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Hence the neglect of polarization of radiation is unavoidable to a large extent. The influence of refraction on atmospheric radiative transfer is of importance only in some special cases, and therefore it is possible to ignore this influence in the general consideration of the problem. Let us now turn to the derivation of the general transfer equation for a stationary field of unpolarized radiation. Let us take an arbitrarily directed ray ( r = direction) and consider an environmental element in the form of a cylinder of unit section, the axis of which coincides with the direction of the ray.
Experimental investigations are in conformity with this conclusion. 10 displays some measurement results for several dielectrics. 40 Radiant Energy. 5%. 2. Thermal Emission of Conductors. The theory of reflection of radiation from metals, owing to its complexity, has not yet been sufficiently worked out. Computations and measurements of the reflectivity of metals show that they are good reflectors of both thermal and visible radiations. Accordingly, the absorptivity (and emissivity) of metals is not high.
Am. 42, No. 9. 7. Plass, G. N. (1963). Spectral band absorptance for atmospheric slant paths. Appl. Opt. 2, No. 5 . 8. Ambartzumian, V. , Mustel, E. , Severny, A. , and Sobolev V. V. (1952). ” Moscow. 9. Milne, E. A,, (1928). Influence of collisions on monochromatic radiative equilibrium. Moritly Notices Roy. Astron. 88, No. 5 . 48 Radiant Energy. The Main Concepts and Definitions 10. Goody, R. M. (1954). ” Cambridge Univ. Press, London and New York. 11. Woolley, R. (1947). Radiative equilibrium in the ionosphere.
Advances in Computers, Vol. 21