48 citations as recorded by crossref.

1. The effect of COVID-19 restrictions on atmospheric new particle formation in Beijing C. Yan et al. 10.5194/acp-22-12207-2022
2. Sulfuric acid, base, and low-volatility organics contribute to aerosol nucleation in urban Houston L. Tiszenkel et al. 10.1038/s43247-025-02310-4
3. Anthropogenic organic aerosol in Europe produced mainly through second-generation oxidation M. Xiao et al. 10.1038/s41561-025-01645-z
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5. Sulfur Dioxide Transported From the Residual Layer Drives Atmospheric Nucleation During Haze Periods in Beijing Y. Wang et al. 10.1029/2022GL100514
6. Survival of newly formed particles in haze conditions R. Marten et al. 10.1039/D2EA00007E
7. Characteristics of new particle formation events in a mountain semi-rural location in India J. Victor et al. 10.1016/j.atmosenv.2024.120414
8. Opinion: Atmospheric multiphase chemistry – past, present, and future J. Abbatt & A. Ravishankara 10.5194/acp-23-9765-2023
9. Optimized procedure for the determination of alkylamines in airborne particulate matter of anthropized areas D. Spolaor et al. 10.5194/ar-1-29-2023
10. The synergistic role of sulfuric acid, ammonia and organics in particle formation over an agricultural land L. Dada et al. 10.1039/D3EA00065F
11. Cluster-dynamics-based parameterization for sulfuric acid–dimethylamine nucleation: comparison and selection through box and three-dimensional modeling J. Shen et al. 10.5194/acp-24-10261-2024
12. 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
13. Synergistic HNO3–H2SO4–NH3 upper tropospheric particle formation M. Wang et al. 10.1038/s41586-022-04605-4
14. Quantum chemical modeling of atmospheric molecular clusters involving inorganic acids and methanesulfonic acid M. Engsvang et al. 10.1063/5.0152517
15. Role of sesquiterpenes in biogenic new particle formation L. Dada et al. 10.1126/sciadv.adi5297
16. Challenges in Observation of Ultrafine Particles: Addressing Estimation Miscalculations and the Necessity of Temporal Trends T. Lin et al. 10.1021/acs.est.4c07460
17. 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
18. Role of gas–molecular cluster–aerosol dynamics in atmospheric new-particle formation T. Olenius & P. Roldin 10.1038/s41598-022-14525-y
19. Observations of particle number size distributions and new particle formation in six Indian locations M. Sebastian et al. 10.5194/acp-22-4491-2022
20. New particle formation at a peri-urban agricultural site J. Kammer et al. 10.1016/j.scitotenv.2022.159370
21. Penguin guano is an important source of climate-relevant aerosol particles in Antarctica M. Boyer et al. 10.1038/s43247-025-02312-2
22. A quantum chemical investigation of the interaction of perfluoropropionic acid with monoethanolamine and sulfuric acid in the atmosphere F. Medeiros et al. 10.1016/j.comptc.2024.114485
23. 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
24. Nonagricultural Emissions Dominate Urban Atmospheric Amines as Revealed by Mobile Measurements Y. Chang et al. 10.1029/2021GL097640
25. Modeling approaches for atmospheric ion–dipole collisions: all-atom trajectory simulations and central field methods I. Neefjes et al. 10.5194/acp-22-11155-2022
26. Emissions of Carbonaceous Particulate Matter and Ultrafine Particles from Vehicles—A Scientific Review in a Cross-Cutting Context of Air Pollution and Climate Change B. Bessagnet et al. 10.3390/app12073623
27. Atmospheric nanoparticle growth D. Stolzenburg et al. 10.1103/RevModPhys.95.045002
28. New particle formation from isoprene under upper-tropospheric conditions J. Shen et al. 10.1038/s41586-024-08196-0
29. Effects of emission sources on the particle number size distribution of ambient air in the residential area S. Harni et al. 10.1016/j.atmosenv.2022.119419
30. Atmospheric new particle formation from the CERN CLOUD experiment J. Kirkby et al. 10.1038/s41561-023-01305-0
31. Assessing the importance of nitric acid and ammonia for particle growth in the polluted boundary layer R. Marten et al. 10.1039/D3EA00001J
32. The Effect of Using a New Parameterization of Nucleation in the WRF-Chem Model on New Particle Formation in a Passive Volcanic Plume S. Arghavani et al. 10.3390/atmos13010015
33. Molecular rearrangement of bicyclic peroxy radicals is a key route to aerosol from aromatics S. Iyer et al. 10.1038/s41467-023-40675-2
34. Sources of ultrafine particles at a rural midland site in Switzerland L. Dada et al. 10.5194/ar-3-315-2025
35. J-GAIN v1.1: a flexible tool to incorporate aerosol formation rates obtained by molecular models into large-scale models D. Yazgi & T. Olenius 10.5194/gmd-16-5237-2023
36. Measurement report: Urban ammonia and amines in Houston, Texas L. Tiszenkel et al. 10.5194/acp-24-11351-2024
37. Iodine oxoacids enhance nucleation of sulfuric acid particles in the atmosphere X. He et al. 10.1126/science.adh2526
38. Synergistic generation mechanisms of SOA and ozone from the photochemical oxidation of 1,3,5-trimethylbenzene: Influence of precursors ratio, temperature and radiation intensity H. Zhang et al. 10.1016/j.atmosres.2023.106924
39. Insight into the reactions of n-, iso-, sec- and tert-Butylperoxy radicals with hydroperoxyl radical in the Atmosphere: Reaction Mechanism, thermodynamic analysis and kinetics Z. Yang et al. 10.1016/j.comptc.2023.114436
40. Contrasting intra-urban variability of ultrafine particle number and fine particle mass concentrations in Dhaka, Bangladesh, and Pittsburgh, USA P. Saha et al. 10.1016/j.atmosenv.2024.120497
41. 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
42. Analysis of new particle formation events and comparisons to simulations of particle number concentrations based on GEOS-Chem–advanced particle microphysics in Beijing, China K. Wang et al. 10.5194/acp-23-4091-2023
43. The synergistic effect of organic and inorganic sulfonic acids promotes new particle formation Y. Ji et al. 10.1016/j.scitotenv.2023.163611
44. Distinct Temperature Trends in the Uptake of Gaseous n-Butylamine on Two Solid Diacids Y. Li et al. 10.1021/acsestair.3c00032
45. 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
46. Atmospheric Nanoparticle Survivability Reduction Due to Charge‐Induced Coagulation Scavenging Enhancement N. Mahfouz & N. Donahue 10.1029/2021GL092758
47. Contribution of Atmospheric Oxygenated Organic Compounds to Particle Growth in an Urban Environment X. Qiao et al. 10.1021/acs.est.1c02095
48. Toward Building a Physical Proxy for Gas-Phase Sulfuric Acid Concentration Based on Its Budget Analysis in Polluted Yangtze River Delta, East China L. Yang et al. 10.1021/acs.est.1c00738