/[MITgcm]/manual/s_examples/baroclinic_gyre/fourlayer.tex
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revision 1.21 by molod, Tue Jun 27 19:08:22 2006 UTC revision 1.26 by jmc, Tue Jan 27 16:26:43 2009 UTC
# Line 7  Line 7 
7  \begin{rawhtml}  \begin{rawhtml}
8  <!-- CMIREDIR:eg-fourlayer: -->  <!-- CMIREDIR:eg-fourlayer: -->
9  \end{rawhtml}  \end{rawhtml}
10    \begin{center}
11    (in directory: {\it verification/tutorial\_baroclinic\_gyre/})
12    \end{center}
13    
14  \bodytext{bgcolor="#FFFFFFFF"}  \bodytext{bgcolor="#FFFFFFFF"}
15    
# Line 352  stability limit of 0.25. Line 355  stability limit of 0.25.
355  \label{SEC:eg_fourl_code_config}  \label{SEC:eg_fourl_code_config}
356    
357  The model configuration for this experiment resides under the  The model configuration for this experiment resides under the
358  directory {\it verification/exp2/}.  The experiment files  directory {\it verification/tutorial\_barotropic\_gyre/}.
359    The experiment files
360  \begin{itemize}  \begin{itemize}
361  \item {\it input/data}  \item {\it input/data}
362  \item {\it input/data.pkg}  \item {\it input/data.pkg}
# Line 417  viscAh=4.E2, Line 421  viscAh=4.E2,
421    coefficient to $1 \times 10^{-2} {\rm m^{2}s^{-1}}$. Boundary    coefficient to $1 \times 10^{-2} {\rm m^{2}s^{-1}}$. Boundary
422    conditions for this operator are specified later.  The variable    conditions for this operator are specified later.  The variable
423    \varlink{viscAh}{viscAh} is read in the routine    \varlink{viscAh}{viscAh} is read in the routine
424    \varlink{INI\_PARMS}{INI_PARMS} and applied in routines    \varlink{INI\_PARMS}{INI_PARMS} and applied in routine
425    \varlink{CALC\_MOM\_RHS}{CALC_MOM_RHS} and    \varlink{MOM\_FLUXFORM}{MOM_FLUXFORM}.
   \varlink{CALC\_GW}{CALC_GW}.  
426    
427  \fbox{  \fbox{
428    \begin{minipage}{5.0in}    \begin{minipage}{5.0in}
429      {\it S/R CALC\_MOM\_RHS}({\it calc\_mom\_rhs.F})      {\it S/R MOM\_FLUXFORM}({\it mom\_fluxform.F})
   \end{minipage}  
 }  
 \fbox{  
   \begin{minipage}{5.0in}  
     {\it S/R CALC\_GW}({\it calc\_gw.F})  
430    \end{minipage}    \end{minipage}
431  }  }
432    
# Line 446  no_slip_sides=.FALSE. Line 444  no_slip_sides=.FALSE.
444    
445    \fbox{    \fbox{
446      \begin{minipage}{5.0in}      \begin{minipage}{5.0in}
447        {\it S/R CALC\_MOM\_RHS}({\it calc\_mom\_rhs.F})        {\it S/R MOM\_FLUXFORM}({\it mom\_fluxform.F})
448      \end{minipage}      \end{minipage}
449    }    }
450    \filelink{calc\_mom\_rhs.F}{calc_mom_rhs.F}    \filelink{mom\_fluxform.F}{pkg-mom_fluxform-mom_fluxform.F}
451        
452  \item Lines 9,  \item Lines 9,
453  \begin{verbatim}  \begin{verbatim}
# Line 460  no_slip_bottom=.TRUE. Line 458  no_slip_bottom=.TRUE.
458    at $z=-H$, where $H$ is the local depth of the domain.  The variable    at $z=-H$, where $H$ is the local depth of the domain.  The variable
459    \varlink{no\_slip\_bottom}{no\_slip\_bottom} is read in the routine    \varlink{no\_slip\_bottom}{no\_slip\_bottom} is read in the routine
460    \filelink{INI\_PARMS}{model-src-ini_parms.F} and is applied in the    \filelink{INI\_PARMS}{model-src-ini_parms.F} and is applied in the
461    routine \varlink{CALC\_MOM\_RHS}{CALC_MOM_RHS}.    routine \varlink{MOM\_FLUXFORM}{MOM_FLUXFORM}.
462    
463    \fbox{    \fbox{
464      \begin{minipage}{5.0in}      \begin{minipage}{5.0in}
465        {\it S/R CALC\_MOM\_RHS}({\it calc\_mom\_rhs.F})        {\it S/R MOM\_FLUXFORM}({\it mom\_fluxform.F})
466      \end{minipage}      \end{minipage}
467    }    }
468    \filelink{calc\_mom\_rhs.F}{calc_mom_rhs.F}    \filelink{mom\_fluxform.F}{pkg-mom_fluxform-mom_fluxform.F}
469    
470  \item Line 10,  \item Line 10,
471  \begin{verbatim}  \begin{verbatim}
# Line 561  usingSphericalPolarGrid=.TRUE., Line 559  usingSphericalPolarGrid=.TRUE.,
559    
560  \item Line 41,  \item Line 41,
561  \begin{verbatim}  \begin{verbatim}
562  phiMin=0.,  ygOrigin=0.,
563  \end{verbatim}  \end{verbatim}
564    This line sets the southern boundary of the modeled domain to    This line sets the southern boundary of the modeled domain to
565    $0^{\circ}$ latitude. This value affects both the generation of the    $0^{\circ}$ latitude. This value affects both the generation of the
# Line 569  phiMin=0., Line 567  phiMin=0.,
567    the initialization of the coriolis force.  Note - it is not required    the initialization of the coriolis force.  Note - it is not required
568    to set a longitude boundary, since the absolute longitude does not    to set a longitude boundary, since the absolute longitude does not
569    alter the kernel equation discretisation.  The variable    alter the kernel equation discretisation.  The variable
570    \varlink{phiMin}{phiMin} is read in the    \varlink{ygOrigin}{ygOrigin} is read in the
571    routine \varlink{INI\_PARMS}{INI_PARMS} and is used in routine    routine \varlink{INI\_PARMS}{INI_PARMS} and is used in routine
572    
573    \fbox{    \fbox{
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