2008
DOI: 10.1007/s11207-008-9157-0
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Angular Momentum Transport in the Sun’s Radiative Zone by Gravito-Inertial Waves

Abstract: Internal gravity waves constitute an efficient process for angular momentum transport over large distances. They are now seen as an important ingredient in understanding the evolution of stellar rotation and can explain the Sun's quasi-flat internal-rotation profile. Because the Sun's rotation frequency is of the same order as that of the waves, it is now necessary to refine our description of wave propagation and to take into account the action of the Coriolis acceleration in a coherent way. To achieve this g… Show more

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Cited by 62 publications
(86 citation statements)
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“…The dynamics of the Sun radiation zone is largely uncertain as suggested by helioseismology (Turck-Chièze et al 2004). It probably involves angular momentum transport through internal waves (Charbonnel & Talon 2005;Mathis et al 2008). Moreover, the mixing of the radiative interior associated with rotation (as in the tachocline) interacts with diffusion along the evolution (Brun et al 1999).…”
Section: Convection Length Scales From the Sunmentioning
confidence: 99%
“…The dynamics of the Sun radiation zone is largely uncertain as suggested by helioseismology (Turck-Chièze et al 2004). It probably involves angular momentum transport through internal waves (Charbonnel & Talon 2005;Mathis et al 2008). Moreover, the mixing of the radiative interior associated with rotation (as in the tachocline) interacts with diffusion along the evolution (Brun et al 1999).…”
Section: Convection Length Scales From the Sunmentioning
confidence: 99%
“…2.5). As shown in Mathis et al (2008) in the hydrodynamical case, this hypothesis allows us to separate the variables in the treatment of the adiabatic dynamical equations. This net variable separation becomes impossible for a general differential rotation law and azimuthal magnetic field (Ω (r, θ), Fig.…”
Section: The Magnetic Topology and Differential Rotationmentioning
confidence: 99%
“…This is due to the choice to study in a first step the "weak differential rotation case" for which Ω s > > ΔΩ. This means that the impact of ΔΩ on θ c;m constitutes only a small correction that does not change its main behaviour (see Mathis et al 2008, in the hydrodynamical case). A general differential rotation in which the critical latitude explicitely depends on the angular rotation profile and on its vertical and latitudinal gradients has been studied in Mathis (2009) in the purely hydrodynamical case and will be studied in Paper III.…”
Section: The Jwkb Approximationmentioning
confidence: 99%
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