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    Three-Dimensional Structure of Forced Gravity Waves and Lee Waves

    Source: Journal of the Atmospheric Sciences:;2004:;Volume( 061 ):;issue: 006::page 664
    Author:
    Sharman, R. D.
    ,
    Wurtele, M. G.
    DOI: 10.1175/1520-0469(2004)061<0664:TSOFGW>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The three-dimensional structure of lee waves is investigated using a combination of linear analysis and numerical simulation. The forcings are represented by flow over a single wave (monochromatic) in the along-stream direction but of limited extent in the cross-stream direction, and by flow over isolated obstacles. The flow structures considered are of constant static stability, and zero, positive, and negative basic-flow shears. Both nonhydrostatic and hydrostatic regimes are studied. Particular emphasis is placed on 1) the cross-stream structure of the waves, 2) the transition from three-dimensional to two-dimensional flow as the breadth of the obstacle is increased, 3) the criteria for three-dimensional nonhydrostatic to hydrostatic transitions, and 4) the effect of obstacle breadth-to-length aspect ratio on the wave drag for this linear system. It is shown that these aspects can in part be understood by relating the gravity waves produced by narrow-breadth obstacles to the ?St. Andrew's Cross? for hydrostatic and nonhydrostatic uniform flow and for hydrostatic shear flow.
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      Three-Dimensional Structure of Forced Gravity Waves and Lee Waves

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4159996
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    contributor authorSharman, R. D.
    contributor authorWurtele, M. G.
    date accessioned2017-06-09T14:38:38Z
    date available2017-06-09T14:38:38Z
    date copyright2004/03/01
    date issued2004
    identifier issn0022-4928
    identifier otherams-23435.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4159996
    description abstractThe three-dimensional structure of lee waves is investigated using a combination of linear analysis and numerical simulation. The forcings are represented by flow over a single wave (monochromatic) in the along-stream direction but of limited extent in the cross-stream direction, and by flow over isolated obstacles. The flow structures considered are of constant static stability, and zero, positive, and negative basic-flow shears. Both nonhydrostatic and hydrostatic regimes are studied. Particular emphasis is placed on 1) the cross-stream structure of the waves, 2) the transition from three-dimensional to two-dimensional flow as the breadth of the obstacle is increased, 3) the criteria for three-dimensional nonhydrostatic to hydrostatic transitions, and 4) the effect of obstacle breadth-to-length aspect ratio on the wave drag for this linear system. It is shown that these aspects can in part be understood by relating the gravity waves produced by narrow-breadth obstacles to the ?St. Andrew's Cross? for hydrostatic and nonhydrostatic uniform flow and for hydrostatic shear flow.
    publisherAmerican Meteorological Society
    titleThree-Dimensional Structure of Forced Gravity Waves and Lee Waves
    typeJournal Paper
    journal volume61
    journal issue6
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(2004)061<0664:TSOFGW>2.0.CO;2
    journal fristpage664
    journal lastpage681
    treeJournal of the Atmospheric Sciences:;2004:;Volume( 061 ):;issue: 006
    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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