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    Applicability of Effective-Medium Theories to problems of Scattering and Absorption by Nonhomogeneous Atmospheric Particles 

    Source: Journal of the Atmospheric Sciences:;1986:;Volume( 043 ):;issue: 005:;page 468
    Author(s): Bohren, Craig F.
    Publisher: American Meteorological Society
    Abstract: Effective-medium theories yield effective dielectric functions (or, equivalently, refractive indices) of composite media. Such theories have been formulated that go beyond the Maxwell-Garnett and Bruggeman theories, which ...
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    Cloud Formation on Descent Revisited 

    Source: Journal of the Atmospheric Sciences:;1986:;Volume( 043 ):;issue: 023:;page 3035
    Author(s): Bohren, Craig F.
    Publisher: American Meteorological Society
    Abstract: tract
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    Radar Backscattering by Melting Snowflakes 

    Source: Journal of Applied Meteorology:;1982:;volume( 021 ):;issue: 012:;page 1937
    Author(s): Battan, Louis J.; Bohren, Craig F.
    Publisher: American Meteorological Society
    Abstract: No abstract available
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    Infrared Backscattering by Irregularly Shaped Particles: A Statistical Approach 

    Source: Journal of Climate and Applied Meteorology:;1984:;volume( 023 ):;issue: 009:;page 1342
    Author(s): Nevitt, Timothy J.; Bohren, Craig F.
    Publisher: American Meteorological Society
    Abstract: Shape can strongly affect scattering by particles at wavelengths near bulk absorption bands. An example is scattering by many components of the atmospheric aerosol at wavelengths in the transmission window centered around ...
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    Green Thunderstorms 

    Source: Bulletin of the American Meteorological Society:;1993:;volume( 074 ):;issue: 011:;page 2185
    Author(s): Bohren, Craig F.; Fraser, Alistair B.
    Publisher: American Meteorological Society
    Abstract: Green thunderstorms are observed occasionally, yet with one exception they have received no scientific attention, experimental or theoretical. Fraser suggested that thunderstorms themselves are not green but that a thick ...
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    Radar Backscattering by Inhomogeneous Precipitation Particles 

    Source: Journal of the Atmospheric Sciences:;1980:;Volume( 037 ):;issue: 008:;page 1821
    Author(s): Bohren, Craig F.; Battan, Louis J.
    Publisher: American Meteorological Society
    Abstract: Calculations of radar backscattering by inhomogeneous precipitation particles require values of the dielectric function of two-component mixtures. Four such dielectric functions are critically examined and their relative ...
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    Viewing the Vagaries and Verities of Virga 

    Source: Monthly Weather Review:;1993:;volume( 121 ):;issue: 008:;page 2429
    Author(s): Fraser, Alistair B.; Bohren, Craig F.
    Publisher: American Meteorological Society
    Abstract: No abstract available.
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    Is Virga Rain That Evaporates before Reaching the Ground? 

    Source: Monthly Weather Review:;1992:;volume( 120 ):;issue: 008:;page 1565
    Author(s): Fraser, Alistair B.; Bohren, Craig F.
    Publisher: American Meteorological Society
    Abstract: The visual phenomenon called virga, a sudden change in the brightness of a precipitation shaft below a cloud, is commonly attributed to evaporation of raindrops. It is said to be rain that does not reach the ground. The ...
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    Backscattering by Nonspherical Hydrometeors as Calculated by the Coupled-Dipole Method: An Application in Radar Meteorology 

    Source: Journal of Atmospheric and Oceanic Technology:;1993:;volume( 010 ):;issue: 004:;page 526
    Author(s): Dungey, Clifton E.; Bohren, Craig F.
    Publisher: American Meteorological Society
    Abstract: The severest test of a theory of scattering by particles is how well it calculates scattering in the backward direction. The coupled-dipole method can be used for accurately calculating backscattering at 94 GHz by hexagonal ...
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    Attenuation of Microwaves by Spherical Hail 

    Source: Journal of Climate and Applied Meteorology:;1986:;Volume( 025 ):;Issue: 008:;page 1155
    Author(s): Battan, Louis J.; Bohren, Craig F.
    Publisher: American Meteorological Society
    Abstract: Calculations have been made of the radar backscattering and attenuation cross sections of dry and spongy ice spheres. One set of calculations was the cross sections of spheres with diameters exponentially distributed. As ...
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