116 citations as recorded by crossref.

1. Dimethyl sulfide control of the clean summertime Arctic aerosol and cloud W. Leaitch et al. 10.12952/journal.elementa.000017
2. The evolution of biomass-burning aerosol size distributions due to coagulation: dependence on fire and meteorological details and parameterization K. Sakamoto et al. 10.5194/acp-16-7709-2016
3. Evaluation of global simulations of aerosol particle and cloud condensation nuclei number, with implications for cloud droplet formation G. Fanourgakis et al. 10.5194/acp-19-8591-2019
4. Mechanism of SOA formation determines magnitude of radiative effects J. Zhu et al. 10.1073/pnas.1712273114
5. The Molecular Identification of Organic Compounds in the Atmosphere: State of the Art and Challenges B. Nozière et al. 10.1021/cr5003485
6. 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
7. The direct and indirect radiative effects of biogenic secondary organic aerosol C. Scott et al. 10.5194/acp-14-447-2014
8. Particle Size Distribution Dynamics Can Help Constrain the Phase State of Secondary Organic Aerosol Y. He et al. 10.1021/acs.est.0c05796
9. Emissions and radiative impacts of sub-10 nm particles from biofuel and fossil fuel cookstoves S. Jathar et al. 10.1080/02786826.2020.1769837
10. Modeling ultrafine particle growth at a pine forest site influenced by anthropogenic pollution during BEACHON-RoMBAS 2011 Y. Cui et al. 10.5194/acp-14-11011-2014
11. Simulation of the effects of low-volatility organic compounds on aerosol number concentrations in Europe D. Patoulias & S. Pandis 10.5194/acp-22-1689-2022
12. Model for acid-base chemistry in nanoparticle growth (MABNAG) T. Yli-Juuti et al. 10.5194/acp-13-12507-2013
13. Size-resolved effective density of submicron particles during summertime in the rural atmosphere of Beijing, China K. Qiao et al. 10.1016/j.jes.2018.01.012
14. New Particle Formation in the Atmosphere: From Molecular Clusters to Global Climate S. Lee et al. 10.1029/2018JD029356
15. Can semi-volatile organic aerosols lead to fewer cloud particles? C. Gao et al. 10.5194/acp-18-14243-2018
16. Organic Condensation and Particle Growth to CCN Sizes in the Summertime Marine Arctic Is Driven by Materials More Semivolatile Than at Continental Sites J. Burkart et al. 10.1002/2017GL075671
17. Processes controlling the annual cycle of Arctic aerosol number and size distributions B. Croft et al. 10.5194/acp-16-3665-2016
18. Impact of gas-to-particle partitioning approaches on the simulated radiative effects of biogenic secondary organic aerosol C. Scott et al. 10.5194/acp-15-12989-2015
19. Evaporation Kinetics of Laboratory-Generated Secondary Organic Aerosols at Elevated Relative Humidity J. Wilson et al. 10.1021/es505331d
20. Nucleation and condensational growth to CCN sizes during a sustained pristine biogenic SOA event in a forested mountain valley J. Pierce et al. 10.5194/acp-12-3147-2012
21. Hydrocarbon composition of tropospheric aerosol in the south of Western Siberia N. Voronetskaya et al. 10.1134/S1024856014060207
22. Modeling particle nucleation and growth over northern California during the 2010 CARES campaign A. Lupascu et al. 10.5194/acp-15-12283-2015
23. Heterogeneous iodine-organic chemistry fast-tracks marine new particle formation R. Huang et al. 10.1073/pnas.2201729119
24. Nucleation and growth of sulfate aerosol in coal-fired power plant plumes: sensitivity to background aerosol and meteorology R. Stevens et al. 10.5194/acp-12-189-2012
25. Synergy between Secondary Organic Aerosols and Long-Range Transport of Polycyclic Aromatic Hydrocarbons A. Zelenyuk et al. 10.1021/es302743z
26. The role of low volatile organics on secondary organic aerosol formation H. Kokkola et al. 10.5194/acp-14-1689-2014
27. Long-term volatility measurements of submicron atmospheric aerosol in Hyytiälä, Finland S. Häkkinen et al. 10.5194/acp-12-10771-2012
28. Dilution and photooxidation driven processes explain the evolution of organic aerosol in wildfire plumes A. Akherati et al. 10.1039/D1EA00082A
29. Implications of low volatility SOA and gas‐phase fragmentation reactions on SOA loadings and their spatial and temporal evolution in the atmosphere M. Shrivastava et al. 10.1002/jgrd.50160
30. Constraints on the Role of Laplace Pressure in Multiphase Reactions and Viscosity of Organic Aerosols S. Petters 10.1029/2022GL098959
31. The role of organic condensation on ultrafine particle growth during nucleation events D. Patoulias et al. 10.5194/acp-15-6337-2015
32. Contribution of sulfuric acid and oxidized organic compounds to particle formation and growth F. Riccobono et al. 10.5194/acp-12-9427-2012
33. Evolution of particle composition in CLOUD nucleation experiments H. Keskinen et al. 10.5194/acp-13-5587-2013
34. Compilation and evaluation of gas phase diffusion coefficients of reactive trace gases in the atmosphere: Volume 2. Diffusivities of organic compounds, pressure-normalised mean free paths, and average Knudsen numbers for gas uptake calculations M. Tang et al. 10.5194/acp-15-5585-2015
35. Chemistry of new particle formation and growth events during wintertime in suburban area of Beijing: Insights from highly polluted atmosphere S. Yang et al. 10.1016/j.atmosres.2021.105553
36. Atmospheric nanoparticle growth D. Stolzenburg et al. 10.1103/RevModPhys.95.045002
37. Source attribution of aerosol size distributions and model evaluation using Whistler Mountain measurements and GEOS-Chem-TOMAS simulations S. D'Andrea et al. 10.5194/acp-16-383-2016
38. Chemistry of new particle growth during springtime in the Seoul metropolitan area, Korea H. Kim & Q. Zhang 10.1016/j.chemosphere.2019.03.072
39. A computationally efficient model to represent the chemistry, thermodynamics, and microphysics of secondary organic aerosols (simpleSOM): model development and application to α-pinene SOA S. Jathar et al. 10.1039/D1EA00014D
40. Tutorial: Dynamic organic growth modeling with a volatility basis set D. Stolzenburg et al. 10.1016/j.jaerosci.2022.106063
41. Thermodynamics and kinetics of atmospheric aerosol particle formation and growth H. Vehkamäki & I. Riipinen 10.1039/c2cs00002d
42. Oxygenated Aromatic Compounds are Important Precursors of Secondary Organic Aerosol in Biomass-Burning Emissions A. Akherati et al. 10.1021/acs.est.0c01345
43. Inorganic salts interact with oxalic acid in submicron particles to form material with low hygroscopicity and volatility G. Drozd et al. 10.5194/acp-14-5205-2014
44. More Than Emissions and Chemistry: Fire Size, Dilution, and Background Aerosol Also Greatly Influence Near‐Field Biomass Burning Aerosol Aging A. Hodshire et al. 10.1029/2018JD029674
45. Experimental determination of chemical diffusion within secondary organic aerosol particles E. Abramson et al. 10.1039/c2cp44013j
46. The contribution of organics to atmospheric nanoparticle growth I. Riipinen et al. 10.1038/ngeo1499
47. Rapid growth of new atmospheric particles by nitric acid and ammonia condensation M. Wang et al. 10.1038/s41586-020-2270-4
48. The potential mechanism of atmospheric new particle formation involving amino acids with multiple functional groups J. Liu et al. 10.1039/D0CP06472F
49. MATRIX-VBS (v1.0): implementing an evolving organic aerosol volatility in an aerosol microphysics model C. Gao et al. 10.5194/gmd-10-751-2017
50. Organic aerosol processing in tropical deep convective clouds: Development of a new model (CRM‐ORG) and implications for sources of particle number B. Murphy et al. 10.1002/2015JD023551
51. Some insights into the condensing vapors driving new particle growth to CCN sizes on the basis of hygroscopicity measurements Z. Wu et al. 10.5194/acp-15-13071-2015
52. Connecting Bulk Viscosity Measurements to Kinetic Limitations on Attaining Equilibrium for a Model Aerosol Composition A. Booth et al. 10.1021/es501705c
53. Saturation Vapor Pressures and Transition Enthalpies of Low-Volatility Organic Molecules of Atmospheric Relevance: From Dicarboxylic Acids to Complex Mixtures M. Bilde et al. 10.1021/cr5005502
54. Particle growth in an isoprene-rich forest: Influences of urban, wildfire, and biogenic air masses M. Gunsch et al. 10.1016/j.atmosenv.2018.01.058
55. Observing HNO3 release dependent upon metal complexes in malonic acid/nitrate droplets X. Shao et al. 10.1016/j.saa.2018.05.026
56. Weak global sensitivity of cloud condensation nuclei and the aerosol indirect effect to Criegee + SO<sub>2</sub> chemistry J. Pierce et al. 10.5194/acp-13-3163-2013
57. Comparison of Daytime and Nighttime New Particle Growth at the HKUST Supersite in Hong Kong H. Man et al. 10.1021/acs.est.5b02143
58. Highly Oxygenated Molecules from Atmospheric Autoxidation of Hydrocarbons: A Prominent Challenge for Chemical Kinetics Studies M. Ehn et al. 10.1002/kin.21130
59. Vapor–Wall Deposition in Chambers: Theoretical Considerations R. McVay et al. 10.1021/es502170j
60. Ozonolysis of <i>α</i>-phellandrene – Part 1: Gas- and particle-phase characterisation F. Mackenzie-Rae et al. 10.5194/acp-17-6583-2017
61. Investigation of particle and vapor wall-loss effects on controlled wood-smoke smog-chamber experiments Q. Bian et al. 10.5194/acp-15-11027-2015
62. Insights into the Formation and Evolution of Individual Compounds in the Particulate Phase during Aromatic Photo-Oxidation K. Pereira et al. 10.1021/acs.est.5b03377
63. Molecular corridors and kinetic regimes in the multiphase chemical evolution of secondary organic aerosol M. Shiraiwa et al. 10.5194/acp-14-8323-2014
64. Under What Conditions Can Equilibrium Gas–Particle Partitioning Be Expected to Hold in the Atmosphere? H. Mai et al. 10.1021/acs.est.5b02587
65. Multiphase Chemistry at the Atmosphere–Biosphere Interface Influencing Climate and Public Health in the Anthropocene U. Pöschl & M. Shiraiwa 10.1021/cr500487s
66. Larger Submicron Particles for Emissions With Residential Burning in Wintertime San Joaquin Valley (Fresno) than for Vehicle Combustion in Summertime South Coast Air Basin (Fontana) R. Betha et al. 10.1029/2017JD026730
67. The potential role of methanesulfonic acid (MSA) in aerosol formation and growth and the associated radiative forcings A. Hodshire et al. 10.5194/acp-19-3137-2019
68. Arctic marine secondary organic aerosol contributes significantly to summertime particle size distributions in the Canadian Arctic Archipelago B. Croft et al. 10.5194/acp-19-2787-2019
69. Aerosol size distribution and radiative forcing response to anthropogenically driven historical changes in biogenic secondary organic aerosol formation S. D'Andrea et al. 10.5194/acp-15-2247-2015
70. Emissions and Possible Environmental Implication of Engineered Nanomaterials (ENMs) in the Atmosphere A. John et al. 10.3390/atmos8050084
71. Reevaluating the contribution of sulfuric acid and the origin of organic compounds in atmospheric nanoparticle growth V. Vakkari et al. 10.1002/2015GL066459
72. Formation and growth of nucleated particles into cloud condensation nuclei: model–measurement comparison D. Westervelt et al. 10.5194/acp-13-7645-2013
73. Particulate matter, air quality and climate: lessons learned and future needs S. Fuzzi et al. 10.5194/acp-15-8217-2015
74. Understanding global secondary organic aerosol amount and size-resolved condensational behavior S. D'Andrea et al. 10.5194/acp-13-11519-2013
75. Particle hygroscopicity during atmospheric new particle formation events: implications for the chemical species contributing to particle growth Z. Wu et al. 10.5194/acp-13-6637-2013
76. Coating surface tension dependence of soot aggregate restructuring E. Schnitzler et al. 10.1016/j.jaerosci.2017.01.005
77. Water vapour effects on secondary organic aerosol formation in isoprene ozonolysis Y. Sakamoto et al. 10.1039/C6CP04521A
78. Semi-empirical parameterization of size-dependent atmospheric nanoparticle growth in continental environments S. Häkkinen et al. 10.5194/acp-13-7665-2013
79. Contributions of volatile and nonvolatile compounds (at 300°C) to condensational growth of atmospheric nanoparticles: An assessment based on 8.5 years of observations at the Central Europe background site Melpitz Z. Wang et al. 10.1002/2016JD025581
80. Modeling kinetic partitioning of secondary organic aerosol and size distribution dynamics: representing effects of volatility, phase state, and particle-phase reaction R. Zaveri et al. 10.5194/acp-14-5153-2014
81. Cloud condensation nuclei production associated with atmospheric nucleation: a synthesis based on existing literature and new results V. Kerminen et al. 10.5194/acp-12-12037-2012
82. Substantially positive contributions of new particle formation to cloud condensation nuclei under low supersaturation in China based on numerical model improvements C. Zhang et al. 10.5194/acp-23-10713-2023
83. New-particle formation, growth and climate-relevant particle production in Egbert, Canada: analysis from 1 year of size-distribution observations J. Pierce et al. 10.5194/acp-14-8647-2014
84. Growth rates of atmospheric molecular clusters based on appearance times and collision–evaporation fluxes: Growth by monomers T. Olenius et al. 10.1016/j.jaerosci.2014.08.008
85. The potential role of organics in new particle formation and initial growth in the remote tropical upper troposphere A. Kupc et al. 10.5194/acp-20-15037-2020
86. 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
87. Antarctic new particle formation from continental biogenic precursors E. Kyrö et al. 10.5194/acp-13-3527-2013
88. Study of new particle formation events in southern Italy A. Dinoi et al. 10.1016/j.atmosenv.2020.117920
89. Modeling anthropogenically controlled secondary organic aerosols in a megacity: a simplified framework for global and climate models A. Hodzic & J. Jimenez 10.5194/gmd-4-901-2011
90. Organic aerosols over Indo-Gangetic Plain: Sources, distributions and climatic implications N. Singh et al. 10.1016/j.atmosenv.2017.03.008
91. Effect of Inorganic Salts on the Volatility of Organic Acids S. Häkkinen et al. 10.1021/es5033103
92. Constraining nucleation, condensation, and chemistry in oxidation flow reactors using size-distribution measurements and aerosol microphysical modeling A. Hodshire et al. 10.5194/acp-18-12433-2018
93. The role of low-volatility organic compounds in initial particle growth in the atmosphere J. Tröstl et al. 10.1038/nature18271
94. Comparing the mechanism of water condensation and evaporation in glassy aerosol D. Bones et al. 10.1073/pnas.1200691109
95. Alkoxy Radical Bond Scissions Explain the Anomalously Low Secondary Organic Aerosol and Organonitrate Yields From α-Pinene + NO3 T. Kurtén et al. 10.1021/acs.jpclett.7b01038
96. Recent advances in understanding secondary organic aerosol: Implications for global climate forcing M. Shrivastava et al. 10.1002/2016RG000540
97. Cloud condensation nuclei droplet growth kinetics of ultrafine particles during anthropogenic nucleation events N. Shantz et al. 10.1016/j.atmosenv.2011.10.049
98. Reduction of anthropogenic emissions enhanced atmospheric new particle formation: Observational evidence during the Beijing 2022 Winter Olympics W. Zhu et al. 10.1016/j.atmosenv.2023.120094
99. The enhancement mechanism of glycolic acid on the formation of atmospheric sulfuric acid–ammonia molecular clusters H. Zhang et al. 10.1063/1.4982929
100. Nonequilibrium atmospheric secondary organic aerosol formation and growth V. Perraud et al. 10.1073/pnas.1119909109
101. Atmospheric new particle formation and growth: review of field observations V. Kerminen et al. 10.1088/1748-9326/aadf3c
102. 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
103. Statistical analysis and environmental impact of pre-existing particle growth events in a Northern Chinese coastal megacity: A 725-day study in 2010–2018 X. Wei et al. 10.1016/j.scitotenv.2024.173227
104. Low temperature growth of sub 10 nm particles by ammonium nitrate condensation N. Donahue et al. 10.1039/D4EA00117F
105. Chemistry of new particle growth in mixed urban and biogenic emissions – insights from CARES A. Setyan et al. 10.5194/acp-14-6477-2014
106. The effect of model spatial resolution on Secondary Organic Aerosol predictions: a case study at Whistler, BC, Canada C. Wainwright et al. 10.5194/acp-12-10911-2012
107. Simulating ultrafine particle formation in Europe using a regional CTM: contribution of primary emissions versus secondary formation to aerosol number concentrations C. Fountoukis et al. 10.5194/acp-12-8663-2012
108. Liquid–Liquid Phase Separation in Supermicrometer and Submicrometer Aerosol Particles M. Freedman 10.1021/acs.accounts.0c00093
109. Global–regional nested simulation of particle number concentration by combing microphysical processes with an evolving organic aerosol module X. Chen et al. 10.5194/acp-21-9343-2021
110. Estimating the saturation vapor pressures of isoprene oxidation products C<sub>5</sub>H<sub>12</sub>O<sub>6</sub> and C<sub>5</sub>H<sub>10</sub>O<sub>6</sub> using COSMO-RS T. Kurtén et al. 10.5194/acp-18-17589-2018
111. Hygroscopicity of nanoparticles produced from homogeneous nucleation in the CLOUD experiments J. Kim et al. 10.5194/acp-16-293-2016
112. Analysis of feedbacks between nucleation rate, survival probability and cloud condensation nuclei formation D. Westervelt et al. 10.5194/acp-14-5577-2014
113. An evaluation of new particle formation events in Helsinki during a Baltic Sea cyanobacterial summer bloom R. Thakur et al. 10.5194/acp-22-6365-2022
114. Theoretical constraints on pure vapor-pressure driven condensation of organics to ultrafine particles N. Donahue et al. 10.1029/2011GL048115
115. Secondary organic aerosol formation from evaporated biofuels: comparison to gasoline and correction for vapor wall losses Y. He et al. 10.1039/D0EM00103A
116. Improving new particle formation simulation by coupling a volatility-basis set (VBS) organic aerosol module in NAQPMS+APM X. Chen et al. 10.1016/j.atmosenv.2019.01.053