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DOI10.5194/acp-21-16293-2021
Nighttime and daytime dark oxidation chemistry in wildfire plumes: An observation and model analysis of FIREX-AQ aircraft data
Decker Z.C.J.; Robinson M.A.; Barsanti K.C.; Bourgeois I.; Coggon M.M.; Digangi J.P.; Diskin G.S.; Flocke F.M.; Franchin A.; Fredrickson C.D.; Gkatzelis G.I.; Hall S.R.; Halliday H.; Holmes C.D.; Huey L.G.; Lee Y.R.; Lindaas J.; Middlebrook A.M.; Montzka D.D.; Moore R.; Neuman J.A.; Nowak J.B.; Palm B.B.; Peischl J.; Piel F.; Rickly P.S.; Rollins A.W.; Ryerson T.B.; Schwantes R.H.; Sekimoto K.; Thornhill L.; Thornton J.A.; Tyndall G.S.; Ullmann K.; Van Rooy P.; Veres P.R.; Warneke C.; Washenfelder R.A.; Weinheimer A.J.; Wiggins E.; Winstead E.; Wisthaler A.; Womack C.; Brown S.S.
发表日期2021
ISSN1680-7316
起始页码16293
结束页码16317
卷号21期号:21
英文摘要Wildfires are increasing in size across the western US, leading to increases in human smoke exposure and associated negative health impacts. The impact of biomass burning (BB) smoke, including wildfires, on regional air quality depends on emissions, transport, and chemistry, including oxidation of emitted BB volatile organic compounds (BBVOCs) by the hydroxyl radical (OH), nitrate radical (NO3), and ozone (O3). During the daytime, when light penetrates the plumes, BBVOCs are oxidized mainly by O3 and OH. In contrast, at night or in optically dense plumes, BBVOCs are oxidized mainly by O3 and NO3. This work focuses on the transition between daytime and nighttime oxidation, which has significant implications for the formation of secondary pollutants and loss of nitrogen oxides (NOxCombining double low lineNO+NO2) and has been understudied. We present wildfire plume observations made during FIREX-AQ (Fire Influence on Regional to Global Environments and Air Quality), a field campaign involving multiple aircraft, ground, satellite, and mobile platforms that took place in the United States in the summer of 2019 to study both wildfire and agricultural burning emissions and atmospheric chemistry. We use observations from two research aircraft, the NASA DC-8 and the NOAA Twin Otter, with a detailed chemical box model, including updated phenolic mechanisms, to analyze smoke sampled during midday, sunset, and nighttime. Aircraft observations suggest a range of NO3 production rates (0.1-1.5 ppbvh-1) in plumes transported during both midday and after dark. Modeled initial instantaneous reactivity toward BBVOCs for NO3, OH, and O3 is 80.1 %, 87.7 %, and 99.6 %, respectively. Initial NO3 reactivity is 10-104 times greater than typical values in forested or urban environments, and reactions with BBVOCs account for >97 % of NO3 loss in sunlit plumes (jNO2 up to 4×10-3s-1), while conventional photochemical NO3 loss through reaction with NO and photolysis are minor pathways. Alkenes and furans are mostly oxidized by OH and O3 (11 %-43 %, 54 %-88 % for alkenes; 18 %-55 %, 39 %-76 %, for furans, respectively), but phenolic oxidation is split between NO3, O3, and OH (26 %-52 %, 22 %-43 %, 16 %-33 %, respectively). Nitrate radical oxidation accounts for 26 %-52 % of phenolic chemical loss in sunset plumes and in an optically thick plume. Nitrocatechol yields varied between 33 % and 45 %, and NO3 chemistry in BB plumes emitted late in the day is responsible for 72 %-92 % (84 % in an optically thick midday plume) of nitrocatechol formation and controls nitrophenolic formation overall. As a result, overnight nitrophenolic formation pathways account for 56%±2% of NOx loss by sunrise the following day. In all but one overnight plume we modeled, there was remaining NOx (13 %-57 %) and BBVOCs (8 %-72 %) at sunrise. © 2021 The Author(s).
语种英语
scopus关键词air quality; atmospheric chemistry; atmospheric plume; NOAA satellite; oxidation; ozone; satellite data; satellite imagery; wildfire
来源期刊ATMOSPHERIC CHEMISTRY AND PHYSICS
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/246457
作者单位NOAA Chemical Sciences Laboratory (CSL), Boulder, CO 80305, United States; Cooperative Institute for Research in Environmental Sciences, University of Colorado Boulder, Boulder, CO 80309, United States; Department of Chemistry, University of Colorado Boulder, Boulder, CO 80309-0215, United States; Department of Chemical and Environmental Engineering, College of Engineering, Center for Environmental Research and Technology (CE-CERT), University of California, Riverside, Riverside, CA 92507, United States; NASA Langley Research Center, MS 483, Hampton, VA 23681, United States; Atmospheric Chemistry Observations and Modeling Laboratory, National Center for Atmospheric Research, Boulder, CO 80301, United States; Department of Atmospheric Sciences, University of Washington, Seattle, WA 98195, United States; Department of Earth, Ocean, and Atmospheric Science, Florida State University, Tallahassee, FL 32304, United States; School of Earth and Atmospheric Sciences, Georgia Institute of Technology, Atlant...
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Decker Z.C.J.,Robinson M.A.,Barsanti K.C.,et al. Nighttime and daytime dark oxidation chemistry in wildfire plumes: An observation and model analysis of FIREX-AQ aircraft data[J],2021,21(21).
APA Decker Z.C.J..,Robinson M.A..,Barsanti K.C..,Bourgeois I..,Coggon M.M..,...&Brown S.S..(2021).Nighttime and daytime dark oxidation chemistry in wildfire plumes: An observation and model analysis of FIREX-AQ aircraft data.ATMOSPHERIC CHEMISTRY AND PHYSICS,21(21).
MLA Decker Z.C.J.,et al."Nighttime and daytime dark oxidation chemistry in wildfire plumes: An observation and model analysis of FIREX-AQ aircraft data".ATMOSPHERIC CHEMISTRY AND PHYSICS 21.21(2021).
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