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  • 1
    Monograph available for loan
    Monograph available for loan
    Bedford, Mass. : Ft. Belvoir Defense Technical Information Center
    Associated volumes
    Call number: MOP 40425 / Mitte
    In: AFCRL
    Description / Table of Contents: The radiance and polarization of multiple scattered light is calculated from the Stoke's vectors by a Monte Carlo method. The exact scattering matrix for a typical haze and for a cloud whose spherical drops have an average radius of 12 microns is calculated from the Mie theory. The Stoke's vector is transformed in a collision by this scattering matrix and the rotation matrix. The two angles which define the photon direction after scattering are chosen by a random process which correctly stimulates the actual distribution functions for both angles. The Monte Carlo results for Rayleigh scattering compare favorably with well known tabulated results. Curves are given of the reflected and transmitted radiances and polarizations for both the haze and cloud models and for several solar angles, optical thicknesses, and surface albedos. The dependence on these various parameters is discussed. (Author).
    Type of Medium: Monograph available for loan
    Pages: 48 p.
    Series Statement: AFCRL 67-0570
    Location: MOP - must be ordered
    Branch Library: GFZ Library
    Location Call Number Expected Availability
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  • 2
    Monograph available for loan
    Monograph available for loan
    Bedford, Mass. : Ft. Belvoir Defense Technical Information Center
    Associated volumes
    Call number: MOP 36246
    In: AFCRL
    Description / Table of Contents: The light reflected and transmitted from clouds with various drop size distributions is calculated by a Monte Carlo technique. Six different models are used for the drop size distribution: isotropic; Rayleigh; haze continental; haze maritime; cumulus; nimbostratus. The scattering function for each model is calculated from the Mie theory. In general the reflected and transmitted radiance for the isotropic and Rayleigh models tend to be similar as are those for the various haze and cloud models. The reflected radiance is less for the haze and cloud models than for the isotropic and Rayleigh models, except for an angle of incidence near the horizon when it is larger around the incident beam direction. The transmitted radiance is always much larger for the haze and cloud models near the incident direction; at distant angles it is less for small and moderate optical thicknesses and greater for large optical thicknesses (all comparisons to isotropic and Rayleigh models). The downward flux, cloud albedo, and mean optical path are discussed. The angular spread of the beam as a function of optical thickness is shown for the nimbostratus model. (Author)
    Type of Medium: Monograph available for loan
    Pages: 44 p.
    Series Statement: AFCRL 67-0428
    Location: MOP - must be ordered
    Branch Library: GFZ Library
    Location Call Number Expected Availability
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