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    The Effects of Filament, Sheet, and Disk Breakup upon the Drop Spectrum

    Source: Journal of the Atmospheric Sciences:;1988:;Volume( 045 ):;issue: 004::page 712
    Author:
    Brown, Philips S.
    DOI: 10.1175/1520-0469(1988)045<0712:TEOFSA>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The coalescence/breakup formulas introduced by Low and List included a new formulation of the coalescence efficiency and a new formulation of the fragment distribution function P, which is written as a weighted sum of three distribution functions, each corresponding to one of three types of fragmentation (filament, sheet and disk). The purpose of this work is to examine in detail the effects of each main component of the Low and List formulas upon the evolution of the drop spectrum. Compared to an earlier formulation, the Low and List coalescence efficiency tends to distribute more water mass from the small-drop range to the 1argee-drop range. The individual processes of filament and sheet breakup tend to produce single peaks in the small-drop end of the spectrum, while disk breakup tends to produce a bimodal distribution with peaks near drop diameters 1 and 2.3 mm. Disk breakup is the dominant type of fragmentation in determining the response time of the system and in causing the destruction of very large-size drops. The combined breakup processes produce a trimodal equilibrium drop distribution. Sheet breakup reinforces the small-drop peak at D = 0.23 mm established by filament breakup to form the principal mode. Sheer and disk breakup act in combination to form the less-prominent secondary and tertiary modes.
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      The Effects of Filament, Sheet, and Disk Breakup upon the Drop Spectrum

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    contributor authorBrown, Philips S.
    date accessioned2017-06-09T14:28:05Z
    date available2017-06-09T14:28:05Z
    date copyright1988/02/01
    date issued1988
    identifier issn0022-4928
    identifier otherams-19760.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4155912
    description abstractThe coalescence/breakup formulas introduced by Low and List included a new formulation of the coalescence efficiency and a new formulation of the fragment distribution function P, which is written as a weighted sum of three distribution functions, each corresponding to one of three types of fragmentation (filament, sheet and disk). The purpose of this work is to examine in detail the effects of each main component of the Low and List formulas upon the evolution of the drop spectrum. Compared to an earlier formulation, the Low and List coalescence efficiency tends to distribute more water mass from the small-drop range to the 1argee-drop range. The individual processes of filament and sheet breakup tend to produce single peaks in the small-drop end of the spectrum, while disk breakup tends to produce a bimodal distribution with peaks near drop diameters 1 and 2.3 mm. Disk breakup is the dominant type of fragmentation in determining the response time of the system and in causing the destruction of very large-size drops. The combined breakup processes produce a trimodal equilibrium drop distribution. Sheet breakup reinforces the small-drop peak at D = 0.23 mm established by filament breakup to form the principal mode. Sheer and disk breakup act in combination to form the less-prominent secondary and tertiary modes.
    publisherAmerican Meteorological Society
    titleThe Effects of Filament, Sheet, and Disk Breakup upon the Drop Spectrum
    typeJournal Paper
    journal volume45
    journal issue4
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1988)045<0712:TEOFSA>2.0.CO;2
    journal fristpage712
    journal lastpage718
    treeJournal of the Atmospheric Sciences:;1988:;Volume( 045 ):;issue: 004
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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