The variation of flow and sediment condition in the Yellow River estuary since 1986 resulted in the atrophy of tail channels, the decrease of ability to convey flow, and more austere of flood prevention.

Response relationship between the bank-full discharge in tail channel and the process of flow-sediment in the Yellow River estuary

Cause analysis of river channel shrinkage at lower reaches of the Yellow River;

Adjustment of sediment transport capacity during channel shrinkage for lower Yellow River;

Discussion on channel shrinkage and its instability of the Lower Yellow River;

Influences of water and sand regulation on Yellow River estuary reach monitored by remote sensing;