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    Subinertial Slope-Trapped Waves in the Northeastern Gulf of Mexico

    Source: Journal of Physical Oceanography:;2009:;Volume( 039 ):;issue: 006::page 1475
    Author:
    Hallock, Z. R.
    ,
    Teague, W. J.
    ,
    Jarosz, E.
    DOI: 10.1175/2009JPO3925.1
    Publisher: American Meteorological Society
    Abstract: Current velocity from moored arrays of acoustic Doppler current profilers (ADCPs) deployed on the outer shelf and slope, south of Mobile Bay in the northeastern Gulf of Mexico, shows evidence of alongslope, generally westward-propagating subinertial baroclinic Kelvin waves with periods of about 16 and 21 days, amplitudes of 5?10 cm s?1, and wavelengths of about 500 km. The observed waves were highly coherent over the slope between about 200 and 500 m and accounted for a significant amount of the current variability below 200 m. The source of the waves could be attributed to effects of the Loop Current on the west Florida slope but is more likely due to direct forcing by Loop Current?generated eddies impacting the experimental area.
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      Subinertial Slope-Trapped Waves in the Northeastern Gulf of Mexico

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4210726
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    contributor authorHallock, Z. R.
    contributor authorTeague, W. J.
    contributor authorJarosz, E.
    date accessioned2017-06-09T16:30:25Z
    date available2017-06-09T16:30:25Z
    date copyright2009/06/01
    date issued2009
    identifier issn0022-3670
    identifier otherams-69095.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4210726
    description abstractCurrent velocity from moored arrays of acoustic Doppler current profilers (ADCPs) deployed on the outer shelf and slope, south of Mobile Bay in the northeastern Gulf of Mexico, shows evidence of alongslope, generally westward-propagating subinertial baroclinic Kelvin waves with periods of about 16 and 21 days, amplitudes of 5?10 cm s?1, and wavelengths of about 500 km. The observed waves were highly coherent over the slope between about 200 and 500 m and accounted for a significant amount of the current variability below 200 m. The source of the waves could be attributed to effects of the Loop Current on the west Florida slope but is more likely due to direct forcing by Loop Current?generated eddies impacting the experimental area.
    publisherAmerican Meteorological Society
    titleSubinertial Slope-Trapped Waves in the Northeastern Gulf of Mexico
    typeJournal Paper
    journal volume39
    journal issue6
    journal titleJournal of Physical Oceanography
    identifier doi10.1175/2009JPO3925.1
    journal fristpage1475
    journal lastpage1485
    treeJournal of Physical Oceanography:;2009:;Volume( 039 ):;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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