--- manual/s_algorithm/text/tracer.tex	2001/11/13 19:01:42	1.11
+++ manual/s_algorithm/text/tracer.tex	2004/04/20 23:32:59	1.16
@@ -1,8 +1,8 @@
-% $Header: /home/ubuntu/mnt/e9_copy/manual/s_algorithm/text/tracer.tex,v 1.11 2001/11/13 19:01:42 adcroft Exp $
+% $Header: /home/ubuntu/mnt/e9_copy/manual/s_algorithm/text/tracer.tex,v 1.16 2004/04/20 23:32:59 edhill Exp $
 % $Name:  $
 
 \section{Tracer equations}
-\label{sec:tracer_equations}
+\label{sect:tracer_equations}
 
 The basic discretization used for the tracer equations is the second
 order piece-wise constant finite volume form of the forced
@@ -15,7 +15,7 @@
 described here.
 
 \subsection{Time-stepping of tracers: ABII}
-\label{sec:tracer_equations_abII}
+\label{sect:tracer_equations_abII}
 
 The default advection scheme is the centered second order method which
 requires a second order or quasi-second order time-stepping scheme to
@@ -123,6 +123,10 @@
 
 
 \section{Linear advection schemes}
+\label{sect:tracer-advection}
+\begin{rawhtml}
+<!-- CMIREDIR:linear_advection_schemes: -->
+\end{rawhtml}
 
 \begin{figure}
 \resizebox{5.5in}{!}{\includegraphics{part2/advect-1d-lo.eps}}
@@ -349,6 +353,9 @@
 
 
 \section{Non-linear advection schemes}
+\begin{rawhtml}
+<!-- CMIREDIR:non-linear_advection_schemes: -->
+\end{rawhtml}
 
 Non-linear advection schemes invoke non-linear interpolation and are
 widely used in computational fluid dynamics (non-linear does not refer
@@ -449,7 +456,7 @@
 
 The DST3 method described above must be used in a forward-in-time
 manner and is stable for $0 \le |c| \le 1$. Although the scheme
-appears to be forward-in-time, it is in fact second order in time and
+appears to be forward-in-time, it is in fact third order in time and
 the accuracy increases with the Courant number! For low Courant
 number, DST3 produces very similar results (indistinguishable in
 Fig.~\ref{fig:advect-1d-lo}) to the linear third order method but for