Diurnal CO2 Defrosting
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>
- - Stay away from frosted surfaces if you can;
- - Reduce the seasonal and/or diurnal sampling resolution (doesn't solve the issue, but dissolves it);
- - Identify the times (LT, Ls) when this issue is apparent and filter out these model results
Issue with Mat1 and materials_krc()
NEEDS TO BE FIXED
does not crash but should not be allowed Issue with materials_krc()
This category currently contains no pages or media.