the change in the basin configuration is dependent in the work of ​

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Deltas are important coastal systems throughout the world. River mouth bars are key

landforms in the development of deltas, are characterized by sediment deposition, and have a high

potential for sediment preservation. Scientists and professionals seek to understand the discrete

response of mouth bars to the various controls governing their evolution. This study utilizes the

numerical modelling software Delft3D to provide additional evidence supporting the

morphological and stratigraphic responses resulting from variations in basin configurations and

allogenic controls (fluvial discharge, tides, basin width). Mud content within the bar increased

analogous to an increase in the tidal modulation, while a decrease in the initial basin depth

reduced mud content. Initial basin slope and lateral confinement had less obvious impacts on

stratigraphy. Finally, variable fluvial discharge and the incorporation of realistic tidal harmonics

produced similar bar morphologies (compared to simulations with constant flow and sinusoidal

tides), yet demonstrated significant differences in bar stratigraphy.

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