Cox, GA, Davies, CJ orcid.org/0000-0002-1074-3815, Livermore, PW orcid.org/0000-0001-7591-6716 et al. (1 more author) (2019) Penetration of boundary-driven flows into a rotating spherical thermally stratified fluid. Journal of Fluid Mechanics, 864. pp. 519-553. ISSN 0022-1120
Abstract
Motivated by the dynamics within terrestrial bodies, we consider a rotating, strongly thermally stratified fluid within a spherical shell subject to a prescribed laterally inhomogeneous heat-flux condition at the outer boundary. Using a numerical model, we explore a broad range of three key dimensionless numbers: a thermal stratification parameter (the relative size of boundary temperature gradients to imposed vertical temperature gradients), 10^−3 ≤ S ≤ 10^4, a buoyancy parameter (the strength of applied boundary heat-flux anomalies), 10^−2 ≤ B ≤ 10^6, and the Ekman number (ratio of viscous to Coriolis forces), 10^−6 ≤ E ≤ 10^−4. We find both steady and time-dependent solutions and delineate the regime boundaries. We focus on steady-state solutions, for which a clear transition is found between a low S regime, in which buoyancy dominates the dynamics, and a high S regime, in which stratification dominates. For the low-S regime, we find that the characteristic flow speed scales as B^2/3, whereas for high-S, the radial and horizontal velocities scale respectively as ur ~ S^−1, uh ~S^−3/4 B^1/4 and are confined within a thin layer of depth (SB)^−1/4 at the outer edge of the domain. For the Earth, if lower mantle heterogeneous structure is due principally to chemical anomalies, we estimate that the core is in the high-S regime and steady flows arising from strong outer boundary thermal anomalies cannot penetrate the stable layer. However, if the mantle heterogeneities are due to thermal anomalies and the heat-flux variation is large, the core will be in a low-S regime in which the stable layer is likely penetrated by boundary-driven flows.
Metadata
Item Type: | Article |
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Authors/Creators: |
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Copyright, Publisher and Additional Information: | © 2019 Cambridge University Press. This article has been published in a revised form in Journal of Fluid Mechanics, https://doi.org/10.1017/jfm.2018.999. This version is free to view and download for private research and study only. Not for re-distribution, re-sale or use in derivative works. Uploaded in accordance with the publisher's self-archiving policy. |
Keywords: | buoyancy-driven instability; rotating flows; stratified flows |
Dates: |
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Institution: | The University of Leeds |
Academic Units: | The University of Leeds > Faculty of Environment (Leeds) > School of Earth and Environment (Leeds) > Inst of Geophysics and Tectonics (IGT) (Leeds) |
Funding Information: | Funder Grant number NERC NE/L011328/1 NERC NE/G014043/1 |
Depositing User: | Symplectic Publications |
Date Deposited: | 15 Feb 2019 13:36 |
Last Modified: | 11 Aug 2019 00:41 |
Status: | Published |
Publisher: | Cambridge University Press |
Identification Number: | 10.1017/jfm.2018.999 |
Open Archives Initiative ID (OAI ID): | oai:eprints.whiterose.ac.uk:142544 |