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    Degree of Interdependence among Atmospheric Optical Thicknesses in Spectral Bands between 0.36–2.4 μm 

    Source: Journal of Applied Meteorology:;1975:;volume( 014 ):;issue: 006:;page 1187
    Author(s): Fraser, Robert S.
    Publisher: American Meteorological Society
    Abstract: The degree of dependence among the atmospheric optical thicknesses that are measured in nonselective absorption bands is studied. The observations were made previously in many spectral bands within the range 0.36?2.4 ?m ...
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    An Iterative Radiative Transfer Code For Ocean-Atmosphere Systems 

    Source: Journal of the Atmospheric Sciences:;1982:;Volume( 039 ):;issue: 003:;page 656
    Author(s): Ahmad, Ziauddin; Fraser, Robert S.
    Publisher: American Meteorological Society
    Abstract: We describe the details of an iterative radiative transfer code for computing the intensity and degree of polarization of diffuse radiation in models of the ocean-atmosphere system. The present code neglects the upwelling ...
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    Light Extinction by Aerosols during Summer Air Pollution 

    Source: Journal of Climate and Applied Meteorology:;1983:;volume( 022 ):;issue: 010:;page 1694
    Author(s): Kaufman, Yoram J.; Fraser, Robert S.
    Publisher: American Meteorological Society
    Abstract: In order to utilize satellite measurements of optical thickness over land for estimating aerosol properties during air pollution episodes the optical thickness was measured from the surface and investigated. Aerosol optical ...
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    Comparison of Results Obtained by Solving the Radiative Transfer Equation with an Iterative Method and a Spherical Harmonies Method 

    Source: Journal of the Atmospheric Sciences:;1977:;Volume( 034 ):;issue: 003:;page 553
    Author(s): Bahethi, Om P.; Fraser, Robert S.
    Publisher: American Meteorological Society
    Abstract: Fluxes and intensifies of light scattered by a model atmosphere are computed by a spherical harmonics approximation and by an iterative method of solving the radiative transfer equation and are compared. The large differences ...
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    Reflectivity of the Atmosphere-Inhomogeneous Surfaces System: Laboratory Simulation 

    Source: Journal of the Atmospheric Sciences:;1984:;Volume( 041 ):;issue: 017:;page 2595
    Author(s): Mekler, Yuri; Kaufman, Yoram J.; Fraser, Robert S.
    Publisher: American Meteorological Society
    Abstract: Theoretical two- and three-dimensional solutions of the radiative transfer equation have been applied to the earth-atmosphere system. Such solutions have not been verified experimentally. A laboratory experiment simulates ...
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    Fossil Fuel and Biomass Burning Effect on Climate—Heating or Cooling? 

    Source: Journal of Climate:;1991:;volume( 004 ):;issue: 006:;page 578
    Author(s): Kaufman, Yoram J.; Fraser, Robert S.; Mahoney, Robert L.
    Publisher: American Meteorological Society
    Abstract: Emission from burning of fossil fuels and biomass (associated with deforestation) generates a radiative forcing on the atmosphere and a possible climate chaw. Emitted trace gases heat the atmosphere through their greenhouse ...
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