|
|
|
Next: 3.13 P coordinate Global
Up: 3.12 Global Ocean MITgcm
Previous: 3.12.2 Discrete Numerical Configuration
Contents
Subsections
3.12.3 Experiment Configuration
The model configuration for this experiment resides under the
directory tutorial_examples/global_ocean_circulation/.
The experiment files
- input/data
- input/data.pkg
- input/eedata,
- input/windx.bin,
- input/windy.bin,
- input/salt.bin,
- input/theta.bin,
- input/SSS.bin,
- input/SST.bin,
- input/topog.bin,
- code/CPP_EEOPTIONS.h
- code/CPP_OPTIONS.h,
- code/SIZE.h.
contain the code customizations and parameter settings for these
experiments. Below we describe the customizations
to these files associated with this experiment.
Figures (-- missing figures --)
show the relaxation temperature (
) and salinity (
)
fields, the wind stress components (
and
), the heat flux (
)
and the net fresh water flux (
) used
in equations
(3.31-3.34).
The figures also indicate the lateral extent and coastline used in the
experiment. Figure (-- missing figure -- ) shows the depth contours of the model domain.
This file, reproduced completely below, specifies the main parameters
for the experiment. The parameters that are significant for this configuration
are
- Lines 7-10 and 11-14
tRef= 16.0 , 15.2 , 14.5 , 13.9 , 13.3 ,
set reference values for potential
temperature and salinity at each model level in units of
and
. The entries are ordered from surface to depth.
Density is calculated from anomalies at each level evaluated
with respect to the reference values set here.
- Line 15,
viscAz=1.E-3,
this line sets the vertical Laplacian dissipation coefficient to
. Boundary conditions
for this operator are specified later. This variable is copied into
model general vertical coordinate variable viscAr.
- Line 16,
viscAh=5.E5,
this line sets the horizontal Laplacian frictional dissipation coefficient to
. Boundary conditions
for this operator are specified later.
- Lines 17,
no_slip_sides=.FALSE.
this line selects a free-slip lateral boundary condition for
the horizontal Laplacian friction operator
e.g.
=0 along boundaries in
and
=0 along boundaries in
.
- Lines 9,
no_slip_bottom=.TRUE.
this line selects a no-slip boundary condition for bottom
boundary condition in the vertical Laplacian friction operator
e.g.
at
, where
is the local depth of the domain.
- Line 19,
diffKhT=1.E3,
this line sets the horizontal diffusion coefficient for temperature
to
. The boundary condition on this
operator is
on
all boundaries.
- Line 20,
diffKzT=3.E-5,
this line sets the vertical diffusion coefficient for temperature
to
. The boundary
condition on this operator is
at both
the upper and lower boundaries.
- Line 21,
diffKhS=1.E3,
this line sets the horizontal diffusion coefficient for salinity
to
. The boundary condition on this
operator is
on
all boundaries.
- Line 22,
diffKzS=3.E-5,
this line sets the vertical diffusion coefficient for salinity
to
. The boundary
condition on this operator is
at both
the upper and lower boundaries.
- Lines 23-26
beta=1.E-11,
These settings do not apply for this experiment.
- Line 27,
gravity=9.81,
Sets the gravitational acceleration coefficient to
.
- Line 28-29,
rigidLid=.FALSE.,
implicitFreeSurface=.TRUE.,
Selects the barotropic pressure equation to be the implicit free surface
formulation.
- Line 30,
eosType='POLY3',
Selects the third order polynomial form of the equation of state.
- Line 31,
readBinaryPrec=32,
Sets format for reading binary input datasets holding model fields to
use 32-bit representation for floating-point numbers.
- Line 36,
cg2dMaxIters=1000,
Sets maximum number of iterations the two-dimensional, conjugate
gradient solver will use, irrespective of convergence
criteria being met.
- Line 37,
cg2dTargetResidual=1.E-13,
Sets the tolerance which the two-dimensional, conjugate
gradient solver will use to test for convergence in equation
2.20 to
.
Solver will iterate until tolerance falls below this value or until the
maximum number of solver iterations is reached.
- Line 42,
startTime=0,
Sets the starting time for the model internal time counter.
When set to non-zero this option implicitly requests a
checkpoint file be read for initial state.
By default the checkpoint file is named according to
the integer number of time steps in the startTime value.
The internal time counter works in seconds.
- Line 43,
endTime=2808000.,
Sets the time (in seconds) at which this simulation will terminate.
At the end of a simulation a checkpoint file is automatically
written so that a numerical experiment can consist of multiple
stages.
- Line 44,
#endTime=62208000000,
A commented out setting for endTime for a 2000 year simulation.
- Line 45,
deltaTmom=2400.0,
Sets the timestep
used in the momentum equations to
.
See section 2.2.
- Line 46,
tauCD=321428.,
Sets the D-grid to C-grid coupling time scale
used in the momentum equations.
- Line 47,
deltaTtracer=108000.,
Sets the default timestep,
, for tracer equations to
.
See section 2.2.
- Line 47,
bathyFile='topog.box'
This line specifies the name of the file from which the domain
bathymetry is read. This file is a two-dimensional (
) map of
depths. This file is assumed to contain 64-bit binary numbers
giving the depth 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 units and orientation of the
depths in this file are the same as used in the MITgcm code. In this
experiment, a depth of
indicates a solid wall and a depth
of
indicates open ocean. The matlab program
input/gendata.m shows an example of how to generate a
bathymetry file.
- Line 50,
zonalWindFile='windx.sin_y'
This line specifies the name of the file from which the x-direction
surface wind stress is read. This file is also a two-dimensional
(
) map and is enumerated and formatted in the same manner as the
bathymetry file. The matlab program input/gendata.m includes example
code to generate a valid
zonalWindFile
file.
other lines in the file input/data are standard values
that are described in the MITgcm Getting Started and MITgcm Parameters
notes.
# ====================
# | Model parameters |
# ====================
#
# Continuous equation parameters
&PARM01
tRef= 16.0 , 15.2 , 14.5 , 13.9 , 13.3 ,
12.4 , 11.3 , 9.9 , 8.4 , 6.7 ,
5.2 , 3.8 , 2.9 , 2.3 , 1.8 ,
1.5 , 1.1 , 0.8 , 0.66, 0.63,
sRef= 34.65, 34.75, 34.82, 34.87, 34.90,
34.90, 34.86, 34.78, 34.69, 34.60,
34.58, 34.62, 34.68, 34.72, 34.73,
34.74, 34.73, 34.73, 34.72, 34.72,
viscAz=1.E-3,
viscAh=5.E5,
no_slip_sides=.FALSE.,
no_slip_bottom=.TRUE.,
diffKhT=1.E3,
diffKzT=3.E-5,
diffKhS=1.E3,
diffKzS=3.E-5,
beta=1.E-11,
f0=1.e-4,
tAlpha=2.E-4,
sBeta =7.4E-4,
gravity=9.81,
rigidLid=.FALSE.,
implicitFreeSurface=.TRUE.,
eosType='LINEAR',
readBinaryPrec=32,
&
# Elliptic solver parameters
&PARM02
cg2dMaxIters=1000,
cg2dTargetResidual=1.E-13,
&
# Time stepping parameters
&PARM03
startTime=311040000,
endTime=622080000,
#endTime=2808000.,
deltaTmom=2400.0,
tauCD=321428.,
deltaTtracer=108000.0,
deltaTClock =108000.0,
cAdjFreq=-1.,
abEps=0.1,
pChkptFreq=0.0,
chkptFreq=0.0,
dumpFreq=2592000.0,
dumpFreq=31104000.,
tauThetaClimRelax=2592000.0,
tauSaltClimRelax=2592000.0,
&
# Gridding parameters
&PARM04
usingCartesianGrid=.FALSE.,
usingSphericalPolarGrid=.TRUE.,
delZ= 5.000000e+01, 5.000000e+01, 5.500000e+01, 6.000000e+01,
6.500000e+01, 7.000000e+01, 8.000000e+01, 9.500000e+01,
1.200000e+02, 1.550000e+02, 2.000000e+02, 2.600000e+02,
3.200000e+02, 4.000000e+02, 4.800000e+02, 5.700000e+02,
6.550000e+02, 7.250000e+02, 7.750000e+02, 8.150000e+02,
phiMin=-80.,
delY=40*4,
delX=90*4,
&
# Input datasets
&PARM05
hydrogThetaFile='theta.bin',
hydrogSaltFile='salt.bin',
bathyFile='topog.bin',
zonalWindFile='windx.bin',
meridWindFile='windy.bin',
thetaClimFile='SST.bin'
saltClimFile='SSS.bin'
&
This file uses standard default values and does not contain
customisations for this experiment.
This file uses standard default values and does not contain
customisations for this experiment.
The input/windx.sin_y file specifies a two-dimensional (
)
map of wind stress ,
, values. The units used are
.
Although
is only a function of
n in this experiment
this file must still define a complete two-dimensional map in order
to be compatible with the standard code for loading forcing fields
in MITgcm. The included matlab program input/gendata.m gives a complete
code for creating the input/windx.sin_y file.
The input/topog.box file specifies a two-dimensional (
)
map of depth values. For this experiment values are either
or
, corresponding respectively to a wall or to deep
ocean. The file contains a raw binary stream of data that is enumerated
in the same way as standard MITgcm two-dimensional, horizontal arrays.
The included matlab program input/gendata.m gives a complete
code for creating the input/topog.box file.
Two lines are customized in this file for the current experiment
- Line 39,
sNx=60,
this line sets
the lateral domain extent in grid points for the
axis aligned with the x-coordinate.
- Line 40,
sNy=60,
this line sets
the lateral domain extent in grid points for the
axis aligned with the y-coordinate.
- Line 49,
Nr=4,
this line sets
the vertical domain extent in grid points.
C $Header: /u/gcmpack/manual/s_examples/global_oce_latlon/code/SIZE.h,v 1.2 2001/09/27 00:58:17 cnh Exp $
C $Name: $
C
C /==========================================================\
C | SIZE.h Declare size of underlying computational grid. |
C |==========================================================|
C | The design here support a three-dimensional model grid |
C | with indices I,J and K. The three-dimensional domain |
C | is comprised of nPx*nSx blocks of size sNx along one axis|
C | nPy*nSy blocks of size sNy along another axis and one |
C | block of size Nz along the final axis. |
C | Blocks have overlap regions of size OLx and OLy along the|
C | dimensions that are subdivided. |
C \==========================================================/
C Voodoo numbers controlling data layout.
C sNx - No. X points in sub-grid.
C sNy - No. Y points in sub-grid.
C OLx - Overlap extent in X.
C OLy - Overlat extent in Y.
C nSx - No. sub-grids in X.
C nSy - No. sub-grids in Y.
C nPx - No. of processes to use in X.
C nPy - No. of processes to use in Y.
C Nx - No. points in X for the total domain.
C Ny - No. points in Y for the total domain.
C Nr - No. points in Z for full process domain.
INTEGER sNx
INTEGER sNy
INTEGER OLx
INTEGER OLy
INTEGER nSx
INTEGER nSy
INTEGER nPx
INTEGER nPy
INTEGER Nx
INTEGER Ny
INTEGER Nr
PARAMETER (
& sNx = 90,
& sNy = 40,
& OLx = 3,
& OLy = 3,
& nSx = 1,
& nSy = 1,
& nPx = 1,
& nPy = 1,
& Nx = sNx*nSx*nPx,
& Ny = sNy*nSy*nPy,
& Nr = 20)
C MAX_OLX - Set to the maximum overlap region size of any array
C MAX_OLY that will be exchanged. Controls the sizing of exch
C routine buufers.
INTEGER MAX_OLX
INTEGER MAX_OLY
PARAMETER ( MAX_OLX = OLx,
& MAX_OLY = OLy )
This file uses standard default values and does not contain
customisations for this experiment.
This file uses standard default values and does not contain
customisations for this experiment.
Other files relevant to this experiment are
- model/src/ini_cori.F. This file initializes the model
coriolis variables fCorU.
- model/src/ini_spherical_polar_grid.F
- model/src/ini_parms.F,
- input/windx.sin_y,
contain the code customisations and parameter settings for this
experiments. Below we describe the customisations
to these files associated with this experiment.
Next: 3.13 P coordinate Global
Up: 3.12 Global Ocean MITgcm
Previous: 3.12.2 Discrete Numerical Configuration
Contents
mitgcm-support@mitgcm.org
Copyright © 2006
Massachusetts Institute of Technology |
Last update 2011-01-09 |
|
|