/[MITgcm]/manual/s_examples/held_suarez_cs/inp_data.templ
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revision 1.1 by jmc, Mon Aug 8 21:09:38 2005 UTC revision 1.2 by jmc, Tue Aug 9 18:46:39 2005 UTC
# Line 13  The parameters that are significant for Line 13  The parameters that are significant for
13   tRef=295.2, 295.5, 295.9, 296.3, 296.7, 297.1, 297.6, 298.1, 298.7, 299.3,   tRef=295.2, 295.5, 295.9, 296.3, 296.7, 297.1, 297.6, 298.1, 298.7, 299.3,
14  \end{verbatim}  \end{verbatim}
15  $\cdots$ \\  $\cdots$ \\
16  set reference values for potential temperature at each model level  set reference values for potential temperature (in Kelvin units)
17  in Kelvin units.  at each model level.
18  The entries are ordered like model level, from surface up to the top.  The entries are ordered like model level, from surface up to the top.
19  Density is calculated from anomalies at each level evaluated  Density is calculated from anomalies at each level evaluated
20  with respect to the reference values set here.  with respect to the reference values set here.
# Line 109  are only permitted for testing/debuging Line 109  are only permitted for testing/debuging
109  \end{verbatim}  \end{verbatim}
110  Select the linear relation between surface geopotential anomaly  Select the linear relation between surface geopotential anomaly
111  and surface pressure anomaly to be evaluated from  and surface pressure anomaly to be evaluated from
112  $\frac{\partial \Phi_s}{\partial p_s} = 1/\rho(\theta_{Ref})$.  $\frac{\partial \Phi_s}{\partial p_s} = 1/\rho(\theta_{Ref})$
113    (see section \ref{sect:phi-freesurface}).
114  Note that using the default (=TRUE), the constant $1/\rho_0$ is  Note that using the default (=TRUE), the constant $1/\rho_0$ is
115  used instead, and is not necessary consistent with other  used instead, and is not necessary consistent with other
116  parts of the geopotential that relies on $\theta_{Ref}$.  parts of the geopotential that relies on $\theta_{Ref}$.
# Line 208  Sets the starting time, in seconds, for Line 209  Sets the starting time, in seconds, for
209  A non-zero starting time requires to read the initial state  A non-zero starting time requires to read the initial state
210  from a pickup file. By default the pickup file is named according  from a pickup file. By default the pickup file is named according
211  to the integer number ({\it nIter0}) of time steps  to the integer number ({\it nIter0}) of time steps
212  in the {\bf startTime} value ($ nIter0 = startTime / deltaT $).  in the {\it startTime} value ($ nIter0 = startTime / deltaT $).
213    
214  \item Line PUT_LINE_NB:#nTimeSteps=,  \item Line PUT_LINE_NB:#nTimeSteps=,
215  \begin{verbatim}  \begin{verbatim}
# Line 242  that are used to restart the simuilation Line 243  that are used to restart the simuilation
243  Sets the time interval, in seconds, bewteen 2 consecutive  Sets the time interval, in seconds, bewteen 2 consecutive
244  "temporary" pickups ("checkpoint frequency") to 1 month.  "temporary" pickups ("checkpoint frequency") to 1 month.
245  The "temporary" pickup file name is alternatively "ckptA"  The "temporary" pickup file name is alternatively "ckptA"
246  and "ckptB", and are designed to be over-written by the  and "ckptB" ; thoses pickup (as opposed to the permanent ones)
247  most recent one.  are designed to be over-written by the model as the simulation
248    progresses.
249    
250  \item Line PUT_LINE_NB:dumpFreq=,  \item Line PUT_LINE_NB:dumpFreq=,
251  \begin{verbatim}  \begin{verbatim}
# Line 257  to 1 month. Line 259  to 1 month.
259  #monitorFreq=43200.,  #monitorFreq=43200.,
260  \end{verbatim}  \end{verbatim}
261  A commented out line setting the frequency (in seconds) for the  A commented out line setting the frequency (in seconds) for the
262  "monitor" output to 12.h respectively. This frequency is fits  "monitor" output to 12.h. This frequency fits
263  better the longer simulation of 1 year.  better the longer simulation of 1 year.
264    
265  \item Line PUT_LINE_NB:usingCurvilinearGrid=,  \item Line PUT_LINE_NB:usingCurvilinearGrid=,

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