The role of eddies and topography in the export of shelf waters from the West Antarctic Peninsula shelf

Brearley, J.A. ORCID: https://orcid.org/0000-0003-3700-8017; Moffat, C.; Venables, H.J. ORCID: https://orcid.org/0000-0002-6445-8462; Meredith, M.P. ORCID: https://orcid.org/0000-0002-7342-7756; Dinniman, D.S.. 2019 The role of eddies and topography in the export of shelf waters from the West Antarctic Peninsula shelf. Journal of Geophysical Research: Oceans, 124 (11). 7718-7743. 10.1029/2018JC014679

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Text (Open Access) © 2019. The Authors. This is an open access article under the terms of the Creative Commons Attribution License, which permits use, distribution and reproduction in any medium, provided the original work is properly cited. Brearley_et_al-2019-Journal_of_Geophysical_Research__Oceans.pdf - Published Version Available under License Creative Commons Attribution 4.0. Download (44MB) | Preview

Abstract/Summary

Oceanic heat strongly influences the glaciers and ice shelves along West Antarctica. Prior studies show that the subsurface onshore heat flux from the Southern Ocean on the shelf occurs through deep, glacially carved channels. The mechanisms enabling the export of colder shelf waters to the open ocean, however, have not been determined. Here, we use ocean glider measurements collected near the mouth of Marguerite Trough (MT), west Antarctic Peninsula, to reveal shelf‐modified cold waters on the slope over a deep (2,700 m) offshore topographic bank. The shelf hydrographic sections show subsurface cold features (θ <=1.5 °C), and associated potential vorticity fields suggest a significant instability‐driven eddy field. Output from a high‐resolution numerical model reveals offshore export modulated by small (6 km), cold‐cored, cyclonic eddies preferentially generated along the slope and at the mouth of MT. While baroclinic and barotropic instabilities appear active in the surrounding open ocean, the former is suppressed along the steep shelf slopes, while the latter appears enhanced. Altimetry and model output reveal the mean slope flow splitting to form an offshore branch over the bank, which eventually forms a large (116 km wide) persistent lee eddy, and an onshore branch in MT. The offshore flow forms a pathway for the small cold‐cored eddies to move offshore, where they contribute significantly to cooling over the bank, including the large lee eddy. These results suggest eddy fluxes, and topographically modulated flows are key mechanisms for shelf water export along this shelf, just as they are for the shoreward warm water transport.

Item Type:	Publication - Article
Digital Object Identifier (DOI):	10.1029/2018JC014679
Date made live:	01 Nov 2019 15:07 +0 (UTC)
URI:	https://nora.nerc.ac.uk/id/eprint/525558

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