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    Extinction and Liquid Water Content Measurements at CO2 Laser wavelengths 

    Source: Journal of Atmospheric and Oceanic Technology:;1987:;volume( 004 ):;issue: 003:;page 391
    Author(s): Nolan, P. F.; Jennings, S. G.
    Publisher: American Meteorological Society
    Abstract: Measurements have been made of both extinction coefficients in an evaporating laboratory cloud at wavelength ? = 10.591 ?m using a CO2 laser, and of liquid water content (LWC) at the center of the cloud using a continuous ...
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    Volatility of Aerosols in the Arid Southwestern United States 

    Source: Journal of the Atmospheric Sciences:;1987:;Volume( 044 ):;issue: 003:;page 562
    Author(s): Pinnick, R. G.; Jennings, S. G.; Fernandez, G.
    Publisher: American Meteorological Society
    Abstract: Volatile properties of aerosols at an isolated rural site in south-central New Mexico were measured with a light-scattering particle counter equipped with a temperature-controlled heated inlet. Intermittent measurements ...
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    Verification of a Linear Relation between IR Extinction, Absorption and Liquid Water Content of Fogs 

    Source: Journal of the Atmospheric Sciences:;1979:;Volume( 036 ):;issue: 008:;page 1577
    Author(s): Pinnick, R. G.; Jennings, S. G.; Chýlek, Petr; Auvermann, H. J.
    Publisher: American Meteorological Society
    Abstract: A linear relationship, independent of the form of the size-distribution, between extinction at wave-lengths around ? = 11 µm, absorption around ? = 3.8 and 9.5 µm, and liquid water content of atmospheric fogs has been ...
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    Vertical Structure in Atmospheric Fog and Haze and Its Effects on Visible and Infrared Extinction 

    Source: Journal of the Atmospheric Sciences:;1978:;Volume( 035 ):;issue: 010:;page 2020
    Author(s): Pinnick, R. G.; Hoihjelle, D. L.; Fernandez, G.; Stenmark, E. B.; Lindberg, J. D.; Hoidale, G. B.; Jennings, S. G.
    Publisher: American Meteorological Society
    Abstract: Vertical structure of the size distribution and number concentration of particulates in atmospheric fog and haze near Grafenwöhr, West Germany, were measured with a balloonborne light-scattering aerosol counter for periods ...
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