--- manual/s_algorithm/text/spatial-discrete.tex	2004/10/13 18:50:54	1.16
+++ manual/s_algorithm/text/spatial-discrete.tex	2006/04/05 01:16:27	1.19
@@ -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 1.19 2006/04/05 01:16:27 jmc 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
@@ -147,8 +150,8 @@
 The model domain is decomposed into tiles and within each tile a
 quasi-regular grid is used. A tile is the basic unit of domain
 decomposition for parallelization but may be used whether parallelized
-or not; see section \ref{sect:tiles} for more details. Although the
-tiles may be patched together in an unstructured manner
+or not; see section \ref{sect:domain_decomposition} for more details. 
+Although the tiles may be patched together in an unstructured manner
 (i.e. irregular or non-tessilating pattern), the interior of tiles is
 a structured grid of quadrilateral cells. The horizontal coordinate
 system is orthogonal curvilinear meaning we can not necessarily treat
@@ -367,7 +370,7 @@
 The above grid (Fig.~\ref{fig:vgrid}a) is known as the cell centered
 approach because the tracer points are at cell centers; the cell
 centers are mid-way between the cell interfaces. 
-This discretisation is selected when the thickness of the
+This discretization is selected when the thickness of the
 levels are provided ({\bf delR}, parameter file {\em data}, 
 namelist {\em PARM04})
 An alternative, the vertex or interface centered approach, is shown in
@@ -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
