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Record W2531805827

Short-term variations in glacier dynamics in the ablation zone of a High Arctic polythermal glacier: relation to seasonal changes in subglacial drainage system structure

2003· article· en· W2531805827 on OpenAlex
RG Bingham, PW Nienow, MJ Sharp

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.

aboutThe title or abstract carries a Canadian signal from the geographic lexicon.
no affNo Canadian affiliation: this work is invisible to an affiliation-only frame.
No Canadian affiliation. An affiliation-only frame, the usual design, would never have seen this work. It is one of the works that make the case for inverting the frame.

Bibliographic record

VenueExplore Bristol Research · 2003
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicCryospheric studies and observations
Canadian institutionsnot available
Fundersnot available
KeywordsGlacierGeologyArcticGlacier ice accumulationCirque glacierGlacier mass balanceTerm (time)Tidewater glacier cycleGeomorphologyClimatologyAblation zoneGlacier terminusPhysical geographyIce streamCryosphereOceanographySea iceGeography
DOInot available

Abstract

fetched live from OpenAlex

Short-term (~daily) variations in glacier surface dynamics, induced by variations in subglacial water pressures, may critically affect glacier response to global warming, and the contribution of glacier runoff to global sea levels, by influencing the transfer of ice to lower altitudes where surface melting is increased. This may be especially significant at High Arctic glaciers, where recent climate models predict that global warming may be exacerbated relative to lower latitudes. Recent field studies have demonstrated that significant short-term velocity variations occur at High Arctic glaciers but it is not known whether these motion anomalies propagate spatially and/or temporally, nor whether they result from changes in the structure of the subglacial drainage system. This study reports on short-term variations in glacier surface motion during two melt-seasons (2000, 2001) across the lower ablation zone of John Evans Glacier, Ellesmere Island, Canada. Here, warm ice (hence subglacial drainage) exists only as a thin (~10 m) layer at the basal interface, and is not present at the margins and terminus. Horizontal and vertical velocities of 33 marker stakes distributed across the lower ablation zone were derived every two days between June and August 2000 and 2001. A simultaneous programme of dye-tracing experiments revealed a significant evolution in the structure of the subglacial drainage system occurred beneath the lower ablation zone each melt-season. The results reveal a 2-4 day 'spring event' of high horizontal and vertical velocities occurs over the lower ablation zone each melt-season 2-3 weeks after the onset of surface melting. This is induced by the sudden penetration of stored surface meltwaters through cold ice to a distributed subglacial drainage system via a crevasse field 5 km above the terminus, inducing high subglacial water pressures and rapid subglacial drainage evolution under the lower ablation zone. After the spring event, horizontal velocities fall (although typically remain higher than overwinter levels until the end of summer) and vertical velocities change sign. Further transient periods of high horizontal surface velocities are observed when high meltwater inputs resume after periods of cold weather, or when unusually high meltwater inputs exceed the capacity of the channelised subglacial drainage system.

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)0.002
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 score0.263
Threshold uncertainty score0.998

Codex and Gemma teacher scores by category

CategoryCodexGemma
Metaresearch0.0020.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0000.002
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 head0.050
GPT teacher head0.288
Teacher spread0.238 · 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