Atmospheric effect on the upwelling radiation at the top of the atmosphere over a stream

Details Atmospheric effect on the upwelling radiation at the top of the atmosphere over a stream Atmospheric effect on the upwelling radiation at the top of the atmosphere over a stream

Apr 1992

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1992em%26p...57...75t&link_type=abstract

Earth, Moon, and Planets (ISSN 0167-9295), vol. 57, no. 1, April 1992, p. 75-84.

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Atmospheric Boundary Layer, Atmospheric Effects, Atmospheric Scattering, Computerized Simulation, Lambert Surface, Aerosols, Optical Thickness, Radiative Transfer

Scientific paper

The atmospheric effect on the upwelling radiation at the top of the atmosphere over a stream is investigated using the Takashima and Masuda (1992) approach, where the atmosphere is bounded by two half Lambert surfaces and by the stream inserted between them. In the computations, the probability of radiation interacting with the respective half surfaces and the stream is calculated based on the assumption of single scattering in the atmosphere. The results of numerical simulation indicate that the surroundings have a significant effect on the radiation from the stream.

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