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contributor authorDu, Shumung
contributor authorWilson, John D.
date accessioned2017-06-09T14:33:30Z
date available2017-06-09T14:33:30Z
date copyright1995/11/01
date issued1995
identifier issn0022-4928
identifier otherams-21617.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4157976
description abstractFrom an analysis of scales in the cloud droplet collision problem, the authors infer that a trajectory model that is to be capable of predicting collisions between droplets of all possible sizes should be of second-order, that is should explicitly model particle acceleration. But for collisions between large droplets (radius about 50 µm or larger), which are still much smaller than raindroplets, a first-order model is appropriate. The relative motion of large droplets are studied with a first-order, two particle trajectory model. Turbulence is found to be unimportant (relative to differential gravitational settling) if the (large) droplet sizes are sufficiently distinct. Zeroth-order two-particle models, of the type hitherto applied to be problem, deteriorate in accuracy as the influence of turbulence on the droplet separation increases, that is, for large σv/v?, where σv is the turbulent velocity scale and v? is the droplet still-air terminal velocity. Under no circumstance is a single-particle model applicable.
publisherAmerican Meteorological Society
titleModelling the Effect of Turbulence on the Collision of Cloud Droplets
typeJournal Paper
journal volume52
journal issue22
journal titleJournal of the Atmospheric Sciences
identifier doi10.1175/1520-0469(1995)052<3849:MTEOTO>2.0.CO;2
journal fristpage3849
journal lastpage3856
treeJournal of the Atmospheric Sciences:;1995:;Volume( 052 ):;issue: 022
contenttypeFulltext


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