 
    141       Poleward of 20\degN, the two "north pole" introduce a weak anisotropy over the ocean areas ($< 1.2$) except in 
     140      South of 20\deg{N} a Mercator grid is used ($e_1 = e_2$) so that the anisotropy ratio is 1. 
     141      Poleward of 20\deg{N}, the two "north pole" introduce a weak anisotropy over the ocean areas ($< 1.2$) except in 
    142142      vicinity of Victoria Island (Canadian Arctic Archipelago). 
    143143    } 
     
    146146%>>>>>>>>>>>>>>>>>>>>>>>>>>>> 
    147147 
    148 The method is applied to Mercator grid ($i.e.$ same zonal and meridional grid spacing) poleward of 20\degN, 
     148The method is applied to Mercator grid (\ie same zonal and meridional grid spacing) poleward of 20\deg{N}, 
    149149so that the Equator is a mesh line, which provides a better numerical solution for equatorial dynamics. 
    150150The choice of the series of embedded ellipses (position of the foci and variation of the ellipses) 
     
    211211For ORCA\_R1 and R025, setting the configuration key to 75 allows to use 75 vertical levels, otherwise 46 are used. 
    212212In the other ORCA configurations, 31 levels are used 
    213 (see \autoref{tab:orca_zgr} \sfcomment{HERE I need to put new table for ORCA2 values} and \autoref{fig:zgr}). 
     213(see \autoref{tab:orca_zgr} %\sfcomment{HERE I need to put new table for ORCA2 values} and \autoref{fig:zgr}). 
    214214 
    215215Only the ORCA\_R2 is provided with all its input files in the \NEMO distribution. 
     
    248248and their contribution to the large scale circulation.  
    249249 
    250 The domain geometry is a closed rectangular basin on the $\beta$-plane centred at $\sim$ 30\degN and 
     250The domain geometry is a closed rectangular basin on the $\beta$-plane centred at $\sim$ 30\deg{N} and 
    251251rotated by 45\deg, 3180~km long, 2120~km wide and 4~km deep (\autoref{fig:MISC_strait_hand}). 
    252252The domain is bounded by vertical walls and by a flat bottom. 
     
    254254The circulation is forced by analytical profiles of wind and buoyancy fluxes. 
    255255The applied forcings vary seasonally in a sinusoidal manner between winter and summer extrema \citep{Levy_al_OM10}.  
    256 The wind stress is zonal and its curl changes sign at 22\degN and 36\degN. 
     256The wind stress is zonal and its curl changes sign at 22\deg{N} and 36\deg{N}. 
    257257It forces a subpolar gyre in the north, a subtropical gyre in the wider part of the domain and 
    258258a small recirculation gyre in the southern corner. 
     
    322322\biblio 
    323323 
     324\pindex 
     325 
    324326\end{document} 
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