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    Inertial Ranges and Small-Scale Intermittency in One-Dimensional Turbulence Models

    Source: Journal of the Atmospheric Sciences:;1993:;Volume( 050 ):;issue: 015::page 2542
    Author:
    Bartello, Peter
    DOI: 10.1175/1520-0469(1993)050<2542:IRASSI>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: A set of one-dimensional turbulence models can be constructed by applying severe D-1 directional Fourier truncation to the D-dimensional fluid equations, allowing for numerical calculation over an extremely wide range of scales. At low resolution a reduced 2D model displayed both inviscid energy-enstrophy equipartition and a spectrum consistent with the enstrophy cascade phenomenology in the decay problem. In the present note, these results are extended by using reduced models to examine both the inverse (D = 2) and direct (D = 3) energy cascades. In addition, higher numerical resolution (up to 4096 grid points) is employed to demonstrate unequivocal adherence to the 2D phenomenologies. Small-scale intermittency in the form of spatially intermittent vorticity gradients is also observed. Simulations based on the reduced 3D model were less successful. Although the truncated inviscid equilibrium agreed with an energy equipratition spectrum, forced-viscous simulations failed to show a clear Kolmogorov range. It is argued that the technique, although not justified for 3D problems, produces an interesting 1D turbulence model when applied to 2D flow.
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      Inertial Ranges and Small-Scale Intermittency in One-Dimensional Turbulence Models

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    https://yetl.yabesh.ir/yetl1/handle/yetl/4157282
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    contributor authorBartello, Peter
    date accessioned2017-06-09T14:31:41Z
    date available2017-06-09T14:31:41Z
    date copyright1993/08/01
    date issued1993
    identifier issn0022-4928
    identifier otherams-20993.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4157282
    description abstractA set of one-dimensional turbulence models can be constructed by applying severe D-1 directional Fourier truncation to the D-dimensional fluid equations, allowing for numerical calculation over an extremely wide range of scales. At low resolution a reduced 2D model displayed both inviscid energy-enstrophy equipartition and a spectrum consistent with the enstrophy cascade phenomenology in the decay problem. In the present note, these results are extended by using reduced models to examine both the inverse (D = 2) and direct (D = 3) energy cascades. In addition, higher numerical resolution (up to 4096 grid points) is employed to demonstrate unequivocal adherence to the 2D phenomenologies. Small-scale intermittency in the form of spatially intermittent vorticity gradients is also observed. Simulations based on the reduced 3D model were less successful. Although the truncated inviscid equilibrium agreed with an energy equipratition spectrum, forced-viscous simulations failed to show a clear Kolmogorov range. It is argued that the technique, although not justified for 3D problems, produces an interesting 1D turbulence model when applied to 2D flow.
    publisherAmerican Meteorological Society
    titleInertial Ranges and Small-Scale Intermittency in One-Dimensional Turbulence Models
    typeJournal Paper
    journal volume50
    journal issue15
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1993)050<2542:IRASSI>2.0.CO;2
    journal fristpage2542
    journal lastpage2546
    treeJournal of the Atmospheric Sciences:;1993:;Volume( 050 ):;issue: 015
    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