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

    The Effect of the New England Seamounts on Gulf Stream Meandering as Observed from Satellite IR Imagery

    Source: Journal of Physical Oceanography:;1986:;Volume( 016 ):;issue: 002::page 386
    Author:
    Cornillon, Peter
    DOI: 10.1175/1520-0485(1986)016<0386:TEOTNE>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: It is commonly held belief that meandering of the Gulf Stream increases dramatically downstream of the New England Seamount chain. In fact this appears not to be the case. The envelope of Gulf Stream northern edges derived from 30 months of satellite data remains constant from 65° to 58°W. Only the mean of the integrated path length normalized by the mean path length appears to increase downstream of the seamounts, but at very nearly the same rate as upstream of them.
    • Download: (342.8Kb)
    • Show Full MetaData Hide Full MetaData
    • Item Order
    • Go To Publisher
    • Price: 5000 Rial
    • Statistics

      The Effect of the New England Seamounts on Gulf Stream Meandering as Observed from Satellite IR Imagery

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4163917
    Collections
    • Journal of Physical Oceanography

    Show full item record

    contributor authorCornillon, Peter
    date accessioned2017-06-09T14:47:48Z
    date available2017-06-09T14:47:48Z
    date copyright1986/02/01
    date issued1986
    identifier issn0022-3670
    identifier otherams-26965.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4163917
    description abstractIt is commonly held belief that meandering of the Gulf Stream increases dramatically downstream of the New England Seamount chain. In fact this appears not to be the case. The envelope of Gulf Stream northern edges derived from 30 months of satellite data remains constant from 65° to 58°W. Only the mean of the integrated path length normalized by the mean path length appears to increase downstream of the seamounts, but at very nearly the same rate as upstream of them.
    publisherAmerican Meteorological Society
    titleThe Effect of the New England Seamounts on Gulf Stream Meandering as Observed from Satellite IR Imagery
    typeJournal Paper
    journal volume16
    journal issue2
    journal titleJournal of Physical Oceanography
    identifier doi10.1175/1520-0485(1986)016<0386:TEOTNE>2.0.CO;2
    journal fristpage386
    journal lastpage389
    treeJournal of Physical Oceanography:;1986:;Volume( 016 ):;issue: 002
    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