--- manual/s_algorithm/text/spatial-discrete.tex	2004/10/13 18:50:54	1.16
+++ manual/s_algorithm/text/spatial-discrete.tex	2004/10/16 03:40:12	1.17
@@ -1,7 +1,10 @@
-% $Header: /home/ubuntu/mnt/e9_copy/manual/s_algorithm/text/spatial-discrete.tex,v 1.16 2004/10/13 18:50:54 jmc Exp $
+% $Header: /home/ubuntu/mnt/e9_copy/manual/s_algorithm/text/spatial-discrete.tex,v 1.17 2004/10/16 03:40:12 edhill Exp $
 % $Name:  $
 
 \section{Spatial discretization of the dynamical equations}
+\begin{rawhtml}
+<!-- CMIREDIR:spatial_discretization_of_dyn_eq: -->
+\end{rawhtml}
 
 Spatial discretization is carried out using the finite volume
 method. This amounts to a grid-point method (namely second-order
@@ -473,6 +476,10 @@
 
 
 \section{Continuity and horizontal pressure gradient terms}
+\begin{rawhtml}
+<!-- CMIREDIR:continuity_and_horizontal_pressure: -->
+\end{rawhtml}
+
 
 The core algorithm is based on the ``C grid'' discretization of the
 continuity equation which can be summarized as:
@@ -511,6 +518,9 @@
 evaporation and only enters the top-level of the {\em ocean} model.
 
 \section{Hydrostatic balance}
+\begin{rawhtml}
+<!-- CMIREDIR:hydrostatic_balance: -->
+\end{rawhtml}
 
 The vertical momentum equation has the hydrostatic or
 quasi-hydrostatic balance on the right hand side. This discretization