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contributor authorHays, Paul B.
contributor authorWu, D. L.
contributor authorHRDI Science Team, The
date accessioned2017-06-09T14:32:34Z
date available2017-06-09T14:32:34Z
date copyright1994/10/01
date issued1994
identifier issn0022-4928
identifier otherams-21296.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4157619
description abstractThis study presents a climatology of mesospheric and lower-thermospheric diurnal tidal winds obtained with the High Resolution Doppler Imager (HRDI) on the Upper Atmosphere Research Satellite (UARS). The observations reveal that although tidal structures are present at all times, like the prevailing zonal winds, they exhibit significant semiannual as well as other shorter-term variations in amplitude. Results are presented for a period extending over more than one year from November 1991 to July 1993. The 1,1 diurnal tidal amplitude of the meridional component, characterized by the value at an altitude of 90 km and a latitude of 22°, ranges from a minimum at solstice of less than 20 m s?1 to an equinox maximum of over 70 m s?1. The vertical wavelength and phase of the tide show only slight variations throughout the year, with a suggestion of semiannual variations in both.
publisherAmerican Meteorological Society
titleObservations of the Diurnal Tide from Space
typeJournal Paper
journal volume51
journal issue20
journal titleJournal of the Atmospheric Sciences
identifier doi10.1175/1520-0469(1994)051<3077:OOTDTF>2.0.CO;2
journal fristpage3077
journal lastpage3093
treeJournal of the Atmospheric Sciences:;1994:;Volume( 051 ):;issue: 020
contenttypeFulltext


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