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

Timestamp:

2018-12-21T15:18:38+01:00 (5 years 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:

• NEMO/trunk/doc/latex/NEMO/subfiles/chap_CONFIG.tex (modified) (8 diffs)

NEMO/trunk/doc/latex/NEMO/subfiles/chap_CONFIG.tex

@@ -65 +65 @@
   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
@@ -103 +103 @@
       \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).
@@ -138 +138 @@
       \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).
     }
@@ -146 +146 @@
 %>>>>>>>>>>>>>>>>>>>>>>>>>>>>
 
-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)
@@ -211 +211 @@
 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.
@@ -248 +248 @@
 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.
@@ -254 +254 @@
 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.
@@ -322 +322 @@
 \biblio
 
+\pindex
+
 \end{document}