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A theory of standing meanders of the Antarctic Circumpolar Current and their response to wind

Citation

Zhang, X and Nikurashin, M and Pena-Molino, B and Rintoul, SR and Doddridge, E, A theory of standing meanders of the Antarctic Circumpolar Current and their response to wind, Journal of Physical Oceanography, 53, (1) pp. 235-251. ISSN 0022-3670 (2022) [Refereed Article]


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Copyright Statement

© 2022 American Meteorological Society.

DOI: doi:10.1175/JPO-D-22-0086.1

Abstract

Standing meanders of the Antarctic Circumpolar Current (ACC) and associated eddy hotspots play an important role for the meridional heat flux and downward momentum transfer in the Southern Ocean. Previous modelling studies show that the vorticity balance characterising standing meanders in the upper ocean is dominated by advection of relative vorticity and stretching. Through the adjustment of this vorticity balance, standing meanders have been suggested to provide a pathway for the transfer of the momentum input by the wind from the surface to the bottom, leading to stronger bottom flows and energy dissipation. However, the dynamics governing the meander formation and its adjustment to wind remain unclear. Here we develop a quasi-geostrophic theory and combine it with a regional model of the Macquarie Ridge region and an idealized channel model to explore the dynamics and vertical structure of standing meanders of the ACC. The results show that the entire vertical structure of the meander, including its dynamics in the upper ocean, is controlled by the bottom flow interacting with topography. Based on our results, we suggest a novel mechanism for the response of the ACC to wind in which ‘flexing’ of the meander, or change in its curvature, is a response to changes in the bottom (barotropic) flow. Stronger bottom flow in response to stronger wind interacts with topography and generates a larger amplitude Rossby wave propagating into the upper ocean. The ACC mean shear aloft amplifies the Rossby wave and leads to a larger amplitude meander in the upper ocean dominated by advection of relative vorticity and stretching.

Item Details

Item Type:Refereed Article
Keywords:ocean circulation, Southern Ocean, meander, topography, Antarctic Circumpolar Current
Research Division:Earth Sciences
Research Group:Oceanography
Research Field:Physical oceanography
Objective Division:Environmental Policy, Climate Change and Natural Hazards
Objective Group:Understanding climate change
Objective Field:Climate change models
UTAS Author:Zhang, X (Miss Xihan Zhang)
UTAS Author:Nikurashin, M (Dr Maxim Nikurashin)
UTAS Author:Pena-Molino, B (Dr Beatriz Pena-Molino)
UTAS Author:Rintoul, SR (Dr Steve Rintoul)
UTAS Author:Doddridge, E (Dr Edward Doddridge)
ID Code:153832
Year Published:2022
Deposited By:Oceans and Cryosphere
Deposited On:2022-10-10
Last Modified:2023-01-25
Downloads:0

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