179 citations as recorded by crossref.

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4. Measured and modelled cloud condensation nuclei number concentration at the high alpine site Jungfraujoch Z. Jurányi et al. 10.5194/acp-10-7891-2010
5. Comparison of six approaches to predicting droplet activation of surface active aerosol – Part 1: moderately surface active organics​​​​​​​ S. Vepsäläinen et al. 10.5194/acp-22-2669-2022
6. Abundance and sources of hydrophilic and hydrophobic water-soluble organic carbon at an urban site in Korea in summer S. Park et al. 10.1039/C1EM10617A
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15. Effects of surface tension time-evolution for CCN activation of a complex organic surfactant J. Lin et al. 10.1039/C9EM00426B
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18. Manipulation and Characterization of Aqueous Sodium Dodecyl Sulfate/Sodium Chloride Aerosol Particles J. Buajarern et al. 10.1021/jp0764034
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23. A unified surface tension model for multi-component salt, organic, and surfactant solutions J. Kleinheins et al. 10.1039/D4CP00678J
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26. Effect of organic compounds on cloud condensation nuclei (CCN) activity of sea spray aerosol produced by bubble bursting M. Moore et al. 10.1016/j.atmosenv.2011.04.034
27. Surface Organic Monolayers Control the Hygroscopic Growth of Submicrometer Particles at High Relative Humidity C. Ruehl & K. Wilson 10.1021/jp502844g
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33. A statistical description of the evolution of cloud condensation nuclei activity during the heterogeneous oxidation of squalane and bis(2-ethylhexyl) sebacate aerosol by hydroxyl radicals C. Harmon et al. 10.1039/c3cp50347j
34. Surface-active organic matter induces salt morphology transitions during new atmospheric particle formation and growth V. Daskalakis et al. 10.1039/C5RA09187J
35. Reconciliation of measurements of hygroscopic growth and critical supersaturation of aerosol particles in central Germany M. Irwin et al. 10.5194/acp-10-11737-2010
36. Establishing the impact of model surfactants on cloud condensation nuclei activity of sea spray aerosol mimics S. Forestieri et al. 10.5194/acp-18-10985-2018
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39. A single parameter representation of hygroscopic growth and cloud condensation nucleus activity – Part 3: Including surfactant partitioning M. Petters & S. Kreidenweis 10.5194/acp-13-1081-2013
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43. Molecular composition and size distribution of sugars, sugar-alcohols and carboxylic acids in airborne particles during a severe urban haze event caused by wheat straw burning G. Wang et al. 10.1016/j.atmosenv.2011.02.045
44. Water-soluble SOA from Alkene ozonolysis: composition and droplet activation kinetics inferences from analysis of CCN activity A. Asa-Awuku et al. 10.5194/acp-10-1585-2010
45. Post-flight analysis of detailed size distributions of warm cloud droplets, as determined in situ by cloud and aerosol spectrometers S. Vâjâiac et al. 10.5194/amt-14-6777-2021
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48. On the impacts of phytoplankton-derived organic matter on the properties of the primary marine aerosol – Part 2: Composition, hygroscopicity and cloud condensation activity E. Fuentes et al. 10.5194/acp-11-2585-2011
49. Technical note: The role of evolving surface tension in the formation of cloud droplets J. Davies et al. 10.5194/acp-19-2933-2019
50. A Molecular Dynamic Study of the Effects of Surface Partitioning on the OH Radical Interactions with Solutes in Multicomponent Aqueous Aerosols T. Masaya & F. Goulay 10.1021/acs.jpca.2c07419
51. Cloud‐nucleating properties of the Amazonian biomass burning aerosol: Cloud condensation nuclei measurements and modeling A. Vestin et al. 10.1029/2006JD008104
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54. Cloud Droplet Activation of Amino Acid Aerosol Particles A. Kristensson et al. 10.1021/jp9055329
55. Surface-Area-to-Volume Ratio Determines Surface Tensions in Microscopic, Surfactant-Containing Droplets A. Bain et al. 10.1021/acscentsci.3c00998
56. Molecular dynamics simulations reveal the assembly mechanism of polysaccharides in marine aerosols L. Sun et al. 10.1039/C4CP03423F
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58. Coatings and clusters of carboxylic acids in carbon‐containing atmospheric particles from spectromicroscopy and their implications for cloud‐nucleating and optical properties S. Takahama et al. 10.1029/2009JD012622
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60. The size-resolved cloud condensation nuclei (CCN) activity and its prediction based on aerosol hygroscopicity and composition in the Pearl Delta River (PRD) region during wintertime 2014 M. Cai et al. 10.5194/acp-18-16419-2018
61. Why would apparent κ linearly change with O/C? Assessing the role of volatility, solubility, and surface activity of organic aerosols S. Nakao 10.1080/02786826.2017.1352082
62. Selected water-soluble organic compounds found in size-resolved aerosols collected from urban, mountain and marine atmospheres over East Asia G. Wang et al. 10.1111/j.1600-0889.2011.00536.x
63. Phase equilibrium of a liquid droplet formed on a solid particle J. Mitrovic 10.1016/j.ces.2006.05.013
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65. Surface Partitioning in Organic–Inorganic Mixtures Contributes to the Size-Dependence of the Phase-State of Atmospheric Nanoparticles J. Werner et al. 10.1021/acs.est.6b00789
66. Cooling Enhancement of Aerosol Particles Due to Surfactant Precipitation M. Beaver et al. 10.1021/jp102437q
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68. Atmosphärische Aerosole: Zusammensetzung, Transformation, Klima‐ und Gesundheitseffekte U. Pöschl 10.1002/ange.200501122
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77. Constraining the Effect of Surfactants on the Hygroscopic Growth of Model Sea Spray Aerosol Particles R. Bramblett & A. Frossard 10.1021/acs.jpca.2c04539
78. Cloud droplet activation of saccharides and levoglucosan particles T. Rosenørn et al. 10.1016/j.atmosenv.2005.11.024
79. Global distribution and climate forcing of marine organic aerosol: 1. Model improvements and evaluation N. Meskhidze et al. 10.5194/acp-11-11689-2011
80. Influence of selected cationic, anionic, and nonionic surfactants on hygroscopic growth of individual aqueous coarse mode aerosol particles B. Swanson & A. Frossard 10.1080/02786826.2022.2144114
81. Hygroscopic properties of Amazonian biomass burning and European background HULIS and investigation of their effects on surface tension with two models linking H-TDMA to CCNC data E. Fors et al. 10.5194/acp-10-5625-2010
82. Surface Tensions of Multicomponent Aqueous Electrolyte Solutions: Predictive Models Based on Binary Limits T. Raatikainen et al. 10.1021/jp7117136
83. Molecular Chirality and Cloud Activation Potentials of Dimeric α-Pinene Oxidation Products A. Bellcross et al. 10.1021/jacs.1c07509
84. Discontinuities in hygroscopic growth below and above water saturation for laboratory surrogates of oligomers in organic atmospheric aerosols N. Hodas et al. 10.5194/acp-16-12767-2016
85. On the contribution of Aitken mode particles to cloud droplet populations at continental background areas – a parametric sensitivity study T. Anttila & V. Kerminen 10.5194/acp-7-4625-2007
86. Hygroscopicity of Organic Compounds as a Function of Carbon Chain Length and Carboxyl, Hydroperoxy, and Carbonyl Functional Groups S. Petters et al. 10.1021/acs.jpca.7b04114
87. A simplified treatment of surfactant effects on cloud drop activation T. Raatikainen & A. Laaksonen 10.5194/gmd-4-107-2011
88. Hydration, Orientation, and Conformation of Methylglyoxal at the Air–Water Interface S. Wren et al. 10.1021/acs.jpca.5b03555
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91. An analytical solution to calculate bulk mole fractions for any number of components in aerosol droplets after considering partitioning to a surface layer D. Topping 10.5194/gmd-3-635-2010
92. A Monolayer Partitioning Scheme for Droplets of Surfactant Solutions J. Malila & N. Prisle 10.1029/2018MS001456
93. In situ aerosol measurements taken during the 2007 COPS field campaign at the Hornisgrinde ground site H. Jones et al. 10.1002/qj.727
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98. The surface tension of surfactant-containing, finite volume droplets B. Bzdek et al. 10.1073/pnas.1915660117
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103. Aerosol hygroscopicity at high (99 to 100%) relative humidities C. Ruehl et al. 10.5194/acp-10-1329-2010
104. Correlation between Surface Tension and the Bulk Dynamics in Salty Atmospheric Aquatic Droplets A. Salameh et al. 10.1021/acs.jpcc.6b01842
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106. Surface tension of mixed inorganic and dicarboxylic acid aqueous solutions at 298.15 K and their importance for cloud activation predictions A. Booth et al. 10.1039/b906849j
107. Correction of approximation errors with Random Forests applied to modelling of cloud droplet formation A. Lipponen et al. 10.5194/gmd-6-2087-2013
108. Model HULIS compounds in nanoaerosol clusters – investigations of surface tension and aggregate formation using molecular dynamics simulations T. Hede et al. 10.5194/acp-11-6549-2011
109. Size-Resolved Surface-Active Substances of Atmospheric Aerosol: Reconsideration of the Impact on Cloud Droplet Formation A. Kroflič et al. 10.1021/acs.est.8b02381
110. Water Activity from Equilibrium Molecular Dynamics Simulations and Kirkwood-Buff Theory M. Lbadaoui-Darvas & S. Takahama 10.1021/acs.jpcb.9b06735
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112. Charge State Dependence of Amino Acid Propensity at Water Surface: Mechanisms Elucidated by Molecular Dynamics Simulations R. Herboth et al. 10.1021/acs.jpca.0c10963
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115. “Effective” Negative Surface Tension:  A Property of Coated Nanoaerosols Relevant to the Atmosphere P. Chakraborty & M. Zachariah 10.1021/jp070226p
116. Strong enrichment of atmospherically relevant organic ions at the aqueous interface: the role of ion pairing and cooperative effects V. Ekholm et al. 10.1039/C8CP04525A
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123. Relationship between hygroscopicity and cloud condensation nuclei activity for urban aerosols in Tokyo M. Mochida et al. 10.1029/2005JD006980
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125. Cloud condensation nuclei activity of six pollenkitts and the influence of their surface activity N. Prisle et al. 10.5194/acp-19-4741-2019
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157. A Lagrangian particle-based numerical model for surfactant-laden droplets at macroscales M. Denys et al. 10.1063/5.0101930
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