MODELING IN N DIMENSIONS USING A WEIGHTING FUNCTION APPROACH
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abstract
A general technique for mathematically modeling n-dimensional geodetic phenomena with arbitrary order continuity is developed. The mathematical model, or approximation, of the geodetic function is a globally valid model composed of an arbitrarily large family of locally valid continuously joining functions. Each local approximation is valid over a hypercube in n space, constructed so that adjacent approximations join with mth order continuity satisfied throughout the model. This technique is based on a unique set of polynomial weighting functions; analytic formulas for the weighting functions for n-dimensional mth order continuous modeling are derived and presented.