On the Stability of Two‐Dimensional Convection in a Layer Heated from Below
Integrity signals
Registry
Cites
Statistics
Claims the paper makes
Claims other papers make about this one
Each is checked against this paper’s own text: does it say what the citing paper says it does?
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)
Cited by
Sorted by citations
Non-linear properties of thermal convection
Busse, F. H. (1978) · Reports on Progress in Physics · doi:10.1088/0034-4885/41/12/003 · Cited by 960 · see citing works
Self-citationSpeculations on the Thermal and Tectonic History of the Earth
McKenzie, D., & Weiss, N. (2007) · Geophysical Journal of the Royal Astronomical Society · doi:10.1111/j.1365-246x.1975.tb05855.x · Cited by 335 · see citing works
Oscillatory and collective instabilities in large Prandtl number convection
Busse, F. H., & Whitehead, J. A. (1974) · Journal of Fluid Mechanics · doi:10.1017/s0022112074000061 · Cited by 186 · see citing works
Self-citationScaling of plate-tectonic convection with pseudoplastic rheology
Korenaga, J. (2010) · Journal of Geophysical Research: Solid Earth · doi:10.1029/2010jb007670 · Cited by 89 · see citing works
“…dissipation, I defineΦc as the viscous335 dissipation within the region abovez∗ = c,336 Φc = ∫ c 0 ( ∫ η∗e∗i je ∗ i jdx ∗ ) dz∗, (31)337 and calculateΦδ , Φδ/2, andΦ (≡ Φ1), whereδ is (on average) the maximum thickness of the338 16 top thermal boundary layer [e.g.,Busse, 1967],339 δ = 2Nu−1.”
- Authors
- Busse, F. H.
- Affiliations
- University of California, Los Angeles (US)
- Corresponding author
- Busse, F. H.
- ORCID
- 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
About these checks
Registry, retraction, Cites and statistics results are computed, not judged, with one exception: a printed reference that no index lists is read once by a model before it counts as a citation error. Claims are extracted by a model and kept only when their quote appears verbatim in the text; each cited source is then checked, with a model’s help, for whether it says what the claim relies on. Those verdicts can be wrong — read the claim’s quote and the cited source before relying on one.
Statistics and arithmetic are recomputed, not judged.
Confidence bands are shown only for fields calibrated on our annotated test set. None is calibrated yet, so no band is shown.
What counts as a claim ›How we measure confidence ›How we check this ›
Are you an author, or do you see a problem with this page? Request a review