Large wood debris that clogged bridges followed by a sudden release: the 2019 flash flood in Catalonia

The aim is the reconstruction of the October 2019 flash flood, that was documented through extensive field work: rainfall (300 mm in just a few hours), flood marks, times of flood passage and witnesses' snapshots and reports, channel changes, log drift (20,000 trees) and woody debris at bridges...

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Detalles Bibliográficos
Autores: Martín Vide, Juan Pedro|||0000-0002-4438-7724, Bateman Pinzón, Allen|||0000-0001-9980-6554, Berenguer Ferrer, Marc|||0000-0001-9208-7032, Ferrer Boix, Carles|||0000-0002-5605-8979, Amengual Pou, Arnau, Campillo Betbese, Manel, Corral Alexandri, Carles|||0000-0001-7705-7548, Llasat Botija, Maria Carmen, Llasat Botija, Montserrat, Gómez Dueñas, Santiago|||0000-0003-2962-4063, Marin-Esteve, Blanca|||0000-0002-3468-5234, Núñez González, Francisco|||0000-0002-3676-2715, Prats Puntí, Arnau, Ruiz Carulla, Roger|||0000-0003-0753-4745, Sosa Pérez, Raul
Tipo de recurso: artículo
Fecha de publicación:2023
País:España
Institución:Universitat Politècnica de Catalunya (UPC)
Repositorio:UPCommons. Portal del coneixement obert de la UPC
Idioma:inglés
OAI Identifier:oai:upcommons.upc.edu:2117/386090
Acceso en línea:https://hdl.handle.net/2117/386090
https://dx.doi.org/10.1016/j.ejrh.2023.101348
Access Level:acceso abierto
Palabra clave:Coarse woody debris
Flood damage
Flash flood
Large wood debris
Bridge hydraulics
Open-channel surge
Torrential flow
Fusta -- Residus
Inundacions -- Danys
Àrees temàtiques de la UPC::Enginyeria civil::Geologia::Riscos geològics
Descripción
Sumario:The aim is the reconstruction of the October 2019 flash flood, that was documented through extensive field work: rainfall (300 mm in just a few hours), flood marks, times of flood passage and witnesses' snapshots and reports, channel changes, log drift (20,000 trees) and woody debris at bridges, as well as large damage and six fatalities. The methods are: hydrological model built for the rainfall-runoff in the basin and the flood routing in the river, use of hydraulic principles such as flow at waterfalls, flow against obstacles (trees), etc. and finally 1D/2D free surface numerical models. The uppermost 100 km2 produced discharges of 700 m3/s (up to 50 m3/s/km2, locally). Three bridges failed, but their cascading failure (when one failure triggers the next one downstream) was not proved. The main channel widened more than 10 times, dragging away soil and vegetation like a bulldozer. The resulting large wood debris that clogged two bridges worsened the inundation. An anomalous flow downstream, probably a surge of around 1090 m3/s, due to the failure of a woody jam at a narrow bridge, took two lives. Water Authority is now warning flood planners that vegetated, torrential basins may cause catastrophic floods in the valley towns, if their narrow bridges are sensitive to woody debris.