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The Cryosphere An interactive open-access journal of the European Geosciences Union
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Volume 12, issue 2
The Cryosphere, 12, 549–564, 2018
https://doi.org/10.5194/tc-12-549-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
The Cryosphere, 12, 549–564, 2018
https://doi.org/10.5194/tc-12-549-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.

Research article 14 Feb 2018

Research article | 14 Feb 2018

Sub-seasonal thaw slump mass wasting is not consistently energy limited at the landscape scale

Simon Zwieback et al.

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Cited articles

Aylsworth, J. M., Burgess, M. M., Desrochers, D. T., Duk-Rodkin, A., Robertson, T., and Traynor, J. A.: Surficial geology, subsurface materials, and thaw sensitivity of sediments, in: The Physical Environment of the Mackenzie Valley, Northwest Territories: A Base Line for the Assessment of Environmental Change, vol. 547, pp. 41–48, Geological Survey of Canada, 2000.
Balser, A. W., Jones, J. B., and Gens, R.: Timing of retrogressive thaw slump initiation in the Noatak Basin, northwest Alaska, USA, J. Geophys. Res.-Earth, 119, 1106–1120, https://doi.org/10.1002/2013JF002889, 2014.
Bamler, R. and Hartl, P.: Synthetic aperture radar interferometry, Inverse Probl., 14, 1–54, 1998.
Barnhart, T.: Morphodynamics of the Selawik Retrogressive Thaw Slump, Northwest Alaska, Master's thesis, Idaho State University, 2013.
Boike, J., Kattenstroth, B., Abramova, K., Bornemann, N., Chetverova, A., Fedorova, I., Fröb, K., Grigoriev, M., Grüber, M., Kutzbach, L., Langer, M., Minke, M., Muster, S., Piel, K., Pfeiffer, E.-M., Stoof, G., Westermann, S., Wischnewski, K., Wille, C., and Hubberten, H.-W.: Baseline characteristics of climate, permafrost and land cover from a new permafrost observatory in the Lena River Delta, Siberia (1998–2011), Biogeosciences, 10, 2105–2128, https://doi.org/10.5194/bg-10-2105-2013, 2013.
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We analyse elevation losses at thaw slumps, at which icy sediments are exposed. As ice requires a large amount of energy to melt, one would expect that mass wasting is governed by the available energy. However, we observe very little mass wasting in June, despite the ample energy supply. Also, in summer, mass wasting is not always energy limited. This highlights the importance of other processes, such as the formation of a protective veneer, in shaping mass wasting at sub-seasonal scales.
We analyse elevation losses at thaw slumps, at which icy sediments are exposed. As ice requires...
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