Tianyang,Black carbon is prescribed in WACCM4. In order to study the impacts of black carbon emissions in the stratosphere, therefore, I would recommend that you use the new BNUKE_C4WBC_L40CN compset that is included in CESM1.2.0. This includes CARMA sectional (bin) microphysics set up for studies of black carbon emissions in the stratopshere. I have used this WACCM-CARMA model for studies of nuclear winter and emissions from space tourism:Mills, M. J., O. B. Toon, R. Turco, D. E. Kinnison, and R. R. Garcia, Catastrophic ozone loss following a regional nuclear conflict, Proc. Nat. Acad. Sci., 105, 5307-5312, doi:10.1073/pnas.0710058105, 2008.Ross, M., M. Mills, and D. Toohey, Potential climate impact of black carbon emitted by rockets, Geophys. Res. Lett., 37, L24810, doi:10.1029/2010GL044548, 2010.The compset is already set up for an RCP4.5 scenario, so this is good for your 2010-2020 study. The CARMA model includes only one size bin for black carbon (with radius 0.1 µm). You could change this to allow for evolution of the size distribution by coagulation, though the coagulation in the atmosphere likely forms chains and sheets in a complex fractal manner.As for your concern about using scientifically validated compsets, the lack of these for WACCM in 1.2.0 just means that we have not yet had time and resources to run long climate runs for any compsets and compare them to our CMIP5 runs to validate the climate. We have not yet validated any of our WACCM RCP compsets in 1.1.1 either, so that should not be a concern for moving to 1.2.0. In your case, you will be doing a sensitivity study, where you will be comparing to control runs that you will do with the same model, so comparison to our CMIP5 runs should be less of a concern.The inclusion of a full ocean will add some computational cost (perhaps 40-50%), but will allow you to include feedback to surface temperatures, which are dominated by the ocean.Cheers,Mike