--- manual/s_examples/deep_convection/convection.tex	2003/07/30 13:42:52	1.4
+++ manual/s_examples/deep_convection/convection.tex	2010/08/27 13:25:31	1.9
@@ -1,6 +1,12 @@
 \section{Surface Driven Convection}
 \label{www:tutorials}
 \label{sect:eg-bconv}
+\begin{rawhtml}
+<!-- CMIREDIR:eg-bconv: -->
+\end{rawhtml}
+\begin{center}
+(in directory: {\it verification/tutorial\_deep\_convection/})
+\end{center}
 
 \bodytext{bgcolor="#FFFFFFFF"}
 
@@ -17,7 +23,7 @@
 \begin{center}
  \resizebox{7.5cm}{5.5cm}{
    \includegraphics*[0.2in,0.7in][10.5in,10.5in]
-   {part3/case_studies/doubly_periodic_convection/simulation_config.eps} }
+   {s_examples/deep_convection/simulation_config.eps} }
 \end{center}
 \caption{Schematic of simulation domain 
 for the surface driven convection experiment. The domain is doubly periodic
@@ -26,9 +32,11 @@
 \label{FIG:eg-bconv-simulation_config}
 \end{figure}
 
-This experiment, figure \ref{FIG:eg-bconv-simulation_config}, showcasing MITgcm's non-hydrostatic capability, was designed to explore 
+This experiment, figure \ref{FIG:eg-bconv-simulation_config}, showcasing MITgcm's non-hydrostatic 
+capability, was designed to explore 
 the temporal and spatial characteristics of convection plumes as they might exist during a 
-period of oceanic deep convection. It is
+period of oceanic deep convection. The files for this experiment can be found in the verification
+directory under tutorial\_deep\_convection. It is
 
 \begin{itemize}
 \item non-hydrostatic 
@@ -82,7 +90,7 @@
 \begin{center}
  \resizebox{15cm}{10cm}{
    \includegraphics*[0.2in,0.7in][10.5in,10.5in]
-   {part3/case_studies/doubly_periodic_convection/verticalsection.ps} }
+   {s_examples/deep_convection/verticalsection.ps} }
 \end{center}
 \caption{
 }
@@ -96,7 +104,7 @@
 \begin{center}
  \resizebox{10cm}{10cm}{
    \includegraphics*[0.2in,0.7in][10.5in,10.5in]
-   {part3/case_studies/doubly_periodic_convection/surfacesection.ps} }
+   {s_examples/deep_convection/surfacesection.ps} }
 \end{center}
 \caption{
 }
@@ -265,7 +273,7 @@
 
 \begin{rawhtml}<PRE>\end{rawhtml}
 \begin{small}
-\input{part3/case_studies/doubly_periodic_convection/code/SIZE.h}
+\input{s_examples/deep_convection/code/SIZE.h}
 \end{small}
 \begin{rawhtml}</PRE>\end{rawhtml}
 
@@ -280,11 +288,11 @@
 
 \item Line 4, 
 \begin{verbatim}
-     4	 tRef=20*20.0,
+     4   tRef=20*20.0,
 \end{verbatim}
 this line sets
 the initial and reference values of potential temperature at each model
-level in units of $^{\circ}$C. Here the value is arbitrary since, in this case, the 
+level in units of $^{\circ}\mathrm{C}$. Here the value is arbitrary since, in this case, the 
 flow evolves independently of the absolute magnitude of the reference temperature.
 For each depth level the initial and reference profiles will be uniform in
 $x$ and $y$. The values specified are read into the
@@ -310,7 +318,7 @@
 
 \item Line 5,
 \begin{verbatim}
-     5	 sRef=20*35.0,
+     5   sRef=20*35.0,
 \end{verbatim}
 this line sets the initial and reference values of salinity at each model
 level in units of ppt. In this case salinity is set to an (arbitrary) uniform value of 
@@ -340,7 +348,7 @@
 
 \item Line 6,
 \begin{verbatim}
-     6	 viscAh=0.1,
+     6   viscAh=0.1,
 \end{verbatim}
 this line sets the horizontal laplacian dissipation coefficient to
 0.1 ${\rm m^{2}s^{-1}}$. Boundary conditions
@@ -371,7 +379,7 @@
 
 \item Line 7,
 \begin{verbatim}
-     7	 viscAz=0.1,
+     7   viscAz=0.1,
 \end{verbatim}
 this line sets the vertical laplacian frictional dissipation coefficient to
 0.1 ${\rm m^{2}s^{-1}}$. Boundary conditions
@@ -782,7 +790,7 @@
 
 \begin{rawhtml}<PRE>\end{rawhtml}
 \begin{small}
-\input{part3/case_studies/doubly_periodic_convection/input/data}
+\input{s_examples/deep_convection/input/data}
 \end{small}
 \begin{rawhtml}</PRE>\end{rawhtml}
 
@@ -816,7 +824,7 @@
 \begin{center}
 % \resizebox{15cm}{10cm}{
 %   \includegraphics*[0.2in,0.7in][10.5in,10.5in]
-%   {part3/case_studies/doubly_periodic_convection/Qsurf.ps} }
+%   {s_examples/deep_convection/Qsurf.ps} }
 \end{center}
 \caption{
 }