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Published online 8 March 2006
Published in Vadose Zone J 5:168-183 (2006)
DOI: 10.2136/vzj2005.0015
© 2006 Soil Science Society of America
677 S. Segoe Rd., Madison, WI 53711 USA
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SPECIAL SECTION: FROM FIELD- TO LANDSCAPE-SCALE VADOSE ZONE PROCESSES

Spatial Analysis of Model Error, Illustrated by Soil Carbon Dioxide Emissions

M. J. Pringle* and R. M. Lark

Rothamsted Research, Harpenden, Hertfordshire, AL5 2JQ, UK
* Corresponding author (matthew.pringle{at}bbsrc.ac.uk)

Received 31 January 2005.

A spatial analysis of model error is required when the observations and model predictions are made at locations in space. This is because: (i) a model may reproduce observed variations better at some spatial scales than others, (ii) the model may be more or less successful at reproducing the relative variability of a process at different spatial scales, and (iii) the spatial pattern of model error may contain information about its possible sources. A geostatistical analysis can address these issues. We developed a model of carbon dioxide (CO2) emissions from soil. The soil (Dystric and Typic Eutrudepts) was sampled on a 1024-m transect at Silsoe, UK. Observed CO2 emissions were compared with model predictions at 156 random locations on the transect. A spatial analysis of the model's error, using a (cross-validated) linear model of coregionalization, revealed details not apparent with a nonspatial analysis. The model could not predict high-frequency fluctuations in CO2 emissions, but could accurately predict lower-frequency fluctuations. Factorial cokriging analysis allowed us to estimate and visualize the low-frequency components. We interpolated model error to unsampled locations, and found bias on soil with relatively large clay contents. Volumetric water content had a weak scale-dependent correlation with model error. We propose the inter-block correlation to quantify the effect of a change of support on the correlation of observations and model predictions; the best pixel size for the prediction of soil CO2 emissions on the transect was 10 to 20 m.

Abbreviations: AIC, Akaike Information Criterion • LMCR, linear model of coregionalization • MAPD, median absolute pair difference • ME, mean error • MVE, minimum-volume ellipsoid • RMSE, root-mean-square-error




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