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Record W4417346654 · doi:10.1002/ppp.70015

Permafrost Mass Wasting in Ice‐Rich Landscapes: Recent Advances (2013 to 2024) on Mechanisms, Dynamics and Impacts

2025· article· en· W4417346654 on OpenAlexafffundabout
Joseph M. Young, Louise Farquharson, Jing‐Jia Luo, Nina Nesterova, Jurjen van der Sluijs, Steven V. Kokelj

Bibliographic record

VenuePermafrost and Periglacial Processes · 2025
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicClimate change and permafrost
Canadian institutionsGovernment of Northwest TerritoriesUniversity of Alberta
FundersNatural Sciences and Engineering Research Council of CanadaScience Fund for Distinguished Young Scholars of Gansu ProvinceDeutscher Akademischer AustauschdienstNational Science Foundation
KeywordsPermafrostMass wastingLandformCircumpolar starClimate changeContext (archaeology)ArcticDebris

Abstract

fetched live from OpenAlex

ABSTRACT Across circumpolar permafrost regions, climate change is destabilizing ice‐rich hillslopes, increasing the frequency and magnitude of thaw‐driven mass wasting. This paper reviews recent studies (2013–2024) on thaw‐driven mass wasting, focusing on the processes, morphology and trajectories of geomorphic change and their implications for infrastructure, ecosystems and carbon impacts. Recent developments in monitoring and remote sensing approaches are also summarized. This review organizes mass wasting types along a continuum of top‐down (active‐layer detachment failures and retrogressive thaw slumps) and bottom‐up (deep‐seated permafrost landslides) mass movements and an intermediary class (frozen debris lobes) where the thermal evolution of permafrost more gradually modifies the behaviour of frozen slopes. Recent contributions and state of knowledge are summarized by distinct circumpolar regions of (1) northwestern Canada, (2) northwestern Russia, (3) the Qinghai–Tibet Plateau and (4) interior and northern Alaska to emphasize how geological legacy, physiography and climate influence variation in dominant modes of permafrost mass wasting. Critical geomorphic thresholds are surpassed across all regions, manifesting as a non‐linear increase in thaw‐driven mass wasting. The range of variation in processes and morphologies and the increasing complexity of mass wasting landforms are broadly related to geological legacy, which is controlled by ground ice, thermal, geomorphic and ecosystem factors, as well as their interaction with climate drivers. Knowledge of geological and climate controls on the different modes of slope failure and a field‐based understanding of process and form establishes critical context for considering future trajectories of permafrost landscape evolution, calibrating remote sensing observations, developing consistent monitoring methods and informing prediction of the environmental and engineering consequences. Lastly, we discuss remote sensing and machine learning applications to capture regional to global‐scale distributions and dynamics of mass wasting features. However, as permafrost landslide dynamics increase, so does the need for upscaling remote sensing and modelling efforts informed by a field‐based understanding of thaw‐driven mass wasting processes, creating opportunities for cross‐disciplinary and international collaboration.

Fetched live from OpenAlex and de-inverted. Abstracts are not stored in this database: the inverted indexes are 8.6 GB of the frame’s 9.3 GB of text, and the host has 13 GB free.

How this classification was reachedexpand

Full frame distilled prediction

Teacher imitation

Not calibrated prevalence, not ground truth. Human validation pending. Learned from the 10,348 direct Codex labels and 10,348 direct Gemma labels. Candidate is the union of thresholded teacher heads; consensus is their intersection. These outputs are machine_predicted_unvalidated and are not human labels or direct frontier model labels.

metaresearch head score (Codex)0.000
metaresearch head score (Gemma)0.000
Version: codex-gemma-dda1882f352aValidation status: machine_predicted_unvalidated
Candidate categoriesMeta-epidemiology (narrow), Insufficient payload (model declined to judge)
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Observational · Consensus signal: Observational
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.125
Threshold uncertainty score1.000

Codex and Gemma teacher scores by category

CategoryCodexGemma
Metaresearch0.0000.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0000.001
Science and technology studies0.0000.000
Scholarly communication0.0000.000
Open science0.0000.000
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.0020.000

Machine scores (provisional)

The two teacher heads of the student model, read on this work. A score orders the frame for review; it never asserts a category, and the validation status ships verbatim with every row.

Baseline scores from an immature model (maturity gate not passed, 7 training rounds). Scores rank; they never assert a category.

Opus teacher head0.014
GPT teacher head0.256
Teacher spread0.242 · how far apart the two teachers sit on this one work
Validation statusscore_only:v0-immature-baseline · verbatim from the scoring run: score_only means the number may rank works, and no category label ships from it

Classification

machine, unvalidated

Machine predicted; a candidate call from one teacher head, not a consensus.

Study designObservational
Domainnot available
GenreEmpirical

How this classification was reached, model by model and score by score, is at the end of the page under "How this classification was reached".

Quick stats

Citations2
Published2025
Admission routes3
Has abstractyes

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