GC073-0006
Future Amazon Hydropower under Climate Change

Friday, 11 December 2020
Poster
Rafael Almeida1, Ayan Santos Fleischmann2, João P. F. Brêda2, Diego S. Cardoso3, Hector Angarita4, Walter Collischonn2, Bruce Forsberg5, Roosevelt García-Villacorta6, Stephen K Hamilton7, Phillip M. Hannam8, Rodrigo C. D. Paiva2, N. LeRoy Poff9, Suresh Sethi10, Qinru Shi11, Carla Gomes11 and Alexander Flecker1, (1)Cornell University, Department of Ecology and Evolutionary Biology, Ithaca, NY, United States, (2)Federal University of Rio Grande do Sul, Institute of Hydraulic Research, Porto Alegre, Brazil, (3)Cornell University, Dyson School of Applied Economics and Management, Ithaca, NY, United States, (4)Stockholm Environment Institute Latin America, Bogotá, Colombia, (5)National Institute of Amazonian Research, Manaus, Brazil, (6)Peruvian Center for Biodiversity and Conservation, Iquitos, Peru, (7)Michigan State University, Kellogg Biological Station & Dept. Integrative Biology, East Lansing, MI, United States, (8)Johns Hopkins University, Institute for Sustainable Energy Policy, Baltimore, MD, United States, (9)Colorado State University, Department of Biology, Fort Collins, CO, United States, (10)Cornell University, Department of Natural Resources, Ithaca, NY, United States, (11)Cornell University, Institute for Computational Sustainability, Ithaca, NY, United States
Abstract:
Current climate and hydrologic models point to significant decreases in precipitation and runoff in many parts of the Amazon River Basin by the end of this century. Implications of this climate change for future hydropower have been little explored across the basin, a global hotspot for future hydropower development. We used a continental-scale hydrologic model forced with an ensemble of general circulation models to project changes in river discharge and hydropower generation at >350 proposed dam sites throughout the Amazon. We found that discharges are projected to slightly increase in the Andean Amazon and sharply decrease in the lowland Amazon. In the lowlands, reductions in hydropower generation are disproportionately larger than reductions in discharge due to an increased frequency of discharges below the minimum usable flows. In the Andes, increased discharge will not necessarily translate into higher hydropower generation if the dams are operated as run-of-river (i.e., with minimal flow regulation). Consideration of climate change-induced alterations in hydropower generation may substantially diminish the economic feasibility of many proposed Amazon hydropower dams. Climate-resilient energy system planning will be fundamental in the Amazon and other hydropower-dependent regions where river discharge regimes will be affected by climate change.