Category:Issues
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: - 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() === | ||
− | out=krc(lat=0.,Mat1="H2O") | + | NEEDS TO BE FIXED |
+ | |||
+ | dv>out=krc(lat=0.,Mat1="H2O") | ||
crashes, but | crashes, but | ||
− | out=krc(lat=0.,Mat1="water_1") | + | dv> out=krc(lat=0.,Mat1="water_1") |
does not crash but should not be allowed | does not crash but should not be allowed | ||
Issue with materials_krc() | Issue with materials_krc() | ||
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− | |||
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Latest revision as of 15:44, 9 November 2016
[edit] 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
[edit] Issue with Mat1 and materials_krc()
NEEDS TO BE FIXED
dv>out=krc(lat=0.,Mat1="H2O")
crashes, but
dv> out=krc(lat=0.,Mat1="water_1")
does not crash but should not be allowed Issue with materials_krc()
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