Changeset 10544

Timestamp:

2019-01-18T14:20:35+01:00 (4 years ago)

Author:

nicolasmartin

Message:

Fixes for LaTeX compilation of NEMO manual

Location:

NEMO/trunk/doc/latex/NEMO

Files:

• main/NEMO_manual.sty (modified) (1 diff)
• subfiles/chap_TRA.tex (modified) (1 diff)
• subfiles/chap_model_basics.tex (modified) (1 diff)
• subfiles/chap_model_basics_zstar.tex (modified) (1 diff)
• subfiles/introduction.tex (modified) (1 diff)

NEMO/trunk/doc/latex/NEMO/main/NEMO_manual.sty

@@ -135 +135 @@
 
 %% Maths
+\newcommand{\lt}{\left}
+\newcommand{\rt}{\right}
 \newcommand{\vect}[1]{\ensuremath{\mathbf{#1}}}
 \newcommand{\pd}[2][]{\ensuremath{\frac{\partial #1}{\partial #2}}}

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

@@ -1219 +1219 @@
   the TEOS-10 rational function approximation for hydrographic data analysis \citep{TEOS10}.
   A key point is that conservative state variables are used:
-  Absolute Salinity (unit: g/kg, notation: $S_A$) and Conservative Temperature (unit: \degC, notation: $\Theta$).
+  Absolute Salinity (unit: g/kg, notation: $S_A$) and Conservative Temperature (unit: \deg{C}, notation: $\Theta$).
   The pressure in decibars is approximated by the depth in meters.
   With TEOS10, the specific heat capacity of sea water, $C_p$, is a constant.

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

@@ -1095 +1095 @@
 where $ \vect U^\ast = \lt( u^\ast,v^\ast,w^\ast \rt)$ is a non-divergent,
 eddy-induced transport velocity. This velocity field is defined by:
-\[
+\begin{gather}
   % \label{eq:PE_eiv}
-  u^\ast &=   \frac{1}{e_3}            \pd[]{k} \lt( A^{eiv} \;        \tilde{r}_1 \rt) \\
-  v^\ast &=   \frac{1}{e_3}            \pd[]{k} \lt( A^{eiv} \;        \tilde{r}_2 \rt) \\
-  w^\ast &= - \frac{1}{e_1 e_2} \lt[   \pd[]{i} \lt( A^{eiv} \; e_2 \, \tilde{r}_1 \rt)
+  u^\ast =   \frac{1}{e_3}            \pd[]{k} \lt( A^{eiv} \;        \tilde{r}_1 \rt) \\
+  v^\ast =   \frac{1}{e_3}            \pd[]{k} \lt( A^{eiv} \;        \tilde{r}_2 \rt) \\
+  w^\ast = - \frac{1}{e_1 e_2} \lt[   \pd[]{i} \lt( A^{eiv} \; e_2 \, \tilde{r}_1 \rt)
                                      + \pd[]{j} \lt( A^{eiv} \; e_1 \, \tilde{r}_2 \rt) \rt]
-\]
+\end{gather}
 where $A^{eiv}$ is the eddy induced velocity coefficient
 (or equivalently the isoneutral thickness diffusivity coefficient),

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

@@ -89 +89 @@
 which imposes a very small time step when an explicit time stepping is used.
 Two methods are proposed to allow a longer time step for the three-dimensional equations:
-the filtered free surface, which is a modification of the continuous equations (see \autoref{eq:PE_flt}),
+the filtered free surface, which is a modification of the continuous equations %(see \autoref{eq:PE_flt}),
 and the split-explicit free surface described below.
 The extra term introduced in the filtered method is calculated implicitly,

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

@@ -165 +165 @@
 After the presentation of the continuous equations (\autoref{chap:PE}),
 the following chapters refer to specific terms of the equations each associated with a group of modules 
-(\autoref{tab:chap}).
+(\autoref{tab:chapters}).
 
 %--------------------------------------------------TABLE--------------------------------------------------