Modeling tidal flow in the great bay estuary, new hampshire, using a depth averaged flooding-dewatering model with application to the bed load transport of coarse sediments

Keyphrases

• New Hampshire 100%
• Great Bay Estuary 100%
• Dewatering 100%
• Bedload Transport 100%
• Coarse Sediment 100%
• Depth-averaged 100%
• Tidal Flow 100%
• Main Channel 66%
• Finite Element Model 33%
• Groundwater 33%
• Current Stress 33%
• Well-mixed 33%
• Lagrangian Particle Tracking 33%
• Sediment Accumulation 33%
• Inertial Term 33%
• Model Use 33%
• Current Measurement 33%
• Freshwater Flow 33%
• Tidal Current 33%
• Coarse Sand 33%
• Gravel 33%
• Eulerian 33%
• Bedload 33%
• Hydrodynamic Calculation 33%
• Pressure Gradient 33%
• Bottom Stress 33%
• Flux Vector 33%
• Hydrodynamic Model 33%
• Sediment Particles 33%
• Non-linear Time 33%
• Tidal Elevation 33%
• Mixed System 33%
• Parametric Method 33%
• Tidal Flat 33%
• Fixed Boundary 33%
• Bottom Friction 33%
• Dynamic Balance 33%
• Tracking Approach 33%
• Finite number 33%
• Estuary Mouths 33%
• Friction Term 33%
• Time Stepping Finite Element Method (TSFEM) 33%
• Long-term Rate 33%

Earth and Planetary Sciences

• Sea Level 100%
• Dewatering 100%
• Tidal Modeling 100%
• Particle Tracking 50%
• Sand and Gravel 50%
• Tidal Current 50%
• Tidal Flat 50%
• Bottom Friction 50%
• Pressure Gradient 50%