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    Double-Diffusive Intrusions on a Finite-Width Thermohaline Front

    Source: Journal of Physical Oceanography:;2004:;Volume( 034 ):;issue: 007::page 1723
    Author:
    Simeonov, Julian
    ,
    Stern, Melvin
    DOI: 10.1175/1520-0485(2004)034<1723:DIOAFT>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: A density-compensated thermohaline front with a finite width L? and total lateral salinity variation ?S superimposed on a finger-favorable thermocline is studied by means of linear theory and nonlinear numerical calculations using parameterized finger fluxes. By retaining the relatively small molecular heat diffusion and the dependence of the finger Nusselt number Nu on the density ratio, it is shown that marginal stability with critical ?S is possible. The lateral fluxes induce a mean vertical velocity w0(x), which can sharpen the front, but when ?S exceeds a certain value the effect of the lateral fluxes exceeds that of w0(x) and the front weakens. Nonlinear 2D spectral calculations showed that the modification of the mean horizontal gradients is small and that the intrusions continue to grow exponentially even after they have produced overturns. By extrapolating the linear theory results beyond the overturning stage, the intrusion velocity was estimated to be proportional to the Brunt?Väisälä frequency multiplied by the intrusion thickness.
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      Double-Diffusive Intrusions on a Finite-Width Thermohaline Front

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4167393
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    contributor authorSimeonov, Julian
    contributor authorStern, Melvin
    date accessioned2017-06-09T14:56:31Z
    date available2017-06-09T14:56:31Z
    date copyright2004/07/01
    date issued2004
    identifier issn0022-3670
    identifier otherams-30092.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4167393
    description abstractA density-compensated thermohaline front with a finite width L? and total lateral salinity variation ?S superimposed on a finger-favorable thermocline is studied by means of linear theory and nonlinear numerical calculations using parameterized finger fluxes. By retaining the relatively small molecular heat diffusion and the dependence of the finger Nusselt number Nu on the density ratio, it is shown that marginal stability with critical ?S is possible. The lateral fluxes induce a mean vertical velocity w0(x), which can sharpen the front, but when ?S exceeds a certain value the effect of the lateral fluxes exceeds that of w0(x) and the front weakens. Nonlinear 2D spectral calculations showed that the modification of the mean horizontal gradients is small and that the intrusions continue to grow exponentially even after they have produced overturns. By extrapolating the linear theory results beyond the overturning stage, the intrusion velocity was estimated to be proportional to the Brunt?Väisälä frequency multiplied by the intrusion thickness.
    publisherAmerican Meteorological Society
    titleDouble-Diffusive Intrusions on a Finite-Width Thermohaline Front
    typeJournal Paper
    journal volume34
    journal issue7
    journal titleJournal of Physical Oceanography
    identifier doi10.1175/1520-0485(2004)034<1723:DIOAFT>2.0.CO;2
    journal fristpage1723
    journal lastpage1740
    treeJournal of Physical Oceanography:;2004:;Volume( 034 ):;issue: 007
    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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