Acceleration and overturning of the Antarctic Slope Current by winds, eddies, and tides

• Published in: Journal of Physical Oceanography
• Main Authors: Stewart, AL, Klocker, A, Menemenlis, D
• Format: Article in Journal/Newspaper
• Language: English
• Published: Amer Meteorological Soc 2019
• Subjects: Earth Sciences; Oceanography; Physical Oceanography; Antarctic; The Antarctic; Antarc*; Sea ice
• Online Access: https://doi.org/10.1175/JPO-D-18-0221.1; http://ecite.utas.edu.au/134357

All exchanges between the open ocean and the Antarctic continental shelf must cross the Antarctic Slope Current (ASC). Previous studies indicate that these exchanges are strongly influenced by mesoscale and tidal variability, yet the mechanisms responsible for setting the ASCs transport and structure have received relatively little attention. In this study the roles of winds, eddies, and tides in accelerating the ASC are investigated using a global oceansea ice simulation with very high resolution (1/48 grid spacing). It is found that the circulation along the continental slope is accelerated both by surface stresses, ultimately sourced from the easterly winds, and by mesoscale eddy vorticity fluxes. At the continental shelf break, the ASC exhibits a narrow (~3050 km), swift (>0.2 m s −1 ) jet, consistent with in situ observations. In this jet the surface stress is substantially reduced, and may even vanish or be directed eastward, because the ocean surface speed matches or exceeds that of the sea ice. The shelfbreak jet is shown to be accelerated by tidal momentum advection, consistent with the phenomenon of tidal rectification. Consequently, the shoreward Ekman transport vanishes and thus the mean overturning circulation that steepens the Antarctic Slope Front (ASF) is primarily due to tidal acceleration. These findings imply that the circulation and mean overturning of the ASC are not only determined by near-Antarctic winds, but also depend crucially on sea ice cover, regionally-dependent mesoscale eddy activity over the continental slope, and the amplitude of tidal flows across the continental shelf break.