Changeset 6997 for trunk/DOC/TexFiles/Chapters/Chap_LDF.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_LDF.tex (modified) (6 diffs)

trunk/DOC/TexFiles/Chapters/Chap_LDF.tex

@@ +1 @@
+\documentclass[NEMO_book]{subfiles}
+\begin{document}
 
 % ================================================================
@@ -228 +230 @@
 %>>>>>>>>>>>>>>>>>>>>>>>>>>>>
 \begin{figure}[!ht]      \begin{center}
-\includegraphics[width=0.70\textwidth]{./TexFiles/Figures/Fig_LDF_ZDF1.pdf}
+\includegraphics[width=0.70\textwidth]{Fig_LDF_ZDF1}
 \caption {    \label{Fig_LDF_ZDF1}
 averaging procedure for isopycnal slope computation.}
@@ -256 +258 @@
 %>>>>>>>>>>>>>>>>>>>>>>>>>>>>
 \begin{figure}[!ht]     \begin{center}
-\includegraphics[width=0.70\textwidth]{./TexFiles/Figures/Fig_eiv_slp.pdf}
+\includegraphics[width=0.70\textwidth]{Fig_eiv_slp}
 \caption {     \label{Fig_eiv_slp}
 Vertical profile of the slope used for lateral mixing in the mixed layer : 
@@ -298 +300 @@
 diffusion along model level surfaces, i.e. using the shear computed along 
 the model levels and with no additional friction at the ocean bottom (see 
-{\S\ref{LBC_coast}).
+\S\ref{LBC_coast}).
 
 
@@ -425 +427 @@
 values are $0$). However, the technique used to compute the isopycnal 
 slopes is intended to get rid of such a background diffusion, since it introduces 
-spurious diapycnal diffusion (see {\S\ref{LDF_slp}).
+spurious diapycnal diffusion (see \S\ref{LDF_slp}).
 
 (4) when an eddy induced advection term is used (\key{traldf\_eiv}), $A^{eiv}$, 
@@ -499 +501 @@
 
 
-
+\end{document}