/[MITgcm]/manual/s_examples/global_oce_latlon/climatalogical_ogcm.tex
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revision 1.13 by edhill, Sat Apr 8 01:50:50 2006 UTC revision 1.16 by jmc, Tue Jan 15 20:04:06 2008 UTC
# Line 7  Line 7 
7  \begin{rawhtml}  \begin{rawhtml}
8  <!-- CMIREDIR:eg-global: -->  <!-- CMIREDIR:eg-global: -->
9  \end{rawhtml}  \end{rawhtml}
10    \begin{center}
11    (in directory: {\it verification/tutorial\_global\_oce\_latlon/})
12    \end{center}
13    
14  \bodytext{bgcolor="#FFFFFFFF"}  \bodytext{bgcolor="#FFFFFFFF"}
15    
# Line 25  This example experiment demonstrates usi Line 28  This example experiment demonstrates usi
28  the planetary ocean circulation. The simulation is configured  the planetary ocean circulation. The simulation is configured
29  with realistic geography and bathymetry on a  with realistic geography and bathymetry on a
30  $4^{\circ} \times 4^{\circ}$ spherical polar grid.  $4^{\circ} \times 4^{\circ}$ spherical polar grid.
31    The files for this experiment are in the verification directory
32    under tutorial\_global\_oce\_latlon.
33  Twenty levels are used in the vertical, ranging in thickness  Twenty levels are used in the vertical, ranging in thickness
34  from $50\,{\rm m}$ at the surface to $815\,{\rm m}$ at depth,  from $50\,{\rm m}$ at the surface to $815\,{\rm m}$ at depth,
35  giving a maximum model depth of $6\,{\rm km}$.  giving a maximum model depth of $6\,{\rm km}$.
# Line 578  See section \ref{SEC:cd_scheme}. Line 583  See section \ref{SEC:cd_scheme}.
583  \fbox{  \fbox{
584  \begin{minipage}{5.0in}  \begin{minipage}{5.0in}
585  {\it S/R INI\_PARMS}({\it ini\_parms.F})\\  {\it S/R INI\_PARMS}({\it ini\_parms.F})\\
586  {\it S/R CALC\_MOM\_RHS}({\it calc\_mom\_rhs.F})  {\it S/R MOM\_FLUXFORM}({\it mom\_fluxform.F})
587  \end{minipage}  \end{minipage}
588  }  }
589    
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