DSD-INT 2015 - uniqueness and generality of delta morphologoy - liang li
1. 1Challenge the future
Uniqueness and generality of
delta morphology
The effect of initial bathymetry perturbations on long-
term morphological modeling
Liang Li
Helena van der Vegt
Joep Storms
Dirkjan Walstra
4. 4Challenge the future
Introduction
Objective
1. Develop a series of indicators for Delft3d models to calculate the
geometry of the morphological patterns.
2. Quantify the effect initial bathymetry perturbations on the delta
morphology
9. 9Challenge the future
Model setup
Model grid and bathymetry
Model parameters Value Unit
Manning 0.03 1
3
s m
Sand diameter 0.00025 m
Sand drydensity 1600 3
kg m
Clayfallingvelocity 0.0015 1
ms
Claydry density 500 3
kg m
Critical shearstressforclay erosion 0.5 2
N m
Morphological accelerationfactor 30 [ - ]
10. 10Challenge the future
Model setup
Initial bathymetry perturbations
1. 1cm perturbations
2. 1000 m3 river discharge
3. 1 m wave height
4. 1 m tidal amplitude
17. 17Challenge the future
Conclusions(2)
1. The uncertainty range induced by small perturbations
varies for different scale of indicators.
1. Small: delta plain
2. Large: channel network