Abstract
A study has been conducted with the aim to verify an expression which relates the entrainment rate in a cumulus cloud to the diameter of that cloud, where the entrainment rate is defined as the fractional increase in cloud mass due to mixing with the environment, per unit height. A series of airplane penetrations of relatively small cumulus clouds, conducted during the summer of 1971, was used as a data base for making entrainment calculations. When a stratification of 23 cloud passes was analyzed, a strong inverse diameter dependence on the mixing rate was evident. For six cloud passes that were described as vigorously growing, well-defined, single isolated towers, the inverse relation was even stronger. There was a strong indication that the cumulus clouds studied were best described as the end result of an evolution of a series of starting plumes, rather than as purely plume or bubble elements.
Cite
CITATION STYLE
McCarthy, J. (1974). FIELD VERIFICATION OF THE RELATIONSHIP BETWEEN ENTRAINMENT RATE AND CUMULUS CLOUD DIAMETER. Journal of the Atmospheric Sciences, 31(4), 1028–1039. https://doi.org/10.1175/1520-0469(1974)031<1028:FVOTRB>2.0.CO;2
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