link Issues
From krc
(Difference between revisions)
Line 12: | Line 12: | ||
---- | ---- | ||
− | |||
− |
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>