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    EFFECT OF RANGE ON APPARENT HEIGHT AND FREQUENCY OF HIGH-ALTITUDE RADAR PRECIPITATION ECHOES 

    Source: Monthly Weather Review:;1969:;volume( 097 ):;issue: 006:;page 429
    Author(s): KANTOR, A. J.; GRANTHAM, D. D.
    Publisher: American Meteorological Society
    Abstract: Overestimation of the height of radar precipitation echoes increases with horizontal distance from the WSR-57 radar as a result of the combined effect of earth curvature, atmospheric refraction, and beam width. Radar ...
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    Effect of Range on Apparent Height and Frequency of High-Altitude Radar Precipitation Echoes 

    Source: Monthly Weather Review:;1970:;volume( 098 ):;issue: 010:;page 748
    Author(s): KANTOR, A. J.; GRANTHAM, D. D.
    Publisher: American Meteorological Society
    Abstract: No Abstract Available.
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    Validity of Reported Extreme Wind Speeds in the Arctic Stratosphere at SST Altitudes 

    Source: Bulletin of the American Meteorological Society:;1970:;volume( 051 ):;issue: 012:;page 1121
    Author(s): Grantham, D. D.; Kantor, A. J.
    Publisher: American Meteorological Society
    Abstract: Wind speeds of more than 100 m sec?1 (sometimes exceeding 150 m sec?1) were often recorded in the Canadian stratosphere prior to the winter of 1967?68, and occasionally recorded over Alaska, Greenland and Eurasian arctic ...
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    Mid-Latitude Humidity to 32 km 

    Source: Journal of the Atmospheric Sciences:;1968:;Volume( 025 ):;issue: 006:;page 1129
    Author(s): Sissenwine, N.; Grantham, D. D.; Salmela, H. A.
    Publisher: American Meteorological Society
    Abstract: The results of 17 northern California soundings of humidity up to 25?30 km, generally a month apart, utilizing a highly sophisticated alpha-radiation hygrometer and associated balloon sounding equipment are described. The ...
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