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Optimization of a Monitoring Network for Sulfur Dioxide

E. P. J. Boer*,a, A. L. M. Dekkersb and A. Steina

a Wageningen University & Research Centre, Mathematical and Statistical Methods Group, Dreyenlaan 4, 6703 HA,Wageningen, the Netherlands
b RIVM, National Institute of Public Health and the Environment, P.O. Box 1, 3720 BA, Bilthoven, the Netherlands



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Fig. 1. Monitoring network of 74 stations in the Netherlands in 1993 coded with the annual average SO2 concentration (µg m-3).

 


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Fig. 2. Estimation locations with corresponding weights based on population density at each location in number of inhabitants per km2 (Criterion II, left). Estimation locations with weights based on residuals of locally weighted regression (Criterion III, right).
 


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Fig. 3. Plots of cross validation values (N = 74) for a range of smoothing parameters for the tricube and the McLain weight function, both isotropic as anisotropic (top). The weight functions with the optimized smoothing parameters (bottom).

 


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Fig. 4. Maps of interpolated SO2 values (N = 74) of the annual average concentration of SO2 by locally weighted regression, hf = 70. Tricube weight function (top) and McLain weight function (bottom).

 


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Fig. 5. Values of {phi}({xi}n) of a monitoring network where sequential monitoring stations are dropped from the original network of 74.

 


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Fig. 6. Monitoring networks (black squares) obtained from the network of 74 monitoring stations by the drop–add algorithm . Tricube weight function, p = 1, anisotropic, and hf = 120 (km), for the three design criteria (AC) (see the Specification of Different Design Criteria section). Same for McLain weight function, hf = 136 (km) (DF).

 





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