/[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 1.9 by jmc, Fri Aug 27 13:25:31 2010 UTC
# Line 4  Line 4 
4  \begin{rawhtml}  \begin{rawhtml}
5  <!-- CMIREDIR:eg-bconv: -->  <!-- CMIREDIR:eg-bconv: -->
6  \end{rawhtml}  \end{rawhtml}
7    \begin{center}
8    (in directory: {\it verification/tutorial\_deep\_convection/})
9    \end{center}
10    
11  \bodytext{bgcolor="#FFFFFFFF"}  \bodytext{bgcolor="#FFFFFFFF"}
12    
# Line 20  Line 23 
23  \begin{center}  \begin{center}
24   \resizebox{7.5cm}{5.5cm}{   \resizebox{7.5cm}{5.5cm}{
25     \includegraphics*[0.2in,0.7in][10.5in,10.5in]     \includegraphics*[0.2in,0.7in][10.5in,10.5in]
26     {part3/case_studies/doubly_periodic_convection/simulation_config.eps} }     {s_examples/deep_convection/simulation_config.eps} }
27  \end{center}  \end{center}
28  \caption{Schematic of simulation domain  \caption{Schematic of simulation domain
29  for the surface driven convection experiment. The domain is doubly periodic  for the surface driven convection experiment. The domain is doubly periodic
# Line 29  with an initially uniform temperature of Line 32  with an initially uniform temperature of
32  \label{FIG:eg-bconv-simulation_config}  \label{FIG:eg-bconv-simulation_config}
33  \end{figure}  \end{figure}
34    
35  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
36    capability, was designed to explore
37  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
38  period of oceanic deep convection. It is  period of oceanic deep convection. The files for this experiment can be found in the verification
39    directory under tutorial\_deep\_convection. It is
40    
41  \begin{itemize}  \begin{itemize}
42  \item non-hydrostatic  \item non-hydrostatic
# Line 85  rotation ($f_o = 10^{-4}$ s$^{-1}$) . Line 90  rotation ($f_o = 10^{-4}$ s$^{-1}$) .
90  \begin{center}  \begin{center}
91   \resizebox{15cm}{10cm}{   \resizebox{15cm}{10cm}{
92     \includegraphics*[0.2in,0.7in][10.5in,10.5in]     \includegraphics*[0.2in,0.7in][10.5in,10.5in]
93     {part3/case_studies/doubly_periodic_convection/verticalsection.ps} }     {s_examples/deep_convection/verticalsection.ps} }
94  \end{center}  \end{center}
95  \caption{  \caption{
96  }  }
# Line 99  rotation ($f_o = 10^{-4}$ s$^{-1}$) . Line 104  rotation ($f_o = 10^{-4}$ s$^{-1}$) .
104  \begin{center}  \begin{center}
105   \resizebox{10cm}{10cm}{   \resizebox{10cm}{10cm}{
106     \includegraphics*[0.2in,0.7in][10.5in,10.5in]     \includegraphics*[0.2in,0.7in][10.5in,10.5in]
107     {part3/case_studies/doubly_periodic_convection/surfacesection.ps} }     {s_examples/deep_convection/surfacesection.ps} }
108  \end{center}  \end{center}
109  \caption{  \caption{
110  }  }
# Line 268  the vertical domain extent in grid point Line 273  the vertical domain extent in grid point
273    
274  \begin{rawhtml}<PRE>\end{rawhtml}  \begin{rawhtml}<PRE>\end{rawhtml}
275  \begin{small}  \begin{small}
276  \input{part3/case_studies/doubly_periodic_convection/code/SIZE.h}  \input{s_examples/deep_convection/code/SIZE.h}
277  \end{small}  \end{small}
278  \begin{rawhtml}</PRE>\end{rawhtml}  \begin{rawhtml}</PRE>\end{rawhtml}
279    
# Line 287  are Line 292  are
292  \end{verbatim}  \end{verbatim}
293  this line sets  this line sets
294  the initial and reference values of potential temperature at each model  the initial and reference values of potential temperature at each model
295  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
296  flow evolves independently of the absolute magnitude of the reference temperature.  flow evolves independently of the absolute magnitude of the reference temperature.
297  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
298  $x$ and $y$. The values specified are read into the  $x$ and $y$. The values specified are read into the
# Line 785  S/R EXTERNAL\_FORCING\_SURF ({\it extern Line 790  S/R EXTERNAL\_FORCING\_SURF ({\it extern
790    
791  \begin{rawhtml}<PRE>\end{rawhtml}  \begin{rawhtml}<PRE>\end{rawhtml}
792  \begin{small}  \begin{small}
793  \input{part3/case_studies/doubly_periodic_convection/input/data}  \input{s_examples/deep_convection/input/data}
794  \end{small}  \end{small}
795  \begin{rawhtml}</PRE>\end{rawhtml}  \begin{rawhtml}</PRE>\end{rawhtml}
796    
# Line 819  directed upwards, according to the model Line 824  directed upwards, according to the model
824  \begin{center}  \begin{center}
825  % \resizebox{15cm}{10cm}{  % \resizebox{15cm}{10cm}{
826  %   \includegraphics*[0.2in,0.7in][10.5in,10.5in]  %   \includegraphics*[0.2in,0.7in][10.5in,10.5in]
827  %   {part3/case_studies/doubly_periodic_convection/Qsurf.ps} }  %   {s_examples/deep_convection/Qsurf.ps} }
828  \end{center}  \end{center}
829  \caption{  \caption{
830  }  }
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