On the ambiguous interpretation of the Turc‐Budyko nondimensional graph

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Estimation of the distribution of annual runoff from climatic variables using copulas (2014, methodology): “=P) to the aridity index (P=E 0) [Andr eassian and Perrin, 2012] is first plotted in Figure 2 to assess the capability of the Budyko formula.”
HESS Opinions : The complementary merits of competing modelling philosophies in hydrology (2017, background): “…runoff coefficients on a range of scales (e.g. annual, seasonal and event-based), which define the partitioning between streamflow and evaporative fluxes (e.g. Budyko, 1974; Donohue et al., 2007; Sivapalan et al., 2011) plus potential deep infiltration losses (e.g. Andréassian and Perrin, 2012).”