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    Efficiency of Mixing Forced by Unsteady Shear Flow

    Source: Journal of Physical Oceanography:;2009:;Volume( 039 ):;issue: 005::page 1150
    Author:
    Inoue, Ryuichiro
    ,
    Smyth, William D.
    DOI: 10.1175/2008JPO3927.1
    Publisher: American Meteorological Society
    Abstract: The dependence of mixing efficiency on time-varying forcing is studied by direct numerical simulation (DNS) of Kelvin?Helmholtz (KH) instability. Time-dependent forcing fields are designed to reproduce a wavelike oscillation by solving the equations of motion in a tilted coordinate frame and allowing the tilt angle to vary in time. Mixing efficiency Γc is defined as the ratio of potential energy gain to dissipation, both averaged over one forcing cycle and first examined via parameters characterizing waves: the minimum Richardson number Rimin and the normalized frequency of the forcing ?/N. The effect of Reynolds number Re0 and the initial random disturbance amplitude b are also examined. In the experiments presented, Γc varies between 0.21 and 0.36 and is controlled by the timing of two events: the emergence of KH billows and the arrival of the deceleration of the mean shear by the wavelike forcing. Here, Γc is higher than a canonical value of 0.2 when the deceleration phase of the forcing suppresses the less efficient turbulence after breakdown of KH billows. However, when Rimin and ?/N are small, KH billows start to develop before Rimin is achieved. Therefore, the forcing accelerates the mean shear and thereby sustains turbulence after the breakdown of KH billows. The canonical value is then reproduced in the DNS. Although larger values of Re0 and b intensify the development of KH billows and modify Γc, this effect is less significant when forcing fields act to sustain turbulence. The time-averaged Thorpe scale and Ozmidov scale are also used to see how mixing is modified by forcing fields and compared with past microstructure measurements. It is found that DNS also corresponds to past observations if the forcing accelerates the mean shear to sustain turbulence.
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      Efficiency of Mixing Forced by Unsteady Shear Flow

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    contributor authorInoue, Ryuichiro
    contributor authorSmyth, William D.
    date accessioned2017-06-09T16:25:12Z
    date available2017-06-09T16:25:12Z
    date copyright2009/05/01
    date issued2009
    identifier issn0022-3670
    identifier otherams-67527.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4208984
    description abstractThe dependence of mixing efficiency on time-varying forcing is studied by direct numerical simulation (DNS) of Kelvin?Helmholtz (KH) instability. Time-dependent forcing fields are designed to reproduce a wavelike oscillation by solving the equations of motion in a tilted coordinate frame and allowing the tilt angle to vary in time. Mixing efficiency Γc is defined as the ratio of potential energy gain to dissipation, both averaged over one forcing cycle and first examined via parameters characterizing waves: the minimum Richardson number Rimin and the normalized frequency of the forcing ?/N. The effect of Reynolds number Re0 and the initial random disturbance amplitude b are also examined. In the experiments presented, Γc varies between 0.21 and 0.36 and is controlled by the timing of two events: the emergence of KH billows and the arrival of the deceleration of the mean shear by the wavelike forcing. Here, Γc is higher than a canonical value of 0.2 when the deceleration phase of the forcing suppresses the less efficient turbulence after breakdown of KH billows. However, when Rimin and ?/N are small, KH billows start to develop before Rimin is achieved. Therefore, the forcing accelerates the mean shear and thereby sustains turbulence after the breakdown of KH billows. The canonical value is then reproduced in the DNS. Although larger values of Re0 and b intensify the development of KH billows and modify Γc, this effect is less significant when forcing fields act to sustain turbulence. The time-averaged Thorpe scale and Ozmidov scale are also used to see how mixing is modified by forcing fields and compared with past microstructure measurements. It is found that DNS also corresponds to past observations if the forcing accelerates the mean shear to sustain turbulence.
    publisherAmerican Meteorological Society
    titleEfficiency of Mixing Forced by Unsteady Shear Flow
    typeJournal Paper
    journal volume39
    journal issue5
    journal titleJournal of Physical Oceanography
    identifier doi10.1175/2008JPO3927.1
    journal fristpage1150
    journal lastpage1166
    treeJournal of Physical Oceanography:;2009:;Volume( 039 ):;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
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