Flood data from 500 years: Rivers and climate change in Europe
- Date:
- July 22, 2020
- Source:
- Vienna University of Technology
- Summary:
- Studying historical documents from 5 centuries, scientists were able to compare flood events from the past with recent flood events in Europe. This combination of historical and hydrological research provides evidence for the strong influence of climate change on rivers and floodings. Floods tend to be larger, the timing has shifted and the relationship between flood occurrence and air temperatures has reversed.
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Overflowing rivers can cause enormous problems: Worldwide, the annual damage caused by river floods is estimated at over 100 billion dollars -- and it continues to rise. To date it has been unclear whether Europe is currently in a flood-rich period from a long-term perspective.
Austrian flood expert Prof. Günter Blöschl from TU Wien (Vienna) has led a large international study involving a total of 34 research groups that provides clear evidence that the past three decades were among the most flood-rich periods in Europe during the past 500 years, and that this period differs from others in terms of its extent, air temperatures and flood seasonality. Compared to the past, floods tend to be larger in many places, the timing has shifted and the relationship between flood occurrence and air temperatures has reversed. In the past, floods tended to occur more frequently in cold phases, while today, global warming is one of the main drivers of their increase. The results of the study have now been published in "Nature" magazine.
Historical data from half a millennium
"From our previous research, we already knew how climate change has affected Europe's floods in the past 50 years," says Alberto Viglione from the Politecnico di Torino, one of the key authors of the publication. "For forecasts of the next decades, however, it is also important to understand whether this is a completely new situation or whether this is just a repetition of something that has already occurred. So far, the available data had not been sufficient to ascertain whether this is the case or not. We have examined this question in great detail and can now say with confidence: Yes, flooding characteristics in recent decades are unlike those of the previous centuries."
For the study, tens of thousands of historical documents containing contemporary flood reports from the period 1500 to 2016 were analysed. The TU Wien team has worked with historians from all over Europe. "The particular challenge of this study consisted in making the very different texts of the different centuries and different cultural regions comparable," explains Andrea Kiss from the Vienna University of Technology, researcher and historian herself, and one of the key authors of the publication. "We managed to achieve this comparability by putting all the texts in their respective historical contexts with painstaking attention to detail."
Formerly cold, now warm: River floods now function differently
The data analysis identified nine flood-rich periods and associated regions. Among the most notable periods were 1560-1580 (western and central Europe), 1760-1800 (most of Europe), 1840-1870 (western and southern Europe) and 1990-2016 (western and central Europe). Comparisons with air temperature reconstructions showed that these historical flood periods were substantially cooler than intervening phases.
"This finding seems to contradict the observation that, in some areas such as in the northwest of Europe, the recent warmer climate is aligned with larger floods," says Günter Blöschl. "Our study shows for the first time that the underlying mechanisms have changed: While, in the past, floods have occurred more frequently under colder conditions, the opposite is the case now. The hydrological conditions of the present are very different from those in the past."
The timing of the floods within the year has also changed. Previously, 41% of Central European floods occurred in the summer, compared to 55% today. These shifts are related to changes in precipitation, evaporation and snowmelt and are an important indicator for distinguishing the role of climate change from that of other controls such as deforestation and river management.
These findings have been made possible by a new data base compiled by the study authors that includes the exact dating of almost all flood events reported by written sources. So far, one had to often rely on other, less precise sources of information, such as lake sediments. It is the first study worldwide to evaluate historical flood periods for an entire continent in such detail.
Better data -- better forecasts
Because of the shift in the flood generating mechanisms, Günter Blöschl advocates the use of tools for flood-risk assessment that capture the physical processes involved, and management strategies that can incorporate the recent changes in risk. "Regardless of the necessary efforts of climate change mitigation, we will see the effects of these changes in the coming decades," says Blöschl. "Flood management must adapt to these new realities."
Video: https://www.youtube.com/watch?time_continue=1&v=fQMqw-P51qs&feature=emb_logo
Story Source:
Materials provided by Vienna University of Technology. Note: Content may be edited for style and length.
Journal Reference:
- Günter Blöschl, Andrea Kiss, Alberto Viglione, Mariano Barriendos, Oliver Böhm, Rudolf Brázdil, Denis Coeur, Gaston Demarée, Maria Carmen Llasat, Neil Macdonald, Dag Retsö, Lars Roald, Petra Schmocker-Fackel, Inês Amorim, Monika Bělínová, Gerardo Benito, Chiara Bertolin, Dario Camuffo, Daniel Cornel, Radosław Doktor, Líbor Elleder, Silvia Enzi, João Carlos Garcia, Rüdiger Glaser, Julia Hall, Klaus Haslinger, Michael Hofstätter, Jürgen Komma, Danuta Limanówka, David Lun, Andrei Panin, Juraj Parajka, Hrvoje Petrić, Fernando S. Rodrigo, Christian Rohr, Johannes Schönbein, Lothar Schulte, Luís Pedro Silva, Willem H. J. Toonen, Peter Valent, Jürgen Waser, Oliver Wetter. Current European flood-rich period exceptional compared with past 500 years. Nature, 2020; 583 (7817): 560 DOI: 10.1038/s41586-020-2478-3
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