Parameterizations of US wildfire and prescribed fire emission ratios and emission factors based on FIREX-AQ aircraft measurements
Authors: Gkatzelis Georgios I. , Coggon Matthew M. , Stockwell Chelsea E. , Hornbrook Rebecca S. , Allen Hannah , Apel Eric C. , Bela Megan M. , Blake Donald R. , Bourgeois Ilann , Brown Steven S. , Campuzano-Jost Pedro , St. Clair Jason M. , Crawford James H. , Crounse John D. , Day Douglas A. , DiGangi Joshua P. , Diskin Glenn S. , Fried Alan , Gilman Jessica B. , Guo Hongyu , Hair Johnathan W. , Halliday Hannah S. , Hanisco Thomas F. , Hannun Reem , Hills Alan , Huey L. Gregory , Jimenez Jose L. , Katich Joseph M. , Lamplugh Aaron , Lee Young Ro , Liao Jin , Lindaas Jakob , McKeen Stuart A. , Mikoviny Tomas , Nault Benjamin A. , Neuman J. Andrew , Nowak John B. , Pagonis Demetrios , Peischl Jeff , Perring Anne E. , Piel Felix , Rickly Pamela S. , Robinson Michael A. , Rollins Andrew W. , Ryerson Thomas B. , Schueneman Melinda K. , Schwantes Rebecca H. , Schwarz Joshua P. , Sekimoto Kanako , Selimovic Vanessa , Shingler Taylor , Tanner David J. , Tomsche Laura , Vasquez Krystal T. , Veres Patrick R. , Washenfelder Rebecca , Weibring Petter , Wennberg Paul O. , Wisthaler Armin , Wolfe Glenn M. , Womack Caroline C. , Xu Lu , Ball Katherine , Yokelson Robert J. , Warneke Carsten 
Published: January 2024

Abstract. Extensive airborne measurements of non-methane organic gases (NMOGs), methane, nitrogen oxides, reduced nitrogen species, and aerosol emissions from US wild and prescribed fires were conducted during the 2019 NOAA/NASA Fire Influence on Regional to Global Environments and Air Quality campaign (FIREX-AQ). Here, we report the atmospheric enhancement ratios (ERs) and inferred emission factors (EFs) for compounds measured on board the NASA DC-8 research aircraft for nine wildfires and one prescribed fire, which encompass a range of vegetation types. We use photochemical proxies to identify young smoke and reduce the effects of chemical degradation on our emissions calculations. ERs and EFs calculated from FIREX-AQ observations agree within a factor of 2, with values reported from previous laboratory and field studies for more than 80 % of the carbon- and nitrogen-containing species. Wildfire emissions are parameterized based on correlations of the sum of NMOGs with reactive nitrogen oxides (NOy) to modified combustion efficiency (MCE) as well as other chemical signatures indicative of flaming/smoldering combustion, including carbon monoxide (CO), nitrogen dioxide (NO2), and black carbon aerosol. The sum of primary NMOG EFs correlates to MCE with an R2 of 0.68 and a slope of −296 ± 51 g kg−1, consistent with previous studies. The sum of the NMOG mixing ratios correlates well with CO with an R2 of 0.98 and a slope of 137 ± 4 ppbv of NMOGs per parts per million by volume (ppmv) of CO, demonstrating that primary NMOG emissions can be estimated from CO. Individual nitrogen-containing species correlate better with NO2, NOy, and black carbon than with CO. More than half of the NOy in fresh plumes is NO2 with an R2 of 0.95 and a ratio of NO2 to NOy of 0.55 ± 0.05 ppbv ppbv−1, highlighting that fast photochemistry had already occurred in the sampled fire plumes. The ratio of NOy to the sum of NMOGs follows trends observed in laboratory experiments and increases exponentially with MCE, due to increased emission of key nitrogen species and reduced emission of NMOGs at higher MCE during flaming combustion. These parameterizations will provide more accurate boundary conditions for modeling and satellite studies of fire plume chemistry and evolution to predict the downwind formation of secondary pollutants, including ozone and secondary organic aerosol.