56 citations as recorded by crossref.

1. Effect of particle size ratio on shear-induced onset of particle motion at low particle Reynolds numbers: From high shielding to roughness N. Topic et al. 10.1063/1.5108800
2. Viewing Earth’s surface as a soft-matter landscape D. Jerolmack & K. Daniels 10.1038/s42254-019-0111-x
3. Laboratory rivers adjust their shape to sediment transport A. Abramian et al. 10.1103/PhysRevE.102.053101
4. The influence of changes in flow regime caused by dam closure on channel planform evolution: insights from flume experiments M. Słowik et al. 10.1007/s12665-021-09437-5
5. Sediment behavior controls equilibrium width of subglacial channels A. DAMSGAARD et al. 10.1017/jog.2017.71
6. Viewing second-order phase transitions as a metaphor for river bifurcations N. Ragno 10.1017/jfm.2023.831
7. Historical and contemporary drivers of knickpoint retreat and morphological evolution along Bayou Pierre, Mississippi L. Stearman & F. Heitmuller 10.1002/rra.4266
8. Mud cohesion governs unvegetated meander migration rates and deposit architecture M. Douglas et al. 10.1130/B37315.1
9. Seismic cycles, earthquakes, landslides and sediment fluxes: Linking tectonics to surface processes using a reduced-complexity model T. Croissant et al. 10.1016/j.geomorph.2019.04.017
10. Textural signatures of sediment supply in gravel-bed rivers: Revisiting the armour ratio D. Vázquez-Tarrío et al. 10.1016/j.earscirev.2020.103211
11. Threshold constraints on the size, shape and stability of alluvial rivers C. Phillips et al. 10.1038/s43017-022-00282-z
12. Floods on Alluvial Fans: Implications for Reworking Rates, Morphology and Fan Hazards A. Leenman et al. 10.1029/2021JF006367
13. Development of robust evolutionary polynomial regression network in the estimation of stable alluvial channel dimensions H. Bonakdari et al. 10.1016/j.geomorph.2019.106895
14. Coupling threshold theory and satellite-derived channel width to estimate the formative discharge of Himalayan foreland rivers K. Gaurav et al. 10.5194/esurf-9-47-2021
15. Effects of initial and boundary conditions on gravel-bed river morphology S. Paudel et al. 10.1016/j.advwatres.2022.104256
16. Sediment load determines the shape of rivers P. Popović et al. 10.1073/pnas.2111215118
17. Scaling behavior of bedload transport: what if Bagnold was right? C. Ancey & A. Recking 10.1016/j.earscirev.2023.104571
18. Sediment supply control on morphodynamic processes in gravel‐bed river widenings C. Rachelly et al. 10.1002/esp.5460
19. Assessing the impact of climate change on sediment discharge using a large ensemble rainfall dataset in Pekerebetsu River basin, Hokkaido R. Kido et al. 10.1186/s40645-023-00580-0
20. Enhanced formulation of the probability principle based on maximum entropy to design the bank profile of channels in geomorphic threshold A. Gholami et al. 10.1007/s00477-019-01679-x
21. The fate of particles in a volumetrically heated convective fluid at high Prandtl number C. Sturtz et al. 10.1017/jfm.2021.862
22. Model for the Formation of Single‐Thread Rivers in Barren Landscapes and Implications for Pre‐Silurian and Martian Fluvial Deposits M. Lapôtre et al. 10.1029/2019JF005156
23. What sets river width? K. Dunne & D. Jerolmack 10.1126/sciadv.abc1505
24. Does the Threshold of Sediment Motion Constrain the Width of an Incising Laboratory River? T. Ashley & K. Strom 10.1029/2022GL099718
25. Predicting river channel pattern based on stream power, bed material and bank strength J. Candel et al. 10.1177/0309133320948831
26. Modelling shear stress distribution in ice-covered streams B. Koyuncu & T. Le 10.1144/SP540-2022-161
27. Lower‐Stage Plane Bed Topography Is an Outcome of Rarefied, Intermittent Sediment Transport T. Ashley et al. 10.1029/2020JF005754
28. Differential Bank Migration Limits the Lifespan and Width of Braided Channel Threads A. Chadwick et al. 10.1029/2021WR031236
29. Entrainment and deposition of boulders in a gravel bed river P. Allemand et al. 10.5194/esurf-11-21-2023
30. The longer arc of channel recovery post-dam removal J. Fields et al. 10.1016/j.geomorph.2024.109442
31. Experimental evidence for bifurcation angles control on abandoned channel fill geometry L. Szewczyk et al. 10.5194/esurf-8-275-2020
32. Rapid post-seismic landslide evacuation boosted by dynamic river width T. Croissant et al. 10.1038/ngeo3005
33. Spatio-temporal variations on alluvial fan channel width in response to grain size on the channel bed under constant upstream boundary conditions H. Shin & W. Kim 10.1038/s41598-025-94465-5
34. Integrating Sequence Stratigraphy and Geostatistical Methods for 3D Lithofacies Modelling of the Tiber Alluvial Plain, Rome, Italy D. Tentori et al. 10.1111/bre.70024
35. Viscous transfer of momentum across a shallow laminar flow O. Devauchelle et al. 10.1017/jfm.2021.1021
36. Evidence of, and a proposed explanation for, bimodal transport states in alluvial rivers K. Dunne & D. Jerolmack 10.5194/esurf-6-583-2018
37. Dynamic Equilibrium Position Prediction Model for the Confluence Area of Nakdong River M. Kim et al. 10.9719/EEG.2023.56.4.435
38. Geomorphic variability of submarine channelized systems along continental margins: Comparison with fluvial meandering channels M. Lemay et al. 10.1016/j.marpetgeo.2020.104295
39. Soft matter physics of the ground beneath our feet A. Voigtländer et al. 10.1039/D4SM00391H
40. Sediment flux‐driven channel geometry adjustment of bedrock and mixed gravel–bedrock rivers E. Baynes et al. 10.1002/esp.4996
41. Earthcasting: Geomorphic Forecasts for Society B. Ferdowsi et al. 10.1029/2021EF002088
42. Streamwise streaks induced by bedload diffusion A. Abramian et al. 10.1017/jfm.2018.1024
43. Bankfull Transport Capacity and the Threshold of Motion in Coarse‐Grained Rivers C. Phillips & D. Jerolmack 10.1029/2019WR025455
44. A Novel Comprehensive Evaluation Method for Estimating the Bank Profile Shape and Dimensions of Stable Channels Using the Maximum Entropy Principle H. Bonakdari et al. 10.3390/e22111218
45. Interplay of River and Tidal Forcings Promotes Loops in Coastal Channel Networks A. Konkol et al. 10.1029/2022GL098284
46. Low-gradient, single-threaded rivers prior to greening of the continents V. Ganti et al. 10.1073/pnas.1901642116
47. Critical transition of incising gravel channel to evacuate alluvial lateral supply S. Cataño-Alvarez 10.1080/02723646.2021.1923368
48. Hydro-morphometric parameters controlling travel distance of pebbles and cobbles in three gravel bed streams L. Gilet et al. 10.1016/j.geomorph.2020.107117
49. How Do Braided Rivers Grow Channel Belts? A. Limaye 10.1029/2020JF005570
50. A method based on the Tsallis entropy for characterizing threshold channel bank profiles A. Gholami et al. 10.1016/j.physa.2019.121089
51. Self-similar growth of a bimodal laboratory fan P. Delorme et al. 10.5194/esurf-5-239-2017
52. Assessment of geomorphological bank evolution of the alluvial threshold rivers based on entropy concept parameters A. Gholami et al. 10.1080/02626667.2019.1608995
53. Quasi‐Universal Length Scale of River Anabranches N. Ragno et al. 10.1029/2022GL099928
54. Shear-induced motion of a bead on regular substrates at small particle Reynolds numbers N. Topic et al. 10.1017/jfm.2022.633
55. Response of submarine braided channels to varying inflow hydrographs: Geomorphic experiments and stratigraphic implications S. Lai et al. 10.1111/sed.13236
56. A single width–discharge regime relationship for individual threads of braided and meandering rivers from the Himalayan Foreland K. Gaurav et al. 10.1016/j.geomorph.2017.07.004