Authors
Muriel Z M Brückner, Andrew P Nicholas, Rolf Aalto, Philip J Ashworth, Jim Best, Thomas Dunne, Renato Paes de Almeida
Published in
Science advances. Volume 12. Issue 35. Pages eaec8647. Aug 28, 2026. Epub Aug 28, 2026.
Abstract
Ongoing and planned hydroelectric dam construction in the Andes will alter water and sediment delivery to downstream rivers, with likely substantial impacts on river and floodplain morphology, hydrology, and habitats. These disturbances will be greatest along laterally dynamic rivers with strong current channel-floodplain coupling, such as Andean foreland rivers. Using a hydro-morphodynamic river model, we show that these floodplains are rapidly transformed through widespread vertical and lateral erosion with persisting long-term effects: Erosion creates secondary floodplains entrenched several meters below pre-dam levels within a century. This degradation of the channel-floodplain complex changes floodplain inundation patterns and frequency and disconnects riparian water bodies from the active river. Such decoupling will be most severe in rivers characterized by high sediment loads and lateral migration rates before dam construction. Our simulations reveal that predictive approaches that neglect geomorphic changes, including lateral river mobility, may be of limited utility in assessing dam impacts on the construction and functioning of wetland habitats.
PMID:
42664333
Bibliographic data and abstract were imported from PubMed on 29 Aug 2026.
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