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    The Effect of Atmospheric Lapse Rates on Balloon Ascent Rates 

    Source: Journal of Applied Meteorology:;1966:;volume( 005 ):;issue: 004:;page 537
    Author(s): Reynolds, Ralph D.
    Publisher: American Meteorological Society
    Abstract: tract
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    Superpressure Balloons as Isentropic/Isopycnic Tracers 

    Source: Journal of Applied Meteorology:;1973:;volume( 012 ):;issue: 002:;page 369
    Author(s): Reynolds, Ralph D.
    Publisher: American Meteorological Society
    Abstract: Synchronous radar, temperature and pressure data of suitable quality, gathered from three balloon flights of the Mountain Wave Project, were analyzed in detail to show the relationships between balloon-depicted waves and ...
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    Ambient Temperature Measurements from Radiosondes Flown on Constant-Level Balloons 

    Source: Journal of Applied Meteorology:;1966:;volume( 005 ):;issue: 003:;page 304
    Author(s): Reynolds, Ralph D.; Lamberth, Roy L.
    Publisher: American Meteorological Society
    Abstract: A cause of erroneous temperatures obtained in the earlier phases of a study using standard radiosondes flown on constant-level balloons at White Sands Missile Range is discussed. A simple and inexpensive modification of ...
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    A High-Resolution Continuous Pressure Sensor Modification for Radiosondes 

    Source: Journal of Applied Meteorology:;1968:;volume( 007 ):;issue: 001:;page 141
    Author(s): Glass, Roy I.; Reynolds, Ralph D.; Lamberth, Roy L.
    Publisher: American Meteorological Society
    Abstract: This paper describes how continuous pressure measurements may be obtained by making a relatively simple modification to any standard or clock-switched radiosonde which can be flown on a rising or floating balloon. The ...
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    Investigation of a Complex Mountain Wave Situation 

    Source: Journal of Applied Meteorology:;1968:;volume( 007 ):;issue: 003:;page 353
    Author(s): Reynolds, Ralph D.; Lamberth, Roy L.; Wurtele, M. G.
    Publisher: American Meteorological Society
    Abstract: A complex mountain lee wave was recorded by radar-tracked superpressure balloons at White Sands Missile Range on 6 May 1965 at a mean altitude of 3.5 km MSL; simultaneously, a very weak wave was recorded at 7 km. The lower ...
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