--- manual/s_overview/text/manual.tex	2001/11/19 14:33:44	1.12
+++ manual/s_overview/text/manual.tex	2002/02/28 19:32:19	1.16
@@ -1,4 +1,4 @@
-% $Header: /home/ubuntu/mnt/e9_copy/manual/s_overview/text/manual.tex,v 1.12 2001/11/19 14:33:44 cnh Exp $
+% $Header: /home/ubuntu/mnt/e9_copy/manual/s_overview/text/manual.tex,v 1.16 2002/02/28 19:32:19 cnh Exp $
 % $Name:  $
 
 %tci%\documentclass[12pt]{book}
@@ -34,12 +34,10 @@
 
 % Section: Overview
 
-% $Header: /home/ubuntu/mnt/e9_copy/manual/s_overview/text/manual.tex,v 1.12 2001/11/19 14:33:44 cnh Exp $
+% $Header: /home/ubuntu/mnt/e9_copy/manual/s_overview/text/manual.tex,v 1.16 2002/02/28 19:32:19 cnh Exp $
 % $Name:  $
 
-\section{Introduction}
-
-This documentation provides the reader with the information necessary to
+This document provides the reader with the information necessary to
 carry out numerical experiments using MITgcm. It gives a comprehensive
 description of the continuous equations on which the model is based, the
 numerical algorithms the model employs and a description of the associated
@@ -49,6 +47,8 @@
 both process and general circulation studies of the atmosphere and ocean are
 also presented.
 
+\section{Introduction}
+
 MITgcm has a number of novel aspects:
 
 \begin{itemize}
@@ -83,10 +83,10 @@
 computational platforms.
 \end{itemize}
 
-Key publications reporting on and charting the development of the model are:
+Key publications reporting on and charting the development of the model are
+\cite{hill:95,marshall:97a,marshall:97b,adcroft:97,marshall:98,adcroft:99,hill:99,maro-eta:99}:
 
 \begin{verbatim}
-
 Hill, C. and J. Marshall, (1995)
 Application of a Parallel Navier-Stokes Model to Ocean Circulation in 
 Parallel Computational Fluid Dynamics
@@ -95,7 +95,7 @@
 Elsevier Science B.V.: New York
 
 Marshall, J., C. Hill, L. Perelman, and A. Adcroft, (1997)
-Hydrostatic, quasi-hydrostatic, and nonhydrostatic ocean modeling,
+Hydrostatic, quasi-hydrostatic, and nonhydrostatic ocean modeling
 J. Geophysical Res., 102(C3), 5733-5752.
 
 Marshall, J., A. Adcroft, C. Hill, L. Perelman, and C. Heisey, (1997)
@@ -119,21 +119,21 @@
 
 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 
 application to Atlantic heat transport variability
 J. Geophysical Res., 104(C12), 29,529-29,547.
 
-
 \end{verbatim}
 
 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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 \section{Illustrations of the model in action}
@@ -294,13 +294,14 @@
 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 +334,7 @@
 \input{part1/lab_figure}
 %%CNHend
 
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 \section{Continuous equations in `r' coordinates}
@@ -1072,7 +1073,7 @@
 Tangent linear and adjoint counterparts of the forward model are described
 in Chapter 5.
 
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 \section{Appendix ATMOSPHERE}
@@ -1199,7 +1200,7 @@
 \frac{D\theta }{Dt} &=&\frac{\mathcal{Q}}{\Pi } 
 \end{eqnarray}
 
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 % $Name:  $
 
 \section{Appendix OCEAN}
@@ -1415,7 +1416,7 @@
 _{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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+% $Header: /home/ubuntu/mnt/e9_copy/manual/s_overview/text/manual.tex,v 1.16 2002/02/28 19:32:19 cnh Exp $
 % $Name:  $
 
 \section{Appendix:OPERATORS}
