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Balasch Solanes, Josep Carles

Barriendos Valve, Mariano

Castelltort, Xavier

Furdada Bellavista, Glòria

Pino González, David

Porras, Leonel

Tuset Mestre, Jordi

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Geophysical Research AbstractsVol. 21, EGU2019-7960, 2019EGU General Assembly 2019© Author(s) 2019. CC Attribution 4.0 license.The Upper Garonne flood series from discharge gauging data (Bossost, Vald’Aran, Spain) and reconstruction of historical floods (Saint-Béat, France)Josep Carles Balasch Solanes (1), Jordi Tuset (2), Gloria Furdada (3), Leonel Porras (3), Xavier Castelltort (1),Mariano Barriendos (4), David Pino (5,6)(1) Department of Environment and Soil Sciences, ETSEA, University of Lleida Lleida, Spain (cbalasch@macs.udl.cat), (2)RIUS Dynamic Fluvial Research Group, University of Lleida, Lleida, Spain , (3) Department of Earth and Ocean Dynamics,University of Barcelona, Barcelona, Spain, (4) Department of History and Archaeology, University of Barcelona, Barcelona,Spain, (5) Department of Physics, Universitat Politècnica de Catalunya, Barcelona, Spain, (6) Institut d’Estudis Espacials deCatalunya (IEEC-UPC), Barcelona, SpainTraditionally, the Val d’Aran in Spain has been considered the headwaters of the Garonne River, an internationalriver that, after a short journey through Spain, goes into France and heads towards its mouth in the Atlantic Oceanafter a journey of more than 647 km. Systematic gauging of the Garonne River are recorded in Bossost near theoutlet of the Aran Valley (647 km2 of the basin), but the series cover a relatively short period (from 1965 to thepresent) and prudence must be exercised when extrapolating the flows corresponding to high return periods. Onepossibility to reduce the uncertainty when carrying out the frequency analysis is to complement the systematicseries with the data of maximum flows from the hydraulic reconstruction of historical floods.In the French town of Saint-Béat (Haute-Garonne), about 20 km downstream of the town of Bossost (Val d’Aran)and in the French part of the basin, the marks reached by the waters in different episodes are available for differentfloods (flood marks) since the year 1778. This information is not available in the Spanish territory of the Garonne.Therefore, the maximum discharges of the historical floods were obtained by the reconstruction of these episodesusing the flood marks registered in Saint-Béat. In each historical flood, the role of the merging of the snow mantlein the headwater as a contributory mechanism to the precipitation in the formation of flood runoff has beenanalyzed simultaneously.The peak flows of the historical floods in the town of Saint-Béat (673 km2 of the basin) have been reconstructedwith the help of the hydraulic model HEC-RAS v. 4.1.0 on a DTM with a resolution of 1m x 1m, consideringthe morphological changes of the bed and the floodplains and their roughness from the old cartography, cadastralplans and detail photographs to recompose the land uses and the vegetation occupation of the flooded areas ineach period.The historical reconstructed peak discharges from the floods of the last 250 years clearly surpass those obtainedin the systematic flow series of the last 50 years, indicating the lack of extreme values contained in said series. Itsinclusion in flood frequency analysis allows reducing the uncertainty of an insufficient time series and improvingthe prediction of low recurrence quantiles in flood risk planning.

The Upper Garonne flood series from discharge gauging data (Bossost, Vald’Aran, Spain) and reconstruction of historical floods (Saint-Béat, France)

https://upcommons.upc.edu/bitstream/2117/167857/1/EGU2019-7960.pdf

The Upper Garonne flood series from discharge gauging data (Bossost, Vald’Aran, Spain) and reconstruction of historical floods (Saint-Béat, France)

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