[MITgcm-support] temperature difference in the horizontal direction cause large velocity
Chun-Yan Zhou
c.zhou at dundee.ac.uk
Fri Dec 16 18:01:46 EST 2011
The temperature difference in horizontal direction are 2º and the
velocity there is 0
Dear all,
Again, I test about the different temperature distribution. The
topography is a slope with deepest 90m. No other forces are applied.
The first case, the temperature decreased with only depth linearly.
The second case, the temperature has a difference 2º in the horizontal
direction, and still decreased with depth.
In first case, the velocity is almost zeros and surface elevation Eta
is also zero, which quite make sense.
The second case, however, the velocity can reach up to 0.2m/s where
the temperature change very quickly in the horizontal direction. It also
cause surface elevation eta around 0.01m.
Why does the temperature difference in the horizontal direction cause
such large velocity and Eta?
Thanks in advance
The data file
# ====================
# | Model parameters |
# ====================
#
# Continuous equation parameters
&PARM01
sRef=60*35.,
viscA4=0.0E4,
viscAh=1.E-3,
viscAz=1.E-5,
no_slip_sides=.FALSE.,
no_slip_bottom=.FALSE.,
diffK4T=0.E4,
diffKhT=1.E-3,
diffKzT=1.E-5,
diffK4S=0.E4,
diffKhS=0.E-2,
diffKzS=0.E-5,
implicitDiffusion=.TRUE.,
implicitViscosity=.TRUE.,
f0=0.e-4,
beta=0.E-11,
eosType='LINEAR',
tAlpha=2.E-4,
sBeta =0.E-4,
gravity=9.81,
gBaro=9.81,
rigidLid=.FALSE.,
saltStepping=.FALSE.,
implicitFreeSurface=.TRUE.,
hFacMin=0.05,
nonHydrostatic=.TRUE.,
readBinaryPrec=64,
#- not safe to use globalFiles in multi-processors runs
#globalFiles=.TRUE.,
staggerTimestep=.TRUE.,
&
# Elliptic solver parameters
&PARM02
cg2dMaxIters=300,
cg2dTargetResidual=1.E-13,
cg3dMaxIters=20,
cg3dTargetResidual=1.E-8,
&
# Time stepping parameters
&PARM03
nIter0=80000,
nTimeSteps=80000,
#nTimeSteps=8640,
deltaT=22.357,
abEps=0.01,
pChkptFreq=447140.,
chkptFreq=0.0,
dumpFreq=223570,
#taveFreq=864000.0,
monitorSelect=2,
monitorFreq=1.,
periodicExternalForcing=.TRUE.,
externForcingPeriod=223.57,
externForcingCycle=44714.,
&
# Gridding parameters
&PARM04
usingCartesianGrid=.TRUE.,
delX=700*500.,
dYspacing=50000.,
delZ=60*1.5,
&
# Input datasets
&PARM05
bathyFile='topog.slope',
hydrogThetaFile='T.init',
&
Chunyan Zhou
Division of Civil Engineering
School of Engineering, Physics and Mathematics
College of Art, Science and Engineering
G19,Fulton Building
University of Dundee
Dundee DD1 4HN
Tel: +44 (0) 1382 385431
The University of Dundee is a registered Scottish charity, No: SC015096
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