Articles | Volume 13, issue 2
https://doi.org/10.5194/acp-13-1081-2013
© Author(s) 2013. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/acp-13-1081-2013
© Author(s) 2013. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
A single parameter representation of hygroscopic growth and cloud condensation nucleus activity – Part 3: Including surfactant partitioning
M. D. Petters
Department of Marine Earth and Atmospheric Sciences, North Carolina State University, Raleigh, NC, USA
S. M. Kreidenweis
Department of Atmospheric Science, Colorado State University, Fort Collins, CO, USA
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- Hygroscopicity of aerosol particles composed of surfactant SDS and its internal mixture with ammonium sulfate at relative humidities up to 99.9% C. Zhang et al. 10.1016/j.atmosenv.2023.119625
- Hygroscopic growth and CCN activity of secondary organic aerosol produced from dark ozonolysis of γ-terpinene H. Bouzidi et al. 10.1016/j.scitotenv.2022.153010
- Accurate Determination of Aerosol Activity Coefficients at Relative Humidities up to 99% Using the Hygroscopicity Tandem Differential Mobility Analyzer Technique S. Suda & M. Petters 10.1080/02786826.2013.807906
- Accurate representations of the physicochemical properties of atmospheric aerosols: when are laboratory measurements of value? A. Marsh et al. 10.1039/C7FD00008A
- Microphysics of liquid water in sub-10 nm ultrafine aerosol particles X. Li & I. Bourg 10.5194/acp-23-2525-2023
- Evidence of Surface-Tension Lowering of Atmospheric Aerosols by Organics from Field Observations in an Urban Atmosphere: Relation to Particle Size and Chemical Composition T. Fan et al. 10.1021/acs.est.4c03141
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