Numerical investigation about effects of flow sediment-storage variation on capacity modelling of morphological evolutions.

• Existing capacity models neglect the effects of flow sediment-storage variation. • Its effects on dam-break flooding and swash flows are numerically studied. • Simplification may lead to under-estimation of erosion or over-estimation of deposition, which considerably affects hydrodynamics. The capacity model based on the Exner equation has been widely used to simulate bed load sediment transport. However, most of their governing equations neglect a sediment storage term (∂ h C e / ∂ t), of which the impact on bed load transport simulation is unknown and needs to be better comprehended. This paper has split the capacity model into two sub-models: one with the sediment storage term and the other without the sediment storage term. The two sub-models are applied to simulate a series of typical bed load transport processes, such as dam-break flooding and swash flows. A comparison of their results is used to shed light on the effect of sediment storage term on flows and morphological evolutions. It is shown that for both dam-break flooding and swash flows, neglection of the inflow sediment storage may lead to under-estimation of bed erosion or over-estimation of bed deposition, which further affects the computed hydrodynamics greatly. Moreover, it is shown that including this factor can improve quantitative accuracy of sediment transport estimation. These indicate an important role of this factor and accordingly the present work provide a numerical justification for using sediment storage terms in capacity models. [ABSTRACT FROM AUTHOR]