Name: Basic Concepts of Kinematic-Wave Models: Usgs Professional Paper 1302 (en Inglés)
Price: 22120.00 CLP
Availability: InStock
Author: Miller, J. E.
ISBN: 9781287011569

portada Basic Concepts of Kinematic-Wave Models: Usgs Professional Paper 1302 (en Inglés)

Formato

Libro Físico

Autor

J. E. Miller

Editorial

Bibliogov

Idioma

Inglés

N° páginas

Encuadernación

Tapa Blanda

Dimensiones

24.6 x 18.9 x 0.2 cm

Peso

0.09 kg.

ISBN13

9781287011569

Categorías

Política y gobierno

Basic Concepts of Kinematic-Wave Models: Usgs Professional Paper 1302 (en Inglés)

J. E. Miller (Autor) · Bibliogov · Tapa Blanda

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Reseña del libro "Basic Concepts of Kinematic-Wave Models: Usgs Professional Paper 1302 (en Inglés)"

The kinematic-wave model is one of a number of approximations of the dynamic-wave model. The dynamic-wave model describes one-dimensional shallow-water waves (unsteady, gradually varied, open-channel flow). The report provides a basic reference on the theory and application of kinematic-wave models and describes the limitations of the model in relation to the other approximations of the dynamic-wave model. In the kinematic-wave approximation, a number of the terms in the equation of motion are assumed to be insignificant. The equation of motion is replaced by an equation describing uniform flow. Thus, the kinematic-wave model is described by the continuity equation and a uniform flow equation such as the well-known Chezy or Manning formulas. Kinematic-wave models are applicable to overland flow where lateral inflow is continuously added and is a large part of the total flow. For channel-routing applications, the kinematic-wave model always predicts a steeper wave with less dispersion and attenuation than actually occurs. The effect of the accumulation of errors in the kinematic-wave model shows that the approximations made in the development of the kinematic-wave equations are not generally justified for most channel-routing applications. Modified flow-routing models can be used which help to stop the accumulation of error that occurs when the kinematic-wave model is applied.