Bibliographic record
Abstract
No abstracts are to be cited without prior reference to the author.In 1997 the Institut für Meereskunde started its RAFOS float program in the eastern North Atlantic. So far, a total of 47 isobaric floats were launched during three cruises at a nominal depth of 1500 m east of Charlie Gibbs Fracture Zone and in the central Iceland Basin. While 16 floats are still on mission the surfaced ones delivered 26 eddy-resolving trajectories. They allow a unique insight into the circulation pattern of the Labrador Sea Water invading the eastern basins. Pathways split into three branches east of the Middle Atlantic Ridge – one parallels the Ridge southwards, a second spreads zonally towards Porcupine Bank, the third fills the eastern side of the Iceland Basin. In fact, a series of stagnation phases and eddy rotations were recorded on the pathways along the western flanks of Hutton Bank. They are superimposed on a northeastward drift. At the tip of the Basin, floats experience a pronounced acceleration by incoming Iceland Scotland Overflow Water from the Faroe Bank Channel. In the course of the basin-wide cyclone the floats are swiftly advected along the Reykjanes Ridge. Finally, the depth keeping floats are detrained from the deepening Overflow core before the latter reaches Charlie Gibbs Fracture Zone. We expect the pertinent helical circulation and its fluctuations to effect directly transformation rates of all engaged watermasses.
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 imitationNot 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.
Distilled classifier scores by category (both heads)
| Category | Codex | Gemma |
|---|---|---|
| Metaresearch | 0.000 | 0.000 |
| Meta-epidemiology (narrow) | 0.000 | 0.000 |
| Meta-epidemiology (broad) | 0.000 | 0.000 |
| Bibliometrics | 0.001 | 0.001 |
| Science and technology studies | 0.000 | 0.000 |
| Scholarly communication | 0.000 | 0.000 |
| Open science | 0.000 | 0.000 |
| Research integrity | 0.000 | 0.000 |
| Insufficient payload (model declined to judge) | 0.003 | 0.001 |
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.
score_only:v0-immature-baseline · verbatim from the scoring run: score_only means the number may rank works, and no category label ships from itClassification
machine, unvalidatedMachine predicted; a candidate call from one source (direct Gemma or distilled Codex), not a consensus.
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".