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--- manual/s_overview/text/manual.tex 2004/10/16 03:40:12 1.21
+++ manual/s_overview/text/manual.tex 2004/10/17 04:15:13 1.22
@@ -1,4 +1,4 @@
-% $Header: /home/ubuntu/mnt/e9_copy/manual/s_overview/text/manual.tex,v 1.21 2004/10/16 03:40:12 edhill Exp $
+% $Header: /home/ubuntu/mnt/e9_copy/manual/s_overview/text/manual.tex,v 1.22 2004/10/17 04:15:13 jmc 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 1.21 2004/10/16 03:40:12 edhill Exp $
+% $Header: /home/ubuntu/mnt/e9_copy/manual/s_overview/text/manual.tex,v 1.22 2004/10/17 04:15:13 jmc Exp $
% $Name: $
This document provides the reader with the information necessary to
@@ -137,7 +137,7 @@
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 1.21 2004/10/16 03:40:12 edhill Exp $
+% $Header: /home/ubuntu/mnt/e9_copy/manual/s_overview/text/manual.tex,v 1.22 2004/10/17 04:15:13 jmc Exp $
% $Name: $
\section{Illustrations of the model in action}
@@ -372,7 +372,7 @@
\input{part1/lab_figure}
%%CNHend
-% $Header: /home/ubuntu/mnt/e9_copy/manual/s_overview/text/manual.tex,v 1.21 2004/10/16 03:40:12 edhill Exp $
+% $Header: /home/ubuntu/mnt/e9_copy/manual/s_overview/text/manual.tex,v 1.22 2004/10/17 04:15:13 jmc Exp $
% $Name: $
\section{Continuous equations in `r' coordinates}
@@ -1123,7 +1123,7 @@
Tangent linear and adjoint counterparts of the forward model are described
in Chapter 5.
-% $Header: /home/ubuntu/mnt/e9_copy/manual/s_overview/text/manual.tex,v 1.21 2004/10/16 03:40:12 edhill Exp $
+% $Header: /home/ubuntu/mnt/e9_copy/manual/s_overview/text/manual.tex,v 1.22 2004/10/17 04:15:13 jmc Exp $
% $Name: $
\section{Appendix ATMOSPHERE}
@@ -1213,6 +1213,7 @@
surface ($\phi $ is imposed and $\omega \neq 0$).
\subsubsection{Splitting the geo-potential}
+\label{sec:hpe-p-geo-potential-split}
For the purposes of initialization and reducing round-off errors, the model
deals with perturbations from reference (or ``standard'') profiles. For
@@ -1251,7 +1252,7 @@
\frac{D\theta }{Dt} &=&\frac{\mathcal{Q}}{\Pi }
\end{eqnarray}
-% $Header: /home/ubuntu/mnt/e9_copy/manual/s_overview/text/manual.tex,v 1.21 2004/10/16 03:40:12 edhill Exp $
+% $Header: /home/ubuntu/mnt/e9_copy/manual/s_overview/text/manual.tex,v 1.22 2004/10/17 04:15:13 jmc Exp $
% $Name: $
\section{Appendix OCEAN}
@@ -1468,7 +1469,7 @@
_{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 1.21 2004/10/16 03:40:12 edhill Exp $
+% $Header: /home/ubuntu/mnt/e9_copy/manual/s_overview/text/manual.tex,v 1.22 2004/10/17 04:15:13 jmc Exp $
% $Name: $
\section{Appendix:OPERATORS}
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