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Record W3164325980 · doi:10.1038/s41467-021-23350-2

Subpolar North Atlantic western boundary density anomalies and the Meridional Overturning Circulation

2021· article· en· W3164325980 on OpenAlexafffund
Feili Li, M. Susan Lozier, Sheldon Bacon, Amy S. Bower, Stuart A. Cunningham, M. Femke de Jong, Brad deYoung, Neil Fraser, Nora Fried, Guoqi Han, N. Penny Holliday, James Holte, Loïc Houpert, Mark Inall, William E. Johns, Sam Jones, Clare Johnson, Johannes Karstensen, Isabela Le Bras, Pascale Lherminier, Xiaopei Lin, Herlé Mercier, Marilena Oltmanns, Astrid Pacini, Tillys Petit, Robert S. Pickart, D. Rayner, Fiammetta Straneo, Virginie Thierry, Martin Visbeck, Igor Yashayaev, Chun Zhou

Bibliographic record

VenueNature Communications · 2021
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicOceanographic and Atmospheric Processes
Canadian institutionsBedford Institute of OceanographyFisheries and Oceans CanadaMemorial University of Newfoundland
FundersNatural Environment Research CouncilFisheries and Oceans CanadaCanadian Space AgencyFundamental Research Funds for the Central UniversitiesBundesministerium für Bildung und ForschungNational Natural Science Foundation of ChinaNatural Sciences and Engineering Research Council of CanadaEuropean CommissionSight Research UKKoninklijk Nederlands Instituut voor Onderzoek der ZeeNational Science Foundation
KeywordsShutdown of thermohaline circulationThermohaline circulationGeologyOceanographyNorth Atlantic Deep WaterBoundary currentClimatologyStructural basinDeep waterCirculation (fluid dynamics)Deep convectionZonal and meridionalBoundary (topology)Ocean currentConvectionGeographyPaleontologyMeteorologyPhysicsMechanics

Abstract

fetched live from OpenAlex

Changes in the Atlantic Meridional Overturning Circulation, which have the potential to drive societally-important climate impacts, have traditionally been linked to the strength of deep water formation in the subpolar North Atlantic. Yet there is neither clear observational evidence nor agreement among models about how changes in deep water formation influence overturning. Here, we use data from a trans-basin mooring array (OSNAP-Overturning in the Subpolar North Atlantic Program) to show that winter convection during 2014-2018 in the interior basin had minimal impact on density changes in the deep western boundary currents in the subpolar basins. Contrary to previous modeling studies, we find no discernable relationship between western boundary changes and subpolar overturning variability over the observational time scales. Our results require a reconsideration of the notion of deep western boundary changes representing overturning characteristics, with implications for constraining the source of overturning variability within and downstream of the subpolar region.

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 categoriesnone
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Observational · Consensus signal: Observational
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.047
Threshold uncertainty score0.997

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 studies0.0010.000
Scholarly communication0.0000.000
Open science0.0000.000
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.0000.000

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 head0.010
GPT teacher head0.219
Teacher spread0.208 · 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 teacher head, not a consensus.

The models applied no category: nothing in the taxonomy fit this work.
Study designObservational
Domainnot available
GenreEmpirical

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

Citations112
Published2021
Admission routes2
Has abstractyes

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