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Record W6887911355 · doi:10.17895/ices.pub.25636542.v1

Recent Decline Of The Labrador Sea Water

2000· other· en· W6887911355 on OpenAlexaboutno aff

Bibliographic record

VenueOpen MIND · 2000
Typeother
Languageen
Field
Topic
Canadian institutionsnot available
Fundersnot available
KeywordsWater massSillStructural basinNorth Atlantic Deep WaterSalinityOutflowWater columnDeep waterChannel (broadcasting)

Abstract

fetched live from OpenAlex

No abstracts are to be cited without prior reference to the author.Convection in the Labrador Sea forms the Intermediate water mass known as the Labrador Sea water (LSW). The LSW can be identified as a homogeneous layer of low stability and salinity throughout the Labrador Sea (Figure 2) and the North Atlantic Sub Polar Gyre. The salinity maximum beneath the LSW identifies the Northeast Atlantic Deep Water (NEADW). NEADW originates in the eastern basin of the North Atlantic as the deepening, dense outflow from the Faroe Bank Channel and flows into the western basin through gaps in the Mid-Atlantic ridge. The deepest layer of the basin is occupied by the Denmark Strait Overflow Water (DSOW) with low temperature and salinity. DSOW originates in the deep dense overflow from the Denmark Strait sill and is the densest water in the northern North Atlantic.

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 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 categoriesInsufficient payload (model declined to judge)
Consensus categoriesInsufficient payload (model declined to judge)
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Not applicable · Consensus signal: Not applicable
GenreCandidate signal: Other · Consensus signal: Other
Teacher disagreement score0.449
Threshold uncertainty score0.921

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 science0.0020.001
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.5290.080

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 head0.034
GPT teacher head0.304
Teacher spread0.271 · 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; both teacher heads agree on what is shown here.

Study designNot applicable
Domainnot available
GenreOther

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

Citations3
Published2000
Admission routes1
Has abstractyes

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