171 citations as recorded by crossref.

1. The importance of vertical velocity variability for estimates of the indirect aerosol effects R. West et al. 10.5194/acp-14-6369-2014
2. Aerosol indirect effects in a multi-scale aerosol-climate model PNNL-MMF M. Wang et al. 10.5194/acp-11-5431-2011
3. Continuous flow hygroscopicity-resolved relaxed eddy accumulation (Hy-Res REA) method of measuring size-resolved sodium chloride particle fluxes N. Meskhidze et al. 10.1080/02786826.2017.1423174
4. Global Modeling of Secondary Organic Aerosol With Organic Nucleation J. Zhu & J. Penner 10.1029/2019JD030414
5. Ion–Molecule Rate Constants for Reactions of Sulfuric Acid with Acetate and Nitrate Ions S. Fomete et al. 10.1021/acs.jpca.2c02072
6. Characterization of particle number size distribution and new particle formation in an urban environment in Lanzhou, China X. Zhang et al. 10.1016/j.jaerosci.2016.10.010
7. Gain Insight into Chemical Components Driving New Particle Growth on a Basis of Particle Hygroscopicity and Volatility Measurements: a Short Review Z. Wu 10.1007/s40726-017-0064-6
8. Impact of sub-grid particle formation in sulfur-rich plumes on particle mass and number concentrations over China Y. Wei et al. 10.1016/j.atmosenv.2021.118711
9. Frequent new particle formation at remote sites in the subboreal forest of North America M. Andreae et al. 10.5194/acp-22-2487-2022
10. Global distribution and climate forcing of marine organic aerosol: 1. Model improvements and evaluation N. Meskhidze et al. 10.5194/acp-11-11689-2011
11. Investigation on semi-direct and indirect climate effects of fossil fuel black carbon aerosol over China B. Zhuang et al. 10.1007/s00704-013-0862-8
12. Sensitivity of the Aerosol Indirect Effect to Subgrid Variability in the Cloud Parameterization of the GFDL Atmosphere General Circulation Model AM3 J. Golaz et al. 10.1175/2010JCLI3945.1
13. Wind speed dependent size-resolved parameterization for the organic mass fraction of sea spray aerosol B. Gantt et al. 10.5194/acp-11-8777-2011
14. Radiative forcing of organic aerosol in the atmosphere and on snow: Effects of SOA and brown carbon G. Lin et al. 10.1002/2013JD021186
15. Representation of nucleation mode microphysics in a global aerosol model with sectional microphysics Y. Lee et al. 10.5194/gmd-6-1221-2013
16. Gas-phase alkylamines in a boreal Scots pine forest air A. Kieloaho et al. 10.1016/j.atmosenv.2013.08.019
17. Constraining cloud droplet number concentration in GCMs suppresses the aerosol indirect effect C. Hoose et al. 10.1029/2009GL038568
18. Primary versus secondary contributions to particle number concentrations in the European boundary layer C. Reddington et al. 10.5194/acp-11-12007-2011
19. The role of organic condensation on ultrafine particle growth during nucleation events D. Patoulias et al. 10.5194/acp-15-6337-2015
20. Vertical profiles of droplet effective radius in shallow convective clouds S. Zhang et al. 10.5194/acp-11-4633-2011
21. Secondary new particle formation in Northern Finland Pallas site between the years 2000 and 2010 E. Asmi et al. 10.5194/acp-11-12959-2011
22. Cirrus clouds in a global climate model with a statistical cirrus cloud scheme M. Wang & J. Penner 10.5194/acp-10-5449-2010
23. Measurements of sub-3 nm particles using a particle size magnifier in different environments: from clean mountain top to polluted megacities J. Kontkanen et al. 10.5194/acp-17-2163-2017
24. Past, present, and future of ultrafine particle exposures in North America A. Presto et al. 10.1016/j.aeaoa.2021.100109
25. Comprehensive modelling study on observed new particle formation at the SORPES station in Nanjing, China X. Huang et al. 10.5194/acp-16-2477-2016
26. 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
27. Explaining global surface aerosol number concentrations in terms of primary emissions and particle formation D. Spracklen et al. 10.5194/acp-10-4775-2010
28. 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
29. A simple model of global aerosol indirect effects S. Ghan et al. 10.1002/jgrd.50567
30. Responses of ocean biogeochemistry to atmospheric supply of lithogenic and pyrogenic iron-containing aerosols A. Ito et al. 10.1017/S0016756819001080
31. H<sub>2</sub>SO<sub>4</sub>–H<sub>2</sub>O binary and H<sub>2</sub>SO<sub>4</sub>–H<sub>2</sub>O–NH<sub>3</sub> ternary homogeneous and ion-mediated nucleation: lookup tables version 1.0 for 3-D modeling application F. Yu et al. 10.5194/gmd-13-2663-2020
32. Thermodynamic properties of nanoparticles during new particle formation events in the atmosphere of North China Plain Z. Wu et al. 10.1016/j.atmosres.2017.01.007
33. Radiative Forcing Associated with Particulate Carbon Emissions Resulting from the Use of Mercury Control Technology G. Lin et al. 10.1021/es502382h
34. Hygroscopicity and chemical composition of Antarctic sub-micrometre aerosol particles and observations of new particle formation E. Asmi et al. 10.5194/acp-10-4253-2010
35. Aerosol indirect effects – general circulation model intercomparison and evaluation with satellite data J. Quaas et al. 10.5194/acp-9-8697-2009
36. Parametric sensitivity analysis of precipitation at global and local scales in the Community Atmosphere Model CAM5 Y. Qian et al. 10.1002/2014MS000354
37. Impact of temperature dependence on the possible contribution of organics to new particle formation in the atmosphere F. Yu et al. 10.5194/acp-17-4997-2017
38. The first estimates of global nucleation mode aerosol concentrations based on satellite measurements M. Kulmala et al. 10.5194/acp-11-10791-2011
39. Processes controlling the annual cycle of Arctic aerosol number and size distributions B. Croft et al. 10.5194/acp-16-3665-2016
40. A tutorial guide on new particle formation experiments using a laminar flow reactor S. Fomete et al. 10.1016/j.jaerosci.2021.105808
41. From aerosol-limited to invigoration of warm convective clouds I. Koren et al. 10.1126/science.1252595
42. Lightning Discharges, Cosmic Rays and Climate S. Kumar et al. 10.1007/s10712-018-9469-z
43. Spatial and temporal variations of new particle formation in East Asia using an NPF‐explicit WRF‐chem model: North‐south contrast in new particle formation frequency H. Matsui et al. 10.1002/jgrd.50821
44. Ultrafine particles over Eastern Australia: an airborne survey W. Junkermann & J. Hacker 10.3402/tellusb.v67.25308
45. Anthropogenic contribution to cloud condensation nuclei and the first aerosol indirect climate effect F. Yu et al. 10.1088/1748-9326/8/2/024029
46. Analysis of nucleation events in the European boundary layer using the regional aerosol–climate model REMO-HAM with a solar radiation-driven OH-proxy J. Pietikäinen et al. 10.5194/acp-14-11711-2014
47. Decadal simulation and comprehensive evaluation of CESM/CAM5.1 with advanced chemistry, aerosol microphysics, and aerosol‐cloud interactions J. He et al. 10.1002/2014MS000360
48. Global simulations of nitrate and ammonium aerosols and their radiative effects L. Xu & J. Penner 10.5194/acp-12-9479-2012
49. Nucleation and growth of sulfate aerosol in coal-fired power plant plumes: sensitivity to background aerosol and meteorology R. Stevens et al. 10.5194/acp-12-189-2012
50. The Emissions Model Intercomparison Project (Emissions-MIP): quantifying model sensitivity to emission characteristics H. Ahsan et al. 10.5194/acp-23-14779-2023
51. Comparison of a global-climate model simulation to a cloud-system resolving model simulation for long-term thin stratocumulus clouds S. Lee et al. 10.5194/acp-9-6497-2009
52. Formation and growth of nucleated particles into cloud condensation nuclei: model–measurement comparison D. Westervelt et al. 10.5194/acp-13-7645-2013
53. Simulation of the size-composition distribution of atmospheric nanoparticles over Europe D. Patoulias et al. 10.5194/acp-18-13639-2018
54. Indirect radiative forcing by ion-mediated nucleation of aerosol F. Yu et al. 10.5194/acp-12-11451-2012
55. Oceanic Dimethyl Sulfide Emission and New Particle Formation around the Coast of Antarctica: A Modeling Study of Seasonal Variations and Comparison with Measurements F. Yu & G. Luo 10.3390/atmos1010034
56. Radiative forcing of the direct aerosol effect from AeroCom Phase II simulations G. Myhre et al. 10.5194/acp-13-1853-2013
57. Regional and global modeling of aerosol optical properties with a size, composition, and mixing state resolved particle microphysics model F. Yu et al. 10.5194/acp-12-5719-2012
58. Effect of Prudhoe Bay emissions on atmospheric aerosol growth events observed in Utqiaġvik (Barrow), Alaska K. Kolesar et al. 10.1016/j.atmosenv.2016.12.019
59. Atmospheric nucleation: highlights of the EUCAARI project and future directions V. Kerminen et al. 10.5194/acp-10-10829-2010
60. Causes and importance of new particle formation in the present‐day and preindustrial atmospheres H. Gordon et al. 10.1002/2017JD026844
61. 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
62. 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
63. The contribution of plume-scale nucleation to global and regional aerosol and CCN concentrations: evaluation and sensitivity to emissions changes R. Stevens & J. Pierce 10.5194/acp-14-13661-2014
64. Aerosol effects on liquid‐water path of thin stratocumulus clouds S. Lee et al. 10.1029/2008JD010513
65. Global cloud condensation nuclei influenced by carbonaceous combustion aerosol D. Spracklen et al. 10.5194/acp-11-9067-2011
66. On the influence of VOCs on new particle growth in a Continental-Mediterranean region F. Gómez-Moreno et al. 10.1088/2515-7620/acacf0
67. Spatial distributions of particle number concentrations in the global troposphere: Simulations, observations, and implications for nucleation mechanisms F. Yu et al. 10.1029/2009JD013473
68. New particle formation induced by anthropogenic–biogenic interactions on the southeastern Tibetan Plateau S. Lai et al. 10.5194/acp-24-2535-2024
69. 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
70. Uncertainty in global CCN concentrations from uncertain aerosol nucleation and primary emission rates J. Pierce & P. Adams 10.5194/acp-9-1339-2009
71. Weak global sensitivity of cloud condensation nuclei and the aerosol indirect effect to Criegee + SO<sub>2</sub> chemistry J. Pierce et al. 10.5194/acp-13-3163-2013
72. 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
73. Observation of new particle formation over a mid-latitude forest facing the North Pacific Y. Han et al. 10.1016/j.atmosenv.2012.09.036
74. Challenges in constraining anthropogenic aerosol effects on cloud radiative forcing using present-day spatiotemporal variability S. Ghan et al. 10.1073/pnas.1514036113
75. 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
76. High Sensitivity of Arctic Black Carbon Radiative Effects to Subgrid Vertical Velocity in Aerosol Activation H. Matsui & N. Moteki 10.1029/2020GL088978
77. Radiative forcing of anthropogenic aerosols on cirrus clouds using a hybrid ice nucleation scheme J. Zhu & J. Penner 10.5194/acp-20-7801-2020
78. 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
79. 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
80. Global modeling of SOA formation from dicarbonyls, epoxides, organic nitrates and peroxides G. Lin et al. 10.5194/acp-12-4743-2012
81. Impact of anthropogenic absorbing aerosols on clouds and precipitation: A review of recent progresses C. Wang 10.1016/j.atmosres.2012.11.005
82. Aerosol nucleation and its role for clouds and Earth's radiative forcing in the aerosol-climate model ECHAM5-HAM J. Kazil et al. 10.5194/acp-10-10733-2010
83. Infrequent occurrence of new particle formation at a semi-rural location, Gadanki, in tropical Southern India V. Kanawade et al. 10.1016/j.atmosenv.2014.05.046
84. Ground-based observation of clusters and nucleation-mode particles in the Amazon D. Wimmer et al. 10.5194/acp-18-13245-2018
85. A parameterization of sub-grid particle formation in sulfur-rich plumes for global- and regional-scale models R. Stevens & J. Pierce 10.5194/acp-13-12117-2013
86. The effect of coal-fired power-plant SO<sub>2</sub> and NO<sub>x</sub> control technologies on aerosol nucleation in the source plumes C. Lonsdale et al. 10.5194/acp-12-11519-2012
87. Sensitivity of global cloud condensation nuclei concentrations to primary sulfate emission parameterizations G. Luo & F. Yu 10.5194/acp-11-1949-2011
88. Air pollution control and decreasing new particle formation lead to strong climate warming R. Makkonen et al. 10.5194/acp-12-1515-2012
89. Decreasing particle number concentrations in a warming atmosphere and implications F. Yu et al. 10.5194/acp-12-2399-2012
90. Seasonal cycle and modal structure of particle number size distribution at Dome C, Antarctica E. Järvinen et al. 10.5194/acp-13-7473-2013
91. Global atmospheric particle formation from CERN CLOUD measurements E. Dunne et al. 10.1126/science.aaf2649
92. On the formation of sulphuric acid – amine clusters in varying atmospheric conditions and its influence on atmospheric new particle formation P. Paasonen et al. 10.5194/acp-12-9113-2012
93. Peroxy radical kinetics and new particle formation M. Schervish & N. Donahue 10.1039/D0EA00017E
94. ARM-Led Improvements in Aerosols in Climate and Climate Models S. Ghan & J. Penner 10.1175/AMSMONOGRAPHS-D-15-0033.1
95. Towards understanding the characteristics of new particle formation in the Eastern Mediterranean R. Baalbaki et al. 10.5194/acp-21-9223-2021
96. New Mechanistic Pathways for the Reactions of Formaldehyde with Formic Acid Catalyzed by Sulfuric Acid and Formaldehyde with Sulfuric Acid Catalyzed by Formic Acid: Formation of Potential Secondary Organic Aerosol Precursors J. Liu et al. 10.1021/acsearthspacechem.1c00002
97. Particle Formation in a Complex Environment D. Dominick et al. 10.3390/atmos10050275
98. Gas-phase alkyl amines in urban air; comparison with a boreal forest site and importance for local atmospheric chemistry H. Hellén et al. 10.1016/j.atmosenv.2014.05.029
99. Spatial extension of nucleating air masses in the Carpathian Basin Z. Németh & I. Salma 10.5194/acp-14-8841-2014
100. High concentrations of sub-3nm clusters and frequent new particle formation observed in the Po Valley, Italy, during the PEGASOS 2012 campaign J. Kontkanen et al. 10.5194/acp-16-1919-2016
101. Atmospheric nanoparticle growth D. Stolzenburg et al. 10.1103/RevModPhys.95.045002
102. 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
103. Intra-urban variability of particulate matter (PM2.5 and PM10) and its relationship with optical properties of aerosols over Delhi, India S. Tiwari et al. 10.1016/j.atmosres.2015.07.007
104. Impact of new particle formation on the concentrations of aerosols and cloud condensation nuclei around Beijing H. Matsui et al. 10.1029/2011JD016025
105. Estimating the contribution of ion–ion recombination to sub-2 nm cluster concentrations from atmospheric measurements J. Kontkanen et al. 10.5194/acp-13-11391-2013
106. Composition of 15–85 nm particles in marine air M. Lawler et al. 10.5194/acp-14-11557-2014
107. Spaceborne observations of the lidar ratio of marine aerosols K. Dawson et al. 10.5194/acp-15-3241-2015
108. Satellite methods underestimate indirect climate forcing by aerosols J. Penner et al. 10.1073/pnas.1018526108
109. Quantification of the volatility of secondary organic compounds in ultrafine particles during nucleation events J. Pierce et al. 10.5194/acp-11-9019-2011
110. Coupled IMPACT aerosol and NCAR CAM3 model: Evaluation of predicted aerosol number and size distribution M. Wang et al. 10.1029/2008JD010459
111. Less atmospheric radiative heating by dust due to the synergy of coarser size and aspherical shape A. Ito et al. 10.5194/acp-21-16869-2021
112. Host model uncertainties in aerosol radiative forcing estimates: results from the AeroCom Prescribed intercomparison study P. Stier et al. 10.5194/acp-13-3245-2013
113. Impact of Quantum Chemistry Parameter Choices and Cluster Distribution Model Settings on Modeled Atmospheric Particle Formation Rates V. Besel et al. 10.1021/acs.jpca.0c03984
114. Anthropogenic Aerosol Indirect Effects in Cirrus Clouds J. Penner et al. 10.1029/2018JD029204
115. Improvement and further development in CESM/CAM5: gas-phase chemistry and inorganic aerosol treatments J. He & Y. Zhang 10.5194/acp-14-9171-2014
116. Seasonal characteristics of PM1, PM2.5, and PM10 over Varanasi during 2019–2020 P. Chauhan et al. 10.3389/frsc.2022.909351
117. Seasonal variation of CCN concentrations and aerosol activation properties in boreal forest S. Sihto et al. 10.5194/acp-11-13269-2011
118. Comparison of a global-climate model to a cloud-system resolving model for the long-term response of thin stratocumulus clouds to preindustrial and present-day aerosol conditions S. Lee & J. Penner 10.5194/acp-10-6371-2010
119. Diurnal and Seasonal Variations of Ultrafine Particle Formation in Anthropogenic SO2Plumes F. Yu 10.1021/es903228a
120. 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
121. Impact of parametric uncertainties on the present-day climate and on the anthropogenic aerosol effect U. Lohmann & S. Ferrachat 10.5194/acp-10-11373-2010
122. What controls the observed size-dependency of the growth rates of sub-10 nm atmospheric particles? J. Kontkanen et al. 10.1039/D1EA00103E
123. 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
124. Decrease in radiative forcing by organic aerosol nucleation, climate, and land use change J. Zhu et al. 10.1038/s41467-019-08407-7
125. Effects of boundary layer particle formation on cloud droplet number and changes in cloud albedo from 1850 to 2000 J. Merikanto et al. 10.5194/acp-10-695-2010
126. Aerosol Properties Observed in the Subtropical North Pacific Boundary Layer T. Royalty et al. 10.1002/2017JD026897
127. Chemistry of Atmospheric Nucleation: On the Recent Advances on Precursor Characterization and Atmospheric Cluster Composition in Connection with Atmospheric New Particle Formation M. Kulmala et al. 10.1146/annurev-physchem-040412-110014
128. Characterization of ultrafine particle number concentration and new particle formation in an urban environment of Taipei, Taiwan H. Cheung et al. 10.5194/acp-13-8935-2013
129. Total aerosol effect: radiative forcing or radiative flux perturbation? U. Lohmann et al. 10.5194/acp-10-3235-2010
130. Temperature effects on sulfuric acid aerosol nucleation and growth: initial results from the TANGENT study L. Tiszenkel et al. 10.5194/acp-19-8915-2019
131. The multi-scale aerosol-climate model PNNL-MMF: model description and evaluation M. Wang et al. 10.5194/gmd-4-137-2011
132. Simulation of the effects of low-volatility organic compounds on aerosol number concentrations in Europe D. Patoulias & S. Pandis 10.5194/acp-22-1689-2022
133. Aerosol physicochemical effects on CCN activation simulated with the chemistry-climate model EMAC D. Chang et al. 10.1016/j.atmosenv.2017.03.036
134. BVOC-aerosol-climate interactions in the global aerosol-climate model ECHAM5.5-HAM2 R. Makkonen et al. 10.5194/acp-12-10077-2012
135. Spring and summer contrast in new particle formation over nine forest areas in North America F. Yu et al. 10.5194/acp-15-13993-2015
136. Composition and temporal behavior of ambient ions in the boreal forest M. Ehn et al. 10.5194/acp-10-8513-2010
137. Molecular Composition and Volatility of Nucleated Particles from α-Pinene Oxidation between −50 °C and +25 °C Q. Ye et al. 10.1021/acs.est.9b03265
138. Boundary layer nucleation as a source of new CCN in savannah environment L. Laakso et al. 10.5194/acp-13-1957-2013
139. Emission Reductions Significantly Reduce the Hemispheric Contrast in Cloud Droplet Number Concentration in Recent Two Decades Y. Cao et al. 10.1029/2022JD037417
140. Experimental and Theoretical Study on the Enhancement of Alkanolamines on Sulfuric Acid Nucleation S. Fomete et al. 10.1021/acs.jpca.2c01672
141. Impact of nucleation on global CCN J. Merikanto et al. 10.5194/acp-9-8601-2009
142. 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
143. CESM/CAM5 improvement and application: comparison and evaluation of updated CB05_GE and MOZART-4 gas-phase mechanisms and associated impacts on global air quality and climate J. He et al. 10.5194/gmd-8-3999-2015
144. Oxidation of SO<sub>2</sub> by stabilized Criegee intermediate (sCI) radicals as a crucial source for atmospheric sulfuric acid concentrations M. Boy et al. 10.5194/acp-13-3865-2013
145. 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
146. 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
147. Parameterizing the formation rate of new particles: The effect of nuclei self-coagulation T. Anttila et al. 10.1016/j.jaerosci.2010.04.008
148. Aerosol forcing based on CAM5 and AM3 meteorological fields C. Zhou et al. 10.5194/acp-12-9629-2012
149. Unexpectedly acidic nanoparticles formed in dimethylamine–ammonia–sulfuric-acid nucleation experiments at CLOUD M. Lawler et al. 10.5194/acp-16-13601-2016
150. Parameterizing cloud condensation nuclei concentrations during HOPE L. Hande et al. 10.5194/acp-16-12059-2016
151. Analysis of feedbacks between nucleation rate, survival probability and cloud condensation nuclei formation D. Westervelt et al. 10.5194/acp-14-5577-2014
152. Simulation of particle size distribution with a global aerosol model: contribution of nucleation to aerosol and CCN number concentrations F. Yu & G. Luo 10.5194/acp-9-7691-2009
153. Limited Role of Malonic Acid in Sulfuric Acid–Dimethylamine New Particle Formation S. Fomete et al. 10.1021/acsomega.3c01643
154. Simulation of particle formation and number concentration over the Eastern United States with the WRF-Chem + APM model G. Luo & F. Yu 10.5194/acp-11-11521-2011
155. The influence of marine environment on the conservation state of Built Heritage: An overview study H. Morillas et al. 10.1016/j.scitotenv.2020.140899
156. Exploring the effect of waterbodies coupled with other environmental parameters to model PM2.5 over Delhi-NCT in northwest India B. Gayen et al. 10.1016/j.apr.2022.101614
157. Atmospheric sub-3 nm particles at high altitudes S. Mirme et al. 10.5194/acp-10-437-2010
158. Characterization of aerosol size distributions and chemical compositions under strong wind and stagnant conditions during haze episodes in Lin’an, China S. Shuangshuang et al. 10.1007/s11869-019-00752-2
159. The influence of marine microbial activities on aerosol production: A laboratory mesocosm study P. Alpert et al. 10.1002/2015JD023469
160. 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
161. Nucleation and Growth of Nanoparticles in the Atmosphere R. Zhang et al. 10.1021/cr2001756
162. Enhanced organic mass fraction and decreased hygroscopicity of cloud condensation nuclei (CCN) during new particle formation events U. Dusek et al. 10.1029/2009GL040930
163. Fast time response measurements of particle size distributions in the 3–60 nm size range with the nucleation mode aerosol size spectrometer C. Williamson et al. 10.5194/amt-11-3491-2018
164. Droplet nucleation: Physically-based parameterizations and comparative evaluation S. Ghan et al. 10.1029/2011MS000074
165. Understanding global secondary organic aerosol amount and size-resolved condensational behavior S. D'Andrea et al. 10.5194/acp-13-11519-2013
166. On radiative forcing of sulphate aerosol produced from ion-promoted nucleation mechanisms in an atmospheric global model H. Fatima et al. 10.1007/s00703-011-0138-8
167. Description and evaluation of a secondary organic aerosol and new particle formation scheme within TM5-MP v1.2 T. Bergman et al. 10.5194/gmd-15-683-2022
168. 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
169. Hygroscopicity and cloud condensation nucleus activity of forest aerosol particles during summer in Wakayama, Japan K. Kawana et al. 10.1002/2016JD025660
170. The Role of Binary and Ion Nucleation of Sulfuric Acid and Water Vapor in the Dynamics of Sulfate Aerosol Formation in the Atmosphere A. Aloyan et al. 10.3103/S1068373921010052
171. Aerosol-induced modification of organised convection and top-of-atmosphere radiation N. Nishant et al. 10.1038/s41612-019-0089-1