Shifted sediment-transport regimes by climate change and amplified hydrological variability in cryosphere-fed rivers

Science Advances
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Abstract

Climate change affects cryosphere-fed rivers and alters seasonal sediment dynamics, affecting cyclical fluvial material supply and year-round water-food-energy provisions to downstream communities. Here, we demonstrate seasonal sediment-transport regime shifts from the 1960s to 2000s in four cryosphere-fed rivers characterized by glacial, nival, pluvial, and mixed regimes, respectively. Spring sees a shift toward pluvial-dominated sediment transport due to less snowmelt and more erosive rainfall. Summer is characterized by intensified glacier meltwater pulses and pluvial events that exceptionally increase sediment fluxes. Our study highlights that the increases in hydroclimatic extremes and cryosphere degradation lead to amplified variability in fluvial fluxes and higher summer sediment peaks, which can threaten downstream river infrastructure safety and ecosystems and worsen glacial/pluvial floods. We further offer a monthly-scale sediment-availability-transport model that can reproduce such regime shifts and thus help facilitate sustainable reservoir operation and river management in wider cryospheric regions under future climate and hydrological change.

Publication type Article
Publication Subtype Journal Article
Title Shifted sediment-transport regimes by climate change and amplified hydrological variability in cryosphere-fed rivers
Series title Science Advances
DOI 10.1126/sciadv.adi5019
Volume 9
Issue 45
Year Published 2023
Language English
Publisher American Association for the Advancement of Science
Contributing office(s) Pacific Coastal and Marine Science Center
Description eadi5019, 12 p.
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