105 citations as recorded by crossref.

1. Measurement of the collision rate coefficients between atmospheric ions and multiply charged aerosol particles in the CERN CLOUD chamber J. Pfeifer et al. 10.5194/acp-23-6703-2023
2. Natural new particle formation at the coastal Antarctic site Neumayer R. Weller et al. 10.5194/acp-15-11399-2015
3. Reevaluating the contribution of sulfuric acid and the origin of organic compounds in atmospheric nanoparticle growth V. Vakkari et al. 10.1002/2015GL066459
4. Size distribution and ionic composition of marine summer aerosol at the continental Antarctic site Kohnen R. Weller et al. 10.5194/acp-18-2413-2018
5. The importance of accounting for enhanced emissions of monoterpenes from new Scots pine foliage in models - A Finnish case study D. Taipale et al. 10.1016/j.aeaoa.2020.100097
6. Growth of sulphuric acid nanoparticles under wet and dry conditions L. Skrabalova et al. 10.5194/acp-14-6461-2014
7. Technical Note: Using DEG-CPCs at upper tropospheric temperatures D. Wimmer et al. 10.5194/acp-15-7547-2015
8. Causes and importance of new particle formation in the present‐day and preindustrial atmospheres H. Gordon et al. 10.1002/2017JD026844
9. Survival probabilities of atmospheric particles: comparison based on theory, cluster population simulations, and observations in Beijing S. Tuovinen et al. 10.5194/acp-22-15071-2022
10. Sub-3 nm Particles Detection in a Large Photoreactor Background: Possible Implications for New Particles Formation Studies in a Smog Chamber J. Boulon et al. 10.1080/02786826.2012.733040
11. Contribution of New Particle Formation to Cloud Condensation Nuclei Activity and its Controlling Factors in a Mountain Region of Inland China M. Cai et al. 10.1029/2020JD034302
12. Modeling the thermodynamics and kinetics of sulfuric acid-dimethylamine-water nanoparticle growth in the CLOUD chamber L. Ahlm et al. 10.1080/02786826.2016.1223268
13. Role of sesquiterpenes in biogenic new particle formation L. Dada et al. 10.1126/sciadv.adi5297
14. Nucleation and Growth of Nanoparticles in the Atmosphere R. Zhang et al. 10.1021/cr2001756
15. 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
16. 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
17. The effect of COVID-19 restrictions on atmospheric new particle formation in Beijing C. Yan et al. 10.5194/acp-22-12207-2022
18. Observation of aerosol size distribution and new particle formation at a mountain site in subtropical Hong Kong H. Guo et al. 10.5194/acp-12-9923-2012
19. Enhanced growth rate of atmospheric particles from sulfuric acid D. Stolzenburg et al. 10.5194/acp-20-7359-2020
20. Investigating three patterns of new particles growing to the size of cloud condensation nuclei in Beijing's urban atmosphere L. Ma et al. 10.5194/acp-21-183-2021
21. A proxy for atmospheric daytime gaseous sulfuric acid concentration in urban Beijing Y. Lu et al. 10.5194/acp-19-1971-2019
22. Aerosol nucleation in an ultra-low ion density environment J. Pedersen et al. 10.1016/j.jaerosci.2012.03.003
23. Differing Mechanisms of New Particle Formation at Two Arctic Sites L. Beck et al. 10.1029/2020GL091334
24. Observations of new particle formation in enhanced UV irradiance zones near cumulus clouds B. Wehner et al. 10.5194/acp-15-11701-2015
25. Semi-empirical parameterization of size-dependent atmospheric nanoparticle growth in continental environments S. Häkkinen et al. 10.5194/acp-13-7665-2013
26. 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
27. The effect of meteorological conditions and atmospheric composition in the occurrence and development of new particle formation (NPF) events in Europe D. Bousiotis et al. 10.5194/acp-21-3345-2021
28. Collective geographical ecoregions and precursor sources driving Arctic new particle formation J. Brean et al. 10.5194/acp-23-2183-2023
29. 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
30. Atmospheric nanoparticle growth D. Stolzenburg et al. 10.1103/RevModPhys.95.045002
31. On the diurnal cycle of urban aerosols, black carbon and the occurrence of new particle formation events in springtime São Paulo, Brazil J. Backman et al. 10.5194/acp-12-11733-2012
32. 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
33. Photo-oxidation of Aromatic Hydrocarbons Produces Low-Volatility Organic Compounds M. Wang et al. 10.1021/acs.est.0c02100
34. Connection of organics to atmospheric new particle formation and growth at an urban site of Beijing Z. Wang et al. 10.1016/j.atmosenv.2014.11.069
35. Influence of aerosol lifetime on the interpretation of nucleation experiments with respect to the first nucleation theorem S. Ehrhart & J. Curtius 10.5194/acp-13-11465-2013
36. Nucleation and growth of sub-3 nm particles in the polluted urban atmosphere of a megacity in China H. Yu et al. 10.5194/acp-16-2641-2016
37. Using measurements of the aerosol charging state in determination of the particle growth rate and the proportion of ion-induced nucleation J. Leppä et al. 10.5194/acp-13-463-2013
38. Ion-induced sulfuric acid–ammonia nucleation drives particle formation in coastal Antarctica T. Jokinen et al. 10.1126/sciadv.aat9744
39. New particle formation, growth and apparent shrinkage at a rural background site in western Saudi Arabia S. Hakala et al. 10.5194/acp-19-10537-2019
40. Identification and quantification of particle growth channels during new particle formation M. Pennington et al. 10.5194/acp-13-10215-2013
41. New particle formation at urban and high-altitude remote sites in the south-eastern Iberian Peninsula J. Casquero-Vera et al. 10.5194/acp-20-14253-2020
42. Aerosol formation and growth rates from chamber experiments using Kalman smoothing M. Ozon et al. 10.5194/acp-21-12595-2021
43. Growth of atmospheric clusters involving cluster–cluster collisions: comparison of different growth rate methods J. Kontkanen et al. 10.5194/acp-16-5545-2016
44. 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
45. Growth rates of nucleation mode particles in Hyytiälä during 2003−2009: variation with particle size, season, data analysis method and ambient conditions T. Yli-Juuti et al. 10.5194/acp-11-12865-2011
46. Numerical simulations of mixing conditions and aerosol dynamics in the CERN CLOUD chamber J. Voigtländer et al. 10.5194/acp-12-2205-2012
47. Characteristics of regional new particle formation in urban and regional background environments in the North China Plain Z. Wang et al. 10.5194/acp-13-12495-2013
48. Ternary homogeneous nucleation of H<sub>2</sub>SO<sub>4</sub>, NH<sub>3</sub>, and H<sub>2</sub>O under conditions relevant to the lower troposphere D. Benson et al. 10.5194/acp-11-4755-2011
49. Ground-based observation of clusters and nucleation-mode particles in the Amazon D. Wimmer et al. 10.5194/acp-18-13245-2018
50. Iodine oxoacids and their roles in sub-3 nm particle growth in polluted urban environments Y. Zhang et al. 10.5194/acp-24-1873-2024
51. New particle formation in the free troposphere: A question of chemistry and timing F. Bianchi et al. 10.1126/science.aad5456
52. Modelling the influence of biotic plant stress on atmospheric aerosol particle processes throughout a growing season D. Taipale et al. 10.5194/acp-21-17389-2021
53. Seasonal cycle and modal structure of particle number size distribution at Dome C, Antarctica E. Järvinen et al. 10.5194/acp-13-7473-2013
54. Absorption of infrasound in the lower and middle clouds of Venus A. Trahan & A. Petculescu 10.1121/10.0001520
55. Tutorial: Dynamic organic growth modeling with a volatility basis set D. Stolzenburg et al. 10.1016/j.jaerosci.2022.106063
56. On the derivation of particle nucleation rates from experimental formation rates A. Kürten et al. 10.5194/acp-15-4063-2015
57. New particle formation and growth at a suburban site and a background site in Hong Kong X. Lyu et al. 10.1016/j.chemosphere.2017.11.060
58. Size-dependent influence of NO x on the growth rates of organic aerosol particles C. Yan et al. 10.1126/sciadv.aay4945
59. Growth of atmospheric nano-particles by heterogeneous nucleation of organic vapor J. Wang et al. 10.5194/acp-13-6523-2013
60. Contribution of sulfuric acid and oxidized organic compounds to particle formation and growth F. Riccobono et al. 10.5194/acp-12-9427-2012
61. Atmospheric new particle formation: real and apparent growth of neutral and charged particles J. Leppä et al. 10.5194/acp-11-4939-2011
62. The driving factors of new particle formation and growth in the polluted boundary layer M. Xiao et al. 10.5194/acp-21-14275-2021
63. New particle formation events in semi-clean South African savannah V. Vakkari et al. 10.5194/acp-11-3333-2011
64. Explaining apparent particle shrinkage related to new particle formation events in western Saudi Arabia does not require evaporation S. Hakala et al. 10.5194/acp-23-9287-2023
65. A chamber study of the influence of boreal BVOC emissions and sulfuric acid on nanoparticle formation rates at ambient concentrations M. Dal Maso et al. 10.5194/acp-16-1955-2016
66. Contribution of Atmospheric Oxygenated Organic Compounds to Particle Growth in an Urban Environment X. Qiao et al. 10.1021/acs.est.1c02095
67. What controls the observed size-dependency of the growth rates of sub-10 nm atmospheric particles? J. Kontkanen et al. 10.1039/D1EA00103E
68. Rapid night-time nanoparticle growth in Delhi driven by biomass-burning emissions S. Mishra et al. 10.1038/s41561-023-01138-x
69. Strong atmospheric new particle formation in winter in urban Shanghai, China S. Xiao et al. 10.5194/acp-15-1769-2015
70. CFD and experimental studies on capture of fine particles by liquid droplets in open spray towers N. Rafidi et al. 10.1016/j.serj.2018.08.003
71. Future vegetation–climate interactions in Eastern Siberia: an assessment of the competing effects of CO<sub>2</sub> and secondary organic aerosols A. Arneth et al. 10.5194/acp-16-5243-2016
72. Rapid growth of organic aerosol nanoparticles over a wide tropospheric temperature range D. Stolzenburg et al. 10.1073/pnas.1807604115
73. Molecular insights into new particle formation in Barcelona, Spain J. Brean et al. 10.5194/acp-20-10029-2020
74. New Insights Into the Composition and Origins of Ultrafine Aerosol in the Summertime High Arctic M. Lawler et al. 10.1029/2021GL094395
75. Laboratory observations of temperature and humidity dependencies of nucleation and growth rates of sub‐3 nm particles H. Yu et al. 10.1002/2016JD025619
76. Open ocean and coastal new particle formation from sulfuric acid and amines around the Antarctic Peninsula J. Brean et al. 10.1038/s41561-021-00751-y
77. Measurement of the nucleation of atmospheric aerosol particles M. Kulmala et al. 10.1038/nprot.2012.091
78. The role of low-volatility organic compounds in initial particle growth in the atmosphere J. Tröstl et al. 10.1038/nature18271
79. Long-term analysis of clear-sky new particle formation events and nonevents in Hyytiälä L. Dada et al. 10.5194/acp-17-6227-2017
80. Atmospheric new particle formation from sulfuric acid and amines in a Chinese megacity L. Yao et al. 10.1126/science.aao4839
81. Aerosol particle formation in the Lithuanian hemi-boreal forest V. Dudoitis et al. 10.3952/physics.v58i3.3817
82. Multicomponent new particle formation from sulfuric acid, ammonia, and biogenic vapors K. Lehtipalo et al. 10.1126/sciadv.aau5363
83. Comparison results of eight oxygenated organic molecules: Unexpected contribution to new particle formation in the atmosphere S. Tan et al. 10.1016/j.atmosenv.2021.118817
84. Sulphuric acid and aerosol particle production in the vicinity of an oil refinery N. Sarnela et al. 10.1016/j.atmosenv.2015.08.033
85. Particle number size distributions and formation and growth rates of different new particle formation types of a megacity in China L. Dai et al. 10.1016/j.jes.2022.07.029
86. New particle formation from sulfuric acid and ammonia: nucleation and growth model based on thermodynamics derived from CLOUD measurements for a wide range of conditions A. Kürten 10.5194/acp-19-5033-2019
87. Nonequilibrium atmospheric secondary organic aerosol formation and growth V. Perraud et al. 10.1073/pnas.1119909109
88. Antarctic new particle formation from continental biogenic precursors E. Kyrö et al. 10.5194/acp-13-3527-2013
89. Effect of ions on sulfuric acid‐water binary particle formation: 2. Experimental data and comparison with QC‐normalized classical nucleation theory J. Duplissy et al. 10.1002/2015JD023539
90. Identification of highly oxygenated organic molecules and their role in aerosol formation in the reaction of limonene with nitrate radical Y. Guo et al. 10.5194/acp-22-11323-2022
91. Size and time-resolved growth rate measurements of 1 to 5 nm freshly formed atmospheric nuclei C. Kuang et al. 10.5194/acp-12-3573-2012
92. The important roles of surface tension and growth rate in the contribution of new particle formation (NPF) to cloud condensation nuclei (CCN) number concentration: evidence from field measurements in southern China M. Cai et al. 10.5194/acp-21-8575-2021
93. 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
94. Climatology of new particle formation at Izaña mountain GAW observatory in the subtropical North Atlantic M. García et al. 10.5194/acp-14-3865-2014
95. 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
96. A large source of low-volatility secondary organic aerosol M. Ehn et al. 10.1038/nature13032
97. Multiple daytime nucleation events in semi-clean savannah and industrial environments in South Africa: analysis based on observations A. Hirsikko et al. 10.5194/acp-13-5523-2013
98. Frequent new particle formation over the high Arctic pack ice by enhanced iodine emissions A. Baccarini et al. 10.1038/s41467-020-18551-0
99. Quantification of the volatility of secondary organic compounds in ultrafine particles during nucleation events J. Pierce et al. 10.5194/acp-11-9019-2011
100. The effect of acid–base clustering and ions on the growth of atmospheric nano-particles K. Lehtipalo et al. 10.1038/ncomms11594
101. Atmospheric new particle formation and growth: review of field observations V. Kerminen et al. 10.1088/1748-9326/aadf3c
102. Simultaneous measurements of particle number size distributions at ground level and 260 m on a meteorological tower in urban Beijing, China W. Du et al. 10.5194/acp-17-6797-2017
103. Laboratory study on new particle formation from the reaction OH + SO<sub>2</sub>: influence of experimental conditions, H<sub>2</sub>O vapour, NH<sub>3</sub> and the amine tert-butylamine on the overall process T. Berndt et al. 10.5194/acp-10-7101-2010
104. The Use of Spectral Methods for the “Ensemble” Assessment of Synthesis Dynamics of the Arabinogalactan-Stabilized Selenium Nanoparticles M. Zvereva et al. 10.1007/s10876-023-02525-5
105. On the roles of sulphuric acid and low-volatility organic vapours in the initial steps of atmospheric new particle formation P. Paasonen et al. 10.5194/acp-10-11223-2010