Geography Reference
In-Depth Information
Index
Geostatistics
Regression
Process based
0.0
0.1
0.2
0.3
0.4
0.5
0.4 0.6 0.8 1.0
E PA / P A (-)
2.0
0.4 0.6 0.8 1.0
E PA / P A (-)
2.0
0.4 0.6 0.8 1.0
E PA / P A (-)
2.0
0.4 0.6 0.8 1.0
E PA / P A (-)
2.0
0.0
0.1
0.2
0.3
0.4
0.5
368 0 2
T A (
368 0 2
T A (
368 0 2
T A (
368 0 2
T A (
C)
C)
C)
C)
0.0
0.1
0.2
0.3
0.4
0.5
3
Elevation (10 2 m a.s.l.)
6
9
12
15
3
Elevation (10 2 m a.s.l.)
6
9
12
15
3
Elevation (10 2 m a.s.l.)
6
9
12
15
3
Elevation (10 2 m a.s.l.)
69 2 5
0.0
0.1
0.2
0.3
0.4
0.5
0.05
0.1 0.5
Area (10 3 km 2 )
1
5
0.05 0.1 0.5
Area (10 3 km 2 )
1
5
0.05 0.1 0.5
Area (10 3 km 2 )
1
5
0.05 0.1 0.5
Area (10 3 km 2 )
15
Figure 7.22. Absolute normalised error (ANE) of predicting the slopes of the FDCs in ungauged basins as a function of aridity (E PA /P A ),
mean annual air temperature T A , mean elevation and catchment area for different parameter regionalisation methods. Lines connect median
efficiencies for the same study. Boxes are 40% - 60% quantiles, whiskers are 20% - 80% quantiles.
 
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