Author
Listed:
- Chunli Dai
(University of Florida)
- Melissa K. Ward Jones
(University of Alaska Fairbanks)
- Jurjen van der Sluijs
(Government of Northwest Territories)
- Nina Nesterova
(Helmholtz Centre for Polar and Marine Research
University of Potsdam)
- Ian M. Howat
(The Ohio State University)
- Anna K. Liljedahl
(Woodwell Climate Research Center)
- Bretwood Higman
(Ground Truth Alaska)
- Jeffrey T. Freymueller
(Michigan State University)
- Steven V. Kokelj
(Government of Northwest Territories)
- Sindhura Sriram
(University of Florida)
Abstract
Retrogressive thaw slumping (RTS) is a mass-wasting process characterized by upslope backwasting and rapid thawing of ice-rich permafrost. High-resolution digital elevation models (DEMs) from ArcticDEM enable the volumetric and soil organic carbon quantification of medium to large disturbance areas undergoing RTS ( ≥10,000 m2) for the Northern Hemisphere. Using DEM time-series analysis and deep learning, we retrieve a total of 2747 disturbance areas undergoing active RTS with a total volume loss of (317.0 ± 0.3) × 106 m3 between 2012 and 2022. Here we show that climatic drivers of RTS activity exhibit latitudinal and regional variations, specifically, the number of precipitation-driven RTS decreases linearly as latitudes increase, whereas temperature-driven RTS increases sharply. Finally, we estimate that 96% of detected RTS thawed ~1.95 × 10–3 Pg carbon per year, equivalent to ~0.2% of annual gradual thaw emission estimates. Our results highlight the complexity of regional RTS dynamics and the importance of high resolution, long-term monitoring efforts.
Suggested Citation
Chunli Dai & Melissa K. Ward Jones & Jurjen van der Sluijs & Nina Nesterova & Ian M. Howat & Anna K. Liljedahl & Bretwood Higman & Jeffrey T. Freymueller & Steven V. Kokelj & Sindhura Sriram, 2025.
"Volumetric quantifications and dynamics of areas undergoing retrogressive thaw slumping in the Northern Hemisphere,"
Nature Communications, Nature, vol. 16(1), pages 1-16, December.
Handle:
RePEc:nat:natcom:v:16:y:2025:i:1:d:10.1038_s41467-025-62017-0
DOI: 10.1038/s41467-025-62017-0
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