The Continuous Spectrum of Linear Couette Flow with the Beta EffectSource: Journal of the Atmospheric Sciences:;1983:;Volume( 040 ):;issue: 009::page 2304Author:Boyd, John P.
DOI: 10.1175/1520-0469(1983)040<2304:TCSOLC>2.0.CO;2Publisher: American Meteorological Society
Abstract: The previously known analytic solution for the unbounded plane Couette flow [i.e., a mean flow U(y)=Sy, S constant] is extended by 1) inclusion of the beta effect, and 2) more general initial conditions. It is shown that the beta effect and sidewall boundaries in latitude both have little or no effect on the physics of the waves. For large times, as already known, the continuous spectrum always decays away algebraically with time. It is shown, however, that before the final decay, the continuous spectrum may grow rapidly for a finite time interval if the latitudinal length scale of the initial perturbation is small in comparison to the zonal scale.
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contributor author | Boyd, John P. | |
date accessioned | 2017-06-09T14:24:10Z | |
date available | 2017-06-09T14:24:10Z | |
date copyright | 1983/09/01 | |
date issued | 1983 | |
identifier issn | 0022-4928 | |
identifier other | ams-18658.pdf | |
identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4154687 | |
description abstract | The previously known analytic solution for the unbounded plane Couette flow [i.e., a mean flow U(y)=Sy, S constant] is extended by 1) inclusion of the beta effect, and 2) more general initial conditions. It is shown that the beta effect and sidewall boundaries in latitude both have little or no effect on the physics of the waves. For large times, as already known, the continuous spectrum always decays away algebraically with time. It is shown, however, that before the final decay, the continuous spectrum may grow rapidly for a finite time interval if the latitudinal length scale of the initial perturbation is small in comparison to the zonal scale. | |
publisher | American Meteorological Society | |
title | The Continuous Spectrum of Linear Couette Flow with the Beta Effect | |
type | Journal Paper | |
journal volume | 40 | |
journal issue | 9 | |
journal title | Journal of the Atmospheric Sciences | |
identifier doi | 10.1175/1520-0469(1983)040<2304:TCSOLC>2.0.CO;2 | |
journal fristpage | 2304 | |
journal lastpage | 2308 | |
tree | Journal of the Atmospheric Sciences:;1983:;Volume( 040 ):;issue: 009 | |
contenttype | Fulltext |