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    Equatorial Current Observations in the Western Indian Ocean in 1975 and 1976

    Source: Journal of Physical Oceanography:;1980:;Volume( 010 ):;issue: 002::page 258
    Author:
    Leetmaa, Ants
    ,
    Stommel, Henry
    DOI: 10.1175/1520-0485(1980)010<0258:ECOITW>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Vertical profiles of current, temperature and salinity were taken in the upper ocean from 3°S to 2°N along 55°30?E in the Indian Ocean during February?June in 1975 and 1976. During both years a strong O(80 cm s?1) equatorial undercurrent was present throughout the measurement period in the vicinity of the equator. A second region of eastward flow above the thermocline was observed at 3°S. During May and June the undercurrent moved southward and merged with the southern region of eastward flow. The meridional flow field was dominated by transients that during strong events were antisymmetric about the equator and had a vertical wavelength of ?180 m. The transient events strongly affected the zonal flow field; during strong events the undercurrent was almost eliminated. This is in contrast to the GATE observations where the undercurrent was advected back and forth across the equator.
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      Equatorial Current Observations in the Western Indian Ocean in 1975 and 1976

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4162870
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    contributor authorLeetmaa, Ants
    contributor authorStommel, Henry
    date accessioned2017-06-09T14:45:19Z
    date available2017-06-09T14:45:19Z
    date copyright1980/02/01
    date issued1980
    identifier issn0022-3670
    identifier otherams-26021.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4162870
    description abstractVertical profiles of current, temperature and salinity were taken in the upper ocean from 3°S to 2°N along 55°30?E in the Indian Ocean during February?June in 1975 and 1976. During both years a strong O(80 cm s?1) equatorial undercurrent was present throughout the measurement period in the vicinity of the equator. A second region of eastward flow above the thermocline was observed at 3°S. During May and June the undercurrent moved southward and merged with the southern region of eastward flow. The meridional flow field was dominated by transients that during strong events were antisymmetric about the equator and had a vertical wavelength of ?180 m. The transient events strongly affected the zonal flow field; during strong events the undercurrent was almost eliminated. This is in contrast to the GATE observations where the undercurrent was advected back and forth across the equator.
    publisherAmerican Meteorological Society
    titleEquatorial Current Observations in the Western Indian Ocean in 1975 and 1976
    typeJournal Paper
    journal volume10
    journal issue2
    journal titleJournal of Physical Oceanography
    identifier doi10.1175/1520-0485(1980)010<0258:ECOITW>2.0.CO;2
    journal fristpage258
    journal lastpage269
    treeJournal of Physical Oceanography:;1980:;Volume( 010 ):;issue: 002
    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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