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Excerpt from Advances in Ionospheric Mapping by Numerical Methods
Geographic Coordinate Functions Gk(y,e) for Analysis of fof2 Median (a geographic latitude, 9 geographic longitude, x modified magnetic dip)functions involving 9, at the geographic poles. This prevents further ambiguous values at the poles. The variable x could also have'been used in the weight factors, in place of A, since cos x 0, when A i This change could be considered in future work, although its effect would perhaps be negligible.
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