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10.1016/s0967-0653(98)83399-1

2000· article· en· W30173043 on OpenAlexvenueno aff
Mario Hoppema, Eberhard Fahrbach, Michael Schröder

Bibliographic record

VenueTime to knit · 2000
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicMarine and coastal ecosystems
Canadian institutionsnot available
Fundersnot available
KeywordsOcean gyreCircumpolar deep waterWeddell Sea Bottom WaterOceanographyWater massGeologyCircumpolar starBoundary currentPlateau (mathematics)Antarctic Intermediate WaterSalinitySea iceAtmospheric sciencesClimatologyDeep waterOcean currentArctic ice packAntarctic sea iceNorth Atlantic Deep WaterEcology

Abstract

fetched live from OpenAlex

Sections from two 'Polarstern' cruises in austral winter 1992 and summer 1992/93 were used to track the course of Circumpolar Deep Water (CDW) in the Weddell Sea. Total inorganic carbon (TCO2) is a valuable tracer for that water mass because it allows to distinguish features that cannot be seen in the distributions of temperature and salinity. Upon entrance into the eastern Weddell Gyre, a shallow maximum in TCO2 at about 200 m (likewise a temperature maximum and oxygen minimum) indicates the depth level to which vertical mixing with Winter Water penetrates the CDW layer in the Weddell Gyre. The lower boundary of this CDW layer, which is not apparent in the temperature and salinity profiles, is a TCO2 maximum at 1000-1500 m (sq27.835), originating through the superposition of the recently advected CDW from the Antarctic Circumpolar Current and the Weddell Sea Deep Water (WSDW) with opposite vertical gradients. A coinciding, weak oxygen minimum is only present on the prime meridian and is probably caused bydifferent biological histories of the CDW and the WSDW underneath. Using this TCO2 maximum, the newly injected CDW can be traced as a well-defined band around the Weddell Sea up to south of the South Orkney plateau. Downstream in the northern limb of the Weddell Gyre at the prime meridian its trace has disappeared.The band of 'new' CDW, as part of the boundary current, envelopes a central area where currents are significantly smaller. In this interior a special modification of CDW, the Central Intermediate Water (CIW), can be distinguished. This water mass is characterised by a secondary TCO2 maximum and oxygen minimum, with no comparable structures in the temperature and salinitiy fields. CIW is enriched in CO2 compared to the CDW that enters the Weddell Gyre and is most pronounced in the western part of the Weddell basin. Data in the west suggest that the CIW is related to the lower part of the 'new'-CDW layer. Thus, the central Weddell basin is replenished from the west side rather than from the east. Within the interior the CDW is further modified by mixing with the WSDW below and by entrainment into the surface layer above. Part of it is also advected out of the Weddell Sea into the bottom layer of the ACC, conveying water that has been biologically enriched in CO2 to the abyssal oceans.

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)0.002
metaresearch head score (Gemma)0.002
Version: metacan-v3-hybrid-931329e0061cValidation 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: none
GenreCandidate signal: Other · Consensus signal: Other
Teacher disagreement score0.008
Threshold uncertainty score0.011

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0020.002
Meta-epidemiology (narrow)0.0040.001
Meta-epidemiology (broad)0.0020.002
Bibliometrics0.0040.002
Science and technology studies0.0020.002
Scholarly communication0.0040.007
Open science0.0050.005
Research integrity0.0080.003
Insufficient payload (model declined to judge)0.9920.994

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 head0.006
GPT teacher head0.148
Teacher spread0.143 · 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; the direct Gemma label and the distilled Codex classifier 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

Citations24
Published2000
Admission routes1
Has abstractyes

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