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    A High-Frequency Radio Acoustic Sounder for Remote Measurement of Atmospheric Winds and Temperature

    Source: Bulletin of the American Meteorological Society:;1977:;volume( 058 ):;issue: 009::page 928
    Author:
    Frankel, Michael S.
    ,
    Chang, Norman J. F.
    ,
    Sanders, Melvin J.
    DOI: 10.1175/1520-0477(1977)058<0928:AHFRAS>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The Radio Acoustic Sounding System (RASS) is used to remotely measure atmospheric temperature profiles. The technique used for these measurements is Doppler tracking of a short, high-intensity acoustic pulse with an RF (electro-magnetic) radar. By measurement of the acoustic pulse propagation speed, temperature can be calculated as a function of altitude. The Stanford University RASS operates at an acoustic frequency of 85Hz. Because of this low frequency and the necessity of high system gain, the unit is too large for mobile applications. Our theoretical analyses show, however, that the RASS could operate at much higher acoustic frequencies and still provide data to altitudes of ?1 km even during periods of moderate to strong atmospheric turbulence. These theoretical analyses have now been supported experimentally. A RASS operating with an acoustic frequency of 1 kHz not only provided Doppler data to altitudes of 1 km, but it also was able to provide a measure of horizontal winds over the same range. These experimental results came from a brief effort to support our theoretical studies. Future experiments could well extend the profiling range and versatility of the high-frequency RASS. Ultimately, we hope that our work will lead to a transportable system to be used for collecting real-time data on atmospheric winds and temperatures.
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      A High-Frequency Radio Acoustic Sounder for Remote Measurement of Atmospheric Winds and Temperature

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4160449
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    contributor authorFrankel, Michael S.
    contributor authorChang, Norman J. F.
    contributor authorSanders, Melvin J.
    date accessioned2017-06-09T14:39:37Z
    date available2017-06-09T14:39:37Z
    date copyright1977/09/01
    date issued1977
    identifier issn0003-0007
    identifier otherams-23843.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4160449
    description abstractThe Radio Acoustic Sounding System (RASS) is used to remotely measure atmospheric temperature profiles. The technique used for these measurements is Doppler tracking of a short, high-intensity acoustic pulse with an RF (electro-magnetic) radar. By measurement of the acoustic pulse propagation speed, temperature can be calculated as a function of altitude. The Stanford University RASS operates at an acoustic frequency of 85Hz. Because of this low frequency and the necessity of high system gain, the unit is too large for mobile applications. Our theoretical analyses show, however, that the RASS could operate at much higher acoustic frequencies and still provide data to altitudes of ?1 km even during periods of moderate to strong atmospheric turbulence. These theoretical analyses have now been supported experimentally. A RASS operating with an acoustic frequency of 1 kHz not only provided Doppler data to altitudes of 1 km, but it also was able to provide a measure of horizontal winds over the same range. These experimental results came from a brief effort to support our theoretical studies. Future experiments could well extend the profiling range and versatility of the high-frequency RASS. Ultimately, we hope that our work will lead to a transportable system to be used for collecting real-time data on atmospheric winds and temperatures.
    publisherAmerican Meteorological Society
    titleA High-Frequency Radio Acoustic Sounder for Remote Measurement of Atmospheric Winds and Temperature
    typeJournal Paper
    journal volume58
    journal issue9
    journal titleBulletin of the American Meteorological Society
    identifier doi10.1175/1520-0477(1977)058<0928:AHFRAS>2.0.CO;2
    journal fristpage928
    journal lastpage934
    treeBulletin of the American Meteorological Society:;1977:;volume( 058 ):;issue: 009
    contenttypeFulltext
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