Behavior of a Sand Ridge Model
نویسنده
چکیده
A model for the formation and evolution of longshore sand ridges in waters deeper than the shoaling region suggests that a possible but by no means exclusive agent for the formation of these bars are weakly nonlinear dispersive long waves. The model describes how these water waves, which are represented by wave packets, and a sandy bottom topography, conspire to produce sand ridges. This study examines the behavior of the model, and investigates how speciic morphological features of the sand ridges depend on the water waves' characteristics.
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