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    Turbulent Dissipation Over the Continental Slope Off Vancouver Island

    Source: Journal of Physical Oceanography:;1983:;Volume( 013 ):;issue: 010::page 1809
    Author:
    Lueck, Rolf G.
    ,
    Crawford, William R.
    ,
    Osborn, Thomas R.
    DOI: 10.1175/1520-0485(1983)013<1809:TDOTCS>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Thirteen profiles of the rate of viscous dissipation of turbulent kinetic energy &epsi? were made over the continental slope off Vancouver Island between 12 and 14 May 1980 in conjunction with CTD and moored current-meter observations. Systematic variability was observed in the vertical but not in the horizontal direction. Above 200 m depth numerous salt-stabilized temperature inversions were seen and dissipation rates were significantly larger than below 200 m. Dissipation rates below 200 m are the lowest ever reported and coincide with a low level of energetics revealed by the current meter moorings. Comparison with the Garrett-Munk internal wave spectrum indicates an e-folding decay time of internal wave energy of ?50 days at depths below 200 m.
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      Turbulent Dissipation Over the Continental Slope Off Vancouver Island

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4163497
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    contributor authorLueck, Rolf G.
    contributor authorCrawford, William R.
    contributor authorOsborn, Thomas R.
    date accessioned2017-06-09T14:46:46Z
    date available2017-06-09T14:46:46Z
    date copyright1983/10/01
    date issued1983
    identifier issn0022-3670
    identifier otherams-26587.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4163497
    description abstractThirteen profiles of the rate of viscous dissipation of turbulent kinetic energy &epsi? were made over the continental slope off Vancouver Island between 12 and 14 May 1980 in conjunction with CTD and moored current-meter observations. Systematic variability was observed in the vertical but not in the horizontal direction. Above 200 m depth numerous salt-stabilized temperature inversions were seen and dissipation rates were significantly larger than below 200 m. Dissipation rates below 200 m are the lowest ever reported and coincide with a low level of energetics revealed by the current meter moorings. Comparison with the Garrett-Munk internal wave spectrum indicates an e-folding decay time of internal wave energy of ?50 days at depths below 200 m.
    publisherAmerican Meteorological Society
    titleTurbulent Dissipation Over the Continental Slope Off Vancouver Island
    typeJournal Paper
    journal volume13
    journal issue10
    journal titleJournal of Physical Oceanography
    identifier doi10.1175/1520-0485(1983)013<1809:TDOTCS>2.0.CO;2
    journal fristpage1809
    journal lastpage1818
    treeJournal of Physical Oceanography:;1983:;Volume( 013 ):;issue: 010
    contenttypeFulltext
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