Hostname: page-component-78c5997874-m6dg7 Total loading time: 0 Render date: 2024-11-19T06:26:33.220Z Has data issue: false hasContentIssue false

On the coupling between spin-up and aspect ratio of vortices in rotating stratified flows: a predictive model

Published online by Cambridge University Press:  20 July 2015

Marius Ungarish*
Affiliation:
Department of Computer Science, Technion, Haifa 32000, Israel
*
Email address for correspondence: [email protected]

Abstract

We consider the long-time (many revolutions) behaviour of an axisymmetric isolated anticyclonic vortex of constant density which floats inside a large ambient linear-stratified fluid rotating with constant ${\it\Omega}$. We have developed a closed simple model for the prediction of the vertical thickness to diameter aspect ratio ${\it\alpha}$ (and actually the shape) and internal angular velocity ${\it\omega}$, relative to the ambient, as functions of time $t$. (In our model ${\it\omega}$ is scaled with ${\it\Omega}$; the literature sometimes uses the Rossby number $Ro={\it\omega}/2$.) This model is an extension of the model of Aubert et al. (J. Fluid Mech., vol. 706, 2012, pp. 34–45) and Hassanzadeh et al. (J. Fluid Mech., vol. 706, 2012, pp. 46–57), which derived the connection between ${\it\alpha}$ and ${\it\omega}$, for prescribed $f=2{\it\Omega}$ and buoyancy frequency of the ambient $\mathscr{N}$. This work adds the balance of angular momentum and resolves the spin-up process of the vortex, which were not accounted for in the previous model. The Ekman number $E={\it\nu}/({\it\Omega}L^{2})$ now enters into the formulation; here ${\it\nu}$ is the coefficient of kinematic viscosity and $L$ is the half-height of the vortex, roughly (a sharper definition is given in the paper). The model can be applied to cases of both fixed-volume and injection-sustained vortices.

The often-cited aspect ratio ${\it\alpha}=0.5f/\mathscr{N}$ corresponds to ${\it\omega}\approx -1$, which is a plausible initial condition for typical systems. We show that the continuous ‘decay’ of ${\it\alpha}$ from that value over many revolutions of the system is indeed governed by the spin-up effect which reduces $|{\it\omega}|$, but with significant differences to the classical spin-up of a fluid in a closed solid container. The spin-up shear torque decays with time because the thickness of the boundary shear layer increases. The layer starts as a double Ekman layer (between two fluids) but it quite quickly expands due to stratification effects, and later due to viscous diffusion. This prolongs the spin-up somewhat beyond the classical $E^{-1/2}/{\it\Omega}$ time interval. Moreover, when $|{\it\omega}|$ becomes small, the momentum of angular inertia of the vortex increases like $(1+(1/3)|{\it\omega}|^{-1})$; this further hinders the spin-up, and prolongs the process.

Comparisons of the prediction of the model with previously published experimental and Navier–Stokes simulation data were performed for four cases. In three cases the agreement is good. In one case, the model predicts a much faster decay than the observed one; we have suggested a plausible explanation for this discrepancy.

Type
Papers
Copyright
© 2015 Cambridge University Press 

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

Armi, L., Hebert, D., Oakey, N., Price, J. F., Richardson, P. L., Rossby, H. T. & Ruddick, B. 1988 The history and decay of a Mediterranean salt lens. Nature 333, 649651.Google Scholar
Aubert, O., Le Bars, M., Le Gal, P. & Marcus, P. S. 2012 The universal aspect ratio of vortices in rotating stratified flows: experiments and observations. J. Fluid Mech. 706, 3445; referred to as ALM12.Google Scholar
Baines, P. G. & Sparks, R. S. J. 2005 Dynamics of volcanic ash clouds from supervolcanic eruptions. Geophys. Res. Lett. 32, L24808.Google Scholar
Flor, J. B., Ungarish, M. & Bush, J. W. M. 2002 Spin-up from rest in a stratified fluid: boundary flow. J. Fluid Mech. 472, 5182.Google Scholar
Gill, A. E. 1981 Homogeneous intrusion in a rotating stratified fluid. J. Fluid Mech. 103, 275295.Google Scholar
Grant, S. A., Sundermeyer, M. A. & Hebert, D. 2011 On the geostrophic adjustment of an isolated lens: dependence on Burger number and initial geometry. J. Phys. Oceanogr. 725741.Google Scholar
Greenspan, H. 1968 The Theory of Rotating Fluids. Cambridge University Press, reprinted by Breukelen Press.Google Scholar
Griffiths, R. W. & Linden, P. 1981 The stability of vortices in a rotating, stratified fluid. J. Fluid Mech. 105, 283316.Google Scholar
Hassanzadeh, P., Marcus, P. S. & Le Gal, P. 2012 The universal aspect ratio of vortices in rotating stratified flows: theory and simulation. J. Fluid Mech. 706, 4657; referred to as HML12.Google Scholar
Hedstrom, K. & Armi, L. 1988 An experimental study of homogeneous lenses in a stratified rotating fluid. J. Fluid Mech. 191, 535556.Google Scholar
Marcus, P. S. 1993 Jupiter’s great red spot and other vortices. Annu. Rev. Astron. Astrophys. 31, 523573.CrossRefGoogle Scholar
Ungarish, M. 1993 Hydrodynamics of Suspensions: Fundamentals of Centrifugal and Gravity Separation. Springer.CrossRefGoogle Scholar
Ungarish, M. 2009 An Introduction to Gravity Currents and Intrusions. Chapman and Hall/CRC.CrossRefGoogle Scholar
Ungarish, M. & Huppert, H. E. 2004 On gravity currents propagating at the base of a stratified ambient: effects of geometrical constraints and rotation. J. Fluid Mech. 521, 69104.Google Scholar
Ungarish, M. & Mang, J. 2003 Spin-up from rest of a two-layer fluid about a vertical axis. J. Fluid Mech. 474, 117145.Google Scholar
Walin, G. 1969 Some aspects of time-dependent motion of a stratified rotating fluid. J. Fluid Mech. 36, 289307.CrossRefGoogle Scholar