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    The Madeira Mode Water

    Source: Journal of Physical Oceanography:;1987:;Volume( 017 ):;issue: 010::page 1561
    Author:
    Siedler, Gerold
    ,
    Kuhl, Anni
    ,
    Zenk, Walter
    DOI: 10.1175/1520-0485(1987)017<1561:TMMW>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Quasi-homogeneous layers in vertical profiles of temperature and salinity in the eastern North Atlantic near Madeira indicate the existence of a subtropical Mode Water in the Eastern Basin. Temperature sections show a maximum horizontal extent of at least 500 km. The frequency distribution analysis of homogeneous layers in a historical XBT dataset shows a Mode Water formation region near and to the north of Madeira. This Mode Water is found at increasing depths and displaced to the west and southwest during the course of the year after its formation by wintertime convection. It disappears almost completely, due to mixing, before the next winter. Volume estimates suggest that this Madeira Mode Water in the eastern Atlantic accounts for 15?20% of the total Central Water formation in the corresponding density range as obtained from tracer studies in the North Atlantic gyre.
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      The Madeira Mode Water

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4164227
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    contributor authorSiedler, Gerold
    contributor authorKuhl, Anni
    contributor authorZenk, Walter
    date accessioned2017-06-09T14:48:33Z
    date available2017-06-09T14:48:33Z
    date copyright1987/10/01
    date issued1987
    identifier issn0022-3670
    identifier otherams-27243.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4164227
    description abstractQuasi-homogeneous layers in vertical profiles of temperature and salinity in the eastern North Atlantic near Madeira indicate the existence of a subtropical Mode Water in the Eastern Basin. Temperature sections show a maximum horizontal extent of at least 500 km. The frequency distribution analysis of homogeneous layers in a historical XBT dataset shows a Mode Water formation region near and to the north of Madeira. This Mode Water is found at increasing depths and displaced to the west and southwest during the course of the year after its formation by wintertime convection. It disappears almost completely, due to mixing, before the next winter. Volume estimates suggest that this Madeira Mode Water in the eastern Atlantic accounts for 15?20% of the total Central Water formation in the corresponding density range as obtained from tracer studies in the North Atlantic gyre.
    publisherAmerican Meteorological Society
    titleThe Madeira Mode Water
    typeJournal Paper
    journal volume17
    journal issue10
    journal titleJournal of Physical Oceanography
    identifier doi10.1175/1520-0485(1987)017<1561:TMMW>2.0.CO;2
    journal fristpage1561
    journal lastpage1570
    treeJournal of Physical Oceanography:;1987:;Volume( 017 ):;issue: 010
    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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