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revision 1.15 by edhill, Wed Jan 28 20:50:14 2004 UTC revision 1.17 by edhill, Thu Jan 29 15:11:39 2004 UTC
# Line 39  http://mitgcm.org/pipermail/mitgcm-suppo Line 39  http://mitgcm.org/pipermail/mitgcm-suppo
39  \begin{rawhtml} </A> \end{rawhtml}  \begin{rawhtml} </A> \end{rawhtml}
40  Essentially all of the MITgcm web pages can be searched using a  Essentially all of the MITgcm web pages can be searched using a
41  popular web crawler such as Google or through our own search facility:  popular web crawler such as Google or through our own search facility:
42    \begin{rawhtml} <A href=http://mitgcm.org/mailman/htdig/ target="idontexist"> \end{rawhtml}
43  \begin{verbatim}  \begin{verbatim}
44  http://mitgcm.org/htdig/  http://mitgcm.org/htdig/
45  \end{verbatim}  \end{verbatim}
# Line 108  To obtain the latest sources type: Line 109  To obtain the latest sources type:
109  \end{verbatim}  \end{verbatim}
110  or to get a specific release type:  or to get a specific release type:
111  \begin{verbatim}  \begin{verbatim}
112  % cvs co -d directory -P -r release1_beta1 MITgcm  % cvs co -P -r checkpoint52i_post  MITgcm
113  \end{verbatim}  \end{verbatim}
114  The MITgcm web site contains further directions concerning the source  The MITgcm web site contains further directions concerning the source
115  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
116  that one may easily view the state of files, revisions, and other  that one may easily view the state of files, revisions, and other
117  development milestones:  development milestones:
118  \begin{rawhtml} <A href=http://mitgcm.org/download target="idontexist"> \end{rawhtml}  \begin{rawhtml} <A href=''http://mitgcm.org/download'' target="idontexist"> \end{rawhtml}
119  \begin{verbatim}  \begin{verbatim}
120  http://mitgcm.org/source_code.html  http://mitgcm.org/source_code.html
121  \end{verbatim}  \end{verbatim}
# Line 129  track of your file versions with respect Line 130  track of your file versions with respect
130  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
131  updates.  More extensive information on using CVS for maintaining  updates.  More extensive information on using CVS for maintaining
132  MITgcm code can be found  MITgcm code can be found
133  \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}
134  here  here
135  \begin{rawhtml} </A> \end{rawhtml}  \begin{rawhtml} </A> \end{rawhtml}
136  .  .
# Line 149  The tar file still contains CVS informat Line 150  The tar file still contains CVS informat
150  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
151  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
152  tar file does not exist, then please contact the developers through  tar file does not exist, then please contact the developers through
153  the MITgcm-support list.  the
154    \begin{rawhtml} <A href=''mailto:MITgcm-support@mitgcm.org"> \end{rawhtml}
155    MITgcm-support@mitgcm.org
156    \begin{rawhtml} </A> \end{rawhtml}
157    mailing list.
158    
159  \paragraph*{Upgrading from an earlier version}  \paragraph*{Upgrading from an earlier version}
160    
# Line 161  your copy instead of downloading the ent Line 166  your copy instead of downloading the ent
166  \end{verbatim}  \end{verbatim}
167  and then issue the cvs update command such as:  and then issue the cvs update command such as:
168  \begin{verbatim}  \begin{verbatim}
169  % cvs -q update -r release1_beta1 -d -P  % cvs -q update -r checkpoint52i_post -d -P
170  \end{verbatim}  \end{verbatim}
171  This will update the ``tag'' to ``release1\_beta1'', add any new  This will update the ``tag'' to ``checkpoint52i\_post'', add any new
172  directories (-d) and remove any empty directories (-P). The -q option  directories (-d) and remove any empty directories (-P). The -q option
173  means be quiet which will reduce the number of messages you'll see in  means be quiet which will reduce the number of messages you'll see in
174  the terminal. If you have modified the code prior to upgrading, CVS  the terminal. If you have modified the code prior to upgrading, CVS
# Line 177  If the list of conflicts scrolled off th Line 182  If the list of conflicts scrolled off th
182  cvs update command and it will report the conflicts. Conflicts are  cvs update command and it will report the conflicts. Conflicts are
183  indicated in the code by the delimites ``$<<<<<<<$'', ``======='' and  indicated in the code by the delimites ``$<<<<<<<$'', ``======='' and
184  ``$>>>>>>>$''. For example,  ``$>>>>>>>$''. For example,
185    {\small
186  \begin{verbatim}  \begin{verbatim}
187  <<<<<<< ini_parms.F  <<<<<<< ini_parms.F
188       & bottomDragLinear,myOwnBottomDragCoefficient,       & bottomDragLinear,myOwnBottomDragCoefficient,
# Line 184  indicated in the code by the delimites ` Line 190  indicated in the code by the delimites `
190       & bottomDragLinear,bottomDragQuadratic,       & bottomDragLinear,bottomDragQuadratic,
191  >>>>>>> 1.18  >>>>>>> 1.18
192  \end{verbatim}  \end{verbatim}
193    }
194  means that you added ``myOwnBottomDragCoefficient'' to a namelist at  means that you added ``myOwnBottomDragCoefficient'' to a namelist at
195  the same time and place that we added ``bottomDragQuadratic''. You  the same time and place that we added ``bottomDragQuadratic''. You
196  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
197  changed to:  changed to:
198    {\small
199  \begin{verbatim}  \begin{verbatim}
200       & bottomDragLinear,bottomDragQuadratic,myOwnBottomDragCoefficient,       & bottomDragLinear,bottomDragQuadratic,myOwnBottomDragCoefficient,
201  \end{verbatim}  \end{verbatim}
202    }
203  and the lines with the delimiters ($<<<<<<$,======,$>>>>>>$) be deleted.  and the lines with the delimiters ($<<<<<<$,======,$>>>>>>$) be deleted.
204  Unless you are making modifications which exactly parallel  Unless you are making modifications which exactly parallel
205  developments we make, these types of conflicts should be rare.  developments we make, these types of conflicts should be rare.
# Line 224  model code. The execution environment su Line 233  model code. The execution environment su
233  \textit{eesupp} directory. The grid point model code is held under the  \textit{eesupp} directory. The grid point model code is held under the
234  \textit{model} directory. Code execution actually starts in the  \textit{model} directory. Code execution actually starts in the
235  \textit{eesupp} routines and not in the \textit{model} routines. For  \textit{eesupp} routines and not in the \textit{model} routines. For
236  this reason the top-level  this reason the top-level \textit{MAIN.F} is in the
237  \textit{MAIN.F} is in the \textit{eesupp/src} directory. In general,  \textit{eesupp/src} directory. In general, end-users should not need
238  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
239  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
240  }. 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
241  the root tree (a detailed description is given in section 3: Code structure).  root tree (a detailed description is given in section 3: Code
242    structure).
243    
244  \begin{itemize}  \begin{itemize}
 \item \textit{bin}: this directory is initially empty. It is the default  
 directory in which to compile the code.  
245    
246    \item \textit{bin}: this directory is initially empty. It is the
247      default directory in which to compile the code.
248      
249  \item \textit{diags}: contains the code relative to time-averaged  \item \textit{diags}: contains the code relative to time-averaged
250  diagnostics. It is subdivided into two subdirectories \textit{inc} and    diagnostics. It is subdivided into two subdirectories \textit{inc}
251  \textit{src} that contain include files (*.\textit{h} files) and Fortran    and \textit{src} that contain include files (*.\textit{h} files) and
252  subroutines (*.\textit{F} files), respectively.    Fortran subroutines (*.\textit{F} files), respectively.
253    
254  \item \textit{doc}: contains brief documentation notes.  \item \textit{doc}: contains brief documentation notes.
255      
256  \item \textit{eesupp}: contains the execution environment source code. Also  \item \textit{eesupp}: contains the execution environment source code.
257  subdivided into two subdirectories \textit{inc} and \textit{src}.    Also subdivided into two subdirectories \textit{inc} and
258      \textit{src}.
259  \item \textit{exe}: this directory is initially empty. It is the default    
260  directory in which to execute the code.  \item \textit{exe}: this directory is initially empty. It is the
261      default directory in which to execute the code.
262  \item \textit{model}: this directory contains the main source code. Also    
263  subdivided into two subdirectories \textit{inc} and \textit{src}.  \item \textit{model}: this directory contains the main source code.
264      Also subdivided into two subdirectories \textit{inc} and
265  \item \textit{pkg}: contains the source code for the packages. Each package    \textit{src}.
266  corresponds to a subdirectory. For example, \textit{gmredi} contains the    
267  code related to the Gent-McWilliams/Redi scheme, \textit{aim} the code  \item \textit{pkg}: contains the source code for the packages. Each
268  relative to the atmospheric intermediate physics. The packages are described    package corresponds to a subdirectory. For example, \textit{gmredi}
269  in detail in section 3.    contains the code related to the Gent-McWilliams/Redi scheme,
270      \textit{aim} the code relative to the atmospheric intermediate
271  \item \textit{tools}: this directory contains various useful tools. For    physics. The packages are described in detail in section 3.
272  example, \textit{genmake2} is a script written in csh (C-shell) that should    
273  be used to generate your makefile. The directory \textit{adjoint} contains  \item \textit{tools}: this directory contains various useful tools.
274  the makefile specific to the Tangent linear and Adjoint Compiler (TAMC) that    For example, \textit{genmake2} is a script written in csh (C-shell)
275  generates the adjoint code. The latter is described in details in part V.    that should be used to generate your makefile. The directory
276      \textit{adjoint} contains the makefile specific to the Tangent
277      linear and Adjoint Compiler (TAMC) that generates the adjoint code.
278      The latter is described in details in part V.
279      
280  \item \textit{utils}: this directory contains various utilities. The  \item \textit{utils}: this directory contains various utilities. The
281  subdirectory \textit{knudsen2} contains code and a makefile that    subdirectory \textit{knudsen2} contains code and a makefile that
282  compute coefficients of the polynomial approximation to the knudsen    compute coefficients of the polynomial approximation to the knudsen
283  formula for an ocean nonlinear equation of state. The \textit{matlab}    formula for an ocean nonlinear equation of state. The
284  subdirectory contains matlab scripts for reading model output directly    \textit{matlab} subdirectory contains matlab scripts for reading
285  into matlab. \textit{scripts} contains C-shell post-processing    model output directly into matlab. \textit{scripts} contains C-shell
286  scripts for joining processor-based and tiled-based model output.    post-processing scripts for joining processor-based and tiled-based
287      model output.
288      
289    \item \textit{verification}: this directory contains the model
290      examples. See section \ref{sect:modelExamples}.
291    
 \item \textit{verification}: this directory contains the model examples. See  
 section \ref{sect:modelExamples}.  
292  \end{itemize}  \end{itemize}
293    
294  \section{Example experiments}  \section{Example experiments}
# Line 294  below. Line 310  below.
310  \subsection{Full list of model examples}  \subsection{Full list of model examples}
311    
312  \begin{enumerate}  \begin{enumerate}
313      
314  \item \textit{exp0} - single layer, ocean double gyre (barotropic with  \item \textit{exp0} - single layer, ocean double gyre (barotropic with
315    free-surface). This experiment is described in detail in section    free-surface). This experiment is described in detail in section
316    \ref{sect:eg-baro}.    \ref{sect:eg-baro}.
# Line 383  Each example directory has the following Line 400  Each example directory has the following
400    
401  \begin{itemize}  \begin{itemize}
402  \item \textit{code}: contains the code particular to the example. At a  \item \textit{code}: contains the code particular to the example. At a
403  minimum, this directory includes the following files:    minimum, this directory includes the following files:
404    
405  \begin{itemize}    \begin{itemize}
406  \item \textit{code/CPP\_EEOPTIONS.h}: declares CPP keys relative to    \item \textit{code/CPP\_EEOPTIONS.h}: declares CPP keys relative to
407    the ``execution environment'' part of the code. The default version      the ``execution environment'' part of the code. The default
408    is located in \textit{eesupp/inc}.      version is located in \textit{eesupp/inc}.
409        
410  \item \textit{code/CPP\_OPTIONS.h}: declares CPP keys relative to the    \item \textit{code/CPP\_OPTIONS.h}: declares CPP keys relative to
411    ``numerical model'' part of the code. The default version is located      the ``numerical model'' part of the code. The default version is
412    in \textit{model/inc}.      located in \textit{model/inc}.
413      
414      \item \textit{code/SIZE.h}: declares size of underlying
415        computational grid.  The default version is located in
416        \textit{model/inc}.
417      \end{itemize}
418      
419      In addition, other include files and subroutines might be present in
420      \textit{code} depending on the particular experiment. See Section 2
421      for more details.
422        
 \item \textit{code/SIZE.h}: declares size of underlying computational  
   grid.  The default version is located in \textit{model/inc}.  
 \end{itemize}  
   
 In addition, other include files and subroutines might be present in  
 \textit{code} depending on the particular experiment. See Section 2  
 for more details.  
   
423  \item \textit{input}: contains the input data files required to run  \item \textit{input}: contains the input data files required to run
424    the example. At a minimum, the \textit{input} directory contains the    the example. At a minimum, the \textit{input} directory contains the
425    following files:    following files:
426    
427  \begin{itemize}    \begin{itemize}
428  \item \textit{input/data}: this file, written as a namelist, specifies    \item \textit{input/data}: this file, written as a namelist,
429    the main parameters for the experiment.      specifies the main parameters for the experiment.
430        
431  \item \textit{input/data.pkg}: contains parameters relative to the    \item \textit{input/data.pkg}: contains parameters relative to the
432    packages used in the experiment.      packages used in the experiment.
433        
434  \item \textit{input/eedata}: this file contains ``execution    \item \textit{input/eedata}: this file contains ``execution
435    environment'' data. At present, this consists of a specification of      environment'' data. At present, this consists of a specification
436    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
437    execution.      execution.
438      \end{itemize}
439      
440      In addition, you will also find in this directory the forcing and
441      topography files as well as the files describing the initial state
442      of the experiment.  This varies from experiment to experiment. See
443      section 2 for more details.
444    
445    \item \textit{results}: this directory contains the output file
446      \textit{output.txt} produced by the simulation example. This file is
447      useful for comparison with your own output when you run the
448      experiment.
449  \end{itemize}  \end{itemize}
450    
451  In addition, you will also find in this directory the forcing and topography  Once you have chosen the example you want to run, you are ready to
452  files as well as the files describing the initial state of the experiment.  compile the code.
 This varies from experiment to experiment. See section 2 for more details.  
   
 \item \textit{results}: this directory contains the output file \textit{%  
 output.txt} produced by the simulation example. This file is useful for  
 comparison with your own output when you run the experiment.  
 \end{itemize}  
   
 Once you have chosen the example you want to run, you are ready to compile  
 the code.  
453    
454  \section{Building the code}  \section{Building the code}
455  \label{sect:buildingCode}  \label{sect:buildingCode}
# Line 437  the code. Line 457  the code.
457  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
458  ({\em Makefile}) that allows us to pre-process source files, specify  ({\em Makefile}) that allows us to pre-process source files, specify
459  compiler and optimization options and also figures out any file  compiler and optimization options and also figures out any file
460  dependencies. We supply a script ({\em genmake}), described in section  dependencies. We supply a script ({\em genmake2}), described in
461  \ref{sect:genmake}, that automatically creates the {\em Makefile} for  section \ref{sect:genmake}, that automatically creates the {\em
462  you. You then need to build the dependencies and compile the code.    Makefile} for you. You then need to build the dependencies and
463    compile the code.
464    
465  As an example, let's assume that you want to build and run experiment  As an example, let's assume that you want to build and run experiment
466  \textit{verification/exp2}. The are multiple ways and places to actually  \textit{verification/exp2}. The are multiple ways and places to
467  do this but here let's build the code in  actually do this but here let's build the code in
468  \textit{verification/exp2/input}:  \textit{verification/exp2/input}:
469  \begin{verbatim}  \begin{verbatim}
470  % cd verification/exp2/input  % cd verification/exp2/input
471  \end{verbatim}  \end{verbatim}
472  First, build the {\em Makefile}:  First, build the {\em Makefile}:
473  \begin{verbatim}  \begin{verbatim}
474  % ../../../tools/genmake -mods=../code  % ../../../tools/genmake2 -mods=../code
475  \end{verbatim}  \end{verbatim}
476  The command line option tells {\em genmake} to override model source  The command line option tells {\em genmake} to override model source
477  code with any files in the directory {\em ./code/}.  code with any files in the directory {\em ./code/}.
478    
479  If there is no \textit{.genmakerc} in the \textit{input} directory, you have  On many systems, the {\em genmake2} program will be able to
480  to use the following options when invoking \textit{genmake}:  automatically recognize the hardware, find compilers and other tools
481    within the user's path (``echo \$PATH''), and then choose an
482    appropriate set of options from the files contained in the {\em
483      tools/build\_options} directory.  Under some circumstances, a user
484    may have to create a new ``optfile'' in order to specify the exact
485    combination of compiler, compiler flags, libraries, and other options
486    necessary to build a particular configuration of MITgcm.  In such
487    cases, it is generally helpful to read the existing ``optfiles'' and
488    mimic their syntax.
489    
490    Through the MITgcm-support list, the MITgcm developers are willing to
491    provide help writing or modifing ``optfiles''.  And we encourage users
492    to post new ``optfiles'' (particularly ones for new machines or
493    architectures) to the
494    \begin{rawhtml} <A href=''mailto:MITgcm-support@mitgcm.org"> \end{rawhtml}
495    MITgcm-support@mitgcm.org
496    \begin{rawhtml} </A> \end{rawhtml}
497    list.
498    
499    To specify an optfile to {\em genmake2}, the syntax is:
500  \begin{verbatim}  \begin{verbatim}
501  % ../../../tools/genmake  -mods=../code  % ../../../tools/genmake2 -mods=../code -of /path/to/optfile
502  \end{verbatim}  \end{verbatim}
503    
504  Next, create the dependencies:  Once a {\em Makefile} has been generated, we create the dependencies:
505  \begin{verbatim}  \begin{verbatim}
506  % make depend  % make depend
507  \end{verbatim}  \end{verbatim}
508  This modifies {\em Makefile} by attaching a [long] list of files on  This modifies the {\em Makefile} by attaching a [long] list of files
509  which other files depend. The purpose of this is to reduce  upon which other files depend. The purpose of this is to reduce
510  re-compilation if and when you start to modify the code. {\tt make  re-compilation if and when you start to modify the code. The {\tt make
511  depend} also created links from the model source to this directory.    depend} command also creates links from the model source to this
512    directory.
513    
514  Now compile the code:  Next compile the code:
515  \begin{verbatim}  \begin{verbatim}
516  % make  % make
517  \end{verbatim}  \end{verbatim}
518  The {\tt make} command creates an executable called \textit{mitgcmuv}.  The {\tt make} command creates an executable called \textit{mitgcmuv}.
519    Additional make ``targets'' are defined within the makefile to aid in
520    the production of adjoint and other versions of MITgcm.
521    
522  Now you are ready to run the model. General instructions for doing so are  Now you are ready to run the model. General instructions for doing so are
523  given in section \ref{sect:runModel}. Here, we can run the model with:  given in section \ref{sect:runModel}. Here, we can run the model with:
# Line 492  executable in the {\em input} directory Line 535  executable in the {\em input} directory
535  convenience. You can also configure and compile the code in other  convenience. You can also configure and compile the code in other
536  locations, for example on a scratch disk with out having to copy the  locations, for example on a scratch disk with out having to copy the
537  entire source tree. The only requirement to do so is you have {\tt  entire source tree. The only requirement to do so is you have {\tt
538  genmake} in your path or you know the absolute path to {\tt genmake}.    genmake2} in your path or you know the absolute path to {\tt
539      genmake2}.
540    
541  The following sections outline some possible methods of organizing you  The following sections outline some possible methods of organizing
542  source and data.  your source and data.
543    
544  \subsubsection{Building from the {\em ../code directory}}  \subsubsection{Building from the {\em ../code directory}}
545    
546  This is just as simple as building in the {\em input/} directory:  This is just as simple as building in the {\em input/} directory:
547  \begin{verbatim}  \begin{verbatim}
548  % cd verification/exp2/code  % cd verification/exp2/code
549  % ../../../tools/genmake  % ../../../tools/genmake2
550  % make depend  % make depend
551  % make  % make
552  \end{verbatim}  \end{verbatim}
# Line 531  within {\em verification/exp2/}: Line 575  within {\em verification/exp2/}:
575  % cd verification/exp2  % cd verification/exp2
576  % mkdir build  % mkdir build
577  % cd build  % cd build
578  % ../../../tools/genmake -mods=../code  % ../../../tools/genmake2 -mods=../code
579  % make depend  % make depend
580  % make  % make
581  \end{verbatim}  \end{verbatim}
# Line 553  running in a new directory each time mig Line 597  running in a new directory each time mig
597  % ./mitgcmuv > output.txt  % ./mitgcmuv > output.txt
598  \end{verbatim}  \end{verbatim}
599    
600  \subsubsection{Building from on a scratch disk}  \subsubsection{Building on a scratch disk}
601    
602  Model object files and output data can use up large amounts of disk  Model object files and output data can use up large amounts of disk
603  space so it is often the case that you will be operating on a large  space so it is often the case that you will be operating on a large
# Line 561  scratch disk. Assuming the model source Line 605  scratch disk. Assuming the model source
605  following commands will build the model in {\em /scratch/exp2-run1}:  following commands will build the model in {\em /scratch/exp2-run1}:
606  \begin{verbatim}  \begin{verbatim}
607  % cd /scratch/exp2-run1  % cd /scratch/exp2-run1
608  % ~/MITgcm/tools/genmake -rootdir=~/MITgcm -mods=~/MITgcm/verification/exp2/code  % ~/MITgcm/tools/genmake2 -rootdir=~/MITgcm \
609      -mods=~/MITgcm/verification/exp2/code
610  % make depend  % make depend
611  % make  % make
612  \end{verbatim}  \end{verbatim}
# Line 577  the one experiment: Line 622  the one experiment:
622  % cd /scratch/exp2  % cd /scratch/exp2
623  % mkdir build  % mkdir build
624  % cd build  % cd build
625  % ~/MITgcm/tools/genmake -rootdir=~/MITgcm -mods=~/MITgcm/verification/exp2/code  % ~/MITgcm/tools/genmake2 -rootdir=~/MITgcm \
626      -mods=~/MITgcm/verification/exp2/code
627  % make depend  % make depend
628  % make  % make
629  % cd ../  % cd ../
# Line 588  the one experiment: Line 634  the one experiment:
634    
635    
636    
637  \subsection{\textit{genmake}}  \subsection{Using \textit{genmake2}}
638  \label{sect:genmake}  \label{sect:genmake}
639    
640  To compile the code, use the script \textit{genmake} located in the \textit{%  To compile the code, first use the program \texttt{genmake2} (located
641  tools} directory. \textit{genmake} is a script that generates the makefile.  in the \textit{tools} directory) to generate a Makefile.
642  It has been written so that the code can be compiled on a wide diversity of  \texttt{genmake2} is a shell script written to work with all
643  machines and systems. However, if it doesn't work the first time on your  ``sh''--compatible shells including bash v1, bash v2, and Bourne.
644  platform, you might need to edit certain lines of \textit{genmake} in the  Internally, \texttt{genmake2} determines the locations of needed
645  section containing the setups for the different machines. The file is  files, the compiler, compiler options, libraries, and Unix tools.  It
646  structured like this:  relies upon a number of ``optfiles'' located in the {\em
647  \begin{verbatim}    tools/build\_options} directory.
648          .  
649          .  The purpose of the optfiles is to provide all the compilation options
650          .  for particular ``platforms'' (where ``platform'' roughly means the
651  general instructions (machine independent)  combination of the hardware and the compiler) and code configurations.
652          .  Given the combinations of possible compilers and library dependencies
653          .  ({\it eg.}  MPI and NetCDF) there may be numerous optfiles available
654          .  for a single machine.  The naming scheme for the majority of the
655      - setup machine 1  optfiles shipped with the code is
656      - setup machine 2  \begin{center}
657      - setup machine 3    {\bf OS\_HARDWARE\_COMPILER }
658      - setup machine 4  \end{center}
659         etc  where
660          .  \begin{description}
661          .  \item[OS] is the name of the operating system (generally the
662          .    lower-case output of the {\tt 'uname'} command)
663  \end{verbatim}  \item[HARDWARE] is a string that describes the CPU type and
664      corresponds to output from the  {\tt 'uname -m'} command:
665  For example, the setup corresponding to a DEC alpha machine is reproduced    \begin{description}
666  here:    \item[ia32] is for ``x86'' machines such as i386, i486, i586, i686,
667  \begin{verbatim}      and athlon
668    case OSF1+mpi:    \item[ia64] is for Intel IA64 systems (eg. Itanium, Itanium2)
669      echo "Configuring for DEC Alpha"    \item[amd64] is AMD x86\_64 systems
670      set CPP        = ( '/usr/bin/cpp -P' )    \item[ppc] is for Mac PowerPC systems
671      set DEFINES    = ( ${DEFINES}  '-DTARGET_DEC -DWORDLENGTH=1' )    \end{description}
672      set KPP        = ( 'kapf' )  \item[COMPILER] is the compiler name (generally, the name of the
673      set KPPFILES   = ( 'main.F' )    FORTRAN executable)
674      set KFLAGS1    = ( '-scan=132 -noconc -cmp=' )  \end{description}
     set FC         = ( 'f77' )  
     set FFLAGS     = ( '-convert big_endian -r8 -extend_source -automatic -call_shared -notransform_loops -align dcommons' )  
     set FOPTIM     = ( '-O5 -fast -tune host -inline all' )  
     set NOOPTFLAGS = ( '-O0' )  
     set LIBS       = ( '-lfmpi -lmpi -lkmp_osfp10 -pthread' )  
     set NOOPTFILES = ( 'barrier.F different_multiple.F external_fields_load.F')  
     set RMFILES    = ( '*.p.out' )  
     breaksw  
 \end{verbatim}  
   
 Typically, these are the lines that you might need to edit to make \textit{%  
 genmake} work on your platform if it doesn't work the first time. \textit{%  
 genmake} understands several options that are described here:  
   
 \begin{itemize}  
 \item -rootdir=dir  
   
 indicates where the model root directory is relative to the directory where  
 you are compiling. This option is not needed if you compile in the \textit{%  
 bin} directory (which is the default compilation directory) or within the  
 \textit{verification} tree.  
   
 \item -mods=dir1,dir2,...  
   
 indicates the relative or absolute paths directories where the sources  
 should take precedence over the default versions (located in \textit{model},  
 \textit{eesupp},...). Typically, this option is used when running the  
 examples, see below.  
   
 \item -enable=pkg1,pkg2,...  
   
 enables packages source code \textit{pkg1}, \textit{pkg2},... when creating  
 the makefile.  
   
 \item -disable=pkg1,pkg2,...  
   
 disables packages source code \textit{pkg1}, \textit{pkg2},... when creating  
 the makefile.  
675    
676  \item -platform=machine  In many cases, the default optfiles are sufficient and will result in
677    usable Makefiles.  However, for some machines or code configurations,
678    new ``optfiles'' must be written. To create a new optfile, it is
679    generally best to start with one of the defaults and modify it to suit
680    your needs.  Like \texttt{genmake2}, the optfiles are all written
681    using a simple ``sh''--compatible syntax.  While nearly all variables
682    used within \texttt{genmake2} may be specified in the optfiles, the
683    critical ones that should be defined are:
684    
685  specifies the platform for which you want the makefile. In general, you  \begin{description}
686  won't need this option. \textit{genmake} will select the right machine for  \item[FC] the FORTRAN compiler (executable) to use
687  you (the one you're working on!). However, this option is useful if you have  \item[DEFINES] the command-line DEFINE options passed to the compiler
688  a choice of several compilers on one machine and you want to use the one  \item[CPP] the C pre-processor to use
689  that is not the default (ex: \texttt{pgf77} instead of \texttt{f77} under  \item[NOOPTFLAGS] options flags for special files that should not be
690  Linux).    optimized
691    \end{description}
692    
693  \item -mpi  For example, the optfile for a typical Red Hat Linux machine (``ia32''
694    architecture) using the GCC (g77) compiler is
695    \begin{verbatim}
696    FC=g77
697    DEFINES='-D_BYTESWAPIO -DWORDLENGTH=4'
698    CPP='cpp  -traditional -P'
699    NOOPTFLAGS='-O0'
700    #  For IEEE, use the "-ffloat-store" option
701    if test "x$IEEE" = x ; then
702        FFLAGS='-Wimplicit -Wunused -Wuninitialized'
703        FOPTIM='-O3 -malign-double -funroll-loops'
704    else
705        FFLAGS='-Wimplicit -Wunused -ffloat-store'
706        FOPTIM='-O0 -malign-double'
707    fi
708    \end{verbatim}
709    
710    If you write an optfile for an unrepresented machine or compiler, you
711    are strongly encouraged to submit the optfile to the MITgcm project
712    for inclusion.  Please send the file to the
713    \begin{rawhtml} <A href="mail-to:MITgcm-support@mitgcm.org"> \end{rawhtml}
714    \begin{center}
715      MITgcm-support@mitgcm.org
716    \end{center}
717    \begin{rawhtml} </A> \end{rawhtml}
718    mailing list.
719    
720  this is used when you want to run the model in parallel processing mode  In addition to the optfiles, \texttt{genmake2} supports a number of
721  under mpi (see section on parallel computation for more details).  helpful command-line options.  A complete list of these options can be
722    obtained from:
723    \begin{verbatim}
724    % genmake2 -h
725    \end{verbatim}
726    
727  \item -jam  The most important command-line options are:
728    \begin{description}
729      
730    \item[\texttt{--optfile=/PATH/FILENAME}] specifies the optfile that
731      should be used for a particular build.
732      
733      If no "optfile" is specified (either through the command line or the
734      MITGCM\_OPTFILE environment variable), genmake2 will try to make a
735      reasonable guess from the list provided in {\em
736        tools/build\_options}.  The method used for making this guess is
737      to first determine the combination of operating system and hardware
738      (eg. "linux\_ia32") and then find a working FORTRAN compiler within
739      the user's path.  When these three items have been identified,
740      genmake2 will try to find an optfile that has a matching name.
741      
742    \item[\texttt{--pdepend=/PATH/FILENAME}] specifies the dependency file
743      used for packages.
744      
745      If not specified, the default dependency file {\em pkg/pkg\_depend}
746      is used.  The syntax for this file is parsed on a line-by-line basis
747      where each line containes either a comment ("\#") or a simple
748      "PKGNAME1 (+|-)PKGNAME2" pairwise rule where the "+" or "-" symbol
749      specifies a "must be used with" or a "must not be used with"
750      relationship, respectively.  If no rule is specified, then it is
751      assumed that the two packages are compatible and will function
752      either with or without each other.
753      
754    \item[\texttt{--pdefault='PKG1 PKG2 PKG3 ...'}] specifies the default
755      set of packages to be used.
756      
757      If not set, the default package list will be read from {\em
758        pkg/pkg\_default}
759      
760    \item[\texttt{--adof=/path/to/file}] specifies the "adjoint" or
761      automatic differentiation options file to be used.  The file is
762      analogous to the ``optfile'' defined above but it specifies
763      information for the AD build process.
764      
765      The default file is located in {\em
766        tools/adjoint\_options/adjoint\_default} and it defines the "TAF"
767      and "TAMC" compilers.  An alternate version is also available at
768      {\em tools/adjoint\_options/adjoint\_staf} that selects the newer
769      "STAF" compiler.  As with any compilers, it is helpful to have their
770      directories listed in your {\tt \$PATH} environment variable.
771      
772    \item[\texttt{--mods='DIR1 DIR2 DIR3 ...'}] specifies a list of
773      directories containing ``modifications''.  These directories contain
774      files with names that may (or may not) exist in the main MITgcm
775      source tree but will be overridden by any identically-named sources
776      within the ``MODS'' directories.
777      
778      The order of precedence for this "name-hiding" is as follows:
779      \begin{itemize}
780      \item ``MODS'' directories (in the order given)
781      \item Packages either explicitly specified or provided by default
782        (in the order given)
783      \item Packages included due to package dependencies (in the order
784        that that package dependencies are parsed)
785      \item The "standard dirs" (which may have been specified by the
786        ``-standarddirs'' option)
787      \end{itemize}
788      
789    \item[\texttt{--make=/path/to/gmake}] Due to the poor handling of
790      soft-links and other bugs common with the \texttt{make} versions
791      provided by commercial Unix vendors, GNU \texttt{make} (sometimes
792      called \texttt{gmake}) should be preferred.  This option provides a
793      means for specifying the make executable to be used.
794    
795  this is used when you want to run the model in parallel processing mode  \end{description}
 under jam (see section on parallel computation for more details).  
 \end{itemize}  
796    
 For some of the examples, there is a file called \textit{.genmakerc} in the  
 \textit{input} directory that has the relevant \textit{genmake} options for  
 that particular example. In this way you don't need to type the options when  
 invoking \textit{genmake}.  
797    
798    
799  \section{Running the model}  \section{Running the model}
# Line 714  normally re-direct the {\em stdout} stre Line 819  normally re-direct the {\em stdout} stre
819  % ./mitgcmuv > output.txt  % ./mitgcmuv > output.txt
820  \end{verbatim}  \end{verbatim}
821    
822  For the example experiments in {\em vericication}, an example of the  For the example experiments in {\em verification}, an example of the
823  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
824  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.
825    
# Line 803  Some examples of reading and visualizing Line 908  Some examples of reading and visualizing
908  \section{Doing it yourself: customizing the code}  \section{Doing it yourself: customizing the code}
909    
910  When you are ready to run the model in the configuration you want, the  When you are ready to run the model in the configuration you want, the
911  easiest thing is to use and adapt the setup of the case studies experiment  easiest thing is to use and adapt the setup of the case studies
912  (described previously) that is the closest to your configuration. Then, the  experiment (described previously) that is the closest to your
913  amount of setup will be minimized. In this section, we focus on the setup  configuration. Then, the amount of setup will be minimized. In this
914  relative to the ''numerical model'' part of the code (the setup relative to  section, we focus on the setup relative to the ``numerical model''
915  the ''execution environment'' part is covered in the parallel implementation  part of the code (the setup relative to the ``execution environment''
916  section) and on the variables and parameters that you are likely to change.  part is covered in the parallel implementation section) and on the
917    variables and parameters that you are likely to change.
918    
919  \subsection{Configuration and setup}  \subsection{Configuration and setup}
920    
921  The CPP keys relative to the ''numerical model'' part of the code are all  The CPP keys relative to the ``numerical model'' part of the code are
922  defined and set in the file \textit{CPP\_OPTIONS.h }in the directory \textit{%  all defined and set in the file \textit{CPP\_OPTIONS.h }in the
923  model/inc }or in one of the \textit{code }directories of the case study  directory \textit{ model/inc }or in one of the \textit{code
924  experiments under \textit{verification.} The model parameters are defined  }directories of the case study experiments under
925  and declared in the file \textit{model/inc/PARAMS.h }and their default  \textit{verification.} The model parameters are defined and declared
926  values are set in the routine \textit{model/src/set\_defaults.F. }The  in the file \textit{model/inc/PARAMS.h }and their default values are
927  default values can be modified in the namelist file \textit{data }which  set in the routine \textit{model/src/set\_defaults.F. }The default
928  needs to be located in the directory where you will run the model. The  values can be modified in the namelist file \textit{data }which needs
929  parameters are initialized in the routine \textit{model/src/ini\_parms.F}.  to be located in the directory where you will run the model. The
930  Look at this routine to see in what part of the namelist the parameters are  parameters are initialized in the routine
931  located.  \textit{model/src/ini\_parms.F}.  Look at this routine to see in what
932    part of the namelist the parameters are located.
933  In what follows the parameters are grouped into categories related to the  
934  computational domain, the equations solved in the model, and the simulation  In what follows the parameters are grouped into categories related to
935  controls.  the computational domain, the equations solved in the model, and the
936    simulation controls.
937    
938  \subsection{Computational domain, geometry and time-discretization}  \subsection{Computational domain, geometry and time-discretization}
939    
940  \begin{itemize}  \begin{description}
941  \item dimensions  \item[dimensions] \
942  \end{itemize}    
943      The number of points in the x, y,\textit{\ }and r\textit{\
944  The number of points in the x, y,\textit{\ }and r\textit{\ }directions are    }directions are represented by the variables \textbf{sNx}\textit{,
945  represented by the variables \textbf{sNx}\textit{, }\textbf{sNy}\textit{, }%    }\textbf{sNy}\textit{, } and \textbf{Nr}\textit{\ }respectively
946  and \textbf{Nr}\textit{\ }respectively which are declared and set in the    which are declared and set in the file \textit{model/inc/SIZE.h.
947  file \textit{model/inc/SIZE.h. }(Again, this assumes a mono-processor    }(Again, this assumes a mono-processor calculation. For
948  calculation. For multiprocessor calculations see section on parallel    multiprocessor calculations see section on parallel implementation.)
949  implementation.)  
950    \item[grid] \
951  \begin{itemize}    
952  \item grid    Three different grids are available: cartesian, spherical polar, and
953  \end{itemize}    curvilinear (including the cubed sphere). The grid is set through
954      the logical variables \textbf{usingCartesianGrid}\textit{, }\textbf{
955  Three different grids are available: cartesian, spherical polar, and      usingSphericalPolarGrid}\textit{, }and \textit{\ }\textbf{
956  curvilinear (including the cubed sphere). The grid is set through the      usingCurvilinearGrid}\textit{. }In the case of spherical and
957  logical variables \textbf{usingCartesianGrid}\textit{, }\textbf{%    curvilinear grids, the southern boundary is defined through the
958  usingSphericalPolarGrid}\textit{, }and \textit{\ }\textbf{%    variable \textbf{phiMin} \textit{\ }which corresponds to the
959  usingCurvilinearGrid}\textit{. }In the case of spherical and curvilinear    latitude of the southern most cell face (in degrees). The resolution
960  grids, the southern boundary is defined through the variable \textbf{phiMin}%    along the x and y directions is controlled by the 1D arrays
961  \textit{\ }which corresponds to the latitude of the southern most cell face    \textbf{delx}\textit{\ }and \textbf{dely}\textit{\ }(in meters in
962  (in degrees). The resolution along the x and y directions is controlled by    the case of a cartesian grid, in degrees otherwise). The vertical
963  the 1D arrays \textbf{delx}\textit{\ }and \textbf{dely}\textit{\ }(in meters    grid spacing is set through the 1D array \textbf{delz }for the ocean
964  in the case of a cartesian grid, in degrees otherwise). The vertical grid    (in meters) or \textbf{delp}\textit{\ }for the atmosphere (in Pa).
965  spacing is set through the 1D array \textbf{delz }for the ocean (in meters)    The variable \textbf{ Ro\_SeaLevel} represents the standard position
966  or \textbf{delp}\textit{\ }for the atmosphere (in Pa). The variable \textbf{%    of Sea-Level in ''R'' coordinate. This is typically set to 0m for
967  Ro\_SeaLevel} represents the standard position of Sea-Level in ''R''    the ocean (default value) and 10$ ^{5}$Pa for the atmosphere. For
968  coordinate. This is typically set to 0m for the ocean (default value) and 10$%    the atmosphere, also set the logical variable \textbf{groundAtK1} to
969  ^{5}$Pa for the atmosphere. For the atmosphere, also set the logical    '.\texttt{TRUE}.'. which put the first level (k=1) at the lower
970  variable \textbf{groundAtK1} to '.\texttt{TRUE}.'. which put the first level    boundary (ground).
971  (k=1) at the lower boundary (ground).    
972      For the cartesian grid case, the Coriolis parameter $f$ is set
973  For the cartesian grid case, the Coriolis parameter $f$ is set through the    through the variables \textbf{f0}\textit{\ }and
974  variables \textbf{f0}\textit{\ }and \textbf{beta}\textit{\ }which correspond    \textbf{beta}\textit{\ }which correspond to the reference Coriolis
975  to the reference Coriolis parameter (in s$^{-1}$) and $\frac{\partial f}{%    parameter (in s$^{-1}$) and $\frac{\partial f}{ \partial y}$(in
976  \partial y}$(in m$^{-1}$s$^{-1}$) respectively. If \textbf{beta }\textit{\ }%    m$^{-1}$s$^{-1}$) respectively. If \textbf{beta }\textit{\ } is set
977  is set to a nonzero value, \textbf{f0}\textit{\ }is the value of $f$ at the    to a nonzero value, \textbf{f0}\textit{\ }is the value of $f$ at the
978  southern edge of the domain.    southern edge of the domain.
979    
980  \begin{itemize}  \item[topography - full and partial cells] \
981  \item topography - full and partial cells    
982  \end{itemize}    The domain bathymetry is read from a file that contains a 2D (x,y)
983      map of depths (in m) for the ocean or pressures (in Pa) for the
984  The domain bathymetry is read from a file that contains a 2D (x,y) map of    atmosphere. The file name is represented by the variable
985  depths (in m) for the ocean or pressures (in Pa) for the atmosphere. The    \textbf{bathyFile}\textit{. }The file is assumed to contain binary
986  file name is represented by the variable \textbf{bathyFile}\textit{. }The    numbers giving the depth (pressure) of the model at each grid cell,
987  file is assumed to contain binary numbers giving the depth (pressure) of the    ordered with the x coordinate varying fastest. The points are
988  model at each grid cell, ordered with the x coordinate varying fastest. The    ordered from low coordinate to high coordinate for both axes. The
989  points are ordered from low coordinate to high coordinate for both axes. The    model code applies without modification to enclosed, periodic, and
990  model code applies without modification to enclosed, periodic, and double    double periodic domains. Periodicity is assumed by default and is
991  periodic domains. Periodicity is assumed by default and is suppressed by    suppressed by setting the depths to 0m for the cells at the limits
992  setting the depths to 0m for the cells at the limits of the computational    of the computational domain (note: not sure this is the case for the
993  domain (note: not sure this is the case for the atmosphere). The precision    atmosphere). The precision with which to read the binary data is
994  with which to read the binary data is controlled by the integer variable    controlled by the integer variable \textbf{readBinaryPrec }which can
995  \textbf{readBinaryPrec }which can take the value \texttt{32} (single    take the value \texttt{32} (single precision) or \texttt{64} (double
996  precision) or \texttt{64} (double precision). See the matlab program \textit{%    precision). See the matlab program \textit{ gendata.m }in the
997  gendata.m }in the \textit{input }directories under \textit{verification }to    \textit{input }directories under \textit{verification }to see how
998  see how the bathymetry files are generated for the case study experiments.    the bathymetry files are generated for the case study experiments.
999      
1000  To use the partial cell capability, the variable \textbf{hFacMin}\textit{\ }%    To use the partial cell capability, the variable
1001  needs to be set to a value between 0 and 1 (it is set to 1 by default)    \textbf{hFacMin}\textit{\ } needs to be set to a value between 0 and
1002  corresponding to the minimum fractional size of the cell. For example if the    1 (it is set to 1 by default) corresponding to the minimum
1003  bottom cell is 500m thick and \textbf{hFacMin}\textit{\ }is set to 0.1, the    fractional size of the cell. For example if the bottom cell is 500m
1004  actual thickness of the cell (i.e. used in the code) can cover a range of    thick and \textbf{hFacMin}\textit{\ }is set to 0.1, the actual
1005  discrete values 50m apart from 50m to 500m depending on the value of the    thickness of the cell (i.e. used in the code) can cover a range of
1006  bottom depth (in \textbf{bathyFile}) at this point.    discrete values 50m apart from 50m to 500m depending on the value of
1007      the bottom depth (in \textbf{bathyFile}) at this point.
1008  Note that the bottom depths (or pressures) need not coincide with the models    
1009  levels as deduced from \textbf{delz}\textit{\ }or\textit{\ }\textbf{delp}%    Note that the bottom depths (or pressures) need not coincide with
1010  \textit{. }The model will interpolate the numbers in \textbf{bathyFile}%    the models levels as deduced from \textbf{delz}\textit{\
1011  \textit{\ }so that they match the levels obtained from \textbf{delz}\textit{%    }or\textit{\ }\textbf{delp} \textit{. }The model will interpolate
1012  \ }or\textit{\ }\textbf{delp}\textit{\ }and \textbf{hFacMin}\textit{. }    the numbers in \textbf{bathyFile} \textit{\ }so that they match the
1013      levels obtained from \textbf{delz}\textit{ \ }or\textit{\
1014  (Note: the atmospheric case is a bit more complicated than what is written    }\textbf{delp}\textit{\ }and \textbf{hFacMin}\textit{. }
1015  here I think. To come soon...)    
1016      (Note: the atmospheric case is a bit more complicated than what is
1017      written here I think. To come soon...)
1018    
1019    \item[time-discretization] \
1020      
1021      The time steps are set through the real variables \textbf{deltaTMom}
1022      and \textbf{deltaTtracer} (in s) which represent the time step for
1023      the momentum and tracer equations, respectively. For synchronous
1024      integrations, simply set the two variables to the same value (or you
1025      can prescribe one time step only through the variable
1026      \textbf{deltaT}). The Adams-Bashforth stabilizing parameter is set
1027      through the variable \textbf{abEps} (dimensionless). The stagger
1028      baroclinic time stepping can be activated by setting the logical
1029      variable \textbf{staggerTimeStep} to '.\texttt{TRUE}.'.
1030    
1031  \begin{itemize}  \end{description}
 \item time-discretization  
 \end{itemize}  
1032    
 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}.'.  
1033    
1034  \subsection{Equation of state}  \subsection{Equation of state}
1035    
# Line 991  useCoriolis, momPressureForcing, momStep Line 1101  useCoriolis, momPressureForcing, momStep
1101  Look at the file \textit{model/inc/PARAMS.h }for a precise definition of  Look at the file \textit{model/inc/PARAMS.h }for a precise definition of
1102  these variables.  these variables.
1103    
1104  \begin{itemize}  \begin{description}
1105  \item initialization  \item[initialization] \
1106  \end{itemize}    
1107      The velocity components are initialized to 0 unless the simulation
1108  The velocity components are initialized to 0 unless the simulation is    is starting from a pickup file (see section on simulation control
1109  starting from a pickup file (see section on simulation control parameters).    parameters).
1110    
1111  \begin{itemize}  \item[forcing] \
1112  \item forcing    
1113  \end{itemize}    This section only applies to the ocean. You need to generate
1114      wind-stress data into two files \textbf{zonalWindFile}\textit{\ }and
1115  This section only applies to the ocean. You need to generate wind-stress    \textbf{ meridWindFile }corresponding to the zonal and meridional
1116  data into two files \textbf{zonalWindFile}\textit{\ }and \textbf{%    components of the wind stress, respectively (if you want the stress
1117  meridWindFile }corresponding to the zonal and meridional components of the    to be along the direction of only one of the model horizontal axes,
1118  wind stress, respectively (if you want the stress to be along the direction    you only need to generate one file). The format of the files is
1119  of only one of the model horizontal axes, you only need to generate one    similar to the bathymetry file. The zonal (meridional) stress data
1120  file). The format of the files is similar to the bathymetry file. The zonal    are assumed to be in Pa and located at U-points (V-points). As for
1121  (meridional) stress data are assumed to be in Pa and located at U-points    the bathymetry, the precision with which to read the binary data is
1122  (V-points). As for the bathymetry, the precision with which to read the    controlled by the variable \textbf{readBinaryPrec}.\textbf{\ } See
1123  binary data is controlled by the variable \textbf{readBinaryPrec}.\textbf{\ }    the matlab program \textit{gendata.m }in the \textit{input
1124  See the matlab program \textit{gendata.m }in the \textit{input }directories    }directories under \textit{verification }to see how simple
1125  under \textit{verification }to see how simple analytical wind forcing data    analytical wind forcing data are generated for the case study
1126  are generated for the case study experiments.    experiments.
1127      
1128  There is also the possibility of prescribing time-dependent periodic    There is also the possibility of prescribing time-dependent periodic
1129  forcing. To do this, concatenate the successive time records into a single    forcing. To do this, concatenate the successive time records into a
1130  file (for each stress component) ordered in a (x, y, t) fashion and set the    single file (for each stress component) ordered in a (x, y, t)
1131  following variables: \textbf{periodicExternalForcing }to '.\texttt{TRUE}.',    fashion and set the following variables:
1132  \textbf{externForcingPeriod }to the period (in s) of which the forcing    \textbf{periodicExternalForcing }to '.\texttt{TRUE}.',
1133  varies (typically 1 month), and \textbf{externForcingCycle }to the repeat    \textbf{externForcingPeriod }to the period (in s) of which the
1134  time (in s) of the forcing (typically 1 year -- note: \textbf{%    forcing varies (typically 1 month), and \textbf{externForcingCycle
1135  externForcingCycle }must be a multiple of \textbf{externForcingPeriod}).    }to the repeat time (in s) of the forcing (typically 1 year -- note:
1136  With these variables set up, the model will interpolate the forcing linearly    \textbf{ externForcingCycle }must be a multiple of
1137  at each iteration.    \textbf{externForcingPeriod}).  With these variables set up, the
1138      model will interpolate the forcing linearly at each iteration.
1139  \begin{itemize}  
1140  \item dissipation  \item[dissipation] \
1141  \end{itemize}    
1142      The lateral eddy viscosity coefficient is specified through the
1143  The lateral eddy viscosity coefficient is specified through the variable    variable \textbf{viscAh}\textit{\ }(in m$^{2}$s$^{-1}$). The
1144  \textbf{viscAh}\textit{\ }(in m$^{2}$s$^{-1}$). The vertical eddy viscosity    vertical eddy viscosity coefficient is specified through the
1145  coefficient is specified through the variable \textbf{viscAz }(in m$^{2}$s$%    variable \textbf{viscAz }(in m$^{2}$s$ ^{-1}$) for the ocean and
1146  ^{-1}$) for the ocean and \textbf{viscAp}\textit{\ }(in Pa$^{2}$s$^{-1}$)    \textbf{viscAp}\textit{\ }(in Pa$^{2}$s$^{-1}$) for the atmosphere.
1147  for the atmosphere. The vertical diffusive fluxes can be computed implicitly    The vertical diffusive fluxes can be computed implicitly by setting
1148  by setting the logical variable \textbf{implicitViscosity }to '.\texttt{TRUE}%    the logical variable \textbf{implicitViscosity }to '.\texttt{TRUE}
1149  .'. In addition, biharmonic mixing can be added as well through the variable    .'. In addition, biharmonic mixing can be added as well through the
1150  \textbf{viscA4}\textit{\ }(in m$^{4}$s$^{-1}$). On a spherical polar grid,    variable \textbf{viscA4}\textit{\ }(in m$^{4}$s$^{-1}$). On a
1151  you might also need to set the variable \textbf{cosPower} which is set to 0    spherical polar grid, you might also need to set the variable
1152  by default and which represents the power of cosine of latitude to multiply    \textbf{cosPower} which is set to 0 by default and which represents
1153  viscosity. Slip or no-slip conditions at lateral and bottom boundaries are    the power of cosine of latitude to multiply viscosity. Slip or
1154  specified through the logical variables \textbf{no\_slip\_sides}\textit{\ }%    no-slip conditions at lateral and bottom boundaries are specified
1155  and \textbf{no\_slip\_bottom}. If set to '\texttt{.FALSE.}', free-slip    through the logical variables \textbf{no\_slip\_sides}\textit{\ }
1156  boundary conditions are applied. If no-slip boundary conditions are applied    and \textbf{no\_slip\_bottom}. If set to '\texttt{.FALSE.}',
1157  at the bottom, a bottom drag can be applied as well. Two forms are    free-slip boundary conditions are applied. If no-slip boundary
1158  available: linear (set the variable \textbf{bottomDragLinear}\textit{\ }in s$%    conditions are applied at the bottom, a bottom drag can be applied
1159  ^{-1}$) and quadratic (set the variable \textbf{bottomDragQuadratic}\textit{%    as well. Two forms are available: linear (set the variable
1160  \ }in m$^{-1}$).    \textbf{bottomDragLinear}\textit{\ }in s$ ^{-1}$) and quadratic (set
1161      the variable \textbf{bottomDragQuadratic}\textit{ \ }in m$^{-1}$).
1162  The Fourier and Shapiro filters are described elsewhere.  
1163      The Fourier and Shapiro filters are described elsewhere.
1164  \begin{itemize}  
1165  \item C-D scheme  \item[C-D scheme] \
1166  \end{itemize}    
1167      If you run at a sufficiently coarse resolution, you will need the
1168      C-D scheme for the computation of the Coriolis terms. The
1169      variable\textbf{\ tauCD}, which represents the C-D scheme coupling
1170      timescale (in s) needs to be set.
1171      
1172    \item[calculation of pressure/geopotential] \
1173      
1174      First, to run a non-hydrostatic ocean simulation, set the logical
1175      variable \textbf{nonHydrostatic} to '.\texttt{TRUE}.'. The pressure
1176      field is then inverted through a 3D elliptic equation. (Note: this
1177      capability is not available for the atmosphere yet.) By default, a
1178      hydrostatic simulation is assumed and a 2D elliptic equation is used
1179      to invert the pressure field. The parameters controlling the
1180      behaviour of the elliptic solvers are the variables
1181      \textbf{cg2dMaxIters}\textit{\ }and \textbf{cg2dTargetResidual } for
1182      the 2D case and \textbf{cg3dMaxIters}\textit{\ }and \textbf{
1183        cg3dTargetResidual }for the 3D case. You probably won't need to
1184      alter the default values (are we sure of this?).
1185      
1186      For the calculation of the surface pressure (for the ocean) or
1187      surface geopotential (for the atmosphere) you need to set the
1188      logical variables \textbf{rigidLid} and
1189      \textbf{implicitFreeSurface}\textit{\ }(set one to '.
1190      \texttt{TRUE}.' and the other to '.\texttt{FALSE}.' depending on how
1191      you want to deal with the ocean upper or atmosphere lower boundary).
1192    
1193  If you run at a sufficiently coarse resolution, you will need the C-D scheme  \end{description}
 for the computation of the Coriolis terms. The variable\textbf{\ tauCD},  
 which represents the C-D scheme coupling timescale (in s) needs to be set.  
   
 \begin{itemize}  
 \item calculation of pressure/geopotential  
 \end{itemize}  
   
 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  
 parameters controlling the behaviour of the elliptic solvers are the  
 variables \textbf{cg2dMaxIters}\textit{\ }and \textbf{cg2dTargetResidual }%  
 for the 2D case and \textbf{cg3dMaxIters}\textit{\ }and \textbf{%  
 cg3dTargetResidual }for the 3D case. You probably won't need to alter the  
 default values (are we sure of this?).  
   
 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).  
1194    
1195  \subsection{Tracer equations}  \subsection{Tracer equations}
1196    
# Line 1086  This section covers the tracer equations Line 1198  This section covers the tracer equations
1198  equation and the salinity (for the ocean) or specific humidity (for the  equation and the salinity (for the ocean) or specific humidity (for the
1199  atmosphere) equation. As for the momentum equations, we only describe for  atmosphere) equation. As for the momentum equations, we only describe for
1200  now the parameters that you are likely to change. The logical variables  now the parameters that you are likely to change. The logical variables
1201  \textbf{tempDiffusion}\textit{, }\textbf{tempAdvection}\textit{, }\textbf{%  \textbf{tempDiffusion}\textit{, }\textbf{tempAdvection}\textit{, }\textbf{
1202  tempForcing}\textit{,} and \textbf{tempStepping} allow you to turn on/off  tempForcing}\textit{,} and \textbf{tempStepping} allow you to turn on/off
1203  terms in the temperature equation (same thing for salinity or specific  terms in the temperature equation (same thing for salinity or specific
1204  humidity with variables \textbf{saltDiffusion}\textit{, }\textbf{%  humidity with variables \textbf{saltDiffusion}\textit{, }\textbf{
1205  saltAdvection}\textit{\ }etc). These variables are all assumed here to be  saltAdvection}\textit{\ }etc). These variables are all assumed here to be
1206  set to '.\texttt{TRUE}.'. Look at file \textit{model/inc/PARAMS.h }for a  set to '.\texttt{TRUE}.'. Look at file \textit{model/inc/PARAMS.h }for a
1207  precise definition.  precise definition.
1208    
1209  \begin{itemize}  \begin{description}
1210  \item initialization  \item[initialization] \
1211  \end{itemize}    
1212      The initial tracer data can be contained in the binary files
1213  The initial tracer data can be contained in the binary files \textbf{%    \textbf{ hydrogThetaFile }and \textbf{hydrogSaltFile}. These files
1214  hydrogThetaFile }and \textbf{hydrogSaltFile}. These files should contain 3D    should contain 3D data ordered in an (x, y, r) fashion with k=1 as
1215  data ordered in an (x, y, r) fashion with k=1 as the first vertical level.    the first vertical level.  If no file names are provided, the
1216  If no file names are provided, the tracers are then initialized with the    tracers are then initialized with the values of \textbf{tRef }and
1217  values of \textbf{tRef }and \textbf{sRef }mentioned above (in the equation    \textbf{sRef }mentioned above (in the equation of state section). In
1218  of state section). In this case, the initial tracer data are uniform in x    this case, the initial tracer data are uniform in x and y for each
1219  and y for each depth level.    depth level.
1220    
1221  \begin{itemize}  \item[forcing] \
1222  \item forcing    
1223  \end{itemize}    This part is more relevant for the ocean, the procedure for the
1224      atmosphere not being completely stabilized at the moment.
1225  This part is more relevant for the ocean, the procedure for the atmosphere    
1226  not being completely stabilized at the moment.    A combination of fluxes data and relaxation terms can be used for
1227      driving the tracer equations. \ For potential temperature, heat flux
1228  A combination of fluxes data and relaxation terms can be used for driving    data (in W/m$ ^{2}$) can be stored in the 2D binary file
1229  the tracer equations. \ For potential temperature, heat flux data (in W/m$%    \textbf{surfQfile}\textit{. }  Alternatively or in addition, the
1230  ^{2}$) can be stored in the 2D binary file \textbf{surfQfile}\textit{. }%    forcing can be specified through a relaxation term. The SST data to
1231  Alternatively or in addition, the forcing can be specified through a    which the model surface temperatures are restored to are supposed to
1232  relaxation term. The SST data to which the model surface temperatures are    be stored in the 2D binary file \textbf{ thetaClimFile}\textit{.
1233  restored to are supposed to be stored in the 2D binary file \textbf{%    }The corresponding relaxation time scale coefficient is set through
1234  thetaClimFile}\textit{. }The corresponding relaxation time scale coefficient    the variable \textbf{tauThetaClimRelax}\textit{\ }(in s). The same
1235  is set through the variable \textbf{tauThetaClimRelax}\textit{\ }(in s). The    procedure applies for salinity with the variable names
1236  same procedure applies for salinity with the variable names \textbf{EmPmRfile%    \textbf{EmPmRfile }\textit{, }\textbf{saltClimFile}\textit{, }and
1237  }\textit{, }\textbf{saltClimFile}\textit{, }and \textbf{tauSaltClimRelax}%    \textbf{tauSaltClimRelax} \textit{\ }for freshwater flux (in m/s)
1238  \textit{\ }for freshwater flux (in m/s) and surface salinity (in ppt) data    and surface salinity (in ppt) data files and relaxation time scale
1239  files and relaxation time scale coefficient (in s), respectively. Also for    coefficient (in s), respectively. Also for salinity, if the CPP key
1240  salinity, if the CPP key \textbf{USE\_NATURAL\_BCS} is turned on, natural    \textbf{USE\_NATURAL\_BCS} is turned on, natural boundary conditions
1241  boundary conditions are applied i.e. when computing the surface salinity    are applied i.e. when computing the surface salinity tendency, the
1242  tendency, the freshwater flux is multiplied by the model surface salinity    freshwater flux is multiplied by the model surface salinity instead
1243  instead of a constant salinity value.    of a constant salinity value.
1244      
1245  As for the other input files, the precision with which to read the data is    As for the other input files, the precision with which to read the
1246  controlled by the variable \textbf{readBinaryPrec}. Time-dependent, periodic    data is controlled by the variable \textbf{readBinaryPrec}.
1247  forcing can be applied as well following the same procedure used for the    Time-dependent, periodic forcing can be applied as well following
1248  wind forcing data (see above).    the same procedure used for the wind forcing data (see above).
1249    
1250  \begin{itemize}  \item[dissipation] \
1251  \item dissipation    
1252  \end{itemize}    Lateral eddy diffusivities for temperature and salinity/specific
1253      humidity are specified through the variables \textbf{diffKhT }and
1254  Lateral eddy diffusivities for temperature and salinity/specific humidity    \textbf{diffKhS } (in m$^{2}$/s). Vertical eddy diffusivities are
1255  are specified through the variables \textbf{diffKhT }and \textbf{diffKhS }%    specified through the variables \textbf{diffKzT }and \textbf{diffKzS
1256  (in m$^{2}$/s). Vertical eddy diffusivities are specified through the    }(in m$^{2}$/s) for the ocean and \textbf{diffKpT }and
1257  variables \textbf{diffKzT }and \textbf{diffKzS }(in m$^{2}$/s) for the ocean    \textbf{diffKpS }(in Pa$^{2}$/s) for the atmosphere. The vertical
1258  and \textbf{diffKpT }and \textbf{diffKpS }(in Pa$^{2}$/s) for the    diffusive fluxes can be computed implicitly by setting the logical
1259  atmosphere. The vertical diffusive fluxes can be computed implicitly by    variable \textbf{implicitDiffusion }to '.\texttt{TRUE} .'. In
1260  setting the logical variable \textbf{implicitDiffusion }to '.\texttt{TRUE}%    addition, biharmonic diffusivities can be specified as well through
1261  .'. In addition, biharmonic diffusivities can be specified as well through    the coefficients \textbf{diffK4T }and \textbf{diffK4S }(in
1262  the coefficients \textbf{diffK4T }and \textbf{diffK4S }(in m$^{4}$/s). Note    m$^{4}$/s). Note that the cosine power scaling (specified through
1263  that the cosine power scaling (specified through \textbf{cosPower }- see the    \textbf{cosPower }- see the momentum equations section) is applied
1264  momentum equations section) is applied to the tracer diffusivities    to the tracer diffusivities (Laplacian and biharmonic) as well. The
1265  (Laplacian and biharmonic) as well. The Gent and McWilliams parameterization    Gent and McWilliams parameterization for oceanic tracers is
1266  for oceanic tracers is described in the package section. Finally, note that    described in the package section. Finally, note that tracers can be
1267  tracers can be also subject to Fourier and Shapiro filtering (see the    also subject to Fourier and Shapiro filtering (see the corresponding
1268  corresponding section on these filters).    section on these filters).
1269    
1270  \begin{itemize}  \item[ocean convection] \
1271  \item ocean convection    
1272  \end{itemize}    Two options are available to parameterize ocean convection: one is
1273      to use the convective adjustment scheme. In this case, you need to
1274      set the variable \textbf{cadjFreq}, which represents the frequency
1275      (in s) with which the adjustment algorithm is called, to a non-zero
1276      value (if set to a negative value by the user, the model will set it
1277      to the tracer time step). The other option is to parameterize
1278      convection with implicit vertical diffusion. To do this, set the
1279      logical variable \textbf{implicitDiffusion }to '.\texttt{TRUE} .'
1280      and the real variable \textbf{ivdc\_kappa }to a value (in m$^{2}$/s)
1281      you wish the tracer vertical diffusivities to have when mixing
1282      tracers vertically due to static instabilities. Note that
1283      \textbf{cadjFreq }and \textbf{ivdc\_kappa }can not both have
1284      non-zero value.
1285    
1286  Two options are available to parameterize ocean convection: one is to use  \end{description}
 the convective adjustment scheme. In this case, you need to set the variable  
 \textbf{cadjFreq}, which represents the frequency (in s) with which the  
 adjustment algorithm is called, to a non-zero value (if set to a negative  
 value by the user, the model will set it to the tracer time step). The other  
 option is to parameterize convection with implicit vertical diffusion. To do  
 this, set the logical variable \textbf{implicitDiffusion }to '.\texttt{TRUE}%  
 .' and the real variable \textbf{ivdc\_kappa }to a value (in m$^{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.  
1287    
1288  \subsection{Simulation controls}  \subsection{Simulation controls}
1289    
# Line 1180  Typically, you will set it to the tracer Line 1294  Typically, you will set it to the tracer
1294  Frequency of checkpointing and dumping of the model state are referenced to  Frequency of checkpointing and dumping of the model state are referenced to
1295  this clock (see below).  this clock (see below).
1296    
1297  \begin{itemize}  \begin{description}
1298  \item run duration  \item[run duration] \
1299  \end{itemize}    
1300      The beginning of a simulation is set by specifying a start time (in
1301  The beginning of a simulation is set by specifying a start time (in s)    s) through the real variable \textbf{startTime }or by specifying an
1302  through the real variable \textbf{startTime }or by specifying an initial    initial iteration number through the integer variable
1303  iteration number through the integer variable \textbf{nIter0}. If these    \textbf{nIter0}. If these variables are set to nonzero values, the
1304  variables are set to nonzero values, the model will look for a ''pickup''    model will look for a ''pickup'' file \textit{pickup.0000nIter0 }to
1305  file \textit{pickup.0000nIter0 }to restart the integration\textit{. }The end    restart the integration\textit{. }The end of a simulation is set
1306  of a simulation is set through the real variable \textbf{endTime }(in s).    through the real variable \textbf{endTime }(in s).  Alternatively,
1307  Alternatively, you can specify instead the number of time steps to execute    you can specify instead the number of time steps to execute through
1308  through the integer variable \textbf{nTimeSteps}.    the integer variable \textbf{nTimeSteps}.
1309    
1310    \item[frequency of output] \
1311      
1312      Real variables defining frequencies (in s) with which output files
1313      are written on disk need to be set up. \textbf{dumpFreq }controls
1314      the frequency with which the instantaneous state of the model is
1315      saved. \textbf{chkPtFreq } and \textbf{pchkPtFreq }control the
1316      output frequency of rolling and permanent checkpoint files,
1317      respectively. See section 1.5.1 Output files for the definition of
1318      model state and checkpoint files. In addition, time-averaged fields
1319      can be written out by setting the variable \textbf{taveFreq} (in s).
1320      The precision with which to write the binary data is controlled by
1321      the integer variable w\textbf{riteBinaryPrec }(set it to \texttt{32}
1322      or \texttt{ 64}).
1323    
1324  \begin{itemize}  \end{description}
 \item frequency of output  
 \end{itemize}  
1325    
 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}).  
1326    
1327  %%% Local Variables:  %%% Local Variables:
1328  %%% mode: latex  %%% mode: latex

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