80 citations as recorded by crossref.

1. The dependence of new particle formation rates on the interaction between cluster growth, evaporation, and condensation sink C. Li et al. 10.1039/D2EA00066K
2. The driving factors of new particle formation and growth in the polluted boundary layer M. Xiao et al. 10.5194/acp-21-14275-2021
3. Acid–Base Clusters during Atmospheric New Particle Formation in Urban Beijing R. Yin et al. 10.1021/acs.est.1c02701
4. Historically Understanding the Spatial Distributions of Particle Surface Area Concentrations Over China Estimated Using a Non-Parametric Machine Learning Method Y. Qiu et al. 10.2139/ssrn.3994600
5. The Levels and Sources of Nitrous Acid (HONO) in Winter of Beijing and Sanmenxia X. Zhang et al. 10.1029/2021JD036278
6. High-resolution vertical distribution and sources of HONO and NO<sub>2</sub> in the nocturnal boundary layer in urban Beijing, China F. Meng et al. 10.5194/acp-20-5071-2020
7. Overview of measurements and current instrumentation for 1–10 nm aerosol particle number size distributions J. Kangasluoma et al. 10.1016/j.jaerosci.2020.105584
8. The striking effect of vertical mixing in the planetary boundary layer on new particle formation in the Yangtze River Delta S. Lai et al. 10.1016/j.scitotenv.2022.154607
9. The effect of COVID-19 restrictions on atmospheric new particle formation in Beijing C. Yan et al. 10.5194/acp-22-12207-2022
10. Assessment of particle size magnifier inversion methods to obtain the particle size distribution from atmospheric measurements T. Chan et al. 10.5194/amt-13-4885-2020
11. 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
12. Dynamics of nanocluster aerosol in the indoor atmosphere during gas cooking S. Patra et al. 10.1093/pnasnexus/pgae044
13. Particle number size distribution and new particle formation in Xiamen, the coastal city of Southeast China in wintertime J. Wang et al. 10.1016/j.scitotenv.2022.154208
14. Investigation of new particle formation at the summit of Mt. Tai, China G. Lv et al. 10.5194/acp-18-2243-2018
15. Chemistry and human exposure implications of secondary organic aerosol production from indoor terpene ozonolysis C. Rosales et al. 10.1126/sciadv.abj9156
16. 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
17. Variation of size-segregated particle number concentrations in wintertime Beijing Y. Zhou et al. 10.5194/acp-20-1201-2020
18. Atmospheric new particle formation in China B. Chu et al. 10.5194/acp-19-115-2019
19. New particle formation (NPF) events in China urban clusters given by sever composite pollution background Q. Zhang et al. 10.1016/j.chemosphere.2020.127842
20. Atmospheric new particle formation and growth: review of field observations V. Kerminen et al. 10.1088/1748-9326/aadf3c
21. Observation of sub-3nm particles and new particle formation at an urban location in India M. Sebastian et al. 10.1016/j.atmosenv.2021.118460
22. Vigorous New Particle Formation Above Polluted Boundary Layer in the North China Plain S. Lai et al. 10.1029/2022GL100301
23. Atmospheric new particle formation in India: Current understanding and knowledge gaps V. Kanawade et al. 10.1016/j.atmosenv.2021.118894
24. 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
25. 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
26. i<sub>N</sub>RACM: incorporating <sup>15</sup>N into the Regional Atmospheric Chemistry Mechanism (RACM) for assessing the role photochemistry plays in controlling the isotopic composition of NO<sub><i>x</i></sub>, NO<sub><i>y</i></sub>, and atmospheric nitrate H. Fang et al. 10.5194/gmd-14-5001-2021
27. OH, HO2, and RO2 radical chemistry in a rural forest environment: measurements, model comparisons, and evidence of a missing radical sink B. Bottorff et al. 10.5194/acp-23-10287-2023
28. Comparison of new particle formation events in urban, agricultural, and arctic environments H. Lee et al. 10.1016/j.atmosenv.2024.120634
29. Measurement report: Contribution of atmospheric new particle formation to ultrafine particle concentration, cloud condensation nuclei, and radiative forcing – results from 5-year observations in central Europe J. Sun et al. 10.5194/acp-24-10667-2024
30. Survival probability of new atmospheric particles: closure between theory and measurements from 1.4 to 100 nm R. Cai et al. 10.5194/acp-22-14571-2022
31. Vertical transport of ultrafine particles and turbulence evolution impact on new particle formation at the surface & Canton Tower H. Wu et al. 10.1016/j.atmosres.2024.107290
32. Particle number size distribution and new particle formation under the influence of biomass burning at a high altitude background site at Mt. Yulong (3410 m), China D. Shang et al. 10.5194/acp-18-15687-2018
33. Towards a concentration closure of sub-6 nm aerosol particles and sub-3 nm atmospheric clusters M. Kulmala et al. 10.1016/j.jaerosci.2021.105878
34. The missing base molecules in atmospheric acid–base nucleation R. Cai et al. 10.1093/nsr/nwac137
35. New particle formation and its CCN enhancement in the Yangtze River Delta under the control of continental and marine air masses X. Fang et al. 10.1016/j.atmosenv.2021.118400
36. Investigating the effectiveness of condensation sink based on heterogeneous nucleation theory S. Tuovinen et al. 10.1016/j.jaerosci.2020.105613
37. Spatial Inhomogeneity of New Particle Formation in the Urban and Mountainous Atmospheres of the North China Plain during the 2022 Winter Olympics D. Shang et al. 10.3390/atmos14091395
38. 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
39. Formation and growth of sub-3 nm particles in megacities: impact of background aerosols C. Deng et al. 10.1039/D0FD00083C
40. Seasonal Characteristics of New Particle Formation and Growth in Urban Beijing C. Deng et al. 10.1021/acs.est.0c00808
41. Historically understanding the spatial distributions of particle surface area concentrations over China estimated using a non-parametric machine learning method Y. Qiu et al. 10.1016/j.scitotenv.2022.153849
42. The effectiveness of the coagulation sink of 3–10 nm atmospheric particles R. Cai et al. 10.5194/acp-22-11529-2022
43. Characteristics of aerosol size distribution and liquid water content under ambient RH conditions in Beijing H. Dai et al. 10.1016/j.atmosenv.2022.119397
44. 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
45. 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
46. Evidence of heterogeneous HONO formation from aerosols and the regional photochemical impact of this HONO source X. Lu et al. 10.1088/1748-9326/aae492
47. 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
48. An indicator for sulfuric acid–amine nucleation in atmospheric environments R. Cai et al. 10.1080/02786826.2021.1922598
49. Seasonal variations in composition and sources of atmospheric ultrafine particles in urban Beijing based on near-continuous measurements X. Li et al. 10.5194/acp-23-14801-2023
50. Contribution of Atmospheric Oxygenated Organic Compounds to Particle Growth in an Urban Environment X. Qiao et al. 10.1021/acs.est.1c02095
51. Significant ultrafine particle emissions from residential solid fuel combustion D. Wang et al. 10.1016/j.scitotenv.2020.136992
52. Interactions between aerosol organic components and liquid water content during haze episodes in Beijing X. Li et al. 10.5194/acp-19-12163-2019
53. Urban aerosol size distributions: a global perspective T. Wu & B. Boor 10.5194/acp-21-8883-2021
54. Formation Mechanisms and Source Apportionments of Nitrate Aerosols in a Megacity of Eastern China Based On Multiple Isotope Observations M. Fan et al. 10.1029/2022JD038129
55. Sulfuric acid–amine nucleation in urban Beijing R. Cai et al. 10.5194/acp-21-2457-2021
56. Recent progress in chemical ionization mass spectrometry and its application in atmospheric environment W. Li et al. 10.1016/j.atmosenv.2024.120426
57. Atmospheric new particle formation characteristics in the Arctic as measured at Mount Zeppelin, Svalbard, from 2016 to 2018 H. Lee et al. 10.5194/acp-20-13425-2020
58. Cold Air Outbreaks Promote New Particle Formation Off the U.S. East Coast A. Corral et al. 10.1029/2021GL096073
59. Observed coupling between air mass history, secondary growth of nucleation mode particles and aerosol pollution levels in Beijing S. Hakala et al. 10.1039/D1EA00089F
60. The impact of the atmospheric turbulence-development tendency on new particle formation: a common finding on three continents H. Wu et al. 10.1093/nsr/nwaa157
61. Formation of nighttime sulfuric acid from the ozonolysis of alkenes in Beijing Y. Guo et al. 10.5194/acp-21-5499-2021
62. Measurement report: Size distributions of urban aerosols down to 1 nm from long-term measurements C. Deng et al. 10.5194/acp-22-13569-2022
63. Estimating the influence of transport on aerosol size distributions during new particle formation events R. Cai et al. 10.5194/acp-18-16587-2018
64. Parameters governing the performance of electrical mobility spectrometers for measuring sub-3 nm particles R. Cai et al. 10.1016/j.jaerosci.2018.11.002
65. Measurement report: New particle formation characteristics at an urban and a mountain station in northern China Y. Zhou et al. 10.5194/acp-21-17885-2021
66. Formation of extremely low-volatility organic compounds from styrene ozonolysis: Implication for nucleation S. Yu et al. 10.1016/j.chemosphere.2022.135459
67. Review of sub-3 nm condensation particle counters, calibrations, and cluster generation methods J. Kangasluoma & M. Attoui 10.1080/02786826.2019.1654084
68. A Study on Elevated Concentrations of Submicrometer Particles in an Urban Atmosphere H. Cho et al. 10.3390/atmos9100393
69. 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
70. Reaction of HOCl with Wood Smoke Aerosol: Impacts on Indoor Air Quality and Outdoor Reactive Chlorine S. Jorga et al. 10.1021/acs.est.2c07577
71. The Synergistic Role of Sulfuric Acid, Bases, and Oxidized Organics Governing New‐Particle Formation in Beijing C. Yan et al. 10.1029/2020GL091944
72. 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
73. Aerosol characteristics in the entrainment interface layer in relation to the marine boundary layer and free troposphere H. Dadashazar et al. 10.5194/acp-18-1495-2018
74. 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
75. Measuring size distributions of atmospheric aerosols using natural air ions Y. Li et al. 10.1080/02786826.2022.2060795
76. The proper view of cluster free energy in nucleation theories R. Cai & J. Kangasluoma 10.1080/02786826.2022.2075250
77. Sulfur Dioxide Transported From the Residual Layer Drives Atmospheric Nucleation During Haze Periods in Beijing Y. Wang et al. 10.1029/2022GL100514
78. Increasing contribution of nighttime nitrogen chemistry to wintertime haze formation in Beijing observed during COVID-19 lockdowns C. Yan et al. 10.1038/s41561-023-01285-1
79. A New Physical Mechanism of Rainfall Facilitation to New Particle Formation S. Zhao et al. 10.1029/2023GL106842
80. New Particle Formation Occurrence in the Urban Atmosphere of Beijing During 2013–2020 D. Shang et al. 10.1029/2022JD038334