Retrogressive thaw slump susceptibility in the northern hemisphere permafrost region

Mean annual temperatures in the Arctic and subarctic have increased in recent decades, increasing the number of permafrost hazards. Retrogressive thaw slumps (RTSs), triggered by the thawing of ground ice in permafrost soil, have become more common in the Arctic. Many studies report an increase in R...

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Bibliographic Details
Published in:Earth Surface Processes and Landforms
Main Authors: Makopoulou, Eirini, Karjalainen, Olli, Elia, Letizia, Blais-Stevens, Andrée, Lantz, Trevor, Lipovsky, Panya, Lombardo, Luigi, Nicu, Ionut Cristi, Rubensdotter, Brita Lena Eleonor Fredin, Rudy, Ashley C.A., Hjort, Jan
Format: Article in Journal/Newspaper
Language:English
Published: 2024
Subjects:
Ice
Online Access:https://hdl.handle.net/11250/3131509
https://doi.org/10.1002/esp.5890