1998
DOI: 10.1016/s0377-0265(97)00028-6
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Wave dispersion in a rotating, differentially-heated fluid model

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Cited by 3 publications
(2 citation statements)
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“…The radial, azimuthal and vertical (or axial) coordinates are denoted r, ϕ and z, respectively, with unit vectors e r , e ϕ and e z . This model is essentially the same as those used in many previous numerical studies, including, for example, [23,2,24,17,12]. With air as the working fluid, it is expected that the Boussinesq approximation will lead to quantitatively accurate results for ∆T < 50 [12], while above this, the results may only be qualitatively accurate.…”
Section: Model Equationsmentioning
confidence: 99%
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“…The radial, azimuthal and vertical (or axial) coordinates are denoted r, ϕ and z, respectively, with unit vectors e r , e ϕ and e z . This model is essentially the same as those used in many previous numerical studies, including, for example, [23,2,24,17,12]. With air as the working fluid, it is expected that the Boussinesq approximation will lead to quantitatively accurate results for ∆T < 50 [12], while above this, the results may only be qualitatively accurate.…”
Section: Model Equationsmentioning
confidence: 99%
“…However, this would not simplify the analysis, and thus, we choose to work with the equations in the form (7) - (9). This follows previous numerical work on this problem [23,2,24,17]. The parameters of interest are the rotation rate Ω and the temperature difference ∆T between the inner and outer annulus walls, because these are the quantities (external variables) that are generally varied in an experiment.…”
Section: Model Equationsmentioning
confidence: 99%