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Layering and turbulence surrounding an anticyclonic oceanic vortex: in situ observations and quasi-geostrophic numerical simulations

Published online by Cambridge University Press:  21 August 2013

Bach Lien Hua ,
Claire Ménesguen ,
Sylvie Le Gentil ,
Richard Schopp ,
Bruno Marsset  and
Hidenori Aiki
Bach Lien Hua
Affiliation:
Laboratoire de Physique des Oceans, IFREMER-CNRS, BP 70, 29280 Plouzané, France
Claire Ménesguen*
Affiliation:
Laboratoire de Physique des Oceans, IFREMER-CNRS, BP 70, 29280 Plouzané, France
Sylvie Le Gentil
Affiliation:
Laboratoire de Physique des Oceans, IFREMER-CNRS, BP 70, 29280 Plouzané, France
Richard Schopp
Affiliation:
Laboratoire de Physique des Oceans, IFREMER-CNRS, BP 70, 29280 Plouzané, France
Bruno Marsset
Affiliation:
Laboratoire de Géophysique et Géodynamique, IFREMER, BP 70, 29280 Plouzané, France
Hidenori Aiki
Affiliation:
JAMSTEC, Yokohama 236-0001, Japan
*
†Email address for correspondence: Claire.Menesguen@ifremer.fr
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Abstract

Evidence of persistent layering, with a vertical stacking of sharp variations in temperature, has been presented recently at the vertical and lateral periphery of energetic oceanic vortices through seismic imaging of the water column. The stacking has vertical scales ranging from a few metres up to 100 m and a lateral spatial coherence of several tens of kilometres comparable with the vortex horizontal size. Inside this layering, in situ data display a $[{ k}_{h}^{- 5/ 3} { k}_{h}^{- 2} ] $ scaling law of horizontal scales for two different quantities, temperature and a proxy for its vertical derivative, but for two different ranges of wavelengths, between 5 and 50 km for temperature and between 500 m and 5 km for its vertical gradient. In this study, we explore the dynamics underlying the layering formation mechanism, through the slow dynamics captured by quasi-geostrophic equations. Three-dimensional high-resolution numerical simulations of the destabilization of a lens-shaped vortex confirm that the vertical stacking of sharp jumps in density at its periphery is the three-dimensional analogue of the preferential wind-up of potential vorticity near a critical radius, a phenomenon which has been documented for barotropic vortices. For a small-Burger (flat) lens vortex, baroclinic instability ensures a sustained growth rate of sharp jumps in temperature near the critical levels of the leading unstable modes. Such results can be obtained for a background stratification which is due to temperature only and does not require the existence of salt anomalies. Aloft and beneath the vortex core, numerical simulations well reproduce the $[{ k}_{h}^{- 5/ 3} { k}_{h}^{- 2} ] $ scaling law of horizontal scales for the vertical derivative of temperature that is observed in situ inside the layering, whatever the background stratification. Such a result stems from the tracer-like behaviour of the vortex stretching component and previous studies have shown that spectra of tracer fields can be steeper than $- 1$, namely in $- 5/ 3$ or $- 2$, if the advection field is very compact spatially, with a $- 5/ 3$ slope corresponding to a spiral advection of the tracer. Such a scaling law could thus be of geometric origin. As for the kinetic and potential energy, the ${ k}_{h}^{- 5/ 3} $ scaling law can be reproduced numerically and is enhanced when the background stratification profile is strongly variable, involving sharp jumps in potential vorticity such as those observed in situ. This raises the possibility of another plausible mechanism leading to a $- 5/ 3$ scaling law, namely surface-quasi-geostrophic (SQG)-like dynamics, although our set-up is more complex than the idealized SQG framework. Energy and enstrophy fluxes have been diagnosed in the numerical quasi-geostrophic simulations. The results emphasize a strong production of energy in the oceanic submesoscales range and a kinetic and potential energy flux from mesoscale to submesoscales range near the critical levels. Such horizontal submesoscale production, which is correlated to the accumulation of thin vertical scales inside the layering, thus has a significant slow dynamical component, well-captured by quasi-geostrophy.

JFM classification

Geophysical and Geological Flows: Geostrophic turbulence Geophysical and Geological Flows: Quasi-geostrophic flows Geophysical and Geological Flows: Stratified flows
Type
Papers
Information
Journal of Fluid Mechanics , Volume 731 , 25 September 2013 , pp. 418 - 442
Copyright
©2013 Cambridge University Press 

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Footnotes

‡

Professor Bach Lien Hua passed away before the final revision of this paper was completed. This manuscript was however written by the first author.

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