Abstract. Various levels of representations of biogeochemical processes in current
biogeochemistry models contribute to a large uncertainty in carbon budget
quantification. Here, we present an uncertainty analysis with a process-based
biogeochemistry model, the Terrestrial Ecosystem Model (TEM), into which detailed microbial mechanisms were incorporated. Ensemble regional simulations with
the new model (MIC-TEM) estimated that the carbon budget of the arctic
ecosystems is 76.0±114.8 Pg C during the 20th century, i.e., -3.1±61.7 Pg C under the RCP 2.6 scenario and 94.7±46 Pg C under the RCP
8.5 scenario during the 21st century. Positive values indicate the regional
carbon sink while negative values are a source to the atmosphere. Compared to
the estimates using a simpler soil decomposition algorithm in TEM, the new
model estimated that the arctic terrestrial ecosystems stored 12 Pg less
carbon over the 20th century, i.e., 19 and 30 Pg C less under the RCP 8.5
and RCP 2.6 scenarios, respectively, during the 21st century. When soil
carbon within depths of 30, 100, and 300 cm was considered as initial carbon
in the 21st century simulations, the region was estimated to accumulate 65.4,
88.6, and 109.8 Pg C, respectively, under the RCP 8.5 scenario. In
contrast, under the RCP 2.6 scenario, the region lost 0.7, 2.2, and 3 Pg C,
respectively, to the atmosphere. We conclude that the future regional carbon
budget evaluation largely depends on whether or not adequate microbial
activities are represented in earth system models and on the sizes of soil
carbon considered in model simulations.