The fresh fluxes we believed inside research to possess figuring C equilibrium incorporated NPP, Hour, flame pollutants (Fire C), biogenic CH

_cuatro emissions (BIO C-CH₄), and lateral C fluxes. NPP is the net uptake of CO_dos by vegetation and represents the difference between photosynthetic uptake and plant respiration. HR is the release of CO₂ to the atmosphere associated with decomposition of dead organic matter. Fire C is the release of C-related compounds to the atmosphere from the combustion of above- and below-ground C pools during fire. We assumed that all of Fire C is CO₂ since the models did not distinguish among species of C emitted (i.e., CO₂, CO, and pyrogenic CH₄). BIO C-CH₄ represents biogenic CH₄ emissions to the atmosphere from the production of methane by methanogenic organisms in the soil minus any uptake in the soil column by methanotrophic organisms. In general, the models in this study do not explicitly consider the CH₄ emissions from lakes in the permafrost region, although their definition of the spatial extent of wetlands may include lakes. Read more

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