Articles | Volume 22, issue 3
https://doi.org/10.5194/nhess-22-831-2022
https://doi.org/10.5194/nhess-22-831-2022
Research article
 | 
11 Mar 2022
Research article |  | 11 Mar 2022

Geo-historical database of flood impacts in Alpine catchments (HIFAVa database, Arve River, France, 1850–2015)

Eva Boisson, Bruno Wilhelm, Emmanuel Garnier, Alain Mélo, Sandrine Anquetin, and Isabelle Ruin

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ACTHYS-Diffusion: Etude pour la restauration des systèmes d'endiguement de l'Arve et du Borne, Fiches d'information historique (FIH) par système d'endiguement, report, 304 pp., 2017. 
Antoine, J.-M.: Vulnérabilité et adaptation des sociétés montagnardes à la torrentialité au cours du Petit Âge Glaciaire dans les Pyrénées, Journal is Sud-Ouest Européen (SOE), 32, 53–66, https://doi.org/10.4000/soe.685, 2011. 
Barriendos, M., Coeur, D., Lang, M., Llasat, M. C., Naulet, R., Lemaitre, F., and Barrera, A.: Stationarity analysis of historical flood series in France and Spain (14th–20th centuries), Nat. Hazards Earth Syst. Sci., 3, 583–592, https://doi.org/10.5194/nhess-3-583-2003, 2003. 
Barriendos, M., Ruiz-Bellet, J. L., Tuset, J., Mazón, J., Balasch, J. C., Pino, D., and Ayala, J. L.: The “Prediflood” database of historical floods in Catalonia (NE Iberian Peninsula) AD 1035–2013, and its potential applications in flood analysis, Hydrol. Earth Syst. Sci., 18, 4807–4823, https://doi.org/10.5194/hess-18-4807-2014, 2014. 
Barriendos, M., Gil-Guirado, S., Pino, D., Tuset, J., Pérez-Morales, A., Alberola, A., Costa, J., Balasch, J. C., Castelltort, X., Mazón, J., and Ruiz-Bellet, J. L.: Climatic and social factors behind the Spanish Mediterranean flood event chronologies from documentary sources (14th–20th centuries), Global Planet. Change, 182, 102997, https://doi.org/10.1016/j.gloplacha.2019.102997, 2019. 
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Short summary
We present the database of Historical Impacts of Floods in the Arve Valley (HIFAVa). It reports flood occurrences and impacts (1850–2015) in a French Alpine catchment. Our results show an increasing occurrence of impacts from 1920 onwards, which is more likely related to indirect source effects and/or increasing exposure rather than hydrological changes. The analysis reveals that small mountain streams caused more impacts (67 %) than the main river.
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