I am setting up a t2d model with single inflow boundary and with dry bed as initial conditions. I understand with inflow boundary i need to have some water at the inflow boundary for the program to calculate inflow velocity. I can use continued computation to accomplish this. In the initial conditions file, I will set initial depth to very small value (say 0.01 m) only for the nodes at the inflow boundary, and zero depth for elsewhere.
Alternatively, i can use source points at the inflow boundary nodes. I will divide the temporal flow by the total number of nodes at inflow boundary, and set the new hydrograph in the source file.
Could anyone comment on both methods? I am also wondering whether there is a better way to model this.
Your inputs are greatly appreciated,
Hailiang