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Record W4299502107

A 3D MODEL FOR TWO COUPLED TURBULENT FLUIDS: NUMERICAL ANALYSIS OF A FINITE ELEMENT APPROXIMATION

2016· preprint· en· W4299502107 on OpenAlexaff
Tomás Chacón Rebollo, Driss Yakoubi

Bibliographic record

VenueHAL (Le Centre pour la Communication Scientifique Directe) · 2016
Typepreprint
Languageen
FieldEngineering
TopicFluid Dynamics and Vibration Analysis
Canadian institutionsUniversité Laval
FundersJunta de Andalucía
KeywordsFinite element methodTurbulenceMechanicsSmoothed finite element methodMixed finite element methodApplied mathematicsMathematicsPhysicsBoundary knot methodThermodynamics
DOInot available

Abstract

fetched live from OpenAlex

This paper deals with the numerical analysis for a finite element approximation of a steady coupled two-fluid RANS turbulence equations, used to model, for example, air-ocean flow interaction. Each fluid is modeled by the coupled steady Stokes equations with the equation for the turbulent kinetic energy TKE. The eddy viscosities for velocity and TKE depend on the energy. The production (source) term for the TKEs is only in L 1 , and the boundary condition for the TKEs on the interface between the two flows depends quadratically on the difference of velocities. To overcome the lack of regularity, we approximate the initial system by a regularized one, in which the eddy viscosities and source terms for the TKEs are regularized by convolution. We perform its finite element discretization, combined with a decoupled iterative lin-earization procedure. We prove that the discrete scheme converges to the continuous one for large enough eddy viscosities in natural norms. Finally, we present some numerical tests where we study the accuracy of the procedure, and simulate a realistic flow in which an imposed wind in the upper atmosphere generates an upwelling in the oceanic flow. 1. Introduction. We consider the numerical analysis for finite element approximation of RANS (Reynolds-Averaged Navier-Stokes) turbulence models, and more precisely of a coupled two-fluid RANS models. This system can model the coupled atmosphere-ocean system, whose accurate numerical simulation is crucial to analyze the main issues related to climate change. From the practical point of view, RANS models are rather diffusive and provide overall predictions of many flows of engineering interest (Cf. Davidson [21]). However, from the mathematical point of view RANS equations are more singular than the Navier-Stokes equations. The main mathematical difficulties comes from the source term (the production term) for the TKE equations which has a L 1 (Ω) regularity only, implying that the TKE equations do not make sense in H −1 (Ω). Their solution must be understood in the renormalized –or entropy– sense (Cf. [1, 7, 6, 8, 9, 10]).

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)0.001
metaresearch head score (Gemma)0.002
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: Simulation or modeling
GenreCandidate signal: Empirical · Consensus signal: none
Teacher disagreement score0.006
Threshold uncertainty score0.011

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0010.002
Meta-epidemiology (narrow)0.0010.001
Meta-epidemiology (broad)0.0010.001
Bibliometrics0.0010.001
Science and technology studies0.0010.001
Scholarly communication0.0010.001
Open science0.0010.001
Research integrity0.0030.001
Insufficient payload (model declined to judge)0.0020.001

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 head0.013
GPT teacher head0.234
Teacher spread0.221 · 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
Published2016
Admission routes1
Has abstractyes

Explore more

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