Earth Surface Dynamics

Papers
(The median citation count of Earth Surface Dynamics is 3. The table below lists those papers that are above that threshold based on CrossRef citation counts [max. 250 papers]. The publications cover those that have been published in the past four years, i.e., from 2022-05-01 to 2026-05-01.)
ArticleCitations
Effect of debris-flow sediment grain-size distribution on fan morphology40
Evolution of submarine canyons and hanging-wall fans: insights from geomorphic experiments and morphodynamic models34
Using repeat UAV-based laser scanning and multispectral imagery to explore eco-geomorphic feedbacks along a river corridor29
Discriminating fluvial fans and deltas: channel network morphometrics reflect distinct formative processes29
Path length and sediment transport estimation from DEMs of difference: a signal processing approach27
The direction of landscape erosion27
Modeling the inhibition effect of straw checkerboard barriers on wind-blown sand25
Modeling memory in gravel-bed rivers: a flow-history-dependent relation for evolving thresholds of motion22
Quantification of post-glacier bedrock surface erosion in the European Alps using 10 Be and optically stimulated luminescence exposure dating22
A simple model for faceted topographies at normal faults based on an extended stream-power law21
Toward a general calibration of the Swiss plate geophone system for fractional bedload transport21
Investigating controls on fluvial grain sizes in post-glacial landscapes using citizen science18
Barchan swarm dynamics from a Two-Flank Agent-Based Model18
A novel acoustic bedload monitoring system with phased microphone arrays and an accelerometer for particle localization and size estimation18
Numerical modelling of the evolution of a river reach with a complex morphology to help define future sustainable restoration decisions17
The effect of lithology on the relationship between denudation rate and chemical weathering pathways – evidence from the eastern Tibetan Plateau17
Investigating the celerity of propagation for small perturbations and dispersive sediment aggradation under a supercritical flow16
Post-glacial reshaping of Alpine topography induced by landsliding16
Constraints on long-term cliff retreat and intertidal weathering at weak rock coasts using cosmogenic 10 Be, nearshore topography and numerical model15
Investigation of stochastic-threshold incision models across a climatic and morphological gradient14
Limited influence of bedrock strength on river profiles: the dominant role of sediment dynamics14
Water level fluctuations drive bank instability in a hypertidal estuary13
Dimensionless argument: a narrow grain size range near 2 mm plays a special role in river sediment transport and morphodynamics13
Estimating surface water availability in high mountain rock slopes using a numerical energy balance model13
The roles of surface processes in porphyry copper deposit preservation12
Late Pleistocene–Holocene denudation, uplift, and morphology evolution of the Armorican Massif (western Europe)12
Mineral surface area in deep weathering profiles reveals the interrelationship of iron oxidation and silicate weathering12
Automated classification of seismic signals recorded on the Åknes rock slope, Western Norway, using a convolutional neural network12
An overview of sedimentary volcanism on Mars12
An efficient approach for inverting rock exhumation from thermochronologic age–elevation relationship12
Experimental study on granite-weathered crust landslides with different residual layer thicknesses under heavy rainfall11
A combined approach of experimental and numerical modeling for 3D hydraulic features of a step-pool unit11
Development of a machine learning model for river bed load11
Building a bimodal landscape: bedrock lithology and bed thickness controls on the morphology of Last Chance Canyon, New Mexico, USA11
Cirque-like alcoves in the northern mid-latitudes of Mars as evidence of glacial erosion11
Unraveling the hydrology and sediment balance of an ungauged lake in the Sudano-Sahelian region of West Africa using remote sensing11
Erosion and weathering in carbonate regions reveal climatic and tectonic drivers of carbonate landscape evolution10
Shape evolution of bulk sediment in headwater streams: effects of rock type and particle size10
The influence of dune lee side shape on time-averaged velocities and turbulence10
Statistical characterization of erosion and sediment transport mechanics in shallow tidal environments – Part 2: Suspended sediment dynamics10
Morphological response to climate-induced flood-event variability in a subarctic river10
Entrainment and deposition of boulders in a gravel bed river10
Grain size dynamics using a new planform model – Part 1: GravelScape description and validation10
Past anthropogenic land use change caused a regime shift of the fluvial response to Holocene climate change in the Chinese Loess Plateau9
Stream laws in analog tectonic-landscape models9
Biogeomorphic modeling to assess the resilience of tidal-marsh restoration to sea level rise and sediment supply9
Use of simple analytical solutions in the calibration of shallow water equation debris flow models9
Rockfall trajectory reconstruction: a flexible method utilizing video footage and high-resolution terrain models9
Downstream rounding rate of pebbles in the Himalaya9
Geology and vegetation control landsliding on forest-managed slopes in scarplands9
Shape still matters: rockfall interactions with trees and deadwood in a mountain forest uncover a new facet of rock shape dependency9
Improving a multi-grain-size total sediment load model through a new standardized reference shear stress for incipient motion and an adjusted saltation height description9
A physics-based model for fluvial valley width9
Grain size dynamics using a new planform model – Part 2: Determining the relative control of autogenic processes and subsidence9
Multi-sensor monitoring and data integration reveal cyclical destabilization of the Äußeres Hochebenkar rock glacier9
Response of modern fluvial sediments to regional tectonic activity along the upper Min River, eastern Tibet8
Massive sediment pulses triggered by a multi-stage 130 000 m 3 alpine cliff fall (Hochvogel, DE–AT)8
Constraining the timing and processes of pediment formation and dissection: implications for long-term evolution in the Western Cape, South Africa8
Comparison of calibration characteristics of different acoustic impact systems for measuring bedload transport in mountain streams8
On the testing of grain shape corrections to bedload transport equations with grain-resolved numerical simulations8
Reconstructing landscapes: an adjoint model of the stream power and diffusion erosion equation8
Ice-buttressing-controlled rock slope failure on a cirque headwall, Lake District, UK8
Short communication: Multiscale topographic complexity analysis with pyTopoComplexity7
Landscape response to tectonic deformation and cyclic climate change since ca. 800 ka in the southern central Andes7
Introducing standardized field methods for fracture-focused surface process research7
Rainfall and tectonic forcing lead to contrasting headwater slope evolutions7
Optimization of passive acoustic bedload monitoring in rivers by signal inversion7
Drainage rearrangement in an intra-continental mountain belt: a case study from the central South Tian Shan, Kyrgyzstan7
Bedload transport fluctuations, flow conditions, and disequilibrium ratio at the Swiss Erlenbach stream: results from 27 years of high-resolution temporal measurements7
Short communication: Forward and inverse analytic models relating river long profile to tectonic uplift history, assuming a nonlinear slope–erosion dependency7
Climate changes and the formation of fluvial terraces in central Amazonia inferred from landscape evolution modeling7
Knickpoints and fixed points: the evolution of fluvial morphology under the combined effect of fault uplift and dam obstruction on a soft bedrock river6
Quantifying the migration rate of drainage divides from high-resolution topographic data6
Spatial and temporal variations in rockwall erosion rates derived from cosmogenic 10 Be in medial moraines at five valley glaciers around Pigne d'Aro6
Flexural isostatic response of continental-scale deltas to climatically driven sea level changes6
Experimental study of time-averaged flow and turbulence over asymmetric tidal dunes6
On the relative role of abiotic and biotic controls in channel network development: insights from scaled tidal flume experiments6
Sediment source and sink identification using Sentinel-2 and a small network of turbidimeters on the Vjosa River6
Probabilistic description of bedload fluxes from the aggregate dynamics of individual grains6
Episodic sediment supply to alluvial fans: implications for fan incision and morphometry6
Self-organization of channels and hillslopes in models of fluvial landform evolution and its potential for solving scaling issues6
At-a-site and between-site variability of bedload transport, inferred from continuous surrogate monitoring, and comparison to predictive equations6
Modeling deadwood for rockfall mitigation assessments in windthrow areas6
Progressive destabilization of a freestanding rock pillar in permafrost on the Matterhorn (Swiss Alps): Hydro-mechanical modeling and analysis5
Size, shape and orientation matter: fast and semi-automatic measurement of grain geometries from 3D point clouds5
Cosmogenic nuclide-derived downcutting rates of canyons within large limestone plateaus of southern Massif Central (France) reveal a different regional speleogenesis of karst networks5
Spatial assessment of sediment production in a badland catchment using repeat LiDAR surveys, Draix, Alpes de Haute-Provence, France5
Slow-moving rock glaciers in marginal periglacial environment of Southern Carpathians5
Short communication: A tool for determining multiscale bedform characteristics from bed elevation data5
Grain size of fluvial gravel bars from close-range UAV imagery – uncertainty in segmentation-based data5
Continuous measurements of valley floor width in mountainous landscapes5
Modeling the formation of toma hills based on fluid dynamics with a modified Voellmy rheology5
Mobile evaporite enhances the cycle of physical–chemical erosion in badlands5
Scaling between volume and runout of rock avalanches explained by a modified Voellmy rheology5
Machine learning prediction of the mass and the velocity of controlled single-block rockfalls from the seismic waves they generate5
The probabilistic nature of dune collisions in 2D5
Time-varying drainage basin development and erosion on volcanic edifices5
Short communication: Concentrated impacts by tree canopy drips – hotspots of soil erosion in forests5
The glacial paleolandscapes of Southern Africa: the legacy of the Late Paleozoic Ice Age5
A numerical model for duricrust formation by laterisation4
Translating deposition ages into erosion rates: inverse landscape evolution modelling and uncertainty analysis4
Patterns and rates of soil movement and shallow failures across several small watersheds on the Seward Peninsula, Alaska4
Old orogen–young topography: lithological contrasts controlling erosion and relief formation in the Bohemian Massif4
Spatially coherent variability in modern orographic precipitation produces asymmetric paleo-glacier extents in flowline models: Olympic Mountains, USA4
GraphFlood 1.0: an efficient algorithm to approximate 2D hydrodynamics for landscape evolution models4
Biomechanical parameters of marram grass ( Calamagrostis arenaria ) for advanced modeling of dune vegetation4
Development of the morphodynamics on Little Ice Age lateral moraines in 10 glacier forefields of the Eastern Alps since the 1950s4
Terrace formation linked to outburst floods at the Diexi palaeo-landslide dam, upper Minjiang River, eastern Tibetan Plateau4
Role of the forcing sources in morphodynamic modelling of an embayed beach4
The impact of bedrock meander cutoffs on 50 kyr scale incision rates, San Juan River, Utah4
Identifying fracture-controlled resonance modes for structural health monitoring: insights from Hunter Canyon Arch (Utah, USA)4
Analysis of autogenic bifurcation processes resulting in river avulsion4
Curvature-based pebble segmentation for reconstructed surface meshes4
Combining seismic signal dynamic inversion and numerical modeling improves landslide process reconstruction4
Higher sediment redistribution rates related to burrowing animals than previously assumed as revealed by time-of-flight-based monitoring4
Localised geomorphic response to channel-spanning leaky wooden dams4
Geospatial modelling of large-wood supply to rivers: a state-of-the-art model comparison in Swiss mountain river catchments4
Effect of hydro-climate variation on biofilm dynamics and its impact in intertidal environments4
Short communication: Potential of Sentinel-1 interferometric synthetic aperture radar (InSAR) and offset tracking in monitoring post-cyclonic landslide activities on Réunion4
Stream hydrology controls on ice cliff evolution and survival on debris-covered glaciers3
MPeat2D – a fully coupled mechanical–ecohydrological model of peatland development in two dimensions3
A landslide runout model for sediment transport, landscape evolution, and hazard assessment applications3
Equilibrium distance from long-range dune interactions3
Subaerial and subglacial seismic characteristics of the largest measured jökulhlaup from the eastern Skaftá cauldron, Iceland3
New experiments to probe the role of fractures in bedrock on river erosion rate and processes3
Evaluating the accuracy of binary classifiers for geomorphic applications3
Feedbacks between the formation of secondary minerals and the infiltration of fluids into the regolith of granitic rocks in different climatic zones (Chilean Coastal Cordillera)3
Testing floc settling velocity models in rivers and freshwater wetlands3
Influence of network geometry on long-term morphodynamics of alluvial rivers3
An extrapolation algorithm for estimating river bed grain size distributions across basins3
Influence of cohesive clay on wave–current ripple dynamics captured in a 3D phase diagram3
Automated riverbed composition analysis using deep learning on underwater images3
Safeguarding Cultural Heritage: Integrating laser scanning, InSAR, vibration monitoring and rockfall/granular flow runout modelling at the Temple of Hatshepsut, Egypt3
Spatiotemporal bedload transport patterns over two-dimensional bedforms3
Width evolution of channel belts as a random walk3
Optimising global landscape evolution models with 10 Be3
Yukon River incision drove organic carbon burial in the Bering Sea during global climate changes at 2.6 and 1 Ma3
Haloturbation in the northern Atacama Desert revealed by a hidden subsurface network of calcium sulfate wedges3
Morphologic and morphometric differences between gullies formed in different substrates on Mars: new insights into the gully formation processes3
Topographic metrics for unveiling fault segmentation and tectono-geomorphic evolution with insights into the impact of inherited topography, Ulsan Fault Zone, South Korea3
Suspended sediment and discharge dynamics in a glaciated alpine environment: identifying crucial areas and time periods on several spatial and temporal scales in the Ötztal, Austria3
Long-runout landslides with associated longitudinal ridges in Iceland as analogues of Martian landslide deposits3
TerraceM-3: integrating machine learning and ICESat-2 altimetry to estimate deformation rates from wave-abrasion terraces3
Geophysical evidence of massive hyperconcentrated push waves with embedded toma hills caused by the Flims rockslide, Switzerland3
Multiple equilibrium configurations in river-dominated deltas3
Decadal-scale decay of landslide-derived fluvial suspended sediment after Typhoon Morakot3
Failure mode of rainfall-induced landslide of granite residual soil, southeastern Guangxi Province, China3
Channel concavity controls planform complexity of branching drainage networks3
Field monitoring of pore water pressure in fully and partly saturated debris flows at Ohya landslide scar, Japan3
Geomorphic imprint of high-mountain floods: insights from the 2022 hydrological extreme across the upper Indus River catchment in the northwestern Himalayas3
Spatiotemporal dynamics of Sentinel-2 NDVI as indicators of bio-hydromorphological interactions: implications for river management3
Alpine hillslope failure in the western US: insights from the Chaos Canyon landslide, Rocky Mountain National Park, USA3
An evaluation of flow-routing algorithms for calculating contributing area on regular grids3
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