Abstract
Spatial environmental processes often exhibit non-stationarity. Modelling the dispersion d(x, y) = E(Z(x) — Z(y))2 , (x, y) ∈ ℝ2 x ℝ2, of a non-stationary spatial process Z(x) has been proposed in the last decade. It consists of deforming bijectively the geographic coordinate x so that the spatial dispersion structure can be considered stationary and isotropic in terms of a new spatial coordinate system. The model is d(x, y) = γβ (∥f(y) — f(x)∥) where f represents a bijective transformation and γβ a stationary and isotropic variogram function with parameters β. The non-parametric family of thin-plate splines was used to compute the deformation with two drawbacks: (i) bijection condition is not ensured (ii) the fitting of the model can be a challenging numerical problem. To avoid these disadvantages we propose to use a parametric family of bijective functions we call Radial Basis Deformations. Bijection is ensured by a constraint on parameters and deformation f is a composition of a small number of radial elementary deformations. The paper presents definition and properties of these Radial Basis Deformations. We apply our parametric approach on a precipitation data set.
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© 1999 Springer Science+Business Media Dordrecht
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Perrin, O., Monestiez, P. (1999). Modelling of Non-Stationary Spatial Structure Using Parametric Radial Basis Deformations. In: Gómez-Hernández, J., Soares, A., Froidevaux, R. (eds) geoENV II — Geostatistics for Environmental Applications. Quantitative Geology and Geostatistics, vol 10. Springer, Dordrecht. https://doi.org/10.1007/978-94-015-9297-0_15
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DOI: https://doi.org/10.1007/978-94-015-9297-0_15
Publisher Name: Springer, Dordrecht
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