The aim of the cruise was chiefly geological-geophysical; thus the main purpose of oceanographic. measurements was that of updating and correcting sound velocity for MB acquisition. CTD casts were collected with a SeaBird probe each 24 hours in the 0-2500m depth range. However, several anomalies with respect to modelled temperature/salinity profiles in this region of the North Atlantic mainly due to the influence of Mediterranean Water in the form of Meddies (Mediterranean eddies) were detected. The Meddies are coherent structures of warm and salt Mediterranean Water advected in the northeast Atlantic. Their thermo-haline properties are in the average 11.8°C, 36 psu with a radius between 25 and 110 km, and thickness between 500 and 1000 (see ref.). In almost all the water measurements such Meddies were detected in the proximity of Ampére , and Unicorn smts. at depths between 700 and 1300 m. Due to the lost of the CTD probe at the end of the 1st leg the remaining water measurements were done with the spare SVP probe usable only down to 1000 m depths. For this reason, no deep data over Seine smt was obtained nor the potential evidence for the existence of Meddies in this area. The physical sensors installed under the ship hull allowed the continual measurement, with a sampling frequency of 5 minutes, of the surface water temperature and salinity. The mean sea-water temperature was around 21.5°C in the Atlantic (starting from 23.5 °C in the Mediterranean). Crossing the Gibraltar Strait, the water temperature decreased to 16-17 °C. A 2°C decrease was also detected at the passage of Bonifacio Strait (between Sardinia and Corsica).
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