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    Numerical Simulation of Three-Dimensional Unsteady Flow past Ice Crystals

    Source: Journal of the Atmospheric Sciences:;1997:;Volume( 054 ):;issue: 018::page 2261
    Author:
    Wang, Pao K.
    ,
    Ji, Wusheng
    DOI: 10.1175/1520-0469(1997)054<2261:NSOTDU>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The unsteady flow fields around falling columnar ice crystals, hexagonal ice plates, and broad-branch crystals are simulated by numerically solving the time-dependent Navier?Stokes equations appropriate for these geometries in the primitive equation form. A predictor?corrector method and a quadratic interpolation for convective kinematics (QUICK) scheme are applied on nonuniform grids to determine the velocity fields. The ice crystals are held in fixed orientation but time-dependent behaviors such as eddy shedding are allowed to occur by imposing an initial perturbation with a magnitude 30% of the free-stream velocity. The computed flow fields cover a Reynolds number range from 0.1 to about 200, being slightly different for different crystal habits. Examples of velocity fields are illustrated. The computed drag coefficients for cylinders agree with experimental values to within a few percent, while those for hexagonal plates agree with experimental values and previous calculations by Pitter et al. to less than 15% even though the aspect ratios are different. The drag coefficients for broad-branch crystals are higher than those for hexagonal plates at the same Reynolds numbers. Special features of flow passing through the branch gaps of broad-branch crystals suggest that it may be possible to use a creeping flow assumption to treat flow passing through spaces in complicated dendritic crystals.
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      Numerical Simulation of Three-Dimensional Unsteady Flow past Ice Crystals

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4158456
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    contributor authorWang, Pao K.
    contributor authorJi, Wusheng
    date accessioned2017-06-09T14:34:40Z
    date available2017-06-09T14:34:40Z
    date copyright1997/09/01
    date issued1997
    identifier issn0022-4928
    identifier otherams-22049.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4158456
    description abstractThe unsteady flow fields around falling columnar ice crystals, hexagonal ice plates, and broad-branch crystals are simulated by numerically solving the time-dependent Navier?Stokes equations appropriate for these geometries in the primitive equation form. A predictor?corrector method and a quadratic interpolation for convective kinematics (QUICK) scheme are applied on nonuniform grids to determine the velocity fields. The ice crystals are held in fixed orientation but time-dependent behaviors such as eddy shedding are allowed to occur by imposing an initial perturbation with a magnitude 30% of the free-stream velocity. The computed flow fields cover a Reynolds number range from 0.1 to about 200, being slightly different for different crystal habits. Examples of velocity fields are illustrated. The computed drag coefficients for cylinders agree with experimental values to within a few percent, while those for hexagonal plates agree with experimental values and previous calculations by Pitter et al. to less than 15% even though the aspect ratios are different. The drag coefficients for broad-branch crystals are higher than those for hexagonal plates at the same Reynolds numbers. Special features of flow passing through the branch gaps of broad-branch crystals suggest that it may be possible to use a creeping flow assumption to treat flow passing through spaces in complicated dendritic crystals.
    publisherAmerican Meteorological Society
    titleNumerical Simulation of Three-Dimensional Unsteady Flow past Ice Crystals
    typeJournal Paper
    journal volume54
    journal issue18
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1997)054<2261:NSOTDU>2.0.CO;2
    journal fristpage2261
    journal lastpage2274
    treeJournal of the Atmospheric Sciences:;1997:;Volume( 054 ):;issue: 018
    contenttypeFulltext
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