1993
DOI: 10.1017/s0022112093000746
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On equatorially trapped boundary inertial waves

Abstract: Solutions of the Poincaré equation describing equatorially trapped three-dimensional boundary travelling waves in rotating spherical systems are discussed. It is shown that the combined effects of Coriolis forces and spherical curvature enable the equatorial region to form an equatorial waveguide tube with characteristic latitudinal radius (2/m)1/2 and radial radius (1/m), where m is azimuthal wavenumber. Inertial waves with sufficiently simple structure along the axis of rotation and sufficiently small azimut… Show more

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Cited by 53 publications
(43 citation statements)
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“…The left three columns correspond to the critical m c = 1 mode of convection. The right columns show the critical inertial m c = 50 equatorially-attached mode of convection, of the type described in Zhang (1993). The size of the equatorial waveguide agrees very well with that of the inertial solutions found in that paper: consequently, due to the high wave number the conduction state is stable in almost all of the body of the fluid.…”
Section: Taylor Number Dependencesupporting
confidence: 82%
See 1 more Smart Citation
“…The left three columns correspond to the critical m c = 1 mode of convection. The right columns show the critical inertial m c = 50 equatorially-attached mode of convection, of the type described in Zhang (1993). The size of the equatorial waveguide agrees very well with that of the inertial solutions found in that paper: consequently, due to the high wave number the conduction state is stable in almost all of the body of the fluid.…”
Section: Taylor Number Dependencesupporting
confidence: 82%
“…In this context, some authors first looked for solutions of the Poincaré equation in rotating spherical geometry. In a paper by Zhang (1993) symmetric and antisymmetric equatorially-attached modes of convection (EA), which travelled azimuthally, in either in the prograde or the retrograde direction, were found. In any of the cases, the latitudinal and radial radii of the waves were r l = (2/m) 1/2 and r r = (1/m), respectively, m being the azimuthal wave number.…”
Section: Introductionmentioning
confidence: 99%
“…Ogilvie & Lin 2004). There also exist geomagnetic variations of non-axisymmetric magnetic flux, dominated by a single wavenumber at the core surface in the equatorial region, that are likely to be indicative of a magnetically modified equatorially trapped inertial wave (Zhang 1993;Finlay & Jackson 2003).…”
Section: Introductionmentioning
confidence: 99%
“…According to Zhang (1993Zhang ( , 1994, the equatorially trapped modes are quasiinertial waves, i.e. at leading order they are solutions of the Poincaré equation.…”
Section: Introductionmentioning
confidence: 99%