ABSTRACT To analyze sediment dynamics in estuaries during floods, a method capable of three-dimensional flows for high-resolution calculations is essential. However, such calculations are computationally intensive for midium to long term periods. We developed a high-speed calculation method for temporal variations in river bed topography and sediment discharge from river basins based on the average component acceleration (ACA) method by shortening the duration of floods. In the ACA method, the local components remained unchanged, and the temporal variation in the average components was amplified. This study developed the ACA method to calculate sediment transport, including bedload and suspended load, around an estuary. The ACA method enabled five times faster than the analysis of riverbed variations and the amount of sediment discharge compared to the conventiola non-accelerated analysis. It also accurately captured the widening of the estuarine sandbar opening during a flood demonstrating its utility for medium- to long-term riverbed-change analysisand its advantage over the other acceleration methods.
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