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Record W2029730484 · doi:10.1080/07055900.2013.877417

A Model Study of the Relationship between Sea-Ice Variability and Surface and Intermediate Water Mass Properties in the Labrador Sea

2014· article· en· W2029730484 on OpenAlexafffundvenueabout
M. A. Cooke, Entcho Demirov, Jieshun Zhu

Bibliographic record

VenueATMOSPHERE-OCEAN · 2014
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicArctic and Antarctic ice dynamics
Canadian institutionsMemorial University of NewfoundlandUniversity of Toronto
FundersCanadian Meteorological and Oceanographic SocietyCanadian Foundation for Climate and Atmospheric Sciences
KeywordsOceanographyGeologyWater massNorth Atlantic Deep WaterSalinitySea iceTemperature salinity diagramsClimatologySea surface temperatureThermohaline circulation

Abstract

fetched live from OpenAlex

Sea ice plays an important role in the variability of the Labrador Sea especially in its most western part adjacent to an important region of deep convection.Winter-to-winter re-emergence and propagation of both sea-ice concentration (SIC) and sea surface temperature anomalies have been observed following years of high SIC in this region.They have potentially important links to water mass properties and freshwater and heat transports in the subpolar North Atlantic.This article builds on the results of two precursor papers and presents results from a coupled sea-ice-ocean model study of the interannual variability of sea ice in the Labrador Sea.The relationships between SIC and water column properties in the subpolar North Atlantic are assessed.Winters with high SIC and strong surface cooling are found to be conducive to intensified convection.Surface and mid-depth temperature and salinity anomalies are observed in the Labrador Sea and the northwestern North Atlantic during winters with anomalous Labrador Sea SIC.These anomalies are found to propagate along the major circulation patterns in the subpolar North Atlantic and to persist for up to three years.RSUM [Traduit par la rdaction] La glace de mer joue un rle important dans la variabilit de la mer du Labrador, surtout dans sa partie la plus l'ouest adjacente une grande rgion de convection profonde.On a observ que la rapparition et la propagation, d'un hiver l'autre, d'anomalies de concentration de glace de mer (CGM) et de temprature de la surface de la mer suivent des annes de forte CGM dans cette rgion.Ces anomalies pourraient tre troitement lies aux proprits des masses d'eau et au transport d'eau douce et de chaleur dans l'Atlantique Nord subpolaire.Cet article fait suite aux rsultats de deux articles prcdents et prsente les rsultats d'une tude de la variabilit interannuelle de la glace de mer dans la mer du Labrador faite l'aide d'un modle coupl glace de merocan.Nous examinons la relations entre la CGM et les proprits de la colonne d'eau dans l'Atlantique Nord subpolaire.Nous constatons que les hivers de CGM leve et de fort refroidissement en surface favorisent une convection intensifie.Nous observons des anomalies de temprature et de salinit la surface et mi-profondeur dans la mer du Labrador et dans le nord-ouest de l'Atlantique Nord durant les hivers o se produisent des anomalies de CGM dans la mer du Labrador.Nous trouvons que ces anomalies se propagent le long des principales configurations de circulation dans l'Atlantique Nord subpolaire et perdurent jusqu' trois ans.

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)0.001
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 score0.177
Threshold uncertainty score0.398

Codex and Gemma teacher scores by category

CategoryCodexGemma
Metaresearch0.0010.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0000.000
Science and technology studies0.0000.000
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 head0.023
GPT teacher head0.212
Teacher spread0.189 · 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

Citations5
Published2014
Admission routes4
Has abstractyes

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