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Record W2040793201 · doi:10.1029/2000jc000680

Improving the utility of ocean circulation models through adjustment of the momentum balance

2001· article· en· W2040793201 on OpenAlexfundaboutno aff
Jinyu Sheng, Richard J. Greatbatch, Daniel G. Wright

Bibliographic record

VenueJournal of Geophysical Research Atmospheres · 2001
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicOceanographic and Atmospheric Processes
Canadian institutionsnot available
FundersNatural Sciences and Engineering Research Council of Canada
KeywordsAdvectionForcing (mathematics)Momentum (technical analysis)Temperature salinity diagramsHydrostatic equilibriumWind stressOcean currentCirculation (fluid dynamics)SalinityMechanicsGeologyClimatologyEnvironmental scienceMeteorologyPhysicsThermodynamics

Abstract

fetched live from OpenAlex

We propose a new method to improve the utility of three‐dimensional ocean circulation models. The method uses climatological temperature and salinity data to adjust the momentum balance of the model, while leaving the tracer equations fully prognostic and unconstrained. The adjustment is accomplished by replacing density in the hydrostatic equation by a linear combination of model‐computed and climatological density. The procedure is equivalent to adding a forcing term to the horizontal momentum equation through a modification of the model's horizontal pressure gradient term. The forcing term modifies the model‐computed velocity field, which, in turn, affects the model‐computed temperature and salinity fields through the advection term (there is no adjustment of the tracer equations carried by the model). Assuming the linear combination coefficient to be invariant in time and space, we suggest a statistical approach to estimating its optimal value. We apply this “semiprognostic” method to the northwest Atlantic. A primitive equation circulation model is initialized with January climatological temperature and salinity and is forced by monthly mean Comprehensive Ocean‐Atmosphere Data Set surface wind stress and heat flux, by restoration of the surface salinity to monthly mean climatology, and by flows through the open boundaries. Both the model‐computed tracer and velocity fields produced using the semiprognostic method show significant improvement over those produced by a purely prognostic calculation; drift of the tracer and velocity fields away from climatology is greatly reduced. Further, convective mixing is explicitly represented, thus improving the utility of results over those obtained from pure diagnostic calculations. The velocity fields obtained with the new approach are somewhat more realistic than those obtained from pure diagnostic calculations. The method reproduces many well‐known circulation features in the region, including the Labrador Current, the Gulf Stream, and the North Atlantic Current. More significantly, the method reproduces reasonably well the seasonal evolution of temperature and salinity in the region despite the fact that the model's tracer fields are not constrained directly by the new method. This result suggests that the semiprognostic approach will be useful for examining the evolution of tracers that are not easily determined by observations.

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 score0.167
Threshold uncertainty score0.365

Codex and Gemma teacher scores by category

CategoryCodexGemma
Metaresearch0.0010.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0000.001
Science and technology studies0.0000.001
Scholarly communication0.0000.000
Open science0.0010.000
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 head0.041
GPT teacher head0.280
Teacher spread0.239 · 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

Citations79
Published2001
Admission routes2
Has abstractyes

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