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    A Subsurface Ribbon of Cool Water over the Continental Shelf off Oregon

    Source: Journal of Physical Oceanography:;1974:;Volume( 004 ):;issue: 003::page 381
    Author:
    Huyer, Adriana
    ,
    Smith, Robert L.
    DOI: 10.1175/1520-0485(1974)004<0381:ASROCW>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Observations of the hydrographic regime over the continental shelf off Oregon from the R/V Yaquina during the summer of 1972 showed the presence of an alongshore, subsurface ribbon of relatively cool water. Its properties and its evolution during the 1972 season are described. Examination of earlier observations showed that evidence of the ribbon was found during the upwelling season in almost every year between 1961 and 1971. It is usually observed when the upwelling index (the monthly mean Ekman transport directed offshore) is high. The ribbon can be accounted for by southward advection of sub-arctic water due to the coastal jet associated with upwelling. A warm temperature anomaly, occurring at somewhat higher salinity, is frequently observed inshore of the ribbon.
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      A Subsurface Ribbon of Cool Water over the Continental Shelf off Oregon

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4162230
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    contributor authorHuyer, Adriana
    contributor authorSmith, Robert L.
    date accessioned2017-06-09T14:43:56Z
    date available2017-06-09T14:43:56Z
    date copyright1974/07/01
    date issued1974
    identifier issn0022-3670
    identifier otherams-25446.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4162230
    description abstractObservations of the hydrographic regime over the continental shelf off Oregon from the R/V Yaquina during the summer of 1972 showed the presence of an alongshore, subsurface ribbon of relatively cool water. Its properties and its evolution during the 1972 season are described. Examination of earlier observations showed that evidence of the ribbon was found during the upwelling season in almost every year between 1961 and 1971. It is usually observed when the upwelling index (the monthly mean Ekman transport directed offshore) is high. The ribbon can be accounted for by southward advection of sub-arctic water due to the coastal jet associated with upwelling. A warm temperature anomaly, occurring at somewhat higher salinity, is frequently observed inshore of the ribbon.
    publisherAmerican Meteorological Society
    titleA Subsurface Ribbon of Cool Water over the Continental Shelf off Oregon
    typeJournal Paper
    journal volume4
    journal issue3
    journal titleJournal of Physical Oceanography
    identifier doi10.1175/1520-0485(1974)004<0381:ASROCW>2.0.CO;2
    journal fristpage381
    journal lastpage391
    treeJournal of Physical Oceanography:;1974:;Volume( 004 ):;issue: 003
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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