Details

Autor(en) / Beteiligte

• Mei, Xuefei
• Dai, Zhijun
• Wei, Wen
• Li, Weihua
• Wang, Jie
• Sheng, Hao

Titel

Secular bathymetric variations of the North Channel in the Changjiang (Yangtze) Estuary, China, 1880–2013: Causes and effects

Ist Teil von

• Geomorphology (Amsterdam, Netherlands), 2018-02, Vol.303, p.30-40

Ort / Verlag

Elsevier B.V

Erscheinungsjahr

2018

Quelle

Elsevier ScienceDirect Journals

Beschreibungen/Notizen

• As the interface between the fluvial upland system and the open coast, global estuaries are facing serious challenges owing to various anthropogenic activities, especially to the Changjiang Estuary. Since the establishment of the Three Gorges Dam (TGD), currently the world's largest hydraulic structure, and certain other local hydraulic engineering structures, the Changjiang Estuary has experienced severe bathymetric variations. It is urgent to analyze the estuarine morphological response to the basin-wide disturbance to enable a better management of estuarine environments. North Channel (NC), the largest anabranched estuary in the Changjiang Estuary, is the focus of this study. Based on the analysis of bathymetric data between 1880 and 2013 and related hydrological data, we developed the first study on the centennial bathymetric variations of the NC. It is found that the bathymetric changes of NC include two main modes, with the first mode representing 64% of the NC variability, which indicates observable deposition in the mouth bar and its outer side area (lower reach); the second mode representing 11% of the NC variability, which further demonstrates channel deepening along the inner side of the mouth bar (upper reach) during 1970–2013. Further, recent erosion observed along the inner side of the mouth bar is caused by riverine sediment decrease, especially in relation to TGD induced sediment trapping since 2003, while the deposition along the lower reach since 2003 can be explained by the landward sediment transport because of flood-tide force strengthen under the joint action of TGD induced seasonal flood discharge decrease and land reclamation induced lower reach narrowing. Generally, the upper and lower NC reach are respectively dominated by fluvial and tidal discharge, however, episodic extreme floods can completely alter the channel morphology by smoothing the entire channel. The results presented herein for the NC enrich our understanding of bathymetric variations of the Changjiang Estuary in response to human activities, which can be well applied to other estuaries subject to similar interferences. [Display omitted] •NC is characterized by erosion in upper reach and deposition along the lower reach.•Extreme floods dominate the episodic disequilibrium of NC evolution.•Riverine and landward sediment availability control the NC morphology.•Sediment trapping and water storage of TGD trigger the recent NC volume variation.