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    Seasonal Flow Reversals of Intermediate Waters in the Canary Current System East of the Canary Islands

    Source: Journal of Physical Oceanography:;2010:;Volume( 040 ):;issue: 008::page 1902
    Author:
    Machín, Francisco
    ,
    Pelegrí, Josep L.
    ,
    Fraile-Nuez, E.
    ,
    Vélez-Belchí, P.
    ,
    López-Laatzen, F.
    ,
    Hernández-Guerra, A.
    DOI: 10.1175/2010JPO4320.1
    Publisher: American Meteorological Society
    Abstract: Two 9-yr current-meter and salinity records, together with climatological data, reveal marked seasonal variability of the intermediate flow at a key location in the Canary Basin. The region is characterized by a summer (July?September) and early fall (October) northward progression of Antarctic Intermediate Water followed by a fall (November?December) intense flow reversal of Mediterranean Water. A Sverdrup-type model confirms that these movements are associated with stretching or shrinking of the intermediate water strata.
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      Seasonal Flow Reversals of Intermediate Waters in the Canary Current System East of the Canary Islands

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4212752
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    contributor authorMachín, Francisco
    contributor authorPelegrí, Josep L.
    contributor authorFraile-Nuez, E.
    contributor authorVélez-Belchí, P.
    contributor authorLópez-Laatzen, F.
    contributor authorHernández-Guerra, A.
    date accessioned2017-06-09T16:36:43Z
    date available2017-06-09T16:36:43Z
    date copyright2010/08/01
    date issued2010
    identifier issn0022-3670
    identifier otherams-70918.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4212752
    description abstractTwo 9-yr current-meter and salinity records, together with climatological data, reveal marked seasonal variability of the intermediate flow at a key location in the Canary Basin. The region is characterized by a summer (July?September) and early fall (October) northward progression of Antarctic Intermediate Water followed by a fall (November?December) intense flow reversal of Mediterranean Water. A Sverdrup-type model confirms that these movements are associated with stretching or shrinking of the intermediate water strata.
    publisherAmerican Meteorological Society
    titleSeasonal Flow Reversals of Intermediate Waters in the Canary Current System East of the Canary Islands
    typeJournal Paper
    journal volume40
    journal issue8
    journal titleJournal of Physical Oceanography
    identifier doi10.1175/2010JPO4320.1
    journal fristpage1902
    journal lastpage1909
    treeJournal of Physical Oceanography:;2010:;Volume( 040 ):;issue: 008
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
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