Articles | Volume 18, issue 2
https://doi.org/10.5194/acp-18-1171-2018
© Author(s) 2018. 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-18-1171-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
The effects of isoprene and NOx on secondary organic aerosols formed through reversible and irreversible uptake to aerosol water
Marwa M. H. El-Sayed
Department of Chemical, Biochemical and Environmental Engineering,
University of Maryland, Baltimore County, Baltimore, MD, USA
Diana L. Ortiz-Montalvo
National Institute of Standards and Technology (NIST), Gaithersburg,
MD, USA
Christopher J. Hennigan
CORRESPONDING AUTHOR
Department of Chemical, Biochemical and Environmental Engineering,
University of Maryland, Baltimore County, Baltimore, MD, USA
Related authors
No articles found.
Vikram Pratap, Christopher J. Hennigan, Bastian Stieger, Andreas Tilgner, Laurent Poulain, Dominik van Pinxteren, Gerald Spindler, and Hartmut Herrmann
Atmos. Chem. Phys., 25, 8871–8889, https://doi.org/10.5194/acp-25-8871-2025, https://doi.org/10.5194/acp-25-8871-2025, 2025
Short summary
Short summary
In this work, we characterize trends in aerosol pH and its controlling factors during the period 2010–2019 at the Melpitz research station in eastern Germany. We find strong trends in aerosol pH and major inorganic species in response to changing emissions. We conduct a detailed thermodynamic analysis of the aerosol system and discuss implications for controlling particulate matter in the region.
Christopher J. Hennigan, Michael McKee, Vikram Pratap, Bryanna Boegner, Jasper Reno, Lucia Garcia, Madison McLaren, and Sara M. Lance
Atmos. Chem. Phys., 23, 14437–14449, https://doi.org/10.5194/acp-23-14437-2023, https://doi.org/10.5194/acp-23-14437-2023, 2023
Short summary
Short summary
This study characterized the optical properties of light-absorbing organic compounds, called brown carbon (BrC), in atmospheric cloud water samples. In all samples, light absorption by BrC increased linearly with increasing pH. There was variability in the sensitivity of the absorption–pH relationship, depending on the degree of influence from fire emissions. Overall, these results show that the climate forcing of BrC is quite strongly affected by its pH-dependent absorption.
Michael A. Battaglia Jr., Nicholas Balasus, Katherine Ball, Vanessa Caicedo, Ruben Delgado, Annmarie G. Carlton, and Christopher J. Hennigan
Atmos. Chem. Phys., 21, 18271–18281, https://doi.org/10.5194/acp-21-18271-2021, https://doi.org/10.5194/acp-21-18271-2021, 2021
Short summary
Short summary
This study characterizes aerosol liquid water content and aerosol pH at a land–water transition site near Baltimore, Maryland. We characterize the effects of unique meteorology associated with the close proximity to the Chesapeake Bay and episodic NH3 events derived from industrial and agricultural sources on aerosol chemistry during the summer. We also examine two events where primary Bay emissions underwent aging in the polluted urban atmosphere.
Nicholas Balasus, Michael A. Battaglia Jr., Katherine Ball, Vanessa Caicedo, Ruben Delgado, Annmarie G. Carlton, and Christopher J. Hennigan
Atmos. Chem. Phys., 21, 13051–13065, https://doi.org/10.5194/acp-21-13051-2021, https://doi.org/10.5194/acp-21-13051-2021, 2021
Short summary
Short summary
Measurements of aerosol and gas composition were carried out at a land–water transition site near Baltimore, MD. Gas-phase ammonia concentrations were highly elevated compared to measurements at a nearby inland site. Our analysis reveals that NH2 was from both industrial and agricultural sources. This had a pronounced effect on aerosol chemical composition at the site, most notably contributing to episodic spikes of aerosol nitrate.
Havala O. T. Pye, Athanasios Nenes, Becky Alexander, Andrew P. Ault, Mary C. Barth, Simon L. Clegg, Jeffrey L. Collett Jr., Kathleen M. Fahey, Christopher J. Hennigan, Hartmut Herrmann, Maria Kanakidou, James T. Kelly, I-Ting Ku, V. Faye McNeill, Nicole Riemer, Thomas Schaefer, Guoliang Shi, Andreas Tilgner, John T. Walker, Tao Wang, Rodney Weber, Jia Xing, Rahul A. Zaveri, and Andreas Zuend
Atmos. Chem. Phys., 20, 4809–4888, https://doi.org/10.5194/acp-20-4809-2020, https://doi.org/10.5194/acp-20-4809-2020, 2020
Short summary
Short summary
Acid rain is recognized for its impacts on human health and ecosystems, and programs to mitigate these effects have had implications for atmospheric acidity. Historical measurements indicate that cloud and fog droplet acidity has changed in recent decades in response to controls on emissions from human activity, while the limited trend data for suspended particles indicate acidity may be relatively constant. This review synthesizes knowledge on the acidity of atmospheric particles and clouds.
Michael A. Battaglia Jr., Rodney J. Weber, Athanasios Nenes, and Christopher J. Hennigan
Atmos. Chem. Phys., 19, 14607–14620, https://doi.org/10.5194/acp-19-14607-2019, https://doi.org/10.5194/acp-19-14607-2019, 2019
Short summary
Short summary
The effects of water-soluble organic carbon (WSOC) on aerosol pH were characterized for aqueous-phase particles containing a mixture of inorganics and organics. The ISORROPIA-II and E-AIM models were used in conjunction with AIOMFAC to quantify the effect of organics on aerosol pH through (1) changes to the aerosol liquid water content and (2) changes to the hydrogen ion activity coefficient. The study included both organic acids and nonacids, at RH levels ranging from 70 to 90 %.
C. J. Hennigan, J. Izumi, A. P. Sullivan, R. J. Weber, and A. Nenes
Atmos. Chem. Phys., 15, 2775–2790, https://doi.org/10.5194/acp-15-2775-2015, https://doi.org/10.5194/acp-15-2775-2015, 2015
Short summary
Short summary
We show that the ion balance and molar ratio methods are unsuitable for use as aerosol pH proxies. Our recommendation is that 1) thermodynamic equilibrium models constrained by both gas and aerosol inputs run in the forward (open) mode, and 2) the phase partitioning of ammonia provides the best predictions of aerosol pH. Given the significance of acidity for numerous chemical processes in the atmosphere, the implications of this study are important and far reaching.
R. Saleh, C. J. Hennigan, G. R. McMeeking, W. K. Chuang, E. S. Robinson, H. Coe, N. M. Donahue, and A. L. Robinson
Atmos. Chem. Phys., 13, 7683–7693, https://doi.org/10.5194/acp-13-7683-2013, https://doi.org/10.5194/acp-13-7683-2013, 2013
Related subject area
Subject: Aerosols | Research Activity: Field Measurements | Altitude Range: Troposphere | Science Focus: Chemistry (chemical composition and reactions)
Climatology of aerosol pH and its controlling factors at the Melpitz continental background site in Central Europe
Technical note: Towards a stronger observational support for haze pollution control by interpreting carbonaceous aerosol results derived from different measurement approaches
Particle flux–gradient relationships in the high Arctic: emission and deposition patterns across three surface types
Advances in characterization of black carbon particles and their associated coatings using the soot-particle aerosol mass spectrometer in Singapore, a complex city environment
Iron isotopes suggest significant aerosol dissolution over the Pacific Ocean
Enrichment of organic nitrogen in fog residuals observed in the Italian Po Valley
Asian dust transport of proteinaceous matter from the Gobi Desert to northern China
Machine-learning-assisted chemical characterization and optical properties of atmospheric brown carbon in Nanjing, China
Technical note: Reconstructing missing surface aerosol elemental carbon data in long-term series with ensemble learning
Enhanced emission of intermediate-volatility/semi-volatile organic matter in gas and particle phases from ship exhausts with low-sulfur fuels
Measurement report: Crustal materials play an increasing role in elevating particle pH – insights from 12-year records in a typical inland city of China
Significant contributions of biomass burning to PM2.5-bound aromatic compounds: insights from field observations and quantum chemical calculations
Measurement report: In-depth characterization of ship emissions during operations in a Mediterranean port
Direct measurement of N2O5 heterogeneous uptake coefficients on atmospheric aerosols in southwestern China and evaluation of current parameterizations
Measurement report: Per- and polyfluoroalkyl substances (PFAS) in particulate matter (PM10) from activated sludge aeration
African dust transported to Barbados in the wintertime lacks indicators of chemical aging
A 60-year atmospheric nitrate isotope record from a southeastern Greenland ice core with minimal postdepositional alteration
Measurement report: Characterization of aerosol hygroscopicity over Southeast Asia during the NASA CAMP2Ex campaign
Long–term Trends in PM2.5 Chemical Composition and Its Impact on Aerosol Properties: Field Observations from 2007 to 2020 in Pearl River Delta, South China
Atmospheric Organosulfate Formation Regulated by Continental Outflows and Marine Emissions over East Asian Marginal Seas
Individual particle compositions and aerosol mixing states at different altitudes over the ocean in East Asia
Molecular characterization of organic aerosols in urban and forested areas of Paris using high-resolution mass spectrometry
Measurement report: Wintertime aerosol characterization at an urban traffic site in Helsinki, Finland
Source apportionment and ecotoxicity of PM2.5 pollution events in a major Southern Hemisphere megacity: influence of a biofuel-impacted fleet and biomass burning
The impacts of pollution sources and temperature on the light absorption of HULIS were revealed by UHPLC-HRMS/MS at the molecular structure level
Effects of Anthropogenic Pollutants on Biogenic Secondary Organic Aerosol Formation in the Atmosphere of Mt. Hua, China
Marine organic aerosol at Mace Head: effects from phytoplankton and source region variability
Elemental composition, iron mineralogy and solubility of anthropogenic and natural mineral dust aerosols in Namibia: a case study analysis from the AEROCLO-sA campaign
Fossil-Dominated SOA Formation in Coastal China: Size-Divergent Pathways of Aqueous Fenton Reactions versus Gas-phase VOC Autoxidation
Measurement report: Sources and meteorology influencing highly time-resolved PM2.5 trace elements at three urban sites in the extremely polluted Indo-Gangetic Plain in India
Formation of highly absorptive secondary brown carbon through nighttime multiphase chemistry of biomass burning emissions
Hydroxymethanesulfonate (HMS) Formation under Urban and Marine Atmosphere: role of aerosol ionic strength
The sources and diurnal variations of submicron aerosols in a coastal-rural environment near Houston, US
Measurement report: Vertically resolved atmospheric properties observed over the Southern Great Plains with the ArcticShark uncrewed aerial system
Unraveling Arctic submicron organic aerosol sources: a year-long study by H-NMR and AMS in Ny-Ålesund, Svalbard
Non-biogenic sources are an important but overlooked contributor to aerosol isoprene-derived organosulfates during winter in northern China
Unveiling single-particle composition, size, shape, and mixing state of freshly emitted Icelandic dust via electron microscopy analysis
The Critical Role of Volatile Organic Compounds Emission in Nitrate Formation in Lhasa, Tibetan Plateau: Insights from Oxygen Isotope Anomaly Measurements
The critical role of aqueous-phase processes in aromatic-derived nitrogen-containing organic aerosol formation in cities with different energy consumption patterns
Characterization of atmospheric water-soluble brown carbon in the Athabasca oil sands region, Canada
Sensitivity of aerosol and cloud properties to coupling strength of marine boundary layer clouds over the northwest Atlantic
Measurement Report: Molecular composition, sources, and evolution of atmospheric organic aerosols in a basin city in China
Burning conditions and transportation pathways determine biomass-burning aerosol properties in the Ascension Island marine boundary layer
Observations of high-time-resolution and size-resolved aerosol chemical composition and microphysics in the central Arctic: implications for climate-relevant particle properties
A critical review of the use of iron isotopes in atmospheric aerosol research
Measurement report: Brown carbon aerosol in rural Germany – sources, chemistry, and diurnal variations
Atmospheric chemistry in East Asia determines the iron solubility of aerosol particles supplied to the North Pacific Ocean
Measurement Report: Polycyclic aromatic hydrocarbons (PAHs) and their alkylated (RPAHs), nitrated (NPAHs) and oxygenated (OPAHs) derivatives in the global marine atmosphere: occurrence, spatial variations, and source apportionment
Multiple eco-regions contribute to the seasonal cycle of Antarctic aerosol size distributions
Seasonal investigation of ultrafine-particle organic composition in an eastern Amazonian rainforest
Vikram Pratap, Christopher J. Hennigan, Bastian Stieger, Andreas Tilgner, Laurent Poulain, Dominik van Pinxteren, Gerald Spindler, and Hartmut Herrmann
Atmos. Chem. Phys., 25, 8871–8889, https://doi.org/10.5194/acp-25-8871-2025, https://doi.org/10.5194/acp-25-8871-2025, 2025
Short summary
Short summary
In this work, we characterize trends in aerosol pH and its controlling factors during the period 2010–2019 at the Melpitz research station in eastern Germany. We find strong trends in aerosol pH and major inorganic species in response to changing emissions. We conduct a detailed thermodynamic analysis of the aerosol system and discuss implications for controlling particulate matter in the region.
Yuan Cheng, Ying-jie Zhong, Zhi-qing Zhang, Xu-bing Cao, and Jiu-meng Liu
Atmos. Chem. Phys., 25, 8493–8505, https://doi.org/10.5194/acp-25-8493-2025, https://doi.org/10.5194/acp-25-8493-2025, 2025
Short summary
Short summary
As an emerging hotspot of atmospheric sciences, northeastern China is distinct due to the frigid winter and the strong emissions from agricultural fires. Based on field campaigns conducted in Harbin, we successively identified the analytical method that could lead to proper results of organic and elemental carbon. Our results are believed to be a support for future efforts in the exploration of PM2.5 sources in northeastern China, which are essential for further improving the regional air quality.
Theresa Mathes, Heather Guy, John Prytherch, Julia Kojoj, Ian Brooks, Sonja Murto, Paul Zieger, Birgit Wehner, Michael Tjernström, and Andreas Held
Atmos. Chem. Phys., 25, 8455–8474, https://doi.org/10.5194/acp-25-8455-2025, https://doi.org/10.5194/acp-25-8455-2025, 2025
Short summary
Short summary
The Arctic is warming faster than the global average and an investigation of aerosol–cloud–sea ice interactions is crucial for studying its climate system. During the ARTofMELT Expedition 2023, particle and sensible heat fluxes were measured over different surfaces. Wide lead surfaces acted as particle sources, with the strongest sensible heat fluxes, while closed ice surfaces acted as particle sinks. In this study, methods to measure these interactions are improved, enhancing our understanding of Arctic climate processes.
Mutian Ma, Laura-Hélèna Rivellini, Yichen Zong, Markus Kraft, Liya E. Yu, and Alex King Yin Lee
Atmos. Chem. Phys., 25, 8185–8211, https://doi.org/10.5194/acp-25-8185-2025, https://doi.org/10.5194/acp-25-8185-2025, 2025
Short summary
Short summary
This work advances our understanding of the emission and atmospheric evolution of black carbon (BC) particles in Singapore, a complex urban environment impacted by multiple local and regional combustion sources, based on the improved source apportionment analysis of real-time aerosol mass spectrometry measurement.
Capucine Camin, François Lacan, Catherine Pradoux, Marie Labatut, Anne Johansen, and James W. Murray
Atmos. Chem. Phys., 25, 8213–8228, https://doi.org/10.5194/acp-25-8213-2025, https://doi.org/10.5194/acp-25-8213-2025, 2025
Short summary
Short summary
This paper presents the chemical and iron isotopic composition of aerosols (> 1 µm) over the equatorial and tropical Pacific Ocean in previously undocumented areas. Analysis of our data suggests that a significant proportion of aerosol iron (∼ 13 %) is not only dissolved but also removed during atmospheric transport. Such removal had not previously been evidenced to our knowledge. This highlights the unique and strong constraints brought by iron isotopes on atmospheric process studies.
Fredrik Mattsson, Almuth Neuberger, Liine Heikkinen, Yvette Gramlich, Marco Paglione, Matteo Rinaldi, Stefano Decesari, Paul Zieger, Ilona Riipinen, and Claudia Mohr
Atmos. Chem. Phys., 25, 7973–7989, https://doi.org/10.5194/acp-25-7973-2025, https://doi.org/10.5194/acp-25-7973-2025, 2025
Short summary
Short summary
This study investigated aerosol–cloud interactions, focusing on organic nitrogen (ON) formation in the aqueous phase. Measurements were conducted in wintertime in the Po Valley, Italy, using aerosol mass spectrometry. The fog was enriched in more hygroscopic inorganic compounds and ON, containing, e.g., imidazoles. The formation of imidazole by aerosol–fog interactions could be confirmed for the first time in atmospheric observations. Findings highlight the role of fog in nitrogen aerosol formation.
Ren-Guo Zhu, Hua-Yun Xiao, Meiju Yin, Hao Xiao, Zhongkui Zhou, Yuanyuan Pan, Guo Wei, and Cheng Liu
Atmos. Chem. Phys., 25, 7699–7718, https://doi.org/10.5194/acp-25-7699-2025, https://doi.org/10.5194/acp-25-7699-2025, 2025
Short summary
Short summary
The concentrations and δ15N isotopic values of CAAs (combined amino acids) in surface soil and plants from the Gobi Desert, as well as in PM2.5 samples from four cities in Northern China, were measured. CAAs transported by Gobi dust were rich in alanine, glycine and glutamic acid. Glycine and leucine in Gobi Desert sources exhibited δ15N depletion by more than 6 ‰ compared to their values in urban PM2.5. Substantial protein-N deposition can be transported by the Gobi Desert to northern China over brief periods.
Yu Huang, Xingru Li, Dan Dan Huang, Ruoyuan Lei, Binhuang Zhou, Yunjiang Zhang, and Xinlei Ge
Atmos. Chem. Phys., 25, 7619–7645, https://doi.org/10.5194/acp-25-7619-2025, https://doi.org/10.5194/acp-25-7619-2025, 2025
Short summary
Short summary
This work comprises a comprehensive investigation into the chemical and optical properties of brown carbon (BrC) in PM2.5 samples collected in Nanjing, China. In particular, we used a machine learning approach to identify a list of key BrC species, which can be a good reference for future studies. Our findings extend understanding of BrC properties and are valuable to the assessment of BrC's impact on air quality and radiative forcing.
Qingxiao Meng, Yunjiang Zhang, Sheng Zhong, Jie Fang, Lili Tang, Yongcai Rao, Minfeng Zhou, Jian Qiu, Xiaofeng Xu, Jean-Eudes Petit, Olivier Favez, and Xinlei Ge
Atmos. Chem. Phys., 25, 7485–7498, https://doi.org/10.5194/acp-25-7485-2025, https://doi.org/10.5194/acp-25-7485-2025, 2025
Short summary
Short summary
We developed a machine-learning-based method to reconstruct missing elemental carbon (EC) data in four Chinese cities from 2013 to 2023. Using machine learning, we filled data gaps and introduced a new approach to analyze EC trends. Our findings reveal a significant decline in EC due to stricter pollution controls, though this slowed after 2020. This study provides a versatile framework for addressing data gaps and supports strategies to reduce urban air pollution and its climate impacts.
Binyu Xiao, Fan Zhang, Zeyu Liu, Yan Zhang, Rui Li, Can Wu, Xinyi Wan, Yi Wang, Yubao Chen, Yong Han, Min Cui, Libo Zhang, Yingjun Chen, and Gehui Wang
Atmos. Chem. Phys., 25, 7053–7069, https://doi.org/10.5194/acp-25-7053-2025, https://doi.org/10.5194/acp-25-7053-2025, 2025
Short summary
Short summary
Intermediate-volatility/semi-volatile organic compounds in gas and particle phases from ship exhausts are enhanced due to the switch of fuels from low sulfur to ultra-low sulfur. The findings indicate that optimization is necessary for the forthcoming global implementation of an ultra-low-sulfur oil policy. Besides, we find that organic diagnostic markers of hopanes in conjunction with the ratio of octadecanoic to tetradecanoic could be considered potential tracers for heavy fuel oil exhausts.
Hongyu Zhang, Shenbo Wang, Zhangsen Dong, Xiao Li, and Ruiqin Zhang
Atmos. Chem. Phys., 25, 6943–6955, https://doi.org/10.5194/acp-25-6943-2025, https://doi.org/10.5194/acp-25-6943-2025, 2025
Short summary
Short summary
Analyzing 12-year Zhengzhou data revealed post-2019 crustal material rebound caused by soil dust resuspension, elevating particle pH. Similar coarse particle increases are observed across cities of the North China Plain. Long-term particle acidity evolution in this region requires an integrated assessment of interactions among acidic precursors, ammonia, and crustal components.
Yanqin Ren, Zhenhai Wu, Fang Bi, Hong Li, Haijie Zhang, Junling Li, Rui Gao, Fangyun Long, Zhengyang Liu, Yuanyuan Ji, and Gehui Wang
Atmos. Chem. Phys., 25, 6975–6990, https://doi.org/10.5194/acp-25-6975-2025, https://doi.org/10.5194/acp-25-6975-2025, 2025
Short summary
Short summary
The daily concentrations of Polycyclic aromatic hydrocarbons (PAHs), oxygenated PAHs (OPAHs), and nitrated phenols (NPs) in PM2.5 were all increased during the heating season. Biomass burning was identified to be the primary source of these aromatic compounds, particularly for PAHs. Phenol and nitrobenzene are two main primary precursors for 4NP, with phenol showing lower reaction barriers. P-Cresol was identified as the primary precursor for the formation of 4-methyl-5-nitrocatechol.
Lise Le Berre, Brice Temime-Roussel, Grazia Maria Lanzafame, Barbara D'Anna, Nicolas Marchand, Stéphane Sauvage, Marvin Dufresne, Liselotte Tinel, Thierry Leonardis, Joel Ferreira de Brito, Alexandre Armengaud, Grégory Gille, Ludovic Lanzi, Romain Bourjot, and Henri Wortham
Atmos. Chem. Phys., 25, 6575–6605, https://doi.org/10.5194/acp-25-6575-2025, https://doi.org/10.5194/acp-25-6575-2025, 2025
Short summary
Short summary
A summer campaign in a Mediterranean port examined pollution caused by ships. Two stations in the port measured pollution levels and captured over 350 ship plumes to study their chemical composition. Results showed that pollution levels, such as ultra-fine particles, were higher in the port than in the city and offer strong support to improve emission inventories. These findings may also serve as reference to assess the benefits of a sulfur Emission Control Area in the Mediterranean in 2025.
Jiayin Li, Tianyu Zhai, Xiaorui Chen, Haichao Wang, Shuyang Xie, Shiyi Chen, Chunmeng Li, Yuanjun Gong, Huabin Dong, and Keding Lu
Atmos. Chem. Phys., 25, 6395–6406, https://doi.org/10.5194/acp-25-6395-2025, https://doi.org/10.5194/acp-25-6395-2025, 2025
Short summary
Short summary
We directly measured the dinitrogen pentoxide (N2O5) uptake coefficient using an aerosol flow tube, which critically impacts the NOx fate and particulate nitrate formation in a typical highland city, Kunming, in China. We found that the performance of current γ (N2O5) parameterizations showed deviations with the varying aerosol liquid water content (ALWC). Such differences would lead to biased estimation of particulate nitrate production potential. We give suggestions for future research directions.
Jishnu Pandamkulangara Kizhakkethil, Zongbo Shi, Anna Bogush, and Ivan Kourtchev
Atmos. Chem. Phys., 25, 5947–5958, https://doi.org/10.5194/acp-25-5947-2025, https://doi.org/10.5194/acp-25-5947-2025, 2025
Short summary
Short summary
Pollution with per- and polyfluoroalkyl substances (PFAS) has received attention due to their environmental persistence and bioaccumulation, but their sources remain poorly understood. PM10 (particulate matter) collected above a scaled-down activated sludge tank treating domestic sewage in the UK was analysed for a range of short-, medium-, and long-chain PFAS. Eight PFAS were detected in the PM10. Our results suggest that wastewater treatment processes, i.e. activated sludge aeration, could aerosolise PFAS into airborne PM.
Haley M. Royer, Michael T. Sheridan, Hope E. Elliott, Edmund Blades, Nurun Nahar Lata, Zezhen Cheng, Swarup China, Zihua Zhu, Andrew P. Ault, and Cassandra J. Gaston
Atmos. Chem. Phys., 25, 5743–5759, https://doi.org/10.5194/acp-25-5743-2025, https://doi.org/10.5194/acp-25-5743-2025, 2025
Short summary
Short summary
Saharan dust transported across the Atlantic to the Caribbean, South America, and North America is hypothesized to undergo chemical processing by acids that enhances cloud droplet formation and nutrient availability. In this study, chemical analysis performed on African dust deposited over Barbados shows that acid tracers are found mostly on sea salt and smoke particles, rather than dust, indicating that dust particles undergo minimal chemical processing.
Zhao Wei, Shohei Hattori, Asuka Tsuruta, Zhuang Jiang, Sakiko Ishino, Koji Fujita, Sumito Matoba, Lei Geng, Alexis Lamothe, Ryu Uemura, Naohiro Yoshida, Joel Savarino, and Yoshinori Iizuka
Atmos. Chem. Phys., 25, 5727–5742, https://doi.org/10.5194/acp-25-5727-2025, https://doi.org/10.5194/acp-25-5727-2025, 2025
Short summary
Short summary
Nitrate isotope records in ice cores reveal changes in NOₓ emissions and atmospheric oxidation chemistry driven by human activity. However, UV-driven postdepositional processes can alter nitrate in snow, making snow accumulation rates critical for preserving these records. This study examines nitrate isotopes in a southeastern Greenland ice core, where high snow accumulation minimizes these effects, providing a reliable archive of atmospheric nitrogen cycling.
Genevieve Rose Lorenzo, Luke D. Ziemba, Avelino F. Arellano, Mary C. Barth, Ewan C. Crosbie, Joshua P. DiGangi, Glenn S. Diskin, Richard Ferrare, Miguel Ricardo A. Hilario, Michael A. Shook, Simone Tilmes, Jian Wang, Qian Xiao, Jun Zhang, and Armin Sorooshian
Atmos. Chem. Phys., 25, 5469–5495, https://doi.org/10.5194/acp-25-5469-2025, https://doi.org/10.5194/acp-25-5469-2025, 2025
Short summary
Short summary
Novel aerosol hygroscopicity analyses of CAMP2Ex (Cloud, Aerosol, and Monsoon Processes Philippines Experiment) field campaign data show low aerosol hygroscopicity values in Southeast Asia. Organic carbon from smoke decreases hygroscopicity to levels more like those in continental than in polluted marine regions. Hygroscopicity changes at cloud level demonstrate how surface particles impact clouds in the region, affecting model representation of aerosol and cloud interactions in similar polluted marine regions with high organic carbon emissions.
Yunfeng He, Xiang Ding, Quanfu He, Yuqing Zhang, Duohong Chen, Tao Zhang, Kong Yang, Junqi Wang, Qian Cheng, Hao Jiang, Zirui Wang, Ping Liu, Xinming Wang, and Michael Boy
EGUsphere, https://doi.org/10.5194/egusphere-2025-2204, https://doi.org/10.5194/egusphere-2025-2204, 2025
Short summary
Short summary
The long-term field measurements in the Pearl River Delta revealed a significant decline in PM2.5 main components. As air quality improved, secondary species became more dominant. In addition, the proportion of nitrate had doubled. The changes in chemical composition led to the reductions in aerosol acidity, liquid water content and light extinction coefficient. Our results help to improve understanding of the secondary species formation under decreasing anthropogenic emissions.
Shubin Li, Yujue Wang, Yiwen Zhang, Yizhe Yi, Yuchen Wang, Yuqi Guo, Chao Yu, Yue Jiang, Jinhui Shi, Chao Zhang, Jialei Zhu, Wei Hu, Jianzhen Yu, Xiaohong Yao, Huiwang Gao, and Min Hu
EGUsphere, https://doi.org/10.5194/egusphere-2025-2154, https://doi.org/10.5194/egusphere-2025-2154, 2025
Short summary
Short summary
Organosulfates (OSs) are an unrecognized and potentially important component in marine organic aerosols. In this study, we quantified and characterized the OSs over East Asian marginal seas. The chemical nature and spatiotemporal distribution of OSs were modified by the joint influence of marine emissions and transported terrestrial pollutants. The results highlight the vital roles of OSs in shaping organic aerosol formation and sulfur cycle during summer in marine boundary layer.
Kouji Adachi, Atsushi Yoshida, Tatsuhiro Mori, Nobuhiro Moteki, Sho Ohata, Kazuyuki Kita, Yoshimi Kawai, and Makoto Koike
EGUsphere, https://doi.org/10.5194/egusphere-2025-2230, https://doi.org/10.5194/egusphere-2025-2230, 2025
Short summary
Short summary
This study measured the compositions and mixing states of individual aerosol particles collected at different altitudes over the western North Pacific by simultaneous sampling from an aircraft and a research vessel. The results showed that they were strongly influenced by Siberian Forest biomass burning and mixed with sea spray, and identified various aerosol compositions at different altitudes, sizes, and aerosol sources, highlighting a wide range of individual particle compositions.
Diana L. Pereira, Chiara Giorio, Aline Gratien, Alexander Zherebker, Gael Noyalet, Servanne Chevaillier, Stéphanie Alage, Elie Almarj, Antonin Bergé, Thomas Bertin, Mathieu Cazaunau, Patrice Coll, Ludovico Di Antonio, Sergio Harb, Johannes Heuser, Cécile Gaimoz, Oscar Guillemant, Brigitte Language, Olivier Lauret, Camilo Macias, Franck Maisonneuve, Bénédicte Picquet-Varrault, Raquel Torres, Sylvain Triquet, Pascal Zapf, Lelia Hawkins, Drew Pronovost, Sydney Riley, Pierre-Marie Flaud, Emilie Perraudin, Pauline Pouyes, Eric Villenave, Alexandre Albinet, Olivier Favez, Robin Aujay-Plouzeau, Vincent Michoud, Christopher Cantrell, Manuela Cirtog, Claudia Di Biagio, Jean-François Doussin, and Paola Formenti
Atmos. Chem. Phys., 25, 4885–4905, https://doi.org/10.5194/acp-25-4885-2025, https://doi.org/10.5194/acp-25-4885-2025, 2025
Short summary
Short summary
In order to study aerosols in environments influenced by anthropogenic and biogenic emissions, we performed analyses of samples collected during the ACROSS (Atmospheric Chemistry Of the Suburban Forest) campaign in summer 2022 in the greater Paris area. After analysis of the chemical composition by means of total carbon determination and high-resolution mass spectrometry, this work highlights the influence of anthropogenic inputs on the chemical composition of both urban and forested areas.
Kimmo Teinilä, Sanna Saarikoski, Henna Lintusaari, Teemu Lepistö, Petteri Marjanen, Minna Aurela, Heidi Hellén, Toni Tykkä, Markus Lampimäki, Janne Lampilahti, Luis Barreira, Timo Mäkelä, Leena Kangas, Juha Hatakka, Sami Harni, Joel Kuula, Jarkko V. Niemi, Harri Portin, Jaakko Yli-Ojanperä, Ville Niemelä, Milja Jäppi, Katrianne Lehtipalo, Joonas Vanhanen, Liisa Pirjola, Hanna E. Manninen, Tuukka Petäjä, Topi Rönkkö, and Hilkka Timonen
Atmos. Chem. Phys., 25, 4907–4928, https://doi.org/10.5194/acp-25-4907-2025, https://doi.org/10.5194/acp-25-4907-2025, 2025
Short summary
Short summary
Physical and chemical properties of particulate matter and concentrations of trace gases were measured in a street canyon in Helsinki, Finland, and an urban background site in January–February 2022 to investigate the effect of wintertime conditions on pollutants. State-of-the-art instruments and a mobile laboratory were used, and the measurement data were analysed further with modelling tools like positive matrix factorization and the Pollution Detection Algorithm.
Guilherme Martins Pereira, Leonardo Yoshiaki Kamigauti, Rubens Fabio Pereira, Djacinto Monteiro dos Santos, Thayná da Silva Santos, José Vinicius Martins, Célia Alves, Cátia Gonçalves, Ismael Casotti Rienda, Nora Kováts, Thiago Nogueira, Luciana Rizzo, Paulo Artaxo, Regina Maura de Miranda, Marcia Akemi Yamasoe, Edmilson Dias de Freitas, Pérola de Castro Vasconcellos, and Maria de Fatima Andrade
Atmos. Chem. Phys., 25, 4587–4616, https://doi.org/10.5194/acp-25-4587-2025, https://doi.org/10.5194/acp-25-4587-2025, 2025
Short summary
Short summary
The chemical composition of fine particulate matter was studied in the megacity of São Paulo (Brazil) during a polluted period. Vehicular-related sources remain relevant; however, a high contribution of biomass burning was observed and correlated with sample ecotoxicity. Emerging biomass burning sources, such as forest fires and sugarcane-bagasse-based power plants, highlight the need for additional control measures alongside stricter rules concerning vehicular emissions.
Tao Qiu, Yanting Qiu, Yongyi Yuan, Rui Su, Xiangxinyue Meng, Jialiang Ma, Xiaofan Wang, Yu Gu, Zhijun Wu, Yang Ning, Xiuyi Hua, Dapeng Liang, and Deming Dong
EGUsphere, https://doi.org/10.5194/egusphere-2025-1808, https://doi.org/10.5194/egusphere-2025-1808, 2025
Short summary
Short summary
Our research reveals that some species from biomass burning and coal combustion dominate the light absorption of organic aerosols during winter. Cold weather helps these species accumulate in aerosols by slowing their degradation and altering atmospheric chemical processes. This means colder regions might experience stronger and more persistent climate impacts. Our findings highlight the importance of local temperatures and pollution sources when tackling climate challenges.
Can Wu, Yubao Chen, Yuwei Sun, Huijun Zhang, Si Zhang, Cong Cao, Jianjun Li, and Gehui Wang
EGUsphere, https://doi.org/10.5194/egusphere-2025-1668, https://doi.org/10.5194/egusphere-2025-1668, 2025
Short summary
Short summary
Biogenic secondary organic aerosol (BSOA), as an important atmospheric component, is prevalent within the boundary layer and can influence air quality and human health. Our observations demonstrate that anthropogenic NOx and the enhanced aerosol water driven by sulfate inhibit BSOA formation in lifting air masses, leading to a moderate reduction in the SOA burden in the upper boundary layer.
Emmanuel Chevassus, Kirsten N. Fossum, Darius Ceburnis, Lu Lei, Chunshui Lin, Wei Xu, Colin O'Dowd, and Jurgita Ovadnevaite
Atmos. Chem. Phys., 25, 4107–4129, https://doi.org/10.5194/acp-25-4107-2025, https://doi.org/10.5194/acp-25-4107-2025, 2025
Short summary
Short summary
This study presents the first source apportionment of organic aerosol at Mace Head via high-resolution mass spectrometry. Introducing transfer entropy as a novel method reveals that aged organic aerosol originates from both open-ocean ozonolysis and local peat-burning oxidation. Methanesulfonic acid and organic sea spray both mirror phytoplankton activity, with the former closely tied to coccolithophore blooms and the latter linked to diatoms, chlorophytes, and cyanobacteria.
Paola Formenti, Chiara Giorio, Karine Desboeufs, Alexander Zherebker, Marco Gaetani, Clarissa Baldo, Gautier Landrot, Simona Montebello, Servanne Chevaillier, Sylvain Triquet, Guillaume Siour, Claudia Di Biagio, Francesco Battaglia, Jean-François Doussin, Anais Feron, Andreas Namwoonde, and Stuart John Piketh
EGUsphere, https://doi.org/10.5194/egusphere-2025-446, https://doi.org/10.5194/egusphere-2025-446, 2025
Short summary
Short summary
The elemental composition and solubility of several metals, including iron, at a coastal site in Namibia in August–September 2017, indicate that natural and anthropogenic dust had different solubility depending on mineralogy but mostly to the processing by fluoride ions from marine emissions, pointing out to the complexity of atmospheric/oceanic interactions in this region of the world influenced by the Benguela current and significant aerosol load.
Jia-Yuan Wang, Meng-Xue Tang, Shan Lu, Ke-Jin Tang, Xing Peng, Ling-Yan He, and Xiao-Feng Huang
EGUsphere, https://doi.org/10.5194/egusphere-2025-1034, https://doi.org/10.5194/egusphere-2025-1034, 2025
Short summary
Short summary
Our study explores how secondary organic aerosols (SOA), a major component of air pollution, form in different particle sizes in a coastal city in China. We found that SOA in fine particles is mainly produced through aqueous chemical reactions, especially those involving iron. In contrast, coarse particles form SOA through reactions with ozone and gases from both fossil fuels and natural sources. These findings highlight the need for size-specific air pollution models.
Ashutosh K. Shukla, Sachchida N. Tripathi, Shamitaksha Talukdar, Vishnu Murari, Sreenivas Gaddamidi, Manousos-Ioannis Manousakas, Vipul Lalchandani, Kuldeep Dixit, Vinayak M. Ruge, Peeyush Khare, Mayank Kumar, Vikram Singh, Neeraj Rastogi, Suresh Tiwari, Atul K. Srivastava, Dilip Ganguly, Kaspar Rudolf Daellenbach, and André S. H. Prévôt
Atmos. Chem. Phys., 25, 3765–3784, https://doi.org/10.5194/acp-25-3765-2025, https://doi.org/10.5194/acp-25-3765-2025, 2025
Short summary
Short summary
Our study delves into the elemental composition of aerosols at three sites across the Indo-Gangetic Plain (IGP), revealing distinct patterns during pollution episodes. We found significant increases in chlorine (Cl)-rich and solid fuel combustion (SFC) sources, indicating dynamic emission sources, agricultural burning impacts, and meteorological influences. Surges in Cl-rich particles during cold periods highlight their role in particle growth under high-relative-humidity conditions.
Ye Kuang, Biao Luo, Shan Huang, Junwen Liu, Weiwei Hu, Yuwen Peng, Duohong Chen, Dingli Yue, Wanyun Xu, Bin Yuan, and Min Shao
Atmos. Chem. Phys., 25, 3737–3752, https://doi.org/10.5194/acp-25-3737-2025, https://doi.org/10.5194/acp-25-3737-2025, 2025
Short summary
Short summary
This research reveals the potential importance of nighttime NO3 radical chemistry and aerosol water in the rapid formation of secondary brown carbon from diluted biomass burning emissions. The findings enhance our understanding of nighttime biomass burning evolution and its implications for climate and regional air quality, especially regarding interactions with background aerosol water and water-rich fogs and clouds.
Rongshuang Xu, Yu-Chi Lin, Siyu Bian, Feng Xie, and Yan-Lin Zhang
EGUsphere, https://doi.org/10.5194/egusphere-2025-683, https://doi.org/10.5194/egusphere-2025-683, 2025
Short summary
Short summary
This work reported the hydroxymethanesulfonate (HMS) level in a continental city and, for the first time, in marine atmosphere. The enhancement by aerosol ionic strength (IS) on HMS formation was quantified which first rise with increasing IS, peaking at 4 mol kg–1 before declining. Given the IS range of marine (2–6) and urban aerosol (6–20 mol kg–1) and the clearly negative correlation between humidity and IS, the moderate IS level under humid condition may notably boost ambient HMS formation.
Jing Li, Jiaoshi Zhang, Xianda Gong, Steven Spielman, Chongai Kuang, Ashish Singh, Maria A. Zawadowicz, Lu Xu, and Jian Wang
EGUsphere, https://doi.org/10.5194/egusphere-2025-726, https://doi.org/10.5194/egusphere-2025-726, 2025
Short summary
Short summary
Using measurements at a rural coastal site, we quantified aerosols in representative air masses and identified major source of organics in Houston area. Our results show cooking aerosol is likely overestimated by earlier studies. Additionally, diurnal variation of highly oxidized organics is mostly driven by air mass changes instead of photochemistry. This study highlights the impacts of emissions, atmospheric chemistry, and meteorology on aerosol properties in the coastal-rural environment.
Fan Mei, Qi Zhang, Damao Zhang, Jerome D. Fast, Gourihar Kulkarni, Mikhail S. Pekour, Christopher R. Niedek, Susanne Glienke, Israel Silber, Beat Schmid, Jason M. Tomlinson, Hardeep S. Mehta, Xena Mansoura, Zezhen Cheng, Gregory W. Vandergrift, Nurun Nahar Lata, Swarup China, and Zihua Zhu
Atmos. Chem. Phys., 25, 3425–3444, https://doi.org/10.5194/acp-25-3425-2025, https://doi.org/10.5194/acp-25-3425-2025, 2025
Short summary
Short summary
This study highlights the unique capability of the ArcticShark, an uncrewed aerial system, in measuring vertically resolved atmospheric properties. Data from 32 research flights in 2023 reveal seasonal patterns and correlations with conventional measurements. The consistency and complementarity of in situ and remote sensing methods are highlighted. The study demonstrates the ArcticShark’s versatility in bridging data gaps and improving the understanding of vertical atmospheric structures.
Marco Paglione, Yufang Hao, Stefano Decesari, Mara Russo, Karam Mansour, Mauro Mazzola, Diego Fellin, Andrea Mazzanti, Emilio Tagliavini, Manousos Ioannis Manousakas, Evangelia Diapouli, Elena Barbaro, Matteo Feltracco, Kaspar Rudolf Daellenbach, and Matteo Rinaldi
EGUsphere, https://doi.org/10.5194/egusphere-2025-760, https://doi.org/10.5194/egusphere-2025-760, 2025
Short summary
Short summary
A year-long set of PM1 samples from Ny-Ålesund, Svalbard, was analyzed by H-NMR and HR-TOF-AMS for the chemical characterization of the organic fraction. Positive Matrix Factorization allowed to identify five organic aerosol sources with specific seasonality. Winter-spring aerosol is dominated by Eurasian pollution, while summer is characterized by biogenic aerosols from marine sources; occasional summertime high OA loadings are associated with wildfire aerosols.
Ting Yang, Yu Xu, Yu-Chen Wang, Yi-Jia Ma, Hong-Wei Xiao, Hao Xiao, and Hua-Yun Xiao
Atmos. Chem. Phys., 25, 2967–2978, https://doi.org/10.5194/acp-25-2967-2025, https://doi.org/10.5194/acp-25-2967-2025, 2025
Short summary
Short summary
Previous measurement–model comparisons of atmospheric isoprene levels showed a significant unidentified source of isoprene in some northern Chinese cities during winter. Here, the first combination of large-scale observations and field combustion experiments provides novel insights into biomass burning emissions as a significant source of isoprene-derived organosulfates during winter in northern cities of China.
Agnesh Panta, Konrad Kandler, Kerstin Schepanski, Andres Alastuey, Pavla Dagsson Waldhauserova, Sylvain Dupont, Melanie Eknayan, Cristina González-Flórez, Adolfo González-Romero, Martina Klose, Mara Montag, Xavier Querol, Jesús Yus-Díez, and Carlos Pérez García-Pando
EGUsphere, https://doi.org/10.5194/egusphere-2025-494, https://doi.org/10.5194/egusphere-2025-494, 2025
Short summary
Short summary
Iceland is among the most active dust source areas in the world. Dust properties are influenced by particle size, mineralogy, shape, and mixing state. This work characterizes freshly emitted individual aerosol particles of Icelandic dust using electron microscopy. Our study provides insights into critical particle-specific information will contribute to better constraining climate models that consider mineralogical variations in their representation of the dust cycle.
Xueqin Zheng, Junwen Liu, Nima Chuduo, Bian Ba, Pengfei Yu, Phu Drolgar, Fang Cao, and Yanlin Zhang
EGUsphere, https://doi.org/10.5194/egusphere-2025-164, https://doi.org/10.5194/egusphere-2025-164, 2025
Short summary
Short summary
In this study, we present the first report on the annual variation of stable oxygen isotope anomalies (∆17O = δ17O - 0.52 × δ18O) in NO3- collected from the urban area of Lhasa , on the Tibetan Plateau, China. Using a Bayesian isotope mixture model, we found that the relative contribution of the NO3+VOC pathway to NO3- formation in spring in Lhasa was several times higher than in urban cities, highlighting the significant influence of VOC transported from outside the Tibetan Plateau.
Yi-Jia Ma, Yu Xu, Ting Yang, Lin Gui, Hong-Wei Xiao, Hao Xiao, and Hua-Yun Xiao
Atmos. Chem. Phys., 25, 2763–2780, https://doi.org/10.5194/acp-25-2763-2025, https://doi.org/10.5194/acp-25-2763-2025, 2025
Short summary
Short summary
The abundance, potential precursors, and main formation mechanisms of nitrogen-containing organic compounds (NOCs) in PM2.5 during winter were compared among cities with different energy consumption patterns. The aerosol NOC pollution during winter in China is closely associated with the intensity of precursor emissions and the aqueous-phase processes. Our results highlight the importance of emission reduction strategies in controlling aerosol NOCs pollution during winter in China.
Dane Blanchard, Mark Gordon, Duc Huy Dang, Paul Andrew Makar, and Julian Aherne
Atmos. Chem. Phys., 25, 2423–2442, https://doi.org/10.5194/acp-25-2423-2025, https://doi.org/10.5194/acp-25-2423-2025, 2025
Short summary
Short summary
This study offers the first known evaluation of water-soluble brown carbon aerosols in the Athabasca oil sands region (AOSR), Canada. Fluorescence spectroscopy analysis of aerosol samples from five regional sites (collected during the summer of 2021) identified oil sands operations as a measurable brown carbon source. Industrial aerosol emissions were unlikely to impact regional radiative forcing. These findings show that fluorescence spectroscopy can be used to monitor brown carbon in the AOSR.
Kira Zeider, Kayla McCauley, Sanja Dmitrovic, Leong Wai Siu, Yonghoon Choi, Ewan C. Crosbie, Joshua P. DiGangi, Glenn S. Diskin, Simon Kirschler, John B. Nowak, Michael A. Shook, Kenneth L. Thornhill, Christiane Voigt, Edward L. Winstead, Luke D. Ziemba, Paquita Zuidema, and Armin Sorooshian
Atmos. Chem. Phys., 25, 2407–2422, https://doi.org/10.5194/acp-25-2407-2025, https://doi.org/10.5194/acp-25-2407-2025, 2025
Short summary
Short summary
In situ aircraft data collected over the northwest Atlantic Ocean are utilized to compare aerosol conditions and turbulence between near-surface and below-cloud-base altitudes for different regimes of coupling strength between those two levels, along with how cloud microphysical properties vary across those regimes. Stronger coupling yields more homogenous aerosol structure vertically along with higher cloud drop concentrations and sea salt influence in clouds.
Junke Zhang, Xinyi Fu, Chunying Chen, Yunfei Su, Siyu Liu, Luyao Chen, Yubao Chen, Gehui Wang, and Andre S. H. Prevot
EGUsphere, https://doi.org/10.5194/egusphere-2025-92, https://doi.org/10.5194/egusphere-2025-92, 2025
Short summary
Short summary
The 125 organic aerosol (OA) compounds in PM2.5 in winter in Chengdu were measured at the molecular level. OA was dominated by fatty acids, phthalate esters, and anhydrosugars, and were deeply influenced by anthropogenic sources. As pollution worsens: secondary inorganic species and secondary organic carbon (OC) dominated the increase in PM2.5; fatty acids and anhydrosugars dominated the increase in OA; and the contribution of secondary formation and biomass burning to OC increased markedly.
Amie Dobracki, Ernie R. Lewis, Arthur J. Sedlacek III, Tyler Tatro, Maria A. Zawadowicz, and Paquita Zuidema
Atmos. Chem. Phys., 25, 2333–2363, https://doi.org/10.5194/acp-25-2333-2025, https://doi.org/10.5194/acp-25-2333-2025, 2025
Short summary
Short summary
Biomass-burning aerosol is commonly present in the marine boundary layer over the southeast Atlantic Ocean between June and October. Our research indicates that burning conditions, aerosol transport pathways, and prolonged oxidation processes (heterogeneous and aqueous phases) determine the chemical, microphysical, and optical properties of the boundary layer aerosol. Notably, we find that the aerosol optical properties can be estimated from the chemical properties alone.
Benjamin Heutte, Nora Bergner, Hélène Angot, Jakob B. Pernov, Lubna Dada, Jessica A. Mirrielees, Ivo Beck, Andrea Baccarini, Matthew Boyer, Jessie M. Creamean, Kaspar R. Daellenbach, Imad El Haddad, Markus M. Frey, Silvia Henning, Tiia Laurila, Vaios Moschos, Tuukka Petäjä, Kerri A. Pratt, Lauriane L. J. Quéléver, Matthew D. Shupe, Paul Zieger, Tuija Jokinen, and Julia Schmale
Atmos. Chem. Phys., 25, 2207–2241, https://doi.org/10.5194/acp-25-2207-2025, https://doi.org/10.5194/acp-25-2207-2025, 2025
Short summary
Short summary
Limited aerosol measurements in the central Arctic hinder our understanding of aerosol–climate interactions in the region. Our year-long observations of aerosol physicochemical properties during the MOSAiC expedition reveal strong seasonal variations in aerosol chemical composition, where the short-term variability is heavily affected by storms in the Arctic. Local wind-generated particles are shown to be an important source of cloud seeds, especially in autumn.
Yifan Zhang, Rui Li, Zachary B. Bunnell, Yizhu Chen, Guanhong Zhu, Jinlong Ma, Guohua Zhang, Tim M. Conway, and Mingjin Tang
EGUsphere, https://doi.org/10.5194/egusphere-2025-474, https://doi.org/10.5194/egusphere-2025-474, 2025
Short summary
Short summary
The sources of aerosol Fe, especially soluble aerosol Fe, remain to be constrained. The stable isotope ratio of Fe (δ56Fe) has emerged as a potential tracer for discriminating and quantifying sources of aerosol Fe. In this review, we examine the state of the field for using δ56Fe as an aerosol source tracer, and constraints on endmember signatures.
Feng Jiang, Harald Saathoff, Uzoamaka Ezenobi, Junwei Song, Hengheng Zhang, Linyu Gao, and Thomas Leisner
Atmos. Chem. Phys., 25, 1917–1930, https://doi.org/10.5194/acp-25-1917-2025, https://doi.org/10.5194/acp-25-1917-2025, 2025
Short summary
Short summary
The chemical composition of brown carbon in the particle and gas phase was determined by mass spectrometry. BrC in the gas phase was mainly controlled by secondary formation and particle-to-gas partitioning. BrC in the particle phase was mainly from secondary formation. This work helps to get a better understanding of diurnal variations and the sources of brown carbon aerosol at a rural location in central Europe.
Kohei Sakata, Shotaro Takano, Atsushi Matsuki, Yasuo Takeichi, Hiroshi Tanimoto, Aya Sakaguchi, Minako Kurisu, and Yoshio Takahashi
EGUsphere, https://doi.org/10.5194/egusphere-2025-161, https://doi.org/10.5194/egusphere-2025-161, 2025
Short summary
Short summary
Deposition of aerosol iron (Fe) into the ocean stimulates primary production and influences the global carbon cycle, although the factors governing the aerosol Fe solubility remain uncertain. Our observations in Japan revealed that both mineral dust and anthropogenic aerosols are significant sources of dissolved Fe, and that atmospheric chemical weathering enhances their solubility. This finding is expected to play a crucial role in estimating the supply of dissolved iron to the ocean.
Rui Li, Yubing Shen, Yumeng Shao, Yining Gao, Ziwei Yao, Qian Liu, Xing Liu, and Guitao Shi
EGUsphere, https://doi.org/10.5194/egusphere-2024-3740, https://doi.org/10.5194/egusphere-2024-3740, 2025
Short summary
Short summary
It is the first time to reveal the global variations of PAHs derivatives in the marine air. We found that marine aerosols in East China Sea (ECS) and Western Pacific (WP) were significantly affected by coal and engine combustion, while those in Bismarck Sea (BS) and East Australian Sea (EAS) were mainly influenced by wildfire and coal combustion. Antarctic Ocean (AO) was dominated by biomass burning and local shipping emissions. This finding help elucidate the mechanism of global PAH cycle.
James Brean, David C. S. Beddows, Eija Asmi, Aki Virkkula, Lauriane L. J. Quéléver, Mikko Sipilä, Floortje Van Den Heuvel, Thomas Lachlan-Cope, Anna Jones, Markus Frey, Angelo Lupi, Jiyeon Park, Young Jun Yoon, Rolf Weller, Giselle L. Marincovich, Gabriela C. Mulena, Roy M. Harrison, and Manuel Dall'Osto
Atmos. Chem. Phys., 25, 1145–1162, https://doi.org/10.5194/acp-25-1145-2025, https://doi.org/10.5194/acp-25-1145-2025, 2025
Short summary
Short summary
Our results emphasise how understanding the geographical variation in surface types across the Antarctic is key to understanding secondary aerosol sources.
Adam E. Thomas, Hayley S. Glicker, Alex B. Guenther, Roger Seco, Oscar Vega Bustillos, Julio Tota, Rodrigo A. F. Souza, and James N. Smith
Atmos. Chem. Phys., 25, 959–977, https://doi.org/10.5194/acp-25-959-2025, https://doi.org/10.5194/acp-25-959-2025, 2025
Short summary
Short summary
We present measurements of the organic composition of ultrafine particles collected from the eastern Amazon, an understudied region that is subjected to increasing human influence. We find that while isoprene chemistry is likely significant for ultrafine-particle growth throughout the year, compounds related to other sources, such as biological-spore emissions and biomass burning, exhibit striking seasonal differences, implying extensive variation in regional ultrafine-particle sources.
Cited articles
Anderson, D. C., Loughner, C. P., Diskin, G., Weinheimer, A., Canty, T. P.,
Salawitch, R. J., Worden, H. M., Fried, A., Mikoviny, T., and Wisthaler, A.:
Measured and modeled CO and NOy in DISCOVER-AQ: An evaluation of
emissions and chemistry over the eastern US, Atmos. Environ., 96, 78–87,
2014.
Atkinson, R. and Arey, J.: Atmospheric Degradation of Volatile Organic
Compounds, Chem. Rev., 103, 4605–4638, https://doi.org/10.1021/cr0206420, 2003.
Battaglia Jr., M. A., Douglas, S., and Hennigan, C. J.: Effect of the Urban
Heat Island on Aerosol pH, Environ. Sci. Technol., 51, 13095, https://doi.org/10.1021/acs.est.7b02786,
2017.
Beyersdorf, A. J., Ziemba, L. D., Chen, G., Corr, C. A., Crawford, J. H.,
Diskin, G. S., Moore, R. H., Thornhill, K. L., Winstead, E. L., and Anderson,
B. E.: The impacts of aerosol loading, composition, and water uptake on
aerosol extinction variability in the Baltimore–Washington, D.C. region,
Atmos. Chem. Phys., 16, 1003–1015, https://doi.org/10.5194/acp-16-1003-2016,
2016.
Budisulistiorini, S. H., Baumann, K., Edgerton, E. S., Bairai, S. T.,
Mueller, S., Shaw, S. L., Knipping, E. M., Gold, A., and Surratt, J. D.:
Seasonal characterization of submicron aerosol chemical composition and
organic aerosol sources in the southeastern United States: Atlanta,
Georgia,and Look Rock, Tennessee, Atmos. Chem. Phys., 16, 5171–5189,
https://doi.org/10.5194/acp-16-5171-2016, 2016.
Budisulistiorini, S. H., Nenes, A., Carlton, A. G., Surratt, J. D., McNeill,
V. F., and Pye, H. O. T.: Simulating Aqueous-Phase Isoprene-Epoxydiol (IEPOX)
Secondary Organic Aerosol Production During the 2013 Southern Oxidant and
Aerosol Study (SOAS), Environ. Sci. Technol., 51, 5026–5034,
https://doi.org/10.1021/acs.est.6b05750, 2017.
Carlton, A. G., Turpin, B. J., Altieri, K. E., Seitzinger, S. P., Mathur, R.,
Roselle, S. J., and Weber, R. J.: CMAQ Model Performance Enhanced When
In-Cloud Secondary Organic Aerosol is Included: Comparisons of Organic Carbon
Predictions with Measurements, Environ. Sci. Technol., 42, 8798–8802,
https://doi.org/10.1021/es801192n, 2008.
Carlton, A. G., Wiedinmyer, C., and Kroll, J. H.: A review of Secondary
Organic Aerosol (SOA) formation from isoprene, Atmos. Chem. Phys., 9,
4987–5005, https://doi.org/10.5194/acp-9-4987-2009, 2009.
Chan Miller, C., Jacob, D. J., Marais, E. A., Yu, K., Travis, K. R., Kim, P.
S., Fisher, J. A., Zhu, L., Wolfe, G. M., Hanisco, T. F., Keutsch, F. N.,
Kaiser, J., Min, K.-E., Brown, S. S., Washenfelder, R. A., González Abad,
G., and Chance, K.: Glyoxal yield from isoprene oxidation and relation to
formaldehyde: chemical mechanism, constraints from SENEX aircraft
observations, and interpretation of OMI satellite data, Atmos. Chem. Phys.,
17, 8725–8738, https://doi.org/10.5194/acp-17-8725-2017, 2017.
De Haan, D. O., Corrigan, A. L., Tolbert, M. A., Jimenez, J. L., Wood, S. E.,
and Turley, J. J.: Secondary Organic Aerosol Formation by Self-Reactions of
Methylglyoxal and Glyoxal in Evaporating Droplets, Environ. Sci. Technol.,
43, 8184–8190, https://doi.org/10.1021/es902152t, 2009.
de Sá, S. S., Palm, B. B., Campuzano-Jost, P., Day, D. A., Newburn, M.
K., Hu, W., Isaacman-VanWertz, G., Yee, L. D., Thalman, R., Brito, J.,
Carbone, S., Artaxo, P., Goldstein, A. H., Manzi, A. O., Souza, R. A. F.,
Mei, F., Shilling, J. E., Springston, S. R., Wang, J., Surratt, J. D.,
Alexander, M. L., Jimenez, J. L., and Martin, S. T.: Influence of urban
pollution on the production of organic particulate matter from isoprene
epoxydiols in central Amazonia, Atmos. Chem. Phys., 17, 6611–6629,
https://doi.org/10.5194/acp-17-6611-2017, 2017.
Ding, X., Zheng, M., Yu, L., Zhang, X., Weber, R. J., Yan, B., Russell, A.
G., Edgerton, E. S., and Wang, X.: Spatial and seasonal trends in biogenic
secondary organic aerosol tracers and water-soluble organic carbon in the
southeastern United States, Environ. Sci. Technol., 42, 5171–5176, 2008.
Donahue, N. M., Robinson, A. L., and Pandis, S. N.: Atmospheric organic
particulate matter: From smoke to secondary organic aerosol, Atmos. Environ.,
43, 94–106, 2009.
Edwards, P. M., Aikin, K. C., Dube, W. P., Fry, J. L., Gilman, J. B., de
Gouw, J. A., Graus, M. G., Hanisco, T. F., Holloway, J., Hubler, G., Kaiser,
J., Keutsch, F. N., Lerner, B. M., Neuman, J. A., Parrish, D. D., Peischl,
J., Pollack, I. B., Ravishankara, A. R., Roberts, J. M., Ryerson, T. B.,
Trainer, M., Veres, P. R., Wolfe, G. M., Warneke, C., and Brown, S. S.:
Transition from high- to low-NOx control of night-time oxidation in the
southeastern US, Nat. Geosci., 10, 490–495, https://doi.org/10.1038/ngeo2976, 2017.
El-Sayed, M. M. H., Wang, Y. Q., and Hennigan, C. J.: Direct atmospheric
evidence for the irreversible formation of aqueous secondary organic aerosol,
Geophys. Res. Lett., 42, 5577–5586, https://doi.org/10.1002/2015gl064556, 2015.
El-Sayed, M. M. H., Amenumey, D., and Hennigan, C. J.: Drying-Induced
Evaporation of Secondary Organic Aerosol during Summer, Environ. Sci.
Technol., 50, 3626–3633, https://doi.org/10.1021/acs.est.5b06002, 2016.
Ervens, B., Carlton, A. G., Turpin, B. J., Altieri, K. E., Kreidenweis, S.
M., and Feingold, G.: Secondary organic aerosol yields from cloud-processing
of isoprene oxidation products, Geophys. Res. Lett., 35, L02816,
https://doi.org/10.1029/2007gl031828, 2008.
Ervens, B., Turpin, B. J., and Weber, R. J.: Secondary organic aerosol
formation in cloud droplets and aqueous particles (aqSOA): a review of
laboratory, field and model studies, Atmos. Chem. Phys., 11, 11069–11102,
https://doi.org/10.5194/acp-11-11069-2011, 2011.
Ervens, B., Sorooshian, A., Lim, Y. B., and Turpin, B. J.: Key parameters
controlling OH-initiated formation of secondary organic aerosol in the
aqueous phase (aqSOA), J. Geophys. Res.-Atmos., 119, 3997–4016,
https://doi.org/10.1002/2013JD021021, 2014.
Faust, J. A., Wong, J. P. S., Lee, A. K. Y., and Abbatt, J. P. D.: Role of
Aerosol Liquid Water in Secondary Organic Aerosol Formation from Volatile
Organic Compounds, Environ. Sci. Technol., 51, 1405–1413,
https://doi.org/10.1021/acs.est.6b04700, 2017.
Fu, T. M., Jacob, D. J., Wittrock, F., Burrows, J. P., Vrekoussis, M., and
Henze, D. K.: Global budgets of atmospheric glyoxal and methylglyoxal, and
implications for formation of secondary organic aerosols, J. Geophys.
Res.-Atmos., 113, D15303, https://doi.org/10.1029/2007jd009505, 2008.
Galloway, M. M., Chhabra, P. S., Chan, A. W. H., Surratt, J. D., Flagan, R.
C., Seinfeld, J. H., and Keutsch, F. N.: Glyoxal uptake on ammonium sulphate
seed aerosol: reaction products and reversibility of uptake under dark and
irradiated conditions, Atmos. Chem. Phys., 9, 3331–3345,
https://doi.org/10.5194/acp-9-3331-2009, 2009.
Gaston, C. J., Riedel, T. P., Zhang, Z., Gold, A., Surratt, J. D., and
Thornton, J. A.: Reactive Uptake of an Isoprene-Derived Epoxydiol to
Submicron Aerosol Particles, Environ. Sci. Technol., 48, 11178–11186,
https://doi.org/10.1021/es5034266, 2014.
Goldstein, A. H., Goulden, M. L., Munger, J. W., Wofsy, S. C., and Geron, C.
D.: Seasonal course of isoprene emissions from a midlatitude deciduous
forest, J. Geophys. Res.-Atmos., 103, 31045–31056, https://doi.org/10.1029/98jd02708,
1998.
Guenther, A. B., Jiang, X., Heald, C. L., Sakulyanontvittaya, T., Duhl, T.,
Emmons, L. K., and Wang, X.: The Model of Emissions of Gases and Aerosols
from Nature version 2.1 (MEGAN2.1): an extended and updated framework for
modeling biogenic emissions, Geosci. Model Dev., 5, 1471–1492,
https://doi.org/10.5194/gmd-5-1471-2012, 2012.
Guo, H., Xu, L., Bougiatioti, A., Cerully, K. M., Capps, S. L., Hite Jr., J.
R., Carlton, A. G., Lee, S.-H., Bergin, M. H., Ng, N. L., Nenes, A., and
Weber, R. J.: Fine-particle water and pH in the southeastern United States,
Atmos. Chem. Phys., 15, 5211–5228, https://doi.org/10.5194/acp-15-5211-2015,
2015.
Guo, H., Sullivan, A. P., Campuzano-Jost, P., Schroder, J. C.,
Lopez-Hilfiker, F. D., Dibb, J. E., Jimenez, J. L., Thornton, J. A., Brown,
S. S., and Nenes, A.: Fine particle pH and the partitioning of nitric acid
during winter in the northeastern United States, J. Geophys. Res.-Atmos.,
121, 10355–10376, https://doi.org/10.1002/2016JD025311, 2016.
He, H., Stehr, J. W., Hains, J. C., Krask, D. J., Doddridge, B. G., Vinnikov,
K. Y., Canty, T. P., Hosley, K. M., Salawitch, R. J., Worden, H. M., and
Dickerson, R. R.: Trends in emissions and concentrations of air pollutants in
the lower troposphere in the Baltimore/Washington airshed from 1997 to 2011,
Atmos. Chem. Phys., 13, 7859–7874, https://doi.org/10.5194/acp-13-7859-2013,
2013.
Heald, C. L., Henze, D. K., Horowitz, L. W., Feddema, J., Lamarque, J. F.,
Guenther, A., Hess, P. G., Vitt, F., Seinfeld, J. H., Goldstein, A. H., and
Fung, I.: Predicted change in global secondary organic aerosol concentrations
in response to future climate, emissions, and land use change, J. Geophys.
Res.-Atmos., 113, D05211, https://doi.org/10.1029/2007jd009092, 2008.
Hennigan, C. J., Bergin, M. H., Dibb, J. E., and Weber, R. J.: Enhanced
secondary organic aerosol formation due to water uptake by fine particles,
Geophys. Res. Lett., 35, L18801, https://doi.org/10.1029/2008gl035046, 2008.
Henze, D. K. and Seinfeld, J. H.: Global secondary organic aerosol from
isoprene oxidation, Geophys. Res. Lett., 33, L09812,
https://doi.org/10.1029/2006gl025976, 2006.
Hodzic, A., Aumont, B., Knote, C., Lee-Taylor, J., Madronich, S., and
Tyndall, G.: Volatility dependence of Henry's law constants of condensable
organics: Application to estimate depositional loss of secondary organic
aerosols, Geophys. Res. Lett., 41, 4795–4804, https://doi.org/10.1002/2014gl060649,
2014.
Hu, W., Palm, B. B., Day, D. A., Campuzano-Jost, P., Krechmer, J. E., Peng,
Z., de Sá, S. S., Martin, S. T., Alexander, M. L., Baumann, K., Hacker,
L., Kiendler-Scharr, A., Koss, A. R., de Gouw, J. A., Goldstein, A. H., Seco,
R., Sjostedt, S. J., Park, J.-H., Guenther, A. B., Kim, S., Canonaco, F.,
Prévôt, A. S. H., Brune, W. H., and Jimenez, J. L.: Volatility and
lifetime against OH heterogeneous reaction of ambient
isoprene-epoxydiols-derived secondary organic aerosol (IEPOX-SOA), Atmos.
Chem. Phys., 16, 11563–11580, https://doi.org/10.5194/acp-16-11563-2016,
2016.
Jathar, S. H., Cappa, C. D., Wexler, A. S., Seinfeld, J. H., and Kleeman, M.
J.: Simulating secondary organic aerosol in a regional air quality model
using the statistical oxidation model – Part 1: Assessing the influence of
constrained multi-generational ageing, Atmos. Chem. Phys., 16, 2309–2322,
https://doi.org/10.5194/acp-16-2309-2016, 2016.
Jimenez, J. L., Canagaratna, M. R., Donahue, N. M., Prevot, A. S. H., Zhang,
Q., Kroll, J. H., DeCarlo, P. F., Allan, J. D., Coe, H., Ng, N. L., Aiken, A.
C., Docherty, K. S., Ulbrich, I. M., Grieshop, A. P., Robinson, A. L.,
Duplissy, J., Smith, J. D., Wilson, K. R., Lanz, V. A., Hueglin, C., Sun, Y.
L., Tian, J., Laaksonen, A., Raatikainen, T., Rautiainen, J., Vaattovaara,
P., Ehn, M., Kulmala, M., Tomlinson, J. M., Collins, D. R., Cubison, M. J.,
Dunlea, J., Huffman, J. A., Onasch, T. B., Alfarra, M. R., Williams, P. I.,
Bower, K., Kondo, Y., Schneider, J., Drewnick, F., Borrmann, S., Weimer, S.,
Demerjian, K., Salcedo, D., Cottrell, L., Griffin, R., Takami, A., Miyoshi,
T., Hatakeyama, S., Shimono, A., Sun, J. Y., Zhang, Y. M., Dzepina, K.,
Kimmel, J. R., Sueper, D., Jayne, J. T., Herndon, S. C., Trimborn, A. M.,
Williams, L. R., Wood, E. C., Middlebrook, A. M., Kolb, C. E., Baltensperger,
U., and Worsnop, D. R.: Evolution of Organic Aerosols in the Atmosphere,
Science, 326, 1525, https://doi.org/10.1126/science.1180353, 2009.
Khlystov, A., Stanier, C. O., Takahama, S., and Pandis, S. N.: Water content
of ambient aerosol during the Pittsburgh air quality study, J. Geophys.
Res.-Atmos., 110, D07S10, https://doi.org/10.1029/2004jd004651, 2005.
Kim, P. S., Jacob, D. J., Fisher, J. A., Travis, K., Yu, K., Zhu, L.,
Yantosca, R. M., Sulprizio, M. P., Jimenez, J. L., Campuzano-Jost, P., Froyd,
K. D., Liao, J., Hair, J. W., Fenn, M. A., Butler, C. F., Wagner, N. L.,
Gordon, T. D., Welti, A., Wennberg, P. O., Crounse, J. D., St. Clair, J. M.,
Teng, A. P., Millet, D. B., Schwarz, J. P., Markovic, M. Z., and Perring, A.
E.: Sources, seasonality, and trends of southeast US aerosol: an integrated
analysis of surface, aircraft, and satellite observations with the GEOS-Chem
chemical transport model, Atmos. Chem. Phys., 15, 10411–10433,
https://doi.org/10.5194/acp-15-10411-2015, 2015.
Kleindienst, T. E., Jaoui, M., Lewandowski, M., Offenberg, J. H., Lewis, C.
W., Bhave, P. V., and Edney, E. O.: Estimates of the contributions of
biogenic and anthropogenic hydrocarbons to secondary organic aerosol at a
southeastern US location, Atmos. Environ., 41, 8288–8300,
https://doi.org/10.1016/j.atmosenv.2007.06.045, 2007.
Kondo, Y., Miyazaki, Y., Takegawa, N., Miyakawa, T., Weber, R. J., Jimenez,
J. L., Zhang, Q., and Worsnop, D. R.: Oxygenated and water-soluble organic
aerosols in Tokyo, J. Geophys. Res.-Atmos., 112, D01203,
https://doi.org/10.1029/2006jd007056, 2007.
Krechmer, J. E., Coggon, M. M., Massoli, P., Nguyen, T. B., Crounse, J. D.,
Hu, W., Day, D. A., Tyndall, G. S., Henze, D. K., and Rivera-Rios, J. C.:
Formation of low volatility organic compounds and secondary organic aerosol
from isoprene hydroxyhydroperoxide low-NO oxidation, Environ. Sci. Technol.,
49, 10330–10339, 2015.
Kroll, J. H. and Seinfeld, J. H.: Chemistry of secondary organic aerosol:
Formation and evolution of low-volatility organics in the atmosphere, Atmos.
Environ., 42, 3593–3624, https://doi.org/10.1016/j.atmosenv.2008.01.003, 2008.
Kroll, J. H., Ng, N. L., Murphy, S. M., Flagan, R. C., and Seinfeld, J. H.:
Secondary organic aerosol formation from isoprene photooxidation under
high-NOx conditions, Geophys. Res. Lett., 32, L18808,
https://doi.org/10.1029/2005gl023637, 2005.
Kroll, J. H., Ng, N. L., Murphy, S. M., Flagan, R. C., and Seinfeld, J. H.:
Secondary Organic Aerosol Formation from Isoprene Photooxidation, Environ.
Sci. Technol., 40, 1869–1877, https://doi.org/10.1021/es0524301, 2006.
Lee, A. K. Y., Zhao, R., Li, R., Liggio, J., Li, S.-M., and Abbatt, J. P. D.:
Formation of Light Absorbing Organo-Nitrogen Species from Evaporation of
Droplets Containing Glyoxal and Ammonium Sulfate, Environ. Sci. Technol., 47,
12819–12826, https://doi.org/10.1021/es402687w, 2013.
Lin, P., Yu, J. Z., Engling, G., and Kalberer, M.: Organosulfates in
humic-like substance fraction isolated from aerosols at seven locations in
East Asia: A study by ultra-high-resolution mass spectrometry, Environ. Sci.
Technol., 46, 13118–13127, 2012.
Liu, J., D'Ambro, E. L., Lee, B. H., Lopez-Hilfiker, F. D., Zaveri, R. A.,
Rivera-Rios, J. C., Keutsch, F. N., Iyer, S., Kurten, T., Zhang, Z., Gold, A.,
Surratt, J. D., Shilling J. E., and Thornton, J. A.:
Efficient isoprene secondary organic aerosol formation from a non-IEPOX
pathway, Environ. Sci. Technol., 50, 9872–9880, 2016.
Liu, Y., Kuwata, M., McKinney, K. A., and Martin, S. T.: Uptake and release
of gaseous species accompanying the reactions of isoprene photo-oxidation
products with sulfate particles, Phys. Chem. Chem. Phys., 18, 1595–1600,
https://doi.org/10.1039/C5CP04551G, 2016.
Lopez-Hilfiker, F. D., Mohr, C., D'Ambro, E. L., Lutz, A., Riedel, T. P.,
Gaston, C. J., Iyer, S., Zhang, Z., Gold, A., Surratt, J. D., Lee, B. H.,
Kurten, T., Hu, W. W., Jimenez, J., Hallquist, M., and Thornton, J. A.:
Molecular Composition and Volatility of Organic Aerosol in the Southeastern
U.S.: Implications for IEPOX Derived SOA, Environ. Sci. Technol., 50,
2200–2209, https://doi.org/10.1021/acs.est.5b04769, 2016.
Marais, E. A., Jacob, D. J., Jimenez, J. L., Campuzano-Jost, P., Day, D. A.,
Hu, W., Krechmer, J., Zhu, L., Kim, P. S., Miller, C. C., Fisher, J. A.,
Travis, K., Yu, K., Hanisco, T. F., Wolfe, G. M., Arkinson, H. L., Pye, H. O.
T., Froyd, K. D., Liao, J., and McNeill, V. F.: Aqueous-phase mechanism for
secondary organic aerosol formation from isoprene: application to the
southeast United States and co-benefit of SO2 emission controls, Atmos.
Chem. Phys., 16, 1603–1618, https://doi.org/10.5194/acp-16-1603-2016, 2016.
McNeill, V. F.: Aqueous Organic Chemistry in the Atmosphere: Sources and
Chemical Processing of Organic Aerosols, Environ. Sci. Technol., 49,
1237–1244, https://doi.org/10.1021/es5043707, 2015.
Ng, N. L., Kroll, J. H., Keywood, M. D., Bahreini, R., Varutbangkul, V.,
Flagan, R. C., Seinfeld, J. H., Lee, A., and Goldstein, A. H.: Contribution
of First- versus Second-Generation Products to Secondary Organic Aerosols
Formed in the Oxidation of Biogenic Hydrocarbons, Environ. Sci. Technol., 40,
2283–2297, https://doi.org/10.1021/es052269u, 2006.
Nguyen, T. B., Coggon, M. M., Bates, K. H., Zhang, X., Schwantes, R. H.,
Schilling, K. A., Loza, C. L., Flagan, R. C., Wennberg, P. O., and Seinfeld,
J. H.: Organic aerosol formation from the reactive uptake of isoprene
epoxydiols (IEPOX) onto non-acidified inorganic seeds, Atmos. Chem. Phys.,
14, 3497–3510, https://doi.org/10.5194/acp-14-3497-2014, 2014.
Nguyen, T. B., Crounse, J. D., Teng, A. P., St. Clair, J. M., Paulot, F.,
Wolfe, G. M., and Wennberg, P. O.: Rapid deposition of oxidized biogenic
compounds to a temperate forest, P. Natl Acad. Sci. USA, 112, E392–E401,
https://doi.org/10.1073/pnas.1418702112, 2015.
Ortiz-Montalvo, D. L., Lim, Y. B., Perri, M. J., Seitzinger, S. P., and
Turpin, B. J.: Volatility and Yield of Glycolaldehyde SOA Formed through
Aqueous Photochemistry and Droplet Evaporation, Aerosol Sci. Technol., 46,
1002–1014, https://doi.org/10.1080/02786826.2012.686676, 2012.
Ortiz-Montalvo, D. L., Häkkinen, S. A. K., Schwier, A. N., Lim, Y. B.,
McNeill, V. F., and Turpin, B. J.: Ammonium Addition (and Aerosol pH) Has a
Dramatic Impact on the Volatility and Yield of Glyoxal Secondary Organic
Aerosol, Environ. Sci. Technol., 48, 255–262, https://doi.org/10.1021/es4035667, 2014.
Palmer, P. I., Jacob, D. J., Fiore, A. M., Martin, R. V., Chance, K., and
Kurosu, T. P.: Mapping isoprene emissions over North America using
formaldehyde column observations from space, J. Geophys. Res.-Atmos., 108,
4180, https://doi.org/10.1029/2002jd002153, 2003.
Pankow, J. F.: Organic particulate material levels in the atmosphere:
Conditions favoring sensitivity to varying relative humidity and temperature,
P. Natl. Acad. Sci. USA, 107, 6682–6686, https://doi.org/10.1073/pnas.1001043107, 2010.
Pankow, J. F., Marks, M. C., Barsanti, K. C., Mahmud, A., Asher, W. E., Li,
J., Ying, Q., Jathar, S. H., and Kleeman, M. J.: Molecular view modeling of
atmospheric organic particulate matter: Incorporating molecular structure and
co-condensation of water, Atmos. Environ., 122, 400–408, 2015.
Paulot, F., Crounse, J. D., Kjaergaard, H. G., Kürten, A., St. Clair, J.
M., Seinfeld, J. H., and Wennberg, P. O.: Unexpected Epoxide Formation in the
Gas-Phase Photooxidation of Isoprene, Science, 325, 730–733, https://doi.org/10.1126/science.1172910,
2009.
Pfister, G. G., Emmons, L. K., Hess, P. G., Lamarque, J. F., Orlando, J. J.,
Walters, S., Guenther, A., Palmer, P. I., and Lawrence, P. J.: Contribution
of isoprene to chemical budgets: A model tracer study with the NCAR CTM
MOZART-4, J. Geophys. Res.-Atmos., 113, D05308, https://doi.org/10.1029/2007JD008948, 2008.
Pruppacher, H. R.: The Role of Cloudphysics in Atmospheric Multiphase
Systems: Ten Basic Statements, in: Chemistry of Multiphase Atmospheric
Systems, edited by: Jaeschke, W., Springer Berlin Heidelberg, Berlin,
Heidelberg, 133–190, 1986.
Psichoudaki, M. and Pandis, S. N.: Atmospheric Aerosol Water-Soluble Organic
Carbon Measurement: A Theoretical Analysis, Environ. Sci. Technol., 47,
9791–9798, https://doi.org/10.1021/es402270y, 2013.
Pye, H. O. T., Pinder, R. W., Piletic, I. R., Xie, Y., Capps, S. L., Lin,
Y.-H., Surratt, J. D., Zhang, Z., Gold, A., Luecken, D. J., Hutzell, W. T.,
Jaoui, M., Offenberg, J. H., Kleindienst, T. E., Lewandowski, M., and Edney,
E. O.: Epoxide Pathways Improve Model Predictions of Isoprene Markers and
Reveal Key Role of Acidity in Aerosol Formation, Environ. Sci. Technol., 47,
11056–11064, https://doi.org/10.1021/es402106h, 2013.
Pye, H. O. T., Murphy, B. N., Xu, L., Ng, N. L., Carlton, A. G., Guo, H.,
Weber, R., Vasilakos, P., Appel, K. W., Budisulistiorini, S. H., Surratt, J.
D., Nenes, A., Hu, W., Jimenez, J. L., Isaacman-VanWertz, G., Misztal, P. K.,
and Goldstein, A. H.: On the implications of aerosol liquid water and phase
separation for organic aerosol mass, Atmos. Chem. Phys., 17, 343–369,
https://doi.org/10.5194/acp-17-343-2017, 2017.
Riedel, T. P., Lin, Y.-H., Budisulistiorini, S. H., Gaston, C. J., Thornton,
J. A., Zhang, Z., Vizuete, W., Gold, A., and Surratt, J. D.: Heterogeneous
Reactions of Isoprene-Derived Epoxides: Reaction Probabilities and Molar
Secondary Organic Aerosol Yield Estimates, Environ. Sci. Technol. Lett., 2,
38–42, https://doi.org/10.1021/ez500406f, 2015.
Riva, M., Budisulistiorini, S. H., Chen, Y., Zhang, Z., D'Ambro, E. L.,
Zhang, X., Gold, A., Turpin, B. J., Thornton, J. A., Canagaratna, M. R., and
Surratt, J. D.: Chemical Characterization of Secondary Organic Aerosol from
Oxidation of Isoprene Hydroxyhydroperoxides, Environ. Sci. Technol., 50,
9889–9899, https://doi.org/10.1021/acs.est.6b02511, 2016.
Riva, M., Budisulistiorini, S. H., Zhang, Z., Gold, A., Thornton, J. A.,
Turpin, B. J., and Surratt, J. D.: Multiphase reactivity of gaseous
hydroperoxide oligomers produced from isoprene ozonolysis in the presence of
acidified aerosols, Atmos. Environ., 152, 314–322, 2017.
Saha, P. K., Khlystov, A., Yahya, K., Zhang, Y., Xu, L., Ng, N. L., and
Grieshop, A. P.: Quantifying the volatility of organic aerosol in the
southeastern US, Atmos. Chem. Phys., 17, 501–520,
https://doi.org/10.5194/acp-17-501-2017, 2017.
Sander, R.: Compilation of Henry's law constants (version 4.0) for water as
solvent, Atmos. Chem. Phys., 15, 4399–4981,
https://doi.org/10.5194/acp-15-4399-2015, 2015.
Sanderson, M. G., Jones, C. D., Collins, W. J., Johnson, C. E., and Derwent,
R. G.: Effect of climate change on isoprene emissions and surface ozone
levels, Geophys. Res. Lett., 30, 1936, https://doi.org/10.1029/2003gl017642, 2003.
Sareen, N., Waxman, E. M., Turpin, B. J., Volkamer, R., and Carlton, A. G.:
Potential of Aerosol Liquid Water to Facilitate Organic Aerosol Formation:
Assessing Knowledge Gaps about Precursors and Partitioning, Environ. Sci.
Technol., 51, 3327–3335, https://doi.org/10.1021/acs.est.6b04540, 2017.
Seinfeld, J. H. and Pankow, J. F.: Organic atmospheric particulate material,
Annu. Rev. Phys. Chem., 54, 121–140, 2003.
Spaulding, R. S., Talbot, R. W., and Charles, M. J.: Optimization of a Mist
Chamber (Cofer Scrubber) for Sampling Water-Soluble Organics in Air, Environ.
Sci. Technol., 36, 1798–1808, https://doi.org/10.1021/es011189x, 2002.
Sullivan, A. P., Weber, R. J., Clements, A. L., Turner, J. R., Bae, M. S.,
and Schauer, J. J.: A method for on-line measurement of water-soluble organic
carbon in ambient aerosol particles: Results from an urban site, Geophys.
Res. Lett., 31, L13105, https://doi.org/10.1029/2004gl019681, 2004.
Sun, Y.-L., Zhang, Q., Schwab, J. J., Demerjian, K. L., Chen, W.-N., Bae,
M.-S., Hung, H.-M., Hogrefe, O., Frank, B., Rattigan, O. V., and Lin, Y.-C.:
Characterization of the sources and processes of organic and inorganic
aerosols in New York city with a high-resolution time-of-flight aerosol mass
apectrometer, Atmos. Chem. Phys., 11, 1581–1602,
https://doi.org/10.5194/acp-11-1581-2011, 2011.
Surratt, J. D., Murphy, S. M., Kroll, J. H., Ng, N. L., Hildebrandt, L.,
Sorooshian, A., Szmigielski, R., Vermeylen, R., Maenhaut, W., Claeys, M.,
Flagan, R. C., and Seinfeld, J. H.: Chemical Composition of Secondary Organic
Aerosol Formed from the Photooxidation of Isoprene, J. Phys. Chem. A, 110,
9665–9690, https://doi.org/10.1021/jp061734m, 2006.
Surratt, J. D., Chan, A. W. H., Eddingsaas, N. C., Chan, M., Loza, C. L.,
Kwan, A. J., Hersey, S. P., Flagan, R. C., Wennberg, P. O., and Seinfeld, J.
H.: Reactive intermediates revealed in secondary organic aerosol formation
from isoprene, P. Natl Acad. Sci. USA, 107, 6640–6645,
https://doi.org/10.1073/pnas.0911114107, 2010.
Timonen, H., Carbone, S., Aurela, M., Saarnio, K., Saarikoski, S., Ng, N. L.,
Canagaratna, M. R., Kulmala, M., Kerminen, V.-M., Worsnop, D. R., and
Hillamo, R.: Characteristics, sources and water-solubility of ambient
submicron organic aerosol in springtime in Helsinki, Finland, J. Aerosol
Sci., 56, 61–77, https://doi.org/10.1016/j.jaerosci.2012.06.005, 2013.
Travis, K. R., Jacob, D. J., Fisher, J. A., Kim, P. S., Marais, E. A., Zhu,
L., Yu, K., Miller, C. C., Yantosca, R. M., Sulprizio, M. P., Thompson, A.
M., Wennberg, P. O., Crounse, J. D., St. Clair, J. M., Cohen, R. C.,
Laughner, J. L., Dibb, J. E., Hall, S. R., Ullmann, K., Wolfe, G. M.,
Pollack, I. B., Peischl, J., Neuman, J. A., and Zhou, X.: Why do models
overestimate surface ozone in the Southeast United States?, Atmos. Chem.
Phys., 16, 13561–13577, https://doi.org/10.5194/acp-16-13561-2016, 2016.
Weber, R. J., Sullivan, A. P., Peltier, R. E., Russell, A., Yan, B., Zheng,
M., de Gouw, J., Warneke, C., Brock, C., Holloway, J. S., Atlas, E. L., and
Edgerton, E.: A study of secondary organic aerosol formation in the
anthropogenic-influenced southeastern United States, J. Geophys. Res.-Atmos.,
112, D13302, https://doi.org/10.1029/2007jd008408, 2007.
Weber, R. J., Guo, H., Russell, A. G., and Nenes, A.: High aerosol acidity
despite declining atmospheric sulfate concentrations over the past 15 years,
Nat. Geosci., 9, 282–285, 2016.
Wong, J. P. S., Lee, A. K. Y., and Abbatt, J. P. D.: Impacts of Sulfate Seed
Acidity and Water Content on Isoprene Secondary Organic Aerosol Formation,
Environ. Sci. Technol., 49, 13215–13221, https://doi.org/10.1021/acs.est.5b02686, 2015.
Xu, L., Kollman, M. S., Song, C., Shilling, J. E., and Ng, N. L.: Effects of
NOx on the Volatility of Secondary Organic Aerosol from Isoprene
Photooxidation, Environ. Sci. Technol., 48, 2253–2262,
https://doi.org/10.1021/es404842g, 2014.
Xu, L., Guo, H., Boyd, C. M., Klein, M., Bougiatioti, A., Cerully, K. M.,
Hite, J. R., Isaacman-VanWertz, G., Kreisberg, N. M., Knote, C., Olson, K.,
Koss, A., Goldstein, A. H., Hering, S. V., de Gouw, J., Baumann, K., Lee,
S.-H., Nenes, A., Weber, R. J., and Ng, N. L.: Effects of anthropogenic
emissions on aerosol formation from isoprene and monoterpenes in the
southeastern United States, P. Natl. Acad. Sci. USA, 112, 37–42,
https://doi.org/10.1073/pnas.1417609112, 2015.
Xu, L., Guo, H., Weber, R. J., and Ng, N. L.: Chemical characterization of
water-soluble organic aerosol in contrasting rural and urban environments in
the southeastern United States, Environ. Sci. Technol., 51, 78–88, 2016.
Xu, L., Guo, H., Weber, R. J., and Ng, N. L.: Chemical Characterization of
Water-Soluble Organic Aerosol in Contrasting Rural and Urban Environments in
the Southeastern United States, Environ. Sci. Technol., 51, 78–88,
https://doi.org/10.1021/acs.est.6b05002, 2017a.
Xu, W., Han, T., Du, W., Wang, Q., Chen, C., Zhao, J., Zhang, Y., Li, J., Fu,
P., Wang, Z., Worsnop, D. R., and Sun, Y.: Effects of Aqueous-Phase and
Photochemical Processing on Secondary Organic Aerosol Formation and Evolution
in Beijing, China, Environ. Sci. Technol., 51, 762–770,
https://doi.org/10.1021/acs.est.6b04498, 2017b.
Ying, Q., Li, J., and Kota, S. H.: Significant Contributions of Isoprene to
Summertime Secondary Organic Aerosol in Eastern United States, Environ. Sci.
Technol., 49, 7834–7842, https://doi.org/10.1021/acs.est.5b02514, 2015.
Yu, K., Jacob, D. J., Fisher, J. A., Kim, P. S., Marais, E. A., Miller, C.
C., Travis, K. R., Zhu, L., Yantosca, R. M., Sulprizio, M. P., Cohen, R. C.,
Dibb, J. E., Fried, A., Mikoviny, T., Ryerson, T. B., Wennberg, P. O., and
Wisthaler, A.: Sensitivity to grid resolution in the ability of a chemical
transport model to simulate observed oxidant chemistry under high-isoprene
conditions, Atmos. Chem. Phys., 16, 4369–4378,
https://doi.org/10.5194/acp-16-4369-2016, 2016.
Zhang, X., Liu, Z., Hecobian, A., Zheng, M., Frank, N. H., Edgerton, E. S.,
and Weber, R. J.: Spatial and seasonal variations of fine particle
water-soluble organic carbon (WSOC) over the southeastern United States:
implications for secondary organic aerosol formation, Atmos. Chem. Phys., 12,
6593–6607, https://doi.org/10.5194/acp-12-6593-2012, 2012.
Zhang, Y. J., Tang, L. L., Sun, Y. L., Favez, O., Canonaco, F., Albinet, A.,
Couvidat, F., Liu, D. T., Jayne, J. T., Wang, Z., Croteau, P. L.,
Canagaratna, M. R., Zhou, H. C., Prevot, A. S. H., and Worsnop, D. R.:
Limited formation of isoprene epoxydiols-derived secondary organic aerosol
under NOx-rich environments in Eastern China, Geophys. Res. Lett., 44,
2035–2043, https://doi.org/10.1002/2016gl072368, 2017.
Short summary
We characterized the reversibility of aqSOA formed from isoprene at a location in the eastern United States. WSOCp evaporation with drying was observed systematically throughout the late spring and summer, indicating reversible aqSOA formation. The absolute reversible aqSOA concentrations, as well as the relative amount of reversible aqSOA, increased with decreasing NOx / isoprene ratios, suggesting that IEPOX or other low-NOx oxidation products were responsible for these effects.
We characterized the reversibility of aqSOA formed from isoprene at a location in the eastern...
Altmetrics
Final-revised paper
Preprint