http://www.cnr.it/ontology/cnr/individuo/prodotto/ID247321
A practical method for analysis of river waves and for kinematic wave routing in natural channel networks (Articolo in rivista)
- Type
- Label
- A practical method for analysis of river waves and for kinematic wave routing in natural channel networks (Articolo in rivista) (literal)
- Anno
- 2000-01-01T00:00:00+01:00 (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#doi
- 10.1002/(SICI)1099-1085(200001)14:1<51::AID-HYP909>3.0.CO;2-Z (literal)
- Alternative label
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#autori
- Moramarco T and Singh V.P. (literal)
- Pagina inizio
- Pagina fine
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#numeroVolume
- Rivista
- Note
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#affiliazioni
- IRPI - CNR Via Madonna Alta, 126 06128 Perugia
Department of Civil and Environmental Engineering, Louisiana State University, Baton Rouge, LA 70803-6405, USA (literal)
- Titolo
- A practical method for analysis of river waves and for kinematic wave routing in natural channel networks (literal)
- Abstract
- The behaviour of river waves is described using a simplified dimensionless form of the momentum equation in
conjunction with the continuity equation. Three dimensionless parameters were derived based on a quantitative
linear analysis. These parameters, which depend on the Froude number of the steady uniform flow and the
geometric characteristics of the river, permit quanti®cation of the influence of inertia and pressure in the
momentum equation. It was found that dynamic and diusion waves occur mainly on gentle channel slopes and
the transition between them is characterized by the Froude number. On the other hand, the kinematic wave has
a wide range of applications. If the channel slope is greater than 1%, the kinematic wave is particularly suitable
for describing the hydraulics of flow. Since slopes in natural channel networks are often greater than 1%, an
analytical solution of the linearized kinematic wave equation with lateral inflow uniformly distributed along the
channel is desirable and was therefore derived. The analytical solution was then implemented in a channel
routing module of an existing simple rainfall-runoff model. The results obtained using the analytical solution
compared well with those obtained from a non-linear kinematic wave model. (literal)
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- Autore CNR
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