Search

Abstract: Three Algerian eddies (open sea big anticyclonic eddies in the Algerian basin, western Mediterranean sea) are studied in detail using altimetric and in situ data. To characterize their spatial structure we make use of the Okubo–Weiss parameter, which allows to separate the flow into vorticity-dominated and deformation-dominated regions. The application of this parameter to geostrophic velocity fields obtained from Sea Level Anomaly maps show that the observed eddies have a spatial structure in close resemblance to that found in coherent vortices of two-dimensional turbulence. These eddies appear to have a rather coherent vorticity-dominated core region surrounded by an outer region dominated by deformation with a very complicated and variable in time structure. This analysis is also applied to CTD data collected across three eddies sampled between 1997 and 1998. From these data eddy cores are equivalently defined as the interior region enclosed by the maximum of azimuthal velocity, and are consistent with the horizontal structures seen in SLA maps. The distinction between the core and the outer region (circulation cell) is particularly important to understand the role of transport and stirring of properties associated to eddies, as illustrated by the observed salinity structure, some selected SST images, and drifter trajectories. The core is characterized by very small isopycnal salinity gradients, while the surrounding cell is characterized by a strong slope of isohalines with respect to isopycnals. Persistent stagnation points are observed around the eddy and correspond to regions of high values of deformation with respect to vorticity. These regions allow analyzing characteristic patterns seen in the corresponding SST images. In addition, drifters trajectories exhibit very different behavior when crossing such regions. [Copyright &y& Elsevier]