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2.4.4 Example 4 -- Paleo run
This is an initial run for a period of one day beginning on September 1,
4050 BC (6000 BP). This namelist defines the earth's orbit, solar
constant, and the volume mixing-ratio for the greenhouse gases. Normally
these values are changed for a paleo-climate simulation.
&CCMEXP
CASEID = 'run04'
CTITLE = 'Paleo-climate run: 4050 BC'
NCDATA = 'SEP1.T42.0198.nc'
BNDTVS = 'T42M5079.nc'
BNDTVO = 'ozn.0596.r8.nc'
IRT =
0
DTIME = 1200.
NSREST = 0
NDENS = 1
NNBDAT = 000901
NNBSEC = 0
NNDBAS = 0
NNSBAS = 0
MFILT = 20
NESTEP = 72
NHTFRQ = 72
INCORBUF = .true.
INCORHST = .true.
INCORRAD = .true.
ECCEN = 0.01868126
OBLIQ = 24.10538
MVELP = 0.87
CO2VMR = 2.80e-4
CH4VMR = 0.700e-6
N2OVMR = 0.275e-6
F11VMR = 0.
F12VMR = 0.
SCON = 1.363e6
/
&LSMEXP
finidat = 'arbitrary initialization'
/
-
ECCEN, OBLIQ, MVELP
-
Set the earth's orbital parameters for year 4050 BC. For the most
accuracy, the parameters ECCEN, OBLIQ, and MVELP
should be set rather than calculating values by using IYEAR_AD.
When IYEAR_AD is specified, the other orbital namelist parameters
are ignored. If you want to calculate the orbital parameters for 4050 BC
using (Berger, 1977) replace the settings for ECCEN, OBLIQ,
and MVELP with.
-
IYEAR_AD = -4050
-
CO2VMR,CH4VMR,N2OVMR,F11VMR,F12VMR
-
Set the volume mixing ratios for the greenhouse gases: CO2,
CH4, N2O, CFC11, and CFC12.
The values are set to values that might be reasonable for 4050 BC.
-
SCON
-
Set the solar constant to 1363 W/m2.
-
BNDTVO,BNDTVS
-
In this example these datasets would not be appropriate for a paleo run.
In general, you will want to create your own datasets to provide these
values.
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Questions on these pages can be sent to...
erik@ucar.edu .
$Name: ccm3_6_6_latest3 $ $Revision: 1.38.2.1 $ $Date: 1999/03/25 21:37:58 $ $Author: erik $