A Geometric Interpretation of Southern Ocean Eddy Form Stress

Autor: David P. Marshall, Roman Nuterman, Markus Jochum, James R. Maddison, Mads Poulsen
Rok vydání: 2019
Předmět:
Zdroj: Poulsen, M B, Jochum, M, Maddison, J R, Marshall, D P & Nuterman, R 2019, ' A Geometric Interpretation of Southern Ocean Eddy Form Stress ', Journal of Physical Oceanography, vol. 49, no. 10, pp. 2553-2570 . https://doi.org/10.1175/JPO-D-18-0220.1
Mads B, P, Markus, J, Maddison, J, Marshall, D P & Nuterman, R 2019, ' A geometric interpretation of Southern Ocean eddy form stress ', Journal of Physical Oceanography, vol. 49, pp. 2553-2570 . https://doi.org/10.1175/JPO-D-18-0220.1
ISSN: 1520-0485
0022-3670
DOI: 10.1175/jpo-d-18-0220.1
Popis: An interpretation of eddy form stress via the geometry described by the Eliassen–Palm flux tensor is explored. Complimentary to previous works on eddy Reynolds stress geometry, this study shows that eddy form stress is fully described by a vertical ellipse, whose size, shape, and orientation with respect to the mean flow shear determine the strength and direction of vertical momentum transfers. Following a recent proposal, this geometric framework is here used to form a Gent–McWilliams eddy transfer coefficient that depends on eddy energy and a nondimensional geometric parameter α, bounded in magnitude by unity. The parameter α expresses the efficiency by which eddies exchange energy with baroclinic mean flow via along-gradient eddy buoyancy flux—a flux equivalent to eddy form stress along mean buoyancy contours. An eddy-resolving ocean general circulation model is used to estimate the spatial structure of α in the Southern Ocean and assess its potential to form a basis for parameterization. The eddy efficiency α averages to a low but positive value of 0.043 within the Antarctic Circumpolar Current, consistent with an inefficient eddy field extracting energy from the mean flow. It is found that the low eddy efficiency is mainly the result of that eddy buoyancy fluxes are weakly anisotropic on average. The eddy efficiency is subject to pronounced vertical structure and is maximum at ~3-km depth, where eddy buoyancy fluxes tend to be directed most downgradient. Since α partly sets the eddy form stress in the Southern Ocean, a parameterization for α must reproduce its vertical structure to provide a faithful representation of vertical stress divergence and eddy forcing.
Databáze: OpenAIRE
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