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

    Poleward Heat Fluxes in Southern Hemisphere Oceans

    Source: Journal of Physical Oceanography:;1978:;Volume( 008 ):;issue: 005::page 785
    Author:
    Bennett, A. F.
    DOI: 10.1175/1520-0485(1978)008<0785:PHFISH>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: A direct estimate of oceanic meridional heat flux at 30°8 yields a result between +1.15 ? 1015 W and +2.27 ? 1015 W. The estimate is based on hydrographic data from individual cruises and climatological wind data. The northward sign of the flux is due largely to the baroclinic flux components, and it contradicts the indirect estimate of Sellers (1966) based on meteorological data only. The mid-ocean eddy field introduces variability into the estimates, but a 95% confidence interval is calculated to be only ±0.8 ? 1015 W. The actual baroclinic heat flux due to the mid-ocean eddies is estimated to be only about 1015 W in magnitude, but the actual barotropic eddy heat flux may be at least as large as 1015 W.
    • Download: (981.0Kb)
    • Show Full MetaData Hide Full MetaData
    • Item Order
    • Go To Publisher
    • Price: 5000 Rial
    • Statistics

      Poleward Heat Fluxes in Southern Hemisphere Oceans

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4162669
    Collections
    • Journal of Physical Oceanography

    Show full item record

    contributor authorBennett, A. F.
    date accessioned2017-06-09T14:44:50Z
    date available2017-06-09T14:44:50Z
    date copyright1978/09/01
    date issued1978
    identifier issn0022-3670
    identifier otherams-25841.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4162669
    description abstractA direct estimate of oceanic meridional heat flux at 30°8 yields a result between +1.15 ? 1015 W and +2.27 ? 1015 W. The estimate is based on hydrographic data from individual cruises and climatological wind data. The northward sign of the flux is due largely to the baroclinic flux components, and it contradicts the indirect estimate of Sellers (1966) based on meteorological data only. The mid-ocean eddy field introduces variability into the estimates, but a 95% confidence interval is calculated to be only ±0.8 ? 1015 W. The actual baroclinic heat flux due to the mid-ocean eddies is estimated to be only about 1015 W in magnitude, but the actual barotropic eddy heat flux may be at least as large as 1015 W.
    publisherAmerican Meteorological Society
    titlePoleward Heat Fluxes in Southern Hemisphere Oceans
    typeJournal Paper
    journal volume8
    journal issue5
    journal titleJournal of Physical Oceanography
    identifier doi10.1175/1520-0485(1978)008<0785:PHFISH>2.0.CO;2
    journal fristpage785
    journal lastpage798
    treeJournal of Physical Oceanography:;1978:;Volume( 008 ):;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