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    HURRICANE SWELL AS A GENERATOR OF MICROSEISMS 

    Source: Journal of Meteorology:;1951:;volume( 008 ):;issue: 005:;page 347
    Author(s): Kammer, E. W.; Dinger, J. E.
    Publisher: American Meteorological Society
    Abstract: Seismographs were operated in the Bahama Islands and on the east coast of the United States during the hurricane season of 1950. Data from these instruments do not support the hypothesis that microseisms originate in the ...
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    Production of Cloud Nuclei by Ultraviolet Radiation 

    Source: Journal of the Atmospheric Sciences:;1973:;Volume( 030 ):;issue: 002:;page 331
    Author(s): Hoppel, W. A.; Dinger, J. E.
    Publisher: American Meteorological Society
    Abstract: No abstract available.
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    SEA SWELL AND MICROSEISMS 

    Source: Journal of Meteorology:;1952:;volume( 009 ):;issue: 006:;page 443
    Author(s): Vigness, Irwin; Kammer, E. W.; Dinger, J. E.; Irving, Laurence
    Publisher: American Meteorological Society
    Abstract: No Abstract Available
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    Vertical Profiles of CCN at Various Geographical Locations 

    Source: Journal of the Atmospheric Sciences:;1973:;Volume( 030 ):;issue: 007:;page 1410
    Author(s): Hoppel, W. A.; Dinger, J. E.; Ruskin, R. E.
    Publisher: American Meteorological Society
    Abstract: Measurements of the number density, volatility and supersaturation spectra of CCN during aircraft soundings to about 15,000 ft MSL over Arizona, Central Pacific, Alaska, and in a convective region over Florida, and on five ...
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    On the Source and Composition of Cloud Nuclei in a Subsident Air Mass over the North Atlantic 

    Source: Journal of the Atmospheric Sciences:;1970:;Volume( 027 ):;issue: 005:;page 791
    Author(s): Dinger, J. E.; Howell, H. B.; Wojciechowski, T. A.
    Publisher: American Meteorological Society
    Abstract: Measurements of the concentration of cloud nuclei, which are activated at a supersaturation of 0.75%, were made aboard an aircraft at various altitudes in a subsident air mass over the North Atlantic Ocean and on the cast ...
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