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    The Destabilizing Effect of the Ground on Kelvin-Helmholtz Waves in the Atmosphere

    Source: Journal of the Atmospheric Sciences:;1976:;Volume( 033 ):;issue: 001::page 59
    Author:
    Lalas, D. P.
    ,
    Einaudi, F.
    ,
    Fua, D.
    DOI: 10.1175/1520-0469(1976)033<0059:TDEOTG>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The simple Kelvin-Helmholtz model for shear zones in the atmosphere is modified, by introducing a solid boundary below to account for the effect of the ground. The new characteristics of neutral and unstable waves that can exist in such configuration are analyzed for various values of wind velocity, depth of the bottom layer, and Brunt-Väisälä frequency. It is shown that the presence of the ground considerably destabilizes waves with long horizontal wavelengths. In particular, long wavelengths are always unstable, so that no neutral stability boundary exists. Furthermore, the solid lower boundary introduces an infinite number of neutral modes, all of which correspond to evanescent waves in the top layer. Finally, the model with the ground is used to calculate the characteristics of the most unstable waves that would be generated for some well-documented observed cases and the calculated values are found to be in reasonable agreement with observations.
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      The Destabilizing Effect of the Ground on Kelvin-Helmholtz Waves in the Atmosphere

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4152817
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    contributor authorLalas, D. P.
    contributor authorEinaudi, F.
    contributor authorFua, D.
    date accessioned2017-06-09T14:18:37Z
    date available2017-06-09T14:18:37Z
    date copyright1976/01/01
    date issued1976
    identifier issn0022-4928
    identifier otherams-16975.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4152817
    description abstractThe simple Kelvin-Helmholtz model for shear zones in the atmosphere is modified, by introducing a solid boundary below to account for the effect of the ground. The new characteristics of neutral and unstable waves that can exist in such configuration are analyzed for various values of wind velocity, depth of the bottom layer, and Brunt-Väisälä frequency. It is shown that the presence of the ground considerably destabilizes waves with long horizontal wavelengths. In particular, long wavelengths are always unstable, so that no neutral stability boundary exists. Furthermore, the solid lower boundary introduces an infinite number of neutral modes, all of which correspond to evanescent waves in the top layer. Finally, the model with the ground is used to calculate the characteristics of the most unstable waves that would be generated for some well-documented observed cases and the calculated values are found to be in reasonable agreement with observations.
    publisherAmerican Meteorological Society
    titleThe Destabilizing Effect of the Ground on Kelvin-Helmholtz Waves in the Atmosphere
    typeJournal Paper
    journal volume33
    journal issue1
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1976)033<0059:TDEOTG>2.0.CO;2
    journal fristpage59
    journal lastpage69
    treeJournal of the Atmospheric Sciences:;1976:;Volume( 033 ):;issue: 001
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
    yabeshDSpacePersian