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Cascading continental-scale floods across Europe in 1342-1343
Andrea Kiss1, Alberto Viglione2, Mariano Barriendos3
1Institute of Hydraulic Engineering and Water Resources Management, Vienna University of Technology, Vienna, Austria. kiss@hydro.tuwien.ac.at.
Extreme European floods occurred in 1342-1343, with four events having 500-1,000 year return periods. This flood sequence prompted significant changes in flood risk management strategies.
Area of Science:
- Environmental Science
- Climate Science
- Historical Hydrology
Background:
- Europe has faced severe floods recently, but understanding historical extreme flood events is crucial for effective flood risk management.
- The Magdalena Flood of 1342 is often cited as the largest flood in Central Europe over the last millennium, yet its characteristics remain incompletely understood.
Purpose of the Study:
- To analyze historical flood data to better understand extreme flood characteristics and their implications for modern flood risk management.
- To investigate the 1342 Magdalena Flood and its context within a broader sequence of European flood events.
Main Methods:
- Analysis of a new documentary dataset detailing major flood events across Europe between late 1341 and 1343.
- Statistical analysis to determine return periods for identified extreme flood events.
Main Results:
- Sixteen major flood events occurred across Europe between late 1341 and 1343.
- Four of these floods (Magdalena, Bartholomew, Candlemas, and Jacob Floods) exhibited return periods of 500-1,000 years.
- 1342 stands out as the year with the most extreme floods in the past 700 years, with 1343 also ranking highly.
Conclusions:
- The 1342-1343 flood sequence was a broader phenomenon than previously recognized, with the Magdalena Flood being part of a larger pattern.
- This extreme flood period had significant socio-economic consequences, leading to a paradigm shift in European flood mitigation.
- A plausible cause for this flood sequence involves volcanic eruptions and Arctic sea ice retreat, highlighting the need for risk management strategies that consider clustered extreme events.
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