Cited by 291Fluid Dynamics and Turbulent FlowsFluid dynamics and aerodynamics studiesNavier-Stokes equation solutions

On the Stability of Two‐Dimensional Convection in a Layer Heated from Below

Busse, F. H.·1967·Journal of Mathematics and Physics

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Crossref · 10.1002/sapm1967461140

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  • Longitudinal rolls are likely to be stabilized by shear and will not change to three-dimensional convection until the Rayleigh number considerably exceeds 22600.

    “it appears likely that longitudinal rolls will be stabilized by the shear flow, and will not change to three-dimensional convection until the Rayleigk number considerably exceeds the value of 22 600 found for”

    From Speculations on the Thermal and Tectonic History of the Earth (2007) · cites this paper as Busse (1967a)

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Authors
Busse, F. H.
Affiliations
University of California, Los Angeles (US)
Corresponding author
Busse, F. H.
Venue
Journal of Mathematics and Physics
Publisher
Wiley
Published
1967-04
Volume
46
Issue
1-4
Pages
140-150
ISSN
  • 0022-2526 (ISSN-L)
  • 0097-1421
OpenAlex
W159546068
Cited by
291
References
0
Citations by year
2026: 1 · 2025: 1 · 2024: 2 · 2023: 4 · 2022: 3 · 2021: 6 · 2020: 3 · 2019: 1 · 2018: 2 · 2017: 5 · 2016: 3 · 2015: 3 · 2014: 2 · 2013: 4 · 2012: 2
FWCI
7.61
Type
journal article
Language
en
Open access
closed
Locations
  • Studies in Applied Mathematics (publishedVersion)
  • ERef Bayreuth (University of Bayreuth) (submittedVersion)
Topics
  • Physical Sciences › Engineering › Computational Mechanics › Fluid Dynamics and Turbulent Flows
  • Physical Sciences › Engineering › Computational Mechanics › Fluid dynamics and aerodynamics studies
  • Physical Sciences › Mathematics › Applied Mathematics › Navier-Stokes equation solutions
Keywords
two-dimensional convection, Rayleigh-Bénard convection, stability analysis, heated fluid layer, thermal convection onset

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