/[MITgcm]/manual/s_examples/deep_convection/convection.tex
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revision 1.5 by edhill, Sat Oct 16 03:40:13 2004 UTC revision 1.7 by molod, Tue Jun 27 19:08:22 2006 UTC
# Line 29  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 287  are Line 289  are
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

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