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    An Autumn Instability Event in the Gasp&aacute: Current

    Source: Journal of Physical Oceanography:;1989:;Volume( 019 ):;issue: 001::page 148
    Author:
    Mertz, Gordon
    ,
    El-sabh, Mohammed I.
    DOI: 10.1175/1520-0485(1989)019<0148:AAIEIT>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The Gaspé Current is a buoyant jet driven primarily by the freshwater discharge from the St. Lawrence estuary. Previously, many incidents of unstable wave development in the3 Gaspé Current have been reported under summer, high runoff, conditions. Here we present satellite infrared images and discuss the occurrence and evolution of an autumn episode of current instability; in the fall, runoff is lower. This event is notable in that the pattern observed differs considerably from that of summer events, apparently due to the offshore shift that of the core of the jet in early autumn. A stability analysis suggests that the Gaspé Current instabilities may grow slightly faster in autumn conditions. The possible role of wind forcing in triggering wave growth is discussed.
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      An Autumn Instability Event in the Gasp&aacute: Current

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    https://yetl.yabesh.ir/yetl1/handle/yetl/4164466
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    contributor authorMertz, Gordon
    contributor authorEl-sabh, Mohammed I.
    date accessioned2017-06-09T14:49:06Z
    date available2017-06-09T14:49:06Z
    date copyright1989/01/01
    date issued1989
    identifier issn0022-3670
    identifier otherams-27459.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4164466
    description abstractThe Gaspé Current is a buoyant jet driven primarily by the freshwater discharge from the St. Lawrence estuary. Previously, many incidents of unstable wave development in the3 Gaspé Current have been reported under summer, high runoff, conditions. Here we present satellite infrared images and discuss the occurrence and evolution of an autumn episode of current instability; in the fall, runoff is lower. This event is notable in that the pattern observed differs considerably from that of summer events, apparently due to the offshore shift that of the core of the jet in early autumn. A stability analysis suggests that the Gaspé Current instabilities may grow slightly faster in autumn conditions. The possible role of wind forcing in triggering wave growth is discussed.
    publisherAmerican Meteorological Society
    titleAn Autumn Instability Event in the Gaspá: Current
    typeJournal Paper
    journal volume19
    journal issue1
    journal titleJournal of Physical Oceanography
    identifier doi10.1175/1520-0485(1989)019<0148:AAIEIT>2.0.CO;2
    journal fristpage148
    journal lastpage156
    treeJournal of Physical Oceanography:;1989:;Volume( 019 ):;issue: 001
    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
    yabeshDSpacePersian