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Akhil Sanjay Potdar, Pierre-Emmanuel Kirstetter, Devon Woods, and Manabendra Saharia

’s representativeness and its predictive power in ungauged basins. Figure 2a shows a scatterplot comparing the predicted and observed peak discharge values that display data pairs grouped along the 1:1 line. A corresponding density-colored scatterplot of the simulated versus observed unit peak discharges ( Fig. 2b ) can be qualitatively compared with Fig. 2a in Gourley et al. (2017) and suggests superior performance in predicting peak flows as compared with the CREST water balance module with kinematic wave

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