Die wechselseitige Beeinflussung von Nordatlantischem Tiefenwasser und Antarktischem Bodenwasser und ihre Rolle für globale Moden der ozeanischen Zirkulation
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.
Bibliographic record
Abstract
Interhemispheric signal transmission in the Atlantic Ocean connects the deep water production regions of both hemispheres. The nature of these interactions and large scale responses to perturbations on time scales of years to millenia have been investigated using a global general circulation model based on the primitive equations coupled to a dynamic-thermodynamic sea ice model with a viscous-plastic rheology. The coupled model reproduces many aspects of today´s oceanic circulation. Testing the model´s sensitivity revealed a strong dependence of the model results from eddy diffusivities, filtering and topographic effects.:p:The internal variability in the ocean-sea ice system has been addressed by analyzing the model results with statistical techniques. A decadal oscillation could be identified in the Southern Ocean. A sequence of Kelvin and Rossby waves carries anomalies in this frequency band northward across the equator.:p:Longer-term variability in the ocean is mainly determined by advective processes. A set of experiments in which the surface boundary conditions were changed showed the necessity to continue integrations over thousands of years until new equilibria are established. Buoyancy changes in the Weddell and Labrador Seas exert a direct effect on the overturning cells of the respective hemisphere. They influence the density structure of the deep ocean and thereby lead to alterations in the strength of the ACC. The model results suggest an influence of the ACC on convective activities in the Southern Ocean. Changing the wind stress south of 30S influences the magnitude of the deep water production of both hemispheres. The interhemispheric effect in these experiments cannot be explained solely by advective mechanisms (contradicting previous studies). Switching off the wind stress over the latitude band of the Drake Passage leads to a slow gradual decrease of the water mass transport in the ACC resulting in an almost complete cessation.
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 imitationNot 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.
Codex and Gemma teacher scores by category
| Category | Codex | Gemma |
|---|---|---|
| Metaresearch | 0.001 | 0.000 |
| Meta-epidemiology (narrow) | 0.002 | 0.002 |
| Meta-epidemiology (broad) | 0.002 | 0.001 |
| Bibliometrics | 0.000 | 0.002 |
| Science and technology studies | 0.001 | 0.000 |
| Scholarly communication | 0.001 | 0.002 |
| Open science | 0.002 | 0.000 |
| Research integrity | 0.002 | 0.002 |
| Insufficient payload (model declined to judge) | 0.006 | 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 it