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Record W6945031100 · doi:10.2312/cr_m45

North Atlantic 1999 - Cruise No. M45 - May 18 - November 4, 1999 - Malaga (Spain) - Las Palmas (Spain)

2000· report· en· W6945031100 on OpenAlexaboutno aff

Bibliographic record

VenueHelmholtz-Zentrum für Polar-und Meeresforschung (Alfred-Wegener-Institut) · 2000
Typereport
Languageen
Field
Topic
Canadian institutionsnot available
Fundersnot available
KeywordsCruiseHydrographyWater massRidgeContext (archaeology)Current (fluid)Meteor (satellite)Structural basinOcean current

Abstract

fetched live from OpenAlex

METEOR cruise M45 took place in the North Atlantic Ocean in 1999 and consisted of five legs. The research activities during the METEOR cruise M45/1, which started in Malaga on 19 May 1999, were related to the scientific programs CANIGO/ESTOC and DOMEST. The DOMEST project concentrates on marine technology and data transmission, mainly tested in the Canary Island region. On this cruise the CANIGO/ESTOC project concentrated on seafloor and water probing. In the morning of June 8 the RV METEOR arrived in Lisbon. During the second leg (Lisbon - St. John's) the aim was the investigation of water mass spreading and mixing within the eastern basin of the eastern North Atlantic. The work was part of the yearly field programmes of the "Sonderforschungsbereich" SFB 460. Elements of the repeat hydrographic survey in the Iceland Basin included observations with CTD and rosette sampler. For determining deep circulation and water mass transformation, nutrients and tracer samples (CFCs, tritium/helium) were taken. In addition an array of moored current meters for monitoring the Overflow Water close to the Reykjanes Ridge was recovered. The array was then partly redeployed for an additional year. RAFOS float observations for the determination of the drift of Labrador Sea Water in the eastern basin were continued during M45/2. The third leg (St. John's - St. John's) focused on the deep circulation and water mass distribution of the Labrador and Irminger seas, also within the context of the SFB 460. The distribution of water masses and circulation was studied along standard repeat sections using current profiling, hydrography and tracer (Freon, tritium/helium) observations. In the Labrador Sea, a number of tomography, convection and boundary current moorings were recovered and redeployed for measuring deep convection activity. A new moored array was deployed off the Grand Banks to measure the export of Deep Water out of the Subpolar North Atlantic. The fourth cruise leg (St. John's - Rendsburg) was devoted to mooring work and hydrographic measurements on sections normal to the southeastern slope of Greenland. It was aimed at repeatedly describing the state of the Denmark Strait overflow as one of the contributions to the EU Project VEINS on the Variability of Exchanges in the Northern Seas. Leg M45/4 METEOR ended on 1 September in the ship yard in Rendsburg. Cruise leg M45/5 started on 1 October 1999 in Bremen and ended on 3 November 1999 in Las Palmas. It was subdivided into two parts with an interim stay in Las Palmas during 20 - 22 October. During the first leg (M45/5a), sedimentological investigations and plankton sampling were carried out in the North Sea, Azores Frontal System and off Cape Ghir (NW Africa) with the purpose to collect data on the reconstruction of paleo-environmental conditions of these regions. During the second leg (M45/5b), equipment testing, mooring work and water column measurements were carried out. Water column sampling, including primary production and particle flux measurements, were carried out around the time-series station ESTOC (European Station for Time-series in the ocean, Canary Islands) as well as off Cape Ghir.

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: Not applicable · Consensus signal: Not applicable
GenreCandidate signal: Other · Consensus signal: none
Teacher disagreement score0.180
Threshold uncertainty score0.359

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0000.000
Meta-epidemiology (narrow)0.0010.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0010.001
Science and technology studies0.0010.000
Scholarly communication0.0010.000
Open science0.0000.000
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.0240.009

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 head0.032
GPT teacher head0.298
Teacher spread0.267 · 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 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

Citations1
Published2000
Admission routes1
Has abstractyes

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