79 |
|
|
80 |
\end{enumerate} |
\end{enumerate} |
81 |
|
|
82 |
|
\subsection{Method 1 - Checkout from CVS} |
83 |
|
\label{sect:cvs_checkout} |
84 |
|
|
85 |
If CVS is available on your system, we strongly encourage you to use it. CVS |
If CVS is available on your system, we strongly encourage you to use it. CVS |
86 |
provides an efficient and elegant way of organizing your code and keeping |
provides an efficient and elegant way of organizing your code and keeping |
87 |
track of your changes. If CVS is not available on your machine, you can also |
track of your changes. If CVS is not available on your machine, you can also |
96 |
\begin{verbatim} |
\begin{verbatim} |
97 |
% export CVSROOT=':pserver:cvsanon@mitgcm.org:/u/gcmpack' |
% export CVSROOT=':pserver:cvsanon@mitgcm.org:/u/gcmpack' |
98 |
\end{verbatim} |
\end{verbatim} |
99 |
in your .profile or .bashrc file. |
in your \texttt{.profile} or \texttt{.bashrc} file. |
100 |
|
|
101 |
|
|
102 |
To get MITgcm through CVS, first register with the MITgcm CVS server |
To get MITgcm through CVS, first register with the MITgcm CVS server |
118 |
code and CVS. It also contains a web interface to our CVS archive so |
code and CVS. It also contains a web interface to our CVS archive so |
119 |
that one may easily view the state of files, revisions, and other |
that one may easily view the state of files, revisions, and other |
120 |
development milestones: |
development milestones: |
121 |
\begin{rawhtml} <A href=http://mitgcm.org/download target="idontexist"> \end{rawhtml} |
\begin{rawhtml} <A href=''http://mitgcm.org/download'' target="idontexist"> \end{rawhtml} |
122 |
\begin{verbatim} |
\begin{verbatim} |
123 |
http://mitgcm.org/source\_code.html |
http://mitgcm.org/source_code.html |
124 |
\end{verbatim} |
\end{verbatim} |
125 |
\begin{rawhtml} </A> \end{rawhtml} |
\begin{rawhtml} </A> \end{rawhtml} |
126 |
|
|
127 |
|
As a convenience, the MITgcm CVS server contains aliases which are |
128 |
|
named subsets of the codebase. These aliases can be especially |
129 |
|
helpful when used over slow internet connections or on machines with |
130 |
|
restricted storage space. Table \ref{tab:cvsModules} contains a list |
131 |
|
of CVS aliases |
132 |
|
\begin{table}[htb] |
133 |
|
\centering |
134 |
|
\begin{tabular}[htb]{|lp{3.25in}|}\hline |
135 |
|
\textbf{Alias Name} & \textbf{Information (directories) Contained} \\\hline |
136 |
|
\texttt{MITgcm\_code} & Only the source code -- none of the verification examples. \\ |
137 |
|
\texttt{MITgcm\_verif\_basic} |
138 |
|
& Source code plus a small set of the verification examples |
139 |
|
(\texttt{global\_ocean.90x40x15}, \texttt{aim.5l\_cs}, \texttt{hs94.128x64x5}, |
140 |
|
\texttt{front\_relax}, and \texttt{plume\_on\_slope}). \\ |
141 |
|
\texttt{MITgcm\_verif\_atmos} & Source code plus all of the atmospheric examples. \\ |
142 |
|
\texttt{MITgcm\_verif\_ocean} & Source code plus all of the oceanic examples. \\ |
143 |
|
\texttt{MITgcm\_verif\_all} & Source code plus all of the |
144 |
|
verification examples. \\\hline |
145 |
|
\end{tabular} |
146 |
|
\caption{MITgcm CVS Modules} |
147 |
|
\label{tab:cvsModules} |
148 |
|
\end{table} |
149 |
|
|
150 |
The checkout process creates a directory called \textit{MITgcm}. If |
The checkout process creates a directory called \textit{MITgcm}. If |
151 |
the directory \textit{MITgcm} exists this command updates your code |
the directory \textit{MITgcm} exists this command updates your code |
155 |
the files in \textit{CVS}! You can also use CVS to download code |
the files in \textit{CVS}! You can also use CVS to download code |
156 |
updates. More extensive information on using CVS for maintaining |
updates. More extensive information on using CVS for maintaining |
157 |
MITgcm code can be found |
MITgcm code can be found |
158 |
\begin{rawhtml} <A href=http://mitgcm.org/usingcvstoget.html target="idontexist"> \end{rawhtml} |
\begin{rawhtml} <A href=''http://mitgcm.org/usingcvstoget.html'' target="idontexist"> \end{rawhtml} |
159 |
here |
here |
160 |
\begin{rawhtml} </A> \end{rawhtml} |
\begin{rawhtml} </A> \end{rawhtml} |
161 |
. |
. |
162 |
|
It is important to note that the CVS aliases in Table |
163 |
|
\ref{tab:cvsModules} cannot be used in conjunction with the CVS |
164 |
|
\texttt{-d DIRNAME} option. However, the \texttt{MITgcm} directories |
165 |
|
they create can be changed to a different name following the check-out: |
166 |
|
\begin{verbatim} |
167 |
|
% cvs co MITgcm_verif_basic |
168 |
|
% mv MITgcm MITgcm_verif_basic |
169 |
|
\end{verbatim} |
170 |
|
|
171 |
|
|
172 |
\paragraph*{Conventional download method} |
\subsection{Method 2 - Tar file download} |
173 |
\label{sect:conventionalDownload} |
\label{sect:conventionalDownload} |
174 |
|
|
175 |
If you do not have CVS on your system, you can download the model as a |
If you do not have CVS on your system, you can download the model as a |
183 |
delete; even if you do not use CVS yourself the information can help |
delete; even if you do not use CVS yourself the information can help |
184 |
us if you should need to send us your copy of the code. If a recent |
us if you should need to send us your copy of the code. If a recent |
185 |
tar file does not exist, then please contact the developers through |
tar file does not exist, then please contact the developers through |
186 |
the MITgcm-support list. |
the |
187 |
|
\begin{rawhtml} <A href=''mailto:MITgcm-support@mitgcm.org"> \end{rawhtml} |
188 |
|
MITgcm-support@mitgcm.org |
189 |
|
\begin{rawhtml} </A> \end{rawhtml} |
190 |
|
mailing list. |
191 |
|
|
192 |
\paragraph*{Upgrading from an earlier version} |
\subsubsection{Upgrading from an earlier version} |
193 |
|
|
194 |
If you already have an earlier version of the code you can ``upgrade'' |
If you already have an earlier version of the code you can ``upgrade'' |
195 |
your copy instead of downloading the entire repository again. First, |
your copy instead of downloading the entire repository again. First, |
215 |
cvs update command and it will report the conflicts. Conflicts are |
cvs update command and it will report the conflicts. Conflicts are |
216 |
indicated in the code by the delimites ``$<<<<<<<$'', ``======='' and |
indicated in the code by the delimites ``$<<<<<<<$'', ``======='' and |
217 |
``$>>>>>>>$''. For example, |
``$>>>>>>>$''. For example, |
218 |
|
{\small |
219 |
\begin{verbatim} |
\begin{verbatim} |
220 |
<<<<<<< ini_parms.F |
<<<<<<< ini_parms.F |
221 |
& bottomDragLinear,myOwnBottomDragCoefficient, |
& bottomDragLinear,myOwnBottomDragCoefficient, |
223 |
& bottomDragLinear,bottomDragQuadratic, |
& bottomDragLinear,bottomDragQuadratic, |
224 |
>>>>>>> 1.18 |
>>>>>>> 1.18 |
225 |
\end{verbatim} |
\end{verbatim} |
226 |
|
} |
227 |
means that you added ``myOwnBottomDragCoefficient'' to a namelist at |
means that you added ``myOwnBottomDragCoefficient'' to a namelist at |
228 |
the same time and place that we added ``bottomDragQuadratic''. You |
the same time and place that we added ``bottomDragQuadratic''. You |
229 |
need to resolve this conflict and in this case the line should be |
need to resolve this conflict and in this case the line should be |
230 |
changed to: |
changed to: |
231 |
|
{\small |
232 |
\begin{verbatim} |
\begin{verbatim} |
233 |
& bottomDragLinear,bottomDragQuadratic,myOwnBottomDragCoefficient, |
& bottomDragLinear,bottomDragQuadratic,myOwnBottomDragCoefficient, |
234 |
\end{verbatim} |
\end{verbatim} |
235 |
|
} |
236 |
and the lines with the delimiters ($<<<<<<$,======,$>>>>>>$) be deleted. |
and the lines with the delimiters ($<<<<<<$,======,$>>>>>>$) be deleted. |
237 |
Unless you are making modifications which exactly parallel |
Unless you are making modifications which exactly parallel |
238 |
developments we make, these types of conflicts should be rare. |
developments we make, these types of conflicts should be rare. |
266 |
\textit{eesupp} directory. The grid point model code is held under the |
\textit{eesupp} directory. The grid point model code is held under the |
267 |
\textit{model} directory. Code execution actually starts in the |
\textit{model} directory. Code execution actually starts in the |
268 |
\textit{eesupp} routines and not in the \textit{model} routines. For |
\textit{eesupp} routines and not in the \textit{model} routines. For |
269 |
this reason the top-level |
this reason the top-level \textit{MAIN.F} is in the |
270 |
\textit{MAIN.F} is in the \textit{eesupp/src} directory. In general, |
\textit{eesupp/src} directory. In general, end-users should not need |
271 |
end-users should not need to worry about this level. The top-level routine |
to worry about this level. The top-level routine for the numerical |
272 |
for the numerical part of the code is in \textit{model/src/THE\_MODEL\_MAIN.F% |
part of the code is in \textit{model/src/THE\_MODEL\_MAIN.F}. Here is |
273 |
}. Here is a brief description of the directory structure of the model under |
a brief description of the directory structure of the model under the |
274 |
the root tree (a detailed description is given in section 3: Code structure). |
root tree (a detailed description is given in section 3: Code |
275 |
|
structure). |
276 |
|
|
277 |
\begin{itemize} |
\begin{itemize} |
|
\item \textit{bin}: this directory is initially empty. It is the default |
|
|
directory in which to compile the code. |
|
278 |
|
|
279 |
|
\item \textit{bin}: this directory is initially empty. It is the |
280 |
|
default directory in which to compile the code. |
281 |
|
|
282 |
\item \textit{diags}: contains the code relative to time-averaged |
\item \textit{diags}: contains the code relative to time-averaged |
283 |
diagnostics. It is subdivided into two subdirectories \textit{inc} and |
diagnostics. It is subdivided into two subdirectories \textit{inc} |
284 |
\textit{src} that contain include files (*.\textit{h} files) and Fortran |
and \textit{src} that contain include files (*.\textit{h} files) and |
285 |
subroutines (*.\textit{F} files), respectively. |
Fortran subroutines (*.\textit{F} files), respectively. |
286 |
|
|
287 |
\item \textit{doc}: contains brief documentation notes. |
\item \textit{doc}: contains brief documentation notes. |
288 |
|
|
289 |
\item \textit{eesupp}: contains the execution environment source code. Also |
\item \textit{eesupp}: contains the execution environment source code. |
290 |
subdivided into two subdirectories \textit{inc} and \textit{src}. |
Also subdivided into two subdirectories \textit{inc} and |
291 |
|
\textit{src}. |
292 |
\item \textit{exe}: this directory is initially empty. It is the default |
|
293 |
directory in which to execute the code. |
\item \textit{exe}: this directory is initially empty. It is the |
294 |
|
default directory in which to execute the code. |
295 |
\item \textit{model}: this directory contains the main source code. Also |
|
296 |
subdivided into two subdirectories \textit{inc} and \textit{src}. |
\item \textit{model}: this directory contains the main source code. |
297 |
|
Also subdivided into two subdirectories \textit{inc} and |
298 |
\item \textit{pkg}: contains the source code for the packages. Each package |
\textit{src}. |
299 |
corresponds to a subdirectory. For example, \textit{gmredi} contains the |
|
300 |
code related to the Gent-McWilliams/Redi scheme, \textit{aim} the code |
\item \textit{pkg}: contains the source code for the packages. Each |
301 |
relative to the atmospheric intermediate physics. The packages are described |
package corresponds to a subdirectory. For example, \textit{gmredi} |
302 |
in detail in section 3. |
contains the code related to the Gent-McWilliams/Redi scheme, |
303 |
|
\textit{aim} the code relative to the atmospheric intermediate |
304 |
\item \textit{tools}: this directory contains various useful tools. For |
physics. The packages are described in detail in section 3. |
305 |
example, \textit{genmake2} is a script written in csh (C-shell) that should |
|
306 |
be used to generate your makefile. The directory \textit{adjoint} contains |
\item \textit{tools}: this directory contains various useful tools. |
307 |
the makefile specific to the Tangent linear and Adjoint Compiler (TAMC) that |
For example, \textit{genmake2} is a script written in csh (C-shell) |
308 |
generates the adjoint code. The latter is described in details in part V. |
that should be used to generate your makefile. The directory |
309 |
|
\textit{adjoint} contains the makefile specific to the Tangent |
310 |
|
linear and Adjoint Compiler (TAMC) that generates the adjoint code. |
311 |
|
The latter is described in details in part V. |
312 |
|
|
313 |
\item \textit{utils}: this directory contains various utilities. The |
\item \textit{utils}: this directory contains various utilities. The |
314 |
subdirectory \textit{knudsen2} contains code and a makefile that |
subdirectory \textit{knudsen2} contains code and a makefile that |
315 |
compute coefficients of the polynomial approximation to the knudsen |
compute coefficients of the polynomial approximation to the knudsen |
316 |
formula for an ocean nonlinear equation of state. The \textit{matlab} |
formula for an ocean nonlinear equation of state. The |
317 |
subdirectory contains matlab scripts for reading model output directly |
\textit{matlab} subdirectory contains matlab scripts for reading |
318 |
into matlab. \textit{scripts} contains C-shell post-processing |
model output directly into matlab. \textit{scripts} contains C-shell |
319 |
scripts for joining processor-based and tiled-based model output. |
post-processing scripts for joining processor-based and tiled-based |
320 |
|
model output. |
321 |
|
|
322 |
|
\item \textit{verification}: this directory contains the model |
323 |
|
examples. See section \ref{sect:modelExamples}. |
324 |
|
|
|
\item \textit{verification}: this directory contains the model examples. See |
|
|
section \ref{sect:modelExamples}. |
|
325 |
\end{itemize} |
\end{itemize} |
326 |
|
|
327 |
\section{Example experiments} |
\section[MITgcm Example Experiments]{Example experiments} |
328 |
\label{sect:modelExamples} |
\label{sect:modelExamples} |
329 |
|
|
330 |
%% a set of twenty-four pre-configured numerical experiments |
%% a set of twenty-four pre-configured numerical experiments |
343 |
\subsection{Full list of model examples} |
\subsection{Full list of model examples} |
344 |
|
|
345 |
\begin{enumerate} |
\begin{enumerate} |
346 |
|
|
347 |
\item \textit{exp0} - single layer, ocean double gyre (barotropic with |
\item \textit{exp0} - single layer, ocean double gyre (barotropic with |
348 |
free-surface). This experiment is described in detail in section |
free-surface). This experiment is described in detail in section |
349 |
\ref{sect:eg-baro}. |
\ref{sect:eg-baro}. |
469 |
of the number of threads to use in $X$ and $Y$ under multithreaded |
of the number of threads to use in $X$ and $Y$ under multithreaded |
470 |
execution. |
execution. |
471 |
\end{itemize} |
\end{itemize} |
472 |
|
|
473 |
In addition, you will also find in this directory the forcing and |
In addition, you will also find in this directory the forcing and |
474 |
topography files as well as the files describing the initial state of |
topography files as well as the files describing the initial state |
475 |
the experiment. This varies from experiment to experiment. See |
of the experiment. This varies from experiment to experiment. See |
476 |
section 2 for more details. |
section 2 for more details. |
477 |
|
|
478 |
\item \textit{results}: this directory contains the output file |
\item \textit{results}: this directory contains the output file |
479 |
\textit{output.txt} produced by the simulation example. This file is |
\textit{output.txt} produced by the simulation example. This file is |
481 |
experiment. |
experiment. |
482 |
\end{itemize} |
\end{itemize} |
483 |
|
|
484 |
Once you have chosen the example you want to run, you are ready to compile |
Once you have chosen the example you want to run, you are ready to |
485 |
the code. |
compile the code. |
486 |
|
|
487 |
\section{Building the code} |
\section[Building MITgcm]{Building the code} |
488 |
\label{sect:buildingCode} |
\label{sect:buildingCode} |
489 |
|
|
490 |
To compile the code, we use the {\em make} program. This uses a file |
To compile the code, we use the {\em make} program. This uses a file |
523 |
Through the MITgcm-support list, the MITgcm developers are willing to |
Through the MITgcm-support list, the MITgcm developers are willing to |
524 |
provide help writing or modifing ``optfiles''. And we encourage users |
provide help writing or modifing ``optfiles''. And we encourage users |
525 |
to post new ``optfiles'' (particularly ones for new machines or |
to post new ``optfiles'' (particularly ones for new machines or |
526 |
architectures) to the MITgcm-support list. |
architectures) to the |
527 |
|
\begin{rawhtml} <A href=''mailto:MITgcm-support@mitgcm.org"> \end{rawhtml} |
528 |
|
MITgcm-support@mitgcm.org |
529 |
|
\begin{rawhtml} </A> \end{rawhtml} |
530 |
|
list. |
531 |
|
|
532 |
To specify an optfile to {\em genmake2}, the syntax is: |
To specify an optfile to {\em genmake2}, the syntax is: |
533 |
\begin{verbatim} |
\begin{verbatim} |
666 |
\end{verbatim} |
\end{verbatim} |
667 |
|
|
668 |
|
|
669 |
|
\subsection{Using \texttt{genmake2}} |
|
\subsection{Using \textit{genmake2}} |
|
670 |
\label{sect:genmake} |
\label{sect:genmake} |
671 |
|
|
672 |
To compile the code, first use the program \texttt{genmake2} (located |
To compile the code, first use the program \texttt{genmake2} (located |
673 |
in the \textit{tools} directory) to generate a Makefile. |
in the \texttt{tools} directory) to generate a Makefile. |
674 |
\texttt{genmake2} is a shell script written to work with all |
\texttt{genmake2} is a shell script written to work with all |
675 |
``sh''--compatible shells including bash v1, bash v2, and Bourne. |
``sh''--compatible shells including bash v1, bash v2, and Bourne. |
676 |
Internally, \texttt{genmake2} determines the locations of needed |
Internally, \texttt{genmake2} determines the locations of needed |
677 |
files, the compiler, compiler options, libraries, and Unix tools. It |
files, the compiler, compiler options, libraries, and Unix tools. It |
678 |
relies upon a number of ``optfiles'' located in the {\em |
relies upon a number of ``optfiles'' located in the |
679 |
tools/build\_options} directory. |
\texttt{tools/build\_options} directory. |
680 |
|
|
681 |
The purpose of the optfiles is to provide all the compilation options |
The purpose of the optfiles is to provide all the compilation options |
682 |
for particular ``platforms'' (where ``platform'' roughly means the |
for particular ``platforms'' (where ``platform'' roughly means the |
759 |
The most important command-line options are: |
The most important command-line options are: |
760 |
\begin{description} |
\begin{description} |
761 |
|
|
762 |
\item[--optfile=/PATH/FILENAME] specifies the optfile that should be |
\item[\texttt{--optfile=/PATH/FILENAME}] specifies the optfile that |
763 |
used for a particular build. |
should be used for a particular build. |
764 |
|
|
765 |
If no "optfile" is specified (either through the command line or the |
If no "optfile" is specified (either through the command line or the |
766 |
MITGCM\_OPTFILE environment variable), genmake2 will try to make a |
MITGCM\_OPTFILE environment variable), genmake2 will try to make a |
771 |
the user's path. When these three items have been identified, |
the user's path. When these three items have been identified, |
772 |
genmake2 will try to find an optfile that has a matching name. |
genmake2 will try to find an optfile that has a matching name. |
773 |
|
|
774 |
\item[--pdepend=/PATH/FILENAME] specifies the dependency file used for |
\item[\texttt{--pdefault='PKG1 PKG2 PKG3 ...'}] specifies the default |
775 |
packages. |
set of packages to be used. The normal order of precedence for |
776 |
|
packages is as follows: |
777 |
|
\begin{enumerate} |
778 |
|
\item If available, the command line (\texttt{--pdefault}) settings |
779 |
|
over-rule any others. |
780 |
|
|
781 |
|
\item Next, \texttt{genmake2} will look for a file named |
782 |
|
``\texttt{packages.conf}'' in the local directory or in any of the |
783 |
|
directories specified with the \texttt{--mods} option. |
784 |
|
|
785 |
|
\item Finally, if neither of the above are available, |
786 |
|
\texttt{genmake2} will use the \texttt{/pkg/pkg\_default} file. |
787 |
|
\end{enumerate} |
788 |
|
|
789 |
|
\item[\texttt{--pdepend=/PATH/FILENAME}] specifies the dependency file |
790 |
|
used for packages. |
791 |
|
|
792 |
If not specified, the default dependency file {\em pkg/pkg\_depend} |
If not specified, the default dependency file {\em pkg/pkg\_depend} |
793 |
is used. The syntax for this file is parsed on a line-by-line basis |
is used. The syntax for this file is parsed on a line-by-line basis |
798 |
assumed that the two packages are compatible and will function |
assumed that the two packages are compatible and will function |
799 |
either with or without each other. |
either with or without each other. |
800 |
|
|
801 |
\item[--pdefault='PKG1 PKG2 PKG3 ...'] specifies the default set of |
\item[\texttt{--adof=/path/to/file}] specifies the "adjoint" or |
802 |
packages to be used. |
automatic differentiation options file to be used. The file is |
803 |
|
analogous to the ``optfile'' defined above but it specifies |
804 |
If not set, the default package list will be read from {\em |
information for the AD build process. |
|
pkg/pkg\_default} |
|
|
|
|
|
\item[--adof=/path/to/file] specifies the "adjoint" or automatic |
|
|
differentiation options file to be used. The file is analogous to |
|
|
the ``optfile'' defined above but it specifies information for the |
|
|
AD build process. |
|
805 |
|
|
806 |
The default file is located in {\em |
The default file is located in {\em |
807 |
tools/adjoint\_options/adjoint\_default} and it defines the "TAF" |
tools/adjoint\_options/adjoint\_default} and it defines the "TAF" |
810 |
"STAF" compiler. As with any compilers, it is helpful to have their |
"STAF" compiler. As with any compilers, it is helpful to have their |
811 |
directories listed in your {\tt \$PATH} environment variable. |
directories listed in your {\tt \$PATH} environment variable. |
812 |
|
|
813 |
\item[--mods='DIR1 DIR2 DIR3 ...'] specifies a list of directories |
\item[\texttt{--mods='DIR1 DIR2 DIR3 ...'}] specifies a list of |
814 |
containing ``modifications''. These directories contain files with |
directories containing ``modifications''. These directories contain |
815 |
names that may (or may not) exist in the main MITgcm source tree but |
files with names that may (or may not) exist in the main MITgcm |
816 |
will be overridden by any identically-named sources within the |
source tree but will be overridden by any identically-named sources |
817 |
``MODS'' directories. |
within the ``MODS'' directories. |
818 |
|
|
819 |
The order of precedence for this "name-hiding" is as follows: |
The order of precedence for this "name-hiding" is as follows: |
820 |
\begin{itemize} |
\begin{itemize} |
827 |
``-standarddirs'' option) |
``-standarddirs'' option) |
828 |
\end{itemize} |
\end{itemize} |
829 |
|
|
830 |
\item[--make=/path/to/gmake] Due to the poor handling of soft-links and |
\item[\texttt{--mpi}] This option enables certain MPI features (using |
831 |
other bugs common with the \texttt{make} versions provided by |
CPP \texttt{\#define}s) within the code and is necessary for MPI |
832 |
commercial Unix vendors, GNU \texttt{make} (sometimes called |
builds (see Section \ref{sect:mpi-build}). |
833 |
\texttt{gmake}) should be preferred. This option provides a means |
|
834 |
for specifying the make executable to be used. |
\item[\texttt{--make=/path/to/gmake}] Due to the poor handling of |
835 |
|
soft-links and other bugs common with the \texttt{make} versions |
836 |
|
provided by commercial Unix vendors, GNU \texttt{make} (sometimes |
837 |
|
called \texttt{gmake}) should be preferred. This option provides a |
838 |
|
means for specifying the make executable to be used. |
839 |
|
|
840 |
|
\item[\texttt{--bash=/path/to/sh}] On some (usually older UNIX) |
841 |
|
machines, the ``bash'' shell is unavailable. To run on these |
842 |
|
systems, \texttt{genmake2} can be invoked using an ``sh'' (that is, |
843 |
|
a Bourne, POSIX, or compatible) shell. The syntax in these |
844 |
|
circumstances is: |
845 |
|
\begin{center} |
846 |
|
\texttt{\% /bin/sh genmake2 -bash=/bin/sh [...options...]} |
847 |
|
\end{center} |
848 |
|
where \texttt{/bin/sh} can be replaced with the full path and name |
849 |
|
of the desired shell. |
850 |
|
|
851 |
\end{description} |
\end{description} |
852 |
|
|
853 |
|
|
854 |
|
\subsection{Building with MPI} |
855 |
|
\label{sect:mpi-build} |
856 |
|
|
857 |
|
Building MITgcm to use MPI libraries can be complicated due to the |
858 |
|
variety of different MPI implementations available, their dependencies |
859 |
|
or interactions with different compilers, and their often ad-hoc |
860 |
|
locations within file systems. For these reasons, its generally a |
861 |
|
good idea to start by finding and reading the documentation for your |
862 |
|
machine(s) and, if necessary, seeking help from your local systems |
863 |
|
administrator. |
864 |
|
|
865 |
|
The steps for building MITgcm with MPI support are: |
866 |
|
\begin{enumerate} |
867 |
|
|
868 |
|
\item Determine the locations of your MPI-enabled compiler and/or MPI |
869 |
|
libraries and put them into an options file as described in Section |
870 |
|
\ref{sect:genmake}. One can start with one of the examples in: |
871 |
|
\begin{rawhtml} <A |
872 |
|
href="http://mitgcm.org/cgi-bin/viewcvs.cgi/MITgcm/tools/build_options/"> |
873 |
|
\end{rawhtml} |
874 |
|
\begin{center} |
875 |
|
\texttt{MITgcm/tools/build\_options/} |
876 |
|
\end{center} |
877 |
|
\begin{rawhtml} </A> \end{rawhtml} |
878 |
|
such as \texttt{linux\_ia32\_g77+mpi\_cg01} or |
879 |
|
\texttt{linux\_ia64\_efc+mpi} and then edit it to suit the machine at |
880 |
|
hand. You may need help from your user guide or local systems |
881 |
|
administrator to determine the exact location of the MPI libraries. |
882 |
|
If libraries are not installed, MPI implementations and related |
883 |
|
tools are available including: |
884 |
|
\begin{itemize} |
885 |
|
\item \begin{rawhtml} <A |
886 |
|
href="http://www-unix.mcs.anl.gov/mpi/mpich/"> |
887 |
|
\end{rawhtml} |
888 |
|
MPICH |
889 |
|
\begin{rawhtml} </A> \end{rawhtml} |
890 |
|
|
891 |
|
\item \begin{rawhtml} <A |
892 |
|
href="http://www.lam-mpi.org/"> |
893 |
|
\end{rawhtml} |
894 |
|
LAM/MPI |
895 |
|
\begin{rawhtml} </A> \end{rawhtml} |
896 |
|
|
897 |
|
\item \begin{rawhtml} <A |
898 |
|
href="http://www.osc.edu/~pw/mpiexec/"> |
899 |
|
\end{rawhtml} |
900 |
|
MPIexec |
901 |
|
\begin{rawhtml} </A> \end{rawhtml} |
902 |
|
\end{itemize} |
903 |
|
|
904 |
|
\item Build the code with the \texttt{genmake2} \texttt{-mpi} option |
905 |
|
(see Section \ref{sect:genmake}) using commands such as: |
906 |
|
{\footnotesize \begin{verbatim} |
907 |
|
% ../../../tools/genmake2 -mods=../code -mpi -of=YOUR_OPTFILE |
908 |
|
% make depend |
909 |
|
% make |
910 |
|
\end{verbatim} } |
911 |
|
|
912 |
|
\item Run the code with the appropriate MPI ``run'' or ``exec'' |
913 |
|
program provided with your particular implementation of MPI. |
914 |
|
Typical MPI packages such as MPICH will use something like: |
915 |
|
\begin{verbatim} |
916 |
|
% mpirun -np 4 -machinefile mf ./mitgcmuv |
917 |
|
\end{verbatim} |
918 |
|
Sightly more complicated scripts may be needed for many machines |
919 |
|
since execution of the code may be controlled by both the MPI |
920 |
|
library and a job scheduling and queueing system such as PBS, |
921 |
|
LoadLeveller, Condor, or any of a number of similar tools. A few |
922 |
|
example scripts (those used for our \begin{rawhtml} <A |
923 |
|
href="http://mitgcm.org/testing.html"> \end{rawhtml}regular |
924 |
|
verification runs\begin{rawhtml} </A> \end{rawhtml}) are available |
925 |
|
at: |
926 |
|
\begin{rawhtml} <A |
927 |
|
href="http://mitgcm.org/cgi-bin/viewcvs.cgi/MITgcm_contrib/test_scripts/"> |
928 |
|
\end{rawhtml} |
929 |
|
{\footnotesize \tt |
930 |
|
http://mitgcm.org/cgi-bin/viewcvs.cgi/MITgcm\_contrib/test\_scripts/ } |
931 |
|
\begin{rawhtml} </A> \end{rawhtml} |
932 |
|
|
933 |
|
\end{enumerate} |
934 |
|
|
935 |
\section{Running the model} |
An example of the above process on the MITgcm cluster (``cg01'') using |
936 |
|
the GNU g77 compiler and the mpich MPI library is: |
937 |
|
|
938 |
|
{\footnotesize \begin{verbatim} |
939 |
|
% cd MITgcm/verification/exp5 |
940 |
|
% mkdir build |
941 |
|
% cd build |
942 |
|
% ../../../tools/genmake2 -mpi -mods=../code \ |
943 |
|
-of=../../../tools/build_options/linux_ia32_g77+mpi_cg01 |
944 |
|
% make depend |
945 |
|
% make |
946 |
|
% cd ../input |
947 |
|
% /usr/local/pkg/mpi/mpi-1.2.4..8a-gm-1.5/g77/bin/mpirun.ch_gm \ |
948 |
|
-machinefile mf --gm-kill 5 -v -np 2 ../build/mitgcmuv |
949 |
|
\end{verbatim} } |
950 |
|
|
951 |
|
|
952 |
|
|
953 |
|
\section[Running MITgcm]{Running the model in prognostic mode} |
954 |
\label{sect:runModel} |
\label{sect:runModel} |
955 |
|
|
956 |
If compilation finished succesfuully (section \ref{sect:buildModel}) |
If compilation finished succesfuully (section \ref{sect:buildingCode}) |
957 |
then an executable called {\em mitgcmuv} will now exist in the local |
then an executable called \texttt{mitgcmuv} will now exist in the |
958 |
directory. |
local directory. |
959 |
|
|
960 |
To run the model as a single process (ie. not in parallel) simply |
To run the model as a single process (ie. not in parallel) simply |
961 |
type: |
type: |
973 |
% ./mitgcmuv > output.txt |
% ./mitgcmuv > output.txt |
974 |
\end{verbatim} |
\end{verbatim} |
975 |
|
|
976 |
For the example experiments in {\em vericication}, an example of the |
For the example experiments in {\em verification}, an example of the |
977 |
output is kept in {\em results/output.txt} for comparison. You can compare |
output is kept in {\em results/output.txt} for comparison. You can compare |
978 |
your {\em output.txt} with this one to check that the set-up works. |
your {\em output.txt} with this one to check that the set-up works. |
979 |
|
|
1059 |
>> for n=1:11; imagesc(eta(:,:,n)');axis ij;colorbar;pause(.5);end |
>> for n=1:11; imagesc(eta(:,:,n)');axis ij;colorbar;pause(.5);end |
1060 |
\end{verbatim} |
\end{verbatim} |
1061 |
|
|
|
\section{Doing it yourself: customizing the code} |
|
|
|
|
|
When you are ready to run the model in the configuration you want, the |
|
|
easiest thing is to use and adapt the setup of the case studies experiment |
|
|
(described previously) that is the closest to your configuration. Then, the |
|
|
amount of setup will be minimized. In this section, we focus on the setup |
|
|
relative to the ''numerical model'' part of the code (the setup relative to |
|
|
the ''execution environment'' part is covered in the parallel implementation |
|
|
section) and on the variables and parameters that you are likely to change. |
|
|
|
|
|
\subsection{Configuration and setup} |
|
|
|
|
|
The CPP keys relative to the ''numerical model'' part of the code are all |
|
|
defined and set in the file \textit{CPP\_OPTIONS.h }in the directory \textit{% |
|
|
model/inc }or in one of the \textit{code }directories of the case study |
|
|
experiments under \textit{verification.} The model parameters are defined |
|
|
and declared in the file \textit{model/inc/PARAMS.h }and their default |
|
|
values are set in the routine \textit{model/src/set\_defaults.F. }The |
|
|
default values can be modified in the namelist file \textit{data }which |
|
|
needs to be located in the directory where you will run the model. The |
|
|
parameters are initialized in the routine \textit{model/src/ini\_parms.F}. |
|
|
Look at this routine to see in what part of the namelist the parameters are |
|
|
located. |
|
|
|
|
|
In what follows the parameters are grouped into categories related to the |
|
|
computational domain, the equations solved in the model, and the simulation |
|
|
controls. |
|
|
|
|
|
\subsection{Computational domain, geometry and time-discretization} |
|
|
|
|
|
\begin{itemize} |
|
|
\item dimensions |
|
|
\end{itemize} |
|
|
|
|
|
The number of points in the x, y,\textit{\ }and r\textit{\ }directions are |
|
|
represented by the variables \textbf{sNx}\textit{, }\textbf{sNy}\textit{, }% |
|
|
and \textbf{Nr}\textit{\ }respectively which are declared and set in the |
|
|
file \textit{model/inc/SIZE.h. }(Again, this assumes a mono-processor |
|
|
calculation. For multiprocessor calculations see section on parallel |
|
|
implementation.) |
|
|
|
|
|
\begin{itemize} |
|
|
\item grid |
|
|
\end{itemize} |
|
|
|
|
|
Three different grids are available: cartesian, spherical polar, and |
|
|
curvilinear (including the cubed sphere). The grid is set through the |
|
|
logical variables \textbf{usingCartesianGrid}\textit{, }\textbf{% |
|
|
usingSphericalPolarGrid}\textit{, }and \textit{\ }\textbf{% |
|
|
usingCurvilinearGrid}\textit{. }In the case of spherical and curvilinear |
|
|
grids, the southern boundary is defined through the variable \textbf{phiMin}% |
|
|
\textit{\ }which corresponds to the latitude of the southern most cell face |
|
|
(in degrees). The resolution along the x and y directions is controlled by |
|
|
the 1D arrays \textbf{delx}\textit{\ }and \textbf{dely}\textit{\ }(in meters |
|
|
in the case of a cartesian grid, in degrees otherwise). The vertical grid |
|
|
spacing is set through the 1D array \textbf{delz }for the ocean (in meters) |
|
|
or \textbf{delp}\textit{\ }for the atmosphere (in Pa). The variable \textbf{% |
|
|
Ro\_SeaLevel} represents the standard position of Sea-Level in ''R'' |
|
|
coordinate. This is typically set to 0m for the ocean (default value) and 10$% |
|
|
^{5}$Pa for the atmosphere. For the atmosphere, also set the logical |
|
|
variable \textbf{groundAtK1} to '.\texttt{TRUE}.'. which put the first level |
|
|
(k=1) at the lower boundary (ground). |
|
|
|
|
|
For the cartesian grid case, the Coriolis parameter $f$ is set through the |
|
|
variables \textbf{f0}\textit{\ }and \textbf{beta}\textit{\ }which correspond |
|
|
to the reference Coriolis parameter (in s$^{-1}$) and $\frac{\partial f}{% |
|
|
\partial y}$(in m$^{-1}$s$^{-1}$) respectively. If \textbf{beta }\textit{\ }% |
|
|
is set to a nonzero value, \textbf{f0}\textit{\ }is the value of $f$ at the |
|
|
southern edge of the domain. |
|
|
|
|
|
\begin{itemize} |
|
|
\item topography - full and partial cells |
|
|
\end{itemize} |
|
|
|
|
|
The domain bathymetry is read from a file that contains a 2D (x,y) map of |
|
|
depths (in m) for the ocean or pressures (in Pa) for the atmosphere. The |
|
|
file name is represented by the variable \textbf{bathyFile}\textit{. }The |
|
|
file is assumed to contain binary numbers giving the depth (pressure) of the |
|
|
model at each grid cell, ordered with the x coordinate varying fastest. The |
|
|
points are ordered from low coordinate to high coordinate for both axes. The |
|
|
model code applies without modification to enclosed, periodic, and double |
|
|
periodic domains. Periodicity is assumed by default and is suppressed by |
|
|
setting the depths to 0m for the cells at the limits of the computational |
|
|
domain (note: not sure this is the case for the atmosphere). The precision |
|
|
with which to read the binary data is controlled by the integer variable |
|
|
\textbf{readBinaryPrec }which can take the value \texttt{32} (single |
|
|
precision) or \texttt{64} (double precision). See the matlab program \textit{% |
|
|
gendata.m }in the \textit{input }directories under \textit{verification }to |
|
|
see how the bathymetry files are generated for the case study experiments. |
|
|
|
|
|
To use the partial cell capability, the variable \textbf{hFacMin}\textit{\ }% |
|
|
needs to be set to a value between 0 and 1 (it is set to 1 by default) |
|
|
corresponding to the minimum fractional size of the cell. For example if the |
|
|
bottom cell is 500m thick and \textbf{hFacMin}\textit{\ }is set to 0.1, the |
|
|
actual thickness of the cell (i.e. used in the code) can cover a range of |
|
|
discrete values 50m apart from 50m to 500m depending on the value of the |
|
|
bottom depth (in \textbf{bathyFile}) at this point. |
|
|
|
|
|
Note that the bottom depths (or pressures) need not coincide with the models |
|
|
levels as deduced from \textbf{delz}\textit{\ }or\textit{\ }\textbf{delp}% |
|
|
\textit{. }The model will interpolate the numbers in \textbf{bathyFile}% |
|
|
\textit{\ }so that they match the levels obtained from \textbf{delz}\textit{% |
|
|
\ }or\textit{\ }\textbf{delp}\textit{\ }and \textbf{hFacMin}\textit{. } |
|
|
|
|
|
(Note: the atmospheric case is a bit more complicated than what is written |
|
|
here I think. To come soon...) |
|
|
|
|
|
\begin{itemize} |
|
|
\item time-discretization |
|
|
\end{itemize} |
|
|
|
|
|
The time steps are set through the real variables \textbf{deltaTMom} |
|
|
and \textbf{deltaTtracer} (in s) which represent the time step for the |
|
|
momentum and tracer equations, respectively. For synchronous |
|
|
integrations, simply set the two variables to the same value (or you |
|
|
can prescribe one time step only through the variable |
|
|
\textbf{deltaT}). The Adams-Bashforth stabilizing parameter is set |
|
|
through the variable \textbf{abEps} (dimensionless). The stagger |
|
|
baroclinic time stepping can be activated by setting the logical |
|
|
variable \textbf{staggerTimeStep} to '.\texttt{TRUE}.'. |
|
|
|
|
|
\subsection{Equation of state} |
|
|
|
|
|
First, because the model equations are written in terms of |
|
|
perturbations, a reference thermodynamic state needs to be specified. |
|
|
This is done through the 1D arrays \textbf{tRef} and \textbf{sRef}. |
|
|
\textbf{tRef} specifies the reference potential temperature profile |
|
|
(in $^{o}$C for the ocean and $^{o}$K for the atmosphere) starting |
|
|
from the level k=1. Similarly, \textbf{sRef} specifies the reference |
|
|
salinity profile (in ppt) for the ocean or the reference specific |
|
|
humidity profile (in g/kg) for the atmosphere. |
|
|
|
|
|
The form of the equation of state is controlled by the character |
|
|
variables \textbf{buoyancyRelation} and \textbf{eosType}. |
|
|
\textbf{buoyancyRelation} is set to '\texttt{OCEANIC}' by default and |
|
|
needs to be set to '\texttt{ATMOSPHERIC}' for atmosphere simulations. |
|
|
In this case, \textbf{eosType} must be set to '\texttt{IDEALGAS}'. |
|
|
For the ocean, two forms of the equation of state are available: |
|
|
linear (set \textbf{eosType} to '\texttt{LINEAR}') and a polynomial |
|
|
approximation to the full nonlinear equation ( set |
|
|
\textbf{eosType}\textit{\ }to '\texttt{POLYNOMIAL}'). In the linear |
|
|
case, you need to specify the thermal and haline expansion |
|
|
coefficients represented by the variables \textbf{tAlpha}\textit{\ |
|
|
}(in K$^{-1}$) and \textbf{sBeta} (in ppt$^{-1}$). For the nonlinear |
|
|
case, you need to generate a file of polynomial coefficients called |
|
|
\textit{POLY3.COEFFS}. To do this, use the program |
|
|
\textit{utils/knudsen2/knudsen2.f} under the model tree (a Makefile is |
|
|
available in the same directory and you will need to edit the number |
|
|
and the values of the vertical levels in \textit{knudsen2.f} so that |
|
|
they match those of your configuration). |
|
|
|
|
|
There there are also higher polynomials for the equation of state: |
|
|
\begin{description} |
|
|
\item['\texttt{UNESCO}':] The UNESCO equation of state formula of |
|
|
Fofonoff and Millard \cite{fofonoff83}. This equation of state |
|
|
assumes in-situ temperature, which is not a model variable; \emph{its use |
|
|
is therefore discouraged, and it is only listed for completeness}. |
|
|
\item['\texttt{JMD95Z}':] A modified UNESCO formula by Jackett and |
|
|
McDougall \cite{jackett95}, which uses the model variable potential |
|
|
temperature as input. The '\texttt{Z}' indicates that this equation |
|
|
of state uses a horizontally and temporally constant pressure |
|
|
$p_{0}=-g\rho_{0}z$. |
|
|
\item['\texttt{JMD95P}':] A modified UNESCO formula by Jackett and |
|
|
McDougall \cite{jackett95}, which uses the model variable potential |
|
|
temperature as input. The '\texttt{P}' indicates that this equation |
|
|
of state uses the actual hydrostatic pressure of the last time |
|
|
step. Lagging the pressure in this way requires an additional pickup |
|
|
file for restarts. |
|
|
\item['\texttt{MDJWF}':] The new, more accurate and less expensive |
|
|
equation of state by McDougall et~al. \cite{mcdougall03}. It also |
|
|
requires lagging the pressure and therefore an additional pickup |
|
|
file for restarts. |
|
|
\end{description} |
|
|
For none of these options an reference profile of temperature or |
|
|
salinity is required. |
|
|
|
|
|
\subsection{Momentum equations} |
|
|
|
|
|
In this section, we only focus for now on the parameters that you are likely |
|
|
to change, i.e. the ones relative to forcing and dissipation for example. |
|
|
The details relevant to the vector-invariant form of the equations and the |
|
|
various advection schemes are not covered for the moment. We assume that you |
|
|
use the standard form of the momentum equations (i.e. the flux-form) with |
|
|
the default advection scheme. Also, there are a few logical variables that |
|
|
allow you to turn on/off various terms in the momentum equation. These |
|
|
variables are called \textbf{momViscosity, momAdvection, momForcing, |
|
|
useCoriolis, momPressureForcing, momStepping}\textit{, }and \textit{\ }% |
|
|
\textbf{metricTerms }and are assumed to be set to '.\texttt{TRUE}.' here. |
|
|
Look at the file \textit{model/inc/PARAMS.h }for a precise definition of |
|
|
these variables. |
|
|
|
|
|
\begin{itemize} |
|
|
\item initialization |
|
|
\end{itemize} |
|
|
|
|
|
The velocity components are initialized to 0 unless the simulation is |
|
|
starting from a pickup file (see section on simulation control parameters). |
|
|
|
|
|
\begin{itemize} |
|
|
\item forcing |
|
|
\end{itemize} |
|
|
|
|
|
This section only applies to the ocean. You need to generate wind-stress |
|
|
data into two files \textbf{zonalWindFile}\textit{\ }and \textbf{% |
|
|
meridWindFile }corresponding to the zonal and meridional components of the |
|
|
wind stress, respectively (if you want the stress to be along the direction |
|
|
of only one of the model horizontal axes, you only need to generate one |
|
|
file). The format of the files is similar to the bathymetry file. The zonal |
|
|
(meridional) stress data are assumed to be in Pa and located at U-points |
|
|
(V-points). As for the bathymetry, the precision with which to read the |
|
|
binary data is controlled by the variable \textbf{readBinaryPrec}.\textbf{\ } |
|
|
See the matlab program \textit{gendata.m }in the \textit{input }directories |
|
|
under \textit{verification }to see how simple analytical wind forcing data |
|
|
are generated for the case study experiments. |
|
|
|
|
|
There is also the possibility of prescribing time-dependent periodic |
|
|
forcing. To do this, concatenate the successive time records into a single |
|
|
file (for each stress component) ordered in a (x, y, t) fashion and set the |
|
|
following variables: \textbf{periodicExternalForcing }to '.\texttt{TRUE}.', |
|
|
\textbf{externForcingPeriod }to the period (in s) of which the forcing |
|
|
varies (typically 1 month), and \textbf{externForcingCycle }to the repeat |
|
|
time (in s) of the forcing (typically 1 year -- note: \textbf{% |
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|
externForcingCycle }must be a multiple of \textbf{externForcingPeriod}). |
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|
With these variables set up, the model will interpolate the forcing linearly |
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|
at each iteration. |
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|
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\begin{itemize} |
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\item dissipation |
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|
\end{itemize} |
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|
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|
The lateral eddy viscosity coefficient is specified through the variable |
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|
\textbf{viscAh}\textit{\ }(in m$^{2}$s$^{-1}$). The vertical eddy viscosity |
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|
coefficient is specified through the variable \textbf{viscAz }(in m$^{2}$s$% |
|
|
^{-1}$) for the ocean and \textbf{viscAp}\textit{\ }(in Pa$^{2}$s$^{-1}$) |
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|
for the atmosphere. The vertical diffusive fluxes can be computed implicitly |
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|
by setting the logical variable \textbf{implicitViscosity }to '.\texttt{TRUE}% |
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|
.'. In addition, biharmonic mixing can be added as well through the variable |
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|
\textbf{viscA4}\textit{\ }(in m$^{4}$s$^{-1}$). On a spherical polar grid, |
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|
you might also need to set the variable \textbf{cosPower} which is set to 0 |
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|
by default and which represents the power of cosine of latitude to multiply |
|
|
viscosity. Slip or no-slip conditions at lateral and bottom boundaries are |
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|
specified through the logical variables \textbf{no\_slip\_sides}\textit{\ }% |
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|
and \textbf{no\_slip\_bottom}. If set to '\texttt{.FALSE.}', free-slip |
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|
boundary conditions are applied. If no-slip boundary conditions are applied |
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|
at the bottom, a bottom drag can be applied as well. Two forms are |
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|
available: linear (set the variable \textbf{bottomDragLinear}\textit{\ }in s$% |
|
|
^{-1}$) and quadratic (set the variable \textbf{bottomDragQuadratic}\textit{% |
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|
\ }in m$^{-1}$). |
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The Fourier and Shapiro filters are described elsewhere. |
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|
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\begin{itemize} |
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\item C-D scheme |
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\end{itemize} |
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|
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|
If you run at a sufficiently coarse resolution, you will need the C-D scheme |
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|
for the computation of the Coriolis terms. The variable\textbf{\ tauCD}, |
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|
which represents the C-D scheme coupling timescale (in s) needs to be set. |
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|
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|
\begin{itemize} |
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|
\item calculation of pressure/geopotential |
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|
\end{itemize} |
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|
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|
First, to run a non-hydrostatic ocean simulation, set the logical variable |
|
|
\textbf{nonHydrostatic} to '.\texttt{TRUE}.'. The pressure field is then |
|
|
inverted through a 3D elliptic equation. (Note: this capability is not |
|
|
available for the atmosphere yet.) By default, a hydrostatic simulation is |
|
|
assumed and a 2D elliptic equation is used to invert the pressure field. The |
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|
parameters controlling the behaviour of the elliptic solvers are the |
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|
variables \textbf{cg2dMaxIters}\textit{\ }and \textbf{cg2dTargetResidual }% |
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|
for the 2D case and \textbf{cg3dMaxIters}\textit{\ }and \textbf{% |
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|
cg3dTargetResidual }for the 3D case. You probably won't need to alter the |
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|
default values (are we sure of this?). |
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|
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|
For the calculation of the surface pressure (for the ocean) or surface |
|
|
geopotential (for the atmosphere) you need to set the logical variables |
|
|
\textbf{rigidLid} and \textbf{implicitFreeSurface}\textit{\ }(set one to '.% |
|
|
\texttt{TRUE}.' and the other to '.\texttt{FALSE}.' depending on how you |
|
|
want to deal with the ocean upper or atmosphere lower boundary). |
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|
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|
\subsection{Tracer equations} |
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|
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|
This section covers the tracer equations i.e. the potential temperature |
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|
equation and the salinity (for the ocean) or specific humidity (for the |
|
|
atmosphere) equation. As for the momentum equations, we only describe for |
|
|
now the parameters that you are likely to change. The logical variables |
|
|
\textbf{tempDiffusion}\textit{, }\textbf{tempAdvection}\textit{, }\textbf{% |
|
|
tempForcing}\textit{,} and \textbf{tempStepping} allow you to turn on/off |
|
|
terms in the temperature equation (same thing for salinity or specific |
|
|
humidity with variables \textbf{saltDiffusion}\textit{, }\textbf{% |
|
|
saltAdvection}\textit{\ }etc). These variables are all assumed here to be |
|
|
set to '.\texttt{TRUE}.'. Look at file \textit{model/inc/PARAMS.h }for a |
|
|
precise definition. |
|
|
|
|
|
\begin{itemize} |
|
|
\item initialization |
|
|
\end{itemize} |
|
|
|
|
|
The initial tracer data can be contained in the binary files \textbf{% |
|
|
hydrogThetaFile }and \textbf{hydrogSaltFile}. These files should contain 3D |
|
|
data ordered in an (x, y, r) fashion with k=1 as the first vertical level. |
|
|
If no file names are provided, the tracers are then initialized with the |
|
|
values of \textbf{tRef }and \textbf{sRef }mentioned above (in the equation |
|
|
of state section). In this case, the initial tracer data are uniform in x |
|
|
and y for each depth level. |
|
|
|
|
|
\begin{itemize} |
|
|
\item forcing |
|
|
\end{itemize} |
|
|
|
|
|
This part is more relevant for the ocean, the procedure for the atmosphere |
|
|
not being completely stabilized at the moment. |
|
|
|
|
|
A combination of fluxes data and relaxation terms can be used for driving |
|
|
the tracer equations. \ For potential temperature, heat flux data (in W/m$% |
|
|
^{2}$) can be stored in the 2D binary file \textbf{surfQfile}\textit{. }% |
|
|
Alternatively or in addition, the forcing can be specified through a |
|
|
relaxation term. The SST data to which the model surface temperatures are |
|
|
restored to are supposed to be stored in the 2D binary file \textbf{% |
|
|
thetaClimFile}\textit{. }The corresponding relaxation time scale coefficient |
|
|
is set through the variable \textbf{tauThetaClimRelax}\textit{\ }(in s). The |
|
|
same procedure applies for salinity with the variable names \textbf{EmPmRfile% |
|
|
}\textit{, }\textbf{saltClimFile}\textit{, }and \textbf{tauSaltClimRelax}% |
|
|
\textit{\ }for freshwater flux (in m/s) and surface salinity (in ppt) data |
|
|
files and relaxation time scale coefficient (in s), respectively. Also for |
|
|
salinity, if the CPP key \textbf{USE\_NATURAL\_BCS} is turned on, natural |
|
|
boundary conditions are applied i.e. when computing the surface salinity |
|
|
tendency, the freshwater flux is multiplied by the model surface salinity |
|
|
instead of a constant salinity value. |
|
|
|
|
|
As for the other input files, the precision with which to read the data is |
|
|
controlled by the variable \textbf{readBinaryPrec}. Time-dependent, periodic |
|
|
forcing can be applied as well following the same procedure used for the |
|
|
wind forcing data (see above). |
|
|
|
|
|
\begin{itemize} |
|
|
\item dissipation |
|
|
\end{itemize} |
|
|
|
|
|
Lateral eddy diffusivities for temperature and salinity/specific humidity |
|
|
are specified through the variables \textbf{diffKhT }and \textbf{diffKhS }% |
|
|
(in m$^{2}$/s). Vertical eddy diffusivities are specified through the |
|
|
variables \textbf{diffKzT }and \textbf{diffKzS }(in m$^{2}$/s) for the ocean |
|
|
and \textbf{diffKpT }and \textbf{diffKpS }(in Pa$^{2}$/s) for the |
|
|
atmosphere. The vertical diffusive fluxes can be computed implicitly by |
|
|
setting the logical variable \textbf{implicitDiffusion }to '.\texttt{TRUE}% |
|
|
.'. In addition, biharmonic diffusivities can be specified as well through |
|
|
the coefficients \textbf{diffK4T }and \textbf{diffK4S }(in m$^{4}$/s). Note |
|
|
that the cosine power scaling (specified through \textbf{cosPower }- see the |
|
|
momentum equations section) is applied to the tracer diffusivities |
|
|
(Laplacian and biharmonic) as well. The Gent and McWilliams parameterization |
|
|
for oceanic tracers is described in the package section. Finally, note that |
|
|
tracers can be also subject to Fourier and Shapiro filtering (see the |
|
|
corresponding section on these filters). |
|
|
|
|
|
\begin{itemize} |
|
|
\item ocean convection |
|
|
\end{itemize} |
|
|
|
|
|
Two options are available to parameterize ocean convection: one is to use |
|
|
the convective adjustment scheme. In this case, you need to set the variable |
|
|
\textbf{cadjFreq}, which represents the frequency (in s) with which the |
|
|
adjustment algorithm is called, to a non-zero value (if set to a negative |
|
|
value by the user, the model will set it to the tracer time step). The other |
|
|
option is to parameterize convection with implicit vertical diffusion. To do |
|
|
this, set the logical variable \textbf{implicitDiffusion }to '.\texttt{TRUE}% |
|
|
.' and the real variable \textbf{ivdc\_kappa }to a value (in m$^{2}$/s) you |
|
|
wish the tracer vertical diffusivities to have when mixing tracers |
|
|
vertically due to static instabilities. Note that \textbf{cadjFreq }and |
|
|
\textbf{ivdc\_kappa }can not both have non-zero value. |
|
|
|
|
|
\subsection{Simulation controls} |
|
|
|
|
|
The model ''clock'' is defined by the variable \textbf{deltaTClock }(in s) |
|
|
which determines the IO frequencies and is used in tagging output. |
|
|
Typically, you will set it to the tracer time step for accelerated runs |
|
|
(otherwise it is simply set to the default time step \textbf{deltaT}). |
|
|
Frequency of checkpointing and dumping of the model state are referenced to |
|
|
this clock (see below). |
|
|
|
|
|
\begin{itemize} |
|
|
\item run duration |
|
|
\end{itemize} |
|
|
|
|
|
The beginning of a simulation is set by specifying a start time (in s) |
|
|
through the real variable \textbf{startTime }or by specifying an initial |
|
|
iteration number through the integer variable \textbf{nIter0}. If these |
|
|
variables are set to nonzero values, the model will look for a ''pickup'' |
|
|
file \textit{pickup.0000nIter0 }to restart the integration\textit{. }The end |
|
|
of a simulation is set through the real variable \textbf{endTime }(in s). |
|
|
Alternatively, you can specify instead the number of time steps to execute |
|
|
through the integer variable \textbf{nTimeSteps}. |
|
|
|
|
|
\begin{itemize} |
|
|
\item frequency of output |
|
|
\end{itemize} |
|
|
|
|
|
Real variables defining frequencies (in s) with which output files are |
|
|
written on disk need to be set up. \textbf{dumpFreq }controls the frequency |
|
|
with which the instantaneous state of the model is saved. \textbf{chkPtFreq }% |
|
|
and \textbf{pchkPtFreq }control the output frequency of rolling and |
|
|
permanent checkpoint files, respectively. See section 1.5.1 Output files for the |
|
|
definition of model state and checkpoint files. In addition, time-averaged |
|
|
fields can be written out by setting the variable \textbf{taveFreq} (in s). |
|
|
The precision with which to write the binary data is controlled by the |
|
|
integer variable w\textbf{riteBinaryPrec }(set it to \texttt{32} or \texttt{% |
|
|
64}). |
|
|
|
|
|
%%% Local Variables: |
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%%% mode: latex |
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%%% TeX-master: t |
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%%% End: |
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