ON THE STRUCTURE OF THE MEAN FLOW IN THE BLANES CANYON AREA (NW MEDITERRANEAN) DURING SUMMER

The MECA 93 oceanographic cruise was carried out in June 1993. The mai n purpose of the experiment was to understand the action of the main d riving mechanisms responsible for the flow variability in the Blanes c anyon area (NW Mediterranean) during summer. A domain of about 4000 km (2) including the canyon was covered by RN Hesperides between 17 and 2 2 June 1993. CTD sampling was performed with characteristic spacing be tween adjacent stations of 7 to 15 km. The water masses distribution o bserved during the cruise corresponds to a classical, well-established summer stratification, with typical surface temperatures above 22 deg rees C. The thermocline was located at a 40 m depth. The TS diagrams r eveal water exchanges across the shelf edge. The surface distributions of temperature and salinity display patches of cool and low-salinity water on the slope. The flow distribution which emerges from ADCP meas urements performed throughout the cruise does not match the fully topo graphically-steered circulation pattern expected on the basis of previ ous model results. The surface currents on the shelf are northeastward s, i.e. opposite to the southwestward general circulation on the conti nental slope. This result is in agreement both with the surface circul ation picture evidenced by a contemporary SAR scene acquired by ERS-1 and with the trajectories of the LCD drifters launched north of the ca nyon at the outset of the cruise. ADCP measurements at depths below 50 m suggest that the prevailing flow pattern on the shelf was reversed below the thermocline. We assume that the inflow of relatively cold an d low-salinity water advected from the Gulf of Lions was responsible f or an inversion of the horizontal pressure gradient which forced the s urface current reversal on the shelf.