[MITgcm-support] NaN output data
yulinghui
sysuylh at 163.com
Sun Dec 8 21:40:03 EST 2013
Dear all:
I apply the OBCS (OBWU=U0*sin(wt)) to generate the internal waves. If my compute zone is extend to 3000km and dx(min)=1000m, the numerical model could continue running without NaN. But if my compute zone is 1500km and dx(min)=200m, the numerical result would have NaN in the output data after about 3 tide cycle. I want to use the high resolution to study the internal solitary wave, how should i do to improve it except reducing the time step(now is 10s).
Best regards
input file data:
# ====================
# | Model parameters |
# ====================
#
# Continuous equation parameters
&PARM01
tRefFile = 'MD.tRef',
sRef= 200*35.,
viscAz=1.E-3,
viscAh=1.E-2,
no_slip_sides=.FALSE.,
no_slip_bottom=.FALSE.,
diffKhT=1.E-2
diffKzT=1.E-3,
f0=1.07E-4,
beta=0.E-11,
eosType='LINEAR',
tAlpha=2.E-4,
sBeta =0.E-4,
gravity=9.81,
implicitFreeSurface=.TRUE.,
exactConserv=.TRUE.
nonHydrostatic=.TRUE.,
hFacMin=0.2,
implicSurfPress=0.5,
implicDiv2DFlow=0.5,
nonlinFreeSurf=0,
hFacInf=0.2,
hFacSup=1.8,
saltStepping=.FALSE.,
staggerTimeStep=.TRUE.
tempAdvScheme=77,
tempVertAdvScheme=77,
#- not safe to use globalFiles in multi-processors runs
#globalFiles=.TRUE.,
readBinaryPrec=64,
writeBinaryPrec=64,
writeStatePrec=64,
&
# Elliptic solver parameters
&PARM02
cg2dMaxIters=1000,
cg2dTargetResidual=1.E-13,
cg3dMaxIters=400,
cg3dTargetResidual=1.E-13,
&
# Time stepping parameters
&PARM03
nIter0=0,
nTimeSteps=44600,
deltaT=10,
abEps=0.1,
pChkptFreq=446000.,
chkptFreq=0.,
dumpFreq=11150
monitorFreq=2500.,
monitorSelect=200,
&
# Gridding parameters
&PARM04
usingCartesianGrid=.TRUE.,
delXfile='delXvar',
delY=1.E3,
delRfile='delZvar',
&
# Input datasets
&PARM05
hydrogThetaFile='T.init',
bathyFile='topog',
&
input data data.obcs
# Open-boundaries
&OBCS_PARM01
OB_Ieast=-1,
OB_Iwest=1,
useOrlanskiEast=.TRUE.,
# useOBCSbalance=.TRUE.,
# OBCS_balanceFacE= 1.,
# OBCS_monitorFreq=4000.,
&
# Orlanski parameters
&OBCS_PARM02
Cmax=0.45,
cVelTimeScale=50.,
&
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