--- manual/s_overview/text/manual.tex	2001/11/19 14:33:44	1.12
+++ manual/s_overview/text/manual.tex	2001/11/21 16:33:17	1.15
@@ -1,4 +1,4 @@
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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:  $
 
 %tci%\documentclass[12pt]{book}
@@ -34,7 +34,7 @@
 
 % Section: Overview
 
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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{Introduction}
@@ -119,8 +119,9 @@
 
 Hill, C, Adcroft,A., Jamous,D., and J. Marshall, (1999)
 A Strategy for Terascale Climate Modeling.
-In Proceedings of the Eight ECMWF Workshop on the Use of Parallel Processors
-in Meteorology
+In Proceedings of the Eighth ECMWF Workshop on the Use of Parallel Processors
+in Meteorology, pages 406-425
+World Scientific Publishing Co: UK
 
 Marotzke, J, Giering,R., Zhang, K.Q., Stammer,D., Hill,C., and T.Lee, (1999)
 Construction of the adjoint MIT ocean general circulation model and 
@@ -133,7 +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.
 
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 % $Name:  $
 
 \section{Illustrations of the model in action}
@@ -294,13 +295,14 @@
 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/globes_figure}
+\input{part1/assim_figure}
 %% CNHend
 
 \subsection{Ocean biogeochemical cycles}
@@ -333,7 +335,7 @@
 \input{part1/lab_figure}
 %%CNHend
 
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 \section{Continuous equations in `r' coordinates}
@@ -1072,7 +1074,7 @@
 Tangent linear and adjoint counterparts of the forward model are described
 in Chapter 5.
 
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 \section{Appendix ATMOSPHERE}
@@ -1199,7 +1201,7 @@
 \frac{D\theta }{Dt} &=&\frac{\mathcal{Q}}{\Pi } 
 \end{eqnarray}
 
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 % $Name:  $
 
 \section{Appendix OCEAN}
@@ -1415,7 +1417,7 @@
 _{nh}=0$ form of these equations that are used throughout the ocean modeling
 community and referred to as the primitive equations (HPE).
 
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 % $Name:  $
 
 \section{Appendix:OPERATORS}