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Salinity and Turbidity Gradients Driven Spatial Heterogeneity of Phytoplankton Community in the Eutrophic Macrotidal Qiantang River‐Estuary‐Coastal Sea Continuum

Journal of Geophysical Research G: Biogeosciences
Abstract The river‐estuary‐coastal sea continuum is usually characterized by drastic tidal fluctuations and significant spatial gradients in salinity, turbidity, and nutrients. However, the response of the phytoplankton community in the continuum to such physicochemical variations remains poorly understood. Here, three cruises in dry,
Zhibing Jiang, Zhi Yang
exaly   +3 more sources

Morphodynamics of the Qiantang Estuary, China: Controls of river flood events and tidal bores

open access: yesMarine Geology, 2018
Abstract The importance of seasonal variations in river discharge on the morphological development of estuaries has been recognized in recent years, yet in situ observations about such variations are rare. Here we report a long-term dataset of bathymetry in the middle reach of the Qiantang Estuary, China, characterized by the presence of a large ...
Shu Gao, Dongfeng Xie, Zheng Bing Wang
exaly   +6 more sources

Source‐to‐sink analysis for the mud and sand in the late‐Quaternary Qiantang River incised‐valley fill and its implications for delta‐shelf–estuary dispersal systems globally

Sedimentology, 2021
AbstractThe Changjiang (i.e. the Yangtze River) debouches a huge amount of sediment to the East China Sea and exerts a significant effect on the evolution of the down‐drift Qiantang River system. This study quantitatively documents the temporal change in the import of Changjiang sand and mud to the late Quaternary Qiantang River incised valley by ...
Xia Zhang   +3 more
openaire   +2 more sources

Impact of human activity on the estuary of the Qiantang River and the reclamation of tidal flats and river regulation

Environmental Geology, 2005
The swing of the main channel of the Qiantang River is controlled by the high-water and low-water changes in the river, as well as the impact of large-scale reclamation of tidal flats. Its evolution in modern times is the result of the combined functions of natural and man-made factors.
Li-Hua Feng
exaly   +2 more sources

Mechanism in Turbulence and High‐Frequency Oscillation Due To Wave‐Current Interactions in Qiantang River Estuary, Hangzhou Bay, China

Journal of Geophysical Research: Oceans
Abstract The world‐renowned tidal bore forms in the Qiantang River Estuary (QRE) and leads to distinctive hydro‐sediment dynamics and the reshaping of coastal geomorphology. This study presents a time series of in situ data of wave, current, and suspended sediment concentration (SSC) in the tidal bore, covering the spring‐neap tidal ...
Li Li   +8 more
openaire   +2 more sources

Salinity Time Series Prediction and Forecasting Using Dynamic Neural Networks in the Qiantang River Estuary

Advanced Science Letters, 2012
The early warning of saltwater intrusion is an important work for ensuring the drinking water supplies. To forecast and predict the daily maximum salinity for the water withdrawn for the waterworks located along the Qiantang River, the nonlinear autoregressive networks with exogenous inputs (NARX) model was applied.
Xingguo Yang   +2 more
openaire   +2 more sources

Facies architecture and depositional model of a macrotidal incised-valley succession (Qiantang River estuary, eastern China), and differences from other macrotidal systems

Geological Society of America Bulletin, 2014
Filling of the modern coastal-zone portion of the Qiantang River (QR) in eastern China was initiated by marine inundation during the transgression after the Last Glacial Maximum and has continued during the Holocene sea-level stillstand. The early part of the fill is transgressive in character, while the younger part is regressive.
X. Zhang   +4 more
openaire   +2 more sources

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