Estimating unconsolidated sediment cover thickness by using the horizontal distance to a bedrock outcrop as secondary information

Unconsolidated sediment cover thickness (<i>D</i>) above bedrock was estimated by using a publicly available well database from Norway, GRANADA. General challenges associated with such databases typically involve clustering and bias. However, if information about the horizontal distan...

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Main Author: N.-O. Kitterød
Format: Article
Language:English
Published: Copernicus Publications 2017-08-01
Series:Hydrology and Earth System Sciences
Online Access:https://www.hydrol-earth-syst-sci.net/21/4195/2017/hess-21-4195-2017.pdf
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spelling doaj-d8efa2d813784bbbbb9db680afe431232020-11-24T22:23:39ZengCopernicus PublicationsHydrology and Earth System Sciences1027-56061607-79382017-08-01214195421110.5194/hess-21-4195-2017Estimating unconsolidated sediment cover thickness by using the horizontal distance to a bedrock outcrop as secondary informationN.-O. Kitterød0N.-O. Kitterød1N.-O. Kitterød2Norwegian University of Life Sciences, Environmental Sciences and Natural Resource Management, P.O. Box 5003, 1432 Ås, NorwayNIBIO – Norwegian Institute of Bioeconomy Research, Water Resources, P.O. Box 115, 1431 Ås, NorwayIrstea, UR HHLY, Centre de Lyon-Villeurbanne, 5 rue de la Doua BP 32108, 69626 Villeurbanne Cedex, FranceUnconsolidated sediment cover thickness (<i>D</i>) above bedrock was estimated by using a publicly available well database from Norway, GRANADA. General challenges associated with such databases typically involve clustering and bias. However, if information about the horizontal distance to the nearest bedrock outcrop (<i>L</i>) is included, does the spatial estimation of <i>D</i> improve? This idea was tested by comparing two cross-validation results: ordinary kriging (OK) where <i>L</i> was disregarded; and co-kriging (CK) where cross-covariance between <i>D</i> and <i>L</i> was included. The analysis showed only minor differences between OK and CK with respect to differences between estimation and true values. However, the CK results gave in general less estimation variance compared to the OK results. All observations were declustered and transformed to standard normal probability density functions before estimation and back-transformed for the cross-validation analysis. The semivariogram analysis gave correlation lengths for <i>D</i> and <i>L</i> of approx. 10 and 6 km. These correlations reduce the estimation variance in the cross-validation analysis because more than 50 % of the data material had two or more observations within a radius of 5 km. The small-scale variance of <i>D</i>, however, was about 50 % of the total variance, which gave an accuracy of less than 60 % for most of the cross-validation cases. Despite the noisy character of the observations, the analysis demonstrated that <i>L</i> can be used as secondary information to reduce the estimation variance of <i>D</i>.https://www.hydrol-earth-syst-sci.net/21/4195/2017/hess-21-4195-2017.pdf
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language English
format Article
sources DOAJ
author N.-O. Kitterød
N.-O. Kitterød
N.-O. Kitterød
spellingShingle N.-O. Kitterød
N.-O. Kitterød
N.-O. Kitterød
Estimating unconsolidated sediment cover thickness by using the horizontal distance to a bedrock outcrop as secondary information
Hydrology and Earth System Sciences
author_facet N.-O. Kitterød
N.-O. Kitterød
N.-O. Kitterød
author_sort N.-O. Kitterød
title Estimating unconsolidated sediment cover thickness by using the horizontal distance to a bedrock outcrop as secondary information
title_short Estimating unconsolidated sediment cover thickness by using the horizontal distance to a bedrock outcrop as secondary information
title_full Estimating unconsolidated sediment cover thickness by using the horizontal distance to a bedrock outcrop as secondary information
title_fullStr Estimating unconsolidated sediment cover thickness by using the horizontal distance to a bedrock outcrop as secondary information
title_full_unstemmed Estimating unconsolidated sediment cover thickness by using the horizontal distance to a bedrock outcrop as secondary information
title_sort estimating unconsolidated sediment cover thickness by using the horizontal distance to a bedrock outcrop as secondary information
publisher Copernicus Publications
series Hydrology and Earth System Sciences
issn 1027-5606
1607-7938
publishDate 2017-08-01
description Unconsolidated sediment cover thickness (<i>D</i>) above bedrock was estimated by using a publicly available well database from Norway, GRANADA. General challenges associated with such databases typically involve clustering and bias. However, if information about the horizontal distance to the nearest bedrock outcrop (<i>L</i>) is included, does the spatial estimation of <i>D</i> improve? This idea was tested by comparing two cross-validation results: ordinary kriging (OK) where <i>L</i> was disregarded; and co-kriging (CK) where cross-covariance between <i>D</i> and <i>L</i> was included. The analysis showed only minor differences between OK and CK with respect to differences between estimation and true values. However, the CK results gave in general less estimation variance compared to the OK results. All observations were declustered and transformed to standard normal probability density functions before estimation and back-transformed for the cross-validation analysis. The semivariogram analysis gave correlation lengths for <i>D</i> and <i>L</i> of approx. 10 and 6 km. These correlations reduce the estimation variance in the cross-validation analysis because more than 50 % of the data material had two or more observations within a radius of 5 km. The small-scale variance of <i>D</i>, however, was about 50 % of the total variance, which gave an accuracy of less than 60 % for most of the cross-validation cases. Despite the noisy character of the observations, the analysis demonstrated that <i>L</i> can be used as secondary information to reduce the estimation variance of <i>D</i>.
url https://www.hydrol-earth-syst-sci.net/21/4195/2017/hess-21-4195-2017.pdf
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