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    Intermittent Turbulence and Oscillations in the Stable Boundary Layer over Land. Part I: A Bulk Model

    Source: Journal of the Atmospheric Sciences:;2002:;Volume( 059 ):;issue: 005::page 942
    Author:
    Van de Wiel, B. J. H.
    ,
    Ronda, R. J.
    ,
    Moene, A. F.
    ,
    De Bruin, H. A. R.
    ,
    Holtslag, A. A. M.
    DOI: 10.1175/1520-0469(2002)059<0942:ITAOIT>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: In the stable boundary layer (SBL) it is observed often that turbulence is not continuous in space and time. This discontinuous, intermittent turbulence causes alternations from the mean evolution of the stratified atmospheric boundary layer, which may result in an oscillatory type of behavior of the near-surface wind speed and temperature. It is well known that intermittent turbulence in the SBL can be generated by various mechanisms. This paper focuses on an intermittency generating mechanism that arises from a direct interaction of the lower atmosphere (first tens of meters) with the vegetation surface, without interaction with the air aloft. It is shown that the essence of this mechanism can be captured by a 1D bulk model of three coupled nonlinear differential equations. In the present paper, numerical runs with the model show that intermittent turbulence is most likely to occur over land surfaces with low vegetation during clear-sky conditions in the presence of a moderate to low synoptical pressure gradient. The existence of a vegetation layer has a strong influence on intermittency dynamics. Due to its small heat capacity, the vegetation temperature is able to quickly respond to rapidly changing conditions. This in turn affects the stability of the lower atmosphere, causing an important feedback mechanism. In addition, it was found that intermittent behavior of SBL models occurs for various first-order closure schemes with different stability functions. However, stability functions that allow turbulent transport beyond the critical Richardson number effectively suppress intermittent?oscillatory behavior. Currently, the latter type of formulations is often used in numerical weather prediction to prevent excessive SBL cooling in very stable conditions. The advantage of using a simplified SBL model, as proposed in the present paper, is that it allows an analytical study of the system, which, in turn, allows theoretical predictions about the occurrence of intermittent SBL behavior (see the companion paper).
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      Intermittent Turbulence and Oscillations in the Stable Boundary Layer over Land. Part I: A Bulk Model

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4159585
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    contributor authorVan de Wiel, B. J. H.
    contributor authorRonda, R. J.
    contributor authorMoene, A. F.
    contributor authorDe Bruin, H. A. R.
    contributor authorHoltslag, A. A. M.
    date accessioned2017-06-09T14:37:32Z
    date available2017-06-09T14:37:32Z
    date copyright2002/03/01
    date issued2002
    identifier issn0022-4928
    identifier otherams-23065.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4159585
    description abstractIn the stable boundary layer (SBL) it is observed often that turbulence is not continuous in space and time. This discontinuous, intermittent turbulence causes alternations from the mean evolution of the stratified atmospheric boundary layer, which may result in an oscillatory type of behavior of the near-surface wind speed and temperature. It is well known that intermittent turbulence in the SBL can be generated by various mechanisms. This paper focuses on an intermittency generating mechanism that arises from a direct interaction of the lower atmosphere (first tens of meters) with the vegetation surface, without interaction with the air aloft. It is shown that the essence of this mechanism can be captured by a 1D bulk model of three coupled nonlinear differential equations. In the present paper, numerical runs with the model show that intermittent turbulence is most likely to occur over land surfaces with low vegetation during clear-sky conditions in the presence of a moderate to low synoptical pressure gradient. The existence of a vegetation layer has a strong influence on intermittency dynamics. Due to its small heat capacity, the vegetation temperature is able to quickly respond to rapidly changing conditions. This in turn affects the stability of the lower atmosphere, causing an important feedback mechanism. In addition, it was found that intermittent behavior of SBL models occurs for various first-order closure schemes with different stability functions. However, stability functions that allow turbulent transport beyond the critical Richardson number effectively suppress intermittent?oscillatory behavior. Currently, the latter type of formulations is often used in numerical weather prediction to prevent excessive SBL cooling in very stable conditions. The advantage of using a simplified SBL model, as proposed in the present paper, is that it allows an analytical study of the system, which, in turn, allows theoretical predictions about the occurrence of intermittent SBL behavior (see the companion paper).
    publisherAmerican Meteorological Society
    titleIntermittent Turbulence and Oscillations in the Stable Boundary Layer over Land. Part I: A Bulk Model
    typeJournal Paper
    journal volume59
    journal issue5
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(2002)059<0942:ITAOIT>2.0.CO;2
    journal fristpage942
    journal lastpage958
    treeJournal of the Atmospheric Sciences:;2002:;Volume( 059 ):;issue: 005
    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