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Stably stratified square cavity subjected to horizontal oscillations: responses to small amplitude forcing

Published online by Cambridge University Press:  22 March 2021

Hezekiah Grayer II
Affiliation:
School of Mathematical and Statistical Sciences, Arizona State University, Tempe, AZ 85287, USA
Jason Yalim
Affiliation:
School of Mathematical and Statistical Sciences, Arizona State University, Tempe, AZ 85287, USA
Bruno D. Welfert
Affiliation:
School of Mathematical and Statistical Sciences, Arizona State University, Tempe, AZ 85287, USA
Juan M. Lopez*
Affiliation:
School of Mathematical and Statistical Sciences, Arizona State University, Tempe, AZ 85287, USA
*
Email address for correspondence: juan.m.lopez@asu.edu

Abstract

A stably stratified fluid-filled two-dimensional square cavity is subjected to harmonic horizontal oscillations with frequencies less than the buoyancy frequency. The static linearly stratified state, which is an equilibrium of the unforced system, is not an equilibrium for any non-zero forcing amplitude. As viscous effects are reduced, the horizontally forced flows computed from the Navier–Stokes–Boussinesq equations tend to have piecewise constant or piecewise linear vorticity within the pattern of characteristic lines originating from the corners of the cavity. These flows are well described in the inviscid limit by a perturbation analysis of the unforced equilibrium using the forcing amplitude as the small perturbation parameter. At first order, this perturbation analysis leads to a forced linear inviscid hyperbolic system subject to boundary conditions and spatio-temporal symmetries associated with the horizontal forcing. A Fredholm alternative determines the type of solutions of this system: either the response is uniquely determined by the forcing, or it is resonant and corresponds to an intrinsic mode of the cavity. Both types of responses are investigated in terms of a waveform function satisfying a set of functional equations and are related to the behaviour of the characteristics of the hyperbolic system. In particular, non-retracing (ergodic) characteristics may lead to fractal responses. Models of viscous dissipation are also formulated to adjust the linear inviscid model for viscous effects obtained in the viscous nonlinear simulations.

Information

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 in any medium, provided the original work is properly cited.
Copyright
© The Author(s), 2021. Published by Cambridge University Press
Figure 0

Figure 1. Schematic of the stably stratified square cavity under harmonic horizontal forcing, together with the effective gravity vector $\boldsymbol {g}_{eff}$ relative to the horizontally oscillating cavity. A snapshot of the vorticity $\eta$ is shown corresponding to buoyancy number $R_N=10^6$, Prandtl number ${Pr}=1$, forcing frequency $\omega =0.71$ and forcing amplitude $\alpha =1.75 \times 10^{-6}$.

Figure 1

Figure 2. Bode plot, consisting of $(a)$ magnitude response curves, $\langle \mathcal {E}\rangle _\tau$ vs. $\omega ^2$, and $(b)$ phase lag response curves, $\varphi$ vs. $\omega ^2$, for $R_N$ as indicated. The rational values indicated are the ratios $r=n/m$ at squared frequencies $\omega ^2=1/(1+r^2)$.

Figure 2

Figure 3. Snapshots of the vorticity $\eta$ at indicated $\omega ^2$ and $R_N$, at times when $\eta$ at the origin is maximal. The supplementary movie 1 animates these response flows over one forcing period.

Figure 3

Figure 4. Snapshots of the temperature deviation $\theta$ at indicated $\omega ^2$ and $R_N$, at times corresponding to a quarter period after $\eta$ is maximal at the origin. The supplementary movie 2 animates these response flows over one forcing period.

Figure 4

Figure 5. Horizontal profiles at $z=0$ of the vorticity $\eta$ and temperature deviation $\theta$ from selected snapshots from figures 3 and 4 at $\omega ^2$ and $R_N$ as indicated.

Figure 5

Figure 6. Waveform function $f_r$ in $[-1.5,1.5]\times [-1.25,1.25]$ and the associated scaled forced responses $\eta _r$ at phase 0 and $\theta _r$ at phase ${\rm \pi} /2$, from (4.15) at $r$ as indicated. The blue curve is the 2-periodic extension of the red curve $f_r$ defined in the interval $[-(1+r)/2,(1+r)/2]$.

Figure 6

Figure 7. Waveform function $f_r$ in $[-1.5,1.5]\times [-1.25,1.25]$ and associated scaled forced responses $\eta _r$ at phase 0 and $\theta _r$ at phase ${\rm \pi} /2$ for a series of rational $r$ values converging to the irrational $1/\sqrt {2}$, corresponding to $\sigma _r^2=2/3$. The blue curve is the 2-periodic extension of the red curve $f_r$ defined in the interval $[-(1+r)/2,(1+r)/2]$.

Figure 7

Figure 8. Zoom-in in the neighbourhood of $(0.5,0)$ for $\eta _r$ at phase 0; (ac) waveform function $f_{1/\sqrt {2}}$ in windows $[-1.5,1.5]\times [-1.25,1.25]$ (a,d), $[0,1]\times [0,1]$ (b,e) and $[s/2, 1-s/2]\times [s, 1]$ (cf) with $s=2\sqrt {2}-2$; (df) $\eta _r$ in regions $[-0.5, 0.5]\times [-0.5, 0.5]$ (square cavity; a,d), $[0, 1/2]\times [-1/4, 1/4]$ (b,e) and $[s/2, 1/2]\times [-(1-s)/4,(1-s)/4]$ (c,f). The supplementary movie 3 shows a continuous zoom-in of the response $\eta _r$ about the point $(x,z)=(0.5,0)$.

Figure 8

Figure 9. Scaled waveform function $f_r$ in $[-1.5,1.5]\times [-1.25,1.25]$ and the associated scaled forced responses $\eta _r$ at phase 0 and $\theta _r$ at phase ${\rm \pi} /2$ for a series of rational $r$ values converging to $r=1$, corresponding to $\sigma _r^2=1/2$. The blue curve is the 2-periodic extension of the red curve $f_r$ defined in the interval $[-(1+r)/2,(1+r)/2]$.

Figure 9

Figure 10. Shifted Euler splines $S_q$, of regularity class $C^{q-1}$, shown in a window $[-1.5,1.5]\times [-1.25,1.25]$: $(a)$$S_1(\zeta -0.5)=E_1(\zeta +0.5)/E_1(0)=2\zeta$ for $-0.5<\zeta <0.5$, $(b)$$S_2(\zeta -0.5)=E_2(\zeta )/E_2(0.5)= 4\zeta (1-\zeta )$ for $0<\zeta <1$, $(c)$$S_3(\zeta -0.5)= -E_3(\zeta +0.5)/E_3(0)=\zeta (3-4\zeta ^2)$ for $-0.5<\zeta <0.5$, and $(d)$$S_\infty (\zeta -0.5)=\sin ({\rm \pi} \zeta )$, where $E_q$ is the Euler polynomial of degree $q$.

Figure 10

Figure 11. Scaled waveform function $f_r$ in $[-1.5,1.5]\times [-1.25,1.25]$ and associated scaled forced response ($\eta _r$ at phase 0 and $\theta _r$ at phase ${\rm \pi} /2$) for two values $r=(300\pm 1)/500$ close to $3/5$ (a,e,i,d,h,l) and eigenmode at $r=3/5$ (b,f,j,c,g,k, associated with opposite scaling). The blue curve is the 2-periodic extension of the red curve $f_r$ defined in the interval $[-(1+r)/2,(1+r)/2]$.

Figure 11

Figure 12. Plots of the vorticity $\eta _r$ and temperature deviation $\theta _r$ associated with the partial sums in the series expansion of $M_{5:3}$ in (4.24), for the number of indicated terms.

Figure 12

Figure 13. Plots of the vorticity $\eta _r$ associated with the partial sums in the series expansion of $R_f$ in (4.32), at $\sigma _r^2$ and a number of terms as indicated.

Figure 13

Figure 14. Plots of the temperature deviation $\theta _r$ associated with the partial sums in the series expansion of $R_f$ in (4.32), at $\sigma _r^2$ and a number of terms as indicated.

Figure 14

Figure 15. Graph of the enstrophy $\langle \mathcal {E}\rangle _\tau$ from (5.1) scaled by $\alpha ^2/r$, evaluated at $10^6$ values $\omega ^2\in (0,1)$ using $(a)$$1+9=10$ terms, $(b)$$\lfloor 1+9/\sqrt {r}\rfloor$ term(s) or $(c)$$\lfloor 1+99/\sqrt {r}\rfloor$ term(s) in the series, where $\lfloor x\rfloor$ represents the integer part of $x$. Also shown in $(c)$ are the scaled curves obtained from DNS for the different values of $R_N$ from figure 2 using the same colours, and a viscous correction factor $\gamma$ from (5.2). The supplementary movie 4 shows a frequency sweep of 9999 inviscid solutions uniformly distributed between $\omega ^2\in (0,1)$ at phase 0 for $\eta _r$ and phase ${\rm \pi} /2$ for $\theta _r$.

Figure 15

Figure 16. Vorticity $\eta$ from DNS at $R_N=10^7$$(a{,}c{,}e{,}g{,}i{,}k{,}m{,}o{,}q)$ and $\eta _r$ from the inviscid theory $(b{,}d{,}f{,}h{,}j{,}l{,}n{,}p{,}r)$, all at phase $0$, at the indicated squared forcing frequencies $\omega ^2$ (with the corresponding $r$ values indicated). The inviscid responses at $\sigma _r^2=0.3$, $0.4$, $0.6$ and $0.7$ are fractal and are obtained as limits of sequences with rational $r$.

Figure 16

Figure 17. Temperature deviation $\theta$ from DNS at $R_N=10^7$$(a{,}c{,}e{,}g{,}i{,}k{,}m{,}o{,}q)$ and $\theta _r$ from the inviscid theory $(b{,}d{,}f{,}h{,}j{,}l{,}n{,}p{,}r)$, all at phase ${\rm \pi} /2$, at the indicated squared forcing frequencies $\omega ^2$ (with the corresponding $r$ values indicated). The inviscid responses at $\sigma _r^2=0.3$, $0.4$, $0.6$ and $0.7$ are fractal and are obtained as limits of sequences with rational $r$.

Figure 17

Figure 18. (gv) Snapshots of $\eta$ and $\theta$ from the DNS limit cycle at $R_N=10^7$ and $\omega ^2=0.6$ over one forcing period (see supplementary movies 1 and 2), while (af,wz,aa,ab) show inviscid standing wave responses at maximal amplitude at $r$ and $\sigma _r^2$ values as indicated.

Figure 18

Figure 19. Horizontal profiles of the (scaled) vorticity $\eta$ and temperature deviation $\theta$ at $z=0$ and $\omega ^2$ as indicated. The black profiles correspond to the inviscid prediction based on the expression (4.22) (for a,b,i,j) or (4.15) (for ch). The waveform function $f_r$ used in these expressions is obtained either explicitly for the cases $\omega ^2=0.5$, $0.8$ and $0.9$ associated with rational values of $r$, or via the series (4.31) truncated to the indicated number of terms for the cases $\omega ^2=0.6$ and $0.7$ associated with irrational values of $r$. An appropriate factor is used to scale the resonant cases (eigenmodes; a,b,i,j) in order to facilitate the comparison with the DNS response obtained at $R_N=10^7$ from figure 5 (here shown in cyan).

Figure 19

Figure 20. Horizontal profiles of the (scaled) vorticity $\eta$ and temperature deviation $\theta$ at $z=0$ similar to figures 19(c,d) and 19(e,f), but using a mollifier rather than hard truncation of the spectral series (4.31) of the waveform function $f_r$ to account for viscous effects.

Figure 20

Figure 21. Panels (ad) show the 2-D $\eta$ and $\theta$ at $R_N=10^6$ and $\omega^2$ as indicated (repeated from figures 3 and 4 for ease of comparison) and panels (eg) show the 3-D $\eta$ and $\theta$ in the spanwise midplane using the same colour levels as in the 2-D cases (ad). Panels (il) show the corresponding isosurfaces of the 3-D solutions (using a different colour map), with the boundary layer regions clipped.

Figure 21

Figure 22. The 2-periodic linear spline $f_{4/11}$. The dots indicate the interpolating points. All data can be obtained from $(x_j,f_j)$, $j=1,3,5,7,9$ and $11$, via the symmetries approximately $x=0$ and $x=0.5$. The range of $x$-values associated with the red part is the range $[-(1+4/11)/2,(1+4/11)/2]\approx [-0.68,0.68]$ where $f$ must be defined in order to evaluate the response everywhere in the square cavity.

Figure 22

Figure 23. Signs of coefficients $a_j$ for $m=11$ and $n$ and $j$ as indicated; blue is negative and red is positive.

Figure 23

Figure 24. $(a)$ Signed complex numbers $2a_j\exp [i(2j-1){\rm \pi} /(2m)]$ for $j=1,\ldots ,m$ with $m=11$. The blue and red nodes correspond to $2a_j=-1$ and $2a_j=1$, respectively, for the $n=4$ case from figure 23. The nodes are labelled by the value of $j$ in the sum (F2). $(b)$ The blue terms $-\exp [i(2j-1){\rm \pi} /(2m)]$ ($\,j=5,6,7$) from $(a)$ are replaced by a red conjugate $\exp [-i(2j-1){\rm \pi} /(2m)]$ and the label in the nodes now represents the value of the counter $\ell$ in the sum (F3). Nodes with successive labels are obtained via multiplication by $\xi =\exp [i(m-n){\rm \pi} /m]$, corresponding to a counter-clockwise turn by an angle equal to $m-n=7$ nodes, starting with $\xi ^{1/2}$ (label 1).

Grayer II et al. supplementary movie 1

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