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    Developing Disturbances in Shear

    Source: Journal of the Atmospheric Sciences:;1987:;Volume( 044 ):;issue: 016::page 2191
    Author:
    Farrell, Brian
    DOI: 10.1175/1520-0469(1987)044<2191:DDIS>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The origin and growth to moderate amplitude of disturbances in shear flow has been traditionally ascribed to the linear modal instability of the flow. Recent work on initial value problems has suggested that nonmodal growth of perturbations may be of equal and perhaps greater importance, at least in cases of rapid development. Examples of robust growth in model problems which support no instabilities and in baroclinic flows with realistic Ekman damping for which the exponential modes have zero or negative growth rates have been shown. Such examples have focused attention on the perturbations which are configured to tap the energy of mean flows. Here a critical examination of these favorably configured perturbations is given, making use of the simple constant free shear barotropic model which allows construction of exact two-dimensional isolated wave packet solutions.
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      Developing Disturbances in Shear

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    contributor authorFarrell, Brian
    date accessioned2017-06-09T14:27:32Z
    date available2017-06-09T14:27:32Z
    date copyright1987/08/01
    date issued1987
    identifier issn0022-4928
    identifier otherams-19595.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4155728
    description abstractThe origin and growth to moderate amplitude of disturbances in shear flow has been traditionally ascribed to the linear modal instability of the flow. Recent work on initial value problems has suggested that nonmodal growth of perturbations may be of equal and perhaps greater importance, at least in cases of rapid development. Examples of robust growth in model problems which support no instabilities and in baroclinic flows with realistic Ekman damping for which the exponential modes have zero or negative growth rates have been shown. Such examples have focused attention on the perturbations which are configured to tap the energy of mean flows. Here a critical examination of these favorably configured perturbations is given, making use of the simple constant free shear barotropic model which allows construction of exact two-dimensional isolated wave packet solutions.
    publisherAmerican Meteorological Society
    titleDeveloping Disturbances in Shear
    typeJournal Paper
    journal volume44
    journal issue16
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1987)044<2191:DDIS>2.0.CO;2
    journal fristpage2191
    journal lastpage2199
    treeJournal of the Atmospheric Sciences:;1987:;Volume( 044 ):;issue: 016
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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