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Diurnal CO<sub>2</sub> condensation and defrosting often leads to rather small instabilities. | Diurnal CO<sub>2</sub> condensation and defrosting often leads to rather small instabilities. | ||
Most often, these instabilities yield surface temperature oscillations of a fraction of a K. | Most often, these instabilities yield surface temperature oscillations of a fraction of a K. | ||
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[[Image:Frosting Defrosting.png|600px| ]] | [[Image:Frosting Defrosting.png|600px| ]] | ||
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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>
