This paper describes a numerical model of three-dimensional beach change as produced by breaking waves and wave-induced currents. Cross-shore lines spaced at intervals alongshore form the basic calculation element, and cross-shore and longshore transport rates are calculated independently on the lines. Transport rates are coupled indirectly through the mass conservation equation and a contouring routine that determines local depth contour orientation for calculating wave transformation. The model has reduced calculation time compared to fully gridded hydrodynamic and beach change models, yet allows representation of complex boundary conditions, coastal structures, and movement of longshore bars and berms. Results of two test series are pres...
Many coasts around the world experience erosion as a result of a lack of sediment supply, local inte...
A numerical model of beach topography evolution was developed. The model includes five sub-models: r...
As increased development and habitation of our shorelines continues unabated, and as science begins ...
The beach topography change in the nearshore zone may be induced by natural phenomena such as wind, ...
An improved 3-D beach evolution model coupled with the shore-line model, named "3D-SHORE",...
A numerical model is developed to predict shoreline changes as a function of deep water wave conditi...
A mathematical model for long-term, three-dimensional shoreline evolution is developed. The combined...
A process-based numerical model has been used to study nearshore hydrodynamics on barred beaches. A ...
A two-dimensional numerical model of nearshore waves, currents, and sediment transport was developed...
In this chapter we consider beach profile and cross-shore sediment transport processes commonly enco...
A numerical model was developed of beach morphological evolution in the vicinity of coastal structur...
This paper presents a mathematical approach and numerical model that simulates beach and dune change...
The authors have developed models for predicting beach changes applicable to various problems on rea...
A numerical model of beach topography evolution due to waves and currents in the vicinity of coastal...
ABSTRACT: In This study develops a quasi-three dimensional numerical model of wave driven coastal cu...
Many coasts around the world experience erosion as a result of a lack of sediment supply, local inte...
A numerical model of beach topography evolution was developed. The model includes five sub-models: r...
As increased development and habitation of our shorelines continues unabated, and as science begins ...
The beach topography change in the nearshore zone may be induced by natural phenomena such as wind, ...
An improved 3-D beach evolution model coupled with the shore-line model, named "3D-SHORE",...
A numerical model is developed to predict shoreline changes as a function of deep water wave conditi...
A mathematical model for long-term, three-dimensional shoreline evolution is developed. The combined...
A process-based numerical model has been used to study nearshore hydrodynamics on barred beaches. A ...
A two-dimensional numerical model of nearshore waves, currents, and sediment transport was developed...
In this chapter we consider beach profile and cross-shore sediment transport processes commonly enco...
A numerical model was developed of beach morphological evolution in the vicinity of coastal structur...
This paper presents a mathematical approach and numerical model that simulates beach and dune change...
The authors have developed models for predicting beach changes applicable to various problems on rea...
A numerical model of beach topography evolution due to waves and currents in the vicinity of coastal...
ABSTRACT: In This study develops a quasi-three dimensional numerical model of wave driven coastal cu...
Many coasts around the world experience erosion as a result of a lack of sediment supply, local inte...
A numerical model of beach topography evolution was developed. The model includes five sub-models: r...
As increased development and habitation of our shorelines continues unabated, and as science begins ...