link Issues
From krc
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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 | ||
| + | OUT = krc(T=190,ls=359.99,hour=4.,lat=12.,lon=12.,DELLS=0.) | ||
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| + | ---- | ||
Revision as of 15:09, 11 January 2019
Diurnal CO2 Ice Instabilities
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.)
