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    Computation of the Streamfunction and Velocity Potential and Reconstruction of the Wind Field

    Source: Monthly Weather Review:;1986:;volume( 114 ):;issue: 008::page 1547
    Author:
    Bijlsma, S. J.
    ,
    Hafkenscheid, L. M.
    ,
    Lynch, Peter
    DOI: 10.1175/1520-0493(1986)114<1547:COTSAV>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: A wind field given over a limited domain can be partitioned into nondivergent and irrotational components in an infinity of ways. A particular solution, selected by requiring the velocity potential to vanish on the boundary, has minimum divergent kinetic energy and is numerically easy to obtain. The reconstruction of the wind field from the vorticity and divergence together with the boundary velocity is more difficult, since the potential equations are coupled by the boundary conditions. A numerical procedure is devised, which solves the two potential equations simultaneously, modifying both interior and boundary values in a converging iterative technique. The method is capable of reconstructing the wind field to any accuracy desired.
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      Computation of the Streamfunction and Velocity Potential and Reconstruction of the Wind Field

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4201585
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    • Monthly Weather Review

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    contributor authorBijlsma, S. J.
    contributor authorHafkenscheid, L. M.
    contributor authorLynch, Peter
    date accessioned2017-06-09T16:05:53Z
    date available2017-06-09T16:05:53Z
    date copyright1986/08/01
    date issued1986
    identifier issn0027-0644
    identifier otherams-60868.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4201585
    description abstractA wind field given over a limited domain can be partitioned into nondivergent and irrotational components in an infinity of ways. A particular solution, selected by requiring the velocity potential to vanish on the boundary, has minimum divergent kinetic energy and is numerically easy to obtain. The reconstruction of the wind field from the vorticity and divergence together with the boundary velocity is more difficult, since the potential equations are coupled by the boundary conditions. A numerical procedure is devised, which solves the two potential equations simultaneously, modifying both interior and boundary values in a converging iterative technique. The method is capable of reconstructing the wind field to any accuracy desired.
    publisherAmerican Meteorological Society
    titleComputation of the Streamfunction and Velocity Potential and Reconstruction of the Wind Field
    typeJournal Paper
    journal volume114
    journal issue8
    journal titleMonthly Weather Review
    identifier doi10.1175/1520-0493(1986)114<1547:COTSAV>2.0.CO;2
    journal fristpage1547
    journal lastpage1551
    treeMonthly Weather Review:;1986:;volume( 114 ):;issue: 008
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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