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    The Spatial Structure of RASS Echoes

    Source: Journal of Atmospheric and Oceanic Technology:;1996:;volume( 013 ):;issue: 006::page 1275
    Author:
    May, Peter T.
    ,
    Adachi, Tatsuhiro
    ,
    Tsuda, Toshitaka
    ,
    Lataitis, Richard J.
    DOI: 10.1175/1520-0426(1996)013<1275:TSSORE>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: An experiment to observe the spatial distribution of radio acoustic sounding system (RASS) echo intensity and Doppler shift using the MU radar is described. Various transmitting configurations are used to confirm that the RASS signal is focused onto a diffraction limited spot approximately the size of the transmitting antenna, except when a very small transmitting array is used where turbulence acting on the acoustic wave smears the spot. The signal fades away from the central spot with values about 6-10 dB lower in intensity next to the main spot. Significant gradients of Doppler shift across the radar antenna are seen in the lower height ranges. This may result in errors as large as a degree in the RASS virtual temperature estimates when large radar antennas and a single acoustic source are used.
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      The Spatial Structure of RASS Echoes

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4147468
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    contributor authorMay, Peter T.
    contributor authorAdachi, Tatsuhiro
    contributor authorTsuda, Toshitaka
    contributor authorLataitis, Richard J.
    date accessioned2017-06-09T14:05:14Z
    date available2017-06-09T14:05:14Z
    date copyright1996/12/01
    date issued1996
    identifier issn0739-0572
    identifier otherams-1216.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4147468
    description abstractAn experiment to observe the spatial distribution of radio acoustic sounding system (RASS) echo intensity and Doppler shift using the MU radar is described. Various transmitting configurations are used to confirm that the RASS signal is focused onto a diffraction limited spot approximately the size of the transmitting antenna, except when a very small transmitting array is used where turbulence acting on the acoustic wave smears the spot. The signal fades away from the central spot with values about 6-10 dB lower in intensity next to the main spot. Significant gradients of Doppler shift across the radar antenna are seen in the lower height ranges. This may result in errors as large as a degree in the RASS virtual temperature estimates when large radar antennas and a single acoustic source are used.
    publisherAmerican Meteorological Society
    titleThe Spatial Structure of RASS Echoes
    typeJournal Paper
    journal volume13
    journal issue6
    journal titleJournal of Atmospheric and Oceanic Technology
    identifier doi10.1175/1520-0426(1996)013<1275:TSSORE>2.0.CO;2
    journal fristpage1275
    journal lastpage1284
    treeJournal of Atmospheric and Oceanic Technology:;1996:;volume( 013 ):;issue: 006
    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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