Modeling morphodynamic evolution in alluvial estuaries
Modeling morphodynamic evolution in alluvial estuaries
UNESCO-IHE PhD Thesis
Wegen, Mick van der
Taylor & Francis Ltd
07/2017
206
Dura
Inglês
9781138424333
15 a 20 dias
540
Descrição não disponível.
1. Framework for Morphodynamic Modeling in Alluvial Estuaries 2. Schematized 1D and 2D Model Results and Western Scheldt Data 3. Bank Erosion and Energy Dissipation in an Idealized Tidal Embayment 4. Morphodynamic Modeling of Tidal Channel Evolution in Comparison to Empirical PA Relationship 5. Reproduction of the Wester Scheldt Bathymetry by means of a Process-Based, Morphodynamic Model 6. Proces-Based, Morphodynamic Hindcast of Decadal Deposition Patterns in San Pablo Bay 1856-1887 7. Conclusions and Recommendations
Este título pertence ao(s) assunto(s) indicados(s). Para ver outros títulos clique no assunto desejado.
Van Der Wegen;western;BSS;scheldt;Western Scheldt;tidal;Tidal Prism;prism;Western Scheldt Estuary;sediment;Morphodynamic Evolution;transport;Sediment Transport;estuary;PA Relationship;bed;Short Basin;level;Bed Level;morphological;Bank Erosion;Bed Slope Effects;Alluvial Estuaries;Critical Shear Stress;Basin Mouth;CS;Suisun Bay;Littoral Drift;Tidal Channels;Mud Fractions;High River Discharge;Ebb Tidal Delta;Deposition Volumes;Low River Discharge;Energy Dissipation
1. Framework for Morphodynamic Modeling in Alluvial Estuaries 2. Schematized 1D and 2D Model Results and Western Scheldt Data 3. Bank Erosion and Energy Dissipation in an Idealized Tidal Embayment 4. Morphodynamic Modeling of Tidal Channel Evolution in Comparison to Empirical PA Relationship 5. Reproduction of the Wester Scheldt Bathymetry by means of a Process-Based, Morphodynamic Model 6. Proces-Based, Morphodynamic Hindcast of Decadal Deposition Patterns in San Pablo Bay 1856-1887 7. Conclusions and Recommendations
Este título pertence ao(s) assunto(s) indicados(s). Para ver outros títulos clique no assunto desejado.
Van Der Wegen;western;BSS;scheldt;Western Scheldt;tidal;Tidal Prism;prism;Western Scheldt Estuary;sediment;Morphodynamic Evolution;transport;Sediment Transport;estuary;PA Relationship;bed;Short Basin;level;Bed Level;morphological;Bank Erosion;Bed Slope Effects;Alluvial Estuaries;Critical Shear Stress;Basin Mouth;CS;Suisun Bay;Littoral Drift;Tidal Channels;Mud Fractions;High River Discharge;Ebb Tidal Delta;Deposition Volumes;Low River Discharge;Energy Dissipation