Changeset 10442 for NEMO/trunk/doc/latex/NEMO/subfiles/annex_A.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/annex_A.tex (modified) (6 diffs)

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

@@ -20 +20 @@
 
 In order to establish the set of Primitive Equation in curvilinear $s$-coordinates
-($i.e.$ an orthogonal curvilinear coordinate in the horizontal and
+(\ie an orthogonal curvilinear coordinate in the horizontal and
 an Arbitrary Lagrangian Eulerian (ALE) coordinate in the vertical),
 we start from the set of equations established in \autoref{subsec:PE_zco_Eq} for
@@ -273 +273 @@
 \]
 leads to the $s-$coordinate formulation of the total $z-$coordinate time derivative,
-$i.e.$ the total $s-$coordinate time derivative :
+\ie the total $s-$coordinate time derivative :
 \begin{align}
   \label{apdx:A_sco_Dt_vect}
@@ -312 +312 @@
 %
 Introducing the vertical scale factor inside the horizontal derivative of the first two terms 
-($i.e.$ the horizontal divergence), it becomes :
+(\ie the horizontal divergence), it becomes :
 \begin{align*}
   {
@@ -355 +355 @@
 \end{align*}
 which leads to the $s-$coordinate flux formulation of the total $s-$coordinate time derivative, 
-$i.e.$ the total $s-$coordinate time derivative in flux form:
+\ie the total $s-$coordinate time derivative in flux form:
 \begin{flalign}
   \label{apdx:A_sco_Dt_flux}
@@ -513 +513 @@
 in particular the pressure gradient.
 By contrast, $\omega$ is not $w$, the third component of the velocity, but the dia-surface velocity component,
-$i.e.$ the volume flux across the moving $s$-surfaces per unit horizontal area. 
+\ie the volume flux across the moving $s$-surfaces per unit horizontal area. 
 
 
@@ -540 +540 @@
 \biblio
 
+\pindex
+
 \end{document}