Persistence and material coherence of a mesoscale ocean eddy

TL;DR

This paper introduces a novel method using dynamic Laplace operators to analyze multi-timescale material transport and coherence in ocean eddies, revealing that eddy transport often occurs via outer rings rather than long-lived cores.

Contribution

The paper presents a new approach to identify and track persistent mesoscale ocean eddies and their material coherence over multiple timescales using eigenfunctions of dynamic Laplace operators.

Findings

The method successfully tracks eddies longer than traditional Eulerian methods.

Material transport is primarily through the eddy's outer ring, not the core.

Eddy coherence timescales are shorter than their persistence in observations.

Abstract

Ocean eddies play an important role in the transport and mixing processes of the ocean due to their ability to transport material, heat, salt, and other tracers across large distances. They exhibit at least two timescales; an Eulerian lifetime associated with persistent identifiable signatures in gridded fields such as vorticity or sea-surface height, and multiple Lagrangian or material coherence timescales that are typically much shorter. We propose a method to study the multi-timescale material transport, leakage, and entrainment by eddies with their surroundings by constructing sequences of finite-time coherent sets, computed as superlevel sets of dominant eigenfunctions of dynamic Laplace operators. The dominant eigenvalues of dynamic Laplace operators defined on time intervals of varying length allows us to identify a maximal coherence timescale that minimizes the rate of mass loss over a domain, per unit flow time. We apply the method to examine the persistence and material coherence of an Agulhas ring, an ocean eddy in the South Atlantic ocean, using particle trajectories derived from a $0.1^\circ$ global numerical ocean simulation. Using a sequence of sliding windows, the method is able to identify and track a persistent eddy feature for a time much longer than the maximal coherence timescale, and with considerably larger material transport than the corresponding eddy feature identified from purely Eulerian information. Furthermore, the median residence times of fluid in the identified feature far exceed the timescale over which fully material motion is guaranteed. Through residence time calculations, we find that this particular eddy does not exhibit a long-lived coherent inner core and that the bulk of material transport is performed by the quasi-coherent outer ring of the eddy.