Category:Issues
From krc
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Bottom Line: | Bottom Line: | ||
| − | : Stay away from frosted surfaces if you can; | + | : - Stay away from frosted surfaces if you can; |
| − | : Reduce the seasonal and/or diurnal sampling resolution (doesn't solve the issue, but dissolves it); | + | : - 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 | + | : - Identify the times (LT, Ls) when this issue is apparent and filter out these model results |
=== Issue with Mat1 and materials_krc() === | === Issue with Mat1 and materials_krc() === | ||
Revision as of 15:01, 9 November 2016
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>
Bottom Line:
- - 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()
out=krc(lat=0.,Mat1="H2O") crashes, but out=krc(lat=0.,Mat1="water_1") does not crash but should not be allowed Issue with materials_krc()
out=krc(lat=0.,N1=55) #ONLY AT ASU?
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