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.
CORE (COnnecting REpositories)
CORE (COnnecting REpositories)