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Record W1534880473 · doi:10.1002/ppp.1849

Eighteen Year Record of Forest Fire Effects on Ground Thermal Regimes and Permafrost in the Central Mackenzie Valley, NWT, Canada

2015· article· en· W1534880473 on OpenAlex

Why this work is in the frame

A frame that forgets how it found something cannot be audited. These are the routes that admitted this work.

affAt least one author lists a Canadian institution in the pinned OpenAlex snapshot.
fundA Canadian funder is recorded on the work.
aboutThe title or abstract carries a Canadian signal from the geographic lexicon.

Bibliographic record

VenuePermafrost and Periglacial Processes · 2015
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicClimate change and permafrost
Canadian institutionsGeological Survey of CanadaNatural Resources Canada
FundersAboriginal Affairs and Northern Development Canada
KeywordsPermafrostTransectGeologyActive layerBorealTaigaVegetation (pathology)InterceptionHydrology (agriculture)Environmental scienceSnowEvapotranspirationPhysical geographyGeomorphologyEcologyOceanographyForestryGeography

Abstract

fetched live from OpenAlex

Abstract Ground thermal conditions following a forest fire in 1994 were investigated along a hillslope transect in the discontinuous permafrost zone adjacent to a pipeline right of way in the central Mackenzie Valley, NWT, Canada. The intensity of the burn and damage to the forest and organic layer were more severe in the upper part of the slope than the bottom. Analysis of ground temperature records between 1995 and 2012 indicates that post‐fire changes to the surface altered the ground temperature regime, likely by allowing more snow to accumulate on the ground in winter (as interception by coniferous trees ceased) and decreasing albedo and evapotranspiration in summer. Active layer thickness at the affected site doubled between 1995 and 1998, before stabilising. Permafrost degradation likely occurred at the top of the slope, where burning was most severe. Towards the end of the study period, ground surface temperatures in the upper portion of the slope were lower than they were post fire (1997), whereas the surface temperatures were higher in the lower portion of the slope. In contrast, little to no change in surface temperature was observed for the Unburnt site. These changes in the burned sites are attributed to the increased re‐establishment of aspen, willow and tamarack in the upper part of the transect. Permafrost appears to be recovering at all burned sites in response to ongoing vegetation succession (except at the top of the slope), which is important for maintaining permafrost under conditions of projected climate warming in this boreal environment. Copyright © 2015 John Wiley & Sons, Ltd.

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.

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 categoriesnone
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Observational · Consensus signal: Observational
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.465
Threshold uncertainty score0.747

Codex and Gemma teacher scores by category

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

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 head0.023
GPT teacher head0.222
Teacher spread0.199 · 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