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    A Comparison of VHF Radar Vertical-Velocity Measurements by a Direct Vertical-Beam Method and by a VAD Technique

    Source: Journal of Atmospheric and Oceanic Technology:;1991:;volume( 008 ):;issue: 006::page 766
    Author:
    Larsen, M. F.
    ,
    Fukao, S.
    ,
    Aruga, O.
    ,
    Yamanaka, M. D.
    ,
    Tsuda, T.
    ,
    Kato, S.
    DOI: 10.1175/1520-0426(1991)008<0766:ACOVRV>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Vertical-velocity measurements made by a direct vertical-beam method are compared to vertical velocities derived from VAD (velocity-azimuth display) measurements over a 27-h period. The results indicate that the two types of measurements in regions where the scatter is isotropic agree well. The largest discrepancies occur in the regions characterized by strong stratification and anisotropic or aspect-sensitive scatter. Although there are various assumptions inherent in the VAD calculations of the vertical velocities, indications are that the source of error is the aspect sensitivity, which produces effective off-vertical pointing angles in the vertical beam when the reflectivity layers are tilted out of the horizontal plane. However, other additional sources of bias or error cannot be excluded.
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      A Comparison of VHF Radar Vertical-Velocity Measurements by a Direct Vertical-Beam Method and by a VAD Technique

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4210955
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    • Journal of Atmospheric and Oceanic Technology

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    contributor authorLarsen, M. F.
    contributor authorFukao, S.
    contributor authorAruga, O.
    contributor authorYamanaka, M. D.
    contributor authorTsuda, T.
    contributor authorKato, S.
    date accessioned2017-06-09T16:31:11Z
    date available2017-06-09T16:31:11Z
    date copyright1991/12/01
    date issued1991
    identifier issn0739-0572
    identifier otherams-693.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4210955
    description abstractVertical-velocity measurements made by a direct vertical-beam method are compared to vertical velocities derived from VAD (velocity-azimuth display) measurements over a 27-h period. The results indicate that the two types of measurements in regions where the scatter is isotropic agree well. The largest discrepancies occur in the regions characterized by strong stratification and anisotropic or aspect-sensitive scatter. Although there are various assumptions inherent in the VAD calculations of the vertical velocities, indications are that the source of error is the aspect sensitivity, which produces effective off-vertical pointing angles in the vertical beam when the reflectivity layers are tilted out of the horizontal plane. However, other additional sources of bias or error cannot be excluded.
    publisherAmerican Meteorological Society
    titleA Comparison of VHF Radar Vertical-Velocity Measurements by a Direct Vertical-Beam Method and by a VAD Technique
    typeJournal Paper
    journal volume8
    journal issue6
    journal titleJournal of Atmospheric and Oceanic Technology
    identifier doi10.1175/1520-0426(1991)008<0766:ACOVRV>2.0.CO;2
    journal fristpage766
    journal lastpage776
    treeJournal of Atmospheric and Oceanic Technology:;1991:;volume( 008 ):;issue: 006
    contenttypeFulltext
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