Dear All,
since I'm quite new to two-dimensional flow modelling I have a more general question and hope you can help me.
I want to simulate the flow along a natural river stream which is constricted by abutments at one location and with piers in between the two abutments. I defined the scope of the model and have three boundary conditions:
1. An Inflow boundary condition with a maximum inflow of 2,275 m³/s,
2. An Inflow boundary condition with a maximum inflow of 760 m³/s,
3. An Outflow boundary condition with a water level of 440.0 m asl.
The domain is shown on the following screenshot:
At the inflow boundaries water levels of 452.0 m asl and 455.0 m asl are expected, respectively (derived from a quick and dirty one-dimensional simulation). This means the water level is 12 m and 15 m higher than at the outflow boundary condition.
What I want to simulate as initial condition is the situation that the main river channel (and maybe part of the floodplains) is filled with water (or at least wetted).
My question now is: How can I define such initial conditions which I can use to simulate as long as necessary to reach a steady state with the above listed boundary conditions?
I tried different approaches and none of them worked satisfactory. Those were, inter alia:
- Initial Elevation of 440.0 m asl: The major share of the domain is dry and there is no water at the inflow boundaries, which leads to a cancellation of the simulation due to problems at the inflow boundaries.
- Initial Elevation of 460.0 m asl: The simulation is aborted as well. I do not really know why. ( see my other topic: "Initial Elevation not maintained - Simulation aborted")
- Sloped Initial Elevation from 440.0 m asl (at the outflow boundary) to 455.0 m asl (at the inflow boundaries): Prepared by the use of Blue Kenue this initial condition also leaded to a cancellation of the simulation.
- Constant Depth of 3.0 m: Simulation cancelled. etc. etc
I hope someone can help me.
Best Regards
Heidi