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<span>I'm really sorry for the disturbance. I found the text of my previous email consisted of error codes, maybe it is related to my email. So I use another email to resend the question. Thank you so much.</span></div>
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<span>Hi everyone,<br>
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<div>Recently, I ran a global ocean model configuration which is similar with the global_with_exf but with 1 grid*1 grid resolution. Strangely, I found the currents were mainly located on the equator (e.g., strong westward currents over eastern equatorial Pacific),
and there are no western boundary currents and ACC.<br>
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<div><br>
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<div>Attached are the currents at the time of 40 years.<br>
</div>
<div><br>
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<div>Here is my data file:<br>
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<div><br>
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<div># ====================<br>
</div>
<div># | Model parameters |<br>
</div>
<div># ====================<br>
</div>
<div>#<br>
</div>
<div># Continuous equation parameters<br>
</div>
<div> &PARM01<br>
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<div> tRef= 13.72 , 12.82 , 11.57 , 10.35 , 9.38 ,<br>
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<div> 8.62 , 7.99 , 7.45 , 6.91 , 6.45 ,<br>
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<div> 5.99 , 5.63 , 5.26 , 4.97 , 4.68 ,<br>
</div>
<div> 4.44 , 4.20 , 4.06 , 3.85 , 3.68 ,<br>
</div>
<div> 3.51 , 3.22 , 2.99 , 2.80 , 2.62 ,<br>
</div>
<div> 2.47 , 1.93 , 1.61 , 1.27 , 1.23 ,<br>
</div>
<div> sRef = 30*34., <br>
</div>
<div> viscAr=1.E-4,<br>
</div>
<div># viscAh=2.E2,<br>
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<div> viscAh=1.E0,<br>
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<div> viscAhGrid=2.E-2,<br>
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<div> diffKhT=0.,<br>
</div>
<div> diffKrT=2.E-5,<br>
</div>
<div> diffKhS=0.,<br>
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<div> diffKrS=2.E-5,<br>
</div>
<div> rhonil=1035.,<br>
</div>
<div> rhoConstFresh=1000.,<br>
</div>
<div> eosType = 'JMD95Z',<br>
</div>
<div> ivdc_kappa=100.,<br>
</div>
<div> implicitDiffusion=.TRUE.,<br>
</div>
<div> allowFreezing=.TRUE.,<br>
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<div> exactConserv=.TRUE.,<br>
</div>
<div> useRealFreshWaterFlux=.TRUE.,<br>
</div>
<div> useCDscheme=.TRUE.,<br>
</div>
<div># turn on looped cells<br>
</div>
<div> hFacMin=.05,<br>
</div>
<div> hFacMindr=50.,<br>
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<div> useSingleCpuIO=.TRUE.,<br>
</div>
<div># set precision of data files<br>
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<div> readBinaryPrec=32,<br>
</div>
<div> &<br>
</div>
<div><br>
</div>
<div># Elliptic solver parameters<br>
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<div> &PARM02<br>
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<div> cg2dMaxIters=500,<br>
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<div> cg2dTargetResidual=1.E-13,<br>
</div>
<div> &<br>
</div>
<div><br>
</div>
<div># Time stepping parameters<br>
</div>
<div> &PARM03<br>
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<div> nIter0 = 0,<br>
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<div> nTimeSteps = 864000,<br>
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<div># 100 years of integration will yield a reasonable flow field<br>
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<div># startTime = 0.,<br>
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<div># endTime = 3110400000.,<br>
</div>
<div> deltaTmom = 300.0,<br>
</div>
<div> tauCD = 321428.,<br>
</div>
<div> deltaTtracer= 1800.0,<br>
</div>
<div> deltaTClock = 3600.0,<br>
</div>
<div># if you are using a version later than checkpoint45d on the main branch<br>
</div>
<div># you can uncomment the following line and increase the time step<br>
</div>
<div># deltaTtracer and deltaTClock to 172800.0 as well to speed up the<br>
</div>
<div># asynchronous time stepping<br>
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<div># deltaTfreesurf = 172800.0,<br>
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<div> abEps = 0.1,<br>
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<div> pChkptFreq= 31104000.,<br>
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<div># dumpFreq= 311040000.,<br>
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<div># dumpFreq= 864000.,<br>
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<div># taveFreq= 311040000.,<br>
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<div> taveFreq= 2592000.,<br>
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<div> monitorFreq=720.,<br>
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<div> &<br>
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<div><br>
</div>
<div># Gridding parameters<br>
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<div> &PARM04<br>
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<div> usingSphericalPolarGrid=.TRUE.,<br>
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<div> delR= 10., 15., 20., 30., 40.,<br>
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<div> 50., 50., 60., 60., 60.,<br>
</div>
<div> 60., 60., 60., 60., 60.,<br>
</div>
<div> 60., 60., 60., 70., 70.,<br>
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<div> 70., 100., 140., 200., 250.,<br>
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<div> 320., 420., 550., 650., 800.,<br>
</div>
<div> ygOrigin=-80.,<br>
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<div> xgOrigin=0.,<br>
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<div> dySpacing=1.,<br>
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<div> dxSpacing=1.,<br>
</div>
<div> &<br>
</div>
<div><br>
</div>
<div># Input datasets<br>
</div>
<div> &PARM05<br>
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<div> bathyFile= 'bathymetry.bin',<br>
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<div># hydrogThetaFile='lev_t.bin',<br>
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<div># hydrogSaltFile= 'lev_s.bin',<br>
</div>
<div> &<br>
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<div>Thank you so much.<br>
</div>
<div>Best,<br>
</div>
<span>Fei</span><br>
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