A method of evaluation of the atmospheric effect on the emergent radiation over the infinite-cliff

Details A method of evaluation of the atmospheric effect on the emergent radiation over the infinite-cliff A method of evaluation of the atmospheric effect on the emergent radiation over the infinite-cliff

Jan 1994

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1994em%26p...64...39t&link_type=abstract

Earth, Moon, and Planets, vol. 64, no. 1, p. 39-46

Statistics

Computation

Atmospheric Effects, Radiative Transfer, Terrestrial Radiation, Computation, Mathematical Models, Numerical Analysis, Remote Sensing

Scientific paper

To evaluate the effect of the cliff on the radiation field, the upwelling radiation at the top of the atmosphere is computed over the cliff using the reflection and transmission functions derived from the doubling-adding method. The model is defined by the plane-parallel homogeneous atmosphere, which is composed of aerosol and molecules, and is bounded by the top level surface, cliff and low level surface. These surfaces may be assumed to be the Lambertian. In the computational procedure, the equation for the emergent radiation is expanded into a series of radiative interaction modes among atmosphere, surfaces and the cliff. In respective modes, probabilities of respective interactions are firstly evaluated. With the aid of these probabilities, the emergent radiation is calculated using the doubling-adding method for the model atmosphere bounded by the surfaces and cliff, where the above radiative interactions are considered up to twice as large to obtain the enough accuracy of simulation. The multiple scattering is considered.

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