I am working on coupling MIMICS+ with CLM-FATES. This is part of the NorSink project, which aims to improve soil C modeling in Norway, but I want to plan for this to be globally applicable. MIMICS+ simulates soil C and N cycling by bacteria and fungi, including plant N acquisition from mycorrhizal fungi.
Betty (also here at UiO) has been working on coupling CLM with MIMICS+. In her work, mycorrhizal pools are represented on the PFT level of CLM.
The big question we should discuss first is, on what level do we simulate decomposition? (column, patch, cohort)? This has tradeoffs between computational reqs and our representation of ecological processes.
Another important question to consider is how will plants allocated C to mycorrhizae? In Betty's work, C allocation is a function of available C, N stress, and a maximum allocation fraction.
I am working on coupling MIMICS+ with CLM-FATES. This is part of the NorSink project, which aims to improve soil C modeling in Norway, but I want to plan for this to be globally applicable. MIMICS+ simulates soil C and N cycling by bacteria and fungi, including plant N acquisition from mycorrhizal fungi.
Betty (also here at UiO) has been working on coupling CLM with MIMICS+. In her work, mycorrhizal pools are represented on the PFT level of CLM.
The big question we should discuss first is, on what level do we simulate decomposition? (column, patch, cohort)? This has tradeoffs between computational reqs and our representation of ecological processes.
Another important question to consider is how will plants allocated C to mycorrhizae? In Betty's work, C allocation is a function of available C, N stress, and a maximum allocation fraction.