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| DOI | 10.3390/W14244098 | ||||
| Año | 2022 | ||||
| Tipo | artículo de investigación |
Citas Totales
Autores Afiliación Chile
Instituciones Chile
% Participación
Internacional
Autores
Afiliación Extranjera
Instituciones
Extranjeras
River flooding is one of the most widespread natural disasters. Projections indicate that climate change will increase flood hazard in many areas around the world. In this study, we investigate the individual and combined effects of sea level rise, flow increase and riparian vegetation encroachment on flood hazard in the lower Biobio River, Chile. Results show that each has the potential to individually increase flood hazard in certain areas, and that individual effects can compound. Encroachment of riparian vegetation onto previously sparsely vegetated areas of the floodplain, likely a result of the Chilean megadrought, causes higher flow resistance and increased flooding during large events. Somewhat counterintuitively, drought has therefore led to an increase in flood hazard in the study area. Drought risk for most land areas across the globe is expected to increase with climate change. Potential future vegetation encroachment should therefore be included as a key variable in riverine flood hazard studies.
| Ord. | Autor | Género | Institución - País |
|---|---|---|---|
| 1 | Schoener, Gerhard | Hombre |
Southern Sandoval Cty Arroyo Flood Control Author - Estados Unidos
Southern Sandoval County Arroyo Flood Control Authority - Estados Unidos |
| 2 | MUNOZ-ORTIZ, ENRIQUE | Hombre |
Universidad Católica de la Santísima Concepción - Chile
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| 3 | ARUMI-RIBERA, JOSE LUIS | Hombre |
Universidad de Concepción - Chile
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| 4 | Stone, Mark C. | Hombre |
UNIV NEW MEXICO - Estados Unidos
The University of New Mexico - Estados Unidos University of New Mexico School of Engineering - Estados Unidos |
| Agradecimiento |
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| This work was supported by the National Science Foundation (grants number 1954140 and 1826709) and by the CRHIAM Center, project ANID/FONDAP/15130015. |
| This study was supported by the Partnerships Along the Headwaters of the Americas for Young Scientists (Pathways) program, an international research experience for students funded by the National Science Foundation (grant number 1954140) and hosted by Washington State University and the University of New Mexico. Special thanks to Mark Stone, Asa Stone, Jan Boll, Benjamin Warner and Alex Fremier for making the experience possible despite many setbacks during the COVID-19 pandemic. We are also grateful to the Centro de Investigación Marítimo Portuario—CIMP UCSC for providing the lidar-based digital elevation model used in this project. Additional funding was provided by the CRHIAM Center, project ANID/FONDAP/15130015. |
| This study was supported by the Partnerships Along the Headwaters of the Americas for Young Scientists (Pathways) program, an international research experience for students funded by the National Science Foundation (grant number 1954140) and hosted by Washington State University and the University of New Mexico. Special thanks to Mark Stone, Asa Stone, Jan Boll, Benjamin Warner and Alex Fremier for making the experience possible despite many setbacks during the COVID-19 pandemic. We are also grateful to the Centro de Investigación Marítimo Portuario—CIMP UCSC for providing the lidar-based digital elevation model used in this project. Additional funding was provided by the CRHIAM Center, project ANID/FONDAP/15130015. |