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A multiscale sampling experiment was carried out in the Gulf ofTaranto (eastern Mediterranean) providing the first synoptic evidence of thelarge-scale circulation structure and associated mesoscale variability. Themapping of the mesoscale and large-scale geostrophic circulation showed thepresence of an anticyclonic large-scale gyre occupying the central open oceanarea of the Gulf of Taranto. On the periphery of the gyre upwelling isevident where surface waters are colder and saltier than at the center of thegyre. Over a 1-week period, the rim current of the gyre undergoes largechanges which are interpreted as baroclinic–barotropic instabilities,generating small-scale cyclonic eddies in the periphery of the anticyclone.The eddies are generally small, one of which can be classified as asubmesoscale eddy due to its size. This eddy field modulates the upwellingregime in the gyre periphery

Marine Rapid Environmental Assessment in the Gulf of Taranto: a multiscale approach