… In Section 3, we discuss the dynamics of sediment transport. Section 4 is devoted to the
linear stability analysis of a flat bed and some nonlinear developments. Finally, finite-size effects …

… By assuming a realistic lag based on the mechanics of bed load transport, a fastest growing
wave at ripple-scales results: similarly, if suspended sediment were included, longer lags …

… dune and ripple formation and for a clarification of the debated role of ripples on the formation
of dunes. … flow and sediment transport rates than do ripples; however, ripples often form on …

… When the tractive force is increased to the point where sediment transport starts, the bed
will be unstable. In the case of fine sediment, ripples are formed, while coarse sediments …

… the bed at small excess bed shear stress; whereas dunes interact with the total flow. In small
… of dunes, postulated that in a flow—which is saturated to carrying capacity with sediment—…

… Oscillating fluid motions accompanying waves and tides also generate sedimentary
ripples and dunes. The ripples formed by translational waves (8, 9) are especially noteworthy …

… We identify two types of bedforms consistent with subaqueous ripples and dunes, and …
of sediment transport we provide a new unifying framework to compare ripples and dunes in …

… Primary ripples are then … ripples become unstable and form secondary ripples with a larger
form drag. Liu (1 957) proposes that the sediment bed acts as a viscous fluid and that ripples …

… 5a–b), where bedform orientation is controlled by orientation of a sediment source (source-bordering
dunes), where a flow changes to a new direction (either through time or with …

… sediment-bed interactions comprises the basis for developing better methods for computing
effective roughnesses of channels in which ripples or dunes … of sediment transport on rippled …