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The role of mixed-layer instabilities in submesoscale turbulence

Callies, Jörn and Flierl, Glenn and Ferrari, Raffaele and Fox-Kemper, Baylor (2016) The role of mixed-layer instabilities in submesoscale turbulence. Journal of Fluid Mechanics, 788 . pp. 5-41. ISSN 0022-1120. https://resolver.caltech.edu/CaltechAUTHORS:20180112-100116271

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Abstract

Upper-ocean turbulence at scales smaller than the mesoscale is believed to exchange surface and thermocline waters, which plays an important role in both physical and biogeochemical budgets. But what energizes this submesoscale turbulence remains a topic of debate. Two mechanisms have been proposed: mesoscale-driven surface frontogenesis and baroclinic mixed-layer instabilities. The goal here is to understand the differences between the dynamics of these two mechanisms, using a simple quasi-geostrophic model. The essence of mesoscale-driven surface frontogenesis is captured by the well-known surface quasi-geostrophic model, which describes the sharpening of surface buoyancy gradients and the subsequent breakup in secondary roll-up instabilities. We formulate a similarly archetypical Eady-like model of submesoscale turbulence induced by mixed-layer instabilities. The model captures the scale and structure of this baroclinic instability in the mixed layer. A wide range of scales are energized through a turbulent inverse cascade of kinetic energy that is fuelled by the submesoscale mixed-layer instability. Major differences to mesoscale-driven surface frontogenesis are that mixed-layer instabilities energize the entire depth of the mixed layer and produce larger vertical velocities. The distribution of energy across scales and in the vertical produced by our simple model of mixed-layer instabilities compares favourably to observations of energetic wintertime submesoscale flows, suggesting that it captures the leading-order balanced dynamics of these flows. The dynamics described here in an oceanographic context have potential applications to other geophysical fluids with layers of different stratifications.


Item Type:Article
Related URLs:
URLURL TypeDescription
https://doi.org/10.1017/jfm.2015.700DOIArticle
ORCID:
AuthorORCID
Callies, Jörn0000-0002-6815-1230
Ferrari, Raffaele0000-0003-1895-4294
Additional Information:© 2016 Cambridge University Press. (Received 23 April 2015; revised 23 September 2015; accepted 24 November 2015; first published online 22 December 2015) Much of this work was conducted at the Geophysical Fluid Dynamics Summer School at the Woods Hole Oceanographic Institution. We gratefully acknowledge the NSF’s support of this program and the fruitful interactions we had with staff and visitors.
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Subject Keywords:geophysical and geological flows, ocean circulation, quasi-geostrophic flows
Record Number:CaltechAUTHORS:20180112-100116271
Persistent URL:https://resolver.caltech.edu/CaltechAUTHORS:20180112-100116271
Official Citation:Callies, J., Flierl, G., Ferrari, R., & Fox-Kemper, B. (2016). The role of mixed-layer instabilities in submesoscale turbulence. Journal of Fluid Mechanics, 788, 5-41. doi:10.1017/jfm.2015.700
Usage Policy:No commercial reproduction, distribution, display or performance rights in this work are provided.
ID Code:84297
Collection:CaltechAUTHORS
Deposited By: George Porter
Deposited On:12 Jan 2018 19:25
Last Modified:09 Oct 2019 19:30

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