Novel Analysis to Quantify Plume Crosswind Heterogeneity Applied to Biomass Burning Smoke.

We present a novel method, the Gaussian observational model for edge to center heterogeneity (GOMECH), to quantify the horizontal chemical structure of plumes. GOMECH fits observations of short-lived emissions or products against a long-lived tracer (e.g., CO) to provide relative metrics for the plume width ( w _i / w _CO ) and center ( b _i / w _CO ). To validate GOMECH, we investigate OH and NO ₃ oxidation processes in smoke plumes sampled during FIREX-AQ (Fire Influence on Regional to Global Environments and Air Quality, a 2019 wildfire smoke study). An analysis of 430 crosswind transects demonstrates that nitrous acid (HONO), a primary source of OH, is narrower than CO ( w _HONO / w _CO = 0.73-0.84 ± 0.01) and maleic anhydride (an OH oxidation product) is enhanced on plume edges ( w _{maleicanhydride} / w _CO = 1.06-1.12 ± 0.01). By contrast, NO ₃ production [P(NO ₃ )] occurs mainly at the plume center ( w _{P(NO 3 )} / w _CO = 0.91-1.00 ± 0.01). Phenolic emissions, highly reactive to OH and NO ₃ , are narrower than CO ( w _phenol / w _CO = 0.96 ± 0.03, w _catechol / w _CO = 0.91 ± 0.01, and w _{methylcatechol} / w _CO = 0.84 ± 0.01), suggesting that plume edge phenolic losses are the greatest. Yet, nitrophenolic aerosol, their oxidation product, is the greatest at the plume center ( w _{nitrophenolicaerosol} / w _CO = 0.95 ± 0.02). In a large plume case study, GOMECH suggests that nitrocatechol aerosol is most associated with P(NO ₃ ). Last, we corroborate GOMECH with a large eddy simulation model which suggests most (55%) of nitrocatechol is produced through NO ₃ in our case study.