5.10 Horizontal Mixing
5.10.2 Description
Horizontal turbulent mixing is specified for the entire model domain by using the
Horizontal momentum mixing model science is provided in Appendix B.7.
| Model Implementation | Description |
|---|---|
| None | No horizontal momentum mixing. |
| Constant | Spatially constant momentum mixing value. |
| Smagorinsky | Smagorinsky turbulence closure for momentum mixing. |
| Wu | Wu momentum mixing formulation. |
| Command | Description |
|---|---|
| Momentum Mixing Model | Required - Selects the momentum mixing model for horizontal sub-grid scale turbulent mixing. |
| Global Horizontal Eddy Viscosity | Conditional - Required when using the Constant, Smagorinsky or Wu Momentum Mixing Model. Assigns the eddy viscosity coefficient or constant value. |
| Global Horizontal Eddy Viscosity Limits | Optional - Sets a minimum and maximum limit on computed eddy viscosity when using the Smagorinsky or Wu Momentum Mixing Model. |
5.10.3 None
This model is the default and excludes the simulation of momentum mixing. Using none is useful for analytical cases and laboratory experiments. It is not recommended for project modelling and an alternative momentum mixing model implementation should be adopted.
5.10.4 Constant
This model applies a spatially constant eddy viscosity value to all cells in the model domain.
5.10.5 Smagorinsky
This model calculates eddy viscosity on a cell by cell basis using local horizontal velocity gradients and cell size. This method is recommended for ocean, coastal, estuarine and lake studies or for models that are likely to be extended to 3D hydrodynamics during a project. The argument to the command
5.10.6 Wu
This model calculates eddy viscosity on a cell by cell basis using local velocity gradients and water depth. Wu is recommended for 2D only simulations in riverine and floodplain areas where cell size can become small relative to the water depth. The argument to the command