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Residual uncertainty estimation using instance based learning with applications to hydrologic forecasting

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Figure

Figure 1. Dependence of error samples on the value of k. For largervalues of k, points are at a greater distance from vt (the predic-tion step), thus compromising the conditioning of the residual errorprobability distribution on vt (Eq
Figure 2. Upper Severn subcatchments with gauging stations (fromLópez López et al., 2014).
Table 1. Basin information for Upper Severn subcatchments (EA,2013; Marsh and Hannaford, 2008).
Table 2. Alpha Index (α) for high flows corresponding to differentlead times of Upper Severn subcatchments.
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