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- Create or refine a computational grid (“*. grd” grd file)
- Extract and interpolate bathymetry data from open source on-line databases on the computational grid (“*.dep” dep file).
- Model specific features
- Delft3D-FLOW: Extract and interpolate tidal boundary conditions from open source on-line databases on the computational grid, creating boundary conditions for the model (“*.bnd” file) and defining a specific roughness for water and land.
- Delft3D-WAVE: Automatic coupling functionality with FLOW
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Delft Dashboard contains a number of Tabs, which can be used to specify additional information to the model. The model can then be used directly tabs which resembles the interface of the Delft3D-FLOW modelling suite but also includes a Toolbox Tab. Using this Toolbox Tab it is possible to apply the selected toolbox. Onces finished the model can directly be used to carry out hydrodynamics, waves, morphodynamics or water quality computations.
Make rectangular grid
After the grid outline is defined within the interface of Delft Dashboard the user can click on ‘Create grid’. The following routines will then be called:
- Determine the origin (xori, yori), spatial resolution (dx, dy), orientation (rot) and maximum bed level required (zmaxZ max) from the specified values in Dashboard.
- Create a full grid between these points (+ some buffer of 5%) based on the bathymetry active in Dashboard (default this is GEBCO ’08). This grid will already be defined in the active coordinate system the user specified (default this is WGS 84) .
- Creation a rectangular grid within the boundaries specified in Dashboard. The grid cells which are above a certain bed level (zmaxZ max) are deleted. A linear interpolation is carried between the full grid and the rectangular grid within the boundaries
Figure: The rectangular grid created for New Zealand. There are no grid cells defined above a certain Z max (m) as can be seen clearly at of this example.
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- Determine which datasets are used and within which limit (zmin Z min and zmax Z max). This feature is especially handy helpful when a different data set is used for the sea part and the land part. An offset can be used in order to shift the bathymetry. Diffusion If selected, diffusion is used in order to define depth values for missing data (NaNs).
- If in quick mode ‘make bathymetry’ is used the active bathymetry in Dashboard (default GEBCO ’08) is applied
- Other bathymetry sets can be important via ‘Bathmetry’ in the Working Space.
- The function will now loop over the different datasets described.
- The bathymetry is first loaded.
- This can be downloaded from the OpenDAP server
- Or from your local directory file if the data needed is used in a previous set-up.
- Bathymetry is applied in the order defined.
- Interpolation from the original grid to the model grid is carried out with a linear interpolation. Only values (that are not NaNs) are taken into account.
- The bathymetry is first loaded.
- If an internal diffusion is applied the remaining non-existing bed levels are filled in based on the mean bed level and after that a smoothing function is applied. This option can be selected in the Working Space under 'Bathymetry'
- If a model offset is applied the whole bathymetry is shifted. An offset of 1 meter means the bed level will be 1 meter lower than the original.
- The bathymetry created is directly visible in Delft Dashboard.
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