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    Latitudinal Distribution of Mixing Rate Caused by the M2 Internal Tide

    Source: Journal of Physical Oceanography:;2006:;Volume( 036 ):;issue: 001::page 35
    Author:
    Tian, Jiwei
    ,
    Zhou, Lei
    ,
    Zhang, Xiaoqian
    DOI: 10.1175/JPO2824.1
    Publisher: American Meteorological Society
    Abstract: Ten years of Ocean Topography Experiment (TOPEX)/Poseidon tidal data and an energy balance relation are used to estimate the mixing rate caused by M2 internal tides in the upper ocean. The results indicate that latitudinal distribution of the mixing rate has a generally symmetrical structure with respect to the equator. The maxima are distributed around 28.9°N and 28.9°S and can be as high as 3.8 ? 10?5 m2 s?1 in the Pacific, 5 ? 10?5 m2 s?1 in the Atlantic, and 3.7 ? 10?5 m2 s?1 in the Indian Oceans. The minimum, which is only 10% of those at 28.9°, is located near the equator. The data imply that midlatitudes are the key regions for internal tide mixing.
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      Latitudinal Distribution of Mixing Rate Caused by the M2 Internal Tide

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4225846
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    contributor authorTian, Jiwei
    contributor authorZhou, Lei
    contributor authorZhang, Xiaoqian
    date accessioned2017-06-09T17:18:00Z
    date available2017-06-09T17:18:00Z
    date copyright2006/01/01
    date issued2006
    identifier issn0022-3670
    identifier otherams-82702.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4225846
    description abstractTen years of Ocean Topography Experiment (TOPEX)/Poseidon tidal data and an energy balance relation are used to estimate the mixing rate caused by M2 internal tides in the upper ocean. The results indicate that latitudinal distribution of the mixing rate has a generally symmetrical structure with respect to the equator. The maxima are distributed around 28.9°N and 28.9°S and can be as high as 3.8 ? 10?5 m2 s?1 in the Pacific, 5 ? 10?5 m2 s?1 in the Atlantic, and 3.7 ? 10?5 m2 s?1 in the Indian Oceans. The minimum, which is only 10% of those at 28.9°, is located near the equator. The data imply that midlatitudes are the key regions for internal tide mixing.
    publisherAmerican Meteorological Society
    titleLatitudinal Distribution of Mixing Rate Caused by the M2 Internal Tide
    typeJournal Paper
    journal volume36
    journal issue1
    journal titleJournal of Physical Oceanography
    identifier doi10.1175/JPO2824.1
    journal fristpage35
    journal lastpage42
    treeJournal of Physical Oceanography:;2006:;Volume( 036 ):;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
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