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Simulation géostatistique conditionnelle×Krigage universel (Krigage avec une tendance)×
DomaineAnalyse spatialeAnalyse spatiale
FamilleRegression modelRegression model
Année d'origine19971969
Auteur d'originePierre Goovaerts; geostatistics traditionGeorges Matheron
TypeStochastic spatial simulationGeostatistical interpolation with spatial trend
Source fondatriceGoovaerts, P. (1997). Geostatistics for Natural Resources Evaluation. Oxford University Press. ISBN: 978-0-19-511538-3Matheron, G. (1963). Principles of geostatistics. Economic Geology, 58(8), 1246–1266. DOI ↗
AliasSequential Gaussian Simulation, SGS, Stochastic Simulation, Koşullu Simülasyonkriging with a trend, kriging with drift, trend kriging, evrensel kriging
Apparentées23
RésuméConditional Geostatistical Simulation — most commonly implemented as Sequential Gaussian Simulation (SGS) — generates multiple stochastic realizations of a spatial random field that are each consistent with observed sample data and with a fitted variogram model. Unlike kriging, which produces a single smoothed estimate, SGS reproduces the full spatial variability of the phenomenon. It is widely used by geoscientists, mining engineers, petroleum engineers, and environmental scientists who need to propagate spatial uncertainty through downstream models.Universal kriging generalizes ordinary kriging to data whose mean varies systematically across space — a spatial trend or 'drift'. It models the mean as a function of the coordinates (or covariates) and krigs the residuals, so it can interpolate variables that drift in a preferred direction, such as temperature falling with latitude or a pollutant gradient, while still returning prediction variances.
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ScholarGateComparer des méthodes: Conditional Geostatistical Simulation · Universal Kriging. Consulté le 2026-06-15 sur https://scholargate.app/fr/compare