River widening in mountain and foothill areas during floods: Insights from a meta-analysis of 51 European Rivers.

Bank erosion Channel planform changes Flood response Geomorphic changes Width ratio

Journal

The Science of the total environment
ISSN: 1879-1026
Titre abrégé: Sci Total Environ
Pays: Netherlands
ID NLM: 0330500

Informations de publication

Date de publication:
10 Dec 2023
Historique:
received: 22 05 2023
revised: 17 07 2023
accepted: 05 08 2023
pubmed: 10 8 2023
medline: 10 8 2023
entrez: 9 8 2023
Statut: ppublish

Résumé

River widening, defined as a lateral expansion of the channel, is a critical process that maintains fluvial ecosystems and is part of the regular functioning of rivers. However, in areas with high population density, channel widening can cause damage during floods. Therefore, for effective flood risk management it is essential to identify river reaches where abrupt channel widening may occur. Despite numerous efforts to predict channel widening, most studies have been limited to single rivers and single flood events, which may not be representative of other conditions. Moreover, a multi-catchment scale approach that covers various settings and flood magnitudes has been lacking. In this study, we fill this gap by compiling a large database comprising 1564 river reaches in several mountain regions in Europe affected by floods of varying magnitudes in the last six decades. By applying a meta-analysis, we aimed to identify the types of floods responsible for more extensive widening, the river reach types where intense widening is more likely to occur, and the hydraulic and morphological variables that explain widening and can aid in predicting widening. Our analysis revealed seven groups of reaches with significantly different responses to floods regarding width ratios (i.e., the ratio between channel width after and before a flood). Among these groups, the river reaches located in the Mediterranean region and affected by extreme floods triggered by short and intense precipitation events showed significantly larger widening than other river reaches in other regions. Additionally, the meta-analysis confirmed valley confinement as a critical morphological variable that controls channel widening but showed that it is not the only controlling factor. We proposed new statistical models to identify river reaches prone to widening, estimate potential channel width after a flood, and compute upper bound width ratios. These findings can inform flood hazard evaluations and the design of mitigation measures.

Identifiants

pubmed: 37558069
pii: S0048-9697(23)04728-9
doi: 10.1016/j.scitotenv.2023.166103
pii:
doi:

Types de publication

Journal Article

Langues

eng

Sous-ensembles de citation

IM

Pagination

166103

Informations de copyright

Copyright © 2023 The Authors. Published by Elsevier B.V. All rights reserved.

Déclaration de conflit d'intérêts

Declaration of competing interest The authors declare that they have no known competing financial interests or personal relationships that could have appeared to influence the work reported in this paper.

Auteurs

V Ruiz-Villanueva (V)

University of Lausanne, Institute of Earth Surface Dynamics (IDYST), Geopolis, UNIL-Mouline, CH-1015 Lausanne, Switzerland. Electronic address: Virginia.Ruiz-Villanueva@unil.ch.

H Piégay (H)

École Normale Supérieure de Lyon, (ENS), France, Environment City Society (EVS) Research unit, UMR 5600, 15 parvis René Descartes, 69342 Lyon, France.

Vittoria Scorpio (V)

Department of Chemical and Geological Sciences, University of Modena and Reggio Emilia, Modena, Italy.

Annette Bachmann (A)

Flussbau AG SAH, Schwarztorstrasse 7, 3007 Bern, Switzerland.

Guillaume Brousse (G)

EDF - R&D - LNHE - 6 Quai Watier, Chatou/Laboratoire d'Hydraulique Saint-Venant - 6 Quai Watier, 78400 Chatou, France.

Marco Cavalli (M)

National Research Council, Research Institute for Geo-Hydrological Protection (CNR IRPI), Corso Stati Uniti 4, 35127 Padova, Italy.

Francesco Comiti (F)

Free University of Bolzano-Bozen, Faculty of Science and Technology, Bolzano, Italy.

Stefano Crema (S)

National Research Council, Research Institute for Geo-Hydrological Protection (CNR IRPI), Corso Stati Uniti 4, 35127 Padova, Italy.

Elena Fernández (E)

INDUROT, University of Oviedo, 33600 Mieres, Asturias, Spain.

Glòria Furdada (G)

RISKNAT Research group, Geomodels Research Institute, Universitat de Barcelona, UB (Spain), Departament de Dinàmica de la Terra i de l'Oceà, Facultat de Ciències de la Terra, c/Martí i Franquès s/n, 08028 Barcelona, Spain.

Hanna Hajdukiewicz (H)

Institute of Nature Conservation, Polish Academy of Sciences, al. Mickiewicza 33, 31-120 Kraków, Poland.

Lukas Hunzinger (L)

Flussbau AG SAH, Schwarztorstrasse 7, 3007 Bern, Switzerland.

Ana Lucía (A)

Geological and Mining Institute of Spain, National Research Council (IGME-CSIC), Ríos Rosas 23, 28003 Madrid, Spain.

Lorenzo Marchi (L)

National Research Council, Research Institute for Geo-Hydrological Protection (CNR IRPI), Corso Stati Uniti 4, 35127 Padova, Italy.

Adina Moraru (A)

Norwegian University of Science and Technology, (NTNU) Department of Civil and Environmental Engineering, S.P. Andersens veg 5, 7031 Trondheim, Norway.

Guillaume Piton (G)

Univ. Grenoble Alpes, INRAE, CNRS, IRD, Grenoble INP, IGE, 38000 Grenoble, France.

Dieter Rickenmann (D)

Swiss Federal Research Institute WSL, Zürcherstrasse 111, CH-8903 Birmensdorf, Switzerland.

Margherita Righini (M)

IUSS - University School for Advanced Studies, 15, 27100 Pavia, Italy.

Nicola Surian (N)

University of Padova, Department of Geosciences, Via G. Gradenigo 6, 35131 Padova, Italy.

Rabab Yassine (R)

EGIS 889 rue de la Vielle Poste CS, Montpellier 34965, France.

Bartłomiej Wyżga (B)

Institute of Nature Conservation, Polish Academy of Sciences, al. Mickiewicza 33, 31-120 Kraków, Poland.

Classifications MeSH