1999
DOI: 10.1002/(sici)1097-0363(19990228)29:4<465::aid-fld797>3.0.co;2-h
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An improved technique for solving two-dimensional shallow water problems

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Cited by 21 publications
(14 citation statements)
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“…Each numerical scheme has some kinds of advantage in 38 certain flow problems but may not perform satisfactorily in a different situation. As a result, 39 the combined or mixed solution schemes have been developed to deal with more complicated 40 issues, such as the FEM-based FVM, FVM-based FEM and hybrid FDM/FVM methods 41 (Guillou and Nguyen, 1999;Du, 2000;Casulli and Zanolli, 2002 The following 2-D shallow water equations (SWEs), sediment transport and bed deformation 71 equations are used for the water-sediment mixture flows as 72 Here it should be noted that the above water flow equations (1) -(2) are not influenced by 85 any sediment transport parameters in equation (3) -(4), and thus they are represented in the 86 uncoupled form, which is in contrast to those used by Cao et al (2011). This is based on the 87 rational that the suspended load is not the dominant sediment transport mode in the present 88 field case studies and the flow structure is not significantly modified by the existence of the 89 sediment mixture.…”
Section: Introduction 1mentioning
confidence: 99%
“…Each numerical scheme has some kinds of advantage in 38 certain flow problems but may not perform satisfactorily in a different situation. As a result, 39 the combined or mixed solution schemes have been developed to deal with more complicated 40 issues, such as the FEM-based FVM, FVM-based FEM and hybrid FDM/FVM methods 41 (Guillou and Nguyen, 1999;Du, 2000;Casulli and Zanolli, 2002 The following 2-D shallow water equations (SWEs), sediment transport and bed deformation 71 equations are used for the water-sediment mixture flows as 72 Here it should be noted that the above water flow equations (1) -(2) are not influenced by 85 any sediment transport parameters in equation (3) -(4), and thus they are represented in the 86 uncoupled form, which is in contrast to those used by Cao et al (2011). This is based on the 87 rational that the suspended load is not the dominant sediment transport mode in the present 88 field case studies and the flow structure is not significantly modified by the existence of the 89 sediment mixture.…”
Section: Introduction 1mentioning
confidence: 99%
“…In the second and the most important remark, we now need to discretize an elliptic equation with a general symmetric matrix K.x/ and not a harmonic averaging of an isotropic tensor (K.x/ D .x/I, where I is the identity matrix) as in (1). In this case, there is no direct way to calculate the numerical flux in terms of the cell-centered values.…”
Section: Finite Volume Discretizationmentioning
confidence: 99%
“…D´C h H ; (2) where H D hCÁ is the total depth with h.x ; y / being the still depth and Á.x ; y ; t / the surface display; and´D OE h; Á is the vertical coordinate in the physical domain that has the origin´D 0 on the still level (see Figure 1). The Poisson equation (1) that is constructed in the Cartesian coordinate has to be modified in the transformed computational domain. Using the principle of chain differentiation, the partial differentiation of a variable in the physical domain is transformed as follows:…”
Section: Introductionmentioning
confidence: 99%
“…The free surface flow in a single lhranch of a river network can be described by the so-called Saint-Venant equations [1][2][3] under the assumption of a hydrostatic pressure and an uniform distribution of the velocity along the vertical axis.…”
Section: Equations For a Single River Bradchmentioning
confidence: 99%
“…The flow can be simulated by one-or two-dimensional mathematical models [1][2][3], depending on the study purpose. However, two-dimensional models are expensive for large river deltas.…”
Section: Introductionmentioning
confidence: 99%