150 citations as recorded by crossref.

1. Model of optical response of marine aerosols to Forbush decreases T. Bondo et al.
2. Seasonal variations in physical characteristics of aerosol particles at the King Sejong Station, Antarctic Peninsula J. Kim et al.
3. Ultrafine Particle Formation and Growth in the Upper Troposphere during the Deep Convective Clouds and Chemistry (DC3) Campaign M. Cooke et al.
4. Survival probability of new atmospheric particles: closure between theory and measurements from 1.4 to 100 nm R. Cai et al.
5. 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.
6. Ion-induced cloud modulation through new particle formation and runaway cloud condensation nuclei production K. Chandrakar et al.
7. Spatial Correlation of Ultrafine Particle Number and Fine Particle Mass at Urban Scales: Implications for Health Assessment P. Saha et al.
8. Lake Spray Aerosol Incorporated into Great Lakes Clouds N. Olson et al.
9. 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. Constraints on global aerosol number concentration, SO2 and condensation sink in UKESM1 using ATom measurements A. Ranjithkumar et al.
11. Chemistry and the Linkages between Air Quality and Climate Change E. von Schneidemesser et al.
12. Opinion: A paradigm shift in investigating the general characteristics of atmospheric new particle formation using field observations M. Kulmala et al.
13. Primary versus secondary contributions to particle number concentrations in the European boundary layer C. Reddington et al.
14. Atmospheric Nanoparticle Survivability Reduction Due to Charge‐Induced Coagulation Scavenging Enhancement N. Mahfouz & N. Donahue
15. Vertically resolved concentration and liquid water content of atmospheric nanoparticles at the US DOE Southern Great Plains site H. Chen et al.
16. Exploring non-linear associations between atmospheric new-particle formation and ambient variables: a mutual information approach M. Zaidan et al.
17. Stochastic effects in H2SO4-H2O cluster growth C. Köhn et al.
18. Does the POA–SOA split matter for global CCN formation? W. Trivitayanurak & P. Adams
19. Evaluation of aerosol number concentrations in NorESM with improved nucleation parameterization R. Makkonen et al.
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.
21. Growth rates during coastal and marine new particle formation in western Ireland M. Ehn et al.
22. Model reactions and natural occurrence of furans from hypersaline environments T. Krause et al.
23. Sensitivity of predicted ultrafine particle size distributions in Europe to different nucleation rate parameterizations using PMCAMx-UF v2.2 D. Patoulias et al.
24. Seasonal significance of new particle formation impacts on cloud condensation nuclei at a mountaintop location N. Hirshorn et al.
25. 大气气溶胶直接测量技术<bold>: </bold>光学和化学特性评论 玉. 张 & 永. 韩
26. On the relation between apparent ion and total particle growth rates in the boreal forest and related chamber experiments L. Gonzalez Carracedo et al.
27. Semi-empirical parameterization of size-dependent atmospheric nanoparticle growth in continental environments S. Häkkinen et al.
28. Systematic satellite observations of the impact of aerosols from passive volcanic degassing on local cloud properties S. Ebmeier et al.
29. Hygroscopic Growth and Deliquescence of NaCl Nanoparticles Coated with Surfactant AOT A. Alshawa et al.
30. A branch scale analytical model for predicting the vegetation collection efficiency of ultrafine particles M. Lin et al.
31. Atmospheric Particle Number Concentrations and New Particle Formation over the Southern Ocean and Antarctica: A Critical Review J. Wang et al.
32. Modelling ultrafine particle growth in a flow tube reactor M. Taylor Jr. et al.
33. Seasonal variations in composition and sources of atmospheric ultrafine particles in urban Beijing based on near-continuous measurements X. Li et al.
34. MECCO: A method to estimate concentrations of condensing organics—Description and evaluation of a Markov chain Monte Carlo application H. Vuollekoski et al.
35. The NPF Effect on CCN Number Concentrations: A Review and Re‐Evaluation of Observations From 35 Sites Worldwide J. Ren et al.
36. Observations of particle number size distributions and new particle formation in six Indian locations M. Sebastian et al.
37. Cosmic rays, clouds and climate K. Carslaw
38. Impacts of new particle formation on aerosol cloud condensation nuclei (CCN) activity in Shanghai: case study C. Leng et al.
39. Online detection of airborne nanoparticle composition with mass spectrometry: Recent advances, challenges, and opportunities X. Li et al.
40. Formation and growth of nucleated particles into cloud condensation nuclei: model–measurement comparison D. Westervelt et al.
41. Strong air pollution causes widespread haze‐clouds over China J. Ma et al.
42. Atmospheric gas-to-particle conversion: why NPF events are observed in megacities? M. Kulmala et al.
43. On the link between atmospheric cloud parameters and cosmic rays J. Christodoulakis et al.
44. Use of hydrous ABE-glycerin-diesel microemulsions in a nonroad diesel engine – Performance and unignorable emissions S. Lin et al.
45. Review on main sources and impacts of urban ultrafine particles: Traffic emissions, nucleation, and climate modulation Q. Li et al.
46. The synergistic role of sulfuric acid, ammonia and organics in particle formation over an agricultural land L. Dada et al.
47. Causes and importance of new particle formation in the present‐day and preindustrial atmospheres H. Gordon et al.
48. 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.
49. Rapid growth of organic aerosol nanoparticles over a wide tropospheric temperature range D. Stolzenburg et al.
50. Multiple new-particle growth pathways observed at the US DOE Southern Great Plains field site A. Hodshire et al.
51. Interactions of sulfuric acid with common atmospheric bases and organic acids: Thermodynamics and implications to new particle formation Y. Li et al.
52. Normalized Cross-Correlations of Solar Cycle and Physical Characteristics of Cloud H. Chang
53. Theoretical constraints on pure vapor-pressure driven condensation of organics to ultrafine particles N. Donahue et al.
54. Weak global sensitivity of cloud condensation nuclei and the aerosol indirect effect to Criegee + SO2 chemistry J. Pierce et al.
55. Approach for Measuring the Chemistry of Individual Particles in the Size Range Critical for Cloud Formation M. Zauscher et al.
56. 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.
57. How do organic vapors contribute to new-particle formation? N. Donahue et al.
58. Quiet New Particle Formation in the Atmosphere M. Kulmala et al.
59. Characteristics of new particle formation events in a mountain semi-rural location in India J. Victor et al.
60. Observation of sub-3nm particles and new particle formation at an urban location in India M. Sebastian et al.
61. Suppression of nucleation mode particles by biomass burning in an urban environment: a case study E. Agus et al.
62. Uncertainty in global CCN concentrations from uncertain aerosol nucleation and primary emission rates J. Pierce & P. Adams
63. Cosmic rays, aerosol formation and cloud-condensation nuclei: sensitivities to model uncertainties E. Snow-Kropla et al.
64. 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.
65. Effects of oligomerization and decomposition on the nanoparticle growth: a model study A. Heitto et al.
66. 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.
67. Nucleation and condensational growth to CCN sizes during a sustained pristine biogenic SOA event in a forested mountain valley J. Pierce et al.
68. Particle growth in an isoprene-rich forest: Influences of urban, wildfire, and biogenic air masses M. Gunsch et al.
69. The effect of coal-fired power-plant SO2 and NOx control technologies on aerosol nucleation in the source plumes C. Lonsdale et al.
70. Size distribution and chemical composition of primary particles emitted during open biomass burning processes: Impacts on cloud condensation nuclei activation L. Chen et al.
71. A review of anthropogenic hazardous particulate matters: general description and adsorbent materials J. Yang et al.
72. Technical note: The enhancement limit of coagulation scavenging of small charged particles N. Mahfouz & N. Donahue
73. 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.
74. Regional new particle formation as modulators of cloud condensation nuclei and cloud droplet number in the eastern Mediterranean P. Kalkavouras et al.
75. Rapid growth of new atmospheric particles by nitric acid and ammonia condensation M. Wang et al.
76. The key role of nanoparticle concentration gradient in aerosol initial growth R. Cai et al.
77. Low-latitude hydroclimate changes related to paleomagnetic variations during the Holocene in coastal southern China T. Zhang et al.
78. Insights on global warming J. Seinfeld
79. Model for acid-base chemistry in nanoparticle growth (MABNAG) T. Yli-Juuti et al.
80. Ultrafine particles over Eastern Australia: an airborne survey W. Junkermann & J. Hacker
81. Aerosol decadal trends – Part 2: In-situ aerosol particle number concentrations at GAW and ACTRIS stations A. Asmi et al.
82. A review of biomass burning: Emissions and impacts on air quality, health and climate in China J. Chen et al.
83. CCN activation of ultrafine biogenic-WSOC under restricted anthropogenic emissions: A study over eastern Himalaya in India M. Dutta et al.
84. Vegetation collection efficiency of ultrafine particles: From single fiber to porous media M. Lin et al.
85. Cloud condensation nuclei properties of South Asian outflow over the northern Indian Ocean during winter V. Nair et al.
86. Measurement of the nucleation of atmospheric aerosol particles M. Kulmala et al.
87. 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.
88. Ion-mediated nucleation as an important global source of tropospheric aerosols F. Yu et al.
89. Parameterization of the effect of sub-grid scale aerosol dynamics on aerosol number emission rates J. Pierce et al.
90. Tropospheric aerosol microphysics simulation with assimilated meteorology: model description and intermodel comparison W. Trivitayanurak et al.
91. The roles of sulfuric acid in new particle formation and growth in the mega-city of Beijing D. Yue et al.
92. The potential role of methanesulfonic acid (MSA) in aerosol formation and growth and the associated radiative forcings A. Hodshire et al.
93. 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.
94. Cosmic rays, aerosols, clouds, and climate: Recent findings from the CLOUD experiment J. Pierce
95. Aerosol–cloud–precipitation interactions. Part 1. The nature and sources of cloud-active aerosols M. Andreae & D. Rosenfeld
96. Size-Resolved Chemical Composition of Sub-20 nm Particles from Methanesulfonic Acid Reactions with Methylamine and Ammonia V. Perraud et al.
97. Atmospheric nanoparticle growth D. Stolzenburg et al.
98. A case study into the measurement of ship emissions from plume intercepts of the NOAA ship Miller Freeman C. Cappa et al.
99. New-particle formation, growth and climate-relevant particle production in Egbert, Canada: analysis from 1 year of size-distribution observations J. Pierce et al.
100. Decreasing particle number concentrations in a warming atmosphere and implications F. Yu et al.
101. Analysis of feedbacks between nucleation rate, survival probability and cloud condensation nuclei formation D. Westervelt et al.
102. Determination of cloud condensation nuclei production from measured new particle formation events C. Kuang et al.
103. Aerosol number size distributions over a coastal semi urban location: Seasonal changes and ultrafine particle bursts S. Babu et al.
104. Quantification of the volatility of secondary organic compounds in ultrafine particles during nucleation events J. Pierce et al.
105. The contribution of new particle formation and subsequent growth to haze formation M. Kulmala et al.
106. Cloud condensation nuclei production associated with atmospheric nucleation: a synthesis based on existing literature and new results V. Kerminen et al.
107. Aerosol absorption and radiative forcing P. Stier et al.
108. Atmospheric Processes and Their Controlling Influence on Cloud Condensation Nuclei Activity D. Farmer et al.
109. Atmospheric nucleation: highlights of the EUCAARI project and future directions V. Kerminen et al.
110. Indirect radiative forcing by ion-mediated nucleation of aerosol F. Yu et al.
111. Sea spray aerosol in the Great Barrier Reef and the presence of nonvolatile organics M. Mallet et al.
112. Molecular dynamics simulation of the local concentration and structure in multicomponent aerosol nanoparticles under atmospheric conditions K. Karadima et al.
113. Contribution of particle formation to global cloud condensation nuclei concentrations D. Spracklen et al.
114. 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.
115. Measurements of Aerosol Chemistry during New Particle Formation Events at a Remote Rural Mountain Site J. Creamean et al.
116. Iodine dioxide nucleation simulations in coastal and remote marine environments H. Vuollekoski et al.
117. Enhanced growth rate of atmospheric particles from sulfuric acid D. Stolzenburg et al.
118. Survival probabilities of atmospheric particles: comparison based on theory, cluster population simulations, and observations in Beijing S. Tuovinen et al.
119. Secondary Organic Aerosol Formation Regulates Cloud Condensation Nuclei in the Global Remote Troposphere M. Liu & H. Matsui
120. 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.
121. Direct measurement techniques for atmospheric aerosol: Optical and chemical properties review Y. Zhang & Y. Han
122. Atmospheric new particle formation: real and apparent growth of neutral and charged particles J. Leppä et al.
123. NPF-induced CCN enhancement over an urban location in Eastern Himalayan Foothills: A campaign-based study B. Das et al.
124. Will black carbon mitigation dampen aerosol indirect forcing? W. Chen et al.
125. The climate effects of ultrafine particles: uncertainties and future perspectives Y. Jin et al.
126. Boundary layer nucleation as a source of new CCN in savannah environment L. Laakso et al.
127. Parameterizing the formation rate of new particles: The effect of nuclei self-coagulation T. Anttila et al.
128. The potential role of organics in new particle formation and initial growth in the remote tropical upper troposphere A. Kupc et al.
129. Aerosols in the Pre-industrial Atmosphere K. Carslaw et al.
130. 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.
131. New Particle Formation and Growth to Climate‐Relevant Aerosols at a Background Remote Site in the Western Himalaya M. Sebastian et al.
132. Impact of nucleation on global CCN J. Merikanto et al.
133. Aerosol size distribution and radiative forcing response to anthropogenically driven historical changes in biogenic secondary organic aerosol formation S. D'Andrea et al.
134. UFP, BC, and PM2.5 measurements and the effect of dispersion conditions on concentration levels in a residential area affected by wood smoke pollution from domestic heating during the winter months P. Bächler et al.
135. Chemically Resolved Respiratory Deposition of Ultrafine Particles Characterized by Number Concentration in the Urban Atmosphere J. Zhai et al.
136. A diagonal volatility basis set to assess the condensation of organic vapors onto particles B. Lopez et al.
137. Size and time-resolved growth rate measurements of 1 to 5 nm freshly formed atmospheric nuclei C. Kuang et al.
138. Chemical competition in nitrate and sulfate formations and its effect on air quality H. Lei & D. Wuebbles
139. Modeling study on aerosol dynamical processes regulating new particle and CCN formation at clean continental areas T. Anttila & V. Kerminen
140. 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.
141. A model study investigating the sensitivity of aerosol forcing to the volatilities of semi-volatile organic compounds M. Irfan et al.
142. Observed coupling between air mass history, secondary growth of nucleation mode particles and aerosol pollution levels in Beijing S. Hakala et al.
143. Improving the performance of portable aerosol size spectrometers for building dense monitoring networks Y. Li et al.
144. Grain type and size of particulate matter from diesel vehicle exhausts analysed by transmission electron microscopy P. Sielicki et al.
145. Key features of new particle formation events at background sites in China and their influence on cloud condensation nuclei X. Shen et al.
146. Identification of New Particle Formation Events Using a You Only Look Once (YOLO) Deep Learning Algorithm R. Bhandari et al.
147. Can cosmic rays affect cloud condensation nuclei by altering new particle formation rates? J. Pierce & P. Adams
148. The magnitude and causes of uncertainty in global model simulations of cloud condensation nuclei L. Lee et al.
149. Understanding global secondary organic aerosol amount and size-resolved condensational behavior S. D'Andrea et al.
150. 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.