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The Yangtze Estuary in China has been intensively influenced by human activities including altered river and sediment discharges in its catchment and local engineering projects in the estuary over the past half century. River sediment discharge has significantly decreased since the 1980s because of upstream dam construction and water-soil conservation. We analyzed bathymetric data from the Yangtze...
Progradation rates of tidal flats at the Chiangjiang River mouth, China, over different periods were examined, based on surveys and historical records. Rapid progradation after the Holocene sea-level rise began about 2000 years ago because of an increase in riverine sediment. The tidal flats at the river mouth have grown at a rate of about 5 km 2 /year and the southern mainland shoreline in...
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