Our comparisons use seven-year time series of output from dynamical and statistical downscaling models. Time series of current-climate precipitation and daily min/max temperature from both approaches are compared with observations and are shown to reproduce climatology better than the raw reanalysis output. As a consequence, both downscaling methods introduce gains to hydrological simulations for basins that are subgrid to the driving global model. Differences between the statistical and dynamical approaches are attributable in part to the way in which each assimilates orographic information. Further analysis shows the ranges of hydrological response that can arise from analyzing climate change impacts with different, but physically plausible, downscaling approaches.
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