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    Sponginess and Drop Shedding of Gyrating Hailstones in a Pressure-Controlled Icing Wind Tunnel

    Source: Journal of the Atmospheric Sciences:;1986:;Volume( 043 ):;issue: 023::page 2813
    Author:
    Lesins, G. B.
    ,
    List, Roland
    DOI: 10.1175/1520-0469(1986)043<2813:SADSOG>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Artificial hailstones were grown in an icing wind tunnel under simulated natural conditions, starting from oblate ice spheroids with major and minor diameters of 2.0 and 1.3 cm respectively, while undergoing symmetric gyration. The experiments were performed at air temperatures from ?25° to ?2°C, air pressures from 35.5 to 102.0 kPa, liquid water contents from 0.5 to 20 g m ?3 and for hailstone spin and nutation/precession rates up to 35 Hz. The net collection efficiency, ice fraction and final aspect ratio were determined for each icing trial. The experimentally determined boundary between growth of ice and spongy deposits agrees well with the theoretical Schumann-Ludlam limit (SLL), adapted for spheroids. This is not necessarily expected since the SLL is based on bulk considerations. Six distinct deposit growth regimes [dry (ice, with some air), moist (wet surface but solid interior), spongy, spongy-shedding, soaked-shedding (soaked: high water content deposit) and dry-shedding] were found by varying air temperature, liquid water content and nutation/procession rate of the hailstones. The rotational effects were divided into three distinct ranges: low (0.5 to 9 Hz), intermediate (9 to 20 Hz) and high (>20 Hz). The fraction of unfrozen accreted water in wet growth that is shed from a hailstone as opposed to being incorporated in spongy ice was determined. Within the experimental conditions the mass amount of liquid water in spongy ice was found to be limited to 50%. Aerodynamic molding, which is the shaping of a nonrigid body by pressure forces, is significant for a variety of wet growth conditions. Other main findings are 1) the shedding of water drops and spongy ice formation can occur concurrently, 2) shedding canine observed during growth of solid deposits if the rotation rates are high enough, 3) millimeter- sized water drops are produced by shedding and 4) the hailstone's angular motion has a significant influence on its growth characteristics.
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      Sponginess and Drop Shedding of Gyrating Hailstones in a Pressure-Controlled Icing Wind Tunnel

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4155521
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    contributor authorLesins, G. B.
    contributor authorList, Roland
    date accessioned2017-06-09T14:26:52Z
    date available2017-06-09T14:26:52Z
    date copyright1986/12/01
    date issued1986
    identifier issn0022-4928
    identifier otherams-19408.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4155521
    description abstractArtificial hailstones were grown in an icing wind tunnel under simulated natural conditions, starting from oblate ice spheroids with major and minor diameters of 2.0 and 1.3 cm respectively, while undergoing symmetric gyration. The experiments were performed at air temperatures from ?25° to ?2°C, air pressures from 35.5 to 102.0 kPa, liquid water contents from 0.5 to 20 g m ?3 and for hailstone spin and nutation/precession rates up to 35 Hz. The net collection efficiency, ice fraction and final aspect ratio were determined for each icing trial. The experimentally determined boundary between growth of ice and spongy deposits agrees well with the theoretical Schumann-Ludlam limit (SLL), adapted for spheroids. This is not necessarily expected since the SLL is based on bulk considerations. Six distinct deposit growth regimes [dry (ice, with some air), moist (wet surface but solid interior), spongy, spongy-shedding, soaked-shedding (soaked: high water content deposit) and dry-shedding] were found by varying air temperature, liquid water content and nutation/procession rate of the hailstones. The rotational effects were divided into three distinct ranges: low (0.5 to 9 Hz), intermediate (9 to 20 Hz) and high (>20 Hz). The fraction of unfrozen accreted water in wet growth that is shed from a hailstone as opposed to being incorporated in spongy ice was determined. Within the experimental conditions the mass amount of liquid water in spongy ice was found to be limited to 50%. Aerodynamic molding, which is the shaping of a nonrigid body by pressure forces, is significant for a variety of wet growth conditions. Other main findings are 1) the shedding of water drops and spongy ice formation can occur concurrently, 2) shedding canine observed during growth of solid deposits if the rotation rates are high enough, 3) millimeter- sized water drops are produced by shedding and 4) the hailstone's angular motion has a significant influence on its growth characteristics.
    publisherAmerican Meteorological Society
    titleSponginess and Drop Shedding of Gyrating Hailstones in a Pressure-Controlled Icing Wind Tunnel
    typeJournal Paper
    journal volume43
    journal issue23
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1986)043<2813:SADSOG>2.0.CO;2
    journal fristpage2813
    journal lastpage2825
    treeJournal of the Atmospheric Sciences:;1986:;Volume( 043 ):;issue: 023
    contenttypeFulltext
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