--- manual/s_overview/introduction.tex	2001/08/08 16:16:16	1.1
+++ manual/s_overview/introduction.tex	2001/09/27 01:57:17	1.2
@@ -1,4 +1,4 @@
-% $Header: /home/ubuntu/mnt/e9_copy/manual/s_overview/Attic/introduction.tex,v 1.1 2001/08/08 16:16:16 adcroft Exp $
+% $Header: /home/ubuntu/mnt/e9_copy/manual/s_overview/Attic/introduction.tex,v 1.2 2001/09/27 01:57:17 cnh Exp $
 % $Name:  $
 
 \section{Introduction}
@@ -18,18 +18,18 @@
 \begin{itemize}
 \item  it can be used to study both atmospheric and oceanic phenomena; one
 hydrodynamical kernel is used to drive forward both atmospheric and oceanic
-models - see fig.1%
+models - see fig.1
 \marginpar{
 Fig.1 One model}\ref{fig:onemodel}
 
 \item  it has a non-hydrostatic capability and so can be used to study both
-small-scale and large scale processes - see fig.2%
+small-scale and large scale processes - see fig.2
 \marginpar{
 Fig.2 All scales}\ref{fig:all-scales}
 
 \item  finite volume techniques are employed yielding an intuitive
 discretization and support for the treatment of irregular geometries using
-orthogonal curvilinear grids and shaved cells - see fig.3%
+orthogonal curvilinear grids and shaved cells - see fig.3
 \marginpar{
 Fig.3 Finite volumes}\ref{fig:Finite volumes}
 
