Convergence in simulating global soil organic carbon by structurally different models after data assimilation
Convergence in simulating global soil organic carbon by structurally different models after data assimilation
The current generation of biogeochemical models produce large uncertainty in carbon-climate feedback projections. Structural differences in these models have been identified as a major source of inter-model uncertainties when simulating soil organic carbon (SOC) dynamics worldwide. However, parameterization could also play a role, particularly when common observational data are used …