Changeset 10442 for NEMO/trunk/doc/latex/NEMO/subfiles/chap_time_domain.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_time_domain.tex (modified) (5 diffs)

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

@@ -22 +22 @@
 Having defined the continuous equations in \autoref{chap:PE}, we need now to choose a time discretization,
 a key feature of an ocean model as it exerts a strong influence on the structure of the computer code
-($i.e.$ on its flowchart).
+(\ie on its flowchart).
 In the present chapter, we provide a general description of the \NEMO time stepping strategy and
 the consequences for the order in which the equations are solved.
@@ -67 +67 @@
 \citep{Mesinger_Arakawa_Bk76}.
 This scheme is widely used for advection processes in low-viscosity fluids.
-It is a time centred scheme, $i.e.$ the RHS in \autoref{eq:STP} is evaluated at time step $t$, the now time step.
+It is a time centred scheme, \ie the RHS in \autoref{eq:STP} is evaluated at time step $t$, the now time step.
 It may be used for momentum and tracer advection, pressure gradient, and Coriolis terms,
 but not for diffusion terms.
@@ -229 +229 @@
 
 In a classical LF-RA environment, the forcing term is centred in time,
-$i.e.$ it is time-stepped over a $2\rdt$ period:
+\ie it is time-stepped over a $2\rdt$ period:
 $x^t  = x^t + 2\rdt Q^t $ where $Q$ is the forcing applied to $x$,
 and the time filter is given by \autoref{eq:STP_asselin} so that $Q$ is redistributed over several time step.
@@ -296 +296 @@
   x^1 = x^0 + \rdt \ \text{RHS}^0
 \]
-This is done simply by keeping the leapfrog environment ($i.e.$ the \autoref{eq:STP} three level time stepping) but
+This is done simply by keeping the leapfrog environment (\ie the \autoref{eq:STP} three level time stepping) but
 setting all $x^0$ (\textit{before}) and $x^{1}$ (\textit{now}) fields equal at the first time step and
 using half the value of $\rdt$.
@@ -408 +408 @@
 \biblio
 
+\pindex
+
 \end{document}