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    The Relationship between Flux Coefficient and Entrainment Ratio in Density Currents

    Source: Journal of Physical Oceanography:;2010:;Volume( 040 ):;issue: 012::page 2713
    Author:
    Wells, Mathew
    ,
    Cenedese, Claudia
    ,
    Caulfield, C. P.
    DOI: 10.1175/2010JPO4225.1
    Publisher: American Meteorological Society
    Abstract: The authors explore the theoretical and empirical relationship between the nonlocal quantities of the entrainment ratio E, the appropriately depth- and time-averaged flux coefficient Γ, and the bulk Froude number Fro in density currents. The main theoretical result is that E = 0.125 Γ Fro2(CU3/CL)/cos?, where ? is the angle of the slope over which the density current flows, CL is the ratio the turbulent length scale to the depth of the density current, and CU is the ratio of the turbulent velocity scale to the mean velocity of the density current. In the case of high bulk Froude numbers Γ ? Fro?2 and (CU3/CL) = C? ? 1, so E ? 0.1, consistent with observations of a constant entrainment ratio in unstratified jets and weakly stratified plumes. For bulk Froude numbers close to one, Γ is constant and has a value in the range of 0.1?0.3, which means that E ? Fro2, again in agreement with observations and previous experiments. For bulk Froude numbers less than one, Γ decreases rapidly with bulk Froude number, explaining the sudden decrease in entrainment ratios that has been observed in all field and experimental observations.
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      The Relationship between Flux Coefficient and Entrainment Ratio in Density Currents

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    contributor authorWells, Mathew
    contributor authorCenedese, Claudia
    contributor authorCaulfield, C. P.
    date accessioned2017-06-09T16:36:37Z
    date available2017-06-09T16:36:37Z
    date copyright2010/12/01
    date issued2010
    identifier issn0022-3670
    identifier otherams-70887.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4212717
    description abstractThe authors explore the theoretical and empirical relationship between the nonlocal quantities of the entrainment ratio E, the appropriately depth- and time-averaged flux coefficient Γ, and the bulk Froude number Fro in density currents. The main theoretical result is that E = 0.125 Γ Fro2(CU3/CL)/cos?, where ? is the angle of the slope over which the density current flows, CL is the ratio the turbulent length scale to the depth of the density current, and CU is the ratio of the turbulent velocity scale to the mean velocity of the density current. In the case of high bulk Froude numbers Γ ? Fro?2 and (CU3/CL) = C? ? 1, so E ? 0.1, consistent with observations of a constant entrainment ratio in unstratified jets and weakly stratified plumes. For bulk Froude numbers close to one, Γ is constant and has a value in the range of 0.1?0.3, which means that E ? Fro2, again in agreement with observations and previous experiments. For bulk Froude numbers less than one, Γ decreases rapidly with bulk Froude number, explaining the sudden decrease in entrainment ratios that has been observed in all field and experimental observations.
    publisherAmerican Meteorological Society
    titleThe Relationship between Flux Coefficient and Entrainment Ratio in Density Currents
    typeJournal Paper
    journal volume40
    journal issue12
    journal titleJournal of Physical Oceanography
    identifier doi10.1175/2010JPO4225.1
    journal fristpage2713
    journal lastpage2727
    treeJournal of Physical Oceanography:;2010:;Volume( 040 ):;issue: 012
    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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