Changeset 998 for trunk/DOC/TexFiles/Chapters/Chap_LDF.tex

Timestamp:

2008-05-28T13:53:22+02:00 (16 years ago)

Author:

gm

Message:

trunk - DOC - update .tex due to the change in position of NEMO_book

File:

• trunk/DOC/TexFiles/Chapters/Chap_LDF.tex (modified) (2 diffs)

trunk/DOC/TexFiles/Chapters/Chap_LDF.tex

@@ -232 +232 @@
 %>>>>>>>>>>>>>>>>>>>>>>>>>>>>
 \begin{figure}[!ht] \label{Fig_LDF_ZDF1}  \begin{center}
-\includegraphics[width=0.70\textwidth]{./Figures/Fig_LDF_ZDF1.pdf}
+\includegraphics[width=0.70\textwidth]{./TexFiles/Figures/Fig_LDF_ZDF1.pdf}
 \caption {averaging procedure for isopycnal slope computation.}
 \end{center}   \end{figure}
@@ -249 +249 @@
 %>>>>>>>>>>>>>>>>>>>>>>>>>>>>
 \begin{figure}[!ht] \label{Fig_eiv_slp}  \begin{center}
-\includegraphics[width=0.70\textwidth]{./Figures/Fig_eiv_slp.pdf}
+\includegraphics[width=0.70\textwidth]{./TexFiles/Figures/Fig_eiv_slp.pdf}
 \caption {Vertical profile of the slope used for lateral mixing in the mixed layer : \textit{(a)} in the real ocean the slope is the iso-neutral slope in the ocean interior and their have to adjust to the surface boundary (i.e. tend to zero at the surface as there is no mixing across the air-sea interface: wall boundary condition). Nevertheless, the profile between surface zero value and interior iso-neutral one is unknown, and especially the value at the based of the mixed layer ; \textit{(b)} profile of slope using a linear tapering of the slope near the surface and imposing a maximum slope of 1/100 ; \textit{(c)} profile of slope actuelly used in \NEMO: linear decrease of the slope from zero at the surface to its ocean interior value computed just below the mixed layer. Note the huge change in the slope at the based of the mixed layer between  \textit{(b)}  and \textit{(c)}. 
 .}