SSF-Svalbard Science Forum
Thaw consolidation of permafrost soils in high-Arctic environments; RiS ID: 11815
The stability of permafrost soils is highly affected by the prevailing thermal regime. With warming ground temperatures and deepening of the active layer, thaw consolidation and associated ground subsidence are likely to occur. This is also expected for the surroundings of Ny-Ålesund, Svalbard.
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