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contributor authorBrown, Philip S.
date accessioned2017-06-09T14:22:44Z
date available2017-06-09T14:22:44Z
date copyright1981/12/01
date issued1981
identifier issn0022-4928
identifier otherams-18260.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4154246
description abstractDiscretization of the collision-breakup equation results in a nonlinear system that can produce highly damped solution components. An analytic expression is derived for the smallest time constant τmin, a parameter used to describe the most rapid decay rate associated with the system. τmin is found to be a measure of the decay time for destruction of the largest drops considered in the model. For Marshall-Palmer distributions N0e?AD, τmin decreases with increasing N0 and with increasing rainfall rate R. τmin determines the maximum time step that can be used to insure computational stability in numerical solution of the breakup equation. For large N0 and R, time steps as small as 1 s may be required to prevent error growth.
publisherAmerican Meteorological Society
titleTime-Constant Variation in the Collision-Breakup Equation
typeJournal Paper
journal volume38
journal issue12
journal titleJournal of the Atmospheric Sciences
identifier doi10.1175/1520-0469(1981)038<2758:TCVITC>2.0.CO;2
journal fristpage2758
journal lastpage2762
treeJournal of the Atmospheric Sciences:;1981:;Volume( 038 ):;issue: 012
contenttypeFulltext


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