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    Radar Measurement of Tidal Winds at Stratospheric Heights over Arecibo

    Source: Journal of the Atmospheric Sciences:;1980:;Volume( 037 ):;issue: 011::page 2540
    Author:
    Fukao, Shoichiro
    ,
    Sato, Toru
    ,
    Yamasaki, Norikazu
    ,
    Harper, Robert M.
    ,
    Kato, Susumu
    DOI: 10.1175/1520-0469(1980)037<2540:RMOTWA>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Wind oscillations of tidal periods that showed a marked downward phase progression were detected at the lower stratosphere using the Arecibo radar. The amplitudes of 1?5 m s?1 were inferred for both diurnal and semidiurnal components, much larger than the values predicted by the classical tidal theory. The vertical wavelengths inferred were also less than the theoretical values; ?5 km for the diurnal component and 2?9 km for the semidiurnal component.
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      Radar Measurement of Tidal Winds at Stratospheric Heights over Arecibo

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4153994
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    • Journal of the Atmospheric Sciences

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    contributor authorFukao, Shoichiro
    contributor authorSato, Toru
    contributor authorYamasaki, Norikazu
    contributor authorHarper, Robert M.
    contributor authorKato, Susumu
    date accessioned2017-06-09T14:21:55Z
    date available2017-06-09T14:21:55Z
    date copyright1980/11/01
    date issued1980
    identifier issn0022-4928
    identifier otherams-18033.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4153994
    description abstractWind oscillations of tidal periods that showed a marked downward phase progression were detected at the lower stratosphere using the Arecibo radar. The amplitudes of 1?5 m s?1 were inferred for both diurnal and semidiurnal components, much larger than the values predicted by the classical tidal theory. The vertical wavelengths inferred were also less than the theoretical values; ?5 km for the diurnal component and 2?9 km for the semidiurnal component.
    publisherAmerican Meteorological Society
    titleRadar Measurement of Tidal Winds at Stratospheric Heights over Arecibo
    typeJournal Paper
    journal volume37
    journal issue11
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1980)037<2540:RMOTWA>2.0.CO;2
    journal fristpage2540
    journal lastpage2544
    treeJournal of the Atmospheric Sciences:;1980:;Volume( 037 ):;issue: 011
    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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