Articles | Volume 11, issue 2
https://doi.org/10.5194/esurf-11-227-2023
https://doi.org/10.5194/esurf-11-227-2023
Research article
 | 
24 Mar 2023
Research article |  | 24 Mar 2023

Patterns and rates of soil movement and shallow failures across several small watersheds on the Seward Peninsula, Alaska

Joanmarie Del Vecchio, Emma R. Lathrop, Julian B. Dann, Christian G. Andresen, Adam D. Collins, Michael M. Fratkin, Simon Zwieback, Rachel C. Glade, and Joel C. Rowland

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Cited articles

Alaska Climate Research Center Data Portal: https://akclimate.org/data/, last access: 23 February 2022. 
Andersen, J. L., Egholm, D. L., Knudsen, M. F., Jansen, J. D., and Nielsen, S. B.: The periglacial engine of mountain erosion – Part 1: Rates of frost cracking and frost creep, Earth Surf. Dynam., 3, 447–462, https://doi.org/10.5194/esurf-3-447-2015, 2015.  
Anderson, R. S.: Modeling the tor-dotted crests, bedrock edges, and parabolic profiles of high alpine surfaces of the Wind River Range, Wyoming, Geomorphology, 46, 35–58, 2002. 
Anderson, R. S., Anderson, S. P., and Tucker, G. E.: Rock damage and regolith transport by frost: an example of climate modulation of the geomorphology of the critical zone, Earth Surf. Proc. Land., 38, 299–316, https://doi.org/10.1002/esp.3330, 2013. 
Ballantyne, C. K.: A 35-Year record of solifluction in a maritime periglacial environment, Permafrost Periglac., 24, 56–66, https://doi.org/10.1002/ppp.1761, 2013. 
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Short summary
In cold regions of the Earth, thawing permafrost can change the landscape, impact ecosystems, and lead to the release of greenhouse gases. In this study we used many observational tools to better understand how sediment moves on permafrost hillslopes. Some topographic change conforms to our understanding of slope stability and sediment transport as developed in temperate landscapes, but much of what we observed needs further explanation by permafrost-specific geomorphic models.
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