Asking the pikas politely…
The frequency of flows mobilizing river bank sediment along a majority of the Gunnison River in the BCNP has significantly declined since 1966, and decreases in the frequency of significant sediment-mobilizing flows were more pronounced for regions within the BC NP where the channel gradient is lower.
Knowledge graph centered on Assessment of Coarse Sediment Mobility in the Blac with 4 nodes and 3 connections. Top connected: ALTERED STREAMFLOW AND SEDIMENT ENTRAINMENT IN THE, Ellen Wohl, Ian M. Dubinski.
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