15Semi-volatile and intermediate-volatility organic compounds (SVOCs and IVOCs) from anthropogenic sources are 16 likely to be important precursors of secondary organic aerosol (SOA) in urban airsheds yet their treatment in most 17 models is based on limited and obsolete data, or completely missing. Additionally, gas-phase oxidation of organic 18 precursors to form SOA is influenced by the presence of nitric oxide (NO), but this influence is poorly constrained in 19 chemical transport models. In this work, we updated the organic aerosol model in the UCD/CIT chemical transport 20 model to include (i) a semi-volatile and reactive treatment of primary organic aerosol (POA), (ii) emissions and SOA 21 formation from IVOCs, (iii) the NO X influence on SOA formation, and (iv) SOA parameterizations for SVOCs and 22 IVOCs that are corrected for vapor wall loss artifacts during chamber experiments. All updates were implemented in 23 the statistical oxidation model (SOM) that simulates the oxidation chemistry, thermodynamics, and gas/particle 24 partitioning of organic aerosol (OA). Model treatment of POA, SVOCs, and IVOCs was based on an interpretation of 25 a comprehensive set of source measurements and resolved broadly by source type. The NO X influence on SOA 26 formation was calculated offline based on measured and modeled VOC:NO X ratios. And finally, the SOA formation 27 from all organic precursors (including SVOCs and IVOCs) was modeled based on recently derived parameterizations 28 that accounted for vapor wall loss artifacts in chamber experiments. The updated model was used to simulate a two 29 week summer episode over southern California at a model resolution of 8 km. (except that from marine sources) to be semi-volatile resulted in a larger reduction in POA mass concentrations and 35 allowed for a better model-measurement comparison at Riverside. Model predictions suggested that both SVOCs 36 (evaporated POA vapors) and IVOCs did not contribute significantly to SOA mass concentrations in the urban areas 37 (<5% and <15% of the total SOA respectively) as the timescales for SOA production appeared to be shorter than the 38 timescales for transport out of the urban airshed. Comparisons of modeled IVOC concentrations with measurements 39 of anthropogenic SOA precursors in southern California seemed to imply that IVOC emissions were underpredicted in 40 our updated model by a factor of 2. We suspect that these missing IVOCs might arise from the use of volatile 41 chemical products such as pesticides, coatings, cleaning agents, and personal care products. Correcting for the vapor 42 wall loss artifact in chamber experiments enhanced SOA mass concentrations although the enhancement was 43 precursor-as well as NO X -dependent. Accounting for the influence of NO X using the VOC:NO X ratios resulted in 44Atmos. Chem. Phys. Discuss., https://doi.org/10.5194/acp-2018-616 Manuscript under review for journal Atmos. Chem. Phys.