link Issues

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>

---

Sets DELLS=0. to avoid this issue but error message: Please do not set both DELLS and DELJUL XXX

OUT = krc(T=190,ls=359.99,hour=4.,lat=12.,lon=12.,DELLS=0.)

---

Under some circumstances, a random line is printed on the screen ("Line is at 1000000") / Assigned to CSE

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.)

---

When running airless body cases, atmospheric parameters (and elevation etc.) are printed on the screen:

---