Abstract:
Megaripples in the combined flow environment of the nearshore are proposed to behave like dunes or large ripples in rivers, tidal estuaries, and deserts. Their profile basically is symmetric and thus significantly different from the traditional asymmetric triangular features observed in steady flows. Similarly their planform often exhibits little directionality, unlike crescentic or lunate steady flow dunes that point in the downstream direction. These characteristics are the result of complex combined flows in the nearshore, including oscillatory flows, wave skewness, and steady currents (undertow, rips and alongshore flows). Recent observations of megaripples in the nearshore suggest that they occur frequently. However, they are rarely considered in studies of flow resistance or sediment transport. In addition, megaripples are thought to be the source of hummocky cross-stratification in sedimentary sequences and are generally attributed to storm waves on inner continental shelves. However, observations show that they also exist inside the surf zone and under lower-energy conditions. A better understanding of their dynamics and thus their occurrence and characteristics would improve the understanding of nearshore wave and circulation dynamics, sediment transport, large-scale morphodynamics, and the resulting sedimentary sequences. It is hypothesized that megaripples in the nearshore are dynamically similar to steady flow features, which are observed in rivers, estuaries and deserts and have been studied in much more detail.
