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Internally heated convection with rotation: bounds on heat transport

Published online by Cambridge University Press:  19 December 2024

Ali Arslan*
Affiliation:
Institute of Geophysics, ETH Zürich, Zürich, CH-8092, Switzerland
*
†Email address for correspondence: ali.arslan@erdw.ethz.ch

Abstract

This work investigates heat transport in rotating internally heated convection, for a horizontally periodic fluid between parallel plates under no-slip and isothermal boundary conditions. The main results are the proof of lower bounds on the mean temperature, $\overline {{\langle {T} \rangle }}$, and the heat flux out of the bottom boundary, ${\mathcal {F}}_B$, at infinite Prandtl number, where the Prandtl number is the non-dimensional ratio of viscous to thermal diffusion. The lower bounds are functions of the Rayleigh number quantifying the ratio of internal heating to diffusion and the Ekman number, $E$, which quantifies the ratio of viscous diffusion to rotation. We utilise two different estimates on the vertical velocity, $w$, one pointwise in the domain (Yan, J. Math. Phys., vol. 45(7), 2004, pp. 2718–2743) and the other an integral estimate over the domain (Constantin et al., Phys. D: Non. Phen., vol. 125, 1999, pp. 275–284), resulting in bounds valid for different regions of buoyancy-to-rotation dominated convection. Furthermore, we demonstrate that similar to rotating Rayleigh–Bénard convection, for small $E$, the critical Rayleigh number for the onset of convection asymptotically scales as $E^{-4/3}$.

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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 (http://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), 2024. Published by Cambridge University Press.
Figure 0

Figure 1.A non-dimensional schematic diagram for rotating uniform IHC. The upper and lower plates are at the same temperature, and the domain is periodic in the $x$ and $y$ directions and rotates about the $z$ axis. Here ${\mathcal {F}}_B$ and ${\mathcal {F}}_T$ are the mean heat fluxes out the bottom and top plates, $\overline {{\langle {T} \rangle }}$ is the mean temperature and $g$ is the acceleration due to gravity.

Figure 1

Figure 2.Illustration of the upper bounds with blue lines on the Nusselt number, $Nu$, in terms of the Rayleigh, $Ra$, and Ekman numbers, $E$, for infinite Prandtl number rotating RBC, between no-slip boundaries. All bounds hold up to constants that determine the exact sizes of the regions and where applicable red text shows the stress-free result in the same region. The bounds in $A$ are due to Constantin et al. (1999). The green dashed line crossing $A$ and $B$ shows the upper bound obtained from the non-hydrostatic quasigeostrophic approximation (Grooms & Whitehead 2014; Pachev et al.2020). In $B$, the crossover from the bound $Ra^{2/5}$ (Doering & Constantin 2001) to $Ra^{4/11}(E^{-1}+1)^{4/11}$ (Yan 2004) is shown by a blue circle. Similarly in region $C$ the crossover from $Ra^{4/11}$ (Yan 2004) to $E^{-4/5} Ra^{1/5}$ (Constantin et al.2001) is shown by a blue square. Region $D$ shows the bounds for buoyancy-driven convection (Otto & Seis 2011; Whitehead & Doering 2011b). The transition from $C$ to $D$ is continuous up to logarithmic corrections (Constantin et al.1999).

Figure 2

Table 1.Summary of the lower bounds on ${\mathcal {F}}_B$ and $\overline {{\langle {T} \rangle }}$ proven in this work. The constants in the bounds are collated in Appendix A for brevity, while $E_0 = 5.4927$, $E_1=8$ and $E_m = 41.4487$. Region I corresponds to buoyancy-dominated convection, region II corresponds to solid body rotation, region III corresponds to buoyancy or rotation-dominated convection and region IV corresponds to rotation-dominated convection provided $R>R_L(E)$ where $R_L$ is the value of $R$ above which the system is linearly unstable.

Figure 3

Figure 3.Plot of $R_L$ against $k$ as given by (3.13) for Ekman numbers ranging from $10^{-37}$ (red) to $10^{-13}$ (yellow). The blue dots represent the minimum $R_L$ in $k$, and the inset demonstrates that the minimum wavenumber $k_m$ varies as $E^{-1/3}$ with a compensated plot.

Figure 4

Figure 4.Illustrations of the lower bounds on the flux out of the bottom boundary, ${\mathcal {F}}_B$, between no-slip and isothermal boundary conditions at infinite $Pr$, the logarithmic corrections in the bounds, table 1, are suppressed for brevity. The blue plot is the bound derived in § 4.4, valid up to $E =E_m\sim 41.4487$ and $E_0 = 4.1688$. The bound derived in § 4.5 is shown with a green dashed line. The dashed horizontal line denotes when all heat transport is by conduction and ${\mathcal {F}}_B=\frac 12$. In $D$, we show the bounds for stress-free (top, red) and no-slip (bottom, blue) at zero rotation (Arslan & Rojas 2024).

Figure 5

Figure 5.Sketches of the functions $\tau (z)$ in (4.10) and $\lambda (z)$ in (4.11) used to prove (1), where $\delta$ is the boundary layer width at the bottom, $\varepsilon$ the boundary layer width at the top of the domain and $a$ is (4.12).

Figure 6

Figure 6.Illustration of the lower bounds on the mean temperature between no-slip and isothermal boundary conditions at infinite $Pr$. The blue plot is the bound derived in § 5.3, valid up to $E_m \sim 41.4487$ and $E_1=8$. The bounds derived in § 5.4 are shown with a green plot. The dashed horizontal line denotes when all heat transport is by conduction and $\overline {{\langle {T} \rangle }}=\frac {1}{12}$. In $D$, we show the previously known best bound for stress-free (top, red) (Whitehead & Doering 2012) and no-slip (bottom, blue) (Whitehead & Doering 2011a) at zero rotation.

Figure 7

Figure 7.Sketches of the functions $\varphi (z)$ in (5.8) used to prove (1), where $\delta$ is the boundary layer widths.

Figure 8

Figure 8.The Rayleigh and Ekman number diagrams for the bounds (4.47), (4.67), (5.23) and (5.34). Grey areas denote regions where the bounds proven in this work do not hold. We plot the regions of validity for the bounds on ${\mathcal {F}}_B$ in (a) and for $\overline {{\langle {T} \rangle }}$ in (b). The blue solid lines correspond to $E= 1.7671 \,R^{-2}$ in (a) and $E=0.3102\, R^{-2/3}$ in (b), with the blue area denoting region IV. The horizontal red solid lines are $E_0 = 5.4927$ in (a) and $E_1 = 8$ in (b) and the red area is region III, where for (b) IIIa is the purple zone with the solid purple line corresponding to $E = 1.9273\, R^{-5/9}$. In both figures, the horizontal yellow lines are $E_m = 41.4487$ with the yellow zone corresponding to region I. The vertical dashed lines are $R_L=26926.6$ and the green dashed lines are the asymptotic result of (3.15). The four main regions are labelled I to IV.

Figure 9

Figure 9.Plots of the ratio of lower bounds on ${\mathcal {F}}_B$ and $\overline {{\langle {T} \rangle }}$ relative to the best-known bounds at zero rotation ${\mathcal {F}}_{B0}$ and $\overline {{\langle {T} \rangle }}_0$ (Whitehead & Doering 2011a; Arslan & Rojas 2024), for $E = 1\times 10^{-16}$ in (a) and (c) and $R=1\times 10^8$ in (b) and (d). In all of the subplots, the blue lines are the lower bounds in region IV, the red lines are the bounds in region III and the yellow lines are the bounds in Region I, while purple lines in (c) and (d) are the bounds valid in regions Ia and IIIa for $\overline {{\langle {T} \rangle }}$. The bounds themselves are in table 1. Vertical dotted lines show the intersections of the regions for each bound.