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Eight methods of computing atmospheric refraction of radio rays are discussed with appropriate theoretical background. These methods are: (1) The high-angle, or astronomical, refraction case; (2) The statistical method; (3) The low-angle, or terrestrial, refraction case (Schulkin's method); (4) The four-thirds earth model; (5) The exponential model; (6) The initial gradient correction method; (7) The departures-from-normal method; (8) A graphical method (Weisbrod's and Anderson's method). Sample computations are included for each of the above methods.
Eight methods of computing atmospheric refraction of radio rays are discussed with appropriate theoretical background. These methods are: the high-angle, or astronomical, refraction case; the statistial method; the low-angle, or terrestrial, refraction case (Schulkin's method); the four-thirds earth model; the exponential model; the initial gradient correction method; the deprtures-from-normal method; and a graphical method (Weisbrod's and Anderson's method). Sample computations are included for each of the methods. (Author).
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