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| | [[Image:Frosting Defrosting.png|600px| ]] | | [[Image:Frosting Defrosting.png|600px| ]] |
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| − | Sets DELLS=0. to avoid this issue but error message: Please do not set both DELLS and DELJUL XXX
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| − | OUT = krc(T=190,ls=359.99,hour=4.,lat=12.,lon=12.,DELLS=0.)
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| − | Under some circumstances, a random line is printed on the screen ("Line is at 1000000") / Assigned to CSE
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| − | OUT = krc(lat = 0., INERTIA = 045., N1 = 32, body = "Jupiter,Europa", bodytype = "minor", N24 = 96, Eclipse = "T", Eclipser="Jupiter_Jupiter", Ecl_Cent_Hr = 12., Bias = 0., Eclipse_Style = 1., Date = 5000.)
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| − | When running airless body cases, atmospheric parameters (and elevation etc.) are printed on the screen, like opacity, elevation, etc.
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| − | This needs to be removed.
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| − | When running a body with made up parameters, an error message appears:
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| − | structure does not contain member: rot
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| − | tmp = generic_porb(e = 0, a = 1., i = 1.3, node = 100.4, peri = 293.9, m = 79.6, rot_per = 200., polera = 273.8, poledec = 0., merid = 7.7, period = 4332.5, name = "IdealJupiterTrojan_like_Comet")
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| − | out = krc( lat = 0., lon = 0, INERTIA = 20., ALBEDO =.05, LKofT = "F", body = tmp, bodytype = "comet")
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Latest revision as of 16:42, 7 March 2019
Diurnal CO2 condensation and defrosting often leads to rather small instabilities.
Most often, these instabilities yield surface temperature oscillations of a fraction of a K.
But near the local time of first frost deposition and last frost removal, oscillations can reach 20+K, without clear consequences for temperatures calculated at other times.
dv> out=krc(lat=-30.,INERTIA=30.)
dv> plot(out.tsurf[,,],"I=30 SI")
dv>
