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    Three-Dimensional Representations of Hexagonal Ice Crystals and Hail Particles of Elliptical Cross Sections

    Source: Journal of the Atmospheric Sciences:;1999:;Volume( 056 ):;issue: 008::page 1089
    Author:
    Wang, Pao K.
    DOI: 10.1175/1520-0469(1999)056<1089:TDROHI>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Mathematical expressions based on earlier ideas of the author are given to describe the three-dimensional surfaces of hexagonal ice crystals and conical graupel and hail particles. In the former class, the expressions closely parallel the expression for prolate spheroid but the cross section is transformed into a hexagon by an expression designed previously. A special transformation containing a preset constant, ε, is implemented so that the three-dimensional, instead of two-dimensional, surface of the crystal is described. In the case of conical particles with elliptical cross sections, the equation that describes a conical body of revolution is modified to describe conical bodies with elliptical cross sections.
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      Three-Dimensional Representations of Hexagonal Ice Crystals and Hail Particles of Elliptical Cross Sections

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4158743
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    contributor authorWang, Pao K.
    date accessioned2017-06-09T14:35:22Z
    date available2017-06-09T14:35:22Z
    date copyright1999/04/01
    date issued1999
    identifier issn0022-4928
    identifier otherams-22307.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4158743
    description abstractMathematical expressions based on earlier ideas of the author are given to describe the three-dimensional surfaces of hexagonal ice crystals and conical graupel and hail particles. In the former class, the expressions closely parallel the expression for prolate spheroid but the cross section is transformed into a hexagon by an expression designed previously. A special transformation containing a preset constant, ε, is implemented so that the three-dimensional, instead of two-dimensional, surface of the crystal is described. In the case of conical particles with elliptical cross sections, the equation that describes a conical body of revolution is modified to describe conical bodies with elliptical cross sections.
    publisherAmerican Meteorological Society
    titleThree-Dimensional Representations of Hexagonal Ice Crystals and Hail Particles of Elliptical Cross Sections
    typeJournal Paper
    journal volume56
    journal issue8
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1999)056<1089:TDROHI>2.0.CO;2
    journal fristpage1089
    journal lastpage1093
    treeJournal of the Atmospheric Sciences:;1999:;Volume( 056 ):;issue: 008
    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
    yabeshDSpacePersian