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    Initiation and Evolution of Updraft Rotation within an Incipient Supercell Thunderstorm 

    Source: Journal of the Atmospheric Sciences:;1992:;Volume( 049 ):;issue: 021:;page 1997
    Author(s): Brown, Rodger A.
    Publisher: American Meteorological Society
    Abstract: One of the distinguishing characteristics of a supercell thunderstorm is the presence of a rotating updraft. During the past 30 years, various hypotheses have been proposed to explain the initiation and maintenance of ...
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    WEATHER NOTE: OCCURRENCE OF SUPERNUMERARY FOGBOWS AT SUBFREEZING TEMPERATURES 

    Source: Monthly Weather Review:;1966:;volume( 094 ):;issue: 001:;page 47
    Author(s): BROWN, RODGER A.
    Publisher: American Meteorological Society
    Abstract: No Abstract Available.
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    Comments on “A Note on the ‘Square Cloud’” 

    Source: Journal of the Atmospheric Sciences:;1967:;Volume( 024 ):;issue: 003:;page 305
    Author(s): Brown, Rodger A.
    Publisher: American Meteorological Society
    Abstract: No abstract available.
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    Mass and Available Energy in Growing Convective Clouds 

    Source: Journal of the Atmospheric Sciences:;1967:;Volume( 024 ):;issue: 003:;page 308
    Author(s): Brown, Rodger A.
    Publisher: American Meteorological Society
    Abstract: Not available
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    A Compositing Approach for Preserving Significant Features in Atmospheric Profiles 

    Source: Monthly Weather Review:;1993:;volume( 121 ):;issue: 003:;page 874
    Author(s): Brown, Rodger A.
    Publisher: American Meteorological Society
    Abstract: Composite profiles of thermodynamic and kinematic variables are prepared to represent the characteristics of the environment within which a particular atmospheric phenomenon occurs. During the averaging process, it is ...
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    Nomogram for Aiding the Interpretation of Tornadic Vortex Signatures Measured by Doppler Radar 

    Source: Weather and Forecasting:;1998:;volume( 013 ):;issue: 002:;page 505
    Author(s): Brown, Rodger A.
    Publisher: American Meteorological Society
    Abstract: A technique is described whereby an investigator can obtain a more representative peak velocity for a tornadic vortex signature (TVS) than can be obtained by using the extreme measured Doppler velocities associated with ...
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    Simulated Tornadic Vortex Signatures of Tornado-Like Vortices Having One- and Two-Celled Structures 

    Source: Journal of Applied Meteorology and Climatology:;2011:;volume( 050 ):;issue: 011:;page 2338
    Author(s): Wood, Vincent T.; Brown, Rodger A.
    Publisher: American Meteorological Society
    Abstract: tornadic vortex signature (TVS) is a degraded Doppler velocity signature that occurs when the tangential velocity core region of a tornado is smaller than the effective beamwidth of a sampling Doppler radar. Early Doppler ...
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    Single Doppler Velocity Signature Interpretation of Nondivergent Environmental Winds 

    Source: Journal of Atmospheric and Oceanic Technology:;1986:;volume( 003 ):;issue: 001:;page 114
    Author(s): Wood, Vincent T.; Brown, Rodger A.
    Publisher: American Meteorological Society
    Abstract: A variety of single Doppler velocity patterns that simulate those observed in a nondivergent environment is presented. Measurements in optically clear air and/or widespread precipitation are simulated, using horizontally ...
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    Effects of Radar Proximity on Single-Doppler Velocity Signatures of Axisymmetric Rotation and Divergence 

    Source: Monthly Weather Review:;1992:;volume( 120 ):;issue: 012:;page 2798
    Author(s): Wood, Vincent T.; Brown, Rodger A.
    Publisher: American Meteorological Society
    Abstract: Geometrical and mathematical relationships are developed to explain the variation with radar range of idealized single-Doppler velocity patterns of axisymmetric rotation and divergence regions. The velocity patterns become ...
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    The Tornadic Vortex Signature: An Update 

    Source: Weather and Forecasting:;2012:;volume( 027 ):;issue: 002:;page 525
    Author(s): Brown, Rodger A.; Wood, Vincent T.
    Publisher: American Meteorological Society
    Abstract: tornadic vortex signature (TVS) is a degraded Doppler velocity signature of a tornado that occurs when the core region of a tornado is smaller than the half-power beamwidth of the sampling Doppler radar. Soon after the TVS ...
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