Current understanding of the role that dunes play in controlling bar and channel-scale processes
and river morphodynamics is incomplete. We present results from a combined numerical
modeling and field monitoring study that isolates the impact of dunes on depth-averaged and
near-bed flow structure, with implications for morphodynamic ...
Current understanding of the role that dunes play in controlling bar and channel-scale processes
and river morphodynamics is incomplete. We present results from a combined numerical
modeling and field monitoring study that isolates the impact of dunes on depth-averaged and
near-bed flow structure, with implications for morphodynamic modeling. Numerical
simulations were conducted using the three-dimensional Computational Fluid Dynamics code
OpenFOAM to quantify the time-averaged flow structure within a 400 m x 100 m channel
using DEMs for which: (i) dunes and bars were present within the model; and (ii) only bar43 scale topographic features were resolved (dunes were removed). Comparison of these two
simulations shows that dunes enhance lateral flows and reduce velocities over bar tops by as
much as 30%. Dunes influence the direction of modeled sediment transport at spatial scales
larger than individual bedforms due to their effect on topographic steering of the near-bed flow
structure. We show that dunes can amplify, dampen or even reverse the deflection of sediment
down lateral bar slopes, and this is closely associated with 3D and obliquely orientated dunes.
Sediment transport patterns calculated using theory implemented in depth-averaged
morphodynamic models suggests that gravitational deflection of sediment is still controlled by
bar-scale topography, even in the presence of dunes. However, improved parameterizations of
flow and sediment transport in depth-averaged morphodynamic models are needed that account for the effects of both dune- and bar- scale morphology on near-bed flow and sediment transport.
