Hydrological and sediment-transport characteristics of the middle and lower Yangtze River: Analysis from a magnitude-frequency perspective

[1]  M. T. Todisco,et al.  Detecting the Drivers of Suspended Sediment Transport in an Intermittent River: An Event-Based Analysis , 2023, SSRN Electronic Journal.

[2]  G. Villarini,et al.  Modeling riverine flood seasonality with mixtures of circular probability density functions , 2022, Journal of Hydrology.

[3]  J. Xia,et al.  Contributions of different sources to sediment transport in the Middle Yangtze River under intensive channel degradation , 2022, CATENA.

[4]  R. Rebelo,et al.  The probability distribution of daily streamflow in perennial rivers of Angola , 2021 .

[5]  Yitian Li,et al.  Response of the gravel–sand transition in the Yangtze River to hydrological and sediment regime changes after upstream damming , 2021, Earth Surface Processes and Landforms.

[6]  Y. Jia,et al.  Effects of air quality and vegetation on algal bloom early warning systems in large lakes in the middle-lower Yangtze River basin. , 2021, Environmental pollution.

[7]  S. Kanae,et al.  Response of vegetation to submergence along Jingjiang Reach of the Yangtze River , 2021, PloS one.

[8]  Wei Zhang,et al.  Spatiotemporal variations in characteristic discharge in the Yangtze River downstream of the Three Gorges Dam. , 2021, The Science of the total environment.

[9]  S. L. Yang,et al.  Declining Sediment Discharge in the Yangtze River From 1956 to 2017: Spatial and Temporal Changes and Their Causes , 2021, Water Resources Research.

[10]  R. Bharti,et al.  Role of effective discharge on morphological changes for a regulated macrochannel river system , 2021, Geomorphology.

[11]  B. Melville,et al.  Hydrodynamics, Sediment Transport and Morphological Features at the Confluence Between the Yangtze River and the Poyang Lake , 2021, Water Resources Research.

[12]  Y. Lyu,et al.  Hydrodynamic and geomorphic adjustments of channel bars in the Yichang-Chenglingji Reach of the Middle Yangtze River in response to the Three Gorges Dam operation , 2020 .

[13]  M. Franca,et al.  Floodplain Land Cover and Flow Hydrodynamic Control of Overbank Sedimentation in Compound Channel Flows , 2019, Water Resources Research.

[14]  G. Parker,et al.  Can Bankfull Discharge and Bankfull Channel Characteristics of an Alluvial Meandering River be Cospecified From a Flow Duration Curve? , 2019, Journal of Geophysical Research: Earth Surface.

[15]  W. Uijttewaal,et al.  Impact of flow variability and sediment characteristics on channel width evolution in laboratory streams , 2018 .

[16]  Yitian Li,et al.  Distribution of erosion intensity in the Jingjiang reach influenced by the Three Gorges Dam , 2018, Earth Surface Processes and Landforms.

[17]  M. T. Todisco,et al.  Identifying a reliable method for estimating suspended sediment load in a temporary river system , 2018 .

[18]  Zhaohua Sun,et al.  Combined effects of multiple large-scale hydraulic engineering on water stages in the middle Yangtze River , 2017 .

[19]  E. Viparelli,et al.  The equilibrium alluvial river under variable flow and its channel‐forming discharge , 2017 .

[20]  C. Xie,et al.  Impacts of Land-Use Changes on the Lakes across the Yangtze Floodplain in China. , 2017, Environmental science & technology.

[21]  Baiyinbaoligao,et al.  Maintaining the connected river-lake relationship in the middle Yangtze River reaches after completion of the Three Gorges Project , 2017 .

[22]  D. Jerolmack,et al.  Self-organization of river channels as a critical filter on climate signals , 2016, Science.

[23]  J. C. Restrepo,et al.  Suspended sediment transport in the Magdalena River (Colombia, South America): Hydrologic regime, rating parameters and effective discharge variability , 2016 .

[24]  S. L. Yang,et al.  Decline of Yangtze River water and sediment discharge: Impact from natural and anthropogenic changes , 2015, Scientific Reports.

[25]  J. Warrick Trend analyses with river sediment rating curves , 2015 .

[26]  R. Sinha,et al.  Effective discharge for suspended sediment transport of the Ganga River and its geomorphic implication , 2014 .

[27]  S. Abt,et al.  Effective discharge in Rocky Mountain headwater streams , 2014 .

[28]  B. Bledsoe,et al.  Physical context for theoretical approaches to sediment transport magnitude‐frequency analysis in alluvial channels , 2014 .

[29]  Paul D. Bates,et al.  Flooding dynamics on the lower Amazon floodplain: 1. Hydraulic controls on water elevation, inundation extent, and river‐floodplain discharge , 2014 .

[30]  Jiahu Jiang,et al.  Large-scale hydrodynamic modeling of the middle Yangtze River Basin with complex river–lake interactions , 2013 .

[31]  E. D. Andrews,et al.  Effective Discharge and the Design of Channel Maintenance Flows for Gravel‐Bed Rivers , 2013 .

[32]  L. Samaniego,et al.  Evaluating multiple performance criteria to calibrate the distributed hydrological model of the upper Neckar catchment , 2013, Environmental Earth Sciences.

[33]  Matthew C. Bowers,et al.  On the distributions of seasonal river flows: Lognormal or power law? , 2012 .

[34]  V. Ferro,et al.  Identifying a dominant discharge for natural rivers in southern Italy , 2012 .

[35]  Qi Zhang,et al.  Effects of the Three Gorges Dam on Yangtze River flow and river interaction with Poyang Lake, China: 2003-2008 , 2012 .

[36]  C. C. Watson,et al.  Estimating channel‐forming discharge in urban watercourses , 2011 .

[37]  M. Church,et al.  Spatial and temporal variation of in‐reach suspended sediment dynamics along the mainstem of Changjiang (Yangtze River), China , 2010 .

[38]  Jiongxin Xu,et al.  Effect of reservoir construction on suspended sediment load in a large river system: thresholds and complex response , 2010 .

[39]  Jing Chen,et al.  Implications of flow control by the Three Gorges Dam on sediment and channel dynamics of the middle Yangtze (Changjiang) River, China , 2010 .

[40]  Jiongxin Xu,et al.  Variability of effective discharge for suspended sediment transport in a large semi-arid river basin , 2010 .

[41]  John Pitlick,et al.  Scaling frequency of channel‐forming flows in snowmelt‐dominated streams , 2010 .

[42]  Yan-Chao Hong,et al.  Assessment of extreme drought and human interference on baseflow of the Yangtze River , 2010 .

[43]  Jingbao Li,et al.  Sedimentation effects of the Dongting Lake Area , 2009 .

[44]  Yiping Guo,et al.  Relative Importance of Hydrological and Sediment-Transport Characteristics Affecting Effective Discharge of Small Urban Streams in Southern Ontario , 2009 .

[45]  M. Doyle,et al.  Channel-Forming Discharge Selection in River Restoration Design , 2007 .

[46]  Zhaoyin Wang,et al.  Sediment budget of the Yangtze River , 2007 .

[47]  W. Graf Downstream hydrologic and geomorphic effects of large dams on American rivers , 2006 .

[48]  F. Comiti,et al.  Effective discharge for sediment transport in a mountain river: Computational approaches and geomorphic effectiveness , 2006 .

[49]  Yoshiki Saito,et al.  Dam impacts on the Changjiang (Yangtze) River sediment discharge to the sea: The past 55 years and after the Three Gorges Dam , 2006 .

[50]  E. Foufoula‐Georgiou,et al.  Fluvial processes and streamflow variability: Interplay in the scale‐frequency continuum and implications for scaling , 2005 .

[51]  P. Goodwin Analytical Solutions for Estimating Effective Discharge , 2004 .

[52]  J. Pitlick,et al.  Magnitude-frequency of bed load transport in mountain streams in Colorado , 2004 .

[53]  J. Stedinger,et al.  Discharge indices for water quality loads , 2003 .

[54]  S. Ryan,et al.  Defining phases of bedload transport using piecewise regression , 2002 .

[55]  M. Wolman,et al.  Effective discharge and gravel‐bed rivers , 2001 .

[56]  Zhongyuan Chen,et al.  Yangtze River of China: historical analysis of discharge variability and sediment flux , 2001 .

[57]  James P. M. Syvitski,et al.  Estimating fluvial sediment transport: The rating parameters , 2000 .

[58]  Richard M. Vogel,et al.  PROBABILITY DISTRIBUTION OF ANNUAL MAXIMUM, MEAN, AND MINIMUM STREAMFLOWS IN THE UNITED STATES , 1996 .

[59]  John M. Melack,et al.  Flooding Hydrology and Mixture Dynamics of Lake Water Derived from Multiple Sources in an Amazon Floodplain Lake , 1995 .

[60]  D. Nash Effective Sediment-Transporting Discharge from Magnitude-Frequency Analysis , 1994, The Journal of Geology.

[61]  Richard M. Vogel,et al.  Closure of "Regional Flow-Duration Curves for Ungauged Sites in Massachusetts" , 1990 .

[62]  E. Andrews Effective and bankfull discharges of streams in the Yampa River basin, Colorado and Wyoming , 1980 .

[63]  G. Williams Bank‐full discharge of rivers , 1978 .

[64]  M. Wolman,et al.  Magnitude and Frequency of Forces in Geomorphic Processes , 1960, The Journal of Geology.

[65]  F. Xue,et al.  Transport characteristics of non-uniform suspended sediment in the Jingjiang Reach after the Three Gorges Project operation , 2021, Journal of Lake Sciences.

[66]  Guo Xiao-h Analysis of sediment transport in Middle Yangtze River after filling of the Three Gorges Reservoir , 2014 .