Abstract. In 2019–2020, Australia experienced its largest wildfire season on
record. Smoke covered hundreds of square kilometers across the southeastern
coast and reached the site of the COALA-2020 (Characterizing Organics and
Aerosol Loading over Australia) field campaign in New South Wales. Using a
subset of nighttime observations made by a proton-transfer-reaction
time-of-flight mass spectrometer (PTR-ToF-MS), we calculate emission ratios
(ERs) and factors (EFs) for 15 volatile organic compounds (VOCs). We
restrict our analysis to VOCs with sufficiently long lifetimes to be
minimally impacted by oxidation over the ∼ 8 h between when
the smoke was emitted and when it arrived at the field site. We use oxidized
VOC to VOC ratios to assess the total amount of radical oxidation: maleic
anhydride / furan to assess OH oxidation, and (cis-2-butenediol + furanone) / furan to assess NO3 oxidation. We examine time series of
O3 and NO2 given their closely linked chemistry with wildfire
plumes and observe their trends during the smoke event. Then we compare ERs
calculated from the freshest portion of the plume to ERs calculated using
the entire nighttime period. Finding good agreement between the two, we are
able to extend our analysis to VOCs measured in more chemically aged
portions of the plume. Our analysis provides ERs and EFs for six compounds not
previously reported for temperate forests in Australia: acrolein (a compound
with significant health impacts), methyl propanoate, methyl methacrylate,
maleic anhydride, benzaldehyde, and creosol. We compare our results with two
studies in similar Australian biomes, and two studies focused on US
temperate forests. We find over half of our EFs are within a factor of 2.5
relative to those presented in Australian biome studies, with nearly all
within a factor of 5, indicating reasonable agreement. For US-focused
studies, we find similar results with over half our EFs within a factor of
2.5, and nearly all within a factor of 5, again indicating reasonably good agreement.
This suggests that comprehensive field measurements of biomass burning VOC
emissions in other regions may be applicable to Australian temperate
forests. Finally, we quantify the magnitude attributable to the primary
compounds contributing to OH reactivity from this plume, finding results
comparable to several US-based wildfire and laboratory studies.