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Record W3126115701 · doi:10.22215/etd/2017-11758

The ground thermal regime of the Peel Plateau, Northwest Territories, Canada

2017· dissertation· en· W3126115701 on OpenAlexaboutno aff
Hugh O'Neill

Bibliographic record

Venuenot available
Typedissertation
Languageen
FieldEarth and Planetary Sciences
TopicClimate change and permafrost
Canadian institutionsnot available
Fundersnot available
KeywordsPermafrostTundraPlateau (mathematics)SnowLeveeVegetation (pathology)Environmental scienceTerrainGeologyPhysical geographyHydrology (agriculture)GeomorphologyAtmospheric sciencesArcticGeotechnical engineeringGeography

Abstract

fetched live from OpenAlex

The ground thermal regime of continuous permafrost was investigated on Peel Plateau, Northwest Territories, Canada. Extensive road maintenance has been necessary on the Plateau due to the thaw of ground ice near the Dempster Highway road embankment. This thesis examines permafrost conditions in undisturbed terrain and in disturbed ground at the road embankment. Field data from 2010-15 provided a systematic examination of permafrost temperatures in forest and tundra vegetation on Peel Plateau and of the thermal disturbance from snow accumulation at the highway. Ground temperatures and measurements of associated controlling factors were used to characterize permafrost conditions across an elevational treeline in undisturbed settings. Permafrost conditions were also examined at the embankment toe and at a snow fence near the road to characterize disturbed ground thermal regimes in the region. Numerical simulations were calibrated with field measurements to assess the influence of varying snow accumulation characteristics (depth, density, rate, timing) on the evolution of ground temperatures at disturbed sites. Annual mean permafrost temperatures increased across treeline from about -2.5 ◦C in lowland forest to about -1.5 ◦C in tundra, coinciding with higher air temperatures due to winter inversions, and earlier snow accumulation at tundra sites. Rapid and deep snow accumulation at the road embankment toe has resulted in annual mean ground temperatures typically just below 0 ◦C, thaw depths in excess of 5 m, and the development of perennially unfrozen zones (taliks). Numerical simulations of the ground thermal regime closely reproduced measured temperatures near the road. This enabled the effect of limiting snow depth and increasing density to be investigated as a potential method to mitigate permafrost thaw. The simulations indicated that ground temperatures and thaw depths may thereby be significantly reduced at the embankment toe. The long-term disturbance to permafrost was then investigated in the field and simulated numerically in two dimensions at a snow fence near the road embankment. A talik developed under the fence after 25 years in the simulation. Permafrost thaw in the simulation continued for several decades without reaching equilibrium, demonstrating the sensitivity of warm permafrost to changes in surface conditions that initiate thermokarst.

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)0.000
metaresearch head score (Gemma)0.000
Version: metacan-v3-hybrid-931329e0061cValidation status: machine_predicted_unvalidated
Candidate categoriesnone
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Observational · Consensus signal: Observational
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.017
Threshold uncertainty score0.125

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0000.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0010.001
Science and technology studies0.0020.001
Scholarly communication0.0010.000
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 head0.018
GPT teacher head0.222
Teacher spread0.203 · 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 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

Citations0
Published2017
Admission routes1
Has abstractyes

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