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    External Rossby Waves in the Two-Layer Model

    Source: Journal of the Atmospheric Sciences:;1987:;Volume( 044 ):;issue: 020::page 2924
    Author:
    Panetta, R. Lee
    ,
    Held, Isaac M.
    ,
    Pierrehumbert, Raymond T.
    DOI: 10.1175/1520-0469(1987)044<2924:ERWITT>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: In order to clarify the extent to which the two-layer model can successfully simulate the remote tropospheric response to localized stationary forcing, the structure of stationary Rossby waves in the two-layer model is compared with that in continuous models. One finds a close correspondence when the two-layer flow is supercritical in the sense of the Phillips' criterion, except for the possibility of upstream propagation in the two-layer model when the lower-layer wind is small. When the two-layer flow is subcritical, the stationary waves can be very seriously distorted. The manner in which neutral modes are spatially or temporally destabilized by damping in the two-layer model is contrasted with similar results for Charney's model.
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      External Rossby Waves in the Two-Layer Model

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4155786
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    contributor authorPanetta, R. Lee
    contributor authorHeld, Isaac M.
    contributor authorPierrehumbert, Raymond T.
    date accessioned2017-06-09T14:27:41Z
    date available2017-06-09T14:27:41Z
    date copyright1987/10/01
    date issued1987
    identifier issn0022-4928
    identifier otherams-19647.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4155786
    description abstractIn order to clarify the extent to which the two-layer model can successfully simulate the remote tropospheric response to localized stationary forcing, the structure of stationary Rossby waves in the two-layer model is compared with that in continuous models. One finds a close correspondence when the two-layer flow is supercritical in the sense of the Phillips' criterion, except for the possibility of upstream propagation in the two-layer model when the lower-layer wind is small. When the two-layer flow is subcritical, the stationary waves can be very seriously distorted. The manner in which neutral modes are spatially or temporally destabilized by damping in the two-layer model is contrasted with similar results for Charney's model.
    publisherAmerican Meteorological Society
    titleExternal Rossby Waves in the Two-Layer Model
    typeJournal Paper
    journal volume44
    journal issue20
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1987)044<2924:ERWITT>2.0.CO;2
    journal fristpage2924
    journal lastpage2933
    treeJournal of the Atmospheric Sciences:;1987:;Volume( 044 ):;issue: 020
    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