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contributor authorBerry, Edwin X.
contributor authorReinhardt, Richard L.
date accessioned2017-06-09T14:17:50Z
date available2017-06-09T14:17:50Z
date copyright1974/11/01
date issued1974
identifier issn0022-4928
identifier otherams-16689.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4152499
description abstractA new parameterization of cloud particle growth combines the effects of accretion and self-collection, and frees the large-hydrometeor water mass and spectral moments to grow independently. The large-hydrometeor water mass grows through accretion in proportion to the cloud water mass. The spectral moments grow through self-collection in proportion to the large-hydrometeor water content. Accretion is also dependent upon the magnitude of the spectral moments and thus an important feedback loop occurs. The spreading or narrowing of the drop spectrum is dependent upon the collection kernel and the relative magnitudes of accretion and self-collection in the region of interest. These effects are included in the parameterization. In order for the spectrum to spread there must exist both the stochastic mode and a sufficiently rapid increase in the collection kernel with drop size.
publisherAmerican Meteorological Society
titleAn Analysis of Cloud Drop Growth by Collection: Part IV. A New Parameterization
typeJournal Paper
journal volume31
journal issue8
journal titleJournal of the Atmospheric Sciences
identifier doi10.1175/1520-0469(1974)031<2127:AAOCDG>2.0.CO;2
journal fristpage2127
journal lastpage2135
treeJournal of the Atmospheric Sciences:;1974:;Volume( 031 ):;issue: 008
contenttypeFulltext


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