Journal cover Journal topic
Earth Surface Dynamics An interactive open-access journal of the European Geosciences Union

Journal metrics

  • IF value: 2.649 IF 2.649
  • IF 5-year<br/> value: 2.688 IF 5-year
  • CiteScore<br/> value: 2.64 CiteScore
  • SNIP value: 0.628 SNIP 0.628
  • SJR value: indexed SJR
  • IPP value: 1.689 IPP 1.689
  • h5-index value: 6 h5-index 6
ESurf cover
Open access Public peer review Article level metrics Moderate APCs
Managing editor:

Editors: Frédéric Herman, Niels Hovius, Douglas Jerolmack, Andreas Lang & A. Joshua West

Earth Surface Dynamics (ESurf) is an international scientific journal dedicated to the publication and discussion of high-quality research on the physical, chemical, and biological processes shaping Earth's surface and their interactions on all scales.

The main subject areas of ESurf comprise field measurements, remote sensing, and experimental and numerical modelling of Earth surface processes, and their interactions with the lithosphere, biosphere, atmosphere, hydrosphere, and pedosphere. ESurf prioritizes studies with general implications for Earth surface science and especially values contributions that straddle discipline boundaries, enhance theory–observation feedback, and/or apply basic principles from physics, chemistry, or biology.


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15 Jun 2017

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New licence & copyright agreement

06 Jun 2017

From 6 June onwards, all newly submitted articles, if accepted for publication, will be distributed under the Creative Commons Attribution 4.0 International License.

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06 Jun 2017

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Recent articles

Highlight articles

Spatial bedrock erosion data from stream channels are important for engineering issues and landscape evolution model assessment. However, acquiring such data is challenging and only few data sets exist. Detecting changes in repeated photographs of painted bedrock surfaces easily allows for semi-quantitative conclusions on the spatial distribution of sediment transport and its effects: abrasion on surfaces facing the streamflow and shielding of surfaces by abundant sediment.

Alexander R. Beer, James W. Kirchner, and Jens M. Turowski

Rapid dissolution of bedrock and regolith mobilised by landslides can be an important control on rates of overall chemical weathering in mountain ranges. In this study we analysed a number of landslides and rivers in Taiwan to better understand why this occurs. We find that sulfuric acid resulting from rapid oxidation of highly reactive sulfides in landslide deposits drives the intense weathering and can set catchment-scale solute budgets. This could be a CO2 source in fast-eroding mountains.

R. Emberson, N. Hovius, A. Galy, and O. Marc

Accurately predicting gravel transport rates in mountain rivers is difficult because of feedbacks with channel morphology. River bed surfaces evolve during floods, influencing transport rates. I propose that the threshold of gravel motion is a state variable for channel reach evolution. I develop a new model to predict how transport thresholds evolve as a function of transport rate, and then use laboratory flume experiments to calibrate and validate the model.

J. P. L. Johnson

In regions formerly, or currently, covered by glaciers, landscapes have largely been shaped by glaciers. Glaciers erode bedrock through three main mechanisms: abrasion, quarrying, and subglacial meltwater erosion (SME). The latter, however, remains enigmatic. We present the first numerical modelling study of bedrock erosion by subglacial water and find that SME is negligible compared to abrasion and quarrying across the glacier, but its localization can explain the formation of bedrock channels.

F. Beaud, G. E. Flowers, and J. G. Venditti

A physical scale model of a gravel-bed braided river was used to measure vertical grain size sorting in the morphological active layer defined as the bed material between the maximum and minimum bed elevation. By normalizing active layer thickness and dividing into 10 sublayers we show that all grain sizes occur with almost equal frequency in all sublayers. Occurrence of patches and strings of coarser material relates to preservation of particular morphotextural features within the active layer.

P. Leduc, P. Ashmore, and J. T. Gardner

Publications Copernicus