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Record W3092437000 · doi:10.22215/etd/2015-10757

Permafrost and Thermokarst Lake Dynamics in the Old Crow Flats, Northern Yukon, Canada

2015· dissertation· en· W3092437000 on OpenAlexaboutno aff
Pascale Roy‐Léveillée

Bibliographic record

Venuenot available
Typedissertation
Languageen
FieldEarth and Planetary Sciences
TopicClimate change and permafrost
Canadian institutionsnot available
Fundersnot available
KeywordsThermokarstPermafrostShoreSnowHydrology (agriculture)GeologyPhysical geographyTundraVegetation (pathology)EcotoneGeomorphologyArcticOceanographyGeographyEcology

Abstract

fetched live from OpenAlex

Aspects of the thaw lake cycle were investigated in Old Crow Flats (OCF), a 5600 km2 peatland with thousands of thermokarst lakes in the continuous permafrost of northern Yukon. It is located in the traditional territory of the Vuntut Gwitch'n, who expressed concern that climatic change may be affecting the permafrost and lakes of OCF. Field data collected in 2008-2011 provided the first assessment of spatial variability in permafrost temperatures across the treeline ecotone in OCF. Lake-bottom temperatures were recorded near the shores of four thermokarst lakes and talik configuration was defined beneath the lakes by jet-drilling to determine conditions controlling permafrost degradation in the area. Analytical and thermal models were used to relate field observations to current theory. Surface and subsurface conditions were examined in three drained lake basins and four expanding lakes to investigate how shore recession, talik development, and sediment deposition during lake expansion control the topography in lake basins after drainage. Permafrost temperature at the depth of zero annual amplitude varied between -5.1ºC and -2.6ºC on the Flats. Within the forest-tundra transition, spatial variability in permafrost temperatures appeared to be controlled by the snow-holding capacity of vegetation and the configuration of land covers in the surrounding landscape, which controlled snow supply. Annual mean lake-bottom temperatures close to shorelines were unaffected by spatial variations in on-ice snow depth, but accumulation of freezing degree-days at the lake bottom varied sufficiently to affect rates of permafrost degradation beneath the lake. Where ice reached the lake bottom, talik development rates were controlled by the ratio of freezing degree days to thawing degree days and the thermal offset in the lake sediment. After lake drainage and permafrost aggradation, thermokarst lake basins in OCF commonly develop depressed margins and raised centres. An elevation difference of up to 2 m was recorded between the margins and centres of drained basins, but this elevation difference was not associated with increased ice-wedge density or increased segregated ice content. A conceptual model based on sediment deposition patterns during lake expansion was proposed to explain the topography of drained lake basins in OCF.

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 score0.065
Threshold uncertainty score0.131

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 studies0.0010.001
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 head0.017
GPT teacher head0.224
Teacher spread0.206 · 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

Citations2
Published2015
Admission routes1
Has abstractyes

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