The Angular Distribution of Diffuse Sky Radiance: An Assessment of the Effects of Haze

1991 ◽  
Vol 113 (3) ◽  
pp. 200-205 ◽  
Author(s):  
M. A. Rosen

The effects of haze on the angular distribution of the diffuse sky radiance are investigated by examining and comparing data for individual clear skies with and without haze, and for other selected sky types, and by modeling and comparing data for such skies. It is found that haze appears to affect the radiance distributions only for clear, partly cloudy, and lightly overcast skies, and that for clear skies, increasing haze increases the absolute sky radiance values. In addition, the radiance distributions for clear skies with haze are found to exhibit characteristics generally similar to those for the nonopaque overcast skies. However, it is also found that the normalized radiance distributions for clear skies with haze, which generally provide clearer illustrations of distribution shape than the absolute radiance distributions, exhibit slightly less intense circumsolar and horizon brightening components than do the normalized distributions for clear skies without haze. In general, a systematic, but complex, relationship appears to exist between haze and the distribution of the diffuse sky radiance. The results may prove useful to several disciplines, including the design of solar technologies.

1990 ◽  
Vol 112 (2) ◽  
pp. 102-109 ◽  
Author(s):  
F. M. F. Siala ◽  
M. A. Rosen ◽  
F. C. Hooper

Both traditional and recently proposed models for the angular distribution of diffuse sky radiance are reviewed and compared. The models considered include basic models, sky-type-specific models, empirical and semi-empirical continuous distribution models, models which account for time-dependent cloud effects and stochastic models.


The methods described in a previous paper have been applied to an examination of the scattering of 4.2 MeV protons by protons. The angular distribution of the scattered protons is found to be isotropic, in the centre-of-mass co-ordinate system of the colliding particles, from 50 to 140° in the angle of scattering. A method of determining the absolute cross-section for proton-proton scattering at different energies, depending on the simultaneous recording of the protons scattered from hydrogen and from heavy nuclei is described, and the conditions necessary for its application at higher energies are discussed.


An external proton beam from the 110 in. Harwell cyclotron has been used to investigate proton-proton scattering at 147 MeV. The angular distribution of the scattering has been studied from 25 to 90° and found to be isotropic, within the limits of error. The absolute differential cross-section for scattering at 90° has been measured in two ways and found to be 4⋅94 ± 0⋅28 millibams. The results can also be used to find the 12 C( p , pn ) 11 C cross-section at 142 MeV.


Author(s):  
P. Echlin ◽  
M. McKoon ◽  
E.S. Taylor ◽  
C.E. Thomas ◽  
K.L. Maloney ◽  
...  

Although sections of frozen salt solutions have been used as standards for x-ray microanalysis, such solutions are less useful when analysed in the bulk form. They are poor thermal and electrical conductors and severe phase separation occurs during the cooling process. Following a suggestion by Whitecross et al we have made up a series of salt solutions containing a small amount of graphite to improve the sample conductivity. In addition, we have incorporated a polymer to ensure the formation of microcrystalline ice and a consequent homogenity of salt dispersion within the frozen matrix. The mixtures have been used to standardize the analytical procedures applied to frozen hydrated bulk specimens based on the peak/background analytical method and to measure the absolute concentration of elements in developing roots.


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