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    Structure and Evolution of a Severe Squall Line over Oklahoma 

    Source: Monthly Weather Review:;1985:;volume( 113 ):;issue: 009:;page 1563
    Author(s): Heymsfield, Gerald M.; Schotz, Steven
    Publisher: American Meteorological Society
    Abstract: A squall line on 2 May 1979 developed in Oklahoma in proximity to a synoptic-scale cold front. This line is analyzed during its growth and mature periods using radar, satellite, sounding and surface data. Some of the cells ...
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    Upper-Level Structure of Oklahoma Tornadic Storms on 2 May 1979. II: Proposed Explanation of “V” Pattern and Internal Warm Region in Infrared Observations 

    Source: Journal of the Atmospheric Sciences:;1983:;Volume( 040 ):;issue: 007:;page 1756
    Author(s): Heymsfield, Gerald M.; Szejwach, Gerard; Schotz, Steven; Blackmer, Roy H.
    Publisher: American Meteorological Society
    Abstract: An analysis of the GOES measurements of a severe thunderstorm anvil on 2 May 1979 presented in Part I (Heymsfield et al.) showed a ?V? shaped region of low infrared temperatures (TBB) and an internal region of high TBB. ...
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    Upper-Level Structure of Oklahoma Tornadic Storms on 2 May 1979. I: Radar and Satellite Observations 

    Source: Journal of the Atmospheric Sciences:;1983:;Volume( 040 ):;issue: 007:;page 1740
    Author(s): Heymsfield, Gerald M.; Blackmer, Roy H.; Schotz, Steven
    Publisher: American Meteorological Society
    Abstract: This paper discusses the observational characteristics of the upper level structure of severe tornadic storms in Oklahoma on 2 May 1979 during SESAME. The data analyzed consist of limited-scan GOES-East and West visible, ...
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