1980
DOI: 10.1080/03091928008243663
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Shear instability of differential rotation in stars

Abstract: The two-dimensional (horizontal) shear instability of a differentially rotating star is examined. A solar-typc rotation law is investigated. and it is found that for equatorial accelerations there is instability when there is a difference of 29% between the angular velocity of the equator and the poles.

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Cited by 76 publications
(45 citation statements)
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“…see Gilman 2000;Brummell et al 2002;Rogers & Glazmaier 2005), or by instabilities (e.g. see Watson 1981;Charbonneau et al 1999) -, we demonstrated how turbulence level and transport are reduced via shearing in a non-trivial manner (see also Burrell 1997;Kim 2004 in a simplified three-dimensional (3D) hydrodynamic turbulence. In particular, turbulent transport of chemical species and angular momentum are shown to become strongly anisotropic with much more efficient transport in the horizontal (latitudinal) direction than in the vertical (radial) direction due to shear stabilisation by a strong radial shear.…”
Section: Introductionmentioning
confidence: 99%
“…see Gilman 2000;Brummell et al 2002;Rogers & Glazmaier 2005), or by instabilities (e.g. see Watson 1981;Charbonneau et al 1999) -, we demonstrated how turbulence level and transport are reduced via shearing in a non-trivial manner (see also Burrell 1997;Kim 2004 in a simplified three-dimensional (3D) hydrodynamic turbulence. In particular, turbulent transport of chemical species and angular momentum are shown to become strongly anisotropic with much more efficient transport in the horizontal (latitudinal) direction than in the vertical (radial) direction due to shear stabilisation by a strong radial shear.…”
Section: Introductionmentioning
confidence: 99%
“…Since this is rapid compared to thermal adjustment times, each set uniformly heats a low-latitude ring at the radial distances of its hot spots. Such rings can be dynamically unstable to horizontal turbulence (Watson 1981;Spiegel & Zahn 1992) and probably become warm shells. A likely observation of a warm ring or shell is discussed in Section 4.1.…”
Section: Rotation Rates and Overlappingmentioning
confidence: 99%
“…However, these works were restricted to the case where the mean flow is sheared in the vertical direction while our differential rotation profile is sheared in the horizontal direction. Using a different approach, Watson (1981) studied the stability of a conical rotation profile similar to ours with respect to non-axisymmetric wavelike perturbations, but was restricted to the case of two-dimensional Rossby waves with negligible radial velocity.…”
Section: Critical Layersmentioning
confidence: 99%