A Note on the Criteria for the Onset of Stationary Parallel-Plate Convection Subject to Mean Vertical MotionSource: Journal of the Atmospheric Sciences:;1983:;Volume( 040 ):;issue: 004::page 1046Author:Lundberg, Peter
DOI: 10.1175/1520-0469(1983)040<1046:ANOTCF>2.0.CO;2Publisher: American Meteorological Society
Abstract: The Benard problem is extended to include the effects of perfectly conducting, but porous, boundaries permitting an average vertical mass flux, characterized by a Peclet number, through the system. The linear stability problem for the onset of stationary convection is solved using a power series technique and it is found that the stability of the system increases for large absolute values of the Peclet number. A detailed comparison with the work of Krishnamurti reveals contradictory results for the magnitude of the horizontal wavenumber as a function of the Péclet number, as well as for the dependence of the stability upon the Prandtl number. These discrepancies and their possible causes are discussed in some detail.
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contributor author | Lundberg, Peter | |
date accessioned | 2017-06-09T14:23:50Z | |
date available | 2017-06-09T14:23:50Z | |
date copyright | 1983/04/01 | |
date issued | 1983 | |
identifier issn | 0022-4928 | |
identifier other | ams-18563.pdf | |
identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4154582 | |
description abstract | The Benard problem is extended to include the effects of perfectly conducting, but porous, boundaries permitting an average vertical mass flux, characterized by a Peclet number, through the system. The linear stability problem for the onset of stationary convection is solved using a power series technique and it is found that the stability of the system increases for large absolute values of the Peclet number. A detailed comparison with the work of Krishnamurti reveals contradictory results for the magnitude of the horizontal wavenumber as a function of the Péclet number, as well as for the dependence of the stability upon the Prandtl number. These discrepancies and their possible causes are discussed in some detail. | |
publisher | American Meteorological Society | |
title | A Note on the Criteria for the Onset of Stationary Parallel-Plate Convection Subject to Mean Vertical Motion | |
type | Journal Paper | |
journal volume | 40 | |
journal issue | 4 | |
journal title | Journal of the Atmospheric Sciences | |
identifier doi | 10.1175/1520-0469(1983)040<1046:ANOTCF>2.0.CO;2 | |
journal fristpage | 1046 | |
journal lastpage | 1050 | |
tree | Journal of the Atmospheric Sciences:;1983:;Volume( 040 ):;issue: 004 | |
contenttype | Fulltext |