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- W2893183325 abstract "Abstract Cloud optical properties are determined not only by the number density n d and mean radius of cloud droplets but also by the shape of the droplet size distribution. The change in cloud optical depth with changing n d , due to the change in distribution shape, is known as the dispersion effect. Droplet relative dispersion is defined as . For the first time, a commonly used effective radius parameterization is tested in a controlled laboratory environment by creating a turbulent cloud. Stochastic condensation growth suggests d independent of n d for a nonprecipitating cloud, hence nearly zero albedo susceptibility due to the dispersion effect. However, for size‐dependent removal, such as in a laboratory cloud or highly clean atmospheric conditions, stochastic condensation produces a weak dispersion effect. The albedo susceptibility due to turbulence broadening has the same sign as the Twomey effect and augments it by order 10%." @default.
- W2893183325 created "2018-10-05" @default.
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- W2893183325 date "2018-10-10" @default.
- W2893183325 modified "2023-10-18" @default.
- W2893183325 title "Dispersion Aerosol Indirect Effect in Turbulent Clouds: Laboratory Measurements of Effective Radius" @default.
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- W2893183325 doi "https://doi.org/10.1029/2018gl079194" @default.
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- W2893183325 hasPublicationYear "2018" @default.
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