The studies focus on the role of turbulent fluctuations in vertical wind and in the microphysical environments in which droplets grow, and represent the effects of droplets mixing together that have encountered different trajectories through the cloud. The effects can be analyzed in terms of two contributions to the variance in supersaturation history, one dependent on the average microphysical environment (specifically, integral radius) of the near environment in which a droplet grows, and the other dependent on the correlation between the integral radius and the updraft along the droplet trajectory. It is suggested that simple turbulent motions in a stochastically varying cloud may provide significant broadening of the cloud droplet spectrum if those motions are accompanied by a variable microphysical structure produced by dry-air entrainment. -from Author
CITATION STYLE
Cooper, W. A. (1989). Effects of variable droplet growth histories on droplet size distributions. Part I: theory. Journal of the Atmospheric Sciences, 46(10), 1301–1311. https://doi.org/10.1175/1520-0469(1989)046<1301:EOVDGH>2.0.CO;2
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