Rate and timing of sedimentation were examined at the altered Nakdong Estuary of Korea.
Altimeter observed episodic sedimentation of 6 cm during summer discharge in the main channel.
Sediment flux gradient was the main mechanism for the deposition during high discharge.
Gradual deposition of 4 cm also corresponds to the long-term rate in the west Nakdong.
Wave-enhanced sediment flux was the primary mechanism for gradual deposition.