YaBeSH Engineering and Technology Library

    • Journals
    • PaperQuest
    • YSE Standards
    • YaBeSH
    • Login
    View Item 
    •   YE&T Library
    • AMS
    • Journal of Physical Oceanography
    • View Item
    •   YE&T Library
    • AMS
    • Journal of Physical Oceanography
    • View Item
    • All Fields
    • Source Title
    • Year
    • Publisher
    • Title
    • Subject
    • Author
    • DOI
    • ISBN
    Advanced Search
    JavaScript is disabled for your browser. Some features of this site may not work without it.

    Archive

    A Numerical Model of the Oceanic Circulation around New Zealand

    Source: Journal of Physical Oceanography:;1979:;Volume( 009 ):;issue: 005::page 892
    Author:
    Bye, J. A. T.
    ,
    Heath, R. A.
    ,
    Sag, T. W.
    DOI: 10.1175/1520-0485(1979)009<0892:ANMOTO>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: A steady-state model of the ocean circulation applied to an ocean area surrounding New Zealand, driven by specified density and wind stress distributions and specified flow at the boundaries of the ocean area, has been used to obtain an estimate of the steady-state flow pattern of ocean circulation around New Zealand. The circulation is shown to be mainly barotropic on the west coast. The only current which is mainly baroclinic is the East Cape Current off the cast coast of the North Island. The value of the stream-function found on the New Zealand coastline suggests that the transport of the western boundary current in the South Pacific Ocean is greater relative to New Zealand than to Australia.
    • Download: (524.1Kb)
    • Show Full MetaData Hide Full MetaData
    • Item Order
    • Go To Publisher
    • Price: 5000 Rial
    • Statistics

      A Numerical Model of the Oceanic Circulation around New Zealand

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4162803
    Collections
    • Journal of Physical Oceanography

    Show full item record

    contributor authorBye, J. A. T.
    contributor authorHeath, R. A.
    contributor authorSag, T. W.
    date accessioned2017-06-09T14:45:11Z
    date available2017-06-09T14:45:11Z
    date copyright1979/09/01
    date issued1979
    identifier issn0022-3670
    identifier otherams-25962.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4162803
    description abstractA steady-state model of the ocean circulation applied to an ocean area surrounding New Zealand, driven by specified density and wind stress distributions and specified flow at the boundaries of the ocean area, has been used to obtain an estimate of the steady-state flow pattern of ocean circulation around New Zealand. The circulation is shown to be mainly barotropic on the west coast. The only current which is mainly baroclinic is the East Cape Current off the cast coast of the North Island. The value of the stream-function found on the New Zealand coastline suggests that the transport of the western boundary current in the South Pacific Ocean is greater relative to New Zealand than to Australia.
    publisherAmerican Meteorological Society
    titleA Numerical Model of the Oceanic Circulation around New Zealand
    typeJournal Paper
    journal volume9
    journal issue5
    journal titleJournal of Physical Oceanography
    identifier doi10.1175/1520-0485(1979)009<0892:ANMOTO>2.0.CO;2
    journal fristpage892
    journal lastpage899
    treeJournal of Physical Oceanography:;1979:;Volume( 009 ):;issue: 005
    contenttypeFulltext
    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
    yabeshDSpacePersian
     
    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
    yabeshDSpacePersian