Replies: 6 comments 6 replies
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Table summarizing key results is linked here |
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@lifang0209, can you help us with fire calibration now that we're running with these changes to fire calculations? Specifically, could you provide a few suggestions for fire tunings we could try (these runs are very slow)? If so, when do you think you could have this to us? Sorry for the added pressure, we're running up against deadlines for contributing to WIEMIP. I've started several hillslope hydrology cases from the wetland branch. The spinup is still ongoing, but a quick look after 150 years of AD spinup suggest the annual burned area is too low (5.8 M km2; see issue note here)
Full diagnostics are posted here case dir: the parameter file I'm using is here |
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@wwieder I'll try to send the tuned parameter tomorrow. |
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@wwieder Hi Will, could you run a 10-year test using the parameter file in your test case user_nl_clm, add: This is just a test case, so I’m not yet sure whether it is over-tuned or under-tuned. I’m traveling with my family, but I should have time tomorrow evening to check the fire simulation from the new test. Also, where is your local path for HH_160_test3? Is it this one: /glade/u/home/wwieder/CTSM? |
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Quick look at the simulation I did with these new parameters in #163 suggests we're getting annual burned area just under 7 M km2. Diagnostic are posted here.
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@wwieder Hi Will, could you use this parameter file for the next run? Not only does soil moisture in natural vegetation columns change when hillslope is active, but the fire calculation structure changes as well. With hillslope off, fire is computed once for all natural vegetation in a grid cell (only one natural vegetation column), using predictors averaged across natural vegetation PFTs. With hillslope on, fire and its predictors are computed separately for each natural vegetation column and then averaged. Once you get the historical transient run finished, I’d like to check the fire simulations again. After all, most of the observations we compare against, not just fire, are for the present day. Parameters tuned only against the 1850 run may have some issues. In particular, I cannot really evaluate deforestation and degradation fires in the 1850 run, because those depend on land-use data to calculate deforestation rates. |
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This is a place to discuss results for WIEMIP simulations
DATM
Hillslope fire modifications
CH4 Fluxes
Generic Crops
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