Refraction in the meridional model of the atmosphere. Algorithm of computations.

Statistics – Computation

Scientific paper

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Refraction: Computer Simulations, Refraction: Earth Atmosphere

Scientific paper

An algorithm of computations is described. Forms of the airstrata of equal density are given. At the zenith distances of 0 - 60° the results obtained using the mean (normal) meridional model of the atmosphere (the so-called three-dimensional atmosphere) are the same (to 0.006″ as those obtained by the spherically-symmetric atmospheric model. At greater zenith distances there are essential differences between the results.

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