A notable drawback in mixed-size sediment morphodynamic modeling is the fact that the most commonly used mathematical model in this field (i.e., the active layer model Hirano, 1971) can be ill-posed under certain circumstances. Under these conditions the model loses its predictive capabilities, as negligible perturbations in the initial or boundary conditions produce significant differences in the solution. In this paper we propose a preconditioning method that regularizes the model to recover well-posedness by altering the time scale of the sediment mixing processes. We compare results of the regularized model to data from four new laboratory experiments conducted under conditions in which the active layer model is ill-posed. The regulariz...
Sediment mobility and memory effects distinguish transport and morphodynamics in fine sediment setti...
Applications of process-based morphodynamic models are often constrained by limited availability of ...
In the mass balance of a riverbed, some terms are usually assumed constant for reasons of simplicity...
A notable drawback in mixed-size sediment morphodynamic modeling is the fact that the most commonly ...
The mixed-size character of sediment is a necessary property to ex- plain physical phenomena such as...
In this paper we analyze the Hirano active layer model used in mixed sediment river morphodynamics c...
The active layer model (Hirano, 1971) is frequently used for modeling mixed-size sediment river morp...
This paper presents an assessment of the strengths and weaknesses of four sediment continuity models...
We present an accurate numerical approximation to the Saint-Venant-Hirano model for mixed-sediment m...
The set of equations used in modelling river morphodynamics needs to be (at least) wellposed to be...
A two-dimensional model describing river morphodynamic processes under mixed-size sediment condition...
A two-dimensional model describing river morphodynamic processes under mixed-size sediment condition...
Abstract Sediment of different size are transported in rivers under the action of flow. The first an...
A new two-layer model for conservation of mixed sediment for bedform-dominated condi-tions is propos...
In Chapter I a derivation of the equations and an extension of the mathematical model will be carrie...
Sediment mobility and memory effects distinguish transport and morphodynamics in fine sediment setti...
Applications of process-based morphodynamic models are often constrained by limited availability of ...
In the mass balance of a riverbed, some terms are usually assumed constant for reasons of simplicity...
A notable drawback in mixed-size sediment morphodynamic modeling is the fact that the most commonly ...
The mixed-size character of sediment is a necessary property to ex- plain physical phenomena such as...
In this paper we analyze the Hirano active layer model used in mixed sediment river morphodynamics c...
The active layer model (Hirano, 1971) is frequently used for modeling mixed-size sediment river morp...
This paper presents an assessment of the strengths and weaknesses of four sediment continuity models...
We present an accurate numerical approximation to the Saint-Venant-Hirano model for mixed-sediment m...
The set of equations used in modelling river morphodynamics needs to be (at least) wellposed to be...
A two-dimensional model describing river morphodynamic processes under mixed-size sediment condition...
A two-dimensional model describing river morphodynamic processes under mixed-size sediment condition...
Abstract Sediment of different size are transported in rivers under the action of flow. The first an...
A new two-layer model for conservation of mixed sediment for bedform-dominated condi-tions is propos...
In Chapter I a derivation of the equations and an extension of the mathematical model will be carrie...
Sediment mobility and memory effects distinguish transport and morphodynamics in fine sediment setti...
Applications of process-based morphodynamic models are often constrained by limited availability of ...
In the mass balance of a riverbed, some terms are usually assumed constant for reasons of simplicity...