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راجع الطرق التي اخترتها جنبًا إلى جنب؛ الصفوف المختلفة مميَّزة.

الكراجينغ العادي×الكْرِيجَة الشاملة (الكْرِيجَة مع اتجاه)×
المجالالتحليل المكانيالتحليل المكاني
العائلةRegression modelRegression model
سنة النشأة19631969
صاحب الطريقةGeorges Matheron (formalising D.G. Krige's empirical work)Georges Matheron
النوعGeostatistical interpolationGeostatistical interpolation with spatial trend
المصدر التأسيسيMatheron, 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 ↗
الأسماء البديلةOK, kriging interpolation, geostatistical interpolation, BLUE spatial predictorkriging with a trend, kriging with drift, trend kriging, evrensel kriging
ذات صلة43
الملخصOrdinary 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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ScholarGateقارن الطرق: Ordinary Kriging · Universal Kriging. استُرجع بتاريخ 2026-06-18 من https://scholargate.app/ar/compare