English

Convection driven by internal heating

Fluid Dynamics 2015-03-13 v2 Geophysics

Abstract

Two-dimensional direct numerical simulations are conducted for convection sustained by uniform internal heating in a horizontal fluid layer. Top and bottom boundary temperatures are fixed and equal. Prandtl numbers range from 0.01 to 100, and Rayleigh numbers (R) are up to 5x10^5 times the critical R at the onset of convection. The asymmetry between upward and downward heat fluxes is non-monotonic in R. In a broad high-R regime, dimensionless mean temperature scales as R^{-1/5}. We discuss the scaling of mean temperature and heat-flux-asymmetry, which we argue are better diagnostic quantities than the conventionally used top and bottom Nusselt numbers.

Keywords

Cite

@article{arxiv.1210.8154,
  title  = {Convection driven by internal heating},
  author = {David Goluskin and Edward A. Spiegel},
  journal= {arXiv preprint arXiv:1210.8154},
  year   = {2015}
}

Comments

14 pages, 8 figures, 6 videos; to appear in Physics Letters A; Color and grayscale versions provided; v2: ancillary videos fixed

R2 v1 2026-06-21T22:30:22.626Z