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    A Three-Dimensional Model of the Northwest European Continental Shelf, with Application to the M4 Tide

    Source: Journal of Physical Oceanography:;1986:;Volume( 016 ):;issue: 005::page 797
    Author:
    Davies, A. M.
    DOI: 10.1175/1520-0485(1986)016<0797:ATDMOT>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The solution of the fully nonlinear three-dimensional hydrodynamic equations in polar coordinates, for tides, is developed using a finite-difference grid in the horizontal and the Galerkin method in the vertical. Using this method a three-dimensional model of the northwest European continental shelf is used to investigate the spatial distribution of the M4 tidal elevations and currants over the shelf. Computed M4 currents are compared with observations and found to he in good agreement in the Celtic Sea, although there are significant errors in the North Sea. The reasons for these discrepancies and the spatial and depth variations in the M4 currants are discussed in detail.
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      A Three-Dimensional Model of the Northwest European Continental Shelf, with Application to the M4 Tide

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4163952
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    contributor authorDavies, A. M.
    date accessioned2017-06-09T14:47:52Z
    date available2017-06-09T14:47:52Z
    date copyright1986/05/01
    date issued1986
    identifier issn0022-3670
    identifier otherams-26997.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4163952
    description abstractThe solution of the fully nonlinear three-dimensional hydrodynamic equations in polar coordinates, for tides, is developed using a finite-difference grid in the horizontal and the Galerkin method in the vertical. Using this method a three-dimensional model of the northwest European continental shelf is used to investigate the spatial distribution of the M4 tidal elevations and currants over the shelf. Computed M4 currents are compared with observations and found to he in good agreement in the Celtic Sea, although there are significant errors in the North Sea. The reasons for these discrepancies and the spatial and depth variations in the M4 currants are discussed in detail.
    publisherAmerican Meteorological Society
    titleA Three-Dimensional Model of the Northwest European Continental Shelf, with Application to the M4 Tide
    typeJournal Paper
    journal volume16
    journal issue5
    journal titleJournal of Physical Oceanography
    identifier doi10.1175/1520-0485(1986)016<0797:ATDMOT>2.0.CO;2
    journal fristpage797
    journal lastpage813
    treeJournal of Physical Oceanography:;1986:;Volume( 016 ):;issue: 005
    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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