Allometric scaling of retrogressive thaw slumps
Abstract ± 1.0 m). An inverse association between RTS volume and relative volumetric error was observed, with uncertainties < < + + + R 2 n = 1522) but also revealed that elongated, shoreline RTS reflects outliers poorly represented by the modelling. These results indicate that variation in the allometric scaling of RTS populations is based on morphometry, terrain position, and complexity of the disturbance area, as well as the method and ontology by which slumps are inventoried. This study highlights the importance of linking field-based knowledge to feature identification and the utility of high-resolution DEMs in quantifying rates of RTS erosion beyond tracking changes in the planimetric area.
- Location
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Deutsche Nationalbibliothek Frankfurt am Main
- Extent
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Online-Ressource
- Language
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Englisch
- Bibliographic citation
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Allometric scaling of retrogressive thaw slumps ; volume:17 ; number:11 ; year:2023 ; pages:4511-4533 ; extent:23
The Cryosphere ; 17, Heft 11 (2023), 4511-4533 (gesamt 23)
- Creator
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van der Sluijs, Jurjen
Kokelj, Steven V.
Tunnicliffe, Jon F.
- DOI
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10.5194/tc-17-4511-2023
- URN
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urn:nbn:de:101:1-2023110203152075470254
- Rights
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Open Access; Der Zugriff auf das Objekt ist unbeschränkt möglich.
- Last update
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14.08.2025, 10:48 AM CEST
Data provider
Deutsche Nationalbibliothek. If you have any questions about the object, please contact the data provider.
Associated
- van der Sluijs, Jurjen
- Kokelj, Steven V.
- Tunnicliffe, Jon F.