--- manual/s_overview/text/manual.tex	2001/11/19 19:58:20	1.13
+++ manual/s_overview/text/manual.tex	2001/11/21 14:13:17	1.14
@@ -1,4 +1,4 @@
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+% $Header: /home/ubuntu/mnt/e9_copy/manual/s_overview/text/manual.tex,v 1.14 2001/11/21 14:13:17 cnh Exp $
 % $Name:  $
 
 %tci%\documentclass[12pt]{book}
@@ -34,7 +34,7 @@
 
 % Section: Overview
 
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 % $Name:  $
 
 \section{Introduction}
@@ -119,8 +119,9 @@
 
 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 
@@ -133,7 +134,7 @@
 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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 \section{Illustrations of the model in action}
@@ -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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 \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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 \section{Appendix:OPERATORS}
