Publication Date:
2011-12-31
Description:
A linear stability analysis was performed in order to study the onset of thermal convection in the presence of a strong viscosity variation, with a special emphasis on the condition for the stagnant-lid (ST) convection where a convection takes place only in a sublayer beneath a highly viscous lid of cold fluid. We consider the temporal evolution (growth or decay) of an infinitesimal perturbation superimposed to a Boussinesq fluid with an infinite Prandtl number which is in a static (motionless) and conductive state in a basally heated planar layer or spherical shell. The viscosity of the fluid is assumed to be exponentially dependent on temperature. The linearized equations for conservations of mass, momentum, and internal (thermal) energy are numerically solved for the critical Rayleigh number, Ra c , as well as the radial profiles of eigenfunctions for infinitesimal perturbations. The above calculations are repeatedly carried out by systematically varying (i) the magnitude of the temperature dependence of viscosity, E , and (ii) the ratio of the inner and outer radii of the spherical shell, γ . A careful analysis of the vertical structure of incipient flows demonstrated that the dominance of the ST convection can be quantitatively identified by the vertical profile of Δ h (a measure of conversion between horizontal and vertical flows), regardless of the model geometries. We also found that, in the spherical shell relevant to the Earth’s mantle ( γ = 0.55), the transition into ST convection takes place at the viscosity contrast across the layer r h @ 10 4 . Taken together with the fact that the threshold value of r η falls in the range of r η for a so-called sluggish-lid convection, our finding suggests that the ST-mode of convection with horizontally elongated convection cells is likely to arise in the Earth’s mantle solely from the temperature-dependent viscosity. Content Type Journal Article Category Original Article Pages 1-20 DOI 10.1007/s00162-011-0250-x Authors Masanori Kameyama, Geodynamics Research Center, Ehime University, Matsuyama, 790-8577 Japan Hiroki Ichikawa, Geodynamics Research Center, Ehime University, Matsuyama, 790-8577 Japan Arata Miyauchi, Geodynamics Research Center, Ehime University, Matsuyama, 790-8577 Japan Journal Theoretical and Computational Fluid Dynamics Online ISSN 1432-2250 Print ISSN 0935-4964
Print ISSN:
0935-4964
Electronic ISSN:
1432-2250
Topics:
Mechanical Engineering, Materials Science, Production Engineering, Mining and Metallurgy, Traffic Engineering, Precision Mechanics
,
Physics
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