Articles | Volume 4, issue 1
https://doi.org/10.5194/esurf-4-237-2016
https://doi.org/10.5194/esurf-4-237-2016
Research article
 | 
10 Mar 2016
Research article |  | 10 Mar 2016

Modelling sediment clasts transport during landscape evolution

Sébastien Carretier, Pierre Martinod, Martin Reich, and Yves Godderis

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Anderson, R. S.: Particle trajectories on hillslopes: Implications for particle age and Be-10 structure, J. Geophys. Res.-Earth, 120, 1626–1644, https://doi.org/10.1002/2015JF003479, 2015.
Anderson, S., Anderson, R., and Tucker, G.: Landscape scale linkages in critical zone evolution, C. R. Geosci., 344, 586–596, 2012.
Andreotti, B., Claudin, P., and Pouliquen, O.: Measurements of the aeolian sand transport saturation length, Geomorphology, 123, 343–348, https://doi.org/10.1016/j.geomorph.2010.08.002, 2010.
Andrews, D. J. and Hanks, T. C.: Scarp degraded by linear diffusion: Inverse solution for age, J. Geophys. Res., 90, 10193–10208, 1985.
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Short summary
We introduce moving clasts (grains, minerals, cobbles) in a landscape evolution model. This coupling has many potential applications, such as sediment provenance or the tracing of weathered material. It fills a gap between long-term landscape dynamics, which are difficult to tackle, and sediment clast populations studied in the field.