346 citations as recorded by crossref.

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8. Measurement report: Long-range transport and the fate of dimethyl sulfide oxidation products in the free troposphere derived from observations at the high-altitude research station Chacaltaya (5240 m a.s.l.) in the Bolivian Andes W. Scholz et al. 10.5194/acp-23-895-2023
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10. An Atmospheric Cluster Database Consisting of Sulfuric Acid, Bases, Organics, and Water J. Elm 10.1021/acsomega.9b00860
11. Peroxy radical kinetics and new particle formation M. Schervish & N. Donahue 10.1039/D0EA00017E
12. CI-Orbitrap: An Analytical Instrument To Study Atmospheric Reactive Organic Species M. Riva et al. 10.1021/acs.analchem.9b02093
13. Effect of temperature on the formation of highly oxygenated organic molecules (HOMs) from alpha-pinene ozonolysis L. Quéléver et al. 10.5194/acp-19-7609-2019
14. Organic aerosol formation from 222 nm germicidal light: ozone-initiated vs. non-ozone pathways M. Goss & J. Kroll 10.1039/D4EM00384E
15. Inversely modeling homogeneous H<sub>2</sub>SO<sub>4</sub> − H<sub>2</sub>O nucleation rate in exhaust-related conditions M. Olin et al. 10.5194/acp-19-6367-2019
16. Evaluating the performance of five different chemical ionization techniques for detecting gaseous oxygenated organic species M. Riva et al. 10.5194/amt-12-2403-2019
17. Evolution of organic carbon during COVID-19 lockdown period: Possible contribution of nocturnal chemistry Z. Feng et al. 10.1016/j.scitotenv.2021.152191
18. Production of extremely low volatile organic compounds from biogenic emissions: Measured yields and atmospheric implications T. Jokinen et al. 10.1073/pnas.1423977112
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20. Highly oxygenated organic molecules produced by the oxidation of benzene and toluene in a wide range of OH exposure and NO<sub><i>x</i></sub> conditions X. Cheng et al. 10.5194/acp-21-12005-2021
21. Airborne flux measurements of ammonia over the southern Great Plains using chemical ionization mass spectrometry S. Schobesberger et al. 10.5194/amt-16-247-2023
22. Chemistry of Atmospheric Nucleation: On the Recent Advances on Precursor Characterization and Atmospheric Cluster Composition in Connection with Atmospheric New Particle Formation M. Kulmala et al. 10.1146/annurev-physchem-040412-110014
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24. A modelling study of OH, NO3 and H2SO4 in 2007–2018 at SMEAR II, Finland: analysis of long-term trends D. Chen et al. 10.1039/D1EA00020A
25. Chemical evolution of atmospheric organic carbon over multiple generations of oxidation G. Isaacman-VanWertz et al. 10.1038/s41557-018-0002-2
26. Molecular insights into new particle formation in Barcelona, Spain J. Brean et al. 10.5194/acp-20-10029-2020
27. Hydration of acetic acid-dimethylamine complex and its atmospheric implications J. Li et al. 10.1016/j.atmosenv.2019.117005
28. 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
29. Ion-induced nucleation of pure biogenic particles J. Kirkby et al. 10.1038/nature17953
30. Enhanced Aerosol Source Identification by Utilizing High Molecular Weight Signals in Aerosol Mass Spectra Y. Zhang et al. 10.1021/acsestair.3c00102
31. Measurement Report: Wintertime new particle formation in the rural area of the North China Plain – influencing factors and possible formation mechanism J. Hong et al. 10.5194/acp-23-5699-2023
32. Formation of highly oxygenated organic molecules from chlorine-atom-initiated oxidation of alpha-pinene Y. Wang et al. 10.5194/acp-20-5145-2020
33. Gas‐Phase Formation of Sulfurous Acid (H2SO3) in the Atmosphere T. Berndt et al. 10.1002/anie.202405572
34. Measurement of ammonia, amines and iodine compounds using protonated water cluster chemical ionization mass spectrometry J. Pfeifer et al. 10.5194/amt-13-2501-2020
35. Capability of CI-Orbitrap for Gas-Phase Analysis in Atmospheric Chemistry: A Comparison with the CI-APi-TOF Technique M. Riva et al. 10.1021/acs.analchem.0c00111
36. Novel insights on new particle formation derived from a pan-european observing system M. Dall’Osto et al. 10.1038/s41598-017-17343-9
37. A cluster-of-functional-groups approach for studying organic enhanced atmospheric cluster formation A. Pedersen et al. 10.5194/ar-2-123-2024
38. Applications of environmental mass spectrometry in atmospheric haze chemistry T. Chen et al. 10.1016/j.trac.2024.117614
39. Sources of Gas-Phase Species in an Art Museum from Comprehensive Real-Time Measurements D. Price et al. 10.1021/acsearthspacechem.1c00229
40. Reactivity of stabilized Criegee intermediates (sCIs) from isoprene and monoterpene ozonolysis toward SO<sub>2</sub> and organic acids M. Sipilä et al. 10.5194/acp-14-12143-2014
41. Terpene emissions from boreal wetlands can initiate stronger atmospheric new particle formation than boreal forests H. Junninen et al. 10.1038/s43247-022-00406-9
42. Using collision-induced dissociation to constrain sensitivity of ammonia chemical ionization mass spectrometry (NH<sub>4</sub><sup>+</sup> CIMS) to oxygenated volatile organic compounds A. Zaytsev et al. 10.5194/amt-12-1861-2019
43. The Silk Road agenda of the Pan-Eurasian Experiment (PEEX) program H. Lappalainen et al. 10.1080/20964471.2018.1437704
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45. Efficient alkane oxidation under combustion engine and atmospheric conditions Z. Wang et al. 10.1038/s42004-020-00445-3
46. Measurement of atmospheric nanoparticles: Bridging the gap between gas-phase molecules and larger particles C. Peng et al. 10.1016/j.jes.2022.03.006
47. 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
48. Review of online measurement techniques for chemical composition of atmospheric clusters and sub-20 nm particles K. Zhang et al. 10.3389/fenvs.2022.937006
49. A central arctic extreme aerosol event triggered by a warm air-mass intrusion L. Dada et al. 10.1038/s41467-022-32872-2
50. Labile Peroxides in Secondary Organic Aerosol M. Krapf et al. 10.1016/j.chempr.2016.09.007
51. Schnelle Autoxidation bildet hochoxidierte RO2‐Radikale in der Atmosphäre T. Jokinen et al. 10.1002/ange.201408566
52. Chemical composition of different size ultrafine particulate matter measured by nanoparticle chemical ionization mass spectrometer W. Wang et al. 10.1016/j.jes.2021.09.036
53. Fragmentation inside proton-transfer-reaction-based mass spectrometers limits the detection of ROOR and ROOH peroxides H. Li et al. 10.5194/amt-15-1811-2022
54. Insights into the Chemistry of Iodine New Particle Formation: The Role of Iodine Oxides and the Source of Iodic Acid J. Gómez Martín et al. 10.1021/jacs.1c12957
55. Trimethylamine Outruns Terpenes and Aromatics in Atmospheric Autoxidation T. Berndt et al. 10.1021/acs.jpca.1c02465
56. Tutorial: Dynamic organic growth modeling with a volatility basis set D. Stolzenburg et al. 10.1016/j.jaerosci.2022.106063
57. Online measurements of water-soluble organic acids in the gas and aerosol phase from the photooxidation of 1,3,5-trimethylbenzene A. Praplan et al. 10.5194/acp-14-8665-2014
58. A theoretical study of temperature dependence of cluster formation from sulfuric acid and ammonia N. Chon et al. 10.1016/j.chemphys.2014.01.010
59. 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
60. Massive Assessment of the Geometries of Atmospheric Molecular Clusters A. Jensen & J. Elm 10.1021/acs.jctc.4c01046
61. Advances on Atmospheric Oxidation Mechanism of Typical Aromatic Hydrocarbons M. Song et al. 10.6023/A21050224
62. Rapid mass growth and enhanced light extinction of atmospheric aerosols during the heating season haze episodes in Beijing revealed by aerosol–chemistry–radiation–boundary layer interaction Z. Lin et al. 10.5194/acp-21-12173-2021
63. Size-resolved online chemical analysis of nanoaerosol particles: a thermal desorption differential mobility analyzer coupled to a chemical ionization time-of-flight mass spectrometer A. Wagner et al. 10.5194/amt-11-5489-2018
64. Direct measurements of semi-volatile organic compound dynamics show near-unity mass accommodation coefficients for diverse aerosols X. Liu et al. 10.1038/s42004-019-0200-x
65. Increased ionization supports growth of aerosols into cloud condensation nuclei H. Svensmark et al. 10.1038/s41467-017-02082-2
66. A review of microbial and chemical assessment of indoor surfaces V. Mihucz et al. 10.1080/05704928.2021.1995870
67. BAECC: A Field Campaign to Elucidate the Impact of Biogenic Aerosols on Clouds and Climate T. Petäjä et al. 10.1175/BAMS-D-14-00199.1
68. Detection of gaseous species during KCl‐induced high‐temperature corrosion by the means of CPFAAS and CI‐APi‐TOF J. Lehmusto et al. 10.1002/maco.201910964
69. Seasonal Characteristics of New Particle Formation and Growth in Urban Beijing C. Deng et al. 10.1021/acs.est.0c00808
70. Atmospheric pressure thermal desorption chemical ionization mass spectrometry for ultra-sensitive explosive detection J. Kangasluoma et al. 10.1016/j.talanta.2022.123653
71. Elucidating the mechanisms of atmospheric new particle formation in the highly polluted Po Valley, Italy J. Cai et al. 10.5194/acp-24-2423-2024
72. Benchmarking Ab Initio Binding Energies of Hydrogen-Bonded Molecular Clusters Based on FTIR Spectroscopy N. Bork et al. 10.1021/jp5037537
73. Major contribution of neutral clusters to new particle formation at the interface between the boundary layer and the free troposphere C. Rose et al. 10.5194/acp-15-3413-2015
74. Atmospheric Sulfuric Acid Dimer Formation in a Polluted Environment K. Yin et al. 10.3390/ijerph19116848
75. Formation of highly oxygenated organic molecules from aromatic compounds U. Molteni et al. 10.5194/acp-18-1909-2018
76. Multi-generation OH oxidation as a source for highly oxygenated organic molecules from aromatics O. Garmash et al. 10.5194/acp-20-515-2020
77. Establishing the structural motifs present in small ammonium and aminium bisulfate clusters of relevance to atmospheric new particle formation J. Kreinbihl et al. 10.1063/5.0015094
78. 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
79. Atmospheric clusters to nanoparticles: Recent progress and challenges in closing the gap in chemical composition J. Smith et al. 10.1016/j.jaerosci.2020.105733
80. Responses of gaseous sulfuric acid and particulate sulfate to reduced SO2 concentration: A perspective from long-term measurements in Beijing X. Li et al. 10.1016/j.scitotenv.2020.137700
81. Machine Learning Reveals the Parameters Affecting the Gaseous Sulfuric Acid Distribution in a Coastal City: Model Construction and Interpretation C. Yang et al. 10.1021/acs.estlett.3c00170
82. Quantification of Gas-Wall Partitioning in Teflon Environmental Chambers Using Rapid Bursts of Low-Volatility Oxidized Species Generated in Situ J. Krechmer et al. 10.1021/acs.est.6b00606
83. Highly oxygenated organic molecule cluster decomposition in atmospheric pressure interface time-of-flight mass spectrometers T. Zanca et al. 10.5194/amt-13-3581-2020
84. Investigation of the Cyclohexene Oxidation Mechanism Through the Direct Measurement of Organic Peroxy Radicals Y. Li et al. 10.1021/acs.est.4c06744
85. Isoprene nitrates drive new particle formation in Amazon’s upper troposphere J. Curtius et al. 10.1038/s41586-024-08192-4
86. 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
87. Peroxy Radical Processes and Product Formation in the OH Radical-Initiated Oxidation of α-Pinene for Near-Atmospheric Conditions T. Berndt 10.1021/acs.jpca.1c05576
88. Role of Gas-Phase Halogen Bonding in Ambient Chemical Ionization Mass Spectrometry Utilizing Iodine J. Ganske et al. 10.1021/acsearthspacechem.9b00030
89. Modeling the formation and growth of atmospheric molecular clusters: A review J. Elm et al. 10.1016/j.jaerosci.2020.105621
90. Characterisation of gaseous iodine species detection using the multi-scheme chemical ionisation inlet 2 with bromide and nitrate chemical ionisation methods X. He et al. 10.5194/amt-16-4461-2023
91. Statistical precision of the intensities retrieved from constrained fitting of overlapping peaks in high-resolution mass spectra M. Cubison & J. Jimenez 10.5194/amt-8-2333-2015
92. Long-term observation of air pollution-weather/climate interactions at the SORPES station: a review and outlook A. Ding et al. 10.1007/s11783-016-0877-3
93. The role of low-volatility organic compounds in initial particle growth in the atmosphere J. Tröstl et al. 10.1038/nature18271
94. Modeling on Fragmentation of Clusters inside a Mass Spectrometer E. Zapadinsky et al. 10.1021/acs.jpca.8b10744
95. Studies on the Conformation, Thermodynamics, and Evaporation Rate Characteristics of Sulfuric Acid and Amines Molecular Clusters Jiao Chen1 J. Chen 10.2139/ssrn.4122791
96. Large Gas-Phase Source of Esters and Other Accretion Products in the Atmosphere O. Peräkylä et al. 10.1021/jacs.2c10398
97. On the potential use of highly oxygenated organic molecules (HOMs) as indicators for ozone formation sensitivity J. Zhang et al. 10.5194/acp-24-2885-2024
98. Vertical characterization of highly oxygenated molecules (HOMs) below and above a boreal forest canopy Q. Zha et al. 10.5194/acp-18-17437-2018
99. Constraining the sensitivity of iodide adduct chemical ionization mass spectrometry to multifunctional organic molecules using the collision limit and thermodynamic stability of iodide ion adducts F. Lopez-Hilfiker et al. 10.5194/amt-9-1505-2016
100. Long-term measurement of sub-3 nm particles and their precursor gases in the boreal forest J. Sulo et al. 10.5194/acp-21-695-2021
101. A study on the fragmentation of sulfuric acid and dimethylamine clusters inside an atmospheric pressure interface time-of-flight mass spectrometer D. Alfaouri et al. 10.5194/amt-15-11-2022
102. High-frequency gaseous and particulate chemical characterization using extractive electrospray ionization mass spectrometry (Dual-Phase-EESI-TOF) C. Lee et al. 10.5194/amt-15-3747-2022
103. A dynamic parameterization of sulfuric acid–dimethylamine nucleation and its application in three-dimensional modeling Y. Li et al. 10.5194/acp-23-8789-2023
104. Orbitool: a software tool for analyzing online Orbitrap mass spectrometry data R. Cai et al. 10.5194/amt-14-2377-2021
105. Unexpected significance of a minor reaction pathway in daytime formation of biogenic highly oxygenated organic compounds H. Shen et al. 10.1126/sciadv.abp8702
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107. Selective deuteration as a tool for resolving autoxidation mechanisms in α-pinene ozonolysis M. Meder et al. 10.5194/acp-23-4373-2023
108. Assessment of the DLPNO Binding Energies of Strongly Noncovalent Bonded Atmospheric Molecular Clusters G. Schmitz & J. Elm 10.1021/acsomega.0c00436
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114. 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
115. Direct Observations of Atmospheric Aerosol Nucleation M. Kulmala et al. 10.1126/science.1227385
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118. Molecular Characterization of Atmospheric Organic Aerosol by Mass Spectrometry M. Johnston & D. Kerecman 10.1146/annurev-anchem-061516-045135
119. New particle formation in the volcanic eruption plume of the Piton de la Fournaise: specific features from a long-term dataset C. Rose et al. 10.5194/acp-19-13243-2019
120. Observations of highly oxidized molecules and particle nucleation in the atmosphere of Beijing J. Brean et al. 10.5194/acp-19-14933-2019
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128. Simultaneous Detection of Alkylamines in the Surface Ocean and Atmosphere of the Antarctic Sympagic Environment M. Dall’Osto et al. 10.1021/acsearthspacechem.9b00028
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151. Molecular Composition of Anthropogenic Oxygenated Organic Molecules and Their Contribution to Organic Aerosol in a Coastal City C. Yang et al. 10.1021/acs.est.3c03244
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178. Using advanced mass spectrometry techniques to fully characterize atmospheric organic carbon: current capabilities and remaining gaps G. Isaacman-VanWertz et al. 10.1039/C7FD00021A
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180. Oxidation product characterization from ozonolysis of the diterpene <i>ent</i>-kaurene Y. Luo et al. 10.5194/acp-22-5619-2022
181. The role of H<sub>2</sub>SO<sub>4</sub>-NH<sub>3</sub> anion clusters in ion-induced aerosol nucleation mechanisms in the boreal forest C. Yan et al. 10.5194/acp-18-13231-2018
182. The Pivotal Role of Heavy Terpenes and Anthropogenic Interactions in New Particle Formation on the Southeastern Qinghai-Tibet Plateau Y. Liu et al. 10.1021/acs.est.4c04112
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185. Clustering, methodology, and mechanistic insights into acetate chemical ionization using high-resolution time-of-flight mass spectrometry P. Brophy & D. Farmer 10.5194/amt-9-3969-2016
186. Insights into atmospheric oxidation processes by performing factor analyses on subranges of mass spectra Y. Zhang et al. 10.5194/acp-20-5945-2020
187. Enhanced growth rate of atmospheric particles from sulfuric acid D. Stolzenburg et al. 10.5194/acp-20-7359-2020
188. An overlooked oxidation mechanism of toluene: computational predictions and experimental validations Z. Fu et al. 10.1039/D3SC03638C
189. The effect of temperature and relative humidity on secondary organic aerosol formation from ozonolysis of Δ3-carene D. Thomsen et al. 10.1039/D3EA00128H
190. Interaction of oxalic acid with methylamine and its atmospheric implications Y. Hong et al. 10.1039/C7RA13670F
191. Peroxy Radical and Product Formation in the Gas-Phase Ozonolysis of α-Pinene under Near-Atmospheric Conditions: Occurrence of an Additional Series of Peroxy Radicals O,O–C10H15O(O2)yO2 with y = 1–3 T. Berndt 10.1021/acs.jpca.2c05094
192. Modeling the Charging of Highly Oxidized Cyclohexene Ozonolysis Products Using Nitrate-Based Chemical Ionization N. Hyttinen et al. 10.1021/acs.jpca.5b01818
193. Diurnal evolution of negative atmospheric ions above the boreal forest: from ground level to the free troposphere L. Beck et al. 10.5194/acp-22-8547-2022
194. Acid–base chemical reaction model for nucleation rates in the polluted atmospheric boundary layer M. Chen et al. 10.1073/pnas.1210285109
195. Gas-Phase Oxidation of Atmospherically Relevant Unsaturated Hydrocarbons by Acyl Peroxy Radicals D. Pasik et al. 10.1021/jacs.4c02523
196. Iodine oxoacids enhance nucleation of sulfuric acid particles in the atmosphere X. He et al. 10.1126/science.adh2526
197. Insights into the molecular composition of semi-volatile aerosols in the summertime central Arctic Ocean using FIGAERO-CIMS K. Siegel et al. 10.1039/D0EA00023J
198. Time-Resolved Measurements of Indoor Chemical Emissions, Deposition, and Reactions in a University Art Museum D. Pagonis et al. 10.1021/acs.est.9b00276
199. Reparameterization of GFN1-xTB for atmospheric molecular clusters: applications to multi-acid–multi-base systems Y. Knattrup et al. 10.1039/D4RA03021D
200. Formation of Highly Oxidized Radicals and Multifunctional Products from the Atmospheric Oxidation of Alkylbenzenes S. Wang et al. 10.1021/acs.est.7b02374
201. Laser Ablation-Aerosol Mass Spectrometry-Chemical Ionization Mass Spectrometry for Ambient Surface Imaging J. Berry et al. 10.1021/acs.analchem.7b05255
202. Highly Oxidized Second-Generation Products from the Gas-Phase Reaction of OH Radicals with Isoprene T. Berndt et al. 10.1021/acs.jpca.6b10987
203. Enhanced detection of aromatic oxidation products using NO3− chemical ionization mass spectrometry with limited nitric acid O. Garmash et al. 10.1039/D4EA00087K
204. Potential pre-industrial–like new particle formation induced by pure biogenic organic vapors in Finnish peatland W. Huang et al. 10.1126/sciadv.adm9191
205. Determination of secondary organic aerosol in particulate matter – Short review J. Klyta & M. Czaplicka 10.1016/j.microc.2020.104997
206. The Synergistic Role of Sulfuric Acid, Bases, and Oxidized Organics Governing New‐Particle Formation in Beijing C. Yan et al. 10.1029/2020GL091944
207. Impact of NO<sub><i>x</i></sub> on secondary organic aerosol (SOA) formation from <i>α</i>-pinene and <i>β</i>-pinene photooxidation: the role of highly oxygenated organic nitrates I. Pullinen et al. 10.5194/acp-20-10125-2020
208. Gas-Phase Ozonolysis of Selected Olefins: The Yield of Stabilized Criegee Intermediate and the Reactivity toward SO2 T. Berndt et al. 10.1021/jz301158u
209. Real-time detection of highly oxidized organosulfates and BSOA marker compounds during the F-BEACh 2014 field study M. Brüggemann et al. 10.5194/acp-17-1453-2017
210. Highly Oxygenated Organic Molecules (HOM) from Gas-Phase Autoxidation Involving Peroxy Radicals: A Key Contributor to Atmospheric Aerosol F. Bianchi et al. 10.1021/acs.chemrev.8b00395
211. Substantial contribution of iodine to Arctic ozone destruction N. Benavent et al. 10.1038/s41561-022-01018-w
212. How well can we predict cluster fragmentation inside a mass spectrometer? M. Passananti et al. 10.1039/C9CC02896J
213. Modeling the Detection of Organic and Inorganic Compounds Using Iodide-Based Chemical Ionization S. Iyer et al. 10.1021/acs.jpca.5b09837
214. Electrospray Ionization–Based Synthesis and Validation of Amine-Sulfuric Acid Clusters of Relevance to Atmospheric New Particle Formation S. Waller et al. 10.1007/s13361-019-02322-3
215. The synergistic role of sulfuric acid, ammonia and organics in particle formation over an agricultural land L. Dada et al. 10.1039/D3EA00065F
216. Sub-3 nm particle size and composition dependent response of a nano-CPC battery J. Kangasluoma et al. 10.5194/amt-7-689-2014
217. Ambient Measurements of Highly Oxidized Gas-Phase Molecules during the Southern Oxidant and Aerosol Study (SOAS) 2013 P. Massoli et al. 10.1021/acsearthspacechem.8b00028
218. The annual cycle and sources of relevant aerosol precursor vapors in the central Arctic during the MOSAiC expedition M. Boyer et al. 10.5194/acp-24-12595-2024
219. Thermodynamics of the formation of sulfuric acid dimers in the binary (H<sub>2</sub>SO<sub>4</sub>–H<sub>2</sub>O) and ternary (H<sub>2</sub>SO<sub>4</sub>–H<sub>2</sub>O–NH<sub>3</sub>) system A. Kürten et al. 10.5194/acp-15-10701-2015
220. Indirect radiative forcing by ion-mediated nucleation of aerosol F. Yu et al. 10.5194/acp-12-11451-2012
221. Measurement of the charging state of 4–70 nm aerosols M. Enghoff & J. Svensmark 10.1016/j.jaerosci.2017.08.009
222. Ion-induced sulfuric acid–ammonia nucleation drives particle formation in coastal Antarctica T. Jokinen et al. 10.1126/sciadv.aat9744
223. Large contribution to secondary organic aerosol from isoprene cloud chemistry H. Lamkaddam et al. 10.1126/sciadv.abe2952
224. Observed in-plume gaseous elemental mercury depletion suggests significant mercury scavenging by volcanic aerosols A. Koenig et al. 10.1039/D3EA00063J
225. On the relation between apparent ion and total particle growth rates in the boreal forest and related chamber experiments L. Gonzalez Carracedo et al. 10.5194/acp-22-13153-2022
226. 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
227. Continuous and comprehensive atmospheric observations in Beijing: a station to understand the complex urban atmospheric environment Y. Liu et al. 10.1080/20964471.2020.1798707
228. Effects of Chemical Complexity on the Autoxidation Mechanisms of Endocyclic Alkene Ozonolysis Products: From Methylcyclohexenes toward Understanding α-Pinene M. Rissanen et al. 10.1021/jp510966g
229. Formation of condensable organic vapors from anthropogenic and biogenic volatile organic compounds (VOCs) is strongly perturbed by NO<sub><i>x</i></sub> in eastern China Y. Liu et al. 10.5194/acp-21-14789-2021
230. Observations and Modeling of Gaseous Nitrated Phenols in Urban Beijing: Insights From Seasonal Comparison and Budget Analysis M. Xia et al. 10.1029/2023JD039551
231. Measurement report: The influence of traffic and new particle formation on the size distribution of 1–800 nm particles in Helsinki – a street canyon and an urban background station comparison M. Okuljar et al. 10.5194/acp-21-9931-2021
232. The Aarhus Chamber Campaign on Highly Oxygenated Organic Molecules and Aerosols (ACCHA): particle formation, organic acids, and dimer esters from <i>α</i>-pinene ozonolysis at different temperatures K. Kristensen et al. 10.5194/acp-20-12549-2020
233. Sulfuric acid–amine nucleation in urban Beijing R. Cai et al. 10.5194/acp-21-2457-2021
234. An Automated and Extremely Sensitive Instrument for Non-Contact Screening of Luggage for Trace Illicit Substances J. Kangasluoma et al. 10.2139/ssrn.4098786
235. A nitrate ion chemical-ionization atmospheric-pressure-interface time-of-flight mass spectrometer (NO3− ToFCIMS) sensitivity study S. Alage et al. 10.5194/amt-17-4709-2024
236. CIMS Sulfuric Acid Detection Efficiency Enhanced by Amines Due to Higher Dipole Moments: A Computational Study O. Kupiainen-Määttä et al. 10.1021/jp4049764
237. Ion mobility spectrometry–mass spectrometry (IMS–MS) for on- and offline analysis of atmospheric gas and aerosol species J. Krechmer et al. 10.5194/amt-9-3245-2016
238. Atmospheric nanoparticle growth D. Stolzenburg et al. 10.1103/RevModPhys.95.045002
239. Atmospheric new particle formation in India: Current understanding and knowledge gaps V. Kanawade et al. 10.1016/j.atmosenv.2021.118894
240. Investigation of new particle formation mechanisms and aerosol processes at Marambio Station, Antarctic Peninsula L. Quéléver et al. 10.5194/acp-22-8417-2022
241. Revealing the sources and sinks of negative cluster ions in an urban environment through quantitative analysis R. Yin et al. 10.5194/acp-23-5279-2023
242. Production of neutral molecular clusters by controlled neutralization of mobility standards G. Steiner et al. 10.1080/02786826.2017.1328103
243. New Particle Formation and Growth Mechanisms in Highly Polluted Environments H. Yu et al. 10.1007/s40726-017-0067-3
244. Unprecedented Ambient Sulfur Trioxide (SO3) Detection: Possible Formation Mechanism and Atmospheric Implications L. Yao et al. 10.1021/acs.estlett.0c00615
245. Combined effects of boundary layer dynamics and atmospheric chemistry on aerosol composition during new particle formation periods L. Hao et al. 10.5194/acp-18-17705-2018
246. Exploring condensable organic vapors and their co-occurrence with PM2.5and O3in winter in Eastern China Y. Liu et al. 10.1039/D2EA00143H
247. Measurement report: Molecular-level investigation of atmospheric cluster ions at the tropical high-altitude research station Chacaltaya (5240 m a.s.l.) in the Bolivian Andes Q. Zha et al. 10.5194/acp-23-4559-2023
248. Field Evidence of Nocturnal Multiphase Production of Iodic Acid D. Li et al. 10.1021/acs.estlett.4c00244
249. Comparison of Gaseous and Particulate Highly Oxygenated Organic Molecules from the Ozonolysis of Terpenes J. Zhao et al. 10.1021/acsestair.4c00121
250. Recent advances in mass spectrometry techniques for atmospheric chemistry research on molecular‐level W. Zhang et al. 10.1002/mas.21857
251. Phase partitioning and volatility of secondary organic aerosol components formed from α-pinene ozonolysis and OH oxidation: the importance of accretion products and other low volatility compounds F. Lopez-Hilfiker et al. 10.5194/acp-15-7765-2015
252. Atmospheric gas-to-particle conversion: why NPF events are observed in megacities? M. Kulmala et al. 10.1039/C6FD00257A
253. Molecular understanding of new-particle formation from α-pinene between −50 and +25 °C M. Simon et al. 10.5194/acp-20-9183-2020
254. How the understanding of atmospheric new particle formation has evolved along with the development of measurement and analysis methods K. Lehtipalo et al. 10.1016/j.jaerosci.2024.106494
255. Toward Modeling the Growth of Large Atmospheric Sulfuric Acid–Ammonia Clusters M. Engsvang et al. 10.1021/acsomega.3c03521
256. Sulfuric acid in the Amazon basin: measurements and evaluation of existing sulfuric acid proxies D. Myers et al. 10.5194/acp-22-10061-2022
257. Correcting bias in log-linear instrument calibrations in the context of chemical ionization mass spectrometry C. Bi et al. 10.5194/amt-14-6551-2021
258. Contribution of Atmospheric Oxygenated Organic Compounds to Particle Growth in an Urban Environment X. Qiao et al. 10.1021/acs.est.1c02095
259. Oxygenated organic molecules produced by low-NOx photooxidation of aromatic compounds: contributions to secondary organic aerosol and steric hindrance X. Cheng et al. 10.5194/acp-24-2099-2024
260. Relative humidity effect on the formation of highly oxidized molecules and new particles during monoterpene oxidation X. Li et al. 10.5194/acp-19-1555-2019
261. Hydroxyl radical-induced formation of highly oxidized organic compounds T. Berndt et al. 10.1038/ncomms13677
262. Improved Configurational Sampling Protocol for Large Atmospheric Molecular Clusters H. Wu et al. 10.1021/acsomega.3c06794
263. Highly Oxygenated Molecules from Atmospheric Autoxidation of Hydrocarbons: A Prominent Challenge for Chemical Kinetics Studies M. Ehn et al. 10.1002/kin.21130
264. A large source of low-volatility secondary organic aerosol M. Ehn et al. 10.1038/nature13032
265. Field Detection of Highly Oxygenated Organic Molecules in Shanghai by Chemical Ionization–Orbitrap Y. Zhang et al. 10.1021/acs.est.1c08346
266. Multicomponent new particle formation from sulfuric acid, ammonia, and biogenic vapors K. Lehtipalo et al. 10.1126/sciadv.aau5363
267. New Particle Formation in the Atmosphere: From Molecular Clusters to Global Climate S. Lee et al. 10.1029/2018JD029356
268. Atmospheric new particle formation from sulfuric acid and amines in a Chinese megacity L. Yao et al. 10.1126/science.aao4839
269. NO at low concentration can enhance the formation of highly oxygenated biogenic molecules in the atmosphere W. Nie et al. 10.1038/s41467-023-39066-4
270. Computational Comparison of Acetate and Nitrate Chemical Ionization of Highly Oxidized Cyclohexene Ozonolysis Intermediates and Products N. Hyttinen et al. 10.1021/acs.jpca.6b12654
271. Performance of a new coaxial ion–molecule reaction region for low-pressure chemical ionization mass spectrometry with reduced instrument wall interactions B. Palm et al. 10.5194/amt-12-5829-2019
272. Quantum chemical modeling of atmospheric molecular clusters involving inorganic acids and methanesulfonic acid M. Engsvang et al. 10.1063/5.0152517
273. Observation of new particle formation and measurement of sulfuric acid, ammonia, amines and highly oxidized organic molecules at a rural site in central Germany A. Kürten et al. 10.5194/acp-16-12793-2016
274. Analysis of atmospheric particle growth based on vapor concentrations measured at the high-altitude GAW station Chacaltaya in the Bolivian Andes A. Heitto et al. 10.5194/acp-24-1315-2024
275. Scanning supersaturation condensation particle counter applied as a nano-CCN counter for size-resolved analysis of the hygroscopicity and chemical composition of nanoparticles Z. Wang et al. 10.5194/amt-8-2161-2015
276. Rapid growth of new atmospheric particles by nitric acid and ammonia condensation M. Wang et al. 10.1038/s41586-020-2270-4
277. Investigation of several proxies to estimate sulfuric acid concentration under volcanic plume conditions C. Rose et al. 10.5194/acp-21-4541-2021
278. Experimental study of H<sub>2</sub>SO<sub>4</sub> aerosol nucleation at high ionization levels M. Tomicic et al. 10.5194/acp-18-5921-2018
279. Understanding vapor nucleation on the molecular level: A review C. Li & R. Signorell 10.1016/j.jaerosci.2020.105676
280. Size-dependent influence of NO x on the growth rates of organic aerosol particles C. Yan et al. 10.1126/sciadv.aay4945
281. New particle formation induced by anthropogenic–biogenic interactions on the southeastern Tibetan Plateau S. Lai et al. 10.5194/acp-24-2535-2024
282. Rapid growth of organic aerosol nanoparticles over a wide tropospheric temperature range D. Stolzenburg et al. 10.1073/pnas.1807604115
283. Formation of highly oxidized multifunctional compounds: autoxidation of peroxy radicals formed in the ozonolysis of alkenes – deduced from structure–product relationships T. Mentel et al. 10.5194/acp-15-6745-2015
284. Uptake of Semivolatile Secondary Organic Aerosol Formed from α-Pinene into Nonvolatile Polyethylene Glycol Probe Particles P. Ye et al. 10.1021/acs.jpca.5b07435
285. Size-segregated particle number and mass concentrations from different emission sources in urban Beijing J. Cai et al. 10.5194/acp-20-12721-2020
286. Impacts of coagulation on the appearance time method for new particle growth rate evaluation and their corrections R. Cai et al. 10.5194/acp-21-2287-2021
287. Traffic-originated nanocluster emission exceeds H<sub>2</sub>SO<sub>4</sub>-driven photochemical new particle formation in an urban area M. Olin et al. 10.5194/acp-20-1-2020
288. Characterization of the mass-dependent transmission efficiency of a CIMS M. Heinritzi et al. 10.5194/amt-9-1449-2016
289. Hydration of Atmospheric Molecular Clusters III: Procedure for Efficient Free Energy Surface Exploration of Large Hydrated Clusters F. Rasmussen et al. 10.1021/acs.jpca.0c02932
290. Progress in Unraveling Atmospheric New Particle Formation and Growth Across the Arctic J. Schmale & A. Baccarini 10.1029/2021GL094198
291. Interaction of oxalic acid with dimethylamine and its atmospheric implications J. Chen et al. 10.1039/C6RA27945G
292. Widespread detection of chlorine oxyacids in the Arctic atmosphere Y. Tham et al. 10.1038/s41467-023-37387-y
293. Unexpected Growth Coordinate in Large Clusters Consisting of Sulfuric Acid and C8H12O6 Tricarboxylic Acid J. Elm 10.1021/acs.jpca.9b00428
294. Influence of anthropogenic emissions on the composition of highly oxygenated organic molecules in Helsinki: a street canyon and urban background station comparison M. Okuljar et al. 10.5194/acp-23-12965-2023
295. Understanding the Formation and Growth of New Atmospheric Particles at the Molecular Level through Laboratory Molecular Beam Experiments Y. Wang et al. 10.1002/cplu.202400108
296. What controls the observed size-dependency of the growth rates of sub-10 nm atmospheric particles? J. Kontkanen et al. 10.1039/D1EA00103E
297. Unexpectedly acidic nanoparticles formed in dimethylamine–ammonia–sulfuric-acid nucleation experiments at CLOUD M. Lawler et al. 10.5194/acp-16-13601-2016
298. New particle formation in the sulfuric acid–dimethylamine–water system: reevaluation of CLOUD chamber measurements and comparison to an aerosol nucleation and growth model A. Kürten et al. 10.5194/acp-18-845-2018
299. Low‐Volatility Vapors and New Particle Formation Over the Southern Ocean During the Antarctic Circumnavigation Expedition A. Baccarini et al. 10.1029/2021JD035126
300. Techniques and instruments used for real-time analysis of atmospheric nanoscale molecular clusters: A review X. Li et al. 10.1016/j.emcon.2015.05.001
301. A versatile vacuum ultraviolet ion source for reduced pressure bipolar chemical ionization mass spectrometry M. Breitenlechner et al. 10.5194/amt-15-1159-2022
302. Neutral molecular cluster formation of sulfuric acid–dimethylamine observed in real time under atmospheric conditions A. Kürten et al. 10.1073/pnas.1404853111
303. Clusteromics I: Principles, Protocols, and Applications to Sulfuric Acid–Base Cluster Formation J. Elm 10.1021/acsomega.1c00306
304. On secondary new particle formation in China M. Kulmala et al. 10.1007/s11783-016-0850-1
305. Effects of gas–wall interactions on measurements of semivolatile compounds and small polar molecules X. Liu et al. 10.5194/amt-12-3137-2019
306. Influence of vegetation on occurrence and time distributions of regional new aerosol particle formation and growth I. Salma et al. 10.5194/acp-21-2861-2021
307. Enigma of Urban Gaseous Oxygenated Organic Molecules: Precursor Type, Role of NOx, and Degree of Oxygenation L. Tian et al. 10.1021/acs.est.2c05047
308. Measurement report: Effects of NOx and seed aerosol on highly oxygenated organic molecules (HOMs) from cyclohexene ozonolysis M. Räty et al. 10.5194/acp-21-7357-2021
309. Relating the hygroscopic properties of submicron aerosol to both gas- and particle-phase chemical composition in a boreal forest environment J. Hong et al. 10.5194/acp-15-11999-2015
310. Formation of Highly Oxygenated Organic Molecules from α-Pinene Ozonolysis: Chemical Characteristics, Mechanism, and Kinetic Model Development U. Molteni et al. 10.1021/acsearthspacechem.9b00035
311. High Gas-Phase Methanesulfonic Acid Production in the OH-Initiated Oxidation of Dimethyl Sulfide at Low Temperatures J. Shen et al. 10.1021/acs.est.2c05154
312. Total sulfate vs. sulfuric acid monomer concenterations in nucleation studies K. Neitola et al. 10.5194/acp-15-3429-2015
313. H2SO4 formation from the gas-phase reaction of stabilized Criegee Intermediates with SO2: Influence of water vapour content and temperature T. Berndt et al. 10.1016/j.atmosenv.2014.02.062
314. Interactions between the atmosphere, cryosphere, and ecosystems at northern high latitudes M. Boy et al. 10.5194/acp-19-2015-2019
315. How volatile components catalyze vapor nucleation C. Li et al. 10.1126/sciadv.abd9954
316. Acid–Base Clusters during Atmospheric New Particle Formation in Urban Beijing R. Yin et al. 10.1021/acs.est.1c02701
317. Evidence for Diverse Biogeochemical Drivers of Boreal Forest New Particle Formation M. Lawler et al. 10.1002/2017GL076394
318. The Interplay Between Hydrogen Bonding and Coulombic Forces in Determining the Structure of Sulfuric Acid-Amine Clusters S. Waller et al. 10.1021/acs.jpclett.8b00161
319. Significant contributions of trimethylamine to sulfuric acid nucleation in polluted environments R. Cai et al. 10.1038/s41612-023-00405-3
320. Online detection of airborne nanoparticle composition with mass spectrometry: Recent advances, challenges, and opportunities X. Li et al. 10.1016/j.trac.2023.117195
321. 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
322. Chemical ionization of clusters formed from sulfuric acid and dimethylamine or diamines C. Jen et al. 10.5194/acp-16-12513-2016
323. Highly Oxidized Multifunctional Organic Compounds Observed in Tropospheric Particles: A Field and Laboratory Study A. Mutzel et al. 10.1021/acs.est.5b00885
324. Autoxidation of Limonene Emitted in a University Art Museum D. Pagonis et al. 10.1021/acs.estlett.9b00425
325. Substantial contribution of transported emissions to organic aerosol in Beijing K. Daellenbach et al. 10.1038/s41561-024-01493-3
326. Sources and sinks driving sulfuric acid concentrations in contrasting environments: implications on proxy calculations L. Dada et al. 10.5194/acp-20-11747-2020
327. Ammonium CI-Orbitrap: a tool for characterizing the reactivity of oxygenated organic molecules D. Li et al. 10.5194/amt-17-5413-2024
328. Analytical methodologies for oxidized organic compounds in the atmosphere A. Tiusanen et al. 10.1039/D3EM00163F
329. Sizing of neutral sub 3nm tungsten oxide clusters using Airmodus Particle Size Magnifier J. Kangasluoma et al. 10.1016/j.jaerosci.2015.05.007
330. Atmospheric Fate of Monoethanolamine: Enhancing New Particle Formation of Sulfuric Acid as an Important Removal Process H. Xie et al. 10.1021/acs.est.7b02294
331. Gasphasenbildung von Schwefliger Säure (H2SO3) in der Atmosphäre T. Berndt et al. 10.1002/ange.202405572
332. Measurement report: Atmospheric new particle formation in a coastal agricultural site explained with binPMF analysis of nitrate CI-APi-TOF spectra M. Olin et al. 10.5194/acp-22-8097-2022
333. Measurement of the nucleation of atmospheric aerosol particles M. Kulmala et al. 10.1038/nprot.2012.091
334. Solar eclipse demonstrating the importance of photochemistry in new particle formation T. Jokinen et al. 10.1038/srep45707
335. Global atmospheric particle formation from CERN CLOUD measurements E. Dunne et al. 10.1126/science.aaf2649
336. Chemistry of new particle growth in mixed urban and biogenic emissions – insights from CARES A. Setyan et al. 10.5194/acp-14-6477-2014
337. Quantification of isomer-resolved iodide chemical ionization mass spectrometry sensitivity and uncertainty using a voltage-scanning approach C. Bi et al. 10.5194/amt-14-6835-2021
338. The missing base molecules in atmospheric acid–base nucleation R. Cai et al. 10.1093/nsr/nwac137
339. Identification and Characterization of the HCl–DMS Gas Phase Molecular Complex via Infrared Spectroscopy and Electronic Structure Calculations N. Bork et al. 10.1021/jp411567x
340. Chemical composition of nanoparticles from <i>α</i>-pinene nucleation and the influence of isoprene and relative humidity at low temperature L. Caudillo et al. 10.5194/acp-21-17099-2021
341. Influence of Aerosol Chemical Composition on Condensation Sink Efficiency and New Particle Formation in Beijing W. Du et al. 10.1021/acs.estlett.2c00159
342. Studies on the conformation, thermodynamics, and evaporation rate characteristics of sulfuric acid and amines molecular clusters J. Chen 10.1016/j.rechem.2022.100527
343. Improving the Sensitivity of Fourier Transform Mass Spectrometer (Orbitrap) for Online Measurements of Atmospheric Vapors R. Cai et al. 10.1021/acs.analchem.2c03403
344. Theoretical and experimental analysis of the core sampling method: Reducing diffusional losses in aerosol sampling line Y. Fu et al. 10.1080/02786826.2019.1608354
345. Seasonal variation in oxygenated organic molecules in urban Beijing and their contribution to secondary organic aerosol Y. Guo et al. 10.5194/acp-22-10077-2022
346. Calibration of a Chemical Ionization Mass Spectrometer for the Measurement of Gaseous Sulfuric Acid A. Kürten et al. 10.1021/jp212123n