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On the inertial wave activity during spin-down in a rapidly rotating penny shaped cylinder: a reduced model

Published online by Cambridge University Press:  06 February 2020

L. Oruba*
Affiliation:
Laboratoire Atmosphères Milieux Observations Spatiales (LATMOS/IPSL), Sorbonne Université, UVSQ, CNRS, Paris, France
A. M. Soward*
Affiliation:
School of Mathematics, Statistics and Physics, Newcastle University, Newcastle upon TyneNE1 7RU, UK
E. Dormy*
Affiliation:
Département de Mathématiques et Applications, UMR-8553, École Normale Supérieure, CNRS, PSL University, 75005Paris, France

Abstract

In a previous paper, Oruba et al. (J. Fluid Mech., vol. 818, 2017, pp. 205–240) considered the ‘primary’ quasi-steady geostrophic (QG) motion of a constant density fluid of viscosity $\unicode[STIX]{x1D708}$ that occurs during linear spin-down in a cylindrical container of radius $r^{\dagger }=L$ and height $z^{\dagger }=H$, rotating rapidly (angular velocity $\unicode[STIX]{x1D6FA}$) about its axis of symmetry subject to mixed rigid and stress-free boundary conditions for the case $L=H$. Here, Direct numerical simulation at large $L=10H$ and Ekman numbers $E=\unicode[STIX]{x1D708}/H^{2}\unicode[STIX]{x1D6FA}$ in the range $=10^{-3}{-}10^{-7}$ reveals inertial wave activity on the spin-down time scale $E^{-1/2}\unicode[STIX]{x1D6FA}^{-1}$. Our analytic study, based on $E\ll 1$, builds on the results of Greenspan & Howard (J. Fluid Mech., vol. 17, 1963, pp. 385–404) for an infinite plane layer $L\rightarrow \infty$. In addition to QG spin-down, they identify a ‘secondary’ set of quasi-maximum frequency $\unicode[STIX]{x1D714}^{\dagger }\rightarrow 2\unicode[STIX]{x1D6FA}$ (MF) inertial waves, which is a manifestation of the transient Ekman layer, decaying algebraically $\propto 1/\surd \,t^{\dagger }$. Here, we acknowledge that the blocking of the meridional parts of both the primary-QG and the secondary-MF spin-down flows by the lateral boundary $r^{\dagger }=L$ provides a trigger for other inertial waves. As we only investigate the response to the primary QG-trigger, we call the model ‘reduced’ and for that only inertial waves with frequencies $\unicode[STIX]{x1D714}^{\dagger }<2\unicode[STIX]{x1D6FA}$ are triggered. We explain the ensuing organised inertial wave structure via an analytic study of the thin disc limit $L\gg H$ restricted to the region $L-r^{\dagger }=O(H)$ far from the axis, where we make a Cartesian approximation of the cylindrical geometry. Other than identifying a small scale fan structure emanating from the corner $[r^{\dagger },z^{\dagger }]=[L,0]$, we show that inertial waves, on the gap length scale $H$, radiated (wave energy flux) away from the outer boundary $r^{\dagger }=L$ (but propagating with a phase velocity towards it) reach a distance determined by the mode with the fastest group velocity.

Information

Type
JFM Papers
Copyright
© The Author(s), 2020. Published by Cambridge University Press
Figure 0

Figure 1. The case $E=10^{-3}$, $\unicode[STIX]{x1D712}$-contours at three distinct instants $t=N\unicode[STIX]{x03C0}/2$ ($N=3,7,11$) when $E^{-1/2}\overline{\unicode[STIX]{x1D712}}_{MF}$ is maximised: panels (a–c), (d–f), (g–i) correspond to $t=4.72$, $11.00$, $17.28$, respectively. (a,d,g) Show the direct numerical simulations $E^{-1/2}\unicode[STIX]{x1D712}_{DNS}$ (colour scale from $-0.3$ to $0.3$); (b,e,h) and (c,f,i) show the filtered DNS, with the geostrophic flow subtracted $\unicode[STIX]{x1D712}_{FNS}$ and the analytic solutions $\unicode[STIX]{x1D712}_{IW}$, respectively (colour scale from $-0.1$ to $0.1$).

Figure 1

Figure 2. As in figure 1 but now at three distinct instants $t=(N+{\textstyle \frac{1}{2}})\unicode[STIX]{x03C0}/2$ ($N=3,7,11$) at which $E^{-1/2}\overline{\unicode[STIX]{x1D712}}_{MF}=0$. Panels (a–c), (d–f), (g–i) correspond to $t=5.50$, $11.79$, $18.07$, respectively.

Figure 2

Figure 3. As in figure 1 but now $v$-contours for the same instants, at which $E^{-1/2}\overline{v}_{MF}=0$ (equivalent to $E^{-1/2}\overline{\unicode[STIX]{x1D712}}_{MF}$ maximised). Panels (a,d,g) show $E^{-1/2}v_{DNS}$ (colour scale from $-30$ to $30$); (b,e,h) and (c,f,i) show $v_{FNS}$ and $v_{IW}$, respectively (colour scale from $-0.5$ to $0.5$).

Figure 3

Figure 4. As in figure 2 but now $v$-contours for the same instants, at which $E^{-1/2}\overline{v}_{MF}$ is maximised (equivalent to $E^{-1/2}\overline{\unicode[STIX]{x1D712}}_{MF}=0$). Panel description as in figure 3.

Figure 4

Figure 5. The meridional speed $E^{-1/2}\sqrt{u^{2}+w^{2}}=r^{-1}|\unicode[STIX]{x1D735}(r\unicode[STIX]{x1D712})|$ at $t=18.07$ as in figure 2(g–i). Respectively, the panels show results for: (a–c) the filtered DNS $\unicode[STIX]{x1D712}_{FNS}$, when (a) $E=10^{-3}$, (b) $E=10^{-5}$, (c) $E=10^{-7}$; (d) the analytic $\unicode[STIX]{x1D712}^{wave}$ in the limit $E\downarrow 0$; (e) the full DNS $E^{-1/2}\unicode[STIX]{x1D712}_{DNS}$ when $E=10^{-7}$ (colour scale from 0 to 3).

Figure 5

Figure 6. The analytic $\unicode[STIX]{x1D712}^{wave}$-contours in the $E\downarrow 0$ limit at sequential times $t=(N+{\textstyle \frac{1}{2}})\unicode[STIX]{x03C0}/2$. (a) $N=3$, (b) $N=7$, (c) $N=11$, cf. figures 2(c), (f), (i) respectively. (d) $N=15$ (colour scale from $-0.1$ to 0.1).

Figure 6

Figure 7. The analytic $v^{wave}$-contours in the $E\downarrow 0$ limit at sequential times $t=N\unicode[STIX]{x03C0}/2$. (a) $N=3$, (b) $N=7$, (c) $N=11$, cf. figures 3(c), (f), (i), respectively. (d) $N=15$ (colour scale from $-0.5$ to 0.5).

Figure 7

Figure 8. The analytic $\unicode[STIX]{x1D712}_{m}^{wave}$-contours in the $E\downarrow 0$ limit (see (4.3)) for the cases $m=1$ at (a) $t=15$, (b) $t=25$, and $m=2$ also at (c) $t=15$, (d) $t=25$ (colour scale from $-0.1$ to 0.1).

Figure 8

Figure 9. The analytic $\unicode[STIX]{x1D712}_{m}^{wave}$-contours in the $E\downarrow 0$ limit (see (4.3)) at fixed $z=z_{m}$, in the $r$–$t$ plane for $\ell =10$. Pertaining to the asymptotic $\ell \gg 1$ results of § 6.3: the solid black line identifies the critical group velocity, i.e. $c_{gc}t+(\ell -r)=0$ with $c_{gc}\doteqdot -0.245/m$ (see (6.21c)) valid for $\ell -r=O(1)$. The dashed black line corresponds to the critical phase velocity $c_{pc}t=r$ with $c_{pc}=-3c_{gc}\doteqdot 0.735/m$ (cf. (6.21d)) also only valid for $\ell -r=O(1)$. (a) $m=1$ with $z_{1}=0.5$; (b) $m=2$ with $z_{2}=0.25$ (colour scale from $-0.1$ to 0.1).

Figure 9

Figure 10. The filtered DNS (FNS) $\unicode[STIX]{x1D712}_{FNS}$-contours at fixed $z=0.5$, as in 9(a). (a) $E=10^{-3}$, (b) $E=10^{-5}$ (colour scale from $-0.1$ to 0.1).

Oruba et al. supplementary movie 1

{\it Movie 1}\\ This movie shows the $\chi$-contours in the case $\Ek=10^{-3}$, as a function of time: (a) the direct numerical simulations $\Ek^{-1/2}\chi_{\tDNS}$ (colour scale from -0.3 to 0.3); (b) the filtered DNS, with the geostrophic flow substracted $\chi_{\tFNS}$ (colour scale from -0.1 to 0.1); (c) the analytic solutions $\chi_{\tIW}$ (colour scale from -0.1 to 0.1).\\

Download Oruba et al. supplementary movie 1(Video)
Video 3.1 MB

Oruba et al. supplementary movie 2

{\it Movie 2}\\ This movie shows the $v$-contours in the case $\Ek=10^{-3}$, as a function of time: (a) the direct numerical simulations $\Ek^{-1/2}v_{\tDNS}$ (colour scale from -30 to 30); (b) the filtered DNS, with the geostrophic flow substracted $v_{\tFNS}$ (colour scale from -0.5 to 0.5); (c) the analytic solutions $v_{\tIW}$ (colour scale from -0.5 to 0.5).\\

Download Oruba et al. supplementary movie 2(Video)
Video 2.8 MB

Oruba et al. supplementary movie 3

{\it Movie 3}\\ This movie shows the $\chi$-contours in the case $\Ek=10^{-5}$, as a function of time: (a) the direct numerical simulations $\Ek^{-1/2}\chi_{\tDNS}$ (colour scale from -0.3 to 0.3); (b) the filtered DNS, with the geostrophic flow substracted $\chi_{\tFNS}$ (colour scale from -0.1 to 0.1); (c) the analytic solutions $\chi_{\tIW}$ (colour scale from -0.1 to 0.1).\\

Download Oruba et al. supplementary movie 3(Video)
Video 4.5 MB

Oruba et al. supplementary movie 4

{\it Movie 4}\\ This movie shows the $v$-contours in the case $\Ek=10^{-5}$, as a function of time: (a) the direct numerical simulations $\Ek^{-1/2}v_{\tDNS}$ (colour scale from -30 to 30); (b) the filtered DNS, with the geostrophic flow substracted $v_{\tFNS}$ (colour scale from -0.5 to 0.5); (c) the analytic solutions $v_{\tIW}$ (colour scale from -0.5 to 0.5).\\

Download Oruba et al. supplementary movie 4(Video)
Video 3 MB

Oruba et al. supplementary movie 5

{\it Movie 5}\\ This movie shows the $\chi$-contours in the case $\Ek=10^{-7}$, as a function of time: (a) the direct numerical simulations $\Ek^{-1/2}\chi_{DNS}$ (colour scale from -0.3 to 0.3); (b) the filtered DNS, with the geostrophic flow substracted $\chi_{FNS}$ (colour scale from -0.1 to 0.1); (c) the analytic solutions $\chi_{IW}$ (colour scale from -0.1 to 0.1).\\

Download Oruba et al. supplementary movie 5(Video)
Video 4.4 MB

Oruba et al. supplementary movie 6

{\it Movie 6}\\ This movie shows the $v$-contours in the case $\Ek=10^{-7}$, as a function of time: (a) the direct numerical simulations $\Ek^{-1/2}v_{\tDNS}$ (colour scale from -30 to 30); (b) the filtered DNS, with the geostrophic flow substracted $v_{\tFNS}$ (colour scale from -0.5 to 0.5); (c) the analytic solutions $v_{\tIW}$ (colour scale from -0.5 to 0.5).\\

Download Oruba et al. supplementary movie 6(Video)
Video 2.9 MB

Oruba et al. supplementary movie 7

{\it Movie 7}\\ This movie shows the meridional speed $E^{-1/2}\sqrt{u^2+w^2}=r^{-1}\bigl|\bfnabla(r\chi)\bigr|$, as a function of time. Respectively, the panels show results for: ($a$)--($c$) the filtered DNS $\chi_\tFNS$, when ($a$) $E=10^{-3}$, ($b$) $E=10^{-5}$, ($c$) $E=10^{-7}$; ($d$) the analytic $\chi^{\rm{wave}}$ in the limit $E\downarrow 0$; ($e$) the full DNS $E^{-1/2}\chi_\tDNS$ when $E=10^{-7}$ (colour scale from $0$ to $3$).

Download Oruba et al. supplementary movie 7(Video)
Video 907.9 KB
Supplementary material: PDF

Oruba et al. supplementary material

Supplementary Data

Download Oruba et al. supplementary material(PDF)
PDF 40.7 KB