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Bekijk de geselecteerde methoden naast elkaar; rijen die verschillen zijn gemarkeerd.

Gewone Kriging×Universeel Kriging (Kriging met een Trend)×
VakgebiedRuimtelijke analyseRuimtelijke analyse
FamilieRegression modelRegression model
Jaar van ontstaan19631969
GrondleggerGeorges Matheron (formalising D.G. Krige's empirical work)Georges Matheron
TypeGeostatistical interpolationGeostatistical interpolation with spatial trend
Oorspronkelijke bronMatheron, G. (1963). Principles of geostatistics. Economic Geology, 58(8), 1246-1266. DOI ↗Matheron, G. (1963). Principles of geostatistics. Economic Geology, 58(8), 1246–1266. DOI ↗
AliassenOK, kriging interpolation, geostatistical interpolation, BLUE spatial predictorkriging with a trend, kriging with drift, trend kriging, evrensel kriging
Verwant43
SamenvattingOrdinary Kriging (OK) is the standard geostatistical method for interpolating a continuous spatial variable at unsampled locations. It derives optimal, unbiased weights from the spatial covariance structure of the data, making it the Best Linear Unbiased Predictor (BLUP) under stationarity assumptions. Unlike simpler distance-based methods, it also provides a prediction uncertainty (kriging variance) at every interpolated point.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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  3. PUBLISHED
  1. v1
  2. 2 Bronnen
  3. PUBLISHED

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ScholarGateMethoden vergelijken: Ordinary Kriging · Universal Kriging. Geraadpleegd op 2026-06-18 via https://scholargate.app/nl/compare