39 citations as recorded by crossref.

1. Review of Smog Chamber Research Trends J. Kim et al.
2. Characteristics of PM2.5 hygroscopicity and the influences of water-soluble ions during haze events in Beijing S. Ge et al.
3. Formation and aging of secondary organic aerosol from toluene: changes in chemical composition, volatility, and hygroscopicity L. Hildebrandt Ruiz et al.
4. Cloud droplet activation of secondary organic aerosol is mainly controlled by molecular weight, not water solubility J. Wang et al.
5. STRAPS v1.0: evaluating a methodology for predicting electron impact ionisation mass spectra for the aerosol mass spectrometer D. Topping et al.
6. Introductory lecture: atmospheric chemistry in the Anthropocene B. Finlayson-Pitts
7. Contrasting Influence of Nitrogen Oxides on the Cloud Condensation Nuclei Activity of Monoterpene‐Derived Secondary Organic Aerosol in Daytime and Nighttime Oxidation C. Zhang et al.
8. Aging of secondary organic aerosol generated from the ozonolysis of α-pinene: effects of ozone, light and temperature C. Denjean et al.
9. Mapping gas-phase organic reactivity and concomitant secondary organic aerosol formation: chemometric dimension reduction techniques for the deconvolution of complex atmospheric data sets K. Wyche et al.
10. Chemistry and the Linkages between Air Quality and Climate Change E. von Schneidemesser et al.
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.
12. Secondary organic aerosol from VOC mixtures in an oxidation flow reactor E. Ahlberg et al.
13. Cloud condensation nuclei activity, droplet growth kinetics, and hygroscopicity of biogenic and anthropogenic secondary organic aerosol (SOA) D. Zhao et al.
14. Characterization of Aerosol Hygroscopicity Over the Northeast Pacific Ocean: Impacts on Prediction of CCN and Stratocumulus Cloud Droplet Number Concentrations B. Schulze et al.
15. Hygroscopicity and CCN activity of atmospheric aerosol particles and their relation to organics: Characteristics of urban aerosols in Nagoya, Japan K. Kawana et al.
16. Why would apparent κ linearly change with O/C? Assessing the role of volatility, solubility, and surface activity of organic aerosols S. Nakao
17. Water uptake of subpollen aerosol particles: hygroscopic growth, cloud condensation nuclei activation, and liquid–liquid phase separation E. Mikhailov et al.
18. Surface Organic Monolayers Control the Hygroscopic Growth of Submicrometer Particles at High Relative Humidity C. Ruehl & K. Wilson
19. On the implications of aerosol liquid water and phase separation for organic aerosol mass H. Pye et al.
20. Emissions of biogenic volatile organic compounds and subsequent photochemical production of secondary organic aerosol in mesocosm studies of temperate and tropical plant species K. Wyche et al.
21. Hygroscopicity of Organic Aerosols and Their Contributions to CCN Concentrations Over a Midlatitude Forest in Japan Y. Deng et al.
22. Influence of pollutants on activity of aerosol cloud condensation nuclei (CCN) during pollution and post-rain periods in Guangzhou, southern China J. Duan et al.
23. Characterisation of the Manchester Aerosol Chamber facility Y. Shao et al.
24. On the evolution of sub- and super-saturated water uptake of secondary organic aerosol in chamber experiments from mixed precursors Y. Wang et al.
25. Droplet activation of wet particles: development of the Wet CCN approach S. Nakao et al.
26. A core-shell box model for simulating viscosity dependent secondary organic aerosol (CSVA) and its application L. Jia & Y. Xu
27. A Significant Portion of Water-Soluble Organic Matter in Fresh Biomass Burning Particles Does Not Contribute to Hygroscopic Growth: An Application of Polarity Segregation by 1-Octanol–Water Partitioning Method J. Chen et al.
28. Atmospheric new particle formation as a source of CCN in the eastern Mediterranean marine boundary layer N. Kalivitis et al.
29. Liquid–Liquid Phase Separation Can Drive Aerosol Droplet Growth in Supersaturated Regimes K. Malek et al.
30. Phase state of ambient aerosol linked with water uptake and chemical aging in the southeastern US A. Pajunoja et al.
31. The efficiency of secondary organic aerosol particles acting as ice-nucleating particles under mixed-phase cloud conditions W. Frey et al.
32. Size‐dependent hygroscopicity parameter (κ) and chemical composition of secondary organic cloud condensation nuclei D. Zhao et al.
33. Contrasting effects of secondary organic aerosol formations on organic aerosol hygroscopicity Y. Kuang et al.
34. Hygroscopic growth and CCN activity of secondary organic aerosol produced from dark ozonolysis of γ-terpinene H. Bouzidi et al.
35. Unveiling the organic contribution to the initial particle growth in 3–10 nm size range K. Zhang et al.
36. Development of lithium attachment mass spectrometry – knudsen effusion and chemical ionisation mass spectrometry (KEMS, CIMS) A. Booth et al.
37. A method for extracting calibrated volatility information from the FIGAERO-HR-ToF-CIMS and its experimental application T. Bannan et al.
38. On the link between hygroscopicity, volatility, and oxidation state of ambient and water-soluble aerosols in the southeastern United States K. Cerully et al.
39. A review of experimental techniques for aerosol hygroscopicity studies M. Tang et al.