EU Budgetary Responses to the ‘Refugee Crisis’: Reconfiguring the Funding Landscape. CEPS Paper Liberty and Security in Europe No. 93/May 2016

This paper analyses the EU budgetary responses to the ‘refugee crisis’ in Europe. The European Commission has proposed several changes to the EU budget as well as the establishment of new funding instruments. The paper explores what the announced funding consists of, what role it plays in policy-making and what issues it generates. Throughout these budgetary responses the search for flexibility has been dominant, motivated by the need to respond more swiftly to humanitarian and operational needs. In addition, the paper argues that beyond implementation or management, the role of funding is also symbolic and communicative. In light of limited competences that are difficult to exercise, funding represents a powerful tool enabling the Commission to shape policy-making in times of crisis. At the same time, the dominant search for flexibility also challenges established funding rules and procedures. It has furthermore led to reduced space for democratic scrutiny by the European Parliament. More profoundly, EU funding for cooperation with third countries to prevent the inflow of refugees and asylum seekers has monetised questions over the responsibility for these individuals. As the EU–Turkey agreement shows, this has created a self-imposed dependence on third countries, with the risk of potentially insatiable demands for EU funding. This paper questions the proportionality and rule of law compliance of allocating funding for the implementation of this agreement. Moreover, it proposes that the Commission take steps to practically safeguard the humanitarian aid principles in the management structures of the new funding instruments, and it stresses the need for more scrutiny of the reconfigured funding landscape by the European Parliament and the European Court of Auditors.

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.