--- manual/s_overview/text/manual.tex	2001/11/21 14:13:17	1.14
+++ manual/s_overview/text/manual.tex	2001/11/21 16:33:17	1.15
@@ -1,4 +1,4 @@
-% $Header: /home/ubuntu/mnt/e9_copy/manual/s_overview/text/manual.tex,v 1.14 2001/11/21 14:13:17 cnh Exp $
+% $Header: /home/ubuntu/mnt/e9_copy/manual/s_overview/text/manual.tex,v 1.15 2001/11/21 16:33:17 cnh Exp $
 % $Name:  $
 
 %tci%\documentclass[12pt]{book}
@@ -34,7 +34,7 @@
 
 % Section: Overview
 
-% $Header: /home/ubuntu/mnt/e9_copy/manual/s_overview/text/manual.tex,v 1.14 2001/11/21 14:13:17 cnh Exp $
+% $Header: /home/ubuntu/mnt/e9_copy/manual/s_overview/text/manual.tex,v 1.15 2001/11/21 16:33:17 cnh Exp $
 % $Name:  $
 
 \section{Introduction}
@@ -134,7 +134,7 @@
 We begin by briefly showing some of the results of the model in action to
 give a feel for the wide range of problems that can be addressed using it.
 
-% $Header: /home/ubuntu/mnt/e9_copy/manual/s_overview/text/manual.tex,v 1.14 2001/11/21 14:13:17 cnh Exp $
+% $Header: /home/ubuntu/mnt/e9_copy/manual/s_overview/text/manual.tex,v 1.15 2001/11/21 16:33:17 cnh Exp $
 % $Name:  $
 
 \section{Illustrations of the model in action}
@@ -295,10 +295,11 @@
 the departure of the model from observations (both remotely sensed and
 in-situ) over an interval of time, is minimized by adjusting `control
 parameters' such as air-sea fluxes, the wind field, the initial conditions
-etc. Figure \ref{fig:assimilated-globes} shows an estimate of the time-mean
-surface elevation of the ocean obtained by bringing the model in to
+etc. Figure \ref{fig:assimilated-globes} shows the large scale planetary
+circulation and a Hopf-Muller plot of Equatorial sea-surface height.
+Both are obtained from assimilation bringing the model in to
 consistency with altimetric and in-situ observations over the period
-1992-1997. {\bf CHANGE THIS TEXT - FIG FROM PATRICK/CARL/DETLEF}
+1992-1997.
 
 %% CNHbegin
 \input{part1/assim_figure}
@@ -334,7 +335,7 @@
 \input{part1/lab_figure}
 %%CNHend
 
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+% $Header: /home/ubuntu/mnt/e9_copy/manual/s_overview/text/manual.tex,v 1.15 2001/11/21 16:33:17 cnh Exp $
 % $Name:  $
 
 \section{Continuous equations in `r' coordinates}
@@ -1073,7 +1074,7 @@
 Tangent linear and adjoint counterparts of the forward model are described
 in Chapter 5.
 
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+% $Header: /home/ubuntu/mnt/e9_copy/manual/s_overview/text/manual.tex,v 1.15 2001/11/21 16:33:17 cnh Exp $
 % $Name:  $
 
 \section{Appendix ATMOSPHERE}
@@ -1200,7 +1201,7 @@
 \frac{D\theta }{Dt} &=&\frac{\mathcal{Q}}{\Pi } 
 \end{eqnarray}
 
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+% $Header: /home/ubuntu/mnt/e9_copy/manual/s_overview/text/manual.tex,v 1.15 2001/11/21 16:33:17 cnh Exp $
 % $Name:  $
 
 \section{Appendix OCEAN}
@@ -1416,7 +1417,7 @@
 _{nh}=0$ form of these equations that are used throughout the ocean modeling
 community and referred to as the primitive equations (HPE).
 
-% $Header: /home/ubuntu/mnt/e9_copy/manual/s_overview/text/manual.tex,v 1.14 2001/11/21 14:13:17 cnh Exp $
+% $Header: /home/ubuntu/mnt/e9_copy/manual/s_overview/text/manual.tex,v 1.15 2001/11/21 16:33:17 cnh Exp $
 % $Name:  $
 
 \section{Appendix:OPERATORS}
