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    Airborne Cloud-Physics Projects From 1974 Through 1984 

    Source: Bulletin of the American Meteorological Society:;1986:;volume( 067 ):;issue: 012:;page 1473
    Author(s): Jeck, Richard K.
    Publisher: American Meteorological Society
    Abstract: Most of the principal airborne cloud-physics projects during the ten-year period 1974-1984 are documented to provide selected information on the type and quantity of microphysical data that have beencollected. The emphasis ...
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    Spatial and Microphysical Characteristics of Low-Ceiling, Temperature-Inverted Clouds in Warm Overrunning and Freezing-Rain Conditions: A Case Study 

    Source: Journal of Applied Meteorology and Climatology:;2011:;volume( 050 ):;issue: 010:;page 2062
    Author(s): Jeck, Richard K.
    Publisher: American Meteorological Society
    Abstract: n-flight microphysical measurements in classical freezing-rain conditions were used to study the vertical and horizontal characteristics of the precipitation and associated low-ceiling, stratiform clouds, which are usually ...
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    Distance-Scaled Water Concentrations versus Mass-Median Drop Size, Temperature, and Altitude in Supercooled Clouds 

    Source: Journal of the Atmospheric Sciences:;2008:;Volume( 065 ):;issue: 007:;page 2087
    Author(s): Jeck, Richard K.
    Publisher: American Meteorological Society
    Abstract: About 28 000 nautical miles (n mi) of select in-flight measurements of liquid water content (LWC), droplet sizes, temperature, and other variables in supercooled clouds from a variety of research projects over portions of ...
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    Aircraft Icing Environment in Low Ceiling Conditions near Washington, D.C. 

    Source: Weather and Forecasting:;1987:;volume( 002 ):;issue: 002:;page 114
    Author(s): Guttman, Nathaniel B.; Jeck, Richard K.
    Publisher: American Meteorological Society
    Abstract: Radiosonde temperature and humidity data were used to deduce the vertical distribution of clouds and aircraft icing conditions near Washington, D.C. when low ceilings occurred with surface temperatures near freezing. ...
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