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.

Standort
Deutsche Nationalbibliothek Frankfurt am Main
Umfang
Online-Ressource
Sprache
Englisch

Erschienen in
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)

Urheber
van der Sluijs, Jurjen
Kokelj, Steven V.
Tunnicliffe, Jon F.

DOI
10.5194/tc-17-4511-2023
URN
urn:nbn:de:101:1-2023110203152075470254
Rechteinformation
Open Access; Der Zugriff auf das Objekt ist unbeschränkt möglich.
Letzte Aktualisierung
14.08.2025, 10:48 MESZ

Datenpartner

Dieses Objekt wird bereitgestellt von:
Deutsche Nationalbibliothek. Bei Fragen zum Objekt wenden Sie sich bitte an den Datenpartner.

Beteiligte

  • van der Sluijs, Jurjen
  • Kokelj, Steven V.
  • Tunnicliffe, Jon F.

Ähnliche Objekte (12)