Z
Zuosheng Yang
Researcher at Ocean University of China
Publications - 111
Citations - 8104
Zuosheng Yang is an academic researcher from Ocean University of China. The author has contributed to research in topics: Sediment & River mouth. The author has an hindex of 39, co-authored 103 publications receiving 6737 citations. Previous affiliations of Zuosheng Yang include Chinese Ministry of Education.
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Flux and fate of Yangtze River sediment delivered to the East China Sea
TL;DR: In this paper, high-resolution seismic profiling and coring in the southern East China Sea during 2003 and 2004 cruises has revealed an elongated (similar to 800 km) distal subaqueous mud wedge extending from the Yangtze River mouth southward off the Zhejiang and Fujian coasts into the Taiwan Strait.
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Stepwise decreases of the Huanghe (Yellow River) sediment load (1950–2005): Impacts of climate change and human activities
TL;DR: The sediment load delivered from the Huanghe (Yellow River) to the sea has decreased sharply to 0.15×10 9 metric tons per year (0.15 Gt/yr) between 2000 and 2005, and now represents only 14% of the widely cited estimate of 1.08 Gt per year as discussed by the authors.
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Dam impacts on the Changjiang (Yangtze) River sediment discharge to the sea: The past 55 years and after the Three Gorges Dam
TL;DR: In this article, the authors show that the sediment budget and sediment erosion data for the Changjiang subaqueous delta will be eroded extensively during the first five decades after the Three Gorges Dam (TGD) operation and then will approach a balance during the next five decades as sediment discharging from TGD again increases.
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Interannual and seasonal variation of the Huanghe (Yellow River) water discharge over the past 50 years: Connections to impacts from ENSO events and dams
TL;DR: In this article, the authors investigated the connection between decreasing water discharges, global El Nino/Southern Oscillation (ENSO) events and anthropogenic impacts in the drainage basin of the Huanghe River in China.
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Sedimentary features of the Yangtze River-derived along-shelf clinoform deposit in the East China Sea
TL;DR: A predominant sigmoidal clinoform deposit extends from the Yangtze River mouth southwards 800 kin along the Chinese coast, reaching water depths of 60 and 90 m and distances up to 100 km offshore as mentioned in this paper.