Journal
JOURNAL OF PHYSICAL OCEANOGRAPHY
Volume 43, Issue 7, Pages 1426-1438Publisher
AMER METEOROLOGICAL SOC
DOI: 10.1175/JPO-D-12-0171.1
Keywords
Eddies; Mesoscale processes; Transport
Categories
Funding
- NSF [CMG0825547]
- NASA [NNX10AE99G]
- NSERC [401839-11]
- NASA [133557, NNX10AE99G] Funding Source: Federal RePORTER
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Mesoscale oceanic eddies are routinely detected from instantaneous velocities derived from satellite altimetry data. While simple to implement, this approach often gives spurious results and hides true material transport. Here it is shown how geodesic transport theory, a recently developed technique from nonlinear dynamical systems, uncovers eddies objectively. Applying this theory to altimetry-derived velocities in the South Atlantic reveals, for the first time, Agulhas rings that preserve their material coherence for several months, while ring candidates yielded by other approaches tend to disperse or leak within weeks. These findings suggest that available velocity-based estimates for the Agulhas leakage, as well as for its impact on ocean circulation and climate, need revision.
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