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    Equatorial Atlantic Velocity and Temperature Observations: February–November 1981

    Source: Journal of Physical Oceanography:;1985:;Volume( 015 ):;issue: 005::page 533
    Author:
    Weisberg, R. H.
    DOI: 10.1175/1520-0485(1985)015<0533:EAVATO>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Upper ocean velocity and temperature measurements were obtained in the central equatorial Atlantic using surface moored current meters from February to November 1981. Distinct seasonal variations were observed in the zonal momentum and temperature on the equator of both the surface South Equatorial Current (SEC) and the subsurface Equatorial Undercurrent (EUC). After initially intensifying during boreal spring the SEC halted abruptly in early summer and the signature associated with this change progressed. At the observational depth of 100 m both speed and temperature increased during early summer with eastward progression and then decreased in fall. Higher frequency motions were also modulated by the seasonal cycle. Notable were the 2?3 week time scale oscillations of the meridional velocity component which appeared most energetically during the summer and fall seasons. Oscillations generally tended to be anisotropic and inhomogeneous. Vertical advection of zonal momentum was an important term in the momentum balance of the zonal velocity component fluctuations.
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      Equatorial Atlantic Velocity and Temperature Observations: February–November 1981

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4163771
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    contributor authorWeisberg, R. H.
    date accessioned2017-06-09T14:47:26Z
    date available2017-06-09T14:47:26Z
    date copyright1985/05/01
    date issued1985
    identifier issn0022-3670
    identifier otherams-26833.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4163771
    description abstractUpper ocean velocity and temperature measurements were obtained in the central equatorial Atlantic using surface moored current meters from February to November 1981. Distinct seasonal variations were observed in the zonal momentum and temperature on the equator of both the surface South Equatorial Current (SEC) and the subsurface Equatorial Undercurrent (EUC). After initially intensifying during boreal spring the SEC halted abruptly in early summer and the signature associated with this change progressed. At the observational depth of 100 m both speed and temperature increased during early summer with eastward progression and then decreased in fall. Higher frequency motions were also modulated by the seasonal cycle. Notable were the 2?3 week time scale oscillations of the meridional velocity component which appeared most energetically during the summer and fall seasons. Oscillations generally tended to be anisotropic and inhomogeneous. Vertical advection of zonal momentum was an important term in the momentum balance of the zonal velocity component fluctuations.
    publisherAmerican Meteorological Society
    titleEquatorial Atlantic Velocity and Temperature Observations: February–November 1981
    typeJournal Paper
    journal volume15
    journal issue5
    journal titleJournal of Physical Oceanography
    identifier doi10.1175/1520-0485(1985)015<0533:EAVATO>2.0.CO;2
    journal fristpage533
    journal lastpage543
    treeJournal of Physical Oceanography:;1985:;Volume( 015 ):;issue: 005
    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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