1989
DOI: 10.1016/0004-6981(89)90110-8
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Kriging and other estimators of spatial field characteristics (with special reference to environmental studies)

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Cited by 40 publications
(13 citation statements)
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“…However, the assumption of stationarity (i.e. that the same pattern of variation can be observed at all locations on the surface) is rarely met in reality (Fedorov 1989). To test this assumption, the mean and variance of the residuals in blocks of approximately 600 km (roughly equivalent to the range of the variogram plots) were considered.…”
Section: Model Limitations and Future Researchmentioning
confidence: 99%
“…However, the assumption of stationarity (i.e. that the same pattern of variation can be observed at all locations on the surface) is rarely met in reality (Fedorov 1989). To test this assumption, the mean and variance of the residuals in blocks of approximately 600 km (roughly equivalent to the range of the variogram plots) were considered.…”
Section: Model Limitations and Future Researchmentioning
confidence: 99%
“…In view of the variety of information sources as given by observations, with all their heterogeneity in terms of accuracy, spatial representativeness, spatial observation density and temporal frequency, and various retrieval techniques on the one hand, and model results on the other hand, advanced data assimilation and inverse modelling techniques provide the appropriate data fusion and analysis technique. Early attempts to analyse tracer fields were based on monovariate kriging techniques in the troposphere (e.g., Fedorov, 1998), and other purely spatial methods in the stratosphere (e.g., Stajner et al, 2001;Struthers et al, 2002). These methods produce chemical state estimates, frequently referred to as analyses, after assimilation of observations in model simulated fields as background.…”
Section: Introductionmentioning
confidence: 99%
“…At a smaller scale, along each profile, it is not possible either to highlight a clear pattern within the dataset. To avoid such erroneous data description (e.g., Fedorov, 1989) it is preferred to attempt another approach. Both CO 2 and 222 Rn data are taken separately and automatically ranged under 10 different concentration classes.…”
Section: Discussionmentioning
confidence: 99%