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Record W7105990301 · doi:10.7939/83029

Investigating the role of extratropical cyclones in North Atlantic deep water formation

2025· dissertation· en· W7105990301 on OpenAlexaboutno aff

Bibliographic record

VenueUniversity of Alberta Library · 2025
Typedissertation
Languageen
FieldEnvironmental Science
TopicClimate variability and models
Canadian institutionsnot available
Fundersnot available
KeywordsExtratropical cycloneForcing (mathematics)Deep convectionNorth Atlantic Deep WaterWater massStormHydrographyThermohaline circulation

Abstract

fetched live from OpenAlex

The Atlantic Meridional Overturning Circulation (AMOC) is a vital mechanism of heat transport in the climate system, but it has been suggested that its strength will change in the coming decades. This strength depends in part on water mass transformations in the North Atlantic, and understanding the factors that contribute to this variability is crucial to predicting the future behaviour of the AMOC. In the Labrador and Nordic Seas, where deep convection occurs and replenishes the deep water masses of the AMOC, atmospheric forcing is a critical factor in the priming and initiation of convection. In particular, extratropical cyclones (ETCs) provide high-frequency forcing that can influence hydrographic properties in the upper water column. These effects can be studied by forcing an ocean model with atmospheric datasets that include such storms, and then analyzing the response of the ocean to them. This thesis will first present background information on the processes of deep convection and deep water formation in the North Atlantic, as well as discussing extratropical cyclones and the air-sea interactions associated with them. Details of the ocean model and atmospheric datasets used to perform this study will be described. ETC statistics are calculated to study seasonal and interannual patterns of storm characteristics. The results indicate that stronger cyclones tend to occur in the cold season, and that the maximum strength of ETCs on a year-to-year basis may correlate with the phase of the NAO. Various properties from the ocean model output are also examined as time series associated with individual cyclones that are detected in the atmospheric datasets. These time series are also averaged to calculate the mean ocean response to various categories of ETCs. We find that individual cyclones may change sea surface temperatures by up to 2°C, though the mean change was around 0.2°C. The density and depth of the mixed layer do increase in response to ETC passage, and these changes persist for at least a week post-cyclone. The depth of the mixed layer also tends to remain somewhat deeper than its pre-cyclone depth even after returning to equilibrium, suggesting that ETCs passing in succession may progressively deepen the mixed layer over time.

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)0.001
Version: metacan-v3-hybrid-931329e0061cValidation status: machine_predicted_unvalidated
Candidate categoriesnone
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Simulation or modeling · Consensus signal: none
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.039
Threshold uncertainty score0.078

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0000.001
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)0.0010.000

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 head0.006
GPT teacher head0.166
Teacher spread0.160 · 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 designSimulation or modeling
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

Citations0
Published2025
Admission routes1
Has abstractyes

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