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Comparar métodos

Examine os métodos selecionados lado a lado; as linhas que diferem ficam destacadas.

Krigagem Universal (Krigagem com Tendência)×Cokrigagem×Ponderação por Distância Inversa (IDW)×
ÁreaAnálise espacialAnálise espacialAnálise espacial
FamíliaRegression modelRegression modelRegression model
Ano de origem196919631968
Autor originalGeorges MatheronGeorges Matheron (geostatistics); multivariate extensionDonald Shepard
TipoGeostatistical interpolation with spatial trendMultivariate geostatistical interpolationDeterministic spatial interpolation
Fonte seminalMatheron, 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 ↗Shepard, D. (1968). A two-dimensional interpolation function for irregularly-spaced data. Proceedings of the 23rd ACM National Conference, 517–524. DOI ↗
Outros nomeskriging with a trend, kriging with drift, trend kriging, evrensel krigingco-kriging, multivariate kriging, ortak krigingIDW, inverse distance interpolation, Shepard's method, ters mesafe ağırlıklı enterpolasyon
Relacionados333
ResumoUniversal 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.Cokriging extends kriging to use one or more correlated secondary variables to improve prediction of a primary variable. When the variable of interest is sparsely sampled but a related, cheaper-to-measure variable is densely sampled, cokriging borrows strength from the secondary variable through their cross-correlation, yielding more accurate interpolations and prediction variances than kriging the primary variable alone.Inverse distance weighting is a simple, deterministic method for estimating values at unsampled locations by taking a weighted average of nearby measured points, where closer points carry more weight. Introduced by Donald Shepard in 1968, it embodies the first law of geography — near things are more related than distant things — and is one of the most widely used interpolation methods in GIS for mapping continuous fields such as rainfall, elevation, or pollution from scattered samples.
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ScholarGateComparar métodos: Universal Kriging · Cokriging · Inverse Distance Weighting. Recuperado em 2026-06-20 de https://scholargate.app/pt/compare