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    Ray Tracing of Gravity Waves as a Possible Warning System for Tornadic Storms and Hurricanes 

    Source: Journal of Applied Meteorology:;1978:;volume( 017 ):;issue: 001:;page 3
    Author(s): Hung, R. J.; Smith, R. E.
    Publisher: American Meteorological Society
    Abstract: Gravity waves with wave periods of 13 to 15 min and horizontal phase velocities of 90 to 220 m s?1 were present in ground-based observations of the upper atmosphere during time periods when tornadoes were occurring and ...
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    Observation of Severe Weather Activities by Doppler Sounder Array 

    Source: Journal of Applied Meteorology:;1975:;volume( 014 ):;issue: 008:;page 1611
    Author(s): Smith, R. E.; Hung, R. J.
    Publisher: American Meteorological Society
    Abstract: A three-dimensional, nine-element, high-frequency cw Doppler sounder array has been used to detect ionospheric disturbances during periods of severe weather, particularly during periods with severe thunderstorms and ...
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    Case Studies of Gravity Waves Associated with Isolated Tornadic Storms on 13 January 1976 

    Source: Journal of Applied Meteorology:;1979:;volume( 018 ):;issue: 004:;page 460
    Author(s): Hung, R. J.; Phan, T.; Smith, R. E.
    Publisher: American Meteorological Society
    Abstract: Penetrative convection, thunderstorms, squall lines, etc., all generate atmospheric gravity waves which can be observed by a ground-based ionospheric Doppler sounder array. Sources of these waves can be determined from ...
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    Gravity Waves and GOES IR Data Study of an Isolated Tornadic Storm on 29 May 1977 

    Source: Monthly Weather Review:;1980:;volume( 108 ):;issue: 004:;page 456
    Author(s): Hung, R. J.; Phan, T.; Lin, D. C.; Smith, R. E.; Jayroe, R. R.; West, S.
    Publisher: American Meteorological Society
    Abstract: Enhanced convection-initiated gravity waves associated with an isolated tornado in the absence of a squall line are investigated. Ray-tracing computations based on data observed on 29 May 1977 indicated that the wave sources ...
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