The research Institutes involved in the project are indebted to Stena Line for making possible the installation and operation of the Blue Box system on their vessels. “
“The Adriatic Sea is a deeply indented gulf of the Mediterranean (ca 800 km long and 200 km wide); it is classified as a semi-enclosed sea. It is situated between the Apennine and Balkan peninsulas, at longitudes between 12°15′E and 19°45′E, and latitudes between 39°45′N and 45°45′N (Figure 1). The southern border of the Adriatic Sea crosses the Strait of Otranto in a line running from the mouth of the River Buttrinto (39°44′) in Albania to Cape Karagol in

Corfu, across this island to Cape Kephali (these two capes are at latitude 39°45′N) and on to Cape MDV3100 Santa Maria di Leuca in Italy (IHO – International Hydrographic Organization 1953). The shallowest part of the Adriatic Sea is the northern Adriatic, a closed basin where, to the north of a line joining Pula and Ancona, depths do not exceed 50 m.

see more The surface circulation of the Adriatic Sea is regarded as a cyclonic meander comprising a northerly flow along the eastern coast and a southerly outgoing flow along the western coast (Orlić et al. 1992). A review of the Adriatic Sea circulation can be found in e.g. Orlić et al. (1992) and Cushman-Roisin et al. (2001). The Adriatic circulation depends strongly on the characteristics of air-sea fluxes of momentum, heat and water at the air-sea interface (Cushman-Roisin et al. 2001). In general, the resultant surface circulation in the Adriatic can be explained as a modification of gradient currents under the influence of tides and blowing winds. For the purposes of this paper special attention will be given to the surface circulation of the northern Adriatic, especially to departures from its general circulation pattern. The double-gyre response of the

northern Adriatic to intense bora winds (a cyclonic gyre north of the Po Delta – Rovinj line and an anticyclonic gyre to the south; Figure 2) Tacrolimus (FK506) has been described by a number of authors, e.g. Zore-Armanda & Gačić (1987), who analysed current meter data, and Orlićet al. (1994), who applied a numerical model. The Istrian Coastal Countercurrent (ICCC) and its year-on-year variability is another interesting phenomenon in the northern Adriatic, observed (e.g. Supić et al. 2000) and reproduced by numerical models (e.g. Cushman-Roisin & Korotenko 2007). A southerly current along the Istrian coast, the ICCC usually appears in the summer season; this is a current reversal in comparison with the general circulation. While Supić et al.