Journal cover Journal topic
Hydrology and Earth System Sciences An interactive open-access journal of the European Geosciences Union
Hydrol. Earth Syst. Sci., 21, 3001-3024, 2017
https://doi.org/10.5194/hess-21-3001-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
Research article
22 Jun 2017
The European 2015 drought from a hydrological perspective
Gregor Laaha1, Tobias Gauster1, Lena M. Tallaksen2, Jean-Philippe Vidal3, Kerstin Stahl4, Christel Prudhomme5,6, Benedikt Heudorfer4, Radek Vlnas7,8, Monica Ionita9, Henny A. J. Van Lanen10, Mary-Jeanne Adler11, Laurie Caillouet3, Claire Delus12, Miriam Fendekova13, Sebastien Gailliez14, Jamie Hannaford5, Daniel Kingston15, Anne F. Van Loon16, Luis Mediero17, Marzena Osuch18, Renata Romanowicz18, Eric Sauquet3, James H. Stagge2, and Wai K. Wong19 1Institute of Applied Statistics and Computing, University of Natural Resources and Life Sciences (BOKU), Vienna, Austria
2Department of Geosciences, University of Oslo, Oslo, Norway
3Irstea, UR HHLY, Hydrology-Hydraulics Research Unit, 69100 Villeurbanne, France
4Hydrology, Faculty of Environment and Natural Resources, University of Freiburg, Freiburg, Germany
5Centre for Ecology and Hydrology, Wallingford, UK
6Department of Geography, Loughborough University, Loughborough, UK
7Faculty of Environmental Sciences, Czech University of Life Sciences Prague, Prague, Czech Republic
8T. G. Masaryk Water Research Institute, Prague, Czech Republic
9Alfred-Wegener-Institute for Polar and Marine Research, Bremerhaven, Germany
10Hydrology and Quantitative Water Management Group, Wageningen University, Wageningen, the Netherlands
11National Institute of Hydrology and Water Management, Bucharest, Romania
12Laboratoire d'Observation des Territoires, Université de Lorraine, Nancy, France
13Department of Hydrogeology,, Comenius University, Bratislava, Slovakia
14Service Public de Wallonie, Jambes, Belgium
15Department of Geography, University of Otago, Dunedin, New Zealand
16Water Science Research Group, School of Geography, Earth, and Environmental Sciences, University of Birmingham, Brimingham, UK
17Department of Hydraulic and Energy Engineering, Technical University of Madrid, Madrid, Spain
18Institute of Geophysics Polish Academy of Sciences, Warsaw, Poland
19Norwegian Water Resources and Energy Directorate, Oslo, Norway
Abstract. In 2015 large parts of Europe were affected by drought. In this paper, we analyze the hydrological footprint (dynamic development over space and time) of the drought of 2015 in terms of both severity (magnitude) and spatial extent and compare it to the extreme drought of 2003. Analyses are based on a range of low flow and hydrological drought indices derived for about 800 streamflow records across Europe, collected in a community effort based on a common protocol. We compare the hydrological footprints of both events with the meteorological footprints, in order to learn from similarities and differences of both perspectives and to draw conclusions for drought management. The region affected by hydrological drought in 2015 differed somewhat from the drought of 2003, with its center located more towards eastern Europe. In terms of low flow magnitude, a region surrounding the Czech Republic was the most affected, with summer low flows that exhibited return intervals of 100 years and more. In terms of deficit volumes, the geographical center of the event was in southern Germany, where the drought lasted a particularly long time. A detailed spatial and temporal assessment of the 2015 event showed that the particular behavior in these regions was partly a result of diverging wetness preconditions in the studied catchments. Extreme droughts emerged where preconditions were particularly dry. In regions with wet preconditions, low flow events developed later and tended to be less severe. For both the 2003 and 2015 events, the onset of the hydrological drought was well correlated with the lowest flow recorded during the event (low flow magnitude), pointing towards a potential for early warning of the severity of streamflow drought. Time series of monthly drought indices (both streamflow- and climate-based indices) showed that meteorological and hydrological events developed differently in space and time, both in terms of extent and severity (magnitude). These results emphasize that drought is a hazard which leaves different footprints on the various components of the water cycle at different spatial and temporal scales. The difference in the dynamic development of meteorological and hydrological drought also implies that impacts on various water-use sectors and river ecology cannot be informed by climate indices alone. Thus, an assessment of drought impacts on water resources requires hydrological data in addition to drought indices based solely on climate data. The transboundary scale of the event also suggests that additional efforts need to be undertaken to make timely pan-European hydrological assessments more operational in the future.

Citation: Laaha, G., Gauster, T., Tallaksen, L. M., Vidal, J.-P., Stahl, K., Prudhomme, C., Heudorfer, B., Vlnas, R., Ionita, M., Van Lanen, H. A. J., Adler, M.-J., Caillouet, L., Delus, C., Fendekova, M., Gailliez, S., Hannaford, J., Kingston, D., Van Loon, A. F., Mediero, L., Osuch, M., Romanowicz, R., Sauquet, E., Stagge, J. H., and Wong, W. K.: The European 2015 drought from a hydrological perspective, Hydrol. Earth Syst. Sci., 21, 3001-3024, https://doi.org/10.5194/hess-21-3001-2017, 2017.
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Short summary
In 2015 large parts of Europe were affected by a drought. In terms of low flow magnitude, a region around the Czech Republic was most affected, with return periods > 100 yr. In terms of deficit volumes, the drought was particularly severe around S. Germany where the event lasted notably long. Meteorological and hydrological events developed differently in space and time. For an assessment of drought impacts on water resources, hydrological data are required in addition to meteorological indices.
In 2015 large parts of Europe were affected by a drought. In terms of low flow magnitude, a...
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