140 citations as recorded by crossref.

1. Model of optical response of marine aerosols to Forbush decreases T. Bondo et al. 10.5194/acp-10-2765-2010
2. Seasonal variations in physical characteristics of aerosol particles at the King Sejong Station, Antarctic Peninsula J. Kim et al. 10.5194/acp-17-12985-2017
3. 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
4. Look Up: Probing the Vertical Profile of New Particle Formation and Growth in the Planetary Boundary Layer With Models and Observations S. O’Donnell et al. 10.1029/2022JD037525
5. Ion-induced cloud modulation through new particle formation and runaway cloud condensation nuclei production K. Chandrakar et al. 10.1093/oxfclm/kgae018
6. Spatial Correlation of Ultrafine Particle Number and Fine Particle Mass at Urban Scales: Implications for Health Assessment P. Saha et al. 10.1021/acs.est.0c02763
7. Lake Spray Aerosol Incorporated into Great Lakes Clouds N. Olson et al. 10.1021/acsearthspacechem.9b00258
8. 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
9. Constraints on global aerosol number concentration, SO2 and condensation sink in UKESM1 using ATom measurements A. Ranjithkumar et al. 10.5194/acp-21-4979-2021
10. Chemistry and the Linkages between Air Quality and Climate Change E. von Schneidemesser et al. 10.1021/acs.chemrev.5b00089
11. Opinion: A paradigm shift in investigating the general characteristics of atmospheric new particle formation using field observations M. Kulmala et al. 10.5194/ar-2-49-2024
12. Primary versus secondary contributions to particle number concentrations in the European boundary layer C. Reddington et al. 10.5194/acp-11-12007-2011
13. Atmospheric Nanoparticle Survivability Reduction Due to Charge‐Induced Coagulation Scavenging Enhancement N. Mahfouz & N. Donahue 10.1029/2021GL092758
14. 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
15. Exploring non-linear associations between atmospheric new-particle formation and ambient variables: a mutual information approach M. Zaidan et al. 10.5194/acp-18-12699-2018
16. Stochastic effects in H2SO4-H2O cluster growth C. Köhn et al. 10.1080/02786826.2020.1755012
17. Postfrontal nanoparticles at Cape Grim: impact on cloud nuclei concentrations J. Gras 10.1071/EN09076
18. Does the POA–SOA split matter for global CCN formation? W. Trivitayanurak & P. Adams 10.5194/acp-14-995-2014
19. Evaluation of aerosol number concentrations in NorESM with improved nucleation parameterization R. Makkonen et al. 10.5194/acp-14-5127-2014
20. Spatial and Longitudinal Distributions of Total Carbon, Nitrogen and Sulfur Together With Water‐Soluble Major Ions in Marine Aerosols Collected From the Western Pacific and Southern Ocean B. Kunwar et al. 10.1029/2022JD037874
21. Growth rates during coastal and marine new particle formation in western Ireland M. Ehn et al. 10.1029/2010JD014292
22. Model reactions and natural occurrence of furans from hypersaline environments T. Krause et al. 10.5194/bg-11-2871-2014
23. Seasonal significance of new particle formation impacts on cloud condensation nuclei at a mountaintop location N. Hirshorn et al. 10.5194/acp-22-15909-2022
24. 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
25. Semi-empirical parameterization of size-dependent atmospheric nanoparticle growth in continental environments S. Häkkinen et al. 10.5194/acp-13-7665-2013
26. Systematic satellite observations of the impact of aerosols from passive volcanic degassing on local cloud properties S. Ebmeier et al. 10.5194/acp-14-10601-2014
27. Hygroscopic Growth and Deliquescence of NaCl Nanoparticles Coated with Surfactant AOT A. Alshawa et al. 10.1021/jp809869r
28. A branch scale analytical model for predicting the vegetation collection efficiency of ultrafine particles M. Lin et al. 10.1016/j.atmosenv.2012.01.004
29. Atmospheric Particle Number Concentrations and New Particle Formation over the Southern Ocean and Antarctica: A Critical Review J. Wang et al. 10.3390/atmos14020402
30. Modelling ultrafine particle growth in a flow tube reactor M. Taylor Jr. et al. 10.5194/amt-15-4663-2022
31. 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
32. MECCO: A method to estimate concentrations of condensing organics—Description and evaluation of a Markov chain Monte Carlo application H. Vuollekoski et al. 10.1016/j.jaerosci.2010.09.004
33. The NPF Effect on CCN Number Concentrations: A Review and Re‐Evaluation of Observations From 35 Sites Worldwide J. Ren et al. 10.1029/2021GL095190
34. Observations of particle number size distributions and new particle formation in six Indian locations M. Sebastian et al. 10.5194/acp-22-4491-2022
35. Cosmic rays, clouds and climate K. Carslaw 10.1038/460332a
36. Impacts of new particle formation on aerosol cloud condensation nuclei (CCN) activity in Shanghai: case study C. Leng et al. 10.5194/acp-14-11353-2014
37. Online detection of airborne nanoparticle composition with mass spectrometry: Recent advances, challenges, and opportunities X. Li et al. 10.1016/j.trac.2023.117195
38. Formation and growth of nucleated particles into cloud condensation nuclei: model–measurement comparison D. Westervelt et al. 10.5194/acp-13-7645-2013
39. Strong air pollution causes widespread haze‐clouds over China J. Ma et al. 10.1029/2009JD013065
40. Atmospheric gas-to-particle conversion: why NPF events are observed in megacities? M. Kulmala et al. 10.1039/C6FD00257A
41. On the link between atmospheric cloud parameters and cosmic rays J. Christodoulakis et al. 10.1016/j.jastp.2019.04.012
42. Use of hydrous ABE-glycerin-diesel microemulsions in a nonroad diesel engine – Performance and unignorable emissions S. Lin et al. 10.1016/j.chemosphere.2021.133244
43. Review on main sources and impacts of urban ultrafine particles: Traffic emissions, nucleation, and climate modulation Q. Li et al. 10.1016/j.aeaoa.2023.100221
44. The synergistic role of sulfuric acid, ammonia and organics in particle formation over an agricultural land L. Dada et al. 10.1039/D3EA00065F
45. Causes and importance of new particle formation in the present‐day and preindustrial atmospheres H. Gordon et al. 10.1002/2017JD026844
46. Incorporation of new particle formation and early growth treatments into WRF/Chem: Model improvement, evaluation, and impacts of anthropogenic aerosols over East Asia C. Cai et al. 10.1016/j.atmosenv.2015.05.046
47. Rapid growth of organic aerosol nanoparticles over a wide tropospheric temperature range D. Stolzenburg et al. 10.1073/pnas.1807604115
48. 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
49. Interactions of sulfuric acid with common atmospheric bases and organic acids: Thermodynamics and implications to new particle formation Y. Li et al. 10.1016/j.jes.2020.03.033
50. Normalized Cross-Correlations of Solar Cycle and Physical Characteristics of Cloud H. Chang 10.5140/JASS.2019.36.4.225
51. Theoretical constraints on pure vapor-pressure driven condensation of organics to ultrafine particles N. Donahue et al. 10.1029/2011GL048115
52. Weak global sensitivity of cloud condensation nuclei and the aerosol indirect effect to Criegee + SO2 chemistry J. Pierce et al. 10.5194/acp-13-3163-2013
53. Approach for Measuring the Chemistry of Individual Particles in the Size Range Critical for Cloud Formation M. Zauscher et al. 10.1021/ac103152g
54. Aerosol size distribution changes in FIREX-AQ biomass burning plumes: the impact of plume concentration on coagulation and OA condensation/evaporation N. June et al. 10.5194/acp-22-12803-2022
55. How do organic vapors contribute to new-particle formation? N. Donahue et al. 10.1039/c3fd00046j
56. Quiet New Particle Formation in the Atmosphere M. Kulmala et al. 10.3389/fenvs.2022.912385
57. Characteristics of new particle formation events in a mountain semi-rural location in India J. Victor et al. 10.1016/j.atmosenv.2024.120414
58. 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
59. Suppression of nucleation mode particles by biomass burning in an urban environment: a case study E. Agus et al. 10.1039/b803871f
60. Uncertainty in global CCN concentrations from uncertain aerosol nucleation and primary emission rates J. Pierce & P. Adams 10.5194/acp-9-1339-2009
61. Cosmic rays, aerosol formation and cloud-condensation nuclei: sensitivities to model uncertainties E. Snow-Kropla et al. 10.5194/acp-11-4001-2011
62. Contribution of regional aerosol nucleation to low-level CCN in an Amazonian deep convective environment: results from a regionally nested global model X. Wang et al. 10.5194/acp-23-4431-2023
63. Effects of oligomerization and decomposition on the nanoparticle growth: a model study A. Heitto et al. 10.5194/acp-22-155-2022
64. Size-resolved aerosol emission factors and new particle formation/growth activity occurring in Mexico City during the MILAGRO 2006 Campaign A. Kalafut-Pettibone et al. 10.5194/acp-11-8861-2011
65. 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
66. 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
67. The effect of coal-fired power-plant SO2 and NOx control technologies on aerosol nucleation in the source plumes C. Lonsdale et al. 10.5194/acp-12-11519-2012
68. Size distribution and chemical composition of primary particles emitted during open biomass burning processes: Impacts on cloud condensation nuclei activation L. Chen et al. 10.1016/j.scitotenv.2019.03.419
69. Technical note: The enhancement limit of coagulation scavenging of small charged particles N. Mahfouz & N. Donahue 10.5194/acp-21-3827-2021
70. 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
71. Regional new particle formation as modulators of cloud condensation nuclei and cloud droplet number in the eastern Mediterranean P. Kalkavouras et al. 10.5194/acp-19-6185-2019
72. Rapid growth of new atmospheric particles by nitric acid and ammonia condensation M. Wang et al. 10.1038/s41586-020-2270-4
73. Low-latitude hydroclimate changes related to paleomagnetic variations during the Holocene in coastal southern China T. Zhang et al. 10.1007/s11707-022-1009-y
74. Insights on global warming J. Seinfeld 10.1002/aic.12780
75. Model for acid-base chemistry in nanoparticle growth (MABNAG) T. Yli-Juuti et al. 10.5194/acp-13-12507-2013
76. Ultrafine particles over Eastern Australia: an airborne survey W. Junkermann & J. Hacker 10.3402/tellusb.v67.25308
77. Aerosol decadal trends – Part 2: In-situ aerosol particle number concentrations at GAW and ACTRIS stations A. Asmi et al. 10.5194/acp-13-895-2013
78. A review of biomass burning: Emissions and impacts on air quality, health and climate in China J. Chen et al. 10.1016/j.scitotenv.2016.11.025
79. CCN activation of ultrafine biogenic-WSOC under restricted anthropogenic emissions: A study over eastern Himalaya in India M. Dutta et al. 10.1016/j.atmosres.2023.106704
80. Vegetation collection efficiency of ultrafine particles: From single fiber to porous media M. Lin et al. 10.1002/2013JD020917
81. Cloud condensation nuclei properties of South Asian outflow over the northern Indian Ocean during winter V. Nair et al. 10.5194/acp-20-3135-2020
82. Measurement of the nucleation of atmospheric aerosol particles M. Kulmala et al. 10.1038/nprot.2012.091
83. Temporal and spatial shifts in the chemical composition of urban coastal rainwaters of Kuwait: The role of air mass trajectory and meteorological variables D. SVV et al. 10.1016/j.scitotenv.2023.165649
84. Ion-mediated nucleation as an important global source of tropospheric aerosols F. Yu et al. 10.5194/acp-8-2537-2008
85. Parameterization of the effect of sub-grid scale aerosol dynamics on aerosol number emission rates J. Pierce et al. 10.1016/j.jaerosci.2008.11.009
86. Tropospheric aerosol microphysics simulation with assimilated meteorology: model description and intermodel comparison W. Trivitayanurak et al. 10.5194/acp-8-3149-2008
87. The roles of sulfuric acid in new particle formation and growth in the mega-city of Beijing D. Yue et al. 10.5194/acp-10-4953-2010
88. 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
89. The Progress in Electron Microscopy Studies of Particulate Matters to Be Used as a Standard Monitoring Method for Air Dust Pollution P. Sielicki et al. 10.1080/10408347.2011.607076
90. Cosmic rays, aerosols, clouds, and climate: Recent findings from the CLOUD experiment J. Pierce 10.1002/2017JD027475
91. Aerosol–cloud–precipitation interactions. Part 1. The nature and sources of cloud-active aerosols M. Andreae & D. Rosenfeld 10.1016/j.earscirev.2008.03.001
92. Size-Resolved Chemical Composition of Sub-20 nm Particles from Methanesulfonic Acid Reactions with Methylamine and Ammonia V. Perraud et al. 10.1021/acsearthspacechem.0c00120
93. Atmospheric nanoparticle growth D. Stolzenburg et al. 10.1103/RevModPhys.95.045002
94. A case study into the measurement of ship emissions from plume intercepts of the NOAA ship Miller Freeman C. Cappa et al. 10.5194/acp-14-1337-2014
95. 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
96. Decreasing particle number concentrations in a warming atmosphere and implications F. Yu et al. 10.5194/acp-12-2399-2012
97. Analysis of feedbacks between nucleation rate, survival probability and cloud condensation nuclei formation D. Westervelt et al. 10.5194/acp-14-5577-2014
98. Determination of cloud condensation nuclei production from measured new particle formation events C. Kuang et al. 10.1029/2009GL037584
99. Aerosol number size distributions over a coastal semi urban location: Seasonal changes and ultrafine particle bursts S. Babu et al. 10.1016/j.scitotenv.2016.03.246
100. Quantification of the volatility of secondary organic compounds in ultrafine particles during nucleation events J. Pierce et al. 10.5194/acp-11-9019-2011
101. The contribution of new particle formation and subsequent growth to haze formation M. Kulmala et al. 10.1039/D1EA00096A
102. 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
103. Aerosol absorption and radiative forcing P. Stier et al. 10.5194/acp-7-5237-2007
104. Atmospheric Processes and Their Controlling Influence on Cloud Condensation Nuclei Activity D. Farmer et al. 10.1021/cr5006292
105. Atmospheric nucleation: highlights of the EUCAARI project and future directions V. Kerminen et al. 10.5194/acp-10-10829-2010
106. Indirect radiative forcing by ion-mediated nucleation of aerosol F. Yu et al. 10.5194/acp-12-11451-2012
107. Sea spray aerosol in the Great Barrier Reef and the presence of nonvolatile organics M. Mallet et al. 10.1002/2016JD024966
108. Molecular dynamics simulation of the local concentration and structure in multicomponent aerosol nanoparticles under atmospheric conditions K. Karadima et al. 10.1039/C7CP02036H
109. Contribution of particle formation to global cloud condensation nuclei concentrations D. Spracklen et al. 10.1029/2007GL033038
110. New particle formation events observed at King Sejong Station, Antarctic Peninsula – Part 1: Physical characteristics and contribution to cloud condensation nuclei J. Kim et al. 10.5194/acp-19-7583-2019
111. Measurements of Aerosol Chemistry during New Particle Formation Events at a Remote Rural Mountain Site J. Creamean et al. 10.1021/es103692f
112. Iodine dioxide nucleation simulations in coastal and remote marine environments H. Vuollekoski et al. 10.1029/2008JD010713
113. Enhanced growth rate of atmospheric particles from sulfuric acid D. Stolzenburg et al. 10.5194/acp-20-7359-2020
114. 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
115. Secondary Organic Aerosol Formation Regulates Cloud Condensation Nuclei in the Global Remote Troposphere M. Liu & H. Matsui 10.1029/2022GL100543
116. Meteorological and trace gas factors affecting the number concentration of atmospheric Aitken (Dp = 50 nm) particles in the continental boundary layer: parameterization using a multivariate mixed effects model S. Mikkonen et al. 10.5194/gmd-4-1-2011
117. Atmospheric new particle formation: real and apparent growth of neutral and charged particles J. Leppä et al. 10.5194/acp-11-4939-2011
118. Will black carbon mitigation dampen aerosol indirect forcing? W. Chen et al. 10.1029/2010GL042886
119. Boundary layer nucleation as a source of new CCN in savannah environment L. Laakso et al. 10.5194/acp-13-1957-2013
120. Parameterizing the formation rate of new particles: The effect of nuclei self-coagulation T. Anttila et al. 10.1016/j.jaerosci.2010.04.008
121. 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
122. Aerosols in the Pre-industrial Atmosphere K. Carslaw et al. 10.1007/s40641-017-0061-2
123. The importance of interstitial particle scavenging by cloud droplets in shaping the remote aerosol size distribution and global aerosol-climate effects J. Pierce et al. 10.5194/acp-15-6147-2015
124. New Particle Formation and Growth to Climate‐Relevant Aerosols at a Background Remote Site in the Western Himalaya M. Sebastian et al. 10.1029/2020JD033267
125. Impact of nucleation on global CCN J. Merikanto et al. 10.5194/acp-9-8601-2009
126. 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
127. Chemically Resolved Respiratory Deposition of Ultrafine Particles Characterized by Number Concentration in the Urban Atmosphere J. Zhai et al. 10.1021/acs.est.4c03279
128. 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
129. Chemical competition in nitrate and sulfate formations and its effect on air quality H. Lei & D. Wuebbles 10.1016/j.atmosenv.2013.08.036
130. Modeling study on aerosol dynamical processes regulating new particle and CCN formation at clean continental areas T. Anttila & V. Kerminen 10.1029/2008GL033371
131. Vapors Are Lost to Walls, Not to Particles on the Wall: Artifact-Corrected Parameters from Chamber Experiments and Implications for Global Secondary Organic Aerosol K. Bilsback et al. 10.1021/acs.est.2c03967
132. A model study investigating the sensitivity of aerosol forcing to the volatilities of semi-volatile organic compounds M. Irfan et al. 10.5194/acp-24-8489-2024
133. 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
134. Improving the performance of portable aerosol size spectrometers for building dense monitoring networks Y. Li et al. 10.1039/D2EA00163B
135. Grain type and size of particulate matter from diesel vehicle exhausts analysed by transmission electron microscopy P. Sielicki et al. 10.1080/09593330.2011.646315
136. Key features of new particle formation events at background sites in China and their influence on cloud condensation nuclei X. Shen et al. 10.1007/s11783-016-0833-2
137. Can cosmic rays affect cloud condensation nuclei by altering new particle formation rates? J. Pierce & P. Adams 10.1029/2009GL037946
138. The magnitude and causes of uncertainty in global model simulations of cloud condensation nuclei L. Lee et al. 10.5194/acp-13-8879-2013
139. Understanding global secondary organic aerosol amount and size-resolved condensational behavior S. D'Andrea et al. 10.5194/acp-13-11519-2013
140. 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