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| المحاكاة الجيواحصائية الشرطية× | الكْرِيجَة الشاملة (الكْرِيجَة مع اتجاه)× | |
|---|---|---|
| المجال | التحليل المكاني | التحليل المكاني |
| العائلة | Regression model | Regression model |
| سنة النشأة≠ | 1997 | 1969 |
| صاحب الطريقة≠ | Pierre Goovaerts; geostatistics tradition | Georges Matheron |
| النوع≠ | Stochastic spatial simulation | Geostatistical interpolation with spatial trend |
| المصدر التأسيسي≠ | Goovaerts, P. (1997). Geostatistics for Natural Resources Evaluation. Oxford University Press. ISBN: 978-0-19-511538-3 | Matheron, G. (1963). Principles of geostatistics. Economic Geology, 58(8), 1246–1266. DOI ↗ |
| الأسماء البديلة | Sequential Gaussian Simulation, SGS, Stochastic Simulation, Koşullu Simülasyon | kriging with a trend, kriging with drift, trend kriging, evrensel kriging |
| ذات صلة≠ | 2 | 3 |
| الملخص≠ | Conditional 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. |
| ScholarGateمجموعة البيانات ↗ |
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