| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 864870 | Procedia IUTAM | 2015 | 8 Pages |
Abstract
Results are presented from two-dimensional direct numerical simulations of sediment wave formation via a succession of erosional and depositional turbidity currents. For currents propagating down a slope, we observe the formation of upstream migrating periodic sediment waves. The strength of the wave formation process is discussed as function of the governing dimensionless parameters.
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