All Stories

  1. Dams trigger long-term river-floodplain decoupling in dynamic Andean foreland rivers
  2. River Sand and Gravel Mining: Global Drivers, Impacts, and Pathways for Sustainable Management
  3. Global patterns of reservoir sedimentation and overlooked risks in small reservoirs
  4. Water scarcity and infrastructure risk of amplified seasonal sediment transport
  5. Dams trigger long-term river-floodplain decoupling in dynamic Andean foreland rivers 
  6. River sand and gravel mining: A global synthesis of drivers, extents and impacts for sustainable management
  7. Path instability of ascending spheres in aging Laponite clay dispersions
  8. From extraction to recovery: Geomorphic and social transformations of gravel mining, Lubha River, Northeast Bangladesh
  9. Anisotropic dispersion of tire wear particle clouds challenges spherical-particle models of microplastic transport
  10. Human alterations to global riverine phosphorus fluxes to the ocean
  11. The impact of natural and anthropogenic factors on erosion in the Northeastern loess Plateau, China, during the past 10,000 years
  12. Quantifying the Form‐Flow‐Saltation Dynamics of Aeolian Sand Ripples
  13. Anthropogenic impacts on the Yellow River Basin
  14. Exacerbating dam-induced fragmentation in China’s river systems
  15. Hydrodynamic processes of incipient meander chute cutoffs: laboratory experiments with  implications for morphodynamics and depth-averaged modeling
  16. Statistical attributes of turbulent flow across porous walls with a geometrically smooth interface: The role of internal wall structure
  17. Hydrodynamic Processes of Incipient Meander Chute Cutoffs: Laboratory Experiments With Implications for Morphodynamics and Depth‐Averaged Modeling
  18. Bank Strength Variability controls the system-scale Morphodynamics of the Solimões River, Brazil
  19. Bedload transport contributions to the microplastic load of the River Waal, Netherlands
  20. Bioswales as potential sinks for tyre wear particle pollution
  21. Coupled evolution of rivers and floodplains
  22. Cryosphere-fed rivers in a warming climate, 1950-205
  23. Propagation of hydro-geomorphic disturbances through continental-scale river basins
  24. Regime shifts in sediment transport driven by warming-intensified cryosphere degradation and hydrological fluctuation
  25. Accelerated River Meander Migration on the Tibetan Plateau Caused by Permafrost Thaw
  26. How Do Vulnerable People Adapt to the Impact of Sedimentation in the Haor Wetlands of Northeastern Bangladesh?
  27. Hydrodynamic processes of incipient meander chute cutoffs: laboratory experiments with  implications for morphodynamics and depth-averaged modeling
  28. Hydrodynamic processes of incipient meander chute cutoffs- implications for morphodynamics and depth-averaged modeling
  29. Flow‐induced interfacial deformation structures (FIDS): Implications for the interpretation of palaeocurrents, flow dynamics and substrate rheology
  30. On the dynamics of aligned inertial particles settling in a quiescent, stratified two-layer medium
  31. Bank strength variability and its impact on the system-scale morphodynamics of the upper Amazon River in Brazil
  32. Decadal evolution of fluvial islands and its controlling factors along the lower Yangtze River
  33. Morphodynamics and depositional architecture of mid‐channel bars in large Amazonian rivers
  34. Controls on the Leeside Angle of Dunes in Shallow Unidirectional Flows
  35. River Damming Impacts on Fish Habitat and Associated Conservation Measures
  36. On the origin of chevron marks and striated grooves, and their use in predicting mud bed rheology
  37. On the settling of aligned spherical particles in various quiescent media
  38. Shifted sediment-transport regimes by climate change and amplified hydrological variability in cryosphere-fed rivers
  39. Bank strength and erodibility in the Amazon River and their control on large-scale river morphodynamics
  40. Field Evidence for the Initiation of Isolated Aeolian Sand Patches
  41. The Paraná River in the argentine plain: A review of its evolution and contemporary characteristics
  42. On the submerged low-Cauchy-number canopy dynamics under unidirectional flows
  43. Effects of low clay concentrations on nearly isotropic turbulence
  44. Beyond just floodwater
  45. How Do Vulnerable People in Bangladesh Experience Environmental Stress From Sedimentation in the Haor Wetlands? An Exploratory Study
  46. The dynamic floor of Yellowstone Lake, Wyoming, USA: The last 14 k.y. of hydrothermal explosions, venting, doming, and faulting
  47. Amplification of downstream flood stage due to damming of fine-grained rivers
  48. Sand mining impact on Poyang Lake: a case study based on high-resolution bathymetry and sub-bottom data
  49. The morphology of fluvial‐tidal dunes: Lower Columbia River, Oregon/Washington, USA
  50. Sedimentary pyrite in carbonaceous shales of the Mamfe Cretaceous basin, SW Cameroon: Morphologies, composition, pyrite framboid size frequency distribution, and formation pathways
  51. Linking dune dynamics and preservation: a unique approach using multibeam and parametric echo sounding time series, River Waal, Netherlands
  52. The effect of sediment qualities on the resistance of deltas to anthropogenic pressures
  53. Topographic perturbation of turbulent boundary layers by low‐angle, early‐stage aeolian dunes
  54. On the turbulence dynamics induced by a surrogate seagrass canopy
  55. The Influence of Three‐Dimensional Topography on Turbulent Flow Structures Over Dunes in Unidirectional Flows
  56. Sand, gravel, and UN Sustainable Development Goals: Conflicts, synergies, and pathways forward
  57. Unsteady dynamics of turbulent flow in the wakes of barchan dunes modulated by overlying boundary-layer structure
  58. Correction to: The mysterious grooves of Volcán Bárcena: a review of the role of streamwise counter-rotating vortices during erosion by dilute pyroclastic density currents
  59. The mysterious grooves of Volcán Bárcena: a review of the role of streamwise counter-rotating vortices during erosion by dilute pyroclastic density currents
  60. The Effect of Biofilms on Turbulent Flow Over Permeable Beds
  61. Using multibeam backscatter strength to analyze the distribution of manganese nodules: A case study of seamounts in the Western Pacific Ocean
  62. The sedimentary architecture of hyperpycnites produced by transient turbulent flows in a shallow lacustrine environment
  63. Rapid gravity flow transformation revealed in a single climbing ripple
  64. Interpreting pre-vegetation landscape dynamics: The Cambrian Lower Mount Simon Sandstone, Illinois, U.S.A.
  65. Influence of Dunes on Channel‐Scale Flow and Sediment Transport in a Sand Bed Braided River
  66. Why do large, deep rivers have low-angle dune beds?: COMMENT
  67. Alluvial architecture of mid‐channel fluvial–tidal barforms: The mesotidal Lower Columbia River, Oregon/Washington, USA
  68. Dune-scale cross-strata across the fluvial-deltaic backwater regime: Preservation potential of an autogenic stratigraphic signature
  69. The Pace of Human-Induced Change in Large Rivers: Stresses, Resilience, and Vulnerability to Extreme Events
  70. Source apportionment of soil heavy metals in fluvial islands, Anhui section of the lower Yangtze River: comparison of APCS–MLR and PMF
  71. An integrated process‐based model of flutes and tool marks in deep‐water environments: Implications for palaeohydraulics, the Bouma sequence and hybrid event beds
  72. Drainage and erosion of Cambodia’s great lake in the middle-late Holocene: The combined role of climatic drying, base-level fall and river capture
  73. Novel Environment Enables PIV Measurements of Turbulent Flow around and within Complex Topographies
  74. Soft-sediment deformation structures as indicators of tectono-volcanic activity during evolution of a lacustrine basin: A case study from the Upper Triassic Ordos Basin, China
  75. Seeing through the fluid dynamics of flexible vegetation and canopy turbulence
  76. The Origin of Aeolian Dunes – PIV measurements of flow structure over early stage protodunes in a refractive-index-matching flume
  77. The effects of fluvial and basal sediment properties on the morphodynamics of deltas undergoing sediment supply reduction
  78. Secondary Flows and Vortex Structure Associated With Isolated and Interacting Barchan Dunes
  79. Dunes in the world’s big rivers are characterized by low-angle lee-side slopes and a complex shape
  80. Experimental evidence of amplitude modulation in permeable-wall turbulence
  81. River bank instability from unsustainable sand mining in the lower Mekong River
  82. River temperature and the thermal-dynamic transport of sediment
  83. Time is running out for sand
  84. Spatial Scales of Turbulent Flow Structures Associated With Interacting Barchan Dunes
  85. Small- and large- scale soft-sediment deformations in a Triassic lacustrine delta caused by overloading and seismicity in the Ordos Basin, central China
  86. PIV measurements of turbulent flow overlying large, cubic- and hexagonally-packed hemisphere arrays
  87. Observations and scaling of tidal mass transport across the lower Ganges–Brahmaputra delta plain: implications for delta management and sustainability
  88. Author Correction: Anthropogenic stresses on the world’s big rivers
  89. Quantification of bedform dynamics and bedload sediment flux in sandy braided rivers from airborne and satellite imagery
  90. Sedimentologic and palaeoenvironmental evolution of the Mamfe Cretaceous Basin (SW Cameroon): Evidence from lithofacies analysis, tectonics and evaporite minerals suite
  91. Describing fluvial systems: linking processes to deposits and stratigraphy
  92. Anthropogenic stresses on the world’s big rivers
  93. Hydrodynamic modelling of tidal-fluvial flows in a large river estuary
  94. On the Causes of Pulsing in Continuous Turbidity Currents
  95. Experimental study of turbulent flow over and within cubically packed walls of spheres: Effects of topography, permeability and wall thickness
  96. The adaptation of dunes to changes in river flow
  97. The Impact of Nonequilibrium Flow on the Structure of Turbulence Over River Dunes
  98. Observations and scaling of tidal mass transport across the lower Ganges-Brahmaputra delta plain: implications for delta management and sustainability
  99. Turbulent Flow Structure Associated With Collision Between Laterally Offset, Fixed-Bed Barchan Dunes
  100. The sedimentology of river confluences
  101. Early burial mud diapirism and its impact on stratigraphic architecture in the Carboniferous of the Shannon Basin, County Clare, Ireland
  102. ‘Boundary’: mapping and visualizing climatically changed landscapes at Kaskawulsh Glacier and Kluane Lake, Yukon
  103. Turbulence Links Momentum and Solute Exchange in Coarse-Grained Streambeds
  104. The significance of superimposed dunes in the Amazon River: Implications for how large rivers are identified in the rock record
  105. The influence of tributary flow density differences on the hydrodynamic behavior of a confluent meander bend and implications for flow mixing
  106. Linking the local vertical variability of permeability and porosity to newly-interpreted lithofacies in the lower Mt. Simon CO2 reservoir
  107. The planform mobility of river channel confluences: Insights from analysis of remotely sensed imagery
  108. An evaluation of the use of a multibeam echo-sounder for observations of suspended sediment
  109. The influence of flow discharge variations on the morphodynamics of a diffluence-confluence unit on a large river
  110. Length scales and statistical characteristics of outer bank roughness for large elongate meander bends: The influence of bank material properties, floodplain vegetation and flow inundation
  111. River piracy and drainage basin reorganization led by climate-driven glacier retreat
  112. A numerical investigation into the importance of bed permeability on determining flow structures over river dunes
  113. Cavitation erosion of bedrock channels
  114. Extreme flood-driven fluvial bank erosion and sediment loads: direct process measurements using integrated Mobile Laser Scanning (MLS) and hydro-acoustic techniques
  115. Three-dimensional flow structure and bed morphology in large elongate meander loops with different outer bank roughness characteristics
  116. Fluvial sediment supply to a mega-delta reduced by shifting tropical-cyclone activity
  117. Comparing the transitional behaviour of kaolinite and bentonite suspension flows
  118. On the evolution and form of coherent flow structures over a gravel bed: Insights from whole flow field visualization and measurement
  119. The alluvial architecture of a suspended sediment dominated meandering river: the Río Bermejo, Argentina
  120. Bedform genesis in bedrock substrates: Insights into formative processes from a new experimental approach and the importance of suspension-dominated abrasion
  121. Spatial variability in bank resistance to erosion on a large meandering, mixed bedrock-alluvial river
  122. Modulation of outer bank erosion by slump blocks: Disentangling the protective and destructive role of failed material on the three-dimensional flow structure
  123. The role of discharge variability in determining alluvial stratigraphy
  124. Extremes in dune preservation: Controls on the completeness of fluvial deposits
  125. Predicting bedforms and primary current stratification in cohesive mixtures of mud and sand
  126. Fluvio-deltaic avulsions during relative sea-level fall
  127. Grain-Size Controls On the Morphology and Internal Geometry of River-Dominated Deltas
  128. Mid to late Holocene geomorphological and sedimentological evolution of the fluvial–tidal zone
  129. Preface
  130. Bed form genesis from bed defects under unidirectional, oscillatory, and combined flows
  131. Effect of bed permeability and hyporheic flow on turbulent flow over bed forms
  132. A unified model for bedform development and equilibrium under unidirectional, oscillatory and combined-flows
  133. The impact of significant input of fine sediment on benthic fauna at tributary junctions: a case study of the Bermejo-Paraguay River confluence, Argentina
  134. A New Phase Diagram for Combined-Flow Bedforms
  135. Scales and causes of heterogeneity in bars in a large multi-channel river: Río Paraná, Argentina
  136. Flow structure and channel morphodynamics of meander bend chute cutoffs: A case study of the Wabash River, USA
  137. Coherent Flow Structures at Earth's Surface
  138. LES of barchan dunes
  139. Paragenetic sequences of carbonate and sulphide minerals of the Mamfe Basin (Cameroon): Indicators of palaeo-fluids, palaeo-oxygen levels and diagenetic zones
  140. A flume experiment on the effect of channel width on the perturbation and recovery of flow in straight pools and riffles with smooth boundaries
  141. Discrimination of bed form scales using robust spline filters and wavelet transforms: Methods and application to synthetic signals and bed forms of the Río Paraná, Argentina
  142. Decimeter-scale in situ mapping of modern cross-bedded dune deposits using parametric echo sounding: A new method for linking river processes and their deposits
  143. Monitoring the generation and evolution of the sediment plume behind towed fishing gears using a multibeam echosounder
  144. Three-dimensional gravity-current flow within a subaqueous bend: Spatial evolution and force balance variations
  145. Deposits of the sandy braided South Saskatchewan River: Implications for the use of modern analogs in reconstructing channel dimensions in reservoir characterization
  146. Velocity Mapping Toolbox (VMT): a processing and visualization suite for moving-vessel ADCP measurements
  147. Bedforms: views and new perspectives from the third international workshop on Marine and River Dune Dynamics (MARID3)
  148. Application of a roughness-length representation to parameterize energy loss in 3-D numerical simulations of large rivers
  149. Flow fields, bed shear stresses, and suspended bed sediment dynamics in bifurcations of a large river
  150. Quantification of the relation between surface morphodynamics and subsurface sedimentological product in sandy braided rivers
  151. Modelling hydrodynamics in the Rio Paraná, Argentina: An evaluation and inter-comparison of reduced-complexity and physics based models applied to a large sand-bed river
  152. Mitigating land loss in coastal Louisiana by controlled diversion of Mississippi River sand
  153. Tributary, distributary and other fluvial patterns: What really represents the norm in the continental rock record?
  154. Sediment mobility and bed armoring in the St Clair River: insights from hydrodynamic modeling
  155. A versatile refractive-index-matched flow facility for studies of complex flow systems across scientific disciplines
  156. Quantifying the dynamics of flow within a permeable bed using time-resolved endoscopic particle imaging velocimetry (EPIV)
  157. An experimental study of discharge partitioning and flow structure at symmetrical bifurcations
  158. Extreme sediment pulses generated by bend cutoffs along a large meandering river
  159. Bed morphology, flow structure, and sediment transport at the outlet of Lake Huron and in the upper St. Clair River
  160. Depositional processes, bedform development and hybrid bed formation in rapidly decelerated cohesive (mud-sand) sediment flows
  161. Particle-image velocimetry measurements of flow over interacting barchan dunes
  162. Wavelets Application to Study the Bedforms of Parana River
  163. Evolution and sedimentology of a channel fill in the sandy braided South Saskatchewan River and its comparison to the deposits of an adjacent compound bar
  164. Sedimentation in deep-sea lobe-elements: implications for the origin of thickening-upward sequences
  165. Preface to Decadal Issue
  166. On determining the geometric and kinematic characteristics of coherent flow structures over a gravel bed: a new approach using combined PLIF-PIV
  167. Fluvial form in modern continental sedimentary basins: Distributive fluvial systems: COMMENT
  168. Coherent flow structures in a depth-limited flow over a gravel surface: The influence of surface roughness
  169. Can we distinguish flood frequency and magnitude in the sedimentological record of rivers?
  170. Response of river-dominated delta channel networks to permanent changes in river discharge
  171. Quantification of braided river channel change using archival digital image analysis
  172. A new methodology for the quantitative visualization of coherent flow structures in alluvial channels using multibeam echo-sounding (MBES)
  173. On the relationship between flow and suspended sediment transport over the crest of a sand dune, Río Paraná, Argentina
  174. Monitoring Suspended Sediment Dynamics Using MBES
  175. The influence of dunes on mixing in a migrating salt-wedge: Fraser River estuary, Canada
  176. Suspended sediment transport and deposition over a dune: Río Paraná, Argentina
  177. The Sedimentology and Alluvial Architecture of a Large Braid Bar, Rio Parana, Argentina
  178. Morphology, flow structure, and suspended bed sediment transport at two large braid-bar confluences
  179. A Phase Diagram for Turbulent, Transitional, and Laminar Clay Suspension Flows
  180. A pilot study of the efficacy of residuum lodges for managing sediment delivery to impoundment reservoirs
  181. Coherent flow structures in a depth-limited flow over a gravel surface: The role of near-bed turbulence and influence of Reynolds number
  182. Discussion of “Transition from Ripples to Dunes” by Arved J. Raudkivi
  183. River response to lateral ground tilting: a synthesis and some implications for the modelling of alluvial architecture in extensional basins
  184. Causes of rapid mixing at a junction of two large rivers: Río Paraná and Río Paraguay, Argentina
  185. The dynamics of turbulent, transitional and laminar clay-laden flow over a fixed current ripple
  186. Reply to Discussion of Imran et al. on “The orientation of helical flow in curved channels” by Corney et al., Sedimentology, 53, 249-257
  187. Comparison of Fixed- and Moving-Vessel Flow Measurements with an aDp in a Large River
  188. The influence of scale, slope and channel geometry on the flow dynamics of submarine channels
  189. The relationship between channel avulsion, flow occupancy and aggradation in braided rivers: insights from an experimental model
  190. Meander-Bend Evolution, Alluvial Architecture, and the Role of Cohesion in Sinuous River Channels: A Flume Study
  191. Dynamics of a river channel confluence with discordant beds: Flow turbulence, bed load sediment transport, and bed morphology
  192. Electrical Resistance Tomography for Suspended Sediment Measurements in Open Channel Flows Using a Novel Sensor Design
  193. Braided Rivers
  194. Bar-top hollows: A new element in the architecture of sandy braided rivers
  195. Flow structure in sinuous submarine channels: Velocity and turbulence structure of an experimental submarine channel
  196. Mean flow, turbulence structure, and bed form superimposition across the ripple-dune transition
  197. The orientation of helical flow in curved channels
  198. The sedimentology and alluvial architecture of the sandy braided South Saskatchewan River, Canada
  199. Bed forms in bimodal sand-gravel sediments: laboratory and field analysis
  200. Form roughness and the absence of secondary flow in a large confluence–diffluence, Rio Paraná, Argentina
  201. Morphology and flow fields of three-dimensional dunes, Rio Paraná, Argentina: Results from simultaneous multibeam echo sounding and acoustic Doppler current profiling
  202. The fluid dynamics of river dunes: A review and some future research directions
  203. Response of sand dunes to variations in tidal flow: Fraser Estuary, Canada
  204. Development and testing of a numerical code for treatment of complex river channel topography in three-dimensional CFD models with structured grids
  205. Measuring flow velocity and sediment transport with an acoustic Doppler current profiler
  206. Whole flow field dynamics and velocity pulsing within natural sediment-laden underflows
  207. Sedimentology and kinematics of a large, retrogressive growth-fault system in Upper Carboniferous deltaic sediments, western Ireland
  208. Measuring Velocity and Shear Stress over Dunes with Acoustic Doppler Profiler
  209. Relationship between sediment supply and avulsion frequency in braided rivers
  210. Three-Dimensional Sedimentary Architecture of a Large, Mid-Channel Sand Braid Bar, Jamuna River, Bangladesh
  211. Sedimentology of the Bengal shelf, Bangladesh: comparison of late Miocene sediments, Sitakund anticline, with the modern, tidally dominated shelf
  212. The use and application of GPR in sandy fluvial environments: methodological considerations
  213. The physical scale modelling of braided alluvial architecture and estimation of subsurface permeability
  214. Computational fluid dynamics and the physical modelling of an upland urban river
  215. Turbulence Modulation in Clay-Rich Sediment-Laden Flows and Some Implications for Sediment Deposition
  216. Quantitative visualization of flow fields associated with alluvial sand dunes: Results from the laboratory and field using ultrasonic and acoustic doppler anemometry
  217. Turbulence and Coherent Flow Structures Associated with Bedform Amalgamation: An Experimental Study of the Ripple-Dune Transition
  218. Ripple formation induced by biogenic mounds—comment
  219. Morphological evolution and dynamics of a large, sand braid-bar, Jamuna River, Bangladesh
  220. The Western Irish Namurian Basin reassessed
  221. Turbulence and Secondary Flow over Sediment Stripes in Weakly Bimodal Bed Material
  222. Three-dimensional structure of flow at a confluence of river channels with discordant beds
  223. Fluid and sediment dynamics of upper stage plane beds
  224. Scour in large braided rivers and the recognition of sequence stratigraphic boundaries
  225. Discussion and Closure: Bed-Load Motion at High Shear Stress: Dune Washout and Plane-Bed Flow
  226. Preservation of planar laminae due to migration of low-relief bed waves over aggrading upper-stage plane beds: comparison of experimental data with theory
  227. Effects of Bed Discordance on Flow Dynamics at Open Channel Confluences
  228. Turbulent flow structure at concordant and discordant open-channel confluences
  229. A scheme for resampling, filtering, and subsampling unevenly spaced laser Doppler anemometer data
  230. Mean flow and turbulence structure over fixed, two-dimensional dunes: implications for sediment transport and bedform stability
  231. Particle Size and Velocity Discrimination in a Sediment-Laden Turbulent Flow Using Phase Doppler Anemometry
  232. Three-Dimensional Flow Structure at Open-Channel Diversions
  233. Effect of Orientation and Size of Helley‐Smith Sampler on Its Efficiency
  234. On experimental reflected density currents and the interpretation of certain turbidites
  235. Drag reduction in turbulent muddy seawater flows and some sedimentary consequences
  236. Bed morphology and sedimentology at the confluence of unequal depth channels
  237. Braided rivers: perspectives and problems
  238. Mechanisms of anabranch avulsion within gravel-bed braided rivers: observations from a scaled physical model
  239. On the entrainment of sediment and initiation of bed defects: insights from recent developments within turbulent boundary layer research
  240. The morphology and dynamics of low amplitude bedwaves upon upper stage plane beds and the preservation of planar laminae
  241. Discussion of “ Development of Bed Features ” by Arved J. Raudkivi and Hans‐H. Witte (September, 1990, Vol. 116, No. 9)
  242. Sedimentology and event timing of a catastrophic volcaniclastic mass flow, Volcan Hudson, Southern Chile
  243. Mixing-layer distortion at the confluence of channels of different depth
  244. REPLY
  245. Fluidization pipes in volcaniclastic mass flows, Volcan Hudson, Southern Chile
  246. Earthquakes, Rivers and Ice: Scientific Research at the Laguna San Rafael, Southern Chile, 1986
  247. Flow, sediment transport and bedform dynamics over the transition from dunes to upper-stage plane beds: implications for the formation of planar laminae
  248. Sediment transport and bed morphology at river channel confluences
  249. Closure to “Separation Zone at Open‐Channel Junctions” by James L. Best and Ian Reid (November, 1984)
  250. The morphology of river channel confluences
  251. Flow separation—a physical process for the concentration of heavy minerals within alluvial channels
  252. Separation Zone at Open‐Channel Junctions