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standard refraction

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standard refraction [′stan·dərd ri′frak·shən]
(electromagnetism)
Refraction which would occur in an idealized atmosphere in which the index of refraction decreases uniformly with height at a rate of 39 × 10-6per kilometer; standard refraction may be included in ground wave calculations by use of an effective earth radius of 8.5 × 106meters, or ⁴⁄₃ the geometrical radius of the earth.


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