--- manual/s_overview/text/manual.tex 2001/11/19 14:33:44 1.12 +++ manual/s_overview/text/manual.tex 2001/11/21 14:13:17 1.14 @@ -1,4 +1,4 @@ -% $Header: /home/ubuntu/mnt/e9_copy/manual/s_overview/text/manual.tex,v 1.12 2001/11/19 14:33:44 cnh Exp $ +% $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 -% $Header: /home/ubuntu/mnt/e9_copy/manual/s_overview/text/manual.tex,v 1.12 2001/11/19 14:33:44 cnh Exp $ +% $Header: /home/ubuntu/mnt/e9_copy/manual/s_overview/text/manual.tex,v 1.14 2001/11/21 14:13:17 cnh Exp $ % $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. -% $Header: /home/ubuntu/mnt/e9_copy/manual/s_overview/text/manual.tex,v 1.12 2001/11/19 14:33:44 cnh Exp $ +% $Header: /home/ubuntu/mnt/e9_copy/manual/s_overview/text/manual.tex,v 1.14 2001/11/21 14:13:17 cnh Exp $ % $Name: $ \section{Illustrations of the model in action} @@ -300,7 +301,7 @@ 1992-1997. {\bf CHANGE THIS TEXT - FIG FROM PATRICK/CARL/DETLEF} %% CNHbegin -\input{part1/globes_figure} +\input{part1/assim_figure} %% CNHend \subsection{Ocean biogeochemical cycles} @@ -333,7 +334,7 @@ \input{part1/lab_figure} %%CNHend -% $Header: /home/ubuntu/mnt/e9_copy/manual/s_overview/text/manual.tex,v 1.12 2001/11/19 14:33:44 cnh Exp $ +% $Header: /home/ubuntu/mnt/e9_copy/manual/s_overview/text/manual.tex,v 1.14 2001/11/21 14:13:17 cnh Exp $ % $Name: $ \section{Continuous equations in `r' coordinates} @@ -1072,7 +1073,7 @@ 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 1.12 2001/11/19 14:33:44 cnh Exp $ +% $Header: /home/ubuntu/mnt/e9_copy/manual/s_overview/text/manual.tex,v 1.14 2001/11/21 14:13:17 cnh Exp $ % $Name: $ \section{Appendix ATMOSPHERE} @@ -1199,7 +1200,7 @@ \frac{D\theta }{Dt} &=&\frac{\mathcal{Q}}{\Pi } \end{eqnarray} -% $Header: /home/ubuntu/mnt/e9_copy/manual/s_overview/text/manual.tex,v 1.12 2001/11/19 14:33:44 cnh Exp $ +% $Header: /home/ubuntu/mnt/e9_copy/manual/s_overview/text/manual.tex,v 1.14 2001/11/21 14:13:17 cnh Exp $ % $Name: $ \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). -% $Header: /home/ubuntu/mnt/e9_copy/manual/s_overview/text/manual.tex,v 1.12 2001/11/19 14:33:44 cnh Exp $ +% $Header: /home/ubuntu/mnt/e9_copy/manual/s_overview/text/manual.tex,v 1.14 2001/11/21 14:13:17 cnh Exp $ % $Name: $ \section{Appendix:OPERATORS}