4.5 Article

Onset of Convection in Rotating Spherical Shells: Variations With Radius Ratio

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EARTH AND SPACE SCIENCE
卷 10, 期 1, 页码 -

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AMER GEOPHYSICAL UNION
DOI: 10.1029/2022EA002606

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planetary interiors; rotating convection; spherical shells; eigenvalue; numerical methods; dynamo theory

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This article studies convection in rotating spherical layers of fluid, focusing on the effect of the radius ratio of the spherical shell on critical quantities. By computing numerical results of critical quantities over a wide range of parameters, it is found that theoretical scaling laws can well explain these variations, but the radius ratio of the spherical shell also has an impact.
Convection in rotating spherical layers of fluid is ubiquitous in spherical astrophysical objects like planets and stars. A complete understanding of the magnetohydrodynamics requires understanding of the linear problem-when convection onsets in these systems. This is a fluid dynamics problem that has been studied since the early 1900s. Theoretical scaling laws exist for the variation of critical quantities-the Rayleigh number Ra-c, the azimuthal wavenumber m(c), and the angular drift frequency omega(c)-with respect to the Ekman number E. However, their variation with the radius ratio chi of the spherical shell is still poorly studied. To address this, we use an open source eigenvalue code Kore to compute these critical quantities over an extensive range of parameters spanning four decades in Ekman number and a dense grid of radius ratio from very thick to very thin shells, focusing on no-slip and fixed temperature boundary conditions. We find that these variations are explained well by the theoretical scaling laws, especially at low E, but variations in radius ratio also exist. We obtain scaling laws of boundary layer thicknesses and spatial extent of onset modes with respect to the Ekman number which differ only slightly from theoretical scalings. We show that our data set can be used to obtain good estimates of critical quantities in the moderate E range, where the vast majority of current geophysical and astrophysical fluid dynamics simulations are performed, yet where asymptotic theory is only moderately accurate. We further verify asymptotic predictions and determine best-fit asymptotic model coefficients.

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