Wednesday, 31 January 2024
Hall E (The Baltimore Convention Center)
Despite significant reductions in ozone precursors in recent decades, the New York-New Jersey-Connecticut area currently surpasses the EPA’s national air quality standard for ozone. Using air samples collected from the Long Island Sound Tropospheric Ozone Study (LISTOS) in the late spring and summers of 2017-2019, we calculate ozone production (PO3) and test its sensitivity to changes in initial concentrations of ozone precursors using a 0-D box model. We find characteristic diurnal and seasonal cycle of PO3 due to changes in observed NO2 and VOCs. We often find PO3 to be VOC limited in downtown NYC, along the Connecticut coast, and central Connecticut. In these samples PO3 is most sensitive to either biogenic VOC or anthropogenic alkenes depending on time of day and season. We also explore the relationships of different metrics for photochemical regime classification (i.e, NOx or VOC limited PO3).
We further compare PO3 calculations using the near explicit Master Chemical Mechanism (MCMv3.3.1) to Carbon Bond 6 revision 2 (CB6r2) for a more direct link to regulatory air quality models. Modeled PO3 is 25% faster in MCMv3.3.1, due largely to the speciation of VOC and organic peroxy radicals. This finding has implications for how condensed mechanisms in regional and global chemical transport models might respond to changing VOC distributions in urban areas.

