Abstract
A model for predicting the formation, disappearance and recovery of a river mouth terrace was developed based on the contour-line-change model considering grain size changes. The topographic changes and grain size changes associated with the flushing process of a flood were first investigated, taking the mouth of the Abe River as the example. Predicted change in the river mouth terrace and grain size changes around the river mouth were in good agreement with the measured, showing the effectiveness of the numerical model.
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