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Supporting Information

Supporting Information can be found in the online version of this article:

Figure S1. Prior T1 field (A) and the absolute adjustments of this field resulting from calibration runs 2A (B), 2B (C), 3A (D), and 3B (E). The classification of the adjustment follows the method of “Natural Breaks” (Jenks), performed on the adjustments in the B run of the corresponding calibration set (consisting of an A and a B run).

Figure S2. Prior T3 field (A) and the absolute adjustments of this field resulting from calibration runs 2A (B), 2B (C), 3A (D), and 3B (E). The classification of the adjustment follows the method of “Natural Breaks” (Jenks), performed on the adjustments in the B run of the corresponding calibration set (consisting of an A and a B run).

Figure S3. Prior conductances of the surface water system (A), and the subdivision of the surface water system in classes “canals” and “other,” both having their own statistical properties.

Table S1. Adjustments of the (untransformed) conductances of the surface water system (with respect to the prior field). Please note: Wiley-Blackwell are not responsible for the content or functionality of any supporting materials supplied by the authors. Any queries (other than missing material) should be directed to the corresponding author for the article.

FilenameFormatSizeDescription
GWAT_607_sm_supmat.pdf620KSupporting info item

Please note: Wiley Blackwell is not responsible for the content or functionality of any supporting information supplied by the authors. Any queries (other than missing content) should be directed to the corresponding author for the article.