The non-dimensional number Y is found representing the ability of the plume system to deliver sediments to the alongshore coastal current.
A critical range of settling velocities exist above which no transport in the costal current is allowed.
Low magnitude and long-lasting floods promote sediment sorting in the continental shelf.
Intermediate flood magnitudes at the limit between subcritical and supercritical flow maximize the alongshore sediment transport.
Intermediate discharge durations maximize the alongshore sediment transport.