--- manual/s_examples/deep_convection/convection.tex	2004/10/16 03:40:13	1.5
+++ manual/s_examples/deep_convection/convection.tex	2008/01/15 18:11:50	1.8
@@ -4,6 +4,9 @@
 \begin{rawhtml}
 <!-- CMIREDIR:eg-bconv: -->
 \end{rawhtml}
+\begin{center}
+(in directory: {\it verification/tutorial\_deep\_convection/})
+\end{center}
 
 \bodytext{bgcolor="#FFFFFFFF"}
 
@@ -29,9 +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 
@@ -287,7 +292,7 @@
 \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