--- manual/s_overview/text/manual_fromjm.tex 2001/10/15 19:34:28 1.3 +++ manual/s_overview/text/manual_fromjm.tex 2006/04/05 02:27:32 1.4 @@ -1,4 +1,4 @@ -% $Header: /home/ubuntu/mnt/e9_copy/manual/s_overview/text/manual_fromjm.tex,v 1.3 2001/10/15 19:34:28 adcroft Exp $ +% $Header: /home/ubuntu/mnt/e9_copy/manual/s_overview/text/manual_fromjm.tex,v 1.4 2006/04/05 02:27:32 edhill Exp $ % $Name: $ \documentclass[12pt]{book} @@ -34,7 +34,7 @@ % Section: Overview -% $Header: /home/ubuntu/mnt/e9_copy/manual/s_overview/text/manual_fromjm.tex,v 1.3 2001/10/15 19:34:28 adcroft Exp $ +% $Header: /home/ubuntu/mnt/e9_copy/manual/s_overview/text/manual_fromjm.tex,v 1.4 2006/04/05 02:27:32 edhill Exp $ % $Name: $ \section{Introduction} @@ -95,12 +95,12 @@ 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_fromjm.tex,v 1.3 2001/10/15 19:34:28 adcroft Exp $ +% $Header: /home/ubuntu/mnt/e9_copy/manual/s_overview/text/manual_fromjm.tex,v 1.4 2006/04/05 02:27:32 edhill Exp $ % $Name: $ \section{Illustrations of the model in action} -The MITgcm has been designed and used to model a wide range of phenomena, +MITgcm has been designed and used to model a wide range of phenomena, from convection on the scale of meters in the ocean to the global pattern of atmospheric winds - see fig.2\ref{fig:all-scales}. To give a flavor of the kinds of problems the model has been used to study, we briefly describe some @@ -286,7 +286,7 @@ %notci%\input{part1/lab_figure} %%CNHend -% $Header: /home/ubuntu/mnt/e9_copy/manual/s_overview/text/manual_fromjm.tex,v 1.3 2001/10/15 19:34:28 adcroft Exp $ +% $Header: /home/ubuntu/mnt/e9_copy/manual/s_overview/text/manual_fromjm.tex,v 1.4 2006/04/05 02:27:32 edhill Exp $ % $Name: $ \section{Continuous equations in `r' coordinates} @@ -674,7 +674,7 @@ which the vertical momentum equation is reduced to a statement of hydrostatic balance and the `traditional approximation' is made in which the Coriolis force is treated approximately and the shallow atmosphere -approximation is made.\ The MITgcm need not make the `traditional +approximation is made. MITgcm need not make the `traditional approximation'. To be able to support consistent non-hydrostatic forms the shallow atmosphere approximation can be relaxed - when dividing through by $ r $ in, for example, (\ref{eq:gu-speherical}), we do not replace $r$ by $a$, @@ -1021,7 +1021,7 @@ Tangent linear and adjoint counterparts of the forward model and described in Chapter 5. -% $Header: /home/ubuntu/mnt/e9_copy/manual/s_overview/text/manual_fromjm.tex,v 1.3 2001/10/15 19:34:28 adcroft Exp $ +% $Header: /home/ubuntu/mnt/e9_copy/manual/s_overview/text/manual_fromjm.tex,v 1.4 2006/04/05 02:27:32 edhill Exp $ % $Name: $ \section{Appendix ATMOSPHERE} @@ -1148,7 +1148,7 @@ \frac{D\theta }{Dt} &=&\frac{\mathcal{Q}}{\Pi } \label{eq:atmos-prime} \end{eqnarray} -% $Header: /home/ubuntu/mnt/e9_copy/manual/s_overview/text/manual_fromjm.tex,v 1.3 2001/10/15 19:34:28 adcroft Exp $ +% $Header: /home/ubuntu/mnt/e9_copy/manual/s_overview/text/manual_fromjm.tex,v 1.4 2006/04/05 02:27:32 edhill Exp $ % $Name: $ \section{Appendix OCEAN} @@ -1364,7 +1364,7 @@ _{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_fromjm.tex,v 1.3 2001/10/15 19:34:28 adcroft Exp $ +% $Header: /home/ubuntu/mnt/e9_copy/manual/s_overview/text/manual_fromjm.tex,v 1.4 2006/04/05 02:27:32 edhill Exp $ % $Name: $ \section{Appendix:OPERATORS}