Changeset 6997 for trunk/DOC/TexFiles/Chapters/Chap_DYN.tex

Timestamp:

2016-10-05T16:26:13+02:00 (8 years ago)

Author:

nicolasmartin

Message:

Duplication of changes in DOC directory for the trunk

File:

• trunk/DOC/TexFiles/Chapters/Chap_DYN.tex (modified) (5 diffs)

trunk/DOC/TexFiles/Chapters/Chap_DYN.tex

@@ +1 @@
+\documentclass[NEMO_book]{subfiles}
+\begin{document}
 % ================================================================
 % Chapter ——— Ocean Dynamics (DYN)
@@ -294 +296 @@
 %>>>>>>>>>>>>>>>>>>>>>>>>>>>>>>>>
 \begin{figure}[!ht]    \begin{center}
-\includegraphics[width=0.70\textwidth]{./TexFiles/Figures/Fig_DYN_een_triad.pdf}
+\includegraphics[width=0.70\textwidth]{Fig_DYN_een_triad}
 \caption{ \label{Fig_DYN_een_triad}  
 Triads used in the energy and enstrophy conserving scheme (een) for 
@@ -663 +665 @@
 $\bullet$ The main hypothesis to compute the ice shelf load is that the ice shelf is in an isostatic equilibrium.
  The top pressure is computed integrating from surface to the base of the ice shelf a reference density profile 
-(prescribed as density of a water at 34.4 PSU and -1.9$\degres C$) and corresponds to the water replaced by the ice shelf. 
+(prescribed as density of a water at 34.4 PSU and -1.9\degC) and corresponds to the water replaced by the ice shelf. 
 This top pressure is constant over time. A detailed description of this method is described in \citet{Losch2008}.\\
 
@@ -827 +829 @@
 %>   >   >   >   >   >   >   >   >   >   >   >   >   >   >   >   >   >   >   >   >   >   >   >   >   >   >   >
 \begin{figure}[!t]    \begin{center}
-\includegraphics[width=0.7\textwidth]{./TexFiles/Figures/Fig_DYN_dynspg_ts.pdf}
+\includegraphics[width=0.7\textwidth]{Fig_DYN_dynspg_ts}
 \caption{  \label{Fig_DYN_dynspg_ts}
 Schematic of the split-explicit time stepping scheme for the external 
@@ -1263 +1265 @@
 
 % ================================================================
+\end{document}