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Record W2034492414 · doi:10.1139/s04-032

Large-scale flow structures and stability in shallow flows

2004· article· en· W2034492414 on OpenAlex

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.

venuePublished in a venue whose home country is Canada.
no affNo Canadian affiliation: this work is invisible to an affiliation-only frame.
No Canadian affiliation. An affiliation-only frame, the usual design, would never have seen this work. It is one of the works that make the case for inverting the frame.

Bibliographic record

VenueJournal of Environmental Engineering and Science · 2004
Typearticle
Languageen
FieldEngineering
TopicFluid Dynamics and Turbulent Flows
Canadian institutionsnot available
Fundersnot available
KeywordsInstabilityWakeMechanicsBase flowGeologyTurbulenceFlow (mathematics)Waves and shallow waterTransverse planeConvectionMixing (physics)Jet (fluid)Inviscid flowPhysicsOceanography

Abstract

fetched live from OpenAlex

Shallow turbulent flows occurring in wide rivers, estuaries, lakes or coastal regions, as well as the atmosphere, are readily susceptible to transverse disturbances that lead to two-dimensional coherent structures. The shallow jet, the shallow wake, and the shallow mixing layer are examples of such flow patterns. A linear stability analysis incorporating the effects of bottom friction and viscosity is applied to these flows to determine the criteria for absolute and convective instability and for stabilization of the flow. All three flow types exhibit instabilities within the range of natural flows. Three mechanisms for large-scale instability generation, namely topographic forcing, transverse velocity shear, and secondary instabilities of the base flow, are compared to the stability calculations. Based on the results, topographic forcing, and to a lesser extent, transverse shear are expected to have both absolute and convective instabilities; whereas, secondary instabilities of the base flow are expected to generate primarily convective instabilities. The resulting large-scale coherent structures greatly influence the mixing and transport of pollutants and momentum that are released into such flows. Key words: shallow flow, shallow jet, shallow wake, shallow mixing layer, linear stability analysis, bottom friction, Chebyshev polynomial method.

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 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: Simulation or modeling · Consensus signal: Simulation or modeling
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.132
Threshold uncertainty score0.351

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 studies0.0000.000
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 head0.003
GPT teacher head0.167
Teacher spread0.163 · 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