Turbulence in Antarctic Circumpolar Current standing meanders.

Lead Research Organisation: University of Southampton
Department Name: Sch of Ocean and Earth Science

Abstract

This proposal is to study the role of turbulent mixing in the meridional overturning circulation of the Southern Ocean and the dynamics of the Antarctic Circumpolar Current (ACC). The project is motivated by the recent discovery of Southern Ocean regions of remarkably intense and widespread turbulence, an observation that defies current theoretical understanding of the circulation based on the assumption of little mixing in the ocean interior. The project is exciting because it will use innovative instrumentation to measure turbulent mixing in the deep Southern Ocean for the first time, to determine its dynamical causes and to assess its impact on the overturning circulation and the transport of the ACC. The focus of the project will be on observing and modelling the circulation and mixing in a standing meander of the ACC north of the Kerguelen Plateau, a dynamically important region of the current system. This novel way of looking at the ACC will provide important new insight into how the current interacts with bottom topography (a crucial issue for understanding what sets the ACC transport), the dynamical nature of the overturning circulation of the Southern Ocean and how this should be represented in ocean circulation and climate models.

Publications

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Naveira Garabato A (2013) The Impact of Small-Scale Topography on the Dynamical Balance of the Ocean in Journal of Physical Oceanography

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Heywood K (2012) Temporal Variability of Diapycnal Mixing in Shag Rocks Passage in Journal of Physical Oceanography

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Trossman D (2015) Internal lee wave closures: Parameter sensitivity and comparison to observations in Journal of Geophysical Research: Oceans

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Polzin K (2014) Finescale parameterizations of turbulent dissipation in Journal of Geophysical Research: Oceans

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Thompson A (2014) Equilibration of the Antarctic Circumpolar Current by Standing Meanders in Journal of Physical Oceanography

 
Description Intense turbulent mixing occurs in the Southern Ocean as the Antarctic Circumpolar Current impinges on small-scale bottom topography and generates internal waves, which subsequently break and cause mixing.
Exploitation Route The findings on mixing above are providing a benchmark for the improvement of representations of oceanic turbulence in climate-scale ocean models.
Sectors Environment

 
Description The findings on mixing above are providing a benchmark for the improvement of representations of oceanic turbulence in climate-scale ocean models.
First Year Of Impact 2012
Sector Other