Comparison of two early warning systems for regional flash flood hazard forecasting

•Two flash flood early warning systems are compared analysing three extreme events.•Hazard is assessed in terms of return period for the whole Liguria region.•Weather radar rainfall is used as input for the warning systems. The anticipation of flash flood events is crucial to issue warnings to mitig...

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Bibliographic Details
Published in:Journal of hydrology (Amsterdam) Vol. 572; pp. 603 - 619
Main Authors: Corral, Carles, Berenguer, Marc, Sempere-Torres, Daniel, Poletti, Laura, Silvestro, Francesco, Rebora, Nicola
Format: Journal Article Publication
Language:English
Published: Elsevier B.V 01-05-2019
Elsevier
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Summary:•Two flash flood early warning systems are compared analysing three extreme events.•Hazard is assessed in terms of return period for the whole Liguria region.•Weather radar rainfall is used as input for the warning systems. The anticipation of flash flood events is crucial to issue warnings to mitigate their impact. This work presents a comparison of two early warning systems for real-time flash flood hazard forecasting at regional scale. The two systems are based in a gridded drainage network and they use weather radar precipitation inputs to assess the hazard level in different points of the study area, considering the return period (in years) as the indicator of the flash flood hazard. The essential difference between the systems is that one is a rainfall-based system (ERICHA), using the upstream basin-aggregated rainfall as the variable to determine the hazard level, while the other (Flood-PROOFS) is a system based on a distributed rainfall-runoff model to compute the streamflows at pixel scale. The comparison has been done for three rainfall events in the autumn of 2014 that resulted in severe flooding in the Liguria region (Northwest of Italy). The results obtained by the two systems show many similarities, particularly for larger catchments and for large return periods (extreme floods).
ISSN:0022-1694
1879-2707
DOI:10.1016/j.jhydrol.2019.03.026