Earth Surface Dynamics

Papers
(The TQCC of Earth Surface Dynamics is 7. 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 2021-05-01 to 2025-05-01.)
ArticleCitations
Bedrock river erosion through dipping layered rocks: quantifying erodibility through kinematic wave speed54
Using repeat UAV-based laser scanning and multispectral imagery to explore eco-geomorphic feedbacks along a river corridor31
Evolution of submarine canyons and hanging-wall fans: insights from geomorphic experiments and morphodynamic models30
From apex to shoreline: fluvio-deltaic architecture for the Holocene Rhine–Meuse delta, the Netherlands28
Modeling the inhibition effect of straw checkerboard barriers on wind-blown sand27
The direction of landscape erosion27
Climatic controls on mountain glacier basal thermal regimes dictate spatial patterns of glacial erosion26
Effect of debris-flow sediment grain-size distribution on fan morphology25
Path length and sediment transport estimation from DEMs of difference: a signal processing approach23
Quantification of post-glacier bedrock surface erosion in the European Alps using10Be and optically stimulated luminescence exposure dating22
Implications of the ongoing rock uplift in NW Himalayan interiors21
Barchan swarm dynamics from a Two-Flank Agent-Based Model21
Landslide-lake outburst floods accelerate downstream hillslope slippage21
Numerical modelling of the evolution of a river reach with a complex morphology to help define future sustainable restoration decisions20
An update on techniques to assess normal-mode behavior of rock arches by ambient vibrations19
The effect of lithology on the relationship between denudation rate and chemical weathering pathways – evidence from the eastern Tibetan Plateau18
A simple model for faceted topographies at normal faults based on an extended stream-power law18
Constraints on long-term cliff retreat and intertidal weathering at weak rock coasts using cosmogenic 10Be, nearshore topography and numerical modelling17
Toward a general calibration of the Swiss plate geophone system for fractional bedload transport17
Relationship between meteoric 10Be and NO3 concentrations in soils along Shackleton Glacier, Antarctica17
Investigation of stochastic-threshold incision models across a climatic and morphological gradient16
Estimating surface water availability in high mountain rock slopes using a numerical energy balance model15
Comparing the transport-limited and ξq models for sediment transport15
An overview of sedimentary volcanism on Mars15
Automated quantification of floating wood pieces in rivers from video monitoring: a new software tool and validation15
Mineral surface area in deep weathering profiles reveals the interrelationship of iron oxidation and silicate weathering14
Development of a machine learning model for river bed load14
An efficient approach for inverting rock exhumation from thermochronologic age–elevation relationship14
Assessing the effect of topography on Cs-137 concentrations within forested soils due to the Fukushima Daiichi Nuclear Power Plant accident, Japan13
Automated classification of seismic signals recorded on the Åknes rock slope, Western Norway, using a convolutional neural network13
Dimensionless argument: a narrow grain size range near 2 mm plays a special role in river sediment transport and morphodynamics13
Water level fluctuations drive bank instability in a hypertidal estuary13
Modeling glacial and fluvial landform evolution at large scales using a stream-power approach13
A hybrid data–model approach to map soil thickness in mountain hillslopes12
Entrainment and deposition of boulders in a gravel bed river12
Relevance of acoustic methods to quantify bedload transport and bedform dynamics in a large sandy-gravel-bed river12
Statistical characterization of erosion and sediment transport mechanics in shallow tidal environments – Part 2: Suspended sediment dynamics12
A combined approach of experimental and numerical modeling for 3D hydraulic features of a step-pool unit12
Building a bimodal landscape: bedrock lithology and bed thickness controls on the morphology of Last Chance Canyon, New Mexico, USA12
Unraveling the hydrology and sediment balance of an ungauged lake in the Sudano-Sahelian region of West Africa using remote sensing12
The influence of dune lee side shape on time-averaged velocities and turbulence11
Rockfall trajectory reconstruction: a flexible method utilizing video footage and high-resolution terrain models11
Erosion and weathering in carbonate regions reveal climatic and tectonic drivers of carbonate landscape evolution11
A physics-based model for fluvial valley width10
Downstream rounding rate of pebbles in the Himalaya10
Stream laws in analog tectonic-landscape models10
Short communication: Runout of rock avalanches limited by basal friction but controlled by fragmentation10
Shape still matters: rockfall interactions with trees and deadwood in a mountain forest uncover a new facet of rock shape dependency9
Geology and vegetation control landsliding on forest-managed slopes in scarplands9
Ice-buttressing-controlled rock slope failure on a cirque headwall, Lake District, UK9
Multi-sensor monitoring and data integration reveal cyclical destabilization of the Äußeres Hochebenkar rock glacier9
Comparison of calibration characteristics of different acoustic impact systems for measuring bedload transport in mountain streams9
Past anthropogenic land use change caused a regime shift of the fluvial response to Holocene climate change in the Chinese Loess Plateau9
Biogeomorphic modeling to assess the resilience of tidal-marsh restoration to sea level rise and sediment supply9
Graphically interpreting how incision thresholds influence topographic and scaling properties of modeled landscapes9
Massive sediment pulses triggered by a multi-stage 130 000 m3 alpine cliff fall (Hochvogel, DE–AT)9
Short communication: Forward and inverse analytic models relating river long profile to tectonic uplift history, assuming a nonlinear slope–erosion dependency8
Response of modern fluvial sediments to regional tectonic activity along the upper Min River, eastern Tibet8
Flexural isostatic response of continental-scale deltas to climatically driven sea level changes8
Constraining the timing and processes of pediment formation and dissection: implications for long-term evolution in the Western Cape, South Africa8
Landscape response to tectonic deformation and cyclic climate change since ca. 800 ka in the southern central Andes8
Pulsed carbon export from mountains by earthquake-triggered landslides explored in a reduced-complexity model8
Climate changes and the formation of fluvial terraces in central Amazonia inferred from landscape evolution modeling8
Bedload transport fluctuations, flow conditions, and disequilibrium ratio at the Swiss Erlenbach stream: results from 27 years of high-resolution temporal measurements8
Optimization of passive acoustic bedload monitoring in rivers by signal inversion8
The landslide velocity8
Sediment source and sink identification using Sentinel-2 and a small network of turbidimeters on the Vjosa River8
Modeling deadwood for rockfall mitigation assessments in windthrow areas7
Controls on the grain size distribution of landslides in Taiwan: the influence of drop height, scar depth and bedrock strength7
Drainage rearrangement in an intra-continental mountain belt: a case study from the central South Tian Shan, Kyrgyzstan7
Spatial and temporal variations in rockwall erosion rates derived from cosmogenic 10Be in medial moraines at five valley glaciers around Pigne d'Arolla, Switzerland7
Probabilistic description of bedload fluxes from the aggregate dynamics of individual grains7
Self-organization of channels and hillslopes in models of fluvial landform evolution and its potential for solving scaling issues7
Knickpoints and fixed points: the evolution of fluvial morphology under the combined effect of fault uplift and dam obstruction on a soft bedrock river7
Introducing standardized field methods for fracture-focused surface process research7
Continuous measurements of valley floor width in mountainous landscapes7
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