A truly multivariate normal score transform based on lagrangian flow
Document Type
Book Chapter
Publication Title
Geostatistics valencia 2016
Publisher
Springer, Cham
Place of Publication
Cham, Switzerland
School
School of Science
RAS ID
26251
Abstract
In many geostatistical applications, a transformation to standard normality is a first step in order to apply standard algorithms in two-point geostatistics. However, in the case of a set of collocated variables, marginal normality of each variable does not imply multivariate normality of the set, and a joint transformation is required. In addition, current methods are not affine equivariant, as should be required for multivariate regionalized data sets without a unique, canonical representation (e.g., vector-valued random fields, compositional random fields, layer cake models). This contribution presents an affine equivariant method of Gaussian anamorphosis based on a flow deformation of the joint sample space of the variables. The method numerically solves the differential equation of a continuous flow deformation that would transform a kernel density estimate of the actual multivariate density of the data into a standard multivariate normal distribution. Properties of the flow anamorphosis are discussed for a synthetic application, and the implementation is illustrated via two data sets derived from Western Australian mining contexts.
DOI
10.1007/978-3-319-46819-8_7
Access Rights
subscription content
Comments
Mueller, U., van den Boogaart, K. G., & Tolosana-Delgado, R. (2017). A truly multivariate normal score transform based on lagrangian flow. In J. Gómez-Hernández, J. Rodrigo-Ilarri, M. E. Rodrigo-Clavero, E. Cassiraga & J. A. Vargas-Guzmán (Eds.), Geostatistics valencia 2016 (pp. 107-118). Springer, Cham. Available here