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    Comparative Chloride Concentrations Between Mauna Loa Observatory and Hilo, Hawaii 

    Source: Journal of Applied Meteorology:;1972:;volume( 011 ):;issue: 004:;page 688
    Author(s): Semonin, Richard G.
    Publisher: American Meteorological Society
    Abstract: Millipore filter samples obtained at the Mauna Loa Observatory and at Hillo, Hawaii, were analyzed for chloride particle concentrations. These data are used in a transport model to determine the removal efficiency of ...
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    Comments on “Collision Efficiency of Water Drops in the Atmosphere” 

    Source: Journal of the Atmospheric Sciences:;1976:;Volume( 033 ):;issue: 009:;page 1826
    Author(s): Cataneo, Robert; Semonin, Richard G.
    Publisher: American Meteorological Society
    Abstract: No abstract available.
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    Chicago Area Program: A Major New Atmospheric Effort 

    Source: Bulletin of the American Meteorological Society:;1978:;volume( 059 ):;issue: 002:;page 153
    Author(s): Changnon, Stanley A.; Semonin, Richard G.
    Publisher: American Meteorological Society
    Abstract: A series of mesoscale meteorological research projects have developed since 1975 in the area over and around the south end of Lake Michigan. These regionally focused projects, under the label of the Chicago Area Program ...
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    Airborne Electrical Measurements in Dust Whirls 

    Source: Journal of the Atmospheric Sciences:;1963:;Volume( 020 ):;issue: 006:;page 622
    Author(s): Bradley, Wayne E.; Semonin, Richard G.
    Publisher: American Meteorological Society
    Abstract: No abstract available.
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    Two Case Studies of the Transport of Dust Storm Aerosol and the Potential for Incorporation into Precipitation 

    Source: Journal of Climate and Applied Meteorology:;1987:;Volume( 026 ):;Issue: 007:;page 763
    Author(s): Doty, Kevin G.; Semonin, Richard G.
    Publisher: American Meteorological Society
    Abstract: To investigate the hypothesis that dust storms enhanced the calcium concentrations in precipitation in the mid-1950s, two case studies were performed for major dust events in the southern Plains of the United States during ...
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    Atmospheric Issues Identified in State Water Resource Planning 

    Source: Bulletin of the American Meteorological Society:;1982:;volume( 063 ):;issue: 004:;page 399
    Author(s): Changnon, Stanley A.; Semonin, Richard G.
    Publisher: American Meteorological Society
    Abstract: Illinois is completing a comprehensive statewide water plan. The plan selects three atmospheric issues, among the 11 identified as key issues facing the state's water resources. The issues selected include climate change ...
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    Sensitivity of a Cloud Microphysical Model to an Urban Environment 

    Source: Journal of Applied Meteorology:;1979:;volume( 018 ):;issue: 009:;page 1118
    Author(s): Ochs, Harry T.; Semonin, Richard G.
    Publisher: American Meteorological Society
    Abstract: Observations showed increased concentrations of cloud condensation nuclei (CCN) in air samples collected over and downwind of St. Louis when compared to upwind samples. Aircraft observations of urban clouds showed corresponding ...
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    METROMEX: an Investigation of Inadvertent Weather Modification 

    Source: Bulletin of the American Meteorological Society:;1971:;volume( 052 ):;issue: 010:;page 958
    Author(s): Changnon, Stanley A.; Huff, Floyd A.; Semonin, Richard G.
    Publisher: American Meteorological Society
    Abstract: METROMEX, a field project designed and now in progress at St. Louis, involves 4 research groups planning and working cooperatively to study inadvertent weather modification by urban-industrial effects, and, in particular, ...
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    Interactions between Equal-Sized Droplets Due to the Wake Effect 

    Source: Journal of the Atmospheric Sciences:;1971:;Volume( 028 ):;issue: 003:;page 416
    Author(s): Cataneo, Robert; Adam, John R.; Semonin, Richard G.
    Publisher: American Meteorological Society
    Abstract: In the development of raindrops from cloud droplets in warm rain, the collision-coalescence process is considered to be the main growth mechanism for droplets of unequal size greater than 20 ?m in diameter. However, due ...
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