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Kriging Biasawan×Autokorelasi Ruang×
BidangAnalisis ReruangAnalisis Reruang
KeluargaRegression modelRegression model
Tahun asal19631950
PengasasGeorges Matheron (formalising D.G. Krige's empirical work)P. A. P. Moran (global measure, 1950); Roy Geary (Geary's C, 1954); Luc Anselin (LISA, 1995)
JenisGeostatistical interpolationSpatial statistic / exploratory spatial data analysis
Sumber perintisMatheron, G. (1963). Principles of geostatistics. Economic Geology, 58(8), 1246-1266. DOI ↗Moran, P. A. P. (1950). Notes on continuous stochastic phenomena. Biometrika, 37(1/2), 17–23. DOI ↗
AliasOK, kriging interpolation, geostatistical interpolation, BLUE spatial predictorspatial dependence, geographic autocorrelation, spatial clustering measure, SA
Berkaitan45
RingkasanOrdinary 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.Spatial autocorrelation quantifies the degree to which a variable's values at nearby locations resemble each other more (positive autocorrelation) or less (negative autocorrelation) than expected by chance. Global indices such as Moran's I summarise the pattern across the entire study area, while local variants reveal clusters and outliers at the level of individual observations.
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ScholarGateBandingkan kaedah: Ordinary Kriging · Spatial Autocorrelation. Dicapai 2026-06-18 daripada https://scholargate.app/ms/compare