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Changeset 998 for trunk/DOC/TexFiles/Chapters/Chap_DOM.tex – NEMO

Ignore:
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:
1 edited

Legend:

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  • trunk/DOC/TexFiles/Chapters/Chap_DOM.tex

    r996 r998  
    4545%>>>>>>>>>>>>>>>>>>>>>>>>>>>> 
    4646\begin{figure}[!tb] \label{Fig_cell}  \begin{center} 
    47 \includegraphics[width=0.90\textwidth]{./Figures/Fig_cell.pdf} 
     47\includegraphics[width=0.90\textwidth]{./TexFiles/Figures/Fig_cell.pdf} 
    4848\caption{Arrangement of variables. $T$ indicates scalar points where temperature,  
    4949salinity, density, pressure and horizontal divergence are defined. ($u$,$v$,$w$)  
     
    220220%>>>>>>>>>>>>>>>>>>>>>>>>>>>> 
    221221\begin{figure}[!tb] \label{Fig_index_hor}  \begin{center} 
    222 \includegraphics[width=0.90\textwidth]{./Figures/Fig_index_hor.pdf} 
     222\includegraphics[width=0.90\textwidth]{./TexFiles/Figures/Fig_index_hor.pdf} 
    223223\caption{Horizontal integer indexing used in the \textsc{Fortran} code. The dashed  
    224224area indicates the cell in which variables contained in arrays have the same  
     
    269269%>>>>>>>>>>>>>>>>>>>>>>>>>>>> 
    270270\begin{figure}[!pt] \label{Fig_index_vert}  \begin{center} 
    271 \includegraphics[width=.90\textwidth]{./Figures/Fig_index_vert.pdf} 
     271\includegraphics[width=.90\textwidth]{./TexFiles/Figures/Fig_index_vert.pdf} 
    272272\caption{Vertical integer indexing used in the \textsc{Fortran } code. Note that  
    273273the $k$-axis is orientated downward. The dashed area indicates the cell in  
     
    374374%>>>>>>>>>>>>>>>>>>>>>>>>>>>> 
    375375\begin{figure}[!t] \label{Fig_zgr_e3}  \begin{center} 
    376 \includegraphics[width=0.90\textwidth]{./Figures/Fig_zgr_e3.pdf} 
     376\includegraphics[width=0.90\textwidth]{./TexFiles/Figures/Fig_zgr_e3.pdf} 
    377377\caption{Comparison of (a) traditional definitions of grid-point position and grid-size  
    378378in the vertical, and (b) analytically derived grid-point position and scale factors. For  
     
    479479%>>>>>>>>>>>>>>>>>>>>>>>>>>>> 
    480480\begin{figure}[!tb] \label{Fig_z_zps_s_sps}  \begin{center} 
    481 \includegraphics[width=1.0\textwidth]{./Figures/Fig_z_zps_s_sps.pdf} 
     481\includegraphics[width=1.0\textwidth]{./TexFiles/Figures/Fig_z_zps_s_sps.pdf} 
    482482\caption{The ocean bottom as seen by the model:  
    483483(a) $z$-coordinate with full step,  
     
    583583%>>>>>>>>>>>>>>>>>>>>>>>>>>>> 
    584584\begin{figure}[!tb] \label{Fig_zgr}  \begin{center} 
    585 \includegraphics[width=0.90\textwidth]{./Figures/Fig_zgr.pdf} 
     585\includegraphics[width=0.90\textwidth]{./TexFiles/Figures/Fig_zgr.pdf} 
    586586\caption{Default vertical mesh for ORCA2: 30 ocean levels (L30). Vertical level  
    587587functions for (a) T-point depth and (b) the associated scale factor as computed  
     
    767767%>>>>>>>>>>>>>>>>>>>>>>>>>>>> 
    768768\begin{figure}[!tb] \label{Fig_sco_function}  \begin{center} 
    769 \includegraphics[width=1.0\textwidth]{./Figures/Fig_sco_function.pdf} 
     769\includegraphics[width=1.0\textwidth]{./TexFiles/Figures/Fig_sco_function.pdf} 
    770770\caption{Examples of the stretching function applied to a sea mont; from left to right: surface, surface and bottom, and bottom intensified resolutions} 
    771771\end{center}   \end{figure} 
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