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    The “Owl Horn” Radar Signature in Developing Southern Plains Supercells 

    Source: Monthly Weather Review:;2005:;volume( 133 ):;issue: 009:;page 2608
    Author(s): Kramar, Matthew R.; Bluestein, Howard B.; Pazmany, Andrew L.; Tuttle, John D.
    Publisher: American Meteorological Society
    Abstract: During spring 2001 in the Southern Plains, a recurring, hitherto undocumented reflectivity signature that the authors have called the ?Owl Horn? signature (because the radar reflectivity pattern resembles the profile of ...
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    An Example of the Use of Mobile, Doppler Radar Data for Tornado Verification 

    Source: Weather and Forecasting:;2009:;volume( 024 ):;issue: 003:;page 884
    Author(s): French, Michael M.; Bluestein, Howard B.; Wicker, Louis J.; Dowell, David C.; Kramar, Matthew R.
    Publisher: American Meteorological Society
    Abstract: On 16 May 2003, two ground-based, mobile, Doppler radars scanned a potentially tornadic supercell in the Texas Panhandle intermittently from ?0200 to 0330 UTC. The storm likely was tornadic, but because it was dark, visual ...
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    High-Resolution, Mobile Doppler Radar Observations of Cyclic Mesocyclogenesis in a Supercell 

    Source: Monthly Weather Review:;2008:;volume( 136 ):;issue: 012:;page 4997
    Author(s): French, Michael M.; Bluestein, Howard B.; Dowell, David C.; Wicker, Louis J.; Kramar, Matthew R.; Pazmany, Andrew L.
    Publisher: American Meteorological Society
    Abstract: On 15 May 2003, two ground-based, mobile, Doppler radars scanned a supercell that moved through the Texas Panhandle and cyclically produced mesocyclones. The two radars collected data from the storm during a rapid cyclic ...
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