Maximum-likelihood estimation of the Matérn covariance structure of isotropic spatial random fields on finite, sampled grids

SUMMARY We present a statistically and computationally efficient spectral-domain maximum-likelihood procedure to solve for the structure of Gaussian spatial random fields within the Matérn covariance hyperclass. For univariate, stationary and isotropic fields, the three controlling parameters are the process variance, smoothness and range. The debiased Whittle likelihood maximization explicitly treats discretization and edge effects for finite sampled regions in parameter estimation and uncertainty quantification. As even the ‘best’ parameter estimate may not be ‘good enough’, we provide a test for whether the model specification itself warrants rejection. Our results are practical and relevant for the study of a variety of geophysical fields, and for spatial interpolation, out-of-sample extension, kriging, machine learning and feature detection of geological data. We present procedural details and high-level results on real-world examples.

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Publication Details

Journal
Geophysical Journal International
Published
2026-01-28
DOI
https://doi.org/10.1093/gji/ggag044
Primary Topic
Soil Geostatistics and Mapping
Type
article
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article

Maximum-likelihood estimation of the Matérn covariance structure of isotropic spatial random fields on finite, sampled grids

G. L. Eggers, Olivia Leigh Walbert, Sofia C. Olhede, Arthur P. Guillaumin et al.
Geophysical Journal International
Soil Geostatistics and Mapping
article

Maximum-likelihood estimation of the Matérn covariance structure of isotropic spatial random fields on finite, sampled grids

G. L. Eggers, Olivia Leigh Walbert, Sofia C. Olhede, Arthur P. Guillaumin, Frederik J. Simons, K Lewis
article en

Abstract

SUMMARY We present a statistically and computationally efficient spectral-domain maximum-likelihood procedure to solve for the structure of Gaussian spatial random fields within the Matérn covariance hyperclass. For univariate, stationary and isotropic fields, the three controlling parameters are the process variance, smoothness and range. The debiased Whittle likelihood maximization explicitly treats discretization and edge effects for finite sampled regions in parameter estimation and uncertainty quantification. As even the ‘best’ parameter estimate may not be ‘good enough’, we provide a test for whether the model specification itself warrants rejection. Our results are practical and relevant for the study of a variety of geophysical fields, and for spatial interpolation, out-of-sample extension, kriging, machine learning and feature detection of geological data. We present procedural details and high-level results on real-world examples.

Geophysical Journal InternationalVol. 245(2)
Wesleyan University (US), Planetary Science Institute (US), Johns Hopkins University (US), Queen Mary University of London (GB), Princeton University (US), Johns Hopkins Medicine (US), École Polytechnique Fédérale de Lausanne (CH)
Openalex Percentile: Top 78%
Soil Geostatistics and Mapping
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Maximum-likelihood estimation of the Matérn covariance structure of isotropic spatial random fields on finite, sampled grids — G. L. Eggers, Olivia Leigh Walbert, et al. · Geophysical Journal International (2026) | TGRS Research Map | TGRS