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The European 2015 drought from a hydrological perspective

The European 2015 drought from a hydrological perspective

Authors :
Laaha, Gregor
Gauster, Tobias
Tallaksen, Lena M.
Vidal, Jean-Philippe
Stahl, Kerstin
Prudhomme, Christel
Heudorfer, Benedikt
Vlnas, Radek
Ionita, Monica
Van Lanen, Henny A.J.
Adler, Mary-Jeanne
Caillouet, Laurie
Delus, Claire
Fendekova, Miriam
Gailliez, Sebastien
Hannaford, Jamie
Kingston, Daniel
Van Loon, Anne F.
Mediero, Luis
Osuch, Marzena
Romanowicz, Renata
Sauquet, Eric
Stagge, James H.
Wong, Wai K.
Laaha, Gregor
Gauster, Tobias
Tallaksen, Lena M.
Vidal, Jean-Philippe
Stahl, Kerstin
Prudhomme, Christel
Heudorfer, Benedikt
Vlnas, Radek
Ionita, Monica
Van Lanen, Henny A.J.
Adler, Mary-Jeanne
Caillouet, Laurie
Delus, Claire
Fendekova, Miriam
Gailliez, Sebastien
Hannaford, Jamie
Kingston, Daniel
Van Loon, Anne F.
Mediero, Luis
Osuch, Marzena
Romanowicz, Renata
Sauquet, Eric
Stagge, James H.
Wong, Wai K.
Publication Year :
2017

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 emphasiz

Details

Database :
OAIster
Notes :
text, English
Publication Type :
Electronic Resource
Accession number :
edsoai.ocn994218265
Document Type :
Electronic Resource