Earth Surface Dynamics

Papers
(The H4-Index of Earth Surface Dynamics is 18. 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 2021-09-01 to 2025-09-01.)
ArticleCitations
Using repeat UAV-based laser scanning and multispectral imagery to explore eco-geomorphic feedbacks along a river corridor56
Evolution of submarine canyons and hanging-wall fans: insights from geomorphic experiments and morphodynamic models36
Path length and sediment transport estimation from DEMs of difference: a signal processing approach31
From apex to shoreline: fluvio-deltaic architecture for the Holocene Rhine–Meuse delta, the Netherlands29
The direction of landscape erosion28
Effect of debris-flow sediment grain-size distribution on fan morphology27
Quantification of post-glacier bedrock surface erosion in the European Alps using10Be and optically stimulated luminescence exposure dating23
Modeling memory in gravel-bed rivers: a flow-history-dependent relation for evolving thresholds of motion23
The effect of lithology on the relationship between denudation rate and chemical weathering pathways – evidence from the eastern Tibetan Plateau22
Modeling the inhibition effect of straw checkerboard barriers on wind-blown sand22
Barchan swarm dynamics from a Two-Flank Agent-Based Model22
Toward a general calibration of the Swiss plate geophone system for fractional bedload transport21
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 vibrations20
A simple model for faceted topographies at normal faults based on an extended stream-power law19
Landslide-lake outburst floods accelerate downstream hillslope slippage19
Comparing the transport-limited and ξ–q models for sediment transport18
Investigation of stochastic-threshold incision models across a climatic and morphological gradient18
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