Published June 18, 2024 | Version v1
Journal article

Analysis of Rayleigh-Bénard convection using latent Dirichlet allocation

  • 1. EM2C, CentraleSupélec, CNRS, Université Paris-Saclay, 8-10 rue Joliot Curie, 91192 Gif-sur-Yvette, France
  • 2. LISN, CNRS, Université Paris-Saclay, Campus Universitaire, Rue Raimond Castaing bâtiment 650, 91190 Gif-sur-Yvette, France

Description

We apply a probabilistic clustering method, latent Dirichlet allocation (LDA), to characterize the large-scale dynamics of Rayleigh-Bénard convection. The method, introduced by Frihat et al. [J. Fluid Mech. 920, A27 (2021)], is applied to a collection of snapshots in the vertical midplanes of a cubic cell for Rayleigh numbers in the range [106,108]. For the convective heat flux, temperature, and kinetic energy, the decomposition identifies latent factors, called motifs, which consist of connex regions of fluid. Each snapshot is modeled with a sparse combination of motifs, the coefficients of which are called the weights. The spatial extent of the motifs varies across the cell and with the Rayleigh number. We show that the method is able to provide a compact representation of the heat flux and displays good generative properties. At all Rayleigh numbers the dominant heat flux motifs consist of elongated structures located mostly within the vertical boundary layers, at a quarter of the cavity height. Their weights depend on the orientation of the large-scale circulation. A simple model relating the conditionally averaged weight of the motifs to the relative strength of the corner rolls and of the large-scale circulation is found to predict well the average large-scale circulation reorientation rate. Application of LDA to the temperature fluctuations shows that temperature motifs are well correlated with heat flux motifs in space as well as in time, and to some lesser extent with kinetic energy motifs. The abrupt decrease of the reorientation rate observed at 108 is associated with a strong concentration of plumes impinging onto the corners of the cell, which decrease the temperature difference within the corner structures. It is also associated with a reinforcement of the longitudinal wind through formation and entrainment of new plumes.

Additional details

Identifiers

DOI
10.1103/PhysRevFluids.9.063502;
Crossref Funder ID
10.13039/501100010190;

Publishing Information

Journal Title
Physical Review Fluids
Journal Volume
9
Journal Issue
6
Journal Page Range
30 pgs.
ISSN
2469-990X

Optional Information

Copyright
©2024 American Physical Society
Contract/Grant/Project number
2023-AD012A62062R1
Notes
Record automatically processed
Funding organization
Grand Équipement National De Calcul Intensif