An EU mechanism on Democracy, the Rule of Law and Fundamental Rights. CEPS Paper in Liberty and Security in Europe No. 91/April 2016 Thursday, 21 April 2016

The European Union is founded on a set of common principles of democracy, the rule of law, and fundamental rights, as enshrined in Article 2 of the Treaty on the European Union. Whereas future Member States are vetted for their compliance with these values before they accede to the Union, no similar method exists to supervise adherence to these foundational principles after accession. EU history proved that this ‘Copenhagen dilemma’ was far from theoretical. EU Member State governments’ adherence to foundational EU values cannot be taken for granted. Violations may happen in individual cases, or in a systemic way, which may go as far as overthrowing the rule of law. Against this background the European Parliament initiated a Legislative Own-Initiative Report on the establishment of an EU mechanism on democracy, the rule of law and fundamental rights and proposed among others a Scoreboard on the basis of common and objective indicators by which foundational values can be measured. This Research Paper assesses the need and possibilities for the establishment of an EU Scoreboard, as well as its related social, economic, legal and political ‘costs and benefits’.

Data compilation of ESOP

The work in this sub-project of ESOP focuses on the advective and convective transforma-tion of water masses in the Greenland Sea and its neighbouring areas. It includes observational work on the sub-mesoscale and analysis of hydrographic data up to the gyre-scale. Observations of active convective plumes were made with a towed chain equipped with up to 80 CTD sensors, giving a horizontal and vertical resolution of the hydrographic fields of a few metres. The observed scales of the penetrative convective plumes compare well with those given by theory. On the mesoscale the structure of homogeneous eddies formed as a result of deep convection was observed and the associated mixing and renewal of the intermediate layers quantified. The relative importance and efficiency of thermal and haline penetrative convection in relation to the surface boundary conditions (heat and salt fluxes and ice cover) and the ambient stratification are studied using the multi year time series of hydro-graphic data in the central Greenland Sea. The modification of the water column of the Greenland Sea gyre through advection from and mixing with water at its rim is assessed on longer time scales. The relative contributions are quantified using modern water mass analysis methods based on inverse techniques. Likewise the convective renewal and the spreading of the Arctic Intermediate Water from its formation area is quantified. The aim is to budget the heat and salt content of the water column, in particular of the low salinity surface layer, and to relate its seasonal and interannual variability to the lateral fluxes and the fluxes at the air-sea-ice interface. This will allow to estimate residence times for the different layers of the Greenland Sea gyre, a quantity important for the description of the Polar Ocean carbon cycle.