| Literature DB >> 28798129 |
Günter Blöschl1, Julia Hall2, Juraj Parajka2, Rui A P Perdigão2, Bruno Merz3, Berit Arheimer4, Giuseppe T Aronica5, Ardian Bilibashi6, Ognjen Bonacci7, Marco Borga8, Ivan Čanjevac9, Attilio Castellarin10, Giovanni B Chirico11, Pierluigi Claps12, Károly Fiala13, Natalia Frolova14, Liudmyla Gorbachova15, Ali Gül16, Jamie Hannaford17, Shaun Harrigan17, Maria Kireeva14, Andrea Kiss2, Thomas R Kjeldsen18, Silvia Kohnová19, Jarkko J Koskela20, Ondrej Ledvinka21, Neil Macdonald22, Maria Mavrova-Guirguinova23, Luis Mediero24, Ralf Merz25, Peter Molnar26, Alberto Montanari10, Conor Murphy27, Marzena Osuch28, Valeryia Ovcharuk29, Ivan Radevski30, Magdalena Rogger2, José L Salinas2, Eric Sauquet31, Mojca Šraj32, Jan Szolgay19, Alberto Viglione2, Elena Volpi33, Donna Wilson34, Klodian Zaimi35, Nenad Živković36.
Abstract
A warming climate is expected to have an impact on the magnitude and timing of river floods; however, no consistent large-scale climate change signal in observed flood magnitudes has been identified so far. We analyzed the timing of river floods in Europe over the past five decades, using a pan-European database from 4262 observational hydrometric stations, and found clear patterns of change in flood timing. Warmer temperatures have led to earlier spring snowmelt floods throughout northeastern Europe; delayed winter storms associated with polar warming have led to later winter floods around the North Sea and some sectors of the Mediterranean coast; and earlier soil moisture maxima have led to earlier winter floods in western Europe. Our results highlight the existence of a clear climate signal in flood observations at the continental scale.Entities:
Year: 2017 PMID: 28798129 DOI: 10.1126/science.aan2506
Source DB: PubMed Journal: Science ISSN: 0036-8075 Impact factor: 47.728