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several locations (e.g., Papalexiou and Koutsoyiannis 2013 ; Blanchet et al. 2016 ). If historical rainfall records are available at multiple sites, regional IDF curves are often generated by (i) spatially interpolating i ( T R , τ ) or parameters of the statistical distributions from local or at-site estimations, or (ii) applying regionalization techniques that merge rain gauges into homogeneous regions to increase robustness in the estimate of the statistical distribution parameters ( Hosking
several locations (e.g., Papalexiou and Koutsoyiannis 2013 ; Blanchet et al. 2016 ). If historical rainfall records are available at multiple sites, regional IDF curves are often generated by (i) spatially interpolating i ( T R , τ ) or parameters of the statistical distributions from local or at-site estimations, or (ii) applying regionalization techniques that merge rain gauges into homogeneous regions to increase robustness in the estimate of the statistical distribution parameters ( Hosking
