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    Dispersion Relation for Continental Shelf Waves When the Shallow Shelf Part Has an Arbitrary Width: Application to the Shelf West of Norway

    Source: Journal of Physical Oceanography:;2015:;Volume( 046 ):;issue: 002::page 537
    Author:
    Drivdal, Magnus
    ,
    Weber, Jan Erik H.
    ,
    Debernard, Jens Boldingh
    DOI: 10.1175/JPO-D-15-0023.1
    Publisher: American Meteorological Society
    Abstract: he dispersion relation for continental shelf waves (CSWs) in a shelf region with an unbounded flat outer ocean, a convex-upward exponential shelf, and an interior flat region of arbitrary width D is derived. The calculations allow for a nonzero divergence of the wave motion. Some consequences of these findings are discussed for the shelf west of Norway, where the shelf at mid-Norway is quite wide, while at Lofoten it is much narrower. Furthermore, north of Lofoten, along the opening to the Barents Sea, the shelf becomes extremely wide. In this region the conditions are nearly met for a double Kelvin wave. The paper discusses how CSWs generated along the common storm track outside southwest Norway modify as they travel along the shelf. The analytical results are compared with results from a numerical barotropic ocean model with realistic shelf topography.
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      Dispersion Relation for Continental Shelf Waves When the Shallow Shelf Part Has an Arbitrary Width: Application to the Shelf West of Norway

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    contributor authorDrivdal, Magnus
    contributor authorWeber, Jan Erik H.
    contributor authorDebernard, Jens Boldingh
    date accessioned2017-06-09T17:21:20Z
    date available2017-06-09T17:21:20Z
    date copyright2016/02/01
    date issued2015
    identifier issn0022-3670
    identifier otherams-83722.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4226979
    description abstracthe dispersion relation for continental shelf waves (CSWs) in a shelf region with an unbounded flat outer ocean, a convex-upward exponential shelf, and an interior flat region of arbitrary width D is derived. The calculations allow for a nonzero divergence of the wave motion. Some consequences of these findings are discussed for the shelf west of Norway, where the shelf at mid-Norway is quite wide, while at Lofoten it is much narrower. Furthermore, north of Lofoten, along the opening to the Barents Sea, the shelf becomes extremely wide. In this region the conditions are nearly met for a double Kelvin wave. The paper discusses how CSWs generated along the common storm track outside southwest Norway modify as they travel along the shelf. The analytical results are compared with results from a numerical barotropic ocean model with realistic shelf topography.
    publisherAmerican Meteorological Society
    titleDispersion Relation for Continental Shelf Waves When the Shallow Shelf Part Has an Arbitrary Width: Application to the Shelf West of Norway
    typeJournal Paper
    journal volume46
    journal issue2
    journal titleJournal of Physical Oceanography
    identifier doi10.1175/JPO-D-15-0023.1
    journal fristpage537
    journal lastpage549
    treeJournal of Physical Oceanography:;2015:;Volume( 046 ):;issue: 002
    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