/[MITgcm]/manual/s_examples/deep_convection/convection.tex
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revision 1.4 by edhill, Wed Jul 30 13:42:52 2003 UTC revision 1.7 by molod, Tue Jun 27 19:08:22 2006 UTC
# Line 1  Line 1 
1  \section{Surface Driven Convection}  \section{Surface Driven Convection}
2  \label{www:tutorials}  \label{www:tutorials}
3  \label{sect:eg-bconv}  \label{sect:eg-bconv}
4    \begin{rawhtml}
5    <!-- CMIREDIR:eg-bconv: -->
6    \end{rawhtml}
7    
8  \bodytext{bgcolor="#FFFFFFFF"}  \bodytext{bgcolor="#FFFFFFFF"}
9    
# Line 26  with an initially uniform temperature of Line 29  with an initially uniform temperature of
29  \label{FIG:eg-bconv-simulation_config}  \label{FIG:eg-bconv-simulation_config}
30  \end{figure}  \end{figure}
31    
32  This experiment, figure \ref{FIG:eg-bconv-simulation_config}, showcasing MITgcm's non-hydrostatic capability, was designed to explore  This experiment, figure \ref{FIG:eg-bconv-simulation_config}, showcasing MITgcm's non-hydrostatic
33    capability, was designed to explore
34  the temporal and spatial characteristics of convection plumes as they might exist during a  the temporal and spatial characteristics of convection plumes as they might exist during a
35  period of oceanic deep convection. It is  period of oceanic deep convection. The files for this experiment can be found in the verification
36    directory under tutorial\_deep\_convection. It is
37    
38  \begin{itemize}  \begin{itemize}
39  \item non-hydrostatic  \item non-hydrostatic
# Line 280  are Line 285  are
285    
286  \item Line 4,  \item Line 4,
287  \begin{verbatim}  \begin{verbatim}
288       4   tRef=20*20.0,       4   tRef=20*20.0,
289  \end{verbatim}  \end{verbatim}
290  this line sets  this line sets
291  the initial and reference values of potential temperature at each model  the initial and reference values of potential temperature at each model
292  level in units of $^{\circ}$C. Here the value is arbitrary since, in this case, the  level in units of $^{\circ}\mathrm{C}$. Here the value is arbitrary since, in this case, the
293  flow evolves independently of the absolute magnitude of the reference temperature.  flow evolves independently of the absolute magnitude of the reference temperature.
294  For each depth level the initial and reference profiles will be uniform in  For each depth level the initial and reference profiles will be uniform in
295  $x$ and $y$. The values specified are read into the  $x$ and $y$. The values specified are read into the
# Line 310  S/R INI\_THETA ({\it ini\_theta.F}) Line 315  S/R INI\_THETA ({\it ini\_theta.F})
315    
316  \item Line 5,  \item Line 5,
317  \begin{verbatim}  \begin{verbatim}
318       5   sRef=20*35.0,       5   sRef=20*35.0,
319  \end{verbatim}  \end{verbatim}
320  this line sets the initial and reference values of salinity at each model  this line sets the initial and reference values of salinity at each model
321  level in units of ppt. In this case salinity is set to an (arbitrary) uniform value of  level in units of ppt. In this case salinity is set to an (arbitrary) uniform value of
# Line 340  S/R INI\_SALT ({\it ini\_salt.F}) Line 345  S/R INI\_SALT ({\it ini\_salt.F})
345    
346  \item Line 6,  \item Line 6,
347  \begin{verbatim}  \begin{verbatim}
348       6   viscAh=0.1,       6   viscAh=0.1,
349  \end{verbatim}  \end{verbatim}
350  this line sets the horizontal laplacian dissipation coefficient to  this line sets the horizontal laplacian dissipation coefficient to
351  0.1 ${\rm m^{2}s^{-1}}$. Boundary conditions  0.1 ${\rm m^{2}s^{-1}}$. Boundary conditions
# Line 371  S/R CALC\_GW ({\it calc\_gw.F}) Line 376  S/R CALC\_GW ({\it calc\_gw.F})
376    
377  \item Line 7,  \item Line 7,
378  \begin{verbatim}  \begin{verbatim}
379       7   viscAz=0.1,       7   viscAz=0.1,
380  \end{verbatim}  \end{verbatim}
381  this line sets the vertical laplacian frictional dissipation coefficient to  this line sets the vertical laplacian frictional dissipation coefficient to
382  0.1 ${\rm m^{2}s^{-1}}$. Boundary conditions  0.1 ${\rm m^{2}s^{-1}}$. Boundary conditions

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