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Changeset 998 for trunk/DOC/TexFiles/Chapters/Chap_TRA.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

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

    r996 r998  
    103103%>>>>>>>>>>>>>>>>>>>>>>>>>>>> 
    104104\begin{figure}[!t] \label{Fig_adv_scheme}  \begin{center} 
    105 \includegraphics[width=0.9\textwidth]{./Figures/Fig_adv_scheme.pdf} 
     105\includegraphics[width=0.9\textwidth]{./TexFiles/Figures/Fig_adv_scheme.pdf} 
    106106\caption{Schematic representation of some ways used to evaluate the tracer value  
    107107at $u$-point and the amount of tracer exchanged between two neighbouring grid  
     
    836836%>>>>>>>>>>>>>>>>>>>>>>>>>>>> 
    837837\begin{figure}[!t] \label{Fig_geothermal}  \begin{center} 
    838 \includegraphics[width=1.0\textwidth]{./Figures/Fig_TRA_geoth.pdf} 
     838\includegraphics[width=1.0\textwidth]{./TexFiles/Figures/Fig_TRA_geoth.pdf} 
    839839\caption{Geothermal Heat flux (in $mW.m^{-2}$) as inferred from the age  
    840840of the sea floor and the formulae of \citet{Stein1992}.} 
     
    933933%>>>>>>>>>>>>>>>>>>>>>>>>>>>> 
    934934\begin{figure}[!t] \label{Fig_bbl}  \begin{center} 
    935 \includegraphics[width=1.0\textwidth]{./Figures/Fig_BBL_adv.pdf} 
     935\includegraphics[width=1.0\textwidth]{./TexFiles/Figures/Fig_BBL_adv.pdf} 
    936936\caption{Advective Bottom Boundary Layer.} 
    937937\end{center}   \end{figure} 
     
    12351235%>>>>>>>>>>>>>>>>>>>>>>>>>>>> 
    12361236\begin{figure}[!p] \label{Fig_Partial_step_scheme}  \begin{center} 
    1237 \includegraphics[width=0.9\textwidth]{./Figures/Partial_step_scheme.pdf} 
     1237\includegraphics[width=0.9\textwidth]{./TexFiles/Figures/Partial_step_scheme.pdf} 
    12381238\caption{ Discretisation of the horizontal difference and average of tracers in the $z$-partial step coordinate (\np{ln\_zps}=.true.) in the case $( e3w_k^{i+1} - e3w_k^i  )>0$. A linear interpolation is used to estimate $\widetilde{T}_k^{i+1}$, the tracer value at the depth of the shallower tracer point of the two adjacent bottom $T$-points. The horizontal difference is then given by: $\delta _{i+1/2} T_k=  \widetilde{T}_k^{\,i+1} -T_k^{\,i}$ and the average by: $\overline{T}_k^{\,i+1/2}= ( \widetilde{T}_k^{\,i+1/2} - T_k^{\,i} ) / 2$.  } 
    12391239\end{center}   \end{figure} 
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