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1. Removed LLoydTaylor variable: instead we keep decomp_scheme, so we…
… can add more decomposition schemes. 2. Added a new decomposition scheme, that is actually based on the original ED-1.0 formulation. The current functions of temperature and soil moisture would make the heterotrophic respiration too low as the optimal would happen only at very high temperatures and very close to the optimal soil moisture, quickly decaying. Somehow the original method that allowed temperature to peak at ~ 35degC and decaying at temperatures above 40degC disappeared during the ED-2.0 -> ED-2.1 transtion. Also, the function for soil moisture quickly dropped for any value other than the optimal, which seems quite different from the original CENTURY model formulation. Last, the rates for slow carbon were one order of magnitude higher than the fast soil, so the slow carbon decays faster than the fast (weird!!!). This was added in ED-1.0, so I changed it only for DECOMP_SCHEME=2, but we should probably ask Paul about this. 3. Added another diagnostic variable in the output: heterotrophic respiration coming from coarse woody debris. 4. Merged the new coefficients for big leaf that Naomi had tuned.
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Marcos Longo
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Jul 29, 2012
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