Abstract

The North Atlantic is the most important sink for atmospheric CO 2 although there still remain uncertainties about the total amount stored by this region and the contribution of the anthropogenic CO 2 (C ANT) that is exchanged between the Mediterranean Sea and the Atlantic Ocean. During the P 3A 2 cruise performed in October 2008 throughout the oceanic area covered by the Gulf of Cádiz and the Strait of Gibraltar, which channelizes the water exchange between the Atlantic and the Mediterranean, extensive measurements of the carbon system parameters (pH, total alkalinity and total inorganic carbon) and others related (dissolved oxygen and nutrients) were carried out to analyze their distribution in the area. In order to study the C ANT spatial variability, three observational methods for C ANT concentration assessment (φC T°, ∆C* and TrOCA) were applied. The three water masses identified in the area, North Atlantic Central Water (NACW), North Atlantic Deep Water (NADW) and Mediterranean Outflow Water (MOW), were shown to contain different C ANT concentration. NADW exhibited the lowest C ANT levels whereas NACW was the most C ANT enriched. Data also indicate a net import of C ANT from the Atlantic towards the Mediterranean through Gibraltar. Specific C ANT inventories showed that MOW contributes in 8–12% to the total specific C ANT inventory of the Gulf of Cádiz.

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