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    Dynamics in the Deep Canada Basin, Arctic Ocean, Inferred by Thermistor Chain Time Series

    Source: Journal of Physical Oceanography:;2007:;Volume( 037 ):;issue: 004::page 1066
    Author:
    Timmermans, M-L.
    ,
    Melling, H.
    ,
    Rainville, L.
    DOI: 10.1175/JPO3032.1
    Publisher: American Meteorological Society
    Abstract: A 50-day time series of high-resolution temperature in the deepest layers of the Canada Basin in the Arctic Ocean indicates that the deep Canada Basin is a dynamically active environment, not the quiet, stable basin often assumed. Vertical motions at the near-inertial (tidal) frequency have amplitudes of 10? 20 m. These vertical displacements are surprisingly large considering the downward near-inertial internal wave energy flux typically observed in the Canada Basin. In addition to motion in the internal-wave frequency band, the measurements indicate distinctive subinertial temperature fluctuations, possibly due to intrusions of new water masses.
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      Dynamics in the Deep Canada Basin, Arctic Ocean, Inferred by Thermistor Chain Time Series

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4226074
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    contributor authorTimmermans, M-L.
    contributor authorMelling, H.
    contributor authorRainville, L.
    date accessioned2017-06-09T17:18:33Z
    date available2017-06-09T17:18:33Z
    date copyright2007/04/01
    date issued2007
    identifier issn0022-3670
    identifier otherams-82908.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4226074
    description abstractA 50-day time series of high-resolution temperature in the deepest layers of the Canada Basin in the Arctic Ocean indicates that the deep Canada Basin is a dynamically active environment, not the quiet, stable basin often assumed. Vertical motions at the near-inertial (tidal) frequency have amplitudes of 10? 20 m. These vertical displacements are surprisingly large considering the downward near-inertial internal wave energy flux typically observed in the Canada Basin. In addition to motion in the internal-wave frequency band, the measurements indicate distinctive subinertial temperature fluctuations, possibly due to intrusions of new water masses.
    publisherAmerican Meteorological Society
    titleDynamics in the Deep Canada Basin, Arctic Ocean, Inferred by Thermistor Chain Time Series
    typeJournal Paper
    journal volume37
    journal issue4
    journal titleJournal of Physical Oceanography
    identifier doi10.1175/JPO3032.1
    journal fristpage1066
    journal lastpage1076
    treeJournal of Physical Oceanography:;2007:;Volume( 037 ):;issue: 004
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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