2022
DOI: 10.1029/2021wr031490
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Effect of Macrorough Sidewalls on Flow Resistance in Steep Rough Channels

Abstract: Step-pool sequences typically form in steep mountain streams. Single step-pool units exist in steep channels with bed slopes exceeding 4% and a continuous step-pool morphology occurs in channels with bed slopes higher than 6%-7% (Church & Zimmermann, 2007;Recking et al., 2012). The flow regime in a step-pool channel is referred to as tumbling flow as the flow alternates between supercritical flow over the steps and subcritical flow in the pools (Whittaker, 1987). Thus, a large amount of flow resistance is attr… Show more

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Cited by 2 publications
(21 citation statements)
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“…The physical experiments were conducted in a tilting flume with a L tot = 9.6 m long test reach at the Laboratory of Hydraulics, Hydrology and Glaciology (VAW) at ETH Zurich. The same experimental setup was used as in Maager et al (2022), thus, only a short description is given herein focusing on additional instrumentation. The experiments were scaled according to Froude-similitude with a scale factor of 20.…”
Section: Methodsmentioning
confidence: 99%
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“…The physical experiments were conducted in a tilting flume with a L tot = 9.6 m long test reach at the Laboratory of Hydraulics, Hydrology and Glaciology (VAW) at ETH Zurich. The same experimental setup was used as in Maager et al (2022), thus, only a short description is given herein focusing on additional instrumentation. The experiments were scaled according to Froude-similitude with a scale factor of 20.…”
Section: Methodsmentioning
confidence: 99%
“…A roughness parameter is assigned to both channel bed and sidewalls, that is, the Darcy-Weisbach sidewall and bed friction factors f w and f b are estimated. For macrorough sidewalls, Maager et al (2022) developed an empirical approach to estimate the sidewall friction factor f w :…”
Section: Test Procedures and Reproducibilitymentioning
confidence: 99%
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