Abstract
Sulfur hexafluoride tracer gas was released during single aircraft passes just above growing convective turrets to study its entrainment into the clouds as they grew through the release altitude. During the early stages of entrainment, the tracer remained mostly out of the cloud and was carried alongside the upper cloud regions by the circulation present there. In each experiment, concentrated tracer was first found on the edges of the turrets. Later, the tracer fixed into the central portions of the turrets where it had diluted considerably and mixed through most of the turret. The observations are consistent with the hypothesis that cloud-top entrainment occurs through a vortex-like circulation that brings air from above the cloud into the central region of the cloud. -from Author
Cite
CITATION STYLE
Stith, J. L. (1992). Observations of cloud-top entrainment in cumuli. Journal of the Atmospheric Sciences, 49(15), 1334–1347. https://doi.org/10.1175/1520-0469(1992)049<1334:OOCTEI>2.0.CO;2
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