196 citations as recorded by crossref.

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3. Mass spectrometry-based Aerosolomics: a new approach to resolve sources, composition, and partitioning of secondary organic aerosol M. Thoma et al. 10.5194/amt-15-7137-2022
4. H-shift and cyclization reactions in unsaturated alkylperoxy radicals near room temperature: propagating or terminating autoxidation? B. Nozière & L. Vereecken 10.1039/D4CP02718C
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9. Structural Diversity of Protonated Citric Acid-Ammonia Clusters and Its Atmospheric Implication S. Zhou et al. 10.1021/acs.jpca.3c05160
10. Effect of NO<sub><i>x</i></sub> on 1,3,5-trimethylbenzene (TMB) oxidation product distribution and particle formation E. Tsiligiannis et al. 10.5194/acp-19-15073-2019
11. Chemical ionization mass spectrometry: Developments and applications for on-line characterization of atmospheric aerosols and trace gases Y. Zhang et al. 10.1016/j.trac.2023.117353
12. Biotic stress: a significant contributor to organic aerosol in Europe? R. Bergström et al. 10.5194/acp-14-13643-2014
13. Schnelle Autoxidation bildet hochoxidierte RO2‐Radikale in der Atmosphäre T. Jokinen et al. 10.1002/ange.201408566
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17. Control of ozonolysis kinetics and aerosol yield by nuances in the molecular structure of volatile organic compounds R. Harvey & G. Petrucci 10.1016/j.atmosenv.2015.09.038
18. New particle formation in the fresh flue-gas plume from a coal-fired power plant: effect of flue-gas cleaning F. Mylläri et al. 10.5194/acp-16-7485-2016
19. Enhancement of atmospheric H<sub>2</sub>SO<sub>4</sub> / H<sub>2</sub>O nucleation: organic oxidation products versus amines T. Berndt et al. 10.5194/acp-14-751-2014
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23. Applications of environmental mass spectrometry in atmospheric haze chemistry T. Chen et al. 10.1016/j.trac.2024.117614
24. Molecular corridors and parameterizations of volatility in the chemical evolution of organic aerosols Y. Li et al. 10.5194/acp-16-3327-2016
25. Reactions of Atmospheric Particulate Stabilized Criegee Intermediates Lead to High-Molecular-Weight Aerosol Components M. Wang et al. 10.1021/acs.est.6b02114
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29. Measurement–model comparison of stabilized Criegee intermediate and highly oxygenated molecule production in the CLOUD chamber N. Sarnela et al. 10.5194/acp-18-2363-2018
30. Trends in stabilisation of Criegee intermediates from alkene ozonolysis M. Newland et al. 10.1039/D0CP00897D
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39. Formation of Low-Volatility Organic Compounds in the Atmosphere: Recent Advancements and Insights K. Barsanti et al. 10.1021/acs.jpclett.6b02969
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42. An Atmospheric Cluster Database Consisting of Sulfuric Acid, Bases, Organics, and Water J. Elm 10.1021/acsomega.9b00860
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44. Multiphase Chemistry at the Atmosphere–Biosphere Interface Influencing Climate and Public Health in the Anthropocene U. Pöschl & M. Shiraiwa 10.1021/cr500487s
45. A reference data set for validating vapor pressure measurement techniques: homologous series of polyethylene glycols U. Krieger et al. 10.5194/amt-11-49-2018
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48. A combined gas- and particle-phase analysis of highly oxygenated organic molecules (HOMs) from α-pinene ozonolysis J. Zhao et al. 10.5194/acp-23-3707-2023
49. Characterization of Highly Oxidized Molecules in Fresh and Aged Biogenic Secondary Organic Aerosol P. Tu et al. 10.1021/acs.analchem.6b00378
50. Modeling the formation and growth of atmospheric molecular clusters: A review J. Elm et al. 10.1016/j.jaerosci.2020.105621
51. Thermodynamics of oligomer formation: implications for secondary organic aerosol formation and reactivity J. DePalma et al. 10.1039/c3cp44586k
52. Changes in the new particle formation and shrinkage events of the atmospheric ions during the COVID-19 lockdown A. Kamra et al. 10.1016/j.uclim.2022.101214
53. Heterogeneous Ozonolysis of Endocyclic Unsaturated Organic Aerosol Proxies: Implications for Criegee Intermediate Dynamics and Later-Generation Reactions Z. Zhao et al. 10.1021/acsearthspacechem.8b00177
54. Investigation of the Cyclohexene Oxidation Mechanism Through the Direct Measurement of Organic Peroxy Radicals Y. Li et al. 10.1021/acs.est.4c06744
55. Evaluating the Applicability of a Real-Time Highly Oxygenated Organic Molecule (HOM)-Based Indicator for Ozone Formation Sensitivity at a Boreal Forest Station J. Zhang et al. 10.1021/acs.estlett.4c00733
56. Highly oxygenated organic molecules with high unsaturation formed upon photochemical aging of soot M. Li et al. 10.1016/j.chempr.2022.06.011
57. Synergistic effect of glutaric acid and ammonia/amine/amide on their hydrates in the clustering: A theoretical study S. Ni et al. 10.1016/j.chemosphere.2021.130063
58. Aerosol particle shrinkage event phenomenology in a South European suburban area during 2009–2015 E. Alonso-Blanco et al. 10.1016/j.atmosenv.2017.04.013
59. Aerosol Chemistry Resolved by Mass Spectrometry: Insights into Particle Growth after Ambient New Particle Formation A. Vogel et al. 10.1021/acs.est.6b01673
60. Gas-phase hydration of glyoxylic acid: Kinetics and atmospheric implications L. Liu et al. 10.1016/j.chemosphere.2017.08.007
61. Measurement report: Insights into the chemical composition and origin of molecular clusters and potential precursor molecules present in the free troposphere over the southern Indian Ocean: observations from the Maïdo Observatory (2150 m a.s.l., Réunion) R. Salignat et al. 10.5194/acp-24-3785-2024
62. Modeling the Detection of Organic and Inorganic Compounds Using Iodide-Based Chemical Ionization S. Iyer et al. 10.1021/acs.jpca.5b09837
63. Recent advances on SOA formation in indoor air, fate and strategies for SOA characterization in indoor air - A review K. Pytel et al. 10.1016/j.scitotenv.2022.156948
64. The role of low volatile organics on secondary organic aerosol formation H. Kokkola et al. 10.5194/acp-14-1689-2014
65. Composition of Ultrafine Particles in Urban Beijing: Measurement Using a Thermal Desorption Chemical Ionization Mass Spectrometer X. Li et al. 10.1021/acs.est.0c06053
66. Multiple new-particle growth pathways observed at the US DOE Southern Great Plains field site A. Hodshire et al. 10.5194/acp-16-9321-2016
67. Molecular Characterization of Atmospheric Organic Aerosol by Mass Spectrometry M. Johnston & D. Kerecman 10.1146/annurev-anchem-061516-045135
68. HOx and NOx production in oxidation flow reactors via photolysis of isopropyl nitrite, isopropyl nitrite-d7, and 1,3-propyl dinitrite at λ = 254, 350, and 369 nm A. Lambe et al. 10.5194/amt-12-299-2019
69. Controlled nitric oxide production via O(<sup>1</sup>D)  + N<sub>2</sub>O reactions for use in oxidation flow reactor studies A. Lambe et al. 10.5194/amt-10-2283-2017
70. Review of Smog Chamber Research Trends J. Kim et al. 10.5572/KOSAE.2023.39.5.866
71. Gas-Phase Ozonolysis of Cycloalkenes: Formation of Highly Oxidized RO2Radicals and Their Reactions with NO, NO2, SO2, and Other RO2Radicals T. Berndt et al. 10.1021/acs.jpca.5b07295
72. Direct Observations of Atmospheric Aerosol Nucleation M. Kulmala et al. 10.1126/science.1227385
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74. Source characterization of highly oxidized multifunctional compounds in a boreal forest environment using positive matrix factorization C. Yan et al. 10.5194/acp-16-12715-2016
75. On the fate of oxygenated organic molecules in atmospheric aerosol particles V. Pospisilova et al. 10.1126/sciadv.aax8922
76. Similarities in STXM-NEXAFS Spectra of Atmospheric Particles and Secondary Organic Aerosol Generated from Glyoxal, α-Pinene, Isoprene, 1,2,4-Trimethylbenzene, and d-Limonene K. Shakya et al. 10.1080/02786826.2013.772950
77. The role of highly oxygenated molecules (HOMs) in determining the composition of ambient ions in the boreal forest F. Bianchi et al. 10.5194/acp-17-13819-2017
78. Characterisation of the Manchester Aerosol Chamber facility Y. Shao et al. 10.5194/amt-15-539-2022
79. Large differences of highly oxygenated organic molecules (HOMs) and low-volatile species in secondary organic aerosols (SOAs) formed from ozonolysis of β-pinene and limonene D. Liu et al. 10.5194/acp-23-8383-2023
80. Vertical characterization of highly oxygenated molecules (HOMs) below and above a boreal forest canopy Q. Zha et al. 10.5194/acp-18-17437-2018
81. Formation of Highly Oxidized Organic Compounds and Secondary Organic Aerosol from α-Thujene Ozonolysis M. Dam et al. 10.1021/acs.jpca.3c02584
82. Superoxide Formation from Aqueous Reactions of Biogenic Secondary Organic Aerosols J. Wei et al. 10.1021/acs.est.0c07789
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85. Undetected biogenic volatile organic compounds from Norway spruce drive total ozone reactivity measurements S. Thomas et al. 10.5194/acp-23-14627-2023
86. Aerosol mass yields of selected biogenic volatile organic compounds – a theoretical study with nearly explicit gas-phase chemistry C. Xavier et al. 10.5194/acp-19-13741-2019
87. <i>α</i>-Pinene secondary organic aerosol at low temperature: chemical composition and implications for particle viscosity W. Huang et al. 10.5194/acp-18-2883-2018
88. Recent advances in understanding secondary organic aerosol: Implications for global climate forcing M. Shrivastava et al. 10.1002/2016RG000540
89. Probing surfaces of atmospherically relevant organic particles by easy ambient sonic-spray ionization mass spectrometry (EASI-MS) L. Wingen & B. Finlayson-Pitts 10.1039/C8SC03851A
90. Vertically resolved concentration and liquid water content of atmospheric nanoparticles at the US DOE Southern Great Plains site H. Chen et al. 10.5194/acp-18-311-2018
91. Highly functionalized organic nitrates in the southeast United States: Contribution to secondary organic aerosol and reactive nitrogen budgets B. Lee et al. 10.1073/pnas.1508108113
92. Rapid Autoxidation Forms Highly Oxidized RO2 Radicals in the Atmosphere T. Jokinen et al. 10.1002/anie.201408566
93. Chemical identification of new particle formation and growth precursors through positive matrix factorization of ambient ion measurements D. Katz et al. 10.5194/acp-23-5567-2023
94. What Is Required for Highly Oxidized Molecules To Form Clusters with Sulfuric Acid? J. Elm et al. 10.1021/acs.jpca.7b03759
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99. New insights into secondary organic aerosol from the ozonolysis of α-pinene from combined infrared spectroscopy and mass spectrometry measurements C. Kidd et al. 10.1039/C4CP03405H
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103. Nanoparticle growth by particle-phase chemistry M. Apsokardu & M. Johnston 10.5194/acp-18-1895-2018
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