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Record W2055645045 · doi:10.1029/2004eo230007

The Mass Balance of the Cryosphere: Observations and Modelling of Contemporary and Future Changes

2004· article· en· W2055645045 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.

Bibliographic record

VenueEos · 2004
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicCryospheric studies and observations
Canadian institutionsUniversity of British Columbia
FundersU.S. Geological SurveyUniversity of British ColumbiaNational Science Foundation
KeywordsCryosphereGlaciologyIce-albedo feedbackFuture sea levelSea iceClimate changeClimatologyMirroringEarth system sciencePhysical geographyEnvironmental scienceGeographyGeologyIce streamOceanographySociology

Abstract

fetched live from OpenAlex

“Vanishing sea ice!” “Disintegrating ice shelves!” “Rising sea level!” Such proclamations illustrate the widening gap between the kind of glaciology that makes newspaper headlines and the kind of glaciology which is reinforced in standard scientific texts. It is as if there were two kinds of ice: a benign form such as that studied by Victorian gentlefolk and a new rogue form, of concern to the Intergovernmental Panel on Climate Change (IPCC). In truth, the difference is one of perspective: ice as a feature of the local land‐ or seascape versus ice as an active component of the Earth system. From the global perspective, the two most important attributes of Earth system ice, a.k.a. the cryosphere, are its high albedo (leading to a positive climate feedback) and the large mass of stored freshwater—roughly 70 m of sea‐level equivalent. These aspects are addressed in several chapters of the IPCC's Third Assessment Report, Climate Change 2001. J. Bamber and T. Payne's ambitious book provides the backstory in the form of a coherent treatise.

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 score0.029
Threshold uncertainty score0.178

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 head0.043
GPT teacher head0.199
Teacher spread0.156 · 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