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• W2912797308 abstract "Abstract Regional climate is an important control on the rate of coarse sediment mobilization and transport in alpine river systems. Changes in climate are then expected to cause a cascade of geomorphic responses, including adjustments in downstream channel morphology. However, the mechanics and sensitivity of channel response to short‐term climate variability remain poorly documented. In the Nooksack River, which drains a glaciated stratovolcano in Washington State, bed elevation changes were inferred from shifting stage‐discharge relations at seven U.S Geological Survey stream gages. Decadal‐scale elevation trends can be explained as a downstream‐propagating channel response to regional climate variability, where periods of persistent warm, dry (cool and wet) conditions corresponded to periods of aggradation (incision). The channel elevation response propagated downstream at a rate of 1 to 4 km per year; propagation rate scaled closely with channel slope. Historical trends in glacier extent and flood intensity both show some potential to explain climate‐sediment linkages, though assessing causation is complicated by the shared climate signal in both records. Results show the influence of the Pacific Decadal Oscillation, with relatively high coarse sediment yields prior to 1950 and since 1980, and notably lower sediment yields from 1950 to 1980. Measured sediment yields from nearby glaciated basins corroborate this history, suggesting a regional consistency to these climate‐sediment linkages. These results document consistent relations between climate, sediment supply, and downstream channel response at the basin scale, with channel responses propagating downstream over periods of decades with little apparent attenuation." @default.
• W2912797308 created "2019-02-21" @default.
• W2912797308 creator A5020905593 @default.
• W2912797308 creator A5088691532 @default.
• W2912797308 date "2019-04-01" @default.
• W2912797308 modified "2023-10-10" @default.
• W2912797308 title "Downstream‐Propagating Channel Responses to Decadal‐Scale Climate Variability in a Glaciated River Basin" @default.
• W2912797308 cites W1456697659 @default.
• W2912797308 cites W1502631916 @default.
• W2912797308 cites W1534672138 @default.
• W2912797308 cites W1573090864 @default.
• W2912797308 cites W1573107272 @default.
• W2912797308 cites W1573723661 @default.
• W2912797308 cites W1774723856 @default.
• W2912797308 cites W1924166902 @default.
• W2912797308 cites W1929725744 @default.
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• W2912797308 cites W2013250053 @default.
• W2912797308 cites W2014930733 @default.
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• W2912797308 doi "https://doi.org/10.1029/2018jf004734" @default.
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