Cited by 278Astro and Planetary ScienceFluid Dynamics and Turbulent FlowsStellar, planetary, and galactic studies

A simple model of convection in the Jovian atmosphere

Busse, F.H.·1976·Icarus

Integrity signals

Registry

Crossref · 10.1016/0019-1035(76)90053-1

Cites

15 of 15 references verified0 citation errors · 0 not checkable

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Recomputing p-values needs the paper’s full text.

Claims the paper makes

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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?

  • Alternating jets on gas giant planets are either shallow, existing above about 10 bars, or deep, extending to tens of thousands of bars.

    “on one hand, the alternating jets on gas giant planets are 'shallow', existing above 10 bars or so [15-17]; on the other hand, zonal jets are 'deep', extending to tens of thousands of bars [18-22].”
  • Existing models posit as the driver of the flow either the differential radiative heating of the upper atmosphere or the intrinsic heat fluxes emanating from the deep interior.

    “Existing models posit as the driver of the flow either the differential radiative heating of the upper atmosphere (e.g., Williams 1979Williams , 2003b) ) or the intrinsic heat fluxes emanating from the deep interior (e.g., Busse 1976;Heimpel et al. 2005;Aurnou et al. 2007;Chan and Mayr 2008;Kaspi et al. 2009).”

    From Mechanisms of Jet Formation on the Giant Planets (2010) · cites this paper as Busse 1976

  • Under conditions of small convective Rossby number and negligible viscous momentum dissipation and thermal diffusion, convective plumes are columns aligned with M_V surfaces because rapid rotation inhibits motion perpendicular to M_V surfaces in the absence of viscous or other stresses.

    “Under these circumstances, convective plumes are columns aligned with M V surfaces because, as above, rapid rotation inhibits motion perpendicular to M V surfaces in the absence of viscous or other stresses (e.g., Busse 1976Busse , 1978;;Kaspi et al. 2009;Jones et al. 2009).”

    From Mechanisms of Jet Formation on the Giant Planets (2010) · cites this paper as Busse 1976

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Authors
Busse, F. H.
Affiliations
University of California, Los Angeles (US)
Corresponding author
Busse, F.H.
Venue
Icarus
Publisher
Elsevier BV
Published
1976-10
Volume
29
Issue
2
Pages
255-260
ISSN
0019-1035 (ISSN-L)
OpenAlex
W2074802867
Cited by
278
References
15
Citations by year
2026: 3 · 2025: 4 · 2024: 5 · 2023: 8 · 2022: 9 · 2021: 6 · 2020: 11 · 2019: 9 · 2018: 34 · 2017: 10 · 2016: 8 · 2015: 9 · 2014: 4 · 2013: 5 · 2012: 7
FWCI
2.52
Type
journal article
Language
en
Open access
closed
Locations
  • Icarus (publishedVersion)
  • ERef Bayreuth (University of Bayreuth) (submittedVersion)
Funders
National Science Foundation
Topics
  • Physical Sciences › Physics and Astronomy › Astronomy and Astrophysics › Astro and Planetary Science
  • Physical Sciences › Engineering › Computational Mechanics › Fluid Dynamics and Turbulent Flows
  • Physical Sciences › Physics and Astronomy › Astronomy and Astrophysics › Stellar, planetary, and galactic studies
Keywords
Jupiter atmosphere, convection, latitudinal structure, internal heating, Boussinesq approximation, eddy viscosity, turbulent flow

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.

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