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    Statistics of the Richardson Number: Mixing Models and Finestructure

    Source: Journal of Physical Oceanography:;1996:;Volume( 026 ):;issue: 008::page 1409
    Author:
    Polzin, Kurt
    DOI: 10.1175/1520-0485(1996)026<1409:SOTRNM>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Parameterization of the dissipation rate of turbulent kinetic energy (?) in terms of Richardson number (Ri = N2/S2) is examined for a variety in internal wave environments. Previous work with these data suggests a scaling of ? ? E2N?2g(w) to within a factor of 2, where E represents a low-wavenumber shear spectral density, N? the background buoyancy frequency, and g(w) a dependence upon average wave frequency content. The alternative Richardson-number-based parameterization of Kunze et al. is also shown to collapse the dissipation data to within a factor of 2. On the basis of a number of theoretical Richardson number probability distributions, however, the nominal (E, N?) scaling of the Kunze et al. model is determined to be E2N?3. The difference between the nominal (N?3) and observed (N?2) scaling is hypothesized to be an effect of turbulent momentum and buoyancy fluxes on the internal wave shear and strain profiles associated with the shear instability. For a statistically homogeneous subset of the data, S2 and N2 are determined to be statistically dependent. It is proposed that the statistical dependence represents both the direct effects of turbulent momentum and buoyancy fluxes decreasing S2 and N2 within a mixing event and the indirect effect of internal waves interacting with permanent buoyancy perturbations resulting from mixing.
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      Statistics of the Richardson Number: Mixing Models and Finestructure

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    contributor authorPolzin, Kurt
    date accessioned2017-06-09T14:52:09Z
    date available2017-06-09T14:52:09Z
    date copyright1996/08/01
    date issued1996
    identifier issn0022-3670
    identifier otherams-28554.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4165683
    description abstractParameterization of the dissipation rate of turbulent kinetic energy (?) in terms of Richardson number (Ri = N2/S2) is examined for a variety in internal wave environments. Previous work with these data suggests a scaling of ? ? E2N?2g(w) to within a factor of 2, where E represents a low-wavenumber shear spectral density, N? the background buoyancy frequency, and g(w) a dependence upon average wave frequency content. The alternative Richardson-number-based parameterization of Kunze et al. is also shown to collapse the dissipation data to within a factor of 2. On the basis of a number of theoretical Richardson number probability distributions, however, the nominal (E, N?) scaling of the Kunze et al. model is determined to be E2N?3. The difference between the nominal (N?3) and observed (N?2) scaling is hypothesized to be an effect of turbulent momentum and buoyancy fluxes on the internal wave shear and strain profiles associated with the shear instability. For a statistically homogeneous subset of the data, S2 and N2 are determined to be statistically dependent. It is proposed that the statistical dependence represents both the direct effects of turbulent momentum and buoyancy fluxes decreasing S2 and N2 within a mixing event and the indirect effect of internal waves interacting with permanent buoyancy perturbations resulting from mixing.
    publisherAmerican Meteorological Society
    titleStatistics of the Richardson Number: Mixing Models and Finestructure
    typeJournal Paper
    journal volume26
    journal issue8
    journal titleJournal of Physical Oceanography
    identifier doi10.1175/1520-0485(1996)026<1409:SOTRNM>2.0.CO;2
    journal fristpage1409
    journal lastpage1425
    treeJournal of Physical Oceanography:;1996:;Volume( 026 ):;issue: 008
    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
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