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    ICE-CRYSTAL GROWTH 

    Source: Journal of Meteorology:;1952:;volume( 009 ):;issue: 001:;page 36
    Author(s): Reynolds, S. E.
    Publisher: American Meteorological Society
    Abstract: Laboratory measurements of the rate of ice-crystal growth by sublimation are found to be in good agreement with Houghton's (1950) calculations. With use of Houghton's data for the growth of ice crystals at relatively warm ...
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    CORRELATION OF THE INITIAL ELECTRIC FIELD AND THE RADAR ECHO IN THUNDERSTORMS 

    Source: Journal of Meteorology:;1956:;volume( 013 ):;issue: 004:;page 376
    Author(s): Reynolds, S. E.; Brook, M.
    Publisher: American Meteorological Society
    Abstract: The time of onset of the initial electrification in a thunderstorm cell has been correlated with the appearance of the initial radar (3 cm) precipitation-echo. The results show that precipitation is a necessary, but not ...
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    THE DISTRIBUTION AND DISCHARGE OF THUNDERSTORM CHARGE-CENTERS 

    Source: Journal of Meteorology:;1955:;volume( 012 ):;issue: 001:;page 1
    Author(s): Reynolds, S. E.; Neill, H. W.
    Publisher: American Meteorological Society
    Abstract: The magnitude and location of the charge centers involved in lightning discharges can be determined from the value of the accompanying gradient change at seven points at the ground. Instrumentation, calibration, observation, ...
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    POSSIBILITIES FOR CLOUD SEEDING AS DETERMINED BY A STUDY OF CLOUD HEIGHT VERSUS PRECIPITATION 

    Source: Journal of Meteorology:;1951:;volume( 008 ):;issue: 006:;page 416
    Author(s): Braham, R. R.; Reynolds, S. E.; Jarrell, J. H.
    Publisher: American Meteorological Society
    Abstract: No Abstract Available
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    THUNDERSTORM CHARGE SEPARATION 

    Source: Journal of Meteorology:;1957:;volume( 014 ):;issue: 005:;page 426
    Author(s): Reynolds, S. E.; Brook, M.; Gourley, Mary Foulks
    Publisher: American Meteorological Society
    Abstract: A description of the known physical properties of a thunderstorm reveals that active charge separation occurs during that stage of the storm's life-cycle in which the growth of graupel by the accretion of supercooled ...
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