Estuaries are regions where rivers flow into the coastal ocean. The physical functioning of estuaries varies greatly and depends on the estuary size, shape, sedimentary characteristics, and external physical forcing by the river, tides, waves, and wind (Wolanski & Elliot, 2016). The net result of these features is the overall water circulation pattern. Sediments are important in estuaries because sediment flux gradients contribute to the depth and texture of the bed and the overall turbidity of the water column which in turn affects estuarine fisheries and navigability. At present, sediment fluxes are changing in estuaries, as humans have modified the shape of estuaries worldwide through activities such as land reclamation, dredging, and the construction of hard engineering structures (Jung et al., 2021;Wang et al., 2015). Land reclamation and dredging are often carried out to create land area and improve navigability, respectively (Winterwerp & Wang, 2013), while hard engineering structures such as breakwaters, riprap, jetties, and seawalls have been designed to absorb wave energy and stabilize the coast (Davis &