Coalescence and Breakup-Induced Oscillations in the Evolution of the Raindrop Size DistributionSource: Journal of the Atmospheric Sciences:;1988:;Volume( 046 ):;issue: 009::page 1186Author:Brown, Philip S.
DOI: 10.1175/1520-0469(1989)046<1186:CABIOI>2.0.CO;2Publisher: American Meteorological Society
Abstract: Models or the coalescence/breakup process yield drop number distributions that approach equilibrium but the number density often is not a monotonic function of time. In some cases, the small-raindrop portion of the distribution rapidly attains high concentration levels before settling back toward an equilibrium position. An eigenanalysis of the coalescence/breakup equation is performed to gain an understanding of the solution behavior near equilibrium. The analysis reveals that the departure of the solution from equilibrium can be expressed as a linear combination of basis functions of the form e?j where Re(?j) < 0 so that the equilibrium drop distribution is asymptotically stable. The exponential basis functions feature a wide range of decay rates, and since Im (?j) ? 0 in some cases, the functions provide evidence of oscillations in the drop spectrum. It is shown that one particular damped oscillation can combine with a rapidly decaying transient to describe very well the nonmonotonic behavior characteristic of model-generated drop spectra. While the physical mechanism behind the oscillation is not yet understood, the initial reversal in the small-drop peak may be explained as rapid response due to filament breakup followed by a slower response due to coalescence. A particular sequence of observed raindrop distributions is found to exhibit a reversal in the spectral peak similar to that produced by the model.
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contributor author | Brown, Philip S. | |
date accessioned | 2017-06-09T14:28:54Z | |
date available | 2017-06-09T14:28:54Z | |
date copyright | 1989/05/01 | |
date issued | 1988 | |
identifier issn | 0022-4928 | |
identifier other | ams-20059.pdf | |
identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4156245 | |
description abstract | Models or the coalescence/breakup process yield drop number distributions that approach equilibrium but the number density often is not a monotonic function of time. In some cases, the small-raindrop portion of the distribution rapidly attains high concentration levels before settling back toward an equilibrium position. An eigenanalysis of the coalescence/breakup equation is performed to gain an understanding of the solution behavior near equilibrium. The analysis reveals that the departure of the solution from equilibrium can be expressed as a linear combination of basis functions of the form e?j where Re(?j) < 0 so that the equilibrium drop distribution is asymptotically stable. The exponential basis functions feature a wide range of decay rates, and since Im (?j) ? 0 in some cases, the functions provide evidence of oscillations in the drop spectrum. It is shown that one particular damped oscillation can combine with a rapidly decaying transient to describe very well the nonmonotonic behavior characteristic of model-generated drop spectra. While the physical mechanism behind the oscillation is not yet understood, the initial reversal in the small-drop peak may be explained as rapid response due to filament breakup followed by a slower response due to coalescence. A particular sequence of observed raindrop distributions is found to exhibit a reversal in the spectral peak similar to that produced by the model. | |
publisher | American Meteorological Society | |
title | Coalescence and Breakup-Induced Oscillations in the Evolution of the Raindrop Size Distribution | |
type | Journal Paper | |
journal volume | 46 | |
journal issue | 9 | |
journal title | Journal of the Atmospheric Sciences | |
identifier doi | 10.1175/1520-0469(1989)046<1186:CABIOI>2.0.CO;2 | |
journal fristpage | 1186 | |
journal lastpage | 1192 | |
tree | Journal of the Atmospheric Sciences:;1988:;Volume( 046 ):;issue: 009 | |
contenttype | Fulltext |