LES simulations reproduce laboratory plunging flows in bedrock-river constriction-pool-widening morphologies and indicate discharge-dependent optimal constrictions (~35% at low flow, ~50% at high flow) for velocity inversion, with peak shear stress at 35%.
Kinematics, topology and significance of dune-related macroturbulence:
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Large Eddy Simulation of Plunging Flows in Laboratory-Scale Bedrock Rivers
LES simulations reproduce laboratory plunging flows in bedrock-river constriction-pool-widening morphologies and indicate discharge-dependent optimal constrictions (~35% at low flow, ~50% at high flow) for velocity inversion, with peak shear stress at 35%.