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The CO2 system in the Mediterranean Sea: a basin wide perspective
[摘要] The Mediterranean Sea (MedSea) is considered a "laboratory basin" being anocean in miniature, suffering dramatic changes in its oceanographic andbiogeochemical conditions derived from natural and anthropogenic forces.Moreover, the MedSea is prone to absorb and store anthropogenic carbon dueto the particular CO2 chemistry and the active overturning circulation.Despite this, water column CO2 measurements covering the whole basinare scarce. This work aims to be a base-line for future studies about theCO2 system space-time variability in the MedSea combining historic andmodern CO2 cruises in the whole area. Here we provide an extensivevertical and longitudinal description of the CO2 system variables(total alkalinity – TA, dissolved inorganic carbon – DIC and pH) along anEast-West transect and across the Sardinia-Sicily passage in the MedSea fromtwo oceanographic cruises conducted in 2011 measuring CO2 variables ina coordinated fashion, the RV Meteor M84/3 and the RV Urania EuroFleets 11,respectively. In this sense, we provide full-depth and length CO2distributions across the MedSea, and property-property plots showing in eachsub-basin post-Eastern Mediterranean Transient (EMT) situation with regardto TA, DIC and pH.

The over-determined CO2 system in 2011 allowed performing the firstinternal consistency analysis for the particularly warm, high salinity andalkalinity MedSea waters. The CO2 constants by Mehrbach et al. (1973)refitted by Dickson and Millero (1987) are recommended. The sensitivity ofthe CO2 system to the atmospheric CO2 increase, DIC and/or TAchanges is evaluated by means of the Revelle and buffer factors.
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[效力级别]  [学科分类] 海洋学与技术
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