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Record W7038475626

Impacts of wildfire on subcanopy energy balance, thermal regime, and permafrost stability in peat plateaus at Scotty Creek, Canada

2024· article· en· W7038475626 on OpenAlexaboutno aff

Bibliographic record

VenueScholars Commons (Wilfrid Laurier University) · 2024
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicClimate change and permafrost
Canadian institutionsnot available
Fundersnot available
KeywordsPermafrostPeatPlateau (mathematics)SnowpackHydrology (agriculture)SnowMoistureWater contentOverheating (electricity)Climate change
DOInot available

Abstract

fetched live from OpenAlex

The stability of permafrost in peatland-dominated regions of northwestern Canada is compromised by ongoing climate warming and increased wildfire activity. This study examines an 8-year record of changes to the surface and subsurface properties of a peat plateau following a low-severity wildfire that occurred in 2014 in a region of thawing, discontinuous permafrost. This is accomplished by comparing the burned portion of a peat plateau to two unburned control sites, one of which is the unburned portion of the same plateau that was affected by the fire. Net radiation was not significantly different one year following the wildfire but became increasingly larger at the Burn site in the following years, supplying a surplus of energy available for ground thaw. This increase in energy inputs coincided with the gradual collapse of the remaining standing dead trees, which is supported by a trend of increasing wind speeds. Soil moisture decreased at the Burn in the first 4 years post-fire before returning and maintaining similar moisture content as the adjacent control site. Ground temperatures were consistently warmer in the summer and colder in the winter compared to the adjacent control site. The cooler winter ground temperatures at the burn were attributed to the snowpack being thinner and denser, and thus less insulative, allowing for more energy to escape the subsurface during the winter seasons. This was not enough to offset the increased inputs of energy endured at the Burn over the summer seasons, as the depth to permafrost increased significantly over the study period and no trend was found for the control sites. The average annual rate of permafrost thaw was 9.6 cm/year at the Burn, compared to 5.6 cm/year at the nearby adjacent control site. The most notable finding was a near-continuous talik (perennially frozen) layer beneath the Burn, a feature known to further accelerate permafrost thaw. The thinner active layer at the Burn required less energy to thaw, leaving more energy available to drive other subsurface processes such as increasing ground temperatures and contributing to greater thaw. The combined impacts of the variables examined suggest that wildfire in this area exacerbates permafrost thaw.

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 score0.057
Threshold uncertainty score0.115

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 studies0.0020.000
Scholarly communication0.0010.000
Open science0.0000.000
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.0010.000

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 head0.015
GPT teacher head0.193
Teacher spread0.177 · 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
Published2024
Admission routes1
Has abstractyes

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