Non-stationary variogram models for geostatistical sampling
optimisation: an empirical investigation using elevation data
Non-stationary variogram models for geostatistical sampling
optimisation: an empirical investigation using elevation data
A problem with use of the geostatistical Kriging error for optimal sampling design is that the design does not adapt locally to the character of spatial variation. This is because a stationary variogram or covariance function is a parameter of the geostatistical model. The objective of this paper was to investigate the utility of non-stationary geostatistics for optimal sampling design. First, a contour data set of Wiltshire was split into 25 equal sub-regions and a local variogram was predicted for each. These variograms were fitted with models and the coefficients used in Kriging to select optimal sample spacings for each sub-region. Large differences existed between the designs for the whole region (based on the global variogram) and for the sub-regions (based on the local variograms). Second, a segmentation approach was used to divide a digital terrain model into separate segments. Segment-based variograms were predicted and fitted with models. Optimal sample spacings were then determined for the whole region and for the sub-regions. It was demonstrated that the global design was inadequate, grossly over-sampling some segments while under-sampling others.
kriging, spatial structure, dem
1285-1300
Atkinson, P.M.
96e96579-56fe-424d-a21c-17b6eed13b0b
LLoyd, C.D.
2d3bd538-2045-4fbb-900c-9f77c386bbc9
October 2007
Atkinson, P.M.
96e96579-56fe-424d-a21c-17b6eed13b0b
LLoyd, C.D.
2d3bd538-2045-4fbb-900c-9f77c386bbc9
Atkinson, P.M. and LLoyd, C.D.
(2007)
Non-stationary variogram models for geostatistical sampling
optimisation: an empirical investigation using elevation data.
Computers & Geosciences, 33 (10), .
(doi:10.1016/j.cageo.2007.05.011).
Abstract
A problem with use of the geostatistical Kriging error for optimal sampling design is that the design does not adapt locally to the character of spatial variation. This is because a stationary variogram or covariance function is a parameter of the geostatistical model. The objective of this paper was to investigate the utility of non-stationary geostatistics for optimal sampling design. First, a contour data set of Wiltshire was split into 25 equal sub-regions and a local variogram was predicted for each. These variograms were fitted with models and the coefficients used in Kriging to select optimal sample spacings for each sub-region. Large differences existed between the designs for the whole region (based on the global variogram) and for the sub-regions (based on the local variograms). Second, a segmentation approach was used to divide a digital terrain model into separate segments. Segment-based variograms were predicted and fitted with models. Optimal sample spacings were then determined for the whole region and for the sub-regions. It was demonstrated that the global design was inadequate, grossly over-sampling some segments while under-sampling others.
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Published date: October 2007
Keywords:
kriging, spatial structure, dem
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Local EPrints ID: 52541
URI: http://eprints.soton.ac.uk/id/eprint/52541
ISSN: 0098-3004
PURE UUID: 0c170114-ca84-4d32-bf82-516b5a4ac1eb
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Date deposited: 09 Jul 2008
Last modified: 16 Mar 2024 02:46
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Author:
P.M. Atkinson
Author:
C.D. LLoyd
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