Global volcanic aerosol properties derived from emissions, 1990–2014, using CESM1(WACCM)

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Tropospheric ozone in CMIP6 simulations (2020, background): “MAM4 has been further modified to incorporate a new prognostic stratospheric aerosol capability (Mills et al., 2016).”
The Climate Response to Stratospheric Aerosol Geoengineering Can Be Tailored Using Multiple Injection Locations (2017, methodology): “Simulations are conducted using a fully coupled chemistry climate model that includes all of these effects; the model is described briefly in section 2 and in more detail by Mills et al. (2016, 2017).”
The Chemistry Mechanism in the Community Earth System Model Version 2 (CESM2) (2020, methodology): “Aerosol surface area density (SAD) is calculated based on the simulated MAM4 aerosol distributions of sulfate, black carbon, primary, and secondary organic aerosol (Mills et al., 2016).”
The Whole Atmosphere Community Climate Model Version 6 (WACCM6) (2019, methodology): “For eruptions inputting more than 3.5 Tg of SO2, we therefore impose a maximum altitude of 20 km, as discussed in Mills et al. (2016) for the case of the 1991 Pinatubo eruption.”