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Rapidly rotating internally heated convection: bounds on long-time averages

Published online by Cambridge University Press:  21 October 2026

Yutong Zhang*
Affiliation:
Institute for Geophysics, ETH Zurich, Sonneggstrasse 5, Zurich 8092, Switzerland
Ali Arslan
Affiliation:
Institute for Geophysics, ETH Zurich, Sonneggstrasse 5, Zurich 8092, Switzerland
Stefano Maffei
Affiliation:
Institute for Geophysics, ETH Zurich, Sonneggstrasse 5, Zurich 8092, Switzerland
Andrew Jackson
Affiliation:
Institute for Geophysics, ETH Zurich, Sonneggstrasse 5, Zurich 8092, Switzerland
*
Corresponding author: Yutong Zhang, yutong.zhang@eaps.ethz.ch

Abstract

Content of image described in text.

Convection on geophysical and astrophysical scales is subject to rapid rotation and strong heating from within the domain. In studying the long-time behaviour of the solutions for such a system, energy identities fail to capture the effects of rotation because the Coriolis force does no work, and rapid rotation can be prohibitive for direct numerical simulations. Instead, we derive an asymptotically reduced model for rapidly rotating convection driven by uniform internal heating between isothermal stress-free boundaries in a plane periodic layer. The main contribution is the proof of bounds on the mean temperature, and the mean vertical convective heat transport, in terms of the Rayleigh and Ekman numbers, in the limit of infinite Prandtl number. The first quantity measures thermal mixing, and the second the asymmetry in heat leaving the bottom and top boundaries due to convection, and unlike Rayleigh–Bénard convection, the two are not a priori related. We employ alternative estimation techniques to those used in previous studies (Grooms & Whitehead, 2014, Nonlinearity, vol. 28, 29), and identify two distinct scaling behaviours for both quantities. Finally, our bounds are optimised, within the methodology, and provide a rigorous constraint for future studies of rotation-dominated internally heated convection.

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Type
JFM Papers
Creative Commons
Creative Common License - CCCreative Common License - BY
This is an Open Access article, distributed under the terms of the Creative Commons Attribution licence (https://creativecommons.org/licenses/by/4.0/), which permits unrestricted re-use, distribution and reproduction, provided the original article is properly cited.
Copyright
© The Author(s), 2026. Published by Cambridge University Press
Figure 0

Figure 1. (a) A schematic diagram of rotating IHC between two isothermal parallel plates with stress-free boundary conditions. The uniform heating source is denoted by S$S$, and H$H$ is the separation between the two plates in the direction of gravity, g$g$. Horizontal periodicities are LxH$L_x H$ and LyH$L_y H$. The convection is subject to global rotation Ω$\varOmega$. Without loss of generality, the boundary temperature is set to Tb=0$T_b = 0$. Circles indicate flow structures with a characteristic vertical scale H$H$ and horizontal scale E1/3H$E^{1/3}H$. (b) The same flow structures shown in dimensionless coordinates. The vertical and horizontal length units are H$H$ and E1/3H$E^{1/3}H$, respectively, with E≪1$E\ll 1$.

Figure 1

Figure 2. A sketch of the background profile (3.14) featuring quadratic boundary layers.

Figure 2

Figure 3. Lower bounds on ⟨Θ⟩V,t$\langle \varTheta \rangle _{V,t}$ from (3.47) (blue solid line) and (3.49) (red dashed line), compared with the uniform upper bound 1/12$1/12$ (grey solid line) and the numerical maximum (black dots) of (3.15) subject to (3.37) and the condition δ≤1/2$\delta \leq 1/2$. Triangle markers denote the R$\mathcal{R}$ value above which (3.47) and (3.49) are valid, with the red triangle corresponding to a lower threshold of nonlinear convective instability, and the star indicating the linear onset of convection.

Figure 3

Figure 4. A sketch of the background field (4.10) with a quadratic boundary layer and linear bulk.

Figure 4

Figure 5. Figure 5 long description.Upper bounds on ⟨wθ⟩V,t$\langle w\theta \rangle _{V,t}$ from (4.24) (blue solid line) and (4.26) (red dashed line), compared with the uniform bounds 0$0$ and 1/2$1/2$ (grey solid lines), along with the numerical minimum (black dots) of (4.11) subject to the condition (4.18) and δ≤1$\delta \leq 1$. The triangle markers denote the R$\mathcal{R}$ value above which (4.24) and (4.26) are valid, and the star indicates the linear onset of convection.

Figure 5

Figure 6. Numerically optimised bounds and corresponding background fields (a,b) ⟨Θ⟩V,t$\langle \varTheta \rangle _{V,t}$ and (c,d) ⟨wθ⟩V,t$\langle w\theta \rangle _{V,t}$. (a,c) Bounds as functions of the reduced Rayleigh number R$\mathcal{R}$. (b,d) The associated optimised background fields ϕ(Z)$\phi (Z)$. (a,b) Numerical lower bound on ⟨Θ⟩V,t$\langle \varTheta \rangle _{V,t}$ (black solid line), the best applicable analytical bound from (3.47) and (3.49) (blue dashed line), and the uniform upper bound 1/12$1/12$ (horizontal dotted line). The inset shows the compensated numerical bound ⟨Θ⟩V,tR3/4$\langle \varTheta \rangle _{V,t}\mathcal{R}^{3/4}$. The highlighted background fields, in blue, red and yellow, correspond respectively to R=6.51×102$\mathcal{R}=6.51\times 10^{2}$, 2.47×103$2.47\times 10^{3}$ and 8.15×103$8.15\times 10^{3}$. (c,d) Numerical upper bound on ⟨wθ⟩V,t$\langle w\theta \rangle _{V,t}$ (black solid line), the uniform bound 1/2$1/2$ (horizontal dotted line), and the best applicable analytical bound from (4.24) and (4.26) (blue dashed line). The blue, red and yellow background fields correspond respectively to R=300$\mathcal{R}=300$, 500$500$ and 1000$1000$. Grey curves show a selection of the remaining computed background fields.

Figure 6

Figure 7. Lower bounds on ⟨Θ⟩V,t$\langle \varTheta \rangle _{V,t}$ from (3.47) and (3.49) as functions of R$R$ for different values of E$E$ (coloured solid lines). The black solid line shows the bound for non-rotating convection, (6.1). Dotted lines indicate regions where the bounds no longer apply.

Figure 7

Figure 8. (a) Smallest root of (C8) for each given k$k$. The star marks the (k,R)$(k,{\mathcal{R}})$ pair corresponding to marginal linear stability. (b) Velocity and temperature modes at marginal linear stability, with C1$C_1$ and C2$C_2$ set to 1.867$1.867$ and 5.783×10−4$5.783\times 10^{-4}$ respectively. (c,d) Amplitudes of the velocity and temperature modes in one horizontal period.