Publication | Open Access
The Relative Importance of Different Flood‐Generating Mechanisms Across Europe
364
Citations
48
References
2019
Year
Hydrological PredictionEngineeringRelative ImportanceHydrologic EngineeringFlood ControlHydrologic HazardEarth ScienceHydroclimate ModelingHydrometeorologyGeographyFlood ForecastingFuture Flood RiskFlood ManagementHydrologyFlash FloodHydrological DisasterWater ResourcesSoil Moisture ExcessFlood Risk Management
Inferring flood mechanisms is key to understanding flood risk, yet a spatially distributed overview across Europe is lacking and studies often assign a single mechanism per catchment despite multiple contributing factors. The study introduces a seasonality‑based method to estimate the relative importance of extreme precipitation, soil moisture excess, and snowmelt as flood drivers, aiming to expose regional mechanisms underlying Europe’s most costly natural hazard to guide future research. The method estimates the relative importance of extreme precipitation, soil moisture excess, and snowmelt by analyzing seasonality statistics of maximum annual flow dates. From 1960 to 2010, few annual floods were driven by rainfall peaks; most were caused by snowmelt or by heavy precipitation combined with high antecedent soil moisture, and the relative importance of these mechanisms has remained largely unchanged over five decades.
Abstract Inferring the mechanisms causing river flooding is key to understanding past, present, and future flood risk. However, a quantitative spatially distributed overview of the mechanisms that drive flooding across Europe is currently unavailable. In addition, studies that classify catchments according to their flood‐driving mechanisms often identify a single mechanism per location, although multiple mechanisms typically contribute to flood risk. We introduce a new method that uses seasonality statistics to estimate the relative importance of extreme precipitation, soil moisture excess, and snowmelt as flood drivers. Applying this method to a European data set of maximum annual flow dates in several thousand catchments reveals that from 1960 to 2010 relatively few annual floods were caused by annual rainfall peaks. Instead, most European floods were caused by snowmelt and by the concurrence of heavy precipitation with high antecedent soil moisture. For most catchments, the relative importance of these mechanisms has not substantially changed during the past five decades. Exposing the regional mechanisms underlying Europe's most costly natural hazard is a key first step in identifying the processes that require most attention in future flood research.
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