--- manual/s_overview/text/manual.tex	2002/02/28 19:32:19	1.16
+++ manual/s_overview/text/manual.tex	2003/08/07 18:27:51	1.17
@@ -1,4 +1,4 @@
-% $Header: /home/ubuntu/mnt/e9_copy/manual/s_overview/text/manual.tex,v 1.16 2002/02/28 19:32:19 cnh Exp $
+% $Header: /home/ubuntu/mnt/e9_copy/manual/s_overview/text/manual.tex,v 1.17 2003/08/07 18:27:51 edhill 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 1.16 2002/02/28 19:32:19 cnh Exp $
+% $Header: /home/ubuntu/mnt/e9_copy/manual/s_overview/text/manual.tex,v 1.17 2003/08/07 18:27:51 edhill Exp $
 % $Name:  $
 
 This document provides the reader with the information necessary to
@@ -133,7 +133,7 @@
 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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+% $Header: /home/ubuntu/mnt/e9_copy/manual/s_overview/text/manual.tex,v 1.17 2003/08/07 18:27:51 edhill Exp $
 % $Name:  $
 
 \section{Illustrations of the model in action}
@@ -322,7 +322,7 @@
 \subsection{Simulations of laboratory experiments}
 
 Figure \ref{fig:lab-simulation} shows MITgcm being used to simulate a 
-laboratory experiment inquiring in to the dynamics of the Antarctic Circumpolar Current (ACC). An
+laboratory experiment inquiring into the dynamics of the Antarctic Circumpolar Current (ACC). An
 initially homogeneous tank of water ($1m$ in diameter) is driven from its
 free surface by a rotating heated disk. The combined action of mechanical
 and thermal forcing creates a lens of fluid which becomes baroclinically
@@ -334,7 +334,7 @@
 \input{part1/lab_figure}
 %%CNHend
 
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+% $Header: /home/ubuntu/mnt/e9_copy/manual/s_overview/text/manual.tex,v 1.17 2003/08/07 18:27:51 edhill Exp $
 % $Name:  $
 
 \section{Continuous equations in `r' coordinates}
@@ -346,8 +346,8 @@
 and encoded. The model variables have different interpretations depending on
 whether the atmosphere or ocean is being studied. Thus, for example, the
 vertical coordinate `$r$' is interpreted as pressure, $p$, if we are
-modeling the atmosphere (left hand side of figure \ref{fig:isomorphic-equations})
-and height, $z$, if we are modeling the ocean (right hand side of figure
+modeling the atmosphere (right hand side of figure \ref{fig:isomorphic-equations})
+and height, $z$, if we are modeling the ocean (left hand side of figure
 \ref{fig:isomorphic-equations}).
 
 %%CNHbegin
@@ -471,12 +471,12 @@
 at fixed and moving $r$ surfaces we set (see figure \ref{fig:zandp-vert-coord}):
 
 \begin{equation}
-\dot{r}=0atr=R_{fixed}(x,y)\text{ (ocean bottom, top of the atmosphere)}
+\dot{r}=0 \text{\ at\ } r=R_{fixed}(x,y)\text{ (ocean bottom, top of the atmosphere)}
 \label{eq:fixedbc}
 \end{equation}
 
 \begin{equation}
-\dot{r}=\frac{Dr}{Dt}atr=R_{moving}\text{ \
+\dot{r}=\frac{Dr}{Dt} \text{\ at\ } r=R_{moving}\text{ \
 (ocean surface,bottom of the atmosphere)}  \label{eq:movingbc}
 \end{equation}
 
@@ -1073,7 +1073,7 @@
 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 1.17 2003/08/07 18:27:51 edhill Exp $
 % $Name:  $
 
 \section{Appendix ATMOSPHERE}
@@ -1200,7 +1200,7 @@
 \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 1.17 2003/08/07 18:27:51 edhill Exp $
 % $Name:  $
 
 \section{Appendix OCEAN}
@@ -1416,7 +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 1.17 2003/08/07 18:27:51 edhill Exp $
 % $Name:  $
 
 \section{Appendix:OPERATORS}