Simulation of organic aerosol formation during the CalNex study: updated mobile emissions and simplified secondary organic aerosol parameterization for intermediate volatility organic compounds

Abstract

We describe simulations using an updated version of the Community Multiscale Air Quality model version 5.3 15 (CMAQ v5.3) to investigate the contribution of intermediate volatile organic compounds (IVOCs) to secondary organic aerosol formation (SOA) in Southern California during the CalNex study. We first derive a model-ready parameterization for SOA formation from IVOC emissions from mobile sources. To account for SOA formation from both diesel and gasoline sources, the parameterization has six lumped precursor species that account for differences in both volatility and molecular structure (aromatic versus aliphatic) of unspeciated IVOC emissions. We also implement new mobile source emission 20 profiles that quantify all IVOCs based on direct measurements. The profiles have been released in SPECIATE 5.0. In the Los Angeles region, gasoline sources emit 4 times more non-methane organic gases (NMOG) than diesel sources, but diesel emits roughly 3 times more IVOCs on an absolute basis. When accounting for IVOCs, the model predicts all mobile sources (including onand off-road gasoline, aircraft and onand off-road diesel) contribute ~1 μg m of SOA in Pasadena, CA, which corresponds to 12% of the measured SOA concentrations during CalNex. Adding mobile-source IVOCs increases the 25 predicted SOA concentration by ~70%. Therefore, IVOCs in mobile source emissions contribute almost as much SOA as traditional precursors such as single-ring aromatics. However, addition of these emissions still does not close either the ambient SOA or IVOC mass balance. To explore the potential contribution of other IVOC sources, we perform two exploratory simulations with varying amounts of IVOC emissions from non-mobile sources. To close the mass balance of primary hydrocarbon IVOCs, IVOCs would need to account for 12% of NMOG emissions from non-mobile sources (or 30 equivalently 30.7 Ton day in Los Angeles-Pasadena region), a value that is well within the reported range of IVOC content from volatile chemical products. To close the SOA mass balance and explain mildly oxygenated IVOCs in Pasadena, an additional 14.8% of non-mobile source NMOG emissions would need to be IVOCs, but assigning an IVOC-to-NMOG ratio https://doi.org/10.5194/acp-2019-986 Preprint. Discussion started: 30 October 2019 c © Author(s) 2019. CC BY 4.0 License.