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Journal ArticleDOI

Differential rotation in stellar convection zones.

Friedrich H. Busse
- 01 Jan 1970 - 
- Vol. 159, pp 629
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TLDR
In this article, the authors extended the analysis of Busse l970a to include the detailed spatial dependence of the meridional circulation as well as of the differential rotation, and the thin shell approximation for a rotating spherical convection layer of a Boussinesq fluid is used.
Abstract
The analysis of an earlier paper (Busse l970a) in which the differential rotation of the Sun was explained as the result of large scale convection in the solar convection zone is extended to include the detailed spatial dependence of the meridional circulation as well as of the differential rotation The thin shell approximation for a rotating spherical convection layer of a Boussinesq fluid is used The asymptotic representation of large order spherical harmonlcs by Hermite functions permits a simple integration of the equations for the meridional circulation and the differential rotation Explicit analytical solutions are given for the case of stressfree boundaries and numerical results are shown in the case of a rigid inner and a free outer boundary The case of stressfree boundaries is rather exceptional and the magnitude of the differential rotation is reduced for more general boundary conditions However, the differential rotation still exhibits the characteristic equatorial acceleration in the case of an inner rigid boundary (auth)

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Non-linear properties of thermal convection

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New perspectives in turbulent Rayleigh-Bénard convection.

TL;DR: Key emphasis is given to the physics and structure of the thermal and velocity boundary layers which play a key role for the better understanding of the turbulent transport of heat and momentum in convection at high and very high Rayleigh numbers.
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Jovian atmospheric dynamics: An update after Galileo and Cassini

TL;DR: A forward modelling approach has been used to relate observations at cloud level to models of shallow or deep jet structure as mentioned in this paper. But the model cannot reproduce all of the observed phenomena, including the stability of Jupiter's zonal jets and the evolution of vortices.
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