--- 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}