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Rolf H. Reichle, Randal D. Koster, Gabriëlle J. M. De Lannoy, Barton A. Forman, Qing Liu, Sarith P. P. Mahanama, and Ally Touré

, ranging in size from 1900 km 2 to 1 400 000 km 2 , were used to assess runoff estimates [ Table 1 ; see Koster et al. (2010) and Mahanama et al. (2012) for details]. The streamflow data were naturalized to account for anthropogenic impacts, including upstream regulation, water withdrawals, and evaporation from reservoir surfaces. Note that some of the basins used by Mahanama et al. (2012) lack sufficient observations during our study period and are thus not considered here. Table 1

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