Articles | Volume 19, issue 6
https://doi.org/10.5194/tc-19-2037-2025
https://doi.org/10.5194/tc-19-2037-2025
Brief communication
 | 
10 Jun 2025
Brief communication |  | 10 Jun 2025

Brief communication: Mimicking periglacial landforms and processes in an ice-rich layered permafrost system with polydisperse melamine materials – a new concept

Emmanuel Léger, François Costard, Rémi Lambert, Albane Saintenoy, Antoine Séjourné, and Maxime Leblanc

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Brief communication: Monitoring active layer dynamics using a lightweight nimble ground-penetrating radar system – a laboratory analogue test case
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Cited articles

Ballantyne, C. K.: Periglacial geomorphology, John Wiley & Sons, 472 pp., ISBN 978-1-4051-0006-9, 2018. a
Costard, F., Dupeyrat, L., Séjourné, A., Bouchard, F., Fedorov, A., and Saint-Bézar, B.: Retrogressive Thaw Slumps on Ice-Rich Permafrost Under Degradation: Results From a Large-Scale Laboratory Simulation, Geophys. Res. Lett., 48, e2020GL091070, https://doi.org/10.1029/2020GL091070, 2020. a, b, c, d, e, f
Fiolleau, S., Uhlemann, S., Shirley, I. A., Wang, C., Wielandt, S., Rowland, J., and Dafflon, B.: Insights on seasonal solifluction processes in warm permafrost Arctic landscape using a dense monitoring approach across adjacent hillslopes, Environ. Res. Lett., 19, 044021, https://doi.org/10.1088/1748-9326/ad28dc, 2024. a
Gautier, E. and Costard, F.: Les systèmes fluviaux à chenaux anastomosés en milieu périglaciaire: la Léna et ses principaux affluents (Sibérie centrale), Géogr. Phys. Quatern., 54, 327–342, https://doi.org/10.7202/005647ar, 2000. a, b
Harris, C., Rea, B., and Davies, M.: Scaled physical modelling of mass movement processes on thawing slopes, Permafrost Periglac., 12, 125–135, 2001. a, b, c
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Short summary
This study explores the use of lightweight plastic particles to reproduce cryo-induced terrestrial geomorphologic features at the laboratory scale within an experiment on permafrost and active-layer thawing. We show that, due to their low density and peculiar hydrodynamic parameters, these lightweight particles, originally designed for river sediment deposition and erosion, are suitable for reproducing cryo-induced 3D geomorphological features found in terrestrial retrogressive thaw slumps.
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