--- manual/s_overview/text/manual_fromjm.tex	2001/10/11 19:36:57	1.2
+++ manual/s_overview/text/manual_fromjm.tex	2006/04/05 02:27:32	1.4
@@ -1,4 +1,4 @@
-% $Header: /home/ubuntu/mnt/e9_copy/manual/s_overview/text/manual_fromjm.tex,v 1.2 2001/10/11 19:36:57 adcroft Exp $
+% $Header: /home/ubuntu/mnt/e9_copy/manual/s_overview/text/manual_fromjm.tex,v 1.4 2006/04/05 02:27:32 edhill Exp $
 % $Name:  $
 
 \documentclass[12pt]{book}
@@ -32,11 +32,9 @@
 \tableofcontents
 
 
-\part{MIT GCM basics}
-
 % Section: Overview
 
-% $Header: /home/ubuntu/mnt/e9_copy/manual/s_overview/text/manual_fromjm.tex,v 1.2 2001/10/11 19:36:57 adcroft Exp $
+% $Header: /home/ubuntu/mnt/e9_copy/manual/s_overview/text/manual_fromjm.tex,v 1.4 2006/04/05 02:27:32 edhill Exp $
 % $Name:  $
 
 \section{Introduction}
@@ -96,14 +94,13 @@
 
 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.
-\pagebreak
 
-% $Header: /home/ubuntu/mnt/e9_copy/manual/s_overview/text/manual_fromjm.tex,v 1.2 2001/10/11 19:36:57 adcroft Exp $
+% $Header: /home/ubuntu/mnt/e9_copy/manual/s_overview/text/manual_fromjm.tex,v 1.4 2006/04/05 02:27:32 edhill Exp $
 % $Name:  $
 
 \section{Illustrations of the model in action}
 
-The MITgcm has been designed and used to model a wide range of phenomena,
+MITgcm has been designed and used to model a wide range of phenomena,
 from convection on the scale of meters in the ocean to the global pattern of
 atmospheric winds - see fig.2\ref{fig:all-scales}. To give a flavor of the
 kinds of problems the model has been used to study, we briefly describe some
@@ -289,7 +286,7 @@
 %notci%\input{part1/lab_figure}
 %%CNHend
 
-% $Header: /home/ubuntu/mnt/e9_copy/manual/s_overview/text/manual_fromjm.tex,v 1.2 2001/10/11 19:36:57 adcroft Exp $
+% $Header: /home/ubuntu/mnt/e9_copy/manual/s_overview/text/manual_fromjm.tex,v 1.4 2006/04/05 02:27:32 edhill Exp $
 % $Name:  $
 
 \section{Continuous equations in `r' coordinates}
@@ -677,7 +674,7 @@
 which the vertical momentum equation is reduced to a statement of
 hydrostatic balance and the `traditional approximation' is made in which the
 Coriolis force is treated approximately and the shallow atmosphere
-approximation is made.\ The MITgcm need not make the `traditional
+approximation is made.  MITgcm need not make the `traditional
 approximation'. To be able to support consistent non-hydrostatic forms the
 shallow atmosphere approximation can be relaxed - when dividing through by $
 r $ in, for example, (\ref{eq:gu-speherical}), we do not replace $r$ by $a$,
@@ -1024,7 +1021,7 @@
 Tangent linear and adjoint counterparts of the forward model and described
 in Chapter 5.
 
-% $Header: /home/ubuntu/mnt/e9_copy/manual/s_overview/text/manual_fromjm.tex,v 1.2 2001/10/11 19:36:57 adcroft Exp $
+% $Header: /home/ubuntu/mnt/e9_copy/manual/s_overview/text/manual_fromjm.tex,v 1.4 2006/04/05 02:27:32 edhill Exp $
 % $Name:  $
 
 \section{Appendix ATMOSPHERE}
@@ -1151,7 +1148,7 @@
 \frac{D\theta }{Dt} &=&\frac{\mathcal{Q}}{\Pi }  \label{eq:atmos-prime}
 \end{eqnarray}
 
-% $Header: /home/ubuntu/mnt/e9_copy/manual/s_overview/text/manual_fromjm.tex,v 1.2 2001/10/11 19:36:57 adcroft Exp $
+% $Header: /home/ubuntu/mnt/e9_copy/manual/s_overview/text/manual_fromjm.tex,v 1.4 2006/04/05 02:27:32 edhill Exp $
 % $Name:  $
 
 \section{Appendix OCEAN}
@@ -1367,7 +1364,7 @@
 _{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_fromjm.tex,v 1.2 2001/10/11 19:36:57 adcroft Exp $
+% $Header: /home/ubuntu/mnt/e9_copy/manual/s_overview/text/manual_fromjm.tex,v 1.4 2006/04/05 02:27:32 edhill Exp $
 % $Name:  $
 
 \section{Appendix:OPERATORS}
