2010
DOI: 10.1007/978-90-481-3674-2
|View full text |Cite
|
Sign up to set email alerts
|

Numerical Modeling in Open Channel Hydraulics

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
2
1
1
1

Citation Types

2
150
0
2

Year Published

2014
2014
2020
2020

Publication Types

Select...
9

Relationship

0
9

Authors

Journals

citations
Cited by 153 publications
(154 citation statements)
references
References 1 publication
2
150
0
2
Order By: Relevance
“…A rainfall pattern is generated by scaling historical rainfall data (for details, see Wüest et al (2010)) iteratively until a desired target discharge at a river gauging station is reached. Such discharge is computed using a runoff model based on the ModClark approach (see Kull and Feldman 1998) and a onedimensional flood model based on the Bernouilli equation (see Szymkiewicz 2010). In addition, such rainfall patterns may trigger landslides.…”
Section: Risk Assessment Methodologymentioning
confidence: 99%
“…A rainfall pattern is generated by scaling historical rainfall data (for details, see Wüest et al (2010)) iteratively until a desired target discharge at a river gauging station is reached. Such discharge is computed using a runoff model based on the ModClark approach (see Kull and Feldman 1998) and a onedimensional flood model based on the Bernouilli equation (see Szymkiewicz 2010). In addition, such rainfall patterns may trigger landslides.…”
Section: Risk Assessment Methodologymentioning
confidence: 99%
“…The governing equations are the incompressible continuity and Reynolds equations in the coordinate system ( x, y, z ) ( Lai, 1986 ;Szymkiewicz, 2010 ),…”
Section: The Governing Equationsmentioning
confidence: 99%
“…We do not report here the steps involved in the integration of Eqs. (1) -( 2 ) because they are shown in many Hydraulics textbooks (for example ( Lai, 1986 ;Szymkiewicz, 2010 ) and cited references). By merging Eqs.…”
Section: The Governing Equationsmentioning
confidence: 99%
“…Segundo Szymkiewicz (2010), quando o transporte de uma substância é dominado pela difusão, o método de diferenças finitas e o de elementos finitos geram resultados satisfatórios na solução da equação para simulação de qualidade de água. No entanto, se o processo de advecção é dominante, espera-se que ocorram oscilações e difusão numérica.…”
Section: Pontounclassified