The Grid-Free Spatial Kernel Predictor for Huge Observation Sets

Abstract Assessment of a continuous spatial variable based on a set of m observations is usually performed in a Gaussian random field framework. The optimal predictor under this model can be presented either as a linear kriging predictor or as a dual kriging predictor. The spatial variable predictor is usually stored in a kriging grid representation of size n . Alternatively, one may define a kernel function representation based on the dual kriging formulation. The latter can be efficiently reduced to the former, but not vice versa. To provide a prediction at an arbitrary location, a piecewise planar interpolation in the actual grid unit is typically required. For the functional representation, the functional value in the actual location must be calculated. The computational challenge of both representations is primarily related to the inversion of the observation covariance $$ ( m \times m ) $$ <mml:math xmlns:mml="http://www.w3.org/1998/Math/MathML"> <mml:mrow> <mml:mo>(</mml:mo> <mml:mi>m</mml:mi> <mml:mo>×</mml:mo> <mml:mi>m</mml:mi> <mml:mo>)</mml:mo> </mml:mrow> </mml:math> -matrix. In large spatial studies with huge sets of observations, and thus huge m , this inversion may not be computationally feasible. Localized kriging predictors are then frequently used to generate the grid representation of the spatial variable. This approach has computational demands proportional to the grid size n . We present a localized kernel predictor to provide a functional representation of the spatial variable. The specification of this localized kernel predictor constitutes the major contribution of this paper. This predictor has computational demands proportional to the number of observations m . This is particularly beneficial in three-dimensional models and spatiotemporal studies where one typically has $$ n \gg m $$ <mml:math xmlns:mml="http://www.w3.org/1998/Math/MathML"> <mml:mrow> <mml:mi>n</mml:mi> <mml:mo>≫</mml:mo> <mml:mi>m</mml:mi> </mml:mrow> </mml:math> . The characteristics of the kernel predictor are demonstrated in an example. A study on real observations indicates that the localized kernel function representation has substantial computational advantages over the localized kriging grid representation. Even generating the grid representation from a kernel function representation appears more computationally efficient than generating it directly using a localized kriging predictor.

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Publication Details

Journal
Mathematical Geosciences
Published
2026-01-13
DOI
https://doi.org/10.1007/s11004-025-10252-y
Primary Topic
Soil Geostatistics and Mapping
Type
article
Field-Weighted Citation Impact
0.00

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article

The Grid-Free Spatial Kernel Predictor for Huge Observation Sets

Henning Omre, Mina Spremic
Mathematical Geosciences
Soil Geostatistics and Mapping
article

The Grid-Free Spatial Kernel Predictor for Huge Observation Sets

Henning Omre, Mina Spremic
article en

Abstract

Abstract Assessment of a continuous spatial variable based on a set of m observations is usually performed in a Gaussian random field framework. The optimal predictor under this model can be presented either as a linear kriging predictor or as a dual kriging predictor. The spatial variable predictor is usually stored in a kriging grid representation of size n . Alternatively, one may define a kernel function representation based on the dual kriging formulation. The latter can be efficiently reduced to the former, but not vice versa. To provide a prediction at an arbitrary location, a piecewise planar interpolation in the actual grid unit is typically required. For the functional representation, the functional value in the actual location must be calculated. The computational challenge of both representations is primarily related to the inversion of the observation covariance $$ ( m \times m ) $$ <mml:math xmlns:mml="http://www.w3.org/1998/Math/MathML"> <mml:mrow> <mml:mo>(</mml:mo> <mml:mi>m</mml:mi> <mml:mo>×</mml:mo> <mml:mi>m</mml:mi> <mml:mo>)</mml:mo> </mml:mrow> </mml:math> -matrix. In large spatial studies with huge sets of observations, and thus huge m , this inversion may not be computationally feasible. Localized kriging predictors are then frequently used to generate the grid representation of the spatial variable. This approach has computational demands proportional to the grid size n . We present a localized kernel predictor to provide a functional representation of the spatial variable. The specification of this localized kernel predictor constitutes the major contribution of this paper. This predictor has computational demands proportional to the number of observations m . This is particularly beneficial in three-dimensional models and spatiotemporal studies where one typically has $$ n \gg m $$ <mml:math xmlns:mml="http://www.w3.org/1998/Math/MathML"> <mml:mrow> <mml:mi>n</mml:mi> <mml:mo>≫</mml:mo> <mml:mi>m</mml:mi> </mml:mrow> </mml:math> . The characteristics of the kernel predictor are demonstrated in an example. A study on real observations indicates that the localized kernel function representation has substantial computational advantages over the localized kriging grid representation. Even generating the grid representation from a kernel function representation appears more computationally efficient than generating it directly using a localized kriging predictor.

Mathematical Geosciences
Norwegian University of Science and Technology (NO), Department of Mathematical Sciences (RU)
Norges Teknisk-Naturvitenskapelige Universitet, Norges Forskningsråd, St. Olavs Hospital Universitetssykehuset i Trondheim, Division of Mathematical Sciences
Openalex Percentile: Top 91%
Soil Geostatistics and Mapping
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