Abstract

Lakes and reservoirs affect the timing and magnitude of streamflow, and are therefore essential hydrological model components, especially in the context of global flood forecasting. However, the parameterization of lake and reservoir routines on a global scale is subject to considerable uncertainty due to lack of information on lake hydrographic characteristics and reservoir operating rules. In this study we estimated the effect of lakes and reservoirs on global daily streamflow simulations of a spatially-distributed LISFLOOD hydrological model. We applied state-of-the-art global sensitivity and uncertainty analyses for selected catchments to examine the effect of uncertain lake and reservoir parameterization on model performance. Streamflow observations from 390 catchments around the globe and multiple performance measures were used to assess model performance.Results indicate a considerable geographical variability in the lake and reservoir effects on the streamflow simulation. Nash-Sutcliffe Efficiency (NSE) and Kling-Gupta Efficiency (KGE) metrics improved for 65% and 38% of catchments respectively, with median skill score values of 0.16 and 0.2 while scores deteriorated for 28% and 52% of the catchments, with median values −0.09 and −0.16, respectively. The effect of reservoirs on extreme high flows was substantial and widespread in the global domain, while the effect of lakes was spatially limited to a few catchments. As indicated by global sensitivity analysis, parameter uncertainty substantially affected uncertainty of model performance. Reservoir parameters often contributed to this uncertainty, although the effect varied widely among catchments. The effect of reservoir parameters on model performance diminished with distance downstream of reservoirs in favor of other parameters, notably groundwater-related parameters and channel Manning’s roughness coefficient. This study underscores the importance of accounting for lakes and, especially, reservoirs and using appropriate parameterization in large-scale hydrological simulations.

Highlights

  • Lakes and man-made reservoirs are key components of terrestrial hydrological systems

  • In this study we focus on estimating lake and reservoir effects on fully spatially distributed, daily streamflow simulations suited for global flood forecasting

  • We estimated the effect of lake and reservoir and their parameterization on daily river streamflow simulations of a global spatially-distributed hydrological model

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Summary

Introduction

Lakes and man-made reservoirs are key components of terrestrial hydrological systems. They affect flow regimes by changing the magnitude and timing of streamflow, usually by attenuating and delaying flows, and through releases from reservoirs which can result in severe downstream floods. Some of the currently used global and continental scale hydrological models (GHMs; Bierkens, 2015; Bierkens et al, 2015; Döll et al, 2003; Coe, 2000; Meigh et al, 1999) that explicitly represent lakes and reservoirs, were used to assess the impacts of lakes and/or reservoirs on global- or regional-scale streamflow simulations

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