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    Buoyant Motion of a Turbulent Thermal

    Source: Journal of the Atmospheric Sciences:;2018:;volume 075:;issue 009::page 3233
    Author:
    Tarshish, Nathaniel
    ,
    Jeevanjee, Nadir
    ,
    Lecoanet, Daniel
    DOI: 10.1175/JAS-D-17-0371.1
    Publisher: American Meteorological Society
    Abstract: AbstractBy introducing an equivalence between magnetostatics and the equations governing buoyant motion, we derive analytical expressions for the acceleration of isolated density anomalies (thermals). In particular, we investigate buoyant acceleration, defined as the sum of the Archimedean buoyancy B and an associated perturbation pressure gradient. For the case of a uniform spherical thermal, the anomaly fluid accelerates at 2B/3, extending the textbook result for the induced mass of a solid sphere to the case of a fluid sphere. For a more general ellipsoidal thermal, we show that the buoyant acceleration is a simple analytical function of the ellipsoid?s aspect ratio. The relevance of these idealized uniform-density results to turbulent thermals is explored by analyzing direct numerical simulations of thermals at a Reynolds number (Re) of 6300. We find that our results fully characterize a thermal?s initial motion over a distance comparable to its length. Beyond this buoyancy-dominated regime, a thermal develops an ellipsoidal vortex circulation and begins to entrain environmental fluid. Our analytical expressions do not describe the total acceleration of this mature thermal, but they still accurately relate the buoyant acceleration to the thermal?s mean Archimedean buoyancy and aspect ratio. Thus, our analytical formulas provide a simple and direct means of estimating the buoyant acceleration of turbulent thermals.
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      Buoyant Motion of a Turbulent Thermal

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    https://yetl.yabesh.ir/yetl1/handle/yetl/4261879
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    contributor authorTarshish, Nathaniel
    contributor authorJeevanjee, Nadir
    contributor authorLecoanet, Daniel
    date accessioned2019-09-19T10:07:54Z
    date available2019-09-19T10:07:54Z
    date copyright6/28/2018 12:00:00 AM
    date issued2018
    identifier otherjas-d-17-0371.1.pdf
    identifier urihttp://yetl.yabesh.ir/yetl1/handle/yetl/4261879
    description abstractAbstractBy introducing an equivalence between magnetostatics and the equations governing buoyant motion, we derive analytical expressions for the acceleration of isolated density anomalies (thermals). In particular, we investigate buoyant acceleration, defined as the sum of the Archimedean buoyancy B and an associated perturbation pressure gradient. For the case of a uniform spherical thermal, the anomaly fluid accelerates at 2B/3, extending the textbook result for the induced mass of a solid sphere to the case of a fluid sphere. For a more general ellipsoidal thermal, we show that the buoyant acceleration is a simple analytical function of the ellipsoid?s aspect ratio. The relevance of these idealized uniform-density results to turbulent thermals is explored by analyzing direct numerical simulations of thermals at a Reynolds number (Re) of 6300. We find that our results fully characterize a thermal?s initial motion over a distance comparable to its length. Beyond this buoyancy-dominated regime, a thermal develops an ellipsoidal vortex circulation and begins to entrain environmental fluid. Our analytical expressions do not describe the total acceleration of this mature thermal, but they still accurately relate the buoyant acceleration to the thermal?s mean Archimedean buoyancy and aspect ratio. Thus, our analytical formulas provide a simple and direct means of estimating the buoyant acceleration of turbulent thermals.
    publisherAmerican Meteorological Society
    titleBuoyant Motion of a Turbulent Thermal
    typeJournal Paper
    journal volume75
    journal issue9
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/JAS-D-17-0371.1
    journal fristpage3233
    journal lastpage3244
    treeJournal of the Atmospheric Sciences:;2018:;volume 075:;issue 009
    contenttypeFulltext
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