94 citations as recorded by crossref.

1. Automated detecting, segmenting and measuring of grains in images of fluvial sediments: The potential for large and precise data from specialist deep learning models and transfer learning D. Mair et al. 10.1002/esp.5755
2. Preservation and transportation of large landslide deposits under decadal and millennial timescales in the Taiwan orogenic belt C. Chen et al. 10.1016/j.geomorph.2022.108402
3. Lithological control on the geomorphic evolution of the Shillong Plateau in Northeast India C. Strong et al. 10.1016/j.geomorph.2019.01.016
4. The influence of lithology on channel geometry and bed sediment organization in mountainous hillslope‐coupled streams M. Fratkin et al. 10.1002/esp.4885
5. Multiband (X, C, L) radar amplitude analysis for a mixed sand- and gravel-bed river in the eastern Central Andes B. Purinton & B. Bookhagen 10.1016/j.rse.2020.111799
6. Glacial-interglacial climate changes recorded by debris flow fan deposits, Owens Valley, California M. D'Arcy et al. 10.1016/j.quascirev.2017.06.002
7. Modelling of sediment supply from torrent catchments in the Western Alps using the sediment contributing area (SCA) approach M. Altmann et al. 10.1002/esp.5046
8. Slope, grain size, and roughness controls on dry sediment transport and storage on steep hillslopes R. DiBiase et al. 10.1002/2016JF003970
9. Does soil erosion rejuvenate the soil phosphorus inventory? A. Eger et al. 10.1016/j.geoderma.2018.06.021
10. Predicting post‐fire debris flow grain sizes and depositional volumes in the Intermountain West, United States S. Wall et al. 10.1002/esp.5480
11. The effect of fragmentation on the distribution of hillslope rock size and abundance: Insights from contrasting field and model data A. Román-Sánchez et al. 10.1016/j.geoderma.2019.06.014
12. The gravel-sand transition and grain size gap in river bed sediments E. Dingle et al. 10.1016/j.earscirev.2021.103838
13. Variable‐Threshold Behavior in Rivers Arising From Hillslope‐Derived Blocks C. Shobe et al. 10.1029/2017JF004575
14. Grain size of fluvial gravel bars from close-range UAV imagery – uncertainty in segmentation-based data D. Mair et al. 10.5194/esurf-10-953-2022
15. Sediment size on talus slopes correlates with fracture spacing on bedrock cliffs: implications for predicting initial sediment size distributions on hillslopes J. Verdian et al. 10.5194/esurf-9-1073-2021
16. Hillslope‐derived blocks retard river incision C. Shobe et al. 10.1002/2016GL069262
17. Sand, Gravel, Cobbles, and Boulders: Detrital Thermochronology Shows that One Size Does Not Tell All C. Lukens et al. 10.1029/2023JF007192
18. Rock properties and sediment caliber govern bedrock river morphology across the Taiwan Central Range J. Carr et al. 10.1126/sciadv.adg6794
19. An automated knickzone selection algorithm (KZ‐Picker) to analyze transient landscapes: Calibration and validation A. Neely et al. 10.1002/2017JF004250
20. Water in the critical zone: soil, water and life from profile to planet M. Kirkby 10.5194/soil-2-631-2016
21. Post-Wildfire Debris Flow and Large Woody Debris Transport Modeling from the North Complex Fire to Lake Oroville T. Wasklewicz et al. 10.3390/w15040762
22. Introducing <i>PebbleCounts</i>: a grain-sizing tool for photo surveys of dynamic gravel-bed rivers B. Purinton & B. Bookhagen 10.5194/esurf-7-859-2019
23. Local topography and erosion rate control regolith thickness along a ridgeline in the Sierra Nevada, California E. Gabet et al. 10.1002/esp.3754
24. The grain size of sediments delivered to steep debris‐flow prone channels prior to and following wildfire A. Neely et al. 10.1002/esp.5819
25. The problem of predicting the size distribution of sediment supplied by hillslopes to rivers L. Sklar et al. 10.1016/j.geomorph.2016.05.005
26. Evidence for Self‐Similar Bedload Transport on Andean Alluvial Fans, Iglesia Basin, South Central Argentina R. Harries et al. 10.1029/2017JF004501
27. Formation of waterfalls by intermittent burial of active faults L. Malatesta & M. Lamb 10.1130/B31743.1
28. Controls on Pebbles’ Size and Shape in Streams of the Swiss Alps C. Litty & F. Schlunegger 10.1086/689183
29. Geomorphic response of a mountain gravel-bed river to an extreme flood in Aberdeenshire, Scotland D. Fieman et al. 10.1144/sjg2019-005
30. Impact of climate on landscape form, sediment transfer and the sedimentary record R. Harries et al. 10.1002/esp.5075
31. How does landslide debris grain size control sediment transport and dynamics? J. Xie et al. 10.1016/j.geomorph.2023.109050
32. Modelling the evolution of debris flows after the 2008 Wenchuan earthquake F. Yang et al. 10.1016/j.enggeo.2023.107152
33. Climate and topography control the size and flux of sediment produced on steep mountain slopes C. Riebe et al. 10.1073/pnas.1503567112
34. Tracking Downstream Variability in Large Grain‐Size Distributions in the South‐Central Andes B. Purinton & B. Bookhagen 10.1029/2021JF006260
35. Measuring the grain‐size distributions of mass movement deposits E. Harvey et al. 10.1002/esp.5337
36. Fluvial geomorphology of the Yan Shan in North China: Implications for drainage evolution and seismic activity X. Yu & A. Yin 10.1016/j.jhydrol.2024.130810
37. Characterizing the transient geomorphic response to base‐level fall in the northeastern Tibetan Plateau H. Zhang et al. 10.1002/2015JF003715
38. Slip slidin' away: A post-glacial environmental history of the Waipaoa River basin B. Gomez & B. Rosser 10.1016/j.geomorph.2017.08.035
39. Effects of Mass Wasting on the Physiochemical Properties of Fluvial Sediments in Puerto Rico Following Hurricane Maria N. Webb et al. 10.1029/2021JF006509
40. The story of a summit nucleus: hillslope boulders and their effect on erosional patterns and landscape morphology in the Chilean Coastal Cordillera E. Lodes et al. 10.5194/esurf-11-305-2023
41. The size, distribution, and mobility of landslides caused by the 2015 Mw7.8 Gorkha earthquake, Nepal K. Roback et al. 10.1016/j.geomorph.2017.01.030
42. Storage and export of soil carbon and mineral surface area along an erosional gradient in the Sierra Nevada, California X. Wang et al. 10.1016/j.geoderma.2018.02.008
43. Kinetically limited weathering at low denudation rates in semiarid climatic conditions J. Schoonejans et al. 10.1002/2015JF003626
44. Does Pebble Abrasion Influence Detrital Age Population Statistics? A Numerical Investigation of Natural Data Sets C. Lavarini et al. 10.1029/2018JF004610
45. Fracture density and grain size controls on the relief structure of bedrock landscapes R. DiBiase et al. 10.1130/G40006.1
46. How many grains are needed for quantifying catchment erosion from tracer thermochronology? A. Madella et al. 10.5194/gchron-4-177-2022
47. Predicting river bed substrate cover proportions across New Zealand A. Haddadchi et al. 10.1016/j.catena.2017.12.014
48. Soil organic carbon and mineral interactions on climatically different hillslopes X. Wang et al. 10.1016/j.geoderma.2018.02.021
49. Measuring alluvial fan sensitivity to past climate changes using a self‐similarity approach to grain‐size fining, Death Valley, California M. D'Arcy et al. 10.1111/sed.12308
50. Straight from the source's mouth: Controls on field‐constrained sediment export across the entire active Corinth Rift, central Greece S. Watkins et al. 10.1111/bre.12444
51. Controls on the hydraulic geometry of alluvial channels: bank stability to gravitational failure, the critical-flow hypothesis, and conservation of mass and energy J. Pelletier 10.5194/esurf-9-379-2021
52. Arrested development: Erosional equilibrium in the southern Sierra Nevada, California, maintained by feedbacks between channel incision and hillslope sediment production R. Callahan et al. 10.1130/B35006.1
53. Coarse sediment supply sets the slope of bedrock channels in rapidly uplifting terrain: Field and topographic evidence from eastern Taiwan L. Lai et al. 10.1002/esp.5200
54. Landslides after wildfire: initiation, magnitude, and mobility F. Rengers et al. 10.1007/s10346-020-01506-3
55. Bio-climate affects hillslope and fluvial sediment grain size along the Chilean Coastal Cordillera S. Terweh et al. 10.1016/j.geomorph.2021.107700
56. Fluvial archives, a valuable record of vertical crustal deformation A. Demoulin et al. 10.1016/j.quascirev.2016.11.011
57. Dynamic bedrock channel width during knickpoint retreat enhances undercutting of coupled hillslopes E. Baynes et al. 10.1002/esp.5477
58. River profile response to normal fault growth and linkage: an example from the Hellenic forearc of south-central Crete, Greece S. Gallen & K. Wegmann 10.5194/esurf-5-161-2017
59. Post-Miocene topographic rejuvenation in an elevated passive continental margin not characterized by a sharp escarpment (northern end of the Mantiqueira Range, Brazil) S. Calegari et al. 10.1016/j.geomorph.2021.107946
60. Canyon shape and erosion dynamics governed by channel-hillslope feedbacks R. Glade et al. 10.1130/G46219.1
61. Human Management Decreased Suspended Particle Size in the Loess Plateau Rivers during the 1980s to the 2010s K. Li et al. 10.3390/su16020799
62. Grain size from source to sink – modern and ancient fining rates T. Reynolds 10.1016/j.earscirev.2024.104699
63. The Lasting Legacy of Megaflood Boulder Deposition in Mountain Rivers S. Morey et al. 10.1029/2023GL105066
64. Denudation systematics inferred from in situ cosmogenic <sup>10</sup>Be concentrations in fine (50–100 µm) and medium (100–250 µm) sediments of the Var River basin, southern French Alps A. Mariotti et al. 10.5194/esurf-7-1059-2019
65. Peripheral gully and landslide erosion on an extreme anthropogenic landscape produced by mountaintop removal coal mining M. Reed & S. Kite 10.1002/esp.4867
66. A New Data‐Driven Bayesian Inversion of Fluvial Topography Clarifies the Tectonic History of the Corinth Rift and Reveals a Channel Steepness Threshold S. Gallen & D. Fernández‐Blanco 10.1029/2020JF005651
67. Gully characteristics across linear troughs in the southern Daliangshan, and its implications for debris mitigation K. Li et al. 10.1007/s10064-023-03293-2
68. Possible threshold controls on sediment grain properties of Peruvian coastal river basins C. Litty et al. 10.5194/esurf-5-571-2017
69. Controls on the grain size distribution of landslides in Taiwan: the influence of drop height, scar depth and bedrock strength O. Marc et al. 10.5194/esurf-9-995-2021
70. Spatial variation of surface erosion rate in a fault zone and its controlling factors X. Li et al. 10.1016/j.geomorph.2023.108802
71. Grain size bias in cosmogenic nuclide studies of stream sediment in steep terrain C. Lukens et al. 10.1002/2016JF003859
72. Temporal variability in detrital <sup>10</sup>Be concentrations in a large Himalayan catchment E. Dingle et al. 10.5194/esurf-6-611-2018
73. Reconceptualising flood risk assessment by incorporating sediment supply H. Liu et al. 10.1016/j.catena.2022.106503
74. Drainage Area, Bedrock Fracture Spacing, and Weathering Controls on Landscape‐Scale Patterns in Surface Sediment Grain Size A. Neely & R. DiBiase 10.1029/2020JF005560
75. Fluvial evacuation of landslide material from bedrock-confined channels under controlled experimental conditions E. Baynes et al. 10.1016/j.geomorph.2020.107359
76. Effects of deep‐seated versus shallow hillslope processes on cosmogenic 10Be concentrations in fluvial sand and gravel S. Tofelde et al. 10.1002/esp.4471
77. Downvalley fining of hillslope sediment in an alpine catchment: implications for downstream fining of sediment flux in mountain rivers L. Sklar et al. 10.1002/esp.4849
78. Understanding the Role of Rainfall and Hydrology in Determining Fluvial Erosion Efficiency E. Deal et al. 10.1002/2017JF004393
79. Long-profile evolution of transport-limited gravel-bed rivers A. Wickert & T. Schildgen 10.5194/esurf-7-17-2019
80. The role of infrequently mobile boulders in modulating landscape evolution and geomorphic hazards C. Shobe et al. 10.1016/j.earscirev.2021.103717
81. Investigation of stochastic-threshold incision models across a climatic and morphological gradient C. Desormeaux et al. 10.5194/esurf-10-473-2022
82. Consistent mineral-associated organic carbon chemistry with variable erosion rates in a mountainous landscape X. Wang et al. 10.1016/j.geoderma.2021.115448
83. The influence of coarse particle abundance and spatial distribution on sediment transport and cluster evolution in steep channels under sediment-starved conditions W. Li et al. 10.1016/j.catena.2023.107199
84. Spatial and temporal analysis of hillslope–channel coupling and implications for the longitudinal profile in a dryland basin K. Michaelides et al. 10.1002/esp.4340
85. Impact of recycling and lateral sediment input on grain size fining trends—Implications for reconstructing tectonic and climate forcings in ancient sedimentary systems R. Harries et al. 10.1111/bre.12349
86. Comparison of three grain size measuring methods applied to coarse-grained gravel deposits P. Garefalakis et al. 10.1016/j.sedgeo.2023.106340
87. Cosmogenic 10Be in river sediment: where grain size matters and why R. van Dongen et al. 10.5194/esurf-7-393-2019
88. Sediment size and abrasion biases in detrital thermochronology C. Lukens et al. 10.1016/j.epsl.2019.115929
89. The relationship between drainage density, erosion rate, and hilltop curvature: Implications for sediment transport processes F. Clubb et al. 10.1002/2015JF003747
90. Sediment controls on the transition from debris flow to fluvial channels in steep mountain ranges A. Neely & R. DiBiase 10.1002/esp.5553
91. Developing, choosing and using landscape evolution models to inform field‐based landscape reconstruction studies A. Temme et al. 10.1002/esp.4162
92. Conglomerate recycling in the Himalayan foreland basin: Implications for grain size and provenance L. Quick et al. 10.1130/B35334.1
93. Scale dependent spatial structuring of mountain river large bed elements maximizes flow resistance J. Wiener & G. Pasternack 10.1016/j.geomorph.2022.108431
94. Lithological controls on hillslope sediment supply: insights from landslide activity and grain size distributions D. Roda‐Boluda et al. 10.1002/esp.4281