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    Steric Contribution to the Seasonal Oscillation of Sea Level off Oregon

    Source: Journal of Physical Oceanography:;1974:;Volume( 004 ):;issue: 003::page 304
    Author:
    Brunson, Burlie A.
    ,
    Elliott, William P.
    DOI: 10.1175/1520-0485(1974)004<0304:SCTTSO>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Thermal, haline and total steric departures of sea level were calculated in a zone up to 165 n mi off Newport, Ore. The thermal and haline components were about equal in magnitudes and in phase, giving low steric sea levels nearshore and high sea levels offshore in summer and the reverse pattern in winter. These results are produced by local oceanographic conditions and reflect seasonal changes in upwelling and the position of the Columbia River plume. In the region close to shore the combined effects of steric and atmospheric-pressure-caused departures do not fully account for the observed variations of sea level. Wind stress variations are likely to be the most important cause but other factors may well contribute.
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      Steric Contribution to the Seasonal Oscillation of Sea Level off Oregon

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4162222
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    contributor authorBrunson, Burlie A.
    contributor authorElliott, William P.
    date accessioned2017-06-09T14:43:55Z
    date available2017-06-09T14:43:55Z
    date copyright1974/07/01
    date issued1974
    identifier issn0022-3670
    identifier otherams-25439.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4162222
    description abstractThermal, haline and total steric departures of sea level were calculated in a zone up to 165 n mi off Newport, Ore. The thermal and haline components were about equal in magnitudes and in phase, giving low steric sea levels nearshore and high sea levels offshore in summer and the reverse pattern in winter. These results are produced by local oceanographic conditions and reflect seasonal changes in upwelling and the position of the Columbia River plume. In the region close to shore the combined effects of steric and atmospheric-pressure-caused departures do not fully account for the observed variations of sea level. Wind stress variations are likely to be the most important cause but other factors may well contribute.
    publisherAmerican Meteorological Society
    titleSteric Contribution to the Seasonal Oscillation of Sea Level off Oregon
    typeJournal Paper
    journal volume4
    journal issue3
    journal titleJournal of Physical Oceanography
    identifier doi10.1175/1520-0485(1974)004<0304:SCTTSO>2.0.CO;2
    journal fristpage304
    journal lastpage309
    treeJournal of Physical Oceanography:;1974:;Volume( 004 ):;issue: 003
    contenttypeFulltext
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