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    A Sensitivity Study of Reduced-Gravity Channel Flows with Application to the Alborán Sea

    Source: Journal of Physical Oceanography:;1988:;Volume( 018 ):;issue: 002::page 373
    Author:
    Werner, Francisco E.
    ,
    Cantos-Figuerola, Alán
    ,
    Parrilla, Gregorio
    DOI: 10.1175/1520-0485(1988)018<0373:ASSORG>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The reduced-gravity response of an hydraulically-forced flow in a rectangular channel is examined numerically. The model parameters were set by observed features of the circulation in the westernmost basin of the Mediterranean Sea?the Alborán Sea. Numerical experiments reveal that the solution depends critically on the inclusion of the momentum advection terms and on the form of the boundary condition on the domain's sidewalls. In particular, while free-slip conditions show a coastally trapped current on the model's southern boundary, no-slip conditions cause the formation of an anticyclonic gyre upon the flow's entry into the basin.
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      A Sensitivity Study of Reduced-Gravity Channel Flows with Application to the Alborán Sea

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4164328
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    contributor authorWerner, Francisco E.
    contributor authorCantos-Figuerola, Alán
    contributor authorParrilla, Gregorio
    date accessioned2017-06-09T14:48:48Z
    date available2017-06-09T14:48:48Z
    date copyright1988/02/01
    date issued1988
    identifier issn0022-3670
    identifier otherams-27334.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4164328
    description abstractThe reduced-gravity response of an hydraulically-forced flow in a rectangular channel is examined numerically. The model parameters were set by observed features of the circulation in the westernmost basin of the Mediterranean Sea?the Alborán Sea. Numerical experiments reveal that the solution depends critically on the inclusion of the momentum advection terms and on the form of the boundary condition on the domain's sidewalls. In particular, while free-slip conditions show a coastally trapped current on the model's southern boundary, no-slip conditions cause the formation of an anticyclonic gyre upon the flow's entry into the basin.
    publisherAmerican Meteorological Society
    titleA Sensitivity Study of Reduced-Gravity Channel Flows with Application to the Alborán Sea
    typeJournal Paper
    journal volume18
    journal issue2
    journal titleJournal of Physical Oceanography
    identifier doi10.1175/1520-0485(1988)018<0373:ASSORG>2.0.CO;2
    journal fristpage373
    journal lastpage383
    treeJournal of Physical Oceanography:;1988:;Volume( 018 ):;issue: 002
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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