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Drifter measurements and satellite altimetry data are merged to reconstructthe surface geostrophic circulation of the Black Sea in the period1999–2009. This combined data set is used to estimate pseudo-Eulerianvelocity statistics for different time periods. Seasonal and interannualvariability of currents and kinetic energy fields are described withparticular attention to the mesoscale and sub-basin coastal eddies. The meancurrents are generally stronger in winter and enhanced speeds are observed inthe period 2002–2006. The most intense activity of sub-basin Batumi Eddyoccurs in summer with greater speeds and dimensions in 2006 and 2008. Thesub-basin Sevastopol Eddy is generated in spring from a meander of the RimCurrent. Mesoscale eddies located along the Anatolia, Caucasus and Crimeacoasts are permanent, quasi-permanent or intermittent features and caninteract and merge with each other, showing high values of kinetic energy

Geostrophic currents and kinetic energies in the Black Sea estimated from merged drifter and satellite altimetry data