Abstract
The engineering of rivers by dams is a formative feature of human-nature systems and the interconnectivity of water, energy, and the climate. Sufficient and broad-based representations of dams in large-scale hydrological models prove essential to mapping their extensive regulation of river flow and biogeochemistry and gauging climate-linked provisions, including freshwater supply and hydropower. We present an integrated modeling framework to investigate future streamflow and hydropower generation in the Contiguous U.S. (1990–2075), leveraging an ensemble of six downscaled and bias-corrected General Circulation Models (GCMs) from the high-end SSP585 scenario of the CMIP6. To achieve this, we develop a reservoir operations and parameterization scheme for 1,384 dams in a high-resolution river network, including simulated hydropower generation for 326 dams. For the GCM ensemble mean, we simulate a widespread increase in regulated streamflow into the late-century (11% annual and 17% in winter for the dam median) with region-specific changes in summer streamflow that feature prominent declines in the Northwest (−7%). Mediation by reservoirs is shown to dampen intra-annual streamflow changes, delivering additional summer releases that partially mitigate declining flows. Total hydropower generation is projected to increase modestly (+3%), with boosted generation in the winter (+9%) and spring (+5%) offsetting declined summer generation (−3.4%), suggesting strong adaptation potential for hydropower in the future energy portfolio. Further analysis reveals that the choice of GCM, particularly in western regions, has significant bearing on projected streamflow and hydropower changes.
| Original language | English |
|---|---|
| Article number | e2025EF006203 |
| Journal | Earth's Future |
| Volume | 13 |
| Issue number | 9 |
| DOIs | |
| State | Published - Sep 2025 |
Funding
The research was supported by the U.S. Department of Energy (DOE) Grid Modernization Laboratory Consortium (GMLC). This paper was authored in part by the National Renewable Energy Laboratory under contract DE‐AC36‐08GO28308, Oak Ridge National Laboratory, managed by UT Battelle, LLC, under contract DE‐AC05‐00OR22725, and Sandia National Laboratories, managed by National Technology and Engineering Solutions of Sandia LLC (a wholly owned subsidiary of Honeywell International Inc.), under contract DE‐NA0003525, with the US DOE. Accordingly, the US government retains and the publisher, by accepting the article for publication, acknowledges that the US government retains a nonexclusive, paid‐up, irrevocable, worldwide license to publish or reproduce the published form of this manuscript or allow others to do so, for US Government purposes. This paper describes objective technical results and analysis. Any subjective views or opinions that might be expressed in the paper do not necessarily represent the views of the U.S. DOE or the U.S. Government. We also acknowledge support by the Advanced Science Research Center and department of Earth and Environmental Sciences, both at the CUNY Graduate Center. We thank D. Vignoles for valuable contributions to data analysis and simulations and S. Turner for providing insight and expertise on the simulations. Lastly, we sincerely thank the Editor, Associate Editor, and reviewers for their constructive and insightful feedback, which significantly improved the focus, presentation, and analysis of our manuscript.
Keywords
- climate change
- dams
- energy-water nexus
- hydropower
- reservoir operations
- simulation