Sediment Cascades 2010
DOI: 10.1002/9780470682876.ch2
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Mountains and Montane Channels

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Cited by 19 publications
(15 citation statements)
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References 92 publications
(110 reference statements)
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“…As a consequence, the increased erosion rates can elevate the sediment delivery from catchments [88] and lakes and reservoirs act as primary sink in the sediment cascade [89]. Increases of sedimentation rate have been observed in many European lakes over the last 100 years, in particular during 1950-1975 period and post-1975.…”
Section: Potential Effects Of Climate Change On Sediment Quality In Rmentioning
confidence: 99%
“…As a consequence, the increased erosion rates can elevate the sediment delivery from catchments [88] and lakes and reservoirs act as primary sink in the sediment cascade [89]. Increases of sedimentation rate have been observed in many European lakes over the last 100 years, in particular during 1950-1975 period and post-1975.…”
Section: Potential Effects Of Climate Change On Sediment Quality In Rmentioning
confidence: 99%
“…Additionally, the experiments showed that the importance of the minimum slope threshold by far outweighs that of the maximum distance threshold, hence we set the latter to infinity. Different thresholds have been suggested for the minimum channel gradient above which bedload transport is maintained: Church (2010) states that, if sediment size is the only criterion, no deposition occurs above a channel gradient of c. 4°, Wichmann (2006) applies a threshold of 3.5°. Here we use a threshold of 2° (Fryirs et al, 2007a, also use this threshold, but it is applied to delineate connectivity across the landscape, not specifically along the channel network) to account for discharge events of higher magnitude which are capable of moving coarse sediments from time to time.…”
Section: Slope Wash and Fluvial Bedload Transportmentioning
confidence: 99%
“…The general behavior of bed load transport and water discharge in the two streams for the 6 years of observations can be characterized by a two‐phase regime (Church, ; Warburton, ). At smaller water discharges, there is no clear dependence of bed load transport intensity ( IMP or Q b ) on water discharge ( Q ), whereas above a certain threshold water discharge Q c there is a steep increase of IMP or Q b with increasing Q (Figure and supporting information Figures S3 and S4).…”
Section: Resultsmentioning
confidence: 99%