Predicting cloud condensation nuclei number concentration based on conventional measurements of aerosol properties in the North China Plain - ScienceDirect
ARM Research Facility
An examination of Köhler theory resulting in an accurate expression for the equilibrium radius ratio of a hygroscopic aerosol particle valid up to and including relative humidity 100% - Lewis - 2008 -
The Köhler equation can be envisaged as the competition between the... | Download Scientific Diagram
An examination of Köhler theory resulting in an accurate expression for the equilibrium radius ratio of a hygroscopic aerosol particle valid up to and including relative humidity 100% - Lewis - 2008 -
An examination of Köhler theory resulting in an accurate expression for the equilibrium radius ratio of a hygroscopic aerosol particle valid up to and including relative humidity 100% - Lewis - 2008 -
5.6 Koehler Theory | METEO 300: Fundamentals of Atmospheric Science
PDF) Refinements to the Köhler's theory of aerosol equilibrium radii, size spectra, and droplet activation: Effects of humidity and insoluble fraction
Cloud droplet activation of mixed model HULIS and NaCl particles: Experimental results and κ-Köhler theory - ScienceDirect
Effects of surface tension time-evolution for CCN activation of a complex organic surfactant - Environmental Science: Processes & Impacts (RSC Publishing) DOI:10.1039/C9EM00426B
THEORY AND PRACTICE OF AEROSOL SCIENCE
Köhler theory - Wikipedia
5.6 Koehler Theory | METEO 300: Fundamentals of Atmospheric Science
Hygroscopicity of polycatechol and polyguaiacol secondary organic aerosol in sub- and supersaturated water vapor environments - Environmental Science: Atmospheres (RSC Publishing) DOI:10.1039/D1EA00063B
Cloud Condensation Nuclei Hygroscopic Parameter Kappa
5.6 Koehler Theory | METEO 300: Fundamentals of Atmospheric Science
Surfactants and cloud droplet activation: A systematic extension of Köhler theory based on analysis of droplet stability: The Journal of Chemical Physics: Vol 154, No 2
Instrument artifacts lead to uncertainties in parameterizations of cloud condensation nucleation
