## Abstract The paper describes a relatively simple model of a nonβprecipitating cumulus cloud that grows by the ascent of successive spherical thermals through the residues of their predecessors, mixing with the surroundings being determined by the relative velocity and the radius of the thermal.
Laboratory studies of the effects of mixing on the evolution of cloud droplet spectra
β Scribed by J. Latham; R. L. Reed
- Publisher
- John Wiley and Sons
- Year
- 1977
- Tongue
- English
- Weight
- 651 KB
- Volume
- 103
- Category
- Article
- ISSN
- 0035-9009
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β¦ Synopsis
Abstract
Experiments were performed in which a cloud of droplets formed by condensation was drawn slowly down a cylindrical tube of length 5 m. the effect on the spectrum of mixingβin humidified but undersaturated air was studied.
The most striking observation was that the mixing process was highly inhomogeneous. Some droplets from all size categories were completely evaporated, while others were not significantly affected by the admixture of undersaturated air. the dispersion of the observable spectrum remained essentially constant. If this spectrum, with substantially reduced water content, was then allowed to grow by producing a supersaturation the measured dispersion increased appreciably. Calculations showed that the spectral evolution observed in a selected experiment was inexplicable in terms of homogeneous mixing, as envisaged by other workers. However, it could be explained by a rudimentary model of inhomogeneous mixing, which was found to offer a qualitative explanation for features of cloud droplet evolution observed by Warner, surrounding which there has been considerable recent discussion. This mixing process can be considered in terms of fluctuations in supersaturation not tied to fluctuations in vertical air velocity.
π SIMILAR VOLUMES
## Abstract The paper describes calculations of the development of dropletβsize spectra in cumulus clouds under the combined effects of condensation and coalescence. It is demonstrated that the concentration of condensation nuclei is a more important factor in controlling the onset of precipitation
## Abstract The evolution of different types of clouds is simulated with a spectral scavenging and microphysics model, DESCAM, coupled to the dynamics of an ascending and entraining airβparcel model. the resulting microphysical properties of the cloud are then coupled with a radiativeβtransfer mode