MétaCan
Menu
← Back to cohort
Record W4408433950 · doi:10.5194/egusphere-egu25-11426

Global, consistent, and efficient production of transient permafrost ensemble simulations for investigating climatic influences on slope failures

2025· preprint· en· W4408433950 on OpenAlexaffabout
Victor Pozsgay, Stephan Gruber, Nicholas Brown

Bibliographic record

Venuenot available
Typepreprint
Languageen
FieldEarth and Planetary Sciences
TopicClimate change and permafrost
Canadian institutionsCarleton University
Fundersnot available
KeywordsPermafrostTransient (computer programming)Environmental scienceProduction (economics)ClimatologyMeteorologyGeologyComputer scienceGeographyEconomicsOceanography

Abstract

fetched live from OpenAlex

The magnitude and frequency of slope failures in permafrost zones have increased in recent decades. Permafrost warming and thawing represent major contributing factors to large slope failures, which have the potential to damage infrastructure and pose a risk to human life and surrounding ecosystems. Understanding the link between permafrost thaw and slope movement is thus crucial for identifying and adapting to related geohazards and increasing public safety in mountain communities.We aim to provide quantitative and time-dependent context for interpreting past events and establish correlations between slope failures and potential driving factors, such as changes in air temperatures, ground temperatures, thaw depth, and water availability. We demonstrate our system by investigating the change in these driving factors and their connection with recent slope movements in northern British Columbia and the Yukon.We developed a simulation workflow to generate 1D ensemble simulations of the ground thermal regime at any point globally, whose parameterization is helped by in-situ observations where available. Furthermore, we model temperature inversions in sub-arctic valleys where cold-air pooling is particularly intense in cold months and use it to correct 75 years of atmospheric reanalysis data forcing, increasing the accuracy and reliability of our results. We then produce summary statistics of drivers at permafrost landslide sites. This full-scale analysis is carried out for sites with varying degrees of remoteness, topographic parameters, and atmospheric conditions, producing an ‘ensemble’ of simulations. This framework allows for consistent and efficient production and analysis of mountain permafrost simulations in relation to slope failures. However, its main strength and appeal lie in its ability to be used globally and for a large number of sites, efficiently. Most workflows are contained in the Python packages SuPerSim and GlobSim, new packages for model testing and for producing climate change scenarios are added.We observe a general increase in extreme events in the variables we analyze compared to earlier decades, and we correlate their timings with those of landslides. Such research may help establish proxies for permafrost landslide preconditioning and triggers, providing a tool to support research and prediction concerning hazards in mountain terrain.

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 machine prediction

Teacher imitation

Not calibrated prevalence, not ground truth. Human validation pending. The Gemma side is a direct model label for every work in the frame, read from the title-only record. The Codex side is a classifier learned from the 10,348 direct Codex labels and calibrated to design-weighted sample rates; fields without enough sample support carry no Codex call. Candidate is the union of the two sides; consensus is their intersection. These outputs are machine_predicted_unvalidated and are not human labels.

metaresearch head score (Codex)0.001
metaresearch head score (Gemma)0.003
Version: metacan-v3-hybrid-931329e0061cValidation status: machine_predicted_unvalidated
Candidate categoriesnone
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Simulation or modeling · Consensus signal: Simulation or modeling
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.039
Threshold uncertainty score0.077

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0010.003
Meta-epidemiology (narrow)0.0010.000
Meta-epidemiology (broad)0.0010.001
Bibliometrics0.0010.001
Science and technology studies0.0010.000
Scholarly communication0.0010.001
Open science0.0010.001
Research integrity0.0010.001
Insufficient payload (model declined to judge)0.0030.001

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 head0.061
GPT teacher head0.298
Teacher spread0.237 · 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 source (direct Gemma or distilled Codex), not a consensus.

The models applied no category: nothing in the taxonomy fit this work.
Study designSimulation or modeling
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

Citations0
Published2025
Admission routes2
Has abstractyes

Explore more

Same topicClimate change and permafrost→French-language works237,207→