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Abstract

Vertical motions within eddies play an important role in the exchange of properties and energy between the upper ocean and the ocean interior. Here we analyze alternating upward and downward cells in anticyclonic eddies in the East Australian Current region using a global eddy‐resolving model. The cells explain over 50% of the variance of vertical velocity within these eddies. We show that the upward and downward cells relate to eddy distortion, defined as the change in eddy shape over time. In anticyclonic eddies in the Southern Hemisphere, an inward distortion is associated with upward motion and an outward distortion is associated with downward motion. We discuss two mechanisms that link eddy distortion to vertical velocity. One mechanism relates to changes in stratification and relative vorticity in the eddy interior. The other mechanism relates to divergence of the horizontal flow in different quadrants of the eddy. We show that mesoscale changes in sea level anomaly can be used to infer the vertical motion within eddies.

Item Type:	Article
Authors/Creators:	Pilo, GS and Oke, PR and Coleman, R and Rykova, T and Ridgway, K
Keywords:	ocean dynamics, mesoscale, ocean eddies, East Australian Current, ocean model, vertical velocity, anticyclonic eddy, eddy distortion, eddy isotropy, ocean modeal, stratification, relative vorticity
Journal or Publication Title:	Journal of Geophysical Research: Oceans
Publisher:	Wiley-Blackwell Publishing, Inc.
ISSN:	2169-9275
DOI / ID Number:	10.1002/2017JC013298
Copyright Information:	Copyright 2018 American Geophysical Union
Related URLs:	Google Scholar: Coleman, R UTAS Profile: Coleman, R
Item Statistics:	View statistics for this item

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