/[MITgcm]/manual/s_examples/deep_convection/convection.tex
ViewVC logotype

Diff of /manual/s_examples/deep_convection/convection.tex

Parent Directory Parent Directory | Revision Log Revision Log | View Revision Graph Revision Graph | View Patch Patch

revision 1.5 by edhill, Sat Oct 16 03:40:13 2004 UTC revision 1.8 by jmc, Tue Jan 15 18:11:50 2008 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 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 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

Legend:
Removed from v.1.5  
changed lines
  Added in v.1.8

  ViewVC Help
Powered by ViewVC 1.1.22