Methoden vergelijken

	Panel Ordinary Kriging	Universeel Kriging (Kriging met een Trend)
Vakgebied	Ruimtelijke analyse	Ruimtelijke analyse
Familie	Regression model	Regression model
Jaar van ontstaan	1963 (Ordinary Kriging origin); panel extensions formalized in 1990s–2000s	1969
Grondlegger	Extension of Ordinary Kriging (Matheron, 1963) to panel/longitudinal spatial settings	Georges Matheron
Type	Geostatistical spatial interpolation	Geostatistical interpolation with spatial trend
Oorspronkelijke bron	Cressie, N. A. C. (1993). Statistics for Spatial Data (revised ed.). Wiley-Interscience. ISBN: 978-0471002550	Matheron, G. (1963). Principles of geostatistics. Economic Geology, 58(8), 1246–1266.
Aliassen	ordinary kriging for panel data, longitudinal ordinary kriging, repeated-measures spatial kriging, panel geostatistical interpolation	kriging with a trend, kriging with drift, trend kriging, evrensel kriging
Verwant	6	3
Samenvatting	Panel Ordinary Kriging extends the classical geostatistical interpolation method — Ordinary Kriging — to panel (longitudinal) datasets where the same set of spatial locations is observed repeatedly over multiple time periods. It produces optimal linear unbiased predictions at unsampled locations for each time slice, accounting for spatial dependence while leveraging the temporal structure of the repeated observations.	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.