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    Biweekly Periodic Deep Flow Variability on the Slope Inshore of the Kuril–Kamchatka Trench

    Source: Journal of Physical Oceanography:;2000:;Volume( 030 ):;issue: 012::page 3249
    Author:
    Uehara, Kazuyuki
    ,
    Miyake, Hideo
    DOI: 10.1175/1520-0485(2000)030<3249:BPDFVO>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Five long-term current records are analyzed to investigate the temporal variability for deep flows, from a single mooring fitted with two current meters on the slope inshore of the southern end of the Kuril?Kamchatka Trench southeast of Cape Erimo, where the Oyashio and a deep western boundary current are considered to flow southwestward together. At 3000 m the spectral peaks of eddy kinetic energy were found at about 2 weeks in all current records. The flow variability with period of 2 weeks at 3000 m was more energetic than that at 1000 m. By applying topographic Rossby wave theory, this variability is thought to be due to bottom-trapped topographic Rossby waves.
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      Biweekly Periodic Deep Flow Variability on the Slope Inshore of the Kuril–Kamchatka Trench

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4166574
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    contributor authorUehara, Kazuyuki
    contributor authorMiyake, Hideo
    date accessioned2017-06-09T14:54:18Z
    date available2017-06-09T14:54:18Z
    date copyright2000/12/01
    date issued2000
    identifier issn0022-3670
    identifier otherams-29356.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4166574
    description abstractFive long-term current records are analyzed to investigate the temporal variability for deep flows, from a single mooring fitted with two current meters on the slope inshore of the southern end of the Kuril?Kamchatka Trench southeast of Cape Erimo, where the Oyashio and a deep western boundary current are considered to flow southwestward together. At 3000 m the spectral peaks of eddy kinetic energy were found at about 2 weeks in all current records. The flow variability with period of 2 weeks at 3000 m was more energetic than that at 1000 m. By applying topographic Rossby wave theory, this variability is thought to be due to bottom-trapped topographic Rossby waves.
    publisherAmerican Meteorological Society
    titleBiweekly Periodic Deep Flow Variability on the Slope Inshore of the Kuril–Kamchatka Trench
    typeJournal Paper
    journal volume30
    journal issue12
    journal titleJournal of Physical Oceanography
    identifier doi10.1175/1520-0485(2000)030<3249:BPDFVO>2.0.CO;2
    journal fristpage3249
    journal lastpage3260
    treeJournal of Physical Oceanography:;2000:;Volume( 030 ):;issue: 012
    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