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    Nonmigrating Diurnal Tides in Mesospheric and Lower-Thermospheric Winds and Temperatures

    Source: Journal of the Atmospheric Sciences:;1999:;Volume( 056 ):;issue: 024::page 4073
    Author:
    Talaat, Elsayed R.
    ,
    Lieberman, Ruth S.
    DOI: 10.1175/1520-0469(1999)056<4073:NDTIMA>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: This paper presents analyses of nonmigrating diurnal tide signatures in High Resolution Doppler Imager mesospheric and lower-thermospheric winds and temperatures. A global comparison of both winds and temperature reveals equatorial features corresponding to nonmigrating tides. Structures interpreted as zonal mean and eastward nonmigrating diurnal tides display consistency between horizontal winds and temperatures. The second symmetric mode is prominent in the zonal mean and wavenumber 1. The gravest antisymmetric mode and the gravest symmetric or Kelvin mode are the main features in zonal wavenumbers 2 and 3. The amplitudes of the tides generally increase with altitude and maximize within 90?110 km.
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      Nonmigrating Diurnal Tides in Mesospheric and Lower-Thermospheric Winds and Temperatures

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4158958
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    contributor authorTalaat, Elsayed R.
    contributor authorLieberman, Ruth S.
    date accessioned2017-06-09T14:35:53Z
    date available2017-06-09T14:35:53Z
    date copyright1999/12/01
    date issued1999
    identifier issn0022-4928
    identifier otherams-22500.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4158958
    description abstractThis paper presents analyses of nonmigrating diurnal tide signatures in High Resolution Doppler Imager mesospheric and lower-thermospheric winds and temperatures. A global comparison of both winds and temperature reveals equatorial features corresponding to nonmigrating tides. Structures interpreted as zonal mean and eastward nonmigrating diurnal tides display consistency between horizontal winds and temperatures. The second symmetric mode is prominent in the zonal mean and wavenumber 1. The gravest antisymmetric mode and the gravest symmetric or Kelvin mode are the main features in zonal wavenumbers 2 and 3. The amplitudes of the tides generally increase with altitude and maximize within 90?110 km.
    publisherAmerican Meteorological Society
    titleNonmigrating Diurnal Tides in Mesospheric and Lower-Thermospheric Winds and Temperatures
    typeJournal Paper
    journal volume56
    journal issue24
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1999)056<4073:NDTIMA>2.0.CO;2
    journal fristpage4073
    journal lastpage4087
    treeJournal of the Atmospheric Sciences:;1999:;Volume( 056 ):;issue: 024
    contenttypeFulltext
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    yabeshDSpacePersian
     
    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
    yabeshDSpacePersian