Evidence for Large-Scale Eddy-Driven Gyres in the North Atlantic
M. Susan Lozier
Analysis of a recent climatological database for the North Atlantic
has detailed an extensive large-scale recirculation system in the
intermediate waters of the North Atlantic basin. The pressure fields
that define this recirculation, coupled with the potential vorticity
fields associated with the recirculating flow, provide observational
evidence for basin-scale eddy-driven flow in the global ocean. The
recirculations are intimately tied to the waters carried southward by
the Deep Western Boundary Current and are therefore likely to affect
the distribution of climatic anomalies in the North Atlantic.
Division of Earth and Ocean Sciences, Nicholas School of the
Environment, Duke University, Box 90230, Durham, NC 27708-0230, USA.