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From classical to ultimate heat fluxes for convection at a vertical wall

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Publication:6096852
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DOI10.1017/JFM.2023.665OpenAlexW4386545564MaRDI QIDQ6096852

Andrew J. Wells

Publication date: 15 September 2023

Published in: Journal of Fluid Mechanics (Search for Journal in Brave)

Full work available at URL: https://doi.org/10.1017/jfm.2023.665


zbMATH Keywords

direct numerical simulationturbulent heat transferconvective boundary layernear-wall sublayer


Mathematics Subject Classification ID

Direct numerical and large eddy simulation of turbulence (76F65) Free convection (76R10) Turbulent boundary layers (76F40) Convective turbulence (76F35) Diffusive and convective heat and mass transfer, heat flow (80A19)





Cites Work

  • A theory for natural convection turbulent boundary layers next to heated vertical surfaces
  • A geophysical-scale model of vertical natural convection boundary layers
  • Changes in the boundary-layer structure at the edge of the ultimate regime in vertical natural convection
  • Enhanced ablation of a vertical ice wall due to an external freshwater plume
  • Asymptotic analysis of the near-wall region of turbulent natural convection flows
  • Turbulent Thermal Convection at Arbitrary Prandtl Number




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