Sediment export, transient landscape response and catchment-scale connectivity following rapid climate warming and Alpine glacier recession
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文摘
Presents one of the few multi-decadal records of coarse (sand and gravel) export from a glaciated river basin. Increasing sediment transport capacity does not explain interannual variability in sediment export. This implies sediment supply is crucial. Connectivity develops in a glaciated basin in response to glacier recession. Fluvial reworking of glacial till may reduce sediment transport rates and so reduce sediment connectivity.

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