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Can the discharge of a hyperconcentrated flow be estimated from paleoflood evidence?

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Can the discharge of a hyperconcentrated flow be estimated from paleoflood evidence?

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Bodoque, J.; Eguibar Galán, MÁ.; Diez-Herrero, A.; Gutierrez-Perez, I.; Ruiz-Villanueva, V. (2011). Can the discharge of a hyperconcentrated flow be estimated from paleoflood evidence?. Water Resources Research. 47(W12535). doi:10.1029/2011WR010380.

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Título: Can the discharge of a hyperconcentrated flow be estimated from paleoflood evidence?
Autor:
Entidad UPV: Universitat Politècnica de València. Departamento de Ingeniería Hidráulica y Medio Ambiente - Departament d'Enginyeria Hidràulica i Medi Ambient
Fecha difusión:
Resumen:
Many flood events involving water and sediments have been characterized using classic hydraulics principles, assuming the existence of critical flow and many other simplifications. In this paper, hyperconcentrated flow ...[+]
Palabras clave: Critical flow , Cross section , Flood event , Hydraulic analysis , Hyperconcentrated flow , Iterative process , Methodological approach , Momentum equation , Peak discharge , Simplifying assumptions , Specific energy , Superelevation , Wetted perimeters , Anoxic sediments , Hydrostatic pressure , Iterative methods , Hydraulics , Calibration , Discharge , Energy efficiency , Estimation method , Geomorphology , Hydraulic property , Hydrostatics , Momentum , Numerical model , Paleoflood , Reconstruction , Uncertainty analysis , Water depth , Water flow
Derechos de uso: Cerrado
Fuente:
Water Resources Research. (issn: 0043-1397 )
DOI: 10.1029/2011WR010380
Editorial:
American Geophysical Union (AGU)
Versión del editor: http://dx.doi.org/10.1029/2011WR010380
Patrocinador:
Spanish Ministry of Science and Innovation CGL2007-62063 CGL2010-19274
Tipo: Artículo

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