Hydrol. Earth Syst. Sci., 21, 1397–1419, 2017 www.hydrol-earth-syst-sci.net/21/1397/2017/ doi:10.5194/hess-21-1397-2017 © Author(s) 2017. CC Attribution 3.0 License. The European 2015 drought from a climatological perspective Monica Ionita1,2, Lena M. Tallaksen3, Daniel G. Kingston4, James H. Stagge3, Gregor Laaha5, Henny A. J. Van Lanen6, Patrick Scholz1, Silvia M. Chelcea7, and Klaus Haslinger8 1Alfred Wegener Institute Helmholtz Center for Polar and Marine Research, Bremerhaven, Germany 2MARUM – Center for Marine Environmental Sciences, University of Bremen, Bremen, Germany 3Department of Geosciences, University of Oslo, Oslo, Norway 4Department of Geography, University of Otago, Otago, New Zealand 5University of Natural Resources and Life Sciences Vienna (BOKU), Institute of Applied Statistics and Computing, Vienna, Austria 6Hydrology and Quantitative Water Management Group, Wageningen University, Wageningen, the Netherlands 7National Institute of Hydrology and Water Management, Bucharest, Romania 8Central Institute for Meteorology and Geodynamics, Vienna, Austria Correspondence to: Monica Ionita (
[email protected]) Received: 9 May 2016 – Discussion started: 19 May 2016 Revised: 27 January 2017 – Accepted: 16 February 2017 – Published: 8 March 2017 Abstract. The summer drought of 2015 affected a large por- positive geopotential height anomalies over Greenland and tion of continental Europe and was one of the most severe northern Canada. Simultaneously, the summer sea surface droughts in the region since summer 2003. The summer temperatures (SSTs) were characterized by large negative of 2015 was characterized by exceptionally high tempera- anomalies in the central North Atlantic Ocean and large pos- tures in many parts of central and eastern Europe, with daily itive anomalies in the Mediterranean basin.