There is a great deal of geographic imbalance in global hydrologic data sets. Outside of the US and parts of Europe, there are many parts of the world that have only sparsely available streamflow gauge networks with only a few years' worth of data (Do et al., 2017;Fekete & Vörösmarty, 2007). Besides streamflow gauges, these regions also lack data on physiographic attributes such as geology and soil depth. Nevertheless, climate change is stressing these parts of the world, and accurate hydrologic simulations are needed for these regions just as much, or even more than for data-rich regions.Catchments across the world are often perceived as being unique from each other, requiring customized model development for each basin (Teutschbein & Seibert, 2012). As a rule of thumb, when we create process-based hydrologic models, our development effort scales roughly linearly to the modeled area, computational effort scales linearly at best, and accuracy is unrelated to the number of basins modeled. It is typically difficult to apply knowledge gained from one basin to another, as parameters or experiences do not transfer easily. As a result, although there have been calls for hydrologic studies to transcend the uniqueness