Gravity Waves Courant Number Tool
Gravity Waves Courant Number
The Courant number is a spatially varied (dataset) dimensionless value representing the time a particle stays in a cell of a mesh/grid. This is based on the size of the element and the speed of that particle. A Courant number of 1.0 implies that a particle(parcel or drop of water) would take one time step to flow through the element. Since cells/elements are not guaranteed to align with the flow field, this number is an approximation. This dataset is computed at nodes so it is uses the average size of the cells/elements attached to the node. Since the typical Courant number calculation requires as an input a velocity as shown in the equation below:
- Time Step: a user specified constant
- NodalSpacing: dependent on the computational grid/mesh
- Velocity: typically computed by hydrodynamic simulation
As noted above, the velocity is typically output from a simulation, so this tool approximates velocity based on the speed of a gravity wave through the water column.
The speed of wave propagation is dependent on the depth of the water column. For purposes of this tool, the speed is assumed to be:
- Note: the variable in the equation above is "Depth", not "Elevation".
Depth is also typically output from a hydrodynamic simulation. For this tool it can be approximated as:
For coastal applications the water level can be assumed as 0.0 (Mean Sea Level) or a constant offset from MSL.
For riverine applications the water level is more difficult to approximate. It may require computing a sloped plane. In this case, negative values should be filtered out.
In all cases, the tool will truncate the depth to a minimum value of 0.1. Velocity only exists in a water column with positive depth.
The tool computes the Courant number at each node in the selected geometry based on the specified time step.
If the input velocity magnitude dataset is transient, the resulting CourantNumber dataset will also be transient.
For numerical solvers that are Courant limited/controlled, any violation of the Courant condition, where the Courant number exceeds the allowable threshold could result in instability. Therefore, the maximum of the Courant number dataset gives an indication of the stability of this mesh for the specified time step parameter.
This tool is intended to assist with numerical engine stability, and possibly the selection of an appropriate time step size.
The Gravity Waves Courant Number tool dialog has the following options:
- Input dataset – Specify the elevation dataset (or depth dataset if using depth option).
- Input dataset is depth – Specify if the input dataset is depth.
- Gravity – Enter the gravity value.
- Use time step – Enter the computational time step value.
- Gravity waves courant number data set – Enter the name for the new gravity wave Courant number dataset. It is recommended to specify a name that references the input. Typically this would include the time step used in the calculation. The velocity dataset used could be referenced. The geometry is not necessary because the dataset resides on that geometry.
SMS – Surface-water Modeling System
|1D Grid • Cartesian Grid • Curvilinear Grid • GIS • Map • Mesh • Particle • Quadtree • Raster • Scatter • UGrid
|3D Structure • FVCOM • Generic • PTM
|ADCIRC • BOUSS-2D • CGWAVE • CMS-Flow • CMS-Wave • GenCade • STWAVE • WAM
|AdH • HEC-RAS • HYDRO AS-2D • RMA2 • RMA4 • SRH-2D • TUFLOW • TUFLOW FV
|Aquaveo • SMS Tutorials • SMS Workflows