A model for the emergence of thermal plumes in Rayleigh–Bénard convection at infinite Prandtl number
From MaRDI portal
Publication:4504826
DOI10.1017/S0022112000008582zbMath0955.76029OpenAlexW4299961903MaRDI QIDQ4504826
Yanick Ricard, C. Lemery, Joel Sommeria
Publication date: 27 February 2001
Published in: Journal of Fluid Mechanics (Search for Journal in Brave)
Full work available at URL: https://doi.org/10.1017/s0022112000008582
thermal boundary layersmoothing methodfinite-time singularitiesthermal plumesEarth's mantlethree-dimensional Rayleigh-Bénard convectiontemperature anomaly
Related Items (2)
Natural fluctuation of sulfur species in volcanic fumaroles ⋮ Four dynamical regimes for a starting plume model
This page was built for publication: A model for the emergence of thermal plumes in Rayleigh–Bénard convection at infinite Prandtl number