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    Quasi-Lagrangian Models of Nascent Thermals

    Source: Monthly Weather Review:;1981:;volume( 109 ):;issue: 009::page 1939
    Author:
    Rambaldi, Sandro
    ,
    Randall, David A.
    DOI: 10.1175/1520-0493(1981)109<1939:QLMONT>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Thermals are modeled by considering their boundaries as self-advecting vortex sheets. Both slab-symmetric and axisymmetiic geometries are considered. Discussion is restricted to the case of a neutral environment, and turbulent processes are not considered. For thermals of circular cross section, the initial accelerations are obtained analytically. A numerical method is developed to simulate the evolution of thermals by time-marching. The vortex sheet is divided into finite segments, whose positions are tracked in a quasi-Lagrangian fashion. Self-advection is considered. A redistribution procedure is adopted to prevent the segments from bunching unmanageably. The induced field of motion is fully determined both inside and outside the thermal. Results show that the axisymmetric thermal rises more quickly than the slab-symmetric thermal, that both thermals develop concave bases, that vorticity maxima occur both within the concavities and on the trailing edges, and that the leading edges are remarkably smooth.
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      Quasi-Lagrangian Models of Nascent Thermals

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4200565
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    contributor authorRambaldi, Sandro
    contributor authorRandall, David A.
    date accessioned2017-06-09T16:03:34Z
    date available2017-06-09T16:03:34Z
    date copyright1981/09/01
    date issued1981
    identifier issn0027-0644
    identifier otherams-59951.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4200565
    description abstractThermals are modeled by considering their boundaries as self-advecting vortex sheets. Both slab-symmetric and axisymmetiic geometries are considered. Discussion is restricted to the case of a neutral environment, and turbulent processes are not considered. For thermals of circular cross section, the initial accelerations are obtained analytically. A numerical method is developed to simulate the evolution of thermals by time-marching. The vortex sheet is divided into finite segments, whose positions are tracked in a quasi-Lagrangian fashion. Self-advection is considered. A redistribution procedure is adopted to prevent the segments from bunching unmanageably. The induced field of motion is fully determined both inside and outside the thermal. Results show that the axisymmetric thermal rises more quickly than the slab-symmetric thermal, that both thermals develop concave bases, that vorticity maxima occur both within the concavities and on the trailing edges, and that the leading edges are remarkably smooth.
    publisherAmerican Meteorological Society
    titleQuasi-Lagrangian Models of Nascent Thermals
    typeJournal Paper
    journal volume109
    journal issue9
    journal titleMonthly Weather Review
    identifier doi10.1175/1520-0493(1981)109<1939:QLMONT>2.0.CO;2
    journal fristpage1939
    journal lastpage1951
    treeMonthly Weather Review:;1981:;volume( 109 ):;issue: 009
    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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