58 citations as recorded by crossref.

1. Connecting the solubility and CCN activation of complex organic aerosols: a theoretical study using solubility distributions I. Riipinen et al. 10.5194/acp-15-6305-2015
2. Comparison of the Yield and Chemical Composition of Secondary Organic Aerosol Generated from the OH and Cl Oxidation of Decamethylcyclopentasiloxane A. Avery et al. 10.1021/acsearthspacechem.2c00304
3. Water soluble organic aerosols in indo gangetic plain (IGP): Insights from aerosol mass spectrometry A. Chakraborty et al. 10.1016/j.scitotenv.2017.05.142
4. Effect of solubility limitation on hygroscopic growth and cloud drop activation of SOA particles produced from traffic exhausts C. Wittbom et al. 10.1007/s10874-018-9380-5
5. Hygroscopicity of organic compounds as a function of organic functionality, water solubility, molecular weight, and oxidation level S. Han et al. 10.5194/acp-22-3985-2022
6. Influence of Functional Groups on Organic Aerosol Cloud Condensation Nucleus Activity S. Suda et al. 10.1021/es502147y
7. Atmospheric Processes and Their Controlling Influence on Cloud Condensation Nuclei Activity D. Farmer et al. 10.1021/cr5006292
8. Hygroscopicity of amino acids and their effect on the water uptake of ammonium sulfate in the mixed aerosol particles Q. Luo et al. 10.1016/j.scitotenv.2020.139318
9. Cloud condensation nuclei activation properties of Mediterranean pollen types considering organic chemical composition and surface tension effects A. Casans et al. 10.1016/j.atmosenv.2023.119961
10. Temperature‐ and Humidity‐Dependent Phase States of Secondary Organic Aerosols S. Petters et al. 10.1029/2018GL080563
11. A Review on Laboratory Studies and Field Measurements of Atmospheric Organic Aerosol Hygroscopicity and Its Parameterization Based on Oxidation Levels Y. Kuang et al. 10.1007/s40726-020-00164-2
12. Secondary organic aerosol formation via multiphase reaction of hydrocarbons in urban atmospheres using CAMx integrated with the UNIPAR model Z. Yu et al. 10.5194/acp-22-9083-2022
13. Polarity-Dependent Chemical Characteristics of Water-Soluble Organic Matter from Laboratory-Generated Biomass-Burning Revealed by 1-Octanol–Water Partitioning W. Lee et al. 10.1021/acs.est.9b01691
14. Processing of biomass-burning aerosol in the eastern Mediterranean during summertime A. Bougiatioti et al. 10.5194/acp-14-4793-2014
15. Atmospheric new particle formation as a source of CCN in the eastern Mediterranean marine boundary layer N. Kalivitis et al. 10.5194/acp-15-9203-2015
16. Cloud droplet activity changes of soot aerosol upon smog chamber ageing C. Wittbom et al. 10.5194/acp-14-9831-2014
17. Humidity-related failures in electronics: effect of binary mixtures of weak organic acid activators K. Piotrowska et al. 10.1007/s10854-018-9896-0
18. An inversion method for polarity distribution of atmospheric water-soluble organic matter W. Lee et al. 10.1080/02786826.2020.1795482
19. Characteristics of Scanning Flow Condensation Particle Counter (SFCPC): A rapid approach for retrieving hygroscopicity and chemical composition of sub-10 nm aerosol particles K. Zhang et al. 10.1080/02786826.2023.2245859
20. Comparison of secondary organic aerosol generated from the oxidation of laboratory precursors by hydroxyl radicals, chlorine atoms, and bromine atoms in an oxidation flow reactor A. Lambe et al. 10.1039/D2EA00018K
21. Oxidative potential of secondary organic aerosols produced from photooxidation of different hydrocarbons using outdoor chamber under ambient sunlight H. Jiang et al. 10.1016/j.atmosenv.2016.02.016
22. 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
23. Liquid–liquid phase separation in atmospherically relevant particles consisting of organic species and inorganic salts Y. You et al. 10.1080/0144235X.2014.890786
24. Reconsideration of surface tension and phase state effects on cloud condensation nuclei activity based on the atomic force microscopy measurement C. Xiong et al. 10.5194/acp-22-16123-2022
25. An interfacial mechanism for cloud droplet formation on organic aerosols C. Ruehl et al. 10.1126/science.aad4889
26. Surface Organic Monolayers Control the Hygroscopic Growth of Submicrometer Particles at High Relative Humidity C. Ruehl & K. Wilson 10.1021/jp502844g
27. Technical note: The role of evolving surface tension in the formation of cloud droplets J. Davies et al. 10.5194/acp-19-2933-2019
28. Characterization and sources of water-soluble organic species in PM2.5 in a remote mountain environment in Southeastern China J. Tao et al. 10.1016/j.atmosenv.2023.120057
29. Gas-Phase Nitrate Radical Production Using Irradiated Ceric Ammonium Nitrate: Insights into Secondary Organic Aerosol Formation from Biogenic and Biomass Burning Precursors A. Lambe et al. 10.1021/acsearthspacechem.4c00293
30. Resolving the mechanisms of hygroscopic growth and cloud condensation nuclei activity for organic particulate matter P. Liu et al. 10.1038/s41467-018-06622-2
31. Technical note: Quantified organic aerosol subsaturated hygroscopicity by a simple optical scatter monitor system through field measurements J. Zhang et al. 10.5194/acp-24-13445-2024
32. Prediction of cloud condensation nuclei activity for organic compounds using functional group contribution methods M. Petters et al. 10.5194/gmd-9-111-2016
33. Hygroscopicity, CCN and volatility properties of submicron atmospheric aerosol in a boreal forest environment during the summer of 2010 J. Hong et al. 10.5194/acp-14-4733-2014
34. Predicting charge density distribution of materials using a local-environment-based graph convolutional network S. Gong et al. 10.1103/PhysRevB.100.184103
35. Cloud droplet activation of secondary organic aerosol is mainly controlled by molecular weight, not water solubility J. Wang et al. 10.5194/acp-19-941-2019
36. Accounting for Cloud Nucleation Activation Mechanism of Secondary Organic Matter from α-Pinene Oxidation Using Experimentally Retrieved Water Solubility Distributions W. Lee et al. 10.1021/acs.est.3c03039
37. Ultraviolet Irradiation Can Increase the Light Absorption and Viscosity of Primary Brown Carbon from Biomass Burning H. Al-Mashala et al. 10.1021/acsearthspacechem.3c00155
38. 1-octanol-water partitioning as a classifier of water soluble organic matters: Implication for solubility distribution M. Kuwata & W. Lee 10.1080/02786826.2017.1283004
39. Water Solubility Distribution of Organic Matter Accounts for the Discrepancy in Hygroscopicity among Sub- and Supersaturated Humidity Regimes W. Lee et al. 10.1021/acs.est.2c04647
40. Liquid–Liquid Phase Separation Can Drive Aerosol Droplet Growth in Supersaturated Regimes K. Malek et al. 10.1021/acsenvironau.3c00015
41. Simulation of aromatic SOA formation using the lumping model integrated with explicit gas-phase kinetic mechanisms and aerosol-phase reactions Y. Im et al. 10.5194/acp-14-4013-2014
42. Hygroscopicity of aerosol particles and CCN activity of nearly hydrophobic particles in the urban atmosphere over Japan during summer S. Ogawa et al. 10.1002/2015JD024636
43. Relative-humidity-dependent organic aerosol thermodynamics via an efficient reduced-complexity model K. Gorkowski et al. 10.5194/acp-19-13383-2019
44. No-Clean Solder Flux Chemistry and Temperature Effects on Humidity-Related Reliability of Electronics K. Piotrowska et al. 10.1007/s11664-018-06862-4
45. Offline analysis of the chemical composition and hygroscopicity of submicrometer aerosol at an Asian outflow receptor site and comparison with online measurements Y. Deng et al. 10.5194/acp-22-5515-2022
46. Hygroscopicity of Organic Aerosols and Their Contributions to CCN Concentrations Over a Midlatitude Forest in Japan Y. Deng et al. 10.1029/2017JD027292
47. Emerging investigator series: aqueous photooxidation of live bacteria with hydroxyl radicals under cloud-like conditions: insights into the production and transformation of biological and organic matter originating from bioaerosols Y. Liu et al. 10.1039/D3EM00090G
48. Simulating the SOA formation of isoprene from partitioning and aerosol phase reactions in the presence of inorganics R. Beardsley & M. Jang 10.5194/acp-16-5993-2016
49. Organic Peroxides in Aerosol: Key Reactive Intermediates for Multiphase Processes in the Atmosphere S. Wang et al. 10.1021/acs.chemrev.2c00430
50. Hygroscopicity of nitrogen-containing organic carbon compounds: o-aminophenol and p-aminophenol K. Malek et al. 10.1039/D2EM00163B
51. 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
52. Relationships of the Hygroscopicity of HULIS With Their Degrees of Oxygenation and Sources in the Urban Atmosphere R. Zhou et al. 10.1029/2022JD037163
53. Exploring the relationship between personal exposure to multiple water-soluble components and ROS in size-resolved PMs in solid fuel combustion households B. Zhang et al. 10.1016/j.envpol.2024.125075
54. Measurement report: Cloud condensation nuclei activity and its variation with organic oxidation level and volatility observed during an aerosol life cycle intensive operational period (ALC-IOP) F. Mei et al. 10.5194/acp-21-13019-2021
55. Aerosol Properties Observed in the Subtropical North Pacific Boundary Layer T. Royalty et al. 10.1002/2017JD026897
56. 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
57. An interfacial mechanism for cloud droplet formation on organic aerosols C. Ruehl et al. 10.1126/science.aad4889
58. Toward the Determination of Joint Volatility-Hygroscopicity Distributions: Development and Response Characterization for Single-Component Aerosol K. Cerully et al. 10.1080/02786826.2013.870326