1968
DOI: 10.1017/s0022112068001655
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Steady fluid flow in a precessing spheroidal shell

Abstract: The linear boundary-layer analysis by Stewartson & Roberts (1963) and by Roberts & Stewartson (1965) for the motion of a viscous fluid inside the spheroidal cavity of a precessing rigid body is extended to include effects due to the nonlinear terms in the boundary-layer equation. The most significant consequence is a differential rotation super-imposed on the constant vorticity flow given by the linear theory. In addition it is shown that a tidal bulge of the cavity forces a fluid motion similar to that caused… Show more

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Cited by 214 publications
(308 citation statements)
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“…It is not understood why these internal shear layers appear on top of the flow in Fig. 13 except for the strongest of them (Busse 1968), but they are a robust feature of both experiments and simulations. The third type is a consequence of the streamline geometry in Fig.…”
Section: Tidally Driven and Precession Driven Dynamosmentioning
confidence: 95%
“…It is not understood why these internal shear layers appear on top of the flow in Fig. 13 except for the strongest of them (Busse 1968), but they are a robust feature of both experiments and simulations. The third type is a consequence of the streamline geometry in Fig.…”
Section: Tidally Driven and Precession Driven Dynamosmentioning
confidence: 95%
“…However, it is generally believed that the effect of the singularities is weak and insignificant because the mass flux from the critical regions is much smaller than that from the rest of the boundary layer (see e.g. Roberts & Stewartson 1965;Busse 1968;Tilgner & Busse 2001).…”
Section: K H Chan and X Liaomentioning
confidence: 99%
“…In particular the occurrence of this 'tidal' instability together with thermal or compositional convection in the molten cores of planets, such as the Earth, might be of prime importance in the generation or in the dynamics of the geomagnetic fields (Kerswell, 1994;Kerswell and Malkus, 1998). Recent measurements of magnetic fields around relatively small planets such as the Jovian moons Io and Ganymède (Kivelson et al, 1996a,b) may reinforce the interest in the study of inertial instabilities such as the elliptical or the precessional ones (Malkus, 1968;Busse, 1968;Noir et al, 2001;Kerswell, 1993;Lorenzani and Tilgner, 2003). Aldridge et al (1997), and Seyed-Mahmoud et al (2000 have performed computations and built as already mentioned, a rotating deformable shell where they observed the presence of the elliptical instability.…”
Section: Introductionmentioning
confidence: 99%