Articles | Volume 21, issue 17
https://doi.org/10.5194/acp-21-13077-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/acp-21-13077-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
03 Sep 2021
Research article |
| 03 Sep 2021
| 03 Sep 2021
Isotopic evidence for dominant secondary production of HONO in near-ground wildfire plumes
Institute at Brown for Environment and Society, Brown University,
Providence, RI, USA
Department of Earth, Environmental and Planetary Sciences, Brown University,
Providence, RI, USA
Jack E. Dibb
Institute for the Study of Earth, Oceans and Space, University of New
Hampshire, Durham, NH, USA
Bruce E. Anderson
NASA Langley Research Center, Hampton, VA, USA
Claire Bekker
Institute at Brown for Environment and Society, Brown University,
Providence, RI, USA
Department of Earth, Environmental and Planetary Sciences, Brown University,
Providence, RI, USA
Danielle E. Blum
Institute at Brown for Environment and Society, Brown University,
Providence, RI, USA
Department of Chemistry, Brown University, Providence, RI, USA
Eric Heim
Institute for the Study of Earth, Oceans and Space, University of New
Hampshire, Durham, NH, USA
Carolyn E. Jordan
NASA Langley Research Center, Hampton, VA, USA
National Institute of Aerospace, Hampton, VA, USA
Emily E. Joyce
Institute at Brown for Environment and Society, Brown University,
Providence, RI, USA
Department of Earth, Environmental and Planetary Sciences, Brown University,
Providence, RI, USA
Jackson H. Kaspari
Department of Chemistry, University of New Hampshire, Durham, NH, USA
Hannah Munro
Institute for the Study of Earth, Oceans and Space, University of New
Hampshire, Durham, NH, USA
Wendell W. Walters
Institute at Brown for Environment and Society, Brown University,
Providence, RI, USA
Department of Earth, Environmental and Planetary Sciences, Brown University,
Providence, RI, USA
Meredith G. Hastings
Institute at Brown for Environment and Society, Brown University,
Providence, RI, USA
Department of Earth, Environmental and Planetary Sciences, Brown University,
Providence, RI, USA
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Atmos. Chem. Phys., 25, 10707–10730, https://doi.org/10.5194/acp-25-10707-2025, https://doi.org/10.5194/acp-25-10707-2025, 2025
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We studied how chemicals released from plants and pollution interact in the atmosphere, affecting air quality and climate. By combining laboratory experiments and chemistry models, we tracked unique chemical fingerprints to understand how nitrogen compounds transform to form particles in the air. Our findings help explain the role of these reactions in pollution and provide tools to improve predictions for cleaner air and better climate policies.
Laura M. D. Heinlein, Junwei He, Michael Oluwatoyin Sunday, Fangzhou Guo, James Campbell, Allison Moon, Sukriti Kapur, Ting Fang, Kasey Edwards, Meeta Cesler-Maloney, Alyssa J. Burns, Jack Dibb, William Simpson, Manabu Shiraiwa, Becky Alexander, Jingqiu Mao, James H. Flynn III, Jochen Stutz, and Cort Anastasio
Atmos. Chem. Phys., 25, 9561–9581, https://doi.org/10.5194/acp-25-9561-2025, https://doi.org/10.5194/acp-25-9561-2025, 2025
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Jason A. Miech, Joshua P. DiGangi, Glenn S. Diskin, Yonghoon Choi, Richard H. Moore, Luke D. Ziemba, Francesca Gallo, Carolyn E. Jordan, Michael A. Shook, Elizabeth B. Wiggins, Edward L. Winstead, Sayantee Roy, Young Ro Lee, Katherine Ball, John D. Crounse, Paul Wennberg, Felix Piel, Stefan Swift, Wojciech Wojnowski, and Armin Wisthaler
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Biomass burning is a significant source of greenhouse gases and airborne pollutants in Asia. Airborne measurements of greenhouse gas enhancement ratios, trace gases, and particle scattering were used to identify air masses impacted by biomass burning over several Asian countries during March and April of 2024. Further analysis using atmospheric transport models and satellite hotspot products was performed to understand the transport history of biomass burning impacted airmasses over Thailand.
Michael Oluwatoyin Sunday, Laura Marie Dahler Heinlein, Junwei He, Allison Moon, Sukriti Kapur, Ting Fang, Kasey C. Edwards, Fangzhou Guo, Jack Dibb, James H. Flynn III, Becky Alexander, Manabu Shiraiwa, and Cort Anastasio
Atmos. Chem. Phys., 25, 5087–5100, https://doi.org/10.5194/acp-25-5087-2025, https://doi.org/10.5194/acp-25-5087-2025, 2025
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Huan Fang and Wendell Walters
EGUsphere, https://doi.org/10.5194/egusphere-2025-923, https://doi.org/10.5194/egusphere-2025-923, 2025
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The Sulfur Tracking Mechanism in CMAQ was used to model the oxygen isotope anomaly (Δ17O) of aerosol sulfate (ASO4) for the first time. This approach allows for a qualitative analysis of sulfate (SO42-) formation processes and comparison with corresponding measurements.
Jan-Lukas Tirpitz, Santo Fedele Colosimo, Nathaniel Brockway, Robert Spurr, Matt Christi, Samuel Hall, Kirk Ullmann, Johnathan Hair, Taylor Shingler, Rodney Weber, Jack Dibb, Richard Moore, Elizabeth Wiggins, Vijay Natraj, Nicolas Theys, and Jochen Stutz
Atmos. Chem. Phys., 25, 1989–2015, https://doi.org/10.5194/acp-25-1989-2025, https://doi.org/10.5194/acp-25-1989-2025, 2025
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We combine plume composition data from the 2019 NASA FIREX-AQ campaign with state-of-the-art radiative transfer modeling techniques to calculate distributions of actinic flux and photolysis frequencies in a wildfire plume. Excellent agreement of the model and observations demonstrates the applicability of this approach to constrain photochemistry in such plumes. We identify limiting factors for the modeling accuracy and discuss spatial and spectral features of the distributions.
Kouji Adachi, Jack E. Dibb, Joseph M. Katich, Joshua P. Schwarz, Hongyu Guo, Pedro Campuzano-Jost, Jose L. Jimenez, Jeff Peischl, Christopher D. Holmes, and James Crawford
Atmos. Chem. Phys., 24, 10985–11004, https://doi.org/10.5194/acp-24-10985-2024, https://doi.org/10.5194/acp-24-10985-2024, 2024
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We examined aerosol particles from wildfires and identified tarballs (TBs) from the Fire Influence on Regional to Global Environments and Air Quality (FIREX-AQ) campaign. This study reveals the compositions, abundance, sizes, and mixing states of TBs and shows that TBs formed as the smoke aged for up to 5 h. This study provides measurements of TBs from various biomass-burning events and ages, enhancing our knowledge of TB emissions and our understanding of their climate impact.
Annelise Waling, Adam Herrington, Katharine Duderstadt, Jack Dibb, and Elizabeth Burakowski
Weather Clim. Dynam., 5, 1117–1135, https://doi.org/10.5194/wcd-5-1117-2024, https://doi.org/10.5194/wcd-5-1117-2024, 2024
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Atmospheric rivers (ARs) are channel-shaped features within the atmosphere that carry moisture from the mid-latitudes to the poles, bringing warm temperatures and moisture that can cause melt in the Arctic. We used variable-resolution grids to model ARs around the Greenland ice sheet and compared this output to uniform-resolution grids and reanalysis products. We found that the variable-resolution grids produced ARs and precipitation that were more similar to observation-based products.
Wendell W. Walters, Masayuki Takeuchi, Nga L. Ng, and Meredith G. Hastings
Geosci. Model Dev., 17, 4673–4687, https://doi.org/10.5194/gmd-17-4673-2024, https://doi.org/10.5194/gmd-17-4673-2024, 2024
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The study introduces a novel chemical mechanism for explicitly tracking oxygen isotope transfer in oxidized reactive nitrogen and odd oxygen using the Regional Atmospheric Chemistry Mechanism, version 2. This model enhances our ability to simulate and compare oxygen isotope compositions of reactive nitrogen, revealing insights into oxidation chemistry. The approach shows promise for improving atmospheric chemistry models and tropospheric oxidation capacity predictions.
Simon Kirschler, Christiane Voigt, Bruce E. Anderson, Gao Chen, Ewan C. Crosbie, Richard A. Ferrare, Valerian Hahn, Johnathan W. Hair, Stefan Kaufmann, Richard H. Moore, David Painemal, Claire E. Robinson, Kevin J. Sanchez, Amy J. Scarino, Taylor J. Shingler, Michael A. Shook, Kenneth L. Thornhill, Edward L. Winstead, Luke D. Ziemba, and Armin Sorooshian
Atmos. Chem. Phys., 23, 10731–10750, https://doi.org/10.5194/acp-23-10731-2023, https://doi.org/10.5194/acp-23-10731-2023, 2023
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In this study we present an overview of liquid and mixed-phase clouds and precipitation in the marine boundary layer over the western North Atlantic Ocean. We compare microphysical properties of pure liquid clouds to mixed-phase clouds and show that the initiation of the ice phase in mixed-phase clouds promotes precipitation. The observational data presented in this study are well suited for investigating the processes that give rise to liquid and mixed-phase clouds, ice, and precipitation.
Jessica M. Burger, Emily Joyce, Meredith G. Hastings, Kurt A. M. Spence, and Katye E. Altieri
Atmos. Chem. Phys., 23, 5605–5622, https://doi.org/10.5194/acp-23-5605-2023, https://doi.org/10.5194/acp-23-5605-2023, 2023
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A seasonal analysis of the nitrogen isotopes of atmospheric nitrate over the remote Southern Ocean reveals that similar natural NOx sources dominate in spring and summer, while winter is representative of background-level conditions. The oxygen isotopes suggest that similar oxidation pathways involving more ozone occur in spring and winter, while the hydroxyl radical is the main oxidant in summer. This work helps to constrain NOx cycling and oxidant budgets in a data-sparse remote marine region.
Haihui Zhu, Randall V. Martin, Betty Croft, Shixian Zhai, Chi Li, Liam Bindle, Jeffrey R. Pierce, Rachel Y.-W. Chang, Bruce E. Anderson, Luke D. Ziemba, Johnathan W. Hair, Richard A. Ferrare, Chris A. Hostetler, Inderjeet Singh, Deepangsu Chatterjee, Jose L. Jimenez, Pedro Campuzano-Jost, Benjamin A. Nault, Jack E. Dibb, Joshua S. Schwarz, and Andrew Weinheimer
Atmos. Chem. Phys., 23, 5023–5042, https://doi.org/10.5194/acp-23-5023-2023, https://doi.org/10.5194/acp-23-5023-2023, 2023
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Particle size of atmospheric aerosol is important for estimating its climate and health effects, but simulating atmospheric aerosol size is computationally demanding. This study derives a simple parameterization of the size of organic and secondary inorganic ambient aerosol that can be applied to atmospheric models. Applying this parameterization allows a better representation of the global spatial pattern of aerosol size, as verified by ground and airborne measurements.
Shixian Zhai, Daniel J. Jacob, Drew C. Pendergrass, Nadia K. Colombi, Viral Shah, Laura Hyesung Yang, Qiang Zhang, Shuxiao Wang, Hwajin Kim, Yele Sun, Jin-Soo Choi, Jin-Soo Park, Gan Luo, Fangqun Yu, Jung-Hun Woo, Younha Kim, Jack E. Dibb, Taehyoung Lee, Jin-Seok Han, Bruce E. Anderson, Ke Li, and Hong Liao
Atmos. Chem. Phys., 23, 4271–4281, https://doi.org/10.5194/acp-23-4271-2023, https://doi.org/10.5194/acp-23-4271-2023, 2023
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Anthropogenic fugitive dust in East Asia not only causes severe coarse particulate matter air pollution problems, but also affects fine particulate nitrate. Due to emission control efforts, coarse PM decreased steadily. We find that the decrease of coarse PM is a major driver for a lack of decrease of fine particulate nitrate, as it allows more nitric acid to form fine particulate nitrate. The continuing decrease of coarse PM requires more stringent ammonia and nitrogen oxides emission controls.
Claire Bekker, Wendell W. Walters, Lee T. Murray, and Meredith G. Hastings
Atmos. Chem. Phys., 23, 4185–4201, https://doi.org/10.5194/acp-23-4185-2023, https://doi.org/10.5194/acp-23-4185-2023, 2023
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Nitrate is a critical component of the atmosphere that degrades air quality and ecosystem health. We have investigated the nitrogen isotope compositions of nitrate from deposition samples collected across the northeastern United States. Spatiotemporal variability in the nitrogen isotope compositions was found to track with nitrate formation chemistry. Our results highlight that nitrogen isotope compositions may be a robust tool for improving model representation of nitrate chemistry.
Heejeong Kim, Wendell W. Walters, Claire Bekker, Lee T. Murray, and Meredith G. Hastings
Atmos. Chem. Phys., 23, 4203–4219, https://doi.org/10.5194/acp-23-4203-2023, https://doi.org/10.5194/acp-23-4203-2023, 2023
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Atmospheric nitrate has an important impact on human and ecosystem health. We evaluated atmospheric nitrate formation pathways in the northeastern US utilizing oxygen isotope compositions, which indicated a significant difference between the phases of nitrate (i.e., gas vs. particle). Comparing the observations with model simulations indicated that N2O5 hydrolysis chemistry was overpredicted. Our study has important implications for improving atmospheric chemistry model representation.
Francesca Gallo, Kevin J. Sanchez, Bruce E. Anderson, Ryan Bennett, Matthew D. Brown, Ewan C. Crosbie, Chris Hostetler, Carolyn Jordan, Melissa Yang Martin, Claire E. Robinson, Lynn M. Russell, Taylor J. Shingler, Michael A. Shook, Kenneth L. Thornhill, Elizabeth B. Wiggins, Edward L. Winstead, Armin Wisthaler, Luke D. Ziemba, and Richard H. Moore
Atmos. Chem. Phys., 23, 1465–1490, https://doi.org/10.5194/acp-23-1465-2023, https://doi.org/10.5194/acp-23-1465-2023, 2023
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We integrate in situ ship- and aircraft-based measurements of aerosol, trace gases, and meteorological parameters collected during the NASA North Atlantic Aerosols and Marine Ecosystems Study (NAAMES) field campaigns in the western North Atlantic Ocean region. A comprehensive characterization of the vertical profiles of aerosol properties under different seasonal regimes is provided for improving the understanding of aerosol key processes and aerosol–cloud interactions in marine regions.
Pamela S. Rickly, Hongyu Guo, Pedro Campuzano-Jost, Jose L. Jimenez, Glenn M. Wolfe, Ryan Bennett, Ilann Bourgeois, John D. Crounse, Jack E. Dibb, Joshua P. DiGangi, Glenn S. Diskin, Maximilian Dollner, Emily M. Gargulinski, Samuel R. Hall, Hannah S. Halliday, Thomas F. Hanisco, Reem A. Hannun, Jin Liao, Richard Moore, Benjamin A. Nault, John B. Nowak, Jeff Peischl, Claire E. Robinson, Thomas Ryerson, Kevin J. Sanchez, Manuel Schöberl, Amber J. Soja, Jason M. St. Clair, Kenneth L. Thornhill, Kirk Ullmann, Paul O. Wennberg, Bernadett Weinzierl, Elizabeth B. Wiggins, Edward L. Winstead, and Andrew W. Rollins
Atmos. Chem. Phys., 22, 15603–15620, https://doi.org/10.5194/acp-22-15603-2022, https://doi.org/10.5194/acp-22-15603-2022, 2022
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Biomass burning sulfur dioxide (SO2) emission factors range from 0.27–1.1 g kg-1 C. Biomass burning SO2 can quickly form sulfate and organosulfur, but these pathways are dependent on liquid water content and pH. Hydroxymethanesulfonate (HMS) appears to be directly emitted from some fire sources but is not the sole contributor to the organosulfur signal. It is shown that HMS and organosulfur chemistry may be an important S(IV) reservoir with the fate dependent on the surrounding conditions.
Rachel A. Bergin, Monica Harkey, Alicia Hoffman, Richard H. Moore, Bruce Anderson, Andreas Beyersdorf, Luke Ziemba, Lee Thornhill, Edward Winstead, Tracey Holloway, and Timothy H. Bertram
Atmos. Chem. Phys., 22, 15449–15468, https://doi.org/10.5194/acp-22-15449-2022, https://doi.org/10.5194/acp-22-15449-2022, 2022
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Correctly predicting aerosol surface area concentrations is important for determining the rate of heterogeneous reactions in chemical transport models. Here, we compare aircraft measurements of aerosol surface area with a regional model. In polluted air masses, we show that the model underpredicts aerosol surface area by a factor of 2. Despite this disagreement, the representation of heterogeneous chemistry still dominates the overall uncertainty in the loss rate of molecules such as N2O5.
Youhua Tang, Patrick C. Campbell, Pius Lee, Rick Saylor, Fanglin Yang, Barry Baker, Daniel Tong, Ariel Stein, Jianping Huang, Ho-Chun Huang, Li Pan, Jeff McQueen, Ivanka Stajner, Jose Tirado-Delgado, Youngsun Jung, Melissa Yang, Ilann Bourgeois, Jeff Peischl, Tom Ryerson, Donald Blake, Joshua Schwarz, Jose-Luis Jimenez, James Crawford, Glenn Diskin, Richard Moore, Johnathan Hair, Greg Huey, Andrew Rollins, Jack Dibb, and Xiaoyang Zhang
Geosci. Model Dev., 15, 7977–7999, https://doi.org/10.5194/gmd-15-7977-2022, https://doi.org/10.5194/gmd-15-7977-2022, 2022
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This paper compares two meteorological datasets for driving a regional air quality model: a regional meteorological model using WRF (WRF-CMAQ) and direct interpolation from an operational global model (GFS-CMAQ). In the comparison with surface measurements and aircraft data in summer 2019, these two methods show mixed performance depending on the corresponding meteorological settings. Direct interpolation is found to be a viable method to drive air quality models.
Wendell W. Walters, Madeline Karod, Emma Willcocks, Bok H. Baek, Danielle E. Blum, and Meredith G. Hastings
Atmos. Chem. Phys., 22, 13431–13448, https://doi.org/10.5194/acp-22-13431-2022, https://doi.org/10.5194/acp-22-13431-2022, 2022
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Atmospheric ammonia and its products are a significant source of urban haze and nitrogen deposition. We have investigated the seasonal source contributions to a mid-sized city in the northeastern US megalopolis utilizing geospatial statistical analysis and novel isotopic constraints, which indicate that vehicle emissions were significant components of the urban-reduced nitrogen budget. Reducing vehicle ammonia emissions should be considered to improve ecosystems and human health.
Ewan Crosbie, Luke D. Ziemba, Michael A. Shook, Claire E. Robinson, Edward L. Winstead, K. Lee Thornhill, Rachel A. Braun, Alexander B. MacDonald, Connor Stahl, Armin Sorooshian, Susan C. van den Heever, Joshua P. DiGangi, Glenn S. Diskin, Sarah Woods, Paola Bañaga, Matthew D. Brown, Francesca Gallo, Miguel Ricardo A. Hilario, Carolyn E. Jordan, Gabrielle R. Leung, Richard H. Moore, Kevin J. Sanchez, Taylor J. Shingler, and Elizabeth B. Wiggins
Atmos. Chem. Phys., 22, 13269–13302, https://doi.org/10.5194/acp-22-13269-2022, https://doi.org/10.5194/acp-22-13269-2022, 2022
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The linkage between cloud droplet and aerosol particle chemical composition was analyzed using samples collected in a polluted tropical marine environment. Variations in the droplet composition were related to physical and dynamical processes in clouds to assess their relative significance across three cases that spanned a range of rainfall amounts. In spite of the pollution, sea salt still remained a major contributor to the droplet composition and was preferentially enhanced in rainwater.
Simon Kirschler, Christiane Voigt, Bruce Anderson, Ramon Campos Braga, Gao Chen, Andrea F. Corral, Ewan Crosbie, Hossein Dadashazar, Richard A. Ferrare, Valerian Hahn, Johannes Hendricks, Stefan Kaufmann, Richard Moore, Mira L. Pöhlker, Claire Robinson, Amy J. Scarino, Dominik Schollmayer, Michael A. Shook, K. Lee Thornhill, Edward Winstead, Luke D. Ziemba, and Armin Sorooshian
Atmos. Chem. Phys., 22, 8299–8319, https://doi.org/10.5194/acp-22-8299-2022, https://doi.org/10.5194/acp-22-8299-2022, 2022
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In this study we show that the vertical velocity dominantly impacts the cloud droplet number concentration (NC) of low-level clouds over the western North Atlantic in the winter and summer season, while the cloud condensation nuclei concentration, aerosol size distribution and chemical composition impact NC within a season. The observational data presented in this study can evaluate and improve the representation of aerosol–cloud interactions for a wide range of conditions.
Linghan Zeng, Jack Dibb, Eric Scheuer, Joseph M. Katich, Joshua P. Schwarz, Ilann Bourgeois, Jeff Peischl, Tom Ryerson, Carsten Warneke, Anne E. Perring, Glenn S. Diskin, Joshua P. DiGangi, John B. Nowak, Richard H. Moore, Elizabeth B. Wiggins, Demetrios Pagonis, Hongyu Guo, Pedro Campuzano-Jost, Jose L. Jimenez, Lu Xu, and Rodney J. Weber
Atmos. Chem. Phys., 22, 8009–8036, https://doi.org/10.5194/acp-22-8009-2022, https://doi.org/10.5194/acp-22-8009-2022, 2022
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Wildfires emit aerosol particles containing brown carbon material that affects visibility and global climate and is toxic. Brown carbon is poorly characterized due to measurement limitations, and its evolution in the atmosphere is not well known. We report on aircraft measurements of brown carbon from large wildfires in the western United States. We compare two methods for measuring brown carbon and study the evolution of brown carbon in the smoke as it moved away from the burning regions.
Katherine R. Travis, James H. Crawford, Gao Chen, Carolyn E. Jordan, Benjamin A. Nault, Hwajin Kim, Jose L. Jimenez, Pedro Campuzano-Jost, Jack E. Dibb, Jung-Hun Woo, Younha Kim, Shixian Zhai, Xuan Wang, Erin E. McDuffie, Gan Luo, Fangqun Yu, Saewung Kim, Isobel J. Simpson, Donald R. Blake, Limseok Chang, and Michelle J. Kim
Atmos. Chem. Phys., 22, 7933–7958, https://doi.org/10.5194/acp-22-7933-2022, https://doi.org/10.5194/acp-22-7933-2022, 2022
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The 2016 Korea–United States Air Quality (KORUS-AQ) field campaign provided a unique set of observations to improve our understanding of PM2.5 pollution in South Korea. Models typically have errors in simulating PM2.5 in this region, which is of concern for the development of control measures. We use KORUS-AQ observations to improve our understanding of the mechanisms driving PM2.5 and the implications of model errors for determining PM2.5 that is attributable to local or foreign sources.
Joseph S. Schlosser, Connor Stahl, Armin Sorooshian, Yen Thi-Hoang Le, Ki-Joon Jeon, Peng Xian, Carolyn E. Jordan, Katherine R. Travis, James H. Crawford, Sung Yong Gong, Hye-Jung Shin, In-Ho Song, and Jong-sang Youn
Atmos. Chem. Phys., 22, 7505–7522, https://doi.org/10.5194/acp-22-7505-2022, https://doi.org/10.5194/acp-22-7505-2022, 2022
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During a major haze pollution episode in March 2019, anthropogenic emissions were dominant in the boundary layer over Incheon and Seoul, South Korea. Using supermicrometer and submicrometer size- and chemistry-resolved aerosol particle measurements taken during this haze pollution period, this work shows that local emissions and a shallow boundary layer, enhanced humidity, and low temperature promoted local heterogeneous formation of secondary inorganic and organic aerosol species.
Joel C. Corbin, Tobias Schripp, Bruce E. Anderson, Greg J. Smallwood, Patrick LeClercq, Ewan C. Crosbie, Steven Achterberg, Philip D. Whitefield, Richard C. Miake-Lye, Zhenhong Yu, Andrew Freedman, Max Trueblood, David Satterfield, Wenyan Liu, Patrick Oßwald, Claire Robinson, Michael A. Shook, Richard H. Moore, and Prem Lobo
Atmos. Meas. Tech., 15, 3223–3242, https://doi.org/10.5194/amt-15-3223-2022, https://doi.org/10.5194/amt-15-3223-2022, 2022
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The combustion of sustainable aviation fuels in aircraft engines produces particulate matter (PM) emissions with different properties than conventional fuels due to changes in fuel composition. Consequently, the response of various diagnostic instruments to PM emissions may be impacted. We found no significant instrument biases in terms of particle mass, number, and size measurements for conventional and sustainable aviation fuel blends despite large differences in the magnitude of emissions.
Meloë S. F. Kacenelenbogen, Qian Tan, Sharon P. Burton, Otto P. Hasekamp, Karl D. Froyd, Yohei Shinozuka, Andreas J. Beyersdorf, Luke Ziemba, Kenneth L. Thornhill, Jack E. Dibb, Taylor Shingler, Armin Sorooshian, Reed W. Espinosa, Vanderlei Martins, Jose L. Jimenez, Pedro Campuzano-Jost, Joshua P. Schwarz, Matthew S. Johnson, Jens Redemann, and Gregory L. Schuster
Atmos. Chem. Phys., 22, 3713–3742, https://doi.org/10.5194/acp-22-3713-2022, https://doi.org/10.5194/acp-22-3713-2022, 2022
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The impact of aerosols on Earth's radiation budget and human health is important and strongly depends on their composition. One desire of our scientific community is to derive the composition of the aerosol from satellite sensors. However, satellites observe aerosol optical properties (and not aerosol composition) based on remote sensing instrumentation. This study assesses how much aerosol optical properties can tell us about aerosol composition.
Kevin J. Sanchez, Bo Zhang, Hongyu Liu, Matthew D. Brown, Ewan C. Crosbie, Francesca Gallo, Johnathan W. Hair, Chris A. Hostetler, Carolyn E. Jordan, Claire E. Robinson, Amy Jo Scarino, Taylor J. Shingler, Michael A. Shook, Kenneth L. Thornhill, Elizabeth B. Wiggins, Edward L. Winstead, Luke D. Ziemba, Georges Saliba, Savannah L. Lewis, Lynn M. Russell, Patricia K. Quinn, Timothy S. Bates, Jack Porter, Thomas G. Bell, Peter Gaube, Eric S. Saltzman, Michael J. Behrenfeld, and Richard H. Moore
Atmos. Chem. Phys., 22, 2795–2815, https://doi.org/10.5194/acp-22-2795-2022, https://doi.org/10.5194/acp-22-2795-2022, 2022
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Atmospheric particle concentrations impact clouds, which strongly impact the amount of sunlight reflected back into space and the overall climate. Measurements of particles over the ocean are rare and expensive to collect, so models are necessary to fill in the gaps by simulating both particle and clouds. However, some measurements are needed to test the accuracy of the models. Here, we measure changes in particles in different weather conditions, which are ideal for comparison with models.
Jessica M. Burger, Julie Granger, Emily Joyce, Meredith G. Hastings, Kurt A. M. Spence, and Katye E. Altieri
Atmos. Chem. Phys., 22, 1081–1096, https://doi.org/10.5194/acp-22-1081-2022, https://doi.org/10.5194/acp-22-1081-2022, 2022
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The nitrogen (N) isotopic composition of atmospheric nitrate in the Southern Ocean (SO) marine boundary layer (MBL) reveals the importance of oceanic alkyl nitrate emissions as a source of reactive N to the atmosphere. The oxygen isotopic composition suggests peroxy radicals contribute up to 63 % to NO oxidation and that nitrate forms via the OH pathway. This work improves our understanding of reactive N sources and cycling in a remote marine region, a proxy for the pre-industrial atmosphere.
Dongwook Kim, Changmin Cho, Seokhan Jeong, Soojin Lee, Benjamin A. Nault, Pedro Campuzano-Jost, Douglas A. Day, Jason C. Schroder, Jose L. Jimenez, Rainer Volkamer, Donald R. Blake, Armin Wisthaler, Alan Fried, Joshua P. DiGangi, Glenn S. Diskin, Sally E. Pusede, Samuel R. Hall, Kirk Ullmann, L. Gregory Huey, David J. Tanner, Jack Dibb, Christoph J. Knote, and Kyung-Eun Min
Atmos. Chem. Phys., 22, 805–821, https://doi.org/10.5194/acp-22-805-2022, https://doi.org/10.5194/acp-22-805-2022, 2022
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CHOCHO was simulated using a 0-D box model constrained by measurements during the KORUS-AQ mission. CHOCHO concentration was high in large cities, aromatics being the most important precursors. Loss path to aerosol was the highest sink, contributing to ~ 20 % of secondary organic aerosol formation. Our work highlights that simple CHOCHO surface uptake approach is valid only for low aerosol conditions and more work is required to understand CHOCHO solubility in high-aerosol conditions.
Tiziana Bräuer, Christiane Voigt, Daniel Sauer, Stefan Kaufmann, Valerian Hahn, Monika Scheibe, Hans Schlager, Felix Huber, Patrick Le Clercq, Richard H. Moore, and Bruce E. Anderson
Atmos. Chem. Phys., 21, 16817–16826, https://doi.org/10.5194/acp-21-16817-2021, https://doi.org/10.5194/acp-21-16817-2021, 2021
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Over half of aviation climate impact is caused by contrails. Biofuels can reduce the ice crystal numbers in contrails and mitigate the climate impact. The experiment ECLIF II/NDMAX in 2018 assessed the effects of biofuels on contrails and aviation emissions. The NASA DC-8 aircraft performed measurements inside the contrail of the DLR A320. One reference fuel and two blends of the biofuel HEFA and kerosene are analysed. We find a max reduction of contrail ice numbers through biofuel use of 40 %.
Shixian Zhai, Daniel J. Jacob, Jared F. Brewer, Ke Li, Jonathan M. Moch, Jhoon Kim, Seoyoung Lee, Hyunkwang Lim, Hyun Chul Lee, Su Keun Kuk, Rokjin J. Park, Jaein I. Jeong, Xuan Wang, Pengfei Liu, Gan Luo, Fangqun Yu, Jun Meng, Randall V. Martin, Katherine R. Travis, Johnathan W. Hair, Bruce E. Anderson, Jack E. Dibb, Jose L. Jimenez, Pedro Campuzano-Jost, Benjamin A. Nault, Jung-Hun Woo, Younha Kim, Qiang Zhang, and Hong Liao
Atmos. Chem. Phys., 21, 16775–16791, https://doi.org/10.5194/acp-21-16775-2021, https://doi.org/10.5194/acp-21-16775-2021, 2021
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Geostationary satellite aerosol optical depth (AOD) has tremendous potential for monitoring surface fine particulate matter (PM2.5). Our study explored the physical relationship between AOD and PM2.5 by integrating data from surface networks, aircraft, and satellites with the GEOS-Chem chemical transport model. We quantitatively showed that accurate simulation of aerosol size distributions, boundary layer depths, relative humidity, coarse particles, and diurnal variations in PM2.5 are essential.
Charles A. Brock, Karl D. Froyd, Maximilian Dollner, Christina J. Williamson, Gregory Schill, Daniel M. Murphy, Nicholas J. Wagner, Agnieszka Kupc, Jose L. Jimenez, Pedro Campuzano-Jost, Benjamin A. Nault, Jason C. Schroder, Douglas A. Day, Derek J. Price, Bernadett Weinzierl, Joshua P. Schwarz, Joseph M. Katich, Siyuan Wang, Linghan Zeng, Rodney Weber, Jack Dibb, Eric Scheuer, Glenn S. Diskin, Joshua P. DiGangi, ThaoPaul Bui, Jonathan M. Dean-Day, Chelsea R. Thompson, Jeff Peischl, Thomas B. Ryerson, Ilann Bourgeois, Bruce C. Daube, Róisín Commane, and Steven C. Wofsy
Atmos. Chem. Phys., 21, 15023–15063, https://doi.org/10.5194/acp-21-15023-2021, https://doi.org/10.5194/acp-21-15023-2021, 2021
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The Atmospheric Tomography Mission was an airborne study that mapped the chemical composition of the remote atmosphere. From this, we developed a comprehensive description of aerosol properties that provides a unique, global-scale dataset against which models can be compared. The data show the polluted nature of the remote atmosphere in the Northern Hemisphere and quantify the contributions of sea salt, dust, soot, biomass burning particles, and pollution particles to the haziness of the sky.
Linghan Zeng, Amy P. Sullivan, Rebecca A. Washenfelder, Jack Dibb, Eric Scheuer, Teresa L. Campos, Joseph M. Katich, Ezra Levin, Michael A. Robinson, and Rodney J. Weber
Atmos. Meas. Tech., 14, 6357–6378, https://doi.org/10.5194/amt-14-6357-2021, https://doi.org/10.5194/amt-14-6357-2021, 2021
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Three online systems for measuring water-soluble brown carbon are compared. A mist chamber and two different particle-into-liquid samplers were deployed on separate research aircraft targeting wildfires and followed a similar detection method using a long-path liquid waveguide with a spectrometer to measure the light absorption from 300 to 700 nm. Detection limits, signal hysteresis and other sampling issues are compared, and further improvements of these liquid-based systems are provided.
Huan Fang, Wendell W. Walters, David Mase, and Greg Michalski
Geosci. Model Dev., 14, 5001–5022, https://doi.org/10.5194/gmd-14-5001-2021, https://doi.org/10.5194/gmd-14-5001-2021, 2021
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A new photochemical reaction scheme that incorporates nitrogen isotopes has been developed to simulate isotope tracers in air pollution. The model contains 16 N compounds, and 96 reactions involving N used in the Regional Atmospheric Chemistry Mechanism (RACM) were replicated using 15N in a new mechanism called iNRACM. The model is able to predict d15N variations in NOx, HONO, and HNO3 that are similar to those observed in aerosol and gases in the troposphere.
J. Brant Dodson, Patrick C. Taylor, Richard H. Moore, David H. Bromwich, Keith M. Hines, Kenneth L. Thornhill, Chelsea A. Corr, Bruce E. Anderson, Edward L. Winstead, and Joseph R. Bennett
Atmos. Chem. Phys., 21, 11563–11580, https://doi.org/10.5194/acp-21-11563-2021, https://doi.org/10.5194/acp-21-11563-2021, 2021
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Aircraft in situ observations of low-level Beaufort Sea cloud properties and thermodynamics from the ARISE campaign are compared with the Arctic System Reanalysis (ASR) to better understand deficiencies in simulated clouds. ASR produces too little cloud water, which coincides with being too warm and dry. In addition, ASR struggles to produce cloud water even in favorable thermodynamic conditions. A random sampling experiment also shows the effects of the limited aircraft sampling on the results.
Richard H. Moore, Elizabeth B. Wiggins, Adam T. Ahern, Stephen Zimmerman, Lauren Montgomery, Pedro Campuzano Jost, Claire E. Robinson, Luke D. Ziemba, Edward L. Winstead, Bruce E. Anderson, Charles A. Brock, Matthew D. Brown, Gao Chen, Ewan C. Crosbie, Hongyu Guo, Jose L. Jimenez, Carolyn E. Jordan, Ming Lyu, Benjamin A. Nault, Nicholas E. Rothfuss, Kevin J. Sanchez, Melinda Schueneman, Taylor J. Shingler, Michael A. Shook, Kenneth L. Thornhill, Nicholas L. Wagner, and Jian Wang
Atmos. Meas. Tech., 14, 4517–4542, https://doi.org/10.5194/amt-14-4517-2021, https://doi.org/10.5194/amt-14-4517-2021, 2021
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Atmospheric particles are everywhere and exist in a range of sizes, from a few nanometers to hundreds of microns. Because particle size determines the behavior of chemical and physical processes, accurately measuring particle sizes is an important and integral part of atmospheric field measurements! Here, we discuss the performance of two commonly used particle sizers and how changes in particle composition and optical properties may result in sizing uncertainties, which we quantify.
Veronica R. Rollinson, Julie Granger, Sydney C. Clark, Mackenzie L. Blanusa, Claudia P. Koerting, Jamie M. P. Vaudrey, Lija A. Treibergs, Holly C. Westbrook, Catherine M. Matassa, Meredith G. Hastings, and Craig R. Tobias
Biogeosciences, 18, 3421–3444, https://doi.org/10.5194/bg-18-3421-2021, https://doi.org/10.5194/bg-18-3421-2021, 2021
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We measured nutrients and the naturally occurring nitrogen (N) and oxygen (O) stable isotope ratios of nitrate discharged from a New England river over an annual cycle, to monitor N loading and identify dominant sources from the watershed. We uncovered a seasonality to loading and sources of N from the watershed. Seasonality in the nitrate isotope ratios also informed on N cycling, conforming to theoretical expectations of riverine nutrient cycling.
Hongyu Guo, Pedro Campuzano-Jost, Benjamin A. Nault, Douglas A. Day, Jason C. Schroder, Dongwook Kim, Jack E. Dibb, Maximilian Dollner, Bernadett Weinzierl, and Jose L. Jimenez
Atmos. Meas. Tech., 14, 3631–3655, https://doi.org/10.5194/amt-14-3631-2021, https://doi.org/10.5194/amt-14-3631-2021, 2021
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We utilize a set of high-quality datasets collected during the NASA Atmospheric Tomography Mission to investigate the impact of differences in observable particle sizes across aerosol instruments in aerosol measurement comparisons. Very good agreement was found between chemically and physically derived submicron aerosol volume. Results support a lack of significant unknown biases in the response of an Aerodyne aerosol mass spectrometer (AMS) when sampling remote aerosols across the globe.
Melinda K. Schueneman, Benjamin A. Nault, Pedro Campuzano-Jost, Duseong S. Jo, Douglas A. Day, Jason C. Schroder, Brett B. Palm, Alma Hodzic, Jack E. Dibb, and Jose L. Jimenez
Atmos. Meas. Tech., 14, 2237–2260, https://doi.org/10.5194/amt-14-2237-2021, https://doi.org/10.5194/amt-14-2237-2021, 2021
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This work focuses on two important properties of the aerosol, acidity, and sulfate composition, which is important for our understanding of aerosol health and environmental impacts. We explore different methods to understand the composition of the aerosol with measurements from a specific instrument and apply those methods to a large dataset. These measurements are confounded by other factors, making it challenging to predict aerosol sulfate composition; pH estimations, however, show promise.
Guitao Shi, Hongmei Ma, Zhengyi Hu, Zhenlou Chen, Chunlei An, Su Jiang, Yuansheng Li, Tianming Ma, Jinhai Yu, Danhe Wang, Siyu Lu, Bo Sun, and Meredith G. Hastings
The Cryosphere, 15, 1087–1095, https://doi.org/10.5194/tc-15-1087-2021, https://doi.org/10.5194/tc-15-1087-2021, 2021
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It is important to understand atmospheric chemistry over Antarctica under a changing climate. Thus snow collected on a traverse from the coast to Dome A was used to investigate variations in snow chemistry. The non-sea-salt fractions of K+, Mg2+, and Ca2+ are associated with terrestrial inputs, and nssCl− is from HCl. In general, proportions of non-sea-salt fractions of ions to the totals are higher in the interior areas than on the coast, and the proportions are higher in summer than in winter.
Carolyn E. Jordan, Ryan M. Stauffer, Brian T. Lamb, Charles H. Hudgins, Kenneth L. Thornhill, Gregory L. Schuster, Richard H. Moore, Ewan C. Crosbie, Edward L. Winstead, Bruce E. Anderson, Robert F. Martin, Michael A. Shook, Luke D. Ziemba, Andreas J. Beyersdorf, Claire E. Robinson, Chelsea A. Corr, and Maria A. Tzortziou
Atmos. Meas. Tech., 14, 695–713, https://doi.org/10.5194/amt-14-695-2021, https://doi.org/10.5194/amt-14-695-2021, 2021
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First field data from a custom-built in situ instrument measuring hyperspectral (300–700 nm, 0.8 nm resolution) ambient atmospheric aerosol extinction are presented. The advantage of this capability is that it can be directly linked to other in situ techniques that measure physical and chemical properties of atmospheric aerosols. Second-order polynomials provided a better fit to the data than traditional power law fits, yielding greater discrimination among distinct ambient aerosol populations.
Carolyn E. Jordan, Ryan M. Stauffer, Brian T. Lamb, Michael Novak, Antonio Mannino, Ewan C. Crosbie, Gregory L. Schuster, Richard H. Moore, Charles H. Hudgins, Kenneth L. Thornhill, Edward L. Winstead, Bruce E. Anderson, Robert F. Martin, Michael A. Shook, Luke D. Ziemba, Andreas J. Beyersdorf, Claire E. Robinson, Chelsea A. Corr, and Maria A. Tzortziou
Atmos. Meas. Tech., 14, 715–736, https://doi.org/10.5194/amt-14-715-2021, https://doi.org/10.5194/amt-14-715-2021, 2021
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In situ measurements of ambient atmospheric aerosol hyperspectral (300–700 nm) optical properties (extinction, total absorption, water- and methanol-soluble absorption) were observed around the Korean peninsula. Such in situ observations provide a direct link between ambient aerosol optical properties and their physicochemical properties. The benefit of hyperspectral measurements is evident as simple mathematical functions could not fully capture the observed spectral detail of ambient aerosols.
Kevin J. Sanchez, Bo Zhang, Hongyu Liu, Georges Saliba, Chia-Li Chen, Savannah L. Lewis, Lynn M. Russell, Michael A. Shook, Ewan C. Crosbie, Luke D. Ziemba, Matthew D. Brown, Taylor J. Shingler, Claire E. Robinson, Elizabeth B. Wiggins, Kenneth L. Thornhill, Edward L. Winstead, Carolyn Jordan, Patricia K. Quinn, Timothy S. Bates, Jack Porter, Thomas G. Bell, Eric S. Saltzman, Michael J. Behrenfeld, and Richard H. Moore
Atmos. Chem. Phys., 21, 831–851, https://doi.org/10.5194/acp-21-831-2021, https://doi.org/10.5194/acp-21-831-2021, 2021
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Models describing atmospheric airflow were combined with satellite measurements representative of marine phytoplankton and other meteorological variables. These combined variables were compared to measured aerosol to identify upwind influences on aerosol concentrations. Results indicate that phytoplankton production rates upwind impact the aerosol mass. Also, results suggest that the condensation of mass onto short-lived large sea spray particles may be a significant sink of aerosol mass.
Benjamin A. Nault, Pedro Campuzano-Jost, Douglas A. Day, Hongyu Guo, Duseong S. Jo, Anne V. Handschy, Demetrios Pagonis, Jason C. Schroder, Melinda K. Schueneman, Michael J. Cubison, Jack E. Dibb, Alma Hodzic, Weiwei Hu, Brett B. Palm, and Jose L. Jimenez
Atmos. Meas. Tech., 13, 6193–6213, https://doi.org/10.5194/amt-13-6193-2020, https://doi.org/10.5194/amt-13-6193-2020, 2020
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Collecting particulate matter, or aerosols, onto filters to be analyzed offline is a widely used method to investigate the mass concentration and chemical composition of the aerosol, especially the inorganic portion. Here, we show that acidic aerosol (sulfuric acid) collected onto filters and then exposed to high ammonia mixing ratios (from human emissions) will lead to biases in the ammonium collected onto filters, and the uptake of ammonia is rapid (< 10 s), which impacts the filter data.
Cited articles
Akagi, S. K., Yokelson, R. J., Wiedinmyer, C., Alvarado, M. J., Reid, J. S.,
Karl, T., Crounse, J. D., and Wennberg, P. O.: Emission factors for open and
domestic biomass burning for use in atmospheric models, Atmos. Chem. Phys.,
11, 4039–4072, https://doi.org/10.5194/acp-11-4039-2011, 2011.
Akagi, S. K., Craven, J. S., Taylor, J. W., McMeeking, G. R., Yokelson, R.
J., Burling, I. R., Urbanski, S. P., Wold, C. E., Seinfeld, J. H., Coe, H.,
Alvarado, M. J., and Weise, D. R.: Evolution of trace gases and particles
emitted by a chaparral fire in California, Atmos. Chem. Phys., 12,
1397–1421, https://doi.org/10.5194/acp-12-1397-2012, 2012.
Alvarado, M. J. and Prinn, R. G.: Formation of ozone and growth of aerosols
in young smoke plumes from biomass burning: 1. Lagrangian parcel studies, J.
Geophys. Res.-Atmos., 114, D09306, https://doi.org/10.1029/2008JD011144,
2009.
Alvarado, M. J., Logan, J. A., Mao, J., Apel, E., Riemer, D., Blake, D.,
Cohen, R. C., Min, K.-E., Perring, A. E., Browne, E. C., Wooldridge, P. J.,
Diskin, G. S., Sachse, G. W., Fuelberg, H., Sessions, W. R., Harrigan, D.
L., Huey, G., Liao, J., Case-Hanks, A., Jimenez, J. L., Cubison, M. J., Vay,
S. A., Weinheimer, A. J., Knapp, D. J., Montzka, D. D., Flocke, F. M.,
Pollack, I. B., Wennberg, P. O., Kurten, A., Crounse, J., Clair, J. M. S.,
Wisthaler, A., Mikoviny, T., Yantosca, R. M., Carouge, C. C., and Le Sager,
P.: Nitrogen oxides and PAN in plumes from boreal fires during ARCTAS-B and
their impact on ozone: an integrated analysis of aircraft and satellite
observations, Atmos. Chem. Phys., 10, 9739–9760,
https://doi.org/10.5194/acp-10-9739-2010, 2010.
Alvarado, M. J., Lonsdale, C. R., Yokelson, R. J., Akagi, S. K., Coe, H.,
Craven, J. S., Fischer, E. V., McMeeking, G. R., Seinfeld, J. H., Soni, T.,
Taylor, J. W., Weise, D. R., and Wold, C. E.: Investigating the links
between ozone and organic aerosol chemistry in a biomass burning plume from
a prescribed fire in California chaparral, Atmos. Chem. Phys., 15,
6667–6688, https://doi.org/10.5194/acp-15-6667-2015, 2015.
Ammann, M., Kalberer, M., Jost, D. T., Tobler, L., Rössler, E., Piguet,
D., Gäggeler, H. W., and Baltensperger, U.: Heterogeneous production of
nitrous acid on soot in polluted air masses, Nature, 395, 157–160,
https://doi.org/10.1038/25965, 1998.
Baergen, A. M. and Donaldson, D. J.: Photochemical Renoxification of Nitric
Acid on Real Urban Grime, Environ. Sci. Technol., 47, 815–820,
https://doi.org/10.1021/es3037862, 2013.
Baergen, A. M. and Donaldson, D. J.: Formation of reactive nitrogen oxides
from urban grime photochemistry, Atmos. Chem. Phys., 16, 6355–6363,
https://doi.org/10.5194/acp-16-6355-2016, 2016.
Baylon, P., Jaffe, D. A., Hall, S. R., Ullmann, K., Alvarado, M. J., and
Lefer, B. L.: Impact of Biomass Burning Plumes on Photolysis Rates and Ozone
Formation at the Mount Bachelor Observatory, J. Geophys. Res.-Atmos., 123,
2272–2284, https://doi.org/10.1002/2017JD027341, 2018.
Berhanu, T. A., Meusinger, C., Erbland, J., Jost, R., Bhattacharya, S. K.,
Johnson, M. S., and Savarino, J.: Laboratory study of nitrate photolysis in
Antarctic snow, II. Isotopic effects and wavelength dependence, J. Chem.
Phys., 140, 244306, https://doi.org/10.1063/1.4882899, 2014.
Berhanu, T. A., Savarino, J., Erbland, J., Vicars, W. C., Preunkert, S.,
Martins, J. F., and Johnson, M. S.: Isotopic effects of nitrate
photochemistry in snow: a field study at Dome C, Antarctica, Atmos. Chem.
Phys., 15, 11243–11256, https://doi.org/10.5194/acp-15-11243-2015, 2015.
Böhlke, J. K., Mroczkowski, S. J., and Coplen, T. B.: Oxygen isotopes in
nitrate: new reference materials for 18O:17O:16O measurements and
observations on nitrate-water equilibration, Rapid Commun. Mass Spectrom.,
17, 1835–1846, https://doi.org/10.1002/rcm.1123, 2003.
Burkholder, J. B., Sander, S. P., Abbatt, J., Barker, J. R., Cappa, C.,
Crounse, J. D., Dibble, T. S., Huie, R. E., Kolb, C. E., Kurylo, M. J.,
Orkin, V. L., Percival, C. J., Wilmouth, D. M. and Wine P. H.: Chemical
Kinetics and Photochemical Data for Use in Atmospheric Studies, Evaluation
No. 19, JPL Publication 19-5, Jet Propulsion Laboratory, Pasadena, 2019.
Casciotti, K. L., Sigman, D. M., Hastings, M. G., Böhlke, J. K., and
Hilkert, A.: Measurement of the Oxygen Isotopic Composition of Nitrate in
Seawater and Freshwater Using the Denitrifier Method, Anal. Chem., 74,
4905–4912, https://doi.org/10.1021/ac020113w, 2002.
Chai, J.: Isotopic evidence for dominant secondary production of HONO in near-ground wildfire plumes, Brown University Open Data Collection, Brown Digital Repository [data set], Brown University Library, https://doi.org/10.26300/k056-fs32 (last access: 15 January 2021), 2020.
Chai, J. and Dibble, T. S.: Pressure Dependence and Kinetic Isotope Effects
in the Absolute Rate Constant for Methoxy Radical Reacting with NO2,
Int. J. Chem. Kinet., 46, 501–511, https://doi.org/10.1002/kin.20865, 2014.
Chai, J. and Hastings, M.: Collection Method for Isotopic Analysis of
Gaseous Nitrous Acid, Anal. Chem., 90, 830–838,
https://doi.org/10.1021/acs.analchem.7b03561, 2018.
Chai, J., Miller, D. J., Scheuer, E., Dibb, J., Selimovic, V., Yokelson, R.,
Zarzana, K. J., Brown, S. S., Koss, A. R., Warneke, C., and Hastings, M.:
Isotopic characterization of nitrogen oxides (NOx), nitrous acid
(HONO), and nitrate (pNO
Cox, R. A., Derwent, R. G., Kearsey, S. V., Batt, L., and Patrick, K. G.:
Photolysis of methyl nitrite: kinetics of the reaction of the methoxy
radical with O2, J. Photochem., 13, 149–163,
https://doi.org/10.1016/0047-2670(80)85006-4, 1980.
de Gouw, J. A., Warneke, C., Stohl, A., Wollny, A. G., Brock, C. A., Cooper,
O. R., Holloway, J. S., Trainer, M., Fehsenfeld, F. C., Atlas, E. L.,
Donnelly, S. G., Stroud, V., and Lueb, A.: Volatile organic compounds
composition of merged and aged forest fire plumes from Alaska and western
Canada, J. Geophys. Res.-Atmos., 111, D10303, https://doi.org/10.1029/2005JD006175,
2006.
Donaldson, M. A., Bish, D. L., and Raff, J. D.: Soil surface acidity plays a
determining role in the atmospheric-terrestrial exchange of nitrous acid,
P. Natl. Acad. Sci. USA, 111, 18472–18477,
https://doi.org/10.1073/pnas.1418545112, 2014a.
Donaldson, M. A., Berke, A. E., and Raff, J. D.: Uptake of Gas Phase Nitrous
Acid onto Boundary Layer Soil Surfaces, Environ. Sci. Technol., 48,
375–383, https://doi.org/10.1021/es404156a, 2014b.
Fibiger, D. L. and Hastings, M. G.: First Measurements of the Nitrogen
Isotopic Composition of NOx from Biomass Burning, Environ. Sci. Technol.,
50, 11569–11574, https://doi.org/10.1021/acs.est.6b03510, 2016.
Fibiger, D. L., Hastings, M. G., Lew, A. F., and Peltier, R. E.: Collection
of NO and NO2 for Isotopic Analysis of NOx Emissions, Anal. Chem., 86,
12115–12121, https://doi.org/10.1021/ac502968e, 2014.
Finlayson-Pitts, B. J., Wingen, L. M., Sumner, A. L., Syomin, D., and
Ramazan, K. A.: The heterogeneous hydrolysis of NO2 in laboratory systems
and in outdoor and indoor atmospheres: An integrated mechanism, Phys. Chem.
Chem. Phys., 5, 223–242, https://doi.org/10.1039/B208564J, 2003.
Fischer, E. V., Jaffe, D. A., Reidmiller, D. R., and Jaeglé, L.:
Meteorological controls on observed peroxyacetyl nitrate at Mount Bachelor
during the spring of 2008, J. Geophys. Res.-Atmos., 115,
https://doi.org/10.1029/2009JD012776, 2010.
Forster, R., Frost, M., Fulle, D., Hamann, H. F., Hippler, H., Schlepegrell,
A., and Troe, J.: High pressure range of the addition of HO to HO, NO,
NO2, and CO, I. Saturated laser induced fluorescence measurements at
298 K, J. Chem. Phys., 103, 2949–2958, https://doi.org/10.1063/1.470482,
1995.
Frey, M. M., Savarino, J., Morin, S., Erbland, J., and Martins, J. M. F.:
Photolysis imprint in the nitrate stable isotope signal in snow and
atmosphere of East Antarctica and implications for reactive nitrogen
cycling, Atmos. Chem. Phys., 9, 8681–8696,
https://doi.org/10.5194/acp-9-8681-2009, 2009.
George, C., Strekowski, R. S., Kleffmann, J., Stemmler, K., and Ammann, M.:
Photoenhanced uptake of gaseous NO2 on solid organic compounds: a
photochemical source of HONO?, Faraday Discuss., 130, 195–210,
https://doi.org/10.1039/b417888m, 2005.
Hanson, D. R.: Surface-Specific Reactions on Liquids, J. Phys. Chem. B, 101,
4998–5001, https://doi.org/10.1021/jp970461f, 1997.
Hastings, M. G., Jarvis, J. C., and Steig, E. J.: Anthropogenic Impacts on
Nitrogen Isotopes of Ice-Core Nitrate, Science, 324, 1288–1288,
https://doi.org/10.1126/science.1170510, 2009.
Jaffe, D. and Briggs, N.: Ozone production from wildfires: A critical
review, Atmos. Environ., 51, 1–10,
https://doi.org/10.1016/j.atmosenv.2011.11.063, 2012.
Jaffe, D. A., Wigder, N., Downey, N., Pfister, G., Boynard, A., and Reid, S.
B.: Impact of Wildfires on Ozone Exceptional Events in the Western U.S.,
Environ. Sci. Technol., 47, 11065–11072, https://doi.org/10.1021/es402164f,
2013.
Kaspari, J. H., Chai, J., Anderson, B. E., Jordan, C. E., Scheuer, E.,
Hastings, M. G., Dibb, J. E.: Influence of Solar Irradiation on Nitrous Acid
Production in Western U.S. Wildfire Smoke, Earth Space Sci. Open Arch.,
https:/doi.org/10.1002/essoar.10506007.1, last access: 15 February 2021.
Kebede, M. A., Bish, D. L., Losovyj, Y., Engelhard, M. H., and Raff, J. D.:
The Role of Iron-Bearing Minerals in NO2 to HONO Conversion on Soil
Surfaces, Environ. Sci. Technol., 50, 8649–8660,
https://doi.org/10.1021/acs.est.6b01915, 2016.
Kleinman, L. I., Daum, P. H., Lee, Y.-N., Senum, G. I., Springston, S. R.,
Wang, J., Berkowitz, C., Hubbe, J., Zaveri, R. A., Brechtel, F. J., Jayne,
J., Onasch, T. B., and Worsnop, D.: Aircraft observations of aerosol
composition and ageing in New England and Mid-Atlantic States during the
summer 2002 New England Air Quality Study field campaign, J. Geophys. Res.-Atmos., 112, D09310, https://doi.org/10.1029/2006JD007786, 2007.
Liu, X., Zhang, Y., Huey, L. G., Yokelson, R. J., Wang, Y., Jimenez, J. L.,
Campuzano-Jost, P., Beyersdorf, A. J., Blake, D. R., Choi, Y., Clair, J. M.
S., Crounse, J. D., Day, D. A., Diskin, G. S., Fried, A., Hall, S. R.,
Hanisco, T. F., King, L. E., Meinardi, S., Mikoviny, T., Palm, B. B.,
Peischl, J., Perring, A. E., Pollack, I. B., Ryerson, T. B., Sachse, G.,
Schwarz, J. P., Simpson, I. J., Tanner, D. J., Thornhill, K. L., Ullmann,
K., Weber, R. J., Wennberg, P. O., Wisthaler, A., Wolfe, G. M., and Ziemba,
L. D.: Agricultural fires in the southeastern U.S. during SEAC4RS: Emissions
of trace gases and particles and evolution of ozone, reactive nitrogen, and
organic aerosol, J. Geophys. Res.-Atmos., 121, 7383–7414,
https://doi.org/10.1002/2016JD025040, 2016.
Madronich, S., Flocke, F. M., Zeng, J., Petropavlovskikh, I., and Lee-Taylor, J.: Tropospheric Ultraviolet and Visible (TUV) Radiation Model, available at: https://www.acom.ucar.edu/Models/TUV/Interactive_TUV/ (last access: 17 March 2020), 2002.
Mark, C. A.: Salmon-Challis National Forest: Salmon-Challis national forest assessment report, available at: https://www.fs.usda.gov/detail/scnf/landmanagement/planning/?cid=fseprd544724 (last access: 12 December 2020), 2018.
Martins-Costa, M. T. C., Anglada, J. M., Francisco, J. S., and
Ruiz-López, M. F.: The Aqueous Surface as an Efficient Transient Stop
for the Reactivity of Gaseous NO2 in Liquid Water, J. Am. Chem. Soc., 142,
20937–20941, https://doi.org/10.1021/jacs.0c10364, 2020.
McClure, C. D. and Jaffe, D. A.: US particulate matter air quality improves
except in wildfire-prone areas, P. Natl. Acad. Sci. USA, 115,
7901–7906, https://doi.org/10.1073/pnas.1804353115, 2018.
Michalski, G., Scott, Z., Kabiling, M., and Thiemens, M. H.: First
measurements and modeling of Δ17O in atmospheric nitrate, Geophys.
Res. Lett., 30, 1870, https://doi.org/10.1029/2003GL017015, 2003.
Michalski, G., Bhattacharya, S. K., and Mase, D. F.: Oxygen Isotope Dynamics
of Atmospheric Nitrate and Its Precursor Molecules, in: Handbook of
Environmental Isotope Geochemistry, Springer, Berlin, Heidelberg, 30, 613–635,
https://doi.org/10.1007/978-3-642-10637-8_30, 2012.
Miller, C. E. and Yung, Y. L.: Photo-induced isotopic fractionation, J. Geophys. Res.-Atmos., 105,
29039–29051, https://doi.org/10.1029/2000JD900388, 2000.
Miller, D. J., Wojtal, P. K., Clark, S. C., and Hastings, M. G.: Vehicle NOx
emission plume isotopic signatures: Spatial variability across the eastern
United States, J. Geophys. Res.-Atmos., 122, 4698–4717,
https://doi.org/10.1002/2016JD025877, 2017.
Monse, E. U., Spindel, W., and Stern, M. J.: Analysis of Isotope-effect
Calculations Illustrated with Exchange Equilibria Among Oxynitrogen
Compounds, in: Isotope Effects in Chemical Processes, Am.
Chem. Soc., 89, 148–184, https://doi.org/10.1021/ba-1969-0089.ch009,
1969.
Ndour, M., D'Anna, B., George, C., Ka, O., Balkanski, Y., Kleffmann, J.,
Stemmler, K., and Ammann, M.: Photoenhanced uptake of NO2 on mineral dust:
Laboratory experiments and model simulations, Geophys. Res. Lett., 35,
L05812, https://doi.org/10.1029/2007GL032006, 2008.
Nie, W., Ding, A. J., Xie, Y. N., Xu, Z., Mao, H., Kerminen, V.-M., Zheng,
L. F., Qi, X. M., Huang, X., Yang, X.-Q., Sun, J. N., Herrmann, E.,
Petäjä, T., Kulmala, M., and Fu, C. B.: Influence of biomass burning
plumes on HONO chemistry in eastern China, Atmos. Chem. Phys., 15,
1147–1159, https://doi.org/10.5194/acp-15-1147-2015, 2015.
Parrington, M., Palmer, P. I., Lewis, A. C., Lee, J. D., Rickard, A. R., Di
Carlo, P., Taylor, J. W., Hopkins, J. R., Punjabi, S., Oram, D. E., Forster,
G., Aruffo, E., Moller, S. J., Bauguitte, S. J.-B., Allan, J. D., Coe, H.,
and Leigh, R. J.: Ozone photochemistry in boreal biomass burning plumes,
Atmos. Chem. Phys., 13, 7321–7341,
https://doi.org/10.5194/acp-13-7321-2013, 2013.
Peng, Q., Palm, B. B., Melander, K. E., Lee, B. H., Hall, S. R., Ullmann,
K., Campos, T., Weinheimer, A. J., Apel, E. C., Hornbrook, R. S., Hills, A.
J., Montzka, D. D., Flocke, F., Hu, L., Permar, W., Wielgasz, C., Lindaas,
J., Pollack, I. B., Fischer, E. V., Bertram, T. H., and Thornton, J. A.:
HONO Emissions from Western U.S. Wildfires Provide Dominant Radical Source
in Fresh Wildfire Smoke, Environ. Sci. Technol., 54, 5954–5963,
https://doi.org/10.1021/acs.est.0c00126, 2020.
Platt, U., Perner, D., Harris, G. W., Winer, A. M., and Pitts, J. N.:
Observations of nitrous acid in an urban atmosphere by differential optical
absorption, Nature, 285, 312–314, https://doi.org/10.1038/285312a0, 1980.
Pöschl, U., Rudich, Y., and Ammann, M.: Kinetic model framework for
aerosol and cloud surface chemistry and gas-particle interactions –
Part 1: General equations, parameters, and terminology, Atmos. Chem. Phys.,
7, 5989–6023, https://doi.org/10.5194/acp-7-5989-2007, 2007.
Scharko, N. K., Martin, E. T., Losovyj, Y., Peters, D. G., and Raff, J. D.:
Evidence for Quinone Redox Chemistry Mediating Daytime and Nighttime
NO2-to-HONO Conversion on Soil Surfaces, Environ. Sci. Technol., 51,
9633–9643, https://doi.org/10.1021/acs.est.7b01363, 2017.
Scheuer, E., Talbot, R. W., Dibb, J. E., Seid, G. K., DeBell, L., and Lefer,
B.: Seasonal distributions of fine aerosol sulfate in the North American
Arctic basin during TOPSE, J. Geophys. Res.-Atmos., 108, 8370,
https://doi.org/10.1029/2001JD001364, 2003.
Selimovic, V., Yokelson, R. J., McMeeking, G. R., and Coefield, S.: In situ
measurements of trace gases, PM, and aerosol optical properties during the
2017 NW US wildfire smoke event, Atmos. Chem. Phys., 19, 3905–3926,
https://doi.org/10.5194/acp-19-3905-2019, 2019.
Selimovic, V., Yokelson, R. J., McMeeking, G. R., and Coefield, S.: Aerosol
Mass and Optical Properties, Smoke Influence on O3, and High NO3 Production
Rates in a Western U.S. City Impacted by Wildfires, J. Geophys. Res.-Atmos.,
125, e2020JD032791, https://doi.org/10.1029/2020JD032791, 2020.
Shi, G., Chai, J., Zhu, Z., Hu, Z., Chen, Z., Yu, J., Ma, T., Ma, H., An,
C., Jiang, S., Tang, X., and Hastings, M. G.: Isotope Fractionation of
Nitrate During Volatilization in Snow: A Field Investigation in Antarctica,
Geophys. Res. Lett., 46, 3287–3297, https://doi.org/10.1029/2019GL081968,
2019.
Sigman, D. M., Casciotti, K. L., Andreani, M., Barford, C., Galanter, M.,
and Böhlke, J. K.: A Bacterial Method for the Nitrogen Isotopic Analysis
of Nitrate in Seawater and Freshwater, Anal. Chem., 73, 4145–4153,
https://doi.org/10.1021/ac010088e, 2001.
Spataro, F. and Ianniello, A.: Sources of atmospheric nitrous acid: State of
the science, current research needs, and future prospects, J. Air Waste Manage., 64,
1232–1250, https://doi.org/10.1080/10962247.2014.952846, 2014.
Stemmler, K., Ammann, M., Donders, C., Kleffmann, J., and George, C.:
Photosensitized reduction of nitrogen dioxide on humic acid as a source of
nitrous acid, Nature, 440, 195–198, https://doi.org/10.1038/nature04603,
2006.
Stockwell, C. E., Yokelson, R. J., Kreidenweis, S. M., Robinson, A. L.,
DeMott, P. J., Sullivan, R. C., Reardon, J., Ryan, K. C., Griffith, D. W.
T., and Stevens, L.: Trace gas emissions from combustion of peat, crop
residue, domestic biofuels, grasses, and other fuels: configuration and
Fourier transform infrared (FTIR) component of the fourth Fire Lab at
Missoula Experiment (FLAME-4), Atmos. Chem. Phys., 14, 9727–9754,
https://doi.org/10.5194/acp-14-9727-2014, 2014.
Su, H., Cheng, Y., Oswald, R., Behrendt, T., Trebs, I., Meixner, F. X.,
Andreae, M. O., Cheng, P., Zhang, Y., and Pöschl, U.: Soil Nitrite as a
Source of Atmospheric HONO and OH Radicals, Science, 333, 1616–1618,
https://doi.org/10.1126/science.1207687, 2011.
Suter, H. U. and Huber, J. R.: S1 potential energy surface of HONO:
Absorption spectrum and photodissociation, Chem. Phys. Lett., 155, 203–209,
https://doi.org/10.1016/0009-2614(89)85350-3, 1989.
Talukdar, R. K., Burkholder, J. B., Schmoltner, A.-M., Roberts, J. M.,
Wilson, R. R., and Ravishankara, A. R.: Investigation of the loss processes
for peroxyacetyl nitrate in the atmosphere: UV photolysis and reaction with
OH, J. Geophys. Res.-Atmos., 100, 14163–14173,
https://doi.org/10.1029/95JD00545, 1995.
Theys, N., Volkamer, R., Müller, J.-F., Zarzana, K. J., Kille, N.,
Clarisse, L., De Smedt, I., Lerot, C., Finkenzeller, H., Hendrick, F.,
Koenig, T. K., Lee, C. F., Knote, C., Yu, H., and Van Roozendael, M.: Global
nitrous acid emissions and levels of regional oxidants enhanced by
wildfires, Nat. Geosci., 13, 681–686,
https://doi.org/10.1038/s41561-020-0637-7, 2020.
Thiemens, M. H.: History and Applications of Mass-Independent Isotope
Effects, Annu. Rev. Earth Planet. Sci., 34, 217–262,
https://doi.org/10.1146/annurev.earth.34.031405.125026, 2006.
Tuite, K., Thomas, J. L., Veres, P. R., Roberts, J. M., Stevens, P. S.,
Griffith, S. M., Dusanter, S., Flynn, J. H., Ahmed, S., Emmons, L., Kim,
S.-W., Washenfelder, R., Young, C., Tsai, C., Pikelnaya, O., and Stutz, J.:
Quantifying nitrous acid formation mechanisms using measured vertical
profiles during the CalNex 2010 campaign and 1D column modeling, J. Geophys.
Res.-Atmos, 126, e2021JD034689, https://doi.org/10.1029/2021JD034689, 2021.
VandenBoer, T. C., Young, C. J., Talukdar, R. K., Markovic, M. Z., Brown, S.
S., Roberts, J. M., and Murphy, J. G.: Nocturnal loss and daytime source of
nitrous acid through reactive uptake and displacement, Nat. Geosci., 8,
55–60, https://doi.org/10.1038/ngeo2298, 2014.
Walters, W. W. and Michalski, G.: Theoretical calculation of nitrogen
isotope equilibrium exchange fractionation factors for various NOy
molecules, Geochim. Cosmochim. Ac., 164, 284–297,
https://doi.org/10.1016/j.gca.2015.05.029, 2015.
Walters, W. W. and Michalski, G.: Theoretical calculation of oxygen
equilibrium isotope fractionation factors involving various NOy molecules,
OH, and H2O and its implications for isotope variations in atmospheric
nitrate, Geochim. Cosmochim. Ac., 191, 89–101,
https://doi.org/10.1016/j.gca.2016.06.039, 2016.
Walters, W. W., Fang, H., and Michalski, G.: Summertime diurnal variations
in the isotopic composition of atmospheric nitrogen dioxide at a small
midwestern United States city, Atmos. Environ., 179, 1–11,
https://doi.org/10.1016/j.atmosenv.2018.01.047, 2018.
Welker, J. M.: Isotopic (δ18O) characteristics of weekly
precipitation collected across the USA: an initial analysis with application
to water source studies, Hydrol. Process., 14, 1449–1464,
https://doi.org/10.1002/1099-1085(20000615)14:8<1449::AID-HYP993>3.0.CO;2-7, 2000.
Westerling, A. L.: Increasing western US forest wildfire activity:
sensitivity to changes in the timing of spring, Phil. Trans. R. Soc. B, 371,
20150178, https://doi.org/10.1098/rstb.2015.0178, 2016.
Westerling, A. L., Hidalgo, H. G., Cayan, D. R., and Swetnam, T. W.: Warming
and Earlier Spring Increase Western U.S. Forest Wildfire Activity, Science,
313, 940–943, https://doi.org/10.1126/science.1128834, 2006.
Wojtal, P. K., Miller, D. J., O'Conner, M., Clark, S. C., and Hastings, M.
G.: Automated, High-resolution Mobile Collection System for the Nitrogen
Isotopic Analysis of NOx, J. Vis. Exp., 118, e54962,
https://doi.org/10.3791/54962, 2016.
Wong, K. W., Tsai, C., Lefer, B., Haman, C., Grossberg, N., Brune, W. H.,
Ren, X., Luke, W., and Stutz, J.: Daytime HONO vertical gradients during
SHARP 2009 in Houston, TX, Atmos. Chem. Phys., 12, 635–652,
https://doi.org/10.5194/acp-12-635-2012, 2012.
Wong, K. W., Tsai, C., Lefer, B., Grossberg, N., and Stutz, J.: Modeling of
daytime HONO vertical gradients during SHARP 2009, Atmos. Chem. Phys., 13,
3587–3601, https://doi.org/10.5194/acp-13-3587-2013, 2013.
Ye, C., Zhou, X., Pu, D., Stutz, J., Festa, J., Spolaor, M., Tsai, C.,
Cantrell, C., Mauldin, R. L., Campos, T., Weinheimer, A., Hornbrook, R. S.,
Apel, E. C., Guenther, A., Kaser, L., Yuan, B., Karl, T., Haggerty, J.,
Hall, S., Ullmann, K., Smith, J. N., Ortega, J., and Knote, C.: Rapid
cycling of reactive nitrogen in the marine boundary layer, Nature, 532,
489–491, https://doi.org/10.1038/nature17195, 2016.
Ye, C., Zhang, N., Gao, H., and Zhou, X.: Photolysis of Particulate Nitrate
as a Source of HONO and NOx, Environ. Sci. Technol., 51, 6849–6856,
https://doi.org/10.1021/acs.est.7b00387, 2017.
Yokelson, R. J., Crounse, J. D., DeCarlo, P. F., Karl, T., Urbanski, S.,
Atlas, E., Campos, T., Shinozuka, Y., Kapustin, V., Clarke, A. D.,
Weinheimer, A., Knapp, D. J., Montzka, D. D., Holloway, J., Weibring, P.,
Flocke, F., Zheng, W., Toohey, D., Wennberg, P. O., Wiedinmyer, C., Mauldin,
L., Fried, A., Richter, D., Walega, J., Jimenez, J. L., Adachi, K., Buseck,
P. R., Hall, S. R., and Shetter, R.: Emissions from biomass burning in the
Yucatan, Atmos. Chem. Phys., 9, 5785–5812,
https://doi.org/10.5194/acp-9-5785-2009, 2009.
Yung, Y. L. and Miller, C. E.: Isotopic Fractionation of Stratospheric
Nitrous Oxide, 278, 1778–1780,
https://doi.org/10.1126/science.278.5344.1778, 1997.
Zhou, X., Zhang, N., TerAvest, M., Tang, D., Hou, J., Bertman, S.,
Alaghmand, M., Shepson, P. B., Carroll, M. A., Griffith, S., Dusanter, S.,
and Stevens, P. S.: Nitric acid photolysis on forest canopy surface as a
source for tropospheric nitrous acid, Nat. Geosci., 4, 440–443,
https://doi.org/10.1038/ngeo1164, 2011.
Short summary
Nitrous acid (HONO) derived from wildfire emissions plays a key role in controlling atmospheric oxidation chemistry. However, the HONO budget remains poorly constrained. By combining the field-observed concentrations and novel isotopic composition (N and O) of HONO and nitrogen oxides (NOx), we quantitatively constrained the relative contribution of each pathway to secondary HONO production and the relative importance of major atmospheric oxidants (ozone versus peroxy) in aged wildfire smoke.
Nitrous acid (HONO) derived from wildfire emissions plays a key role in controlling atmospheric...
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